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The Project Gutenberg eBook of A text-book of assaying
This eBook is for the use of anyone anywhere in the United States and most other parts
of the world at no cost and with almost no restrictions whatsoever. You may copy it,
give it away or re-use it under the terms of the Project Gutenberg License included
with this eBook or online at www.gutenberg.org. If you are not located in the United
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using this eBook.
Title: A text-book of assaying
for the use of those connected with mines.
Author: C. Beringer
J. J. Beringer
Release date: July 3, 2006 [eBook #18751]
Language: English
Other information and formats: www.gutenberg.org/ebooks/18751
Credits: E-text prepared by Peter Yearsley, Josephine Paolucci, and the Project
Gutenberg Online Distributed Proofreading Team
*** START OF THE PROJECT GUTENBERG EBOOK A TEXT-BOOK OF ASSAYING
***
E-text prepared by Peter Yearsley, Josephine Paolucci,
and the Project Gutenberg Online Distributed Proofreading Team
(http://www.pgdp.net/)
Transcriber's Note:
Parentheses have been added to clarify fractions. Letters in brackets with a = sign before it
means that the letters have a macron over them, e.g. H[=A=c] signifies that the Ac has a
macron over it.
This eBook is for the use of anyone anywhere in the United States and most other parts
of the world at no cost and with almost no restrictions whatsoever. You may copy it,
give it away or re-use it under the terms of the Project Gutenberg License included
with this eBook or online at www.gutenberg.org. If you are not located in the United
States, you will have to check the laws of the country where you are located before
using this eBook.
Title: A text-book of assaying
for the use of those connected with mines.
Author: C. Beringer
J. J. Beringer
Release date: July 3, 2006 [eBook #18751]
Language: English
Other information and formats: www.gutenberg.org/ebooks/18751
Credits: E-text prepared by Peter Yearsley, Josephine Paolucci, and the Project
Gutenberg Online Distributed Proofreading Team
*** START OF THE PROJECT GUTENBERG EBOOK A TEXT-BOOK OF ASSAYING
***
E-text prepared by Peter Yearsley, Josephine Paolucci,
and the Project Gutenberg Online Distributed Proofreading Team
(http://www.pgdp.net/)
Transcriber's Note:
Parentheses have been added to clarify fractions. Letters in brackets with a = sign before it
means that the letters have a macron over them, e.g. H[=A=c] signifies that the Ac has a
macron over it.
Page 4
Minor typographical errors have been corrected. Footnotes have been moved to the end of
the chapter, and all advertisements have been moved to the end of the book.
the chapter, and all advertisements have been moved to the end of the book.
Page 5
A TEXT-BOOK OF ASSAYING:
FOR THE USE OF THOSE CONNECTED WITH MINES.
BY
FOR THE USE OF THOSE CONNECTED WITH MINES.
BY
Page 6
C. AND J. J. BERINGER.
REVISED BY
REVISED BY
Page 7
J. J. BERINGER,
ASSOC. OF THE ROYAL SCHOOL OF MINES; FELLOW OF THE CHEMICAL
SOCIETY AND OF THE INST. OF CHEMISTRY; PRINCIPAL OF THE CAMBORNE
MINING SCHOOL; AND LATE PUBLIC ANALYST FOR THE COUNTY OF
CORNWALL.
With numerous Diagrams and Tables.
NINTH EDITION.
LONDON:
CHARLES GRIFFIN AND COMPANY, Limited,
EXETER STREET, STRAND.
1904.
[All rights reserved.]
ASSOC. OF THE ROYAL SCHOOL OF MINES; FELLOW OF THE CHEMICAL
SOCIETY AND OF THE INST. OF CHEMISTRY; PRINCIPAL OF THE CAMBORNE
MINING SCHOOL; AND LATE PUBLIC ANALYST FOR THE COUNTY OF
CORNWALL.
With numerous Diagrams and Tables.
NINTH EDITION.
LONDON:
CHARLES GRIFFIN AND COMPANY, Limited,
EXETER STREET, STRAND.
1904.
[All rights reserved.]
Page 8
PUBLISHER'S NOTE TO THE NINTH EDITION
The continued popularity of the present work, the last edition of which was published only a
little over a year ago, continues to be a source of gratification to the publishers, who have
much pleasure in issuing the present edition.
January 1904.
The continued popularity of the present work, the last edition of which was published only a
little over a year ago, continues to be a source of gratification to the publishers, who have
much pleasure in issuing the present edition.
January 1904.
Page 9
PREFACE TO THE SIXTH EDITION
The principal changes in this edition are additions to the articles on Gold, Cyanides, and
Nickel, and a much enlarged Index. The additional matter covers more than forty pages.
J. J. BERINGER.
Camborne,
January 1900.
The principal changes in this edition are additions to the articles on Gold, Cyanides, and
Nickel, and a much enlarged Index. The additional matter covers more than forty pages.
J. J. BERINGER.
Camborne,
January 1900.
Page 10
PREFACE.
The Text-book now offered to the public has been prepared to meet the existing want of a
practical "handy book" for the Assayer.
To mining men the word "assaying" conveys a sufficiently clear meaning, but it is difficult
to define. Some writers limit it to the determination of silver and gold, and others imagine
that it has only to do with "furnace-work." These limitations are not recognised in practice.
In fact, assaying is becoming wider in its scope, and the distinction between "assayers" and
"analysts" will in time be difficult to detect. We have endeavoured rather to give what will
be of use to the assayer than to cover the ground within the limits of a faulty definition.
At first our intention was to supply a description of those substances only which have a
commercial value, but on consideration we have added short accounts of the rarer elements,
since they are frequently met with, and occasionally affect the accuracy of an assay.
Under the more important methods we have given the results of a series of experiments
showing the effect of varying conditions on the accuracy of the process. Such experiments
are often made by assayers, but seldom recorded. Statements like those generally made—
that "this or that substance interferes"—are insufficient. It is necessary to know under what
conditions and to what extent.
Students learning any particular process cannot do better than repeat such a series of
experiments. By this means they will, at the same time, acquire the skill necessary for
performing an assay and a confidence in their results based upon work under different
conditions.
The electrolytic method of copper assaying given under Copper is a modification of
Luckow's; it was introduced by us into the offices of the Rio Tinto Copper Company, and
has been in use for many years with success. This modification is now employed in copper-
works in Spain, Germany, and England, and is used in place of the dry assay for the
commercial valuation of copper ores.
We have adhered to the gram and the "c.c." as the units of weight and volume. Those who
prefer working with grains and grain-measures can use the figures given, multiplied by ten.
For example:—When 1 gram is mentioned, 10 grains should be used, and 10 grain-
measures take the place of 1 "c.c." It is not advisable to mix the two systems, as by using
gram weights and grain-measures.
We have intentionally to a large extent omitted to mention the names of those who have
originated or modified the various processes. The practice of naming a process after its
discoverer has developed of late years, and is becoming objectionable. It is a graceful thing
to name a gas-burner after Bunsen, or a condenser after Liebig; but when the practice has
developed so far that one is directed to "Finkenerise" a residue, or to use the "Reichert-
Meissl-Wollny" process, it is time to stop.
The Text-book now offered to the public has been prepared to meet the existing want of a
practical "handy book" for the Assayer.
To mining men the word "assaying" conveys a sufficiently clear meaning, but it is difficult
to define. Some writers limit it to the determination of silver and gold, and others imagine
that it has only to do with "furnace-work." These limitations are not recognised in practice.
In fact, assaying is becoming wider in its scope, and the distinction between "assayers" and
"analysts" will in time be difficult to detect. We have endeavoured rather to give what will
be of use to the assayer than to cover the ground within the limits of a faulty definition.
At first our intention was to supply a description of those substances only which have a
commercial value, but on consideration we have added short accounts of the rarer elements,
since they are frequently met with, and occasionally affect the accuracy of an assay.
Under the more important methods we have given the results of a series of experiments
showing the effect of varying conditions on the accuracy of the process. Such experiments
are often made by assayers, but seldom recorded. Statements like those generally made—
that "this or that substance interferes"—are insufficient. It is necessary to know under what
conditions and to what extent.
Students learning any particular process cannot do better than repeat such a series of
experiments. By this means they will, at the same time, acquire the skill necessary for
performing an assay and a confidence in their results based upon work under different
conditions.
The electrolytic method of copper assaying given under Copper is a modification of
Luckow's; it was introduced by us into the offices of the Rio Tinto Copper Company, and
has been in use for many years with success. This modification is now employed in copper-
works in Spain, Germany, and England, and is used in place of the dry assay for the
commercial valuation of copper ores.
We have adhered to the gram and the "c.c." as the units of weight and volume. Those who
prefer working with grains and grain-measures can use the figures given, multiplied by ten.
For example:—When 1 gram is mentioned, 10 grains should be used, and 10 grain-
measures take the place of 1 "c.c." It is not advisable to mix the two systems, as by using
gram weights and grain-measures.
We have intentionally to a large extent omitted to mention the names of those who have
originated or modified the various processes. The practice of naming a process after its
discoverer has developed of late years, and is becoming objectionable. It is a graceful thing
to name a gas-burner after Bunsen, or a condenser after Liebig; but when the practice has
developed so far that one is directed to "Finkenerise" a residue, or to use the "Reichert-
Meissl-Wollny" process, it is time to stop.
Page 11
We are indebted to the standard works of Allen, Crookes, Fresenius, Lunge, Michell, Percy,
and Sutton, and wish to express our sense of special indebtedness to Mr. Richard Smith, of
the Royal School of Mines. One or two of the illustrations are taken from Mr. Sexton's
excellent little book on Qualitative Analysis. Our obligation to some others is mentioned in
the text.
Finally, we have to thank for assistance in the experimental work Messrs. Bailey, Beswick,
Clarke, Grant, Higgins, and Smith.
THE AUTHORS.
Camborne, Nov. 1889.
and Sutton, and wish to express our sense of special indebtedness to Mr. Richard Smith, of
the Royal School of Mines. One or two of the illustrations are taken from Mr. Sexton's
excellent little book on Qualitative Analysis. Our obligation to some others is mentioned in
the text.
Finally, we have to thank for assistance in the experimental work Messrs. Bailey, Beswick,
Clarke, Grant, Higgins, and Smith.
THE AUTHORS.
Camborne, Nov. 1889.
Page 12
CONTENTS.
PART I.
CHAPTER I.
INTRODUCTORY.
Page
Object of assaying 1
Sampling 1
Drying: determination of moisture 5
Calculation and statement of results 7
Laboratory books and report forms 9
Quantity to be taken for an assay 11
Exercises 14
CHAPTER II.
METHODS OF ASSAYING.—DRY GRAVIMETRIC METHODS.
Methods of assaying 15
Gravimetric methods 15
Mechanical separations 16
Dry assays 16
(a) Fluxes 16
(b) Reducing agents 21
(c) Oxidising agents 22
(d) Apparatus 24
CHAPTER III.
WET GRAVIMETRIC METHODS.
Wet gravimetric methods 27
(a) Solution 29
(b) Precipitation 30
(c) Filtration 31
(d) Drying and igniting 32
CHAPTER IV.
VOLUMETRIC ASSAYS.
Titrometric assays 35
(a) Standard solutions 36
(b) Standardising 37
PART I.
CHAPTER I.
INTRODUCTORY.
Page
Object of assaying 1
Sampling 1
Drying: determination of moisture 5
Calculation and statement of results 7
Laboratory books and report forms 9
Quantity to be taken for an assay 11
Exercises 14
CHAPTER II.
METHODS OF ASSAYING.—DRY GRAVIMETRIC METHODS.
Methods of assaying 15
Gravimetric methods 15
Mechanical separations 16
Dry assays 16
(a) Fluxes 16
(b) Reducing agents 21
(c) Oxidising agents 22
(d) Apparatus 24
CHAPTER III.
WET GRAVIMETRIC METHODS.
Wet gravimetric methods 27
(a) Solution 29
(b) Precipitation 30
(c) Filtration 31
(d) Drying and igniting 32
CHAPTER IV.
VOLUMETRIC ASSAYS.
Titrometric assays 35
(a) Standard solutions 36
(b) Standardising 37
Page 13
(c) Methods of working 42
(d) Indirect titration 43
Colorimetric assays 44
Gasometric assays 44
CHAPTER V.
WEIGHING AND MEASURING.
Weighing 47
Measuring liquids 49
(a) Graduated flasks 49
(b) Pipettes 50
(c) Burettes 51
Measuring gases 52
CHAPTER VI.
REAGENTS.
Acids, &c. 54
Bases, salts, &c. 59
CHAPTER VII.
Formulæ, equations, &c. 68
CHAPTER VIII.
SPECIFIC GRAVITY.
Introductory 75
Determination of specific gravity—
(a) Hydrometers 76
(b) Specific gravity bottles 78
Calculations depending on specific gravity 84
PART II.
CHAPTER IX.
SILVER, GOLD, PLATINUM, CYANIDES, MERCURY.
Silver—Detection 87
Dry assay 87
(1) Scorification 88
(2) Pot assays, average ores 90
" ores with metallic oxides 91
" ores with metallic sulphides 91
(d) Indirect titration 43
Colorimetric assays 44
Gasometric assays 44
CHAPTER V.
WEIGHING AND MEASURING.
Weighing 47
Measuring liquids 49
(a) Graduated flasks 49
(b) Pipettes 50
(c) Burettes 51
Measuring gases 52
CHAPTER VI.
REAGENTS.
Acids, &c. 54
Bases, salts, &c. 59
CHAPTER VII.
Formulæ, equations, &c. 68
CHAPTER VIII.
SPECIFIC GRAVITY.
Introductory 75
Determination of specific gravity—
(a) Hydrometers 76
(b) Specific gravity bottles 78
Calculations depending on specific gravity 84
PART II.
CHAPTER IX.
SILVER, GOLD, PLATINUM, CYANIDES, MERCURY.
Silver—Detection 87
Dry assay 87
(1) Scorification 88
(2) Pot assays, average ores 90
" ores with metallic oxides 91
" ores with metallic sulphides 91
Page 14
Explanatory notes on the fusion 93
The effect of charcoal, flour, &c. 94
The effect of nitre 95
The effect of mineral sulphides 95
(3) Cupellation 98
The loss of silver 101
Condition affecting the loss 102
Methods of correction 103
Lead required for cupellation 105
(4) Calculation of the results in ounces to the ton of 2240 lbs. Table 107
Ores with metallic particles 108
(5) Explanatory notes 110
(6) Examples of dry silver assays 113
Wet assays 116
Gravimetric method 117
Gay-Lussac's method 119
Volhard's method 121
A modified Gay-Lussac 123
Volhard's method applied to arsenic 124
Gold—Detection 126
Amalgamation assay 126
Dry assay 127
(1) Size of charges 127
(2) Sampling 127
(3) Assay tons 131
(4) Small buttons, weighing 131
" " measuring 133
(5) Concentration in lead 136
Quartz ores 136
Ores with oxide of iron 138
Ores with metallic sulphides 139
(6) Cyanide charges, residues, &c. 140
(7) Cupellation 142
Cupels 142
Cupellation temperature 143
Cupellation loss 145
(8) Inquartation 146
(9) Flatting 149
(10) Parting, in flasks 151
" in test tubes 152
" in glazed crucibles 153
The effect of charcoal, flour, &c. 94
The effect of nitre 95
The effect of mineral sulphides 95
(3) Cupellation 98
The loss of silver 101
Condition affecting the loss 102
Methods of correction 103
Lead required for cupellation 105
(4) Calculation of the results in ounces to the ton of 2240 lbs. Table 107
Ores with metallic particles 108
(5) Explanatory notes 110
(6) Examples of dry silver assays 113
Wet assays 116
Gravimetric method 117
Gay-Lussac's method 119
Volhard's method 121
A modified Gay-Lussac 123
Volhard's method applied to arsenic 124
Gold—Detection 126
Amalgamation assay 126
Dry assay 127
(1) Size of charges 127
(2) Sampling 127
(3) Assay tons 131
(4) Small buttons, weighing 131
" " measuring 133
(5) Concentration in lead 136
Quartz ores 136
Ores with oxide of iron 138
Ores with metallic sulphides 139
(6) Cyanide charges, residues, &c. 140
(7) Cupellation 142
Cupels 142
Cupellation temperature 143
Cupellation loss 145
(8) Inquartation 146
(9) Flatting 149
(10) Parting, in flasks 151
" in test tubes 152
" in glazed crucibles 153
Page 15
" Loss, &c. 154
(11) Check assays, surcharge 154
(12) Bullion assays in special apparatus 156
Silver, &c., in gold bullion 157
(13) Sampling of base bullion, &c. 157
Cyanides—Commercial cyanides 160
Double cyanides 161
Prussic acid 162
Gold-dissolving power of cyanide liquor 162
Assay for cyanide strength 163, 165
Assay of commercial cyanide 167
Alkalinity of cyanides 167
Acidity of ores 168
Metals in cyanide liquors 169
Cyanicides 169
Platinum 170
Iridium 171
Mercury 171
Dry assay 172
Wet method 173
CHAPTER X.
COPPER, LEAD, THALLIUM, BISMUTH, ANTIMONY.
Copper—Introductory 175
Dry assay 176
Valuation of copper ores 181
Wet methods 183
(1) Electrolytic assay 184
Volumetric methods 194
(1) Cyanide method 194
(2) Iodide method 199
(3) Colorimetric method 203
Examination of commercial copper 205
Lead 211
Dry assay 211
Wet assay 213
(1) Gravimetric method 213
(2) Volumetric method 214
(3) Colorimetric method 218
Thallium 219
Bismuth 220
(11) Check assays, surcharge 154
(12) Bullion assays in special apparatus 156
Silver, &c., in gold bullion 157
(13) Sampling of base bullion, &c. 157
Cyanides—Commercial cyanides 160
Double cyanides 161
Prussic acid 162
Gold-dissolving power of cyanide liquor 162
Assay for cyanide strength 163, 165
Assay of commercial cyanide 167
Alkalinity of cyanides 167
Acidity of ores 168
Metals in cyanide liquors 169
Cyanicides 169
Platinum 170
Iridium 171
Mercury 171
Dry assay 172
Wet method 173
CHAPTER X.
COPPER, LEAD, THALLIUM, BISMUTH, ANTIMONY.
Copper—Introductory 175
Dry assay 176
Valuation of copper ores 181
Wet methods 183
(1) Electrolytic assay 184
Volumetric methods 194
(1) Cyanide method 194
(2) Iodide method 199
(3) Colorimetric method 203
Examination of commercial copper 205
Lead 211
Dry assay 211
Wet assay 213
(1) Gravimetric method 213
(2) Volumetric method 214
(3) Colorimetric method 218
Thallium 219
Bismuth 220
Page 16
Dry assay 221
Wet method 221
(1) Gravimetric determination 222
(2) Colorimetric assay 223
Antimony 225
Dry assay 225
Wet method 227
(1) Gravimetric assay 228
(2) Volumetric method 229
CHAPTER XI.
IRON, NICKEL, COBALT, ZINC, CADMIUM.
Iron 231
Gravimetric determination 233
Permanganate and bichromate methods 234
Stannous chloride method 244
Colorimetric determination 247
Nickel 251
Dry assay 251
Electrolytic assay 254
Titration by cyanide 255
Cobalt 259
Zinc 261
Gravimetric method 262
Volumetric method 263
Gasometric method 266
Cadmium 269
CHAPTER XII.
TIN, TUNGSTEN, TITANIUM.
Tin 271
Vanning 273
Dry assay 276
Detection, &c. 279
Gravimetric determination 281
Volumetric determination 282
Examples 284
Titanium 292
Tungsten 295
Niobic and Tantalic Oxides 297
Wet method 221
(1) Gravimetric determination 222
(2) Colorimetric assay 223
Antimony 225
Dry assay 225
Wet method 227
(1) Gravimetric assay 228
(2) Volumetric method 229
CHAPTER XI.
IRON, NICKEL, COBALT, ZINC, CADMIUM.
Iron 231
Gravimetric determination 233
Permanganate and bichromate methods 234
Stannous chloride method 244
Colorimetric determination 247
Nickel 251
Dry assay 251
Electrolytic assay 254
Titration by cyanide 255
Cobalt 259
Zinc 261
Gravimetric method 262
Volumetric method 263
Gasometric method 266
Cadmium 269
CHAPTER XII.
TIN, TUNGSTEN, TITANIUM.
Tin 271
Vanning 273
Dry assay 276
Detection, &c. 279
Gravimetric determination 281
Volumetric determination 282
Examples 284
Titanium 292
Tungsten 295
Niobic and Tantalic Oxides 297
Page 17
CHAPTER XIII.
MANGANESE, CHROMIUM, ETC.
Manganese 298
Gravimetric determination 300
Volumetric determination 300
Ferrous sulphate assay 301
Iodine assay 302
Colorimetric determination 306
Chromium 307
Vanadium 310
Molybdenum 311
Uranium 312
CHAPTER XIV.
EARTHS, ALKALINE EARTHS, ALKALIES.
Alumina 314
Thoria 317
Zirconia 317
Cerium 318
Lanthanum and Didymium 319
Yttria 319
Beryllia 319
Lime 320
Strontia 324
Baryta 326
Magnesia 328
The Alkalies 330
Sodium 334
Potassium 336
Lithium 338
Cæsium 339
Rubidium 340
Ammonium 340
PART III.
CHAPTER XV.
OXYGEN AND OXIDES—THE HALOGENS.
Oxygen 344
Oxides 345
MANGANESE, CHROMIUM, ETC.
Manganese 298
Gravimetric determination 300
Volumetric determination 300
Ferrous sulphate assay 301
Iodine assay 302
Colorimetric determination 306
Chromium 307
Vanadium 310
Molybdenum 311
Uranium 312
CHAPTER XIV.
EARTHS, ALKALINE EARTHS, ALKALIES.
Alumina 314
Thoria 317
Zirconia 317
Cerium 318
Lanthanum and Didymium 319
Yttria 319
Beryllia 319
Lime 320
Strontia 324
Baryta 326
Magnesia 328
The Alkalies 330
Sodium 334
Potassium 336
Lithium 338
Cæsium 339
Rubidium 340
Ammonium 340
PART III.
CHAPTER XV.
OXYGEN AND OXIDES—THE HALOGENS.
Oxygen 344
Oxides 345
Page 18
Water 350
The Halogens 358
Chlorine 359
Bromine 361
Iodine 362
Fluorine 363
CHAPTER XVI.
SULPHUR AND SULPHATES.
Sulphur 367
Gravimetric determination 369
Volumetric determination 370
Sulphates 377
Selenium 379
Tellurium 379
CHAPTER XVII.
ARSENIC, PHOSPHORUS, NITROGEN.
Arsenic 381
Gravimetric determination 383
Volumetric method, "iodine" 384
" " "uranic acetate" 389
Phosphorus 394
Gravimetric determination 396
Volumetric determination 397
Nitrogen and Nitrates 400
CHAPTER XVIII.
SILICON, CARBON, BORON.
Silicon and Silicates 405
Carbon and Carbonates 414
Coals 418
Shales 420
Carbonates 424
Boron and Borates 429
APPENDIX A.
Table of atomic weights and other constants 433
Table for converting degrees of the centigrade thermometer
into degrees of Fahrenheit's scale 435
Tables showing strengths of aqueous solutions of nitric and hydrochloric acids,
The Halogens 358
Chlorine 359
Bromine 361
Iodine 362
Fluorine 363
CHAPTER XVI.
SULPHUR AND SULPHATES.
Sulphur 367
Gravimetric determination 369
Volumetric determination 370
Sulphates 377
Selenium 379
Tellurium 379
CHAPTER XVII.
ARSENIC, PHOSPHORUS, NITROGEN.
Arsenic 381
Gravimetric determination 383
Volumetric method, "iodine" 384
" " "uranic acetate" 389
Phosphorus 394
Gravimetric determination 396
Volumetric determination 397
Nitrogen and Nitrates 400
CHAPTER XVIII.
SILICON, CARBON, BORON.
Silicon and Silicates 405
Carbon and Carbonates 414
Coals 418
Shales 420
Carbonates 424
Boron and Borates 429
APPENDIX A.
Table of atomic weights and other constants 433
Table for converting degrees of the centigrade thermometer
into degrees of Fahrenheit's scale 435
Tables showing strengths of aqueous solutions of nitric and hydrochloric acids,
Page 19
of ammonia and of sulphuric acid 436
APPENDIX B.
Estimation of small quantities of gold 440
Practical notes on the iodide process of copper assaying 441
Method of separating cobalt and nickel 442
APPENDIX C.
A lecture on the theory of sampling 444
Index 450
APPENDIX B.
Estimation of small quantities of gold 440
Practical notes on the iodide process of copper assaying 441
Method of separating cobalt and nickel 442
APPENDIX C.
A lecture on the theory of sampling 444
Index 450
Page 20
A TEXT-BOOK OF ASSAYING.
Page 21
CHAPTER I.
INTRODUCTORY.
Assaying has for its object the determination of the quantities of those constituents of a
material which add to or detract from its value in the arts and manufactures. The methods of
assaying are mainly those of analytical chemistry, and are limited by various practical
considerations to the determination of the constituents of a small parcel, which is frequently
only a few grains, and rarely more than a few ounces, in weight. From these determinations
calculations are made, which have reference to a mass of material of, perhaps, hundreds of
tons. But in all cases, whether the mass under consideration be large or small, whether the
material be obtained by mining, grown, or manufactured, the assayer is supposed to receive
a small quantity, called "the sample," which is, or ought to be, the exact counterpart of the
mass of material that is being dealt with. The taking and making of this sample is termed
"sampling"; and the men whose special work it is to select such samples are "the samplers."
But although "sampling" is thus distinct from "assaying," the assayer should be familiar
with the principles of sampling, and rigorous in the application of these principles in the
selecting, from the sample sent him, that smaller portion upon which he performs his
operations.
Sampling.—In the case of gases, there is absolutely no trouble in mixing. The only
difficulty is in drawing off a fair sample where, as in flues, the body of the gas is in motion,
and varies a little in composition from time to time. In this case, care must be taken to draw
off uniformly a sufficient volume of the gas during a prolonged period; any portion of this
larger volume may then be taken for the analytical operation.
In the case of liquids, which mix more or less easily—and this class includes metals, &c., in
the state of fusion—more or less severe agitation, followed by the immediate withdrawal of
a portion, will yield a fairly representative sample.
In the case of solids, the whole mass must be crushed, and, if not already of fairly uniform
quality, mixed, before sampling can take place. Most of the material which a sampler is
called upon to deal with, is, however, in a more or less divided state and fairly uniform. In
practice it is assumed that 5 per cent. of the whole (= 1/20th), if taken in portions of equal
weight and at frequent and regular intervals, will represent the mass from which it was
taken. Taking a heap of ore, A, and selecting one out of every twenty spade-, bag-, barrow-,
or wagon-fuls, according to the quantity of stuff in the heap, there is obtained a second
heap, B, containing one-twentieth of the stuff of the heap A. If we crush the stuff in B until
this heap contains approximately the same number of stones as A did—which means,
crushing every stone in B into about twenty pieces—B will become the counterpart of A.
Selecting in the same manner 5 per cent. of B, there is got a third heap, C. This alternate
INTRODUCTORY.
Assaying has for its object the determination of the quantities of those constituents of a
material which add to or detract from its value in the arts and manufactures. The methods of
assaying are mainly those of analytical chemistry, and are limited by various practical
considerations to the determination of the constituents of a small parcel, which is frequently
only a few grains, and rarely more than a few ounces, in weight. From these determinations
calculations are made, which have reference to a mass of material of, perhaps, hundreds of
tons. But in all cases, whether the mass under consideration be large or small, whether the
material be obtained by mining, grown, or manufactured, the assayer is supposed to receive
a small quantity, called "the sample," which is, or ought to be, the exact counterpart of the
mass of material that is being dealt with. The taking and making of this sample is termed
"sampling"; and the men whose special work it is to select such samples are "the samplers."
But although "sampling" is thus distinct from "assaying," the assayer should be familiar
with the principles of sampling, and rigorous in the application of these principles in the
selecting, from the sample sent him, that smaller portion upon which he performs his
operations.
Sampling.—In the case of gases, there is absolutely no trouble in mixing. The only
difficulty is in drawing off a fair sample where, as in flues, the body of the gas is in motion,
and varies a little in composition from time to time. In this case, care must be taken to draw
off uniformly a sufficient volume of the gas during a prolonged period; any portion of this
larger volume may then be taken for the analytical operation.
In the case of liquids, which mix more or less easily—and this class includes metals, &c., in
the state of fusion—more or less severe agitation, followed by the immediate withdrawal of
a portion, will yield a fairly representative sample.
In the case of solids, the whole mass must be crushed, and, if not already of fairly uniform
quality, mixed, before sampling can take place. Most of the material which a sampler is
called upon to deal with, is, however, in a more or less divided state and fairly uniform. In
practice it is assumed that 5 per cent. of the whole (= 1/20th), if taken in portions of equal
weight and at frequent and regular intervals, will represent the mass from which it was
taken. Taking a heap of ore, A, and selecting one out of every twenty spade-, bag-, barrow-,
or wagon-fuls, according to the quantity of stuff in the heap, there is obtained a second
heap, B, containing one-twentieth of the stuff of the heap A. If we crush the stuff in B until
this heap contains approximately the same number of stones as A did—which means,
crushing every stone in B into about twenty pieces—B will become the counterpart of A.
Selecting in the same manner 5 per cent. of B, there is got a third heap, C. This alternate
Page 22
reduction and pulverising must be carried on until a sample of suitable size is obtained. This
may be expressed very clearly thus:—
A = 1000 tons of rocks and lumpy ore.
B = 50 " " rough stones, 1/20th of A.
C = 2.5 " " small stones, 1/20th of B.
D = 0.125 " " coarse powder, 1/20th of C.
If the material to be sampled is already a dry powder, 5 per cent. of it should be heaped in a
cone; each lot being added on the apex of the cone already formed, so that it may distribute
itself by falling evenly in all directions. When the cone is completed, convert it into a low
frustrum of a cone by drawing stuff uniformly and in a direct line from the centre to the
circumference. Draw two diameters at right angles to each other, and reserving any two
alternate quarters, reject the others. Mix; and form another cone, and proceed until a sample
is got of the bulk required.
This is the usual plan, and all samples should be treated in this way when the stuff is fine
enough to fall evenly down the sides of a cone.
Samples as they reach the assay office are seldom in a fit state for the work of the assayer;
they are generally too coarse, and ought always to be more than he wants for any particular
determination. The portion he requires should never be taken at hap-hazard; the sample
must be reduced systematically to the quantity required.
1. If the sample is a liquid: it is sufficient to shake the bottle, and take out a measured or
weighed quantity for the assay.
2. If a liquid with a solid in suspension: measure the whole of it. Filter. Make up the filtrate
with the wash-water or water to the original bulk. Assay it. Dry and weigh the residue, and
make a separate assay of it.
3. If of a creamy consistency, free from heavy particles: mix well; spread out evenly on a
glazed tile. Take up equal portions at equal distances. Mix and assay.
may be expressed very clearly thus:—
A = 1000 tons of rocks and lumpy ore.
B = 50 " " rough stones, 1/20th of A.
C = 2.5 " " small stones, 1/20th of B.
D = 0.125 " " coarse powder, 1/20th of C.
If the material to be sampled is already a dry powder, 5 per cent. of it should be heaped in a
cone; each lot being added on the apex of the cone already formed, so that it may distribute
itself by falling evenly in all directions. When the cone is completed, convert it into a low
frustrum of a cone by drawing stuff uniformly and in a direct line from the centre to the
circumference. Draw two diameters at right angles to each other, and reserving any two
alternate quarters, reject the others. Mix; and form another cone, and proceed until a sample
is got of the bulk required.
This is the usual plan, and all samples should be treated in this way when the stuff is fine
enough to fall evenly down the sides of a cone.
Samples as they reach the assay office are seldom in a fit state for the work of the assayer;
they are generally too coarse, and ought always to be more than he wants for any particular
determination. The portion he requires should never be taken at hap-hazard; the sample
must be reduced systematically to the quantity required.
1. If the sample is a liquid: it is sufficient to shake the bottle, and take out a measured or
weighed quantity for the assay.
2. If a liquid with a solid in suspension: measure the whole of it. Filter. Make up the filtrate
with the wash-water or water to the original bulk. Assay it. Dry and weigh the residue, and
make a separate assay of it.
3. If of a creamy consistency, free from heavy particles: mix well; spread out evenly on a
glazed tile. Take up equal portions at equal distances. Mix and assay.
Page 23
4. If a mud of coarse and fine particles, or of particles of unequal density: weigh and
transfer to a porcelain dish, or weigh in the dish. Dry at 100° C., weigh. Treat the residue as
a solid capable of being powdered.
5. If a solid capable of being powdered, or already powdered: heap up into a cone; flatten
with a spatula; divide along two diameters at right angles, and carefully reject the whole of
two alternate quarters, brushing away any fine powder. Mix the other quarters, and repeat (if
necessary). For small quantities a fine state of division is essential.
6. If a solid with metallic particles: powder and pass through a sieve; the metallic particles
will not pass through. Weigh both portions and assay separately. Sifting should be followed
by a very thorough mixing.
7. If a metal or alloy in bar or ingot: clean the upper surface of the bar, and bore through
the bar. Use the borings. If the ingot or bar is small, cut it through and file the section.
Filings must be freed from fragments of the file by means of a magnet; and from oil, if any
be present, by washing with a suitable solvent.[1] Where practicable, metals and alloys are
best sampled by melting and granulating. The student must carefully avoid any chance of
mixing dirt or particles of other samples with the particular sample which he is preparing.
One ore should be done at a time, and when finished, it should be labelled and wrapped up,
or bottled, before starting on a fresh sample.
When an ore requires to be very finely ground in an agate mortar, it is often advisable to
mix with a little pure alcohol and rub until free from grit; dry at 100° C. and mix well
before weighing.
When an assay is required of a quantity of ore made up of parcels of different weight and
quality, each parcel should be separately sampled and parts of each sample, bearing to each
other the same proportion by weight as the original parcels, should be taken and mixed. For
example, a lot of ore is made up of one parcel of A, 570 tons, one of B, 180 tons, and
another of C, 50 tons; a sample representing the whole may be got by mixing 57 parts of a
sample of A with 18 parts of a sample of B, and 5 parts of a sample of C.
transfer to a porcelain dish, or weigh in the dish. Dry at 100° C., weigh. Treat the residue as
a solid capable of being powdered.
5. If a solid capable of being powdered, or already powdered: heap up into a cone; flatten
with a spatula; divide along two diameters at right angles, and carefully reject the whole of
two alternate quarters, brushing away any fine powder. Mix the other quarters, and repeat (if
necessary). For small quantities a fine state of division is essential.
6. If a solid with metallic particles: powder and pass through a sieve; the metallic particles
will not pass through. Weigh both portions and assay separately. Sifting should be followed
by a very thorough mixing.
7. If a metal or alloy in bar or ingot: clean the upper surface of the bar, and bore through
the bar. Use the borings. If the ingot or bar is small, cut it through and file the section.
Filings must be freed from fragments of the file by means of a magnet; and from oil, if any
be present, by washing with a suitable solvent.[1] Where practicable, metals and alloys are
best sampled by melting and granulating. The student must carefully avoid any chance of
mixing dirt or particles of other samples with the particular sample which he is preparing.
One ore should be done at a time, and when finished, it should be labelled and wrapped up,
or bottled, before starting on a fresh sample.
When an ore requires to be very finely ground in an agate mortar, it is often advisable to
mix with a little pure alcohol and rub until free from grit; dry at 100° C. and mix well
before weighing.
When an assay is required of a quantity of ore made up of parcels of different weight and
quality, each parcel should be separately sampled and parts of each sample, bearing to each
other the same proportion by weight as the original parcels, should be taken and mixed. For
example, a lot of ore is made up of one parcel of A, 570 tons, one of B, 180 tons, and
another of C, 50 tons; a sample representing the whole may be got by mixing 57 parts of a
sample of A with 18 parts of a sample of B, and 5 parts of a sample of C.
Page 24
A bruising plate, like that in fig. 2, is convenient for general office work. The slab is of cast
iron, about an inch thick. It is firmly supported on a solid block of wood, and pivoted for
convenience in emptying. The bruising-hammer is steel-faced, about 4 inches square, and 1-
1/2 inch thick. The block is firmly fixed to a small table or tressel, so that the slab is about 2
feet 6 inches from the ground. The slab is cleaned, and the sample collected with the help of
a stiff-haired brush.
Drying: Determination of Moisture.—In practice, the moisture is generally determined by
the samplers, and the proportion is specified in grains per pound on the label attached to the
sample when it reaches the assay office. The method adopted is usually to dry 1 lb. = 7000
grs. of the ore in a frying-pan heated over a gas flame, or in an ordinary oven, until a cold
bright piece of metal or glass is no longer damped when held over it. The loss of weight in
grains = moisture.
Properly, however, this work should be done by the assayer, if only for the following
reason. It is assumed that the dry ore of the sampler and of the assayer are the same thing;
according to the nature of the ore, this may or may not be the case. The assayer, however,
uses the sample which he has dried for his moisture-determination, as the dry ore on which
he makes his other assays, and no variation in moisture would influence the other and more
important determinations. Some ores are sent to the smelter with from 5 to 15 per cent. of
adherent water. In these cases it is best to spread out the sample, and taking equal portions
fairly at regular intervals, weigh into a Berlin dish 20 grams. This should then be dried over
a sand-bath, or if the ore is likely to be injured by excess of heat, over a water-bath until the
weight is constant. The loss of weight multiplied by 5 gives the percentage of water present.
Example:—
Weight of dish + wolfram 32.67 grms.
" " dish 12.67 "
———
" " wolfram 20.00 "
" " dish + wolfram 32.67 "
" " " dried 30.15 "
———
" " water 2.52 "
2.52 × 5 = 12.6 12.6%.
There are other ores which are not apparently wet, but in the state called "air-dried." It is
easier to take fair samples of these, and, consequently, it is not necessary to use so large a
quantity as 20 grams. But with a smaller quantity, extra precautions must be taken. All dry
solids at ordinary temperatures absorb moisture from the air. The amount varies with the
nature of the material and with the quantity of surface exposed. Light bulky powders absorb
more than heavy ones, because of the greater condensing surface. It is on this account that it
is well to weigh substances, which have been dried, between close-fitting watch-glasses.
The method of determining moisture is to weigh out into the glasses 5 grams of ore, and dry
iron, about an inch thick. It is firmly supported on a solid block of wood, and pivoted for
convenience in emptying. The bruising-hammer is steel-faced, about 4 inches square, and 1-
1/2 inch thick. The block is firmly fixed to a small table or tressel, so that the slab is about 2
feet 6 inches from the ground. The slab is cleaned, and the sample collected with the help of
a stiff-haired brush.
Drying: Determination of Moisture.—In practice, the moisture is generally determined by
the samplers, and the proportion is specified in grains per pound on the label attached to the
sample when it reaches the assay office. The method adopted is usually to dry 1 lb. = 7000
grs. of the ore in a frying-pan heated over a gas flame, or in an ordinary oven, until a cold
bright piece of metal or glass is no longer damped when held over it. The loss of weight in
grains = moisture.
Properly, however, this work should be done by the assayer, if only for the following
reason. It is assumed that the dry ore of the sampler and of the assayer are the same thing;
according to the nature of the ore, this may or may not be the case. The assayer, however,
uses the sample which he has dried for his moisture-determination, as the dry ore on which
he makes his other assays, and no variation in moisture would influence the other and more
important determinations. Some ores are sent to the smelter with from 5 to 15 per cent. of
adherent water. In these cases it is best to spread out the sample, and taking equal portions
fairly at regular intervals, weigh into a Berlin dish 20 grams. This should then be dried over
a sand-bath, or if the ore is likely to be injured by excess of heat, over a water-bath until the
weight is constant. The loss of weight multiplied by 5 gives the percentage of water present.
Example:—
Weight of dish + wolfram 32.67 grms.
" " dish 12.67 "
———
" " wolfram 20.00 "
" " dish + wolfram 32.67 "
" " " dried 30.15 "
———
" " water 2.52 "
2.52 × 5 = 12.6 12.6%.
There are other ores which are not apparently wet, but in the state called "air-dried." It is
easier to take fair samples of these, and, consequently, it is not necessary to use so large a
quantity as 20 grams. But with a smaller quantity, extra precautions must be taken. All dry
solids at ordinary temperatures absorb moisture from the air. The amount varies with the
nature of the material and with the quantity of surface exposed. Light bulky powders absorb
more than heavy ones, because of the greater condensing surface. It is on this account that it
is well to weigh substances, which have been dried, between close-fitting watch-glasses.
The method of determining moisture is to weigh out into the glasses 5 grams of ore, and dry
Page 25
in the water-oven until there is no further loss of weight. On taking the glasses out of the
oven, they should be at once closed, the clip put on, and after cooling in a desiccator
weighed. If after a second trial the loss is the same, or only increased by a milligram, the
determination is finished.
Example:—
Weight of glasses + pyrites 31.0470 grms.
" " glasses 26.0470 "
———
" " pyrites 5.0000 "
" " glasses + pyrites, dried 1 hour 30.8965 "
" " " " dried 1-1/2 " 30.8957 "
" " " " 31.0470 "
" " " " dried 30.8957 "
———
" " moisture 0.1513 "
0.1513 × 20 = 3.026 3.02%.
Sometimes it may be advisable to dry 10 grams, in which case multiplying the loss by 10
will give the percentage. The dried ore should be transferred to a weighing-tube (fig. 3), and
reserved for the subsequent determinations. The weighing-tube with the ore must be
marked, and kept in a desiccator.
Most ores and inorganic substances can be dried, and their moisture determined by the loss
in this way. When, however, the substance contains another somewhat volatile ingredient, it
oven, they should be at once closed, the clip put on, and after cooling in a desiccator
weighed. If after a second trial the loss is the same, or only increased by a milligram, the
determination is finished.
Example:—
Weight of glasses + pyrites 31.0470 grms.
" " glasses 26.0470 "
———
" " pyrites 5.0000 "
" " glasses + pyrites, dried 1 hour 30.8965 "
" " " " dried 1-1/2 " 30.8957 "
" " " " 31.0470 "
" " " " dried 30.8957 "
———
" " moisture 0.1513 "
0.1513 × 20 = 3.026 3.02%.
Sometimes it may be advisable to dry 10 grams, in which case multiplying the loss by 10
will give the percentage. The dried ore should be transferred to a weighing-tube (fig. 3), and
reserved for the subsequent determinations. The weighing-tube with the ore must be
marked, and kept in a desiccator.
Most ores and inorganic substances can be dried, and their moisture determined by the loss
in this way. When, however, the substance contains another somewhat volatile ingredient, it
Page 26
is exposed over sulphuric acid in a desiccator for two days (if in vacuo, all the better), and
the loss determined. Moisture in dynamite should be determined in this way.
When water is simply mechanically mixed with a substance it presents but little difficulty.
The combined water is a different matter. Slaked lime, even when perfectly dry, contains
much water; and if the water of soda crystals were separated and frozen, it would occupy a
volume equal to that of the original crystals. Perfectly dry substances may contain much
water, and this combined water is retained by different materials with very unequal vigour.
Sodium sulphate and sodium phosphate crystals lose water even when exposed under
ordinary conditions to dry air. Soda crystals when heated melt, and at a moderate
temperature give off their water with ebullition. The temperature at which all the water is
given up varies with each particular salt; the actual determination of the water in each case
will require somewhat different treatment. Such determinations, however, are seldom
required; and from a practical point of view this combined water causes no trouble.
In assaying ores, we term "moisture" all water which is lost by exposure in a water-oven at
100° C., and the "dry ore" is the ore which has been dried at this temperature. No
advantage, but rather endless confusion, would be caused by varying the temperature with
the object of estimating the whole of the water which a hydrated salt may contain. The
results of the assay of the other components should be calculated on the "dry ore." One
advantage of this is obvious:—The dry ore has a constant composition, and the results of all
assays of it will be the same, no matter when made; the moisture, however, may vary from
day to day, and would be influenced by a passing shower of rain. It is well to limit this
variability to the moisture by considering it apart, and thus avoid having the percentage, say,
of copper rising and falling under the influence of the weather.
In the case of certain salts, however, such as soda crystals and hydrated sulphate of copper
(when these constitute the bulk of the substance to be assayed), it is as well to perform the
assay on the moist, or at any rate air-dried, substance.[2] It would be equally convenient to
calculate on the substance dried at 100° C.; but in this case it would be well, in order to
avoid a somewhat shallow criticism, to replace the term "moisture" by the longer but
equivalent phrase "water lost at 100° C."
Calculation and Statement of Results.—By far the most generally convenient method of
stating the results of an assay is that of the percentage or parts in a hundred, and to avoid a
needlessly troublesome calculation it is well to take such a quantity of ore for each assay as
by a simple multiplication will yield the percentage. In these calculations decimals are
freely employed, and students should make themselves familiar with the methods of using
them.
Other methods of statement are in use, and have advantages in certain special cases. With
bullion the parts in a thousand are given, and in those cases in which the percentage is very
small, as in water analysis, it is convenient to report on parts in 100,000, or even on parts
per 1,000,000. These are easily got from the corresponding percentages by shifting the
decimal point one, three, or four places to the right. Thus 92.5 per cent. is 925 per thousand;
and 0.0036 per cent. is 3.6 per 100,000, or 36 per million.
the loss determined. Moisture in dynamite should be determined in this way.
When water is simply mechanically mixed with a substance it presents but little difficulty.
The combined water is a different matter. Slaked lime, even when perfectly dry, contains
much water; and if the water of soda crystals were separated and frozen, it would occupy a
volume equal to that of the original crystals. Perfectly dry substances may contain much
water, and this combined water is retained by different materials with very unequal vigour.
Sodium sulphate and sodium phosphate crystals lose water even when exposed under
ordinary conditions to dry air. Soda crystals when heated melt, and at a moderate
temperature give off their water with ebullition. The temperature at which all the water is
given up varies with each particular salt; the actual determination of the water in each case
will require somewhat different treatment. Such determinations, however, are seldom
required; and from a practical point of view this combined water causes no trouble.
In assaying ores, we term "moisture" all water which is lost by exposure in a water-oven at
100° C., and the "dry ore" is the ore which has been dried at this temperature. No
advantage, but rather endless confusion, would be caused by varying the temperature with
the object of estimating the whole of the water which a hydrated salt may contain. The
results of the assay of the other components should be calculated on the "dry ore." One
advantage of this is obvious:—The dry ore has a constant composition, and the results of all
assays of it will be the same, no matter when made; the moisture, however, may vary from
day to day, and would be influenced by a passing shower of rain. It is well to limit this
variability to the moisture by considering it apart, and thus avoid having the percentage, say,
of copper rising and falling under the influence of the weather.
In the case of certain salts, however, such as soda crystals and hydrated sulphate of copper
(when these constitute the bulk of the substance to be assayed), it is as well to perform the
assay on the moist, or at any rate air-dried, substance.[2] It would be equally convenient to
calculate on the substance dried at 100° C.; but in this case it would be well, in order to
avoid a somewhat shallow criticism, to replace the term "moisture" by the longer but
equivalent phrase "water lost at 100° C."
Calculation and Statement of Results.—By far the most generally convenient method of
stating the results of an assay is that of the percentage or parts in a hundred, and to avoid a
needlessly troublesome calculation it is well to take such a quantity of ore for each assay as
by a simple multiplication will yield the percentage. In these calculations decimals are
freely employed, and students should make themselves familiar with the methods of using
them.
Other methods of statement are in use, and have advantages in certain special cases. With
bullion the parts in a thousand are given, and in those cases in which the percentage is very
small, as in water analysis, it is convenient to report on parts in 100,000, or even on parts
per 1,000,000. These are easily got from the corresponding percentages by shifting the
decimal point one, three, or four places to the right. Thus 92.5 per cent. is 925 per thousand;
and 0.0036 per cent. is 3.6 per 100,000, or 36 per million.
Page 27
With ores of tin, silver, and gold, the result is stated as so many cwts., lbs., or ozs., in the
ton. With dressed tin ores as they are sent to the smelter, the produce is given in cwts. and
quarters to the ton. The corresponding percentage may be obtained by multiplying by five;
or, inversely, if the percentage is given, the produce may be got by dividing by five. A
produce of 13-1/2 equals a percentage of 13.5 × 5 = 67.5; and a percentage of 70.0 equals a
produce of 70 / 5 = 14. With tin ores as raised (in which the percentage is small) the
reduction must be carried to pounds per ton. One per cent. equals 22.4 lbs. to the ton;
consequently, if we multiply the percentage by 22.4, the produce will be given. Thus, if an
ore contains 6.7 per cent. of oxide of tin, the produce is 6.7 × 22.4 = 150 lbs. (or 1 cwt., 1
quarter, and 10 lbs.) to the ton. With gold and silver ores, the proportion of precious metal is
small, and it is necessary to carry the reduction to ozs. and dwts. to the ton; and since gold
and silver are sold by troy weight, whilst the ton is avoirdupois, it is of importance to
remember that the ounces in the two systems are not the same. A ton contains 15,680,000
grains, which equal 653,333.3 dwts. or 32,666.6 ozs. (troy). The following rules are useful:
—
To get ozs. (troy) per ton, multiply parts per 100,000 by 0.327;
To get dwts. per ton, multiply parts per 100,000 by 6.53;
To get grains per ton, multiply parts per 100,000 by 156.8.
Where liquids are being assayed, cubic centimetres are held to be equivalent to grams, and
the usual method of statement is, "so many parts by weight in so many by measure." Where
the statement is made as grams per litre or grains per gallon, there can be no doubt as to
what is meant; and even if it be expressed in parts per 100,000, parts by weight in a
measured volume must be understood unless the contrary is expressly stated.
In some cases, where the density of the solution differs greatly from that of water, the
percentage by weight may be given; and in others, mixtures of two or more liquids, the
percentages may be given by volume or by weight; as so many c.c. in 100 c.c., or as so
many grams in 100 grams, or even as so many grams in 100 c.c. In such cases it must be
distinctly shown which method of statement is adopted.
One grain per gallon means 1 grain in 70,000 grain-measures, or one part in 70,000.
Dividing by 7 and multiplying by 10 will convert grains per gallon into parts per 100,000.
Inversely, dividing by 10 and multiplying by 7, will convert parts per 100,000 into grains
per gallon.
Grams per litre are parts per 1000; multiplying by 100 will give parts per 100,000, and
multiplying by 70 will give grains per gallon.
Among foreign systems of weights, the French is by far the best. Kilograms (2.205 lbs.) per
quintal (220.5 lbs.) are parts per cent.; and grams (15.43 grs.) per quintal are parts per
100,000. From the rule already given, grams per quintal may be converted into ounces to
the ton by multiplying by 0.327.
The German loths per centner (1/2 oz. (avoirdupois) to 100 lbs.) equal parts per 3200; they
are converted into parts per cent. by dividing by 32, or into ounces (troy) per ton by
ton. With dressed tin ores as they are sent to the smelter, the produce is given in cwts. and
quarters to the ton. The corresponding percentage may be obtained by multiplying by five;
or, inversely, if the percentage is given, the produce may be got by dividing by five. A
produce of 13-1/2 equals a percentage of 13.5 × 5 = 67.5; and a percentage of 70.0 equals a
produce of 70 / 5 = 14. With tin ores as raised (in which the percentage is small) the
reduction must be carried to pounds per ton. One per cent. equals 22.4 lbs. to the ton;
consequently, if we multiply the percentage by 22.4, the produce will be given. Thus, if an
ore contains 6.7 per cent. of oxide of tin, the produce is 6.7 × 22.4 = 150 lbs. (or 1 cwt., 1
quarter, and 10 lbs.) to the ton. With gold and silver ores, the proportion of precious metal is
small, and it is necessary to carry the reduction to ozs. and dwts. to the ton; and since gold
and silver are sold by troy weight, whilst the ton is avoirdupois, it is of importance to
remember that the ounces in the two systems are not the same. A ton contains 15,680,000
grains, which equal 653,333.3 dwts. or 32,666.6 ozs. (troy). The following rules are useful:
—
To get ozs. (troy) per ton, multiply parts per 100,000 by 0.327;
To get dwts. per ton, multiply parts per 100,000 by 6.53;
To get grains per ton, multiply parts per 100,000 by 156.8.
Where liquids are being assayed, cubic centimetres are held to be equivalent to grams, and
the usual method of statement is, "so many parts by weight in so many by measure." Where
the statement is made as grams per litre or grains per gallon, there can be no doubt as to
what is meant; and even if it be expressed in parts per 100,000, parts by weight in a
measured volume must be understood unless the contrary is expressly stated.
In some cases, where the density of the solution differs greatly from that of water, the
percentage by weight may be given; and in others, mixtures of two or more liquids, the
percentages may be given by volume or by weight; as so many c.c. in 100 c.c., or as so
many grams in 100 grams, or even as so many grams in 100 c.c. In such cases it must be
distinctly shown which method of statement is adopted.
One grain per gallon means 1 grain in 70,000 grain-measures, or one part in 70,000.
Dividing by 7 and multiplying by 10 will convert grains per gallon into parts per 100,000.
Inversely, dividing by 10 and multiplying by 7, will convert parts per 100,000 into grains
per gallon.
Grams per litre are parts per 1000; multiplying by 100 will give parts per 100,000, and
multiplying by 70 will give grains per gallon.
Among foreign systems of weights, the French is by far the best. Kilograms (2.205 lbs.) per
quintal (220.5 lbs.) are parts per cent.; and grams (15.43 grs.) per quintal are parts per
100,000. From the rule already given, grams per quintal may be converted into ounces to
the ton by multiplying by 0.327.
The German loths per centner (1/2 oz. (avoirdupois) to 100 lbs.) equal parts per 3200; they
are converted into parts per cent. by dividing by 32, or into ounces (troy) per ton by
Page 28
multiplying by 10.208.
In the United States, as a sort of compromise between the avoirdupois and metric systems, a
ton is taken as 2000 lbs. There, too, the custom is adopted of reporting the gold and silver
contents of an ore as so many dollars and cents to the ton. In the case of gold, an ounce is
considered to be worth 20.6718 dollars. With silver, the nominal value is 1.2929 dollars per
ounce, but frequently in assay reports it is taken as one dollar. The practice is objectionable.
The prices of metals vary with the fluctuations of the market, and if the assayer fixed the
price, the date of his report would be all important; if, on the other hand, he takes a fixed
price which does not at all times agree with the market one, it leaves a path open for the
deception of those unacquainted with the custom. American "dollars on the ton of 2000 lbs."
may be converted into "ounces in the ton of 2240 lbs." by dividing by 1.1544 in the case of
silver, and by 18.457 in the case of gold.
Laboratory Books and Report Forms.—The record which the assayer makes of his work
must be clear and neat, so that reference, even after an interval of years, should be certain
and easy. One method should be adopted and adhered to. Where there are a large number of
samples, three books are required.
Sample Book.—This contains particulars of the samples (marks, &c.), which are entered by
the office-clerk as they arrive. He at the same time puts on each sample the distinguishing
number.
Example of Page of Sample Book.
Date. Number. Sample. Remarks.
Feb. 1482 Tough Copper For Arsenic.
" 2X Piece of Metal For Ni and Cu.
" 483 Tough Copper.
" 73 Silver Precipitate, 4 casks, 24 cwt. 1 qr. With Letter.
" 494 Purple Ore, 200 tons.
" 1 J.T. Lead Ore, 1 J.T. From Corsica.
" 2 J.T. " 2 J.T.
Laboratory Book. This is the Assayer's note-book, in which he enters clearly the particulars
of his work—the results obtained, as well as how these results were arrived at. The
calculations should be done on scrap-paper, and should not be entered, although, of course,
detail enough must be shown to enable the results to be recalculated.
Example of Page of Laboratory Book.
____________________________________________________________
Purple Ore 5 grams
19/10/89 0.0042 grm.
0.0021 "
———
In the United States, as a sort of compromise between the avoirdupois and metric systems, a
ton is taken as 2000 lbs. There, too, the custom is adopted of reporting the gold and silver
contents of an ore as so many dollars and cents to the ton. In the case of gold, an ounce is
considered to be worth 20.6718 dollars. With silver, the nominal value is 1.2929 dollars per
ounce, but frequently in assay reports it is taken as one dollar. The practice is objectionable.
The prices of metals vary with the fluctuations of the market, and if the assayer fixed the
price, the date of his report would be all important; if, on the other hand, he takes a fixed
price which does not at all times agree with the market one, it leaves a path open for the
deception of those unacquainted with the custom. American "dollars on the ton of 2000 lbs."
may be converted into "ounces in the ton of 2240 lbs." by dividing by 1.1544 in the case of
silver, and by 18.457 in the case of gold.
Laboratory Books and Report Forms.—The record which the assayer makes of his work
must be clear and neat, so that reference, even after an interval of years, should be certain
and easy. One method should be adopted and adhered to. Where there are a large number of
samples, three books are required.
Sample Book.—This contains particulars of the samples (marks, &c.), which are entered by
the office-clerk as they arrive. He at the same time puts on each sample the distinguishing
number.
Example of Page of Sample Book.
Date. Number. Sample. Remarks.
Feb. 1482 Tough Copper For Arsenic.
" 2X Piece of Metal For Ni and Cu.
" 483 Tough Copper.
" 73 Silver Precipitate, 4 casks, 24 cwt. 1 qr. With Letter.
" 494 Purple Ore, 200 tons.
" 1 J.T. Lead Ore, 1 J.T. From Corsica.
" 2 J.T. " 2 J.T.
Laboratory Book. This is the Assayer's note-book, in which he enters clearly the particulars
of his work—the results obtained, as well as how these results were arrived at. The
calculations should be done on scrap-paper, and should not be entered, although, of course,
detail enough must be shown to enable the results to be recalculated.
Example of Page of Laboratory Book.
____________________________________________________________
Purple Ore 5 grams
19/10/89 0.0042 grm.
0.0021 "
———
Page 29
Colorimetric 0.0063 × 20 = 0.13% Copper
______________________________________________________________
482
Tough Copper 10 grams
Feb. 1/89 10.5 c.c. Uranium.
= 0.52% Arsenic
______________________________________________________________
2082
Tough Copper 10 grams
12.7 c.c. Uranium.
= 0.63% Arsenic
______________________________________________________________
491 10 grams
Tough Copper 13.7 c.c. Uranium
Feb. 1/89
= 0.68% Arsenic
______________________________________________________________
Standard of Uranium acetate.
0.150 gram As2O3 = 23.3 c.c. Uranium.
∴ 100 cc. Uranium = 0.5 gram As.
______________________________________________________________
10071 5 grams
Tin Ore Cruc. and SnO2 9.6065 grms.
Feb. 3/89 Cruc. and Ash 9.4235 "
———
SnO2 = 0.1830 = 2.88% Tin
______________________________________________________________
The Assay Book.—This is the Official book, and is a combination of the Sample and
Laboratory books. It corresponds with the report-forms. Without being loaded with detail, it
should contain sufficient to characterise each sample.
Example of Page of Assay Book.
Description of Sample.
Water Lost Assay on the Date
Date. Material. Weight. No.
at 100° C. Dry Material. Reported.
1889 ton cwt qrs lbs
Feb. Tough cake
... ... ... ... 482 ... Arsenic, 0.52% 7
1 copper
Tough cake
" ... ... ... ... 2082 ... Arsenic, 0.63% 7
copper
Tough cake
" ... ... ... ... 491 ... Arsenic, 0.68% 7
copper
Feb. Nickel disc for
... ... ... ... X ... Copper, 73.75 7
2 C.R.
______________________________________________________________
482
Tough Copper 10 grams
Feb. 1/89 10.5 c.c. Uranium.
= 0.52% Arsenic
______________________________________________________________
2082
Tough Copper 10 grams
12.7 c.c. Uranium.
= 0.63% Arsenic
______________________________________________________________
491 10 grams
Tough Copper 13.7 c.c. Uranium
Feb. 1/89
= 0.68% Arsenic
______________________________________________________________
Standard of Uranium acetate.
0.150 gram As2O3 = 23.3 c.c. Uranium.
∴ 100 cc. Uranium = 0.5 gram As.
______________________________________________________________
10071 5 grams
Tin Ore Cruc. and SnO2 9.6065 grms.
Feb. 3/89 Cruc. and Ash 9.4235 "
———
SnO2 = 0.1830 = 2.88% Tin
______________________________________________________________
The Assay Book.—This is the Official book, and is a combination of the Sample and
Laboratory books. It corresponds with the report-forms. Without being loaded with detail, it
should contain sufficient to characterise each sample.
Example of Page of Assay Book.
Description of Sample.
Water Lost Assay on the Date
Date. Material. Weight. No.
at 100° C. Dry Material. Reported.
1889 ton cwt qrs lbs
Feb. Tough cake
... ... ... ... 482 ... Arsenic, 0.52% 7
1 copper
Tough cake
" ... ... ... ... 2082 ... Arsenic, 0.63% 7
copper
Tough cake
" ... ... ... ... 491 ... Arsenic, 0.68% 7
copper
Feb. Nickel disc for
... ... ... ... X ... Copper, 73.75 7
2 C.R.
Page 30
Nickel, 24.34
Iron, 2.18
———
100.27
———
Silver
" precipitate, 4 ... 24 1 0 73 Not det. Silver, 4.851 10
casks
Gold, 0.0215 ...
Lead, 19.37 ...
Zinc, 2.00 ...
Silver, 1584.7
...
ozs. per ton
Gold, 7.0 ozs.
...
per ton
Copper,
" Purple ore ... 200... ... ... 494 Not det. 11
0.13%
Sulphur
...
0.15%
When the number of samples is small, the Sample Book may be omitted, and the entries
made in the Assay Book as the samples arrive.
Report-forms. These should entail as little writing as possible in making out the report. For
general purposes the form given on p. 12 is useful.
The quantity of substance to be taken for any particular assay depends largely upon the
method of assay adopted. There are, however, some general considerations which should be
remembered, and some devices for simplifying the calculations which should be discussed.
The smaller the percentage of the substance to be determined, the larger should be the
amount of the ore taken. The following table will give a general idea as to this:—
Percentage of the substance to be determined. Amount of ore, &c. to be weighed.
100-10 1 gram.
10-5 2 grams.
5-1 5 "
1-0.1 10 "
0.1-0.01 20 "
Iron, 2.18
———
100.27
———
Silver
" precipitate, 4 ... 24 1 0 73 Not det. Silver, 4.851 10
casks
Gold, 0.0215 ...
Lead, 19.37 ...
Zinc, 2.00 ...
Silver, 1584.7
...
ozs. per ton
Gold, 7.0 ozs.
...
per ton
Copper,
" Purple ore ... 200... ... ... 494 Not det. 11
0.13%
Sulphur
...
0.15%
When the number of samples is small, the Sample Book may be omitted, and the entries
made in the Assay Book as the samples arrive.
Report-forms. These should entail as little writing as possible in making out the report. For
general purposes the form given on p. 12 is useful.
The quantity of substance to be taken for any particular assay depends largely upon the
method of assay adopted. There are, however, some general considerations which should be
remembered, and some devices for simplifying the calculations which should be discussed.
The smaller the percentage of the substance to be determined, the larger should be the
amount of the ore taken. The following table will give a general idea as to this:—
Percentage of the substance to be determined. Amount of ore, &c. to be weighed.
100-10 1 gram.
10-5 2 grams.
5-1 5 "
1-0.1 10 "
0.1-0.01 20 "
Page 31
ASSAY NOTE
The rougher the method of assay adopted, the larger should be the quantity of ore taken. If
the degree of accuracy attainable with the methods and instruments at the assayer's service
is known, it is easy to calculate what quantity should be taken for any particular case. If the
results are good within 0.001 gram, then, taking 1 gram of ore we can report within 0.1 per
cent., or if they are good within 0.0002 gram, taking 20 grams of ore, we can report within 1
part per 100,000, or very closely within 6-1/2 dwt. to the ton. If it is wished to be yet more
particular in reporting, larger quantities must be taken. The difficulty of manipulating very
small or very large precipitates, &c., must be borne in mind. So, too, must the fact that the
greater the weight of the final product of an assay, the less, as a rule, is the percentage error.
The distinction between absolute and percentage error, often overlooked, is important. If 0.5
gram of silver be cupelled with 20 grams of lead, there may be obtained a button of 0.495
gram; the absolute loss is 0.005 gram, and this equals 1 per cent. of the silver present.
Similarly, cupelling 0.1 gram, the resulting button may be 0.098; the absolute loss is only
0.002 gram, but this equals 2 per cent. of the silver present. In the same way the student
should see that the two results, 91.5 per cent. and 92.0 per cent., are really more concordant
than the results 9.1 per cent. and 9.2 per cent.
A device often adopted in practice where a large number of assays of one kind are made,
and the report is given as so many ounces or pounds to the ton, is that known as the assay
ton. The assay ton may be any arbitrary and convenient weight, but its subdivisions must
bear to it the same relations as pounds and ounces bear to the actual ton. On the other hand,
in a laboratory where many kinds of work are performed, different sets of weights of this
kind would only tend to confusion, even if they were not unnecessary. With a set of gram
weights and its subdivisions anything may be done. If it is desired to report as pounds to the
ton, then, since there are 2240 lbs. to the ton, a weight of 2.240 grams may be taken as the
assay ton, and each 0.001 gram yielded will equal 1 lb., or 22.4 grams may represent the
ton, and each 0.01 gram a pound. Similarly, since there are 32,666.6 ozs. troy to the ton; if
we take 32.6667 grams as the assay ton, each 0.001 gram will equal 1 oz. to the ton. In
some cases it may be convenient to have, in addition to the usual gram weights, one or other
of the "assay tons" mentioned above, but generally it is better to work on a purely decimal
The rougher the method of assay adopted, the larger should be the quantity of ore taken. If
the degree of accuracy attainable with the methods and instruments at the assayer's service
is known, it is easy to calculate what quantity should be taken for any particular case. If the
results are good within 0.001 gram, then, taking 1 gram of ore we can report within 0.1 per
cent., or if they are good within 0.0002 gram, taking 20 grams of ore, we can report within 1
part per 100,000, or very closely within 6-1/2 dwt. to the ton. If it is wished to be yet more
particular in reporting, larger quantities must be taken. The difficulty of manipulating very
small or very large precipitates, &c., must be borne in mind. So, too, must the fact that the
greater the weight of the final product of an assay, the less, as a rule, is the percentage error.
The distinction between absolute and percentage error, often overlooked, is important. If 0.5
gram of silver be cupelled with 20 grams of lead, there may be obtained a button of 0.495
gram; the absolute loss is 0.005 gram, and this equals 1 per cent. of the silver present.
Similarly, cupelling 0.1 gram, the resulting button may be 0.098; the absolute loss is only
0.002 gram, but this equals 2 per cent. of the silver present. In the same way the student
should see that the two results, 91.5 per cent. and 92.0 per cent., are really more concordant
than the results 9.1 per cent. and 9.2 per cent.
A device often adopted in practice where a large number of assays of one kind are made,
and the report is given as so many ounces or pounds to the ton, is that known as the assay
ton. The assay ton may be any arbitrary and convenient weight, but its subdivisions must
bear to it the same relations as pounds and ounces bear to the actual ton. On the other hand,
in a laboratory where many kinds of work are performed, different sets of weights of this
kind would only tend to confusion, even if they were not unnecessary. With a set of gram
weights and its subdivisions anything may be done. If it is desired to report as pounds to the
ton, then, since there are 2240 lbs. to the ton, a weight of 2.240 grams may be taken as the
assay ton, and each 0.001 gram yielded will equal 1 lb., or 22.4 grams may represent the
ton, and each 0.01 gram a pound. Similarly, since there are 32,666.6 ozs. troy to the ton; if
we take 32.6667 grams as the assay ton, each 0.001 gram will equal 1 oz. to the ton. In
some cases it may be convenient to have, in addition to the usual gram weights, one or other
of the "assay tons" mentioned above, but generally it is better to work on a purely decimal
Page 32
system, and convert when required into ounces per ton, &c., either by actual calculation or
by reference to a set of tables.
Practical Exercises.
The student should practise such calculations as the following:—
1. Calculate the percentages in the following cases:—
(a) Ore taken, 2 grams; copper found, 0.2155.
(b) " 1.5 gram; iron found, 0.8340.
(c) " 30 grams; lead found, 23.2.
2. Calculate the parts per thousand in the following:—
(a) Bullion taken, 1.1 gram; silver found, 1.017.
(b) " 1.14 gram; silver found, 1.026.
(c) " 0.6 gram; gold found, 0.5500.
3. Calculate parts per 100,000 in the following:—
(a) Ore taken, 20 grams; silver found, 0.0075.
(b) " 50 grams; gold found, 0.0026.
(c) Water taken, 500 c.c.; solids found, 0.1205.
4. Calculate cwts. to the ton in the following:—
(a) Ore taken, 5 grams; tin found, 2.816.
(b) " 5 grams; tin found, 3.128.
(c) An ore with 68.2 per cent. of tin.
5. Calculate lbs. to the ton in the following:—
(a) An ore with 3.28 per cent. oxide of tin.
(b) Ore taken, 20 grams; oxide of tin found, 1.67.
6. Calculate ozs. (troy) to the ton in the following:—
(a) Ore taken, 50 grams; gold found, 0.0035.
(b) " 20 grams; silver found, 0.0287.
(c) " 25 grains; silver found, 0.0164.
7. Calculate in grains per gallon:—
(a) 0.51 gram per litre.
(b) 24.6 parts per 100,000.
(c) Solution taken, 100 c.c.; copper found, 0.0045 gram.
(d) " 50 c.c.; iron found, 0.165 gram.
8. Convert into ozs. (troy) per ton:—
(a) 7 loths per centner.
(b) 30 grams per quintal.
(c) 15 parts per 100,000.
by reference to a set of tables.
Practical Exercises.
The student should practise such calculations as the following:—
1. Calculate the percentages in the following cases:—
(a) Ore taken, 2 grams; copper found, 0.2155.
(b) " 1.5 gram; iron found, 0.8340.
(c) " 30 grams; lead found, 23.2.
2. Calculate the parts per thousand in the following:—
(a) Bullion taken, 1.1 gram; silver found, 1.017.
(b) " 1.14 gram; silver found, 1.026.
(c) " 0.6 gram; gold found, 0.5500.
3. Calculate parts per 100,000 in the following:—
(a) Ore taken, 20 grams; silver found, 0.0075.
(b) " 50 grams; gold found, 0.0026.
(c) Water taken, 500 c.c.; solids found, 0.1205.
4. Calculate cwts. to the ton in the following:—
(a) Ore taken, 5 grams; tin found, 2.816.
(b) " 5 grams; tin found, 3.128.
(c) An ore with 68.2 per cent. of tin.
5. Calculate lbs. to the ton in the following:—
(a) An ore with 3.28 per cent. oxide of tin.
(b) Ore taken, 20 grams; oxide of tin found, 1.67.
6. Calculate ozs. (troy) to the ton in the following:—
(a) Ore taken, 50 grams; gold found, 0.0035.
(b) " 20 grams; silver found, 0.0287.
(c) " 25 grains; silver found, 0.0164.
7. Calculate in grains per gallon:—
(a) 0.51 gram per litre.
(b) 24.6 parts per 100,000.
(c) Solution taken, 100 c.c.; copper found, 0.0045 gram.
(d) " 50 c.c.; iron found, 0.165 gram.
8. Convert into ozs. (troy) per ton:—
(a) 7 loths per centner.
(b) 30 grams per quintal.
(c) 15 parts per 100,000.
Page 33
FOOTNOTES:
[1] Ether or carbon bisulphide.
[2] Such substances are best dried by pressing between folds of dry filter-paper.
[1] Ether or carbon bisulphide.
[2] Such substances are best dried by pressing between folds of dry filter-paper.
Page 34
CHAPTER II.
METHODS OF ASSAYING.—DRY GRAVIMETRIC METHODS.
The methods of assaying are best classed under two heads, Gravimetric and Volumetric, in
the former of which the final results are weighed, whilst in the latter they are measured. A
commoner and older division is expressed in the terms much used in practice—wet assays
and dry assays. Wet assays include all those in which solvents, &c. (liquid at the ordinary
temperature), are mainly used; and dry assays, those in which solid re-agents are almost
exclusively employed. Dry assays form a branch of gravimetric work, and we shall include
under this head all those assays requiring the help of a wind furnace. Wet assays, as
generally understood, would include not only those which we class as wet gravimetric
assays, but also all the volumetric processes.
Gravimetric Methods aim at the separation of the substance from the other matters present
in the ore, so that it may be weighed; and, therefore, they must yield the whole of the
substance in a pure state. It is not necessary that a metal should be weighed as metal; it may
be weighed in the form of a compound of definite and well known composition. For
example, one part by weight of silver chloride contains (and, if pure, always contains)
0.7527 part of silver; and a quantity of this metal can be as exactly determined by weighing
it as chloride as by weighing it in the metallic state. But in either case the metal or its
chloride must be pure.
Exact purity and complete separation are not easily obtained; and methods are used which
are defective in one or both of these respects. It is well to note that an impure product
increases the result, whilst a loss of the substance decreases it; so that if both defects exist in
a process they tend to neutralise each other. Of dry methods generally, it may be said that
they neither give the whole of the substance nor give it pure; so that they are only calculated
to show the amount of metal that can be extracted on a manufacturing scale, and not the
actual quantity of it present. Their determinations are generally rough and always low. The
gold and silver determinations, however, will compare very favourably with any of the other
processes for the estimation of these metals in their ores.
The calculation of the results of a gravimetric assay has already been referred to. If the
result is to be stated as percentage, it may always be done by the following rule:—Multiply
the weight of the substance got by the percentage of metal it contains, and divide by the
weight of ore taken.
Gravimetric methods are divided into three groups: (1) mechanical separations; (2) dry
methods; and (3) wet methods.
Mechanical Separations.—Under this head are classed the method of assaying tin ores,
known as vanning, and the amalgamation assay for gold. A set of sieves to determine the
METHODS OF ASSAYING.—DRY GRAVIMETRIC METHODS.
The methods of assaying are best classed under two heads, Gravimetric and Volumetric, in
the former of which the final results are weighed, whilst in the latter they are measured. A
commoner and older division is expressed in the terms much used in practice—wet assays
and dry assays. Wet assays include all those in which solvents, &c. (liquid at the ordinary
temperature), are mainly used; and dry assays, those in which solid re-agents are almost
exclusively employed. Dry assays form a branch of gravimetric work, and we shall include
under this head all those assays requiring the help of a wind furnace. Wet assays, as
generally understood, would include not only those which we class as wet gravimetric
assays, but also all the volumetric processes.
Gravimetric Methods aim at the separation of the substance from the other matters present
in the ore, so that it may be weighed; and, therefore, they must yield the whole of the
substance in a pure state. It is not necessary that a metal should be weighed as metal; it may
be weighed in the form of a compound of definite and well known composition. For
example, one part by weight of silver chloride contains (and, if pure, always contains)
0.7527 part of silver; and a quantity of this metal can be as exactly determined by weighing
it as chloride as by weighing it in the metallic state. But in either case the metal or its
chloride must be pure.
Exact purity and complete separation are not easily obtained; and methods are used which
are defective in one or both of these respects. It is well to note that an impure product
increases the result, whilst a loss of the substance decreases it; so that if both defects exist in
a process they tend to neutralise each other. Of dry methods generally, it may be said that
they neither give the whole of the substance nor give it pure; so that they are only calculated
to show the amount of metal that can be extracted on a manufacturing scale, and not the
actual quantity of it present. Their determinations are generally rough and always low. The
gold and silver determinations, however, will compare very favourably with any of the other
processes for the estimation of these metals in their ores.
The calculation of the results of a gravimetric assay has already been referred to. If the
result is to be stated as percentage, it may always be done by the following rule:—Multiply
the weight of the substance got by the percentage of metal it contains, and divide by the
weight of ore taken.
Gravimetric methods are divided into three groups: (1) mechanical separations; (2) dry
methods; and (3) wet methods.
Mechanical Separations.—Under this head are classed the method of assaying tin ores,
known as vanning, and the amalgamation assay for gold. A set of sieves to determine the
Page 35
relative proportion of powders of different degrees of fineness is sometimes useful. A set
with 10, 20, 40 and 80 meshes to the inch is convenient.
Dry Assays.—An important distinction between wet and dry methods of assaying is, that in
the former the substance is got into the liquid state by solution, whilst in the latter fusion is
taken advantage of.
The difference between solution and fusion is easily illustrated: a lump of sugar heated over
a candle-flame melts or fuses; suspended in water it dissolves. Many substances which are
insoluble or infusible of themselves, become soluble or fusible when mixed with certain
others; thus, in this way, solution is got with the aid of reagents, and fusion with the help of
fluxes. For example, lead is insoluble in water, but if nitric acid be added, the metal rapidly
disappears. It is convenient, but somewhat inaccurate, to say that the acid dissolves the lead.
If the lead be acted on by nitric acid alone, without water, it is converted into a white
powder, which does not dissolve until water is added; in this case it is obvious that the water
is the solvent. The function of the acid is to convert the lead into a soluble compound.
Fluxes may act as true solvents. Fused carbonate of soda dissolves baric carbonate, and
perhaps in many slags true solution occurs; but in the great majority of cases a flux is a
solid reagent added for the purpose of forming a fusible compound with the earthy or stony
minerals of the ore. Few of the minerals which occur in the gangue of an ore are fusible;
and still fewer are sufficiently fusible for the purposes of the assayer, consequently the
subject is one of importance, and it ought to be treated on chemical principles. An idea of
the composition of some of the more frequently occurring rocks may be gathered from the
following table, which represents rough averages:—
Oxide of Lime and
Silica. Alumina. Alkalies.
iron Magnesia.
% % % % %
80-
Sandstone, grit, quartzite, &c. — — — —
100
Granite, gneiss, quartz- 5-8 Less in
70-75 13-20 2 2
porphyry, fire-clay, &c. fire-clay.
Mica-schist 65 18 5 3 3
Trachyte, syenite 60 17 7 4-7 6-9
Clay-slate 60 18 10 8 3
Diorite 54 17 12 9 3-4
Horneblende-rock 50 18 15 12 3-4
Brick-clay 50 34 8 6 —
China-clay 47 39 — — —
Basalt, dolerite, &c. 50 15 15 16 3
Serpentine 44 — — 44 —
Chalk, limestone, dolomite, &c. — — — 45-55 —
with 10, 20, 40 and 80 meshes to the inch is convenient.
Dry Assays.—An important distinction between wet and dry methods of assaying is, that in
the former the substance is got into the liquid state by solution, whilst in the latter fusion is
taken advantage of.
The difference between solution and fusion is easily illustrated: a lump of sugar heated over
a candle-flame melts or fuses; suspended in water it dissolves. Many substances which are
insoluble or infusible of themselves, become soluble or fusible when mixed with certain
others; thus, in this way, solution is got with the aid of reagents, and fusion with the help of
fluxes. For example, lead is insoluble in water, but if nitric acid be added, the metal rapidly
disappears. It is convenient, but somewhat inaccurate, to say that the acid dissolves the lead.
If the lead be acted on by nitric acid alone, without water, it is converted into a white
powder, which does not dissolve until water is added; in this case it is obvious that the water
is the solvent. The function of the acid is to convert the lead into a soluble compound.
Fluxes may act as true solvents. Fused carbonate of soda dissolves baric carbonate, and
perhaps in many slags true solution occurs; but in the great majority of cases a flux is a
solid reagent added for the purpose of forming a fusible compound with the earthy or stony
minerals of the ore. Few of the minerals which occur in the gangue of an ore are fusible;
and still fewer are sufficiently fusible for the purposes of the assayer, consequently the
subject is one of importance, and it ought to be treated on chemical principles. An idea of
the composition of some of the more frequently occurring rocks may be gathered from the
following table, which represents rough averages:—
Oxide of Lime and
Silica. Alumina. Alkalies.
iron Magnesia.
% % % % %
80-
Sandstone, grit, quartzite, &c. — — — —
100
Granite, gneiss, quartz- 5-8 Less in
70-75 13-20 2 2
porphyry, fire-clay, &c. fire-clay.
Mica-schist 65 18 5 3 3
Trachyte, syenite 60 17 7 4-7 6-9
Clay-slate 60 18 10 8 3
Diorite 54 17 12 9 3-4
Horneblende-rock 50 18 15 12 3-4
Brick-clay 50 34 8 6 —
China-clay 47 39 — — —
Basalt, dolerite, &c. 50 15 15 16 3
Serpentine 44 — — 44 —
Chalk, limestone, dolomite, &c. — — — 45-55 —
Page 36
Silica itself, and the silicates of alumina, of lime, and of magnesia, are practically infusible;
the silicates of soda, of potash, and of iron are easily fusible if the base (soda, potash, or
oxide of iron) be present in sufficient quantity, and if, in the case of the iron, it is present
mainly as lower oxide (ferrous silicate). The addition of lime, oxide of iron, or alkali to
silicate of alumina results in the formation of a double silicate of alumina and lime, or of
alumina and iron, &c., all of which are easily fusible. Similarly, if to a silicate of lime we
add oxide of iron, or soda, or even alumina, a fusible double silicate will be formed. Thus
lime, soda, oxide of iron, and clay, are fluxes when properly used; but since lime, clay (and
oxide of iron if there be any tendency to form peroxide), are of themselves infusible, any
excess of these fluxes would tend to stiffen and render pasty the resulting slag. So, too,
soda, which is a very strong base, may act prejudicially if it be in sufficient excess to set
free notable quantities of lime and magnesia, which but for that excess would exist in
combination as complex fusible silicates. There are many minerals which with but little
soda form a glass, but with more yield a lumpy scoriacious mass. There are many minerals,
too, which are already basic (for example, calcite), and which, when present, demand either
a less basic or an acid flux according to the proportions in which they exist. For purposes of
this kind borax, or glass, or clay with more or less soda may be used, and of these borax is
by far the most generally useful. An objection to too basic a slag (and a very important one)
is the speed with which it corrodes ordinary crucibles. These crucibles, consisting of quartz
and clay, are rapidly attacked by lime, soda and bases generally.
In considering what is and what is not a good slag, certain chemical properties are of
importance. If a mixture of many substances be fused and allowed to solidify in a crucible,
there will be found some or all of the following. At the bottom of the crucible (fig. 4) a
button of metal, resting on this a speise; then a regulus, next a slag made up of silicates and
borates and metallic oxides, and lastly, on the top another layer of slag, mainly made up of
fusible chlorides and sulphates. In assaying operations the object is generally to concentrate
the metal sought for in a button of metal, speise or regulus, and to leave the earthy and other
impurities as far as possible in the slag; whether there be one or two layers of slag is a
matter of indifference;[3] but the chemical action of the lower layer upon the speise, or
regulus, or metal, is of great importance.
the silicates of soda, of potash, and of iron are easily fusible if the base (soda, potash, or
oxide of iron) be present in sufficient quantity, and if, in the case of the iron, it is present
mainly as lower oxide (ferrous silicate). The addition of lime, oxide of iron, or alkali to
silicate of alumina results in the formation of a double silicate of alumina and lime, or of
alumina and iron, &c., all of which are easily fusible. Similarly, if to a silicate of lime we
add oxide of iron, or soda, or even alumina, a fusible double silicate will be formed. Thus
lime, soda, oxide of iron, and clay, are fluxes when properly used; but since lime, clay (and
oxide of iron if there be any tendency to form peroxide), are of themselves infusible, any
excess of these fluxes would tend to stiffen and render pasty the resulting slag. So, too,
soda, which is a very strong base, may act prejudicially if it be in sufficient excess to set
free notable quantities of lime and magnesia, which but for that excess would exist in
combination as complex fusible silicates. There are many minerals which with but little
soda form a glass, but with more yield a lumpy scoriacious mass. There are many minerals,
too, which are already basic (for example, calcite), and which, when present, demand either
a less basic or an acid flux according to the proportions in which they exist. For purposes of
this kind borax, or glass, or clay with more or less soda may be used, and of these borax is
by far the most generally useful. An objection to too basic a slag (and a very important one)
is the speed with which it corrodes ordinary crucibles. These crucibles, consisting of quartz
and clay, are rapidly attacked by lime, soda and bases generally.
In considering what is and what is not a good slag, certain chemical properties are of
importance. If a mixture of many substances be fused and allowed to solidify in a crucible,
there will be found some or all of the following. At the bottom of the crucible (fig. 4) a
button of metal, resting on this a speise; then a regulus, next a slag made up of silicates and
borates and metallic oxides, and lastly, on the top another layer of slag, mainly made up of
fusible chlorides and sulphates. In assaying operations the object is generally to concentrate
the metal sought for in a button of metal, speise or regulus, and to leave the earthy and other
impurities as far as possible in the slag; whether there be one or two layers of slag is a
matter of indifference;[3] but the chemical action of the lower layer upon the speise, or
regulus, or metal, is of great importance.
Page 37
A regulus is a compound of one or more of the metals with sulphur; it is usually brittle,
often crystalline, and of a dull somewhat greasy lustre. It is essential that the slag, when
solid, shall be so much more brittle than the regulus, that it shall be easy to crumble, and
remove it without breaking the latter; and it must not be basic. The effect of fusing a regulus
with a basic slag is well seen when sulphide of lead is fused with carbonate of soda; the
result is a button of metal (more or less pure), and a slag containing sulphides of lead and
sodium; and again, if sulphide of lead be fused with an excess of oxide of lead, a button of
lead will be got, and a slag which is simply oxide of lead (with whatever it may have taken
up from the crucible), or if a sufficient excess has not been used, oxide of lead mixed with
some sulphide. When (as is most frequently the case) the desire is to prevent the formation
of regulus, these reactions may be taken advantage of, but otherwise the use of a flux
having any such tendency must be avoided. A good slag (from which a regulus may be
easily separated) may be obtained by fusing, say, 20 grams of ore with borax 15 grams,
powdered glass 15 grams, fluor spar, 20 grams, and lime 20 grams; by quenching the slag in
water as soon as it has solidified, it is rendered very brittle.
Sulphide of iron formed during an assay will remain diffused through the slag, instead of
fusing into a button of regulus, if the slag contain sulphide of sodium. The same is true of
other sulphides if not present in too great a quantity, and if the temperature is not too high.
Speises are compounds of a metal or metals with arsenic. They are chiefly of interest in the
metallurgy of nickel, cobalt, and tin. They are formed by heating the metal or ore in covered
crucibles with arsenic and, if necessary, a reducing agent. The product is fused with more
arsenic under a slag, consisting mainly of borax. They are very fusible, brittle compounds.
On exposure to the air at a red heat the arsenic and the metal simultaneously oxidize. When
iron, cobalt, nickel, and copper are present in the same speise, they are eliminated in the
order mentioned.
Slags from which metals are to be separated should not be too acid; at least, in those cases
in which the metal is to be reduced from a compound, as well as separated from earthy
impurities. Where the object is simply to get a button of metal from a substance in which it
is already in the metallic state, but mixed with dross (made up of metallic oxides, such as
those of zinc or iron), from which it is desired to separate it, an acid flux like borax is best;
or, if the metal is easily fusible, and there would be danger of loss of metal by oxidation or
volatilising, it may be melted under a layer of resin or fat. Common salt is sometimes used
with a similar object, and is often useful. Under certain conditions, however, it has a
tendency to cause the formation of volatile chlorides with a consequent loss of metal.
In the great majority of cases, the fusion of the metal is accompanied by reduction from the
state of oxide; in these the slag should be basic. It is not easy to reduce the whole of a
reducible oxide (say oxide of copper or of iron) from a slag in which it exists as a borate or
silicate; there should be at least enough soda present to liberate it. When the object is to
separate one metal, say copper, without reducing an unnecessary amount of another (iron) at
the same time, a slag with a good deal of borax is a distinct advantage. The slag then will
probably not be free from copper, so that it will be necessary to powder and mix the slag
with some soda and a reducing agent, and to again fuse the slag in order to separate this
often crystalline, and of a dull somewhat greasy lustre. It is essential that the slag, when
solid, shall be so much more brittle than the regulus, that it shall be easy to crumble, and
remove it without breaking the latter; and it must not be basic. The effect of fusing a regulus
with a basic slag is well seen when sulphide of lead is fused with carbonate of soda; the
result is a button of metal (more or less pure), and a slag containing sulphides of lead and
sodium; and again, if sulphide of lead be fused with an excess of oxide of lead, a button of
lead will be got, and a slag which is simply oxide of lead (with whatever it may have taken
up from the crucible), or if a sufficient excess has not been used, oxide of lead mixed with
some sulphide. When (as is most frequently the case) the desire is to prevent the formation
of regulus, these reactions may be taken advantage of, but otherwise the use of a flux
having any such tendency must be avoided. A good slag (from which a regulus may be
easily separated) may be obtained by fusing, say, 20 grams of ore with borax 15 grams,
powdered glass 15 grams, fluor spar, 20 grams, and lime 20 grams; by quenching the slag in
water as soon as it has solidified, it is rendered very brittle.
Sulphide of iron formed during an assay will remain diffused through the slag, instead of
fusing into a button of regulus, if the slag contain sulphide of sodium. The same is true of
other sulphides if not present in too great a quantity, and if the temperature is not too high.
Speises are compounds of a metal or metals with arsenic. They are chiefly of interest in the
metallurgy of nickel, cobalt, and tin. They are formed by heating the metal or ore in covered
crucibles with arsenic and, if necessary, a reducing agent. The product is fused with more
arsenic under a slag, consisting mainly of borax. They are very fusible, brittle compounds.
On exposure to the air at a red heat the arsenic and the metal simultaneously oxidize. When
iron, cobalt, nickel, and copper are present in the same speise, they are eliminated in the
order mentioned.
Slags from which metals are to be separated should not be too acid; at least, in those cases
in which the metal is to be reduced from a compound, as well as separated from earthy
impurities. Where the object is simply to get a button of metal from a substance in which it
is already in the metallic state, but mixed with dross (made up of metallic oxides, such as
those of zinc or iron), from which it is desired to separate it, an acid flux like borax is best;
or, if the metal is easily fusible, and there would be danger of loss of metal by oxidation or
volatilising, it may be melted under a layer of resin or fat. Common salt is sometimes used
with a similar object, and is often useful. Under certain conditions, however, it has a
tendency to cause the formation of volatile chlorides with a consequent loss of metal.
In the great majority of cases, the fusion of the metal is accompanied by reduction from the
state of oxide; in these the slag should be basic. It is not easy to reduce the whole of a
reducible oxide (say oxide of copper or of iron) from a slag in which it exists as a borate or
silicate; there should be at least enough soda present to liberate it. When the object is to
separate one metal, say copper, without reducing an unnecessary amount of another (iron) at
the same time, a slag with a good deal of borax is a distinct advantage. The slag then will
probably not be free from copper, so that it will be necessary to powder and mix the slag
with some soda and a reducing agent, and to again fuse the slag in order to separate this
Page 38
residual metal. In all those cases in which the slag retains an oxide of a heavy metal, this
cleaning of the slag is advisable, and in the case of rich ores necessary. Slags containing
sulphides are especially apt to retain the more easily reducible metals.
The following are the ordinary and most useful fluxes:—
Soda.—The powdered bicarbonate, sold by druggists as "carbonate of soda," is generally
used. It gives off its water and excess of carbonic acid readily and without fusion. Where
the melting down is performed rapidly, the escaping gas is apt to cause trouble by frothing,
and so causing waste of the material. Ordinary carbonate of soda, when hydrated (soda
crystals), melts easily, and gives off its water with ebullition. It is unfit for use in assaying,
but when dried it can be used instead of the bicarbonate. One part of the dried carbonate is
equivalent to rather more than one and a half parts of the bicarbonate. From two to four
parts of the flux are amply sufficient to yield a fluid slag with one part of earthy matter. This
statement is also true of the fluxes which follow.
Borax is a hydrated biborate of soda, containing nearly half its weight of water. When
heated it swells up, loses its water, and fuses into a glass. The swelling up may become a
source of loss in the assay by pushing some of the contents out of the crucible. To avoid
this, fused or dried borax may be used, in which case a little more than half the amount of
borax indicated will suffice. Borax will flux almost anything, but it is especially valuable in
fluxing lime, &c., and metallic oxides; as also in those cases in which it is desired to keep
certain of the latter in the slag and out of the button of metal.
Oxide of Lead, in the form of red lead or litharge, is a valuable flux; it easily dissolves
those metallic oxides which are either infusible or difficultly fusible of themselves, such as
oxides of iron or copper. The resulting slag is strongly basic and very corrosive; no crucible
will long withstand the attack of a fused mixture of oxides of lead and copper. With
silicates, also, it forms very fusible double silicates; but in the absence of silicates and
borates it has no action upon lime or magnesia. Whether the lead be added as litharge or as
red lead, it will exist in the slag as monoxide (litharge); the excess of oxygen of the red lead
is thus available for oxidising purposes. If this oxidising power is prejudicial, it may be
neutralised by mixing the red lead with 1 per cent. of charcoal.
Glass: broken beakers and flasks, cleaned, dried, and powdered will do. It should be free
from lead.
Fluor: fluor-spar as free as possible from other minerals, powdered. It helps to flux
phosphate of lime, &c., and infusible silicates.
Lime: should be fresh and powdered. It must not be slaked. Powdered white marble
(carbonate of lime) will do; but nearly double the quantity must be taken. One part of lime
produces the same effect as 1.8 parts of the carbonate of lime.
Tartar and "black flux," are reducing agents as well as fluxes. The "black flux," which may
be obtained by heating tartar, is a mixture of carbonate of potash and charcoal.
cleaning of the slag is advisable, and in the case of rich ores necessary. Slags containing
sulphides are especially apt to retain the more easily reducible metals.
The following are the ordinary and most useful fluxes:—
Soda.—The powdered bicarbonate, sold by druggists as "carbonate of soda," is generally
used. It gives off its water and excess of carbonic acid readily and without fusion. Where
the melting down is performed rapidly, the escaping gas is apt to cause trouble by frothing,
and so causing waste of the material. Ordinary carbonate of soda, when hydrated (soda
crystals), melts easily, and gives off its water with ebullition. It is unfit for use in assaying,
but when dried it can be used instead of the bicarbonate. One part of the dried carbonate is
equivalent to rather more than one and a half parts of the bicarbonate. From two to four
parts of the flux are amply sufficient to yield a fluid slag with one part of earthy matter. This
statement is also true of the fluxes which follow.
Borax is a hydrated biborate of soda, containing nearly half its weight of water. When
heated it swells up, loses its water, and fuses into a glass. The swelling up may become a
source of loss in the assay by pushing some of the contents out of the crucible. To avoid
this, fused or dried borax may be used, in which case a little more than half the amount of
borax indicated will suffice. Borax will flux almost anything, but it is especially valuable in
fluxing lime, &c., and metallic oxides; as also in those cases in which it is desired to keep
certain of the latter in the slag and out of the button of metal.
Oxide of Lead, in the form of red lead or litharge, is a valuable flux; it easily dissolves
those metallic oxides which are either infusible or difficultly fusible of themselves, such as
oxides of iron or copper. The resulting slag is strongly basic and very corrosive; no crucible
will long withstand the attack of a fused mixture of oxides of lead and copper. With
silicates, also, it forms very fusible double silicates; but in the absence of silicates and
borates it has no action upon lime or magnesia. Whether the lead be added as litharge or as
red lead, it will exist in the slag as monoxide (litharge); the excess of oxygen of the red lead
is thus available for oxidising purposes. If this oxidising power is prejudicial, it may be
neutralised by mixing the red lead with 1 per cent. of charcoal.
Glass: broken beakers and flasks, cleaned, dried, and powdered will do. It should be free
from lead.
Fluor: fluor-spar as free as possible from other minerals, powdered. It helps to flux
phosphate of lime, &c., and infusible silicates.
Lime: should be fresh and powdered. It must not be slaked. Powdered white marble
(carbonate of lime) will do; but nearly double the quantity must be taken. One part of lime
produces the same effect as 1.8 parts of the carbonate of lime.
Tartar and "black flux," are reducing agents as well as fluxes. The "black flux," which may
be obtained by heating tartar, is a mixture of carbonate of potash and charcoal.
Page 39
Reducing Agents.—The distinction between reducing agents and fluxes (too often ignored)
is an important one. Fluxes yield slags; reducing agents give buttons of regulus or of metal.
The action of a reducing agent is the separation of the oxygen or sulphur from the metal
with which it is combined. For example, the mineral anglesite (lead sulphate) is a
compound of lead, sulphur, and oxygen; by carefully heating it with charcoal the oxygen is
taken away by the charcoal, and a regulus of lead sulphide remains. If the regulus be then
fused with metallic iron the sulphur is removed by the iron, and metallic lead is left. The
charcoal and the iron are reducing agents. But in defining a reducing agent as one which
removes oxygen, or sulphur, from a metallic compound so as to set the metal free, it must
be remembered that sulphur itself will reduce metallic lead from fused litharge, and that
oxygen will similarly set free the metal in fused lead sulphide. There is no impropriety in
describing sulphur as a reducing agent; but it is absurd to call oxygen one. Some confusion
will be avoided if these substances and those which are opposite to them in property be
classed as oxidising and de-oxidising, sulphurising, and de-sulphurising agents. Most
oxidising agents also act as de-sulphurisers.
The de-oxidising agents most in use are the following:—
Charcoal.—Powdered wood charcoal; it contains more or less hygroscopic moisture and
about 3 or 4 per cent. of ash. The rest may be considered carbon. Carbon heated with
metallic oxides takes the oxygen; at low temperatures it forms carbon dioxide, and at higher
ones, carbon monoxide. Other conditions besides that of temperature have an influence in
producing these results; and as the quantity of charcoal required to complete a definite
reaction varies with these, it should be calculated from the results of immediate experience
rather than from theoretical considerations.
Flour.—Ordinary wheat flour is convenient in use. On being heated it gives off
inflammable gases which have a certain reducing effect, and a residue of finely divided
carbon is left. It is likely to vary in the quantity of moisture it contains. Two parts of flour
should be used where one part of charcoal would be otherwise required.
Tartar.—This is crude hydric potassic tartrate; the purified salt, cream of tartar, may be
used. On being heated it gives off inflammable gases, and leaves a residue formed of
potassic carbonate mixed with finely divided carbon. Five parts of tartar should be used in
the place of one of charcoal.
Anthracite or Culm is a kind of coal containing 90 per cent. or more of carbon. It gives off
no inflammable gas. It is denser, and takes longer in burning, than charcoal. Its reducing
effect is little inferior to that of charcoal. Almost any organic substance can be used as a
reducing agent, but it is well not to select one which melts, swells up, or gives off much
water and gas when heated in the furnace.
Potassic Cyanide is an easily fusible and somewhat volatile salt, which, when fused,
readily removes oxygen and sulphur from metallic compounds, and forms potassic cyanate
or sulphocyanate as the case may be. Commercial samples vary much in purity; some
contain less than 50 per cent. of the salt. For assaying, only the better qualities should be
used.
is an important one. Fluxes yield slags; reducing agents give buttons of regulus or of metal.
The action of a reducing agent is the separation of the oxygen or sulphur from the metal
with which it is combined. For example, the mineral anglesite (lead sulphate) is a
compound of lead, sulphur, and oxygen; by carefully heating it with charcoal the oxygen is
taken away by the charcoal, and a regulus of lead sulphide remains. If the regulus be then
fused with metallic iron the sulphur is removed by the iron, and metallic lead is left. The
charcoal and the iron are reducing agents. But in defining a reducing agent as one which
removes oxygen, or sulphur, from a metallic compound so as to set the metal free, it must
be remembered that sulphur itself will reduce metallic lead from fused litharge, and that
oxygen will similarly set free the metal in fused lead sulphide. There is no impropriety in
describing sulphur as a reducing agent; but it is absurd to call oxygen one. Some confusion
will be avoided if these substances and those which are opposite to them in property be
classed as oxidising and de-oxidising, sulphurising, and de-sulphurising agents. Most
oxidising agents also act as de-sulphurisers.
The de-oxidising agents most in use are the following:—
Charcoal.—Powdered wood charcoal; it contains more or less hygroscopic moisture and
about 3 or 4 per cent. of ash. The rest may be considered carbon. Carbon heated with
metallic oxides takes the oxygen; at low temperatures it forms carbon dioxide, and at higher
ones, carbon monoxide. Other conditions besides that of temperature have an influence in
producing these results; and as the quantity of charcoal required to complete a definite
reaction varies with these, it should be calculated from the results of immediate experience
rather than from theoretical considerations.
Flour.—Ordinary wheat flour is convenient in use. On being heated it gives off
inflammable gases which have a certain reducing effect, and a residue of finely divided
carbon is left. It is likely to vary in the quantity of moisture it contains. Two parts of flour
should be used where one part of charcoal would be otherwise required.
Tartar.—This is crude hydric potassic tartrate; the purified salt, cream of tartar, may be
used. On being heated it gives off inflammable gases, and leaves a residue formed of
potassic carbonate mixed with finely divided carbon. Five parts of tartar should be used in
the place of one of charcoal.
Anthracite or Culm is a kind of coal containing 90 per cent. or more of carbon. It gives off
no inflammable gas. It is denser, and takes longer in burning, than charcoal. Its reducing
effect is little inferior to that of charcoal. Almost any organic substance can be used as a
reducing agent, but it is well not to select one which melts, swells up, or gives off much
water and gas when heated in the furnace.
Potassic Cyanide is an easily fusible and somewhat volatile salt, which, when fused,
readily removes oxygen and sulphur from metallic compounds, and forms potassic cyanate
or sulphocyanate as the case may be. Commercial samples vary much in purity; some
contain less than 50 per cent. of the salt. For assaying, only the better qualities should be
used.
Page 40
Iron is a de-sulphurising rather than a de-oxidising agent. Iron is used in the form of rods,
1/2-inch in diameter, or of nails, or of hoop iron. In the last case it should be thin enough to
be bent without difficulty. Wrought iron crucibles are very useful in the processes required
for making galena assays.
The chief oxidising agents (which are also de-sulphurisers) are the following:—
Nitre, or Potassic Nitrate.—This salt fuses very easily to a watery liquid. It oxidises most
combustible substances with deflagration, and thereby converts sulphides into sulphates,
arsenides into arsenates, and most metals into oxides. In the presence of strong bases, such
as soda, the whole of the sulphur is fully oxidised; but in many cases some arsenic is apt to
escape, and to give rise to a peculiar garlic-like odour. The sulphates of soda and potash are
thus formed, and float as a watery liquid on the surface of the slag.
Red lead is an oxide of lead. About one-quarter of its oxygen is very loosely held, and,
hence, is available for oxidising purposes, without any separation of metallic lead. The rest
of the oxygen is also available; but for each part of oxygen given off, about 13 parts of
metallic lead are deposited. In silver assays this power of readily giving up oxygen is made
use of. The residual oxide (litharge) acts as a flux.
Hot air is the oxidising agent in roasting operations. The sulphur and arsenic of such
minerals as mispickel and pyrites are oxidised by the hot air and pass off as sulphur dioxide
and "white arsenic." The metals generally remain in the form of oxide, mixed with more or
less sulphate and arsenate. The residue may remain as a powdery substance (a calx), in
which case the process of roasting is termed calcination; or it may be a pasty mass or liquid.
In the calcination of somewhat fusible minerals, the roasting should be done at a low
temperature to avoid clotting; arsenic and sulphur being with difficulty burnt off from the
clotted mineral. A low temperature, however, favours the formation of sulphates; and these
(if not removed) would reappear in a subsequent reduction as sulphides. These sulphates
may be decomposed by a higher temperature towards the end of the operation; their
removal is rendered more certain by rubbing up the calx with some culm and re-roasting, or
by strongly heating the calx after the addition of solid ammonic carbonate. In roasting
operations, as large a surface of the substance as possible should be exposed to the air. If
done in a crucible, the crucible should be of the Cornish type, short and open, not long and
narrow. For calcinations, roasting dishes are useful: these are broad and shallow, not unlike
saucers, but unglazed. In those cases in which the products of the roasting are liquid at the
temperature used, a scorifier (fig. 38) is suitable if it is desired to keep the liquid; but if the
liquid is best drained off as quickly as it is formed, a cupel (fig. 5) should be used.
1/2-inch in diameter, or of nails, or of hoop iron. In the last case it should be thin enough to
be bent without difficulty. Wrought iron crucibles are very useful in the processes required
for making galena assays.
The chief oxidising agents (which are also de-sulphurisers) are the following:—
Nitre, or Potassic Nitrate.—This salt fuses very easily to a watery liquid. It oxidises most
combustible substances with deflagration, and thereby converts sulphides into sulphates,
arsenides into arsenates, and most metals into oxides. In the presence of strong bases, such
as soda, the whole of the sulphur is fully oxidised; but in many cases some arsenic is apt to
escape, and to give rise to a peculiar garlic-like odour. The sulphates of soda and potash are
thus formed, and float as a watery liquid on the surface of the slag.
Red lead is an oxide of lead. About one-quarter of its oxygen is very loosely held, and,
hence, is available for oxidising purposes, without any separation of metallic lead. The rest
of the oxygen is also available; but for each part of oxygen given off, about 13 parts of
metallic lead are deposited. In silver assays this power of readily giving up oxygen is made
use of. The residual oxide (litharge) acts as a flux.
Hot air is the oxidising agent in roasting operations. The sulphur and arsenic of such
minerals as mispickel and pyrites are oxidised by the hot air and pass off as sulphur dioxide
and "white arsenic." The metals generally remain in the form of oxide, mixed with more or
less sulphate and arsenate. The residue may remain as a powdery substance (a calx), in
which case the process of roasting is termed calcination; or it may be a pasty mass or liquid.
In the calcination of somewhat fusible minerals, the roasting should be done at a low
temperature to avoid clotting; arsenic and sulphur being with difficulty burnt off from the
clotted mineral. A low temperature, however, favours the formation of sulphates; and these
(if not removed) would reappear in a subsequent reduction as sulphides. These sulphates
may be decomposed by a higher temperature towards the end of the operation; their
removal is rendered more certain by rubbing up the calx with some culm and re-roasting, or
by strongly heating the calx after the addition of solid ammonic carbonate. In roasting
operations, as large a surface of the substance as possible should be exposed to the air. If
done in a crucible, the crucible should be of the Cornish type, short and open, not long and
narrow. For calcinations, roasting dishes are useful: these are broad and shallow, not unlike
saucers, but unglazed. In those cases in which the products of the roasting are liquid at the
temperature used, a scorifier (fig. 38) is suitable if it is desired to keep the liquid; but if the
liquid is best drained off as quickly as it is formed, a cupel (fig. 5) should be used.
Page 41
A scorifier is essentially a roasting dish sufficiently thick to resist, for a time, the corrosive
action of the fused metallic oxides it is to contain. The essential property of a cupel is, that it
is sufficiently porous to allow the fused oxide to drain into it as fast as it is formed. It should
be large enough to absorb the whole of the liquid; and of course must be made of a material
upon which the liquid has no corrosive action. Cupels do not bear transport well; hence the
assayer generally has to make them, or to supervise their making. A quantity of bone ash is
carefully mixed with water so that no lumps are formed, and the mixture is then worked up
by rubbing between the hands. The bone ash is sufficiently wet when its cohesion is such
that it can be pressed into a lump, and yet be easily crumbled into powder. Cupel moulds
should be purchased. They are generally made of turned iron or brass. They consist of three
parts (1) a hollow cylinder; (2) a disc of metal; and (3) a piston for compressing the bone
ash and shaping the top of the cupel. The disc forms a false bottom for the cylinder. This is
put in its place, and the cylinder filled (or nearly so) with the moistened bone ash. The bone
ash is then pressed into shape with the piston, and the cupel finished with the help of three
or four smart blows from a mallet. Before removing the piston, turn it half-way round upon
its axis so as to loosen and smooth the face of the cupel. The cupel is got out by pressing up
the disc of metal forming the false bottom; the removal is more easily effected if the mould
is somewhat conical, instead of cylindrical, in form. The cupels are put in a warm place to
dry for two or three days. A conveniently sized cupel is 1-1/4 inches in diameter and about
3/4 inch high. The cavity of the cupel is about 1/4 inch deep, and something of the shape
shown in fig. 5.
action of the fused metallic oxides it is to contain. The essential property of a cupel is, that it
is sufficiently porous to allow the fused oxide to drain into it as fast as it is formed. It should
be large enough to absorb the whole of the liquid; and of course must be made of a material
upon which the liquid has no corrosive action. Cupels do not bear transport well; hence the
assayer generally has to make them, or to supervise their making. A quantity of bone ash is
carefully mixed with water so that no lumps are formed, and the mixture is then worked up
by rubbing between the hands. The bone ash is sufficiently wet when its cohesion is such
that it can be pressed into a lump, and yet be easily crumbled into powder. Cupel moulds
should be purchased. They are generally made of turned iron or brass. They consist of three
parts (1) a hollow cylinder; (2) a disc of metal; and (3) a piston for compressing the bone
ash and shaping the top of the cupel. The disc forms a false bottom for the cylinder. This is
put in its place, and the cylinder filled (or nearly so) with the moistened bone ash. The bone
ash is then pressed into shape with the piston, and the cupel finished with the help of three
or four smart blows from a mallet. Before removing the piston, turn it half-way round upon
its axis so as to loosen and smooth the face of the cupel. The cupel is got out by pressing up
the disc of metal forming the false bottom; the removal is more easily effected if the mould
is somewhat conical, instead of cylindrical, in form. The cupels are put in a warm place to
dry for two or three days. A conveniently sized cupel is 1-1/4 inches in diameter and about
3/4 inch high. The cavity of the cupel is about 1/4 inch deep, and something of the shape
shown in fig. 5.
Page 42
Page 43
There are two kinds of furnaces required, the "wind" and "muffle" furnaces. These are built
of brick, fire-brick, of course, being used for the lining. They are connected with a chimney
that will provide a good draught. Figure 6 shows a section of the wind furnace, fig. 7 a
section of the muffle furnace, and fig. 8 a general view of a group comprising a muffle and
two wind furnaces suitable for general work. When in operation, the furnaces are covered
with iron-bound tiles. The opening under the door of the muffle is closed with a loosely
fitting brick. The floor of the muffle is protected with a layer of bone-ash, which absorbs
any oxide of lead that may be accidentally spilt. The fire bars should be easily removable.
Few tools are wanted; the most important are some cast-iron moulds, tongs (fig. 9), stirrers
for calcining (fig. 10), and light tongs of a special form for handling scorifiers and cupels
(see Silver).
The coke used should be of good quality; the formation of a fused ash (clinker), in any
quantity, causes ceaseless trouble, and requires frequent removal. The coke should be
broken into lumps of a uniform size (about 2 in. across) before being brought into the office.
The furnace should be well packed by stirring, raising the coke and not ramming it, and it
should be uniformly heated, not hot below and cold above. In lighting a furnace, a start is
made with wood and charcoal, this readily ignites and sets fire to the coke, which of itself
does not kindle easily.
of brick, fire-brick, of course, being used for the lining. They are connected with a chimney
that will provide a good draught. Figure 6 shows a section of the wind furnace, fig. 7 a
section of the muffle furnace, and fig. 8 a general view of a group comprising a muffle and
two wind furnaces suitable for general work. When in operation, the furnaces are covered
with iron-bound tiles. The opening under the door of the muffle is closed with a loosely
fitting brick. The floor of the muffle is protected with a layer of bone-ash, which absorbs
any oxide of lead that may be accidentally spilt. The fire bars should be easily removable.
Few tools are wanted; the most important are some cast-iron moulds, tongs (fig. 9), stirrers
for calcining (fig. 10), and light tongs of a special form for handling scorifiers and cupels
(see Silver).
The coke used should be of good quality; the formation of a fused ash (clinker), in any
quantity, causes ceaseless trouble, and requires frequent removal. The coke should be
broken into lumps of a uniform size (about 2 in. across) before being brought into the office.
The furnace should be well packed by stirring, raising the coke and not ramming it, and it
should be uniformly heated, not hot below and cold above. In lighting a furnace, a start is
made with wood and charcoal, this readily ignites and sets fire to the coke, which of itself
does not kindle easily.
Page 44
In commencing work, add (if necessary) fresh coke, and mix well; make hollows, and into
these put old crucibles; pack around with coke, so that the surface shall be concave, sloping
upwards from the mouths of the crucibles to the sides of the furnace; close the furnace, and,
when uniformly heated, substitute for the empty crucibles those which contain the assays. It
is rarely advisable to have a very hot fire at first, because with a gradual heat the gases and
steam quietly escape through the unfused mass, while with too strong a heat these might
make some of the matter in the crucible overflow. Moreover, if the heat should be too strong
at first, the flux might melt and run to the bottom of the crucible, leaving the quartz, &c., as
a pasty mass above; with a gentler heat combination is completed, and the subsequent
fiercer heat simply melts the fusible compound into homogeneous slag.
The fused material may be left in the crucible and separated from it by breaking when cold.
It is generally more convenient to pour it into cast-iron moulds. These moulds should be dry
and smooth. They act best when warmed and oiled or black-leaded.
Air entering through the fire-bars of a furnace and coming in contact with hot coke
combines with it, forming a very hot mixture of carbonic acid and nitrogen; this ascending,
comes in contact with more coke, and the carbonic acid is reduced to carbonic oxide; at the
top of the furnace, or in the flue, the carbonic oxide meeting fresh air, combines with the
oxygen therein and re-forms carbonic acid. In the first and third of these reactions, much
heat is evolved; in the second, the furnace is cooled a little. It must always be remembered,
that the carbonic oxide of the furnace gases is a reducing agent. When these gases are likely
to exert a prejudicial effect, and a strongly oxidising atmosphere is required, the work is
best done in a muffle.
FOOTNOTES:
[3] There is an exception to this, as when the slag is liable to be acted on when exposed to the air
and to the gases of the furnace. In this case a layer of fused common salt floating on the slag, so
as to protect it from the air and furnace gases, is a distinct advantage.
these put old crucibles; pack around with coke, so that the surface shall be concave, sloping
upwards from the mouths of the crucibles to the sides of the furnace; close the furnace, and,
when uniformly heated, substitute for the empty crucibles those which contain the assays. It
is rarely advisable to have a very hot fire at first, because with a gradual heat the gases and
steam quietly escape through the unfused mass, while with too strong a heat these might
make some of the matter in the crucible overflow. Moreover, if the heat should be too strong
at first, the flux might melt and run to the bottom of the crucible, leaving the quartz, &c., as
a pasty mass above; with a gentler heat combination is completed, and the subsequent
fiercer heat simply melts the fusible compound into homogeneous slag.
The fused material may be left in the crucible and separated from it by breaking when cold.
It is generally more convenient to pour it into cast-iron moulds. These moulds should be dry
and smooth. They act best when warmed and oiled or black-leaded.
Air entering through the fire-bars of a furnace and coming in contact with hot coke
combines with it, forming a very hot mixture of carbonic acid and nitrogen; this ascending,
comes in contact with more coke, and the carbonic acid is reduced to carbonic oxide; at the
top of the furnace, or in the flue, the carbonic oxide meeting fresh air, combines with the
oxygen therein and re-forms carbonic acid. In the first and third of these reactions, much
heat is evolved; in the second, the furnace is cooled a little. It must always be remembered,
that the carbonic oxide of the furnace gases is a reducing agent. When these gases are likely
to exert a prejudicial effect, and a strongly oxidising atmosphere is required, the work is
best done in a muffle.
FOOTNOTES:
[3] There is an exception to this, as when the slag is liable to be acted on when exposed to the air
and to the gases of the furnace. In this case a layer of fused common salt floating on the slag, so
as to protect it from the air and furnace gases, is a distinct advantage.
Page 45
CHAPTER III.
WET GRAVIMETRIC METHODS.
In dry assays the metal is almost always separated and weighed as metal; in wet gravimetric
assays the metal is more usually weighed in the form of a definite compound of known
composition. The general methods of working resemble those of ordinary chemical
analysis, and their successful working is greatly helped by a knowledge of, at any rate,
those compounds of the metal which enable it to be separated, and of those which are the
most convenient forms in which it can be weighed. But the work of the assayer differs from
that of the analyst, inasmuch as the bulk of his estimations are made upon material of
practically the same kind, varying only in richness; consequently in assaying, it is possible
(and necessary) to work on such a definite plan as will involve the least amount of labour in
weighing and calculating.
The assayer connected with mining has generally two classes of material to deal with: those
comparatively rich and those comparatively poor. For example, silver in bullion and in ores;
copper precipitates or regulus, and copper ores and slags; and "black tin" and tin ores. He is
only occasionally called on to assay the intermediate products. It is indispensable that he
should have an approximate knowledge of the substance to be determined. With new ores
this information is best got by a qualitative testing. Knowing that only certain bodies are
present, it is evident that the number of separations can be reduced, and that simple methods
can be devised for arriving at the results sought for. The best method is that which involves
the least number of separations. The reactions must be sharp and complete, and yet not be
liable to error under varying conditions.
To bring the richer and poorer materials under the same conditions for the assay, a small
weight, say 1 gram of the richer, and a larger weight (5 or 10 grams) of the poorer,
substance is weighed up. A method is then adopted which will concentrate the whole of the
metal (either during or after solution) in a product which need not necessarily be pure. The
work on this product is comparatively easy. In separating small quantities of a substance
from a large bulk of impurities, the group separations must not as a rule be too much relied
on. Very large precipitates carry down small quantities of bodies not belonging to the group,
more especially when there is a tendency to form weak double compounds. The re-
dissolving and re-precipitating of bulky precipitates should be avoided.
When a large number of assays of the same kind have to be carried out, a plan something
like the following is adopted:—The samples, after having been dried, are placed in order on
a table at the left hand of the assayer. He takes the first, marks it with a number, samples
and weighs up the quantity required, and transfers it to a flask, which is similarly marked.
As the weighings are finished, the samples are placed in the same order on his right hand.
The assistant takes the flasks in batches of four or five at a time to the fume cupboard,
where he adds a measured quantity of acid. When solution has been effected, dilution with a
WET GRAVIMETRIC METHODS.
In dry assays the metal is almost always separated and weighed as metal; in wet gravimetric
assays the metal is more usually weighed in the form of a definite compound of known
composition. The general methods of working resemble those of ordinary chemical
analysis, and their successful working is greatly helped by a knowledge of, at any rate,
those compounds of the metal which enable it to be separated, and of those which are the
most convenient forms in which it can be weighed. But the work of the assayer differs from
that of the analyst, inasmuch as the bulk of his estimations are made upon material of
practically the same kind, varying only in richness; consequently in assaying, it is possible
(and necessary) to work on such a definite plan as will involve the least amount of labour in
weighing and calculating.
The assayer connected with mining has generally two classes of material to deal with: those
comparatively rich and those comparatively poor. For example, silver in bullion and in ores;
copper precipitates or regulus, and copper ores and slags; and "black tin" and tin ores. He is
only occasionally called on to assay the intermediate products. It is indispensable that he
should have an approximate knowledge of the substance to be determined. With new ores
this information is best got by a qualitative testing. Knowing that only certain bodies are
present, it is evident that the number of separations can be reduced, and that simple methods
can be devised for arriving at the results sought for. The best method is that which involves
the least number of separations. The reactions must be sharp and complete, and yet not be
liable to error under varying conditions.
To bring the richer and poorer materials under the same conditions for the assay, a small
weight, say 1 gram of the richer, and a larger weight (5 or 10 grams) of the poorer,
substance is weighed up. A method is then adopted which will concentrate the whole of the
metal (either during or after solution) in a product which need not necessarily be pure. The
work on this product is comparatively easy. In separating small quantities of a substance
from a large bulk of impurities, the group separations must not as a rule be too much relied
on. Very large precipitates carry down small quantities of bodies not belonging to the group,
more especially when there is a tendency to form weak double compounds. The re-
dissolving and re-precipitating of bulky precipitates should be avoided.
When a large number of assays of the same kind have to be carried out, a plan something
like the following is adopted:—The samples, after having been dried, are placed in order on
a table at the left hand of the assayer. He takes the first, marks it with a number, samples
and weighs up the quantity required, and transfers it to a flask, which is similarly marked.
As the weighings are finished, the samples are placed in the same order on his right hand.
The assistant takes the flasks in batches of four or five at a time to the fume cupboard,
where he adds a measured quantity of acid. When solution has been effected, dilution with a
Page 46
measured volume is generally necessary. The assayer sees to this and (whilst the funnels
and filters are being prepared) makes any separation that is necessary. The filters are
arranged in order on a rack (fig. 11), and need not be marked unless the precipitates or
residues have subsequently to be dried. The filters are washed with hot water, and if the
filtrates are wanted flasks are placed beneath, if not, the solution is drained off down the
sink. Precipitation or reduction (or whatever it may be) is now made; the assistant filters the
prepared samples, one at a time, whilst the assayer is engaged with the others. The same
style of work is continued until the assays are completed. If one should be spoiled, it is
better to allow it to stand over for assaying along with the next batch. If one filters slowly or
is in any way less forward than the rest, it may lessen the accuracy of the other assays,
owing to oxidation, &c., it should, therefore, be put on one side. The assays are dealt with in
batches of ten or twenty, so that a large quantity of work can be quickly finished.
When the assays are finished, it is the duty of the assistant to clean the apparatus (with
reagents, if necessary), and to put the vessels in the place set apart for them. Flasks are best
kept inverted on a rack, so that they may be dry and clean by the next morning. Berlin
crucibles must be cleaned and ignited.
The amount of apparatus employed should be as little as is feasible. The assay should be
carried out as much as possible in the same flask. The bench must be clean, and altogether
free from apparatus not in actual use. Crucibles and dishes in which weighings are made
should be marked with numbers or letters; and their weights recorded, together with the date
of weighing, in a small ledger, which is kept in the drawer of the balance. By this means a
record of the "wear" of each piece of apparatus is obtained, and, what is more important,
much weighing is saved, and increased confidence is gained. The weight of each piece of
apparatus need not be taken daily. It will be seen from the record in the book and a
knowledge of the use it has been put to how often a checking of the weight is necessary.
The entries are made in black lead as follows:—
and filters are being prepared) makes any separation that is necessary. The filters are
arranged in order on a rack (fig. 11), and need not be marked unless the precipitates or
residues have subsequently to be dried. The filters are washed with hot water, and if the
filtrates are wanted flasks are placed beneath, if not, the solution is drained off down the
sink. Precipitation or reduction (or whatever it may be) is now made; the assistant filters the
prepared samples, one at a time, whilst the assayer is engaged with the others. The same
style of work is continued until the assays are completed. If one should be spoiled, it is
better to allow it to stand over for assaying along with the next batch. If one filters slowly or
is in any way less forward than the rest, it may lessen the accuracy of the other assays,
owing to oxidation, &c., it should, therefore, be put on one side. The assays are dealt with in
batches of ten or twenty, so that a large quantity of work can be quickly finished.
When the assays are finished, it is the duty of the assistant to clean the apparatus (with
reagents, if necessary), and to put the vessels in the place set apart for them. Flasks are best
kept inverted on a rack, so that they may be dry and clean by the next morning. Berlin
crucibles must be cleaned and ignited.
The amount of apparatus employed should be as little as is feasible. The assay should be
carried out as much as possible in the same flask. The bench must be clean, and altogether
free from apparatus not in actual use. Crucibles and dishes in which weighings are made
should be marked with numbers or letters; and their weights recorded, together with the date
of weighing, in a small ledger, which is kept in the drawer of the balance. By this means a
record of the "wear" of each piece of apparatus is obtained, and, what is more important,
much weighing is saved, and increased confidence is gained. The weight of each piece of
apparatus need not be taken daily. It will be seen from the record in the book and a
knowledge of the use it has been put to how often a checking of the weight is necessary.
The entries are made in black lead as follows:—
Page 47
Dish, A. Feb. 3 9.4210 grams.
5 9.4225
6 9.4230
7 9.4200
Platinum vessels and apparatus lose, and porcelain ones slightly gain, weight
with continued use.
The special details of the work is given under each assay; certain general
instructions will be given here.
Solution.—It is not always necessary to get the whole of the mineral in solution,
provided the body sought for is either completely dissolved or altogether left in
the residue. It is often only by a qualitative examination of the solution (or
residue, as the case may be) that the assayer can satisfy himself that it is free
from the substance sought. But previous experience with the same kind of ore
will show to what extent this testing is necessary.
Solution is generally best effected in flasks; but where the resulting liquid has
afterwards to be evaporated to dryness and ignited, evaporating dishes (fig. 12)
are used. With them clock glasses are used as covers during solution to avoid
loss through effervescence. Evaporating dishes are also best when an insoluble
residue has to be collected, since it is difficult to wash out most residues from a
flask. Bumping occurs less frequently in dishes than in flasks.
After the addition of the acid, and mixing by agitation, the vessel containing the
substance is heated. This is best done on the "hot plate" (fig. 13). This consists
of a slab of cast iron about half or three-quarters of an inch thick, supported on
loose fire bricks, and heated by two or three ring burners (figs. 14 and 15). The
5 9.4225
6 9.4230
7 9.4200
Platinum vessels and apparatus lose, and porcelain ones slightly gain, weight
with continued use.
The special details of the work is given under each assay; certain general
instructions will be given here.
Solution.—It is not always necessary to get the whole of the mineral in solution,
provided the body sought for is either completely dissolved or altogether left in
the residue. It is often only by a qualitative examination of the solution (or
residue, as the case may be) that the assayer can satisfy himself that it is free
from the substance sought. But previous experience with the same kind of ore
will show to what extent this testing is necessary.
Solution is generally best effected in flasks; but where the resulting liquid has
afterwards to be evaporated to dryness and ignited, evaporating dishes (fig. 12)
are used. With them clock glasses are used as covers during solution to avoid
loss through effervescence. Evaporating dishes are also best when an insoluble
residue has to be collected, since it is difficult to wash out most residues from a
flask. Bumping occurs less frequently in dishes than in flasks.
After the addition of the acid, and mixing by agitation, the vessel containing the
substance is heated. This is best done on the "hot plate" (fig. 13). This consists
of a slab of cast iron about half or three-quarters of an inch thick, supported on
loose fire bricks, and heated by two or three ring burners (figs. 14 and 15). The
Page 48
burners are connected to the gas supply by means of lead tubing, to which they
are soldered. Flasks and dishes after being put on the plate are not further
handled until solution is complete or the evaporation is carried to dryness. The
hot plate is contained in a cupboard so as to be out of the reach of cold draughts.
The action of the acids and other solvents is described in the chapter on
Reagents.
Precipitation.—In precipitating add sufficient of the reagent to complete the
reaction. The student must be on his guard against adding a very large excess,
are soldered. Flasks and dishes after being put on the plate are not further
handled until solution is complete or the evaporation is carried to dryness. The
hot plate is contained in a cupboard so as to be out of the reach of cold draughts.
The action of the acids and other solvents is described in the chapter on
Reagents.
Precipitation.—In precipitating add sufficient of the reagent to complete the
reaction. The student must be on his guard against adding a very large excess,
Page 49
which is the commoner error. In some reactions the finishing point is obvious
enough; either no more precipitate is formed, or a precipitate is completely
dissolved, or some well-marked colour or odour is developed or removed.
In those cases in which there is no such indication, theoretical considerations
should keep the use of reagents within reasonable limits. The solutions of the
reagents (see Reagents) are generally of five or ten per cent. strength. A small
excess over that demanded by theory should be sufficient.
enough; either no more precipitate is formed, or a precipitate is completely
dissolved, or some well-marked colour or odour is developed or removed.
In those cases in which there is no such indication, theoretical considerations
should keep the use of reagents within reasonable limits. The solutions of the
reagents (see Reagents) are generally of five or ten per cent. strength. A small
excess over that demanded by theory should be sufficient.
Page 50
Filtration.—Solutions are best filtered hot whenever the assay allows of this
being so done. The precipitate should be allowed to settle, and the clear liquid
decanted on the filter with the aid of a glass rod if necessary. The filter-paper
must not be too large, but at the same time it must not be overloaded with the
precipitate. There should be ample room for washing. For general use three sizes
of filter-paper are sufficient. Common quick filtering-paper (English) is best for
most work in assaying. The specially prepared paper (Swedish or Rhenish) is
used for collecting those precipitates which have to be weighed. The papers are
folded as shown in fig. 16, and should not project above the funnel. The filter-
paper works better if damped with hot water. In special cases filtering is
hastened by means of an air-pump. The apparatus used consists of a water-jet
(fig. 17), which is connected with the tap, as also with a bottle fitted as shown in
fig. 18. The pump draws the air out from the bottle, and atmospheric pressure
forces the liquid through the filter-paper. The bottom of the funnel is provided
being so done. The precipitate should be allowed to settle, and the clear liquid
decanted on the filter with the aid of a glass rod if necessary. The filter-paper
must not be too large, but at the same time it must not be overloaded with the
precipitate. There should be ample room for washing. For general use three sizes
of filter-paper are sufficient. Common quick filtering-paper (English) is best for
most work in assaying. The specially prepared paper (Swedish or Rhenish) is
used for collecting those precipitates which have to be weighed. The papers are
folded as shown in fig. 16, and should not project above the funnel. The filter-
paper works better if damped with hot water. In special cases filtering is
hastened by means of an air-pump. The apparatus used consists of a water-jet
(fig. 17), which is connected with the tap, as also with a bottle fitted as shown in
fig. 18. The pump draws the air out from the bottle, and atmospheric pressure
forces the liquid through the filter-paper. The bottom of the funnel is provided
Page 51
with a platinum cone, which supports the filter-paper, and prevents its breaking.
The pump is only used in exceptional cases; nearly all the filtrations required by
the assayer can be made without it. The usual methods of supporting the funnel
during filtration are shown in fig. 19. Where the filtrate is not wanted, pickle
bottles make convenient supports. After the precipitate has been thrown on the
filter, it is washed. In washing, several washings with a small quantity of water
are more effective than a few with a larger quantity of that fluid. The upper edge
of the filter-paper is specially liable to escape complete washing. Excessive
washing must be avoided; the point at which the washing is complete is found
by collecting a little of the filtrate and testing it. The precipitate is removed from
the filter-paper for further treatment by opening out the paper and by washing
the precipitate with a jet of water from a wash-bottle into a beaker, or back
through the funnel into the flask. In some cases, when the precipitate has to be
dissolved in anything in which it is readily soluble, solution is effected in the
filter itself allowing the liquid to run through as it is formed.
Drying and Igniting.—Precipitates, as a rule, require drying before being
ignited. With small precipitates the filter-paper may be opened out, and placed
on a warm asbestos slab till dry; or the funnel and the filter with the precipitate
is placed in a warm place, and supported by any convenient means. The heat
must never be sufficient to char the paper. Some precipitates must be dried at a
temperature not higher than 100°C. These are placed in the water-oven (fig. 20),
and, when apparently dry, they are taken from the funnel, placed between
glasses, and then left in the oven till they cease to lose weight. Such precipitates
are collected on tared filters. Those precipitates which will stand a higher
temperature are dried in the hot-air oven at a temperature of from 120° to 150°.
The drying is continued until they appear to be free from moisture, and until the
precipitate ceases to adhere to the filter. In drying sulphides the heat must not be
raised to the melting point of sulphur, since, if there is any free sulphur present,
it fuses and filters through.
The pump is only used in exceptional cases; nearly all the filtrations required by
the assayer can be made without it. The usual methods of supporting the funnel
during filtration are shown in fig. 19. Where the filtrate is not wanted, pickle
bottles make convenient supports. After the precipitate has been thrown on the
filter, it is washed. In washing, several washings with a small quantity of water
are more effective than a few with a larger quantity of that fluid. The upper edge
of the filter-paper is specially liable to escape complete washing. Excessive
washing must be avoided; the point at which the washing is complete is found
by collecting a little of the filtrate and testing it. The precipitate is removed from
the filter-paper for further treatment by opening out the paper and by washing
the precipitate with a jet of water from a wash-bottle into a beaker, or back
through the funnel into the flask. In some cases, when the precipitate has to be
dissolved in anything in which it is readily soluble, solution is effected in the
filter itself allowing the liquid to run through as it is formed.
Drying and Igniting.—Precipitates, as a rule, require drying before being
ignited. With small precipitates the filter-paper may be opened out, and placed
on a warm asbestos slab till dry; or the funnel and the filter with the precipitate
is placed in a warm place, and supported by any convenient means. The heat
must never be sufficient to char the paper. Some precipitates must be dried at a
temperature not higher than 100°C. These are placed in the water-oven (fig. 20),
and, when apparently dry, they are taken from the funnel, placed between
glasses, and then left in the oven till they cease to lose weight. Such precipitates
are collected on tared filters. Those precipitates which will stand a higher
temperature are dried in the hot-air oven at a temperature of from 120° to 150°.
The drying is continued until they appear to be free from moisture, and until the
precipitate ceases to adhere to the filter. In drying sulphides the heat must not be
raised to the melting point of sulphur, since, if there is any free sulphur present,
it fuses and filters through.
Page 52
The precipitate, having been dried, is transferred to a watch-glass. The filter-
paper is opened out over a sheet of note-paper, and, with a camel-hair brush, the
precipitate is gently brought into the glass. Most precipitates come away easily,
and the transfer can be made without apparent loss. The watch-glass is covered
by the funnel, and the filter-paper (folded into a quadrant) held by the tweezers
and set fire to with the flame of a Bunsen burner. It is allowed to burn over the
crucible, into which the black bulky ash is allowed to drop, and two or three
drops of nitric acid are then added. The crucible is placed on a pipe-stem
triangle (fig. 21), supported on a tripod. It is at first heated gently with a Bunsen
burner, and afterwards more strongly, until the residue is free from carbon. It is
cooled, and treated with any acid necessary to convert the small amount of
precipitate into the state in which it is to be weighed; heated again, and cooled.
The main precipitate is transferred to the crucible, and the heating repeated very
gently at first, but more strongly towards the end of the operation. It is next
placed in the muffle, and, after two or three minutes at a red heat, it is removed
and allowed to cool in the desiccator before weighing. This is for bodies that
will bear a red heat; for those compounds that require a lower temperature the
heating in the muffle is omitted. The muffle used for this purpose must not be
used at the same time for cupelling; a gas muffle (fig. 22), such as one of
paper is opened out over a sheet of note-paper, and, with a camel-hair brush, the
precipitate is gently brought into the glass. Most precipitates come away easily,
and the transfer can be made without apparent loss. The watch-glass is covered
by the funnel, and the filter-paper (folded into a quadrant) held by the tweezers
and set fire to with the flame of a Bunsen burner. It is allowed to burn over the
crucible, into which the black bulky ash is allowed to drop, and two or three
drops of nitric acid are then added. The crucible is placed on a pipe-stem
triangle (fig. 21), supported on a tripod. It is at first heated gently with a Bunsen
burner, and afterwards more strongly, until the residue is free from carbon. It is
cooled, and treated with any acid necessary to convert the small amount of
precipitate into the state in which it is to be weighed; heated again, and cooled.
The main precipitate is transferred to the crucible, and the heating repeated very
gently at first, but more strongly towards the end of the operation. It is next
placed in the muffle, and, after two or three minutes at a red heat, it is removed
and allowed to cool in the desiccator before weighing. This is for bodies that
will bear a red heat; for those compounds that require a lower temperature the
heating in the muffle is omitted. The muffle used for this purpose must not be
used at the same time for cupelling; a gas muffle (fig. 22), such as one of
Page 53
Fletcher's, is best. A desiccator (fig. 23) is an air-tight vessel which prevents
access of moisture, &c., to the substance. Usually the air in it is kept dry by
means of a basin containing sulphuric acid.
access of moisture, &c., to the substance. Usually the air in it is kept dry by
means of a basin containing sulphuric acid.
Page 54
The crucible is removed from the muffle with the tongs and carried to the
desiccator. It is best, in an office, to have a large desiccator permanently fixed
alongside the balance, into which all substances may be put before being
weighed. The substance is removed from the bench or muffle in the small hand
apparatus generally sold, and carried to the balance room to be transferred to the
large desiccator, where it is allowed to become thoroughly cold before being
weighed. Twenty minutes is generally the time allowed after ignition before it is
advisable to weigh. Bodies allowed to cool in the air after they have been ignited
will absorb moisture, and hot bodies placed in the balance-pan will disturb the
equilibrium and show false results. Compounds that absorb moisture must be
weighed quickly; they should, therefore, be weighed in covered vessels. Such
compounds are detected by their continually-increasing weight. They should be
ignited and weighed again in a well-covered dish.
Substances that have been washed with alcohol, ether, or any readily volatile
liquid are dried in the water oven. They quickly dry if there is no water present,
and are generally fit for weighing in less than one hour. Sometimes drying for a
few minutes only will be sufficient.
The weight of the crucible and precipitate having been obtained, the weight of
the crucible and ash is deducted; for example—
desiccator. It is best, in an office, to have a large desiccator permanently fixed
alongside the balance, into which all substances may be put before being
weighed. The substance is removed from the bench or muffle in the small hand
apparatus generally sold, and carried to the balance room to be transferred to the
large desiccator, where it is allowed to become thoroughly cold before being
weighed. Twenty minutes is generally the time allowed after ignition before it is
advisable to weigh. Bodies allowed to cool in the air after they have been ignited
will absorb moisture, and hot bodies placed in the balance-pan will disturb the
equilibrium and show false results. Compounds that absorb moisture must be
weighed quickly; they should, therefore, be weighed in covered vessels. Such
compounds are detected by their continually-increasing weight. They should be
ignited and weighed again in a well-covered dish.
Substances that have been washed with alcohol, ether, or any readily volatile
liquid are dried in the water oven. They quickly dry if there is no water present,
and are generally fit for weighing in less than one hour. Sometimes drying for a
few minutes only will be sufficient.
The weight of the crucible and precipitate having been obtained, the weight of
the crucible and ash is deducted; for example—
Page 55
Crucible and precipitate 10.183grams.
Crucible and ash 9.527 "
———
0.656 "
The weight of the ash is best added to that of the crucible. The amount of ash in
filter-papers must not be neglected, although papers are now made almost free
from ash, and the amount to be deducted is found by taking eight or ten papers
and burning them until they become white, and then weighing the ash. The
amount varies from 0.004 to 0.0005 gram for different papers. Having
determined the ash, place in the balance-drawer three of the filter-papers pinned
together, with the weights marked on them in the way shown in fig. 24, so as to
be readily seen when there is occasion to refer to them.
It must be remembered that the determination of small quantities of substances
generally involves the use of reagents which are often contaminated, as an
impurity, with the body sought for. Thus, in assaying silver, the oxide of lead or
metallic lead used is rarely free from silver; and in the case of arsenic, the acids,
zinc or ferric chloride are sure to contain arsenic. The same observation applies
to the precipitation of lead by zinc, &c. The errors caused by these impurities are
more marked in the determination of material having small quantities of metal
than in that of ores which contain larger quantities. Errors of this kind are
counteracted or neutralised by "blank" or "blind" determinations. These consist
Crucible and ash 9.527 "
———
0.656 "
The weight of the ash is best added to that of the crucible. The amount of ash in
filter-papers must not be neglected, although papers are now made almost free
from ash, and the amount to be deducted is found by taking eight or ten papers
and burning them until they become white, and then weighing the ash. The
amount varies from 0.004 to 0.0005 gram for different papers. Having
determined the ash, place in the balance-drawer three of the filter-papers pinned
together, with the weights marked on them in the way shown in fig. 24, so as to
be readily seen when there is occasion to refer to them.
It must be remembered that the determination of small quantities of substances
generally involves the use of reagents which are often contaminated, as an
impurity, with the body sought for. Thus, in assaying silver, the oxide of lead or
metallic lead used is rarely free from silver; and in the case of arsenic, the acids,
zinc or ferric chloride are sure to contain arsenic. The same observation applies
to the precipitation of lead by zinc, &c. The errors caused by these impurities are
more marked in the determination of material having small quantities of metal
than in that of ores which contain larger quantities. Errors of this kind are
counteracted or neutralised by "blank" or "blind" determinations. These consist
Page 56
in carrying out by the side of and during the assay a duplicate experiment with
the reagents only, which are thereby subjected to the same processes of solution,
evaporation, filtration, &c. The final result thus obtained is deducted from that
given by the assay, the difference gives the corrected result. In some cases,
where it is desired or necessary to have a tangible residue or precipitate, some
pure inert material is added.
the reagents only, which are thereby subjected to the same processes of solution,
evaporation, filtration, &c. The final result thus obtained is deducted from that
given by the assay, the difference gives the corrected result. In some cases,
where it is desired or necessary to have a tangible residue or precipitate, some
pure inert material is added.
Page 57
CHAPTER IV.
VOLUMETRIC ASSAYS.
These have been already described as those in which the results are got by
measuring, either—(1) the volume of a reagent required to complete some
reaction, or (2) the volume of the resulting product. For example, if a
permanganate of potash solution be added to a solution containing a weighed
amount of iron, dissolved in sulphuric acid, the strong colour of the
permanganate of potash will be removed until a certain quantity of it has been
added. Repeating the experiment, it will be found that the same amount of iron
decolorises the same volume of the permanganate solution within certain narrow
limits of variation, known as "error of experiment." This error is due to variation
in the method of working and to slight differences in the weighings and
measurings; it is present in all experimental methods, although the limits of
variation are wider in some than in others. Apart from this error of experiment,
however, it is certain that a given volume of the permanganate of potash solution
corresponds to a definite weight of iron, so that if either is known the other may
be calculated. Similarly, if a known weight of zinc (or of carbonate of lime) be
dissolved in hydrochloric acid, a gas will be given off which can be measured,
and so long as the conditions of the experiment do not vary, the same weight of
zinc (or of carbonate of lime) gives off the same volume of gas. The weight of
the one can be determined from the volume of the other.
Or, again, the quantity of some substances may be measured by the colour of
their solutions, on the principle that, other things being equal, the colour of a
solution depends upon the quantity of colouring matter present. So that if two
solutions of the same substance are equally coloured they are of equal strength.
In this way an unknown may be compared with a known strength, and a fairly
accurate determination may be made. These three illustrations serve as types of
the three chief classes of volumetric assays—titrometric, gasometric, and
colorimetric.
Titrometric Assays.—Within the limits of the error of experiment, a definite
volume of a solution or gas represents a certain weight of metal or other
substance, hence the exact weight may be determined by experiment. The error
of experiment may be reduced to insignificant dimensions by repeating the
VOLUMETRIC ASSAYS.
These have been already described as those in which the results are got by
measuring, either—(1) the volume of a reagent required to complete some
reaction, or (2) the volume of the resulting product. For example, if a
permanganate of potash solution be added to a solution containing a weighed
amount of iron, dissolved in sulphuric acid, the strong colour of the
permanganate of potash will be removed until a certain quantity of it has been
added. Repeating the experiment, it will be found that the same amount of iron
decolorises the same volume of the permanganate solution within certain narrow
limits of variation, known as "error of experiment." This error is due to variation
in the method of working and to slight differences in the weighings and
measurings; it is present in all experimental methods, although the limits of
variation are wider in some than in others. Apart from this error of experiment,
however, it is certain that a given volume of the permanganate of potash solution
corresponds to a definite weight of iron, so that if either is known the other may
be calculated. Similarly, if a known weight of zinc (or of carbonate of lime) be
dissolved in hydrochloric acid, a gas will be given off which can be measured,
and so long as the conditions of the experiment do not vary, the same weight of
zinc (or of carbonate of lime) gives off the same volume of gas. The weight of
the one can be determined from the volume of the other.
Or, again, the quantity of some substances may be measured by the colour of
their solutions, on the principle that, other things being equal, the colour of a
solution depends upon the quantity of colouring matter present. So that if two
solutions of the same substance are equally coloured they are of equal strength.
In this way an unknown may be compared with a known strength, and a fairly
accurate determination may be made. These three illustrations serve as types of
the three chief classes of volumetric assays—titrometric, gasometric, and
colorimetric.
Titrometric Assays.—Within the limits of the error of experiment, a definite
volume of a solution or gas represents a certain weight of metal or other
substance, hence the exact weight may be determined by experiment. The error
of experiment may be reduced to insignificant dimensions by repeating the
Page 58
experiment, and taking the mean of three or four determinations. This will at the
same time show the amount of variation. Thus, if 0.5 gram of iron were
dissolved and found to require 50.3 cubic centimetres of the solution of
permanganate of potash, and if on repeating, 50.4, 50.2, and 50.3 c.c. were
required, the experimenter would be justified in saying that 50.3 c.c. of the
permanganate solution represent 0.5 gram of iron, and that his results were good
within 0.2 c.c. of the permanganate solution. So that if in an unknown solution
of iron, 50.5 c.c. of the permanganate solution were used up, he could state with
confidence that it contained a little more than 0.5 gram of iron. With a larger
experience the confidence would increase, and with practice the experimental
error will diminish.
But supposing that the unknown solution required, say, 100.5 instead of 50.5
c.c., he would not be justified in saying that, since 50.3 c.c. are equivalent to 0.5
gram, 100.6 c.c. are equivalent to twice that amount; and that, consequently, the
unknown solution contained a little less than 1 gram of iron; or, at least, he could
not say it except he (or some one else) had determined it by experiment. But if
on dissolving 1 gram of iron, he found it to require 100.6 c.c. of the solution,
and in another experiment with 0.8 gram of iron that 80.5 c.c. of the solution
were required, he would be justified in stating that the volume of solution
required is proportional to the quantity of metal present. There are a large
number of volumetric assays of which this is true, but that it is true in any
particular case can only be proved by experiment. Even where true it is well not
to rest too much weight upon it, and in all cases the quantity of metal taken, to
determine the strength of the solution used, should not differ widely from that
present in the assay. There are certain terms which should be explained here.
When the solution of a reagent is applied under such conditions that the volume
added can be correctly determined, the operation is called "titrating," the
solution of the reagent used the "standard solution," and the process of
determining the strength of the standard solution is "standardising." The
"standard" is the quantity of metal equivalent to 100 c.c. of the standard
solution.
Standard Solutions.—In making these the salt is accurately weighed and
transferred to a litre flask, or to the graduated cylinder, and dissolved. The
method of dissolving it varies in special cases, and instructions for these will be
found under the respective assays. Generally it is dissolved in a small quantity of
liquid, and then diluted to the mark. For those substances that require the aid of
heat, the solution is made in a pint flask, cooled, and transferred; after which the
flask is well washed out. After dilution, the liquids in the measuring vessel must
same time show the amount of variation. Thus, if 0.5 gram of iron were
dissolved and found to require 50.3 cubic centimetres of the solution of
permanganate of potash, and if on repeating, 50.4, 50.2, and 50.3 c.c. were
required, the experimenter would be justified in saying that 50.3 c.c. of the
permanganate solution represent 0.5 gram of iron, and that his results were good
within 0.2 c.c. of the permanganate solution. So that if in an unknown solution
of iron, 50.5 c.c. of the permanganate solution were used up, he could state with
confidence that it contained a little more than 0.5 gram of iron. With a larger
experience the confidence would increase, and with practice the experimental
error will diminish.
But supposing that the unknown solution required, say, 100.5 instead of 50.5
c.c., he would not be justified in saying that, since 50.3 c.c. are equivalent to 0.5
gram, 100.6 c.c. are equivalent to twice that amount; and that, consequently, the
unknown solution contained a little less than 1 gram of iron; or, at least, he could
not say it except he (or some one else) had determined it by experiment. But if
on dissolving 1 gram of iron, he found it to require 100.6 c.c. of the solution,
and in another experiment with 0.8 gram of iron that 80.5 c.c. of the solution
were required, he would be justified in stating that the volume of solution
required is proportional to the quantity of metal present. There are a large
number of volumetric assays of which this is true, but that it is true in any
particular case can only be proved by experiment. Even where true it is well not
to rest too much weight upon it, and in all cases the quantity of metal taken, to
determine the strength of the solution used, should not differ widely from that
present in the assay. There are certain terms which should be explained here.
When the solution of a reagent is applied under such conditions that the volume
added can be correctly determined, the operation is called "titrating," the
solution of the reagent used the "standard solution," and the process of
determining the strength of the standard solution is "standardising." The
"standard" is the quantity of metal equivalent to 100 c.c. of the standard
solution.
Standard Solutions.—In making these the salt is accurately weighed and
transferred to a litre flask, or to the graduated cylinder, and dissolved. The
method of dissolving it varies in special cases, and instructions for these will be
found under the respective assays. Generally it is dissolved in a small quantity of
liquid, and then diluted to the mark. For those substances that require the aid of
heat, the solution is made in a pint flask, cooled, and transferred; after which the
flask is well washed out. After dilution, the liquids in the measuring vessel must
Page 59
be thoroughly mixed by shaking. This is more easily and better done in the
cylinder than in the litre flask. The solution is next transferred to a dry
"Winchester" bottle and labelled. The label may be rendered permanent by
waxing it.
Standard solutions should not be kept in a place exposed to direct sunlight.
Oxidising and reducing solutions, such as those of permanganate of potash,
ferrous sulphate, iodine, hyposulphite of soda, &c., gradually weaken in
strength; the solutions of other salts are more stable; while those of potassium
bichromate and baric chloride are almost permanent. Solutions of potassium
permanganate may be kept for a month or so without much change. The
solutions of hyposulphite of soda and of iodine should be examined weekly.
Ferrous sulphate solutions, if acidulated with sulphuric acid, may be depended
on for two or three weeks without fresh standardising. Before filling the burette,
the "Winchester" bottle should be well shaken and a portion of about 50 or 100
c.c. poured into a dry beaker or test-glass. Besides the standard solutions, which
are required for titrating an assay, permanent solutions of the metal or acid of
equivalent strength are very useful. When the finishing point of a titration has
been overstepped (i.e., the assay has been "overdone"), a measured volume, say
5 or 10 c.c., of a solution containing the same metal may be added. The titration
can then be continued, but more cautiously, and the value in "c.c." for the
quantity added be deducted from the final reading.
Standardising.—Suppose the object is to standardise a solution of
permanganate similar to that referred to above. A convenient quantity of iron
(say 0.5 gram) would be weighed out, dissolved in dilute sulphuric acid, and the
solution titrated. Suppose 49.6 c.c. of the permanganate solution are required,
then
49.6 : 0.5 :: 100 : x
x = 1.008 gram.
This result, 1.008 gram, is the "standard." When a gas is measured, the standard
may be calculated in the same way. For example: with 0.224 gram of zinc, 75.8
c.c. of gas were obtained. Then the quantity of zinc equivalent to 100 c.c. of the
gas is got by the proportion.
75.8 : 0.224 :: 100 : x
x = 0.2955 gram.
Using the term "standard" in this sense, the following rules hold good:—
cylinder than in the litre flask. The solution is next transferred to a dry
"Winchester" bottle and labelled. The label may be rendered permanent by
waxing it.
Standard solutions should not be kept in a place exposed to direct sunlight.
Oxidising and reducing solutions, such as those of permanganate of potash,
ferrous sulphate, iodine, hyposulphite of soda, &c., gradually weaken in
strength; the solutions of other salts are more stable; while those of potassium
bichromate and baric chloride are almost permanent. Solutions of potassium
permanganate may be kept for a month or so without much change. The
solutions of hyposulphite of soda and of iodine should be examined weekly.
Ferrous sulphate solutions, if acidulated with sulphuric acid, may be depended
on for two or three weeks without fresh standardising. Before filling the burette,
the "Winchester" bottle should be well shaken and a portion of about 50 or 100
c.c. poured into a dry beaker or test-glass. Besides the standard solutions, which
are required for titrating an assay, permanent solutions of the metal or acid of
equivalent strength are very useful. When the finishing point of a titration has
been overstepped (i.e., the assay has been "overdone"), a measured volume, say
5 or 10 c.c., of a solution containing the same metal may be added. The titration
can then be continued, but more cautiously, and the value in "c.c." for the
quantity added be deducted from the final reading.
Standardising.—Suppose the object is to standardise a solution of
permanganate similar to that referred to above. A convenient quantity of iron
(say 0.5 gram) would be weighed out, dissolved in dilute sulphuric acid, and the
solution titrated. Suppose 49.6 c.c. of the permanganate solution are required,
then
49.6 : 0.5 :: 100 : x
x = 1.008 gram.
This result, 1.008 gram, is the "standard." When a gas is measured, the standard
may be calculated in the same way. For example: with 0.224 gram of zinc, 75.8
c.c. of gas were obtained. Then the quantity of zinc equivalent to 100 c.c. of the
gas is got by the proportion.
75.8 : 0.224 :: 100 : x
x = 0.2955 gram.
Using the term "standard" in this sense, the following rules hold good:—
Page 60
To find the weight of metal in a given substance:—Multiply the standard by the
number of c.c. used and divide by 100. For example: a piece of zinc was
dissolved and the gas evolved measured 73.9 c.c. Then by the rule, 0.2955 ×
73.9 / 100 should give the weight of the piece of zinc. This gives 0.2184 gram.
To find the percentage of metal in a given substance:—Multiply the standard by
the number of c.c. used and divide by the weight of substance taken. For
example: if 2 grams of a mineral were taken, and if on titrating with the
permanganate solution (standard 1.008) 60.4 c.c. were required, then
(1.008×60.4)/2 = 30.44. This is the percentage.
If the standard is exactly 1 gram, and 1 gram of ore is always taken, these
calculations become very simple. The "c.c." used give at once the percentage, or
divided by 100 give the weight of metal.
If it is desired to have a solution with a standard exactly 1.0 gram, it is best first
to make one rather stronger than this, and then to standardise carefully. Divide
1000 by the standard thus obtained and the result will be the number of c.c.
which must be taken and be diluted with water to 1 litre. For example: suppose
the standard is 1.008, then 1000/1.008 gives 992, and if 992 c.c. be taken and
diluted with water to 1000 c.c. a solution of the desired strength will be
obtained. The standard of this should be confirmed. A simpler calculation for the
same purpose is to multiply the standard by 1000; this will give the number of
c.c. to which 1 litre of the solution should be diluted. In the above example a
litre should be diluted to 1008 c.c.
It has been assumed in these rules that the titration has yielded proportional
results; but these are not always obtained. There can be no doubt that in any
actual re-action the proportion between any two re-agents is a fixed one, and that
if we double one of these then exactly twice as much of the other will enter into
the re-action; but in the working it may very well be that no re-action at all will
take place until after a certain excess of one or of both of the re-agents is
present. In titrating lead with a chromate of potash solution, for example, it is
possible that at the end of the titration a small quantity of the lead may remain
unacted on; and it is certain that a small excess of the chromate is present in the
solution. So, too, in precipitating a solution of silver with a standard solution of
common salt, a point is reached at which a small quantity of each remains in
solution; a further addition either of silver or of salt will cause a precipitate, and
a similar phenomenon has been observed in precipitating a hydrochloric acid
solution of a sulphate with baric chloride. The excess of one or other of the re-
agents may be large or small; or, in some cases, they may neutralise each other.
number of c.c. used and divide by 100. For example: a piece of zinc was
dissolved and the gas evolved measured 73.9 c.c. Then by the rule, 0.2955 ×
73.9 / 100 should give the weight of the piece of zinc. This gives 0.2184 gram.
To find the percentage of metal in a given substance:—Multiply the standard by
the number of c.c. used and divide by the weight of substance taken. For
example: if 2 grams of a mineral were taken, and if on titrating with the
permanganate solution (standard 1.008) 60.4 c.c. were required, then
(1.008×60.4)/2 = 30.44. This is the percentage.
If the standard is exactly 1 gram, and 1 gram of ore is always taken, these
calculations become very simple. The "c.c." used give at once the percentage, or
divided by 100 give the weight of metal.
If it is desired to have a solution with a standard exactly 1.0 gram, it is best first
to make one rather stronger than this, and then to standardise carefully. Divide
1000 by the standard thus obtained and the result will be the number of c.c.
which must be taken and be diluted with water to 1 litre. For example: suppose
the standard is 1.008, then 1000/1.008 gives 992, and if 992 c.c. be taken and
diluted with water to 1000 c.c. a solution of the desired strength will be
obtained. The standard of this should be confirmed. A simpler calculation for the
same purpose is to multiply the standard by 1000; this will give the number of
c.c. to which 1 litre of the solution should be diluted. In the above example a
litre should be diluted to 1008 c.c.
It has been assumed in these rules that the titration has yielded proportional
results; but these are not always obtained. There can be no doubt that in any
actual re-action the proportion between any two re-agents is a fixed one, and that
if we double one of these then exactly twice as much of the other will enter into
the re-action; but in the working it may very well be that no re-action at all will
take place until after a certain excess of one or of both of the re-agents is
present. In titrating lead with a chromate of potash solution, for example, it is
possible that at the end of the titration a small quantity of the lead may remain
unacted on; and it is certain that a small excess of the chromate is present in the
solution. So, too, in precipitating a solution of silver with a standard solution of
common salt, a point is reached at which a small quantity of each remains in
solution; a further addition either of silver or of salt will cause a precipitate, and
a similar phenomenon has been observed in precipitating a hydrochloric acid
solution of a sulphate with baric chloride. The excess of one or other of the re-
agents may be large or small; or, in some cases, they may neutralise each other.
Page 61
Considerations like these emphasise the necessity for uniformity in the mode of
working. Whether a process yields proportional results, or not, will be seen from
a series of standardisings. Having obtained these, the results should be arranged
as in the table, placing the quantities of metal used in the order of weight in the
first column, the volumes measured in the second, and the standards calculated
in the third. If the results are proportional, these standards will vary more or less,
according to the delicacy of the process, but there will be no apparent order in
the variation. The average of the standards should then be taken.
Weight. Volume found.Standard
0.2160 gram72.9 c.c. 0.2963
0.2185 " 73.9 " 0.2957
0.2365 " 79.9 " 0.2959
0.2440 " 82.3 " 0.2964
0.2555 " 85.9 " 0.2974
Any inclination that may be felt for obtaining an appearance of greater accuracy
by ignoring the last result must be resisted. For, although it would make no
practical difference whether the mean standard is taken as 0.2961 or 0.2963, it is
well not to ignore the possibility that an error of 0.4 c.c. may arise. A result
should only be ignored when the cause of its variation is known.
In this series the results are proportional, but the range of weights (0.216-0.2555
gram) is small. All processes yield fairly proportional results if the quantities
vary within narrow limits.
As to results which are not proportional, it is best to take some imaginary
examples, and then to apply the lesson to an actual one. A series of titrations of a
copper solution by means of a solution of potassic cyanide gave the following
results:—
Copper taken.Cyanide used. Standard.
0.1 gram 11.9 c.c. 0.8403
0.2 " 23.7 " 0.8438
0.3 " 35.6 " 0.8426
0.4 " 47.6 " 0.8403
These are proportional, but by using a larger quantity of acid and ammonia in
the work preliminary to titration, we might have had to use 1 c.c. of cyanide
working. Whether a process yields proportional results, or not, will be seen from
a series of standardisings. Having obtained these, the results should be arranged
as in the table, placing the quantities of metal used in the order of weight in the
first column, the volumes measured in the second, and the standards calculated
in the third. If the results are proportional, these standards will vary more or less,
according to the delicacy of the process, but there will be no apparent order in
the variation. The average of the standards should then be taken.
Weight. Volume found.Standard
0.2160 gram72.9 c.c. 0.2963
0.2185 " 73.9 " 0.2957
0.2365 " 79.9 " 0.2959
0.2440 " 82.3 " 0.2964
0.2555 " 85.9 " 0.2974
Any inclination that may be felt for obtaining an appearance of greater accuracy
by ignoring the last result must be resisted. For, although it would make no
practical difference whether the mean standard is taken as 0.2961 or 0.2963, it is
well not to ignore the possibility that an error of 0.4 c.c. may arise. A result
should only be ignored when the cause of its variation is known.
In this series the results are proportional, but the range of weights (0.216-0.2555
gram) is small. All processes yield fairly proportional results if the quantities
vary within narrow limits.
As to results which are not proportional, it is best to take some imaginary
examples, and then to apply the lesson to an actual one. A series of titrations of a
copper solution by means of a solution of potassic cyanide gave the following
results:—
Copper taken.Cyanide used. Standard.
0.1 gram 11.9 c.c. 0.8403
0.2 " 23.7 " 0.8438
0.3 " 35.6 " 0.8426
0.4 " 47.6 " 0.8403
These are proportional, but by using a larger quantity of acid and ammonia in
the work preliminary to titration, we might have had to use 1 c.c. of cyanide
Page 62
solution more in each case before the finishing point was reached. The results
would then have been:
Copper taken.Cyanide used. Standard.
0.1 gram 12.9 c.c. 0.7752
0.2 " 24.7 " 0.8097
0.3 " 36.6 " 0.8191
0.4 " 48.6 " 0.8230
It will be noted that the value of the standard increases with the weight of metal
used; and calculations from the mean standard will be incorrect.
By subtracting the lowest standardising from the highest, a third result is got free
from any error common to the other two; thus:—
0.4 gram= 48.6 c.c. "cyanide."
0.1 " = 12.9 " "
—— ——
0.3 " = 35.7 " "
And the standard calculated from this corrected result is 0.8404. Further, if 0.3
gram requires 35.7 c.c., then 0.1 gram should require 11.9 c.c., or 1.0 c.c. less
than that actually found.
We may therefore use the following rules for working processes which do not
yield proportional results. Make a series of two or three titrations, using very
different quantities of metal in each. Subtract the lowest of these from the
highest, and calculate the standard with the remainder. Calculate the volume
required by this standard in any case, and find the excess or deficit, as the case
may be. If an excess, subtract it from the result of each titration; if a deficit, add
it; and use the standard in the usual way. The following table shows an actual
example:—
Chalk taken. Gas obtained. Standard.
0.0873 gram17.8 c.c. 0.4904
0.1305 " 27.3 " 0.4780
0.1690 " 35.8 " 0.4721
0.1905 " 40.4 " 0.4715
0.2460 " 52.5 " 0.4686
would then have been:
Copper taken.Cyanide used. Standard.
0.1 gram 12.9 c.c. 0.7752
0.2 " 24.7 " 0.8097
0.3 " 36.6 " 0.8191
0.4 " 48.6 " 0.8230
It will be noted that the value of the standard increases with the weight of metal
used; and calculations from the mean standard will be incorrect.
By subtracting the lowest standardising from the highest, a third result is got free
from any error common to the other two; thus:—
0.4 gram= 48.6 c.c. "cyanide."
0.1 " = 12.9 " "
—— ——
0.3 " = 35.7 " "
And the standard calculated from this corrected result is 0.8404. Further, if 0.3
gram requires 35.7 c.c., then 0.1 gram should require 11.9 c.c., or 1.0 c.c. less
than that actually found.
We may therefore use the following rules for working processes which do not
yield proportional results. Make a series of two or three titrations, using very
different quantities of metal in each. Subtract the lowest of these from the
highest, and calculate the standard with the remainder. Calculate the volume
required by this standard in any case, and find the excess or deficit, as the case
may be. If an excess, subtract it from the result of each titration; if a deficit, add
it; and use the standard in the usual way. The following table shows an actual
example:—
Chalk taken. Gas obtained. Standard.
0.0873 gram17.8 c.c. 0.4904
0.1305 " 27.3 " 0.4780
0.1690 " 35.8 " 0.4721
0.1905 " 40.4 " 0.4715
0.2460 " 52.5 " 0.4686
Page 63
0.3000 " 64.0 " 0.4687
It will be seen that the standard decreases as the quantity of chalk increases; this
points to a deficiency in the quantity of gas evolved.
Then
0.3000 = 64.0 c.c.
0.0873 = 17.8 "
———= ——
0.2127 = 46.2 "
and 0.2127×100/46.2 = 0.4604. Then, multiplying the weight of chalk taken by
100, and dividing by 0.4604, we get the calculated results of the following table:
—
Chalk taken. Gas found. Gas calculated. Difference.
0.0873 gram17.8 c.c. 18.9 c.c. -1.1 c.c.
0.1305 " 27.3 " 28.3 " -1.0 "
0.1690 " 35.8 " 36.7 " -0.9 "
0.1905 " 40.4 " 41.4 " -1.0 "
0.2460 " 52.5 " 53.4 " -0.9 "
0.3000 " 64.0 " 65.1 " -1.1 "
By adding 1 c.c. to the quantity of gas obtained, and taking 0.4604 as the
standard, the calculated results will agree with those found with a variation of
0.1 c.c. When a large number of assays of the same kind are being made, this
method of calculation is convenient; when, however, only one or two
determinations are in question, it is easier to make a couple of standardisings,
taking quantities as nearly as possible the same as those present in the assays.
Sometimes it is necessary to draw up a table which will show, without
calculation, the weight of substance equivalent to a given volume of gas or of
solution. The substance used for standardising should be, whenever possible, a
pure sample of the substance to be determined—that is, for copper assays pure
copper should be used, for iron assays pure iron, and so on; but when this cannot
be got an impure substance may be used, provided it contains a known
percentage of the metal, and that the impurities present are not such as will
interfere with the accuracy of the assay. Including compounds with these, the
standard may be calculated by multiplying the standard got in the usual way, by
It will be seen that the standard decreases as the quantity of chalk increases; this
points to a deficiency in the quantity of gas evolved.
Then
0.3000 = 64.0 c.c.
0.0873 = 17.8 "
———= ——
0.2127 = 46.2 "
and 0.2127×100/46.2 = 0.4604. Then, multiplying the weight of chalk taken by
100, and dividing by 0.4604, we get the calculated results of the following table:
—
Chalk taken. Gas found. Gas calculated. Difference.
0.0873 gram17.8 c.c. 18.9 c.c. -1.1 c.c.
0.1305 " 27.3 " 28.3 " -1.0 "
0.1690 " 35.8 " 36.7 " -0.9 "
0.1905 " 40.4 " 41.4 " -1.0 "
0.2460 " 52.5 " 53.4 " -0.9 "
0.3000 " 64.0 " 65.1 " -1.1 "
By adding 1 c.c. to the quantity of gas obtained, and taking 0.4604 as the
standard, the calculated results will agree with those found with a variation of
0.1 c.c. When a large number of assays of the same kind are being made, this
method of calculation is convenient; when, however, only one or two
determinations are in question, it is easier to make a couple of standardisings,
taking quantities as nearly as possible the same as those present in the assays.
Sometimes it is necessary to draw up a table which will show, without
calculation, the weight of substance equivalent to a given volume of gas or of
solution. The substance used for standardising should be, whenever possible, a
pure sample of the substance to be determined—that is, for copper assays pure
copper should be used, for iron assays pure iron, and so on; but when this cannot
be got an impure substance may be used, provided it contains a known
percentage of the metal, and that the impurities present are not such as will
interfere with the accuracy of the assay. Including compounds with these, the
standard may be calculated by multiplying the standard got in the usual way, by
Page 64
the percentage of metal in the compound or impure substance, and dividing by
100. If, for example, the standard 1.008 gram was obtained by using a sample of
iron containing 99.7 per cent. of metal, the corrected standard would be
1.008×99.7/100 = 1.005.
In volumetric analysis the change brought about must be one in which the end of
the reaction is rendered prominent either by a change of colour or by the
presence or absence of a precipitate. If the end of the reaction or finishing-point
is not of itself visible, then it must be rendered visible by the use of a third
reagent called an indicator.
For example, the action of sulphuric acid upon soda results in nothing which
makes the action conspicuous; if, however, litmus or phenolphthalein be added
the change from blue to red in the first case, or from red to colourless in the
second, renders the finishing-point evident. Some indicators cannot be added to
the assay solution without spoiling the result; in which case portions of the assay
solution must be withdrawn from time to time and tested. This withdrawal of
portions of the assay solution, if rashly done, must result in loss; if, however, the
solution is not concentrated, and if the portions are only withdrawn towards the
end of the titration, the loss is very trifling, and will not show-up on the result.
The usual plan adopted is to have a solution of the indicator placed in drops at
fairly equal intervals distributed over a clean and dry white porcelain-plate: a
drop or two of the solution to be tested is then brought in contact with one of
these and the effect noted. Another plan is to have thin blotting-paper, moistened
with a solution of the indicator and dried; a drop of the solution to be tested
placed on this shows the characteristic change. When the assay solution contains
a suspended solid which interferes with the test, a prepared paper covered with
an ordinary filter-paper answers very well; a drop of the solution to be tested is
placed on the filter-paper, and, sinking through, shows its effect on the paper
below.
Except when otherwise stated, all titrations should be made at the ordinary
temperature; cooling, if necessary, by holding the flask under the tap. When a
titration is directed to be made in a boiling solution, it must be remembered that
the standard solution is cold, and that every addition lowers the temperature of
the assay.
On running the solution from the burette into the assay, do not let it run down
the side of the flask. If a portion of the assay has to be withdrawn for testing,
shake the flask to ensure mixing, and then take out a drop with the test-rod; the
neglect of these precautions may give a finishing-point too early. This is
100. If, for example, the standard 1.008 gram was obtained by using a sample of
iron containing 99.7 per cent. of metal, the corrected standard would be
1.008×99.7/100 = 1.005.
In volumetric analysis the change brought about must be one in which the end of
the reaction is rendered prominent either by a change of colour or by the
presence or absence of a precipitate. If the end of the reaction or finishing-point
is not of itself visible, then it must be rendered visible by the use of a third
reagent called an indicator.
For example, the action of sulphuric acid upon soda results in nothing which
makes the action conspicuous; if, however, litmus or phenolphthalein be added
the change from blue to red in the first case, or from red to colourless in the
second, renders the finishing-point evident. Some indicators cannot be added to
the assay solution without spoiling the result; in which case portions of the assay
solution must be withdrawn from time to time and tested. This withdrawal of
portions of the assay solution, if rashly done, must result in loss; if, however, the
solution is not concentrated, and if the portions are only withdrawn towards the
end of the titration, the loss is very trifling, and will not show-up on the result.
The usual plan adopted is to have a solution of the indicator placed in drops at
fairly equal intervals distributed over a clean and dry white porcelain-plate: a
drop or two of the solution to be tested is then brought in contact with one of
these and the effect noted. Another plan is to have thin blotting-paper, moistened
with a solution of the indicator and dried; a drop of the solution to be tested
placed on this shows the characteristic change. When the assay solution contains
a suspended solid which interferes with the test, a prepared paper covered with
an ordinary filter-paper answers very well; a drop of the solution to be tested is
placed on the filter-paper, and, sinking through, shows its effect on the paper
below.
Except when otherwise stated, all titrations should be made at the ordinary
temperature; cooling, if necessary, by holding the flask under the tap. When a
titration is directed to be made in a boiling solution, it must be remembered that
the standard solution is cold, and that every addition lowers the temperature of
the assay.
On running the solution from the burette into the assay, do not let it run down
the side of the flask. If a portion of the assay has to be withdrawn for testing,
shake the flask to ensure mixing, and then take out a drop with the test-rod; the
neglect of these precautions may give a finishing-point too early. This is
Page 65
generally indicated by a sudden finish, in which case on shaking the flask and
again testing no reaction is got. Do not remove the drop on the point of the
burette with the test-rod; let it remain where it is or drop it into the solution by
carefully opening the clip.
Generally the methods of working are as follows:—
(1) When the finishing-point depends on a change of colour in the solution.—
Increase the bulk of the assay up to from 100 to 150 c.c. with water. Boil or
cool, as the case may be. Run in the standard solution from a burette speedily,
until the re-agent appears to have a slower action, and shake or stir all the time.
Then run 1 c.c. or so at a time, still stirring, and finally add drops until the
colour change is got.
(2) When an outside-indicator is used.—Pour the standard solution from a
burette into the assay until 5 or 6 c.c. from the finishing-point; then run in 1 c.c.
at a time (stirring and testing on the plate between each) until the indicator
shows the change wanted, and deduct 0.5 c.c. for excess. When greater accuracy
is sought for a duplicate assay is made. In this case the standard solution is run
in close up to the end, and the operation is finished off with a few drops at a
time.
(3) Where the finishing-point depends upon the absence of a precipitate and no
outside-indicator is used.—As in the last case, run in the standard solution up to
within a few c.c. of the end, then run in 1 c.c. at a time until a precipitate is no
longer formed, but here 1.5 c.c. must be deducted for excess, since it is evident
that the whole of the last "c.c." must have been, and a portion of the previous
one may have been, in excess.
Indirect Titration.—The action of permanganate of potash upon a ferrous
solution is one of oxidation, hence it is evident that if any other oxidising agent
is present it will count as permanganate. In such a case the titration can be used
(indirectly) to estimate the quantity of such oxidising agent, by determining how
much less of the permanganate is used. For example, suppose that 1 gram of iron
dissolved in sulphuric acid requires 100 c.c. of standard permanganate to fully
oxidise it, but that the same amount of iron only requires 35.6 c.c. of the same
standard permanganate if it has been previously heated with 0.5 gram of black
oxide of manganese. Here it is evident that 0.5 gram of black oxide does the
work of 64.4 c.c.[4] of the permanganate solution, and that these quantities are
equivalent; moreover, if 64.4 c.c. correspond with 0.5 gram, then 100 c.c.
correspond with 0.7764 which is the standard. On theoretical grounds, and by a
again testing no reaction is got. Do not remove the drop on the point of the
burette with the test-rod; let it remain where it is or drop it into the solution by
carefully opening the clip.
Generally the methods of working are as follows:—
(1) When the finishing-point depends on a change of colour in the solution.—
Increase the bulk of the assay up to from 100 to 150 c.c. with water. Boil or
cool, as the case may be. Run in the standard solution from a burette speedily,
until the re-agent appears to have a slower action, and shake or stir all the time.
Then run 1 c.c. or so at a time, still stirring, and finally add drops until the
colour change is got.
(2) When an outside-indicator is used.—Pour the standard solution from a
burette into the assay until 5 or 6 c.c. from the finishing-point; then run in 1 c.c.
at a time (stirring and testing on the plate between each) until the indicator
shows the change wanted, and deduct 0.5 c.c. for excess. When greater accuracy
is sought for a duplicate assay is made. In this case the standard solution is run
in close up to the end, and the operation is finished off with a few drops at a
time.
(3) Where the finishing-point depends upon the absence of a precipitate and no
outside-indicator is used.—As in the last case, run in the standard solution up to
within a few c.c. of the end, then run in 1 c.c. at a time until a precipitate is no
longer formed, but here 1.5 c.c. must be deducted for excess, since it is evident
that the whole of the last "c.c." must have been, and a portion of the previous
one may have been, in excess.
Indirect Titration.—The action of permanganate of potash upon a ferrous
solution is one of oxidation, hence it is evident that if any other oxidising agent
is present it will count as permanganate. In such a case the titration can be used
(indirectly) to estimate the quantity of such oxidising agent, by determining how
much less of the permanganate is used. For example, suppose that 1 gram of iron
dissolved in sulphuric acid requires 100 c.c. of standard permanganate to fully
oxidise it, but that the same amount of iron only requires 35.6 c.c. of the same
standard permanganate if it has been previously heated with 0.5 gram of black
oxide of manganese. Here it is evident that 0.5 gram of black oxide does the
work of 64.4 c.c.[4] of the permanganate solution, and that these quantities are
equivalent; moreover, if 64.4 c.c. correspond with 0.5 gram, then 100 c.c.
correspond with 0.7764 which is the standard. On theoretical grounds, and by a
Page 66
method of calculation which will be explained further on (under the heading
"Calculations from Formulæ"), it can be found that if the standard for iron is 1
gram, that for the black oxide will be 0.7764 gram.
The principles of these indirect titrations become clearer when expressed in a
condensed form. Thus, in the example selected, and using the formulæ Fe =
Iron, KMnO4 = permanganate of potash, and MnO2 = oxide of manganese, we
have:—
(1) 1 gram Fe = 100 c.c. KMnO4
(2) 1 gram Fe = 35.6 c.c. KMnO4 + 0.5 gram MnO2
∴ 100 c.c. KMnO4 = 35.6 c.c. KMnO4 + 0.5 gram MnO2
(100 - 35.6) c.c. KMnO4 = 0.5 gram MnO2
64.4 c.c. KMnO4 = 0.5 gram MnO2
The iron does not enter into the calculation if the same quantity is present in the
two experiments.
An indirect titration thus requires three determinations, but if more than one
assay is to be carried on, two of these need not be repeated. The standard is
calculated in the usual way.
Colorimetric Assays.—These are assays in which the colour imparted to a
solution by some compound of the metal to be determined is taken advantage of;
the depth of colour depending on the quantity of metal present. They are
generally used for the determination of such small quantities as are too minute to
be weighed. The method of working is as follows:—A measured portion of the
assay solution (generally 2/3, 1/2, 1/3, or 1/4 of the whole), coloured by the
substance to be estimated, is placed in a white glass cylinder standing on a sheet
of white paper or glazed porcelain. Into an exactly similar cylinder is placed the
same amount of re-agents, &c., as the portion of the assay solution contains, and
then water is added until the solutions are of nearly equal bulk. Next, a standard
solution of the metal being estimated is run in from a burette, the mixture being
stirred after each addition until the colour approaches that of the assay. The bulk
of the two solutions is equalised by adding water. Then more standard solution is
added until the tints are very nearly alike. Next, the amount added is read off
from the burette, still more is poured in until the colour is slightly darker than
that of the assay, and the burette read off again. The mean of the readings is
taken, and gives the quantity of metal added. It equals the quantity of metal in
"Calculations from Formulæ"), it can be found that if the standard for iron is 1
gram, that for the black oxide will be 0.7764 gram.
The principles of these indirect titrations become clearer when expressed in a
condensed form. Thus, in the example selected, and using the formulæ Fe =
Iron, KMnO4 = permanganate of potash, and MnO2 = oxide of manganese, we
have:—
(1) 1 gram Fe = 100 c.c. KMnO4
(2) 1 gram Fe = 35.6 c.c. KMnO4 + 0.5 gram MnO2
∴ 100 c.c. KMnO4 = 35.6 c.c. KMnO4 + 0.5 gram MnO2
(100 - 35.6) c.c. KMnO4 = 0.5 gram MnO2
64.4 c.c. KMnO4 = 0.5 gram MnO2
The iron does not enter into the calculation if the same quantity is present in the
two experiments.
An indirect titration thus requires three determinations, but if more than one
assay is to be carried on, two of these need not be repeated. The standard is
calculated in the usual way.
Colorimetric Assays.—These are assays in which the colour imparted to a
solution by some compound of the metal to be determined is taken advantage of;
the depth of colour depending on the quantity of metal present. They are
generally used for the determination of such small quantities as are too minute to
be weighed. The method of working is as follows:—A measured portion of the
assay solution (generally 2/3, 1/2, 1/3, or 1/4 of the whole), coloured by the
substance to be estimated, is placed in a white glass cylinder standing on a sheet
of white paper or glazed porcelain. Into an exactly similar cylinder is placed the
same amount of re-agents, &c., as the portion of the assay solution contains, and
then water is added until the solutions are of nearly equal bulk. Next, a standard
solution of the metal being estimated is run in from a burette, the mixture being
stirred after each addition until the colour approaches that of the assay. The bulk
of the two solutions is equalised by adding water. Then more standard solution is
added until the tints are very nearly alike. Next, the amount added is read off
from the burette, still more is poured in until the colour is slightly darker than
that of the assay, and the burette read off again. The mean of the readings is
taken, and gives the quantity of metal added. It equals the quantity of metal in
Page 67
the portion of the assay. If this portion was one-half of the whole, multiply by
two; if one-third, multiply by three, and so on. When the quantity of metal in
very dilute solutions is to be determined, it is sometimes necessary to
concentrate the solutions by boiling them down before applying the re-agent
which produces the coloured compound. Such concentration does not affect the
calculations.
Gasometric Assays.—Gasometric methods are not much used by assayers, and,
therefore, those students who wish to study them more fully than the limits of
this work will permit, are recommended to consult Winkler and Lunge's text-
book on the subject. The methods are without doubt capable of a more extended
application. In measuring liquids, ordinary variations of temperature have but
little effect, and variations of atmospheric pressure have none at all, whereas
with gases it is different. Thus, 100 c.c. of an ordinary aqueous solution would,
if heated from 10° C. to 20° C., expand to about 100.15 c.c. 100 c.c. of a gas
similarly warmed would expand to about 103.5 c.c., and a fall of one inch in the
barometer would have a very similar effect. And in measuring gases we have not
only to take into account variations in volume due to changes in temperature and
atmospheric pressure, but also that which is observed when a gas is measured
wet and dry. Water gives off vapour at all temperatures, but the amount of
vapour is larger as the temperature increases.
By ignoring these considerations, errors of 3 or 4 per cent. are easily made; but,
fortunately, the corrections are simple, and it is easy to construct a piece of
apparatus by means of which they may be reduced to a simple calculation by the
rule of three.
The volume of a gas is, in practice, usually reduced to that which it would be at
a temperature of 0° C., when the column of mercury in the barometer is 760
mm. high. But, although convenient, this practice is not always necessary. The
only thing required is some way of checking the variations in volume, and of
calculating what the corrected volume would be under certain fixed conditions.
Suppose that at the time a series of standardisings is being made, 100 c.c. of air
were confined in a graduated tube over moist mercury. These 100 c.c. would
vary in volume from day to day, but it would always be true of them that they
would measure 100 c.c. under the same conditions as those under which the
standardisings were made. If, then, in making an actual assay, 35.4 c.c. of gas
were obtained, and the air in the tube measured 105 c.c., we should be justified
in saying, that if the conditions had been those of the standardising, the 105 c.c.
would have measured 100 c.c., and the 35.4 c.c. would have been 33.7; for 105:
two; if one-third, multiply by three, and so on. When the quantity of metal in
very dilute solutions is to be determined, it is sometimes necessary to
concentrate the solutions by boiling them down before applying the re-agent
which produces the coloured compound. Such concentration does not affect the
calculations.
Gasometric Assays.—Gasometric methods are not much used by assayers, and,
therefore, those students who wish to study them more fully than the limits of
this work will permit, are recommended to consult Winkler and Lunge's text-
book on the subject. The methods are without doubt capable of a more extended
application. In measuring liquids, ordinary variations of temperature have but
little effect, and variations of atmospheric pressure have none at all, whereas
with gases it is different. Thus, 100 c.c. of an ordinary aqueous solution would,
if heated from 10° C. to 20° C., expand to about 100.15 c.c. 100 c.c. of a gas
similarly warmed would expand to about 103.5 c.c., and a fall of one inch in the
barometer would have a very similar effect. And in measuring gases we have not
only to take into account variations in volume due to changes in temperature and
atmospheric pressure, but also that which is observed when a gas is measured
wet and dry. Water gives off vapour at all temperatures, but the amount of
vapour is larger as the temperature increases.
By ignoring these considerations, errors of 3 or 4 per cent. are easily made; but,
fortunately, the corrections are simple, and it is easy to construct a piece of
apparatus by means of which they may be reduced to a simple calculation by the
rule of three.
The volume of a gas is, in practice, usually reduced to that which it would be at
a temperature of 0° C., when the column of mercury in the barometer is 760
mm. high. But, although convenient, this practice is not always necessary. The
only thing required is some way of checking the variations in volume, and of
calculating what the corrected volume would be under certain fixed conditions.
Suppose that at the time a series of standardisings is being made, 100 c.c. of air
were confined in a graduated tube over moist mercury. These 100 c.c. would
vary in volume from day to day, but it would always be true of them that they
would measure 100 c.c. under the same conditions as those under which the
standardisings were made. If, then, in making an actual assay, 35.4 c.c. of gas
were obtained, and the air in the tube measured 105 c.c., we should be justified
in saying, that if the conditions had been those of the standardising, the 105 c.c.
would have measured 100 c.c., and the 35.4 c.c. would have been 33.7; for 105:
Page 68
100:: 35.4: 33.7. The rule for using such a piece of apparatus for correcting
volumes is:—Multiply the c.c. of gas obtained by 100, and divide by the number
of c.c. of air in the apparatus.
If it is desired to calculate the volumes under standard conditions (that is, the gas
dry, at 0° C. and 760 mm. barometric pressure) the calculations are easily
performed, but the temperature and pressure must be known.
Correction for Moisture.—The "vapour tension" of water has been accurately
determined for various temperatures, and it may be looked upon as
counteracting the barometric pressure. For example, at 15° C. the vapour tension
equals 12.7 millimetres of mercury; if the barometer stood at 750 mm., the
correction for moisture would be made by subtracting 12.7 from 750, and taking
737.3 mm. to be the true barometric pressure.
The vapour tensions for temperatures from 0° C. to 20° C. are as follows:—
Temp. Tension. Temp. Tension. Temp. Tension.
0° 4.6 mm. 7° 7.5 mm. 14° 11.9 mm.
1° 4.9 mm. 8° 8.0 mm. 15° 12.7 mm.
2° 5.3 mm. 9° 8.6 mm. 16° 13.5 mm.
3° 5.7 mm. 10° 9.2 mm. 17° 14.4 mm.
4° 6.1 mm. 11° 9.8 mm. 18° 15.3 mm.
5° 6.5 mm. 12° 10.5 mm. 19° 16.3 mm.
6° 7.0 mm. 13° 11.2 mm. 20° 17.4 mm.
The correction for pressure is:—Multiply the volume by the actual pressure and
divide by 760.
The correction for temperature:—Multiply the volume by 273 and divide by the
temperature (in degrees Centigrade) added to 273.
For all three corrections the following rules hold good. To reduce to 0° C. and
760 mm. dry.
Volume × 0.3592 × (Pressure-tension)
Corrected volume = ———————————————————
Temperature + 273
To find the volume, which a given volume under standard conditions would
assume, if those conditions are altered.
volumes is:—Multiply the c.c. of gas obtained by 100, and divide by the number
of c.c. of air in the apparatus.
If it is desired to calculate the volumes under standard conditions (that is, the gas
dry, at 0° C. and 760 mm. barometric pressure) the calculations are easily
performed, but the temperature and pressure must be known.
Correction for Moisture.—The "vapour tension" of water has been accurately
determined for various temperatures, and it may be looked upon as
counteracting the barometric pressure. For example, at 15° C. the vapour tension
equals 12.7 millimetres of mercury; if the barometer stood at 750 mm., the
correction for moisture would be made by subtracting 12.7 from 750, and taking
737.3 mm. to be the true barometric pressure.
The vapour tensions for temperatures from 0° C. to 20° C. are as follows:—
Temp. Tension. Temp. Tension. Temp. Tension.
0° 4.6 mm. 7° 7.5 mm. 14° 11.9 mm.
1° 4.9 mm. 8° 8.0 mm. 15° 12.7 mm.
2° 5.3 mm. 9° 8.6 mm. 16° 13.5 mm.
3° 5.7 mm. 10° 9.2 mm. 17° 14.4 mm.
4° 6.1 mm. 11° 9.8 mm. 18° 15.3 mm.
5° 6.5 mm. 12° 10.5 mm. 19° 16.3 mm.
6° 7.0 mm. 13° 11.2 mm. 20° 17.4 mm.
The correction for pressure is:—Multiply the volume by the actual pressure and
divide by 760.
The correction for temperature:—Multiply the volume by 273 and divide by the
temperature (in degrees Centigrade) added to 273.
For all three corrections the following rules hold good. To reduce to 0° C. and
760 mm. dry.
Volume × 0.3592 × (Pressure-tension)
Corrected volume = ———————————————————
Temperature + 273
To find the volume, which a given volume under standard conditions would
assume, if those conditions are altered.
Page 69
Volume × 2.784 × (Temperature + 273)
Resulting volume = ——————————————————
Pressure - tension
As an example, we will suppose that it is desired to enclose in the apparatus
referred to on p. 45, a volume of air, which, when dry (at 0° C. and 760 mm.),
shall measure 100 c.c., whilst the actual temperature is 15° C., and the pressure
750 mm.
The second formula is the one to be used, and we get 108.7 c.c.
100 c.c.×2.784×288
Required volume = ———————————
750-12.7
80179.2
= ————
737.3
= 108.7 c.c.
FOOTNOTES:
[4] 100-35.6 = 64.4.
Resulting volume = ——————————————————
Pressure - tension
As an example, we will suppose that it is desired to enclose in the apparatus
referred to on p. 45, a volume of air, which, when dry (at 0° C. and 760 mm.),
shall measure 100 c.c., whilst the actual temperature is 15° C., and the pressure
750 mm.
The second formula is the one to be used, and we get 108.7 c.c.
100 c.c.×2.784×288
Required volume = ———————————
750-12.7
80179.2
= ————
737.3
= 108.7 c.c.
FOOTNOTES:
[4] 100-35.6 = 64.4.
Page 70
CHAPTER V.
WEIGHING AND MEASURING.
Weighing.—The system of weights and measures which we have adopted is the
French or metric system; in this the gram (15.43 grains) is the unit of weight; the
only other weight frequently referred to is the milligram, which is 0.001, or
1/1000 gram. The unit of volume is the cubic centimetre, which is
approximately the volume of 1 gram of water, and which thus bears to the gram
the same relation as grain-measures bear to grains. It is usual to write and even
pronounce cubic centimetre shortly as c.c., and the only other denomination of
volume we shall have occasion to use is the "litre," which measures 1000 c.c.,
and is roughly 1-3/4 pints.
The weights used are kept in boxes in a definite order, so that the weights on the
balance can be counted as well by noting those which are absent from the box as
by counting those present on the scale-pan. The weights run 50, 20, 10, 10, 5, 2,
1, 1 and 1 grams, and are formed of brass. The fractions of the gram are
generally made of platinum or of aluminium, and are arranged in the following
order:—0.5, 0.2, 0.1, 0.1, and 0.05, 0.02, 0.01, 0.01. These may be marked in
this way, or they may be marked 500, 200, 100, 100, 50, 20, 10, 10; the 500
meaning 500 milligrams.
Some makers send out weights in the series 50, 20, 20, 10, &c.
Weights of less than 0.01 gram are generally present in a box, but it is much
more convenient to work with a rider. This is a piece of wire which in the pan
weighs 0.01 gram; it is made in such a form that it will ride on the beam, and its
effective weight decreases as it approaches the centre. If the arm of the beam is
divided into tenths, then each tenth counting from the centre outward equals
0.001 gram or 1 milligram, and if these tenths be further subdivided the fractions
of a milligram are obtained; and these give figures in the fourth place of
decimals. A fairly good balance should be sensitive to 0.0001 gram. The weights
must never be touched with the fingers, and the forceps for moving them is used
for no other purpose. When not in actual use the box is kept closed. The weights
must not be allowed to remain on the pan of the balance. The balance-case must
not be open without some reason. It must be fixed level, and, once fixed, must
WEIGHING AND MEASURING.
Weighing.—The system of weights and measures which we have adopted is the
French or metric system; in this the gram (15.43 grains) is the unit of weight; the
only other weight frequently referred to is the milligram, which is 0.001, or
1/1000 gram. The unit of volume is the cubic centimetre, which is
approximately the volume of 1 gram of water, and which thus bears to the gram
the same relation as grain-measures bear to grains. It is usual to write and even
pronounce cubic centimetre shortly as c.c., and the only other denomination of
volume we shall have occasion to use is the "litre," which measures 1000 c.c.,
and is roughly 1-3/4 pints.
The weights used are kept in boxes in a definite order, so that the weights on the
balance can be counted as well by noting those which are absent from the box as
by counting those present on the scale-pan. The weights run 50, 20, 10, 10, 5, 2,
1, 1 and 1 grams, and are formed of brass. The fractions of the gram are
generally made of platinum or of aluminium, and are arranged in the following
order:—0.5, 0.2, 0.1, 0.1, and 0.05, 0.02, 0.01, 0.01. These may be marked in
this way, or they may be marked 500, 200, 100, 100, 50, 20, 10, 10; the 500
meaning 500 milligrams.
Some makers send out weights in the series 50, 20, 20, 10, &c.
Weights of less than 0.01 gram are generally present in a box, but it is much
more convenient to work with a rider. This is a piece of wire which in the pan
weighs 0.01 gram; it is made in such a form that it will ride on the beam, and its
effective weight decreases as it approaches the centre. If the arm of the beam is
divided into tenths, then each tenth counting from the centre outward equals
0.001 gram or 1 milligram, and if these tenths be further subdivided the fractions
of a milligram are obtained; and these give figures in the fourth place of
decimals. A fairly good balance should be sensitive to 0.0001 gram. The weights
must never be touched with the fingers, and the forceps for moving them is used
for no other purpose. When not in actual use the box is kept closed. The weights
must not be allowed to remain on the pan of the balance. The balance-case must
not be open without some reason. It must be fixed level, and, once fixed, must
Page 71
not be needlessly moved. The bench on which it stands should be used for no
other purpose, and no one should be allowed to lean upon it.
When using a balance sit directly in front of it. Ordinarily the substance to be
weighed is best put on the pan to the user's left; the weights and the rider are
then easily manipulated. Powders, &c., should not be weighed directly on the
balance; a counterpoised watch-glass or metal scoop (fig. 25) should be used. In
some cases it is advisable to use a weighing-bottle. This is a light, well-
stoppered bottle (fig. 3) containing the powdered ore. It is first filled and
weighed; then some of the substance is carefully poured from it into a beaker or
other vessel, and it is weighed again; the difference in the two weighings gives
the weight of substance taken. A substance must always be cold when weighed,
and large glass vessels should be allowed to stand in the balance-box a little
while before being weighed. Always have the balance at rest when putting on or
taking off anything from the pans. Put the weights on systematically. In using
the rider (except you have a reason to the contrary), put it on at the 5; if this is
too much, then try it at the 3; if then the weights are too little, try at the 4, if still
not enough, the correct weight must be between the 4 and 5; try half-way
between.
It is best to work with the balance vibrating; equilibrium is established when the
vibration to the left is the mean of the preceding and succeeding vibrations to the
right. For example, if it vibrates 6 divisions to the right on one swing, and 5
divisions on the next, the intermediate vibration to the left should have been 5-
1/2.
Note whether the substance increases in weight whilst on the balance. If it does
it may be because it was put on warm, and is cooling, or it may be because it is
taking up moisture from the air. Substances which take up moisture rapidly
should be weighed in clipped watch-glasses or in light-weighing bottles or tubes.
Students, in recording the weights, should first read off those missing from the
box, writing down each order of figures as determined; first tens, then units, and
so on. Remember that the first four platinum weights give the figures of the first
other purpose, and no one should be allowed to lean upon it.
When using a balance sit directly in front of it. Ordinarily the substance to be
weighed is best put on the pan to the user's left; the weights and the rider are
then easily manipulated. Powders, &c., should not be weighed directly on the
balance; a counterpoised watch-glass or metal scoop (fig. 25) should be used. In
some cases it is advisable to use a weighing-bottle. This is a light, well-
stoppered bottle (fig. 3) containing the powdered ore. It is first filled and
weighed; then some of the substance is carefully poured from it into a beaker or
other vessel, and it is weighed again; the difference in the two weighings gives
the weight of substance taken. A substance must always be cold when weighed,
and large glass vessels should be allowed to stand in the balance-box a little
while before being weighed. Always have the balance at rest when putting on or
taking off anything from the pans. Put the weights on systematically. In using
the rider (except you have a reason to the contrary), put it on at the 5; if this is
too much, then try it at the 3; if then the weights are too little, try at the 4, if still
not enough, the correct weight must be between the 4 and 5; try half-way
between.
It is best to work with the balance vibrating; equilibrium is established when the
vibration to the left is the mean of the preceding and succeeding vibrations to the
right. For example, if it vibrates 6 divisions to the right on one swing, and 5
divisions on the next, the intermediate vibration to the left should have been 5-
1/2.
Note whether the substance increases in weight whilst on the balance. If it does
it may be because it was put on warm, and is cooling, or it may be because it is
taking up moisture from the air. Substances which take up moisture rapidly
should be weighed in clipped watch-glasses or in light-weighing bottles or tubes.
Students, in recording the weights, should first read off those missing from the
box, writing down each order of figures as determined; first tens, then units, and
so on. Remember that the first four platinum weights give the figures of the first
Page 72
place of decimals, the second four give the second place, and that the third and
fourth places are given by the rider. Having taken down the figures, confirm
them by reading off the weights as you put them back into the box. Do not rest a
weight on the palm of your hand for convenience in reading the mark upon it.
Remember one weight lost from a box spoils the set. Do not take it for granted
that the balance is in equilibrium before you start weighing: try it.
Measuring Liquids.—For coarse work, such as measuring acids for dissolving
ores, graduated glasses similar to those used by druggists may be used. It is well
to have two sizes—a smaller graduated into divisions of 5 c.c. (fig. 26), and a
larger with divisions equal to 10 c.c. No measurement of importance should be
made in a vessel of this kind, as a slight variation in level causes a serious error.
Graduated flasks must be used when anything has to be made up to a definite
bulk, or when a fixed volume has to be collected. If, for example, a certain
weight of substance has to be dissolved and diluted to a litre, or if the first 50
c.c. of a distillate has to be collected, a flask should be used. Each flask is
graduated for one particular quantity; the most useful sizes are 1000 c.c., 500
c.c., 200 c.c., 100 c.c., and 50 c.c. The mark should be in the narrowest part of
the neck, and should be tangential to the curved surface of the liquid when the
fourth places are given by the rider. Having taken down the figures, confirm
them by reading off the weights as you put them back into the box. Do not rest a
weight on the palm of your hand for convenience in reading the mark upon it.
Remember one weight lost from a box spoils the set. Do not take it for granted
that the balance is in equilibrium before you start weighing: try it.
Measuring Liquids.—For coarse work, such as measuring acids for dissolving
ores, graduated glasses similar to those used by druggists may be used. It is well
to have two sizes—a smaller graduated into divisions of 5 c.c. (fig. 26), and a
larger with divisions equal to 10 c.c. No measurement of importance should be
made in a vessel of this kind, as a slight variation in level causes a serious error.
Graduated flasks must be used when anything has to be made up to a definite
bulk, or when a fixed volume has to be collected. If, for example, a certain
weight of substance has to be dissolved and diluted to a litre, or if the first 50
c.c. of a distillate has to be collected, a flask should be used. Each flask is
graduated for one particular quantity; the most useful sizes are 1000 c.c., 500
c.c., 200 c.c., 100 c.c., and 50 c.c. The mark should be in the narrowest part of
the neck, and should be tangential to the curved surface of the liquid when the
Page 73
flask contains the exact volume specified. The level of a curved surface of liquid
is at first somewhat difficult to read: the beginner is in doubt whether the surface
should be taken at a, b, or c (fig. 27). It is best to take the lowest reading c. In
some lights it is difficult to find this; in such cases a piece of white paper or card
held behind and a little below, so as to throw light up and against the curved
surface, will render it clear. In reading, one should look neither up at nor down
upon the surface, but the eye should be on the same level with it. It must be kept
in mind that flasks contain the quantity specified, but deliver less than this by
the amount remaining in them and damping the sides. If it is desired to transfer
the contents say of a 100 c.c. flask to a beaker, it will be necessary to complete
the transfer by rinsing out the flask and adding the washings; otherwise there
will be a sensible loss. Graduated cylinders (fig. 28) are convenient for
preparing standard solutions.
is at first somewhat difficult to read: the beginner is in doubt whether the surface
should be taken at a, b, or c (fig. 27). It is best to take the lowest reading c. In
some lights it is difficult to find this; in such cases a piece of white paper or card
held behind and a little below, so as to throw light up and against the curved
surface, will render it clear. In reading, one should look neither up at nor down
upon the surface, but the eye should be on the same level with it. It must be kept
in mind that flasks contain the quantity specified, but deliver less than this by
the amount remaining in them and damping the sides. If it is desired to transfer
the contents say of a 100 c.c. flask to a beaker, it will be necessary to complete
the transfer by rinsing out the flask and adding the washings; otherwise there
will be a sensible loss. Graduated cylinders (fig. 28) are convenient for
preparing standard solutions.
Page 74
Pipettes and burettes are graduated to deliver the quantities specified. The
principle of the pipette, and the advantages and disadvantages of its various
forms, may be understood by considering the first form shown in fig. 29. It is
essentially a bulbed tube drawn out to a jet at its lower end, and having on each
principle of the pipette, and the advantages and disadvantages of its various
forms, may be understood by considering the first form shown in fig. 29. It is
essentially a bulbed tube drawn out to a jet at its lower end, and having on each
Page 75
side of the bulb a mark so placed that when the surface of the liquid falls from
the upper to the lower mark the instrument shall deliver exactly 100 c.c. The
bore of the jet should be of such a size as will allow the level of the liquid to fall
at the rate of about one foot in two minutes. If it runs more quickly than this, an
appreciable error arises from the varying amount of liquid remaining, and
damping the sides of the bulb. The flow of liquid from a pipette must not be
hastened by blowing into it. The lower tube or nose of the pipette should be long
enough to reach into the bottle or flask containing the liquid about to be
measured. The pipette is filled by sucking at the open end with the mouth; this
method of filling renders the use of the instrument dangerous for such liquids as
strong acids, ammonia, and such poisonous solutions as that of potassic cyanide.
One attempt with a fairly strong solution of ammonia will teach the beginner a
very useful lesson. As soon as the liquid rises above the upper mark in the
pipette, the mouth is withdrawn, and the pipette quickly closed by pressing the
upper aperture with the index finger of the right hand; it is well to have the
finger slightly moist, but not damp. The neck of the pipette should be long
enough to allow its being firmly grasped by the fingers and thumb of the right
hand without inconvenience. The pipette is first held in a vertical position long
enough to allow any moisture outside the tube to run down, and then the liquid
is allowed to run out to the level of the upper mark; this is easily effected by
lessening the pressure. If the finger is wet, the flow will be jerky, and good work
impossible. The pipette is next held over the vessel into which the 100 c.c. are to
be put, and the liquid allowed to run out. When the bulb is nearly empty, the
flow should be checked by replacing the finger, and the liquid allowed to escape
slowly until the lower mark is reached. The pipette is then withdrawn; it is in the
withdrawing that the disadvantage of this particular form[5] makes itself felt. It
must be withdrawn very steadily, as the slightest shock causes the remaining
column of liquid to vibrate, whereby air is drawn in and the liquid is forced out.
This disadvantage is got rid of by making the mouth of the jet the lower limit,
or, in other words, allowing the instrument to empty itself. There are two forms
of such pipettes; in the one generally recommended in Gay-Lussac's silver assay
(the last shown in fig. 29) the nose is replaced by a jet. This is most conveniently
filled by stopping the jet with the finger, and allowing the liquid to flow in a fine
stream into the neck until the pipette is filled, and then working as just
described. The other form is the one in general use; in fact, a long nose to a
pipette is so convenient that it may almost be said to be necessary. But the
accuracy is slightly diminished; a long narrow tube makes a poor measuring
instrument because of the amount of liquid it finally retains. A defect possessed
by both forms is the retention of a drop of varying size in the nozzle. Whatever
the upper to the lower mark the instrument shall deliver exactly 100 c.c. The
bore of the jet should be of such a size as will allow the level of the liquid to fall
at the rate of about one foot in two minutes. If it runs more quickly than this, an
appreciable error arises from the varying amount of liquid remaining, and
damping the sides of the bulb. The flow of liquid from a pipette must not be
hastened by blowing into it. The lower tube or nose of the pipette should be long
enough to reach into the bottle or flask containing the liquid about to be
measured. The pipette is filled by sucking at the open end with the mouth; this
method of filling renders the use of the instrument dangerous for such liquids as
strong acids, ammonia, and such poisonous solutions as that of potassic cyanide.
One attempt with a fairly strong solution of ammonia will teach the beginner a
very useful lesson. As soon as the liquid rises above the upper mark in the
pipette, the mouth is withdrawn, and the pipette quickly closed by pressing the
upper aperture with the index finger of the right hand; it is well to have the
finger slightly moist, but not damp. The neck of the pipette should be long
enough to allow its being firmly grasped by the fingers and thumb of the right
hand without inconvenience. The pipette is first held in a vertical position long
enough to allow any moisture outside the tube to run down, and then the liquid
is allowed to run out to the level of the upper mark; this is easily effected by
lessening the pressure. If the finger is wet, the flow will be jerky, and good work
impossible. The pipette is next held over the vessel into which the 100 c.c. are to
be put, and the liquid allowed to run out. When the bulb is nearly empty, the
flow should be checked by replacing the finger, and the liquid allowed to escape
slowly until the lower mark is reached. The pipette is then withdrawn; it is in the
withdrawing that the disadvantage of this particular form[5] makes itself felt. It
must be withdrawn very steadily, as the slightest shock causes the remaining
column of liquid to vibrate, whereby air is drawn in and the liquid is forced out.
This disadvantage is got rid of by making the mouth of the jet the lower limit,
or, in other words, allowing the instrument to empty itself. There are two forms
of such pipettes; in the one generally recommended in Gay-Lussac's silver assay
(the last shown in fig. 29) the nose is replaced by a jet. This is most conveniently
filled by stopping the jet with the finger, and allowing the liquid to flow in a fine
stream into the neck until the pipette is filled, and then working as just
described. The other form is the one in general use; in fact, a long nose to a
pipette is so convenient that it may almost be said to be necessary. But the
accuracy is slightly diminished; a long narrow tube makes a poor measuring
instrument because of the amount of liquid it finally retains. A defect possessed
by both forms is the retention of a drop of varying size in the nozzle. Whatever
Page 76
method is adopted for removing this drop must be always adhered to. The most
convenient form is the one last described, and the most useful sizes are 100 c.c.,
50 c.c., 20 c.c., 10 c.c., and 5 c.c. Ten c.c. pipettes graduated into tenths of a
cubic centimetre are very useful: those are best in which the graduation stops
short of the bottom.
All measurements should be made at the ordinary temperature; and, before being
used, the pipette should be rinsed out with a cubic centimetre or so of the
solution to be measured. After using, it should be washed out with water.
Burettes differ mainly from pipettes in having the flow of liquid controlled from
below instead of from above. The best form is that known as Mohr's, one kind of
which is provided with a glass stopcock, while the other has a piece of india-
rubber tube compressed by a clip. The latter cannot be used for solutions of
permanganate of potash or of iodine, or of any substance which acts on india-
rubber; but in other respects there is little to choose between the two kinds. A
burette delivering 100 c.c., and graduated into fifths (i.e., each division = 0.2
c.c.), is a very convenient size. For some kinds of work, 50 c.c. divided into
tenths (i.e., each division = 0.1 c.c.) may be selected.
Burettes may be fixed in any convenient stand; they must be vertical and should
be so placed that the assayer can read any part of the graduated scale without
straining. When not in use, they should be kept full of water. When using a
burette, the water must be run out; the burette is next rinsed with some of the
solution to be used, and drained; and then it is filled with the solution. Next
squeeze the india-rubber tube so as to disentangle air-bubbles and, by smartly
opening the clip, allow the tube and jet to be filled; see that no bubbles of air are
left. Then run out cautiously until the level of the liquid in the burette stands at
zero. In reading the level with very dark-coloured liquids it is convenient to read
from the level a (fig. 27), and, provided it is done in each reading, there is no
objection to this. The accuracy of the reading of a burette is sensibly increased
by the use of an Erdmann float. This is an elongated bulb, weighted with
mercury, and fitting (somewhat loosely) the tube of the burette. It floats in the
solution, and is marked with a horizontal line; this line is taken as the level of
the liquid. If the burette is filled from the top, the float rises with aggravating
slowness, and this is its chief disadvantage. The float must come to rest before
any reading is made.
convenient form is the one last described, and the most useful sizes are 100 c.c.,
50 c.c., 20 c.c., 10 c.c., and 5 c.c. Ten c.c. pipettes graduated into tenths of a
cubic centimetre are very useful: those are best in which the graduation stops
short of the bottom.
All measurements should be made at the ordinary temperature; and, before being
used, the pipette should be rinsed out with a cubic centimetre or so of the
solution to be measured. After using, it should be washed out with water.
Burettes differ mainly from pipettes in having the flow of liquid controlled from
below instead of from above. The best form is that known as Mohr's, one kind of
which is provided with a glass stopcock, while the other has a piece of india-
rubber tube compressed by a clip. The latter cannot be used for solutions of
permanganate of potash or of iodine, or of any substance which acts on india-
rubber; but in other respects there is little to choose between the two kinds. A
burette delivering 100 c.c., and graduated into fifths (i.e., each division = 0.2
c.c.), is a very convenient size. For some kinds of work, 50 c.c. divided into
tenths (i.e., each division = 0.1 c.c.) may be selected.
Burettes may be fixed in any convenient stand; they must be vertical and should
be so placed that the assayer can read any part of the graduated scale without
straining. When not in use, they should be kept full of water. When using a
burette, the water must be run out; the burette is next rinsed with some of the
solution to be used, and drained; and then it is filled with the solution. Next
squeeze the india-rubber tube so as to disentangle air-bubbles and, by smartly
opening the clip, allow the tube and jet to be filled; see that no bubbles of air are
left. Then run out cautiously until the level of the liquid in the burette stands at
zero. In reading the level with very dark-coloured liquids it is convenient to read
from the level a (fig. 27), and, provided it is done in each reading, there is no
objection to this. The accuracy of the reading of a burette is sensibly increased
by the use of an Erdmann float. This is an elongated bulb, weighted with
mercury, and fitting (somewhat loosely) the tube of the burette. It floats in the
solution, and is marked with a horizontal line; this line is taken as the level of
the liquid. If the burette is filled from the top, the float rises with aggravating
slowness, and this is its chief disadvantage. The float must come to rest before
any reading is made.
Page 77
A convenient plan for filling a burette from below is shown in fig. 30. The
diagram explains itself. The bottle containing the standard solution is connected
with the burette by a syphon arrangement through the glass tube and T-piece.
The flow of liquid into the burette is controlled by the clip. When this clip is
opened, the burette fills; and when it is closed, the burette is ready for use in the
ordinary way.
Measuring Gases.—Lange's nitrometer (fig. 69) is a very convenient
instrument for many gasometric methods. It requires the use of a fair quantity of
mercury. In fig. 31, there is a representation of a piece of apparatus easily fitted
up from the ordinary material of a laboratory. It is one which will serve some
useful purposes. It consists of a wide-mouthed bottle fitted (by preference) with
a rubber cork. The cork is perforated, and in the perforation is placed a glass
tube which communicates with the burette. The burette is connected by a rubber
tube and a Y-piece, either with another burette or with a piece of ordinary
combustion-tube of about the same size. The wide-mouthed bottle contains
either a short test-tube or an ordinary phial with its neck cut off. In working the
apparatus the weighed substance is put in the bottle and the re-agent which is to
act on it, in the test-tube; the cork is then inserted. The liquid in the two burettes
diagram explains itself. The bottle containing the standard solution is connected
with the burette by a syphon arrangement through the glass tube and T-piece.
The flow of liquid into the burette is controlled by the clip. When this clip is
opened, the burette fills; and when it is closed, the burette is ready for use in the
ordinary way.
Measuring Gases.—Lange's nitrometer (fig. 69) is a very convenient
instrument for many gasometric methods. It requires the use of a fair quantity of
mercury. In fig. 31, there is a representation of a piece of apparatus easily fitted
up from the ordinary material of a laboratory. It is one which will serve some
useful purposes. It consists of a wide-mouthed bottle fitted (by preference) with
a rubber cork. The cork is perforated, and in the perforation is placed a glass
tube which communicates with the burette. The burette is connected by a rubber
tube and a Y-piece, either with another burette or with a piece of ordinary
combustion-tube of about the same size. The wide-mouthed bottle contains
either a short test-tube or an ordinary phial with its neck cut off. In working the
apparatus the weighed substance is put in the bottle and the re-agent which is to
act on it, in the test-tube; the cork is then inserted. The liquid in the two burettes
Page 78
is next brought to the same level, either by pouring it in at a or running it out at
b. The level of the liquid in the apparatus for correcting variation in volume is
then read and noted. Next, after seeing that the level of the liquid in the burette
has not changed, turn the bottle over on its side so that the re-agent in the test-
tube shall be upset into the bottle. Then, as the volume of the gas increases,
lower the liquid in the burette by running it out at b, and at the same time keep
the level in a half an inch or so lower than that in the burette. When the action
has finished bring the liquid in the two vessels to the same level and read off the
burette. This part of the work must always be done in the same manner.
The volume corrector for gas analysis is a graduated glass tube of 120 c.c.
capacity inverted over a narrow glass cylinder of mercury. It contains 0.2 or 0.3
c.c. of water and a volume of air, which, if dry and under standard conditions,
would measure 100 c.c. The actual volume varies from day to day, and is read
off at any time by bringing the mercury inside and outside to the same level.
This is done by raising or lowering the tube, as may be required. Any volume of
gas obtained in an assay can be corrected to standard temperature and pressure
by multiplying by 100 and dividing by the number of c.c. in the corrector at the
time the assay is made.
b. The level of the liquid in the apparatus for correcting variation in volume is
then read and noted. Next, after seeing that the level of the liquid in the burette
has not changed, turn the bottle over on its side so that the re-agent in the test-
tube shall be upset into the bottle. Then, as the volume of the gas increases,
lower the liquid in the burette by running it out at b, and at the same time keep
the level in a half an inch or so lower than that in the burette. When the action
has finished bring the liquid in the two vessels to the same level and read off the
burette. This part of the work must always be done in the same manner.
The volume corrector for gas analysis is a graduated glass tube of 120 c.c.
capacity inverted over a narrow glass cylinder of mercury. It contains 0.2 or 0.3
c.c. of water and a volume of air, which, if dry and under standard conditions,
would measure 100 c.c. The actual volume varies from day to day, and is read
off at any time by bringing the mercury inside and outside to the same level.
This is done by raising or lowering the tube, as may be required. Any volume of
gas obtained in an assay can be corrected to standard temperature and pressure
by multiplying by 100 and dividing by the number of c.c. in the corrector at the
time the assay is made.
Page 79
FOOTNOTES:
[5] It is best to use this form with a glass stopcock, or with an india-rubber tube and
clip, after the manner of a Mohr's burette.
[5] It is best to use this form with a glass stopcock, or with an india-rubber tube and
clip, after the manner of a Mohr's burette.
Page 80
CHAPTER VI.
RE-AGENTS.—ACIDS, ETC.
Acetic Acid, H[=A=c] or C2H4O2. (sp. gr. 1.044, containing 33 per cent. real
acid).—An organic acid, forming a class of salts, acetates, which are for the
most part soluble in water, and which, on ignition, leave the oxide or carbonate
of the metal. It is almost always used in those cases where mineral acids are
objectionable. To convert, for example, a solution of a substance in hydrochloric
acid into a solution of the same in acetic acid, alkali should be added in excess
and then acetic acid. Many compounds are insoluble in acetic acid, which are
soluble in mineral acids, such as ferric phosphate, ferric arsenate, zinc sulphide,
calcium oxalate, &c., so that the use of acetic acid is valuable in some
separations. The commercial acid is strong enough for most purposes, and is
used without dilution.
"Aqua Regia" is a mixture of 1 part by measure of nitric acid and 3 parts of
hydrochloric acid. The acids react forming what is practically a solution of
chlorine.[6] The mixture is best made when wanted, and is chiefly used for the
solution of gold and platinum and for "opening up" sulphides. When solutions in
aqua regia are evaporated, chlorides are left.
Bromine, Br. (sp. gr. 3.0). Practically pure bromine.—It is a heavy reddish-
brown liquid and very volatile. It boils at 60° C., and, consequently, must be
kept in a cool place. It gives off brown irritating vapours, which render its use
very objectionable. Generally it answers the same purpose as aqua regia, and is
employed where the addition of nitric acid to a solution has to be specially
avoided. It is also used for dissolving metals only from ores which contain
metallic oxides not desired in the solution.
"Bromine Water" is simply bromine shaken up with water till no more is
dissolved.
Carbonic Acid, CO2.—A heavy gas, somewhat soluble in water; it is mainly
used for providing an atmosphere in which substances may be dissolved,
titrated, &c., without fear of oxidation. It is also used in titrating arsenic assays
with "iodine" when a feeble acid is required to prevent the absorption of iodine
RE-AGENTS.—ACIDS, ETC.
Acetic Acid, H[=A=c] or C2H4O2. (sp. gr. 1.044, containing 33 per cent. real
acid).—An organic acid, forming a class of salts, acetates, which are for the
most part soluble in water, and which, on ignition, leave the oxide or carbonate
of the metal. It is almost always used in those cases where mineral acids are
objectionable. To convert, for example, a solution of a substance in hydrochloric
acid into a solution of the same in acetic acid, alkali should be added in excess
and then acetic acid. Many compounds are insoluble in acetic acid, which are
soluble in mineral acids, such as ferric phosphate, ferric arsenate, zinc sulphide,
calcium oxalate, &c., so that the use of acetic acid is valuable in some
separations. The commercial acid is strong enough for most purposes, and is
used without dilution.
"Aqua Regia" is a mixture of 1 part by measure of nitric acid and 3 parts of
hydrochloric acid. The acids react forming what is practically a solution of
chlorine.[6] The mixture is best made when wanted, and is chiefly used for the
solution of gold and platinum and for "opening up" sulphides. When solutions in
aqua regia are evaporated, chlorides are left.
Bromine, Br. (sp. gr. 3.0). Practically pure bromine.—It is a heavy reddish-
brown liquid and very volatile. It boils at 60° C., and, consequently, must be
kept in a cool place. It gives off brown irritating vapours, which render its use
very objectionable. Generally it answers the same purpose as aqua regia, and is
employed where the addition of nitric acid to a solution has to be specially
avoided. It is also used for dissolving metals only from ores which contain
metallic oxides not desired in the solution.
"Bromine Water" is simply bromine shaken up with water till no more is
dissolved.
Carbonic Acid, CO2.—A heavy gas, somewhat soluble in water; it is mainly
used for providing an atmosphere in which substances may be dissolved,
titrated, &c., without fear of oxidation. It is also used in titrating arsenic assays
with "iodine" when a feeble acid is required to prevent the absorption of iodine
Page 81
by the alkaline carbonate. It is prepared when wanted in solution, by adding a
gram or so of bicarbonate of soda and then as much acid as will decompose the
bicarbonate mentioned. When a quantity of the gas is wanted, it is prepared, in
an apparatus like that used for sulphuretted hydrogen, by acting on fragments of
marble or limestone with dilute hydrochloric acid.
Citric Acid (H3[=C=i] or C6H8O7.H2O) is an organic acid which occurs in
colourless crystals, soluble in less than their weight of water. The solution must
be freshly prepared, as it gets mouldy when kept. It forms a comparatively
unimportant class of salts (citrates). It is used in the determination of phosphoric
acid, chiefly for the purpose of preventing the precipitation of phosphates of iron
and alumina by ammonia, and in a few similar cases. The commercial crystals
are used; they should be free from sulphuric acid and leave no ash on ignition.
Hydrochloric Acid, HCl in water, (sp. gr. 1.16. It contains 32 per cent. of
hydrogen chloride).—It is sometimes called "muriatic acid," and when impure,
"spirit of salt." The acid solution should be colourless and free from arsenic,
iron, and sulphuric acid. It forms an important family of salts, the chlorides. It is
the best acid for dissolving metallic oxides and carbonates, and is always used
by the assayer when oxidising agents are to be avoided. The acid is used without
dilution when no directions are expressly given to dilute it. It has no action on
the following metals: gold, platinum, arsenic, and mercury; it very slightly
attacks antimony, bismuth, lead, silver, and copper. Tin is more soluble in it, but
with difficulty; whilst iron, zinc, nickel, cobalt, cadmium, and aluminium easily
dissolve with evolution of hydrogen and the formation of the lower chloride if
the metal forms more than one class of salts. All the metallic oxides, except a
few of the native and rarer oxides, are dissolved by it with the formation of
chlorides of the metal and water.
Dilute Hydrochloric Acid is made by diluting the strong acid with an equal
volume of water. This is used for dissolving precipitates obtained in the general
course of analysis and the more easily soluble metals.
Hydrofluoric Acid, HF.—A solution in water may be purchased in gutta-percha
or lead bottles. It is of variable strength and doubtful purity. It must always be
examined quantitatively for the residue left on evaporation. It is used
occasionally for the examination of silicates. It attacks silica, forming fluoride of
silicon, which is a gas. When the introduction of another base will not interfere
with the assay, the substance may be mixed in the platinum dish with fluoride of
ammonium, or of potassium, or of calcium, and hydrochloric acid, instead of
treating it with the commercial acid. It is only required in special work. The
gram or so of bicarbonate of soda and then as much acid as will decompose the
bicarbonate mentioned. When a quantity of the gas is wanted, it is prepared, in
an apparatus like that used for sulphuretted hydrogen, by acting on fragments of
marble or limestone with dilute hydrochloric acid.
Citric Acid (H3[=C=i] or C6H8O7.H2O) is an organic acid which occurs in
colourless crystals, soluble in less than their weight of water. The solution must
be freshly prepared, as it gets mouldy when kept. It forms a comparatively
unimportant class of salts (citrates). It is used in the determination of phosphoric
acid, chiefly for the purpose of preventing the precipitation of phosphates of iron
and alumina by ammonia, and in a few similar cases. The commercial crystals
are used; they should be free from sulphuric acid and leave no ash on ignition.
Hydrochloric Acid, HCl in water, (sp. gr. 1.16. It contains 32 per cent. of
hydrogen chloride).—It is sometimes called "muriatic acid," and when impure,
"spirit of salt." The acid solution should be colourless and free from arsenic,
iron, and sulphuric acid. It forms an important family of salts, the chlorides. It is
the best acid for dissolving metallic oxides and carbonates, and is always used
by the assayer when oxidising agents are to be avoided. The acid is used without
dilution when no directions are expressly given to dilute it. It has no action on
the following metals: gold, platinum, arsenic, and mercury; it very slightly
attacks antimony, bismuth, lead, silver, and copper. Tin is more soluble in it, but
with difficulty; whilst iron, zinc, nickel, cobalt, cadmium, and aluminium easily
dissolve with evolution of hydrogen and the formation of the lower chloride if
the metal forms more than one class of salts. All the metallic oxides, except a
few of the native and rarer oxides, are dissolved by it with the formation of
chlorides of the metal and water.
Dilute Hydrochloric Acid is made by diluting the strong acid with an equal
volume of water. This is used for dissolving precipitates obtained in the general
course of analysis and the more easily soluble metals.
Hydrofluoric Acid, HF.—A solution in water may be purchased in gutta-percha
or lead bottles. It is of variable strength and doubtful purity. It must always be
examined quantitatively for the residue left on evaporation. It is used
occasionally for the examination of silicates. It attacks silica, forming fluoride of
silicon, which is a gas. When the introduction of another base will not interfere
with the assay, the substance may be mixed in the platinum dish with fluoride of
ammonium, or of potassium, or of calcium, and hydrochloric acid, instead of
treating it with the commercial acid. It is only required in special work. The
Page 82
fumes and acid are dangerous, and, of course, glass or porcelain vessels cannot
be used with it.
Iodine, I.—This can be obtained in commerce quite pure, and is often used for
standardising. It is very slightly soluble in water, but readily dissolves in
potassium iodide solution. It closely resembles chlorine and bromine in its
properties, and can be used for dissolving metals without, at the same time,
attacking any oxide which may be present. It is chiefly used as an oxidizing
agent in volumetric work, being sharp in its reactions and easily detected in
minute quantities. It cannot be used in alkaline solutions, since it reacts with the
hydrates, and even with the carbonates, to form iodides and iodates. Iodine is
soluble in alcohol.
Nitric Acid, HNO3. (Sp. gr. 1.42; boiling point 121° C.; contains 70 per cent. by
weight of hydrogen nitrate).—It is convenient to remember that one c.c. of this
contains 1 gram of real acid. It combines the properties of an acid and of an
oxidising agent. One c.c. contains 0.76 gram of oxygen, most of which is very
loosely held, and easily given up to metals and other oxidisable substances.
Consequently it will dissolve many metals, &c., upon which hydrochloric acid
has no action. All sulphides (that of mercury excepted) are attacked by it, and for
the most part rendered soluble. It has no action on gold or platinum, and very
little on aluminium. The strong acid at the ordinary temperature does not act on
iron or tin; and in most cases it acts better when diluted. Some nitrates being
insoluble in nitric acid, form a protecting coat to the metal which hinders further
action. Where the strong acid does act the action is very violent, so that
generally it is better to use the dilute acid. When iron has been immersed in
strong nitric acid it not only remains unacted on, but assumes a passive state; so
that if, after being wiped, it is then placed in the dilute acid, it will not dissolve.
Tin and antimony are converted into insoluble oxides, while the other metals
(with the exception of those already mentioned) dissolve as nitrates. During the
solution of the metal red fumes are given off, which mainly consist of nitrogen
peroxide. The solution is often coloured brown or green because of dissolved
oxides of nitrogen, which must be got rid of by boiling. Generally some
ammonium nitrate is formed, especially in the cases of zinc, iron, and tin, when
these are acted on by cold dilute acid. Sulphur, phosphorus, and arsenic are
converted into sulphuric, phosphoric, and arsenic acids respectively, when
boiled with the strong acid.
Dilute Nitric Acid.—Dilute 1 volume of the strong acid with 2 of water.
be used with it.
Iodine, I.—This can be obtained in commerce quite pure, and is often used for
standardising. It is very slightly soluble in water, but readily dissolves in
potassium iodide solution. It closely resembles chlorine and bromine in its
properties, and can be used for dissolving metals without, at the same time,
attacking any oxide which may be present. It is chiefly used as an oxidizing
agent in volumetric work, being sharp in its reactions and easily detected in
minute quantities. It cannot be used in alkaline solutions, since it reacts with the
hydrates, and even with the carbonates, to form iodides and iodates. Iodine is
soluble in alcohol.
Nitric Acid, HNO3. (Sp. gr. 1.42; boiling point 121° C.; contains 70 per cent. by
weight of hydrogen nitrate).—It is convenient to remember that one c.c. of this
contains 1 gram of real acid. It combines the properties of an acid and of an
oxidising agent. One c.c. contains 0.76 gram of oxygen, most of which is very
loosely held, and easily given up to metals and other oxidisable substances.
Consequently it will dissolve many metals, &c., upon which hydrochloric acid
has no action. All sulphides (that of mercury excepted) are attacked by it, and for
the most part rendered soluble. It has no action on gold or platinum, and very
little on aluminium. The strong acid at the ordinary temperature does not act on
iron or tin; and in most cases it acts better when diluted. Some nitrates being
insoluble in nitric acid, form a protecting coat to the metal which hinders further
action. Where the strong acid does act the action is very violent, so that
generally it is better to use the dilute acid. When iron has been immersed in
strong nitric acid it not only remains unacted on, but assumes a passive state; so
that if, after being wiped, it is then placed in the dilute acid, it will not dissolve.
Tin and antimony are converted into insoluble oxides, while the other metals
(with the exception of those already mentioned) dissolve as nitrates. During the
solution of the metal red fumes are given off, which mainly consist of nitrogen
peroxide. The solution is often coloured brown or green because of dissolved
oxides of nitrogen, which must be got rid of by boiling. Generally some
ammonium nitrate is formed, especially in the cases of zinc, iron, and tin, when
these are acted on by cold dilute acid. Sulphur, phosphorus, and arsenic are
converted into sulphuric, phosphoric, and arsenic acids respectively, when
boiled with the strong acid.
Dilute Nitric Acid.—Dilute 1 volume of the strong acid with 2 of water.
Page 83
Oxalic Acid, H2O or (H2C2O4.2H2O.)—This is an organic acid in colourless
crystals. It forms a family of salts—the oxalates. It is used in standardising;
being a crystallised and permanent acid, it can be readily weighed. It is also used
in separations, many of the oxalates being insoluble. For general use make a 10
per cent. solution. Use the commercially pure acid. On ignition the acid should
leave no residue.
Sulphuretted Hydrogen. Hydrosulphuric acid, SH2.—A gas largely used in
assaying, since by its action it allows of the metals being conveniently classed
into groups. It is soluble in water, this liquid dissolving at the ordinary
temperature about three times its volume of the gas. The solution is only useful
for testing. In separations, a current of the gas must always be used. It is best
prepared in an apparatus like that shown in fig. 32, by acting on ferrous sulphide
with dilute hydrochloric acid. When iron has to be subsequently determined in
the assay solution, the gas should be washed by bubbling it through water in the
smaller bottle; but for most purposes washing can be dispensed with. The gas is
very objectionable, and operations with it must be carried out in a cupboard with
a good draught. When the precipitation has been completed, the apparatus
should always be washed out. The effect of this acid on solutions of the metals is
to form sulphides. All the metallic sulphides are insoluble in water; but some are
soluble in alkaline, and some in acid, solutions. If sulphuretted hydrogen is
passed through an acid solution containing the metals till no further precipitation
takes place, a precipitate will be formed containing sulphides insoluble in the
acid. On filtering, adding ammonia (to render the filtrate alkaline), and again
passing the gas, a further precipitate will be obtained, consisting of sulphides
crystals. It forms a family of salts—the oxalates. It is used in standardising;
being a crystallised and permanent acid, it can be readily weighed. It is also used
in separations, many of the oxalates being insoluble. For general use make a 10
per cent. solution. Use the commercially pure acid. On ignition the acid should
leave no residue.
Sulphuretted Hydrogen. Hydrosulphuric acid, SH2.—A gas largely used in
assaying, since by its action it allows of the metals being conveniently classed
into groups. It is soluble in water, this liquid dissolving at the ordinary
temperature about three times its volume of the gas. The solution is only useful
for testing. In separations, a current of the gas must always be used. It is best
prepared in an apparatus like that shown in fig. 32, by acting on ferrous sulphide
with dilute hydrochloric acid. When iron has to be subsequently determined in
the assay solution, the gas should be washed by bubbling it through water in the
smaller bottle; but for most purposes washing can be dispensed with. The gas is
very objectionable, and operations with it must be carried out in a cupboard with
a good draught. When the precipitation has been completed, the apparatus
should always be washed out. The effect of this acid on solutions of the metals is
to form sulphides. All the metallic sulphides are insoluble in water; but some are
soluble in alkaline, and some in acid, solutions. If sulphuretted hydrogen is
passed through an acid solution containing the metals till no further precipitation
takes place, a precipitate will be formed containing sulphides insoluble in the
acid. On filtering, adding ammonia (to render the filtrate alkaline), and again
passing the gas, a further precipitate will be obtained, consisting of sulphides
Page 84
insoluble in an alkaline solution, but not precipitable in an acid one; the filtrate
may also contain sulphides not precipitable in an acid solution, which are
soluble in an alkaline one; these will be thrown down on neutralising. Again, the
metals precipitated in the acid solution form sulphides which may be divided
into groups, the one consisting of those which are soluble, and the other of those
which are not soluble, in alkalies. This classification is shown in the following
summary:—
1. Precipitable in an acid solution.
(a) Soluble in Alkalies.—Sulphides of As, Sb, Sn, Au, Pt, Ir, Mo, Te, and Se.
(b) Insoluble in Alkalies.—Sulphides of Ag, Pb, Hg, Bi, Cu, Cd, Pd, Rh, Os,
and Ru.
2. Not precipitated in an acid solution, but thrown down in an alkaline one.
Sulphides of Mn, Zn, Fe, Ni, Co, In, Tl, and Ga.
These can again be divided into those which are dissolved by dilute acids and
those which are not.
3. Not precipitated in an acid or alkaline solution, but thrown
down on neutralising the latter.
Sulphides of V and W.
Sulphuretted hydrogen is a strong reducing agent. Ferric salts are thereby
quickly reduced to ferrous; in hot solutions nitric acid is decomposed. These
changes are marked by a precipitation of sulphur, and the student must be
careful to pass the gas sufficiently long, and not be too hasty in concluding that
no sulphide will form because it does not at once make its appearance. The best
indication that it has been passed long enough is the smell of the gas in the
solution after shaking.
Sulphurous Acid, H2SO3.—The reagent used may be regarded as a saturated
solution of sulphur dioxide in water. It may be purchased, and keeps for a long
time. It may be made by heating copper with sulphuric acid and passing the gas
formed into water. The heat should be withdrawn when the gas is coming off
freely. It is used as a reducing agent, and should not be diluted.
may also contain sulphides not precipitable in an acid solution, which are
soluble in an alkaline one; these will be thrown down on neutralising. Again, the
metals precipitated in the acid solution form sulphides which may be divided
into groups, the one consisting of those which are soluble, and the other of those
which are not soluble, in alkalies. This classification is shown in the following
summary:—
1. Precipitable in an acid solution.
(a) Soluble in Alkalies.—Sulphides of As, Sb, Sn, Au, Pt, Ir, Mo, Te, and Se.
(b) Insoluble in Alkalies.—Sulphides of Ag, Pb, Hg, Bi, Cu, Cd, Pd, Rh, Os,
and Ru.
2. Not precipitated in an acid solution, but thrown down in an alkaline one.
Sulphides of Mn, Zn, Fe, Ni, Co, In, Tl, and Ga.
These can again be divided into those which are dissolved by dilute acids and
those which are not.
3. Not precipitated in an acid or alkaline solution, but thrown
down on neutralising the latter.
Sulphides of V and W.
Sulphuretted hydrogen is a strong reducing agent. Ferric salts are thereby
quickly reduced to ferrous; in hot solutions nitric acid is decomposed. These
changes are marked by a precipitation of sulphur, and the student must be
careful to pass the gas sufficiently long, and not be too hasty in concluding that
no sulphide will form because it does not at once make its appearance. The best
indication that it has been passed long enough is the smell of the gas in the
solution after shaking.
Sulphurous Acid, H2SO3.—The reagent used may be regarded as a saturated
solution of sulphur dioxide in water. It may be purchased, and keeps for a long
time. It may be made by heating copper with sulphuric acid and passing the gas
formed into water. The heat should be withdrawn when the gas is coming off
freely. It is used as a reducing agent, and should not be diluted.
Page 85
Sulphuric Acid, H2SO4. (Sp. gr. 1.84, containing 96 per cent. of real acid,
H2SO4.)—This acid forms insoluble sulphates with salts of lead, strontium, and
barium. It has a high boiling point, 290° C., and, when evaporated with salts of
the more volatile acids, converts them into sulphates. When nitrates or chlorides
are objectionable in a solution, evaporation with sulphuric acid removes them.
In working with this acid caution is necessary, since, on mixing with water, great
heat is evolved; and, if either the acid or water has been previously heated, a
serious accident may result. In diluting the acid it should be poured into cold
water. Glass vessels containing boiling sulphuric acid should be handled as little
as possible, and should not be cooled under the tap. The action of diluted
sulphuric acid on metals closely resembles that of dilute hydrochloric acid.
Magnesium, aluminium, iron, zinc, nickel, cobalt, manganese, and cadmium
dissolve, with evolution of hydrogen, in the cold acid, or when warmed. The
action of hot and strong sulphuric acid is altogether different; it acts as an
oxidising agent, and is itself reduced to sulphur dioxide or even to sulphur. The
following metals are attacked in this way:—copper, bismuth, mercury, silver,
antimony, tin, and lead. Gold, platinum, and arsenic are not affected. This
property is made use of in parting silver from gold and platinum. Metallic
sulphides are similarly attacked; but this method of opening up minerals has the
disadvantage of giving rise to the formation of anhydrous sulphates of iron, &c.,
which are not readily dissolved when afterwards diluted. The use of sulphuric
acid in assaying is (for these reasons) to be avoided. Its chief use is as a drying
agent, since it has a strong affinity for water. Air under a bell jar may be kept dry
by means of a basin of sulphuric acid, and gases bubbled through it are freed
from water-vapour.
Dilute Sulphuric Acid.—This is made by diluting 1 volume of the strong acid
with 4 of water.
Tartaric Acid, H2[=T] or C4H6O6.—A crystallised organic acid, soluble in less
than its own weight of water, or in less than three parts of alcohol. It is used for
the same purposes as citric acid is. The solution is made when required.
BASES, SALTS, &c.
Alcohol, C2H6O. (Commercial alcohol of sp. gr. 0.838; it contains 84 per cent.
by weight of alcohol.)—It should burn with a non-luminous flame and leave no
residue. It is used for washing precipitates where water is inapplicable, and for
facilitating drying.
H2SO4.)—This acid forms insoluble sulphates with salts of lead, strontium, and
barium. It has a high boiling point, 290° C., and, when evaporated with salts of
the more volatile acids, converts them into sulphates. When nitrates or chlorides
are objectionable in a solution, evaporation with sulphuric acid removes them.
In working with this acid caution is necessary, since, on mixing with water, great
heat is evolved; and, if either the acid or water has been previously heated, a
serious accident may result. In diluting the acid it should be poured into cold
water. Glass vessels containing boiling sulphuric acid should be handled as little
as possible, and should not be cooled under the tap. The action of diluted
sulphuric acid on metals closely resembles that of dilute hydrochloric acid.
Magnesium, aluminium, iron, zinc, nickel, cobalt, manganese, and cadmium
dissolve, with evolution of hydrogen, in the cold acid, or when warmed. The
action of hot and strong sulphuric acid is altogether different; it acts as an
oxidising agent, and is itself reduced to sulphur dioxide or even to sulphur. The
following metals are attacked in this way:—copper, bismuth, mercury, silver,
antimony, tin, and lead. Gold, platinum, and arsenic are not affected. This
property is made use of in parting silver from gold and platinum. Metallic
sulphides are similarly attacked; but this method of opening up minerals has the
disadvantage of giving rise to the formation of anhydrous sulphates of iron, &c.,
which are not readily dissolved when afterwards diluted. The use of sulphuric
acid in assaying is (for these reasons) to be avoided. Its chief use is as a drying
agent, since it has a strong affinity for water. Air under a bell jar may be kept dry
by means of a basin of sulphuric acid, and gases bubbled through it are freed
from water-vapour.
Dilute Sulphuric Acid.—This is made by diluting 1 volume of the strong acid
with 4 of water.
Tartaric Acid, H2[=T] or C4H6O6.—A crystallised organic acid, soluble in less
than its own weight of water, or in less than three parts of alcohol. It is used for
the same purposes as citric acid is. The solution is made when required.
BASES, SALTS, &c.
Alcohol, C2H6O. (Commercial alcohol of sp. gr. 0.838; it contains 84 per cent.
by weight of alcohol.)—It should burn with a non-luminous flame and leave no
residue. It is used for washing precipitates where water is inapplicable, and for
facilitating drying.
Page 86
Ammonia, NH3. (Commercial ammonia, a solution having a sp. gr. of 0.88 to
0.89, and containing about 33 per cent. of ammonia.)—It is used as an alkali
(more commonly than soda or potash), since an excess of it is easily removed by
boiling. The salts of ammonium formed by it may be removed by igniting, or by
evaporating in a porcelain dish with an excess of nitric acid. It differs in a
marked way from soda or potash in its solvent action on the oxides or hydrates
of the metals. Salts of the following metals are soluble in an ammoniacal
solution in the presence of ammonic chloride:—copper, cadmium, silver, nickel,
cobalt, manganese, zinc, magnesium, sodium, potassium, and the alkaline earths.
Dilute Ammonia is made by diluting 1 vol. of commercial ammonia with 2 of
water. The dilute ammonia is always used; but in assays for copper a stronger
solution (1 of strong ammonia to 1 of water) is required.
Ammonic Carbonate (Am2CO3) is prepared by dissolving one part of the
commercial sesquicarbonate of ammonia in four parts of water, and adding one
part of strong ammonia.
Ammonic Bicarbonate (HAmCO3) is prepared by saturating a solution of the
sesquicarbonate of ammonia with carbon dioxide.
Ammonic Chloride, AmCl.—Use the commercial salt in a 20 per cent. solution
in water. The salt should leave no residue on ignition.
Ammonic Molybdate.—The solution is prepared as follows:—Dissolve 100
grams of the powdered commercial salt in 200 c.c. of dilute ammonia, and pour
the solution in a slow stream into 750 c.c. of dilute nitric acid; make up to 1 litre,
and allow the mixture to settle before using. It is used for the purpose of
separating phosphoric oxide from bases and from other acids, and also as a test
for phosphates and arsenates. In using this solution the substance must be
dissolved in nitric acid, and a considerable excess of the reagent added (50 c.c.
is sufficient to precipitate 0.1 gram P2O5); when the phosphate is in excess no
precipitate will be got. The precipitate is phospho-molybdate of ammonia.
Ammonic Nitrate (AmNO3) is used in the separation of phosphoric oxide by
the molybdate method, and occasionally for destroying organic matter. It is
soluble in less than its own weight of water. The solution is made when wanted.
Ammonic Oxalate (Am2C2O4.2H2O) is used chiefly for the separation of lime.
The solution is made by dissolving 15 grams of the salt in 100 c.c. of water.
0.89, and containing about 33 per cent. of ammonia.)—It is used as an alkali
(more commonly than soda or potash), since an excess of it is easily removed by
boiling. The salts of ammonium formed by it may be removed by igniting, or by
evaporating in a porcelain dish with an excess of nitric acid. It differs in a
marked way from soda or potash in its solvent action on the oxides or hydrates
of the metals. Salts of the following metals are soluble in an ammoniacal
solution in the presence of ammonic chloride:—copper, cadmium, silver, nickel,
cobalt, manganese, zinc, magnesium, sodium, potassium, and the alkaline earths.
Dilute Ammonia is made by diluting 1 vol. of commercial ammonia with 2 of
water. The dilute ammonia is always used; but in assays for copper a stronger
solution (1 of strong ammonia to 1 of water) is required.
Ammonic Carbonate (Am2CO3) is prepared by dissolving one part of the
commercial sesquicarbonate of ammonia in four parts of water, and adding one
part of strong ammonia.
Ammonic Bicarbonate (HAmCO3) is prepared by saturating a solution of the
sesquicarbonate of ammonia with carbon dioxide.
Ammonic Chloride, AmCl.—Use the commercial salt in a 20 per cent. solution
in water. The salt should leave no residue on ignition.
Ammonic Molybdate.—The solution is prepared as follows:—Dissolve 100
grams of the powdered commercial salt in 200 c.c. of dilute ammonia, and pour
the solution in a slow stream into 750 c.c. of dilute nitric acid; make up to 1 litre,
and allow the mixture to settle before using. It is used for the purpose of
separating phosphoric oxide from bases and from other acids, and also as a test
for phosphates and arsenates. In using this solution the substance must be
dissolved in nitric acid, and a considerable excess of the reagent added (50 c.c.
is sufficient to precipitate 0.1 gram P2O5); when the phosphate is in excess no
precipitate will be got. The precipitate is phospho-molybdate of ammonia.
Ammonic Nitrate (AmNO3) is used in the separation of phosphoric oxide by
the molybdate method, and occasionally for destroying organic matter. It is
soluble in less than its own weight of water. The solution is made when wanted.
Ammonic Oxalate (Am2C2O4.2H2O) is used chiefly for the separation of lime.
The solution is made by dissolving 15 grams of the salt in 100 c.c. of water.
Page 87
Ammonic Sulphide may be purchased in the state of a strong solution. It is
yellow, and contains the disulphide, S2Am2. It serves the same purpose as is
obtained by passing a current of sulphuretted hydrogen through an ammoniacal
solution; but has the disadvantage of loading the solution with sulphur, which is
precipitated when the solution is subsequently acidified. It is useful for
dissolving the lower sulphide of tin (SnS).
Baric Carbonate (BaCO3) is sometimes used for precipitating the weaker
bases. It should be prepared when wanted by precipitating a solution of baric
chloride with ammonic carbonate and washing. The moist precipitate is used
without drying.
Baric Chloride, BaCl2.2H2O.—A crystallised salt, soluble in 2-1/2 parts of
water. It is used for the detection and separation of sulphates. Make a 10 per
cent. solution.
"Black Flux."—A mixture of finely divided carbon with carbonate of potash or
with carbonates of potash and soda. It is prepared by heating tartar or "rochelle
salt" until no more combustible gas is given off. One gram will reduce about 2
grams of lead from litharge.
Borax, Na2B4O7.10H2O.—It is chiefly used as a flux in dry assaying, as already
described. It is also used in testing before the blowpipe; many metallic oxides
impart a characteristic colour to a bead of borax in which they have been fused.
Calcium Chloride.—The crystallised salt is CaCl2.6H2O; dried at 200° C. it
becomes CaCl2.2H2O, and when fused it becomes dehydrated. The fused salt,
broken into small lumps, is used for drying gases. It combines with water, giving
off much heat; and dissolves in a little more than its own weight of water. Strong
solutions may be used in baths in which temperatures above the boiling-point of
water are required. One part of the salt and 2 of water give a solution boiling at
112°, and a solution of 2 parts of the salt in 1 of water boils at 158°. The salt is
very little used as a reagent.
Calcium Fluoride or "Fluor Spar," CaF2.—The mineral is used as a flux in dry
assaying; it renders slags which are thick from the presence of phosphates, &c.,
very fluid. Mixed with hydrochloric acid it may sometimes be used instead of
hydrofluoric acid.
yellow, and contains the disulphide, S2Am2. It serves the same purpose as is
obtained by passing a current of sulphuretted hydrogen through an ammoniacal
solution; but has the disadvantage of loading the solution with sulphur, which is
precipitated when the solution is subsequently acidified. It is useful for
dissolving the lower sulphide of tin (SnS).
Baric Carbonate (BaCO3) is sometimes used for precipitating the weaker
bases. It should be prepared when wanted by precipitating a solution of baric
chloride with ammonic carbonate and washing. The moist precipitate is used
without drying.
Baric Chloride, BaCl2.2H2O.—A crystallised salt, soluble in 2-1/2 parts of
water. It is used for the detection and separation of sulphates. Make a 10 per
cent. solution.
"Black Flux."—A mixture of finely divided carbon with carbonate of potash or
with carbonates of potash and soda. It is prepared by heating tartar or "rochelle
salt" until no more combustible gas is given off. One gram will reduce about 2
grams of lead from litharge.
Borax, Na2B4O7.10H2O.—It is chiefly used as a flux in dry assaying, as already
described. It is also used in testing before the blowpipe; many metallic oxides
impart a characteristic colour to a bead of borax in which they have been fused.
Calcium Chloride.—The crystallised salt is CaCl2.6H2O; dried at 200° C. it
becomes CaCl2.2H2O, and when fused it becomes dehydrated. The fused salt,
broken into small lumps, is used for drying gases. It combines with water, giving
off much heat; and dissolves in a little more than its own weight of water. Strong
solutions may be used in baths in which temperatures above the boiling-point of
water are required. One part of the salt and 2 of water give a solution boiling at
112°, and a solution of 2 parts of the salt in 1 of water boils at 158°. The salt is
very little used as a reagent.
Calcium Fluoride or "Fluor Spar," CaF2.—The mineral is used as a flux in dry
assaying; it renders slags which are thick from the presence of phosphates, &c.,
very fluid. Mixed with hydrochloric acid it may sometimes be used instead of
hydrofluoric acid.
Page 88
Calcium Carbonate, CaCO3.—It is precipitated in a pure state by ammonic
carbonate from a solution of calcium chloride. It is used for standardising. In the
impure state, as marble or limestone, it is used in the preparation of carbonic
acid.
Calcium Hydrate or "Lime Water."—This is used in testing for carbon
dioxide and in estimating the amount of that gas present in air. It may be made
by slaking quicklime and digesting the slaked lime with water. One hundred c.c.
of water at 15° C. dissolves 0.1368 grams of the hydrate (CaH2O2), and hot
water dissolves still less. "Milk of lime" is slaked lime suspended in water.
Cobalt Nitrate (Co(NO3)2.6H2O) is used in a 10 per cent. solution for the
detection of oxides of zinc, aluminium, &c.; on ignition with which it forms
characteristically coloured compounds.
Copper, Cu.—Pure copper, as obtained by electrolysis, can be purchased. This
only should be used.
Copper Oxide, CuO.—It occurs as a black, heavy, and gritty power, and is used
for the oxidation of carbon and hydrogen in organic substances. It should be
ignited and cooled out of contact with air just before using, since it is
hygroscopic. Oxide of copper which has been used may be again utilised after
calcination.
Copper Sulphate (CuSO4.5H2O) contains 25.4 per cent. of copper. It is used in
the outer cell of a Daniell-battery. The commercial salt is used for this purpose.
The re-crystallised and pure salt is used for preparing the anhydrous sulphate,
which is used for detecting moisture in gases. For this purpose it is dried at 200°
C. till no trace of green or blue colour remains. It must be prepared when
wanted. It may be conveniently used in the form of pumice-stone, saturated with
a solution of the salt and dried. Traces of moisture develop a green colour.
Ferric Chloride, Fe2Cl6. (When crystallised, Fe2Cl6.6H2O.)—The solution is
prepared as described under iron. The commercial salt contains arsenic, and,
since the chief use of ferric chloride is for the determination of this substance, it
must be purified (see under Arsenic).
Ferric Sulphate (Fe2(SO4)3) is a yellowish white deliquescent salt. It is used as
an indicator in volumetric silver assaying, and for the separation of iodine from
bromine. It may be purchased as iron alum, Am2Fe2(SO4)4.24H2O. But it is best
carbonate from a solution of calcium chloride. It is used for standardising. In the
impure state, as marble or limestone, it is used in the preparation of carbonic
acid.
Calcium Hydrate or "Lime Water."—This is used in testing for carbon
dioxide and in estimating the amount of that gas present in air. It may be made
by slaking quicklime and digesting the slaked lime with water. One hundred c.c.
of water at 15° C. dissolves 0.1368 grams of the hydrate (CaH2O2), and hot
water dissolves still less. "Milk of lime" is slaked lime suspended in water.
Cobalt Nitrate (Co(NO3)2.6H2O) is used in a 10 per cent. solution for the
detection of oxides of zinc, aluminium, &c.; on ignition with which it forms
characteristically coloured compounds.
Copper, Cu.—Pure copper, as obtained by electrolysis, can be purchased. This
only should be used.
Copper Oxide, CuO.—It occurs as a black, heavy, and gritty power, and is used
for the oxidation of carbon and hydrogen in organic substances. It should be
ignited and cooled out of contact with air just before using, since it is
hygroscopic. Oxide of copper which has been used may be again utilised after
calcination.
Copper Sulphate (CuSO4.5H2O) contains 25.4 per cent. of copper. It is used in
the outer cell of a Daniell-battery. The commercial salt is used for this purpose.
The re-crystallised and pure salt is used for preparing the anhydrous sulphate,
which is used for detecting moisture in gases. For this purpose it is dried at 200°
C. till no trace of green or blue colour remains. It must be prepared when
wanted. It may be conveniently used in the form of pumice-stone, saturated with
a solution of the salt and dried. Traces of moisture develop a green colour.
Ferric Chloride, Fe2Cl6. (When crystallised, Fe2Cl6.6H2O.)—The solution is
prepared as described under iron. The commercial salt contains arsenic, and,
since the chief use of ferric chloride is for the determination of this substance, it
must be purified (see under Arsenic).
Ferric Sulphate (Fe2(SO4)3) is a yellowish white deliquescent salt. It is used as
an indicator in volumetric silver assaying, and for the separation of iodine from
bromine. It may be purchased as iron alum, Am2Fe2(SO4)4.24H2O. But it is best
Page 89
prepared by adding strong sulphuric acid to ferric hydrate in equivalent
proportions. Use it as a solution containing 2 or 3 per cent. of iron.
Ferrous Sulphate, FeSO4.7H2O.—The granulated form is best, and can be
purchased pure. It is used for standardising. It keeps better in crystals than in
solution. It is readily soluble in water, but the solution is best made with the help
of a little free acid. As a re-agent use a 10 per cent. solution. The crystals should
be clear bluish-green; if their colour is dark green, brown, or blue, they should
be rejected.
Ferrous Sulphide (FeS) is used for the preparation of sulphuretted hydrogen. It
may be purchased and broken in small lumps, nut-size, for use.
"Fusion Mixture" (K2CO3.Na2CO3) is a mixture of potassic and sodic
carbonates in the proportions of 13 of the former to 10 of the latter, by weight. It
is hygroscopic. A mixture of the bicarbonates is better, being purer and less apt
to get damp.
Gallic Acid (C7H6O5.H2O) is an organic acid, occurring as a pale fawn-coloured
crystalline powder, soluble in 100 parts of cold water, or in 3 parts of boiling
water. It is used for the determination of antimony. A 10 per cent. solution in
warm water is made when required.
Hydrogen (H) is a gas. It is obtained by acting on zinc with dilute hydrochloric
or sulphuric acid. It is used as a reducing agent, and for providing an atmosphere
free from oxygen. It reduces metallic oxides at a high temperature. It must be
freed from water; and special precautions should be taken to prevent an
admixture with air. It is generally required in a current which can be continued
for an hour or more without interruption. The preparation can be conveniently
carried out in the apparatus shown (fig. 33). A quart bottle is half filled with
sheet zinc, and connected with bulbs filled with sulphuric acid, and with a
calcium chloride tube. The last is connected with the apparatus through which
the gas has to be passed. Dilute hydrochloric acid mixed with a few cubic
centimetres (20 c.c. to 1 pint) of stannous chloride sol. to fix any dissolved
oxygen, is placed in the funnel, and let into the bottle by opening the stopcock
when required. Care must be taken to let the hydrogen escape for some time
before starting the reduction.
proportions. Use it as a solution containing 2 or 3 per cent. of iron.
Ferrous Sulphate, FeSO4.7H2O.—The granulated form is best, and can be
purchased pure. It is used for standardising. It keeps better in crystals than in
solution. It is readily soluble in water, but the solution is best made with the help
of a little free acid. As a re-agent use a 10 per cent. solution. The crystals should
be clear bluish-green; if their colour is dark green, brown, or blue, they should
be rejected.
Ferrous Sulphide (FeS) is used for the preparation of sulphuretted hydrogen. It
may be purchased and broken in small lumps, nut-size, for use.
"Fusion Mixture" (K2CO3.Na2CO3) is a mixture of potassic and sodic
carbonates in the proportions of 13 of the former to 10 of the latter, by weight. It
is hygroscopic. A mixture of the bicarbonates is better, being purer and less apt
to get damp.
Gallic Acid (C7H6O5.H2O) is an organic acid, occurring as a pale fawn-coloured
crystalline powder, soluble in 100 parts of cold water, or in 3 parts of boiling
water. It is used for the determination of antimony. A 10 per cent. solution in
warm water is made when required.
Hydrogen (H) is a gas. It is obtained by acting on zinc with dilute hydrochloric
or sulphuric acid. It is used as a reducing agent, and for providing an atmosphere
free from oxygen. It reduces metallic oxides at a high temperature. It must be
freed from water; and special precautions should be taken to prevent an
admixture with air. It is generally required in a current which can be continued
for an hour or more without interruption. The preparation can be conveniently
carried out in the apparatus shown (fig. 33). A quart bottle is half filled with
sheet zinc, and connected with bulbs filled with sulphuric acid, and with a
calcium chloride tube. The last is connected with the apparatus through which
the gas has to be passed. Dilute hydrochloric acid mixed with a few cubic
centimetres (20 c.c. to 1 pint) of stannous chloride sol. to fix any dissolved
oxygen, is placed in the funnel, and let into the bottle by opening the stopcock
when required. Care must be taken to let the hydrogen escape for some time
before starting the reduction.
Page 90
Gold, Au.—Gold, obtained by cupelling and "parting," is for most purposes
sufficiently pure. It is best kept in the shape of foil. When the purer metal is
required, gold should be dissolved in aqua regia, the solution evaporated to a
paste, diluted, allowed to stand, and filtered. The filtered solution is acidified
with hydrochloric acid, warmed, and precipitated with sodium sulphite. The
precipitate is collected, washed, and fused on charcoal.
Iron, Fe.—The soft wire (thin) is used for standardising. Rods are used in dry
assays as a desulphurising agent. Steel must not be used, since it is not pure, and
contains a variable amount of iron.
Lead, Pb.—Granulated lead or lead-foil is used in the dry assay for silver and
gold, and in the preparation of lead salts. It can be obtained very pure, but
always contains more or less silver, 1 or 2 milligrams in 100 grams. The amount
of silver it contains must be determined and recorded.
Lead Acetate (Pb[=A=c]2.3H2O, or Pb(C2H3O2)2.3H2O) is used as a test,
specially for the detection and estimation of sulphuretted hydrogen. Prepare a 10
per cent. solution for use.
Lead Nitrate (Pb(NO3)2) can be purchased pure. It is used for standardising.
Lead Dioxide (PbO2) occurs as a dark-brown powder. It is used as an oxidizing
agent and for absorbing sulphurous oxide. It can be prepared by digesting red
lead with warm dilute nitric acid; washing and drying the residue.
sufficiently pure. It is best kept in the shape of foil. When the purer metal is
required, gold should be dissolved in aqua regia, the solution evaporated to a
paste, diluted, allowed to stand, and filtered. The filtered solution is acidified
with hydrochloric acid, warmed, and precipitated with sodium sulphite. The
precipitate is collected, washed, and fused on charcoal.
Iron, Fe.—The soft wire (thin) is used for standardising. Rods are used in dry
assays as a desulphurising agent. Steel must not be used, since it is not pure, and
contains a variable amount of iron.
Lead, Pb.—Granulated lead or lead-foil is used in the dry assay for silver and
gold, and in the preparation of lead salts. It can be obtained very pure, but
always contains more or less silver, 1 or 2 milligrams in 100 grams. The amount
of silver it contains must be determined and recorded.
Lead Acetate (Pb[=A=c]2.3H2O, or Pb(C2H3O2)2.3H2O) is used as a test,
specially for the detection and estimation of sulphuretted hydrogen. Prepare a 10
per cent. solution for use.
Lead Nitrate (Pb(NO3)2) can be purchased pure. It is used for standardising.
Lead Dioxide (PbO2) occurs as a dark-brown powder. It is used as an oxidizing
agent and for absorbing sulphurous oxide. It can be prepared by digesting red
lead with warm dilute nitric acid; washing and drying the residue.
Page 91
"Litharge," PbO.—It can be purchased as a yellow heavy powder. It is used in
dry assaying as a flux, as a desulphurising agent, and also as a source of lead. It
always contains some silver, the amount of which must be determined.
Litmus.—This is an organic colouring matter which is turned red by acids and
blue by alkalies. For ordinary purposes it is best used as litmus paper, which
may be purchased in small books. A solution is prepared by digesting 15 or 20
grams of the commercial litmus in 100 c.c. of water on the water bath. After
being allowed to settle, it is filtered and made just faintly red with acetic acid.
Then there is added a drop or two of a solution of soda and 10 c.c. of alcohol. It
should be kept in a loosely-covered bottle.
Magnesia, MgO.—It may be purchased as "calcined magnesia." It is used for
making "magnesia mixture," and should be kept in a corked wide-mouthed
bottle.
"Magnesia Mixture."—Dissolve 22 grams of magnesia in about a quarter of a
litre of dilute hydrochloric acid, avoiding excess. Add 5 grams of magnesia, boil,
and filter. Add 300 grams of ammonic chloride, and 250 c.c. of strong ammonia;
and dilute with water to 2 litres. It should be kept in a stoppered winchester.
Magnesium Sulphate, MgSO4.7H2O.—It can be purchased very pure, and is
occasionally used as a standard salt.
Manganese Dioxide, MnO2.—It is used in the preparation of chlorine. The
commercial article is not pure, but is sufficiently so for this purpose.
Marble, CaCO3.—Fragments of the white crystalline variety only should be
used. It is used as a source of lime and of carbon dioxide.
Mercury, Hg.—This can be purchased pure. It should have a bright surface,
flow without a tail, and leave no residue on ignition. It is used as a standard; for
amalgamation; and as a confining liquid in gas analysis.
Mercuric Chloride (HgCl2) may be purchased pure. Make a 5 per cent. solution
in water. It is used for destroying an excess of stannous chloride; for removing
sulphuretted hydrogen from solution; and as a test for stannous salts.
Microcosmic Salt, HAmNaPO4.8H2O.—When fused NaPO3 is formed. It is
used in testing for metallic oxides and silica before the blowpipe. The crystals
are sometimes used as a standard for phosphoric acid.
dry assaying as a flux, as a desulphurising agent, and also as a source of lead. It
always contains some silver, the amount of which must be determined.
Litmus.—This is an organic colouring matter which is turned red by acids and
blue by alkalies. For ordinary purposes it is best used as litmus paper, which
may be purchased in small books. A solution is prepared by digesting 15 or 20
grams of the commercial litmus in 100 c.c. of water on the water bath. After
being allowed to settle, it is filtered and made just faintly red with acetic acid.
Then there is added a drop or two of a solution of soda and 10 c.c. of alcohol. It
should be kept in a loosely-covered bottle.
Magnesia, MgO.—It may be purchased as "calcined magnesia." It is used for
making "magnesia mixture," and should be kept in a corked wide-mouthed
bottle.
"Magnesia Mixture."—Dissolve 22 grams of magnesia in about a quarter of a
litre of dilute hydrochloric acid, avoiding excess. Add 5 grams of magnesia, boil,
and filter. Add 300 grams of ammonic chloride, and 250 c.c. of strong ammonia;
and dilute with water to 2 litres. It should be kept in a stoppered winchester.
Magnesium Sulphate, MgSO4.7H2O.—It can be purchased very pure, and is
occasionally used as a standard salt.
Manganese Dioxide, MnO2.—It is used in the preparation of chlorine. The
commercial article is not pure, but is sufficiently so for this purpose.
Marble, CaCO3.—Fragments of the white crystalline variety only should be
used. It is used as a source of lime and of carbon dioxide.
Mercury, Hg.—This can be purchased pure. It should have a bright surface,
flow without a tail, and leave no residue on ignition. It is used as a standard; for
amalgamation; and as a confining liquid in gas analysis.
Mercuric Chloride (HgCl2) may be purchased pure. Make a 5 per cent. solution
in water. It is used for destroying an excess of stannous chloride; for removing
sulphuretted hydrogen from solution; and as a test for stannous salts.
Microcosmic Salt, HAmNaPO4.8H2O.—When fused NaPO3 is formed. It is
used in testing for metallic oxides and silica before the blowpipe. The crystals
are sometimes used as a standard for phosphoric acid.
Page 92
"Nessler's Solution."—Mode of preparation: Dissolve 35 grams of potassium
iodide in 100 c.c. of water; dissolve 17 grams of mercuric chloride in 300 c.c. of
water, and pour this solution into that of the iodide till a permanent precipitate is
produced; make up to 1 litre with a 20 per cent. solution of potash; add mercuric
chloride till a precipitate is again formed; allow to settle and decant. It is used
for detecting ammonia.
Nitre.—This is potassium nitrate.
Platinum Chloride, 2HCl.PtCl4. (In the crystallised form it has 6H2O).—It may
be made as follows:—Take 5 grams of clean platinum scrap and dissolve in a
flask at a gentle heat in 50 c.c. of hydrochloric acid with the occasional addition
of some nitric acid; evaporate to a paste; and then dissolve in 100 c.c. of water.
It is used for separating and determining potassium.
Phenolphthalein is an organic compound used as an indicator; more especially
in determining the weaker acids, it cannot be used in the presence of ammonia.
Dissolve half a gram in 100 c.c. of dilute alcohol.
Potassium Bicarbonate, KHCO3.—It may be purchased pure; on ignition it
leaves the carbonate, K2CO3, which may be used as a standard.
Potassium Cyanide, KCN.—It is used in the dry assay as a reducing agent. The
commercial salt is very impure. Purchase that sold as potassic cyanide (gold)
which contains about 95 per cent. of KCN. It is used for copper assaying and
occasionally in separation. Make a 10 per cent. solution when wanted.
Potassium Bichromate, K2Cr2O7. It may be purchased nearly pure. It is used as
an oxidising agent, for determining iron; and as a test solution. For this last
purpose a 10 per cent. solution is prepared.
Potassium Chlorate (KClO3) can be purchased pure. It is used with
hydrochloric acid as a substitute for aqua regia.
Potassium Ferrocyanide (K4Fe(CN)6.3H2O), or "yellow prussiate of potash,"
is used as a test; as an indicator; and for the determination of zinc. Make a 5 per
cent. solution.
Potassium Ferricyanide (K6Fe2(CN)12), or "red prussiate of potash," is used
for testing; and as an indicator. Make a 5 per cent. solution when wanted, as it
decomposes on keeping.
iodide in 100 c.c. of water; dissolve 17 grams of mercuric chloride in 300 c.c. of
water, and pour this solution into that of the iodide till a permanent precipitate is
produced; make up to 1 litre with a 20 per cent. solution of potash; add mercuric
chloride till a precipitate is again formed; allow to settle and decant. It is used
for detecting ammonia.
Nitre.—This is potassium nitrate.
Platinum Chloride, 2HCl.PtCl4. (In the crystallised form it has 6H2O).—It may
be made as follows:—Take 5 grams of clean platinum scrap and dissolve in a
flask at a gentle heat in 50 c.c. of hydrochloric acid with the occasional addition
of some nitric acid; evaporate to a paste; and then dissolve in 100 c.c. of water.
It is used for separating and determining potassium.
Phenolphthalein is an organic compound used as an indicator; more especially
in determining the weaker acids, it cannot be used in the presence of ammonia.
Dissolve half a gram in 100 c.c. of dilute alcohol.
Potassium Bicarbonate, KHCO3.—It may be purchased pure; on ignition it
leaves the carbonate, K2CO3, which may be used as a standard.
Potassium Cyanide, KCN.—It is used in the dry assay as a reducing agent. The
commercial salt is very impure. Purchase that sold as potassic cyanide (gold)
which contains about 95 per cent. of KCN. It is used for copper assaying and
occasionally in separation. Make a 10 per cent. solution when wanted.
Potassium Bichromate, K2Cr2O7. It may be purchased nearly pure. It is used as
an oxidising agent, for determining iron; and as a test solution. For this last
purpose a 10 per cent. solution is prepared.
Potassium Chlorate (KClO3) can be purchased pure. It is used with
hydrochloric acid as a substitute for aqua regia.
Potassium Ferrocyanide (K4Fe(CN)6.3H2O), or "yellow prussiate of potash,"
is used as a test; as an indicator; and for the determination of zinc. Make a 5 per
cent. solution.
Potassium Ferricyanide (K6Fe2(CN)12), or "red prussiate of potash," is used
for testing; and as an indicator. Make a 5 per cent. solution when wanted, as it
decomposes on keeping.
Page 93
Potassium Hydrate, KHO. Purchase that purified with alcohol. It is an alkali,
and is used for absorbing carbonic acid, &c.
Potassium Iodide, KI. It may be purchased nearly pure. It is used as a test and
for dissolving iodine. It should be used in a 10 per cent. solution freshly made.
The solution decomposes on exposure to light, with separation of iodine.
Potassium Nitrate (KNO3) can be purchased pure. It is used in the dry way as
an oxidizing agent. It is very fusible. It decomposes at a low temperature into
potassium nitrite (KNO2) and free oxygen; and at a higher temperature leaves
potash (K2O). It oxidizes sulphur and carbon with explosive violence. This
action may be moderated by mixing the nitre with carbonate of soda, common
salt, or some other inert body.
Potassium Nitrite, KNO2.—The commercial article is not pure, but is
sufficiently so for the purpose required. A saturated solution is used in the
separation of cobalt; the solution is made when wanted.
Potassium Permanganate, KMnO4.—This salt can be purchased sufficiently
pure. It is much used as an oxidizing agent.
Potassium Bisulphate (KHSO4) is used as a dry reagent for opening up
minerals. It fuses; and at a much higher temperature is converted into potassium
sulphate with loss of sulphuric acid.
Potassium Sulphocyanate (KCNS) is used for the detection and determination
of traces of ferric iron; as also in the separation of silver and copper from some
of the other metals. Make a 10 per cent. solution. It should show no colour on
the addition of hydrochloric acid.
"Red Lead" (Pb3O4) is used in the dry assay as a flux instead of litharge, from
which it differs in containing a little more oxygen. When acted on by nitric acid
a brown residue of lead dioxide is left, nitrate of lead going into solution. Like
litharge it always carries silver; about 2 milligrams in 100 grams.
Silver, Ag.—Pure silver in foil is required as a standard. It may be prepared as
follows:—Dissolve scrap silver in dilute nitric acid and decant off from any
residue; dilute the solution with hot water and add hydrochloric acid until there
is no further precipitate, stir; allow the precipitate to settle; decant and wash; dry
the precipitate, mix it with twice its bulk of carbonate of soda and fuse the
and is used for absorbing carbonic acid, &c.
Potassium Iodide, KI. It may be purchased nearly pure. It is used as a test and
for dissolving iodine. It should be used in a 10 per cent. solution freshly made.
The solution decomposes on exposure to light, with separation of iodine.
Potassium Nitrate (KNO3) can be purchased pure. It is used in the dry way as
an oxidizing agent. It is very fusible. It decomposes at a low temperature into
potassium nitrite (KNO2) and free oxygen; and at a higher temperature leaves
potash (K2O). It oxidizes sulphur and carbon with explosive violence. This
action may be moderated by mixing the nitre with carbonate of soda, common
salt, or some other inert body.
Potassium Nitrite, KNO2.—The commercial article is not pure, but is
sufficiently so for the purpose required. A saturated solution is used in the
separation of cobalt; the solution is made when wanted.
Potassium Permanganate, KMnO4.—This salt can be purchased sufficiently
pure. It is much used as an oxidizing agent.
Potassium Bisulphate (KHSO4) is used as a dry reagent for opening up
minerals. It fuses; and at a much higher temperature is converted into potassium
sulphate with loss of sulphuric acid.
Potassium Sulphocyanate (KCNS) is used for the detection and determination
of traces of ferric iron; as also in the separation of silver and copper from some
of the other metals. Make a 10 per cent. solution. It should show no colour on
the addition of hydrochloric acid.
"Red Lead" (Pb3O4) is used in the dry assay as a flux instead of litharge, from
which it differs in containing a little more oxygen. When acted on by nitric acid
a brown residue of lead dioxide is left, nitrate of lead going into solution. Like
litharge it always carries silver; about 2 milligrams in 100 grams.
Silver, Ag.—Pure silver in foil is required as a standard. It may be prepared as
follows:—Dissolve scrap silver in dilute nitric acid and decant off from any
residue; dilute the solution with hot water and add hydrochloric acid until there
is no further precipitate, stir; allow the precipitate to settle; decant and wash; dry
the precipitate, mix it with twice its bulk of carbonate of soda and fuse the
Page 94
mixture in a crucible until tranquil; clean the button and roll or hammer it into
foil.
Sodium Acetate, NaC2H3O2.3H2O.—The crystals may be purchased
sufficiently pure. Make a 20 per cent. solution in water. It is used for replacing
mineral acids by acetic acid.[7]
Sodium Acetate and Acetic Acid.—A solution is used in the determination of
phosphates and arsenates; 100 grams of the salt is dissolved in 500 c.c. of acetic
acid, and diluted with water to one litre.
Sodium Bicarbonate (NaHCO3)is used as a flux in dry methods. On ignition it
leaves the carbonate (Na2CO3), which is used as a standard reagent. Make a 20
per cent. solution of the carbonate for use. It should be free from chlorides or
sulphates, or if impure the amount of impurities must be determined.
Sodium Hydrate, NaHO. It may be purchased in sticks, which should be kept in
a well-corked bottle. It is sometimes called "caustic soda." It is a strong alkali. It
is used for neutralizing acid solutions and for separations where ammonia is
unsuitable. Make a 5 per cent. solution for use.
Sodium Hyposulphite, Na2S2O8.5H2O.—It may be purchased pure. It is
generally known as "hypo." It is used as a standard.
Sodium Sulphite (Na2SO3.7H2O) is used as a reducing agent.
Sodium Phosphate, Na2HPO4.12H2O. The crystals may be purchased pure, but
they effloresce in dry air with loss of water. It is used as a standard and for
precipitating magnesia, &c. Make a 10 per cent. solution.
Stannous Chloride, SnCl2.2H2O.—The crystals are best purchased. If kept dry
and free from air they are fairly permanent. A solution is made by dissolving 20
grams in 10 c.c. of hydrochloric acid and diluting to 1 litre. The solution is not
permanent. It is a strong reducing agent, and is chiefly used in solution for this
purpose.
Tin, Sn.—Grain tin should be purchased. It is not pure, but contains 99.5 per
cent. of the metal. The chief impurity is copper. It can be used as a standard.
When acted on with hot hydrochloric acid it slowly dissolves (more rapidly in
contact with platinum) and forms stannous chloride.
foil.
Sodium Acetate, NaC2H3O2.3H2O.—The crystals may be purchased
sufficiently pure. Make a 20 per cent. solution in water. It is used for replacing
mineral acids by acetic acid.[7]
Sodium Acetate and Acetic Acid.—A solution is used in the determination of
phosphates and arsenates; 100 grams of the salt is dissolved in 500 c.c. of acetic
acid, and diluted with water to one litre.
Sodium Bicarbonate (NaHCO3)is used as a flux in dry methods. On ignition it
leaves the carbonate (Na2CO3), which is used as a standard reagent. Make a 20
per cent. solution of the carbonate for use. It should be free from chlorides or
sulphates, or if impure the amount of impurities must be determined.
Sodium Hydrate, NaHO. It may be purchased in sticks, which should be kept in
a well-corked bottle. It is sometimes called "caustic soda." It is a strong alkali. It
is used for neutralizing acid solutions and for separations where ammonia is
unsuitable. Make a 5 per cent. solution for use.
Sodium Hyposulphite, Na2S2O8.5H2O.—It may be purchased pure. It is
generally known as "hypo." It is used as a standard.
Sodium Sulphite (Na2SO3.7H2O) is used as a reducing agent.
Sodium Phosphate, Na2HPO4.12H2O. The crystals may be purchased pure, but
they effloresce in dry air with loss of water. It is used as a standard and for
precipitating magnesia, &c. Make a 10 per cent. solution.
Stannous Chloride, SnCl2.2H2O.—The crystals are best purchased. If kept dry
and free from air they are fairly permanent. A solution is made by dissolving 20
grams in 10 c.c. of hydrochloric acid and diluting to 1 litre. The solution is not
permanent. It is a strong reducing agent, and is chiefly used in solution for this
purpose.
Tin, Sn.—Grain tin should be purchased. It is not pure, but contains 99.5 per
cent. of the metal. The chief impurity is copper. It can be used as a standard.
When acted on with hot hydrochloric acid it slowly dissolves (more rapidly in
contact with platinum) and forms stannous chloride.
Page 95
Uranium Acetate, UO2(C2H3O2)2.H2O.—It is best purchased in crystals. The
solution is used for the determination of phosphates and arsenates. A solution of
3 per cent. strength is occasionally used as an indicator.
Uranium Nitrate, UO2(NO3)2.6H2O.—This salt is very soluble in water and is
sometimes used instead of the acetate, which is somewhat difficult to dissolve.
"Water," H2O.—Spring or well water is sufficiently pure for most purposes,
100 c.c. will leave a residue of from 10 to 30 milligrams, so that where a salt has
to be dissolved out, evaporated, and weighed it should be replaced by distilled
water. Rain water, melted snow, &c., always leave less residue than spring
water; but in other respects they are often dirtier. Distilled water is best prepared
in the office, a glass or tin condenser being used.
Zinc, Zn.—It is sold in a granulated form or in sticks. It generally contains over
1 per cent. of lead, with a little iron and arsenic. It is used for separating metals
from their solutions, and generally as a reducing agent. For the preparation of
hydrogen, and in most other cases, scrap sheet zinc may be used.
Zinc Oxide, ZnO.—The commercial oxide sometimes contains carbonate.
Zinc Sulphate, ZnSO4.7H2O.—It is occasionally used as a standard, and can be
purchased nearly pure.
FOOTNOTES:
[6] 3HCl + HNO3 = Cl2 + NOCl + 2H2O.
[7] NaC2H3O2 + HCl = H4C2O2 + NaCl.
solution is used for the determination of phosphates and arsenates. A solution of
3 per cent. strength is occasionally used as an indicator.
Uranium Nitrate, UO2(NO3)2.6H2O.—This salt is very soluble in water and is
sometimes used instead of the acetate, which is somewhat difficult to dissolve.
"Water," H2O.—Spring or well water is sufficiently pure for most purposes,
100 c.c. will leave a residue of from 10 to 30 milligrams, so that where a salt has
to be dissolved out, evaporated, and weighed it should be replaced by distilled
water. Rain water, melted snow, &c., always leave less residue than spring
water; but in other respects they are often dirtier. Distilled water is best prepared
in the office, a glass or tin condenser being used.
Zinc, Zn.—It is sold in a granulated form or in sticks. It generally contains over
1 per cent. of lead, with a little iron and arsenic. It is used for separating metals
from their solutions, and generally as a reducing agent. For the preparation of
hydrogen, and in most other cases, scrap sheet zinc may be used.
Zinc Oxide, ZnO.—The commercial oxide sometimes contains carbonate.
Zinc Sulphate, ZnSO4.7H2O.—It is occasionally used as a standard, and can be
purchased nearly pure.
FOOTNOTES:
[6] 3HCl + HNO3 = Cl2 + NOCl + 2H2O.
[7] NaC2H3O2 + HCl = H4C2O2 + NaCl.
Page 96
CHAPTER VII.
FORMULÆ, EQUATIONS, ETC.
Formulæ and equations are a kind of short hand for expressing briefly and in the
language of the atomic theory the facts of chemical composition and reaction.
The convenience of this method of expressing the facts justifies a short
description of it here.
On comparing the percentage composition of a series of compounds the
proportions in which the elements combine appears to be regulated by no simple
law. For example:
Realgar. Orpiment. Mispickel. Pyrites.
Arsenic 71.4 60.9 46.0 —
Sulphur 28.6 39.1 19.6 53.3
Iron — — 34.4 46.7
——— ——— ——— ———
100.0 100.0 100.0 100.0
But if in these examples the composition is calculated, not on 100 parts, but on
107, 246, 163, and 120 parts respectively, evidence of a simple law becomes
apparent.
Realgar. Orpiment. Mispickel. Pyrites.
Arsenic 75.0 150.0 75.0 —
Sulphur 32.0 96.0 32.0 64.0
Iron — — 56.0 56.0
——— ——— ——— ———
107.0 246.0 163.0 120.0
It will be seen that the proportion of arsenic is 75 or twice 75, that of iron is 56,
and that of sulphur 32 or some simple multiple of 32. The series of examples
might be extended indefinitely, and it would still be found that the "combining
proportions" held good. The number 75 is spoken of as the "combining weight,"
or, more frequently, as the "atomic weight" of arsenic. Similarly 56 is the atomic
FORMULÆ, EQUATIONS, ETC.
Formulæ and equations are a kind of short hand for expressing briefly and in the
language of the atomic theory the facts of chemical composition and reaction.
The convenience of this method of expressing the facts justifies a short
description of it here.
On comparing the percentage composition of a series of compounds the
proportions in which the elements combine appears to be regulated by no simple
law. For example:
Realgar. Orpiment. Mispickel. Pyrites.
Arsenic 71.4 60.9 46.0 —
Sulphur 28.6 39.1 19.6 53.3
Iron — — 34.4 46.7
——— ——— ——— ———
100.0 100.0 100.0 100.0
But if in these examples the composition is calculated, not on 100 parts, but on
107, 246, 163, and 120 parts respectively, evidence of a simple law becomes
apparent.
Realgar. Orpiment. Mispickel. Pyrites.
Arsenic 75.0 150.0 75.0 —
Sulphur 32.0 96.0 32.0 64.0
Iron — — 56.0 56.0
——— ——— ——— ———
107.0 246.0 163.0 120.0
It will be seen that the proportion of arsenic is 75 or twice 75, that of iron is 56,
and that of sulphur 32 or some simple multiple of 32. The series of examples
might be extended indefinitely, and it would still be found that the "combining
proportions" held good. The number 75 is spoken of as the "combining weight,"
or, more frequently, as the "atomic weight" of arsenic. Similarly 56 is the atomic
Page 97
weight of iron, and 32 the atomic weight of sulphur. The importance of this law
of chemical combination is altogether independent of the atomic theory; but this
theory furnishes the simplest explanation of the facts. According to it a chemical
compound is made up of exactly similar groups of particles. The particles of
each elementary substance are all alike, but differ from those of other elements
in weight. Ultimate particles are called atoms, and the groups of atoms are called
molecules. The atomic weight of any particular element is the weight of its atom
compared with the weight of an atom of hydrogen. The atom of sulphur, for
instance, is 32 times as heavy as the atom of hydrogen, and the atomic weight of
sulphur is 32. The molecular weight is the sum of the atomic weights of the
group. The molecule of pyrites contains two atoms of sulphur and one of iron:
on referring to the table of atomic weights it will be seen that the atomic weights
are—sulphur 32, and iron 56. The molecular weight, therefore, is 32 + 32 + 56
—that is, 120. The meaning of this is, 120 parts by weight of iron pyrites contain
64 parts of sulphur and 56 parts of iron; and this is true whether the "parts by
weight" be grains or tons.
The symbol or formula of an atom is generally the initial letter or letters of the
Latin or English name of the substance. The atom of hydrogen is written H, that
of oxygen O, of sulphur S, of iron (ferrum) Fe, and so on. A list of these symbols
is given in the table of atomic weights.
The formula of a molecule is obtained by placing together the symbols of the
contained atoms. Thus, Fe represents an atom of iron, S an atom of sulphur,
while FeS represents the molecule of sulphide of iron as containing one atom of
each element.
When more than one atom of an element is present this is shown by writing a
figure under and after the symbol; thus, FeS2 represents a molecule with one
atom of iron and two atoms of sulphur, Fe2S3 similarly shows one with two
atoms of iron and three of sulphur. When a group of atoms is enclosed in
brackets, a figure after and under the bracket multiplies all within it; for
example, Pb(NO3)2 is another way of writing PbN2O6. Sometimes it is
convenient to represent the atoms of a molecule as divided into two or more
groups; this may be done by writing the formulæ of the groups, and separating
each simple formula by a full stop. Slaked lime, for instance, has the formula
CaH2O2; or, as already explained, we may write it Ca(HO)2; or, if for purposes
of explanation we wished to look on it as lime (CaO) and water (H2O), we could
write it CaO.H2O. A plus sign (+) has a different meaning; CaO + H2O indicates
of chemical combination is altogether independent of the atomic theory; but this
theory furnishes the simplest explanation of the facts. According to it a chemical
compound is made up of exactly similar groups of particles. The particles of
each elementary substance are all alike, but differ from those of other elements
in weight. Ultimate particles are called atoms, and the groups of atoms are called
molecules. The atomic weight of any particular element is the weight of its atom
compared with the weight of an atom of hydrogen. The atom of sulphur, for
instance, is 32 times as heavy as the atom of hydrogen, and the atomic weight of
sulphur is 32. The molecular weight is the sum of the atomic weights of the
group. The molecule of pyrites contains two atoms of sulphur and one of iron:
on referring to the table of atomic weights it will be seen that the atomic weights
are—sulphur 32, and iron 56. The molecular weight, therefore, is 32 + 32 + 56
—that is, 120. The meaning of this is, 120 parts by weight of iron pyrites contain
64 parts of sulphur and 56 parts of iron; and this is true whether the "parts by
weight" be grains or tons.
The symbol or formula of an atom is generally the initial letter or letters of the
Latin or English name of the substance. The atom of hydrogen is written H, that
of oxygen O, of sulphur S, of iron (ferrum) Fe, and so on. A list of these symbols
is given in the table of atomic weights.
The formula of a molecule is obtained by placing together the symbols of the
contained atoms. Thus, Fe represents an atom of iron, S an atom of sulphur,
while FeS represents the molecule of sulphide of iron as containing one atom of
each element.
When more than one atom of an element is present this is shown by writing a
figure under and after the symbol; thus, FeS2 represents a molecule with one
atom of iron and two atoms of sulphur, Fe2S3 similarly shows one with two
atoms of iron and three of sulphur. When a group of atoms is enclosed in
brackets, a figure after and under the bracket multiplies all within it; for
example, Pb(NO3)2 is another way of writing PbN2O6. Sometimes it is
convenient to represent the atoms of a molecule as divided into two or more
groups; this may be done by writing the formulæ of the groups, and separating
each simple formula by a full stop. Slaked lime, for instance, has the formula
CaH2O2; or, as already explained, we may write it Ca(HO)2; or, if for purposes
of explanation we wished to look on it as lime (CaO) and water (H2O), we could
write it CaO.H2O. A plus sign (+) has a different meaning; CaO + H2O indicates
Page 98
quantities of two substances, water and lime, which are separate from each
other. The sign of equality (=) is generally used to separate a statement of the
reagents used from another statement of the products of the reaction; it may be
translated into the word "yields" or "becomes." The two statements form an
equation.
Ignoring the quantitative relation, the meaning of the equation CaO + H2O =
CaO.H2O is: "lime and water yield slaked lime." By referring to a table of
atomic weights we can elicit the quantitative relations thus:—
CaO + H2O = CaH2O2
↓ ↓ ↓
Ca = 40 H2 = 2 = 1×2 Ca = 40
O = 16 O = 16 H2 = 2 = 1×2
—— —— O2 = 32 = 16×2
56 18 ——
74
Or, putting it in words, 56 parts of lime combine with 18 parts of water to form
74 parts of slaked lime. This equation enables one to answer such a question as
this:—How much lime must be used to produce 1 cwt. of slaked lime? for, if 74
lbs. of slaked lime require 56 lbs. of lime, 112 lbs. will require (56 × 112)/74, or
about 84-3/4 lbs.
As another example having a closer bearing on assaying take the following
question:—"In order to assay 5 grams of 'black tin' (SnO2) by the cyanide
process, how much potassic cyanide (KCN) will be required?" The reaction is
SnO2 + 2KCN = Sn + 2KCNO
↓ ↓
Sn = 118 K = 39
O2 = 32 C = 12
—— N = 14
150 ——
65×2 = 130
What is sought for here is the relation between the quantities of SnO2 and KCN.
Note that a figure before a formula multiplies all that follows up to the next stop
other. The sign of equality (=) is generally used to separate a statement of the
reagents used from another statement of the products of the reaction; it may be
translated into the word "yields" or "becomes." The two statements form an
equation.
Ignoring the quantitative relation, the meaning of the equation CaO + H2O =
CaO.H2O is: "lime and water yield slaked lime." By referring to a table of
atomic weights we can elicit the quantitative relations thus:—
CaO + H2O = CaH2O2
↓ ↓ ↓
Ca = 40 H2 = 2 = 1×2 Ca = 40
O = 16 O = 16 H2 = 2 = 1×2
—— —— O2 = 32 = 16×2
56 18 ——
74
Or, putting it in words, 56 parts of lime combine with 18 parts of water to form
74 parts of slaked lime. This equation enables one to answer such a question as
this:—How much lime must be used to produce 1 cwt. of slaked lime? for, if 74
lbs. of slaked lime require 56 lbs. of lime, 112 lbs. will require (56 × 112)/74, or
about 84-3/4 lbs.
As another example having a closer bearing on assaying take the following
question:—"In order to assay 5 grams of 'black tin' (SnO2) by the cyanide
process, how much potassic cyanide (KCN) will be required?" The reaction is
SnO2 + 2KCN = Sn + 2KCNO
↓ ↓
Sn = 118 K = 39
O2 = 32 C = 12
—— N = 14
150 ——
65×2 = 130
What is sought for here is the relation between the quantities of SnO2 and KCN.
Note that a figure before a formula multiplies all that follows up to the next stop
Page 99
or plus or equality sign. The question is now resolved to this: if 150 grams of
oxide of tin require 130 grams of cyanide, how much will 5 grams require?
150 : 130 :: 5 : x
x = 4.33 grams.
A problem of frequent occurrence is to find the percentage composition of a
substance when its formula has been given. For example: "What percentage of
iron is contained in a mineral having the formula 2Fe2O3.3H2O?" Bringing this
formula together we have Fe4H6O9. Find the molecular weight.
Fe4 = 224 = 56×4
H6 = 6 = 1×6
O9 = 144 = 16×9
——
374
Then we get: 374 parts of the mineral contain 224 of iron. How much will 100
contain?
374 : 224 :: 100 : x
x = 59.89.
And the answer to the question is 59.89 per cent.
Again, suppose the question is of this kind:—"How much crystallised copper
sulphate (CuSO4.5H2O) will be required to make 2 litres of a solution, 1 c.c. of
which shall contain 0.0010 gram of copper?"
A litre is 1000 c.c., so, therefore, 2 litres of the solution must contain 0.001 gram
× 2000, or 2 grams. How much crystallised copper sulphate will contain this
amount of metal?
Cu = 63.3
S = 32.0
O4 = 64.0 = 16×4
5H2O = 90.0 = 18×5
————
249.3
oxide of tin require 130 grams of cyanide, how much will 5 grams require?
150 : 130 :: 5 : x
x = 4.33 grams.
A problem of frequent occurrence is to find the percentage composition of a
substance when its formula has been given. For example: "What percentage of
iron is contained in a mineral having the formula 2Fe2O3.3H2O?" Bringing this
formula together we have Fe4H6O9. Find the molecular weight.
Fe4 = 224 = 56×4
H6 = 6 = 1×6
O9 = 144 = 16×9
——
374
Then we get: 374 parts of the mineral contain 224 of iron. How much will 100
contain?
374 : 224 :: 100 : x
x = 59.89.
And the answer to the question is 59.89 per cent.
Again, suppose the question is of this kind:—"How much crystallised copper
sulphate (CuSO4.5H2O) will be required to make 2 litres of a solution, 1 c.c. of
which shall contain 0.0010 gram of copper?"
A litre is 1000 c.c., so, therefore, 2 litres of the solution must contain 0.001 gram
× 2000, or 2 grams. How much crystallised copper sulphate will contain this
amount of metal?
Cu = 63.3
S = 32.0
O4 = 64.0 = 16×4
5H2O = 90.0 = 18×5
————
249.3
Page 100
If 63.3 grams of copper are contained in 249.3 grams of sulphate, in how much
is 2 grams contained.
63.3 : 249.3 :: 2 grams : x
x = 7.8769 grams.
The answer is, 7.8769 grams must be taken.
As a sample of another class of problem similar in nature to the last (but a little
more complicated) take the following:—"What weight of permanganate of
potash must be taken to make 2 litres of a solution, 100 c.c. of which shall be
equivalent to 1 gram of iron?" In the first place the 2 litres must be equivalent to
20 grams of iron, for there are 20 × 100 c.c. in two litres. In the titration of iron
by permanganate solution there are two reactions. First in dissolving the iron
Fe + H2SO4 = FeSO4 + H2
↓
56
and second, in the actual titration,
10FeSO4 + 2KMnO4 + 9H2SO4= 2MnSO4 + 5Fe2(SO4)3 + 2KHSO4 + 8H2O
↓
K = 39
Mn = 55
O4= 64
——
158 × 2 = 316
As before, attention is confined to the two substances under consideration—viz.,
Fe and KMnO4. In the second equation, we find 316 parts of the permanganate
are required for 10 molecules of FeSO4; and in the first equation 56 parts of iron
are equivalent to one molecule of FeSO4, therefore 560 of iron are equivalent to
316 of permanganate; and the question is, How much of the permanganate will
be equivalent to 20 grams of iron?
560 : 316 :: 20 grams : x.
x = 11.286 grams.
The answer is 11.286 grams.
is 2 grams contained.
63.3 : 249.3 :: 2 grams : x
x = 7.8769 grams.
The answer is, 7.8769 grams must be taken.
As a sample of another class of problem similar in nature to the last (but a little
more complicated) take the following:—"What weight of permanganate of
potash must be taken to make 2 litres of a solution, 100 c.c. of which shall be
equivalent to 1 gram of iron?" In the first place the 2 litres must be equivalent to
20 grams of iron, for there are 20 × 100 c.c. in two litres. In the titration of iron
by permanganate solution there are two reactions. First in dissolving the iron
Fe + H2SO4 = FeSO4 + H2
↓
56
and second, in the actual titration,
10FeSO4 + 2KMnO4 + 9H2SO4= 2MnSO4 + 5Fe2(SO4)3 + 2KHSO4 + 8H2O
↓
K = 39
Mn = 55
O4= 64
——
158 × 2 = 316
As before, attention is confined to the two substances under consideration—viz.,
Fe and KMnO4. In the second equation, we find 316 parts of the permanganate
are required for 10 molecules of FeSO4; and in the first equation 56 parts of iron
are equivalent to one molecule of FeSO4, therefore 560 of iron are equivalent to
316 of permanganate; and the question is, How much of the permanganate will
be equivalent to 20 grams of iron?
560 : 316 :: 20 grams : x.
x = 11.286 grams.
The answer is 11.286 grams.
Page 101
Very similar to this last problem is the question suggested under the head
"Indirect Titration" (p. 43). "If 100 c.c. of the standard permanganate solution
are equivalent to 1 gram of iron, how much peroxide of manganese will they be
equivalent to?" The equation for dissolving the iron is already given; the second
equation is
2FeSO4 + MnO2 + 2H2SO4 = Fe2(SO4)2 + MnSO4 + 2H2O
↓
Mn = 55
O2 = 32
——
87
It will be seen that 87 grams of peroxide of manganese are equivalent to 112
grams of iron. How much then is equivalent to 1 gram of iron?
112 : 87 :: 1 gram : x
x = 0.7767 gram.
It is sometimes convenient to calculate the formula of a substance from its
analysis. The method of calculating is shown by the following example.
Required the formula of a mineral which gave the following figures on analysis:
—
Cupric oxide (CuO) 10.58
Ferrous oxide (FeO) 15.69
Zinc oxide (ZnO) 0.35
Sulphuric oxide (SO2) 28.82
Water (H2O) 44.71
——————
100.15
First find the molecular weights of CuO, FeO, &c., and divide the corresponding
percentages by these figures. Thus, CuO = 63.3+16 = 79.3 and 10.58 divided by
79.3 gives 0.1334. Similarly FeO = 56+16 = 72 and 15.69 divided by 72 gives
0.2179. Treated in the same way the oxide of zinc, sulphuric oxide and water
give as results 0.0043, 0.3602 and 2.484.
Classify the results as follows:—
"Indirect Titration" (p. 43). "If 100 c.c. of the standard permanganate solution
are equivalent to 1 gram of iron, how much peroxide of manganese will they be
equivalent to?" The equation for dissolving the iron is already given; the second
equation is
2FeSO4 + MnO2 + 2H2SO4 = Fe2(SO4)2 + MnSO4 + 2H2O
↓
Mn = 55
O2 = 32
——
87
It will be seen that 87 grams of peroxide of manganese are equivalent to 112
grams of iron. How much then is equivalent to 1 gram of iron?
112 : 87 :: 1 gram : x
x = 0.7767 gram.
It is sometimes convenient to calculate the formula of a substance from its
analysis. The method of calculating is shown by the following example.
Required the formula of a mineral which gave the following figures on analysis:
—
Cupric oxide (CuO) 10.58
Ferrous oxide (FeO) 15.69
Zinc oxide (ZnO) 0.35
Sulphuric oxide (SO2) 28.82
Water (H2O) 44.71
——————
100.15
First find the molecular weights of CuO, FeO, &c., and divide the corresponding
percentages by these figures. Thus, CuO = 63.3+16 = 79.3 and 10.58 divided by
79.3 gives 0.1334. Similarly FeO = 56+16 = 72 and 15.69 divided by 72 gives
0.2179. Treated in the same way the oxide of zinc, sulphuric oxide and water
give as results 0.0043, 0.3602 and 2.484.
Classify the results as follows:—
Page 102
Bases. Acids. Water.
CuO 0.1334 SO3 0.3602 H2O 2.484
FeO 0.2179
ZnO 0.0043
—————————— —————————— ——————————
RO 0.3556 RO3 0.3602 R2O 2.484
The figures 0.3556, 0.3602 and 2.484 should be then divided by the lowest of
them—i.e., 0.3556; or where, as in this case, two of the figures are very near
each other the mean of these may be taken—i.e., 0.3579. Whichever is taken the
figures got will be approximately 1, 1 and 7. The formula is then RO.SO3.7H2O
in which R is nearly 2/5ths copper, 3/5ths iron and a little zinc.
This formula requires the following percentage composition, which for the sake
of comparison is placed side by side with the actual results.
Calculated. Found.
Cupric oxide 11.29 10.58
Ferrous oxide 15.37 15.69
Zinc oxide nil 0.35
Sulphuric oxide 28.47 28.82
Water 44.84 44.71
——————
99.97 100.15
Trimming the results of an analysis to make them fit in more closely with the
calculations from the formula would be foolish as well as dishonest. There can
be no doubt that the actual analytical results represent the composition of the
specimen much more closely than the formula does; although perhaps other
specimens of the same mineral would yield results which would group
themselves better around the calculated results than around those of the first
specimen analysed. It must be remembered that substances are rarely found pure
either in nature or in the arts; so that in most cases the formula only gives an
approximation to the truth. In the case of hydrated salts there is generally a
difficulty in getting the salt with exactly the right proportion of water.
PRACTICAL EXERCISES.
CuO 0.1334 SO3 0.3602 H2O 2.484
FeO 0.2179
ZnO 0.0043
—————————— —————————— ——————————
RO 0.3556 RO3 0.3602 R2O 2.484
The figures 0.3556, 0.3602 and 2.484 should be then divided by the lowest of
them—i.e., 0.3556; or where, as in this case, two of the figures are very near
each other the mean of these may be taken—i.e., 0.3579. Whichever is taken the
figures got will be approximately 1, 1 and 7. The formula is then RO.SO3.7H2O
in which R is nearly 2/5ths copper, 3/5ths iron and a little zinc.
This formula requires the following percentage composition, which for the sake
of comparison is placed side by side with the actual results.
Calculated. Found.
Cupric oxide 11.29 10.58
Ferrous oxide 15.37 15.69
Zinc oxide nil 0.35
Sulphuric oxide 28.47 28.82
Water 44.84 44.71
——————
99.97 100.15
Trimming the results of an analysis to make them fit in more closely with the
calculations from the formula would be foolish as well as dishonest. There can
be no doubt that the actual analytical results represent the composition of the
specimen much more closely than the formula does; although perhaps other
specimens of the same mineral would yield results which would group
themselves better around the calculated results than around those of the first
specimen analysed. It must be remembered that substances are rarely found pure
either in nature or in the arts; so that in most cases the formula only gives an
approximation to the truth. In the case of hydrated salts there is generally a
difficulty in getting the salt with exactly the right proportion of water.
PRACTICAL EXERCISES.
Page 103
The following calculations may be made:—
1. Calculate standards in the following cases—
(a) Silver taken, 1.003 gram. Standard salt used, 100.15 c.c.
(b) Iron taken, 0.7 gram. Bichromate used, 69.6 c.c.
2. Calculate percentages:—
(a) Ore taken, 1 gram. Solution used, 65.2 c.c. Standard, 0.987 gram.
(b) Ore taken, 1 gram. Barium sulphate got, 1.432 gram. Barium sulphate
contains 13.73 per cent. of sulphur, and the percentage of sulphur in the ore is
wanted.
(c) Barium sulphate is BaSO4. Calculate the percentage of sulphur it contains,
for use in the preceding question.
3. A method of estimating the quantity of peroxide in a manganese ore is based
on the following reactions:—
(1) MnO2 + 4HCl = MnCl2 + Cl2 + 2H2O.
(2) Cl + KI = KCl + I.
To how much MnO2 is 1 gram of Iodine (I) equivalent?
4. A mineral has the following composition:—
Carbonic acid (CO2) 19.09
Copper oxide (CuO) 71.46
Water (H2O) 9.02
What is its formula?
5. How much copper is contained in 1.5 gram of crystallized copper sulphate
(CuSO4.5H2O)? How much of these crystals must be taken to give 0.4 gram of
copper?
6. How much ferrous sulphate crystals (FeSO4.7H2O) must be taken to yield 2
1. Calculate standards in the following cases—
(a) Silver taken, 1.003 gram. Standard salt used, 100.15 c.c.
(b) Iron taken, 0.7 gram. Bichromate used, 69.6 c.c.
2. Calculate percentages:—
(a) Ore taken, 1 gram. Solution used, 65.2 c.c. Standard, 0.987 gram.
(b) Ore taken, 1 gram. Barium sulphate got, 1.432 gram. Barium sulphate
contains 13.73 per cent. of sulphur, and the percentage of sulphur in the ore is
wanted.
(c) Barium sulphate is BaSO4. Calculate the percentage of sulphur it contains,
for use in the preceding question.
3. A method of estimating the quantity of peroxide in a manganese ore is based
on the following reactions:—
(1) MnO2 + 4HCl = MnCl2 + Cl2 + 2H2O.
(2) Cl + KI = KCl + I.
To how much MnO2 is 1 gram of Iodine (I) equivalent?
4. A mineral has the following composition:—
Carbonic acid (CO2) 19.09
Copper oxide (CuO) 71.46
Water (H2O) 9.02
What is its formula?
5. How much copper is contained in 1.5 gram of crystallized copper sulphate
(CuSO4.5H2O)? How much of these crystals must be taken to give 0.4 gram of
copper?
6. How much ferrous sulphate crystals (FeSO4.7H2O) must be taken to yield 2
Page 104
litres of a solution, 100 c.c. of which shall contain 0.56 gram of iron?
7. Galena is PbS, and hæmatite Fe2O3. What percentages of metal do these
minerals contain?
7. Galena is PbS, and hæmatite Fe2O3. What percentages of metal do these
minerals contain?
Page 105
CHAPTER VIII
SPECIFIC GRAVITY.
The relation of the weight of a substance to its volume should be kept in mind in
all cases where both weight and volume are dealt with. Students are apt to
imagine that on mixing equal volumes of, say, sulphuric acid and water, an acid
of half the strength must be obtained. If the statement of strength is in parts by
weight this will lead to considerable error. For example, 100 c.c. of sulphuric
acid containing 98 per cent. by weight of real acid, will, if diluted with 100 c.c.
of water, yield a solution containing not 49 per cent. by weight, but about 63.5
per cent. of the acid. The reason is this: the 100 c.c. of sulphuric acid weighs 184
grams, and contains 180.32 grams of real acid, while the 100 c.c. of water
weighs only 100 grams; the mixed water and acid weighs 284 grams, and
contains 180.32 of real acid, which is equivalent to nearly 63.5 per cent. by
weight. If, however, the method of statement be volumetric, it would be correct
to say that doubling the volume halves the strength: if 100 c.c. of brine contains
10 grams of salt, and is diluted with water to 200 c.c., it would be of one-half the
former strength, that is, 100 c.c. of the solution would contain 5 grams of salt.
This confusion is avoided by always stating the strengths as so many grams or
"c.c." in 100 c.c. of the liquid. But obviously it would be advantageous to be
able to determine quickly the weight of any particular substance corresponding
to 1 c.c. or some other given volume. Moreover, in descriptions of processes the
strengths of acids and solutions are frequently defined neither by their
gravimetric nor volumetric composition, but by a statement either of specific
gravity or of the degrees registered by Twaddell's or Beaumé's hydrometer.
Thus, in the description of the process of gold parting, one writer gives: "The
acid should be of 1.2 specific gravity"; and another says: "The acid must not be
stronger than 32° Beaumé."
These considerations justify an account of the subject in such a work as this.
And on other grounds the determination of a specific gravity is one of the
operations with which an assayer should be familiar.
The meaning of "specific gravity" is present in the mind of every one who uses
the sentence "lead is heavier than water." This is meaningless except some such
SPECIFIC GRAVITY.
The relation of the weight of a substance to its volume should be kept in mind in
all cases where both weight and volume are dealt with. Students are apt to
imagine that on mixing equal volumes of, say, sulphuric acid and water, an acid
of half the strength must be obtained. If the statement of strength is in parts by
weight this will lead to considerable error. For example, 100 c.c. of sulphuric
acid containing 98 per cent. by weight of real acid, will, if diluted with 100 c.c.
of water, yield a solution containing not 49 per cent. by weight, but about 63.5
per cent. of the acid. The reason is this: the 100 c.c. of sulphuric acid weighs 184
grams, and contains 180.32 grams of real acid, while the 100 c.c. of water
weighs only 100 grams; the mixed water and acid weighs 284 grams, and
contains 180.32 of real acid, which is equivalent to nearly 63.5 per cent. by
weight. If, however, the method of statement be volumetric, it would be correct
to say that doubling the volume halves the strength: if 100 c.c. of brine contains
10 grams of salt, and is diluted with water to 200 c.c., it would be of one-half the
former strength, that is, 100 c.c. of the solution would contain 5 grams of salt.
This confusion is avoided by always stating the strengths as so many grams or
"c.c." in 100 c.c. of the liquid. But obviously it would be advantageous to be
able to determine quickly the weight of any particular substance corresponding
to 1 c.c. or some other given volume. Moreover, in descriptions of processes the
strengths of acids and solutions are frequently defined neither by their
gravimetric nor volumetric composition, but by a statement either of specific
gravity or of the degrees registered by Twaddell's or Beaumé's hydrometer.
Thus, in the description of the process of gold parting, one writer gives: "The
acid should be of 1.2 specific gravity"; and another says: "The acid must not be
stronger than 32° Beaumé."
These considerations justify an account of the subject in such a work as this.
And on other grounds the determination of a specific gravity is one of the
operations with which an assayer should be familiar.
The meaning of "specific gravity" is present in the mind of every one who uses
the sentence "lead is heavier than water." This is meaningless except some such
Page 106
phrase as "bulk for bulk" be added. Make the sentence quantitative by saying:
"bulk for bulk lead is 11.36 times heavier than water," and one has the exact
meaning of: "the specific gravity of lead is 11.36." A table of the specific
gravities of liquids and solids shows how many times heavier the substances are
than water.
It is better, however, to look upon the specific gravity (written shortly, sp. g.) as
the weight of a substance divided by its volume. In the metric system, 1 c.c. of
water at 4° C. weighs with sufficient exactness 1 gram; consequently, the sp. g.,
which states how many times heavier than water the substance is, also expresses
the weight in grams of one c.c. of it. So that if a 100 c.c. flask of nitric acid
weighs, after the weight of the flask has been deducted, 120 grams, 1 c.c. of the
acid weighs 1.2 gram, and the sp. g. is 1.2. The specific gravity, then, may be
determined by dividing the weight of a substance in grams by its volume in c.c.;
but it is more convenient in practice to determine it by dividing the weight of the
substance by the weight of an equal volume of water. And since the volumes of
all substances, water included, vary with the temperature, the temperature at
which the sp. g. is determined should be recorded. Even then there is room for
ambiguity to the extent that such a statement as the following, "the specific
gravity of the substance at 50° C. is 0.9010," may mean when compared with
water at 50° C. or 4° C., or even 15.5° C. For practical purposes it should mean
the first of these, for in the actual experiments the water and the substance are
compared at the same temperature, and it is well to give the statement of results
without any superfluous calculation. In the metric system the standard
temperature is 4° C., for it is at this point that 1 c.c. of water weighs exactly 1
gram. In England, the standard temperature is 60° F. (15.5° C.), which is
supposed to be an average temperature of the balance-room. The convenience of
the English standard, however, is merely apparent; it demands warming
sometimes and sometimes cooling. For most purposes it is more convenient to
select a temperature sufficiently high to avoid the necessity of cooling at any
time. Warming to the required temperature gives very little trouble.
Determination of Specific Gravity.—There is a quick and easy method of
determining the density or sp. g. of a liquid, based upon the fact that a floating
body is buoyed up more by a heavy liquid than by a light one. The method is
more remarkable for speed than accuracy, but still is sufficiently exact. The
piece of apparatus used for the purpose is endowed with a variety of names—sp.
g. spindle, hydrometer, areometer, salimeter, alcoholimeter, lactometer, and so
on, according to the special liquid upon which it is intended to be used. It
consists of a float with a sinker at one end and a graduated tube or rod at the
"bulk for bulk lead is 11.36 times heavier than water," and one has the exact
meaning of: "the specific gravity of lead is 11.36." A table of the specific
gravities of liquids and solids shows how many times heavier the substances are
than water.
It is better, however, to look upon the specific gravity (written shortly, sp. g.) as
the weight of a substance divided by its volume. In the metric system, 1 c.c. of
water at 4° C. weighs with sufficient exactness 1 gram; consequently, the sp. g.,
which states how many times heavier than water the substance is, also expresses
the weight in grams of one c.c. of it. So that if a 100 c.c. flask of nitric acid
weighs, after the weight of the flask has been deducted, 120 grams, 1 c.c. of the
acid weighs 1.2 gram, and the sp. g. is 1.2. The specific gravity, then, may be
determined by dividing the weight of a substance in grams by its volume in c.c.;
but it is more convenient in practice to determine it by dividing the weight of the
substance by the weight of an equal volume of water. And since the volumes of
all substances, water included, vary with the temperature, the temperature at
which the sp. g. is determined should be recorded. Even then there is room for
ambiguity to the extent that such a statement as the following, "the specific
gravity of the substance at 50° C. is 0.9010," may mean when compared with
water at 50° C. or 4° C., or even 15.5° C. For practical purposes it should mean
the first of these, for in the actual experiments the water and the substance are
compared at the same temperature, and it is well to give the statement of results
without any superfluous calculation. In the metric system the standard
temperature is 4° C., for it is at this point that 1 c.c. of water weighs exactly 1
gram. In England, the standard temperature is 60° F. (15.5° C.), which is
supposed to be an average temperature of the balance-room. The convenience of
the English standard, however, is merely apparent; it demands warming
sometimes and sometimes cooling. For most purposes it is more convenient to
select a temperature sufficiently high to avoid the necessity of cooling at any
time. Warming to the required temperature gives very little trouble.
Determination of Specific Gravity.—There is a quick and easy method of
determining the density or sp. g. of a liquid, based upon the fact that a floating
body is buoyed up more by a heavy liquid than by a light one. The method is
more remarkable for speed than accuracy, but still is sufficiently exact. The
piece of apparatus used for the purpose is endowed with a variety of names—sp.
g. spindle, hydrometer, areometer, salimeter, alcoholimeter, lactometer, and so
on, according to the special liquid upon which it is intended to be used. It
consists of a float with a sinker at one end and a graduated tube or rod at the
Page 107
other. It is made of metal or glass. Generally two are required, one for liquids
ranging in sp. g. from 1.000 to 2.000, and another, which will indicate a sp. g.
between 0.700 and 1.000. The range depends on the size of the instrument. For
special work, in which variations within narrow limits are to be determined,
more delicate instruments with a narrower range are made.
ranging in sp. g. from 1.000 to 2.000, and another, which will indicate a sp. g.
between 0.700 and 1.000. The range depends on the size of the instrument. For
special work, in which variations within narrow limits are to be determined,
more delicate instruments with a narrower range are made.
Page 108
In using a hydrometer, the liquid to be tested is placed in a cylinder (fig. 34)
tall enough to allow the instrument to float, and not too narrow. The
temperature is taken, and the hydrometer is immersed in the fluid. The mark
on the hydrometer stem, level with the surface of the liquid, is read off.
With transparent liquids it is best to read the mark under and over the water
surface and take the mean.
The graduation of hydrometers is not made to any uniform system. Those
marked in degrees Baumé or Twaddell, or according to specific gravity, are
most commonly used. The degrees on Baumé's hydrometer agree among
themselves in being at equal distances along the stem; but they are
proportional neither to the specific gravity, nor to the percentage of salt in
the solution. They may be converted into an ordinary statement of specific
gravity by the following formulæ:—
Sp. g. = 144.3/(144.3-degrees Baumé.)
tall enough to allow the instrument to float, and not too narrow. The
temperature is taken, and the hydrometer is immersed in the fluid. The mark
on the hydrometer stem, level with the surface of the liquid, is read off.
With transparent liquids it is best to read the mark under and over the water
surface and take the mean.
The graduation of hydrometers is not made to any uniform system. Those
marked in degrees Baumé or Twaddell, or according to specific gravity, are
most commonly used. The degrees on Baumé's hydrometer agree among
themselves in being at equal distances along the stem; but they are
proportional neither to the specific gravity, nor to the percentage of salt in
the solution. They may be converted into an ordinary statement of specific
gravity by the following formulæ:—
Sp. g. = 144.3/(144.3-degrees Baumé.)
Page 109
or putting the rule in words, subtract the degrees Baumé from 144.3, and
divide 144.3 with the number thus obtained. For example: 32° Baumé
equals a sp. g. of 1.285.
144.3/(144.3-32) = 144.3/(112.3) = 1.285
This rule is for liquids heavier than water; for the lighter liquids the rule is
as follows:—
Sp. g. = 146/(136 + degrees Baumé.)
or in words divide 146 by the number of degrees Baumé added to 136. For
example: ammonia of 30° Beaumé has a sp. g. of 0.880 (nearly).
146/(136+30) = 146/166 = 0.8795
A simple series of calculations enables one to convert a Beaumé hydrometer
into one showing the actual sp. g. Graduation, according to sp. g. is the
most convenient for general purposes. In these instruments the distances
between the divisions become less as the densities increase.
Twaddell's hydrometer is graduated in this way: Each degree Twaddell is
0.005 in excess of unity. To convert into sp. g. multiply the degrees
Twaddell by 0.005, and add 1. For example: 25° Twaddell equals a sp. g. of
1.125.
25×.005 = 0.125; + 1.000 = 1.125.
There is a practice which ignores the decimal point and speaks of a sp. g. of
1125 instead of 1.125. In some cases it is convenient, and inasmuch as no
substance has a real sp. g. of much over 20, it can lead to no confusion. The
figures expressed in this way represent the weight of a litre in grams.
Some hydrometers are graduated so as to show at a glance the percentage
composition of the liquid they are intended to be used with. Gay-Lussac
designed one to show the alcoholic strength of mixtures of alcohol and
water; the construction of others upon the same principle is easy and
perhaps useful. But when the principle is applied to complex liquids and
mixed solutions, it is misleading.
divide 144.3 with the number thus obtained. For example: 32° Baumé
equals a sp. g. of 1.285.
144.3/(144.3-32) = 144.3/(112.3) = 1.285
This rule is for liquids heavier than water; for the lighter liquids the rule is
as follows:—
Sp. g. = 146/(136 + degrees Baumé.)
or in words divide 146 by the number of degrees Baumé added to 136. For
example: ammonia of 30° Beaumé has a sp. g. of 0.880 (nearly).
146/(136+30) = 146/166 = 0.8795
A simple series of calculations enables one to convert a Beaumé hydrometer
into one showing the actual sp. g. Graduation, according to sp. g. is the
most convenient for general purposes. In these instruments the distances
between the divisions become less as the densities increase.
Twaddell's hydrometer is graduated in this way: Each degree Twaddell is
0.005 in excess of unity. To convert into sp. g. multiply the degrees
Twaddell by 0.005, and add 1. For example: 25° Twaddell equals a sp. g. of
1.125.
25×.005 = 0.125; + 1.000 = 1.125.
There is a practice which ignores the decimal point and speaks of a sp. g. of
1125 instead of 1.125. In some cases it is convenient, and inasmuch as no
substance has a real sp. g. of much over 20, it can lead to no confusion. The
figures expressed in this way represent the weight of a litre in grams.
Some hydrometers are graduated so as to show at a glance the percentage
composition of the liquid they are intended to be used with. Gay-Lussac
designed one to show the alcoholic strength of mixtures of alcohol and
water; the construction of others upon the same principle is easy and
perhaps useful. But when the principle is applied to complex liquids and
mixed solutions, it is misleading.
Page 110
The various methods of graduation ought all to give place to one showing a
simple statement of the sp. g.
The method of determining sp. g. with the hydrometer is obviously
inapplicable to the case of solids, and in the case of liquids it should not be
used where exact figures are required. There are several other methods
which may be used, but on the whole those with the specific gravity bottle
are most convenient.
The specific gravity bottle (fig. 35) is a light flask of about 25 c.c.
capacity, provided with a well-fitting perforated stopper. It is essentially a
graduated flask, which measures a constant volume, but it does not much
matter what the volume is.
In taking the sp. g. of a liquid (or, what is the same thing, a fused solid)
there is wanted the weights (1) of the flaskful of water and (2) of the
flaskful of the liquid. Dividing the second by the first gives the required sp.
g. The actual weighings required are—
(1) of the dry and empty flask,
(2) of the flask filled with water, and
(3) of the flask filled with the liquid.
simple statement of the sp. g.
The method of determining sp. g. with the hydrometer is obviously
inapplicable to the case of solids, and in the case of liquids it should not be
used where exact figures are required. There are several other methods
which may be used, but on the whole those with the specific gravity bottle
are most convenient.
The specific gravity bottle (fig. 35) is a light flask of about 25 c.c.
capacity, provided with a well-fitting perforated stopper. It is essentially a
graduated flask, which measures a constant volume, but it does not much
matter what the volume is.
In taking the sp. g. of a liquid (or, what is the same thing, a fused solid)
there is wanted the weights (1) of the flaskful of water and (2) of the
flaskful of the liquid. Dividing the second by the first gives the required sp.
g. The actual weighings required are—
(1) of the dry and empty flask,
(2) of the flask filled with water, and
(3) of the flask filled with the liquid.
Page 111
The weighing of the flask once made need not be often repeated. It is well
to do so now and then for safety's sake; but one weighing will serve for a
large number of determinations. The same remarks apply to the weighing of
the bottle filled with water. The bottle is dried by rinsing out first with
alcohol and afterwards with ether; ether is very volatile, and a short
exposure in a warm place will soon drive off the little remaining about the
sides. The ether vapour should be sucked out through a glass tube. See that
the bore of the stopper is dry as well as the bottle. Let the dry bottle stand in
the box of the balance for a minute or two before weighing. The weight is,
strictly speaking, not that of the empty bottle, but of the bottle filled with
air. The empty bottle would weigh from 20 to 30 milligrams less.
Correcting for this would, in most cases, only make a difference in the
fourth place of decimals,[8] so that it is better to ignore the error.
The weight of the flask filled with water is got by filling it with distilled
water, and inserting the stopper. The excess of water will overflow at the
margin and through the bore. The bottle is wiped with a soft, dry cloth,
taking care not to squeeze or warm the bottle. The bottle will remain filled
to the top of the stopper. It is allowed to stand in the balance box for a
minute or two, and then weighed.
Distilled water, as stated, should be used; the use of ordinary water may
increase the weight by 5 or 6 milligrams. Many waters, if they have not
previously been boiled, give off bubbles of air which render the weighing
worthless.
The temperature of the water is of greater importance; lowering the
temperature 2° will increase the weight by 10 or 12 milligrams. A beaker of
water may be warmed or cooled to the required temperature; then the bottle
is filled from it, and quickly weighed. If the balance-room is cooler than the
water, the latter will draw back into the bottle, and a few small bubbles of
air will enter; but even in extreme cases this will only increase the weight
by a very small fraction of a milligram. There is more trouble caused when
the room is warmer, for the liquid then expands and protrudes as a drop
resting on the top of the stopper. There will in this case be loss by
evaporation, which in the case of the more volatile liquids, such as alcohol,
is serious. To prevent this loss, as well as any that may arise by overflow,
the stopper should be dilated above into a small cup, A (fig. 36), which may
to do so now and then for safety's sake; but one weighing will serve for a
large number of determinations. The same remarks apply to the weighing of
the bottle filled with water. The bottle is dried by rinsing out first with
alcohol and afterwards with ether; ether is very volatile, and a short
exposure in a warm place will soon drive off the little remaining about the
sides. The ether vapour should be sucked out through a glass tube. See that
the bore of the stopper is dry as well as the bottle. Let the dry bottle stand in
the box of the balance for a minute or two before weighing. The weight is,
strictly speaking, not that of the empty bottle, but of the bottle filled with
air. The empty bottle would weigh from 20 to 30 milligrams less.
Correcting for this would, in most cases, only make a difference in the
fourth place of decimals,[8] so that it is better to ignore the error.
The weight of the flask filled with water is got by filling it with distilled
water, and inserting the stopper. The excess of water will overflow at the
margin and through the bore. The bottle is wiped with a soft, dry cloth,
taking care not to squeeze or warm the bottle. The bottle will remain filled
to the top of the stopper. It is allowed to stand in the balance box for a
minute or two, and then weighed.
Distilled water, as stated, should be used; the use of ordinary water may
increase the weight by 5 or 6 milligrams. Many waters, if they have not
previously been boiled, give off bubbles of air which render the weighing
worthless.
The temperature of the water is of greater importance; lowering the
temperature 2° will increase the weight by 10 or 12 milligrams. A beaker of
water may be warmed or cooled to the required temperature; then the bottle
is filled from it, and quickly weighed. If the balance-room is cooler than the
water, the latter will draw back into the bottle, and a few small bubbles of
air will enter; but even in extreme cases this will only increase the weight
by a very small fraction of a milligram. There is more trouble caused when
the room is warmer, for the liquid then expands and protrudes as a drop
resting on the top of the stopper. There will in this case be loss by
evaporation, which in the case of the more volatile liquids, such as alcohol,
is serious. To prevent this loss, as well as any that may arise by overflow,
the stopper should be dilated above into a small cup, A (fig. 36), which may
Page 112
itself be stoppered. In a bottle of this kind the neck of the stopper is
graduated, and the bottle is considered full when the liquid stands at the
level of the mark in the neck. On inserting the stopper, the liquid rises into
the cup, and is reduced to the level of the mark by absorption with pieces of
filter-paper.
For most purposes, however, there is no need for cooling and allowing
room for subsequent expansion. The assayer, as a rule, can select his own
standard temperature, and may choose one which will always necessitate
warming. It will be handier in this case to have a bottle with a thermometer
stopper. Of the two types shown in fig. 37, that with the external
thermometer tube (A) is more generally useful.
graduated, and the bottle is considered full when the liquid stands at the
level of the mark in the neck. On inserting the stopper, the liquid rises into
the cup, and is reduced to the level of the mark by absorption with pieces of
filter-paper.
For most purposes, however, there is no need for cooling and allowing
room for subsequent expansion. The assayer, as a rule, can select his own
standard temperature, and may choose one which will always necessitate
warming. It will be handier in this case to have a bottle with a thermometer
stopper. Of the two types shown in fig. 37, that with the external
thermometer tube (A) is more generally useful.
Page 113
The bottle is filled at a lower temperature, and is then gently warmed so as
to slowly raise the temperature to the required degree. The superfluous
liquid is then at once wiped off, and the bottle cooled and weighed.
The weight of the flask filled with the liquid whose sp. g. has to be
determined is ascertained in a similar way. Of course the temperature must
be the same. If the liquid does not mix with water, the bottle should be dried
before filling, but otherwise the flask need only be rinsed out two or three
times with the liquid.
Having obtained the three weighings, deduct the weight of the bottle from
each of the others to get the weights of the water and liquid respectively.
Divide the latter by the former, the result shows the sp. g. As an example,
take the following, in which a rather large sp. g. bottle was used:—
1. Weight of bottle 39.299gram
2. Weight of bottle and water 81.884 "
3. Weight of bottle and paraffin 73.146 "
By subtracting 1 from 2 and 3 the result is as follows:—
81.884 grams 73.146 grams
39.299 " 39.299 "
—————— ——————
to slowly raise the temperature to the required degree. The superfluous
liquid is then at once wiped off, and the bottle cooled and weighed.
The weight of the flask filled with the liquid whose sp. g. has to be
determined is ascertained in a similar way. Of course the temperature must
be the same. If the liquid does not mix with water, the bottle should be dried
before filling, but otherwise the flask need only be rinsed out two or three
times with the liquid.
Having obtained the three weighings, deduct the weight of the bottle from
each of the others to get the weights of the water and liquid respectively.
Divide the latter by the former, the result shows the sp. g. As an example,
take the following, in which a rather large sp. g. bottle was used:—
1. Weight of bottle 39.299gram
2. Weight of bottle and water 81.884 "
3. Weight of bottle and paraffin 73.146 "
By subtracting 1 from 2 and 3 the result is as follows:—
81.884 grams 73.146 grams
39.299 " 39.299 "
—————— ——————
Page 114
42.585 of water. 33.847 of paraffin.
Divide the weight of the paraffin by that of the water—
42.585)33.8470(0.7948
29.8095
——————
.......
The sp. g. of the paraffin is 0.7948.
The sp. g. of a fusible solid may be obtained in the same way at a
temperature some degrees above its fusing point.
The sp. g. of a solid in powder or gravel sufficiently fine to pass through the
neck of the bottle is easily determined. If the bottle filled with water weighs
50 grams, and there is placed on the pan alongside of it 20 grams of a sand,
the weight of the two together will of course be 70 grams. But if the sand is
put in the bottle, it evidently displaces its own bulk of water; and if, on
again weighing, the weight is found to be 62 instead of 70 grams, it is
because the 20 grams of sand has displaced 8 grams of water. Bulk for bulk,
the sand is 2-1/2 times as heavy.
In practice, the weight of the bottle filled with water will probably be
already known; if not, it must be determined. A certain quantity, say 20
grams, of the powdered substance is then transferred carefully to the bottle.
The bottle need not be dry inside, but its neck and outside must be. In
making this transference a careful worker will make no loss, and the mode
of working saves a little time. But it is better to weigh the dry flask; put into
it 10 to 20 grams of the powder, and weigh again. The increase in weight
gives accurately the weight of powder in the bottle. About two-thirds fill the
bottle with distilled water, and mix with the powder by gentle shaking. Air
bubbles will disentangle themselves, and rise to the surface of the water.
Wash back anything adhering to the stopper with a jet of water, and fill the
bottle almost to overflowing. Allow it to stand for a minute or so; replace
the stopper; warm to the required temperature; take off the superfluous
moisture; wipe and weigh. As an example, take the following:—
1. Weightof bottle 12.681 grams
Divide the weight of the paraffin by that of the water—
42.585)33.8470(0.7948
29.8095
——————
.......
The sp. g. of the paraffin is 0.7948.
The sp. g. of a fusible solid may be obtained in the same way at a
temperature some degrees above its fusing point.
The sp. g. of a solid in powder or gravel sufficiently fine to pass through the
neck of the bottle is easily determined. If the bottle filled with water weighs
50 grams, and there is placed on the pan alongside of it 20 grams of a sand,
the weight of the two together will of course be 70 grams. But if the sand is
put in the bottle, it evidently displaces its own bulk of water; and if, on
again weighing, the weight is found to be 62 instead of 70 grams, it is
because the 20 grams of sand has displaced 8 grams of water. Bulk for bulk,
the sand is 2-1/2 times as heavy.
In practice, the weight of the bottle filled with water will probably be
already known; if not, it must be determined. A certain quantity, say 20
grams, of the powdered substance is then transferred carefully to the bottle.
The bottle need not be dry inside, but its neck and outside must be. In
making this transference a careful worker will make no loss, and the mode
of working saves a little time. But it is better to weigh the dry flask; put into
it 10 to 20 grams of the powder, and weigh again. The increase in weight
gives accurately the weight of powder in the bottle. About two-thirds fill the
bottle with distilled water, and mix with the powder by gentle shaking. Air
bubbles will disentangle themselves, and rise to the surface of the water.
Wash back anything adhering to the stopper with a jet of water, and fill the
bottle almost to overflowing. Allow it to stand for a minute or so; replace
the stopper; warm to the required temperature; take off the superfluous
moisture; wipe and weigh. As an example, take the following:—
1. Weightof bottle 12.681 grams
Page 115
2. " " bottle filled with water 37.708 "
3. " " bottle with wolfram 40.821 "
4. " " bottle with wolfram and water 61.199 "
Subtract (1) from (3) to get the weight of wolfram taken:
40.821 grams
12.681 "
——————
28.140 "
add the weight of the wolfram to the weight of the bottle filled with water:
28.140 grams
37.708 "
——————
65.848 "
subtract (4) from this to get the weight of water displaced:
65.848 grams
61.199 "
——————
4.649 "
Divide the weight of the wolfram by the weight of the water displaced to
get sp. g.:
4.649)28.140(6.053
27.894
———————
......
If the solid is soluble in water, or has a tendency to float, some liquid other
than water is used. Paraffin oil or oil of turpentine will do. The process is as
follows:—The weight of the dry and empty bottle having been determined,
add a sufficiency of the substance and weigh again to find how much has
been added. Fill up with paraffin oil and weigh again. Clean out the
substance by rinsing with paraffin; fill up and weigh. Calculate the sp. g. as
if water had been used, and multiply by the sp. g. of the paraffin.
3. " " bottle with wolfram 40.821 "
4. " " bottle with wolfram and water 61.199 "
Subtract (1) from (3) to get the weight of wolfram taken:
40.821 grams
12.681 "
——————
28.140 "
add the weight of the wolfram to the weight of the bottle filled with water:
28.140 grams
37.708 "
——————
65.848 "
subtract (4) from this to get the weight of water displaced:
65.848 grams
61.199 "
——————
4.649 "
Divide the weight of the wolfram by the weight of the water displaced to
get sp. g.:
4.649)28.140(6.053
27.894
———————
......
If the solid is soluble in water, or has a tendency to float, some liquid other
than water is used. Paraffin oil or oil of turpentine will do. The process is as
follows:—The weight of the dry and empty bottle having been determined,
add a sufficiency of the substance and weigh again to find how much has
been added. Fill up with paraffin oil and weigh again. Clean out the
substance by rinsing with paraffin; fill up and weigh. Calculate the sp. g. as
if water had been used, and multiply by the sp. g. of the paraffin.
Page 116
For example:
1.Weightof bottle 39.299grams
2." " bottle and nitre 57.830"
3." " bottle and paraffin 73.146"
4." " bottle and paraffin and nitre 84.665"
5." " bottle and water 81.884"
First from (1),(3), and (5), calculate the sp. g. of the paraffin as already
shown. It will be 0.7948. Deduct (1) from (2) to get the weight of the nitre:
57.830 grams
39.299 "
——————
18.531 "
add this to (3):
18.531 grams
73.146 "
——————
91.677 "
and deduct (4) to find the weight of the equal bulk of paraffin.
91.677 grams
84.665 "
——————
7.012 "
divide the weight of the nitre by the weight of the paraffin:
7.012)18.531(2.6427
——————
......
The sp. g., taking paraffin as the standard instead of water, is 2.6427.
Multiply this by the sp. g. of paraffin, 0.7948, and the result is 2.1004 as the
sp. g. of nitre compared with water.
1.Weightof bottle 39.299grams
2." " bottle and nitre 57.830"
3." " bottle and paraffin 73.146"
4." " bottle and paraffin and nitre 84.665"
5." " bottle and water 81.884"
First from (1),(3), and (5), calculate the sp. g. of the paraffin as already
shown. It will be 0.7948. Deduct (1) from (2) to get the weight of the nitre:
57.830 grams
39.299 "
——————
18.531 "
add this to (3):
18.531 grams
73.146 "
——————
91.677 "
and deduct (4) to find the weight of the equal bulk of paraffin.
91.677 grams
84.665 "
——————
7.012 "
divide the weight of the nitre by the weight of the paraffin:
7.012)18.531(2.6427
——————
......
The sp. g., taking paraffin as the standard instead of water, is 2.6427.
Multiply this by the sp. g. of paraffin, 0.7948, and the result is 2.1004 as the
sp. g. of nitre compared with water.
Page 117
Similarly, a sp. g. compared with water at say 50° C. can be converted into
one compared with water at standard temperature, by multiplying by the sp.
g. of water at 50° C. The following table gives the sp. g. of water at various
temperatures:—
Degrees Degrees Degrees
Sp. G. Sp. G. Sp. G.
Centigrade. Centigrade. Centigrade.
4° 1.0000 20° 0.9982 40° 0.9923
10° 0.9997 25° 0.9971 50° 0.9881
15° 0.9991 30° 0.9957 100° 0.9586
If, for example, a substance at 50° C. has a sp. g. of 0.9010 as compared
with water at 50° C., it will have (compared with water at 4° C.) a sp. g. of
0.9010 × 0.9881; or 0.8903. The figures 0.8903 represent the sp. g. of the
substance at 50° C. compared with water at 4° C. Except in comparing the
sp. gravities of the same substance at different temperatures, a calculation
of this kind serves no useful purpose.
In taking the specific gravity of a solid not in powder, a lump of it is freed
from loose particles and its exact weight determined. By means of a horse
hair with a slip knot it is suspended to the balance, and beneath it is placed,
out of contact with the balance pan, a beaker of distilled water. The horse
hair must be long enough to keep the mineral well beneath the surface of
the water so as to allow the balance to vibrate. Air bubbles are removed by
touching with a camel-hair pencil. Whilst the mineral is suspended in water
the weight is again taken. It will weigh less than before, and the difference
between the two weighings gives the weight of water (and consequently the
volume) displaced by the mineral. The weight in air divided by the
difference is the specific gravity. Thus
Weight in air 3.2170 grams
Weight in water 2.7050 "
———
Difference 0.5120 gram
3.2170/0.5120 equals 6.28, the sp. g.
one compared with water at standard temperature, by multiplying by the sp.
g. of water at 50° C. The following table gives the sp. g. of water at various
temperatures:—
Degrees Degrees Degrees
Sp. G. Sp. G. Sp. G.
Centigrade. Centigrade. Centigrade.
4° 1.0000 20° 0.9982 40° 0.9923
10° 0.9997 25° 0.9971 50° 0.9881
15° 0.9991 30° 0.9957 100° 0.9586
If, for example, a substance at 50° C. has a sp. g. of 0.9010 as compared
with water at 50° C., it will have (compared with water at 4° C.) a sp. g. of
0.9010 × 0.9881; or 0.8903. The figures 0.8903 represent the sp. g. of the
substance at 50° C. compared with water at 4° C. Except in comparing the
sp. gravities of the same substance at different temperatures, a calculation
of this kind serves no useful purpose.
In taking the specific gravity of a solid not in powder, a lump of it is freed
from loose particles and its exact weight determined. By means of a horse
hair with a slip knot it is suspended to the balance, and beneath it is placed,
out of contact with the balance pan, a beaker of distilled water. The horse
hair must be long enough to keep the mineral well beneath the surface of
the water so as to allow the balance to vibrate. Air bubbles are removed by
touching with a camel-hair pencil. Whilst the mineral is suspended in water
the weight is again taken. It will weigh less than before, and the difference
between the two weighings gives the weight of water (and consequently the
volume) displaced by the mineral. The weight in air divided by the
difference is the specific gravity. Thus
Weight in air 3.2170 grams
Weight in water 2.7050 "
———
Difference 0.5120 gram
3.2170/0.5120 equals 6.28, the sp. g.
Page 118
The sp. g. of a substance depends mainly on its composition, but is affected
by certain conditions. The effect of temperature has been already
considered. Air holes and empty spaces lessen the specific gravity of
otherwise solid bodies; and metals, which after fusion become imperfect
solids, have their density increased by hammering or rolling. But metals
when free from pores have their density diminished when rolled, without
annealing. The effects of these conditions are slight when compared with
those due to the presence of impurities.
For simple substances, or mixtures of only two substances, a determination
of sp. g. is a sufficient check on the composition for many practical
purposes; and with more complex mixtures, such as slags and some of the
products of dressing operations in which the material does not differ much
in its nature from time to time, such a determination will yield information
of considerable value, and afford a check upon the proper working of a
process.
When the mixing of two substances is accompanied by a change in volume,
the sp. g. of the mixture can only be learnt by experiment. But when the
substances have no such action on each other the resulting sp. g. can be
calculated. Some of these calculations have a practical interest as well as an
educational value. Students should practise them so as to become familiar
with the relations between weight and volume.
When substances are mixed by volume, the sp. g. of the mixture is the mean
of those of its constituents, and may be calculated in the usual way for
obtaining averages. 1 c.c. of a substance having a sp. g. of 1.4 mixed with 1
c.c. of another having a sp. g. of 1.0 will yield 2 c.c. of a substance having a
sp. g. of 1.2. If, however, we write gram instead of c.c. in the above
statement, the resulting sp. g. will be 1.16. The simplest plan is to remember
that the sp. g. is the weight divided by the volume (sp. g. = w/v) and the sp.
g. of a mixture is the sum of the weights divided by the sum of the volumes
(sp. g. = (w + w' + w", &c.)/(v + v' + v", &c.)). In the above example the
sum of the volumes is 2 c.c.; the weights (got by multiplying each volume
by its corresponding sp. g.) are 1.4 gram and 1 gram. The sum of the
weights divided by the sum of the volumes is 2.4/2 or 1.2.
by certain conditions. The effect of temperature has been already
considered. Air holes and empty spaces lessen the specific gravity of
otherwise solid bodies; and metals, which after fusion become imperfect
solids, have their density increased by hammering or rolling. But metals
when free from pores have their density diminished when rolled, without
annealing. The effects of these conditions are slight when compared with
those due to the presence of impurities.
For simple substances, or mixtures of only two substances, a determination
of sp. g. is a sufficient check on the composition for many practical
purposes; and with more complex mixtures, such as slags and some of the
products of dressing operations in which the material does not differ much
in its nature from time to time, such a determination will yield information
of considerable value, and afford a check upon the proper working of a
process.
When the mixing of two substances is accompanied by a change in volume,
the sp. g. of the mixture can only be learnt by experiment. But when the
substances have no such action on each other the resulting sp. g. can be
calculated. Some of these calculations have a practical interest as well as an
educational value. Students should practise them so as to become familiar
with the relations between weight and volume.
When substances are mixed by volume, the sp. g. of the mixture is the mean
of those of its constituents, and may be calculated in the usual way for
obtaining averages. 1 c.c. of a substance having a sp. g. of 1.4 mixed with 1
c.c. of another having a sp. g. of 1.0 will yield 2 c.c. of a substance having a
sp. g. of 1.2. If, however, we write gram instead of c.c. in the above
statement, the resulting sp. g. will be 1.16. The simplest plan is to remember
that the sp. g. is the weight divided by the volume (sp. g. = w/v) and the sp.
g. of a mixture is the sum of the weights divided by the sum of the volumes
(sp. g. = (w + w' + w", &c.)/(v + v' + v", &c.)). In the above example the
sum of the volumes is 2 c.c.; the weights (got by multiplying each volume
by its corresponding sp. g.) are 1.4 gram and 1 gram. The sum of the
weights divided by the sum of the volumes is 2.4/2 or 1.2.
Page 119
The sp. g. of a mixture of 10 c.c. of a substance having a sp. g. of 1.2, with
15 c.c. of another having a sp. g. of 1.5 may be thus found:—
sp. g. = (12+22.5)/(10+15) = 1.38
multiply each volume by its sp. g. to get its weight:
10×1.2 = 12 15×1.5 = 22.5
add these together (12+22.5 = 34.5) and divide by the sum of the volumes
(10+15 = 25):
25)34.5(1.38
25
—
95, &c.
The sp. g. will be 1.38, provided the mixture is not accompanied by any
change of volume.
The same formula will serve when the proportion of the ingredients is given
by weight. A mixture of 4 parts by weight of galena (sp. g. 7.5) with 5 parts
of blende (sp. g. 4) will have a sp. g. of 5.06:
sp. g. = (4+5)/(0.53+1.25) = 9/1.78 = 5.06
It is necessary in this case to calculate the volumes of the galena and of the
blende, which is done by dividing the weights by the sp. gravities: thus, 4
divided by 7.5 gives 0.53 and 5 divided by 4 gives 1.25.
The converse problem is a little more difficult. Given the sp. g. of a mixture
and of each of the two ingredients, the percentage by weight of the heavier
ingredient may be ascertained by the following rule, which is best
expressed as a formula. There are three sp. gravities given; if the highest be
written H, the lowest L and that of the mixture M, then:
Percentage of heavier mineral = (100×H×(M-L))/(M×(H-L))
Suppose a sample of tailings has a sp. g. of 3.0, and is made up of quartz
(sp. g. 2.6) and pyrites (sp. g. 5.1): then the percentage of pyrites is 27:
(100×5.1×(3-2.6))/(3×(5.1-2.6)) = (510×0.4)/(3×2.5) = 204/7.5 = 27.2
15 c.c. of another having a sp. g. of 1.5 may be thus found:—
sp. g. = (12+22.5)/(10+15) = 1.38
multiply each volume by its sp. g. to get its weight:
10×1.2 = 12 15×1.5 = 22.5
add these together (12+22.5 = 34.5) and divide by the sum of the volumes
(10+15 = 25):
25)34.5(1.38
25
—
95, &c.
The sp. g. will be 1.38, provided the mixture is not accompanied by any
change of volume.
The same formula will serve when the proportion of the ingredients is given
by weight. A mixture of 4 parts by weight of galena (sp. g. 7.5) with 5 parts
of blende (sp. g. 4) will have a sp. g. of 5.06:
sp. g. = (4+5)/(0.53+1.25) = 9/1.78 = 5.06
It is necessary in this case to calculate the volumes of the galena and of the
blende, which is done by dividing the weights by the sp. gravities: thus, 4
divided by 7.5 gives 0.53 and 5 divided by 4 gives 1.25.
The converse problem is a little more difficult. Given the sp. g. of a mixture
and of each of the two ingredients, the percentage by weight of the heavier
ingredient may be ascertained by the following rule, which is best
expressed as a formula. There are three sp. gravities given; if the highest be
written H, the lowest L and that of the mixture M, then:
Percentage of heavier mineral = (100×H×(M-L))/(M×(H-L))
Suppose a sample of tailings has a sp. g. of 3.0, and is made up of quartz
(sp. g. 2.6) and pyrites (sp. g. 5.1): then the percentage of pyrites is 27:
(100×5.1×(3-2.6))/(3×(5.1-2.6)) = (510×0.4)/(3×2.5) = 204/7.5 = 27.2
Page 120
The same problem could be solved with the help of a little algebra by the
rule already given, as thus: the sp. g. of a mixture equals the sum of the
weights of the constituents divided by the sum of the volumes. Then 100
grams of the tailings with x per cent. of pyrites contain 100-x per cent. of
quartz. The sum of the weights is 100. The volume of the pyrites is x/5.1
and of the quartz (100-x)/2.6.
Then we have by the rule
3 = 100/((x/5.1)+(100-x)/2.6)
3 = 1326/(510-2.5x)
204 = 7.5x
and x = 27.2
If the percentage (P) and sp. g. (H) of one constituent and the sp. g. (M) of
the mixture are known, the sp. g. of the other constituent may be calculated
by the following formula, in which x is the required sp. g.:
x = ((100-P)×M×H)/((100×H)-(P×M))
For example, "tailings" (sp. g. 3.0) containing 27.2 per cent. of pyrites (sp.
g. 5.1) will contain (100-27.2), 72.8 per cent. of earthy matter having a
mean sp. g. of x:
x = ((100-27.2)×3×5.1)/((100×5.1)-(27.2×3))
= 1113.84/428.4 = 2.6
The differences in sp. g. corresponding to differences in strength have been
carefully determined and tabulated in the case of the stronger acids and of
many other liquids. Such tables are given at the end of this book.
To Calculate the Weight of a Measured Volume of Mineral or Rock.—
Multiply the cubic feet by 62.4 and then multiply by the sp. g. of the stuff,
the answer gives the weight in pounds. For example, 100 cubic feet of
quartz weighs 100×62.4×2.6 = 16,224 lbs. The weight of any mass of
mineral of known extent and sp. g. is ascertained in this way.
The following table gives the specific gravities of some of the commoner
minerals.
rule already given, as thus: the sp. g. of a mixture equals the sum of the
weights of the constituents divided by the sum of the volumes. Then 100
grams of the tailings with x per cent. of pyrites contain 100-x per cent. of
quartz. The sum of the weights is 100. The volume of the pyrites is x/5.1
and of the quartz (100-x)/2.6.
Then we have by the rule
3 = 100/((x/5.1)+(100-x)/2.6)
3 = 1326/(510-2.5x)
204 = 7.5x
and x = 27.2
If the percentage (P) and sp. g. (H) of one constituent and the sp. g. (M) of
the mixture are known, the sp. g. of the other constituent may be calculated
by the following formula, in which x is the required sp. g.:
x = ((100-P)×M×H)/((100×H)-(P×M))
For example, "tailings" (sp. g. 3.0) containing 27.2 per cent. of pyrites (sp.
g. 5.1) will contain (100-27.2), 72.8 per cent. of earthy matter having a
mean sp. g. of x:
x = ((100-27.2)×3×5.1)/((100×5.1)-(27.2×3))
= 1113.84/428.4 = 2.6
The differences in sp. g. corresponding to differences in strength have been
carefully determined and tabulated in the case of the stronger acids and of
many other liquids. Such tables are given at the end of this book.
To Calculate the Weight of a Measured Volume of Mineral or Rock.—
Multiply the cubic feet by 62.4 and then multiply by the sp. g. of the stuff,
the answer gives the weight in pounds. For example, 100 cubic feet of
quartz weighs 100×62.4×2.6 = 16,224 lbs. The weight of any mass of
mineral of known extent and sp. g. is ascertained in this way.
The following table gives the specific gravities of some of the commoner
minerals.
Page 121
Barytes 4.5
Blende 4.0
Calcite 2.6
Cassiterite 6.9
Chalybite 3.8
Copper pyrites 4.2
Fluor 3.1
Galena 7.5
Hæmatite 5.0
Mispickel 6.2
Pyrites 5.0
Quartz 2.6
FOOTNOTES:
[8] The difference of 20 or 30 milligrams is disregarded here because it detracts
equally from the actual weight of the water and liquid to be determined. If the
liquid is a heavy one the difference shows itself in the third or second place of
decimals. The correction may be made by deducting from the weight of the flask
0.0012 grams for each gram of water it holds.
Blende 4.0
Calcite 2.6
Cassiterite 6.9
Chalybite 3.8
Copper pyrites 4.2
Fluor 3.1
Galena 7.5
Hæmatite 5.0
Mispickel 6.2
Pyrites 5.0
Quartz 2.6
FOOTNOTES:
[8] The difference of 20 or 30 milligrams is disregarded here because it detracts
equally from the actual weight of the water and liquid to be determined. If the
liquid is a heavy one the difference shows itself in the third or second place of
decimals. The correction may be made by deducting from the weight of the flask
0.0012 grams for each gram of water it holds.
Page 122
PART II.—THE METALS.
Page 123
CHAPTER IX.
SILVER, GOLD, CYANIDES, PLATINUM, MERCURY.
SILVER.
Silver is widely diffused, and has been found in most mining districts. It
occurs native in sufficient quantity to constitute one of the chief ores of the
metal. It also occurs combined with sulphur (as in argentite), with sulphur
and antimony (as in stephanite or brittle silver ore, and in pyrargyrite or
ruby silver), and with copper, sulphur, antimony, and arsenic, as in
polybasite. Chloride of silver occurs native as horn silver or kerargyrite.
Silver is found in the ores of other metals, such as fahlerz, which sometimes
contains from two to ten per cent. of the metal, and galena, which is an
important source of it; in fact, galena is never found entirely free from
silver. It is present also in greater or less quantity in the ores of copper and
zinc.
Silver dissolves readily in nitric acid, forming silver nitrate. It only forms
one family of salts, and of these the chloride and nitrate are of chief
importance to the assayer. The formation of the chloride of silver on the
addition of hydrochloric acid or a soluble chloride to the nitric acid
solution, serves for the recognition and separation of silver. The precipitated
chloride is white (becoming violet on exposure to light), insoluble in nitric
acid, soluble in ammonia, hyposulphite of soda, or concentrated solutions of
chlorides. The best confirmatory test is made by wrapping the precipitate in
a little sheet lead, and cupelling, when the silver will be left in the metallic
state, and is easily recognized.
Dry Assay.—This assay is made up of two parts: (1) the concentration of
the silver in a button of lead; and (2) the cupellation of the resulting alloy.
The concentration of the button of lead may be effected either by
scorification or by fusion in a crucible.
SILVER, GOLD, CYANIDES, PLATINUM, MERCURY.
SILVER.
Silver is widely diffused, and has been found in most mining districts. It
occurs native in sufficient quantity to constitute one of the chief ores of the
metal. It also occurs combined with sulphur (as in argentite), with sulphur
and antimony (as in stephanite or brittle silver ore, and in pyrargyrite or
ruby silver), and with copper, sulphur, antimony, and arsenic, as in
polybasite. Chloride of silver occurs native as horn silver or kerargyrite.
Silver is found in the ores of other metals, such as fahlerz, which sometimes
contains from two to ten per cent. of the metal, and galena, which is an
important source of it; in fact, galena is never found entirely free from
silver. It is present also in greater or less quantity in the ores of copper and
zinc.
Silver dissolves readily in nitric acid, forming silver nitrate. It only forms
one family of salts, and of these the chloride and nitrate are of chief
importance to the assayer. The formation of the chloride of silver on the
addition of hydrochloric acid or a soluble chloride to the nitric acid
solution, serves for the recognition and separation of silver. The precipitated
chloride is white (becoming violet on exposure to light), insoluble in nitric
acid, soluble in ammonia, hyposulphite of soda, or concentrated solutions of
chlorides. The best confirmatory test is made by wrapping the precipitate in
a little sheet lead, and cupelling, when the silver will be left in the metallic
state, and is easily recognized.
Dry Assay.—This assay is made up of two parts: (1) the concentration of
the silver in a button of lead; and (2) the cupellation of the resulting alloy.
The concentration of the button of lead may be effected either by
scorification or by fusion in a crucible.
Page 124
The scorification assay is performed in a scorifier, which is a shallow open-
mouthed dish about 2-1/2 inches across, with a very thick bottom to enable
it to withstand the corrosive action of the slag. A charge of more than 3 or 5
grams of the ore cannot be worked in one, and with such small charges the
unavoidable variations have a serious effect on the figures reported. A
difference of one milligram on the weight of the button of silver got
represents a difference of 6 or 10 ounces per ton. With rich ores such
variation is unavoidable under any conditions, and the only safe plan is to
take the mean of several assays. But with poorer ores the accuracy of the
assay, as well as convenience in working, is much increased by working in
a crucible with larger charges.
In scorification the proportion of lead required for scorifying 1 gram of ore
is in average cases from 10 to 15 grams, sinking in the case of galena to 2
grams, and rising with earthy and refractory substances to from 30 to 40
grams. But by fusing in a crucible with well-selected fluxes, a proportion of
4 of flux to 1 of ore is generally sufficient; and not only is the proportion of
added matter less, but it is also easier to manipulate large quantities in
crucibles, so that, although in some cases the crucible assay is more
troublesome and less satisfactory, yet with poor and earthy ores it is the best
method of dealing with them; while when properly worked it yields results
as accurate as scorification does. As a general rule, if more than 5 grams of
ore must be taken, the crucible assay should be adopted.
Scorification Assay.—The charge of ore is usually 3 grams, sometimes 5;
the lead varies from 30 to 70 grams, and the quantity of soda, borax, or
powdered glass added varies from 0.3 to 3 or 4 grams. It is generally
recommended to have the lead granulated,[9] and to mix the ore with about
half of it in the scorifier; then to put on the rest of the lead; and finally to
mouthed dish about 2-1/2 inches across, with a very thick bottom to enable
it to withstand the corrosive action of the slag. A charge of more than 3 or 5
grams of the ore cannot be worked in one, and with such small charges the
unavoidable variations have a serious effect on the figures reported. A
difference of one milligram on the weight of the button of silver got
represents a difference of 6 or 10 ounces per ton. With rich ores such
variation is unavoidable under any conditions, and the only safe plan is to
take the mean of several assays. But with poorer ores the accuracy of the
assay, as well as convenience in working, is much increased by working in
a crucible with larger charges.
In scorification the proportion of lead required for scorifying 1 gram of ore
is in average cases from 10 to 15 grams, sinking in the case of galena to 2
grams, and rising with earthy and refractory substances to from 30 to 40
grams. But by fusing in a crucible with well-selected fluxes, a proportion of
4 of flux to 1 of ore is generally sufficient; and not only is the proportion of
added matter less, but it is also easier to manipulate large quantities in
crucibles, so that, although in some cases the crucible assay is more
troublesome and less satisfactory, yet with poor and earthy ores it is the best
method of dealing with them; while when properly worked it yields results
as accurate as scorification does. As a general rule, if more than 5 grams of
ore must be taken, the crucible assay should be adopted.
Scorification Assay.—The charge of ore is usually 3 grams, sometimes 5;
the lead varies from 30 to 70 grams, and the quantity of soda, borax, or
powdered glass added varies from 0.3 to 3 or 4 grams. It is generally
recommended to have the lead granulated,[9] and to mix the ore with about
half of it in the scorifier; then to put on the rest of the lead; and finally to
Page 125
sprinkle the borax or glass on the top. It answers just as well, however, to
use the lead in the shape of foil, and wrap the ore up in it; and if the ore
contains much sulphur, the borax may with advantage be added (wrapped in
a little tissue paper) some five or ten minutes after the operation has started.
The process of scorification is as follows:—A scorifier (fig. 38) of
convenient size having been selected (one 2-1/2 inches across is most
generally useful), it is dried at a gentle heat for about ten minutes. The
charge is then put into it, and it is introduced, with the help of a scorifier
tongs (fig. 39), into a muffle heated considerably above redness. The muffle
is then closed, and when the metal has melted down, it is opened, but the
temperature is kept up. A ring of slag will, after a time, form around the
metal, and when this appearance (known as the eye) presents itself, the
temperature may be lowered. When the eye has disappeared—that is, when
the layer of slag has quite closed in—a pinch of powdered culm wrapped in
tissue paper is added. As soon as the slag has again become tranquil, the
scorifier is taken out, and its contents are poured into a mould (fig. 40), the
slag is detached, and saved. If the button of metal weighs more than 30
grams, its size is reduced by another scorification in the same scorifier,
which should have been replaced in the muffle immediately after the
contents had been poured out. If the ore is not a very rich one, the button of
lead will carry practically all the silver; but with rich ores it is more
satisfactory to save the slag, and subsequently to melt it down with the
cupel on which the lead has been treated, so as to recover the silver lost in
the slag, together with that absorbed in the cupel, at one operation. Or, if the
cupellation loss is neglected or calculated in some other manner, the slag or
slags from the scorifier may be powdered and mixed with 20 grams of
oxide of lead, 5 grams of borax, and 1 gram of charcoal. This should be
melted down in a small crucible, and the resulting button of lead cupelled.
use the lead in the shape of foil, and wrap the ore up in it; and if the ore
contains much sulphur, the borax may with advantage be added (wrapped in
a little tissue paper) some five or ten minutes after the operation has started.
The process of scorification is as follows:—A scorifier (fig. 38) of
convenient size having been selected (one 2-1/2 inches across is most
generally useful), it is dried at a gentle heat for about ten minutes. The
charge is then put into it, and it is introduced, with the help of a scorifier
tongs (fig. 39), into a muffle heated considerably above redness. The muffle
is then closed, and when the metal has melted down, it is opened, but the
temperature is kept up. A ring of slag will, after a time, form around the
metal, and when this appearance (known as the eye) presents itself, the
temperature may be lowered. When the eye has disappeared—that is, when
the layer of slag has quite closed in—a pinch of powdered culm wrapped in
tissue paper is added. As soon as the slag has again become tranquil, the
scorifier is taken out, and its contents are poured into a mould (fig. 40), the
slag is detached, and saved. If the button of metal weighs more than 30
grams, its size is reduced by another scorification in the same scorifier,
which should have been replaced in the muffle immediately after the
contents had been poured out. If the ore is not a very rich one, the button of
lead will carry practically all the silver; but with rich ores it is more
satisfactory to save the slag, and subsequently to melt it down with the
cupel on which the lead has been treated, so as to recover the silver lost in
the slag, together with that absorbed in the cupel, at one operation. Or, if the
cupellation loss is neglected or calculated in some other manner, the slag or
slags from the scorifier may be powdered and mixed with 20 grams of
oxide of lead, 5 grams of borax, and 1 gram of charcoal. This should be
melted down in a small crucible, and the resulting button of lead cupelled.
Page 126
If the scorification has been unsatisfactory, the quantity of silver obtained
from the slag will be by no means inconsiderable. The usual explanation is
that with sulphury ores compounds of metallic oxides and sulphides
(oxysulphides) are formed, which remain in the slag, retaining considerable
quantities of the precious metal. It is said that under certain conditions such
a slag may contain as much as 10 per cent. of silver. An excess of lead and a
high temperature prevents the formation of these oxysulphides. But if much
silver is present in the ore, the slag cannot be safely thrown away, even if
sulphur is absent, and the process has been satisfactorily performed.
If the crust which appears on the surface of the lead does not clear, add a
small lump of borax and 20 grams more lead; then close the muffle, and
keep the temperature as high as possible. If the slag forms properly, but
shows unfused or only half-fused lumps, even when the scorification has
proceeded for some time, add more borax, and stir with an iron rod. The
slag adhering to the rod must be detached by hammering, and replaced in
the scorifier.
If the ore consists largely of quartz, soda should be added instead of borax;
or, if it contains much copper, powdered quartz may be used. If the scorifier
at the end of an operation is more than usually corroded, the borax should
be replaced in subsequent assays on similar ores by powdered glass or
quartz.
from the slag will be by no means inconsiderable. The usual explanation is
that with sulphury ores compounds of metallic oxides and sulphides
(oxysulphides) are formed, which remain in the slag, retaining considerable
quantities of the precious metal. It is said that under certain conditions such
a slag may contain as much as 10 per cent. of silver. An excess of lead and a
high temperature prevents the formation of these oxysulphides. But if much
silver is present in the ore, the slag cannot be safely thrown away, even if
sulphur is absent, and the process has been satisfactorily performed.
If the crust which appears on the surface of the lead does not clear, add a
small lump of borax and 20 grams more lead; then close the muffle, and
keep the temperature as high as possible. If the slag forms properly, but
shows unfused or only half-fused lumps, even when the scorification has
proceeded for some time, add more borax, and stir with an iron rod. The
slag adhering to the rod must be detached by hammering, and replaced in
the scorifier.
If the ore consists largely of quartz, soda should be added instead of borax;
or, if it contains much copper, powdered quartz may be used. If the scorifier
at the end of an operation is more than usually corroded, the borax should
be replaced in subsequent assays on similar ores by powdered glass or
quartz.
Page 127
If a fairly fluid slag is formed which does not clear from the metal and show
the eye, more lead and a higher temperature is wanted.
As a general rule, it may be stated that when a scorification is
unsatisfactory, what is wanted is more heat, more lead, or more borax.
It is a safe plan when work has to be done on a strange ore, to make three or
four assays with varying quantities of lead. The proportion of lead is right
when a further addition does not yield a higher result. The proper
proportion having been found, a note of it should be made for future use.
POT ASSAYS.
The object of the fusion in a crucible, like that of scorification, is to
concentrate the silver in a button of lead which is to be subsequently
cupelled; and to retain the earthy and waste matters in the slag. It is
necessary to consider the quality of the slag and the weight and quality of
the lead. The slag when fused should be liquid and homogeneous, and not
too corrosive on the crucible. The button of lead should be soft, malleable,
and free from a coating of regulus.[10] In weight it should not differ much
from the ore taken. With 20 grams of ore, for example, a button of lead
weighing from 18 to 25 grams will be satisfactory: less than this would
leave an undue proportion of silver in the slag; and more would be
unnecessarily large for cupelling, and would increase the loss in that
operation.
With average ores, take 20 grams of the powdered ore and mix with 30
grams of "soda," 40 grams of red-lead or litharge, 5 grams of borax, and
from 2 to 2.5 grams of flour, and place in an E crucible (Battersea round).
Put these in the furnace at a red heat, cover the crucible, and gradually raise
the temperature until the whole charge has melted down and is in a state of
tranquil fusion. Pour into a mould, and replace the crucible in the furnace.
As soon as the lead is solid, detach the slag and put it back into the crucible;
and when it is again fluid, charge on to it with a copper scoop a mixture of
20 grams of oxide of lead, and 1 gram of charcoal: when fusion has again
become tranquil, pour and detach the button of lead. The lead buttons
should be hammered into discs with rounded edges, and be freed from slag;
the eye, more lead and a higher temperature is wanted.
As a general rule, it may be stated that when a scorification is
unsatisfactory, what is wanted is more heat, more lead, or more borax.
It is a safe plan when work has to be done on a strange ore, to make three or
four assays with varying quantities of lead. The proportion of lead is right
when a further addition does not yield a higher result. The proper
proportion having been found, a note of it should be made for future use.
POT ASSAYS.
The object of the fusion in a crucible, like that of scorification, is to
concentrate the silver in a button of lead which is to be subsequently
cupelled; and to retain the earthy and waste matters in the slag. It is
necessary to consider the quality of the slag and the weight and quality of
the lead. The slag when fused should be liquid and homogeneous, and not
too corrosive on the crucible. The button of lead should be soft, malleable,
and free from a coating of regulus.[10] In weight it should not differ much
from the ore taken. With 20 grams of ore, for example, a button of lead
weighing from 18 to 25 grams will be satisfactory: less than this would
leave an undue proportion of silver in the slag; and more would be
unnecessarily large for cupelling, and would increase the loss in that
operation.
With average ores, take 20 grams of the powdered ore and mix with 30
grams of "soda," 40 grams of red-lead or litharge, 5 grams of borax, and
from 2 to 2.5 grams of flour, and place in an E crucible (Battersea round).
Put these in the furnace at a red heat, cover the crucible, and gradually raise
the temperature until the whole charge has melted down and is in a state of
tranquil fusion. Pour into a mould, and replace the crucible in the furnace.
As soon as the lead is solid, detach the slag and put it back into the crucible;
and when it is again fluid, charge on to it with a copper scoop a mixture of
20 grams of oxide of lead, and 1 gram of charcoal: when fusion has again
become tranquil, pour and detach the button of lead. The lead buttons
should be hammered into discs with rounded edges, and be freed from slag;
Page 128
if too big for a cupel they may be scorified together in a small scorifier, but
it is better to cupel them separately.
Ores containing Metallic Oxides.—Peroxides of iron, manganese, and
copper interfere by counteracting the effect of the charcoal or flour, and
thus reducing the size of the lead button. Peroxide of iron will reduce the
weight of lead by a little more than its own weight; and peroxide of
manganese has about twice this effect. When these oxides are present an
additional quantity of flour must be used, and precautions must be taken to
prevent reoxidation of the slag by the furnace gases. This may best be
prevented by using a layer of common salt as a cover to the charge. When
the ores contain a good deal of quartz or stony matter, the fluxes just given
(for average ores) will do; but the proportion of soda should be diminished,
and that of the borax, oxide of lead, and flour increased as the quantity of
metallic oxides become greater. If the ore contains practically no quartz, the
soda may be altogether omitted, and some glass or powdered quartz added.
The following charge may be taken as an example: weigh up 20 grams of
the powdered ore, 15 grams each of "soda" and borax, 60 grams of oxide of
lead, and 5 grams of flour. Mix and place them in an E crucible, and cover
with a layer of from a quarter to half an inch of common salt. Place in the
furnace as before. The salt will give off a considerable amount of fume,
which will, to a certain extent, conceal the state of the charge: when the
crucible has been in the furnace for about 25 minutes remove it and pour
out the contents immediately. With ores that produce a thick slag the
addition of 5 grams of fluor spar will be an advantage. It may happen that
with an unknown ore the first assay will be more or less unsatisfactory: but
from it the necessity for adding more or less flour will be learnt, and a
second assay, with the necessary modification of the charge, should give a
good result.
Ores containing much Sulphides.—Ores of this class may be easily
recognized, either by the appearance of the minerals they contain or by the
odour of sulphurous oxide (SO2) which they evolve when roasted on a
spatula. The sulphides most commonly present, in addition to the
sulphurized minerals of silver, are pyrites, galena, blende, and mispickel.
When they are present in only a moderate amount, their effect is simply to
increase the weight of the button of lead; and this is easily counteracted by
reducing the amount of flour, or by omitting it. When in larger amounts,
it is better to cupel them separately.
Ores containing Metallic Oxides.—Peroxides of iron, manganese, and
copper interfere by counteracting the effect of the charcoal or flour, and
thus reducing the size of the lead button. Peroxide of iron will reduce the
weight of lead by a little more than its own weight; and peroxide of
manganese has about twice this effect. When these oxides are present an
additional quantity of flour must be used, and precautions must be taken to
prevent reoxidation of the slag by the furnace gases. This may best be
prevented by using a layer of common salt as a cover to the charge. When
the ores contain a good deal of quartz or stony matter, the fluxes just given
(for average ores) will do; but the proportion of soda should be diminished,
and that of the borax, oxide of lead, and flour increased as the quantity of
metallic oxides become greater. If the ore contains practically no quartz, the
soda may be altogether omitted, and some glass or powdered quartz added.
The following charge may be taken as an example: weigh up 20 grams of
the powdered ore, 15 grams each of "soda" and borax, 60 grams of oxide of
lead, and 5 grams of flour. Mix and place them in an E crucible, and cover
with a layer of from a quarter to half an inch of common salt. Place in the
furnace as before. The salt will give off a considerable amount of fume,
which will, to a certain extent, conceal the state of the charge: when the
crucible has been in the furnace for about 25 minutes remove it and pour
out the contents immediately. With ores that produce a thick slag the
addition of 5 grams of fluor spar will be an advantage. It may happen that
with an unknown ore the first assay will be more or less unsatisfactory: but
from it the necessity for adding more or less flour will be learnt, and a
second assay, with the necessary modification of the charge, should give a
good result.
Ores containing much Sulphides.—Ores of this class may be easily
recognized, either by the appearance of the minerals they contain or by the
odour of sulphurous oxide (SO2) which they evolve when roasted on a
spatula. The sulphides most commonly present, in addition to the
sulphurized minerals of silver, are pyrites, galena, blende, and mispickel.
When they are present in only a moderate amount, their effect is simply to
increase the weight of the button of lead; and this is easily counteracted by
reducing the amount of flour, or by omitting it. When in larger amounts,
Page 129
they not only yield large buttons, but also render the metal sulphury,
sometimes even giving a button of regulus instead of lead. This last evil
may be remedied (1) by putting in a rod of iron as soon as the charge has
fused, or (2) it may be counteracted by a proper addition of nitre, or (3)
when the sulphides present are only those of iron or copper the sulphur may
be removed by calcining, and the ore converted into one of the class
containing metallic oxides. The calcination is effected as follows:—Weigh
up 20 grams of the powdered ore and place it in a wide-mouthed crucible
sufficiently large to perform the subsequent melting down in. The roasting
must be done at a gentle heat at first, so as to avoid clotting: the mouth of
the crucible should project considerably above the coke, and should slope
forward towards the worker. The charge must be occasionally stirred with
the stirrer (fig. 10) so as to expose fresh surfaces to the action of the air, and
to prevent adhesion to the sides of the crucible. The stirrer should not be
removed till the calcination is finished. The temperature should be raised at
the end to a good red heat; and (to ensure the decomposition of any sulphate
that may be formed) the roasted ore should be rubbed up in a mortar with a
pinch of anthracite, and again calcined. It is then mixed with fluxes as
described, and fused in the same crucible.
The calcination of an ore is a work occupying a good deal of time, and, in
most cases, it is better to take advantage of the desulphurizing power of red
lead or nitre. Red lead by itself will do, but a large quantity of it will be
required; 1 part of a metallic sulphide needs from 20 to 50 parts of red lead
to yield a button free from sulphur; whereas at most from 2 to 2-1/2 parts of
nitre are sufficient. There is sometimes an advantage in having a
considerable excess of oxide of lead in the slag, but where there is no such
reason, 2 parts of red lead to 1 of ore is enough. A charge which will do for
most sulphides is the following: 20 grams of ore, 40 to 100 grams of red
lead, 20 grams of "soda," 5 of borax, and sufficient nitre (or perhaps flour)
to give a button of about 25 grams of lead. How much this must be (if not
already known) may be approximately determined by fusing 3 grams of the
ore and 3 grams of "soda" in a small crucible (C) with 50 grams of litharge
(not red lead) under a cover of salt, and weighing the resulting button of
lead. Subtract 3 from the weight of lead obtained, and the difference
multiplied by 1.3 will give the quantity in grams of nitre required. If the
button of lead weighs less than 3 grams flour must be added. If this is not
sometimes even giving a button of regulus instead of lead. This last evil
may be remedied (1) by putting in a rod of iron as soon as the charge has
fused, or (2) it may be counteracted by a proper addition of nitre, or (3)
when the sulphides present are only those of iron or copper the sulphur may
be removed by calcining, and the ore converted into one of the class
containing metallic oxides. The calcination is effected as follows:—Weigh
up 20 grams of the powdered ore and place it in a wide-mouthed crucible
sufficiently large to perform the subsequent melting down in. The roasting
must be done at a gentle heat at first, so as to avoid clotting: the mouth of
the crucible should project considerably above the coke, and should slope
forward towards the worker. The charge must be occasionally stirred with
the stirrer (fig. 10) so as to expose fresh surfaces to the action of the air, and
to prevent adhesion to the sides of the crucible. The stirrer should not be
removed till the calcination is finished. The temperature should be raised at
the end to a good red heat; and (to ensure the decomposition of any sulphate
that may be formed) the roasted ore should be rubbed up in a mortar with a
pinch of anthracite, and again calcined. It is then mixed with fluxes as
described, and fused in the same crucible.
The calcination of an ore is a work occupying a good deal of time, and, in
most cases, it is better to take advantage of the desulphurizing power of red
lead or nitre. Red lead by itself will do, but a large quantity of it will be
required; 1 part of a metallic sulphide needs from 20 to 50 parts of red lead
to yield a button free from sulphur; whereas at most from 2 to 2-1/2 parts of
nitre are sufficient. There is sometimes an advantage in having a
considerable excess of oxide of lead in the slag, but where there is no such
reason, 2 parts of red lead to 1 of ore is enough. A charge which will do for
most sulphides is the following: 20 grams of ore, 40 to 100 grams of red
lead, 20 grams of "soda," 5 of borax, and sufficient nitre (or perhaps flour)
to give a button of about 25 grams of lead. How much this must be (if not
already known) may be approximately determined by fusing 3 grams of the
ore and 3 grams of "soda" in a small crucible (C) with 50 grams of litharge
(not red lead) under a cover of salt, and weighing the resulting button of
lead. Subtract 3 from the weight of lead obtained, and the difference
multiplied by 1.3 will give the quantity in grams of nitre required. If the
button of lead weighs less than 3 grams flour must be added. If this is not
Page 130
satisfactory repeat the assay, adding an extra gram of nitre for each 4 grams
of lead in excess of that required, or 1 gram of flour for a 12-gram
deficiency.
In the method in which iron is used as a de-sulphurising agent, only as
much oxide of lead should be added as will give a button of lead of the
required size. Rather a large button of lead should be got, and the slag
should be strongly alkaline; if the ore does not already carry a large amount
of sulphur some should be added. The fusion should be performed at a low
temperature (similar to that for a galena assay), and should be continued for
some time after it has become tranquil. Take 20 grams of the ore, 40 grams
of "soda," 40 grams of oxide of lead, and 5 or 10 grams of borax; place this
mixture in a crucible (with a rod of iron, as in the galena assay), cover, and
fuse for about half an hour. Take out the rod, washing it in the slag, and, in a
minute or two, pour. Clean and cupel the button of lead.
General Remarks on the Fusion.—Other things being equal, the smaller
the quantity of the slag the better, provided there is sufficient to cover the
metal. The presence of peroxides of the heavy metals is prejudicial, since
they tend to increase the quantity of silver retained in the slag. It may be
given as a general rule that when iron, copper, manganese, &c., are present,
there is a more than ordinary need for cleaning the slags, and care must be
taken to keep these metals in the state of lower oxide.
In selecting the fluxes, it should be remembered that soda is the best for
quartz, and borax for lime and metallic oxides. And that with ores almost
free from gangue some quartz or glass should be added to protect the
crucible. Two parts of soda are enough to flux 1 part of quartz; whilst of
borax, or oxide of lead, 4 parts are barely sufficient. Oxide of lead has the
advantage of being heavy and so does not occupy much space in the
crucible; on the other hand, if the melting down be performed too quickly,
or if oxide of lead only is used, this high specific gravity is a disadvantage,
for the lighter earthy matter floats as a pasty mass on the more fluid oxide
of lead, and thus escapes its action.
When metallic sulphides are present in the ore, an excess of oxide of lead
helps to keep the sulphur out of the button of metal. In addition to the oxide
of lead required as a flux, some will be required to provide the lead in
of lead in excess of that required, or 1 gram of flour for a 12-gram
deficiency.
In the method in which iron is used as a de-sulphurising agent, only as
much oxide of lead should be added as will give a button of lead of the
required size. Rather a large button of lead should be got, and the slag
should be strongly alkaline; if the ore does not already carry a large amount
of sulphur some should be added. The fusion should be performed at a low
temperature (similar to that for a galena assay), and should be continued for
some time after it has become tranquil. Take 20 grams of the ore, 40 grams
of "soda," 40 grams of oxide of lead, and 5 or 10 grams of borax; place this
mixture in a crucible (with a rod of iron, as in the galena assay), cover, and
fuse for about half an hour. Take out the rod, washing it in the slag, and, in a
minute or two, pour. Clean and cupel the button of lead.
General Remarks on the Fusion.—Other things being equal, the smaller
the quantity of the slag the better, provided there is sufficient to cover the
metal. The presence of peroxides of the heavy metals is prejudicial, since
they tend to increase the quantity of silver retained in the slag. It may be
given as a general rule that when iron, copper, manganese, &c., are present,
there is a more than ordinary need for cleaning the slags, and care must be
taken to keep these metals in the state of lower oxide.
In selecting the fluxes, it should be remembered that soda is the best for
quartz, and borax for lime and metallic oxides. And that with ores almost
free from gangue some quartz or glass should be added to protect the
crucible. Two parts of soda are enough to flux 1 part of quartz; whilst of
borax, or oxide of lead, 4 parts are barely sufficient. Oxide of lead has the
advantage of being heavy and so does not occupy much space in the
crucible; on the other hand, if the melting down be performed too quickly,
or if oxide of lead only is used, this high specific gravity is a disadvantage,
for the lighter earthy matter floats as a pasty mass on the more fluid oxide
of lead, and thus escapes its action.
When metallic sulphides are present in the ore, an excess of oxide of lead
helps to keep the sulphur out of the button of metal. In addition to the oxide
of lead required as a flux, some will be required to provide the lead in
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which the silver is to be collected. Oxide of lead, mixed with charcoal or
flour, yields, when heated, a multitude of minute buttons of metal uniformly
distributed through the mass of the charge; as the charge melts down these
run together and fall to the bottom; this shower of lead collects the silver
more easily than a single button at the bottom of the crucible could do. Only
that portion of the oxide of lead which remains in the slag can be
considered as a flux; very often the first indication of an excessive
reduction of lead is the pastiness of the slag rendered thick by the
withdrawal of the oxide of lead which would have kept it fluid. If, in an
assay, it is found that 5 parts of flux are not sufficient for 1 part of ore, the
remedy lies in using a different flux rather than in taking a larger quantity.
On the Reducing Effect of Charcoal, Flour, and Tartar.—The weight to be
got from a given charge will depend (provided sufficient oxide of lead is
present) upon the proportion of the reducing agents in it. We have thought it
well to illustrate this part of the subject by a series of experiments which the
learner will do well to practise for himself before proceeding to the assay of
actual ores. Take 80 grams of litharge and 20 grams of a mixture of borax
and soda. Fuse three lots (1) with 1.5 gram of charcoal, (2) with 3 grams of
flour, and (3) with 7.5 grams of tartar. Weigh the buttons of lead obtained,
and divide each by the weight of reducing agent used. The results will differ
somewhat with the dryness and quality of the flour, etc., used; in one series
of experiments they were as follows:—
Gram. Grams. Gram. Grams.
1.5 charcoal gave 34.0 lead ∴ 1 charcoal = 22.6 lead.
3.0 flour " 33.5 " ∴ 1 flour = 11.2 "
7.5 tartar " 38.0 " ∴ 1 tartar = 5.0 "
The use of flour as a reducing agent has many advantages, and it is well to
remember that 1 gram of flour reduces about 11 grams of lead; and that
charcoal has twice, and tartar one-half, this reducing effect.
On the Reducing Effect of Charcoal, &c., on Red Lead.—It is often easier
to obtain red lead of good quality than it is litharge, and by a large number
of assayers red lead is the form of oxide of lead always used. Red lead,
however, contains an excess of oxygen which will use up some of the
reducing agent before lead separates out. On making a series of experiments
flour, yields, when heated, a multitude of minute buttons of metal uniformly
distributed through the mass of the charge; as the charge melts down these
run together and fall to the bottom; this shower of lead collects the silver
more easily than a single button at the bottom of the crucible could do. Only
that portion of the oxide of lead which remains in the slag can be
considered as a flux; very often the first indication of an excessive
reduction of lead is the pastiness of the slag rendered thick by the
withdrawal of the oxide of lead which would have kept it fluid. If, in an
assay, it is found that 5 parts of flux are not sufficient for 1 part of ore, the
remedy lies in using a different flux rather than in taking a larger quantity.
On the Reducing Effect of Charcoal, Flour, and Tartar.—The weight to be
got from a given charge will depend (provided sufficient oxide of lead is
present) upon the proportion of the reducing agents in it. We have thought it
well to illustrate this part of the subject by a series of experiments which the
learner will do well to practise for himself before proceeding to the assay of
actual ores. Take 80 grams of litharge and 20 grams of a mixture of borax
and soda. Fuse three lots (1) with 1.5 gram of charcoal, (2) with 3 grams of
flour, and (3) with 7.5 grams of tartar. Weigh the buttons of lead obtained,
and divide each by the weight of reducing agent used. The results will differ
somewhat with the dryness and quality of the flour, etc., used; in one series
of experiments they were as follows:—
Gram. Grams. Gram. Grams.
1.5 charcoal gave 34.0 lead ∴ 1 charcoal = 22.6 lead.
3.0 flour " 33.5 " ∴ 1 flour = 11.2 "
7.5 tartar " 38.0 " ∴ 1 tartar = 5.0 "
The use of flour as a reducing agent has many advantages, and it is well to
remember that 1 gram of flour reduces about 11 grams of lead; and that
charcoal has twice, and tartar one-half, this reducing effect.
On the Reducing Effect of Charcoal, &c., on Red Lead.—It is often easier
to obtain red lead of good quality than it is litharge, and by a large number
of assayers red lead is the form of oxide of lead always used. Red lead,
however, contains an excess of oxygen which will use up some of the
reducing agent before lead separates out. On making a series of experiments
Page 132
(similar to the last, but using 80 grams of red lead instead of the litharge)
the results were, with the same quantities of the reducing agents:—
With charcoal, 18grams of lead.
" flour, 18 " "
" tartar, 22 " "
Comparing these with the results with litharge, in the previous table it will
be seen that the same quantity of reducing agent has in each case brought
down 16 grams less of lead, so that a larger amount of the reducing agent
must be added to get a button of the same weight as that obtained with
litharge. To get a button of a desired weight, say 22 grams, we must add
reducing agent sufficient to throw down 22 + 16 or 38 grams of lead, which
would require 3.4 grams of flour. If this amount of flour is fused with 80
grams of red lead, a button of lead weighing 22 grams will be formed, the
other 16 grams being kept up by the oxygen of the red lead.
If the quantity of red lead differs from 80 grams, this rule must be modified.
With 40 grams of red lead, for example, we should add an excess of
reducing agent sufficient to throw down 8 grams of lead instead of 16.
Similarly, with 160 grams of red lead, we should add enough to throw down
32 grams.
The following rule will enable one to calculate the weight of flour required
to produce a button of lead of any desired weight from any given quantity
of red lead. Each 5 grams of red lead present diminishes the weight of the
lead by 1 gram. If then we divide the weight of red lead in a charge by 5,
and add this to the weight of lead required, the sum divided by 11 will give
the weight of flour which must be added. Using 80 grams of red lead and
wanting a button of 20 grams, we should add 3.3 grams of flour.
80/5 = 16; 16+20 = 36; 36/11 = 3.3 nearly.
The following are some results obtained which will illustrate the rule:—
Red Lead used. Flour used. Lead got.
40 grams 3grams 25.0grams
100 " 3 " 13.5 "
the results were, with the same quantities of the reducing agents:—
With charcoal, 18grams of lead.
" flour, 18 " "
" tartar, 22 " "
Comparing these with the results with litharge, in the previous table it will
be seen that the same quantity of reducing agent has in each case brought
down 16 grams less of lead, so that a larger amount of the reducing agent
must be added to get a button of the same weight as that obtained with
litharge. To get a button of a desired weight, say 22 grams, we must add
reducing agent sufficient to throw down 22 + 16 or 38 grams of lead, which
would require 3.4 grams of flour. If this amount of flour is fused with 80
grams of red lead, a button of lead weighing 22 grams will be formed, the
other 16 grams being kept up by the oxygen of the red lead.
If the quantity of red lead differs from 80 grams, this rule must be modified.
With 40 grams of red lead, for example, we should add an excess of
reducing agent sufficient to throw down 8 grams of lead instead of 16.
Similarly, with 160 grams of red lead, we should add enough to throw down
32 grams.
The following rule will enable one to calculate the weight of flour required
to produce a button of lead of any desired weight from any given quantity
of red lead. Each 5 grams of red lead present diminishes the weight of the
lead by 1 gram. If then we divide the weight of red lead in a charge by 5,
and add this to the weight of lead required, the sum divided by 11 will give
the weight of flour which must be added. Using 80 grams of red lead and
wanting a button of 20 grams, we should add 3.3 grams of flour.
80/5 = 16; 16+20 = 36; 36/11 = 3.3 nearly.
The following are some results obtained which will illustrate the rule:—
Red Lead used. Flour used. Lead got.
40 grams 3grams 25.0grams
100 " 3 " 13.5 "
Page 133
80 " 4 " 30.0 "
80 " 5 " 40.0 "
On the Reducing Effect of Metallic Sulphides, and the Counteracting Effect
of Nitre.—The sulphides found in ores will reduce a button of lead from
oxide of lead just as flour does; and, as charcoal, flour and tartar differ in
their reducing power, so equal weights of the different mineral sulphides
throw down different weights of lead.
One gram of iron pyrites yields about 11 grams of lead. One gram of copper
pyrites, blende, fahlerz, or mispickel, yields 7 or 8 grams of lead, whilst 1
gram of antimonite will give 6, and 1 gram of galena only a little over 3
grams. It is evident that if an ore carries much of these sulphides, the
quantity of lead reduced will be very much larger than that required for an
assay. To counteract this effect nitre is added; 1 gram is added for each 4
grams of lead in excess of that required. For example: with a 20-gram
charge of an ore containing 50 per cent. of pyrites, if no nitre were added,
110 grams of lead would be got; or, if there was not sufficient oxide of lead
to yield this quantity of metal, the button would be sulphury. To reduce the
weight of the button by 80 grammes, we should add 20 grams of nitre, if
litharge were used; or if red lead were used, we should add 16 grams of
nitre, since the oxidizing effect of 20 grams of red lead is equivalent to that
of 1 of nitre, and since 80 grams of red lead are generally used in a charge.
Two assays of an ore of this kind with these quantities of nitre gave 26.0
grams of lead with litharge, and 22.5 grams with red lead.
It is best to use in these assays 80 grams of red lead, 20 of soda, and 5 of
borax, with 20 grams of the ore. If the lead got by the preliminary fusion in
a small crucible with litharge (described under "ores containing much
sulphides") is known, the following table will indicate the quantity of nitre,
or flour, to be added with this charge:—
Lead got in Preliminary Fusion Flour to be added Nitre to be added to
with 3 grams of Ore. to the Assay. the Assay.
0.0 gram 3.3 grams none
3.0 grams 1.3 gram —
6.0 " none 4.0 grams
9.0 " — 9.0 "
80 " 5 " 40.0 "
On the Reducing Effect of Metallic Sulphides, and the Counteracting Effect
of Nitre.—The sulphides found in ores will reduce a button of lead from
oxide of lead just as flour does; and, as charcoal, flour and tartar differ in
their reducing power, so equal weights of the different mineral sulphides
throw down different weights of lead.
One gram of iron pyrites yields about 11 grams of lead. One gram of copper
pyrites, blende, fahlerz, or mispickel, yields 7 or 8 grams of lead, whilst 1
gram of antimonite will give 6, and 1 gram of galena only a little over 3
grams. It is evident that if an ore carries much of these sulphides, the
quantity of lead reduced will be very much larger than that required for an
assay. To counteract this effect nitre is added; 1 gram is added for each 4
grams of lead in excess of that required. For example: with a 20-gram
charge of an ore containing 50 per cent. of pyrites, if no nitre were added,
110 grams of lead would be got; or, if there was not sufficient oxide of lead
to yield this quantity of metal, the button would be sulphury. To reduce the
weight of the button by 80 grammes, we should add 20 grams of nitre, if
litharge were used; or if red lead were used, we should add 16 grams of
nitre, since the oxidizing effect of 20 grams of red lead is equivalent to that
of 1 of nitre, and since 80 grams of red lead are generally used in a charge.
Two assays of an ore of this kind with these quantities of nitre gave 26.0
grams of lead with litharge, and 22.5 grams with red lead.
It is best to use in these assays 80 grams of red lead, 20 of soda, and 5 of
borax, with 20 grams of the ore. If the lead got by the preliminary fusion in
a small crucible with litharge (described under "ores containing much
sulphides") is known, the following table will indicate the quantity of nitre,
or flour, to be added with this charge:—
Lead got in Preliminary Fusion Flour to be added Nitre to be added to
with 3 grams of Ore. to the Assay. the Assay.
0.0 gram 3.3 grams none
3.0 grams 1.3 gram —
6.0 " none 4.0 grams
9.0 " — 9.0 "
Page 134
12.0 " — 14.0 "
15.0 " — 19.0 "
18.0 " — 24.0 "
21.0 " — 29.0 "
If litharge is used in the assay instead of red lead 4 grams more nitre, or 1.5
gram less flour must be used. When more than a few grams of nitre are
added to a charge the proportion of "soda" and borax should be increased,
because one of the products of the reaction of nitre upon sulphides in the
presence of soda is sulphate of soda, and because the "soda" thus used up
no longer serves as a flux; more borax should be added, as it is the best flux
for the metallic oxides which are formed in the process. If in an assay too
large a button of lead is got, even after this calculation has been made, and
the assay is repeated, add 1 gram more nitre for each 4 grams of lead in
excess. Sometimes the assay appears tranquil before the nitre has produced
its full effect; in such cases it is well to seize the crucible with the tongs and
mix its fused contents by rotating them; if this causes an effervescence, the
crucible should be replaced in the fire and the fusion continued. The
following experiments will illustrate the extent to which the above rules
may be relied on. In all of them the standard flux was used, viz.:—80 grams
of red lead, 20 of soda, and 5 of borax.
Pyrites 5 5 5 5 2.5 5 10 15 20
Quartz — 20 — 20 17.515 10 5
Nitre — — 5 5 — 4 16 28.5 41
Lead got 42.5 36.0 16.0 19.0 11.5 22.522.5 26.5 27.5
Copper Pyrites 8 8 8 8
Quartz — 12 — 12
Nitre — — 4 4
Lead got 47.5 34.033.026.0
Antimonite 8 8 8 8
Quartz — 12 — 12
Nitre — — 4 4
Lead got 29.0 26.013.013.0
Galena 10 10 10 10 15 20
15.0 " — 19.0 "
18.0 " — 24.0 "
21.0 " — 29.0 "
If litharge is used in the assay instead of red lead 4 grams more nitre, or 1.5
gram less flour must be used. When more than a few grams of nitre are
added to a charge the proportion of "soda" and borax should be increased,
because one of the products of the reaction of nitre upon sulphides in the
presence of soda is sulphate of soda, and because the "soda" thus used up
no longer serves as a flux; more borax should be added, as it is the best flux
for the metallic oxides which are formed in the process. If in an assay too
large a button of lead is got, even after this calculation has been made, and
the assay is repeated, add 1 gram more nitre for each 4 grams of lead in
excess. Sometimes the assay appears tranquil before the nitre has produced
its full effect; in such cases it is well to seize the crucible with the tongs and
mix its fused contents by rotating them; if this causes an effervescence, the
crucible should be replaced in the fire and the fusion continued. The
following experiments will illustrate the extent to which the above rules
may be relied on. In all of them the standard flux was used, viz.:—80 grams
of red lead, 20 of soda, and 5 of borax.
Pyrites 5 5 5 5 2.5 5 10 15 20
Quartz — 20 — 20 17.515 10 5
Nitre — — 5 5 — 4 16 28.5 41
Lead got 42.5 36.0 16.0 19.0 11.5 22.522.5 26.5 27.5
Copper Pyrites 8 8 8 8
Quartz — 12 — 12
Nitre — — 4 4
Lead got 47.5 34.033.026.0
Antimonite 8 8 8 8
Quartz — 12 — 12
Nitre — — 4 4
Lead got 29.0 26.013.013.0
Galena 10 10 10 10 15 20
Page 135
Quartz. — 15 — 15 5 —
Nitre — — 3 3 3.5 7
Lead got 17.019.08.08.018.518.5
A similar set of experiments, with 80 grams of litharge instead of 80 grams
of red lead, gave:—
Pyrites 4 4 4 4 7 10
Quartz — 15 — 15 13 10
Nitre — — 5 5 12.520
Lead got 46.5 40.5 25.524.527.026.5
Copper Pyrites 5 5 5 5
Quartz — 15 — 15
Nitre — — 5 5
Lead got 44.5 32.5 23.025.0
Blende 5 5 5 5 10
Quartz — 15 — 15 10
Nitre — — 5 5 15
Lead got 41.5 38.5 21.522.521.6
Antimonite 5 5 5 5 10
Quartz — 15 — 15 10
Nitre — — 5 5 10
Lead got 31.0 32.5 11.5 12.518.7
Galena 10 10 10 10 15 20
Quartz — 15 — 15 5 —
Nitre — — 5 5 7.5 11
Lead got 33.5 33.5 13.014.019.522.7
The variation in some of these experiments, in which we might have
expected similar results, is due to the fact that the sulphur, and in some
cases the metals, are capable of two degrees of oxidation. For example:
theoretically 1 gram of iron pyrites (FeS2) would yield 8.6 grams of lead if
the sulphur were oxidised to sulphurous oxide (SO2), and the iron to ferrous
oxide (FeO); whilst if the sulphur were oxidised to sulphate (SO3), and the
iron to ferric oxide, 12.9 grams of lead will be thrown down. Similarly the
Nitre — — 3 3 3.5 7
Lead got 17.019.08.08.018.518.5
A similar set of experiments, with 80 grams of litharge instead of 80 grams
of red lead, gave:—
Pyrites 4 4 4 4 7 10
Quartz — 15 — 15 13 10
Nitre — — 5 5 12.520
Lead got 46.5 40.5 25.524.527.026.5
Copper Pyrites 5 5 5 5
Quartz — 15 — 15
Nitre — — 5 5
Lead got 44.5 32.5 23.025.0
Blende 5 5 5 5 10
Quartz — 15 — 15 10
Nitre — — 5 5 15
Lead got 41.5 38.5 21.522.521.6
Antimonite 5 5 5 5 10
Quartz — 15 — 15 10
Nitre — — 5 5 10
Lead got 31.0 32.5 11.5 12.518.7
Galena 10 10 10 10 15 20
Quartz — 15 — 15 5 —
Nitre — — 5 5 7.5 11
Lead got 33.5 33.5 13.014.019.522.7
The variation in some of these experiments, in which we might have
expected similar results, is due to the fact that the sulphur, and in some
cases the metals, are capable of two degrees of oxidation. For example:
theoretically 1 gram of iron pyrites (FeS2) would yield 8.6 grams of lead if
the sulphur were oxidised to sulphurous oxide (SO2), and the iron to ferrous
oxide (FeO); whilst if the sulphur were oxidised to sulphate (SO3), and the
iron to ferric oxide, 12.9 grams of lead will be thrown down. Similarly the
Page 136
yield with copper pyrites would be 7.5 or 11.6; with blende, 6.4 or 8.5; with
antimonite, 5.5 or 8; and with galena, 2.6 or 3.4. As regards the metals, the
lower oxide will always be formed if the assay is carried out properly (fused
under a cover, and with a sufficiency of reducing agent). But the proportion
of sulphur oxidised completely will vary with the conditions of the assay.
With a slag containing much soda the tendency will be to form sulphate,
and, in consequence, a big reduction of lead; whilst with an acid slag
containing much quartz the tendency will be for the sulphur to go off as
sulphurous oxide (SO2). In a fusion with litharge alone all the sulphur will
be liberated as the lower oxide, whilst with much soda it will be wholly
converted into sulphate. For example: 3 grams of an ore containing a good
deal of pyrites and a little galena, gave, when fused with litharge, 16.5
grams of lead. A similar charge, containing in addition 20.0 grams of soda,
gave 22.5 grams of lead.
It will be noted from the experiments that 1 gram of nitre kept up on the
average 4 grams of lead; the range being from 3.2 with acid slags to 5.3
with very basic ones. These facts serve to explain some apparently irregular
results got in practice.
CUPELLATION.
The process is as follows:—The cupels, which should have been made
some time before and stored in a dry place, are first cleaned by gentle
rubbing with the finger and blowing off the loose dust; and then placed in a
hot muffle and heated to redness for from 5 to 10 minutes before the alloy
to be cupelled is placed on them. The reasons for this are sufficiently
obvious: the sudden evolution of much steam will blow a cupel to pieces;
and, if the whole of the water has not been removed before the cupel is
filled with molten lead, the escaping steam will bubble through, and scatter
about particles of the metal. If some particles of unburnt carbon remain in
the bone ash, a similar result will be produced by the escape of bubbles of
carbonic acid as soon as the fused litharge comes in contact with them. The
cupels having been prepared are arranged in a definite order in the muffle,
and the assay buttons are arranged in a corresponding order on some
suitable tray (cupel tray, fig. 41); the heat of the muffle being at bright
redness. Then with the help of the tongs (fig. 42) the assay buttons should
antimonite, 5.5 or 8; and with galena, 2.6 or 3.4. As regards the metals, the
lower oxide will always be formed if the assay is carried out properly (fused
under a cover, and with a sufficiency of reducing agent). But the proportion
of sulphur oxidised completely will vary with the conditions of the assay.
With a slag containing much soda the tendency will be to form sulphate,
and, in consequence, a big reduction of lead; whilst with an acid slag
containing much quartz the tendency will be for the sulphur to go off as
sulphurous oxide (SO2). In a fusion with litharge alone all the sulphur will
be liberated as the lower oxide, whilst with much soda it will be wholly
converted into sulphate. For example: 3 grams of an ore containing a good
deal of pyrites and a little galena, gave, when fused with litharge, 16.5
grams of lead. A similar charge, containing in addition 20.0 grams of soda,
gave 22.5 grams of lead.
It will be noted from the experiments that 1 gram of nitre kept up on the
average 4 grams of lead; the range being from 3.2 with acid slags to 5.3
with very basic ones. These facts serve to explain some apparently irregular
results got in practice.
CUPELLATION.
The process is as follows:—The cupels, which should have been made
some time before and stored in a dry place, are first cleaned by gentle
rubbing with the finger and blowing off the loose dust; and then placed in a
hot muffle and heated to redness for from 5 to 10 minutes before the alloy
to be cupelled is placed on them. The reasons for this are sufficiently
obvious: the sudden evolution of much steam will blow a cupel to pieces;
and, if the whole of the water has not been removed before the cupel is
filled with molten lead, the escaping steam will bubble through, and scatter
about particles of the metal. If some particles of unburnt carbon remain in
the bone ash, a similar result will be produced by the escape of bubbles of
carbonic acid as soon as the fused litharge comes in contact with them. The
cupels having been prepared are arranged in a definite order in the muffle,
and the assay buttons are arranged in a corresponding order on some
suitable tray (cupel tray, fig. 41); the heat of the muffle being at bright
redness. Then with the help of the tongs (fig. 42) the assay buttons should
Page 137
be placed each in its proper cupel; a note having been previously made of
the position it is to occupy, and the door of the muffle closed.
This part of the work should be done promptly, so as not to unduly cool the
muffle: the start requires a fairly high temperature, and is a critical part of
the process. A black crust forms at once on the surface of the lead; but this
ought soon to fuse and flow in greasy drops from off the face of the metal,
so as to leave the latter fluid with a well-defined outline, and much brighter
than the cupel. If this clearing does not take place, the buttons are said to be
frozen; in which case the temperature must be raised, some pieces of
charcoal put in the muffle, and the door closed. If they still do not clear, the
heat must have been much too low, and it is best to reject them and repeat
the assays.
When the buttons have cleared it is well to check the draught of the furnace,
and to partly open the door of the muffle, so as to work at as low a
temperature as is compatible with the continuation of the process.[11] Too
low a temperature is indicated by the freezing of the buttons and the
consequent spoiling of the assays. Experience soon enables one to judge
when the heat is getting too low. A commoner error is to have the heat too
high: it should be remembered that that which was high enough to clear the
buttons at starting is more than sufficient to keep the process going. At the
finish a higher temperature is again required: therefore the door of the
muffle should be closed and the furnace urged. The finish is easily
recognised. The drops of litharge which in the earlier stages flow steadily
the position it is to occupy, and the door of the muffle closed.
This part of the work should be done promptly, so as not to unduly cool the
muffle: the start requires a fairly high temperature, and is a critical part of
the process. A black crust forms at once on the surface of the lead; but this
ought soon to fuse and flow in greasy drops from off the face of the metal,
so as to leave the latter fluid with a well-defined outline, and much brighter
than the cupel. If this clearing does not take place, the buttons are said to be
frozen; in which case the temperature must be raised, some pieces of
charcoal put in the muffle, and the door closed. If they still do not clear, the
heat must have been much too low, and it is best to reject them and repeat
the assays.
When the buttons have cleared it is well to check the draught of the furnace,
and to partly open the door of the muffle, so as to work at as low a
temperature as is compatible with the continuation of the process.[11] Too
low a temperature is indicated by the freezing of the buttons and the
consequent spoiling of the assays. Experience soon enables one to judge
when the heat is getting too low. A commoner error is to have the heat too
high: it should be remembered that that which was high enough to clear the
buttons at starting is more than sufficient to keep the process going. At the
finish a higher temperature is again required: therefore the door of the
muffle should be closed and the furnace urged. The finish is easily
recognised. The drops of litharge which in the earlier stages flow steadily
Page 138
from the surface of the alloy, thin off later to a luminous film. At the end
this film appears in commotion, then presents a brilliant play of colours,
and, with a sudden extinction, the operation is finished. The metal again
glows for an instant whilst becoming solid.
If the button is a small one the cupel is withdrawn at once and placed on
that square of the cupel tray which corresponds to the position it occupied
in the muffle. If, however, it is fairly large precautions must be taken to
prevent spirting.
Molten silver dissolves oxygen from the air and gives it off on solidifying;
the escape of the gas on sudden cooling is violent and, by throwing off
particles of the metal, may cause loss. This is called "vegetation" or
"spirting." The silver is apparently solid when spirting takes place; the crust
breaks suddenly and some of the metal is forced out. The evil is best
guarded against by slow cooling and avoiding draughts. With large buttons
of silver precautions should never be omitted. One plan is to allow the
cupels to cool in the muffle itself, the mouth being closed with hot charcoal.
Another is to cover the cupel with another cupel previously heated to
redness; in this case the silver cools between two hot cupels, and, of course,
cools slowly. A third plan is to withdraw the cupel to the door of the muffle,
holding it until it begins to get solid and then immediately to put it back into
the hotter part of the muffle.
Silver remains after cupellation in flattened elliptical buttons, adhering but
only slightly to the cupel. Its upper surface should show faint markings as if
it were crystalline. The presence of platinum renders it still more
crystalline, but removes the characteristic lustre and renders the metal dull
and grey. Copper, if not completely removed, has a very marked effect on
the appearance of the button: the metal is spread out, damping, as it were,
and firmly adhering to the cupel, which latter in the neighbourhood of the
metal is almost black with oxide of copper. Sometimes the silver button is
globular, or even more sharply rounded on its under than on its upper
surface; it is said that this is due to the presence of lead. Gold may be
present even to the extent of 50 per cent. without showing any yellow
colour.
this film appears in commotion, then presents a brilliant play of colours,
and, with a sudden extinction, the operation is finished. The metal again
glows for an instant whilst becoming solid.
If the button is a small one the cupel is withdrawn at once and placed on
that square of the cupel tray which corresponds to the position it occupied
in the muffle. If, however, it is fairly large precautions must be taken to
prevent spirting.
Molten silver dissolves oxygen from the air and gives it off on solidifying;
the escape of the gas on sudden cooling is violent and, by throwing off
particles of the metal, may cause loss. This is called "vegetation" or
"spirting." The silver is apparently solid when spirting takes place; the crust
breaks suddenly and some of the metal is forced out. The evil is best
guarded against by slow cooling and avoiding draughts. With large buttons
of silver precautions should never be omitted. One plan is to allow the
cupels to cool in the muffle itself, the mouth being closed with hot charcoal.
Another is to cover the cupel with another cupel previously heated to
redness; in this case the silver cools between two hot cupels, and, of course,
cools slowly. A third plan is to withdraw the cupel to the door of the muffle,
holding it until it begins to get solid and then immediately to put it back into
the hotter part of the muffle.
Silver remains after cupellation in flattened elliptical buttons, adhering but
only slightly to the cupel. Its upper surface should show faint markings as if
it were crystalline. The presence of platinum renders it still more
crystalline, but removes the characteristic lustre and renders the metal dull
and grey. Copper, if not completely removed, has a very marked effect on
the appearance of the button: the metal is spread out, damping, as it were,
and firmly adhering to the cupel, which latter in the neighbourhood of the
metal is almost black with oxide of copper. Sometimes the silver button is
globular, or even more sharply rounded on its under than on its upper
surface; it is said that this is due to the presence of lead. Gold may be
present even to the extent of 50 per cent. without showing any yellow
colour.
Page 139
The appearance of the cupel affords some useful information. The presence
of cracks evidently due to shrinkage indicates a badly made cupel. If,
however, they are accompanied by a peculiar unfolding of the cupel, the
margin losing its distinctness, it is because of the presence of antimony.
When lead is the only easily oxidisable metal present, the stained portion of
cupel is yellow when cold. A greenish tint may be due to small quantities of
copper or, perhaps, nickel, cobalt, or platinum. Larger quantities of copper
give a greenish grey or almost black colour. A dark green and corroded
cupel may be due to iron. Rings of pale-coloured scoria may be due to tin,
zinc, antimony, or arsenic. When the cupel shows signs of the presence of
these metals in objectionable quantity, it is well to repeat the assay and
scorify so as to remove them before cupellation.
The button should be detached from the cold cupel by seizing with a pair of
pliers: the under surface should be distorted by squeezing or hammering the
button so as to loosen the adhering bone ash. The cleaning is easily
completed by rubbing with a clean hard brush. After cleaning the buttons
are best put on a tray of marked watch-glasses, and then taken to the
balance and weighed. The weight of silver got needs a small correction; (1)
by deducting for the amount of silver introduced by the lead or oxide of
lead used in the assay;[12] and (2) by adding for the cupellation loss.
Loss in Cupellation.—During the whole process of cupelling a silver lead
alloy a more or less abundant fume may be observed rising from the cupel.
This furnishes an evident loss of lead and a possible loss of silver; for
although silver at the temperature of cupellation gives off no appreciable
vapour, it is known that such fume formed on a large scale contains silver. It
is, however, difficult to believe that the small amount of lead vapourised
carries with it a weighable amount of silver. That it does not do so in the
ordinary way of working is shown by the fact that a button of silver equal in
weight to the silver lost in cupelling may be got by smelting the cupel and
cupelling the resulting button of lead. The loss of silver by volatilisation is
altogether inconsiderable, unless the temperature at which the operation is
performed is much too high.
Another possible source of loss is the infiltration of small particles of alloy
into the cupel. The cupel is necessarily porous, and particles of metal may
perhaps drain into it, more especially if the bone ash is not in fine powder;
of cracks evidently due to shrinkage indicates a badly made cupel. If,
however, they are accompanied by a peculiar unfolding of the cupel, the
margin losing its distinctness, it is because of the presence of antimony.
When lead is the only easily oxidisable metal present, the stained portion of
cupel is yellow when cold. A greenish tint may be due to small quantities of
copper or, perhaps, nickel, cobalt, or platinum. Larger quantities of copper
give a greenish grey or almost black colour. A dark green and corroded
cupel may be due to iron. Rings of pale-coloured scoria may be due to tin,
zinc, antimony, or arsenic. When the cupel shows signs of the presence of
these metals in objectionable quantity, it is well to repeat the assay and
scorify so as to remove them before cupellation.
The button should be detached from the cold cupel by seizing with a pair of
pliers: the under surface should be distorted by squeezing or hammering the
button so as to loosen the adhering bone ash. The cleaning is easily
completed by rubbing with a clean hard brush. After cleaning the buttons
are best put on a tray of marked watch-glasses, and then taken to the
balance and weighed. The weight of silver got needs a small correction; (1)
by deducting for the amount of silver introduced by the lead or oxide of
lead used in the assay;[12] and (2) by adding for the cupellation loss.
Loss in Cupellation.—During the whole process of cupelling a silver lead
alloy a more or less abundant fume may be observed rising from the cupel.
This furnishes an evident loss of lead and a possible loss of silver; for
although silver at the temperature of cupellation gives off no appreciable
vapour, it is known that such fume formed on a large scale contains silver. It
is, however, difficult to believe that the small amount of lead vapourised
carries with it a weighable amount of silver. That it does not do so in the
ordinary way of working is shown by the fact that a button of silver equal in
weight to the silver lost in cupelling may be got by smelting the cupel and
cupelling the resulting button of lead. The loss of silver by volatilisation is
altogether inconsiderable, unless the temperature at which the operation is
performed is much too high.
Another possible source of loss is the infiltration of small particles of alloy
into the cupel. The cupel is necessarily porous, and particles of metal may
perhaps drain into it, more especially if the bone ash is not in fine powder;
Page 140
but if this is the main source of loss it is hard to see why, in cupelling equal
weights of silver and gold, the loss is not equal in each case. It is not easy to
believe that the mere filtration of the fused alloy will effect such a change in
the proportion of the metals as that which actually occurs. For example: a
cupel on which an alloy consisting of 0.80 gram of silver, 0.47 gram of
gold, and 25 grams of lead had been cupelled, was found to contain 7-1/2
milligrams of silver, and rather less than half a milligram of gold.
Assuming, for the sake of argument, that the gold present had filtered into
the cupel in the form of small drops of alloy, it would have been
accompanied by less than a milligram of silver, and the presence of the
extra 6 or 7 milligrams of silver must have been due to a different cause.
There can, thus, be little doubt that the cause of the greater part of the
"cupellation loss" is a chemical one and cannot be counteracted by a
mechanical contrivance.[13] In cupellation, then, there is a loss, apart from
imperfect working, inherent in the process itself; and as the amount of this
loss varies under different conditions, it is necessary to study it somewhat in
detail.
The following experiments are taken without selection from the work of
one student. Three experiments were made for each determination, and the
mean result is given. By "range" is meant the difference between the
highest and lowest result and the percentage loss is calculated on the silver
present. The silver added in the lead used has been deducted.
Effect of Varying Lead.—In each experiment 0.4 gram of silver was taken
and cupelled with the lead. The silver loss and "range" are expressed in
milligrams.
Lead Used. Silver Lost. Range.Percentage Loss.
Grams.
10 6.5 1.0 1.62
20 7.0 1.0 1.75
40 12.0 1.5 3.00
60 12.7 0.5 3.17
The loss increases with the lead used.
weights of silver and gold, the loss is not equal in each case. It is not easy to
believe that the mere filtration of the fused alloy will effect such a change in
the proportion of the metals as that which actually occurs. For example: a
cupel on which an alloy consisting of 0.80 gram of silver, 0.47 gram of
gold, and 25 grams of lead had been cupelled, was found to contain 7-1/2
milligrams of silver, and rather less than half a milligram of gold.
Assuming, for the sake of argument, that the gold present had filtered into
the cupel in the form of small drops of alloy, it would have been
accompanied by less than a milligram of silver, and the presence of the
extra 6 or 7 milligrams of silver must have been due to a different cause.
There can, thus, be little doubt that the cause of the greater part of the
"cupellation loss" is a chemical one and cannot be counteracted by a
mechanical contrivance.[13] In cupellation, then, there is a loss, apart from
imperfect working, inherent in the process itself; and as the amount of this
loss varies under different conditions, it is necessary to study it somewhat in
detail.
The following experiments are taken without selection from the work of
one student. Three experiments were made for each determination, and the
mean result is given. By "range" is meant the difference between the
highest and lowest result and the percentage loss is calculated on the silver
present. The silver added in the lead used has been deducted.
Effect of Varying Lead.—In each experiment 0.4 gram of silver was taken
and cupelled with the lead. The silver loss and "range" are expressed in
milligrams.
Lead Used. Silver Lost. Range.Percentage Loss.
Grams.
10 6.5 1.0 1.62
20 7.0 1.0 1.75
40 12.0 1.5 3.00
60 12.7 0.5 3.17
The loss increases with the lead used.
Page 141
Effect of Varying Temperature.—0.4 gram of silver was cupelled with 20
grams of lead.
Temperature. Silver Lost. Range.Percentage Loss.
Bright red 7.0 1.0 1.75
Clear yellow 17.3 1.7 4.32
The difference in temperature in these experiments was much greater than
would occur even with careless work.
Effect of Varying Silver.—20 grams of lead were used in each cupellation.
Silver Taken. Silver Lost. Range.Percentage Loss.
Milligrams.
12.50.7 0.2 5.6
25.01.4 0.1 5.6
50.01.6 0.4 3.2
100.02.9 0.3 2.9
200.05.6 0.5 2.8
400.07.0 1.0 1.7
800.09.7 1.0 1.2
It will be seen that, although the quantity of silver lost increases with the
silver present, the percentage loss is greater on the smaller buttons.
The following results are often quoted:—Cupelling 1 grain of silver with 10
grains of lead, the loss was 1.22 per cent.; 10 grains of silver with 100
grains of lead, loss 1.13 per cent.; 25 grains of silver cupelled with 250
grains of lead, lost 1.07 per cent. The proportion of silver to lead was the
same in the three experiments, and the largest button gave the best result.
Evidently, if the quantities of lead had been the same in the three
experiments (say, 250 grains in each case), the loss on the smaller quantities
of silver would appear worse in the comparison.
In judging these results, it must be borne in mind that it is difficult to
regulate the temperature, &c., in consecutive experiments so as to get
exactly similar results, so that the range in consecutive cupellations is
greater than that in a batch cupelled side by side.
grams of lead.
Temperature. Silver Lost. Range.Percentage Loss.
Bright red 7.0 1.0 1.75
Clear yellow 17.3 1.7 4.32
The difference in temperature in these experiments was much greater than
would occur even with careless work.
Effect of Varying Silver.—20 grams of lead were used in each cupellation.
Silver Taken. Silver Lost. Range.Percentage Loss.
Milligrams.
12.50.7 0.2 5.6
25.01.4 0.1 5.6
50.01.6 0.4 3.2
100.02.9 0.3 2.9
200.05.6 0.5 2.8
400.07.0 1.0 1.7
800.09.7 1.0 1.2
It will be seen that, although the quantity of silver lost increases with the
silver present, the percentage loss is greater on the smaller buttons.
The following results are often quoted:—Cupelling 1 grain of silver with 10
grains of lead, the loss was 1.22 per cent.; 10 grains of silver with 100
grains of lead, loss 1.13 per cent.; 25 grains of silver cupelled with 250
grains of lead, lost 1.07 per cent. The proportion of silver to lead was the
same in the three experiments, and the largest button gave the best result.
Evidently, if the quantities of lead had been the same in the three
experiments (say, 250 grains in each case), the loss on the smaller quantities
of silver would appear worse in the comparison.
In judging these results, it must be borne in mind that it is difficult to
regulate the temperature, &c., in consecutive experiments so as to get
exactly similar results, so that the range in consecutive cupellations is
greater than that in a batch cupelled side by side.
Page 142
Effect of Copper and Antimony.—0.1 gram of silver was cupelled with 20
grams of lead, and to one batch 0.5 gram of antimony, and to another 0.5
gram of copper was added.
Silver Lost. Range.Loss in Percentage.
Without addition 2.9 0.3 2.9
With antimony 3.2 0.2 3.2
With copper 4.9 1.7 4.9
Perhaps the antimony has so small an effect because it is eliminated in the
earlier part of the process, while the silver is still alloyed with, and
protected by, a large proportion of lead; whilst the copper on the other hand
makes its fiercest attack towards the close, when the silver is least capable
of resisting it. The ill effects of copper are most strongly felt when the
quantity of lead present is not sufficient to remove it: the coppery button of
silver got under these conditions is very considerably less than the weight
of silver originally taken.
Although the above is a fair statement of the loss attending average work, it
will not do in very important and exact work to place too much reliance on
the figures given, or, indeed, on any other set of figures, with the object of
correcting the result of an assay. Each man must rely on his own work.
It is easy to determine what allowance must be made for the loss in
cupellation by cupelling side by side with the assay piece an alloy of similar
and known composition. For, if the two pieces are very nearly alike, we may
justly conclude that the loss on each will be the same; and if, further, we
take the average of three or four such determinations we shall get results
accurate within 0.1 per cent. The method of getting such results may be best
explained by one or two illustrations. This method of working is termed
"assaying by checks."
Suppose we have an alloy of silver and lead in unknown proportions and
that by cupelling two lots of 10 grams each there is got from I. 0.1226 gram
of silver, and from II. 0.1229 gram. We should know from general
experience that the actual quantity of silver present was from 2 to 4
milligrams more than this. To determine more exactly what the loss is, the
following plan is recommended:—The two silver buttons are wrapped up
grams of lead, and to one batch 0.5 gram of antimony, and to another 0.5
gram of copper was added.
Silver Lost. Range.Loss in Percentage.
Without addition 2.9 0.3 2.9
With antimony 3.2 0.2 3.2
With copper 4.9 1.7 4.9
Perhaps the antimony has so small an effect because it is eliminated in the
earlier part of the process, while the silver is still alloyed with, and
protected by, a large proportion of lead; whilst the copper on the other hand
makes its fiercest attack towards the close, when the silver is least capable
of resisting it. The ill effects of copper are most strongly felt when the
quantity of lead present is not sufficient to remove it: the coppery button of
silver got under these conditions is very considerably less than the weight
of silver originally taken.
Although the above is a fair statement of the loss attending average work, it
will not do in very important and exact work to place too much reliance on
the figures given, or, indeed, on any other set of figures, with the object of
correcting the result of an assay. Each man must rely on his own work.
It is easy to determine what allowance must be made for the loss in
cupellation by cupelling side by side with the assay piece an alloy of similar
and known composition. For, if the two pieces are very nearly alike, we may
justly conclude that the loss on each will be the same; and if, further, we
take the average of three or four such determinations we shall get results
accurate within 0.1 per cent. The method of getting such results may be best
explained by one or two illustrations. This method of working is termed
"assaying by checks."
Suppose we have an alloy of silver and lead in unknown proportions and
that by cupelling two lots of 10 grams each there is got from I. 0.1226 gram
of silver, and from II. 0.1229 gram. We should know from general
experience that the actual quantity of silver present was from 2 to 4
milligrams more than this. To determine more exactly what the loss is, the
following plan is recommended:—The two silver buttons are wrapped up
Page 143
each in 10 grams of lead, and cupelled side by side with two other lots of 10
grams of the original alloy. If now the two buttons I. and II. weigh 0.1202
and 0.1203, they will have suffered in this second cupellation an average
loss of 2.5 milligrams. Suppose the two fresh lots of alloy gave 0.1233 and
0.1235 of silver, the average loss on these would also be 2.5 milligrams.
Add this loss to each result, and take the mean; which is in this case 0.1259.
If copper is present in the alloy as well as silver, it is necessary to add about
the same quantity of copper to the checks as is supposed, or known, to be
present in the assays. If the substance to be assayed is an alloy of silver and
copper, first cupel 0.5 gram of it, with, say, 10 grams of lead, and weigh the
resulting button of silver, in order to get an approximate knowledge of its
composition. Suppose the button weighs 0.3935 gram. We know that this is
below the truth: for the sake of round numbers take it as 0.4, and assume
that the rest of the alloy (0.1 gram) was copper. Two check pieces are then
weighed out, each containing 0.4 gram silver and 0.1 gram of copper
wrapped in 5 grams of lead. Of course the silver must be pure. And there is
also weighed out two (or better, four) assay pieces each containing half a
gram of the alloy wrapped in 5 grams of lead. The whole lot are then
cupelled as nearly as possible under the same conditions. With four assay
pieces, the cupels should be placed close together in two rows of three
across the muffle; the two check pieces are put in the middle cupels.
Suppose the buttons of silver got weighed as follows:—
Check pieces I. 0.3940II. 0.3945
Assay pieces I. 0.3905II. 0.3912
III. 0.3910IV. 0.3909
The average loss on the two check pieces is 5.7 milligrams, and the average
result of the four assay pieces is 0.3909. Add the average loss to the average
result, and there is got the corrected result, 0.3966. And if 0.5 gram of alloy
contain 0.3966 of silver, 1000 will contain 793.2 of silver, and this is the
degree of fineness.
A correction for the loss in cupellation is always made in this way when
rich alloys are being assayed; and in the case of rich ores it may be done
after the manner of the first of the above illustrations. There is another
method of working which relies more on experiment. This is to smelt the
grams of the original alloy. If now the two buttons I. and II. weigh 0.1202
and 0.1203, they will have suffered in this second cupellation an average
loss of 2.5 milligrams. Suppose the two fresh lots of alloy gave 0.1233 and
0.1235 of silver, the average loss on these would also be 2.5 milligrams.
Add this loss to each result, and take the mean; which is in this case 0.1259.
If copper is present in the alloy as well as silver, it is necessary to add about
the same quantity of copper to the checks as is supposed, or known, to be
present in the assays. If the substance to be assayed is an alloy of silver and
copper, first cupel 0.5 gram of it, with, say, 10 grams of lead, and weigh the
resulting button of silver, in order to get an approximate knowledge of its
composition. Suppose the button weighs 0.3935 gram. We know that this is
below the truth: for the sake of round numbers take it as 0.4, and assume
that the rest of the alloy (0.1 gram) was copper. Two check pieces are then
weighed out, each containing 0.4 gram silver and 0.1 gram of copper
wrapped in 5 grams of lead. Of course the silver must be pure. And there is
also weighed out two (or better, four) assay pieces each containing half a
gram of the alloy wrapped in 5 grams of lead. The whole lot are then
cupelled as nearly as possible under the same conditions. With four assay
pieces, the cupels should be placed close together in two rows of three
across the muffle; the two check pieces are put in the middle cupels.
Suppose the buttons of silver got weighed as follows:—
Check pieces I. 0.3940II. 0.3945
Assay pieces I. 0.3905II. 0.3912
III. 0.3910IV. 0.3909
The average loss on the two check pieces is 5.7 milligrams, and the average
result of the four assay pieces is 0.3909. Add the average loss to the average
result, and there is got the corrected result, 0.3966. And if 0.5 gram of alloy
contain 0.3966 of silver, 1000 will contain 793.2 of silver, and this is the
degree of fineness.
A correction for the loss in cupellation is always made in this way when
rich alloys are being assayed; and in the case of rich ores it may be done
after the manner of the first of the above illustrations. There is another
method of working which relies more on experiment. This is to smelt the
Page 144
cupel as described further on (p. 114), and to again cupel the resulting
button of lead. The button of silver got in this second cupellation is added to
that first obtained. It will sometimes, but not often, happen that the two
buttons together will slightly exceed in weight the silver which was actually
present. This is because of the retention in the buttons of a small quantity of
lead. It has been stated that the proportion of lead thus retained may be as
much as 1% of the silver present; this, however, can only be under
exceptional conditions. A determination of the actual silver in the buttons
got in the series of cupellations quoted on pages 102, 103, gave an average
percentage of 99.85, so that even with the larger buttons the effect of the
retained lead would be only to increase the weight by about 1 milligram. In
the method of working with checks, the retained lead has no disturbing
influence.
The proportion of lead required for the cupellation of any particular alloy
requires consideration. With too much lead the time occupied in the process
is increased, and so is the loss of silver; on the other hand, too little lead is
of greater disadvantage than too much. From 8 to 16 parts of lead are
required for each part of silver alloy, or, if gold is present, about twice as
much as this must be used. For the cupellation of 1 gram of a silver copper
alloy containing different percentages of copper, the following quantities of
lead should be used:—
Percentage of Copper in Alloy. Lead Required.
5 6grams
10 8 "
20 10 "
30 12 "
40 14 "
50-100 16-18 "
The alloy, in not too large pieces, is wrapped in the required weight of lead
foil and charged into the cupel at once; or the lead may be put in first, and,
when the cupellation has fairly started, the alloy may be added wrapped in
tissue paper; or a portion of the lead may be first started and the alloy
wrapped in the remaining lead and subsequently added. The cupellation of
large quantities of alloy or of alloys which contain tin, antimony, iron, or
button of lead. The button of silver got in this second cupellation is added to
that first obtained. It will sometimes, but not often, happen that the two
buttons together will slightly exceed in weight the silver which was actually
present. This is because of the retention in the buttons of a small quantity of
lead. It has been stated that the proportion of lead thus retained may be as
much as 1% of the silver present; this, however, can only be under
exceptional conditions. A determination of the actual silver in the buttons
got in the series of cupellations quoted on pages 102, 103, gave an average
percentage of 99.85, so that even with the larger buttons the effect of the
retained lead would be only to increase the weight by about 1 milligram. In
the method of working with checks, the retained lead has no disturbing
influence.
The proportion of lead required for the cupellation of any particular alloy
requires consideration. With too much lead the time occupied in the process
is increased, and so is the loss of silver; on the other hand, too little lead is
of greater disadvantage than too much. From 8 to 16 parts of lead are
required for each part of silver alloy, or, if gold is present, about twice as
much as this must be used. For the cupellation of 1 gram of a silver copper
alloy containing different percentages of copper, the following quantities of
lead should be used:—
Percentage of Copper in Alloy. Lead Required.
5 6grams
10 8 "
20 10 "
30 12 "
40 14 "
50-100 16-18 "
The alloy, in not too large pieces, is wrapped in the required weight of lead
foil and charged into the cupel at once; or the lead may be put in first, and,
when the cupellation has fairly started, the alloy may be added wrapped in
tissue paper; or a portion of the lead may be first started and the alloy
wrapped in the remaining lead and subsequently added. The cupellation of
large quantities of alloy or of alloys which contain tin, antimony, iron, or
Page 145
any substance which produces a scoria, or corrodes the cupel, must be
preceded by a scorification. The advantages of this are that the slag is
poorer in precious metal than that found on a cupel and is more easily
collected and cleaned; that larger quantities of metal can be treated, and
that, even if the substance is in part infusible, or produces at the start a
clinkery mass or scoria, the oxide of lead gradually accumulates, fluxes the
solid matters, and produces a good final result; but if the oxide of lead by
itself is not sufficient for the purpose, borax or some other flux can be
easily added.
If the button of silver got is very small its weight may be estimated from its
size; but it must be remembered that the weight varies as the cube of the
diameter. If one button has twice the diameter of another it is eight times as
heavy and so on. Scales specially constructed for measuring silver and gold
buttons may be purchased; but it is much better to make the measurement
with the help of a microscope provided with an eyepiece micrometer.
If the length of the long diameter of a silver button be taken the following
table will give the corresponding weight in milligrams:—
Diameter. Weight.Diameter. Weight.
0.04 inch 3.6 0.015 inch 0.19
0.035 " 2.4 0.014 " 0.15
0.03 " 1.5 0.013 " 0.12
0.025 " 0.9 0.012 " 0.097
0.02 " 0.45 0.011 " 0.075
0.019 " 0.4 0.010 " 0.056
0.018 " 0.33 0.008 " 0.028
0.017 " 0.27 0.006 " 0.012
0.016 " 0.23 0.004 " 0.004
The weight of a corresponding button of gold is got by multiplying by 2.25.
These figures are based on those given by Plattner, and apply only to
buttons of such shape as those left after cupellation. A sphere of silver 0.01
inch in diameter would weigh 0.09 milligram, and a similar sphere of gold
weighs 0.167 milligram.
preceded by a scorification. The advantages of this are that the slag is
poorer in precious metal than that found on a cupel and is more easily
collected and cleaned; that larger quantities of metal can be treated, and
that, even if the substance is in part infusible, or produces at the start a
clinkery mass or scoria, the oxide of lead gradually accumulates, fluxes the
solid matters, and produces a good final result; but if the oxide of lead by
itself is not sufficient for the purpose, borax or some other flux can be
easily added.
If the button of silver got is very small its weight may be estimated from its
size; but it must be remembered that the weight varies as the cube of the
diameter. If one button has twice the diameter of another it is eight times as
heavy and so on. Scales specially constructed for measuring silver and gold
buttons may be purchased; but it is much better to make the measurement
with the help of a microscope provided with an eyepiece micrometer.
If the length of the long diameter of a silver button be taken the following
table will give the corresponding weight in milligrams:—
Diameter. Weight.Diameter. Weight.
0.04 inch 3.6 0.015 inch 0.19
0.035 " 2.4 0.014 " 0.15
0.03 " 1.5 0.013 " 0.12
0.025 " 0.9 0.012 " 0.097
0.02 " 0.45 0.011 " 0.075
0.019 " 0.4 0.010 " 0.056
0.018 " 0.33 0.008 " 0.028
0.017 " 0.27 0.006 " 0.012
0.016 " 0.23 0.004 " 0.004
The weight of a corresponding button of gold is got by multiplying by 2.25.
These figures are based on those given by Plattner, and apply only to
buttons of such shape as those left after cupellation. A sphere of silver 0.01
inch in diameter would weigh 0.09 milligram, and a similar sphere of gold
weighs 0.167 milligram.
Page 146
It is safer, however, to compare with a micrometer the diameter of the
button whose weight has to be determined with that of a standard button of
nearly equal size whose weight is known. The weights of the two buttons
are proportional to the cubes of their diameters. This plan of working is
described more fully in Appendix B., page 440.
Calculation of the Results.—After deducting for the silver added, and
correcting for the cupellation loss, the calculation is made in the usual way;
reporting as so many parts per thousand in the case of rich alloys and as so
many ounces and pennyweights, or better as ounces and decimals of an
ounce, in the case of poor alloys and ores.
In this last case, however, it is less fatiguing to refer to a set of tables which
give, either directly or by means of simple addition, the produce
corresponding to any weight obtained from certain given weights of the
substance. The following table gives the produce in ounces and decimals of
an ounce per ton of 2240 pounds:—
Weight of Metal Weight of Ore
got. taken.
5 20 50 100
3 grams.
grams. grams. grams. grams.
0.0001 1.09 0.65 0.16 0.06 0.03
0.0002 2.18 1.31 0.33 0.13 0.06
0.0003 3.27 1.96 0.49 0.20 0.10
0.0004 4.36 2.61 0.65 0.26 0.13
0.0005 5.44 3.27 0.82 0.33 0.16
0.0006 6.53 3.92 0.98 0.39 0.19
0.0007 7.62 4.57 1.14 0.46 0.23
0.0008 8.71 5.23 1.31 0.52 0.26
0.0009 9.80 5.88 1.47 0.59 0.29
0.001 10.89 6.53 1.63 0.65 0.33
0.002 21.78 13.07 3.27 1.31 0.65
0.003 32.67 19.60 4.90 1.96 0.98
0.004 43.56 26.13 6.53 2.61 1.31
0.005 54.44 32.67 8.17 3.27 1.63
button whose weight has to be determined with that of a standard button of
nearly equal size whose weight is known. The weights of the two buttons
are proportional to the cubes of their diameters. This plan of working is
described more fully in Appendix B., page 440.
Calculation of the Results.—After deducting for the silver added, and
correcting for the cupellation loss, the calculation is made in the usual way;
reporting as so many parts per thousand in the case of rich alloys and as so
many ounces and pennyweights, or better as ounces and decimals of an
ounce, in the case of poor alloys and ores.
In this last case, however, it is less fatiguing to refer to a set of tables which
give, either directly or by means of simple addition, the produce
corresponding to any weight obtained from certain given weights of the
substance. The following table gives the produce in ounces and decimals of
an ounce per ton of 2240 pounds:—
Weight of Metal Weight of Ore
got. taken.
5 20 50 100
3 grams.
grams. grams. grams. grams.
0.0001 1.09 0.65 0.16 0.06 0.03
0.0002 2.18 1.31 0.33 0.13 0.06
0.0003 3.27 1.96 0.49 0.20 0.10
0.0004 4.36 2.61 0.65 0.26 0.13
0.0005 5.44 3.27 0.82 0.33 0.16
0.0006 6.53 3.92 0.98 0.39 0.19
0.0007 7.62 4.57 1.14 0.46 0.23
0.0008 8.71 5.23 1.31 0.52 0.26
0.0009 9.80 5.88 1.47 0.59 0.29
0.001 10.89 6.53 1.63 0.65 0.33
0.002 21.78 13.07 3.27 1.31 0.65
0.003 32.67 19.60 4.90 1.96 0.98
0.004 43.56 26.13 6.53 2.61 1.31
0.005 54.44 32.67 8.17 3.27 1.63
Page 147
0.006 65.33 39.20 9.80 3.92 1.96
0.007 76.22 45.73 11.43 4.57 2.29
0.008 87.11 52.27 13.07 5.23 2.61
0.009 98.00 58.80 14.70 5.88 2.94
0.01 108.89 65.33 16.33 6.53 3.27
0.02 217.78 130.67 32.67 13.07 6.53
0.03 326.67 196.00 49.00 19.60 9.80
0.04 435.56 261.33 65.33 26.13 13.07
0.05 544.44 326.67 81.67 32.67 16.33
0.06 653.33 392.00 98.00 39.20 19.60
0.07 762.22 457.33 114.33 45.73 22.87
0.08 871.11 522.67 130.67 52.27 26.13
0.09 980.00 588.00 147.00 58.80 29.40
0.1 1088.89 653.33 163.33 65.33 32.67
0.2 2177.78 1306.67 326.67 130.67 65.33
0.3 3266.67 1960.00 490.00 196.00 98.00
0.4 4355.56 2613.33 653.33 261.33 130.67
0.5 5444.44 3266.67 816.67 326.67 163.33
0.6 6533.33 3920.00 980.00 392.00 196.00
0.7 7622.22 4573.33 1143.33 457.33 228.67
0.8 8711.11 5226.67 1306.67 522.67 261.33
0.9 9800.00 5880.00 1470.00 588.00 294.00
1.0 10888.89 6533.33 1633.33 653.33 326.67
When, as in this table, the fraction of an ounce is expressed by two places
of decimals, it may be reduced to pennyweights (dwts.) by dividing by 5.
For example, 0.40 of an ounce is 8 dwts. The fraction of a dwt. similarly
expressed may be converted into grains with sufficient exactness by
dividing by 4. Thus, 1.63 ozs. equal 1 oz. 12.60 dwts., or 1 oz. 12 dwts. 15
grains. In England it is usual to report in ounces and decimals of an ounce.
The way to use the table is best shown by an example. Suppose a button of
silver weighing 0.0435 gram was obtained from 20 grams of ore. Look
down the 20-gram column of the table, and select the values corresponding
to each figure of the weight, thus:—
0.007 76.22 45.73 11.43 4.57 2.29
0.008 87.11 52.27 13.07 5.23 2.61
0.009 98.00 58.80 14.70 5.88 2.94
0.01 108.89 65.33 16.33 6.53 3.27
0.02 217.78 130.67 32.67 13.07 6.53
0.03 326.67 196.00 49.00 19.60 9.80
0.04 435.56 261.33 65.33 26.13 13.07
0.05 544.44 326.67 81.67 32.67 16.33
0.06 653.33 392.00 98.00 39.20 19.60
0.07 762.22 457.33 114.33 45.73 22.87
0.08 871.11 522.67 130.67 52.27 26.13
0.09 980.00 588.00 147.00 58.80 29.40
0.1 1088.89 653.33 163.33 65.33 32.67
0.2 2177.78 1306.67 326.67 130.67 65.33
0.3 3266.67 1960.00 490.00 196.00 98.00
0.4 4355.56 2613.33 653.33 261.33 130.67
0.5 5444.44 3266.67 816.67 326.67 163.33
0.6 6533.33 3920.00 980.00 392.00 196.00
0.7 7622.22 4573.33 1143.33 457.33 228.67
0.8 8711.11 5226.67 1306.67 522.67 261.33
0.9 9800.00 5880.00 1470.00 588.00 294.00
1.0 10888.89 6533.33 1633.33 653.33 326.67
When, as in this table, the fraction of an ounce is expressed by two places
of decimals, it may be reduced to pennyweights (dwts.) by dividing by 5.
For example, 0.40 of an ounce is 8 dwts. The fraction of a dwt. similarly
expressed may be converted into grains with sufficient exactness by
dividing by 4. Thus, 1.63 ozs. equal 1 oz. 12.60 dwts., or 1 oz. 12 dwts. 15
grains. In England it is usual to report in ounces and decimals of an ounce.
The way to use the table is best shown by an example. Suppose a button of
silver weighing 0.0435 gram was obtained from 20 grams of ore. Look
down the 20-gram column of the table, and select the values corresponding
to each figure of the weight, thus:—
Page 148
0.04 = 65.33 ozs. to the ton
0.003 = 4.90 "
0.0005 = 0.82 "
——————
0.0435 = 71.05 "
Add these together. The produce is 71.05 ozs., or 71 ozs. 1 dwt. to the ton.
Or, suppose an ore is known to contain 1.24 per cent. of silver. Look down
the 100-gram column, select the values, and add them together as before.
1.0 = 326.67 ozs. per ton
0.2 = 65.33 "
0.04 = 13.07 "
——————
1.24 = 405.07 "
This gives 405 ozs. 1 dwt. 10 grains to the ton.
The calculation becomes more complicated when, as is frequently the case,
the ore contains metallic particles. These show themselves by refusing to
pass through the sieve when the ore is powdered. When they are present, a
large portion, or if feasible the whole, of the sample is powdered and sifted.
The weights of the sifted portion and of the "metallics," or prills, are taken;
the sum of these weights gives that of the whole of the sample taken. It is
very important that nothing be lost during the operation of powdering.
Each portion has to be assayed separately. It is usual to assay a portion of
the sifted sample, say, 20 or 50 grams, and to add to the produce of this its
share of the "metallics." This way of calculating, which is more convenient
than correct, is illustrated by the following example:—
Weight of whole sample 400grams
Made up of sifted portions 399 "
" "Metallics" 1 "
————
400 "
0.003 = 4.90 "
0.0005 = 0.82 "
——————
0.0435 = 71.05 "
Add these together. The produce is 71.05 ozs., or 71 ozs. 1 dwt. to the ton.
Or, suppose an ore is known to contain 1.24 per cent. of silver. Look down
the 100-gram column, select the values, and add them together as before.
1.0 = 326.67 ozs. per ton
0.2 = 65.33 "
0.04 = 13.07 "
——————
1.24 = 405.07 "
This gives 405 ozs. 1 dwt. 10 grains to the ton.
The calculation becomes more complicated when, as is frequently the case,
the ore contains metallic particles. These show themselves by refusing to
pass through the sieve when the ore is powdered. When they are present, a
large portion, or if feasible the whole, of the sample is powdered and sifted.
The weights of the sifted portion and of the "metallics," or prills, are taken;
the sum of these weights gives that of the whole of the sample taken. It is
very important that nothing be lost during the operation of powdering.
Each portion has to be assayed separately. It is usual to assay a portion of
the sifted sample, say, 20 or 50 grams, and to add to the produce of this its
share of the "metallics." This way of calculating, which is more convenient
than correct, is illustrated by the following example:—
Weight of whole sample 400grams
Made up of sifted portions 399 "
" "Metallics" 1 "
————
400 "
Page 149
Twenty grams of the sifted portion, when assayed, gave 0.1050 gram of
silver. The whole of the "metallics" scorified and cupelled gave 0.842 gram
of silver. Since the 20 grams assayed was 1-20th of the whole, 1-20th part
of the 0.842 gram of silver (from the metallics) must be added to its
produce. We thus get 0.1471 gram (0.1050 + 0.0421).
Referring to the 20 gram column, we get—
0.1 = 163.33
0.04 = 65.33
0.007 = 11.43
0.0001 = 0.16
—————————
0.1471 = 240.25 ounces per ton.
A more legitimate method of calculation is as follows:—Calculate
separately the produce of each fraction as if they were from different ores.
Multiply each produce (best stated in per cents.) by the weight of the
corresponding fraction. Add together the products, and divide by the weight
of the whole sample. Taking the same example for illustration, we have:—
Metallics.—Weight 1 gram.
1 gram of it yielded 0.842 grams of silver.
∴ Produce = 84.2 per cent.
Produce multiplied by the weight is still 84.2.
Sifted Portion.—Weight 399 grams.
20 grams of it yielded 0.105 gram of silver.
∴ Produce = 0.525 per cent.
Produce multiplied by weight (0.525 × 399) is 209.475.
Add together; and divide by 400, the weight of the whole sample—
84.2
209.475
———-
400) 293.675 (0.7342
0.7342 is the total produce of the ore in per cents.
silver. The whole of the "metallics" scorified and cupelled gave 0.842 gram
of silver. Since the 20 grams assayed was 1-20th of the whole, 1-20th part
of the 0.842 gram of silver (from the metallics) must be added to its
produce. We thus get 0.1471 gram (0.1050 + 0.0421).
Referring to the 20 gram column, we get—
0.1 = 163.33
0.04 = 65.33
0.007 = 11.43
0.0001 = 0.16
—————————
0.1471 = 240.25 ounces per ton.
A more legitimate method of calculation is as follows:—Calculate
separately the produce of each fraction as if they were from different ores.
Multiply each produce (best stated in per cents.) by the weight of the
corresponding fraction. Add together the products, and divide by the weight
of the whole sample. Taking the same example for illustration, we have:—
Metallics.—Weight 1 gram.
1 gram of it yielded 0.842 grams of silver.
∴ Produce = 84.2 per cent.
Produce multiplied by the weight is still 84.2.
Sifted Portion.—Weight 399 grams.
20 grams of it yielded 0.105 gram of silver.
∴ Produce = 0.525 per cent.
Produce multiplied by weight (0.525 × 399) is 209.475.
Add together; and divide by 400, the weight of the whole sample—
84.2
209.475
———-
400) 293.675 (0.7342
0.7342 is the total produce of the ore in per cents.
Page 150
Referring to the 100-gram column in the table we find 239.84 ounces to the
ton as the produce.
0.7 = 228.67
0.03 = 9.80
0.004 = 1.31
0.0002 = 0.06
———
239.84
Comparing this with the result calculated by the first method—viz., 240.26,
we see that that was 0.38 oz., or between 7 and 8 dwts. too high.
With ores containing "metallics" it is of great importance to powder the
whole of the selected sample without loss during the process; and of even
greater importance to well mix the sifted portion, of which the last portions
to come through the sieve are apt to be more than ordinarily rich through
the grinding down of some portions of the metallic prills.
Remarks on Cupellation.—Cupellation is at once the neatest and the most
important of the dry methods of assaying. Its purpose is to remove easily
oxidisable metals, such as lead and copper, from silver and gold, which are
oxidisable with difficulty. Metals of the first class are often spoken of as
base, and gold and silver as noble metals.
When lead is exposed to the action of air at a temperature a little above
redness, it combines with the oxygen of the air to form litharge, an oxide of
lead, which at the temperature of its formation is a liquid. Consequently, if
the lead rests on a porous support, which allows the fused litharge to drain
away as fast as it is formed, a fresh surface of the lead will be continually
exposed to the action of the air, and the operation goes on until the whole of
the lead has been removed. Silver or gold exposed to similar treatment does
not oxidise, but retains its metallic condition; so that an alloy of lead and
silver similarly treated would yield its lead as oxide, which would sink into
the support, while the silver would remain as a button of metal.
The porous support, which is called a cupel(fig. 5), should absorb the slag
(oxide of lead, etc.) just as a sponge absorbs water, but must be sufficiently
fine-grained to be impervious to the molten metal. At first sight it appears
ton as the produce.
0.7 = 228.67
0.03 = 9.80
0.004 = 1.31
0.0002 = 0.06
———
239.84
Comparing this with the result calculated by the first method—viz., 240.26,
we see that that was 0.38 oz., or between 7 and 8 dwts. too high.
With ores containing "metallics" it is of great importance to powder the
whole of the selected sample without loss during the process; and of even
greater importance to well mix the sifted portion, of which the last portions
to come through the sieve are apt to be more than ordinarily rich through
the grinding down of some portions of the metallic prills.
Remarks on Cupellation.—Cupellation is at once the neatest and the most
important of the dry methods of assaying. Its purpose is to remove easily
oxidisable metals, such as lead and copper, from silver and gold, which are
oxidisable with difficulty. Metals of the first class are often spoken of as
base, and gold and silver as noble metals.
When lead is exposed to the action of air at a temperature a little above
redness, it combines with the oxygen of the air to form litharge, an oxide of
lead, which at the temperature of its formation is a liquid. Consequently, if
the lead rests on a porous support, which allows the fused litharge to drain
away as fast as it is formed, a fresh surface of the lead will be continually
exposed to the action of the air, and the operation goes on until the whole of
the lead has been removed. Silver or gold exposed to similar treatment does
not oxidise, but retains its metallic condition; so that an alloy of lead and
silver similarly treated would yield its lead as oxide, which would sink into
the support, while the silver would remain as a button of metal.
The porous support, which is called a cupel(fig. 5), should absorb the slag
(oxide of lead, etc.) just as a sponge absorbs water, but must be sufficiently
fine-grained to be impervious to the molten metal. At first sight it appears
Page 151
difficult to filter, as it were, a fluid slag from a fluid metal; but an ordinary
filter-paper damped with oil will allow oils to run through and yet retain the
water; but damped with water it will allow water to run through and retain
oils. Similarly, fused slags damp and filter through a cupel, but the molten
metal not damping it withdraws itself into a button, which is retained.
Although, of course, if the cupel is very coarse-grained the metal may sink
into the hollows.
Copper, antimony, tin, and most other metals, form powdery oxides, which
are not of themselves easily fusible, and it is necessary when these are
present to add some solvent or flux to render the oxide sufficiently fluid.
Fortunately, oxide of lead is sufficient for the purpose; hence, mixed oxides
of copper and lead, provided the lead is present in proper proportion, form a
fluid slag. In separating copper from silver or gold, advantage is taken of
this fact; for, although we cannot cupel an alloy of copper and silver, it is
easy to cupel an alloy of copper, silver and lead. If, however, the lead is not
present in sufficient quantity, the whole of the copper will not be removed,
and the button of silver, still retaining copper, will be found embedded in a
coating of black oxide of copper. Copper oxidises less easily than lead does;
and, consequently, the alloy which is being cupelled becomes relatively
richer in copper as the operation proceeds. It is on this account that the ill-
effects of the copper make themselves felt at the close of the operation, and
that the oxide of copper is found accumulated around the button of silver.
Tin and antimony, on the other hand, are more easily oxidised; and the
tendency of their oxides to thicken the slag makes itself felt at the
commencement: if the button of alloy once frees itself from the ring or crust
of unfused oxide first formed, the cupellation proceeds quietly, and leaves a
clean button of silver in the centre. But in either case the cupellation is
imperfect, and should be repeated with a larger proportion of lead. An
unfused and, consequently, unabsorbed slag tends to retain small buttons of
alloy or metal, and thus cause serious loss.
There is a principle underlying many of the phenomena of dry silver
assaying which the student should endeavour to understand; and which
serves to emphasise and explain some facts which without an explanation
may present difficulties. If a button of melted lead be covered with a layer
of slag rich in oxide of lead, and a second metal be added, this other metal
distributes itself between the metal and slag in proportions which depend
filter-paper damped with oil will allow oils to run through and yet retain the
water; but damped with water it will allow water to run through and retain
oils. Similarly, fused slags damp and filter through a cupel, but the molten
metal not damping it withdraws itself into a button, which is retained.
Although, of course, if the cupel is very coarse-grained the metal may sink
into the hollows.
Copper, antimony, tin, and most other metals, form powdery oxides, which
are not of themselves easily fusible, and it is necessary when these are
present to add some solvent or flux to render the oxide sufficiently fluid.
Fortunately, oxide of lead is sufficient for the purpose; hence, mixed oxides
of copper and lead, provided the lead is present in proper proportion, form a
fluid slag. In separating copper from silver or gold, advantage is taken of
this fact; for, although we cannot cupel an alloy of copper and silver, it is
easy to cupel an alloy of copper, silver and lead. If, however, the lead is not
present in sufficient quantity, the whole of the copper will not be removed,
and the button of silver, still retaining copper, will be found embedded in a
coating of black oxide of copper. Copper oxidises less easily than lead does;
and, consequently, the alloy which is being cupelled becomes relatively
richer in copper as the operation proceeds. It is on this account that the ill-
effects of the copper make themselves felt at the close of the operation, and
that the oxide of copper is found accumulated around the button of silver.
Tin and antimony, on the other hand, are more easily oxidised; and the
tendency of their oxides to thicken the slag makes itself felt at the
commencement: if the button of alloy once frees itself from the ring or crust
of unfused oxide first formed, the cupellation proceeds quietly, and leaves a
clean button of silver in the centre. But in either case the cupellation is
imperfect, and should be repeated with a larger proportion of lead. An
unfused and, consequently, unabsorbed slag tends to retain small buttons of
alloy or metal, and thus cause serious loss.
There is a principle underlying many of the phenomena of dry silver
assaying which the student should endeavour to understand; and which
serves to emphasise and explain some facts which without an explanation
may present difficulties. If a button of melted lead be covered with a layer
of slag rich in oxide of lead, and a second metal be added, this other metal
distributes itself between the metal and slag in proportions which depend
Page 152
mainly upon the ease with which it is oxidised, and to a large extent upon
the relative quantities of material present. Easily oxidisable metals such as
zinc, iron, antimony and tin, will go mainly into the slag, and, if the
proportion of the slag is large, very little will go into the metal. On the other
hand, with metals oxidisable with difficulty, such as silver, gold, and
platinum, the reverse holds true; nearly the whole of the metals will go into
the lead, and very little into the slag. If, however, the slag be very rich, say
in antimony, the lead will contain antimony; and, on the other hand, if the
lead be very rich in silver, the slag will contain silver in appreciable
quantity. Copper, which is near lead in the facility with which it is oxidised,
will serve for the purpose of a detailed example. The results of actual
analyses of metal and slag formed in contact with each other are shown in
the following table:—
Percentage Composition of the Metal.
Lead. Copper.
6.8 93.2
20.0 80.0
28.0 72.0
32.0 68.0
85.0 15.0
Percentage Composition of the Slag.
Lead. Copper.
71.4 21.4
78.0 17.0
80.0 12.5
86.0 6.7
90.0 3.6
It will be seen from this table that the slag is always much richer in lead and
poorer in copper than the metal with which it is in contact. The ratio of lead
to copper in these five samples is:—
In the Metal. In the Slag.
the relative quantities of material present. Easily oxidisable metals such as
zinc, iron, antimony and tin, will go mainly into the slag, and, if the
proportion of the slag is large, very little will go into the metal. On the other
hand, with metals oxidisable with difficulty, such as silver, gold, and
platinum, the reverse holds true; nearly the whole of the metals will go into
the lead, and very little into the slag. If, however, the slag be very rich, say
in antimony, the lead will contain antimony; and, on the other hand, if the
lead be very rich in silver, the slag will contain silver in appreciable
quantity. Copper, which is near lead in the facility with which it is oxidised,
will serve for the purpose of a detailed example. The results of actual
analyses of metal and slag formed in contact with each other are shown in
the following table:—
Percentage Composition of the Metal.
Lead. Copper.
6.8 93.2
20.0 80.0
28.0 72.0
32.0 68.0
85.0 15.0
Percentage Composition of the Slag.
Lead. Copper.
71.4 21.4
78.0 17.0
80.0 12.5
86.0 6.7
90.0 3.6
It will be seen from this table that the slag is always much richer in lead and
poorer in copper than the metal with which it is in contact. The ratio of lead
to copper in these five samples is:—
In the Metal. In the Slag.
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1 : 14 1 : 0.3
1:4 1 : 0.2
1 : 2.5 1 : 0.16
1:2 1 : 0.08
1 : 0.16 1 : 0.04
Assuming these figures to be correct, the following statement is
approximately true. On oxidising an alloy of 10 grams of copper and 10
grams of lead, and pouring off the slag when 3 grams of lead have gone into
it, there will be a loss of (owing to the slag carrying it off) about 0.2 gram
of copper. On repeating the operation, the next 3 grams of lead will carry
with them about 0.5 gram of copper; and on again repeating, 3 grams of
lead will remove 0.8 gram of copper. Finally, the last gram of lead will
carry with it 0.3 gram of copper, and there will be left a button of copper
weighing 8.3 grams. The slag will have carried off altogether 1.7 gram of
copper, which is 17 per cent. of the metal originally present.
With the more perfect exposure to the air, and quicker removal of the slag,
which results from heating on a cupel, the loss would be heavier. Karsten
got by actual experiment on cupelling copper and lead in equal proportions,
a loss of 21.25 per cent.
Going back to the example: if the slag were collected and fused with a
suitable reducing agent so as to convert, say, half of it into metal, that half
would contain nearly the whole of the copper (such a reduction is called
"cleaning the slag"). On reoxidising this metal, another button of copper is
formed which, added to the first, would reduce the loss from 17 per cent. to,
say, 7 or 8 per cent. And it is conceivable that by a series of similar
operations, almost the whole of the 10 grams of copper originally taken
might be recovered. In practice the problem is (as far as the copper is
concerned) not how to save, but how most easily to remove it; and since the
removal of this metal is quicker from an alloy containing not too much lead,
it is evident that two or three operations with small quantities of lead will be
more effectual than a single treatment with a larger quantity. With those
metals (tin, antimony, &c.) which pass quickly into the slag, the contrary is
true; hence with these it is necessary to have enough lead present, so that
the slag formed at the outset shall contain enough oxide of lead to make it
fluid. As silver is so much less easily oxidised than copper, we should
1:4 1 : 0.2
1 : 2.5 1 : 0.16
1:2 1 : 0.08
1 : 0.16 1 : 0.04
Assuming these figures to be correct, the following statement is
approximately true. On oxidising an alloy of 10 grams of copper and 10
grams of lead, and pouring off the slag when 3 grams of lead have gone into
it, there will be a loss of (owing to the slag carrying it off) about 0.2 gram
of copper. On repeating the operation, the next 3 grams of lead will carry
with them about 0.5 gram of copper; and on again repeating, 3 grams of
lead will remove 0.8 gram of copper. Finally, the last gram of lead will
carry with it 0.3 gram of copper, and there will be left a button of copper
weighing 8.3 grams. The slag will have carried off altogether 1.7 gram of
copper, which is 17 per cent. of the metal originally present.
With the more perfect exposure to the air, and quicker removal of the slag,
which results from heating on a cupel, the loss would be heavier. Karsten
got by actual experiment on cupelling copper and lead in equal proportions,
a loss of 21.25 per cent.
Going back to the example: if the slag were collected and fused with a
suitable reducing agent so as to convert, say, half of it into metal, that half
would contain nearly the whole of the copper (such a reduction is called
"cleaning the slag"). On reoxidising this metal, another button of copper is
formed which, added to the first, would reduce the loss from 17 per cent. to,
say, 7 or 8 per cent. And it is conceivable that by a series of similar
operations, almost the whole of the 10 grams of copper originally taken
might be recovered. In practice the problem is (as far as the copper is
concerned) not how to save, but how most easily to remove it; and since the
removal of this metal is quicker from an alloy containing not too much lead,
it is evident that two or three operations with small quantities of lead will be
more effectual than a single treatment with a larger quantity. With those
metals (tin, antimony, &c.) which pass quickly into the slag, the contrary is
true; hence with these it is necessary to have enough lead present, so that
the slag formed at the outset shall contain enough oxide of lead to make it
fluid. As silver is so much less easily oxidised than copper, we should
Page 154
reasonably expect that the proportion of silver carried off in the oxide of
lead would be considerably less than that of the copper indicated in the
above example. Indeed, there are one or two facts which tend to encourage
the hope that the operation may be conducted without any loss. If a piece of
pure silver foil is exposed on a cupel to air at the usual temperature of
cupellation, it undergoes very little change; it does not even fuse; it loses
nothing in weight, and does not oxidise. In fact, even if oxide of silver were
formed under these conditions, it could not continue to exist, for it is
decomposed into silver and oxygen at a temperature considerably below
redness. On the other hand, oxide of silver is not reduced to metal by heat
alone, when mixed with an excess of oxide of lead; while metallic silver is
converted into oxide when heated with the higher oxides of lead, copper,
and some other metals. That silver, and even gold (which is more difficult
to oxidise than silver), may be carried off in the slag in this way, is in
agreement with general experience. If 10 grams of silver are cupelled with
10 grams of lead, there will be a loss of about 50 milligrams of silver,
which is in round numbers 1-30th of the corresponding copper loss; with 10
grams of gold and 10 grams of lead, the loss will be 4 or 5 milligrams,
which is about 1-12th of the corresponding silver loss.
Determination of Silver in Assay Lead.—Scorify 50 grams of the lead
with 0.5 gram of powdered quartz or glass at not too high a temperature.
When the eye has "closed in," pour; reject the slag, and cupel the button of
lead. Remove the cupel from the muffle immediately the operation is
finished. Weigh, and make a prominent note of the result in the assay book,
as so many milligrams of silver contained in 100 grams of lead.
Determination of Silver in Red Lead or Litharge.—Fuse 100 grams of
the oxide with from 10 to 20 grams of borax; and in the case of litharge
with 2 grams or with red lead 4 grams of flour. Cupel the lead, and weigh
the button of silver. Note the result as in the last case.
Determination of Silver in Argentiferous Lead.—Be careful in taking the
sample, since with rich silver lead alloys the error from bad sampling may
amount to several parts per cent. Cupel two lots of 20 grams each, and
weigh the buttons of silver. Add to these the estimated cupel loss, and
calculate the result. Or wrap each button of silver in 20 grams of assay lead,
and re-cupel side by side with two fresh lots of 20 grams each of the alloy.
lead would be considerably less than that of the copper indicated in the
above example. Indeed, there are one or two facts which tend to encourage
the hope that the operation may be conducted without any loss. If a piece of
pure silver foil is exposed on a cupel to air at the usual temperature of
cupellation, it undergoes very little change; it does not even fuse; it loses
nothing in weight, and does not oxidise. In fact, even if oxide of silver were
formed under these conditions, it could not continue to exist, for it is
decomposed into silver and oxygen at a temperature considerably below
redness. On the other hand, oxide of silver is not reduced to metal by heat
alone, when mixed with an excess of oxide of lead; while metallic silver is
converted into oxide when heated with the higher oxides of lead, copper,
and some other metals. That silver, and even gold (which is more difficult
to oxidise than silver), may be carried off in the slag in this way, is in
agreement with general experience. If 10 grams of silver are cupelled with
10 grams of lead, there will be a loss of about 50 milligrams of silver,
which is in round numbers 1-30th of the corresponding copper loss; with 10
grams of gold and 10 grams of lead, the loss will be 4 or 5 milligrams,
which is about 1-12th of the corresponding silver loss.
Determination of Silver in Assay Lead.—Scorify 50 grams of the lead
with 0.5 gram of powdered quartz or glass at not too high a temperature.
When the eye has "closed in," pour; reject the slag, and cupel the button of
lead. Remove the cupel from the muffle immediately the operation is
finished. Weigh, and make a prominent note of the result in the assay book,
as so many milligrams of silver contained in 100 grams of lead.
Determination of Silver in Red Lead or Litharge.—Fuse 100 grams of
the oxide with from 10 to 20 grams of borax; and in the case of litharge
with 2 grams or with red lead 4 grams of flour. Cupel the lead, and weigh
the button of silver. Note the result as in the last case.
Determination of Silver in Argentiferous Lead.—Be careful in taking the
sample, since with rich silver lead alloys the error from bad sampling may
amount to several parts per cent. Cupel two lots of 20 grams each, and
weigh the buttons of silver. Add to these the estimated cupel loss, and
calculate the result. Or wrap each button of silver in 20 grams of assay lead,
and re-cupel side by side with two fresh lots of 20 grams each of the alloy.
Page 155
Calculate the loss incurred, and add on to the weight of the two fresh
buttons got.
Determination of Silver in Bullion.—The remarks made under the last
heading as to the importance of correct sampling apply with equal force
here. Make a preliminary assay by cupelling 0.1 gram of the alloy with 1
gram of assay lead; calculate the percentage composition. Refer to the table
on page 105 to find what weight of lead is required for cupelling 1 gram of
alloy.
Weigh out four lots of 1 gram each, and wrap them in the required quantity
of lead. Make two check pieces by weighing up two lots of fine silver equal
to that which you believe to be present in the assay pieces; add copper to
make up the weight to 1 gram, and wrap in the same quantity of lead as was
used for the assays.
Prepare six cupels and charge them in the annexed order (fig. 43), and
cupel. Guard against spirting. Clean and weigh the buttons of silver. Add
the mean loss on the two check pieces to the mean weight of the four assay
pieces; this multiplied by 1000 will give the degree of fineness.
Determination of Silver in Copper.—The silver is best separated in the
wet way before cupelling, but if the proportion is not too small, it can be
buttons got.
Determination of Silver in Bullion.—The remarks made under the last
heading as to the importance of correct sampling apply with equal force
here. Make a preliminary assay by cupelling 0.1 gram of the alloy with 1
gram of assay lead; calculate the percentage composition. Refer to the table
on page 105 to find what weight of lead is required for cupelling 1 gram of
alloy.
Weigh out four lots of 1 gram each, and wrap them in the required quantity
of lead. Make two check pieces by weighing up two lots of fine silver equal
to that which you believe to be present in the assay pieces; add copper to
make up the weight to 1 gram, and wrap in the same quantity of lead as was
used for the assays.
Prepare six cupels and charge them in the annexed order (fig. 43), and
cupel. Guard against spirting. Clean and weigh the buttons of silver. Add
the mean loss on the two check pieces to the mean weight of the four assay
pieces; this multiplied by 1000 will give the degree of fineness.
Determination of Silver in Copper.—The silver is best separated in the
wet way before cupelling, but if the proportion is not too small, it can be
Page 156
found by cupellation. Weigh up 3 grams of the metal, wrap in 30 grams of
sheet lead, and cupel; when the cupellation has proceeded for fifteen
minutes, add 20 grams more lead, and continue till finished. Weigh the
button of silver.
The cupellation loss will be five or six per cent. of the silver present.
Determine it by powdering the saturated portion of the cupel and fusing in a
large Cornish crucible with 30 grams each of soda and borax, 10 grams of
fluor spar, and 1-1/2 gram of charcoal. Cupel the resulting button of lead,
and add 10 grams more of lead towards the close of the operation. Deduct
the weight of silver contained in the lead used from the weight of the two
buttons, and calculate to ounces to the ton.
In an experiment in which 0.1975 gram of silver was present, the weight of
the button from the first cupellation was 0.1867, and that of the button from
the second, after correcting for the lead added, was 0.0110 gram.
Determination of Silver in Galena. By Pot Assay.—Mix 20 grams of the
powdered ore with 30 grams of red lead, 20 grams of soda, and 5 grams of
borax, as also with from 7 to 10 grams of nitre. Fuse and pour. Clean the
slag if the ore is rich. Cupel the buttons of lead. Make the usual corrections
and calculate in ounces to the ton.
By Scorification.—Take 10 grams of the ore, 30 grams of lead, and 0.5
gram of borax. Scorify, clean the slag by adding anthracite after the "eye"
has closed in: cupel the button of lead. Weigh the button of silver, make the
necessary corrections, and calculate to ounces to the ton.
The determination may also be made by cupelling the button of lead got in
the dry lead assay.
A sample of galena determined by the three methods gave the following
results:—
By pot assay 7.18 ozs. per ton.
" scorification 7.02 "
" lead assay 6.72 "
sheet lead, and cupel; when the cupellation has proceeded for fifteen
minutes, add 20 grams more lead, and continue till finished. Weigh the
button of silver.
The cupellation loss will be five or six per cent. of the silver present.
Determine it by powdering the saturated portion of the cupel and fusing in a
large Cornish crucible with 30 grams each of soda and borax, 10 grams of
fluor spar, and 1-1/2 gram of charcoal. Cupel the resulting button of lead,
and add 10 grams more of lead towards the close of the operation. Deduct
the weight of silver contained in the lead used from the weight of the two
buttons, and calculate to ounces to the ton.
In an experiment in which 0.1975 gram of silver was present, the weight of
the button from the first cupellation was 0.1867, and that of the button from
the second, after correcting for the lead added, was 0.0110 gram.
Determination of Silver in Galena. By Pot Assay.—Mix 20 grams of the
powdered ore with 30 grams of red lead, 20 grams of soda, and 5 grams of
borax, as also with from 7 to 10 grams of nitre. Fuse and pour. Clean the
slag if the ore is rich. Cupel the buttons of lead. Make the usual corrections
and calculate in ounces to the ton.
By Scorification.—Take 10 grams of the ore, 30 grams of lead, and 0.5
gram of borax. Scorify, clean the slag by adding anthracite after the "eye"
has closed in: cupel the button of lead. Weigh the button of silver, make the
necessary corrections, and calculate to ounces to the ton.
The determination may also be made by cupelling the button of lead got in
the dry lead assay.
A sample of galena determined by the three methods gave the following
results:—
By pot assay 7.18 ozs. per ton.
" scorification 7.02 "
" lead assay 6.72 "
Page 157
Determination of Silver in an Ore. By Pot Assay.—Take 20 grams of the
powdered ore and mix with 30 grams of soda, 40 grams of red lead, and 5
grams of borax, as also with from 2 to 3 grams of flour. Fuse: pour. Clean
the slag by fusing with 20 grams of red lead and two grams of flour. Cupel
the buttons of lead; weigh; make the necessary corrections, and calculate to
ounces to the ton.
By Scorification.—Take 5 grams of the powdered ore, 50 grams of lead, and
0.5 gram of "soda" or borax. Scorify. Clean the slag by fusing in a crucible
as in the pot assay. Cupel, &c.
Examples.—By Pot Assay.—Ore taken 20 grams.
Silver got 0.2893 gram
Silver from slag 0.0060 "
Silver lost in cupellation 0.0100 "
———
0.3053 "
Deduct silver in red lead 0.0017 "
———
Silver in ore 0.3036 " = 495.9 ozs. per ton.
By Scorification.—Ore taken, 3 grams.
Silver got. 0.0425 gram
Silver from slag 0.0022 "
Silver lost in cupellation 0.0020 "
———
0.0467 "
Deduct silver in lead 0.0015 "
———
Silver in ore 0.0452 " = 492.2 ozs. per ton.
Determination of Silver in Silver Precipitate.—This substance contains,
in addition to metallic silver and gold, sulphates of lead and lime; oxides of
zinc, copper, and iron; and more or less organic matter. The sample as
powdered ore and mix with 30 grams of soda, 40 grams of red lead, and 5
grams of borax, as also with from 2 to 3 grams of flour. Fuse: pour. Clean
the slag by fusing with 20 grams of red lead and two grams of flour. Cupel
the buttons of lead; weigh; make the necessary corrections, and calculate to
ounces to the ton.
By Scorification.—Take 5 grams of the powdered ore, 50 grams of lead, and
0.5 gram of "soda" or borax. Scorify. Clean the slag by fusing in a crucible
as in the pot assay. Cupel, &c.
Examples.—By Pot Assay.—Ore taken 20 grams.
Silver got 0.2893 gram
Silver from slag 0.0060 "
Silver lost in cupellation 0.0100 "
———
0.3053 "
Deduct silver in red lead 0.0017 "
———
Silver in ore 0.3036 " = 495.9 ozs. per ton.
By Scorification.—Ore taken, 3 grams.
Silver got. 0.0425 gram
Silver from slag 0.0022 "
Silver lost in cupellation 0.0020 "
———
0.0467 "
Deduct silver in lead 0.0015 "
———
Silver in ore 0.0452 " = 492.2 ozs. per ton.
Determination of Silver in Silver Precipitate.—This substance contains,
in addition to metallic silver and gold, sulphates of lead and lime; oxides of
zinc, copper, and iron; and more or less organic matter. The sample as
Page 158
received is generally free from "water at 100° C."; and, since it rapidly
absorbs water, care should be taken in weighing it.
Since it contains combined water it is not suited for scorifying; therefore the
determination of silver and gold (fine metal) is made by pot assay. Weigh
up 5 grams of the precipitate, mix with 100 grams of litharge and 1 gram of
charcoal. Melt in a crucible at a moderate heat and pour. Detach the slag,
replace in the crucible, and, when fused, add a mixture of 20 grams of
litharge and 1 gram of charcoal. When the fusion is again tranquil, pour;
and cupel the two buttons of lead.
In a sample worked in this manner the mean of four determinations gave
0.6819 gram of "fine metal"; deducting 1 milligram for the silver contained
in the oxide of lead, and adding 8 milligrams for the cupellation loss, there
is got 0.6889 gram or 13.778 per cent. of silver (and gold) in the sample.
Determination of Silver in Burnt Ores. By Pot Assay.—Roasted
cupriferous pyrites containing small quantities of gold and silver comes
under this heading. The following mixture will give a fluid slag which is
heavy and tough when cold:—
Ore. Borax. Sand.Litharge. Charcoal.
100 50 50 100 7
Mix; place in a large crucible; cover with salt; and melt down under cover.
When fused drop in an iron rod for a few minutes, and about a couple of
minutes after its withdrawal, pour the charge quickly into a large conical
mould. The button of lead should weigh about 50 grams. Cupel and weigh
the silver. The litharge may be replaced by red lead, in which case another
gram of charcoal powder must be added.
In our experience the results obtained by this method are about 20 per cent.
less than the actual content of the ore. The results of two assays, after
deducting for the silver in the litharge used, were 3.9 and 4.1 milligrams;
and a third assay, in which 5.4 milligrams of silver had been added, gave
9.2, which, after deducting the added silver, leaves 3.8 milligrams. The
average of the three results is 3.9 milligrams from the 100 grams of ore.
absorbs water, care should be taken in weighing it.
Since it contains combined water it is not suited for scorifying; therefore the
determination of silver and gold (fine metal) is made by pot assay. Weigh
up 5 grams of the precipitate, mix with 100 grams of litharge and 1 gram of
charcoal. Melt in a crucible at a moderate heat and pour. Detach the slag,
replace in the crucible, and, when fused, add a mixture of 20 grams of
litharge and 1 gram of charcoal. When the fusion is again tranquil, pour;
and cupel the two buttons of lead.
In a sample worked in this manner the mean of four determinations gave
0.6819 gram of "fine metal"; deducting 1 milligram for the silver contained
in the oxide of lead, and adding 8 milligrams for the cupellation loss, there
is got 0.6889 gram or 13.778 per cent. of silver (and gold) in the sample.
Determination of Silver in Burnt Ores. By Pot Assay.—Roasted
cupriferous pyrites containing small quantities of gold and silver comes
under this heading. The following mixture will give a fluid slag which is
heavy and tough when cold:—
Ore. Borax. Sand.Litharge. Charcoal.
100 50 50 100 7
Mix; place in a large crucible; cover with salt; and melt down under cover.
When fused drop in an iron rod for a few minutes, and about a couple of
minutes after its withdrawal, pour the charge quickly into a large conical
mould. The button of lead should weigh about 50 grams. Cupel and weigh
the silver. The litharge may be replaced by red lead, in which case another
gram of charcoal powder must be added.
In our experience the results obtained by this method are about 20 per cent.
less than the actual content of the ore. The results of two assays, after
deducting for the silver in the litharge used, were 3.9 and 4.1 milligrams;
and a third assay, in which 5.4 milligrams of silver had been added, gave
9.2, which, after deducting the added silver, leaves 3.8 milligrams. The
average of the three results is 3.9 milligrams from the 100 grams of ore.
Page 159
Two lots of 100 grams of the same ore treated in the wet way gave 5.2 and
5.0 milligrams of silver. Burnt ores from Spanish pyrites carry about 0.005
per cent. of silver.
WET METHODS.
Silver is got into solution from its ores by attacking with nitric acid, but it is
best, after dissolving, to cautiously add dilute hydrochloric acid, and to
carefully avoid excess. If the quantity of silver is very small the solution is
allowed to stand twenty-four hours, but, otherwise, it is warmed and filtered
as soon as it clears. Dry the residue and concentrate the silver in a button of
lead by pot method or scorification, according to the amount of stony matter
present. Cupel the lead, and the resulting button will be free from all metals,
except perhaps gold. It may be weighed; or dissolved in nitric acid, and the
silver determined gravimetrically in the diluted and filtered solution. It is
better to weigh the metal and afterwards to determine the gold in it,
estimating the silver by difference. Silver alloys are dissolved in dilute
nitric acid (free from chlorides), diluted, and filtered. The solution is then
ready for gravimetric determination.
Sulphuretted hydrogen precipitates silver (like copper), completely, even
from fairly acid solutions.
GRAVIMETRIC DETERMINATION.
Add dilute hydrochloric acid in small excess to the hot dilute solution,
which must contain free nitric acid. Heat and stir until the solution clears.
Decant through a small filter, and wash with hot water, acidulated at first
with a little nitric acid if bismuth is suspected to be present. Dry quickly,
transfer as much as possible of the precipitate to a watch-glass; burn and
ignite the filter paper, treating the ash first with two drops of nitric acid and
then with one of hydrochloric, and again dry. Add the rest of the silver
chloride and heat slowly over a Bunsen burner until it begins to fuse. Cool
and weigh.
The precipitate is silver chloride (AgCl) and contains 75.27 per cent. of
silver. The moist precipitate is heavy and curdy; it is decomposed by direct
5.0 milligrams of silver. Burnt ores from Spanish pyrites carry about 0.005
per cent. of silver.
WET METHODS.
Silver is got into solution from its ores by attacking with nitric acid, but it is
best, after dissolving, to cautiously add dilute hydrochloric acid, and to
carefully avoid excess. If the quantity of silver is very small the solution is
allowed to stand twenty-four hours, but, otherwise, it is warmed and filtered
as soon as it clears. Dry the residue and concentrate the silver in a button of
lead by pot method or scorification, according to the amount of stony matter
present. Cupel the lead, and the resulting button will be free from all metals,
except perhaps gold. It may be weighed; or dissolved in nitric acid, and the
silver determined gravimetrically in the diluted and filtered solution. It is
better to weigh the metal and afterwards to determine the gold in it,
estimating the silver by difference. Silver alloys are dissolved in dilute
nitric acid (free from chlorides), diluted, and filtered. The solution is then
ready for gravimetric determination.
Sulphuretted hydrogen precipitates silver (like copper), completely, even
from fairly acid solutions.
GRAVIMETRIC DETERMINATION.
Add dilute hydrochloric acid in small excess to the hot dilute solution,
which must contain free nitric acid. Heat and stir until the solution clears.
Decant through a small filter, and wash with hot water, acidulated at first
with a little nitric acid if bismuth is suspected to be present. Dry quickly,
transfer as much as possible of the precipitate to a watch-glass; burn and
ignite the filter paper, treating the ash first with two drops of nitric acid and
then with one of hydrochloric, and again dry. Add the rest of the silver
chloride and heat slowly over a Bunsen burner until it begins to fuse. Cool
and weigh.
The precipitate is silver chloride (AgCl) and contains 75.27 per cent. of
silver. The moist precipitate is heavy and curdy; it is decomposed by direct
Page 160
sunlight, becoming violet under its influence. When heated it is yellowish;
and, since it is volatile at a high temperature, it must not, in drying, be
heated above its fusing point. The fused chloride can be removed from the
crucible (to which it adheres strongly) by digesting with dilute acid and
zinc.
For the determination of silver in nearly pure bullion the following process
is used:—Weigh up 1.5054 gram of the alloy. With this amount of alloy
each 2 milligrams of silver chloride formed is equivalent to 1 degree of
fineness, so that the weight of the silver chloride obtained (stated in
milligrams and divided by 2) will give the degree of fineness. Transfer to a
bottle (known as "bottles for the Indian mint assay") and dissolve in 10 c.c.
of dilute nitric acid, then make up with water to 200 c.c. and add 3 c.c. of
dilute hydrochloric acid. Allow to stand a few minutes and then shake. Fill
the bottle completely with water, allow to settle, and syphon off the clear
liquid; pour on more water, shake gently to break up the lumps, and again
fill the bottle with water. Invert over the mouth of the bottle a porous
Wedgwood crucible, somewhat similar to those used in gold parting. Take
firm hold of the crucible and bottle, and invert promptly so that the silver
chloride may be collected in the crucible. Allow to stand a little while for
the precipitate to settle, and then carefully remove the crucible under water.
[14]
Drain off most of the water and break up the silver chloride with the
help of a well-rounded glass rod. This greatly facilitates the subsequent
drying. Dry first on the water bath and then on the iron plate. Remove the
dried silver chloride, by inverting the crucible, and weigh it.
As an example, 3 determinations of silver in a coin carried out in this way
gave:—
and, since it is volatile at a high temperature, it must not, in drying, be
heated above its fusing point. The fused chloride can be removed from the
crucible (to which it adheres strongly) by digesting with dilute acid and
zinc.
For the determination of silver in nearly pure bullion the following process
is used:—Weigh up 1.5054 gram of the alloy. With this amount of alloy
each 2 milligrams of silver chloride formed is equivalent to 1 degree of
fineness, so that the weight of the silver chloride obtained (stated in
milligrams and divided by 2) will give the degree of fineness. Transfer to a
bottle (known as "bottles for the Indian mint assay") and dissolve in 10 c.c.
of dilute nitric acid, then make up with water to 200 c.c. and add 3 c.c. of
dilute hydrochloric acid. Allow to stand a few minutes and then shake. Fill
the bottle completely with water, allow to settle, and syphon off the clear
liquid; pour on more water, shake gently to break up the lumps, and again
fill the bottle with water. Invert over the mouth of the bottle a porous
Wedgwood crucible, somewhat similar to those used in gold parting. Take
firm hold of the crucible and bottle, and invert promptly so that the silver
chloride may be collected in the crucible. Allow to stand a little while for
the precipitate to settle, and then carefully remove the crucible under water.
[14]
Drain off most of the water and break up the silver chloride with the
help of a well-rounded glass rod. This greatly facilitates the subsequent
drying. Dry first on the water bath and then on the iron plate. Remove the
dried silver chloride, by inverting the crucible, and weigh it.
As an example, 3 determinations of silver in a coin carried out in this way
gave:—
Page 161
(1) 1.8500gram AgCl = 925.0 fineness.
(2) 1.8498 " = 924.9 "
(3) 1.8502 " = 925.1 "
Determination of Silver in Burnt Ores.—Take 100 grams of the ore and
place in a large beaker of 2-1/2 litres capacity, and cover with 375 c.c. of
hydrochloric acid. Boil for half an hour until the oxides are dissolved and
the residue looks like sand and pyrites; then add 20 c.c. of nitric acid, and
boil till free from nitrous fumes. Dilute to 2 litres with water, and pass a
current of sulphuretted hydrogen till the iron is reduced, the copper and
silver precipitated, and the liquor smells of the gas. This takes about one
hour and a half.
Filter off the precipitate (rejecting the solution) and wash with warm water.
Dry and transfer to an evaporating dish, adding the ashes of the filter paper.
Heat gently with a Bunsen burner until the sulphur burns, and then calcine
until no more sulphurous oxide comes off. When cold add 30 c.c. of nitric
acid, boil and dilute to 100 c.c. Add 1 c.c. of very dilute hydrochloric acid
(1 to 100),[15] stir well, and allow to stand overnight. Decant on to a
Swedish filter paper, dry and calcine.
Mix the ashes with 100 grams of litharge and 1 gram of charcoal, and fuse
in a small crucible. Detach the button of lead and cupel. Weigh and make
the usual corrections. As an example, 100 grams of ore treated in this way
gave 5.8 milligrams of silver; deducting 0.8 for the silver added in the oxide
of lead leaves 5 milligrams obtained from the ore. Another experiment on
100 grams of the same ore to which 5 milligrams of silver had been added
gave 11.0 milligrams. Deduct 5.8 for the silver added; this leaves 5.2
milligrams as the silver obtained from the ore. These give, as a mean result,
0.0051 per cent., or 1.66 ounce per ton.
Determination of Silver in Commercial Copper.—For the method of
doing this, with an example and experiment, see under the heading of
Examination of Commercial Copper.
VOLUMETRIC METHODS.
(2) 1.8498 " = 924.9 "
(3) 1.8502 " = 925.1 "
Determination of Silver in Burnt Ores.—Take 100 grams of the ore and
place in a large beaker of 2-1/2 litres capacity, and cover with 375 c.c. of
hydrochloric acid. Boil for half an hour until the oxides are dissolved and
the residue looks like sand and pyrites; then add 20 c.c. of nitric acid, and
boil till free from nitrous fumes. Dilute to 2 litres with water, and pass a
current of sulphuretted hydrogen till the iron is reduced, the copper and
silver precipitated, and the liquor smells of the gas. This takes about one
hour and a half.
Filter off the precipitate (rejecting the solution) and wash with warm water.
Dry and transfer to an evaporating dish, adding the ashes of the filter paper.
Heat gently with a Bunsen burner until the sulphur burns, and then calcine
until no more sulphurous oxide comes off. When cold add 30 c.c. of nitric
acid, boil and dilute to 100 c.c. Add 1 c.c. of very dilute hydrochloric acid
(1 to 100),[15] stir well, and allow to stand overnight. Decant on to a
Swedish filter paper, dry and calcine.
Mix the ashes with 100 grams of litharge and 1 gram of charcoal, and fuse
in a small crucible. Detach the button of lead and cupel. Weigh and make
the usual corrections. As an example, 100 grams of ore treated in this way
gave 5.8 milligrams of silver; deducting 0.8 for the silver added in the oxide
of lead leaves 5 milligrams obtained from the ore. Another experiment on
100 grams of the same ore to which 5 milligrams of silver had been added
gave 11.0 milligrams. Deduct 5.8 for the silver added; this leaves 5.2
milligrams as the silver obtained from the ore. These give, as a mean result,
0.0051 per cent., or 1.66 ounce per ton.
Determination of Silver in Commercial Copper.—For the method of
doing this, with an example and experiment, see under the heading of
Examination of Commercial Copper.
VOLUMETRIC METHODS.
Page 162
There are two of these, one adapted for the determination of silver in alloys
of approximately known composition, and the other of more general
application. The first of these, generally known as "Gay-Lussac's" method
is, as regards its working, perfect in principle; but it requires a practically
constant quantity of silver, that is, one which varies by a few milligrams
only in each determination. It is a confirmatory method rather than a
determinative one. The other is known as "Volhard's," and resembles in
principle and method an ordinary volumetric process.
Gay-Lussac's method is based on the precipitation of silver from a nitric
acid solution by a solution of sodium chloride. The point at which the whole
of the silver is precipitated being recognised by the standard solution
ceasing to give a precipitate. The process depends for its success upon, (1)
the ease which silver chloride separates out from the solution leaving it
clear after shaking, and, (2), the cloudiness produced by the reaction of very
small quantities of silver nitrate and sodium chloride. In working, a quantity
of the sodium chloride solution equal to 1 gram of silver is added at once to
the assay; and, when the solution has been rendered clear by shaking, the
residual silver (which should not exceed a few milligrams) is estimated with
the help of a weaker solution of sodium chloride. The success in working
evidently depends upon the accuracy with which the first addition of the
salt solution is made. On this account the standard solution is run in from a
special pipette capable of delivering a practically invariable volume of
solution. It is not so important that this shall deliver exactly 100 c.c. as that
in two consecutive deliveries the volume shall not differ by more than 0.05
c.c. The dilute salt solution is one-tenth of the strength of that first run in,
and 1 c.c. of it is equivalent to 1 milligram of silver. Ordinarily it is run in 1
c.c. at a time (and an ordinary burette may be used for this purpose),
shaking between each addition until it ceases to give a precipitate. If many
such additions have to be made the operation not only becomes tedious, but
the solution also ceases to clear after shaking, so that it becomes impossible
to determine the finishing point.
If the assay contains less than one gram of silver the first addition of the
dilute salt solution of course produces no precipitate. Five milligrams of
silver in solution (5 c.c.) is then added, and the assay proceeded with in the
usual way; 5 milligrams of silver being deducted from the amount found.
of approximately known composition, and the other of more general
application. The first of these, generally known as "Gay-Lussac's" method
is, as regards its working, perfect in principle; but it requires a practically
constant quantity of silver, that is, one which varies by a few milligrams
only in each determination. It is a confirmatory method rather than a
determinative one. The other is known as "Volhard's," and resembles in
principle and method an ordinary volumetric process.
Gay-Lussac's method is based on the precipitation of silver from a nitric
acid solution by a solution of sodium chloride. The point at which the whole
of the silver is precipitated being recognised by the standard solution
ceasing to give a precipitate. The process depends for its success upon, (1)
the ease which silver chloride separates out from the solution leaving it
clear after shaking, and, (2), the cloudiness produced by the reaction of very
small quantities of silver nitrate and sodium chloride. In working, a quantity
of the sodium chloride solution equal to 1 gram of silver is added at once to
the assay; and, when the solution has been rendered clear by shaking, the
residual silver (which should not exceed a few milligrams) is estimated with
the help of a weaker solution of sodium chloride. The success in working
evidently depends upon the accuracy with which the first addition of the
salt solution is made. On this account the standard solution is run in from a
special pipette capable of delivering a practically invariable volume of
solution. It is not so important that this shall deliver exactly 100 c.c. as that
in two consecutive deliveries the volume shall not differ by more than 0.05
c.c. The dilute salt solution is one-tenth of the strength of that first run in,
and 1 c.c. of it is equivalent to 1 milligram of silver. Ordinarily it is run in 1
c.c. at a time (and an ordinary burette may be used for this purpose),
shaking between each addition until it ceases to give a precipitate. If many
such additions have to be made the operation not only becomes tedious, but
the solution also ceases to clear after shaking, so that it becomes impossible
to determine the finishing point.
If the assay contains less than one gram of silver the first addition of the
dilute salt solution of course produces no precipitate. Five milligrams of
silver in solution (5 c.c.) is then added, and the assay proceeded with in the
usual way; 5 milligrams of silver being deducted from the amount found.
Page 163
There is required for the assay a standard solution of sodium chloride,
which is prepared by dissolving 5.4162 grams of the salt (made by
neutralizing carbonate of soda with hydrochloric acid) in water and diluting
to one litre. 100 c.c. of this is equivalent to 1 gram of silver.
The weaker solution of salt is made by diluting 100 c.c. of the stronger one
to one litre. One c.c. of this will equal 1 milligram of silver, or 0.1 c.c. of
the stronger solution.
A standard solution of silver equivalent to the dilute salt solution is made
by dissolving 1 gram of fine silver in 10 c.c. of dilute nitric acid, and
diluting with water to one litre.
The solution of salt is standardised as follows:—Weigh up 1.003 gram of
fine silver and dissolve in 25 c.c. of dilute nitric acid in a bottle provided
with a well-fitting flat-headed stopper. Heat on the water bath to assist
solution, resting the bottle in an inclined position. When dissolved blow out
the nitrous fumes with the help of a glass tube bent at right angles. Run in
which is prepared by dissolving 5.4162 grams of the salt (made by
neutralizing carbonate of soda with hydrochloric acid) in water and diluting
to one litre. 100 c.c. of this is equivalent to 1 gram of silver.
The weaker solution of salt is made by diluting 100 c.c. of the stronger one
to one litre. One c.c. of this will equal 1 milligram of silver, or 0.1 c.c. of
the stronger solution.
A standard solution of silver equivalent to the dilute salt solution is made
by dissolving 1 gram of fine silver in 10 c.c. of dilute nitric acid, and
diluting with water to one litre.
The solution of salt is standardised as follows:—Weigh up 1.003 gram of
fine silver and dissolve in 25 c.c. of dilute nitric acid in a bottle provided
with a well-fitting flat-headed stopper. Heat on the water bath to assist
solution, resting the bottle in an inclined position. When dissolved blow out
the nitrous fumes with the help of a glass tube bent at right angles. Run in
Page 164
from a stoppered pipette (as shown in fig. 44) 100 c.c. of the standard salt
solution, and shake vigorously until the solution clears. Fill an ordinary
burette with the weaker standard salt solution, and run 1 c.c. into the assay
bottle, letting it run down the side so that it forms a layer resting on the
assay solution. If any silver remains in solution a cloudy layer will be
formed at the junction where the two liquids meet. This is best observed
against a black background If a cloudiness is seen, shake, to clear the liquid,
and run in another c.c. of salt, and continue this until a cloudiness is no
longer visible. Deduct 1.5 c.c. from the amount of the weaker sodium
chloride solution run in. Divide the corrected reading by 10, and add to the
100 c.c. This will give the volume of strong salt solution equivalent to the
silver taken.
If the first addition of the weaker salt solution causes no cloudiness add 5
c.c. of the silver solution from an ordinary pipette, shake, and then run in
the weaker salt solution, working as before. These 5 milligrams of silver
added must be allowed for before calculating. As an example:—1.0100
gram of fine silver was taken for standardising a solution and 4 c.c. of the
weaker salt solution were run in. Deducting 1.5 and dividing by 10 gives
0.25 c.c. to be added to the 100 c.c.
100.25 : 1.0100 :: 100 : x
x = 1.0075
which is the standard of the salt solution.
The method of working an assay may be gathered from the following
example:—In the determination of silver in some buttons left after
cupellation, it was assumed that these would contain 99.5 per cent. of silver.
For the assay it was necessary to take a quantity that should contain a little
more than 1.0075 grams of silver; then
99.5 : 100 :: 1.0075 : x
x = 1.0125
To ensure a slight excess, there was taken 1.0150 gram of the buttons,
which was treated in exactly the same way as for the standardising. The
quantity of the weaker salt solution required was 7 c.c.; deducting 1.5 c.c.,
and dividing by 10, gives 100.55 c.c. of strong salt solution, which is
solution, and shake vigorously until the solution clears. Fill an ordinary
burette with the weaker standard salt solution, and run 1 c.c. into the assay
bottle, letting it run down the side so that it forms a layer resting on the
assay solution. If any silver remains in solution a cloudy layer will be
formed at the junction where the two liquids meet. This is best observed
against a black background If a cloudiness is seen, shake, to clear the liquid,
and run in another c.c. of salt, and continue this until a cloudiness is no
longer visible. Deduct 1.5 c.c. from the amount of the weaker sodium
chloride solution run in. Divide the corrected reading by 10, and add to the
100 c.c. This will give the volume of strong salt solution equivalent to the
silver taken.
If the first addition of the weaker salt solution causes no cloudiness add 5
c.c. of the silver solution from an ordinary pipette, shake, and then run in
the weaker salt solution, working as before. These 5 milligrams of silver
added must be allowed for before calculating. As an example:—1.0100
gram of fine silver was taken for standardising a solution and 4 c.c. of the
weaker salt solution were run in. Deducting 1.5 and dividing by 10 gives
0.25 c.c. to be added to the 100 c.c.
100.25 : 1.0100 :: 100 : x
x = 1.0075
which is the standard of the salt solution.
The method of working an assay may be gathered from the following
example:—In the determination of silver in some buttons left after
cupellation, it was assumed that these would contain 99.5 per cent. of silver.
For the assay it was necessary to take a quantity that should contain a little
more than 1.0075 grams of silver; then
99.5 : 100 :: 1.0075 : x
x = 1.0125
To ensure a slight excess, there was taken 1.0150 gram of the buttons,
which was treated in exactly the same way as for the standardising. The
quantity of the weaker salt solution required was 7 c.c.; deducting 1.5 c.c.,
and dividing by 10, gives 100.55 c.c. of strong salt solution, which is
Page 165
equivalent to 1.0130 gram of silver. This being obtained from 1.015 gram of
alloy, is equal to 99.8 per cent., or 998.0 fine.
The Effect of Temperature.—The standardising and the assay must be
done at the same time, since a difference of 5° C. makes a difference of 0.1
c.c. in measuring the 100 c.c. of strong solution of salt. It is always best to
prepare a standard with each batch of assays.
SULPHOCYANATE METHOD.—Volhard's process is based upon the
precipitation of silver in nitric acid solutions with potassium sulphocyanate,
the finishing point being the development of a reddish-brown colour,
produced by the action of the excess of sulphocyanate upon ferric sulphate.
The white sulphocyanate settles readily, leaving the liquor clear; and a
persistent brown coloration in the liquid indicates the finish. The assay must
be carried out in the cold; and water free from chlorides[16] must be used.
The standard sulphocyanate of potassium solution is made by dissolving 4-
1/2 or 5 grams of the salt (KCyS) in water, and diluting to 1 litre. 100 c.c.
are about equivalent to 0.5 gram of silver.
The standard silver nitrate solution is made by dissolving 5 grams of fine
silver in 50 c.c. of dilute nitric acid, boiling off nitrous fumes, and diluting
to 1 litre.
The indicator is a saturated solution of iron alum, or a solution of ferric
sulphate of equivalent strength made by titrating acid ferrous sulphate with
potassium permanganate. Use 2 c.c. for each assay.
The sulphocyanate solution is standardised by placing 50 c.c. of the silver
nitrate solution in a flask with 20 c.c. of dilute nitric acid, diluting to 100
c.c. with water, and running in the sulphocyanate until the greater part of
the silver is precipitated; then adding 2 c.c. of the ferric indicator, and
continuing the titration until a reddish-brown colour is developed, and
remains permanent after shaking continuously. The assay is similarly
performed, the silver being used in the state of a nitric acid solution.
The effect of variations in the conditions of the assay may be seen from the
following experiments, in which 20 c.c. of standard silver nitrate were used:
—
alloy, is equal to 99.8 per cent., or 998.0 fine.
The Effect of Temperature.—The standardising and the assay must be
done at the same time, since a difference of 5° C. makes a difference of 0.1
c.c. in measuring the 100 c.c. of strong solution of salt. It is always best to
prepare a standard with each batch of assays.
SULPHOCYANATE METHOD.—Volhard's process is based upon the
precipitation of silver in nitric acid solutions with potassium sulphocyanate,
the finishing point being the development of a reddish-brown colour,
produced by the action of the excess of sulphocyanate upon ferric sulphate.
The white sulphocyanate settles readily, leaving the liquor clear; and a
persistent brown coloration in the liquid indicates the finish. The assay must
be carried out in the cold; and water free from chlorides[16] must be used.
The standard sulphocyanate of potassium solution is made by dissolving 4-
1/2 or 5 grams of the salt (KCyS) in water, and diluting to 1 litre. 100 c.c.
are about equivalent to 0.5 gram of silver.
The standard silver nitrate solution is made by dissolving 5 grams of fine
silver in 50 c.c. of dilute nitric acid, boiling off nitrous fumes, and diluting
to 1 litre.
The indicator is a saturated solution of iron alum, or a solution of ferric
sulphate of equivalent strength made by titrating acid ferrous sulphate with
potassium permanganate. Use 2 c.c. for each assay.
The sulphocyanate solution is standardised by placing 50 c.c. of the silver
nitrate solution in a flask with 20 c.c. of dilute nitric acid, diluting to 100
c.c. with water, and running in the sulphocyanate until the greater part of
the silver is precipitated; then adding 2 c.c. of the ferric indicator, and
continuing the titration until a reddish-brown colour is developed, and
remains permanent after shaking continuously. The assay is similarly
performed, the silver being used in the state of a nitric acid solution.
The effect of variations in the conditions of the assay may be seen from the
following experiments, in which 20 c.c. of standard silver nitrate were used:
—
Page 166
Effect of Varying Temperature:—
Temperature 10° C. 30° C. 70° C. 100° C.
Sulphocyanate reqd. 19.6 c.c. 19.3 c.c. 19.0 c.c. 18.6 c.c.
Effect of Varying Nitric Acid:—Varying nitric acid has no effect, except
that with a fairly acid solution the finishing point is somewhat sharper.
Nitric acid added 5 c.c. 10 c.c. 20 c.c. 50 c.c.
Sulphocyanate reqd. 19.6 c.c. 19.5 c.c. 19.6 c.c. 19.6 c.c.
Effect of Varying Bulk:—
Bulk 50 c.c. 100 c.c. 200 c.c. 300 c.c.
Sulphocyanate reqd. 19.5 c.c. 19.6 c.c. 19.6 c.c. 19.7 c.c.
Effect of Varying Ammonic Nitrate:—
Ammonic nitrate 0 gram 1 gram 5 grams 10 grams
Sulphocyanate reqd. 19.6 c.c. 19.6 c.c. 19.7 c.c. 19.9 c.c.
Effect of Varying Silver:—
Silver added 1 c.c. 10 c.c. 20 c.c. 50 c.c. 100 c.c.
Sulphocyanate reqd.1.0 c.c. 9.70 c.c. 19.6 c.c. 49.4 c.c. 99.0 c.c.
This method is valuable for determining silver in salts, alloys, and
solutions, where no more than an ordinary degree of accuracy is demanded.
It is easy, and applicable under most of the usual conditions. Its greatest
disadvantage is the brown coloration produced by the sulphocyanate when
the assay is nearly, but not quite, finished; and the slowness with which this
is removed on shaking up with the precipitate. This is worse with large
quantities of precipitate, and if about 1 gram of silver is present, it gives an
indefiniteness to the finish which lowers the precision of the process to
about 1 in 500; this is useless for the assays of bullion. One writer states
that this inconvenience is due to portions of liquid being entangled in the
precipitate, but it appears much more likely to be due to the action of the
precipitate itself. In attempting to apply the process to the assay of bullion
Temperature 10° C. 30° C. 70° C. 100° C.
Sulphocyanate reqd. 19.6 c.c. 19.3 c.c. 19.0 c.c. 18.6 c.c.
Effect of Varying Nitric Acid:—Varying nitric acid has no effect, except
that with a fairly acid solution the finishing point is somewhat sharper.
Nitric acid added 5 c.c. 10 c.c. 20 c.c. 50 c.c.
Sulphocyanate reqd. 19.6 c.c. 19.5 c.c. 19.6 c.c. 19.6 c.c.
Effect of Varying Bulk:—
Bulk 50 c.c. 100 c.c. 200 c.c. 300 c.c.
Sulphocyanate reqd. 19.5 c.c. 19.6 c.c. 19.6 c.c. 19.7 c.c.
Effect of Varying Ammonic Nitrate:—
Ammonic nitrate 0 gram 1 gram 5 grams 10 grams
Sulphocyanate reqd. 19.6 c.c. 19.6 c.c. 19.7 c.c. 19.9 c.c.
Effect of Varying Silver:—
Silver added 1 c.c. 10 c.c. 20 c.c. 50 c.c. 100 c.c.
Sulphocyanate reqd.1.0 c.c. 9.70 c.c. 19.6 c.c. 49.4 c.c. 99.0 c.c.
This method is valuable for determining silver in salts, alloys, and
solutions, where no more than an ordinary degree of accuracy is demanded.
It is easy, and applicable under most of the usual conditions. Its greatest
disadvantage is the brown coloration produced by the sulphocyanate when
the assay is nearly, but not quite, finished; and the slowness with which this
is removed on shaking up with the precipitate. This is worse with large
quantities of precipitate, and if about 1 gram of silver is present, it gives an
indefiniteness to the finish which lowers the precision of the process to
about 1 in 500; this is useless for the assays of bullion. One writer states
that this inconvenience is due to portions of liquid being entangled in the
precipitate, but it appears much more likely to be due to the action of the
precipitate itself. In attempting to apply the process to the assay of bullion
Page 167
by working it on the principle of a Gay-Lussac assay, it was found that a
very considerable excess of silver was required to complete the reaction. In
these experiments 100 c.c. of "sulphocyanate" (very accurately measured)
was run into the solution containing the weighed portion of bullion (fine
silver) and, after shaking the solution, was filtered. In the filtrate the
remaining silver, if there should be any, was determined by the ordinary
titration, but with "sulphocyanate" of one-tenth the strength. This final
titration was quite satisfactory. The amount of silver precipitated by the first
100 c.c., however, varied with the quantity of silver present as in the
following series.[17]
Silver present. Silver precipitated.
1.1342gram. 1.1322gram.
1.1375" 1.1335"
1.1405" 1.1351"
1.1484" 1.1379"
These, of course, preclude a method of the kind aimed at, and at the same
time emphasise the importance of uniformity of work in the ordinary
process. In the determination of chlorides in sea-water, Dittmar used a
combined method: precipitating the bulk of the silver as chloride, and after
filtering, determining the small excess of silver by sulphocyanate. This
modification answers admirably when applied to the assay of bullion. In the
ordinary Gay-Lussac method, the precipitation of the bulk of the silver by
the 100 c.c. of salt solution leaves nothing to be desired, either as to ease in
working or accuracy of result; the silver precipitate settles quickly, and
leaves a clear liquor admirably fitted for the determination of the few
milligrams of silver remaining in solution. But the method of determining
this residual silver by adding successive small quantities of salt so long as
they continue to give a precipitate is unsatisfactory, and, judged on its own
merits apart from the rest of the process, could hardly escape condemnation.
It is clumsy in practice, for the continued adding of small portions of salt
solution is laborious and becomes impossible with more than a few
milligrams of silver in solution. The proposed modification is simple;
having precipitated the silver with the 100 c.c. of salt solution, as described
under Gay-Lussac's method (page 120), shake till the liquor clears, and
filter into a flask, washing with a little distilled water. Add 2 c.c. of "ferric
very considerable excess of silver was required to complete the reaction. In
these experiments 100 c.c. of "sulphocyanate" (very accurately measured)
was run into the solution containing the weighed portion of bullion (fine
silver) and, after shaking the solution, was filtered. In the filtrate the
remaining silver, if there should be any, was determined by the ordinary
titration, but with "sulphocyanate" of one-tenth the strength. This final
titration was quite satisfactory. The amount of silver precipitated by the first
100 c.c., however, varied with the quantity of silver present as in the
following series.[17]
Silver present. Silver precipitated.
1.1342gram. 1.1322gram.
1.1375" 1.1335"
1.1405" 1.1351"
1.1484" 1.1379"
These, of course, preclude a method of the kind aimed at, and at the same
time emphasise the importance of uniformity of work in the ordinary
process. In the determination of chlorides in sea-water, Dittmar used a
combined method: precipitating the bulk of the silver as chloride, and after
filtering, determining the small excess of silver by sulphocyanate. This
modification answers admirably when applied to the assay of bullion. In the
ordinary Gay-Lussac method, the precipitation of the bulk of the silver by
the 100 c.c. of salt solution leaves nothing to be desired, either as to ease in
working or accuracy of result; the silver precipitate settles quickly, and
leaves a clear liquor admirably fitted for the determination of the few
milligrams of silver remaining in solution. But the method of determining
this residual silver by adding successive small quantities of salt so long as
they continue to give a precipitate is unsatisfactory, and, judged on its own
merits apart from the rest of the process, could hardly escape condemnation.
It is clumsy in practice, for the continued adding of small portions of salt
solution is laborious and becomes impossible with more than a few
milligrams of silver in solution. The proposed modification is simple;
having precipitated the silver with the 100 c.c. of salt solution, as described
under Gay-Lussac's method (page 120), shake till the liquor clears, and
filter into a flask, washing with a little distilled water. Add 2 c.c. of "ferric
Page 168
indicator" to the filtrate and titrate with a standard "sulphocyanate solution"
made by diluting the ordinary standard solution to such an extent that 100
c.c. after diluting shall be equivalent to 0.1 gram of silver.[18] Calculate the
weight of silver found by "sulphocyanate" and add it to the weight which
100 c.c. of the salt solution will precipitate.
An advantage of this modification is that an excess of 15 milligrams may be
determined as easily and exactly as 5. In standardising the salt solution,
then, weigh up, say 1.0150 gram of pure silver, dissolve and titrate.
Suppose 13.5 c.c. of "sulphocyanate" required; then these are equivalent to
.0135 gram of silver, (100 c.c. = .1); the silver precipitated by the salt is
1.0150-.0135—i.e., 1.0015 gram, which is the standard.
Application of the Method to Assays for Arsenic.—If silver nitrate be
added to a neutral solution of an arsenate of one of the alkali metals, silver
arsenate (Ag3AsO4), is thrown down as a dark-red precipitate. If, after
adding excess of silver nitrate to insure a complete precipitation, the
arsenate of silver be filtered off, the weight of the arsenic could be
estimated from the weight of silver arsenate formed. But this may be done
much more conveniently by dissolving the precipitate in nitric acid, and
titrating with sulphocyanate; the silver found will be to the arsenic present
as 324 (108×3) is to 75.
The mineral is best treated by the method given in the third paragraph on
page 382; but the solution, after being acidified with nitric acid, should be
made exactly neutral with ammonia. A small excess of silver nitrate should
then be added, and since acid is liberated in the reaction, the liquor must
again be neutralised.[19] The precipitate must then be filtered off, and
washed with distilled water. Then dissolve it in the paper by slowly running
over it 20 c.c. of dilute nitric acid. Wash the filter with distilled water,
collecting with the filtrate in a small flask. Add 2 c.c. of "ferric indicator"
and titrate.
If the sulphocyanate solution be made up with 11 or 12 grams of the
potassium salt to the litre, and be then standardised and diluted, so that for
100 c.c. it shall equal 1.08 gram of silver, (see p. 38), then it will also equal
.25 gram of arsenic (As). Except for ores rich in arsenic, it will be better to
work with a solution one half this strength. The standard as calculated from
made by diluting the ordinary standard solution to such an extent that 100
c.c. after diluting shall be equivalent to 0.1 gram of silver.[18] Calculate the
weight of silver found by "sulphocyanate" and add it to the weight which
100 c.c. of the salt solution will precipitate.
An advantage of this modification is that an excess of 15 milligrams may be
determined as easily and exactly as 5. In standardising the salt solution,
then, weigh up, say 1.0150 gram of pure silver, dissolve and titrate.
Suppose 13.5 c.c. of "sulphocyanate" required; then these are equivalent to
.0135 gram of silver, (100 c.c. = .1); the silver precipitated by the salt is
1.0150-.0135—i.e., 1.0015 gram, which is the standard.
Application of the Method to Assays for Arsenic.—If silver nitrate be
added to a neutral solution of an arsenate of one of the alkali metals, silver
arsenate (Ag3AsO4), is thrown down as a dark-red precipitate. If, after
adding excess of silver nitrate to insure a complete precipitation, the
arsenate of silver be filtered off, the weight of the arsenic could be
estimated from the weight of silver arsenate formed. But this may be done
much more conveniently by dissolving the precipitate in nitric acid, and
titrating with sulphocyanate; the silver found will be to the arsenic present
as 324 (108×3) is to 75.
The mineral is best treated by the method given in the third paragraph on
page 382; but the solution, after being acidified with nitric acid, should be
made exactly neutral with ammonia. A small excess of silver nitrate should
then be added, and since acid is liberated in the reaction, the liquor must
again be neutralised.[19] The precipitate must then be filtered off, and
washed with distilled water. Then dissolve it in the paper by slowly running
over it 20 c.c. of dilute nitric acid. Wash the filter with distilled water,
collecting with the filtrate in a small flask. Add 2 c.c. of "ferric indicator"
and titrate.
If the sulphocyanate solution be made up with 11 or 12 grams of the
potassium salt to the litre, and be then standardised and diluted, so that for
100 c.c. it shall equal 1.08 gram of silver, (see p. 38), then it will also equal
.25 gram of arsenic (As). Except for ores rich in arsenic, it will be better to
work with a solution one half this strength. The standard as calculated from
Page 169
an experiment with pure silver should be checked by another using pure
resublimed white arsenic, As2O3, which contains 75.75 % of the metal. The
quantity of white arsenic taken, .1 or .2 gram, should contain about as much
arsenic as will be present in the assays. It is converted into sodium arsenate
by evaporating to a small bulk with nitric acid and neutralising with soda.
The precipitation and titration of the silver arsenate should be exactly as in
the assays.
The difficulty of the method is in the neutralising; which has to be very
carefully done since silver arsenate is soluble in even faintly acid solutions;
one drop of nitric acid in 100 c.c. of water is enough to produce an
absolutely worthless result; and an excess of acid much less than this is still
very prejudicial. The addition of a little sodium acetate to the solution after
the final neutralising has a good effect.
Arsenic in Mispickel.—Weigh up .250 gram of the finely-powdered ore,
and place in a Berlin crucible about 1-1/4 or 1-1/2 inch in diameter. Treat
with 10 or 12 drops, one drop at a time, of strong nitric acid, warm very
gently, but avoid much heating. Put on a thin layer of nitre, and rather more
than half fill the crucible with a mixture of equal parts of soda and nitre.
Heat quickly in the blow-pipe flame, and when the mass is fused and
effervescing, withdraw and allow to cool. Boil out with water, filter and
wash. Insert a piece of litmus paper and cautiously neutralise with nitric
acid, using ammonia to neutralise any accidental excess of the acid. Add a
gram or so of ammonium nitrate and silver nitrate in excess, neutralise
again with ammonia and add two or three grams of sodium acetate. Filter
off the precipitate, wash and titrate. In the fusion care should be taken to
avoid much effervescence (an excess of the soda mitigates this) and the
operation should be stopped as soon as the whole has entered into fusion.
COLORIMETRIC DETERMINATION.
There is, properly speaking, no colorimetric method, but the following,
which is sometimes used, is based on similar principles. It is useful for the
determination of small quantities of silver in substances which yield clear
solutions with nitric acid.
resublimed white arsenic, As2O3, which contains 75.75 % of the metal. The
quantity of white arsenic taken, .1 or .2 gram, should contain about as much
arsenic as will be present in the assays. It is converted into sodium arsenate
by evaporating to a small bulk with nitric acid and neutralising with soda.
The precipitation and titration of the silver arsenate should be exactly as in
the assays.
The difficulty of the method is in the neutralising; which has to be very
carefully done since silver arsenate is soluble in even faintly acid solutions;
one drop of nitric acid in 100 c.c. of water is enough to produce an
absolutely worthless result; and an excess of acid much less than this is still
very prejudicial. The addition of a little sodium acetate to the solution after
the final neutralising has a good effect.
Arsenic in Mispickel.—Weigh up .250 gram of the finely-powdered ore,
and place in a Berlin crucible about 1-1/4 or 1-1/2 inch in diameter. Treat
with 10 or 12 drops, one drop at a time, of strong nitric acid, warm very
gently, but avoid much heating. Put on a thin layer of nitre, and rather more
than half fill the crucible with a mixture of equal parts of soda and nitre.
Heat quickly in the blow-pipe flame, and when the mass is fused and
effervescing, withdraw and allow to cool. Boil out with water, filter and
wash. Insert a piece of litmus paper and cautiously neutralise with nitric
acid, using ammonia to neutralise any accidental excess of the acid. Add a
gram or so of ammonium nitrate and silver nitrate in excess, neutralise
again with ammonia and add two or three grams of sodium acetate. Filter
off the precipitate, wash and titrate. In the fusion care should be taken to
avoid much effervescence (an excess of the soda mitigates this) and the
operation should be stopped as soon as the whole has entered into fusion.
COLORIMETRIC DETERMINATION.
There is, properly speaking, no colorimetric method, but the following,
which is sometimes used, is based on similar principles. It is useful for the
determination of small quantities of silver in substances which yield clear
solutions with nitric acid.
Page 170
Dissolve a weighed quantity of the substance in nitric acid, and dilute to a
definite bulk. Divide into two equal parts. To one, add a drop or two of
dilute hydrochloric acid, stir and filter. To the other, add a similar amount of
dilute acid, and then to the filtered portion run in from a burette standard
silver nitrate (1 c.c. = 0.5 milligram silver) until the solutions are equally
turbid. Calculate in the usual way.
GOLD.
Gold occurs in nature chiefly as metal. It always contains more or less
silver, and, in alluvial sands, &c., may be associated with platinum and
iridium.
Gold is insoluble in hydrochloric or nitric acid, but is dissolved by aqua
regia or by solutions of iodine, bromine, or chlorine. It is taken up by
mercury, forming an amalgam, from which the mercury may be driven off
by heat.
When gold occurs in particles of any size, it is readily detected by its
appearance, but when finely disseminated through a large quantity of rock,
it is separated and detected by the amalgamation assay—described below—
or by a process of washing somewhat similar to vanning, or by the
following test:—Powder and, if necessary, roast 50 to 100 grams of the ore,
put on it three or four crystals of iodine and enough alcohol to cover it;
allow to stand for half an hour; a piece of filter paper moistened with the
liquid and burnt leaves an ash with a distinctly purple tint if any gold is
present. It is better, however, to filter off the solution, evaporate, and ignite.
Then, either take up with mercury, and ignite the amalgam so as to get a
speck of the metallic gold; or treat with a few drops of aqua regia, and test
the solution with stannous chloride: a purple coloration indicates gold.
AMALGAMATION ASSAY.—This does not attempt to give the total
produce of gold, but rather the quantity which can be extracted on a large
scale; therefore it should imitate as closely as possible the process adopted
in the mine or district for extracting the metal.
Take 2 lbs of the ore in powder and roast; make into a stiff paste with hot
water and rub up for an hour or so with a little mercury. Wash off the sand
definite bulk. Divide into two equal parts. To one, add a drop or two of
dilute hydrochloric acid, stir and filter. To the other, add a similar amount of
dilute acid, and then to the filtered portion run in from a burette standard
silver nitrate (1 c.c. = 0.5 milligram silver) until the solutions are equally
turbid. Calculate in the usual way.
GOLD.
Gold occurs in nature chiefly as metal. It always contains more or less
silver, and, in alluvial sands, &c., may be associated with platinum and
iridium.
Gold is insoluble in hydrochloric or nitric acid, but is dissolved by aqua
regia or by solutions of iodine, bromine, or chlorine. It is taken up by
mercury, forming an amalgam, from which the mercury may be driven off
by heat.
When gold occurs in particles of any size, it is readily detected by its
appearance, but when finely disseminated through a large quantity of rock,
it is separated and detected by the amalgamation assay—described below—
or by a process of washing somewhat similar to vanning, or by the
following test:—Powder and, if necessary, roast 50 to 100 grams of the ore,
put on it three or four crystals of iodine and enough alcohol to cover it;
allow to stand for half an hour; a piece of filter paper moistened with the
liquid and burnt leaves an ash with a distinctly purple tint if any gold is
present. It is better, however, to filter off the solution, evaporate, and ignite.
Then, either take up with mercury, and ignite the amalgam so as to get a
speck of the metallic gold; or treat with a few drops of aqua regia, and test
the solution with stannous chloride: a purple coloration indicates gold.
AMALGAMATION ASSAY.—This does not attempt to give the total
produce of gold, but rather the quantity which can be extracted on a large
scale; therefore it should imitate as closely as possible the process adopted
in the mine or district for extracting the metal.
Take 2 lbs of the ore in powder and roast; make into a stiff paste with hot
water and rub up for an hour or so with a little mercury. Wash off the sand
Page 171
carefully, and collect the amalgam. Drive off the mercury by heat, and
weigh the residual gold. It is best to cupel it with lead before weighing.
In an experiment on a lot of ore which contained 0.189 gram of gold, 0.179
gram was obtained by the above process, equal to about 94-1/2 per cent.
recovered. With ores generally, the yield may be from 80 to 90 per cent. of
the actual gold present.
DRY ASSAY.
The dry assay of gold ores resembles in its main particulars the dry assay
for silver by the crucible method; and for much that is of importance in its
discussion the student is referred to what is written under Silver on pp. 90-
113.
Size of Assay Charges.—Gold ores rarely contain more than a few ounces,
often only a few pennyweights of gold to the ton; consequently, the button
of gold obtainable from such quantities of ore as may be conveniently
worked by assaying methods is often so small as to require more than
ordinary care in its manipulation. One milligram of gold forms a button of
about the size of one of the full-stops on this page, and compared with a
million similar particles of quartz (about four ounces), represents a produce
of a quarter of an ounce to the ton: a proportion such as the assayer is
frequently called on to determine. It is evident, therefore, that a charge of
half an ounce or less of the ore, such as is usual with silver ores, would
demand of the worker both skill and care in the handling of the minute
quantity of gold to be obtained from it. Fortunately the work is simple and
precise, so that in practised hands and with only a 5-gram charge the assay
of a 5-dwt. ore is practicable; with so small a charge, however, the result is
barely perceptible on a sensitive balance: the button of gold should be
measured under a microscope. It follows, therefore, that larger charges of
say 50, 100, or even 200 grams, have an advantage in that they lessen the
strain on the worker's attention, and, except in the case of the poorest
mineral, bring the button of gold within the scope of the balance. On the
other hand, the inconvenience of the larger charges lies in the amount of
fluxes and consequent size of the crucibles required to flux them.
weigh the residual gold. It is best to cupel it with lead before weighing.
In an experiment on a lot of ore which contained 0.189 gram of gold, 0.179
gram was obtained by the above process, equal to about 94-1/2 per cent.
recovered. With ores generally, the yield may be from 80 to 90 per cent. of
the actual gold present.
DRY ASSAY.
The dry assay of gold ores resembles in its main particulars the dry assay
for silver by the crucible method; and for much that is of importance in its
discussion the student is referred to what is written under Silver on pp. 90-
113.
Size of Assay Charges.—Gold ores rarely contain more than a few ounces,
often only a few pennyweights of gold to the ton; consequently, the button
of gold obtainable from such quantities of ore as may be conveniently
worked by assaying methods is often so small as to require more than
ordinary care in its manipulation. One milligram of gold forms a button of
about the size of one of the full-stops on this page, and compared with a
million similar particles of quartz (about four ounces), represents a produce
of a quarter of an ounce to the ton: a proportion such as the assayer is
frequently called on to determine. It is evident, therefore, that a charge of
half an ounce or less of the ore, such as is usual with silver ores, would
demand of the worker both skill and care in the handling of the minute
quantity of gold to be obtained from it. Fortunately the work is simple and
precise, so that in practised hands and with only a 5-gram charge the assay
of a 5-dwt. ore is practicable; with so small a charge, however, the result is
barely perceptible on a sensitive balance: the button of gold should be
measured under a microscope. It follows, therefore, that larger charges of
say 50, 100, or even 200 grams, have an advantage in that they lessen the
strain on the worker's attention, and, except in the case of the poorest
mineral, bring the button of gold within the scope of the balance. On the
other hand, the inconvenience of the larger charges lies in the amount of
fluxes and consequent size of the crucibles required to flux them.
Page 172
Sampling.—A further consideration in favour of the larger charges is the
matter of sampling. In preparing his ore, the student should ask himself
what reasonable expectation he has that the portion he puts in the furnace
will be of average richness. The larger charges are likely to be nearer than
the smaller ones to the average of the parcel of ore from which they are
taken. In explanation of this, let us suppose a large heap of 5-dwt. ore, in
sand of the coarseness of full-stops, and containing all its gold in particles
of 1 milligram, as uniformly distributed as care and labour in the mixing
can accomplish. Such a heap could not possibly occur in practice, but it will
serve for purposes of illustration. Now, one ton of the sand, however taken,
would contain appreciably the same quantity of gold as any other ton. For a
ton would contain about 8000 particles of gold; and even if two separate
tons differed by as much as 100 particles (which they are just likely to do),
this would mean only a difference of 1 or 2 grains to the ton. On the other
hand, two portions of 14 lbs., which should contain on the average 50
particles of gold, are likely enough to differ by 10 particles, and this,
calculated on a ton, means a difference of 1 dwt. It is easy to see that
something like this should be true; for on calculating the 14-lb. lot up to a
ton, the deviation from the average, whatever it may be, is multiplied by
160; whereas, if the ton were made up by adding 14-lb. lot to 14-lb. lot, up
to the full tale, then a large proportion of the errors (some being in excess
and some in defect) would neutralise each other. An average which is
practically true when dealing with thousands, and perhaps sufficiently exact
with hundreds, would be merely misleading when applied to tens and units.
Reasonable safety in sampling, then, is dependent largely on the number of
particles of gold in the charge taken, and the risk of an abnormal result is
less, the larger the charge taken.
By doubling the charge, however, we merely double the number of
particles. Powdering finely is much more effective; for, since the weight of
a particle varies as the cube of the diameter, halving the diameter of the
particles increases their number eight-fold. If, now, we modify our
illustration by assuming the particles to have only one-sixth the diameter of
a full-stop (which would represent a powder of a fineness not unusual in
ores prepared for assaying), we should multiply the number of particles by
200 (6 × 6 × 6 = 216). We should then reasonably expect a 14-lb. parcel of
the powder to give as safe a sample as a ton of the sand would give; and
matter of sampling. In preparing his ore, the student should ask himself
what reasonable expectation he has that the portion he puts in the furnace
will be of average richness. The larger charges are likely to be nearer than
the smaller ones to the average of the parcel of ore from which they are
taken. In explanation of this, let us suppose a large heap of 5-dwt. ore, in
sand of the coarseness of full-stops, and containing all its gold in particles
of 1 milligram, as uniformly distributed as care and labour in the mixing
can accomplish. Such a heap could not possibly occur in practice, but it will
serve for purposes of illustration. Now, one ton of the sand, however taken,
would contain appreciably the same quantity of gold as any other ton. For a
ton would contain about 8000 particles of gold; and even if two separate
tons differed by as much as 100 particles (which they are just likely to do),
this would mean only a difference of 1 or 2 grains to the ton. On the other
hand, two portions of 14 lbs., which should contain on the average 50
particles of gold, are likely enough to differ by 10 particles, and this,
calculated on a ton, means a difference of 1 dwt. It is easy to see that
something like this should be true; for on calculating the 14-lb. lot up to a
ton, the deviation from the average, whatever it may be, is multiplied by
160; whereas, if the ton were made up by adding 14-lb. lot to 14-lb. lot, up
to the full tale, then a large proportion of the errors (some being in excess
and some in defect) would neutralise each other. An average which is
practically true when dealing with thousands, and perhaps sufficiently exact
with hundreds, would be merely misleading when applied to tens and units.
Reasonable safety in sampling, then, is dependent largely on the number of
particles of gold in the charge taken, and the risk of an abnormal result is
less, the larger the charge taken.
By doubling the charge, however, we merely double the number of
particles. Powdering finely is much more effective; for, since the weight of
a particle varies as the cube of the diameter, halving the diameter of the
particles increases their number eight-fold. If, now, we modify our
illustration by assuming the particles to have only one-sixth the diameter of
a full-stop (which would represent a powder of a fineness not unusual in
ores prepared for assaying), we should multiply the number of particles by
200 (6 × 6 × 6 = 216). We should then reasonably expect a 14-lb. parcel of
the powder to give as safe a sample as a ton of the sand would give; and
Page 173
portions of a size fit for crucible work, say 50 or 100 grams, would be as
safe as 10 or 20-lb. samples of the coarser stuff. For example, 60 grams of
such powder would contain, for a 5-dwt. ore, about 100 particles; and in the
majority of cases the error due to sampling would be less than 10 or 12
grains to the ton, and would only occasionally exceed a pennyweight. With
richer ores the actual deviation stated as so much to the ton of ore might be
greater, but it would represent a smaller proportion, stated in percentage of
the gold actually present, and would ultimately fall within the limits of
unavoidable error.
It will be seen that the size of the quartz particles has no direct bearing on
the argument; and, in fact, the coarseness of the quartz only interferes by
preventing the uniform mixing of the sand and by binding together several
particles of gold; in this last case, particles so united must, of course, count
as one larger particle. Now, there are some natural ores in which the gold
particles are all very small; with these fine powdering and mixing yields a
product from which a sample may be safely taken. Then, again, in
"tailings," before or after treatment with cyanide, we have a similar
material, inasmuch as the coarser gold has been removed by previous
amalgamation. With these, it is not unusual to take the portion for assay
without any further powdering, since they are poor in gold, and have
already been stamped and passed through a sieve of say thirty holes to the
inch (linear).
But there are other ores, in lump showing no visible gold, which contain the
gold in all possible degrees of fineness, from say prills of a milligram or so
down to a most impalpable powder. The treatment of these cannot be so
simple and straightforward. Suppose a parcel of 1000 grams (say 2 lbs.) of
such ore in fine powder, containing on an average 1 particle of 1 milligram
(the presence or absence of which makes a difference of .6 dwt. on the ton),
10 others of about .5 milligram (each representing .3 dwt.), and 100 others,
which are too coarse to pass through an 80 sieve, and having an average
weight of .1 milligram (each .06 dwt.), and that the rest of the gold,
equivalent altogether to 2 ounces to the ton, is so finely divided that a
charge of 50 grams may be taken without any considerable risk of its
interfering with the sampling. Then in a 50-gram charge there would be one
chance in twenty of getting the milligram particle, in which case the result
would be 12.35 dwts. too high; on the other hand, if it were not present the
safe as 10 or 20-lb. samples of the coarser stuff. For example, 60 grams of
such powder would contain, for a 5-dwt. ore, about 100 particles; and in the
majority of cases the error due to sampling would be less than 10 or 12
grains to the ton, and would only occasionally exceed a pennyweight. With
richer ores the actual deviation stated as so much to the ton of ore might be
greater, but it would represent a smaller proportion, stated in percentage of
the gold actually present, and would ultimately fall within the limits of
unavoidable error.
It will be seen that the size of the quartz particles has no direct bearing on
the argument; and, in fact, the coarseness of the quartz only interferes by
preventing the uniform mixing of the sand and by binding together several
particles of gold; in this last case, particles so united must, of course, count
as one larger particle. Now, there are some natural ores in which the gold
particles are all very small; with these fine powdering and mixing yields a
product from which a sample may be safely taken. Then, again, in
"tailings," before or after treatment with cyanide, we have a similar
material, inasmuch as the coarser gold has been removed by previous
amalgamation. With these, it is not unusual to take the portion for assay
without any further powdering, since they are poor in gold, and have
already been stamped and passed through a sieve of say thirty holes to the
inch (linear).
But there are other ores, in lump showing no visible gold, which contain the
gold in all possible degrees of fineness, from say prills of a milligram or so
down to a most impalpable powder. The treatment of these cannot be so
simple and straightforward. Suppose a parcel of 1000 grams (say 2 lbs.) of
such ore in fine powder, containing on an average 1 particle of 1 milligram
(the presence or absence of which makes a difference of .6 dwt. on the ton),
10 others of about .5 milligram (each representing .3 dwt.), and 100 others,
which are too coarse to pass through an 80 sieve, and having an average
weight of .1 milligram (each .06 dwt.), and that the rest of the gold,
equivalent altogether to 2 ounces to the ton, is so finely divided that a
charge of 50 grams may be taken without any considerable risk of its
interfering with the sampling. Then in a 50-gram charge there would be one
chance in twenty of getting the milligram particle, in which case the result
would be 12.35 dwts. too high; on the other hand, if it were not present the
Page 174
result would on this account be .65 dwt. too low. Of the ten .5-milligram
particles, it is as likely as not that one will be present, and its presence or
absence would cause an error of 3.3 dwts., more or less. Of the 100
particles of .1 milligram, there would probably be from 3 to 7, instead of 5,
the proper number; this would mean a variation of 2.6 dwts. from the true
proportion. So that the probable result would range about 5 dwts. more or
less than the 2-1/2 ozs., which is the true produce, and there are possibilities
of astounding results. It is true that the majority of the results would be well
within these limits, and now and again the heart of the student would be
gladdened by a beautiful concordance in duplicate assays; nevertheless,
there can be no reasonable expectation of a good assay, and to work in this
way, on a 50-gram charge, would be to court failure. The coarse gold must
ruin the assay.
The difficulty may be met by concentrating the whole of the coarse gold in
a small fraction of the ore, by sifting and making a separate assay of this
fraction. A portion of the ore, of about 1000 grams, is ground to a very fine
powder and passed through an 80 sieve, re-grinding when necessary, until
only 20 or 30 grams is left of the coarser powder. This is mixed with fluxes
and carried through as a separate assay. The sifted portion is thoroughly
mixed, and a portion of it, say 30 or 50 grams, taken for assay. The weights
of the two portions must be known, and care must be taken that nothing is
lost in the powdering. The method of calculating the mean result from the
two assays is shown on page 109. In this way of working there is no
advantage in continuing the grinding until the coarser fraction is reduced to
a gram or so—rather the contrary; and rubbing on until all the gold is sent
through the sieve is to be distinctly avoided. The student must bear in mind
that what he is aiming at is the exclusion of all coarse gold from the portion
of ore of which he is going to take only a fraction.
The question of the smaller sampling of gold ores has been dwelt on at
considerable length, as befits its importance, in order that the student may
be impressed with a sense of its true meaning. Sampling is not a mystery,
nor does the art lie in any subtle manner of division. It is, of course,
absolutely necessary that the stuff to be sampled shall be well mixed, and
the fractions taken, so that each part of the little heap shall contribute its
share to the sample. Moreover, it must be remembered that tossing about is
a poor sort of mixing, and that everything tending to separate the large from
particles, it is as likely as not that one will be present, and its presence or
absence would cause an error of 3.3 dwts., more or less. Of the 100
particles of .1 milligram, there would probably be from 3 to 7, instead of 5,
the proper number; this would mean a variation of 2.6 dwts. from the true
proportion. So that the probable result would range about 5 dwts. more or
less than the 2-1/2 ozs., which is the true produce, and there are possibilities
of astounding results. It is true that the majority of the results would be well
within these limits, and now and again the heart of the student would be
gladdened by a beautiful concordance in duplicate assays; nevertheless,
there can be no reasonable expectation of a good assay, and to work in this
way, on a 50-gram charge, would be to court failure. The coarse gold must
ruin the assay.
The difficulty may be met by concentrating the whole of the coarse gold in
a small fraction of the ore, by sifting and making a separate assay of this
fraction. A portion of the ore, of about 1000 grams, is ground to a very fine
powder and passed through an 80 sieve, re-grinding when necessary, until
only 20 or 30 grams is left of the coarser powder. This is mixed with fluxes
and carried through as a separate assay. The sifted portion is thoroughly
mixed, and a portion of it, say 30 or 50 grams, taken for assay. The weights
of the two portions must be known, and care must be taken that nothing is
lost in the powdering. The method of calculating the mean result from the
two assays is shown on page 109. In this way of working there is no
advantage in continuing the grinding until the coarser fraction is reduced to
a gram or so—rather the contrary; and rubbing on until all the gold is sent
through the sieve is to be distinctly avoided. The student must bear in mind
that what he is aiming at is the exclusion of all coarse gold from the portion
of ore of which he is going to take only a fraction.
The question of the smaller sampling of gold ores has been dwelt on at
considerable length, as befits its importance, in order that the student may
be impressed with a sense of its true meaning. Sampling is not a mystery,
nor does the art lie in any subtle manner of division. It is, of course,
absolutely necessary that the stuff to be sampled shall be well mixed, and
the fractions taken, so that each part of the little heap shall contribute its
share to the sample. Moreover, it must be remembered that tossing about is
a poor sort of mixing, and that everything tending to separate the large from
Page 175
the small, the light from the heavy, or the soft from the hard (as happens in
sifting), must be avoided, or, if unavoidable, must be remedied by
subsequent mixing.
With a well-taken sample, we may rely on a great majority of our results
falling within normal limits of error; but nothing can be more certain than
that, in a moderately large experience we shall get, now and again,
deviations much more considerable. These erratic assays can only be met by
the method of working duplicates, which call attention to the fault by
discordant results. Such faulty assays should be repeated in duplicate, so
that we may rest the decision on three out of four determinations.
The likelihood of two very faulty assays being concordant is remote; but
with very important work, as in selling parcels of ore, even this risk should
be avoided, as concordance in these cases is demanded in the reports of two
or more assayers. The following actual reports on a disputed assay will
illustrate this: (a) 5 ozs. 1 dwt.; (b) 5 ozs. 10 dwts. 12 grains; (c) 5 ozs. 11
dwts.; (d) 5 ozs. 11 dwts. 12 grs. The mean result of several assays, unless
there be some fault in the method, will be very fairly exact; and individual
assays, with an uncertainty of 1 in 20, may, by repetition, have this reduced
to 1 in 100 or less.
Assay Tons, etc.—Having decided on taking a larger or smaller portion, the
exact quantity to be used will be either some round number of grams, such
as 50 or 100, easily calculable into percentage; or it will be that known as
the "Assay Ton" (see page 13) or some simple multiple or fraction of it,
which is easily calculable into ounces. The reports, too, are at least as often
made as ounces in the short ton of 2000 lbs., as on the more orthodox ton of
2240 lbs. Now the short ton is equal to 29,166.6 troy ounces; and the
corresponding "assay ton" is got from it by replacing ounces by milligrams.
The advantage of its use is that if one assay ton of ore has been taken, the
number of milligrams of gold obtained is also the number of ounces of gold
in a ton of the ore, and there is absolutely no calculation. Even if half an
assay ton has been taken the only calculation needed is multiplying the
milligrams by two. On the other hand with a charge of two assay tons the
milligrams need halving. Where weights of this kind (i.e., assay tons) are
not at hand they may be easily extemporised out of buttons of tin or some
suitable metal, and it is better to do this than to array out the grams and its
sifting), must be avoided, or, if unavoidable, must be remedied by
subsequent mixing.
With a well-taken sample, we may rely on a great majority of our results
falling within normal limits of error; but nothing can be more certain than
that, in a moderately large experience we shall get, now and again,
deviations much more considerable. These erratic assays can only be met by
the method of working duplicates, which call attention to the fault by
discordant results. Such faulty assays should be repeated in duplicate, so
that we may rest the decision on three out of four determinations.
The likelihood of two very faulty assays being concordant is remote; but
with very important work, as in selling parcels of ore, even this risk should
be avoided, as concordance in these cases is demanded in the reports of two
or more assayers. The following actual reports on a disputed assay will
illustrate this: (a) 5 ozs. 1 dwt.; (b) 5 ozs. 10 dwts. 12 grains; (c) 5 ozs. 11
dwts.; (d) 5 ozs. 11 dwts. 12 grs. The mean result of several assays, unless
there be some fault in the method, will be very fairly exact; and individual
assays, with an uncertainty of 1 in 20, may, by repetition, have this reduced
to 1 in 100 or less.
Assay Tons, etc.—Having decided on taking a larger or smaller portion, the
exact quantity to be used will be either some round number of grams, such
as 50 or 100, easily calculable into percentage; or it will be that known as
the "Assay Ton" (see page 13) or some simple multiple or fraction of it,
which is easily calculable into ounces. The reports, too, are at least as often
made as ounces in the short ton of 2000 lbs., as on the more orthodox ton of
2240 lbs. Now the short ton is equal to 29,166.6 troy ounces; and the
corresponding "assay ton" is got from it by replacing ounces by milligrams.
The advantage of its use is that if one assay ton of ore has been taken, the
number of milligrams of gold obtained is also the number of ounces of gold
in a ton of the ore, and there is absolutely no calculation. Even if half an
assay ton has been taken the only calculation needed is multiplying the
milligrams by two. On the other hand with a charge of two assay tons the
milligrams need halving. Where weights of this kind (i.e., assay tons) are
not at hand they may be easily extemporised out of buttons of tin or some
suitable metal, and it is better to do this than to array out the grams and its
Page 176
fractions at each weighing. The sets of "assay tons," however, are easily
purchased. As stated on page 13, the assay ton for 2240 lbs. is 32.6667
grams; and for the short ton, 29.1667 grams. If, however, the round number
of grams be used and the result brought by calculation to the produce on
100 grams, the conversion to ounces to the ton may be quickly effected by
the help of the table on page 107. As this table only deals with the ton of
2240 lbs., it is supplemented here by a shortened one dealing only with the
produce of 100 grams and stating the result in ounces troy to the short ton
of 2000 lbs.
Estimation of Small Quantities of Gold.—By the Balance. In estimating
minute quantities of gold there are one or two points, of importance to an
assayer only in this assay, where they will often allow one to avoid the
working of inconveniently large charges. One of these is known as
"weighing by the method of
TABLE FOR CALCULATING OUNCES TO THE SHORT TON FROM
THE YIELD OF GOLD FROM 100 GRAMS OF ORE.
Ounces to the Ounces to the Ounces to the
Milligram. Milligram. Milligram.
Ton. Ton. Ton.
0.01 0.003 0.4 0.117 7.0 2.042
0.02 0.006 0.5 0.145 8.0 2.333
0.03 0.009 0.6 0.175 9.0 2.625
0.04 0.012 0.7 0.204 10.0 2.916
0.05 0.014 0.8 0.233 20.0 5.833
0.06 0.017 0.9 0.262 30.0 8.750
0.07 0.020 1.0 0.292 40.0 11.666
0.08 0.023 2.0 0.583 50.0 14.583
0.09 0.026 3.0 0.875 60.0 17.500
0.10 0.029 4.0 1.167 70.0 20.416
0.20 0.058 5.0 1.458 80.0 23.333
0.30 0.087 6.0 1.750 90.0 26.250
vibrations." Suppose a balance at rest in perfect equilibrium, with the
pointer exactly over the middle point of the scale. Let the scale be a series
of points at equal distances along a horizontal line; then, if a small weight
purchased. As stated on page 13, the assay ton for 2240 lbs. is 32.6667
grams; and for the short ton, 29.1667 grams. If, however, the round number
of grams be used and the result brought by calculation to the produce on
100 grams, the conversion to ounces to the ton may be quickly effected by
the help of the table on page 107. As this table only deals with the ton of
2240 lbs., it is supplemented here by a shortened one dealing only with the
produce of 100 grams and stating the result in ounces troy to the short ton
of 2000 lbs.
Estimation of Small Quantities of Gold.—By the Balance. In estimating
minute quantities of gold there are one or two points, of importance to an
assayer only in this assay, where they will often allow one to avoid the
working of inconveniently large charges. One of these is known as
"weighing by the method of
TABLE FOR CALCULATING OUNCES TO THE SHORT TON FROM
THE YIELD OF GOLD FROM 100 GRAMS OF ORE.
Ounces to the Ounces to the Ounces to the
Milligram. Milligram. Milligram.
Ton. Ton. Ton.
0.01 0.003 0.4 0.117 7.0 2.042
0.02 0.006 0.5 0.145 8.0 2.333
0.03 0.009 0.6 0.175 9.0 2.625
0.04 0.012 0.7 0.204 10.0 2.916
0.05 0.014 0.8 0.233 20.0 5.833
0.06 0.017 0.9 0.262 30.0 8.750
0.07 0.020 1.0 0.292 40.0 11.666
0.08 0.023 2.0 0.583 50.0 14.583
0.09 0.026 3.0 0.875 60.0 17.500
0.10 0.029 4.0 1.167 70.0 20.416
0.20 0.058 5.0 1.458 80.0 23.333
0.30 0.087 6.0 1.750 90.0 26.250
vibrations." Suppose a balance at rest in perfect equilibrium, with the
pointer exactly over the middle point of the scale. Let the scale be a series
of points at equal distances along a horizontal line; then, if a small weight
Page 177
be placed on one pan, the pointer will deviate from its vertical position and
come to rest opposite some definite part of the scale, which will depend
upon the magnitude of the weight added. The law determining this position
is a very simple one; the deviation as measured along the points of the scale
varies directly as the weight added. For example, with an ordinarily
sensitive balance, such as is used for general purposes, one milligram will
move the pointer along, say, three divisions of the scale; then two
milligrams will move it six divisions; half a milligram, one and a half
divisions; and so on. Of course, with a more sensitive balance the
deviations will be greater. Now the point at which the needle comes to rest
is also the middle point about which it vibrates when swinging. For
example, if the needle swings from the third to the seventh division on the
right then [(7+3)/2] it will come to rest on the fifth. In working by this
method the following conventions are useful: Always place the button to be
weighed on the left pan of the balance, the weights on the right; count the
divisions of the scale from the centre to right and left, marking the former +
and the latter -; thus -5 is the fifth division to the left. Then the position of
rest is half the algebraic sum of two readings. For example, let the readings
be 7 to the right and 3 to the left, then (+7-3)/2 = +2. The mean division is
the second division to the right. If the student will place himself in front of
a balance and repeat the following observations and replace the figures here
given by his own, he will have no difficulty in grasping the method. First
determine the bias of the balance; suppose the unloaded balance swings
+1.25 and -1; the bias then is (1.25-1)/2 = +.125 or one-eighth of a division
to the right. Now having put on the button to be weighed let the readings be
+7.5 and +9.25, and (7.5+9.25)/2 = +8.375. Then the effect of the button
has been to move the pointer from +.125 to +8.375, or 8.25 divisions to the
right; we should, therefore, add the weight equivalent of 8.25 divisions to
the weights, whatever they may be on the right hand pan of the balance; if
the divisions were to the left (- divisions) we should subtract. The value of 1
division is easily determined. Suppose the button in the example were a 1
milligram weight, then we should have found that 1 milligram = 8.25
divisions ∴ 1 division = .121 milligram. This method of working adds very
considerably to the power of a balance in distinguishing small quantities.
come to rest opposite some definite part of the scale, which will depend
upon the magnitude of the weight added. The law determining this position
is a very simple one; the deviation as measured along the points of the scale
varies directly as the weight added. For example, with an ordinarily
sensitive balance, such as is used for general purposes, one milligram will
move the pointer along, say, three divisions of the scale; then two
milligrams will move it six divisions; half a milligram, one and a half
divisions; and so on. Of course, with a more sensitive balance the
deviations will be greater. Now the point at which the needle comes to rest
is also the middle point about which it vibrates when swinging. For
example, if the needle swings from the third to the seventh division on the
right then [(7+3)/2] it will come to rest on the fifth. In working by this
method the following conventions are useful: Always place the button to be
weighed on the left pan of the balance, the weights on the right; count the
divisions of the scale from the centre to right and left, marking the former +
and the latter -; thus -5 is the fifth division to the left. Then the position of
rest is half the algebraic sum of two readings. For example, let the readings
be 7 to the right and 3 to the left, then (+7-3)/2 = +2. The mean division is
the second division to the right. If the student will place himself in front of
a balance and repeat the following observations and replace the figures here
given by his own, he will have no difficulty in grasping the method. First
determine the bias of the balance; suppose the unloaded balance swings
+1.25 and -1; the bias then is (1.25-1)/2 = +.125 or one-eighth of a division
to the right. Now having put on the button to be weighed let the readings be
+7.5 and +9.25, and (7.5+9.25)/2 = +8.375. Then the effect of the button
has been to move the pointer from +.125 to +8.375, or 8.25 divisions to the
right; we should, therefore, add the weight equivalent of 8.25 divisions to
the weights, whatever they may be on the right hand pan of the balance; if
the divisions were to the left (- divisions) we should subtract. The value of 1
division is easily determined. Suppose the button in the example were a 1
milligram weight, then we should have found that 1 milligram = 8.25
divisions ∴ 1 division = .121 milligram. This method of working adds very
considerably to the power of a balance in distinguishing small quantities.
Page 178
By the Microscope.—The use of the microscope also is a real advantage in
estimating the weights of minute buttons of gold where there is no undue
risk in sampling, and where an error of say 1 in 20 on the quantity of gold is
tolerable. For ores with copper, lead, zinc, &c., as well as for tailings rather
poor in gold, this leaves a wide field of usefulness. The method is described
on page 440, but the description needs supplementing for those who are not
accustomed to the use of a microscope. The eye-piece of a microscope (fig.
44a, A) unscrews at a, showing a diaphragm at b, which will serve as a
support for an eye-piece micrometer. This last, B, is a scale engraved on
glass, and may be purchased of any optical instrument maker, though it may
be necessary to send the eye-piece to have it properly fitted. When resting
on the diaphragm it is in focus for the upper lens, so that on looking through
the microscope, the scale is clearly seen in whatever position the instrument
may be as regards the object being looked at. Suppose this to be a small
button of gold on a shallow, flat watch-glass, on the stage of the
microscope. Bring the button under the "objective" (i.e., the nose of the
microscope), which should be about a quarter of an inch above the watch-
glass; then looking through the instrument, raise the tube until the button of
gold, or at least some dust on the glass, comes into focus. If the button is
not in the field, rest the thumbs and index fingers, using both hands, on the
estimating the weights of minute buttons of gold where there is no undue
risk in sampling, and where an error of say 1 in 20 on the quantity of gold is
tolerable. For ores with copper, lead, zinc, &c., as well as for tailings rather
poor in gold, this leaves a wide field of usefulness. The method is described
on page 440, but the description needs supplementing for those who are not
accustomed to the use of a microscope. The eye-piece of a microscope (fig.
44a, A) unscrews at a, showing a diaphragm at b, which will serve as a
support for an eye-piece micrometer. This last, B, is a scale engraved on
glass, and may be purchased of any optical instrument maker, though it may
be necessary to send the eye-piece to have it properly fitted. When resting
on the diaphragm it is in focus for the upper lens, so that on looking through
the microscope, the scale is clearly seen in whatever position the instrument
may be as regards the object being looked at. Suppose this to be a small
button of gold on a shallow, flat watch-glass, on the stage of the
microscope. Bring the button under the "objective" (i.e., the nose of the
microscope), which should be about a quarter of an inch above the watch-
glass; then looking through the instrument, raise the tube until the button of
gold, or at least some dust on the glass, comes into focus. If the button is
not in the field, rest the thumbs and index fingers, using both hands, on the
Page 179
edge of the watch-glass, pressing lightly but steadily, and give the glass a
slow, short, sweeping motion; the button will perhaps appear as an ill-
defined blackness, because not quite in focus. Bring this into the centre of
the field. Raise or lower the microscope until the button appears with sharp
outlines. If the scale does not cover the button, rotate the eye-piece; this will
bring the scale into a new position. Since the divisions over the button are
less distinct than the others, it is best to read the latter. Thus, in fig. 44b,
there are 36 divisions on one side of the button, and 35 on the other, making
altogether 71. The whole scale is 80, therefore the diameter of the button is
9 divisions. The value of each division obviously varies with the
magnifying power employed. With most microscopes there is a telescopic
arrangement whereby the tube may be lengthened; if this be done and the
button again brought in focus, it will be seen that, as measured on the scale,
the button is much larger than before. It is evident, therefore, the
micrometer must always be used in the same way. The method given in the
appendix (page 440), for finding the value of the scale when gold buttons
are to be measured is easy and satisfactory. When the button of gold is so
small that there is considerable risk of losing it in transferring to a watch-
glass, it may be measured on the cupel, but for this purpose it must be well
illuminated; this is best done by concentrating light on it with a lens, or with
what comes to the same thing, a clean flask filled with water.
slow, short, sweeping motion; the button will perhaps appear as an ill-
defined blackness, because not quite in focus. Bring this into the centre of
the field. Raise or lower the microscope until the button appears with sharp
outlines. If the scale does not cover the button, rotate the eye-piece; this will
bring the scale into a new position. Since the divisions over the button are
less distinct than the others, it is best to read the latter. Thus, in fig. 44b,
there are 36 divisions on one side of the button, and 35 on the other, making
altogether 71. The whole scale is 80, therefore the diameter of the button is
9 divisions. The value of each division obviously varies with the
magnifying power employed. With most microscopes there is a telescopic
arrangement whereby the tube may be lengthened; if this be done and the
button again brought in focus, it will be seen that, as measured on the scale,
the button is much larger than before. It is evident, therefore, the
micrometer must always be used in the same way. The method given in the
appendix (page 440), for finding the value of the scale when gold buttons
are to be measured is easy and satisfactory. When the button of gold is so
small that there is considerable risk of losing it in transferring to a watch-
glass, it may be measured on the cupel, but for this purpose it must be well
illuminated; this is best done by concentrating light on it with a lens, or with
what comes to the same thing, a clean flask filled with water.
Page 180
Most assayers, however, using a micrometer in this way, would like to
know its absolute value. To do this, a stage micrometer must be purchased.
This is like an ordinary microscope slide (fig. 44a, C), and when looked at
through a microscope it shows (fig. 44c) lines ruled on the glass at distances
of tenths and hundredths of a millimetre, ten of each, so that the full scale is
1.1 mm. In the case illustrated, 60 divisions of the scale in the eye-piece are
just equal to the 1.1 mm., therefore 1 division equals .0183 mm. A cube of
this diameter would contain (.0183×.0183×.0183) .0000061285 cubic mm.
The corresponding sphere is got by multiplying by .5236; this gives
.000003209 cb. mm. The weight of 1 cb. mm. of water is 1 milligram; and,
since gold is 19.2 times as heavy as water (sp. g. = 19.2), the contents in cb.
mm. must be multiplied by 19.2. This gives .0000616 milligram as the
weight of a sphere of gold measuring 1 division.
If every result had to be calculated in this way the method would be very
laborious; but, having the figures for the first division, those of the others
may be calculated by multiplying by the cube of the corresponding number.
Thus, for the third division (3×3×3 = 27), the content of the cube
(.0000061285×27) is .0001655 cb. mm.; the content of the sphere
(.000003209×27) is .0000866 cb. mm.; and the corresponding sphere of
gold (.0000616×27) is .00166 milligram. With the help of a table of cubes
know its absolute value. To do this, a stage micrometer must be purchased.
This is like an ordinary microscope slide (fig. 44a, C), and when looked at
through a microscope it shows (fig. 44c) lines ruled on the glass at distances
of tenths and hundredths of a millimetre, ten of each, so that the full scale is
1.1 mm. In the case illustrated, 60 divisions of the scale in the eye-piece are
just equal to the 1.1 mm., therefore 1 division equals .0183 mm. A cube of
this diameter would contain (.0183×.0183×.0183) .0000061285 cubic mm.
The corresponding sphere is got by multiplying by .5236; this gives
.000003209 cb. mm. The weight of 1 cb. mm. of water is 1 milligram; and,
since gold is 19.2 times as heavy as water (sp. g. = 19.2), the contents in cb.
mm. must be multiplied by 19.2. This gives .0000616 milligram as the
weight of a sphere of gold measuring 1 division.
If every result had to be calculated in this way the method would be very
laborious; but, having the figures for the first division, those of the others
may be calculated by multiplying by the cube of the corresponding number.
Thus, for the third division (3×3×3 = 27), the content of the cube
(.0000061285×27) is .0001655 cb. mm.; the content of the sphere
(.000003209×27) is .0000866 cb. mm.; and the corresponding sphere of
gold (.0000616×27) is .00166 milligram. With the help of a table of cubes
Page 181
the whole calculation for 25 or 30 divisions may be made in half an hour,
and the results preserved in the form of a table will simplify all future work.
Assay Operations.—The actual work of the assay resolves itself into three
operations:—(1) The fusion of the ore and concentration of the "fine metal"
(i.e., gold and silver) in a button of lead; (2) The cupellation of the lead,
whereby a button of fine metal is obtained; and (3) the "parting" of the gold
which separates it from the accompanying silver. The following description
takes the order as here given, but the student, in learning the method, should
first practise cupellation if he has not already done so; next he should
practise the separation of gold from silver, taking known weights of fine
gold (p. 63), varying from .5 or .3 gram down to quite minute quantities,
and not resting satisfied until a sensitive balance can barely distinguish
between the weights of gold taken and found. It may be noted here that if he
has not a flatting mill at his disposal, then for large buttons it is better to
make an alloy with eight or nine parts of silver to one of gold, and attack it
with acid without previous flattening, rather than accept the risk and labour
of beating out a less easily attacked alloy to the necessary thinness with a
hammer. It is only after a sense of security in gold parting has been
acquired, that the attack of an ore can be profitably accomplished, and even
then simple and easy ores should be first taken, passing on to others more
difficult, either because of a more complex mineral composition or a
difficulty in sampling.
Concentration of the fine Metal in Lead.—The best flux for quartz,
which makes up the earthy matter of most gold ores, is soda, and this is best
added as carbonate or bicarbonate. By theory,[20] 50 grams of quartz will
require 88.5 grams of the carbonate, or 140 grams of the bicarbonate, to
form sodium silicate, which is a glassy, easily-fusible substance, making a
good slag. If the bicarbonate is used, and heat is applied gradually, steam
and carbonic acid are given off at a comparatively low temperature, and the
carbonate is left; at a higher temperature (about 800° C., or a cherry-red
heat) the carbonate fuses attacking the quartz, and giving off more carbonic
acid; as the heat increases, and the attack on the quartz (which of itself is
infusible) becomes complete, the whole mass settles down to a liquid
sodium silicate, which is sufficiently fluid to allow the gold and lead to
settle to the bottom. The fluid slag does to a certain extent dissolve some of
the crucible, but not seriously. In a perfect working of this experiment, the
and the results preserved in the form of a table will simplify all future work.
Assay Operations.—The actual work of the assay resolves itself into three
operations:—(1) The fusion of the ore and concentration of the "fine metal"
(i.e., gold and silver) in a button of lead; (2) The cupellation of the lead,
whereby a button of fine metal is obtained; and (3) the "parting" of the gold
which separates it from the accompanying silver. The following description
takes the order as here given, but the student, in learning the method, should
first practise cupellation if he has not already done so; next he should
practise the separation of gold from silver, taking known weights of fine
gold (p. 63), varying from .5 or .3 gram down to quite minute quantities,
and not resting satisfied until a sensitive balance can barely distinguish
between the weights of gold taken and found. It may be noted here that if he
has not a flatting mill at his disposal, then for large buttons it is better to
make an alloy with eight or nine parts of silver to one of gold, and attack it
with acid without previous flattening, rather than accept the risk and labour
of beating out a less easily attacked alloy to the necessary thinness with a
hammer. It is only after a sense of security in gold parting has been
acquired, that the attack of an ore can be profitably accomplished, and even
then simple and easy ores should be first taken, passing on to others more
difficult, either because of a more complex mineral composition or a
difficulty in sampling.
Concentration of the fine Metal in Lead.—The best flux for quartz,
which makes up the earthy matter of most gold ores, is soda, and this is best
added as carbonate or bicarbonate. By theory,[20] 50 grams of quartz will
require 88.5 grams of the carbonate, or 140 grams of the bicarbonate, to
form sodium silicate, which is a glassy, easily-fusible substance, making a
good slag. If the bicarbonate is used, and heat is applied gradually, steam
and carbonic acid are given off at a comparatively low temperature, and the
carbonate is left; at a higher temperature (about 800° C., or a cherry-red
heat) the carbonate fuses attacking the quartz, and giving off more carbonic
acid; as the heat increases, and the attack on the quartz (which of itself is
infusible) becomes complete, the whole mass settles down to a liquid
sodium silicate, which is sufficiently fluid to allow the gold and lead to
settle to the bottom. The fluid slag does to a certain extent dissolve some of
the crucible, but not seriously. In a perfect working of this experiment, the
Page 182
first evolution of gases (steam and carbonic acid) should be gentle, so as to
run no risk of its blowing the fine powder out of the crucible; and the heat
at which the second evolution of carbonic acid is produced should be
maintained until the reaction is completed, so that there may be little or no
formation of gas in the fused mass to cause an effervescence which may
force some of the charge over the edges of the crucible. Of course, in
practice the ideal fusion is not attained, but there is no difficulty in
approaching it closely enough to prevent the charge at any time rising above
the level it reached at first in the crucible, and this should be accomplished.
It is usual with quartzose ores to rely mainly on the action of carbonate of
soda, but not entirely. Litharge is also used; it forms, on fusion with quartz,
a silicate of lead, which is a yellow glass, easily fusible, and more fluid in
the furnace than silicate of soda is. By theory, 50 grams of quartz would
require 186 grams of litharge.[21] The reaction takes place without evolution
of gas, and in its working the only point is to so regulate the heat that the
litharge shall not fuse and drain under the unattacked quartz, leaving it as a
pasty mass on the surface. Now, if in making up a charge for 50 grams of
ore, we took 100 grams of bicarbonate of soda (equivalent to about 63
grams of the carbonate), this being five-sevenths of 140 grams (which by
itself would be sufficient), leaves two-sevenths of the quartz to be fluxed by
other reagents: two-sevenths of 186 grams (say 52 grams) of litharge would
serve for this purpose. But if we used 10 grams of borax, which has a
fluxing action about equal to that of the litharge, then 40 grams of the latter,
or (making an allowance for the quartz being not quite pure) say 35 grams,
will suffice. The fluxes, then, for the 50 grams of ore would be: bicarbonate
of soda 100 grams, litharge 35 grams, and borax 10 grams; we could
decrease any of these, and proportionately increase either or both of the
others, and still rely on getting a fusible slag, which is the whole of the
function of a flux, considered simply as a flux. It should be remembered,
however, that the slag is a bi-silicate or acid slag, and that its acid character
is increased by increasing the proportion of borax.
But in addition to the fluxes there is required about 30 or 40 grams of lead
to collect the silver and gold. This is best added as litharge (say 40 grams)
and flour (4 grams), or charcoal powder (2 grams). See pages 93 and 94.
The full charge, then, would be:
run no risk of its blowing the fine powder out of the crucible; and the heat
at which the second evolution of carbonic acid is produced should be
maintained until the reaction is completed, so that there may be little or no
formation of gas in the fused mass to cause an effervescence which may
force some of the charge over the edges of the crucible. Of course, in
practice the ideal fusion is not attained, but there is no difficulty in
approaching it closely enough to prevent the charge at any time rising above
the level it reached at first in the crucible, and this should be accomplished.
It is usual with quartzose ores to rely mainly on the action of carbonate of
soda, but not entirely. Litharge is also used; it forms, on fusion with quartz,
a silicate of lead, which is a yellow glass, easily fusible, and more fluid in
the furnace than silicate of soda is. By theory, 50 grams of quartz would
require 186 grams of litharge.[21] The reaction takes place without evolution
of gas, and in its working the only point is to so regulate the heat that the
litharge shall not fuse and drain under the unattacked quartz, leaving it as a
pasty mass on the surface. Now, if in making up a charge for 50 grams of
ore, we took 100 grams of bicarbonate of soda (equivalent to about 63
grams of the carbonate), this being five-sevenths of 140 grams (which by
itself would be sufficient), leaves two-sevenths of the quartz to be fluxed by
other reagents: two-sevenths of 186 grams (say 52 grams) of litharge would
serve for this purpose. But if we used 10 grams of borax, which has a
fluxing action about equal to that of the litharge, then 40 grams of the latter,
or (making an allowance for the quartz being not quite pure) say 35 grams,
will suffice. The fluxes, then, for the 50 grams of ore would be: bicarbonate
of soda 100 grams, litharge 35 grams, and borax 10 grams; we could
decrease any of these, and proportionately increase either or both of the
others, and still rely on getting a fusible slag, which is the whole of the
function of a flux, considered simply as a flux. It should be remembered,
however, that the slag is a bi-silicate or acid slag, and that its acid character
is increased by increasing the proportion of borax.
But in addition to the fluxes there is required about 30 or 40 grams of lead
to collect the silver and gold. This is best added as litharge (say 40 grams)
and flour (4 grams), or charcoal powder (2 grams). See pages 93 and 94.
The full charge, then, would be:
Page 183
Ore 50 grams.
Bicarbonate of soda 100 "
Litharge 75 "
Borax 10 "
Flour 4 "
These should be mixed, placed in a suitable crucible (a G Battersea, round,
will do), and heated, at first at a red heat, but finally much hotter, so as to
get a fluid and clean slag. When the charge has been in tranquil fusion for
some little time, take it out and pour it into an iron mould. When cold,
detach the button of lead. The slag should be glassy, all through alike, and
easily separable from the metal. With ordinary ores, this slag may be
considered as free from gold. In an experiment in which 90 milligrams of
gold were added, the full amount was obtained from the lead produced by
the first fusion. But in certain cases, more especially where large amounts
of metallic oxides are present, the slag is not so clean, and with these the
slag should be powdered, mixed with 40 grams of litharge and 4 of flour,
and melted again; it is an advantage to add a small prill of say 2 or 3
milligrams of silver to the charge, as it insures a visible product in the
cupellation. Indeed, this last precaution is a good one to be taken wherever
there is reason to expect very small buttons. It has the further advantage,
that, if the quantity of silver necessary for inquartation is known, the right
quantity may be added here, so as to save a subsequent operation.
Ores containing Oxides of Iron.—Of the metallic oxides likely to be
present in a slag, oxide of iron is the most important. Gold is occasionally
found in a matrix of this substance, and in the assay of "concentrates"
largely made up of pyrites, this oxide will be formed in the preliminary
calcination. Now, the lower oxide of iron (ferrous oxide, FeO) is easy to
deal with; fused borax will dissolve about its own weight of it, and a silicate
of soda (such as makes up the bulk of a slag in a gold assay) will take up at
least half as much. But the higher oxide (ferric oxide, Fe2O3) is more
refractory; even 6 parts of borax yields a poor product, and slags with any
considerable percentage of it are not satisfactory. A student attempting to
recover gold from some hæmatite (in which there was about half an ounce
of the metal), found in the slag nearly a gram of gold, although in the first
fusion the slag appeared perfectly fluid. There is, however, no difficulty in
Bicarbonate of soda 100 "
Litharge 75 "
Borax 10 "
Flour 4 "
These should be mixed, placed in a suitable crucible (a G Battersea, round,
will do), and heated, at first at a red heat, but finally much hotter, so as to
get a fluid and clean slag. When the charge has been in tranquil fusion for
some little time, take it out and pour it into an iron mould. When cold,
detach the button of lead. The slag should be glassy, all through alike, and
easily separable from the metal. With ordinary ores, this slag may be
considered as free from gold. In an experiment in which 90 milligrams of
gold were added, the full amount was obtained from the lead produced by
the first fusion. But in certain cases, more especially where large amounts
of metallic oxides are present, the slag is not so clean, and with these the
slag should be powdered, mixed with 40 grams of litharge and 4 of flour,
and melted again; it is an advantage to add a small prill of say 2 or 3
milligrams of silver to the charge, as it insures a visible product in the
cupellation. Indeed, this last precaution is a good one to be taken wherever
there is reason to expect very small buttons. It has the further advantage,
that, if the quantity of silver necessary for inquartation is known, the right
quantity may be added here, so as to save a subsequent operation.
Ores containing Oxides of Iron.—Of the metallic oxides likely to be
present in a slag, oxide of iron is the most important. Gold is occasionally
found in a matrix of this substance, and in the assay of "concentrates"
largely made up of pyrites, this oxide will be formed in the preliminary
calcination. Now, the lower oxide of iron (ferrous oxide, FeO) is easy to
deal with; fused borax will dissolve about its own weight of it, and a silicate
of soda (such as makes up the bulk of a slag in a gold assay) will take up at
least half as much. But the higher oxide (ferric oxide, Fe2O3) is more
refractory; even 6 parts of borax yields a poor product, and slags with any
considerable percentage of it are not satisfactory. A student attempting to
recover gold from some hæmatite (in which there was about half an ounce
of the metal), found in the slag nearly a gram of gold, although in the first
fusion the slag appeared perfectly fluid. There is, however, no difficulty in
Page 184
getting good slags, even with large quantities of iron. For example, with 50
grams of ferric oxide, 10 of quartz, 30 of borax, 30 of soda,[22] 50 of
litharge, and 7 of flour, the result was quite satisfactory. So, too, was 25 of
quartz, 50 of soda, 50 of litharge, and 7 of flour. It is well, however, in such
cases to have an ample proportion of flux and to aim at a larger button of
lead than usual by increasing the proportion of flour or charcoal (see also
page 91). A charge used on the Randt for roasted "concentrates" (which we
may roughly speak of as quartz and ferric oxide), is one assay ton (about 30
grams) each of ore, soda, and borax, and one and a half assay ton of litharge
and 2 grams of charcoal. Whilst, for the same material, from which most of
the gold has been extracted by "chloridising," 2.5 tons each of ore, borax,
and soda, 4 of litharge, and 4 grams of charcoal are needed. This quantity
requires a large crucible (I Battersea, round). In this the proportion of
silicate of soda and borax counted together is to the oxide of iron as 4 to 1,
on the supposition that the quartz and oxide of iron of the ore are in about
equal quantities; but, in the larger charge especially, much oxide of lead
would also remain as a flux.
Ores containing Sulphides.—In assaying ores containing a large
proportion of pyrites or mispickel, or both, the best plan is to take a portion
and calcine so as to convert it into a product of the kind just considered. The
weighed portion of ore should be placed in a clean crucible and be heated to
incipient redness: with pyrites the first effect is to drive off about half the
sulphur as vapour which burns as flame over the ore. At this stage care
should be taken that there is no great increase of temperature, otherwise
there may be more or less fusion, which would spoil the operation. When
the sulphur flame ceases the solid sulphide of iron burns with visible
incandescence and the charge should now be stirred with a flattened iron
rod so as to expose fresh portions to the air. The top of the furnace must be
open, so that air may have free access to the crucible. When stirring is no
longer followed by visible burning the heat may be raised to full redness.
The crucible is then lifted out (the stirrer still resting in it) and if the charge
gives off no odour of burning sulphur it is shaken out into an iron mortar
and mixed with the fluxes, taking care to clean the stirrer in the mixture.
The charge is then replaced in the crucible in which the roasting was done
and fused in the furnace. The resulting button of lead is cupelled for fine
metal. Ores rich in sulphides requiring this treatment are frequently
grams of ferric oxide, 10 of quartz, 30 of borax, 30 of soda,[22] 50 of
litharge, and 7 of flour, the result was quite satisfactory. So, too, was 25 of
quartz, 50 of soda, 50 of litharge, and 7 of flour. It is well, however, in such
cases to have an ample proportion of flux and to aim at a larger button of
lead than usual by increasing the proportion of flour or charcoal (see also
page 91). A charge used on the Randt for roasted "concentrates" (which we
may roughly speak of as quartz and ferric oxide), is one assay ton (about 30
grams) each of ore, soda, and borax, and one and a half assay ton of litharge
and 2 grams of charcoal. Whilst, for the same material, from which most of
the gold has been extracted by "chloridising," 2.5 tons each of ore, borax,
and soda, 4 of litharge, and 4 grams of charcoal are needed. This quantity
requires a large crucible (I Battersea, round). In this the proportion of
silicate of soda and borax counted together is to the oxide of iron as 4 to 1,
on the supposition that the quartz and oxide of iron of the ore are in about
equal quantities; but, in the larger charge especially, much oxide of lead
would also remain as a flux.
Ores containing Sulphides.—In assaying ores containing a large
proportion of pyrites or mispickel, or both, the best plan is to take a portion
and calcine so as to convert it into a product of the kind just considered. The
weighed portion of ore should be placed in a clean crucible and be heated to
incipient redness: with pyrites the first effect is to drive off about half the
sulphur as vapour which burns as flame over the ore. At this stage care
should be taken that there is no great increase of temperature, otherwise
there may be more or less fusion, which would spoil the operation. When
the sulphur flame ceases the solid sulphide of iron burns with visible
incandescence and the charge should now be stirred with a flattened iron
rod so as to expose fresh portions to the air. The top of the furnace must be
open, so that air may have free access to the crucible. When stirring is no
longer followed by visible burning the heat may be raised to full redness.
The crucible is then lifted out (the stirrer still resting in it) and if the charge
gives off no odour of burning sulphur it is shaken out into an iron mortar
and mixed with the fluxes, taking care to clean the stirrer in the mixture.
The charge is then replaced in the crucible in which the roasting was done
and fused in the furnace. The resulting button of lead is cupelled for fine
metal. Ores rich in sulphides requiring this treatment are frequently
Page 185
"concentrates." For their assay take 1 assay ton (30 grams), calcine and mix
with an equal weight of soda and of borax (30 grams each), and half as
much again of litharge (1.5 tons or 45 grams), and with 2 grams of charcoal
or 5 grams of flour.
Where the sulphides are present in smaller proportion (10 per cent. or less),
they may be taken as serving the purpose of flour or charcoal (see page 95);
the sulphur and iron are oxidised at the expense of the litharge with a
consequent separation of lead as metal. If the proportion of sulphides is not
sufficient to give a large enough button of lead, some charcoal or flour
should be added. On the other hand, if they are in small excess and give a
button of lead somewhat sulphury, i.e., hard and brittle, it may be remedied
by the judicious addition of nitre; this last reagent, however, should not be
used in large quantity. A plan much used to prevent sulphury buttons is to
insert an iron rod or a nail in the charge in the crucible; the iron takes the
sulphur forming sulphide of iron which in moderate quantity does not form
a separate layer of matte but dissolves in the slag. A slag formed of 50
grams of quartz, 100 soda, and some borax, may take up in this way some
10 or 12 grams of sulphide of iron. If, however, an ore gives a layer of
matte or speise, it is best to repeat the assay by the method of calcining
before fusion.
Cyanide Charges, etc.—In assaying the "tailings" which are to be treated
in a cyaniding plant the following charge is used:
Tailings 3 assay tons or 100grams.
Litharge 4.5 " 150 "
Soda 4.5 " 150 "
Borax .75 " 25 "
The sand is assayed without any further crushing and the assay is made in
duplicate.
The residues after treatment with cyanide, differing from the tailings merely
in being poorer in gold because of the extraction by the solution of cyanide,
are run down with the same fluxes in the same relative proportions. But
four charges of 2.5 assay tons (say 75 grams) are worked, and two of the
resulting buttons are scorified together and then cupelled, etc., so as to give
with an equal weight of soda and of borax (30 grams each), and half as
much again of litharge (1.5 tons or 45 grams), and with 2 grams of charcoal
or 5 grams of flour.
Where the sulphides are present in smaller proportion (10 per cent. or less),
they may be taken as serving the purpose of flour or charcoal (see page 95);
the sulphur and iron are oxidised at the expense of the litharge with a
consequent separation of lead as metal. If the proportion of sulphides is not
sufficient to give a large enough button of lead, some charcoal or flour
should be added. On the other hand, if they are in small excess and give a
button of lead somewhat sulphury, i.e., hard and brittle, it may be remedied
by the judicious addition of nitre; this last reagent, however, should not be
used in large quantity. A plan much used to prevent sulphury buttons is to
insert an iron rod or a nail in the charge in the crucible; the iron takes the
sulphur forming sulphide of iron which in moderate quantity does not form
a separate layer of matte but dissolves in the slag. A slag formed of 50
grams of quartz, 100 soda, and some borax, may take up in this way some
10 or 12 grams of sulphide of iron. If, however, an ore gives a layer of
matte or speise, it is best to repeat the assay by the method of calcining
before fusion.
Cyanide Charges, etc.—In assaying the "tailings" which are to be treated
in a cyaniding plant the following charge is used:
Tailings 3 assay tons or 100grams.
Litharge 4.5 " 150 "
Soda 4.5 " 150 "
Borax .75 " 25 "
The sand is assayed without any further crushing and the assay is made in
duplicate.
The residues after treatment with cyanide, differing from the tailings merely
in being poorer in gold because of the extraction by the solution of cyanide,
are run down with the same fluxes in the same relative proportions. But
four charges of 2.5 assay tons (say 75 grams) are worked, and two of the
resulting buttons are scorified together and then cupelled, etc., so as to give
Page 186
duplicate assays on charges of 5 assay tons. This is one of the cases in
which it is desirable to add a small portion of silver before cupelling.
In assaying the "cyanide liquors" for gold, 2 assay tons of the liquor are
measured out (58.3 c.c. for the ton of 2000 lbs., 65.3 c.c. for the other) and
are evaporated to dryness in a lead dish weighing about 35 grams. Such a
dish is easily extemporised out of a piece of lead foil, if the ordinary vessel
is not at hand; but care must be taken that the lead is free from gold. The
dish with the dried residue is then scorified and the resulting button of lead
is cupelled.
In some cases the fusion of the ore may be replaced by a treatment with
solution of cyanide of potassium and the gold recovered from the solution
in the way just described. For this purpose the ore should be in not too fine
powder, otherwise there will be great difficulty in filtering; a sand which
will pass a 30 sieve and having no large proportion of very fine stuff will
do. Not less than 200 grams should be taken; and as an extraction apparatus
which it is desirable to add a small portion of silver before cupelling.
In assaying the "cyanide liquors" for gold, 2 assay tons of the liquor are
measured out (58.3 c.c. for the ton of 2000 lbs., 65.3 c.c. for the other) and
are evaporated to dryness in a lead dish weighing about 35 grams. Such a
dish is easily extemporised out of a piece of lead foil, if the ordinary vessel
is not at hand; but care must be taken that the lead is free from gold. The
dish with the dried residue is then scorified and the resulting button of lead
is cupelled.
In some cases the fusion of the ore may be replaced by a treatment with
solution of cyanide of potassium and the gold recovered from the solution
in the way just described. For this purpose the ore should be in not too fine
powder, otherwise there will be great difficulty in filtering; a sand which
will pass a 30 sieve and having no large proportion of very fine stuff will
do. Not less than 200 grams should be taken; and as an extraction apparatus
Page 187
a bell jar capable of holding half as much again may be used. Such a jar
may be extemporised by cutting off the bottom of a bottle by leading a
crack around it with a red hot poker; or a lamp chimney will serve the
purpose. The smaller mouth of the jar is closed by a perforated cork
provided with a clipped tube after the manner of a burette (see fig. 44d). In
the jar, just over the cork, put a plug of loose asbestos or glass wool, or a
piece of sponge to act as a filter; a layer of broken glass, coarse at the
bottom and fine at the top, will serve the same purpose. On this, place the
charge of ore to be extracted. Prepare a solution of cyanide of potassium in
water, with 5 or 10 grams of the salt to the litre. It may be that the whole
point of the assay depends on the solution being of a definite strength; as,
for example, where the relative efficiency of solutions of different strengths
is being determined, when it will be best to estimate the quantity of cyanide
of potassium in the dilute solution by the method given at the end of this
article (page 160). Pour the cyanide solution on to the ore, letting the first
portions to come through run into the beaker, but as soon as the ore is
thoroughly wetted close the clip and allow to stand for several hours. Then,
opening the clip, run through more cyanide solution and then water, so as to
wash the gold-carrying liquor thoroughly into the beaker. It is no matter if
the liquor is a little bit turbid; transfer it to a lead dish, evaporate, scorify,
and cupel in the usual fashion.
The assay of gold-zinc slimes, which is the precipitate formed by zinc
acting on cyanide solutions of gold, may be made by wrapping 2 or 3 grams
in 40 grams of sheet lead and scorifying, cupelling, &c. The amount of
impurity in the stuff varies greatly; it is usually calcined and mixed
thoroughly with soda 40 per cent., borax 30 per cent., and sand 10 per cent.,
and melted in graphite pots. The buttons of bullion obtained are afterwards
remelted with borax and run into bars, the fineness of which varies from
600 to 830 thousandths. The bars are sampled by chipping off diagonally
opposite corners: or better, by drilling, the drillings being freed from pieces
of steel with the help of a magnet.
Cupellation.[23]—The cupellation of lead for gold differs very little from
that of lead carrying silver. When the gold is accompanied by a larger
proportion of silver, and both have to be determined, the cupellation must
be conducted exactly as in a silver assay, the usual precautions being taken
to moderate the temperature so as to lessen the cupellation loss and to
may be extemporised by cutting off the bottom of a bottle by leading a
crack around it with a red hot poker; or a lamp chimney will serve the
purpose. The smaller mouth of the jar is closed by a perforated cork
provided with a clipped tube after the manner of a burette (see fig. 44d). In
the jar, just over the cork, put a plug of loose asbestos or glass wool, or a
piece of sponge to act as a filter; a layer of broken glass, coarse at the
bottom and fine at the top, will serve the same purpose. On this, place the
charge of ore to be extracted. Prepare a solution of cyanide of potassium in
water, with 5 or 10 grams of the salt to the litre. It may be that the whole
point of the assay depends on the solution being of a definite strength; as,
for example, where the relative efficiency of solutions of different strengths
is being determined, when it will be best to estimate the quantity of cyanide
of potassium in the dilute solution by the method given at the end of this
article (page 160). Pour the cyanide solution on to the ore, letting the first
portions to come through run into the beaker, but as soon as the ore is
thoroughly wetted close the clip and allow to stand for several hours. Then,
opening the clip, run through more cyanide solution and then water, so as to
wash the gold-carrying liquor thoroughly into the beaker. It is no matter if
the liquor is a little bit turbid; transfer it to a lead dish, evaporate, scorify,
and cupel in the usual fashion.
The assay of gold-zinc slimes, which is the precipitate formed by zinc
acting on cyanide solutions of gold, may be made by wrapping 2 or 3 grams
in 40 grams of sheet lead and scorifying, cupelling, &c. The amount of
impurity in the stuff varies greatly; it is usually calcined and mixed
thoroughly with soda 40 per cent., borax 30 per cent., and sand 10 per cent.,
and melted in graphite pots. The buttons of bullion obtained are afterwards
remelted with borax and run into bars, the fineness of which varies from
600 to 830 thousandths. The bars are sampled by chipping off diagonally
opposite corners: or better, by drilling, the drillings being freed from pieces
of steel with the help of a magnet.
Cupellation.[23]—The cupellation of lead for gold differs very little from
that of lead carrying silver. When the gold is accompanied by a larger
proportion of silver, and both have to be determined, the cupellation must
be conducted exactly as in a silver assay, the usual precautions being taken
to moderate the temperature so as to lessen the cupellation loss and to
Page 188
promote a slow and undisturbed solidification in order to avoid spirting. If,
however, the gold predominates the finish should be effected at a higher
heat, as the melting-point of gold is 100° higher than that of silver. The bad
effect of a higher temperature in increasing the cupellation loss need hardly
be considered in the case of such small buttons of gold as are obtained in
assaying gold ores, as any loss there may be is hardly appreciable by the
balance. With larger quantities of gold, however (as in assaying gold
bullion), this loss becomes important; and it is therefore necessary to very
carefully regulate the temperature of the muffle so as to minimise the loss.
The cupels are made of well-burnt bone-ash, of the fineness of coarse
wheat flour, moistened with one-twelfth its weight of water and compressed
into shape in suitable moulds. The moulds sold for this purpose are often of
unsuitable shape. Since lead has a specific gravity of over 11, a cup to hold
from 15 to 25 grams of molten lead need not have a capacity of more than
about 2 c.c. A hollow about 1 inch across and 1/4 inch deep is sufficient;
and the body of the cupel to absorb this weight of lead should itself weigh
from 20 to 25 grams. The button of lead in a gold assay may be twice as
heavy as this. For these larger buttons a hollow 1-1/3 inch across and 1/3
inch deep will be sufficient. If these larger cupels are not at hand the larger
buttons will have to be reduced in size by a scorification before cupelling.
In some cases this preliminary scorification is advantageous or even
necessary: this may be because the lead is hard and impure, or it may be
that a very small button of gold is expected. In the latter case it is best to
scorify the lead down to something less than 1 gram, and to perform the
cupellation on a specially prepared small fine cupel. These small cupels are
best made by grinding the unsaturated portion of a used cupel to a fine
powder, and compressing the dry powder into a small Berlin crucible or
scorifier; the face should be made quite smooth by pressure from a pestle.
On such cupels a small speck of gold (less than .01 milligram) will be left
in a good shape and easily visible; but the cupel must be withdrawn from
the muffle as soon as the cupellation is finished to make sure of always
getting the button in good condition. In places, such as Mints, where large
numbers of bullion assays are regularly made a special form of cupel is
used so that not less than six dozen assays may all be cupelled at the same
time in a muffle of ordinary size. These cupels are square blocks, a little
less than 2 inches across, and a little more than three quarters of an inch
however, the gold predominates the finish should be effected at a higher
heat, as the melting-point of gold is 100° higher than that of silver. The bad
effect of a higher temperature in increasing the cupellation loss need hardly
be considered in the case of such small buttons of gold as are obtained in
assaying gold ores, as any loss there may be is hardly appreciable by the
balance. With larger quantities of gold, however (as in assaying gold
bullion), this loss becomes important; and it is therefore necessary to very
carefully regulate the temperature of the muffle so as to minimise the loss.
The cupels are made of well-burnt bone-ash, of the fineness of coarse
wheat flour, moistened with one-twelfth its weight of water and compressed
into shape in suitable moulds. The moulds sold for this purpose are often of
unsuitable shape. Since lead has a specific gravity of over 11, a cup to hold
from 15 to 25 grams of molten lead need not have a capacity of more than
about 2 c.c. A hollow about 1 inch across and 1/4 inch deep is sufficient;
and the body of the cupel to absorb this weight of lead should itself weigh
from 20 to 25 grams. The button of lead in a gold assay may be twice as
heavy as this. For these larger buttons a hollow 1-1/3 inch across and 1/3
inch deep will be sufficient. If these larger cupels are not at hand the larger
buttons will have to be reduced in size by a scorification before cupelling.
In some cases this preliminary scorification is advantageous or even
necessary: this may be because the lead is hard and impure, or it may be
that a very small button of gold is expected. In the latter case it is best to
scorify the lead down to something less than 1 gram, and to perform the
cupellation on a specially prepared small fine cupel. These small cupels are
best made by grinding the unsaturated portion of a used cupel to a fine
powder, and compressing the dry powder into a small Berlin crucible or
scorifier; the face should be made quite smooth by pressure from a pestle.
On such cupels a small speck of gold (less than .01 milligram) will be left
in a good shape and easily visible; but the cupel must be withdrawn from
the muffle as soon as the cupellation is finished to make sure of always
getting the button in good condition. In places, such as Mints, where large
numbers of bullion assays are regularly made a special form of cupel is
used so that not less than six dozen assays may all be cupelled at the same
time in a muffle of ordinary size. These cupels are square blocks, a little
less than 2 inches across, and a little more than three quarters of an inch
Page 189
deep. Each block carries four hollows of about .7 inch across and .3 inch
deep. A muffle, on a floor space of 6 inches by 12, would take 3 of these
blocks abreast and 6 deep, and thus provide the means for 72 assays.[24]
Cupels made with wet bone-ash should be slowly dried; and if in the muffle
they can be slowly brought to an orange-red heat it is all the better. Under
no circumstances must the lead be placed on the cupel before the latter has
been so thoroughly heated that it can no longer give off steam or gas of any
kind. For this gas bubbling through the molten metal spatters it, thus
spoiling one assay and throwing doubt on all the rest. Again, the risk of
freezing at the start is much greater with a cupel which has not been
properly heated.
The best plan is to do all the cupellations in batches. After the muffle has
cooled down for the withdrawal of the last batch, and the old cupels have
been taken out, the new cupels for the next batch should be put in their
place. The furnace should then be stoked and made ready for the next
cupellations; by the time the furnace is ready the cupels will be ready also.
There should be no unnecessary handling of the cupels once they have been
placed in the muffle.
The cupellation temperature for gold is an orange-red heat or perhaps a
little hotter. Beginners, who are apt to overheat their furnace, should avoid a
heat which can properly be called yellow. Dr. T.K. Rose[25] has determined
the temperature of a muffle during the cupellation of gold-silver alloys at
the Royal Mint. In one muffle the temperature ranged from 1065° to 1095°
C.; the lower temperature was of course in the front of the muffle. In
another it ranged from 1022° to 1062°, and here the muffle appeared to the
eye "decidedly cooler than usual." The alloy left after cupelling was made
up of 1 part of gold to 2-1/2 parts of silver, and was fused at 952°; hence the
usual temperature of cupellation was, say, 120° or 130° above the melting-
point of the residual metal. To obtain some real knowledge as to the
meaning of these figures, the student should prepare pointed pieces of the
following metals: silver, which melts at 945°; gold, which melts at 1035°;
and an alloy, half silver, half gold, which melts at 990°. These should be
placed on clean cupels in a muffle almost entirely closed; the temperature
should be very slowly raised, and the appearance of the muffle when each
metal begins to melt should be carefully noted. The cupelling temperature
deep. A muffle, on a floor space of 6 inches by 12, would take 3 of these
blocks abreast and 6 deep, and thus provide the means for 72 assays.[24]
Cupels made with wet bone-ash should be slowly dried; and if in the muffle
they can be slowly brought to an orange-red heat it is all the better. Under
no circumstances must the lead be placed on the cupel before the latter has
been so thoroughly heated that it can no longer give off steam or gas of any
kind. For this gas bubbling through the molten metal spatters it, thus
spoiling one assay and throwing doubt on all the rest. Again, the risk of
freezing at the start is much greater with a cupel which has not been
properly heated.
The best plan is to do all the cupellations in batches. After the muffle has
cooled down for the withdrawal of the last batch, and the old cupels have
been taken out, the new cupels for the next batch should be put in their
place. The furnace should then be stoked and made ready for the next
cupellations; by the time the furnace is ready the cupels will be ready also.
There should be no unnecessary handling of the cupels once they have been
placed in the muffle.
The cupellation temperature for gold is an orange-red heat or perhaps a
little hotter. Beginners, who are apt to overheat their furnace, should avoid a
heat which can properly be called yellow. Dr. T.K. Rose[25] has determined
the temperature of a muffle during the cupellation of gold-silver alloys at
the Royal Mint. In one muffle the temperature ranged from 1065° to 1095°
C.; the lower temperature was of course in the front of the muffle. In
another it ranged from 1022° to 1062°, and here the muffle appeared to the
eye "decidedly cooler than usual." The alloy left after cupelling was made
up of 1 part of gold to 2-1/2 parts of silver, and was fused at 952°; hence the
usual temperature of cupellation was, say, 120° or 130° above the melting-
point of the residual metal. To obtain some real knowledge as to the
meaning of these figures, the student should prepare pointed pieces of the
following metals: silver, which melts at 945°; gold, which melts at 1035°;
and an alloy, half silver, half gold, which melts at 990°. These should be
placed on clean cupels in a muffle almost entirely closed; the temperature
should be very slowly raised, and the appearance of the muffle when each
metal begins to melt should be carefully noted. The cupelling temperature
Page 190
in Dr. Rose's experiment was as much above the melting-point of gold as
this is above that of the silver-gold alloy. The finish of the cupellation of
gold or gold-silver alloys is practically the same as with pure silver; there is
the same thinning out of the litharge into a luminous film which becomes
iridescent before the brightening. But the danger of spirting decreases as the
proportion of gold becomes greater, and disappears when the gold is much
over 30 per cent. Nevertheless it is well to let such buttons become solid
undisturbed and protected from draughts in the body of the muffle. This
means closing the muffle and allowing the furnace to cool down somewhat
before withdrawing the cupels. Buttons solidified in this way are more
malleable than when they are withdrawn promptly on the finish of the
cupellation. This is important with large buttons, as in a bullion assay. On
the other hand, very small buttons, especially such as have to be measured
rather than weighed, should be withdrawn as soon as the luminous film has
disappeared. For when this is done the button can be loosened from the
cupel by merely touching it with the point of a pin, and is then safely and
easily transferred to a watch glass by touching it with the head of a pin
which has been moistened. It adheres to this, and if the pin is not too wet
comes off at once on touching the glass, or in any case will do so on gentle
warming.
Molten gold, with little or no silver, has a peculiar colour which is easy to
recognise; it is more globular than a button of silver of the same size would
be, and it shows less adhesion to the cupel. Just after becoming solid it
glows beautifully, and this is so marked that it is a valuable help in finding
the position of a button when it is more than ordinarily minute.
If the button left from cupellation is yellow it is at least half gold, and a
rough guess as to the proportion of gold may be made from its yellowness;
the rest of the metal is generally silver. The presence of platinum or one of
the platinum group of metals makes the surface of the button dull and
crystalline. The native alloy of osmium and iridium does not alloy with
gold, however, but falls to the bottom of the molten metal. It shows itself in
the subsequent parting as a black spot or streak on the under surface.
The buttons are removed from the cupel with a pair of pliers and then
brushed to remove adherent litharge and bone-ash. Some assayers advise
cleaning by dipping in warm dilute hydrochloric acid followed by washing
this is above that of the silver-gold alloy. The finish of the cupellation of
gold or gold-silver alloys is practically the same as with pure silver; there is
the same thinning out of the litharge into a luminous film which becomes
iridescent before the brightening. But the danger of spirting decreases as the
proportion of gold becomes greater, and disappears when the gold is much
over 30 per cent. Nevertheless it is well to let such buttons become solid
undisturbed and protected from draughts in the body of the muffle. This
means closing the muffle and allowing the furnace to cool down somewhat
before withdrawing the cupels. Buttons solidified in this way are more
malleable than when they are withdrawn promptly on the finish of the
cupellation. This is important with large buttons, as in a bullion assay. On
the other hand, very small buttons, especially such as have to be measured
rather than weighed, should be withdrawn as soon as the luminous film has
disappeared. For when this is done the button can be loosened from the
cupel by merely touching it with the point of a pin, and is then safely and
easily transferred to a watch glass by touching it with the head of a pin
which has been moistened. It adheres to this, and if the pin is not too wet
comes off at once on touching the glass, or in any case will do so on gentle
warming.
Molten gold, with little or no silver, has a peculiar colour which is easy to
recognise; it is more globular than a button of silver of the same size would
be, and it shows less adhesion to the cupel. Just after becoming solid it
glows beautifully, and this is so marked that it is a valuable help in finding
the position of a button when it is more than ordinarily minute.
If the button left from cupellation is yellow it is at least half gold, and a
rough guess as to the proportion of gold may be made from its yellowness;
the rest of the metal is generally silver. The presence of platinum or one of
the platinum group of metals makes the surface of the button dull and
crystalline. The native alloy of osmium and iridium does not alloy with
gold, however, but falls to the bottom of the molten metal. It shows itself in
the subsequent parting as a black spot or streak on the under surface.
The buttons are removed from the cupel with a pair of pliers and then
brushed to remove adherent litharge and bone-ash. Some assayers advise
cleaning by dipping in warm dilute hydrochloric acid followed by washing
Page 191
in water and drying. The button is next weighed. When the quantity of
silver obtained is not required to be known the weighing may sometimes be
omitted. The next operation in either case is parting either with or without a
previous inquartation.
The loss of gold in cupellation is by no means always inconsiderable. In
three cupellations of 1 gram of gold with 20 grams of lead made purposely
at a very high temperature the cupel absorbed 6.04, 6.20, and 6.45
milligrams of gold. Hence at a high temperature there may easily be a loss
of more than half a per cent. of the gold. In ten cupellations with the same
quantities of gold and lead, but at an ordinary temperature, the gold
recovered from the cupels varied from 1.37 to 1.92 milligrams, and gave an
average of 1.59 milligrams. In round numbers the cupellation loss of pure
gold is .15 per cent.
But if the gold be alloyed with silver the loss is diminished, as is shown by
the following experiments. Gold, .3 gram, was cupelled with 10 grams of
lead and varying amounts of silver, and the cupels were assayed for gold
with the following results:
Silver in the alloy .3 gram .6 gram .9 gram
Gold in the cupel .47 milligram .32 milligram .17 milligram
These, calculated on the .3 gram of gold, give the loss as .157, .107 and
.057 per cent. respectively. The effect of copper, on the other hand, is to
increase the cupellation loss, which, silver being absent, may from this
cause rise to .3 per cent., even when the temperature is not excessive.
In the ordinary assay of gold-copper alloys a constant weight of the alloy is
always taken; hence as the weight of copper in a cupel charge increases, the
weight of gold decreases. The silver, on the other hand, is always very
nearly two and a half times as much as the gold, whatever its quantity may
be. But the cupellation loss is smaller with less gold and greater with more
copper, and it so happens in these assays that these two opposites nearly
neutralise one another. Mr. W.F. Lowe[26] found the gold recoverable from
the cupels on which 20 grains of gold bullion had been treated varied only
between .014 and .015 grain (i.e. from .07 to .075 per cent. of the bullion
treated), although the quality of the bullion varied from 9 to 22 carat.[27]
silver obtained is not required to be known the weighing may sometimes be
omitted. The next operation in either case is parting either with or without a
previous inquartation.
The loss of gold in cupellation is by no means always inconsiderable. In
three cupellations of 1 gram of gold with 20 grams of lead made purposely
at a very high temperature the cupel absorbed 6.04, 6.20, and 6.45
milligrams of gold. Hence at a high temperature there may easily be a loss
of more than half a per cent. of the gold. In ten cupellations with the same
quantities of gold and lead, but at an ordinary temperature, the gold
recovered from the cupels varied from 1.37 to 1.92 milligrams, and gave an
average of 1.59 milligrams. In round numbers the cupellation loss of pure
gold is .15 per cent.
But if the gold be alloyed with silver the loss is diminished, as is shown by
the following experiments. Gold, .3 gram, was cupelled with 10 grams of
lead and varying amounts of silver, and the cupels were assayed for gold
with the following results:
Silver in the alloy .3 gram .6 gram .9 gram
Gold in the cupel .47 milligram .32 milligram .17 milligram
These, calculated on the .3 gram of gold, give the loss as .157, .107 and
.057 per cent. respectively. The effect of copper, on the other hand, is to
increase the cupellation loss, which, silver being absent, may from this
cause rise to .3 per cent., even when the temperature is not excessive.
In the ordinary assay of gold-copper alloys a constant weight of the alloy is
always taken; hence as the weight of copper in a cupel charge increases, the
weight of gold decreases. The silver, on the other hand, is always very
nearly two and a half times as much as the gold, whatever its quantity may
be. But the cupellation loss is smaller with less gold and greater with more
copper, and it so happens in these assays that these two opposites nearly
neutralise one another. Mr. W.F. Lowe[26] found the gold recoverable from
the cupels on which 20 grains of gold bullion had been treated varied only
between .014 and .015 grain (i.e. from .07 to .075 per cent. of the bullion
treated), although the quality of the bullion varied from 9 to 22 carat.[27]
Page 192
But in the poorest bullion there was only 7.5 grains of pure gold, while in
the richest there were 18.3 grains; yet each lost on the cupel the same
weight of gold, viz., .014 grain. When reckoned in percentages of the actual
gold present the losses are .187 per cent. and .076 per cent. respectively.
The heavier percentage loss is mainly due to the increased quantity of
copper.
As with silver so with gold the predominant cause of the cupellation loss is
the solution of the metal in the molten litharge which passes into the cupel.
Three lots of 1 gram of gold cupelled each with 20 grams of lead
repeatedly, so as to make 13 cupellations in all, lost in actual weight 35.72
milligrams. The gold recovered from the cupels amounted altogether to
34.56 milligrams. This shows that, compared with the absorption by the
cupel, the other causes of loss are inconsiderable.
The loss of gold by volatilisation is, however, a real one. The dust from the
flues of assay furnaces has been tested on several occasions and found to
contain gold, though in small quantity. Thus Mr. Lowe found .073 per cent.
of silver and .00033 per cent. of gold in such a material. The lead volatilised
from a gold bullion assay would need to be ten times as rich as this to
account for a loss of gold equal to the hundredth part of a milligram. Dr.
Rose, in the paper already quoted, believes that on a .5 gram charge of
standard bullion the loss from volatilisation is not less than .025 nor more
than .05 milligram of gold.
By way of conclusion it may be said that the cupellation loss of gold is
about .07 per cent., and that it is largely met or even over corrected by a
compensating error due to silver retained in the gold after parting.
Inquartation.—The method of separating the gold from the silver in gold-
silver alloys by boiling with nitric acid does not act equally well in all
cases. An alloy half silver half gold, rolled to thin sheet and boiled for half
an hour with nitric acid, may still retain more than two-thirds of its silver.
An alloy of 1 part gold and 1.7 parts of silver gives up practically the whole
of its silver under similar treatment. The gold is left in a coherent, though
easily broken, sheet retaining the shape of the original alloy. The gold thus
left is quite spongy and porous, so that the acid can penetrate into its
innermost portions. But if the silver is in large excess in the alloy, the
the richest there were 18.3 grains; yet each lost on the cupel the same
weight of gold, viz., .014 grain. When reckoned in percentages of the actual
gold present the losses are .187 per cent. and .076 per cent. respectively.
The heavier percentage loss is mainly due to the increased quantity of
copper.
As with silver so with gold the predominant cause of the cupellation loss is
the solution of the metal in the molten litharge which passes into the cupel.
Three lots of 1 gram of gold cupelled each with 20 grams of lead
repeatedly, so as to make 13 cupellations in all, lost in actual weight 35.72
milligrams. The gold recovered from the cupels amounted altogether to
34.56 milligrams. This shows that, compared with the absorption by the
cupel, the other causes of loss are inconsiderable.
The loss of gold by volatilisation is, however, a real one. The dust from the
flues of assay furnaces has been tested on several occasions and found to
contain gold, though in small quantity. Thus Mr. Lowe found .073 per cent.
of silver and .00033 per cent. of gold in such a material. The lead volatilised
from a gold bullion assay would need to be ten times as rich as this to
account for a loss of gold equal to the hundredth part of a milligram. Dr.
Rose, in the paper already quoted, believes that on a .5 gram charge of
standard bullion the loss from volatilisation is not less than .025 nor more
than .05 milligram of gold.
By way of conclusion it may be said that the cupellation loss of gold is
about .07 per cent., and that it is largely met or even over corrected by a
compensating error due to silver retained in the gold after parting.
Inquartation.—The method of separating the gold from the silver in gold-
silver alloys by boiling with nitric acid does not act equally well in all
cases. An alloy half silver half gold, rolled to thin sheet and boiled for half
an hour with nitric acid, may still retain more than two-thirds of its silver.
An alloy of 1 part gold and 1.7 parts of silver gives up practically the whole
of its silver under similar treatment. The gold is left in a coherent, though
easily broken, sheet retaining the shape of the original alloy. The gold thus
left is quite spongy and porous, so that the acid can penetrate into its
innermost portions. But if the silver is in large excess in the alloy, the
Page 193
removal of the silver is less complete, and the residual gold, instead of
holding together in a form easy to manipulate, falls to a powder which
requires care and time in its treatment. The older assayers, therefore, added
silver to their gold in such proportion that the alloy for parting should be
one quarter gold to three quarters silver. This operation they called
inquartation.
The modern practice is to aim at getting an alloy with 2-1/2 parts of silver
and 1 part of gold. In gold bullion assays this proportion should be obtained
with fair exactness. And in the parting of such gold buttons as are obtained
in assaying ores it is well to aim at this proportion, though absolute
precision is not a matter of importance.
If the button left on cupelling the lead from an assay of an ore appears
white, it is best to assume that it already contains at least a sufficiency of
silver, in the absence of any knowledge to the contrary. This will be true in
almost all cases. But if, on parting, it does not lose at least two-thirds of its
weight, this indicates that the assumption was not justified; and also what
quantity of silver must be added to the button before again attempting to
part. Generally the fault will be in the other direction; the silver will be in
excess and the gold will break up and demand very careful treatment.
If, however, such a button is yellow, then, from its weight and depth of
colour, a rough estimate can be made of how much gold is contained in it.
Silver must be added to make the total weight 3-1/2 times as much as that
of the gold supposed to be present. Thus, if the button weighs 10 milligrams
and is supposed to contain 8 milligrams of gold, then 8 multiplied by 3-1/2
is 28; the button must, in such case, be made up to 28 milligrams by adding
18 milligrams of silver. In judging of the quality of the gold button, no
ordinary error will very seriously affect the result. If, in the example just
given, the quantity of gold present was really 7 or even 9 milligrams of
gold, the resulting alloy would still have been suitable for such partings. In
fact, in routine assays, where the quantity as well as the quality of the gold
is known within fair limits, it is often the custom to add the silver for
inquartation to the lead during the first cupellation.
But in the assay of rich gold alloys such approximate work will not do. If
the composition is not already known with a fair degree of accuracy
holding together in a form easy to manipulate, falls to a powder which
requires care and time in its treatment. The older assayers, therefore, added
silver to their gold in such proportion that the alloy for parting should be
one quarter gold to three quarters silver. This operation they called
inquartation.
The modern practice is to aim at getting an alloy with 2-1/2 parts of silver
and 1 part of gold. In gold bullion assays this proportion should be obtained
with fair exactness. And in the parting of such gold buttons as are obtained
in assaying ores it is well to aim at this proportion, though absolute
precision is not a matter of importance.
If the button left on cupelling the lead from an assay of an ore appears
white, it is best to assume that it already contains at least a sufficiency of
silver, in the absence of any knowledge to the contrary. This will be true in
almost all cases. But if, on parting, it does not lose at least two-thirds of its
weight, this indicates that the assumption was not justified; and also what
quantity of silver must be added to the button before again attempting to
part. Generally the fault will be in the other direction; the silver will be in
excess and the gold will break up and demand very careful treatment.
If, however, such a button is yellow, then, from its weight and depth of
colour, a rough estimate can be made of how much gold is contained in it.
Silver must be added to make the total weight 3-1/2 times as much as that
of the gold supposed to be present. Thus, if the button weighs 10 milligrams
and is supposed to contain 8 milligrams of gold, then 8 multiplied by 3-1/2
is 28; the button must, in such case, be made up to 28 milligrams by adding
18 milligrams of silver. In judging of the quality of the gold button, no
ordinary error will very seriously affect the result. If, in the example just
given, the quantity of gold present was really 7 or even 9 milligrams of
gold, the resulting alloy would still have been suitable for such partings. In
fact, in routine assays, where the quantity as well as the quality of the gold
is known within fair limits, it is often the custom to add the silver for
inquartation to the lead during the first cupellation.
But in the assay of rich gold alloys such approximate work will not do. If
the composition is not already known with a fair degree of accuracy
Page 194
preliminary assays must be made. Weigh up two lots of 100 milligrams of
the alloy and wrap each in 3 grams of lead. To one add 300 milligrams of
silver. Cupel both. The button containing the added silver must be flattened
and boiled with 15 c.c. of nitric acid; and the resulting gold must be
washed, dried, ignited and weighed. This, in milligrams, gives directly the
percentage of gold. The weight of the other button gives the percentage of
gold and silver; the difference between the two gives the percentage of
silver. The rest will, perhaps, be copper.
The composition of the alloy being known, or having been determined as
just described, the calculation of how much silver must be added is fairly
simple. The following is an example. Suppose the bullion contains 92 per
cent. of gold, 1 per cent. of silver and 7 per cent. of copper, and that .5 gram
of it is to be taken for an assay. The .5 gram, then, will contain
Gold .460gram
Silver .005"
Copper .035"
But the total silver required is .46 gram × 2.5. This equals 1.15. Allowing
for the .005 gram of silver already present, 1.145 gram of silver must be
added.
The silver is incorporated with the gold, and at the same time the copper is
eliminated, by cupelling with sheet lead. How much sheet lead must be
used will depend partly on how much bullion is taken, partly on how much
copper it contains. Four grams of lead will do for a .5 gram charge; and for
a .3 gram charge, 3 grams may be used. But with 20 per cent. of copper
these amounts should be doubled; with 40 per cent. of copper they should
be trebled; and with over 60 per cent. of copper four times as much lead
should be used. For small buttons of gold as little lead as may be relied on
to start cupelling may be taken; the lead may conveniently be in the form of
little cups made by folding lead foil on a piece of glass rod. With a large
number of bullion assays systematically worked and checked a simple plan
would be to always use the quantity of lead required by the alloy containing
most copper which turns up for assay. This weight, cut out of lead foil,
would be kept in stock folded into little bags ready to receive the bullion
and silver.
the alloy and wrap each in 3 grams of lead. To one add 300 milligrams of
silver. Cupel both. The button containing the added silver must be flattened
and boiled with 15 c.c. of nitric acid; and the resulting gold must be
washed, dried, ignited and weighed. This, in milligrams, gives directly the
percentage of gold. The weight of the other button gives the percentage of
gold and silver; the difference between the two gives the percentage of
silver. The rest will, perhaps, be copper.
The composition of the alloy being known, or having been determined as
just described, the calculation of how much silver must be added is fairly
simple. The following is an example. Suppose the bullion contains 92 per
cent. of gold, 1 per cent. of silver and 7 per cent. of copper, and that .5 gram
of it is to be taken for an assay. The .5 gram, then, will contain
Gold .460gram
Silver .005"
Copper .035"
But the total silver required is .46 gram × 2.5. This equals 1.15. Allowing
for the .005 gram of silver already present, 1.145 gram of silver must be
added.
The silver is incorporated with the gold, and at the same time the copper is
eliminated, by cupelling with sheet lead. How much sheet lead must be
used will depend partly on how much bullion is taken, partly on how much
copper it contains. Four grams of lead will do for a .5 gram charge; and for
a .3 gram charge, 3 grams may be used. But with 20 per cent. of copper
these amounts should be doubled; with 40 per cent. of copper they should
be trebled; and with over 60 per cent. of copper four times as much lead
should be used. For small buttons of gold as little lead as may be relied on
to start cupelling may be taken; the lead may conveniently be in the form of
little cups made by folding lead foil on a piece of glass rod. With a large
number of bullion assays systematically worked and checked a simple plan
would be to always use the quantity of lead required by the alloy containing
most copper which turns up for assay. This weight, cut out of lead foil,
would be kept in stock folded into little bags ready to receive the bullion
and silver.
Page 195
The silver used for inquartation must, of course, be free from gold and is
best prepared by the assayer who is to use it (see p. 66). It should not be in
long strips or angular pieces likely to perforate the lead in which it is
folded. When wrapped in the lead it should be in the middle and should
make as compact a parcel as possible.
Each little parcel, as completed, should be placed on a tray in its properly
numbered compartment. Its position here should correspond to that it will
occupy in the muffle and eventually in the cupel tray. The cupellation must
be made with all the requisite precautions. A good smooth malleable button
is needed for the next operation, which is known as flatting.
Flatting.—Small buttons, such as are got in assaying most gold ores, are
placed on a polished steel anvil and flattened by one or two blows with a
hammer. The flattened discs are heated to dull redness on a clean cupel and
are then ready for parting. Somewhat larger buttons may be similarly
treated, but they should be annealed (i.e. heated to redness and allowed to
cool) during the flattening. The silver-gold alloy left from the cupellation is
soft and bends like lead; but after hammering or rolling it becomes harder,
gets a spring in it like a piece of mainspring and cracks or splits somewhat
easily. There should be no cracks or stripping or even roughness on the
flattened metal, since such defects may cause the loss of small particles
either during the flattening or in the subsequent treatment with acid. The
softness of the metal is restored by heating. In bullion assays the flatting of
best prepared by the assayer who is to use it (see p. 66). It should not be in
long strips or angular pieces likely to perforate the lead in which it is
folded. When wrapped in the lead it should be in the middle and should
make as compact a parcel as possible.
Each little parcel, as completed, should be placed on a tray in its properly
numbered compartment. Its position here should correspond to that it will
occupy in the muffle and eventually in the cupel tray. The cupellation must
be made with all the requisite precautions. A good smooth malleable button
is needed for the next operation, which is known as flatting.
Flatting.—Small buttons, such as are got in assaying most gold ores, are
placed on a polished steel anvil and flattened by one or two blows with a
hammer. The flattened discs are heated to dull redness on a clean cupel and
are then ready for parting. Somewhat larger buttons may be similarly
treated, but they should be annealed (i.e. heated to redness and allowed to
cool) during the flattening. The silver-gold alloy left from the cupellation is
soft and bends like lead; but after hammering or rolling it becomes harder,
gets a spring in it like a piece of mainspring and cracks or splits somewhat
easily. There should be no cracks or stripping or even roughness on the
flattened metal, since such defects may cause the loss of small particles
either during the flattening or in the subsequent treatment with acid. The
softness of the metal is restored by heating. In bullion assays the flatting of
Page 196
the buttons requires care and practice for its skilful working. The strips of
alloy for parting should be of uniform thickness and condition so that the
action of the acid shall be equal in all cases. The button is taken from the
cupel, cleaned and placed on the anvil: it is then struck a heavy blow which
widens it to about 3/4 inch in diameter; this blow is followed by two others,
one a little in front, the other behind, which lengthen the disc and give a
very blunt roof-like slope to its upper face. It should then be annealed. This
may be done by putting it in a just red-hot scorifier heated in a muffle: it
very soon attains the right heat and may then be transferred to a cold
scorifier; the hot scorifier should be put back into the muffle. The softened
disc is then taken to the rolls (Fig. 45). The rolls are loosened until the disc
can be pressed between them. Looking through the interval between them
the rolls should appear exactly parallel; if they are not, one adjusting screw
should be loosened and the other tightened until parallelism is obtained. The
rolls are now turned and the disc should be drawn through without any great
effort. Beginners are apt to err by trying to do too much with one turn of the
handle. It is easy to stop whilst the rolls are only just gripping the metal and
then to bring the disc back by reversing the action. If the disc was originally
level and the rolls are parallel, the metal will appear as a strip which has
been merely lengthened. If the rolls are tighter on one side the strip will be
bowed; the tighter side will correspond with the outer curve of the crescent.
A mistake of this kind may be amended by passing the strip through the
rolls the other way, so as to reverse the irregularity and so straighten the
strip. The screw on the looser side should then be tightened until parallelism
is obtained; after which more care should be taken to tighten the two screws
equally. The rolling should be stopped when the strip is 3 or 4 inches long
and of the thickness of an ordinary visiting card. The strip should be
annealed during the rolling and again at the finish.
Parting.—The thin sheet of metal is dropped into hot dilute nitric acid and
boiled for five or six minutes after the brisk action of the acid on the metal
has ceased. At this stage nearly all the silver has gone into solution as
nitrate of silver and the acid is charged with this salt. This acid is poured off
and the residual metal is again boiled for from 20 to 30 minutes with a
second lot of stronger acid. This leaves the gold almost pure, though it may
still retain from .05 to .1 per cent. of silver. Treatment with the first acid
only would probably leave three or four times as much.
alloy for parting should be of uniform thickness and condition so that the
action of the acid shall be equal in all cases. The button is taken from the
cupel, cleaned and placed on the anvil: it is then struck a heavy blow which
widens it to about 3/4 inch in diameter; this blow is followed by two others,
one a little in front, the other behind, which lengthen the disc and give a
very blunt roof-like slope to its upper face. It should then be annealed. This
may be done by putting it in a just red-hot scorifier heated in a muffle: it
very soon attains the right heat and may then be transferred to a cold
scorifier; the hot scorifier should be put back into the muffle. The softened
disc is then taken to the rolls (Fig. 45). The rolls are loosened until the disc
can be pressed between them. Looking through the interval between them
the rolls should appear exactly parallel; if they are not, one adjusting screw
should be loosened and the other tightened until parallelism is obtained. The
rolls are now turned and the disc should be drawn through without any great
effort. Beginners are apt to err by trying to do too much with one turn of the
handle. It is easy to stop whilst the rolls are only just gripping the metal and
then to bring the disc back by reversing the action. If the disc was originally
level and the rolls are parallel, the metal will appear as a strip which has
been merely lengthened. If the rolls are tighter on one side the strip will be
bowed; the tighter side will correspond with the outer curve of the crescent.
A mistake of this kind may be amended by passing the strip through the
rolls the other way, so as to reverse the irregularity and so straighten the
strip. The screw on the looser side should then be tightened until parallelism
is obtained; after which more care should be taken to tighten the two screws
equally. The rolling should be stopped when the strip is 3 or 4 inches long
and of the thickness of an ordinary visiting card. The strip should be
annealed during the rolling and again at the finish.
Parting.—The thin sheet of metal is dropped into hot dilute nitric acid and
boiled for five or six minutes after the brisk action of the acid on the metal
has ceased. At this stage nearly all the silver has gone into solution as
nitrate of silver and the acid is charged with this salt. This acid is poured off
and the residual metal is again boiled for from 20 to 30 minutes with a
second lot of stronger acid. This leaves the gold almost pure, though it may
still retain from .05 to .1 per cent. of silver. Treatment with the first acid
only would probably leave three or four times as much.
Page 197
The nitric acid used should be free from hydrochloric, sulphuric, iodic and
telluric acids. In testing it for the first of these add nitrate of silver and
dilute with distilled water; there should be no turbidity. In testing for the
others evaporate three lots in dishes over a water-bath. Test one for
sulphates by adding water and barium chloride. Test another for iodates by
taking up with a little water, adding a few drops of starch paste and then
dilute sulphurous acid solution a little at a time; there should be no blue
colour. Test the third for tellurium by heating with 1 c.c. of strong sulphuric
acid until dense fumes come off; allow to cool considerably; a piece of tin
foil added to the warm acid develops a fine purple colour if only a trace of
tellurium is present.
The presence of lower oxides of nitrogen, which impart a brown colour to
the acid, is objectionable; they, however, are removed by boiling the diluted
acid before using it for parting. It is usual to keep a stock of the acid
suitably diluted to the two strengths required for the parting. These are
known as the parting acids. The first parting acid is the weaker and is used
in the first attack on the metal. The specific gravity generally recommended
for it is about 1.2. It may be prepared either by diluting the strong acid with
about its own volume of distilled water, or by suitably diluting the second
parting acid which has been already used in an assay; the small proportion
of silver this contains is not harmful for this purpose. The second parting
acid has a specific gravity of about 1.3, and may be made by diluting the
strong acid with half its volume of distilled water.
Parting in Flasks.—Flasks are most convenient for the larger partings, as in
bullion assays; and should always be used for this purpose unless some of
the special parting apparatus, like that used in Mints, is available. Many
assayers use flasks, though of a smaller size, for the ordinary partings in
assaying gold ores. The flasks are either bulbs with long necks (Fig. 46)
which ought to be heated on rose burners of special construction; or they
are small flat-bottomed conical flasks which may be conveniently heated on
a hot-plate and are, in this respect, much easier to deal with in general work.
The following instructions apply to the parting of an alloy containing a few
decigrams of gold together with the proper proportion of silver.
telluric acids. In testing it for the first of these add nitrate of silver and
dilute with distilled water; there should be no turbidity. In testing for the
others evaporate three lots in dishes over a water-bath. Test one for
sulphates by adding water and barium chloride. Test another for iodates by
taking up with a little water, adding a few drops of starch paste and then
dilute sulphurous acid solution a little at a time; there should be no blue
colour. Test the third for tellurium by heating with 1 c.c. of strong sulphuric
acid until dense fumes come off; allow to cool considerably; a piece of tin
foil added to the warm acid develops a fine purple colour if only a trace of
tellurium is present.
The presence of lower oxides of nitrogen, which impart a brown colour to
the acid, is objectionable; they, however, are removed by boiling the diluted
acid before using it for parting. It is usual to keep a stock of the acid
suitably diluted to the two strengths required for the parting. These are
known as the parting acids. The first parting acid is the weaker and is used
in the first attack on the metal. The specific gravity generally recommended
for it is about 1.2. It may be prepared either by diluting the strong acid with
about its own volume of distilled water, or by suitably diluting the second
parting acid which has been already used in an assay; the small proportion
of silver this contains is not harmful for this purpose. The second parting
acid has a specific gravity of about 1.3, and may be made by diluting the
strong acid with half its volume of distilled water.
Parting in Flasks.—Flasks are most convenient for the larger partings, as in
bullion assays; and should always be used for this purpose unless some of
the special parting apparatus, like that used in Mints, is available. Many
assayers use flasks, though of a smaller size, for the ordinary partings in
assaying gold ores. The flasks are either bulbs with long necks (Fig. 46)
which ought to be heated on rose burners of special construction; or they
are small flat-bottomed conical flasks which may be conveniently heated on
a hot-plate and are, in this respect, much easier to deal with in general work.
The following instructions apply to the parting of an alloy containing a few
decigrams of gold together with the proper proportion of silver.
Page 198
The strip from the rolls, after being softened by annealing, is folded on
itself on a glass rod into a roll or cornet. It should be so plastic that it will
retain the shape thus given it and not spring open on removing the pressure
of the fingers. About 50 c.c. of the first parting acid are placed in a 6-ounce
conical flask and heated to boiling; the flask is then withdrawn, and tilted a
little to one side, whilst the cornet is cautiously dropped into it; there will be
a sudden issue of hot vapours and a prompt withdrawal of the hand is
advisable. The flask is replaced on the hot plate and the acid is kept boiling
for 10 or 15 minutes. The flask is then withdrawn and the acid diluted with
about an equal volume of distilled water. If the flask has a thick glass band
around its neck, a little way down,[28] care must be taken to use hot water,
for any sudden chill will certainly crack the flask where it is thus thickened.
The liquor is carefully decanted into a clean beaker and is then thrown into
a jar marked "waste silver." About 40 c.c. of the second parting acid, heated
to boiling, is then poured into the flask, which is then replaced on the hot
plate. The boiling is continued for 15 or 20 minutes or even longer. At this
stage bumping has to be specially guarded against; after a little experience
it is easy to see when this is imminent and the flask should be withdrawn to
a cooler part of the plate; it is better to prolong the heating at a temperature
itself on a glass rod into a roll or cornet. It should be so plastic that it will
retain the shape thus given it and not spring open on removing the pressure
of the fingers. About 50 c.c. of the first parting acid are placed in a 6-ounce
conical flask and heated to boiling; the flask is then withdrawn, and tilted a
little to one side, whilst the cornet is cautiously dropped into it; there will be
a sudden issue of hot vapours and a prompt withdrawal of the hand is
advisable. The flask is replaced on the hot plate and the acid is kept boiling
for 10 or 15 minutes. The flask is then withdrawn and the acid diluted with
about an equal volume of distilled water. If the flask has a thick glass band
around its neck, a little way down,[28] care must be taken to use hot water,
for any sudden chill will certainly crack the flask where it is thus thickened.
The liquor is carefully decanted into a clean beaker and is then thrown into
a jar marked "waste silver." About 40 c.c. of the second parting acid, heated
to boiling, is then poured into the flask, which is then replaced on the hot
plate. The boiling is continued for 15 or 20 minutes or even longer. At this
stage bumping has to be specially guarded against; after a little experience
it is easy to see when this is imminent and the flask should be withdrawn to
a cooler part of the plate; it is better to prolong the heating at a temperature
Page 199
below boiling than to run the risk of disaster. Some of the older writers,
however, are rather insistent on vigorous boiling with large bubbles. The
addition of a small ball of well-burnt clay of about the size of a pea has
been recommended, as it lessens the tendency to irregular and dangerous
boiling. At the end of the treatment with the second acid the flask is
withdrawn from the plate and the acid is diluted with an equal volume of
distilled water. The liquor is carefully decanted into a beaker, and then
poured into a jar or Winchester marked "acid waste"; it serves for making
the first parting acid. The flask is then washed twice with hot distilled
water; the washings must be carefully decanted from the gold. The flask is
then filled with water. A parting cup (size B) is then placed over its mouth,
like a thimble on the tip of a finger. This cup is of unglazed porous
earthenware of such texture that it absorbs the last few drops of water left
on drying; and with a surface to which the gold does not adhere even on
ignition. The gold should fall out cleanly and completely on merely
inverting the cup over the pan of the balance. The flask and cup are then
inverted so that the flask stands mouth down in the cup; a little of the water
from the flask flows into the cup, but only a little. The gold falls steadily
through the water into the cup. When time has been allowed for even the
finest of the gold to have settled into the cup, the flask is removed. This is
easiest done under water. The cup, with the flask still resting in it, is dipped
under water in a basin; as soon as the neck of the flask is immersed the
crucible can safely be drawn away from under it and then lifted out of the
water. The flask should not be taken away first, for the rush of water from it
may easily sweep the gold out of the cup. The water in the cup is then
drained off and the cup is dried at not too high a temperature; for if the last
drop or two of water should boil there is danger of spattering the gold out of
the crucible. When it is dry, the cup is heated on a pipe-clay triangle over a
Bunsen burner, or on a slab of asbestos in a muffle, to a dull-red heat. This
brings the gold to "colour"; that is, the loose tender dark coloured gold
becomes bright yellow and coherent; and is in a state fit to be transferred to
the balance and weighed. All unnecessary transferences must be avoided.
As soon as the cup is cool it may be inverted over the pan of the balance,
when the gold will fall out cleanly or, at the worst, a gentle tap with the
finger will be sufficient to detach it.
however, are rather insistent on vigorous boiling with large bubbles. The
addition of a small ball of well-burnt clay of about the size of a pea has
been recommended, as it lessens the tendency to irregular and dangerous
boiling. At the end of the treatment with the second acid the flask is
withdrawn from the plate and the acid is diluted with an equal volume of
distilled water. The liquor is carefully decanted into a beaker, and then
poured into a jar or Winchester marked "acid waste"; it serves for making
the first parting acid. The flask is then washed twice with hot distilled
water; the washings must be carefully decanted from the gold. The flask is
then filled with water. A parting cup (size B) is then placed over its mouth,
like a thimble on the tip of a finger. This cup is of unglazed porous
earthenware of such texture that it absorbs the last few drops of water left
on drying; and with a surface to which the gold does not adhere even on
ignition. The gold should fall out cleanly and completely on merely
inverting the cup over the pan of the balance. The flask and cup are then
inverted so that the flask stands mouth down in the cup; a little of the water
from the flask flows into the cup, but only a little. The gold falls steadily
through the water into the cup. When time has been allowed for even the
finest of the gold to have settled into the cup, the flask is removed. This is
easiest done under water. The cup, with the flask still resting in it, is dipped
under water in a basin; as soon as the neck of the flask is immersed the
crucible can safely be drawn away from under it and then lifted out of the
water. The flask should not be taken away first, for the rush of water from it
may easily sweep the gold out of the cup. The water in the cup is then
drained off and the cup is dried at not too high a temperature; for if the last
drop or two of water should boil there is danger of spattering the gold out of
the crucible. When it is dry, the cup is heated on a pipe-clay triangle over a
Bunsen burner, or on a slab of asbestos in a muffle, to a dull-red heat. This
brings the gold to "colour"; that is, the loose tender dark coloured gold
becomes bright yellow and coherent; and is in a state fit to be transferred to
the balance and weighed. All unnecessary transferences must be avoided.
As soon as the cup is cool it may be inverted over the pan of the balance,
when the gold will fall out cleanly or, at the worst, a gentle tap with the
finger will be sufficient to detach it.
Page 200
Parting in test-tubes, or in the smaller conical flasks, is used in the assay of
gold ores of ordinary richness. The work is exactly like that just described
in all its main features. Generally speaking much less acid will be used; for
example, in test-tubes and for small buttons, 3 or 4 c.c. of each acid is quite
enough. Again, the action need not be so prolonged; 10 or 15 minutes in
each acid is sufficient. So, too, the heating may be less; it is very convenient
to support the test-tubes in a water-bath, or merely to rest them in a beaker
of boiling water; and there is no serious objection to doing this. A smaller
parting cup should be used; the A size is suitable. The button, on the other
hand, should be beaten thinner than is needed for the larger partings. If the
silver should be in excess and the gold becomes much broken up, ample
time should be given for subsidence from the test-tube or flask into the
parting cup.
Parting in glazed crucibles or dishes.—This method of working has the
advantage that there is no transference of the gold until it is placed on the
pan of the balance. On the other hand, in the boiling more care is required
in adjusting the temperature. The following instructions apply to the
treatment of very small buttons, to which the method is more particularly
applicable; but very little modification is needed for the treatment of larger
buttons. The smallest sized Berlin crucibles answer admirably. They should
be cleaned by treatment with hot and strong sulphuric acid, followed by
washing in distilled water; the comfort and ease of working mainly depends
on the thoroughness of this cleaning. The crucible, one-third full with the
first parting acid, is heated on the hot plate until the acid is almost boiling.
The flattened and annealed button is dropped into it and the heating
continued with, at most, gentle boiling for a few minutes. The crucible is
then filled with distilled water, which cools it enough for easy handling; and
when the gold has settled the liquor is poured off along a glass rod into a
clean beaker. Any greasiness of the crucible makes itself felt here and is
very objectionable. The crucible is then one-third filled with the second
parting acid and the heating resumed, care being taken not to raise the
temperature too high; this should be continued much longer than before, say
for five or ten minutes or even longer according to the size of the button.
Distilled water is again added and, when it is drained off, the washing with
distilled water is twice repeated. It will not be possible to drain off the last
drop of water; but if the gold is coherent, the crucible can be so inclined
gold ores of ordinary richness. The work is exactly like that just described
in all its main features. Generally speaking much less acid will be used; for
example, in test-tubes and for small buttons, 3 or 4 c.c. of each acid is quite
enough. Again, the action need not be so prolonged; 10 or 15 minutes in
each acid is sufficient. So, too, the heating may be less; it is very convenient
to support the test-tubes in a water-bath, or merely to rest them in a beaker
of boiling water; and there is no serious objection to doing this. A smaller
parting cup should be used; the A size is suitable. The button, on the other
hand, should be beaten thinner than is needed for the larger partings. If the
silver should be in excess and the gold becomes much broken up, ample
time should be given for subsidence from the test-tube or flask into the
parting cup.
Parting in glazed crucibles or dishes.—This method of working has the
advantage that there is no transference of the gold until it is placed on the
pan of the balance. On the other hand, in the boiling more care is required
in adjusting the temperature. The following instructions apply to the
treatment of very small buttons, to which the method is more particularly
applicable; but very little modification is needed for the treatment of larger
buttons. The smallest sized Berlin crucibles answer admirably. They should
be cleaned by treatment with hot and strong sulphuric acid, followed by
washing in distilled water; the comfort and ease of working mainly depends
on the thoroughness of this cleaning. The crucible, one-third full with the
first parting acid, is heated on the hot plate until the acid is almost boiling.
The flattened and annealed button is dropped into it and the heating
continued with, at most, gentle boiling for a few minutes. The crucible is
then filled with distilled water, which cools it enough for easy handling; and
when the gold has settled the liquor is poured off along a glass rod into a
clean beaker. Any greasiness of the crucible makes itself felt here and is
very objectionable. The crucible is then one-third filled with the second
parting acid and the heating resumed, care being taken not to raise the
temperature too high; this should be continued much longer than before, say
for five or ten minutes or even longer according to the size of the button.
Distilled water is again added and, when it is drained off, the washing with
distilled water is twice repeated. It will not be possible to drain off the last
drop of water; but if the gold is coherent, the crucible can be so inclined
Page 201
that this drop drains away from the gold, in which case the drying can be
done rapidly; the boiling of the water will do no harm. But when the gold is
much broken up, it will collect in the middle of this drop and the drying
must be done gently; best by putting the crucible in a warm place. When
dry, the crucible is heated till the gold changes colour, but the heat must be
kept well below redness. When cold, the gold is transferred directly to the
pan of the balance. With minute specks of gold which will require
measuring, it is best to put a small piece of lead foil (say .1 gram) in the
crucible over the gold, and then heat the crucible to above redness over a
blowpipe. Whilst the lead is oxidising it is easily swept round in a bath of
molten litharge by merely tilting the crucible. In this way any separated
specks of gold can be taken up with certainty. When the worker is satisfied
that the lead has had ample opportunity for taking up the gold, the lead must
be kept in one place and the heat slowly lowered. By this means the button
becomes supported in comparatively pure litharge and when solid can be
picked out quite easily with a pair of pliers and in a very clean condition.
The lead button is then cupelled on a very fine cupel, as already described.
The method of working last described destroys the crucible. If the gold is
not quite so small this may be avoided. A small piece of lead foil should be
hammered out until it is perfectly flexible. It is then shaped into a tray and
the gold is transferred to it. The lead is then folded over, with the help of
two pins; and cupelled.
If the crucible shows a black stain on heating it is because some silver
remains through bad washing. It shows poor work and the assay should be
repeated.
The silver retained in the gold after parting is, in bullion assays, an
important matter; it is roughly equal to the loss of gold due to absorption by
the cupel. Mr. Lowe working on .5 oz. of gold, obtained by parting in
assaying bullion, found it to contain .123 per cent. of silver. Dr. Rose in
some special assay pieces found by a less direct method of assaying, from
.06 to .09 per cent. of silver. The proportion of silver retained varies in a
marked way with the proportion of gold to silver in the alloy before parting.
It is generally stated that the retained silver is least when this proportion is 1
to 2-1/2, and more or less silver than this leads to a less pure gold after
parting.
done rapidly; the boiling of the water will do no harm. But when the gold is
much broken up, it will collect in the middle of this drop and the drying
must be done gently; best by putting the crucible in a warm place. When
dry, the crucible is heated till the gold changes colour, but the heat must be
kept well below redness. When cold, the gold is transferred directly to the
pan of the balance. With minute specks of gold which will require
measuring, it is best to put a small piece of lead foil (say .1 gram) in the
crucible over the gold, and then heat the crucible to above redness over a
blowpipe. Whilst the lead is oxidising it is easily swept round in a bath of
molten litharge by merely tilting the crucible. In this way any separated
specks of gold can be taken up with certainty. When the worker is satisfied
that the lead has had ample opportunity for taking up the gold, the lead must
be kept in one place and the heat slowly lowered. By this means the button
becomes supported in comparatively pure litharge and when solid can be
picked out quite easily with a pair of pliers and in a very clean condition.
The lead button is then cupelled on a very fine cupel, as already described.
The method of working last described destroys the crucible. If the gold is
not quite so small this may be avoided. A small piece of lead foil should be
hammered out until it is perfectly flexible. It is then shaped into a tray and
the gold is transferred to it. The lead is then folded over, with the help of
two pins; and cupelled.
If the crucible shows a black stain on heating it is because some silver
remains through bad washing. It shows poor work and the assay should be
repeated.
The silver retained in the gold after parting is, in bullion assays, an
important matter; it is roughly equal to the loss of gold due to absorption by
the cupel. Mr. Lowe working on .5 oz. of gold, obtained by parting in
assaying bullion, found it to contain .123 per cent. of silver. Dr. Rose in
some special assay pieces found by a less direct method of assaying, from
.06 to .09 per cent. of silver. The proportion of silver retained varies in a
marked way with the proportion of gold to silver in the alloy before parting.
It is generally stated that the retained silver is least when this proportion is 1
to 2-1/2, and more or less silver than this leads to a less pure gold after
parting.
Page 202
Platinum in an alloy being parted is dissolved along with the silver either
altogether or in part. It imparts a straw yellow colour to the parting acid.
Palladium gives an orange colour to the acid.
The loss of gold by solution in the acid during parting is small, but easily
demonstrable. On a 500-milligram charge of bullion it may amount to from
.05 to .15 milligram; i.e. from .01 to .03 per cent. It is due to gold actually
dissolved and not merely held in suspension.
Assaying with checks. Surcharge.—It will be seen from what has been
stated that the errors in gold parting are of two kinds: viz. (1) a loss of gold
on the cupel and to a less extent by solution in the acid, and (2) an apparent
gain of gold due to the retention of silver in the parted material. Both errors
are small, and as they are of an opposite character they tend to neutralise
each other. Hence they are altogether without effect on the accuracy of the
assays of ores when the total gold is reckoned in milligrams. And even with
the larger amounts present in bullion assays their influence is so small that
an uncorrected result is still fairly accurate; the resultant error would not be
more than one part in two or three thousand.
It is customary to report the purity of bullion, or its fineness as it is called,
in parts per thousand of bullion. The sum of the errors of an assay, which is
called the surcharge, is reported in the same way. Thus a surcharge of + .3
means that the gold as weighed was .3 part per 1000 more than the gold
actually present. But a surcharge - .3 means that on the whole there was a
loss of .3 part per 1000 in the assay.
Speaking roughly the retained silver will vary with the weight of gold
present; if one alloy contains twice as much gold as another the retained
silver will be about twice as much also. On the other hand, as already
explained, the cupellation loss on the poorer alloy is as much as, or even
more than, with the richer one, because of the copper, &c. present. With
rich gold alloys the silver more than compensates for the loss and the
surcharge is positive; but with poorer alloys the loss is greater and the
surcharge is negative.
In Mints and places where bullion assays must be made with the highest
attainable accuracy, the surcharge is determined by experiment, and the
proper correction is made in the reports on the bullion. This is done by
altogether or in part. It imparts a straw yellow colour to the parting acid.
Palladium gives an orange colour to the acid.
The loss of gold by solution in the acid during parting is small, but easily
demonstrable. On a 500-milligram charge of bullion it may amount to from
.05 to .15 milligram; i.e. from .01 to .03 per cent. It is due to gold actually
dissolved and not merely held in suspension.
Assaying with checks. Surcharge.—It will be seen from what has been
stated that the errors in gold parting are of two kinds: viz. (1) a loss of gold
on the cupel and to a less extent by solution in the acid, and (2) an apparent
gain of gold due to the retention of silver in the parted material. Both errors
are small, and as they are of an opposite character they tend to neutralise
each other. Hence they are altogether without effect on the accuracy of the
assays of ores when the total gold is reckoned in milligrams. And even with
the larger amounts present in bullion assays their influence is so small that
an uncorrected result is still fairly accurate; the resultant error would not be
more than one part in two or three thousand.
It is customary to report the purity of bullion, or its fineness as it is called,
in parts per thousand of bullion. The sum of the errors of an assay, which is
called the surcharge, is reported in the same way. Thus a surcharge of + .3
means that the gold as weighed was .3 part per 1000 more than the gold
actually present. But a surcharge - .3 means that on the whole there was a
loss of .3 part per 1000 in the assay.
Speaking roughly the retained silver will vary with the weight of gold
present; if one alloy contains twice as much gold as another the retained
silver will be about twice as much also. On the other hand, as already
explained, the cupellation loss on the poorer alloy is as much as, or even
more than, with the richer one, because of the copper, &c. present. With
rich gold alloys the silver more than compensates for the loss and the
surcharge is positive; but with poorer alloys the loss is greater and the
surcharge is negative.
In Mints and places where bullion assays must be made with the highest
attainable accuracy, the surcharge is determined by experiment, and the
proper correction is made in the reports on the bullion. This is done by
Page 203
making assays of gold of the highest degree of purity alongside of those of
the bullion whose quality has to be determined. These "checks" are so made
that they do not differ from the actual assays in any material point. Thus,
being of the same quality and weight and undergoing exactly the same
treatment, they may reasonably be expected to have the same surcharge as
the assays they imitate. Suppose the bullion being assayed varies only a
little, up or down, from 900 gold and 100 copper in the thousand, and that
.5 gram of it is used in each assay. A quantity of gold differing only a little
from .450 gram would be very exactly weighed and placed with .050 gram
of copper in the same weight of lead as is being used in the other assays. It
would be cupelled, parted, &c., as nearly as possible under the same
conditions as the actual assays. Suppose the pure gold weighed .45016 gram
and the parted gold weighed .45025 gram, the gain in weight, .00009 gram,
would be deducted from the actual assays. A surcharge correction is never
applied except to bullion of the same quality as that represented by the
"check assay" it was calculated from.
It is evident that unless the gold is of the highest degree of purity these
check assays will introduce an error almost equal to that which it is
designed to remedy. Moreover, to work the checks to the greatest
advantage, a very systematic and uniform method of working must be
adopted.
Parting in special apparatus.—One plan for obtaining greater uniformity
is to stamp each cornet with a number for purposes of identification, and to
treat several, including one or more check assays in the same acid contained
in a beaker; all the assays under these conditions evidently receive precisely
the same acid treatment. Such a plan can of course only be adopted where
there is no risk of the gold breaking up during the parting. An improvement
on this is to have a porcelain basin[29] about 8-1/2 inches in diameter and
with a capacity of about 1-1/2 litres. It is provided with a porcelain cover
with 30 numbered holes through which tubes dip into the acid. The cover is
removable. The tubes are like test-tubes and are supported by the cover;
their bottoms are perforated with holes or slits. The acid is placed in the
basin and boiled over a flat burner; it enters the tubes through the slits. The
cornets are placed each in its proper tube. When the boiling is finished, the
cover with the tubes is lifted and at the same time the acid drains back into
the basin. A dip into a basin of distilled water washes at one operation all 30
the bullion whose quality has to be determined. These "checks" are so made
that they do not differ from the actual assays in any material point. Thus,
being of the same quality and weight and undergoing exactly the same
treatment, they may reasonably be expected to have the same surcharge as
the assays they imitate. Suppose the bullion being assayed varies only a
little, up or down, from 900 gold and 100 copper in the thousand, and that
.5 gram of it is used in each assay. A quantity of gold differing only a little
from .450 gram would be very exactly weighed and placed with .050 gram
of copper in the same weight of lead as is being used in the other assays. It
would be cupelled, parted, &c., as nearly as possible under the same
conditions as the actual assays. Suppose the pure gold weighed .45016 gram
and the parted gold weighed .45025 gram, the gain in weight, .00009 gram,
would be deducted from the actual assays. A surcharge correction is never
applied except to bullion of the same quality as that represented by the
"check assay" it was calculated from.
It is evident that unless the gold is of the highest degree of purity these
check assays will introduce an error almost equal to that which it is
designed to remedy. Moreover, to work the checks to the greatest
advantage, a very systematic and uniform method of working must be
adopted.
Parting in special apparatus.—One plan for obtaining greater uniformity
is to stamp each cornet with a number for purposes of identification, and to
treat several, including one or more check assays in the same acid contained
in a beaker; all the assays under these conditions evidently receive precisely
the same acid treatment. Such a plan can of course only be adopted where
there is no risk of the gold breaking up during the parting. An improvement
on this is to have a porcelain basin[29] about 8-1/2 inches in diameter and
with a capacity of about 1-1/2 litres. It is provided with a porcelain cover
with 30 numbered holes through which tubes dip into the acid. The cover is
removable. The tubes are like test-tubes and are supported by the cover;
their bottoms are perforated with holes or slits. The acid is placed in the
basin and boiled over a flat burner; it enters the tubes through the slits. The
cornets are placed each in its proper tube. When the boiling is finished, the
cover with the tubes is lifted and at the same time the acid drains back into
the basin. A dip into a basin of distilled water washes at one operation all 30
Page 204
assays. The cover is then put on a basin containing the stronger parting acid
which is already boiling. This boiling is continued for half an hour. The
cover with the 30 cornets is then lifted out from the acid and dipped two or
three times in distilled water to wash off the last traces of acid. To transfer
the cornets from the tubes to the porous cups the whole of the tube must be
dipped under the water; otherwise the operation is exactly as when working
with test-tubes.
A still simpler method of working is to use small platinum cups[30] provided
with fine slits which admit the acid but retain the gold. A number of these,
say 60, are supported on a platinum tray. The parting acids are boiled in
platinum dishes under a hood; and the 60 cornets (each in its proper cup)
are placed in the acid all at once: the tray carrying the cups is provided with
a handle suitable for this purpose. After a proper boiling the tray is lifted out
of the weaker acid into the stronger one, where it undergoes the second
boiling. It is next dipped several times in distilled water and lastly, after a
gentle drying, it is raised to an annealing temperature which must not be too
high for fear of the gold sticking to the platinum. After cooling, the cornets
are transferred from the platinum cups directly to the pan of the balance.
Here all 60 cornets have exactly the same treatment and the "checks" may
be compared with great exactness with the other assays accompanying
them. There is, too, a great saving of labour.[31]
Silver, &c., in gold bullion.—The base metals are generally determined by
cupelling .5 gram of the alloy with 5 grams of lead. The loss in cupellation
having been allowed for by any of the usual methods (see p. 104) the gold
and silver contents are given. By deducting the gold the proportion of silver
is obtained. The silver is generally determined by difference in this way. If
it is desired to dissolve out the copper, silver, &c., and to determine them in
the wet way, the gold must first be alloyed with a sufficiency of some other
metal to render it amenable to the attack by acid. Cadmium is the metal
generally recommended, and the alloy is made by melting together a
weighed portion of the gold with five or six times its weight of cadmium in
a Berlin crucible and under a thin layer of potassium cyanide.
Lead with gold or silver.—Large quantities of lead carrying gold and silver
are sold to refiners in bars weighing about 100 lbs. each. The assay of these
which is already boiling. This boiling is continued for half an hour. The
cover with the 30 cornets is then lifted out from the acid and dipped two or
three times in distilled water to wash off the last traces of acid. To transfer
the cornets from the tubes to the porous cups the whole of the tube must be
dipped under the water; otherwise the operation is exactly as when working
with test-tubes.
A still simpler method of working is to use small platinum cups[30] provided
with fine slits which admit the acid but retain the gold. A number of these,
say 60, are supported on a platinum tray. The parting acids are boiled in
platinum dishes under a hood; and the 60 cornets (each in its proper cup)
are placed in the acid all at once: the tray carrying the cups is provided with
a handle suitable for this purpose. After a proper boiling the tray is lifted out
of the weaker acid into the stronger one, where it undergoes the second
boiling. It is next dipped several times in distilled water and lastly, after a
gentle drying, it is raised to an annealing temperature which must not be too
high for fear of the gold sticking to the platinum. After cooling, the cornets
are transferred from the platinum cups directly to the pan of the balance.
Here all 60 cornets have exactly the same treatment and the "checks" may
be compared with great exactness with the other assays accompanying
them. There is, too, a great saving of labour.[31]
Silver, &c., in gold bullion.—The base metals are generally determined by
cupelling .5 gram of the alloy with 5 grams of lead. The loss in cupellation
having been allowed for by any of the usual methods (see p. 104) the gold
and silver contents are given. By deducting the gold the proportion of silver
is obtained. The silver is generally determined by difference in this way. If
it is desired to dissolve out the copper, silver, &c., and to determine them in
the wet way, the gold must first be alloyed with a sufficiency of some other
metal to render it amenable to the attack by acid. Cadmium is the metal
generally recommended, and the alloy is made by melting together a
weighed portion of the gold with five or six times its weight of cadmium in
a Berlin crucible and under a thin layer of potassium cyanide.
Lead with gold or silver.—Large quantities of lead carrying gold and silver
are sold to refiners in bars weighing about 100 lbs. each. The assay of these
Page 205
alloys presents no special difficulties, but the sampling of them is a question
which may be profitably discussed.[32]
A molten metal may be conceived to have all the physical states observed in
ordinary liquids, although these cannot be actually seen owing to its
opaqueness. There is no doubt that pure lead at a temperature only a little
above its melting-point can contain a large proportion of gold in such a
manner that it may in a figurative way be spoken of as a clear solution. Any
small portion withdrawn from the molten metal would afford a perfect
sample. The same would be true of any pure alloy of lead and silver in
which the silver does not exceed the proportion of 2-1/2 per cent.[33] On the
other hand, if the molten metal contains much more than .5 per cent. of
zinc, more than .1 per cent. of copper, or a larger quantity of silver, it may
be likened to a turbid liquor. The resemblance holds good so far that if the
molten lead be further heated, whereby its solvent power on the added
metal is increased, the turbidity will disappear, or at least be considerably
diminished. A portion taken at random from such a molten metal may, or
may not, give a good sample. The suspended insoluble matter will tend to
concentrate itself in the upper or lower parts of the liquid according to
whether it is heavier or lighter than it; and this separation may occur with
extreme slowness or with fair rapidity. However, it is generally agreed that
in the case of such alloys as occur in practice, samples taken in this way are
quite satisfactory and are the best obtainable. The precautions insisted on
are that the lead shall be made as hot as practicable; that it shall be stirred
up at the time of taking the sample; and that the portion withdrawn shall be
taken out with a ladle at least as hot as the molten metal. The further
precaution that if any dross be on the surface of the metal it shall be
skimmed off and separately sampled and assayed is almost too obvious to
require mention. An alternative and, perhaps, better way of taking the
sample is to withdraw portions at equal intervals from the stream of metal
whilst the pot is being emptied; equal weights taken from these portions and
mixed (by melting or in some other way) give a fair sample of the whole. In
addition, separate assays of each portion will show to what extent the metal
lacks uniformity in composition For example, samples taken at the
beginning, middle, and end of a run gave the following results in ozs. of
silver per ton: 475, 472, 466, showing an average result of 471 ozs. Fifteen
fractions taken at regular intervals during the same pouring ranged from
which may be profitably discussed.[32]
A molten metal may be conceived to have all the physical states observed in
ordinary liquids, although these cannot be actually seen owing to its
opaqueness. There is no doubt that pure lead at a temperature only a little
above its melting-point can contain a large proportion of gold in such a
manner that it may in a figurative way be spoken of as a clear solution. Any
small portion withdrawn from the molten metal would afford a perfect
sample. The same would be true of any pure alloy of lead and silver in
which the silver does not exceed the proportion of 2-1/2 per cent.[33] On the
other hand, if the molten metal contains much more than .5 per cent. of
zinc, more than .1 per cent. of copper, or a larger quantity of silver, it may
be likened to a turbid liquor. The resemblance holds good so far that if the
molten lead be further heated, whereby its solvent power on the added
metal is increased, the turbidity will disappear, or at least be considerably
diminished. A portion taken at random from such a molten metal may, or
may not, give a good sample. The suspended insoluble matter will tend to
concentrate itself in the upper or lower parts of the liquid according to
whether it is heavier or lighter than it; and this separation may occur with
extreme slowness or with fair rapidity. However, it is generally agreed that
in the case of such alloys as occur in practice, samples taken in this way are
quite satisfactory and are the best obtainable. The precautions insisted on
are that the lead shall be made as hot as practicable; that it shall be stirred
up at the time of taking the sample; and that the portion withdrawn shall be
taken out with a ladle at least as hot as the molten metal. The further
precaution that if any dross be on the surface of the metal it shall be
skimmed off and separately sampled and assayed is almost too obvious to
require mention. An alternative and, perhaps, better way of taking the
sample is to withdraw portions at equal intervals from the stream of metal
whilst the pot is being emptied; equal weights taken from these portions and
mixed (by melting or in some other way) give a fair sample of the whole. In
addition, separate assays of each portion will show to what extent the metal
lacks uniformity in composition For example, samples taken at the
beginning, middle, and end of a run gave the following results in ozs. of
silver per ton: 475, 472, 466, showing an average result of 471 ozs. Fifteen
fractions taken at regular intervals during the same pouring ranged from
Page 206
475 ozs. to 464 ozs.: the average result was 469.8 ozs. The same lead cast
into bars and sampled by sawing gave an average of 470 ozs.[34] In another
case[35] samples drawn at the beginning, middle, and end of a run gave
1345 ozs., 1335 ozs. and 1331 ozs. The mean result in such cases is always
a reasonably safe one, but evidently where the metal varies a good deal it is
safer to take more than three dips.
Imagine such lead run into moulds and allowed to become solid as bars; the
difference between bar and bar would not be greater than that between
corresponding dip samples. But in each bar the distribution of the silver and
gold is very seriously affected during solidification. Chips taken from the
same bar of auriferous lead may show in one place 23 ozs. of gold to the
ton, in another 39 ozs.; similarly with silver they may vary as much as from
900 ozs. to 1500 ozs. to the ton.
This rearrangement of the constituents of a bar takes place whilst the lead is
partly solid, partly liquid. The most useful conception of such half-
solidified metal is that of a felted spongy mass of skeleton crystals of
comparatively pure lead saturated with a still fluid enriched alloy. If the
solidification of an ingot of impure tin be watched it will be evident that the
frosted appearance of the surface is due to the withdrawal of the fluid
portion from a mat of crystals of purer tin which have been for some time
solid and a contraction of the mass. The shrinking of the last part to become
solid is further shown by the collapse of the surface of the ingot where
weakest; that is, a furrow is formed on the flat surface. In other cases of
fused metal there is expansion instead of contraction in this final stage of
the solidification, and the enriched alloy then causes the upper face of the
ingot to bulge outwards. There are other causes effecting the redistribution
of the metals through the ingot. There can be no general rule of wide
application showing which part of a bar is richest and which poorest in the
precious metals. This will depend on the quantities of gold or silver, on the
quantities and kinds of other metals present and on the manner of casting.
The student is advised to consult Mr. Claudet's paper which has been
already referred to.
The best method of sampling such bars is to melt them all down and to take
a dip sample of the molten metal in one or other of the methods already
described. According to Mr. Claudet this should be done in all cases where
into bars and sampled by sawing gave an average of 470 ozs.[34] In another
case[35] samples drawn at the beginning, middle, and end of a run gave
1345 ozs., 1335 ozs. and 1331 ozs. The mean result in such cases is always
a reasonably safe one, but evidently where the metal varies a good deal it is
safer to take more than three dips.
Imagine such lead run into moulds and allowed to become solid as bars; the
difference between bar and bar would not be greater than that between
corresponding dip samples. But in each bar the distribution of the silver and
gold is very seriously affected during solidification. Chips taken from the
same bar of auriferous lead may show in one place 23 ozs. of gold to the
ton, in another 39 ozs.; similarly with silver they may vary as much as from
900 ozs. to 1500 ozs. to the ton.
This rearrangement of the constituents of a bar takes place whilst the lead is
partly solid, partly liquid. The most useful conception of such half-
solidified metal is that of a felted spongy mass of skeleton crystals of
comparatively pure lead saturated with a still fluid enriched alloy. If the
solidification of an ingot of impure tin be watched it will be evident that the
frosted appearance of the surface is due to the withdrawal of the fluid
portion from a mat of crystals of purer tin which have been for some time
solid and a contraction of the mass. The shrinking of the last part to become
solid is further shown by the collapse of the surface of the ingot where
weakest; that is, a furrow is formed on the flat surface. In other cases of
fused metal there is expansion instead of contraction in this final stage of
the solidification, and the enriched alloy then causes the upper face of the
ingot to bulge outwards. There are other causes effecting the redistribution
of the metals through the ingot. There can be no general rule of wide
application showing which part of a bar is richest and which poorest in the
precious metals. This will depend on the quantities of gold or silver, on the
quantities and kinds of other metals present and on the manner of casting.
The student is advised to consult Mr. Claudet's paper which has been
already referred to.
The best method of sampling such bars is to melt them all down and to take
a dip sample of the molten metal in one or other of the methods already
described. According to Mr. Claudet this should be done in all cases where
Page 207
the gold exceeds one or two ounces or where the silver exceeds 200 ozs. to
the ton. If during the melting down some dross has formed this must be
skimmed off, weighed and separately sampled and assayed. The clean lead
also must be weighed, sampled and assayed. The mean result must be
calculated. Thus 14 tons 5 cwts. of clean lead assaying 32 ozs. to the ton
will contain 456 ozs. of silver; 15 cwt. dross assaying 20 ozs. to the ton will
contain 15 ozs. of silver. The 15 tons of lead and dross will contain 471 ozs.
of silver or 31.4 ozs. per ton.
Of the methods of sampling which avoid melting the bars, that known as
sawing is the only one which is thoroughly satisfactory. In it the bars are
brought to a circular saw having fine teeth and are sawn across either
completely or halfway through; in this way a quantity of lead sawdust is
obtained (say 1 lb. or so from a bar) which represents exactly the average of
the bar along the particular cross section taken and approximately that of
the whole bar. A bar of lead, which by dip assay gave 334 ozs. to the ton,
gave on three transverse sections 333 ozs., 335 ozs. and 331 ozs. The
variation may be greater than this, but with a large number of bars, where
each bar is cut across in as far as possible a different place, these variations
tend to neutralise each other and a good sample is obtained. Two or three
cwt. of sawdust may be obtained in this way; this is thoroughly mixed and
reduced by quartering in the usual way or by a mechanical sampler. A
sample of 2 or 3 lbs. is sent to the assayer. This being contaminated with the
oil used in lubricating the saw is freed from it by washing with carbon
bisulphide, ether or benzene and dried. Then, after mixing, 100 to 200
grams of it are carefully weighed and placed in a hot crucible, the heat of
which should be sufficient to melt all the lead. The molten lead should not
be overheated and should show no loss due to the melting. The removal of
the oil may have decreased the weight by perhaps one half per cent. If the
lead gives dross on heating it may be melted under 10 or 20 grams of
potassium cyanide, which prevents the formation of dross. Samples are
sometimes taken with a drill, gouge or chisel, though no method of this kind
is quite satisfactory. One plan adopted is to use a punch which, when driven
into the bar, gives a core or rod of metal about half as long as the bar is
thick and about one-eighth of an inch across. With five bars side by side it
is customary to drive in the punch at one end on the first bar, and at the
opposite end on the last one, and on the others in intermediate positions in
the ton. If during the melting down some dross has formed this must be
skimmed off, weighed and separately sampled and assayed. The clean lead
also must be weighed, sampled and assayed. The mean result must be
calculated. Thus 14 tons 5 cwts. of clean lead assaying 32 ozs. to the ton
will contain 456 ozs. of silver; 15 cwt. dross assaying 20 ozs. to the ton will
contain 15 ozs. of silver. The 15 tons of lead and dross will contain 471 ozs.
of silver or 31.4 ozs. per ton.
Of the methods of sampling which avoid melting the bars, that known as
sawing is the only one which is thoroughly satisfactory. In it the bars are
brought to a circular saw having fine teeth and are sawn across either
completely or halfway through; in this way a quantity of lead sawdust is
obtained (say 1 lb. or so from a bar) which represents exactly the average of
the bar along the particular cross section taken and approximately that of
the whole bar. A bar of lead, which by dip assay gave 334 ozs. to the ton,
gave on three transverse sections 333 ozs., 335 ozs. and 331 ozs. The
variation may be greater than this, but with a large number of bars, where
each bar is cut across in as far as possible a different place, these variations
tend to neutralise each other and a good sample is obtained. Two or three
cwt. of sawdust may be obtained in this way; this is thoroughly mixed and
reduced by quartering in the usual way or by a mechanical sampler. A
sample of 2 or 3 lbs. is sent to the assayer. This being contaminated with the
oil used in lubricating the saw is freed from it by washing with carbon
bisulphide, ether or benzene and dried. Then, after mixing, 100 to 200
grams of it are carefully weighed and placed in a hot crucible, the heat of
which should be sufficient to melt all the lead. The molten lead should not
be overheated and should show no loss due to the melting. The removal of
the oil may have decreased the weight by perhaps one half per cent. If the
lead gives dross on heating it may be melted under 10 or 20 grams of
potassium cyanide, which prevents the formation of dross. Samples are
sometimes taken with a drill, gouge or chisel, though no method of this kind
is quite satisfactory. One plan adopted is to use a punch which, when driven
into the bar, gives a core or rod of metal about half as long as the bar is
thick and about one-eighth of an inch across. With five bars side by side it
is customary to drive in the punch at one end on the first bar, and at the
opposite end on the last one, and on the others in intermediate positions in
Page 208
such a manner that all the holes will be along a diagonal of the rectangle
enclosing the bars. The bars are then turned over and similar portions
punched out through the bottoms of the bars and along the other diagonal.
Or one set of five may be sampled along the top and the next set along the
bottom of the bars.
Silver and gold present in bars of copper are subject to the same irregularity
of distribution as in lead. The sampling of such bars is guided by the same
principles.[36]
CYANIDES.
The cyanides ought perhaps to be considered along with chlorides,
bromides and iodides in Chapter XV. But they are treated here because they
owe their importance to their use in the extraction of gold and because their
determination has become a part of the ordinary work of an assayer of gold
ores.
Formerly, the cyanide most easily obtained in commerce was potassium
cyanide; and it was generally sold in cakes which might contain as little as
40 per cent. or as much as 95 per cent. of the pure salt. It became customary
to express the quality of a sample of commercial cyanide by saying it
contained so much per cent. of potassium cyanide. The commercial product
now made by improved methods of manufacture is actually sodium
cyanide, but is called "potassium cyanide" (probably with the words
"double salt" on the label); it contains cyanide equivalent to something over
100 per cent. of potassium cyanide in addition to a large proportion of
sodium carbonate and other impurities. What is wanted in most cases is
merely a soluble cyanide, and it is a matter of indifference whether the base
be sodium or potassium. But since 49 parts of sodium cyanide (NaCN = 49)
are equivalent to 65 parts of potassium cyanide (KCN = 65) it is evident
that a pure sample of sodium cyanide would contain cyanide equivalent to
little less than 133 per cent. of potassium cyanide. Therefore a sample of
cyanide reported on in this way may be rich in cyanide, and yet have much
impurity.
The commonest impurity in commercial cyanide is carbonate of sodium or
potassium. This may be tested for by dissolving, say, 2 grams in a little
enclosing the bars. The bars are then turned over and similar portions
punched out through the bottoms of the bars and along the other diagonal.
Or one set of five may be sampled along the top and the next set along the
bottom of the bars.
Silver and gold present in bars of copper are subject to the same irregularity
of distribution as in lead. The sampling of such bars is guided by the same
principles.[36]
CYANIDES.
The cyanides ought perhaps to be considered along with chlorides,
bromides and iodides in Chapter XV. But they are treated here because they
owe their importance to their use in the extraction of gold and because their
determination has become a part of the ordinary work of an assayer of gold
ores.
Formerly, the cyanide most easily obtained in commerce was potassium
cyanide; and it was generally sold in cakes which might contain as little as
40 per cent. or as much as 95 per cent. of the pure salt. It became customary
to express the quality of a sample of commercial cyanide by saying it
contained so much per cent. of potassium cyanide. The commercial product
now made by improved methods of manufacture is actually sodium
cyanide, but is called "potassium cyanide" (probably with the words
"double salt" on the label); it contains cyanide equivalent to something over
100 per cent. of potassium cyanide in addition to a large proportion of
sodium carbonate and other impurities. What is wanted in most cases is
merely a soluble cyanide, and it is a matter of indifference whether the base
be sodium or potassium. But since 49 parts of sodium cyanide (NaCN = 49)
are equivalent to 65 parts of potassium cyanide (KCN = 65) it is evident
that a pure sample of sodium cyanide would contain cyanide equivalent to
little less than 133 per cent. of potassium cyanide. Therefore a sample of
cyanide reported on in this way may be rich in cyanide, and yet have much
impurity.
The commonest impurity in commercial cyanide is carbonate of sodium or
potassium. This may be tested for by dissolving, say, 2 grams in a little
Page 209
water and adding barium chloride. There may be formed a white precipitate
of barium carbonate, which if filtered off, washed and treated with acid,
will dissolve with effervescence. Cyanate may be tested for in the solution
from which the barium carbonate has been filtered by adding a little soda
and boiling; if cyanates are present they decompose, giving off ammonia
(which may be tested for in the steam) and yielding a further precipitate of
barium carbonate.[37] If the soda alone gave a further precipitate of barium
carbonate, this may, perhaps, be due to the presence of bicarbonates.
Alkaline sulphides may be present in small quantity in commercial cyanide.
Their presence is shown at once when the sample is being tested for its
strength in cyanide, inasmuch as the first few drops of silver nitrate solution
produce at once a darkening of the liquor. A special test for sulphide may be
made by adding a drop or two of solution of acetate of lead to four or five
c.c. of soda solution and adding this to a clear solution of the suspected
cyanide. This will cause a black precipitate or colour, if any sulphide is
present.
The cyanides of the heavier metals combine with the alkaline cyanides to
form double cyanides. Some of these, ferrocyanide and ferricyanide of
potassium for example, have such characteristic properties that the fact that
they are cyanides may be overlooked. Others, such as potassium zinc
cyanide (K2ZnCy4), have much less distinctiveness: they behave more or
less as a mixture of two cyanides and are, moreover, so easily decomposed
that it may be doubted if they can exist in dilute alkaline solutions. In
reporting the cyanide strength of a cyanide liquor as equivalent to so much
per cent. of potassium cyanide, there is a question as to whether the cyanide
present in the form of any of these double cyanides should be taken into
account. It must be remembered that the object of the assay is not to learn
how much of the cyanide exists in the solution as actual potassium cyanide;
reporting the strength in terms of this salt is a mere matter of convenience;
what is really desired is to know how much of the cyanide present in the
liquor is "free" or "available" for the purposes of dissolving gold. Every one
is agreed as to the exclusion of such cyanides as the following: potassium
ferrocyanide (K4FeCy6), potassium ferricyanide (K3FeCy6), potassium
silver cyanide (KAgCy2), and potassium aurocyanide (KAuCy2); and the
double cyanides with copper or nickel. But with cyanide liquors containing
zinc the position is less satisfactory. One method of assay gives a lower
of barium carbonate, which if filtered off, washed and treated with acid,
will dissolve with effervescence. Cyanate may be tested for in the solution
from which the barium carbonate has been filtered by adding a little soda
and boiling; if cyanates are present they decompose, giving off ammonia
(which may be tested for in the steam) and yielding a further precipitate of
barium carbonate.[37] If the soda alone gave a further precipitate of barium
carbonate, this may, perhaps, be due to the presence of bicarbonates.
Alkaline sulphides may be present in small quantity in commercial cyanide.
Their presence is shown at once when the sample is being tested for its
strength in cyanide, inasmuch as the first few drops of silver nitrate solution
produce at once a darkening of the liquor. A special test for sulphide may be
made by adding a drop or two of solution of acetate of lead to four or five
c.c. of soda solution and adding this to a clear solution of the suspected
cyanide. This will cause a black precipitate or colour, if any sulphide is
present.
The cyanides of the heavier metals combine with the alkaline cyanides to
form double cyanides. Some of these, ferrocyanide and ferricyanide of
potassium for example, have such characteristic properties that the fact that
they are cyanides may be overlooked. Others, such as potassium zinc
cyanide (K2ZnCy4), have much less distinctiveness: they behave more or
less as a mixture of two cyanides and are, moreover, so easily decomposed
that it may be doubted if they can exist in dilute alkaline solutions. In
reporting the cyanide strength of a cyanide liquor as equivalent to so much
per cent. of potassium cyanide, there is a question as to whether the cyanide
present in the form of any of these double cyanides should be taken into
account. It must be remembered that the object of the assay is not to learn
how much of the cyanide exists in the solution as actual potassium cyanide;
reporting the strength in terms of this salt is a mere matter of convenience;
what is really desired is to know how much of the cyanide present in the
liquor is "free" or "available" for the purposes of dissolving gold. Every one
is agreed as to the exclusion of such cyanides as the following: potassium
ferrocyanide (K4FeCy6), potassium ferricyanide (K3FeCy6), potassium
silver cyanide (KAgCy2), and potassium aurocyanide (KAuCy2); and the
double cyanides with copper or nickel. But with cyanide liquors containing
zinc the position is less satisfactory. One method of assay gives a lower
Page 210
proportion of cyanide when this metal is present; and the loss of available
cyanide thus reported depends, though in a fitful and uncertain way, upon
the quantity of zinc present. The other method of assay reports as full a
strength in cyanide as if no zinc were present. Unfortunately, using both
methods and accepting the difference in the results as a measure of the
quantity of zinc present, or at any rate of the zinc present as cyanide, is not
satisfactory. It appears best to use the method which ignores the zinc; and to
determine the amount of zinc by a special assay of the liquor for this metal.
The cyanide present as hydrogen cyanide or prussic acid (HCy) is
practically useless as a gold solvent. Hence any report on the strength of a
cyanide liquor which assigned to this the same value as its equivalent of
alkaline cyanide would be misleading. On the other hand, it is "available
cyanide" inasmuch as a proper addition of sodium hydrate[38] would restore
its value. The question of the presence or absence of free prussic acid is
involved in the larger one as to whether the cyanide solution has the right
degree of alkalinity. The assay for "cyanide" should include the hydrogen
cyanide with the rest.
A rough test of the power of a cyanide liquor for dissolving gold may be
made by floating a gold leaf on its surface and noting the time required for
its solution. This test might, perhaps, be improved by taking, say, 20 c.c. of
the liquor and adding three or four gold leaves so that the gold shall always
be in considerable excess. The liquor should not be diluted as this will
affect the result. It should be allowed to stand for a definite time, say at
least two or three hours, or better, that corresponding to the time the liquor
is left in contact with the ore in actual practice. The liquor should then be
filtered off and, with the washings, be evaporated in a lead dish as in the
assay of cyanide liquors for gold (p. 141). The gold obtained on cupelling,
less any gold and silver originally present in the liquor, would be the
measure of the gold dissolving power.
THE ASSAY FOR CYANIDE BY TITRATION WITH SILVER
NITRATE.
The determination of the quantity of a cyanide is made by finding how
much silver nitrate is required to convert the whole of the cyanide into
cyanide thus reported depends, though in a fitful and uncertain way, upon
the quantity of zinc present. The other method of assay reports as full a
strength in cyanide as if no zinc were present. Unfortunately, using both
methods and accepting the difference in the results as a measure of the
quantity of zinc present, or at any rate of the zinc present as cyanide, is not
satisfactory. It appears best to use the method which ignores the zinc; and to
determine the amount of zinc by a special assay of the liquor for this metal.
The cyanide present as hydrogen cyanide or prussic acid (HCy) is
practically useless as a gold solvent. Hence any report on the strength of a
cyanide liquor which assigned to this the same value as its equivalent of
alkaline cyanide would be misleading. On the other hand, it is "available
cyanide" inasmuch as a proper addition of sodium hydrate[38] would restore
its value. The question of the presence or absence of free prussic acid is
involved in the larger one as to whether the cyanide solution has the right
degree of alkalinity. The assay for "cyanide" should include the hydrogen
cyanide with the rest.
A rough test of the power of a cyanide liquor for dissolving gold may be
made by floating a gold leaf on its surface and noting the time required for
its solution. This test might, perhaps, be improved by taking, say, 20 c.c. of
the liquor and adding three or four gold leaves so that the gold shall always
be in considerable excess. The liquor should not be diluted as this will
affect the result. It should be allowed to stand for a definite time, say at
least two or three hours, or better, that corresponding to the time the liquor
is left in contact with the ore in actual practice. The liquor should then be
filtered off and, with the washings, be evaporated in a lead dish as in the
assay of cyanide liquors for gold (p. 141). The gold obtained on cupelling,
less any gold and silver originally present in the liquor, would be the
measure of the gold dissolving power.
THE ASSAY FOR CYANIDE BY TITRATION WITH SILVER
NITRATE.
The determination of the quantity of a cyanide is made by finding how
much silver nitrate is required to convert the whole of the cyanide into
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potassium silver cyanide[39] or one of the allied compounds. It will be seen
from the equation that 170 parts by weight of silver nitrate are required for
130 parts by weight of potassium cyanide. As already explained it is
customary to report the cyanide-strength in terms of potassium cyanide,
even when only the sodium salt is present. One gram of potassium cyanide
will require 1.3076 gram of silver nitrate. The standard solution of silver
nitrate is made by dissolving 13.076 grams of silver nitrate in distilled
water and diluting to 1 litre; 100 c.c. of such a solution are equivalent to 1
gram of potassium cyanide.[40]
The titration is performed in the usual way, running the standard solution of
silver nitrate into a solution containing a known weight or volume of the
material containing the cyanide. The finishing point is determined in one of
two ways, both of which are largely used. In the first place, as long as there
remains any free cyanide in the solution the silver nitrate will combine with
it forming the double cyanide and yielding a clear solution; but as soon as
all the free cyanide is used up the silver nitrate will react with the double
cyanide[41] forming silver cyanide, which separates as a white precipitate
and renders the solution turbid. But, in the second place, if potassium iodide
is present in the solution the excess of silver nitrate will react with it,[42]
rather than with the double cyanide; and silver iodide will separate as a
yellowish turbidity which is easily recognised.
In working with pure solutions, the two finishing points give the same
results; and this is true even when there is much difference in the degree of
dilution. The finishing point with the iodide, however, has an advantage in
precision. Moreover, it is but little affected by variations in alkalinity, which
render the other finishing point quite useless. The great difference between
the two is shown when zinc is present in the solution. In this case, when
working without the iodide, the first appearance of a turbidity is less
distinct; the turbidity increases on standing and as a finishing point is
unsatisfactory. It can be determined with precision only by very systematic
working and after some experience. The turbidity is due to the separation of
an insoluble zinc compound. A most important point (to which reference
has already been made) is that less silver nitrate is required to give this
turbidity and, consequently, a lower strength in cyanide is reported. On the
from the equation that 170 parts by weight of silver nitrate are required for
130 parts by weight of potassium cyanide. As already explained it is
customary to report the cyanide-strength in terms of potassium cyanide,
even when only the sodium salt is present. One gram of potassium cyanide
will require 1.3076 gram of silver nitrate. The standard solution of silver
nitrate is made by dissolving 13.076 grams of silver nitrate in distilled
water and diluting to 1 litre; 100 c.c. of such a solution are equivalent to 1
gram of potassium cyanide.[40]
The titration is performed in the usual way, running the standard solution of
silver nitrate into a solution containing a known weight or volume of the
material containing the cyanide. The finishing point is determined in one of
two ways, both of which are largely used. In the first place, as long as there
remains any free cyanide in the solution the silver nitrate will combine with
it forming the double cyanide and yielding a clear solution; but as soon as
all the free cyanide is used up the silver nitrate will react with the double
cyanide[41] forming silver cyanide, which separates as a white precipitate
and renders the solution turbid. But, in the second place, if potassium iodide
is present in the solution the excess of silver nitrate will react with it,[42]
rather than with the double cyanide; and silver iodide will separate as a
yellowish turbidity which is easily recognised.
In working with pure solutions, the two finishing points give the same
results; and this is true even when there is much difference in the degree of
dilution. The finishing point with the iodide, however, has an advantage in
precision. Moreover, it is but little affected by variations in alkalinity, which
render the other finishing point quite useless. The great difference between
the two is shown when zinc is present in the solution. In this case, when
working without the iodide, the first appearance of a turbidity is less
distinct; the turbidity increases on standing and as a finishing point is
unsatisfactory. It can be determined with precision only by very systematic
working and after some experience. The turbidity is due to the separation of
an insoluble zinc compound. A most important point (to which reference
has already been made) is that less silver nitrate is required to give this
turbidity and, consequently, a lower strength in cyanide is reported. On the
Page 212
other hand, as much silver nitrate is required to give the yellow turbidity
due to silver iodide as would be required if no zinc were present.
Unfortunately the difference in the two titrations does not depend merely on
the quantity of zinc present; as it is also influenced by the extent of dilution,
the degree of alkalinity of the solution, and the quantity of cyanide present.
In an experiment with .055 gram of zinc sulphate and .1 gram of potassium
cyanide the difference in the two finishing points was only .1 c.c.; whereas
with .4 gram of potassium cyanide, the other conditions being the same, the
difference was 1.5 c.c. of standard silver nitrate. On the assumption that all
the zinc was present as potassium zinc cyanide (K2ZnCy4) the difference
should have been 5 c.c. in each case. Again, repeating the experiment with
.4 gram of potassium cyanide, but with .11 gram of crystallised zinc
sulphate, the difference was 6.5 c.c.: that is, merely doubling the quantity of
zinc increased the difference by more than four times. Hence it would
appear better to use the method with the iodide and make a separate assay
for the zinc. But since the student may be called on to use the other method,
he is advised to practice it also.
The assay without iodide.—The standard solution of silver nitrate is
placed in a small burette divided into tenths of a c.c. Ten c.c. of the cyanide
solution to be assayed is transferred to a small flask and diluted with water
to about 70 c.c. The silver solution is then run in from the burette (with
constant shaking of the flask), a little at a time but somewhat rapidly, until a
permanent turbidity appears. Since 1 c.c. of the silver nitrate solution
corresponds to .01 gram of potassium cyanide, it also corresponds to .1 per
cent. of this salt counted on the 10 c.c. of cyanide solution taken. The
titration should be performed in a fairly good uniform light. The learner
should practice on a fairly pure solution of potassium cyanide at first, and
this may conveniently have a strength of about 1 per cent. For practice with
solutions containing zinc make a solution containing 1.1 gram of
crystallised zinc sulphate in 100 c.c. and slowly add measured quantities of
from 1 to 5 c.c. of this to the 10 c.c. of cyanide liquor before diluting for the
titration.
If a cyanide solution blackens on the addition of the silver nitrate it contains
sulphide. In this case, shake up a considerable bulk of the liquor with a few
due to silver iodide as would be required if no zinc were present.
Unfortunately the difference in the two titrations does not depend merely on
the quantity of zinc present; as it is also influenced by the extent of dilution,
the degree of alkalinity of the solution, and the quantity of cyanide present.
In an experiment with .055 gram of zinc sulphate and .1 gram of potassium
cyanide the difference in the two finishing points was only .1 c.c.; whereas
with .4 gram of potassium cyanide, the other conditions being the same, the
difference was 1.5 c.c. of standard silver nitrate. On the assumption that all
the zinc was present as potassium zinc cyanide (K2ZnCy4) the difference
should have been 5 c.c. in each case. Again, repeating the experiment with
.4 gram of potassium cyanide, but with .11 gram of crystallised zinc
sulphate, the difference was 6.5 c.c.: that is, merely doubling the quantity of
zinc increased the difference by more than four times. Hence it would
appear better to use the method with the iodide and make a separate assay
for the zinc. But since the student may be called on to use the other method,
he is advised to practice it also.
The assay without iodide.—The standard solution of silver nitrate is
placed in a small burette divided into tenths of a c.c. Ten c.c. of the cyanide
solution to be assayed is transferred to a small flask and diluted with water
to about 70 c.c. The silver solution is then run in from the burette (with
constant shaking of the flask), a little at a time but somewhat rapidly, until a
permanent turbidity appears. Since 1 c.c. of the silver nitrate solution
corresponds to .01 gram of potassium cyanide, it also corresponds to .1 per
cent. of this salt counted on the 10 c.c. of cyanide solution taken. The
titration should be performed in a fairly good uniform light. The learner
should practice on a fairly pure solution of potassium cyanide at first, and
this may conveniently have a strength of about 1 per cent. For practice with
solutions containing zinc make a solution containing 1.1 gram of
crystallised zinc sulphate in 100 c.c. and slowly add measured quantities of
from 1 to 5 c.c. of this to the 10 c.c. of cyanide liquor before diluting for the
titration.
If a cyanide solution blackens on the addition of the silver nitrate it contains
sulphide. In this case, shake up a considerable bulk of the liquor with a few
Page 213
grams of lead carbonate, allow to settle and make the assay on 10 c.c. of the
clear liquor.
If the cyanide liquor be suspected to contain free prussic acid, take 10 c.c.
for the assay as usual; but, before titrating, add .1 or .2 gram of sodium
carbonate. On no condition must caustic soda or ammonia be added. The
difference between the results, with and without the addition of carbonate of
soda, is supposed to measure the quantity of free prussic acid. If this has to
be reported it is best done as "prussic acid equivalent to ... per cent. of
potassium cyanide." Suppose, for example, the difference in the two
titrations equals 1 c.c. of standard silver nitrate; the prussic acid found
would be equivalent to .1 per cent. of potassium cyanide.
The assay with iodide.—The standard solution of silver nitrate is placed in
a burette divided into tenths of a c.c. Take 10 c.c. of the cyanide liquor,
which should previously have been treated with white lead for the removal
of sulphides if these happened to be present. Transfer to a small flask, add 3
or 4 drops of a solution of potassium iodide and 2 or 3 c.c. of a solution of
sodium hydrate; dilute to 60 or 70 c.c. with water. If much zinc is present
the soda may be increased to 20 or 30 c.c. with advantage. The standard
solution should be run in somewhat rapidly, but a little at a time, so that the
precipitate at first formed shall be small and have only a momentary
existence. The titration is continued until there is a permanent yellowish
turbidity. The most satisfactory and exact finish is got by ignoring any faint
suspicion of a turbidity and accepting the unmistakable turbidity which the
next drop of silver nitrate is sure to produce. This finishing point gives
results which are exactly proportional to the quantity of cyanide present;
and it can be recognised with more than ordinary precision even in
solutions which are not otherwise perfectly clear.
Each c.c. of the standard silver nitrate solution corresponds to .01 gram of
potassium cyanide; and if 10 c.c. of the liquor are taken for assay this
corresponds to .1 per cent. or 2 lbs. to the short ton or 2.24 lbs. to the long
ton. As already explained the result should be reported as "cyanide
equivalent to so much per cent. of potassium cyanide."
The following experimental results were obtained with a solution of
potassium cyanide made up to contain about 1.2 per cent. of the salt.
clear liquor.
If the cyanide liquor be suspected to contain free prussic acid, take 10 c.c.
for the assay as usual; but, before titrating, add .1 or .2 gram of sodium
carbonate. On no condition must caustic soda or ammonia be added. The
difference between the results, with and without the addition of carbonate of
soda, is supposed to measure the quantity of free prussic acid. If this has to
be reported it is best done as "prussic acid equivalent to ... per cent. of
potassium cyanide." Suppose, for example, the difference in the two
titrations equals 1 c.c. of standard silver nitrate; the prussic acid found
would be equivalent to .1 per cent. of potassium cyanide.
The assay with iodide.—The standard solution of silver nitrate is placed in
a burette divided into tenths of a c.c. Take 10 c.c. of the cyanide liquor,
which should previously have been treated with white lead for the removal
of sulphides if these happened to be present. Transfer to a small flask, add 3
or 4 drops of a solution of potassium iodide and 2 or 3 c.c. of a solution of
sodium hydrate; dilute to 60 or 70 c.c. with water. If much zinc is present
the soda may be increased to 20 or 30 c.c. with advantage. The standard
solution should be run in somewhat rapidly, but a little at a time, so that the
precipitate at first formed shall be small and have only a momentary
existence. The titration is continued until there is a permanent yellowish
turbidity. The most satisfactory and exact finish is got by ignoring any faint
suspicion of a turbidity and accepting the unmistakable turbidity which the
next drop of silver nitrate is sure to produce. This finishing point gives
results which are exactly proportional to the quantity of cyanide present;
and it can be recognised with more than ordinary precision even in
solutions which are not otherwise perfectly clear.
Each c.c. of the standard silver nitrate solution corresponds to .01 gram of
potassium cyanide; and if 10 c.c. of the liquor are taken for assay this
corresponds to .1 per cent. or 2 lbs. to the short ton or 2.24 lbs. to the long
ton. As already explained the result should be reported as "cyanide
equivalent to so much per cent. of potassium cyanide."
The following experimental results were obtained with a solution of
potassium cyanide made up to contain about 1.2 per cent. of the salt.
Page 214
Effect of varying cyanide.—The bulk before titration was in each case 60
c.c.; 2 c.c. of soda and 3 drops of potassium iodide were used in each case.
Cyanide added 40 c.c. 30 c.c. 20 c.c. 10 c.c. 5 c.c. 1 c.c.
Silver required 47.0 c.c. 35.25 c.c. 23.5 c.c. 11.7 c.c. 5.8 c.c. 1.15 c.c.
Accepting the result for 40 c.c. as correct, the others are in very satisfactory
agreement.
Effect of varying dilution.—The conditions were those of the 40 c.c.
experiment in the last series; but varying amounts of water were used in
diluting.
Water added none 100 c.c. 200 c.c. 400 c.c.
Silver required 47.0 c.c. 47.0 c.c. 47.0 c.c. 47.05 c.c.
Very considerable dilution therefore has no effect.
Effect of varying soda.—The conditions were those of the 40 c.c.
experiment in the first series, except that varying amounts of soda solution
were used.
Soda added none 10 c.c. 30 c.c.
Silver required 46.95 c.c. 47.0 c.c. 47.0 c.c.
This alkali therefore has no prejudicial effect.
Effect of ammonia.—Soda causes turbidity in some cyanide liquors; with
these it should be replaced by 2 or 3 c.c. of dilute ammonia with a gram or
so of ammonium chloride. The following experiments with dilute ammonia
show that larger quantities of this reagent must be avoided.
Ammonia added none 10 c.c. 30 c.c. 60 c.c.
Silver required 46.95 c.c. 47.15 c.c. 47.7 c.c. 49.5 c.c.
Effect of sodium bicarbonate.—In this experiment 1 gram of bicarbonate
of soda was used instead of the soda or ammonia of the other experiments.
The silver nitrate required was only 46.45 c.c. instead of the 47.0 c.c. which
c.c.; 2 c.c. of soda and 3 drops of potassium iodide were used in each case.
Cyanide added 40 c.c. 30 c.c. 20 c.c. 10 c.c. 5 c.c. 1 c.c.
Silver required 47.0 c.c. 35.25 c.c. 23.5 c.c. 11.7 c.c. 5.8 c.c. 1.15 c.c.
Accepting the result for 40 c.c. as correct, the others are in very satisfactory
agreement.
Effect of varying dilution.—The conditions were those of the 40 c.c.
experiment in the last series; but varying amounts of water were used in
diluting.
Water added none 100 c.c. 200 c.c. 400 c.c.
Silver required 47.0 c.c. 47.0 c.c. 47.0 c.c. 47.05 c.c.
Very considerable dilution therefore has no effect.
Effect of varying soda.—The conditions were those of the 40 c.c.
experiment in the first series, except that varying amounts of soda solution
were used.
Soda added none 10 c.c. 30 c.c.
Silver required 46.95 c.c. 47.0 c.c. 47.0 c.c.
This alkali therefore has no prejudicial effect.
Effect of ammonia.—Soda causes turbidity in some cyanide liquors; with
these it should be replaced by 2 or 3 c.c. of dilute ammonia with a gram or
so of ammonium chloride. The following experiments with dilute ammonia
show that larger quantities of this reagent must be avoided.
Ammonia added none 10 c.c. 30 c.c. 60 c.c.
Silver required 46.95 c.c. 47.15 c.c. 47.7 c.c. 49.5 c.c.
Effect of sodium bicarbonate.—In this experiment 1 gram of bicarbonate
of soda was used instead of the soda or ammonia of the other experiments.
The silver nitrate required was only 46.45 c.c. instead of the 47.0 c.c. which
Page 215
is the normal result. This is probably due to the liberation of prussic acid
and shows the importance of having the solution alkaline.
Effect of zinc.—In each experiment 40 c.c. of the cyanide solution and .5
gram of zinc sulphate crystals were used and the bulk was made up to 100
c.c. before titrating.
and shows the importance of having the solution alkaline.
Effect of zinc.—In each experiment 40 c.c. of the cyanide solution and .5
gram of zinc sulphate crystals were used and the bulk was made up to 100
c.c. before titrating.
Page 216
Soda added 1 c.c. 5 c.c. 10 c.c. 25 c.c.
Silver required 47.1 c.c. 47.0 c.c. 46.9 c.c. 46.9 c.c.
The work was easier with the more alkaline solutions. The titration in the
presence of zinc is comparatively easy, but, in learning it, it is well to have
a burette with cyanide so that if a titration be overdone it can be brought
back by the addition of 1 or 2 c.c. more cyanide and the finish repeated; a
quarter of an hour's work in this way will ensure confidence in the method.
Effect of other substances.—It was found that an alkaline cyanate,
sulphocyanate, ferrocyanide, nitrite, borate, silicate or carbonate has no
effect. The ferricyanide had a small influence and, as might be expected,
hyposulphite is fatal to the assay. The addition of salts of lead and cadmium
was without effect. On the other hand, nickel produces its full effect; and
the quantity of nickel added can be calculated with accuracy from the extent
of its interference with the titration.
Assay of commercial cyanide of potassium.—Break off 20 or 30 grams of
the cyanide in clean fresh pieces, weigh accurately to the nearest centigram.
Dissolve in water containing a little sodium hydroxide; transfer to a 2-litre
flask: dilute to 2 litres; add a few grams of white lead; shake up and allow
to settle. Run 50 c.c. of the clear liquor from a burette into an 8 oz. flask;
add 2 or 3 c.c. of soda solution and 3 drops of potassium iodide. Titrate with
the standard solution of silver nitrate. The percentage may be calculated by
multiplying the number of c.c. used by 40 (50 c.c. is one fortieth of the 2
litres) and dividing by the weight of commercial cyanide originally taken.
Alkalinity of commercial potassium cyanide and of cyanide solutions.—
Hydrocyanic acid like carbonic acid has no action on methyl-orange;[43]
hence the alkaline cyanides may be titrated with "normal acid" as easily as
the carbonates or hydrates. 100 c.c. of normal acid will neutralise 6.5 grams
of pure potassium cyanide.[44] A solution of commercial cyanide prepared
as for the assay last described, but best without the addition of white lead,
may be used for the test. Take 50 c.c. of it; tint faintly yellow with methyl-
orange and titrate with normal acid till the liquor acquires a permanent
reddish tint. In the case of the purer samples of cyanide the quantity of acid
used will correspond exactly with that required to neutralise the actual
quantity of cyanide present as determined by the assay with nitrate of silver.
Silver required 47.1 c.c. 47.0 c.c. 46.9 c.c. 46.9 c.c.
The work was easier with the more alkaline solutions. The titration in the
presence of zinc is comparatively easy, but, in learning it, it is well to have
a burette with cyanide so that if a titration be overdone it can be brought
back by the addition of 1 or 2 c.c. more cyanide and the finish repeated; a
quarter of an hour's work in this way will ensure confidence in the method.
Effect of other substances.—It was found that an alkaline cyanate,
sulphocyanate, ferrocyanide, nitrite, borate, silicate or carbonate has no
effect. The ferricyanide had a small influence and, as might be expected,
hyposulphite is fatal to the assay. The addition of salts of lead and cadmium
was without effect. On the other hand, nickel produces its full effect; and
the quantity of nickel added can be calculated with accuracy from the extent
of its interference with the titration.
Assay of commercial cyanide of potassium.—Break off 20 or 30 grams of
the cyanide in clean fresh pieces, weigh accurately to the nearest centigram.
Dissolve in water containing a little sodium hydroxide; transfer to a 2-litre
flask: dilute to 2 litres; add a few grams of white lead; shake up and allow
to settle. Run 50 c.c. of the clear liquor from a burette into an 8 oz. flask;
add 2 or 3 c.c. of soda solution and 3 drops of potassium iodide. Titrate with
the standard solution of silver nitrate. The percentage may be calculated by
multiplying the number of c.c. used by 40 (50 c.c. is one fortieth of the 2
litres) and dividing by the weight of commercial cyanide originally taken.
Alkalinity of commercial potassium cyanide and of cyanide solutions.—
Hydrocyanic acid like carbonic acid has no action on methyl-orange;[43]
hence the alkaline cyanides may be titrated with "normal acid" as easily as
the carbonates or hydrates. 100 c.c. of normal acid will neutralise 6.5 grams
of pure potassium cyanide.[44] A solution of commercial cyanide prepared
as for the assay last described, but best without the addition of white lead,
may be used for the test. Take 50 c.c. of it; tint faintly yellow with methyl-
orange and titrate with normal acid till the liquor acquires a permanent
reddish tint. In the case of the purer samples of cyanide the quantity of acid
used will correspond exactly with that required to neutralise the actual
quantity of cyanide present as determined by the assay with nitrate of silver.
Page 217
The less pure samples will show an excess of alkalinity because of the
presence of sodium carbonate or of potassium carbonate.
In comparing the alkalinity and cyanide strength of a solution the simplest
plan is to take 65 c.c. of the solution and titrate with normal acid; for in this
case each c.c. of normal acid corresponds to .1 per cent. of potassium
cyanide. In systematic assays of this kind, the alkalinity would no doubt be
generally in excess of that required by the cyanide present: there would be
no inconvenience in recording such excess in terms of potassium cyanide.
Determination of the acidity of an ore.—Most ores have the power of
destroying more or less of the alkalinity of a cyanide solution and in a
proportionate degree of damaging its efficiency. An assay is needed to
determine how much lime or soda must be added for each ton of ore in
order to counteract this. Whether this acidity should be reported in terms of
the lime or of the soda required to neutralise it will depend on which of
these reagents is to be used in the actual practice. Again, if the ore is
washed with water before treating with cyanide on the large scale, then the
assay should be made of the acidity of the ore after a similar washing.
The standard solutions of acid and alkali used for this determination may
be one-fifth normal. 200 c.c. of the normal solution should be diluted to 1
litre in each case, 1 c.c. of the resulting solutions would be equivalent to 8
milligrams of soda (NaHO) or 5.6 milligrams of lime, CaO. It must be
remembered this refers to the pure bases in each case. Suppose it is desired
to report as so many lbs. of lime to the short ton (2000 lbs.) of ore. Since 1
c.c. of the standard solution is equivalent to 5.6 milligrams of lime, if we
take 2000 times this weight of ore (i.e. 11,200 milligrams or 11.2 grams) for
the assay, each c.c. of standard solution will be equivalent to 1 lb. of lime to
the short ton.[45]
Total acidity.—Weigh out 11.2 grams of the ore, place them in a four-inch
evaporating dish and measure on to it from a burette 10 or 20 c.c. of the
standard solution of soda. Stir the soda solution into the ore and allow to
stand for 15 or 20 minutes with occasional stirring. Stir up with 30 or 40
c.c. of water, float a piece of litmus paper on the liquid and titrate with the
standard solution of acid. If the ore is strictly neutral the quantity of "acid"
required to redden the litmus will be the same as the quantity of "soda"
presence of sodium carbonate or of potassium carbonate.
In comparing the alkalinity and cyanide strength of a solution the simplest
plan is to take 65 c.c. of the solution and titrate with normal acid; for in this
case each c.c. of normal acid corresponds to .1 per cent. of potassium
cyanide. In systematic assays of this kind, the alkalinity would no doubt be
generally in excess of that required by the cyanide present: there would be
no inconvenience in recording such excess in terms of potassium cyanide.
Determination of the acidity of an ore.—Most ores have the power of
destroying more or less of the alkalinity of a cyanide solution and in a
proportionate degree of damaging its efficiency. An assay is needed to
determine how much lime or soda must be added for each ton of ore in
order to counteract this. Whether this acidity should be reported in terms of
the lime or of the soda required to neutralise it will depend on which of
these reagents is to be used in the actual practice. Again, if the ore is
washed with water before treating with cyanide on the large scale, then the
assay should be made of the acidity of the ore after a similar washing.
The standard solutions of acid and alkali used for this determination may
be one-fifth normal. 200 c.c. of the normal solution should be diluted to 1
litre in each case, 1 c.c. of the resulting solutions would be equivalent to 8
milligrams of soda (NaHO) or 5.6 milligrams of lime, CaO. It must be
remembered this refers to the pure bases in each case. Suppose it is desired
to report as so many lbs. of lime to the short ton (2000 lbs.) of ore. Since 1
c.c. of the standard solution is equivalent to 5.6 milligrams of lime, if we
take 2000 times this weight of ore (i.e. 11,200 milligrams or 11.2 grams) for
the assay, each c.c. of standard solution will be equivalent to 1 lb. of lime to
the short ton.[45]
Total acidity.—Weigh out 11.2 grams of the ore, place them in a four-inch
evaporating dish and measure on to it from a burette 10 or 20 c.c. of the
standard solution of soda. Stir the soda solution into the ore and allow to
stand for 15 or 20 minutes with occasional stirring. Stir up with 30 or 40
c.c. of water, float a piece of litmus paper on the liquid and titrate with the
standard solution of acid. If the ore is strictly neutral the quantity of "acid"
required to redden the litmus will be the same as the quantity of "soda"
Page 218
originally used. If the ore is acid, less acid will be used. For example, if 10
c.c. of soda were used and only 7 c.c. of acid were required, the ore will
have done the work of the remaining 3 c.c. of acid. And the ton of ore will
require 3 lbs. of lime to neutralise its acidity.
Acidity after washing.—Take 11.2 grams of the ore; wash thoroughly with
water and immediately treat the residue, without drying, exactly as just
described.
Examination of cyanide solutions for metals, &c.—Take a measured
quantity of the solution, say 20 c.c.[46] and evaporate in a small dish with,
say, half a c.c. of strong sulphuric acid. Evaporate at first, on a water-bath in
a well ventilated place, but finish off with a naked Bunsen flame, using a
high temperature at the end in order to completely decompose the more
refractory double cyanides. Allow to cool; moisten with strong hydrochloric
acid; warm with a little water and test for the metals in the solution by the
ordinary methods. Since the quantities of the metals likely to be present
may be given in milligrams the work must be carefully performed. It may
be worth while to determine the proportions of lime and magnesia as well
as those of the metals proper.
Or the 20 c.c. of cyanide liquor may be evaporated with 5 c.c. of strong
nitric acid to dryness and gently ignited and the residue taken up with 2 or 3
c.c. of strong hydrochloric acid.
Copper, iron, and zinc can be rapidly determined in such a solution, as
follows. Dilute with water to 10 or 15 c.c., add an excess of ammonia, and
filter. The precipitate will contain the iron as ferric hydrate; dissolve it in a
little hot dilute sulphuric acid: reduce with sulphuretted hydrogen; boil off
the excess of gas, cool and titrate with standard potassium permanganate (p.
236). Determine the copper in the filtrate colorimetrically (p. 203); but
avoid further dilution. Then add dilute hydrochloric acid, so as to have an
excess of 4 or 5 c.c. after neutralising the ammonia; add some clean strips
of lead foil, and boil until the solution has for some time become colourless.
Titrate with standard potassium ferrocyanide (p. 263) without further
dilution, and bearing in mind that at most only one or two c.c. will be
required.
c.c. of soda were used and only 7 c.c. of acid were required, the ore will
have done the work of the remaining 3 c.c. of acid. And the ton of ore will
require 3 lbs. of lime to neutralise its acidity.
Acidity after washing.—Take 11.2 grams of the ore; wash thoroughly with
water and immediately treat the residue, without drying, exactly as just
described.
Examination of cyanide solutions for metals, &c.—Take a measured
quantity of the solution, say 20 c.c.[46] and evaporate in a small dish with,
say, half a c.c. of strong sulphuric acid. Evaporate at first, on a water-bath in
a well ventilated place, but finish off with a naked Bunsen flame, using a
high temperature at the end in order to completely decompose the more
refractory double cyanides. Allow to cool; moisten with strong hydrochloric
acid; warm with a little water and test for the metals in the solution by the
ordinary methods. Since the quantities of the metals likely to be present
may be given in milligrams the work must be carefully performed. It may
be worth while to determine the proportions of lime and magnesia as well
as those of the metals proper.
Or the 20 c.c. of cyanide liquor may be evaporated with 5 c.c. of strong
nitric acid to dryness and gently ignited and the residue taken up with 2 or 3
c.c. of strong hydrochloric acid.
Copper, iron, and zinc can be rapidly determined in such a solution, as
follows. Dilute with water to 10 or 15 c.c., add an excess of ammonia, and
filter. The precipitate will contain the iron as ferric hydrate; dissolve it in a
little hot dilute sulphuric acid: reduce with sulphuretted hydrogen; boil off
the excess of gas, cool and titrate with standard potassium permanganate (p.
236). Determine the copper in the filtrate colorimetrically (p. 203); but
avoid further dilution. Then add dilute hydrochloric acid, so as to have an
excess of 4 or 5 c.c. after neutralising the ammonia; add some clean strips
of lead foil, and boil until the solution has for some time become colourless.
Titrate with standard potassium ferrocyanide (p. 263) without further
dilution, and bearing in mind that at most only one or two c.c. will be
required.
Page 219
Examination of an ore for "cyanicides."—Place 100 grams of the ore
with 200 c.c. of a cyanide solution of known strength (say .1 or .2 per cent.)
in a bottle and agitate for a definite time, such as one or two days. Filter off
some of the liquor and assay for cyanide, using say 20 c.c. Calculate how
much cyanide has been destroyed in the operation. Evaporate 20 c.c. with
sulphuric or nitric acid and examine for metal. Test another portion for
sulphides, &c.
The student who has mastered the methods of assaying can greatly improve
himself by working out such problems as the above.
PLATINUM.
Platinum occurs in nature in alluvial deposits associated with gold and some
rare metals, generally in fine metallic grains, and, occasionally, in nuggets.
It is a grey metal with a high specific gravity, 21.5 when pure and about
18.0 in native specimens. It is fusible only at the highest temperature, and is
not acted on by acids.
It is dissolved by warm aqua regia, forming a solution of "platinic chloride,"
H2PtCl6. This substance on evaporation remains as a brownish red
deliquescent mass; on drying at 300° C. it is converted into platinous
chloride, PtCl2, and becomes insoluble, and at a higher temperature it is
converted into platinum. All platinum compounds yield the metal in this
way. Platinic chloride combines with other chlorides to form double salts,
of which the ammonic and potassic platino-chlorides are the most
important.
Platinum alone is not soluble in nitric acid; but when alloyed with other
metals which dissolve in this acid it too is dissolved; so that in gold parting,
for example, if platinum was present, some, or perhaps the whole of it
would go into solution with the silver. Such alloys, however, when treated
with hot sulphuric acid leave the platinum in the residue with the gold.
Platinum is detected when in the metallic state by its physical characters
and insolubility in acids. In alloys it may be found by dissolving them in
nitric acid or in aqua regia, evaporating with hydrochloric acid, and treating
with 200 c.c. of a cyanide solution of known strength (say .1 or .2 per cent.)
in a bottle and agitate for a definite time, such as one or two days. Filter off
some of the liquor and assay for cyanide, using say 20 c.c. Calculate how
much cyanide has been destroyed in the operation. Evaporate 20 c.c. with
sulphuric or nitric acid and examine for metal. Test another portion for
sulphides, &c.
The student who has mastered the methods of assaying can greatly improve
himself by working out such problems as the above.
PLATINUM.
Platinum occurs in nature in alluvial deposits associated with gold and some
rare metals, generally in fine metallic grains, and, occasionally, in nuggets.
It is a grey metal with a high specific gravity, 21.5 when pure and about
18.0 in native specimens. It is fusible only at the highest temperature, and is
not acted on by acids.
It is dissolved by warm aqua regia, forming a solution of "platinic chloride,"
H2PtCl6. This substance on evaporation remains as a brownish red
deliquescent mass; on drying at 300° C. it is converted into platinous
chloride, PtCl2, and becomes insoluble, and at a higher temperature it is
converted into platinum. All platinum compounds yield the metal in this
way. Platinic chloride combines with other chlorides to form double salts,
of which the ammonic and potassic platino-chlorides are the most
important.
Platinum alone is not soluble in nitric acid; but when alloyed with other
metals which dissolve in this acid it too is dissolved; so that in gold parting,
for example, if platinum was present, some, or perhaps the whole of it
would go into solution with the silver. Such alloys, however, when treated
with hot sulphuric acid leave the platinum in the residue with the gold.
Platinum is detected when in the metallic state by its physical characters
and insolubility in acids. In alloys it may be found by dissolving them in
nitric acid or in aqua regia, evaporating with hydrochloric acid, and treating
Page 220
the filtrate with ammonic chloride and alcohol. A heavy yellow precipitate
marks its presence.
The assay of bullion, or of an alloy containing platinum, may be made as
follows: Take 0.2 gram of the alloy and an equal weight of fine silver, cupel
with sheet lead, and weigh. The loss in weight, after deducting that of the
silver added, gives the weight of the base metals, copper, lead, &c. Flatten
the button and part by boiling with strong sulphuric acid for several
minutes. When cold, wash, anneal, and weigh. The weight is that of the
platinum and gold. The silver may be got by difference. Re-cupel the metal
thus got with 12 or 15 times its weight of silver, flatten and part the gold
with nitric acid in the usual way (see under Gold), and the platinum will
dissolve. The gold may contain an alloy of osmium and iridium; if so, it
should be weighed and treated with aqua regia. The osmiridium will remain
as an insoluble residue, which can be separated and weighed. Its weight
deducted from that previously ascertained will give the weight of the gold.
When the platinum only is required, the alloy must be dissolved by
prolonged treatment with aqua regia, the solution evaporated to dryness,
and the residue extracted with water. The solution thus obtained is treated
with ammonic chloride in large excess and with some alcohol. A sparingly
soluble[47] yellow ammonic platinum chloride is thrown down, mixed,
perhaps, with the corresponding salts of other metals of the platinum group.
Gold will be in solution. The solution is allowed to stand for some time, and
then the precipitate is filtered off, washed with alcohol, dried, and
transferred (wrapped in the filter paper) to a weighed crucible. It is ignited,
gently at first, as there is danger of volatilising some of the platinum
chloride, and afterwards intensely. With large quantities of platinum the
ignition should be performed in an atmosphere of hydrogen. Cool and
weigh as metallic platinum.
IRIDIUM
Occurs in nature alloyed with osmium as osmiridium or iridosmine, which
is "rather abundant in the auriferous beach sands of Northern California"
(Dana). It occurs in bright metallic scales, which do not alloy with lead, and
are insoluble in aqua regia. Iridium also occurs in most platinum ores, and
marks its presence.
The assay of bullion, or of an alloy containing platinum, may be made as
follows: Take 0.2 gram of the alloy and an equal weight of fine silver, cupel
with sheet lead, and weigh. The loss in weight, after deducting that of the
silver added, gives the weight of the base metals, copper, lead, &c. Flatten
the button and part by boiling with strong sulphuric acid for several
minutes. When cold, wash, anneal, and weigh. The weight is that of the
platinum and gold. The silver may be got by difference. Re-cupel the metal
thus got with 12 or 15 times its weight of silver, flatten and part the gold
with nitric acid in the usual way (see under Gold), and the platinum will
dissolve. The gold may contain an alloy of osmium and iridium; if so, it
should be weighed and treated with aqua regia. The osmiridium will remain
as an insoluble residue, which can be separated and weighed. Its weight
deducted from that previously ascertained will give the weight of the gold.
When the platinum only is required, the alloy must be dissolved by
prolonged treatment with aqua regia, the solution evaporated to dryness,
and the residue extracted with water. The solution thus obtained is treated
with ammonic chloride in large excess and with some alcohol. A sparingly
soluble[47] yellow ammonic platinum chloride is thrown down, mixed,
perhaps, with the corresponding salts of other metals of the platinum group.
Gold will be in solution. The solution is allowed to stand for some time, and
then the precipitate is filtered off, washed with alcohol, dried, and
transferred (wrapped in the filter paper) to a weighed crucible. It is ignited,
gently at first, as there is danger of volatilising some of the platinum
chloride, and afterwards intensely. With large quantities of platinum the
ignition should be performed in an atmosphere of hydrogen. Cool and
weigh as metallic platinum.
IRIDIUM
Occurs in nature alloyed with osmium as osmiridium or iridosmine, which
is "rather abundant in the auriferous beach sands of Northern California"
(Dana). It occurs in bright metallic scales, which do not alloy with lead, and
are insoluble in aqua regia. Iridium also occurs in most platinum ores, and
Page 221
forms as much as two per cent. of some commercial platinum. In chemical
properties it resembles platinum, but the ammonic irido-chloride has a dark
red colour, and on ignition leaves metallic iridium, which does not dissolve
in aqua regia diluted with four or five times its volume of water and heated
to a temperature of 40° or 50° C.
The other metals of the platinum group are Palladium, Rhodium, Osmium,
and Ruthenium. They differ from gold, platinum, and iridium by the
insolubility of their sulphides in a solution of sodium sulphide. Palladium is
distinguished by the insolubility of its iodide; and Osmium by the volatility
of its oxide on boiling with nitric acid.
MERCURY.
Mercury occurs native and, occasionally, alloyed with gold or silver in
natural amalgams; but its chief ore is the sulphide, cinnabar. It is
comparatively rare, being mined for only in a few districts. It is chiefly used
in the extraction of gold and silver from their ores (amalgamation); for
silvering mirrors, &c.
Mercury forms two series of salts, mercurous and mercuric, but for the
purposes of the assayer the most important property is the ease with which
it can be reduced to the metallic state from either of these. Mercury itself is
soluble in nitric acid, forming, when the acid is hot and strong, mercuric
nitrate. Cinnabar is soluble only in aqua regia. Mercurous salts are generally
insoluble, and may be converted into mercuric salts by prolonged boiling
with oxidising agents (nitric acid or aqua regia). The salts of mercury are
volatile, and, if heated with a reducing agent or some body capable of fixing
the acid, metallic mercury is given off, which may be condensed and
collected.
Mercury is separated from its solutions by zinc or copper, or it may be
thrown down by stannous chloride, which, when in excess, gives a grey
powder of metallic mercury, or, if dilute, a white crystalline precipitate of
mercurous chloride. Nitric acid solutions of mercury yield the metal on
electrolysis; and, if the pole on which the metal comes down be made of
gold or copper, or is coated with these, the separated mercury will adhere
thereto. It may then be washed and weighed.
properties it resembles platinum, but the ammonic irido-chloride has a dark
red colour, and on ignition leaves metallic iridium, which does not dissolve
in aqua regia diluted with four or five times its volume of water and heated
to a temperature of 40° or 50° C.
The other metals of the platinum group are Palladium, Rhodium, Osmium,
and Ruthenium. They differ from gold, platinum, and iridium by the
insolubility of their sulphides in a solution of sodium sulphide. Palladium is
distinguished by the insolubility of its iodide; and Osmium by the volatility
of its oxide on boiling with nitric acid.
MERCURY.
Mercury occurs native and, occasionally, alloyed with gold or silver in
natural amalgams; but its chief ore is the sulphide, cinnabar. It is
comparatively rare, being mined for only in a few districts. It is chiefly used
in the extraction of gold and silver from their ores (amalgamation); for
silvering mirrors, &c.
Mercury forms two series of salts, mercurous and mercuric, but for the
purposes of the assayer the most important property is the ease with which
it can be reduced to the metallic state from either of these. Mercury itself is
soluble in nitric acid, forming, when the acid is hot and strong, mercuric
nitrate. Cinnabar is soluble only in aqua regia. Mercurous salts are generally
insoluble, and may be converted into mercuric salts by prolonged boiling
with oxidising agents (nitric acid or aqua regia). The salts of mercury are
volatile, and, if heated with a reducing agent or some body capable of fixing
the acid, metallic mercury is given off, which may be condensed and
collected.
Mercury is separated from its solutions by zinc or copper, or it may be
thrown down by stannous chloride, which, when in excess, gives a grey
powder of metallic mercury, or, if dilute, a white crystalline precipitate of
mercurous chloride. Nitric acid solutions of mercury yield the metal on
electrolysis; and, if the pole on which the metal comes down be made of
gold or copper, or is coated with these, the separated mercury will adhere
thereto. It may then be washed and weighed.
Page 222
The best tests for mercury next to obtaining globules of the metal are: (1) a
black precipitate with sulphuretted hydrogen from acid solutions, which is
insoluble in nitric acid; and (2) a white precipitate with stannous chloride.
DRY METHOD.
Weigh up 5 grams, if the ore is rich, or 10 grams, if a poorer mineral. Take a
piece of combustion tube from 18 inches to 2 feet long, closed at one end,
and place in it some powdered magnesite, so as to fill it to a depth of 2 or 3
inches, and on that a layer of an equal quantity of powdered lime (not
slaked). Mix the weighed sample of ore in a mortar with 10 grams of finely
powdered lime and transfer to the tube; rinse out the mortar with a little
more lime, and add the rinsings. Cover with a layer of six or seven inches
more lime and a loosely fitting plug of asbestos. Draw out the tube before
the blowpipe to the shape shown in fig. 47, avoiding the formation of a
ridge or hollow at the bend which might collect the mercury. Tap gently,
holding the tube nearly horizontal, so as to allow sufficient space above the
mixture for the passage of the gases and vapours which are formed. Place
the tube in a "tube furnace," and, when in position, place a small beaker of
water so that it shall just close the opening of the tube. The point of the tube
should not more than touch the surface of the water. Bring the tube
gradually to a red heat, commencing by heating the lime just behind the
asbestos plug, and travelling slowly backwards. When the portion of the
tube containing the ore has been heated to redness for some time the heat is
carried back to the end of the tube. The magnesite readily gives up carbonic
acid, which fills the tube and sweeps the mercury vapour before it. Some of
the mercury will have dropped into the beaker, and some will remain as
drops adhering to the upper part of the neck. Whilst the tube is still hot cut
off the neck of the tube just in front of the asbestos plug (a drop of water
from the wash bottle will do this), and wash the mercury from the neck into
black precipitate with sulphuretted hydrogen from acid solutions, which is
insoluble in nitric acid; and (2) a white precipitate with stannous chloride.
DRY METHOD.
Weigh up 5 grams, if the ore is rich, or 10 grams, if a poorer mineral. Take a
piece of combustion tube from 18 inches to 2 feet long, closed at one end,
and place in it some powdered magnesite, so as to fill it to a depth of 2 or 3
inches, and on that a layer of an equal quantity of powdered lime (not
slaked). Mix the weighed sample of ore in a mortar with 10 grams of finely
powdered lime and transfer to the tube; rinse out the mortar with a little
more lime, and add the rinsings. Cover with a layer of six or seven inches
more lime and a loosely fitting plug of asbestos. Draw out the tube before
the blowpipe to the shape shown in fig. 47, avoiding the formation of a
ridge or hollow at the bend which might collect the mercury. Tap gently,
holding the tube nearly horizontal, so as to allow sufficient space above the
mixture for the passage of the gases and vapours which are formed. Place
the tube in a "tube furnace," and, when in position, place a small beaker of
water so that it shall just close the opening of the tube. The point of the tube
should not more than touch the surface of the water. Bring the tube
gradually to a red heat, commencing by heating the lime just behind the
asbestos plug, and travelling slowly backwards. When the portion of the
tube containing the ore has been heated to redness for some time the heat is
carried back to the end of the tube. The magnesite readily gives up carbonic
acid, which fills the tube and sweeps the mercury vapour before it. Some of
the mercury will have dropped into the beaker, and some will remain as
drops adhering to the upper part of the neck. Whilst the tube is still hot cut
off the neck of the tube just in front of the asbestos plug (a drop of water
from the wash bottle will do this), and wash the mercury from the neck into
Page 223
the beaker. The mercury easily collects into a globule, which must be
transferred, after decanting off the bulk of the water, to a weighed Berlin
crucible. The water is removed from the crucible, first by the help of filter
paper, and then by exposing in a desiccator over sulphuric acid, where it
should be left until its weight remains constant. It should not be warmed.
Example:—5 grams of an ore treated in this way gave 4.265 grams of
mercury, equivalent to 85.3 per cent. Pure cinnabar contains 86.2 per cent.
WET METHODS.
Solution.—Since solutions of chloride of mercury cannot be boiled without
risk of loss,[48] nitric acid solutions should be used wherever possible. No
mercury-containing minerals are insoluble in acids; but cinnabar requires
aqua regia for solution. In dissolving this mineral nitric acid should be used,
with just as much hydrochloric acid as will suffice to take it up.
To separate the mercury, pass sulphuretted hydrogen in considerable excess
through the somewhat dilute solution. The precipitate should be black,
although it comes down at first very light coloured. It is filtered, washed,
and transferred back to the beaker, and then digested with warm ammonic
sulphide. The residue, filtered, washed, and boiled with dilute nitric acid,
will, in the absence of much lead, be pure mercuric sulphide. If much lead
is present, a portion may be precipitated as sulphate, but can be removed by
washing with ammonic acetate. To get the mercury into solution, cover with
nitric acid and a few drops of hydrochloric, and warm till solution is
effected. Dilute with water to 50 or 100 c.c.
GRAVIMETRIC DETERMINATION.
This may be made by electrolysis. The same apparatus as is used for the
electrolytic copper assay may be employed, but instead of a cylinder of
platinum one cut out of sheet copper should be taken, or the platinum one
may be coated with an evenly deposited layer of copper. Fix the spiral and
weighed copper cylinder in position, couple up the battery, and when this
has been done put the nitric acid solution of the mercury in its place.[49] The
student had better refer to the description of the Electrolytic Copper Assay.
transferred, after decanting off the bulk of the water, to a weighed Berlin
crucible. The water is removed from the crucible, first by the help of filter
paper, and then by exposing in a desiccator over sulphuric acid, where it
should be left until its weight remains constant. It should not be warmed.
Example:—5 grams of an ore treated in this way gave 4.265 grams of
mercury, equivalent to 85.3 per cent. Pure cinnabar contains 86.2 per cent.
WET METHODS.
Solution.—Since solutions of chloride of mercury cannot be boiled without
risk of loss,[48] nitric acid solutions should be used wherever possible. No
mercury-containing minerals are insoluble in acids; but cinnabar requires
aqua regia for solution. In dissolving this mineral nitric acid should be used,
with just as much hydrochloric acid as will suffice to take it up.
To separate the mercury, pass sulphuretted hydrogen in considerable excess
through the somewhat dilute solution. The precipitate should be black,
although it comes down at first very light coloured. It is filtered, washed,
and transferred back to the beaker, and then digested with warm ammonic
sulphide. The residue, filtered, washed, and boiled with dilute nitric acid,
will, in the absence of much lead, be pure mercuric sulphide. If much lead
is present, a portion may be precipitated as sulphate, but can be removed by
washing with ammonic acetate. To get the mercury into solution, cover with
nitric acid and a few drops of hydrochloric, and warm till solution is
effected. Dilute with water to 50 or 100 c.c.
GRAVIMETRIC DETERMINATION.
This may be made by electrolysis. The same apparatus as is used for the
electrolytic copper assay may be employed, but instead of a cylinder of
platinum one cut out of sheet copper should be taken, or the platinum one
may be coated with an evenly deposited layer of copper. Fix the spiral and
weighed copper cylinder in position, couple up the battery, and when this
has been done put the nitric acid solution of the mercury in its place.[49] The
student had better refer to the description of the Electrolytic Copper Assay.
Page 224
The mercury comes down readily, and the precipitation is complete in a few
hours: it is better to leave it overnight to make sure of complete reduction.
Disconnect the apparatus, and wash the cylinder, first with cold water, then
with alcohol. Dry by placing in the water oven for two or three minutes.
Cool and weigh: the increase in weight gives the amount of metallic
mercury.
It must be remembered that copper will precipitate mercury without the aid
of the battery; but in this case copper will go into solution with a
consequent loss in the weight of the cylinder: this must be avoided by
connecting the battery before immersing the electrodes in the assay
solution. The electrolysed solution should be treated with an excess of
ammonia, when a blue coloration will indicate copper, in which case the
electrolysis is unsatisfactory. With a little care this need not happen. Gold
cylinders may preferably be used instead of copper; but on platinum the
deposit of mercury is grey and non-adherent, so that it cannot be washed
and weighed.
VOLUMETRIC METHODS.
Several methods have been devised: for the details of these the student is
referred to Sutton's "Handbook of Volumetric Analysis."
QUESTIONS.
1. The specific gravity of mercury is 13.596. What volume would 8 grams
occupy?
2. If 3.169 grams of cinnabar gave 2.718 grams of mercury, what would be
the percentage of the metal in the ore?
3. Pour solution of mercuric chloride on mercury and explain what happens.
4. On dissolving 0.3 gram of mercury in hot nitric acid, and passing
sulphuretted hydrogen in excess through the diluted solution, what weight
of precipitate will be got?
hours: it is better to leave it overnight to make sure of complete reduction.
Disconnect the apparatus, and wash the cylinder, first with cold water, then
with alcohol. Dry by placing in the water oven for two or three minutes.
Cool and weigh: the increase in weight gives the amount of metallic
mercury.
It must be remembered that copper will precipitate mercury without the aid
of the battery; but in this case copper will go into solution with a
consequent loss in the weight of the cylinder: this must be avoided by
connecting the battery before immersing the electrodes in the assay
solution. The electrolysed solution should be treated with an excess of
ammonia, when a blue coloration will indicate copper, in which case the
electrolysis is unsatisfactory. With a little care this need not happen. Gold
cylinders may preferably be used instead of copper; but on platinum the
deposit of mercury is grey and non-adherent, so that it cannot be washed
and weighed.
VOLUMETRIC METHODS.
Several methods have been devised: for the details of these the student is
referred to Sutton's "Handbook of Volumetric Analysis."
QUESTIONS.
1. The specific gravity of mercury is 13.596. What volume would 8 grams
occupy?
2. If 3.169 grams of cinnabar gave 2.718 grams of mercury, what would be
the percentage of the metal in the ore?
3. Pour solution of mercuric chloride on mercury and explain what happens.
4. On dissolving 0.3 gram of mercury in hot nitric acid, and passing
sulphuretted hydrogen in excess through the diluted solution, what weight
of precipitate will be got?
Page 225
FOOTNOTES:
[9] Lead may be granulated by heating it to a little above the melting point,
pouring it into a closed wooden box, and rapidly agitating it as it solidifies.
[10] A rod of iron placed in the crucible with the assays will decompose any
regulus that may be formed.
[11] With buttons poor in silver the lowering of the temperature at this stage is
not a matter of importance.
[12] 100 grams of the lead, or of its oxide, will contain from 1.5 to 2.5
milligrams.
[13] Still the precautions of having cupels well made from bone ash in fine
powder, and of working the cupellation at as low a temperature as possible are
very proper ones, provided they are not carried to an absurd excess.
[14] Be careful to remove the crucible before taking the bottle out of the basin of
water; if this is not done the chloride may be washed out of it.
[15] 1 c.c. of this dilute acid will precipitate 8 or 9 milligrams of silver.
[16] Chlorides interfere not merely by removing silver as insoluble silver
chloride, but also by making it difficult to get a good finishing point, owing to
the silver chloride removing the colour from the reddened solution.
[17] These results were obtained when using ammonium sulphocyanate, and
cannot be explained by the presence of such impurities as chlorides, &c.
[18] Multiply the standard by 1000, and dilute 100 c.c. of the standard solution
to the resulting number of c.c. Thus, with a solution of a standard .495, dilute
100 c.c. to 495 c.c., using, of course, distilled water.
[19] HNa2AsO4 + 3AgNO3 = Ag3AsO4 + HNO3 + 2NaNO3.
[20]
SiO2 + Na2CO3 = CO2 + Na2SiO3
SiO2 + 2NaHCO3 = 2CO2 + Na2SiO3 + H2O.
[21] PbO + SiO2 = PbSiO3
[22] Here and elsewhere in this article when a flux is spoken of as soda the
bicarbonate is meant.
[23] See the description of the process commencing on p. 98 and the explanatory
remarks on p. 110.
[24] Percy, Metallurgy of Silver and Gold, p. 258.
[25] "Limits of Accuracy attained in Gold-bullion Assay," Trans. Chem. Soc.,
1893.
[9] Lead may be granulated by heating it to a little above the melting point,
pouring it into a closed wooden box, and rapidly agitating it as it solidifies.
[10] A rod of iron placed in the crucible with the assays will decompose any
regulus that may be formed.
[11] With buttons poor in silver the lowering of the temperature at this stage is
not a matter of importance.
[12] 100 grams of the lead, or of its oxide, will contain from 1.5 to 2.5
milligrams.
[13] Still the precautions of having cupels well made from bone ash in fine
powder, and of working the cupellation at as low a temperature as possible are
very proper ones, provided they are not carried to an absurd excess.
[14] Be careful to remove the crucible before taking the bottle out of the basin of
water; if this is not done the chloride may be washed out of it.
[15] 1 c.c. of this dilute acid will precipitate 8 or 9 milligrams of silver.
[16] Chlorides interfere not merely by removing silver as insoluble silver
chloride, but also by making it difficult to get a good finishing point, owing to
the silver chloride removing the colour from the reddened solution.
[17] These results were obtained when using ammonium sulphocyanate, and
cannot be explained by the presence of such impurities as chlorides, &c.
[18] Multiply the standard by 1000, and dilute 100 c.c. of the standard solution
to the resulting number of c.c. Thus, with a solution of a standard .495, dilute
100 c.c. to 495 c.c., using, of course, distilled water.
[19] HNa2AsO4 + 3AgNO3 = Ag3AsO4 + HNO3 + 2NaNO3.
[20]
SiO2 + Na2CO3 = CO2 + Na2SiO3
SiO2 + 2NaHCO3 = 2CO2 + Na2SiO3 + H2O.
[21] PbO + SiO2 = PbSiO3
[22] Here and elsewhere in this article when a flux is spoken of as soda the
bicarbonate is meant.
[23] See the description of the process commencing on p. 98 and the explanatory
remarks on p. 110.
[24] Percy, Metallurgy of Silver and Gold, p. 258.
[25] "Limits of Accuracy attained in Gold-bullion Assay," Trans. Chem. Soc.,
1893.
Page 226
[26] "Assaying and Hall-marking at the Chester Assay Office." W.F. Lowe.
Journ. Soc. Chem. Industry, Sept. 1889.
[27] Fine or pure gold is 24 carat. Nine carat gold therefore contains 9 parts of
gold in 24 of the alloy; eighteen carat gold contains 18 parts of gold in 24; and
so on.
[28] The mouth of the flask must not have a rim around it.
[29] See "Assaying and Hall-marking at the Chester Assay Office," by W.F.
Lowe. Journ. Soc. Chem. Industry, Sept. 1889.
[30] Percy, Metallurgy of Silver and Gold, p. 263.
[31] See also "The Assaying of Gold Bullion," by C. Whitehead and T. Ulke.
Eng. and Mining Journal, New York, Feb. 12, 1898.
[32] Consult Percy's Metallurgy of Silver and Gold, p. 172; A.C. Claudet, Trans.
Inst. Mining and Metallurgy, vol. vi. p. 29; G.M. Roberts Trans. Amer. Inst.
Mining Engineers, Buffalo Meeting, 1898; J. and H.S. Pattinson, Journ. Soc.
Chem. Industry, vol. xi. p. 321.
[33] Heycock and Neville, Journ. Chem. Soc., 1892, p. 907.
[34] G.M. Roberts.
[35] A.C. Claudet.
[36] "The Sampling of Argentiferous and Auriferous Copper," by A.R. Ledoux.
Journ. Canadian Mining Institute, 1899.
[37] NaCNO + BaCl2 + NaHO + H2O = NH3 + BaCO3 + 2 NaCl.
[38] HCy + NaHO = NaCy + H2O.
[39] 2KCN + AgNO3 = KAg(CN)2 + KNO3.
[40] If it be desired to make a solution so that 100 c.c. shall be equivalent to 1
gram of sodium cyanide, then 18.085 grams of silver nitrate should be taken for
each litre.
[41] AgNO3 + KAgCy2 = 2 AgCy + KNO3.
[42] AgNO3 + KI = AgI + KNO3.
[43] See pp. 322, 323, and 324 for a description of the methods for measuring
the quantity of acid or alkali.
[44] KCN + HCl = KCl + HCN
[45] Taking 16.0 grams of ore, each c.c. = 1 lb. of soda to the short ton. The
corresponding figures for the long ton are 12.544 grams for lime and 17.92
grams for soda.
[46] In which case each .01 gram of metal found equals 1 lb to the short ton of
solution.
Journ. Soc. Chem. Industry, Sept. 1889.
[27] Fine or pure gold is 24 carat. Nine carat gold therefore contains 9 parts of
gold in 24 of the alloy; eighteen carat gold contains 18 parts of gold in 24; and
so on.
[28] The mouth of the flask must not have a rim around it.
[29] See "Assaying and Hall-marking at the Chester Assay Office," by W.F.
Lowe. Journ. Soc. Chem. Industry, Sept. 1889.
[30] Percy, Metallurgy of Silver and Gold, p. 263.
[31] See also "The Assaying of Gold Bullion," by C. Whitehead and T. Ulke.
Eng. and Mining Journal, New York, Feb. 12, 1898.
[32] Consult Percy's Metallurgy of Silver and Gold, p. 172; A.C. Claudet, Trans.
Inst. Mining and Metallurgy, vol. vi. p. 29; G.M. Roberts Trans. Amer. Inst.
Mining Engineers, Buffalo Meeting, 1898; J. and H.S. Pattinson, Journ. Soc.
Chem. Industry, vol. xi. p. 321.
[33] Heycock and Neville, Journ. Chem. Soc., 1892, p. 907.
[34] G.M. Roberts.
[35] A.C. Claudet.
[36] "The Sampling of Argentiferous and Auriferous Copper," by A.R. Ledoux.
Journ. Canadian Mining Institute, 1899.
[37] NaCNO + BaCl2 + NaHO + H2O = NH3 + BaCO3 + 2 NaCl.
[38] HCy + NaHO = NaCy + H2O.
[39] 2KCN + AgNO3 = KAg(CN)2 + KNO3.
[40] If it be desired to make a solution so that 100 c.c. shall be equivalent to 1
gram of sodium cyanide, then 18.085 grams of silver nitrate should be taken for
each litre.
[41] AgNO3 + KAgCy2 = 2 AgCy + KNO3.
[42] AgNO3 + KI = AgI + KNO3.
[43] See pp. 322, 323, and 324 for a description of the methods for measuring
the quantity of acid or alkali.
[44] KCN + HCl = KCl + HCN
[45] Taking 16.0 grams of ore, each c.c. = 1 lb. of soda to the short ton. The
corresponding figures for the long ton are 12.544 grams for lime and 17.92
grams for soda.
[46] In which case each .01 gram of metal found equals 1 lb to the short ton of
solution.
Page 227
[47] 100 c.c. of water dissolves 0.66 gram of the salt; it is almost insoluble in
alcohol or in solutions of ammonic chloride.
[48] According to Personne mercuric chloride is not volatilised from boiling
solutions when alkaline chlorides are present.
[49] The solution should contain about 0.25 gram of mercury, and a large excess
of nitric acid must be avoided.
alcohol or in solutions of ammonic chloride.
[48] According to Personne mercuric chloride is not volatilised from boiling
solutions when alkaline chlorides are present.
[49] The solution should contain about 0.25 gram of mercury, and a large excess
of nitric acid must be avoided.
Page 228
CHAPTER X.
COPPER—LEAD—THALLIUM—BISMUTH—ANTIMONY.
COPPER.
Copper occurs native in large quantities, especially in the Lake Superior
district; in this state it is generally pure. More frequently it is found in
combination. The ores of copper may be classed as oxides and sulphides.
The most abundant oxidised ores are the carbonates, malachite and
chessylite; the silicates, as also the red and black oxides, occur less
abundantly. All these yield their copper in solution on boiling with
hydrochloric acid.
The sulphides are more abundant. Copper pyrites (or yellow ore), erubescite
(or purple ore), and chalcocite (or grey ore) are the most important. Iron
pyrites generally carries copper and is frequently associated with the above-
mentioned minerals. These are all attacked by nitric acid. They nearly all
contain a small quantity of organic matter, and frequently considerable
quantities of lead, zinc, silver, gold, arsenic, bismuth, &c.
The copper ores are often concentrated on the mine before being sent into
the market, either by smelting, when the product is a regulus or matte, or by
a wet method of extraction, yielding cement copper or precipitate. A regulus
is a sulphide of copper and iron, carrying from 30 to 40 per cent. of copper.
A precipitate, which is generally in the form of powder, consists mainly of
metallic copper. Either regulus or precipitate may be readily dissolved in
nitric acid.
Copper forms two classes of salts, cuprous and cupric. The former are pale
coloured and of little importance to the assayer. They are easily and
completely converted into cupric by oxidising agents. Cupric compounds
are generally green or blue, and are soluble in ammonia, forming deep blue
solutions.
COPPER—LEAD—THALLIUM—BISMUTH—ANTIMONY.
COPPER.
Copper occurs native in large quantities, especially in the Lake Superior
district; in this state it is generally pure. More frequently it is found in
combination. The ores of copper may be classed as oxides and sulphides.
The most abundant oxidised ores are the carbonates, malachite and
chessylite; the silicates, as also the red and black oxides, occur less
abundantly. All these yield their copper in solution on boiling with
hydrochloric acid.
The sulphides are more abundant. Copper pyrites (or yellow ore), erubescite
(or purple ore), and chalcocite (or grey ore) are the most important. Iron
pyrites generally carries copper and is frequently associated with the above-
mentioned minerals. These are all attacked by nitric acid. They nearly all
contain a small quantity of organic matter, and frequently considerable
quantities of lead, zinc, silver, gold, arsenic, bismuth, &c.
The copper ores are often concentrated on the mine before being sent into
the market, either by smelting, when the product is a regulus or matte, or by
a wet method of extraction, yielding cement copper or precipitate. A regulus
is a sulphide of copper and iron, carrying from 30 to 40 per cent. of copper.
A precipitate, which is generally in the form of powder, consists mainly of
metallic copper. Either regulus or precipitate may be readily dissolved in
nitric acid.
Copper forms two classes of salts, cuprous and cupric. The former are pale
coloured and of little importance to the assayer. They are easily and
completely converted into cupric by oxidising agents. Cupric compounds
are generally green or blue, and are soluble in ammonia, forming deep blue
solutions.
Page 229
DRY ASSAY.
That, for copper, next after those for gold and silver, holds a more important
position than any other dry assay. The sale of copper ores has been
regulated almost solely in the past by assays made on the Cornish method.
It is not pretended that this method gives the actual content of copper, but it
gives the purchaser an idea of the quantity and quality of the metal that can
be got by smelting. The process is itself one of smelting on a small scale. As
might be expected, however, the assay produce and the smelting produce
are not the same, there being a smaller loss of copper in the smelting. The
method has worked very well, but when applied to the purchase of low
class ores (from which the whole of the copper is extracted by wet methods)
it is unsatisfactory. The following table, which embodies the results of
several years' experience with copper assays, shows the loss of copper on
ores of varying produce. The figures in the fourth column show how rapidly
the proportion of copper lost increases as the percentage of copper in the
ore falls below 30 per cent. For material with more than 30 per cent. the
proportion lost is in inverse proportion to the copper present.
LOSS OF COPPER.
Copper present. Dry Assay. Margin. Loss on 100 Parts of Copper.
Per cent. Per cent. Per cent.
100 98 2.0 2.0
95 92-1/2 2.5 2.6
90 87-3/8 2.6 2.9
85 82-3/8 2.6 3.0
80 77-3/8 2.6 3.2
75 72-3/8 2.6 3.5
70 67-1/2 2.5 3.6
65 62-1/2 2.5 3.8
60 57-5/8 2.4 4.0
55 52-3/4 2.3 4.2
50 47-3/4 2.2 4.4
45 43 2.0 4.5
That, for copper, next after those for gold and silver, holds a more important
position than any other dry assay. The sale of copper ores has been
regulated almost solely in the past by assays made on the Cornish method.
It is not pretended that this method gives the actual content of copper, but it
gives the purchaser an idea of the quantity and quality of the metal that can
be got by smelting. The process is itself one of smelting on a small scale. As
might be expected, however, the assay produce and the smelting produce
are not the same, there being a smaller loss of copper in the smelting. The
method has worked very well, but when applied to the purchase of low
class ores (from which the whole of the copper is extracted by wet methods)
it is unsatisfactory. The following table, which embodies the results of
several years' experience with copper assays, shows the loss of copper on
ores of varying produce. The figures in the fourth column show how rapidly
the proportion of copper lost increases as the percentage of copper in the
ore falls below 30 per cent. For material with more than 30 per cent. the
proportion lost is in inverse proportion to the copper present.
LOSS OF COPPER.
Copper present. Dry Assay. Margin. Loss on 100 Parts of Copper.
Per cent. Per cent. Per cent.
100 98 2.0 2.0
95 92-1/2 2.5 2.6
90 87-3/8 2.6 2.9
85 82-3/8 2.6 3.0
80 77-3/8 2.6 3.2
75 72-3/8 2.6 3.5
70 67-1/2 2.5 3.6
65 62-1/2 2.5 3.8
60 57-5/8 2.4 4.0
55 52-3/4 2.3 4.2
50 47-3/4 2.2 4.4
45 43 2.0 4.5
Page 230
40 38-1/8 1.8 4.6
35 33-1/4 1.7 4.8
30 28-1/2 1.50 5.0
25 23-1/2 1.50 6.0
20 18-1/2 1.56 7.8
18 16-1/2 1.53 8.5
16 14-1/2 1.48 9.3
14 12-5/8 1.40 10.0
12 10-5/8 1.37 11.4
10 8-3/4 1.28 12.8
8 6-7/8 1.14 14.3
6 5 1.05 17.5
5 4 1.00 20.0
4 3 1.00 25.0
3.75 2-3/4 0.97 26.0
3.50 2-9/16 0.94 27.0
3.25 2-5/16 0.91 28.0
3.00 2-1/8 0.87 29.0
2.75 1-15/16 0.82 30.0
2.50 1-3/4 0.77 31.0
2.25 1-1/2 0.72 32.0
2.00 1-5/16 0.66 33.0
The wet assay being known, the dry assay can be calculated with the help of
the above table by deducting the amount in the column headed "margin"
opposite the corresponding percentage. For example, if the wet assay gives
a produce of 17.12 per cent., there should be deducted 1.5; the dry assay
would then be 15.62, or, since the fractions are always expressed in eighths,
15-5/8. With impure ores, containing from 25 to 50 per cent. of copper, the
differences may be perhaps 1/4 greater.
Wet methods are gradually replacing the dry assay, and it is probable that in
the future they will supersede it; for stock-taking, and the various
determinations required in smelting works and on mines, they are generally
adopted, because they give the actual copper contents, and since it is
obvious that a knowledge of this is more valuable to the miner and smelter.
35 33-1/4 1.7 4.8
30 28-1/2 1.50 5.0
25 23-1/2 1.50 6.0
20 18-1/2 1.56 7.8
18 16-1/2 1.53 8.5
16 14-1/2 1.48 9.3
14 12-5/8 1.40 10.0
12 10-5/8 1.37 11.4
10 8-3/4 1.28 12.8
8 6-7/8 1.14 14.3
6 5 1.05 17.5
5 4 1.00 20.0
4 3 1.00 25.0
3.75 2-3/4 0.97 26.0
3.50 2-9/16 0.94 27.0
3.25 2-5/16 0.91 28.0
3.00 2-1/8 0.87 29.0
2.75 1-15/16 0.82 30.0
2.50 1-3/4 0.77 31.0
2.25 1-1/2 0.72 32.0
2.00 1-5/16 0.66 33.0
The wet assay being known, the dry assay can be calculated with the help of
the above table by deducting the amount in the column headed "margin"
opposite the corresponding percentage. For example, if the wet assay gives
a produce of 17.12 per cent., there should be deducted 1.5; the dry assay
would then be 15.62, or, since the fractions are always expressed in eighths,
15-5/8. With impure ores, containing from 25 to 50 per cent. of copper, the
differences may be perhaps 1/4 greater.
Wet methods are gradually replacing the dry assay, and it is probable that in
the future they will supersede it; for stock-taking, and the various
determinations required in smelting works and on mines, they are generally
adopted, because they give the actual copper contents, and since it is
obvious that a knowledge of this is more valuable to the miner and smelter.
Page 231
Moreover, the working of the dry method has been monopolised by a small
ring of assayers, with the double result of exciting outside jealousy and,
worse still, of retarding the development and improvement of the process.
The principal stages of the dry assay are: (1) the concentration of the copper
in a regulus; (2) the separation of the sulphur by calcining; (3) the reduction
of the copper by fusion; and (4) the refining of the metal obtained.
The whole of these operations are not necessary with all copper material.
Ores are worked through all the stages; with mattes, the preliminary fusion
for regulus is omitted; precipitates are simply fused for coarse copper, and
refined; and blister or bar coppers are refined, or, if very pure, subjected
merely to washing.
The quantity of ore generally taken is 400 grains, and is known as "a full
trial"; but for rich material, containing more than 50 per cent. of copper, "a
half trial," or 200 grains, is used.
Fusion for Regulus.—The ore (either with or without a previous imperfect
roasting to get rid of any excess of sulphur) is mixed with borax, glass,
lime, and fluor spar; and, in some cases, with nitre, or iron pyrites,
according to the quality of the ore. The mixture is placed in a large Cornish
crucible, and heated as uniformly as possible in the wind furnace, gradually
raising the temperature so as to melt down the charge in from 15 to 20
minutes. The crucible is removed and its contents poured into an iron
mould. When the slag is solid, it is taken up with tweezers and quenched in
water. The regulus is easily detached from the slag. It should be convex
above and easily broken, have a reddish brown colour, and contain from 40
to 60 per cent. of copper. A regulus with more than this is "too fine," and
with less "too coarse." A regulus which is too fine is round, compact, hard,
and of a dark bluish grey on the freshly broken surface. A coarse regulus is
flat and coarse grained, and more nearly resembles sulphide of iron in
fracture and colour.
If an assay yields a regulus "too coarse," a fresh determination is made with
more nitre added, or the roasting is carried further. With low class ores a
somewhat coarse regulus is an advantage. If, on the other hand, the regulus
is too fine, less nitre or less roasting is the remedy. With grey copper ores
and the oxidised ores, iron pyrites is added.
ring of assayers, with the double result of exciting outside jealousy and,
worse still, of retarding the development and improvement of the process.
The principal stages of the dry assay are: (1) the concentration of the copper
in a regulus; (2) the separation of the sulphur by calcining; (3) the reduction
of the copper by fusion; and (4) the refining of the metal obtained.
The whole of these operations are not necessary with all copper material.
Ores are worked through all the stages; with mattes, the preliminary fusion
for regulus is omitted; precipitates are simply fused for coarse copper, and
refined; and blister or bar coppers are refined, or, if very pure, subjected
merely to washing.
The quantity of ore generally taken is 400 grains, and is known as "a full
trial"; but for rich material, containing more than 50 per cent. of copper, "a
half trial," or 200 grains, is used.
Fusion for Regulus.—The ore (either with or without a previous imperfect
roasting to get rid of any excess of sulphur) is mixed with borax, glass,
lime, and fluor spar; and, in some cases, with nitre, or iron pyrites,
according to the quality of the ore. The mixture is placed in a large Cornish
crucible, and heated as uniformly as possible in the wind furnace, gradually
raising the temperature so as to melt down the charge in from 15 to 20
minutes. The crucible is removed and its contents poured into an iron
mould. When the slag is solid, it is taken up with tweezers and quenched in
water. The regulus is easily detached from the slag. It should be convex
above and easily broken, have a reddish brown colour, and contain from 40
to 60 per cent. of copper. A regulus with more than this is "too fine," and
with less "too coarse." A regulus which is too fine is round, compact, hard,
and of a dark bluish grey on the freshly broken surface. A coarse regulus is
flat and coarse grained, and more nearly resembles sulphide of iron in
fracture and colour.
If an assay yields a regulus "too coarse," a fresh determination is made with
more nitre added, or the roasting is carried further. With low class ores a
somewhat coarse regulus is an advantage. If, on the other hand, the regulus
is too fine, less nitre or less roasting is the remedy. With grey copper ores
and the oxidised ores, iron pyrites is added.
Page 232
Calcining the Regulus.—It is powdered in an iron mortar and transferred
to a small Cornish crucible, or (if the roasting is to be done in the muffle) to
a roasting dish or scorifier. The calcining is carried out at a dull red heat,
which is gradually increased. The charge requires constant stirring at first to
prevent clotting, but towards the end it becomes sandy and requires less
attention. If the temperature during calcination has been too low sulphates
are formed, which are again reduced to sulphides in the subsequent fusion.
To prevent this the roasted regulus is recalcined at a higher temperature,
after being rubbed up with a little anthracite. The roasted substance must
not smell of burning sulphur when hot. It is practically a mixture of the
oxides of copper and iron.
Fusion for Coarse Copper.—The calcined regulus is mixed with a flux
consisting of borax and carbonate of soda, with more or less tartar
according to its weight. Some "assayers" use both tartar and nitre, the
former of course being in excess. The charge is returned to the crucible in
which it was calcined, and is melted down at a high temperature, and, as
soon as tranquil, poured. When solid it is quenched and the button of metal
separated.
The slag is black and glassy. The small quantity of copper which it retains is
recovered by a subsequent "cleaning," together with the slags from the next
operation.
The button of "coarse copper" obtained must be free from a coating of
regulus. It will vary somewhat in appearance according to the nature and
quantity of the impurities.
Refining the Coarse Copper.—The same crucible is put back in the
furnace, deep down and under the crevice between the two bricks. When it
has attained the temperature of the furnace the coarse copper is dropped
into it and the furnace closed. The copper will melt almost at once with a
dull surface, which after a time clears, showing an "eye." Some refining
flux is then shot in from the scoop (fig. 48), and, when the assay is again
fluid, it is poured. When cold the button of metal is separated.
to a small Cornish crucible, or (if the roasting is to be done in the muffle) to
a roasting dish or scorifier. The calcining is carried out at a dull red heat,
which is gradually increased. The charge requires constant stirring at first to
prevent clotting, but towards the end it becomes sandy and requires less
attention. If the temperature during calcination has been too low sulphates
are formed, which are again reduced to sulphides in the subsequent fusion.
To prevent this the roasted regulus is recalcined at a higher temperature,
after being rubbed up with a little anthracite. The roasted substance must
not smell of burning sulphur when hot. It is practically a mixture of the
oxides of copper and iron.
Fusion for Coarse Copper.—The calcined regulus is mixed with a flux
consisting of borax and carbonate of soda, with more or less tartar
according to its weight. Some "assayers" use both tartar and nitre, the
former of course being in excess. The charge is returned to the crucible in
which it was calcined, and is melted down at a high temperature, and, as
soon as tranquil, poured. When solid it is quenched and the button of metal
separated.
The slag is black and glassy. The small quantity of copper which it retains is
recovered by a subsequent "cleaning," together with the slags from the next
operation.
The button of "coarse copper" obtained must be free from a coating of
regulus. It will vary somewhat in appearance according to the nature and
quantity of the impurities.
Refining the Coarse Copper.—The same crucible is put back in the
furnace, deep down and under the crevice between the two bricks. When it
has attained the temperature of the furnace the coarse copper is dropped
into it and the furnace closed. The copper will melt almost at once with a
dull surface, which after a time clears, showing an "eye." Some refining
flux is then shot in from the scoop (fig. 48), and, when the assay is again
fluid, it is poured. When cold the button of metal is separated.
Page 233
The button of "fine" copper is flat or pitted on its upper surface, and is
coated with a thin orange film; it must have the appearance of good copper.
If it is covered with a red or purple film, it is overdone or "burnt." If, on the
other hand, it has a rough, dull appearance, it is not sufficiently refined.
Assays that have been "burnt" are rejected. Those not sufficiently fine are
treated as "coarse copper," and again put through the refining operation.
Cleaning the Slags.—These are roughly powdered and re-fused with tartar,
etc., as in the fusion for coarse copper. The button of metal got is separated
(if big enough refined) and weighed.
The details of the process are slightly varied by different assayers: the
following will be good practice for the student.
Determination of Copper in Copper Pyrites.—Powder, dry, and weigh up
20 grams of the ore. Mix with 20 grams each of powdered lime and fluor,
15 grams each of powdered glass and borax, and 5 or 10 grams of nitre.
Transfer to a large Cornish crucible and fuse under a loose cover at a high
temperature for from 15 to 20 minutes. When fluid and tranquil pour into a
mould. When the slag has solidified, but whilst still hot, quench by dipping
two or three times in cold water. Avoid leaving it in the water so long that it
does not dry after removal. When cold separate the button, or perhaps
buttons, of regulus by crumbling the slag between the fingers. See that the
slag is free from regulus. It should be light coloured when cold and very
fluid when hot. Reject the slag.
Powder the regulus in a mortar and transfer to a small crucible. Calcine,
with occasional stirring, until no odour of sulphurous oxide can be detected.
coated with a thin orange film; it must have the appearance of good copper.
If it is covered with a red or purple film, it is overdone or "burnt." If, on the
other hand, it has a rough, dull appearance, it is not sufficiently refined.
Assays that have been "burnt" are rejected. Those not sufficiently fine are
treated as "coarse copper," and again put through the refining operation.
Cleaning the Slags.—These are roughly powdered and re-fused with tartar,
etc., as in the fusion for coarse copper. The button of metal got is separated
(if big enough refined) and weighed.
The details of the process are slightly varied by different assayers: the
following will be good practice for the student.
Determination of Copper in Copper Pyrites.—Powder, dry, and weigh up
20 grams of the ore. Mix with 20 grams each of powdered lime and fluor,
15 grams each of powdered glass and borax, and 5 or 10 grams of nitre.
Transfer to a large Cornish crucible and fuse under a loose cover at a high
temperature for from 15 to 20 minutes. When fluid and tranquil pour into a
mould. When the slag has solidified, but whilst still hot, quench by dipping
two or three times in cold water. Avoid leaving it in the water so long that it
does not dry after removal. When cold separate the button, or perhaps
buttons, of regulus by crumbling the slag between the fingers. See that the
slag is free from regulus. It should be light coloured when cold and very
fluid when hot. Reject the slag.
Powder the regulus in a mortar and transfer to a small crucible. Calcine,
with occasional stirring, until no odour of sulphurous oxide can be detected.
Page 234
Shake back into the mortar, rub up with about 1 gram of powdered
anthracite, and re-calcine for 10 minutes longer.
Mix the calcined regulus with 10 grams of tartar, 20 grams of soda, and 3
grams of borax; and replace in the crucible used for calcining. Fuse at a
bright red heat for 10 or 15 minutes. Pour, when tranquil.
As soon as solid, quench in water, separate the button of copper, and save
the slag.
To refine the copper a very hot fire is wanted, and the fuel should not be too
low down in the furnace. Place the crucible well down in the fire and in the
middle of the furnace. The same crucible is used, or, if a new one is taken, it
must be glazed with a little borax. When the crucible is at a good red heat,
above the fusing point of copper, drop the button of copper into it, and close
the furnace. Watch through the crevice, and, as soon as the button has
melted and appears clear showing an eye, shoot in 10 grams of refining
flux, close the furnace, and, in a few minutes, pour; then separate the button
of copper. Add the slag to that from the coarse copper fusion, and powder.
Mix with 5 grams of tartar, 0.5 gram of powdered charcoal, and 2 grams of
soda. Fuse in the same crucible, and, when tranquil, pour; quench, and pick
out the prills of metal.
If the copper thus got from the slags is coarse looking and large in amount,
it must be refined; but, if small in quantity, it may be taken as four-fifths
copper. The combined results multiplied by five give the percentage of
copper.
The refining flux is made by mixing 3 parts (by measure) of powdered
nitre, 2-1\2 of tartar, and 1 of salt. Put in a large crucible, and stir with a
red-hot iron until action has ceased. This operation should be carried out in
a well-ventilated spot.
For pure ores in which the copper is present, either as metal or oxide, and
free from sulphur, arsenic, &c., the concentration of the copper in a regulus
may be omitted, and the metal obtained in a pure state by a single fusion.[50]
It is necessary to get a fluid neutral slag with the addition of as small an
amount of flux as possible. The fusion should be made at a high
temperature, so as not to occupy more than from 20 to 25 minutes. Thirty
anthracite, and re-calcine for 10 minutes longer.
Mix the calcined regulus with 10 grams of tartar, 20 grams of soda, and 3
grams of borax; and replace in the crucible used for calcining. Fuse at a
bright red heat for 10 or 15 minutes. Pour, when tranquil.
As soon as solid, quench in water, separate the button of copper, and save
the slag.
To refine the copper a very hot fire is wanted, and the fuel should not be too
low down in the furnace. Place the crucible well down in the fire and in the
middle of the furnace. The same crucible is used, or, if a new one is taken, it
must be glazed with a little borax. When the crucible is at a good red heat,
above the fusing point of copper, drop the button of copper into it, and close
the furnace. Watch through the crevice, and, as soon as the button has
melted and appears clear showing an eye, shoot in 10 grams of refining
flux, close the furnace, and, in a few minutes, pour; then separate the button
of copper. Add the slag to that from the coarse copper fusion, and powder.
Mix with 5 grams of tartar, 0.5 gram of powdered charcoal, and 2 grams of
soda. Fuse in the same crucible, and, when tranquil, pour; quench, and pick
out the prills of metal.
If the copper thus got from the slags is coarse looking and large in amount,
it must be refined; but, if small in quantity, it may be taken as four-fifths
copper. The combined results multiplied by five give the percentage of
copper.
The refining flux is made by mixing 3 parts (by measure) of powdered
nitre, 2-1\2 of tartar, and 1 of salt. Put in a large crucible, and stir with a
red-hot iron until action has ceased. This operation should be carried out in
a well-ventilated spot.
For pure ores in which the copper is present, either as metal or oxide, and
free from sulphur, arsenic, &c., the concentration of the copper in a regulus
may be omitted, and the metal obtained in a pure state by a single fusion.[50]
It is necessary to get a fluid neutral slag with the addition of as small an
amount of flux as possible. The fusion should be made at a high
temperature, so as not to occupy more than from 20 to 25 minutes. Thirty
Page 235
grams of ore is taken for a charge, mixed with 20 grams of cream of tartar,
and 10 grams each of dried borax and soda. If the gangue of the ore is basic,
carrying much oxide of iron or lime, silica is added, in quantity not
exceeding 10 grams. If, on the other hand, the gangue is mainly quartz,
oxide of iron up to 7 grams must be added.
Example.—Twenty grams of copper pyrites, known to contain 27.6 per
cent. of copper, gave by the method first described 5.22 grams of copper,
equalling 26-1/8 per cent. Another sample of 20 grams of the same ore,
calcined, fused with 40 grams of nitre, and washed to ensure the removal of
arsenic and sulphur, and treated according to the second method, gave a
button weighing 5.27 grams, equalling 26-3/8 per cent. The ore contained a
considerable quantity of lead. Lead renders the assay more difficult, since
after calcination it remains as lead sulphate, and in the fusion for coarse
copper reappears as a regulus on the button.
The Estimation of Moisture.—The Cornish dry assayer very seldom
makes a moisture determination. He dries the samples by placing the papers
containing them on the iron plate of the furnace.
It is well known that by buying the copper contents of pyrites by Cornish
assay, burning off the sulphur, and converting the copper into precipitate, a
large excess is obtained.
NOTES ON THE VALUATION OF COPPER ORES.
Closely bound up with the practice of dry copper assaying is that of valuing
a parcel of copper ore. The methods by which the valuation is made have
been described by Mr. Westmoreland,[51] and are briefly as follows:—The
produce of the parcel is settled by two assayers, one acting for the buyer,
the other for the seller; with the help, in case of non-agreement, of a third,
or referee, whose decision is final. The dry assayers who do this are in most
cases helped, and sometimes, perhaps, controlled, by wet assays made for
one or both of the parties in the transaction.
In the case of "ticketing," the parcels are purchased by the smelters by
tender, and the value of any particular parcel is calculated from the average
price paid, as follows:—The "standard," or absolute value of each ton of
and 10 grams each of dried borax and soda. If the gangue of the ore is basic,
carrying much oxide of iron or lime, silica is added, in quantity not
exceeding 10 grams. If, on the other hand, the gangue is mainly quartz,
oxide of iron up to 7 grams must be added.
Example.—Twenty grams of copper pyrites, known to contain 27.6 per
cent. of copper, gave by the method first described 5.22 grams of copper,
equalling 26-1/8 per cent. Another sample of 20 grams of the same ore,
calcined, fused with 40 grams of nitre, and washed to ensure the removal of
arsenic and sulphur, and treated according to the second method, gave a
button weighing 5.27 grams, equalling 26-3/8 per cent. The ore contained a
considerable quantity of lead. Lead renders the assay more difficult, since
after calcination it remains as lead sulphate, and in the fusion for coarse
copper reappears as a regulus on the button.
The Estimation of Moisture.—The Cornish dry assayer very seldom
makes a moisture determination. He dries the samples by placing the papers
containing them on the iron plate of the furnace.
It is well known that by buying the copper contents of pyrites by Cornish
assay, burning off the sulphur, and converting the copper into precipitate, a
large excess is obtained.
NOTES ON THE VALUATION OF COPPER ORES.
Closely bound up with the practice of dry copper assaying is that of valuing
a parcel of copper ore. The methods by which the valuation is made have
been described by Mr. Westmoreland,[51] and are briefly as follows:—The
produce of the parcel is settled by two assayers, one acting for the buyer,
the other for the seller; with the help, in case of non-agreement, of a third,
or referee, whose decision is final. The dry assayers who do this are in most
cases helped, and sometimes, perhaps, controlled, by wet assays made for
one or both of the parties in the transaction.
In the case of "ticketing," the parcels are purchased by the smelters by
tender, and the value of any particular parcel is calculated from the average
price paid, as follows:—The "standard," or absolute value of each ton of
Page 236
fine copper in the ore, is the price the smelters have paid for it, plus the
returning charges or cost of smelting the quantity of ore in which it is
contained. The value of any particular parcel of ore is that of the quantity of
fine copper it contains, calculated on this standard, minus the returning
charges. The ton consists of 21 cwts., and it is assumed that the "settled"
produce is the actual yield of the ore.
If at a ticketing in Cornwall 985 tons of ore containing 63.3 tons of fine
copper (by dry assay) brought £2591 12s., the standard would be £83 15s.
This is calculated as follows:—The returning charge is fixed at 55s. per ton
of ore. This on 985 tons will amount to £2708 15s. Add this to the actual
price paid, and there is got £5300 as the value of the fine copper present.
The weight of copper in these 985 tons being 63.3 tons, the standard is
£5300/63.3, or £83 15s. (nearly).
The value of a parcel of 150 tons of a 6 per cent. ore on the same standard
would be arrived at as follows:—The 150 tons at 6 per cent. would contain
9 tons (150×6/100) of fine copper. This, at £83 15s. per ton, would give
£753 15s. From this must be deducted the returning charges on 150 tons of
ore at 55s. per ton, or £412 10s. This leaves £341 5s. as the value of the
parcel.
At Swansea the returning charge is less than in Cornwall, and varies with
the quality of the ore. This appears equitable, since in smelting there are
some costs which are dependent simply on the number of tons treated, and
others which increase with the richness. The returning charge then is made
up of two parts, one fixed at so much (12s. 2d.) per ton of ore treated, and
the other so much (3s. 9d.) per unit of metal in the ore. In this way the
returning charge on a ton of ore of 8-3/4 produce would be 12s. 2d.+(8-
3/4×3s. 9d.), or £2 5s.
If, for example, Chili bars, containing 96 per cent. of copper, bring £50 per
ton, the standard is £71 9s. 4d. It is got at in this way. The returning charge
on a 96 per cent. ore is 12s. 2d.+(96×3s. 9d.), or £18 12s. 2d. This added to
£50 gives £68 12s. 2d., and this multiplied by 100 and divided by 96 (100
tons of the bars will contain 96 tons of fine copper) will give £71 9s. 4d.
The price of 100 tons of pyrites, containing 2-1/4 per cent. of copper by dry
assay, would be got on this standard as follows:—The parcel of ore would
returning charges or cost of smelting the quantity of ore in which it is
contained. The value of any particular parcel of ore is that of the quantity of
fine copper it contains, calculated on this standard, minus the returning
charges. The ton consists of 21 cwts., and it is assumed that the "settled"
produce is the actual yield of the ore.
If at a ticketing in Cornwall 985 tons of ore containing 63.3 tons of fine
copper (by dry assay) brought £2591 12s., the standard would be £83 15s.
This is calculated as follows:—The returning charge is fixed at 55s. per ton
of ore. This on 985 tons will amount to £2708 15s. Add this to the actual
price paid, and there is got £5300 as the value of the fine copper present.
The weight of copper in these 985 tons being 63.3 tons, the standard is
£5300/63.3, or £83 15s. (nearly).
The value of a parcel of 150 tons of a 6 per cent. ore on the same standard
would be arrived at as follows:—The 150 tons at 6 per cent. would contain
9 tons (150×6/100) of fine copper. This, at £83 15s. per ton, would give
£753 15s. From this must be deducted the returning charges on 150 tons of
ore at 55s. per ton, or £412 10s. This leaves £341 5s. as the value of the
parcel.
At Swansea the returning charge is less than in Cornwall, and varies with
the quality of the ore. This appears equitable, since in smelting there are
some costs which are dependent simply on the number of tons treated, and
others which increase with the richness. The returning charge then is made
up of two parts, one fixed at so much (12s. 2d.) per ton of ore treated, and
the other so much (3s. 9d.) per unit of metal in the ore. In this way the
returning charge on a ton of ore of 8-3/4 produce would be 12s. 2d.+(8-
3/4×3s. 9d.), or £2 5s.
If, for example, Chili bars, containing 96 per cent. of copper, bring £50 per
ton, the standard is £71 9s. 4d. It is got at in this way. The returning charge
on a 96 per cent. ore is 12s. 2d.+(96×3s. 9d.), or £18 12s. 2d. This added to
£50 gives £68 12s. 2d., and this multiplied by 100 and divided by 96 (100
tons of the bars will contain 96 tons of fine copper) will give £71 9s. 4d.
The price of 100 tons of pyrites, containing 2-1/4 per cent. of copper by dry
assay, would be got on this standard as follows:—The parcel of ore would
Page 237
contain 2-1/4 tons of copper. This multiplied by the standard gives £160
16s. 0d. From this must be deducted the returning charge, which for 1 ton of
ore of this produce would be 12s. 2d. + (2-1/4 × 3s. 9d.) or £1 0s. 7d., and
on the 100 tons is £102 18s. 4d. This would leave £57 17s. 10d. as the price
of the parcel, or 11s. 7d. per ton. This would be on the standard returning
charge of 45s. (for 8-3/4 per cent. ore); if a smaller returning charge was
agreed on, say 38s., the difference in this case, 7s., would be added to the
price per ton.
WET METHODS.
The solubility of the ores of copper in acid has already been described, but
certain furnace products, such as slags, are best opened up by fusion with
fusion mixture and a little nitre.
The method of dissolving varies with the nature of the ore. With 5 grams of
pyrites, a single evaporation with 20 c.c. of nitric acid will give a residue
completely soluble in 30 c.c. of hydrochloric acid. If the ore carries oxide of
iron or similar bodies, these are first dissolved up by boiling with 20 c.c. of
hydrochloric acid, and the residue attacked by an addition of 5 c.c. of nitric.
When silicates decomposable by acid are present, the solution is evaporated
to dryness to render the silica insoluble; the residue extracted with 30 c.c. of
hydrochloric acid, and diluted with water to 150 c.c. It is advisable to have
the copper in solution as chloride. To separate the copper, heat the solution
nearly to boiling (best in a pint flask), and pass a rapid current of
sulphuretted hydrogen for four or five minutes until the precipitate settles
readily and the liquid smells of the gas. When iron is present it will be
reduced to the ferrous state before the copper sulphide begins to separate.
The copper appears as a brown coloration or black precipitate according to
the quantity present. Filter through a coarse filter, wash with hot water
containing sulphuretted hydrogen, if necessary. Wash the precipitate back
into the flask, boil with 10 c.c. of nitric acid, add soda till alkaline, and pass
sulphuretted hydrogen again. Warm and filter, wash and redissolve in nitric
acid, neutralise with ammonia, add ammonic carbonate, boil and filter. The
copper freed from impurities will be in the solution. Acidulate and
reprecipitate with sulphuretted hydrogen. When the nature of the impurities
will allow it, this process may be shortened to first filtering off the gangue,
16s. 0d. From this must be deducted the returning charge, which for 1 ton of
ore of this produce would be 12s. 2d. + (2-1/4 × 3s. 9d.) or £1 0s. 7d., and
on the 100 tons is £102 18s. 4d. This would leave £57 17s. 10d. as the price
of the parcel, or 11s. 7d. per ton. This would be on the standard returning
charge of 45s. (for 8-3/4 per cent. ore); if a smaller returning charge was
agreed on, say 38s., the difference in this case, 7s., would be added to the
price per ton.
WET METHODS.
The solubility of the ores of copper in acid has already been described, but
certain furnace products, such as slags, are best opened up by fusion with
fusion mixture and a little nitre.
The method of dissolving varies with the nature of the ore. With 5 grams of
pyrites, a single evaporation with 20 c.c. of nitric acid will give a residue
completely soluble in 30 c.c. of hydrochloric acid. If the ore carries oxide of
iron or similar bodies, these are first dissolved up by boiling with 20 c.c. of
hydrochloric acid, and the residue attacked by an addition of 5 c.c. of nitric.
When silicates decomposable by acid are present, the solution is evaporated
to dryness to render the silica insoluble; the residue extracted with 30 c.c. of
hydrochloric acid, and diluted with water to 150 c.c. It is advisable to have
the copper in solution as chloride. To separate the copper, heat the solution
nearly to boiling (best in a pint flask), and pass a rapid current of
sulphuretted hydrogen for four or five minutes until the precipitate settles
readily and the liquid smells of the gas. When iron is present it will be
reduced to the ferrous state before the copper sulphide begins to separate.
The copper appears as a brown coloration or black precipitate according to
the quantity present. Filter through a coarse filter, wash with hot water
containing sulphuretted hydrogen, if necessary. Wash the precipitate back
into the flask, boil with 10 c.c. of nitric acid, add soda till alkaline, and pass
sulphuretted hydrogen again. Warm and filter, wash and redissolve in nitric
acid, neutralise with ammonia, add ammonic carbonate, boil and filter. The
copper freed from impurities will be in the solution. Acidulate and
reprecipitate with sulphuretted hydrogen. When the nature of the impurities
will allow it, this process may be shortened to first filtering off the gangue,
Page 238
then precipitating with sulphuretted hydrogen and washing the precipitate
on the filter first with water and then with ammonium sulphide.
Having separated the copper as sulphide, its weight is determined as
follows. Dry and transfer to a weighed porcelain crucible, mix with a little
pure sulphur, and ignite at a red heat for 5 or 10 minutes in a current of
hydrogen. Allow to cool while the hydrogen is still passing. Weigh. The
subsulphide of copper thus obtained contains 79.85 per cent. of copper; it is
a greyish-black crystalline mass, which loses no weight on ignition if air is
excluded.
Copper may be separated from its solutions by means of sodium
hyposulphite. The solution is freed from hydrochloric and nitric acids by
evaporation with sulphuric acid; diluted to about a quarter of a litre; heated
nearly to boiling; and treated with a hot solution of sodium hyposulphite
(added a little at a time) until the precipitate settles and leaves the solution
free from colour. The solution contains suspended sulphur. The precipitate
is easily washed, and under the proper conditions the separation is
complete, but the separation with sulphuretted hydrogen is more
satisfactory, since the conditions as to acidity, &c., need not be so exact.
Zinc or iron is sometimes used for separating copper from its solutions, but
they are not to be recommended.
ELECTROLYTIC ASSAY.
The separation of copper by means of a current of electricity is largely
made use of, and forms the basis of the most satisfactory method for the
determination of this metal. If the wire closing an electric circuit be broken,
and the two ends immersed in a beaker of acidulated water or solution of
any salt, the electricity will pass through the liquid, bringing about some
remarkable changes. Hydrogen and the metals will be liberated around that
part of the wire connected with the zinc end of the battery, and oxygen,
chlorine, and the acid radicals will be set free around the other. Different
metals are deposited in this way with varying degrees of ease, and whether
or not any particular metal will be deposited depends—(1) on the conditions
of the solution as regards acid and other substances present, and (2) on the
intensity of the current of electricity used. For analytical purposes the metal
on the filter first with water and then with ammonium sulphide.
Having separated the copper as sulphide, its weight is determined as
follows. Dry and transfer to a weighed porcelain crucible, mix with a little
pure sulphur, and ignite at a red heat for 5 or 10 minutes in a current of
hydrogen. Allow to cool while the hydrogen is still passing. Weigh. The
subsulphide of copper thus obtained contains 79.85 per cent. of copper; it is
a greyish-black crystalline mass, which loses no weight on ignition if air is
excluded.
Copper may be separated from its solutions by means of sodium
hyposulphite. The solution is freed from hydrochloric and nitric acids by
evaporation with sulphuric acid; diluted to about a quarter of a litre; heated
nearly to boiling; and treated with a hot solution of sodium hyposulphite
(added a little at a time) until the precipitate settles and leaves the solution
free from colour. The solution contains suspended sulphur. The precipitate
is easily washed, and under the proper conditions the separation is
complete, but the separation with sulphuretted hydrogen is more
satisfactory, since the conditions as to acidity, &c., need not be so exact.
Zinc or iron is sometimes used for separating copper from its solutions, but
they are not to be recommended.
ELECTROLYTIC ASSAY.
The separation of copper by means of a current of electricity is largely
made use of, and forms the basis of the most satisfactory method for the
determination of this metal. If the wire closing an electric circuit be broken,
and the two ends immersed in a beaker of acidulated water or solution of
any salt, the electricity will pass through the liquid, bringing about some
remarkable changes. Hydrogen and the metals will be liberated around that
part of the wire connected with the zinc end of the battery, and oxygen,
chlorine, and the acid radicals will be set free around the other. Different
metals are deposited in this way with varying degrees of ease, and whether
or not any particular metal will be deposited depends—(1) on the conditions
of the solution as regards acid and other substances present, and (2) on the
intensity of the current of electricity used. For analytical purposes the metal
Page 239
should be deposited not only free from the other metals present, but also as
a firm coherent film, which may afterwards be manipulated without fear of
loss. This is, in the case of copper and many other metals, effected by a
simple control of the conditions. It is necessary that the electrodes, or wires
which bring the electricity into the solution, should be made of a material to
which the deposited metal will adhere, and which will not be attacked by
substances originally present or set free in the solution. They are generally
made of platinum. There are various arrangements of apparatus used for this
purpose, but the following plan and method of working is simple and
effective, and has been in daily use with very satisfactory results for the last
five or six years.
The battery used is made up of two Daniell cells, coupled up for intensity as
shown in fig. 49—that is, with the copper of one connected with the zinc of
the other. For eight or ten assays daily the quart size should be used, but for
four or five two pint cells will be sufficient.
The outer pot of each cell is made of sheet copper, and must be clean and
free from solder on the inside. It is provided near the top with a perforated
copper shelf in the shape of a ring, into which the inner or porous cell
loosely fits. It is charged with a saturated solution of copper sulphate, and
crystals of this salt must be added, and always kept in excess. When the
battery is at work copper is being deposited on the inner surface of this pot.
a firm coherent film, which may afterwards be manipulated without fear of
loss. This is, in the case of copper and many other metals, effected by a
simple control of the conditions. It is necessary that the electrodes, or wires
which bring the electricity into the solution, should be made of a material to
which the deposited metal will adhere, and which will not be attacked by
substances originally present or set free in the solution. They are generally
made of platinum. There are various arrangements of apparatus used for this
purpose, but the following plan and method of working is simple and
effective, and has been in daily use with very satisfactory results for the last
five or six years.
The battery used is made up of two Daniell cells, coupled up for intensity as
shown in fig. 49—that is, with the copper of one connected with the zinc of
the other. For eight or ten assays daily the quart size should be used, but for
four or five two pint cells will be sufficient.
The outer pot of each cell is made of sheet copper, and must be clean and
free from solder on the inside. It is provided near the top with a perforated
copper shelf in the shape of a ring, into which the inner or porous cell
loosely fits. It is charged with a saturated solution of copper sulphate, and
crystals of this salt must be added, and always kept in excess. When the
battery is at work copper is being deposited on the inner surface of this pot.
Page 240
The inner or porous pot contains the zinc rod, and is charged with a dilute
acid, made by diluting one volume of sulphuric acid up to ten with water.
The object of the porous pot is to prevent the mixing of the acid and copper
sulphate solutions, without interrupting the flow of electricity. The copper
sulphate solution will last for months, but the acid must be emptied out and
recharged daily.
The zinc rods must be well amalgamated by rubbing with mercury under
dilute acid until they show a uniformly bright surface. They should not
produce a brisk effervescence when placed in the acid in the porous pot
before coupling up.
The battery when working is apt to become dirty from the "creeping" of the
copper and zinc sulphate solution. It must be kept away from the working
bench, and is best kept in a box on the floor.
The connection of the battery with, and the fixing of, the electrodes may be
made by any suitable arrangement, but the following is a very convenient
plan. The wire from the zinc is connected by means of a binding screw with
a piece of stout copper wire, which, at a distance sufficiently great to allow
of easy coupling with the battery, is led along the back of a piece of hard
wood. This is fixed horizontally about one foot above the working bench.
The general arrangement is shown in fig. 50, in which, however, for the
sake of economy of space, the battery is placed on the working bench
instead of on the floor. The piece of wood is one inch square and three or
four feet long. It is perforated from front to back at distances of six inches
by a number of small holes, in which are inserted screws like that shown in
fig. 51. These are known as "terminals," and may be obtained of any
electrician. The head of each screw is soldered to the wire mentioned above
acid, made by diluting one volume of sulphuric acid up to ten with water.
The object of the porous pot is to prevent the mixing of the acid and copper
sulphate solutions, without interrupting the flow of electricity. The copper
sulphate solution will last for months, but the acid must be emptied out and
recharged daily.
The zinc rods must be well amalgamated by rubbing with mercury under
dilute acid until they show a uniformly bright surface. They should not
produce a brisk effervescence when placed in the acid in the porous pot
before coupling up.
The battery when working is apt to become dirty from the "creeping" of the
copper and zinc sulphate solution. It must be kept away from the working
bench, and is best kept in a box on the floor.
The connection of the battery with, and the fixing of, the electrodes may be
made by any suitable arrangement, but the following is a very convenient
plan. The wire from the zinc is connected by means of a binding screw with
a piece of stout copper wire, which, at a distance sufficiently great to allow
of easy coupling with the battery, is led along the back of a piece of hard
wood. This is fixed horizontally about one foot above the working bench.
The general arrangement is shown in fig. 50, in which, however, for the
sake of economy of space, the battery is placed on the working bench
instead of on the floor. The piece of wood is one inch square and three or
four feet long. It is perforated from front to back at distances of six inches
by a number of small holes, in which are inserted screws like that shown in
fig. 51. These are known as "terminals," and may be obtained of any
electrician. The head of each screw is soldered to the wire mentioned above
Page 241
as running along the back and as being connected with the zinc end of the
battery. These terminals serve to fix the electrodes on which the copper is to
be deposited. The wire from the copper end of the battery is similarly
connected by a connecting screw (fig. 52) with another wire (H in fig. 53),
which runs along the top of the rod and has soldered to it, at distances of six
inches, cylindrical spirals of copper wire. These should project from the rod
at points about half-way between the terminals already described. They may
be made by wrapping copper wire around a black-lead pencil for a length of
about three inches.
battery. These terminals serve to fix the electrodes on which the copper is to
be deposited. The wire from the copper end of the battery is similarly
connected by a connecting screw (fig. 52) with another wire (H in fig. 53),
which runs along the top of the rod and has soldered to it, at distances of six
inches, cylindrical spirals of copper wire. These should project from the rod
at points about half-way between the terminals already described. They may
be made by wrapping copper wire around a black-lead pencil for a length of
about three inches.
Page 242
The rod is perforated from top to bottom with a series of small holes, one in
advance of each terminal but as near it as possible. Into these short pieces of
glass tube are inserted to ensure insulation. These receive the other
electrodes, which are connected with the wire leading to the copper end of
the battery, through the spirals, with the help of a binding screw. The figure
will make this clear. (Fig. 53.)
advance of each terminal but as near it as possible. Into these short pieces of
glass tube are inserted to ensure insulation. These receive the other
electrodes, which are connected with the wire leading to the copper end of
the battery, through the spirals, with the help of a binding screw. The figure
will make this clear. (Fig. 53.)
Page 243
The electrodes consist of a platinum spiral and cylinder. The spiral should
have the shape shown in A, fig. 54. When in work it is passed through one
of the holes fitted with glass tubes and connected with the copper end of the
battery. The thickness of the wire of which it is made is unimportant,
provided it is stout enough to keep its form and does not easily bend. The
spiral will weigh about 8 grams. The cylinder (C, fig. 54) will weigh about
12 grams. It should have the shape shown in the figure. In working it is
clamped to one of the terminals, and on it the copper is deposited. A
cylinder will serve for the deposition of from 1 to 1.5 gram of copper. It is
made by rivetting a square piece of foil on to a stiff piece of wire, and then
bending into shape over a glass tube or piece of rounded wood. Each
cylinder carries a distinctive number, and is marked by impressing Roman
numerals on the foil with the blade of a knife. The weight of each is
carefully taken and recorded. They lose slightly in weight when in use, but
the loss is uniform, and averages half a milligram per month when in daily
use. The cylinders are cleaned from deposited copper by dissolving off with
nitric acid and washing with water; and from grease by igniting.
have the shape shown in A, fig. 54. When in work it is passed through one
of the holes fitted with glass tubes and connected with the copper end of the
battery. The thickness of the wire of which it is made is unimportant,
provided it is stout enough to keep its form and does not easily bend. The
spiral will weigh about 8 grams. The cylinder (C, fig. 54) will weigh about
12 grams. It should have the shape shown in the figure. In working it is
clamped to one of the terminals, and on it the copper is deposited. A
cylinder will serve for the deposition of from 1 to 1.5 gram of copper. It is
made by rivetting a square piece of foil on to a stiff piece of wire, and then
bending into shape over a glass tube or piece of rounded wood. Each
cylinder carries a distinctive number, and is marked by impressing Roman
numerals on the foil with the blade of a knife. The weight of each is
carefully taken and recorded. They lose slightly in weight when in use, but
the loss is uniform, and averages half a milligram per month when in daily
use. The cylinders are cleaned from deposited copper by dissolving off with
nitric acid and washing with water; and from grease by igniting.
Page 244
The beakers, to contain the solution of copper to be electrolysed, are
ordinary tall beakers of about 200 c.c. capacity, and are marked off at 100
c.c. and 150 c.c. They are supported on movable stands, consisting of
wooden blocks about six inches high and three inches across. The bar of
wood which carries the connecting wires and electrodes is permanently
fixed over the working bench, at such a height that, with the beakers resting
on these blocks, the electrodes shall be in position for working.
To fix the electrodes to the rod, remove the stand and beaker and pass the
long limb of the spiral up through one of the glass tubes. Connect it with the
free end of the copper spiral by means of a connecting screw (fig. 52), and
then draw out and bend the copper spiral so that the platinum one may hang
freely. Screw the wire of the cylinder to the terminal, and, if necessary, bend
it so that the cylinder itself may be brought to encircle the rod of the spiral
in the manner shown in fig. 53.
The general method of working is as follows:—The quantity of ore to be
taken for an assay varies with the richness of the ore, as is shown in the
following table:—
Percentage of Copper in the Ore. Quantity of Ore to be taken.
1 to 5 5 grams
5 to 10 3 "
10 to 30 2 "
30 to 50 1.5 "
50 to 100 1 "
The weighed quantity of ore is dissolved by evaporating with nitric acid and
taking up with hydrochloric, as already described. Any coloured residue
which may be left is generally organic matter: it is filtered off, calcined, and
any copper it contains is estimated colorimetrically. Nearly always,
however, the residue is white and sandy. The copper is separated from the
solution as sulphide by means of a rapid current of sulphuretted hydrogen.
The liquid is decanted off through a filter, the precipitate washed once with
hot water and then rinsed back into the flask (the filter paper being opened
out) with a jet of water from a wash bottle. Fifteen c.c. of nitric acid are
added to the contents of the flask, which are then briskly boiled until the
bulk is reduced to less than 10 c.c. The boiling down is carried out in a
ordinary tall beakers of about 200 c.c. capacity, and are marked off at 100
c.c. and 150 c.c. They are supported on movable stands, consisting of
wooden blocks about six inches high and three inches across. The bar of
wood which carries the connecting wires and electrodes is permanently
fixed over the working bench, at such a height that, with the beakers resting
on these blocks, the electrodes shall be in position for working.
To fix the electrodes to the rod, remove the stand and beaker and pass the
long limb of the spiral up through one of the glass tubes. Connect it with the
free end of the copper spiral by means of a connecting screw (fig. 52), and
then draw out and bend the copper spiral so that the platinum one may hang
freely. Screw the wire of the cylinder to the terminal, and, if necessary, bend
it so that the cylinder itself may be brought to encircle the rod of the spiral
in the manner shown in fig. 53.
The general method of working is as follows:—The quantity of ore to be
taken for an assay varies with the richness of the ore, as is shown in the
following table:—
Percentage of Copper in the Ore. Quantity of Ore to be taken.
1 to 5 5 grams
5 to 10 3 "
10 to 30 2 "
30 to 50 1.5 "
50 to 100 1 "
The weighed quantity of ore is dissolved by evaporating with nitric acid and
taking up with hydrochloric, as already described. Any coloured residue
which may be left is generally organic matter: it is filtered off, calcined, and
any copper it contains is estimated colorimetrically. Nearly always,
however, the residue is white and sandy. The copper is separated from the
solution as sulphide by means of a rapid current of sulphuretted hydrogen.
The liquid is decanted off through a filter, the precipitate washed once with
hot water and then rinsed back into the flask (the filter paper being opened
out) with a jet of water from a wash bottle. Fifteen c.c. of nitric acid are
added to the contents of the flask, which are then briskly boiled until the
bulk is reduced to less than 10 c.c. The boiling down is carried out in a
Page 245
cupboard free from cold draughts, so as to prevent the condensation of acid
and steam in the neck of the flask. Twenty c.c. of water are next added, and
the solution is warmed, and filtered into one of the beakers for electrolysis.
The filtrate and washings are diluted with water to the 100 c.c. mark, and
the solution is then ready for the battery. It must not contain more than 10
per cent. by volume of nitric acid.
The number and weight of the platinum cylinder having been recorded,
both electrodes are fixed in position and the wooden block removed from
under them. The beaker containing the copper solution is then brought up
into its place with one hand, and the block replaced with the other so as to
support it. All the assays having been got into position, the connecting wires
are joined to the battery. If everything is right bubbles of oxygen at once
stream off from the spiral, and the cylinder becomes tarnished by a deposit
of copper. If the oxygen comes off but no copper is deposited, it is because
the assay solution contains too much nitric acid. If no action whatever takes
place, it is because the current is not passing. In this case examine the
connections to see that they are clean and secure, and the connecting wires
to see that they are not touching each other.
The action is allowed to go on for sixteen or seventeen hours, so that it is
best to let the current act overnight. In the morning the solutions will appear
colourless, and a slow stream of oxygen will still be coming off from the
spiral.
A wash-bottle with cold distilled water and two beakers, one with distilled
water and the other with alcohol, are got ready. The block is then removed,
the spiral loosened and lowered with the beaker. The cylinder is next
detached and washed with a stream of water from the wash-bottle, the
washings being added to the original solution. The current from the battery
is not stopped until all the cylinders are washed. After being dipped in the
beaker of water and once or twice in that with the alcohol, it is dried in the
water-oven for about three minutes, and then weighed. The increase in
weight is due to deposited copper. This should be salmon-red in colour,
satin-like or crystalline in appearance, and in an even coherent deposit, not
removed by rubbing. It is permanent in air when dry, but sulphuretted
hydrogen quickly tarnishes it, producing coloured films. With ores
containing even very small proportions of bismuth, the deposited copper
and steam in the neck of the flask. Twenty c.c. of water are next added, and
the solution is warmed, and filtered into one of the beakers for electrolysis.
The filtrate and washings are diluted with water to the 100 c.c. mark, and
the solution is then ready for the battery. It must not contain more than 10
per cent. by volume of nitric acid.
The number and weight of the platinum cylinder having been recorded,
both electrodes are fixed in position and the wooden block removed from
under them. The beaker containing the copper solution is then brought up
into its place with one hand, and the block replaced with the other so as to
support it. All the assays having been got into position, the connecting wires
are joined to the battery. If everything is right bubbles of oxygen at once
stream off from the spiral, and the cylinder becomes tarnished by a deposit
of copper. If the oxygen comes off but no copper is deposited, it is because
the assay solution contains too much nitric acid. If no action whatever takes
place, it is because the current is not passing. In this case examine the
connections to see that they are clean and secure, and the connecting wires
to see that they are not touching each other.
The action is allowed to go on for sixteen or seventeen hours, so that it is
best to let the current act overnight. In the morning the solutions will appear
colourless, and a slow stream of oxygen will still be coming off from the
spiral.
A wash-bottle with cold distilled water and two beakers, one with distilled
water and the other with alcohol, are got ready. The block is then removed,
the spiral loosened and lowered with the beaker. The cylinder is next
detached and washed with a stream of water from the wash-bottle, the
washings being added to the original solution. The current from the battery
is not stopped until all the cylinders are washed. After being dipped in the
beaker of water and once or twice in that with the alcohol, it is dried in the
water-oven for about three minutes, and then weighed. The increase in
weight is due to deposited copper. This should be salmon-red in colour,
satin-like or crystalline in appearance, and in an even coherent deposit, not
removed by rubbing. It is permanent in air when dry, but sulphuretted
hydrogen quickly tarnishes it, producing coloured films. With ores
containing even very small proportions of bismuth, the deposited copper
Page 246
has a dark grey colour, and when much of this metal is present the copper is
coated with a grey shaggy deposit.
It still remains to determine any copper left undeposited in the solution.
This does not generally exceed four or five milligrams, and is estimated
colorimetrically. Thirty c.c. of dilute ammonia (one of strong ammonia
mixed with one of water) are added to the electrolysed solution, which is
then diluted up to the 150 c.c. mark with water. It is mixed, using the spiral
as stirrer, and, after standing a few minutes to allow the precipitate to settle,
100 c.c. of it are filtered off through a dry filter for the colorimetric
determination. Since only two-thirds of the solution are taken for this, the
quantity of copper found must be increased by one-half to get the quantity
actually present.
The colorimetric determination may be made in the manner described
under that head, but where a number of assays are being carried out it is
more convenient to have a series of standard phials containing known
amounts of copper in ammoniacal solution. By comparing the measured
volume of the assay solution with these, the amount of copper present is
coated with a grey shaggy deposit.
It still remains to determine any copper left undeposited in the solution.
This does not generally exceed four or five milligrams, and is estimated
colorimetrically. Thirty c.c. of dilute ammonia (one of strong ammonia
mixed with one of water) are added to the electrolysed solution, which is
then diluted up to the 150 c.c. mark with water. It is mixed, using the spiral
as stirrer, and, after standing a few minutes to allow the precipitate to settle,
100 c.c. of it are filtered off through a dry filter for the colorimetric
determination. Since only two-thirds of the solution are taken for this, the
quantity of copper found must be increased by one-half to get the quantity
actually present.
The colorimetric determination may be made in the manner described
under that head, but where a number of assays are being carried out it is
more convenient to have a series of standard phials containing known
amounts of copper in ammoniacal solution. By comparing the measured
volume of the assay solution with these, the amount of copper present is
Page 247
determined at a glance. These standard bottles, however, can only be
economically used where a large number of assays are being made daily.
A convenient plan is to get a quantity of white glass four-ounce phials, like
that in fig. 55, and to label them so that they shall contain 100 c.c. when
filled up to the bottom of the labels. The labels should be rendered
permanent by coating with wax, and be marked with numbers indicating the
milligrams of copper present. The bottles are stopped with new clean corks,
and contain, in addition to the specified quantity of copper, 6 c.c. of nitric
acid and 10 c.c. of strong ammonia, with sufficient water to make up the
bulk to 100 c.c. The copper is best added by running in the requisite amount
of a standard solution of copper, each c.c. of which contains 0.001 gram of
the metal.
The standard bottles should be refilled once every three or four months,
since their colorimetric value becomes slowly less on keeping. The
following determinations of a set which had been in use for three months
will illustrate this. The figures indicate milligrams of copper in 100 c.c.: the
first row gives the nominal and the second row the actual colorimetric value
of the standards. The difference between the two shows the deterioration.
1 2 3 4 6 8 10 12 14
1 2 3 3.7 5.5 7.5 9 11 13
The amount of copper in the assay is got by increasing that found
colorimetrically by one-half and adding to that found on the platinum
cylinder. The percentage is calculated in the usual way. The following
examples will illustrate this, as well as the method of recording the work in
the laboratory book:—
_____________________________________________
Cylinder I. + Cu 9.5410
Cylinder I. 9.5170
——————
0.0240
By colour 100 c.c. = 0.0015}
0.0007} 0.0022
—————— ——————
0.0022 0.0262
IX. Sample. Took 5 grams.
economically used where a large number of assays are being made daily.
A convenient plan is to get a quantity of white glass four-ounce phials, like
that in fig. 55, and to label them so that they shall contain 100 c.c. when
filled up to the bottom of the labels. The labels should be rendered
permanent by coating with wax, and be marked with numbers indicating the
milligrams of copper present. The bottles are stopped with new clean corks,
and contain, in addition to the specified quantity of copper, 6 c.c. of nitric
acid and 10 c.c. of strong ammonia, with sufficient water to make up the
bulk to 100 c.c. The copper is best added by running in the requisite amount
of a standard solution of copper, each c.c. of which contains 0.001 gram of
the metal.
The standard bottles should be refilled once every three or four months,
since their colorimetric value becomes slowly less on keeping. The
following determinations of a set which had been in use for three months
will illustrate this. The figures indicate milligrams of copper in 100 c.c.: the
first row gives the nominal and the second row the actual colorimetric value
of the standards. The difference between the two shows the deterioration.
1 2 3 4 6 8 10 12 14
1 2 3 3.7 5.5 7.5 9 11 13
The amount of copper in the assay is got by increasing that found
colorimetrically by one-half and adding to that found on the platinum
cylinder. The percentage is calculated in the usual way. The following
examples will illustrate this, as well as the method of recording the work in
the laboratory book:—
_____________________________________________
Cylinder I. + Cu 9.5410
Cylinder I. 9.5170
——————
0.0240
By colour 100 c.c. = 0.0015}
0.0007} 0.0022
—————— ——————
0.0022 0.0262
IX. Sample. Took 5 grams.
Page 248
Copper = 0.52%
_____________________________________________
Cylinder VI. + Cu 10.5705
Cylinder VI. 10.0437
——————
0.5268
By colour, 100 c.c. = 0.0070}
0.0035} 0.0105
—————— ——————
0.0105 0.5373
Matte, No. 1070. Took 1.5 gram.
Copper = 35.82%
_____________________________________________
Cylinder XIII. + Cu 12.0352
Cylinder XIII. 11.0405
——————
0.9947
By colour 100 c.c. = 0.0005}
0.0002} 0.0007
—————— ——————
0.0007 0.9954
X. Sample, Cake copper. Took 1.0053 gram.
Copper = 99.00%
____________________________________________
In the electrolytic assay of metals, alloys, precipitates, and other bodies rich
in copper, the preliminary separation of the copper by sulphuretted
hydrogen is unnecessary. It is sufficient to dissolve the weighed sample in
10 c.c. of nitric acid, boil off nitrous fumes, dilute to 100 c.c. with water,
and then electrolyse.
General Considerations.—In the preliminary work with the copper
sulphide there is a small loss owing to its imperfect removal in washing the
filter paper, and another small loss in dissolving in nitric acid owing to the
retention of particles in the fused globules of sulphur. To determine its
amount the filter-papers and sulphur were collected from forty assays, and
the copper in them determined. The average amount of copper in each assay
was 0.175 gram; that left on the filter paper was 0.00067 gram; and that
retained by the sulphur 0.00003 gram; thus showing an average loss from
both sources of 0.00070 gram. The determinations from another lot of forty-
two similar assays gave on an average
Copper left on filter paper 0.00070gram
_____________________________________________
Cylinder VI. + Cu 10.5705
Cylinder VI. 10.0437
——————
0.5268
By colour, 100 c.c. = 0.0070}
0.0035} 0.0105
—————— ——————
0.0105 0.5373
Matte, No. 1070. Took 1.5 gram.
Copper = 35.82%
_____________________________________________
Cylinder XIII. + Cu 12.0352
Cylinder XIII. 11.0405
——————
0.9947
By colour 100 c.c. = 0.0005}
0.0002} 0.0007
—————— ——————
0.0007 0.9954
X. Sample, Cake copper. Took 1.0053 gram.
Copper = 99.00%
____________________________________________
In the electrolytic assay of metals, alloys, precipitates, and other bodies rich
in copper, the preliminary separation of the copper by sulphuretted
hydrogen is unnecessary. It is sufficient to dissolve the weighed sample in
10 c.c. of nitric acid, boil off nitrous fumes, dilute to 100 c.c. with water,
and then electrolyse.
General Considerations.—In the preliminary work with the copper
sulphide there is a small loss owing to its imperfect removal in washing the
filter paper, and another small loss in dissolving in nitric acid owing to the
retention of particles in the fused globules of sulphur. To determine its
amount the filter-papers and sulphur were collected from forty assays, and
the copper in them determined. The average amount of copper in each assay
was 0.175 gram; that left on the filter paper was 0.00067 gram; and that
retained by the sulphur 0.00003 gram; thus showing an average loss from
both sources of 0.00070 gram. The determinations from another lot of forty-
two similar assays gave on an average
Copper left on filter paper 0.00070gram
Page 249
Copper retained by sulphur. 0.00004"
The loss from these sources is trifling, and need only be considered when
great accuracy is required.
The deposition of the copper under the conditions given is satisfactory, but,
as already stated, if the solution contain more than 10 per cent. of nitric acid
it is not thrown down at all; or if a stronger current is used, say that from
three Bunsen cells, it will be precipitated in an arborescent brittle form, ill
adapted for weighing. It may be noted here that increasing the size of the
cells does not necessarily increase the intensity of the current.
In two determinations on pure electrotype copper the following results were
obtained:—
Copper Taken. Copper Found.
0.8988 gram 0.8985 gram
0.8305 " 0.8303 "
The presence of salts of ammonia, &c., somewhat retards the deposition,
but has no other ill effect.
The organic matter generally present in copper ores interferes more
especially in the colorimetric determination of the residual copper. It can be
detected on dissolving the ore as a light black residue insoluble in nitric
acid. It is filtered off at once, or, if only present in small amount, it is
carried on in the ordinary process of the assay and separated in the last
filtration before electrolysis.
The following experiments were made to test the effect of the presence of
salts of foreign metals in the solution during the precipitation of copper by
electrolysis:—
Copper Taken. Other Metal Added. Copper Found.
0.1000 gram 0.1000 gram of silver 0.1800
0.1050 " 0.1000 " " 0.2000
0.1030 " 0.1000 " mercury 0.2010
0.1037 " 0.1000 " " 0.2015
The loss from these sources is trifling, and need only be considered when
great accuracy is required.
The deposition of the copper under the conditions given is satisfactory, but,
as already stated, if the solution contain more than 10 per cent. of nitric acid
it is not thrown down at all; or if a stronger current is used, say that from
three Bunsen cells, it will be precipitated in an arborescent brittle form, ill
adapted for weighing. It may be noted here that increasing the size of the
cells does not necessarily increase the intensity of the current.
In two determinations on pure electrotype copper the following results were
obtained:—
Copper Taken. Copper Found.
0.8988 gram 0.8985 gram
0.8305 " 0.8303 "
The presence of salts of ammonia, &c., somewhat retards the deposition,
but has no other ill effect.
The organic matter generally present in copper ores interferes more
especially in the colorimetric determination of the residual copper. It can be
detected on dissolving the ore as a light black residue insoluble in nitric
acid. It is filtered off at once, or, if only present in small amount, it is
carried on in the ordinary process of the assay and separated in the last
filtration before electrolysis.
The following experiments were made to test the effect of the presence of
salts of foreign metals in the solution during the precipitation of copper by
electrolysis:—
Copper Taken. Other Metal Added. Copper Found.
0.1000 gram 0.1000 gram of silver 0.1800
0.1050 " 0.1000 " " 0.2000
0.1030 " 0.1000 " mercury 0.2010
0.1037 " 0.1000 " " 0.2015
Page 250
0.1020 " 0.1000 " lead 0.1020
0.1030 " 0.1000 " " 0.1028
0.1010 " 0.1000 " arsenic 0.1010
0.1007 " 0.1000 " " 0.1022
0.1030 " 0.1000 " antimony 0.1050
0.1034 " 0.1000 " " 0.1057
0.0990 " 0.1200 " tin 0.0990
0.1014 " 0.1000 " " 0.1015
0.1000 " 0.1000 " bismuth 0.1662
0.1040 " 0.1000 " of cadmium 0.1052
0.1009 " 0.1300 " zinc 0.1017
0.1014 " 0.1000 " nickel 0.1007
0.1079 " 0.1200 " iron 0.1089
0.1054 " 0.1000 " chromium (Cr2O3) 0.1035
0.1034 " 0.1000 " " (K2CrO4) 0.1010
0.1075 " 0.1000 " aluminium 0.1078
0.1010 " 0.1000 " manganese 0.0980
It will be seen from these that mercury, silver, and bismuth are the only
metals which are precipitable[52] along with the copper under the conditions
of the assay. Mercury, which if present would interfere, is separated because
of the insolubility of its sulphide in nitric acid.
Bismuth is precipitated only after the main portion of the copper is thrown
down. It renders the copper obviously unsuitable for weighing. It darkens,
or forms a greyish coating on, the copper; and this darkening is a delicate
test for bismuth. In assaying ores containing about three and a half per cent.
of copper, and known to contain bismuth in quantities scarcely detectable in
ordinary analysis, the metal deposited was distinctly greyish in colour, and
would not be mistaken for pure copper. Ten grams of this impure copper
were collected and analysed, with the following results:—
Copper 99.46per cent.
Bismuth 00.30 "
Iron 00.14 "
0.1030 " 0.1000 " " 0.1028
0.1010 " 0.1000 " arsenic 0.1010
0.1007 " 0.1000 " " 0.1022
0.1030 " 0.1000 " antimony 0.1050
0.1034 " 0.1000 " " 0.1057
0.0990 " 0.1200 " tin 0.0990
0.1014 " 0.1000 " " 0.1015
0.1000 " 0.1000 " bismuth 0.1662
0.1040 " 0.1000 " of cadmium 0.1052
0.1009 " 0.1300 " zinc 0.1017
0.1014 " 0.1000 " nickel 0.1007
0.1079 " 0.1200 " iron 0.1089
0.1054 " 0.1000 " chromium (Cr2O3) 0.1035
0.1034 " 0.1000 " " (K2CrO4) 0.1010
0.1075 " 0.1000 " aluminium 0.1078
0.1010 " 0.1000 " manganese 0.0980
It will be seen from these that mercury, silver, and bismuth are the only
metals which are precipitable[52] along with the copper under the conditions
of the assay. Mercury, which if present would interfere, is separated because
of the insolubility of its sulphide in nitric acid.
Bismuth is precipitated only after the main portion of the copper is thrown
down. It renders the copper obviously unsuitable for weighing. It darkens,
or forms a greyish coating on, the copper; and this darkening is a delicate
test for bismuth. In assaying ores containing about three and a half per cent.
of copper, and known to contain bismuth in quantities scarcely detectable in
ordinary analysis, the metal deposited was distinctly greyish in colour, and
would not be mistaken for pure copper. Ten grams of this impure copper
were collected and analysed, with the following results:—
Copper 99.46per cent.
Bismuth 00.30 "
Iron 00.14 "
Page 251
Arsenic 00.10 "
———
100.00
The quantity of copper got in each assay was 0.175 gram, and consequently
the bismuth averaged 0.00053 gram.
To separate the bismuth in such a case the deposit is dissolved off by
warming it in the original solution. The bismuth is precipitated by the
addition of ammonic carbonate, and the solution, after filtering and
acidifying with nitric acid, is re-electrolysed.
Determination of Copper in Commercial Copper.—Take from 1 to 1.5
gram, weigh carefully, and transfer to a beaker; add 20 c.c. of water and 10
c.c. of nitric acid; cover with a clock glass, and allow to dissolve with
moderate action; boil off nitrous fumes, dilute to 100 c.c., and electrolyse.
The cylinder must be carefully weighed, and the electrolysis allowed to
proceed for 24 hours. The weight found will be that of the copper and silver.
The silver in it must be determined[53] and deducted.
Determination of Copper in Brass, German Silver, or Bronze.—Treat in
the same manner as commercial copper. If nickel is present, the few
milligrams of copper remaining in the electrolysed solution should be
separated with sulphuretted hydrogen, the precipitated sulphide dissolved in
nitric acid, and determined colorimetrically.
VOLUMETRIC PROCESSES.
There are two of these in use, one based on the decolorising effect of
potassic cyanide upon an ammoniacal copper solution, and the other upon
the measurement of the quantity of iodine liberated from potassic iodide by
the copper salt. The cyanide process is the more generally used, and when
carefully worked, "on certain understood and orthodox conditions," yields
good results; but probably there is no method of assaying where a slight
deviation from these conditions so surely leads to error. An operator has no
difficulty in getting concordant results with duplicate assays; yet different
assayers, working, without bias, on the same material, get results uniformly
higher or lower; a difference evidently due to variations in the mode of
———
100.00
The quantity of copper got in each assay was 0.175 gram, and consequently
the bismuth averaged 0.00053 gram.
To separate the bismuth in such a case the deposit is dissolved off by
warming it in the original solution. The bismuth is precipitated by the
addition of ammonic carbonate, and the solution, after filtering and
acidifying with nitric acid, is re-electrolysed.
Determination of Copper in Commercial Copper.—Take from 1 to 1.5
gram, weigh carefully, and transfer to a beaker; add 20 c.c. of water and 10
c.c. of nitric acid; cover with a clock glass, and allow to dissolve with
moderate action; boil off nitrous fumes, dilute to 100 c.c., and electrolyse.
The cylinder must be carefully weighed, and the electrolysis allowed to
proceed for 24 hours. The weight found will be that of the copper and silver.
The silver in it must be determined[53] and deducted.
Determination of Copper in Brass, German Silver, or Bronze.—Treat in
the same manner as commercial copper. If nickel is present, the few
milligrams of copper remaining in the electrolysed solution should be
separated with sulphuretted hydrogen, the precipitated sulphide dissolved in
nitric acid, and determined colorimetrically.
VOLUMETRIC PROCESSES.
There are two of these in use, one based on the decolorising effect of
potassic cyanide upon an ammoniacal copper solution, and the other upon
the measurement of the quantity of iodine liberated from potassic iodide by
the copper salt. The cyanide process is the more generally used, and when
carefully worked, "on certain understood and orthodox conditions," yields
good results; but probably there is no method of assaying where a slight
deviation from these conditions so surely leads to error. An operator has no
difficulty in getting concordant results with duplicate assays; yet different
assayers, working, without bias, on the same material, get results uniformly
higher or lower; a difference evidently due to variations in the mode of
Page 252
working. Where a large number of results are wanted quickly it is a very
convenient method. The iodide process is very satisfactory when worked
under the proper conditions.
CYANIDE METHOD.
The process is based upon the facts—(1) that when ammonia is added in
excess to a solution containing cupric salts, ammoniacal copper compounds
are formed which give to the solution a deep blue colour; and (2) that when
potassic cyanide is added in sufficient quantity to such a solution the colour
is removed, double cyanides of copper and potassium or ammonium being
formed.[54] In the explanation generally given the formation of cuprous
cyanide is supposed[55]; but in practice it is found that one part of copper
requires rather more than four parts of cyanide, which agrees with the
former, rather than the latter, explanation.
Reliance on the accuracy of the process cannot rest upon the supposition
that the cyanide required for decoloration is proportional to the copper
present, for varying quantities of ammonia salts, ammonia and water, and
differences of temperature have an important effect. The results are
concordant and exact only when the cyanide is standardised under the same
conditions as it is used. It is best to have the assay solution and that used for
standardising as nearly as possible alike, and to titrate the two solutions side
by side. This demands an approximate knowledge of the quantity of copper
contained in the ore and a separation of the bulk of the impurities.
For the titration there is required a standard solution of potassium cyanide
made by dissolving 42 grams of the salt, known to dealers as Potassium
Cyanide (Gold), in water and diluting to one litre: 100 c.c. of this will be
about equivalent to one gram of copper. For poor ores the solution may
conveniently be made half this strength.
The solution of the ore and the separation of the copper as sulphide are
effected in the same ways as have been already described for electrolysis.
Similarly, too, the sulphide is attacked with 15 c.c. of nitric acid and the
assay boiled down to 10 c.c. Add 20 c.c. of water and warm, filter into a
pint flask, wash well with water, and dilute to about 150 c.c.; add 30 c.c. of
dilute ammonia, and cool.
convenient method. The iodide process is very satisfactory when worked
under the proper conditions.
CYANIDE METHOD.
The process is based upon the facts—(1) that when ammonia is added in
excess to a solution containing cupric salts, ammoniacal copper compounds
are formed which give to the solution a deep blue colour; and (2) that when
potassic cyanide is added in sufficient quantity to such a solution the colour
is removed, double cyanides of copper and potassium or ammonium being
formed.[54] In the explanation generally given the formation of cuprous
cyanide is supposed[55]; but in practice it is found that one part of copper
requires rather more than four parts of cyanide, which agrees with the
former, rather than the latter, explanation.
Reliance on the accuracy of the process cannot rest upon the supposition
that the cyanide required for decoloration is proportional to the copper
present, for varying quantities of ammonia salts, ammonia and water, and
differences of temperature have an important effect. The results are
concordant and exact only when the cyanide is standardised under the same
conditions as it is used. It is best to have the assay solution and that used for
standardising as nearly as possible alike, and to titrate the two solutions side
by side. This demands an approximate knowledge of the quantity of copper
contained in the ore and a separation of the bulk of the impurities.
For the titration there is required a standard solution of potassium cyanide
made by dissolving 42 grams of the salt, known to dealers as Potassium
Cyanide (Gold), in water and diluting to one litre: 100 c.c. of this will be
about equivalent to one gram of copper. For poor ores the solution may
conveniently be made half this strength.
The solution of the ore and the separation of the copper as sulphide are
effected in the same ways as have been already described for electrolysis.
Similarly, too, the sulphide is attacked with 15 c.c. of nitric acid and the
assay boiled down to 10 c.c. Add 20 c.c. of water and warm, filter into a
pint flask, wash well with water, and dilute to about 150 c.c.; add 30 c.c. of
dilute ammonia, and cool.
Page 253
Prepare a standard by dissolving a quantity of electrotype copper (judged to
be about the same as that contained in the assay) in 20 c.c. of water and 10
c.c. of nitric acid, boil off the nitrous fumes, and dilute to 150 c.c.: add 30
c.c. of dilute ammonia and cool.
Fill a burette with the standard cyanide solution. The burette with syphon
arrangement, figured on page 52, is used. A number of titrations can be
carried on at the same time provided the quantity of copper present in each
is about the same. This is regulated in weighing up the ore. The flasks must
of course be marked, and should be arranged in series on a bench in front of
a good light and at such a height that the liquid can be looked through
without stooping. Supposing about 50 c.c. of cyanide will be required, 30
c.c. should be run into each, and each addition be recorded as soon as made;
then run 15 c.c. into each. The solutions will now probably show marked
differences of tint: add 1 c.c. of cyanide to the lighter ones and more to the
darker, so as to bring the colours to about the same depth of tint. They
should all be of nearly equal tint just before finishing. At the end add half a
c.c. at a time until the colours are completely discharged. A piece of damp
filter paper held between the light and the flask assists in judging the colour
when nearly finished. Overdone assays show a straw yellow colour which
deepens on standing.
The following will illustrate the notes recorded of five such assays and one
standard:—
(1) 30 c.c. 15c.c. 5 c.c. 2 c.c. 1c.c. 1/2 c.c. — c.c. = 53-1/2 c.c.
(2) 30 " 15" 1 " 1 " 1" 1/2 " — " = 48-1/2 "
(3) 30 " 15" 3 " 1 " 1" 1/2 " — " = 50-1/2 "
(4) 30 " 15" 5 " 2 " 1" 1/2 " 1/2 " = 54 "
(5) 30 " 15" 2 " 1 " 1" 1/2 " — " = 49-1/2 "
(6) 30 " 15" 2 " 1 " 1" 1/2 " 1/2 " = 50 standard
Three grams of ore were taken, and the standard contained 0.480 gram of
copper.
In this series the difference of half a c.c. means about 0.15 per cent. on the
ore; with a little practice it is easy to estimate whether the whole or half of
the last addition should be counted.
be about the same as that contained in the assay) in 20 c.c. of water and 10
c.c. of nitric acid, boil off the nitrous fumes, and dilute to 150 c.c.: add 30
c.c. of dilute ammonia and cool.
Fill a burette with the standard cyanide solution. The burette with syphon
arrangement, figured on page 52, is used. A number of titrations can be
carried on at the same time provided the quantity of copper present in each
is about the same. This is regulated in weighing up the ore. The flasks must
of course be marked, and should be arranged in series on a bench in front of
a good light and at such a height that the liquid can be looked through
without stooping. Supposing about 50 c.c. of cyanide will be required, 30
c.c. should be run into each, and each addition be recorded as soon as made;
then run 15 c.c. into each. The solutions will now probably show marked
differences of tint: add 1 c.c. of cyanide to the lighter ones and more to the
darker, so as to bring the colours to about the same depth of tint. They
should all be of nearly equal tint just before finishing. At the end add half a
c.c. at a time until the colours are completely discharged. A piece of damp
filter paper held between the light and the flask assists in judging the colour
when nearly finished. Overdone assays show a straw yellow colour which
deepens on standing.
The following will illustrate the notes recorded of five such assays and one
standard:—
(1) 30 c.c. 15c.c. 5 c.c. 2 c.c. 1c.c. 1/2 c.c. — c.c. = 53-1/2 c.c.
(2) 30 " 15" 1 " 1 " 1" 1/2 " — " = 48-1/2 "
(3) 30 " 15" 3 " 1 " 1" 1/2 " — " = 50-1/2 "
(4) 30 " 15" 5 " 2 " 1" 1/2 " 1/2 " = 54 "
(5) 30 " 15" 2 " 1 " 1" 1/2 " — " = 49-1/2 "
(6) 30 " 15" 2 " 1 " 1" 1/2 " 1/2 " = 50 standard
Three grams of ore were taken, and the standard contained 0.480 gram of
copper.
In this series the difference of half a c.c. means about 0.15 per cent. on the
ore; with a little practice it is easy to estimate whether the whole or half of
the last addition should be counted.
Page 254
To get satisfactory results, the manner of finishing once adopted must be
adhered to.
The following experiments show the effect of variation in the conditions of
the assay:—Use a solution of copper nitrate, made by dissolving 10 grams
of copper in 50 c.c. of water and 35 c.c. of nitric acid, and diluting to a litre.
100 c.c. = 1 gram of copper.
Effect of Varying Temperature.—In these experiments 20 c.c. of copper
nitrate were used, with 10 c.c. of nitric acid, 30 c.c. of dilute ammonia, and
water to 200 c.c. The results were—
Temperature 15° 30° 70° 100°
Cyanide required 21.5 c.c. 20.8 c.c. 19.7 c.c. 18.8 c.c.
The temperature is that of the solution before titrating. These show the
importance of always cooling before titrating, and of titrating the assay and
standard at the same temperature.
Effect of Varying Bulk.—The quantities of copper, acid, and ammonia
were the same as in the last-mentioned experiments. The results were:—
Bulk 100.0 c.c. 200.0c.c. 300.0 c.c. 400.0c.c.
Cyanide required 23.3 " 21.7 " 21.4 " 21.4 "
These show that large variations in bulk must be avoided.
Effect of Varying Ammonia.—The quantities of copper and acid were the
same as in the series of experiments last noticed. The bulk was 200 c.c. The
results were:—
Dilute ammonia 20.0 c.c. 30.0 c.c. 50.0 c.c. 100.0c.c.
Cyanide required 20.9 " 21.7 " 22.3 " 24.6 "
Effect of Varying Acid.—The quantities of copper and water were the
same as in the last-noticed set of experiments: 30 c.c. of dilute ammonia
were used.
Nitric acid 5.0 c.c. 10.0c.c. 15.0 c.c.
adhered to.
The following experiments show the effect of variation in the conditions of
the assay:—Use a solution of copper nitrate, made by dissolving 10 grams
of copper in 50 c.c. of water and 35 c.c. of nitric acid, and diluting to a litre.
100 c.c. = 1 gram of copper.
Effect of Varying Temperature.—In these experiments 20 c.c. of copper
nitrate were used, with 10 c.c. of nitric acid, 30 c.c. of dilute ammonia, and
water to 200 c.c. The results were—
Temperature 15° 30° 70° 100°
Cyanide required 21.5 c.c. 20.8 c.c. 19.7 c.c. 18.8 c.c.
The temperature is that of the solution before titrating. These show the
importance of always cooling before titrating, and of titrating the assay and
standard at the same temperature.
Effect of Varying Bulk.—The quantities of copper, acid, and ammonia
were the same as in the last-mentioned experiments. The results were:—
Bulk 100.0 c.c. 200.0c.c. 300.0 c.c. 400.0c.c.
Cyanide required 23.3 " 21.7 " 21.4 " 21.4 "
These show that large variations in bulk must be avoided.
Effect of Varying Ammonia.—The quantities of copper and acid were the
same as in the series of experiments last noticed. The bulk was 200 c.c. The
results were:—
Dilute ammonia 20.0 c.c. 30.0 c.c. 50.0 c.c. 100.0c.c.
Cyanide required 20.9 " 21.7 " 22.3 " 24.6 "
Effect of Varying Acid.—The quantities of copper and water were the
same as in the last-noticed set of experiments: 30 c.c. of dilute ammonia
were used.
Nitric acid 5.0 c.c. 10.0c.c. 15.0 c.c.
Page 255
Cyanide required 21.6 " 21.7" 21.5 "
On adding nitric acid to the solution it combines with a portion of the
ammonia to form ammonic nitrate; it will be seen from the last series of
experiments that the lessening of the amount of free ammonia will decrease
the quantity of cyanide required; but, on the other hand, the ammonic
nitrate which is at the same time formed will increase the amount required;
under the conditions of the assay these two effects neutralise each other, and
such differences in the quantity of acid as are likely to occur are
unimportant.
Effect of Varying Ammonic Salts.—The quantities of copper, water, and
ammonia were the same as in the last mentioned set of experiments, but no
nitric acid was used.
Ammonic nitrate added1 gram 5 grams 10 grams 20 grams
Cyanide required 21.2 c.c. 22.1 c.c. 23.1 c.c. 24.1 c.c.
These show that combined ammonia seriously affects the titration, and that
the principle sometimes recommended of neutralising the acid with
ammonia, and then adding a constant quantity of ammonia, is not a good
one, because there is then an interference both by the ammonia and by the
variable quantity of ammonic salts.
The same quantity of combined ammonia has the same effect, whether it is
present as sulphate, nitrate, chloride, or acetate, as the following
experiments show. Four lots of 20 c.c. of "copper nitrate" were taken, and
20 c.c. of dilute ammonia added to each. These were carefully neutralised
with the respective acids, rendered alkaline with 30 c.c. more of ammonia,
cooled, diluted to bulk, and titrated. The results were:—
With sulphuric acid 22.5c.c. of cyanide
" nitric acid 22.6 " "
" hydrochloric acid 22.6 " "
" acetic acid 22.5 " "
Effect of Foreign Salts.—Sulphates, nitrates and chlorides of sodium or
potassium have no action, whilst the hydrates, carbonates, bicarbonates,
On adding nitric acid to the solution it combines with a portion of the
ammonia to form ammonic nitrate; it will be seen from the last series of
experiments that the lessening of the amount of free ammonia will decrease
the quantity of cyanide required; but, on the other hand, the ammonic
nitrate which is at the same time formed will increase the amount required;
under the conditions of the assay these two effects neutralise each other, and
such differences in the quantity of acid as are likely to occur are
unimportant.
Effect of Varying Ammonic Salts.—The quantities of copper, water, and
ammonia were the same as in the last mentioned set of experiments, but no
nitric acid was used.
Ammonic nitrate added1 gram 5 grams 10 grams 20 grams
Cyanide required 21.2 c.c. 22.1 c.c. 23.1 c.c. 24.1 c.c.
These show that combined ammonia seriously affects the titration, and that
the principle sometimes recommended of neutralising the acid with
ammonia, and then adding a constant quantity of ammonia, is not a good
one, because there is then an interference both by the ammonia and by the
variable quantity of ammonic salts.
The same quantity of combined ammonia has the same effect, whether it is
present as sulphate, nitrate, chloride, or acetate, as the following
experiments show. Four lots of 20 c.c. of "copper nitrate" were taken, and
20 c.c. of dilute ammonia added to each. These were carefully neutralised
with the respective acids, rendered alkaline with 30 c.c. more of ammonia,
cooled, diluted to bulk, and titrated. The results were:—
With sulphuric acid 22.5c.c. of cyanide
" nitric acid 22.6 " "
" hydrochloric acid 22.6 " "
" acetic acid 22.5 " "
Effect of Foreign Salts.—Sulphates, nitrates and chlorides of sodium or
potassium have no action, whilst the hydrates, carbonates, bicarbonates,
Page 256
sulphites, and nitrites have an important effect. The interference of
ammonic salts has already been shown.
Salts of silver, zinc, and nickel react with cyanide just as copper does, and
consequently interfere. Ferrous salts are sure to be absent, and ferric salts
yield ferric hydrate with the ammonia, which is not acted on by the cyanide,
but, owing to its bulkiness, it settles slowly; this lengthens the time required
for titration, and so modifies the manner of working. An assay should not be
worked with ferric hydrate present, unless the standard contains about the
same amount of it. On mines it is often inconvenient to separate the copper
by means of sulphuretted hydrogen; hence it is customary to titrate without
previous separation. In this case, instead of standardising the cyanide with
electrotype copper, a standard ore should be used. This should be an ore (of
the same kind as those being assayed) in which the copper has been
carefully determined.
Effect of Varying Copper.—In these experiments 10 c.c. of nitric acid, 30
c.c. of ammonia, and water to 200 c.c. were used.
Copper nitrate present 1.0c.c. 10.0 c.c. 20.0c.c. 50.0c.c. 100.0c.c.
Cyanide required 0.7" 11.2 " 21.7" 54.5" 108.1"
These results show that under the conditions laid down the various causes
of disturbance nearly neutralise one another, and the results within a fair
range are practically proportional.
Determination of Copper in Copper Pyrites.—Weigh up 2 grams of the
dried and powdered ore, and place in an evaporating dish about four inches
in diameter. Cover with 20 c.c. of nitric acid and put on a hot plate.
Evaporate to dryness without further handling. Allow to cool and take up
with 30 c.c. of hydrochloric acid, boil, dilute, and transfer to a pint flask,
filtering if necessary. Make up the bulk with the washings to about 150 c.c.
Precipitate with sulphuretted hydrogen, filter, and wash back the precipitate
into the flask. Add 15 c.c. of nitric acid, and boil down rapidly to 10 c.c.
Dilute, add 30 c.c. of dilute ammonia, make up to 150 c.c., and cool. For the
standard, weigh up 0.5 gram of copper, more or less, according to the
quantity judged to be present in the assay. Dissolve in 20 c.c. of dilute nitric
acid, boil off nitrous fumes, add 30 c.c. of dilute ammonia, make up to the
ammonic salts has already been shown.
Salts of silver, zinc, and nickel react with cyanide just as copper does, and
consequently interfere. Ferrous salts are sure to be absent, and ferric salts
yield ferric hydrate with the ammonia, which is not acted on by the cyanide,
but, owing to its bulkiness, it settles slowly; this lengthens the time required
for titration, and so modifies the manner of working. An assay should not be
worked with ferric hydrate present, unless the standard contains about the
same amount of it. On mines it is often inconvenient to separate the copper
by means of sulphuretted hydrogen; hence it is customary to titrate without
previous separation. In this case, instead of standardising the cyanide with
electrotype copper, a standard ore should be used. This should be an ore (of
the same kind as those being assayed) in which the copper has been
carefully determined.
Effect of Varying Copper.—In these experiments 10 c.c. of nitric acid, 30
c.c. of ammonia, and water to 200 c.c. were used.
Copper nitrate present 1.0c.c. 10.0 c.c. 20.0c.c. 50.0c.c. 100.0c.c.
Cyanide required 0.7" 11.2 " 21.7" 54.5" 108.1"
These results show that under the conditions laid down the various causes
of disturbance nearly neutralise one another, and the results within a fair
range are practically proportional.
Determination of Copper in Copper Pyrites.—Weigh up 2 grams of the
dried and powdered ore, and place in an evaporating dish about four inches
in diameter. Cover with 20 c.c. of nitric acid and put on a hot plate.
Evaporate to dryness without further handling. Allow to cool and take up
with 30 c.c. of hydrochloric acid, boil, dilute, and transfer to a pint flask,
filtering if necessary. Make up the bulk with the washings to about 150 c.c.
Precipitate with sulphuretted hydrogen, filter, and wash back the precipitate
into the flask. Add 15 c.c. of nitric acid, and boil down rapidly to 10 c.c.
Dilute, add 30 c.c. of dilute ammonia, make up to 150 c.c., and cool. For the
standard, weigh up 0.5 gram of copper, more or less, according to the
quantity judged to be present in the assay. Dissolve in 20 c.c. of dilute nitric
acid, boil off nitrous fumes, add 30 c.c. of dilute ammonia, make up to the
Page 257
same bulk as that of the assay, and cool. Titrate the two solutions side by
side and as nearly as possible in the same manner.
Since the assay solution is often turbid from the presence of small quantities
of lead and of iron from incomplete washing, and since this slight
precipitate is very slow in settling, the standard can hardly be compared
strictly with the assay. This can be counteracted by precipitating in both
solutions a mixture of ferric and aluminic hydrates, which settles readily
and leaves the supernatant liquor clear. To effect this, boil the nitric acid
solutions with 30 c.c. of a solution containing 15 grams each of alum and
ferrous sulphate to the litre. In an actual determination 2 grams of the ore
were taken and compared with 0.5 gram of copper. The assay required 57.7
c.c. of cyanide and the standard 52.5 c.c.
52.5 : 0.5 :: 57.7 : 0.5495
This on 2 grams of ore = 27.47 per cent.; the same sample by electrolysis
gave 27.60 per cent. of copper.
Determination without Previous Separation.—Dissolve up 2 grams as
before, but, instead of passing sulphuretted hydrogen, add 30 c.c. of dilute
ammonia, shake well, and cool. Prepare a standard by dissolving 0.5 gram
of copper in 1 c.c. of nitric acid, add 0.6 gram of iron in the form of ferric
chloride and 20 c.c. of hydrochloric acid, dilute to about 150 c.c., add 30
c.c. of dilute ammonia, and cool. Titrate the two solutions side by side. In a
determination on the sample last used, 58 c.c. were required for the assay
and 53 c.c. for the standard, which indicates 27.3 per cent. of copper.
This method of working is somewhat rough.
IODIDE METHOD.
This is based upon the fact that when potassic iodide in excess is added to a
strong solution of a cupric salt in a faintly acid solution, cuprous iodide is
formed and an equivalent of iodine liberated.[56] The iodine is measured by
titrating with a solution of sodium hyposulphite,[57] using starch paste as
indicator. The iodine is soluble in the excess of potassium iodide, forming a
deep brown solution; the hyposulphite is added until this brown colour is
side and as nearly as possible in the same manner.
Since the assay solution is often turbid from the presence of small quantities
of lead and of iron from incomplete washing, and since this slight
precipitate is very slow in settling, the standard can hardly be compared
strictly with the assay. This can be counteracted by precipitating in both
solutions a mixture of ferric and aluminic hydrates, which settles readily
and leaves the supernatant liquor clear. To effect this, boil the nitric acid
solutions with 30 c.c. of a solution containing 15 grams each of alum and
ferrous sulphate to the litre. In an actual determination 2 grams of the ore
were taken and compared with 0.5 gram of copper. The assay required 57.7
c.c. of cyanide and the standard 52.5 c.c.
52.5 : 0.5 :: 57.7 : 0.5495
This on 2 grams of ore = 27.47 per cent.; the same sample by electrolysis
gave 27.60 per cent. of copper.
Determination without Previous Separation.—Dissolve up 2 grams as
before, but, instead of passing sulphuretted hydrogen, add 30 c.c. of dilute
ammonia, shake well, and cool. Prepare a standard by dissolving 0.5 gram
of copper in 1 c.c. of nitric acid, add 0.6 gram of iron in the form of ferric
chloride and 20 c.c. of hydrochloric acid, dilute to about 150 c.c., add 30
c.c. of dilute ammonia, and cool. Titrate the two solutions side by side. In a
determination on the sample last used, 58 c.c. were required for the assay
and 53 c.c. for the standard, which indicates 27.3 per cent. of copper.
This method of working is somewhat rough.
IODIDE METHOD.
This is based upon the fact that when potassic iodide in excess is added to a
strong solution of a cupric salt in a faintly acid solution, cuprous iodide is
formed and an equivalent of iodine liberated.[56] The iodine is measured by
titrating with a solution of sodium hyposulphite,[57] using starch paste as
indicator. The iodine is soluble in the excess of potassium iodide, forming a
deep brown solution; the hyposulphite is added until this brown colour is
Page 258
almost removed. Starch paste is then added, and strikes with the remaining
iodine a dirty blue colour. The addition of the "hypo" is continued until the
blue colour is discharged. The end reaction is sharp; a drop is sufficient to
complete it.
As regards the titration, the process leaves little to be desired; the quantity
of "hypo" required is strictly proportional to the copper present, and
ordinary variations in the conditions of working are without effect. The
presence of salts of bismuth masks the end reaction because of the strong
colour imparted to the solution by the iodide of bismuth. Under certain
conditions there is a return of the blue colour in the assay solution after the
finishing point has apparently been reached, which is a heavy tax on the
patience and confidence of the operator. This is specially apt to occur when
sodium acetate is present, although it may also be due to excessive dilution.
The standard "hypo" solution is made by dissolving 39.18 grams of the
crystallised salt (Na2S2O3.5H2O) in water and diluting to one litre. One
hundred c.c. will equal one gram of copper.
The starch solution is made by mixing 1 gram of starch into a thin paste
with cold water, pouring it into 200 c.c. of boiling water, and continuing the
boiling for a minute or so. The solution must be cold before use, and about
2 c.c. is used for each assay. It should not be added until the bulk of the
iodine has been reduced.
To standardise the "hypo," weigh up 0.3 or 0.4 gram of pure copper,
dissolve in 5 c.c. of dilute nitric acid, boil off nitrous fumes, and dilute with
an equal bulk of cold water. Add "soda" solution until a permanent
precipitate is obtained, and then 1 c.c. of acetic acid. This should yield a
clear solution. Fill an ordinary burette with the "hypo." Add 3 grams of
potassium iodide crystals to the copper solution, and, when these are
dissolved, dilute to 100 c.c. with water. Run in the "hypo" solution rather
quickly until the brown colour is nearly discharged—i.e., to within 3 or 4
c.c. of the finish. Add 2 c.c. of the starch solution, and continue the addition
of the "hypo" a few drops at a time until the tint suddenly changes to a
cream colour. The blue colour must not return on standing three or four
minutes. Calculate the standard in the usual way.
iodine a dirty blue colour. The addition of the "hypo" is continued until the
blue colour is discharged. The end reaction is sharp; a drop is sufficient to
complete it.
As regards the titration, the process leaves little to be desired; the quantity
of "hypo" required is strictly proportional to the copper present, and
ordinary variations in the conditions of working are without effect. The
presence of salts of bismuth masks the end reaction because of the strong
colour imparted to the solution by the iodide of bismuth. Under certain
conditions there is a return of the blue colour in the assay solution after the
finishing point has apparently been reached, which is a heavy tax on the
patience and confidence of the operator. This is specially apt to occur when
sodium acetate is present, although it may also be due to excessive dilution.
The standard "hypo" solution is made by dissolving 39.18 grams of the
crystallised salt (Na2S2O3.5H2O) in water and diluting to one litre. One
hundred c.c. will equal one gram of copper.
The starch solution is made by mixing 1 gram of starch into a thin paste
with cold water, pouring it into 200 c.c. of boiling water, and continuing the
boiling for a minute or so. The solution must be cold before use, and about
2 c.c. is used for each assay. It should not be added until the bulk of the
iodine has been reduced.
To standardise the "hypo," weigh up 0.3 or 0.4 gram of pure copper,
dissolve in 5 c.c. of dilute nitric acid, boil off nitrous fumes, and dilute with
an equal bulk of cold water. Add "soda" solution until a permanent
precipitate is obtained, and then 1 c.c. of acetic acid. This should yield a
clear solution. Fill an ordinary burette with the "hypo." Add 3 grams of
potassium iodide crystals to the copper solution, and, when these are
dissolved, dilute to 100 c.c. with water. Run in the "hypo" solution rather
quickly until the brown colour is nearly discharged—i.e., to within 3 or 4
c.c. of the finish. Add 2 c.c. of the starch solution, and continue the addition
of the "hypo" a few drops at a time until the tint suddenly changes to a
cream colour. The blue colour must not return on standing three or four
minutes. Calculate the standard in the usual way.
Page 259
In assaying ores, the copper is dissolved and separated with sulphuretted
hydrogen as in the other processes, but the sulphide should be washed more
completely to ensure the absence of iron salts.
The following experiments show the effect of variation in the conditions of
the assay. Use a solution of copper sulphate containing 39.38 grams of
copper sulphate crystals (CuSO4.5H2O) in the litre. 100 c.c. equal 1.00
gram of copper.
Effect of Varying Temperature.—The assay after the addition of the
potassic iodide must be kept cold, else iodine may be volatilised.
Effect of Varying Potassium Iodide.—In various descriptions of the
process the amount of iodide required is variously stated at from "a few
crystals" to as much as 10 grams. The proportion required by theory for 1
gram of copper is a little over 5 grams: an excess, however, is required to
keep the liberated iodine in solution. On economic grounds this excess
should not be extravagant; if the student uses 10 parts of the iodide for each
part of copper in the assay he will have sufficient. In the experiments there
were used 20 c.c. of the copper sulphate, with varying amounts of potassic
iodide, and the following results were got:—
Potassic iodide added 1.5 gram3 grams 5 grams
"Hypo" required 20.0 c.c. 20.0 c.c. 20.0 c.c.
In these the iodide was added direct to the solution containing the copper,
which was afterwards diluted to 100 c.c. and titrated. In another series the
iodide was added after the dilution to 100 c.c., and the results were:—
Potassic iodide added 1.5 gram3 grams 5 grams 10 grams
"Hypo" required 20.0 c.c. 20.1 c.c. 20.0 c.c. 20.0 c.c.
Effect of Varying Bulk.—In these experiments, 20 c.c. of copper sulphate
were taken, 3 grams of potassic iodide added, and also water to the required
bulk.
Bulk 20.0 c.c. 100.0c.c. 200.0c.c. 500.0 c.c.
"Hypo" required 20.0 " 20.0 " 20.0 " 19.9 "
hydrogen as in the other processes, but the sulphide should be washed more
completely to ensure the absence of iron salts.
The following experiments show the effect of variation in the conditions of
the assay. Use a solution of copper sulphate containing 39.38 grams of
copper sulphate crystals (CuSO4.5H2O) in the litre. 100 c.c. equal 1.00
gram of copper.
Effect of Varying Temperature.—The assay after the addition of the
potassic iodide must be kept cold, else iodine may be volatilised.
Effect of Varying Potassium Iodide.—In various descriptions of the
process the amount of iodide required is variously stated at from "a few
crystals" to as much as 10 grams. The proportion required by theory for 1
gram of copper is a little over 5 grams: an excess, however, is required to
keep the liberated iodine in solution. On economic grounds this excess
should not be extravagant; if the student uses 10 parts of the iodide for each
part of copper in the assay he will have sufficient. In the experiments there
were used 20 c.c. of the copper sulphate, with varying amounts of potassic
iodide, and the following results were got:—
Potassic iodide added 1.5 gram3 grams 5 grams
"Hypo" required 20.0 c.c. 20.0 c.c. 20.0 c.c.
In these the iodide was added direct to the solution containing the copper,
which was afterwards diluted to 100 c.c. and titrated. In another series the
iodide was added after the dilution to 100 c.c., and the results were:—
Potassic iodide added 1.5 gram3 grams 5 grams 10 grams
"Hypo" required 20.0 c.c. 20.1 c.c. 20.0 c.c. 20.0 c.c.
Effect of Varying Bulk.—In these experiments, 20 c.c. of copper sulphate
were taken, 3 grams of potassic iodide added, and also water to the required
bulk.
Bulk 20.0 c.c. 100.0c.c. 200.0c.c. 500.0 c.c.
"Hypo" required 20.0 " 20.0 " 20.0 " 19.9 "
Page 260
In the last of these experiments the colour was discharged at 18 c.c., but
gradually returned until 19.9 c.c. had been run in. It will be seen that
considerable variation in bulk does not interfere.
Effect of Acetic Acid.—These experiments were like the last series
mentioned, but the bulk was 100 c.c., and varying amounts of acetic acid
were added.
Acetic acid added 0c.c. 1.0c.c. 5.0 c.c. 10.0c.c. 20.0 c.c.
"Hypo" required 20.0" 20.1" 20.1 " 20.0" 20.2 "
Acetic acid, then, does not interfere to any serious extent.
Effect of Varying Sodium Acetate.—These experiments were like those
last mentioned, but without acetic acid, and with varying amounts of
sodium acetate.
Sodium acetate added 0 gram 1 gram 2 grams 5 grams 10 grams
"Hypo" required 20.0 c.c. 20.0 c.c. 20.2 c.c. 19.3 c.c. 18.2 c.c.
In the 5 grams experiment, when the finishing point had been apparently
reached the colour slowly returned; but as the results generally on titrating
were not satisfactory a repetition of the experiment was made with the
addition of 5 c.c. of acetic acid, which gave an equally bad result.
Effect of Foreign Salts.—The conditions of these experiments were the
same as before. The salts were added and dissolved before the addition of
the potassium iodide. Using 5 grams (or in the case of the acids, 5 c.c.), the
results were as follows:—
Salt added — dilute H2SO4 Acetic acid NaAc NaCl
"Hypo" required 20.0 c.c. 20.0 c.c. 20.1 c.c. 19.3 c.c. 20.1 c.c.
Salt added KNO3 Na2SO4 AmCl Am2SO4
"Hypo" required 20.2 c.c. 18.7 c.c. 20.0 c.c. 19.9 c.c.
The low result with the sulphate of soda was evidently due to the formation
of a sparingly soluble double salt, which removed copper from the solution;
gradually returned until 19.9 c.c. had been run in. It will be seen that
considerable variation in bulk does not interfere.
Effect of Acetic Acid.—These experiments were like the last series
mentioned, but the bulk was 100 c.c., and varying amounts of acetic acid
were added.
Acetic acid added 0c.c. 1.0c.c. 5.0 c.c. 10.0c.c. 20.0 c.c.
"Hypo" required 20.0" 20.1" 20.1 " 20.0" 20.2 "
Acetic acid, then, does not interfere to any serious extent.
Effect of Varying Sodium Acetate.—These experiments were like those
last mentioned, but without acetic acid, and with varying amounts of
sodium acetate.
Sodium acetate added 0 gram 1 gram 2 grams 5 grams 10 grams
"Hypo" required 20.0 c.c. 20.0 c.c. 20.2 c.c. 19.3 c.c. 18.2 c.c.
In the 5 grams experiment, when the finishing point had been apparently
reached the colour slowly returned; but as the results generally on titrating
were not satisfactory a repetition of the experiment was made with the
addition of 5 c.c. of acetic acid, which gave an equally bad result.
Effect of Foreign Salts.—The conditions of these experiments were the
same as before. The salts were added and dissolved before the addition of
the potassium iodide. Using 5 grams (or in the case of the acids, 5 c.c.), the
results were as follows:—
Salt added — dilute H2SO4 Acetic acid NaAc NaCl
"Hypo" required 20.0 c.c. 20.0 c.c. 20.1 c.c. 19.3 c.c. 20.1 c.c.
Salt added KNO3 Na2SO4 AmCl Am2SO4
"Hypo" required 20.2 c.c. 18.7 c.c. 20.0 c.c. 19.9 c.c.
The low result with the sulphate of soda was evidently due to the formation
of a sparingly soluble double salt, which removed copper from the solution;
Page 261
on adding a little acetic acid the full amount of "hypo" was required. The
effect of the presence of certain metals is important. The method of
determining it was to add the substance to the solution containing the
copper, and partly precipitate with soda solution; then treating with 1 c.c. of
acetic acid, adding the iodide, and proceeding as before.
Substance Added. "Hypo" Required,
- 20. c.c
0.050 gram arsenic as As2O5 20.0 "
0.050 " antimony as SbCl5 19.8 "
0.050 " lead as Pb(NO3)2 20.1 "
A similar experiment with 0.050 gram of bismuth nitrate could not be
determined, the end-reaction being masked. Bismuth iodide is soluble in
potassic iodide, forming a brown solution, the colour of which is very
similar to that produced by iodine; and although it does not strike a blue
colour with starch, "hypo" has an action on it.
A similar experiment with 0.050 gram of iron as ferric chloride required
22.3 c.c. of "hypo," and the colour returned on standing. This shows that
ferric acetate liberates iodine under the conditions of the assay. Trying to
counteract this, by adding to a similar solution 0.5 gram of phosphate of
soda dissolved in a little water, 19.7 c.c. of "hypo" were required instead of
20.0, but the assay showed signs of returning colour.
In standardising, the same result was obtained, whether the copper was
present as nitrate or sulphate before neutralising.
Effect of Varying Copper.—With the same conditions as before, but with
varying amounts of copper and a proportionally increasing quantity of
iodide, the results were:—
Copper present 1.0c.c. 10.0c.c. 20.0c.c. 50.0c.c. 100.0c.c.
"Hypo" required 1.0" 10.0" 20.0" 50.0" 100.0"
showing the results to be exactly proportional.[58]
effect of the presence of certain metals is important. The method of
determining it was to add the substance to the solution containing the
copper, and partly precipitate with soda solution; then treating with 1 c.c. of
acetic acid, adding the iodide, and proceeding as before.
Substance Added. "Hypo" Required,
- 20. c.c
0.050 gram arsenic as As2O5 20.0 "
0.050 " antimony as SbCl5 19.8 "
0.050 " lead as Pb(NO3)2 20.1 "
A similar experiment with 0.050 gram of bismuth nitrate could not be
determined, the end-reaction being masked. Bismuth iodide is soluble in
potassic iodide, forming a brown solution, the colour of which is very
similar to that produced by iodine; and although it does not strike a blue
colour with starch, "hypo" has an action on it.
A similar experiment with 0.050 gram of iron as ferric chloride required
22.3 c.c. of "hypo," and the colour returned on standing. This shows that
ferric acetate liberates iodine under the conditions of the assay. Trying to
counteract this, by adding to a similar solution 0.5 gram of phosphate of
soda dissolved in a little water, 19.7 c.c. of "hypo" were required instead of
20.0, but the assay showed signs of returning colour.
In standardising, the same result was obtained, whether the copper was
present as nitrate or sulphate before neutralising.
Effect of Varying Copper.—With the same conditions as before, but with
varying amounts of copper and a proportionally increasing quantity of
iodide, the results were:—
Copper present 1.0c.c. 10.0c.c. 20.0c.c. 50.0c.c. 100.0c.c.
"Hypo" required 1.0" 10.0" 20.0" 50.0" 100.0"
showing the results to be exactly proportional.[58]
Page 262
Determination of Copper in Copper Pyrites.—Take 2 grams of the dried
and powdered ore and treat in a porcelain dish with 20 c.c. of nitric acid,
and evaporate to dryness. Take up with 30 c.c. of hydrochloric acid, dilute,
and transfer to a pint flask; make up with water to 200 c.c., warm, and pass
sulphuretted hydrogen to excess. Filter, and wash the precipitate with water
acidified with sulphuric acid. Wash the precipitate back into the flask, and
dissolve with 15 c.c. of nitric acid. Evaporate almost to dryness; add 20 c.c.
of water, and boil till free from nitrous fumes; filter off the sulphur and
gangue; neutralise with soda, avoiding excess; add 1 or 2 c.c. of acetic acid,
and shake till clear. Add 5 grams of potassium iodide, dilute to 100 c.c., and
titrate. The following is an example:—
0.5 gram of copper required 50.5c.c. "hypo."
The assay required 55.6" "
which is equal to 27.5 per cent. of copper.
COLORIMETRIC PROCESS.
This is based on the blue coloration of ammoniacal copper solutions. The
quantity of copper in 100 c.c. of the assay solution should not be more than
15 milligrams, or less than half a milligram. It is not so delicate as most
other colorimetric methods, but nevertheless is a very useful one.
The manner of working is the same as that described under iron.
Standard Copper Solution.—Weigh up 0.5 gram of electrotype copper,
dissolve in 10 c.c. of nitric acid, boil off nitrous fumes, and dilute to 1 litre.
1 c.c. = 0.5 milligram.
In nearly all cases it will be necessary to separate the copper with
sulphuretted hydrogen from a solution of about 5 grams of the material to
be assayed. The filter paper containing the sulphide (and, probably, much
sulphur) is dried and burnt. The ashes are dissolved in 5 c.c. of dilute nitric
acid, 10 c.c. of dilute ammonia added, and the solution filtered through a
coarse filter into a Nessler tube, washing the paper with a little dilute
ammonia.
and powdered ore and treat in a porcelain dish with 20 c.c. of nitric acid,
and evaporate to dryness. Take up with 30 c.c. of hydrochloric acid, dilute,
and transfer to a pint flask; make up with water to 200 c.c., warm, and pass
sulphuretted hydrogen to excess. Filter, and wash the precipitate with water
acidified with sulphuric acid. Wash the precipitate back into the flask, and
dissolve with 15 c.c. of nitric acid. Evaporate almost to dryness; add 20 c.c.
of water, and boil till free from nitrous fumes; filter off the sulphur and
gangue; neutralise with soda, avoiding excess; add 1 or 2 c.c. of acetic acid,
and shake till clear. Add 5 grams of potassium iodide, dilute to 100 c.c., and
titrate. The following is an example:—
0.5 gram of copper required 50.5c.c. "hypo."
The assay required 55.6" "
which is equal to 27.5 per cent. of copper.
COLORIMETRIC PROCESS.
This is based on the blue coloration of ammoniacal copper solutions. The
quantity of copper in 100 c.c. of the assay solution should not be more than
15 milligrams, or less than half a milligram. It is not so delicate as most
other colorimetric methods, but nevertheless is a very useful one.
The manner of working is the same as that described under iron.
Standard Copper Solution.—Weigh up 0.5 gram of electrotype copper,
dissolve in 10 c.c. of nitric acid, boil off nitrous fumes, and dilute to 1 litre.
1 c.c. = 0.5 milligram.
In nearly all cases it will be necessary to separate the copper with
sulphuretted hydrogen from a solution of about 5 grams of the material to
be assayed. The filter paper containing the sulphide (and, probably, much
sulphur) is dried and burnt. The ashes are dissolved in 5 c.c. of dilute nitric
acid, 10 c.c. of dilute ammonia added, and the solution filtered through a
coarse filter into a Nessler tube, washing the paper with a little dilute
ammonia.
Page 263
The estimation of the colour and calculation of the result are made in the
way described on page 44.
The effect of varying conditions on the assay may be seen from the
following experiments.
Effect of Varying Temperature.—The effect of increased temperature is to
slightly decrease the colour, but this can only be observed when a fair
quantity of copper is present.
1.0 c.c. at 15° showed the colour of 1.0c.c. at 70°
2.5 " " " 2.7 "
5.0 " " " 5.0 "
10.0 " " " 9.0 "
Effect of Varying Ammonia.—The solution must, of course, contain free
ammonia; about 5 c.c. of dilute ammonia in 50 c.c. bulk is the quantity to be
used in the experiments. A larger quantity affects the results, giving lower
readings and altering the tint. With small quantities of ammonia the colour
approaches a violet; with larger, a sky-blue.
2.5 c.c. with 25c.c. of strong ammonia read 2.2c.c.
5.0 " " " " " 4.0 "
10.0 " " " " " 8.0 "
Effect of Ammonic Salts.—The following table shows the results after
addition of ammonic salts:—
C.c. With 10 grams With 10 grams With 10 grams
Present. Ammonic Nitrate. Ammonic Chloride. Ammonic Sulphate.
2.5 2.5 2.5 2.0
5.0 5.0 5.3 4.3
10.0 10.0 10.0 8.5
These show that sulphates should be avoided, and either nitrate or chloride
solutions be used in the standard as well as in the assay.
way described on page 44.
The effect of varying conditions on the assay may be seen from the
following experiments.
Effect of Varying Temperature.—The effect of increased temperature is to
slightly decrease the colour, but this can only be observed when a fair
quantity of copper is present.
1.0 c.c. at 15° showed the colour of 1.0c.c. at 70°
2.5 " " " 2.7 "
5.0 " " " 5.0 "
10.0 " " " 9.0 "
Effect of Varying Ammonia.—The solution must, of course, contain free
ammonia; about 5 c.c. of dilute ammonia in 50 c.c. bulk is the quantity to be
used in the experiments. A larger quantity affects the results, giving lower
readings and altering the tint. With small quantities of ammonia the colour
approaches a violet; with larger, a sky-blue.
2.5 c.c. with 25c.c. of strong ammonia read 2.2c.c.
5.0 " " " " " 4.0 "
10.0 " " " " " 8.0 "
Effect of Ammonic Salts.—The following table shows the results after
addition of ammonic salts:—
C.c. With 10 grams With 10 grams With 10 grams
Present. Ammonic Nitrate. Ammonic Chloride. Ammonic Sulphate.
2.5 2.5 2.5 2.0
5.0 5.0 5.3 4.3
10.0 10.0 10.0 8.5
These show that sulphates should be avoided, and either nitrate or chloride
solutions be used in the standard as well as in the assay.
Page 264
Determination of Copper in a Manganese Ore.—Treat 3 grams of the ore
with 20 c.c. of hydrochloric acid, and evaporate to dryness. Take up with 10
c.c. of hydrochloric acid; dilute to about 200 c.c., and pass sulphuretted
hydrogen until the solution smells of the gas; filter, burn, take up with 5 c.c.
of dilute nitric acid, add 10 c.c. of dilute ammonia, and filter into the
Nessler tube, and make up with the washings to 50 c.c. Into the "standard"
tube put 5 c.c. of dilute nitric acid and 10 c.c. of dilute ammonia. Make up
to nearly 50 c.c. with water, and run in the standard copper until the colours
are equal. In a determination 4 c.c. (= 2.0 milligrams of copper) were
required; this in 3 grams of ore = 0.07 per cent.
Determination of Copper in "Black Tin."—Weigh up 3 grams of the
dried ore, boil with 10 c.c. of hydrochloric acid, and afterwards add 1 c.c. of
nitric; boil off nitrous fumes, evaporate to about 5 c.c., dilute to 50 c.c., add
20 c.c. of dilute ammonia; stir, and filter. If much iron is present, dissolve
the precipitate of ferric hydrate in acid, and reprecipitate with ammonia.
Mix the two filtrates, and dilute to 100 c.c. Take 50 c.c. for the test. A
sample of 3 grams of an ore treated in this way required 5.2 c.c. of standard
copper to produce equality of tint. This gives 0.35 per cent.
Determination of Copper in Tin.—Weigh up 1 gram of the sample,
transfer to an evaporating dish, and cover with 30 c.c. of aqua regia. Warm
until the metal has dissolved, then evaporate almost to dryness. Take up
with a few c.c. of hydrochloric acid and again evaporate.
Dissolve the residue in 10 c.c. of dilute hydrochloric acid and transfer to a
100 c.c. flask. Add 10 c.c. of dilute ammonia and make up with water to the
containing mark.
Filter off 50 c.c. of the solution into a Nessler glass and determine the
copper in it colorimetrically.
EXAMINATION OF COMMERCIAL COPPER.
Very pure copper can be obtained in commerce, owing to the demand for
metal of "high conductivity" for electrical purposes, which practically
means for metal free from impurities.
with 20 c.c. of hydrochloric acid, and evaporate to dryness. Take up with 10
c.c. of hydrochloric acid; dilute to about 200 c.c., and pass sulphuretted
hydrogen until the solution smells of the gas; filter, burn, take up with 5 c.c.
of dilute nitric acid, add 10 c.c. of dilute ammonia, and filter into the
Nessler tube, and make up with the washings to 50 c.c. Into the "standard"
tube put 5 c.c. of dilute nitric acid and 10 c.c. of dilute ammonia. Make up
to nearly 50 c.c. with water, and run in the standard copper until the colours
are equal. In a determination 4 c.c. (= 2.0 milligrams of copper) were
required; this in 3 grams of ore = 0.07 per cent.
Determination of Copper in "Black Tin."—Weigh up 3 grams of the
dried ore, boil with 10 c.c. of hydrochloric acid, and afterwards add 1 c.c. of
nitric; boil off nitrous fumes, evaporate to about 5 c.c., dilute to 50 c.c., add
20 c.c. of dilute ammonia; stir, and filter. If much iron is present, dissolve
the precipitate of ferric hydrate in acid, and reprecipitate with ammonia.
Mix the two filtrates, and dilute to 100 c.c. Take 50 c.c. for the test. A
sample of 3 grams of an ore treated in this way required 5.2 c.c. of standard
copper to produce equality of tint. This gives 0.35 per cent.
Determination of Copper in Tin.—Weigh up 1 gram of the sample,
transfer to an evaporating dish, and cover with 30 c.c. of aqua regia. Warm
until the metal has dissolved, then evaporate almost to dryness. Take up
with a few c.c. of hydrochloric acid and again evaporate.
Dissolve the residue in 10 c.c. of dilute hydrochloric acid and transfer to a
100 c.c. flask. Add 10 c.c. of dilute ammonia and make up with water to the
containing mark.
Filter off 50 c.c. of the solution into a Nessler glass and determine the
copper in it colorimetrically.
EXAMINATION OF COMMERCIAL COPPER.
Very pure copper can be obtained in commerce, owing to the demand for
metal of "high conductivity" for electrical purposes, which practically
means for metal free from impurities.
Page 265
Much of the metal sold contains as much as one per cent. of foreign
substances, of which arsenic is the most important. The other elements to be
looked for are bismuth, lead, antimony, silver, gold, iron, nickel, cobalt,
sulphur, and oxygen. In "blister copper" (which is the unrefined metal),
aluminium, silicon, and phosphorus may be met with.
Oxygen.—All commercial copper carries oxygen; most of it is present as
cuprous oxide, which is dissolved by molten copper. The estimation of
oxygen is often made "by difference." The copper and the other impurities
being determined, the rest is assumed to be oxygen. Probably this is nearly
correct, but the whole of the oxygen should not be ascribed to cuprous
oxide; for any arsenic the metal contained would be present as cuprous
arsenite, since arsenide of copper and cuprous oxide could not exist
together at the temperature of fusion without interacting. In the report of the
analysis, it is best to state the proportion of oxygen thus:—
Oxygen ——— per cent. by difference.
There is a method of determination by fusing 5 or 10 grams in a brasqued
crucible, and counting the loss as oxygen; and another method for the
determination of cuprous oxide based on the reaction of this substance with
nitrate of silver.[59] About 2 grams of silver nitrate, dissolved in 100 c.c. of
water, is allowed to act upon 1 gram of the copper in the cold. The
precipitate is filtered off, washed thoroughly with water, and the basic salt
dissolved and determined colorimetrically.
One part of copper found represents 1.68 part of cuprous oxide, or 0.19 part
of oxygen. Copper generally carries from 0.1 to 0.2 per cent. of oxygen.
Silver is found in most samples, but occurs in variable proportions; when it
amounts to 30 ounces per ton it has a commercial value. To determine its
amount, dissolve 10 grams of the copper in 35 c.c. of nitric acid and 50 c.c.
of water, boil off nitrous fumes, and dilute to about 100 c.c. One or two c.c.
of dilute hydrochloric acid (one to 100 of water) are added, stirred in, and
the precipitate allowed to settle for twenty-four hours. Filter through a
double Swedish paper, dry, burn, and cupel the ashes with one gram of
sheet lead.
substances, of which arsenic is the most important. The other elements to be
looked for are bismuth, lead, antimony, silver, gold, iron, nickel, cobalt,
sulphur, and oxygen. In "blister copper" (which is the unrefined metal),
aluminium, silicon, and phosphorus may be met with.
Oxygen.—All commercial copper carries oxygen; most of it is present as
cuprous oxide, which is dissolved by molten copper. The estimation of
oxygen is often made "by difference." The copper and the other impurities
being determined, the rest is assumed to be oxygen. Probably this is nearly
correct, but the whole of the oxygen should not be ascribed to cuprous
oxide; for any arsenic the metal contained would be present as cuprous
arsenite, since arsenide of copper and cuprous oxide could not exist
together at the temperature of fusion without interacting. In the report of the
analysis, it is best to state the proportion of oxygen thus:—
Oxygen ——— per cent. by difference.
There is a method of determination by fusing 5 or 10 grams in a brasqued
crucible, and counting the loss as oxygen; and another method for the
determination of cuprous oxide based on the reaction of this substance with
nitrate of silver.[59] About 2 grams of silver nitrate, dissolved in 100 c.c. of
water, is allowed to act upon 1 gram of the copper in the cold. The
precipitate is filtered off, washed thoroughly with water, and the basic salt
dissolved and determined colorimetrically.
One part of copper found represents 1.68 part of cuprous oxide, or 0.19 part
of oxygen. Copper generally carries from 0.1 to 0.2 per cent. of oxygen.
Silver is found in most samples, but occurs in variable proportions; when it
amounts to 30 ounces per ton it has a commercial value. To determine its
amount, dissolve 10 grams of the copper in 35 c.c. of nitric acid and 50 c.c.
of water, boil off nitrous fumes, and dilute to about 100 c.c. One or two c.c.
of dilute hydrochloric acid (one to 100 of water) are added, stirred in, and
the precipitate allowed to settle for twenty-four hours. Filter through a
double Swedish paper, dry, burn, and cupel the ashes with one gram of
sheet lead.
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Ten grams of a sample of copper gave in this way 4.7 milligrams of silver.
Ten grams of the same copper, to which 24 milligrams of silver had been
added gave 28.2 milligrams.
Gold.—To determine it, dissolve 10, 20, or 50 grams of the sample in 35,
70, or 175 c.c. of nitric acid and an equal volume of water, boil till free
from nitrous fumes, and dilute to double its volume. Allow to stand for
some time, decant on to a filter, dry, burn, and cupel the ashes with 1 gram
of sheet lead. If silver is present, owing to traces of chlorides in the re-
agents used, "parting" will be necessary. (See Gold.)
Working in this way on 20 grams of copper, to which 1.8 milligram of gold
had been added, a button weighing 2.0 milligrams was obtained.
Antimony is not a frequent impurity of copper: it can be detected in
quantities over 0.1 per cent. by a white residue of Sb2O4, insoluble in nitric
acid. With material containing only small quantities of antimony the white
oxide does not show itself for some time, but on long-continued boiling it
separates as a fine powder. It is best (when looking for it) to evaporate the
nitric acid solution to the crystallising point, to add a little fresh nitric acid
and water, and then to filter off the precipitate. After weighing it should be
examined for arsenic and bismuth.
Lead.—Refined coppers are often free from lead, anything more than traces
being seldom found; in coarse coppers it is sometimes present in
considerable quantities.
Its presence may be detected in the estimation of the copper electrolytically,
the platinum spiral becoming coated with a brown or black deposit of lead
dioxide. The depth of colour varies with the lead present, and obviously
could be made the basis of an approximate estimation. The colour shows
itself within an hour or so, but is best observed when all the copper has
been deposited.
Electrolysing a solution of one gram of pure copper, to which 0.5 milligram
of lead had been added, the deposit was dark brown; in a similar solution
with 1 milligram of lead it was much darker, and with 2 milligrams it was
black. Under the conditions of the assay the dioxide cannot be weighed, as
it partly dissolves on breaking the current. When lead has been found, its
Ten grams of the same copper, to which 24 milligrams of silver had been
added gave 28.2 milligrams.
Gold.—To determine it, dissolve 10, 20, or 50 grams of the sample in 35,
70, or 175 c.c. of nitric acid and an equal volume of water, boil till free
from nitrous fumes, and dilute to double its volume. Allow to stand for
some time, decant on to a filter, dry, burn, and cupel the ashes with 1 gram
of sheet lead. If silver is present, owing to traces of chlorides in the re-
agents used, "parting" will be necessary. (See Gold.)
Working in this way on 20 grams of copper, to which 1.8 milligram of gold
had been added, a button weighing 2.0 milligrams was obtained.
Antimony is not a frequent impurity of copper: it can be detected in
quantities over 0.1 per cent. by a white residue of Sb2O4, insoluble in nitric
acid. With material containing only small quantities of antimony the white
oxide does not show itself for some time, but on long-continued boiling it
separates as a fine powder. It is best (when looking for it) to evaporate the
nitric acid solution to the crystallising point, to add a little fresh nitric acid
and water, and then to filter off the precipitate. After weighing it should be
examined for arsenic and bismuth.
Lead.—Refined coppers are often free from lead, anything more than traces
being seldom found; in coarse coppers it is sometimes present in
considerable quantities.
Its presence may be detected in the estimation of the copper electrolytically,
the platinum spiral becoming coated with a brown or black deposit of lead
dioxide. The depth of colour varies with the lead present, and obviously
could be made the basis of an approximate estimation. The colour shows
itself within an hour or so, but is best observed when all the copper has
been deposited.
Electrolysing a solution of one gram of pure copper, to which 0.5 milligram
of lead had been added, the deposit was dark brown; in a similar solution
with 1 milligram of lead it was much darker, and with 2 milligrams it was
black. Under the conditions of the assay the dioxide cannot be weighed, as
it partly dissolves on breaking the current. When lead has been found, its
Page 267
quantity may be estimated by evaporating to dryness the nitric acid solution
to which an excess of sulphuric acid has been added, taking up with water,
and filtering off and weighing the lead sulphate.
The separation of traces of lead as chromate is a fairly good one. Dissolve 5
grams of the copper in 17 c.c. of nitric acid and an equal volume of water;
boil off nitrous fumes, neutralise with soda, and afterwards acidulate with
acetic acid; and dilute to a litre. Add 20 grams of sodium acetate, warm, and
precipitate the lead with a dilute solution of potassium chromate. Copper
chromate (yellow) may be at the same time thrown down, but it is readily
soluble on diluting. Filter off the precipitate; wash it into a beaker and pass
sulphuretted hydrogen; oxidise the sulphide and weigh as lead sulphate.
Treated in this way 5 grams of copper yielded sulphate of lead equal to 2.0
milligrams of lead. Five grams of the same sample to which 10 milligrams
of lead were added gave 11.4 milligrams.
Nickel and Cobalt.—Nickel is always present in larger or smaller
quantities in commercial copper, and, perhaps, has an influence on the
properties of the metal. It is determined as follows:—Dissolve 10 grams of
the copper in 35 c.c. of nitric acid and an equal bulk of water, boil off
nitrous fumes and neutralise with soda, add 2 grams of carbonate of soda
dissolved in water, boil, and filter. Acidify the filtrate with 2 or 3 c.c. of
dilute nitric acid and dilute to 1 or 1-1/2 litres. Pass sulphuretted hydrogen
through the cold solution till the copper is all down and the liquid smells of
the gas. Filter and evaporate the filtrate to a small bulk, and determine the
nickel by electrolysing the solution rendered ammoniacal, or by
precipitating as sulphide and weighing as sulphate. (See under Nickel.) The
precipitate, after weighing, should be tested for cobalt. If present it is
separated with potassium nitrite as described under Cobalt. Ten grams of
copper gave 6.0 milligrams of nickel; and another lot of 10 grams of the
same copper, to which 10.0 milligrams of nickel had been added, gave 17.2
milligrams.
Sulphur.—The amount of sulphur in refined copper is very small, seldom
exceeding 0.005 per cent. In coarse copper, as might be expected, it is found
in larger quantities.
to which an excess of sulphuric acid has been added, taking up with water,
and filtering off and weighing the lead sulphate.
The separation of traces of lead as chromate is a fairly good one. Dissolve 5
grams of the copper in 17 c.c. of nitric acid and an equal volume of water;
boil off nitrous fumes, neutralise with soda, and afterwards acidulate with
acetic acid; and dilute to a litre. Add 20 grams of sodium acetate, warm, and
precipitate the lead with a dilute solution of potassium chromate. Copper
chromate (yellow) may be at the same time thrown down, but it is readily
soluble on diluting. Filter off the precipitate; wash it into a beaker and pass
sulphuretted hydrogen; oxidise the sulphide and weigh as lead sulphate.
Treated in this way 5 grams of copper yielded sulphate of lead equal to 2.0
milligrams of lead. Five grams of the same sample to which 10 milligrams
of lead were added gave 11.4 milligrams.
Nickel and Cobalt.—Nickel is always present in larger or smaller
quantities in commercial copper, and, perhaps, has an influence on the
properties of the metal. It is determined as follows:—Dissolve 10 grams of
the copper in 35 c.c. of nitric acid and an equal bulk of water, boil off
nitrous fumes and neutralise with soda, add 2 grams of carbonate of soda
dissolved in water, boil, and filter. Acidify the filtrate with 2 or 3 c.c. of
dilute nitric acid and dilute to 1 or 1-1/2 litres. Pass sulphuretted hydrogen
through the cold solution till the copper is all down and the liquid smells of
the gas. Filter and evaporate the filtrate to a small bulk, and determine the
nickel by electrolysing the solution rendered ammoniacal, or by
precipitating as sulphide and weighing as sulphate. (See under Nickel.) The
precipitate, after weighing, should be tested for cobalt. If present it is
separated with potassium nitrite as described under Cobalt. Ten grams of
copper gave 6.0 milligrams of nickel; and another lot of 10 grams of the
same copper, to which 10.0 milligrams of nickel had been added, gave 17.2
milligrams.
Sulphur.—The amount of sulphur in refined copper is very small, seldom
exceeding 0.005 per cent. In coarse copper, as might be expected, it is found
in larger quantities.
Page 268
In determining it, it is first converted into sulphuric acid, and then
precipitated and weighed as barium sulphate. The precipitation cannot be
effected from a nitric acid solution. Ten grams of copper are dissolved in
nitric acid, as for the other determinations, and then boiled with excess of
hydrochloric acid till the nitric acid is completely removed. There is then
added a few drops of a dilute solution of baric chloride, and the solution is
allowed to stand for some hours. The baric sulphate is filtered off and
weighed.
The necessity for precipitating from a hydrochloric acid solution is seen
from the following determinations. In each experiment 10 grams of copper
was used, and a known weight of sulphur, in the form of copper sulphate,
added.
precipitated and weighed as barium sulphate. The precipitation cannot be
effected from a nitric acid solution. Ten grams of copper are dissolved in
nitric acid, as for the other determinations, and then boiled with excess of
hydrochloric acid till the nitric acid is completely removed. There is then
added a few drops of a dilute solution of baric chloride, and the solution is
allowed to stand for some hours. The baric sulphate is filtered off and
weighed.
The necessity for precipitating from a hydrochloric acid solution is seen
from the following determinations. In each experiment 10 grams of copper
was used, and a known weight of sulphur, in the form of copper sulphate,
added.
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Sulphur Sulphur found in Hydrochloric Sulphur found in Nitric
added. Acid Solution. Acid Solution.
5 milligrams 8 milligrams 0.03 milligrams
10 " 11 " 0.03 "
15 " 17 " 12.00 "
Bismuth.—Nearly all samples of copper contain bismuth, but only in small
quantities. It is best determined colorimetrically as described under
Bismuth. The method of concentrating and preparing the solution for
colorimetric assay is as follows. Dissolve 10 grams of copper in nitric acid,
as in the other determinations; neutralise with soda; add 1 or 1.5 grams of
bicarbonate of soda and boil for ten minutes; filter, dissolve the precipitate
in hot dilute sulphuric acid; add sulphurous acid and potassium iodide in
excess, and boil till free from iodine. Filter and dilute to 500 c.c. Take 50
c.c. of the yellow solution for the determination. A few c.c. of a dilute
solution of sulphurous acid (1 in 100) will prevent the liberation of iodine.
The following experiments test the method of separation. Ten grams of
copper were treated as above and precipitated with 1.5 gram of "soda;" the
precipitate contained 0.6 milligram of bismuth (= 0.006 per cent.). The
filtrate treated with another 1.5 gram of "soda" gave a precipitate which was
free from bismuth. To the filtrate from this was added 1.0 milligram of
bismuth, and another fraction was precipitated with 1.5 gram of "soda." In
this precipitate was found 1.0 milligram of bismuth. To the filtrate another
milligram of bismuth was added and the separation with "soda" repeated.
The bismuth was separated from this precipitate with ammonic carbonate
before determination, and 0.9 milligram was found.
Arsenic.—The proportion of arsenic in copper varies from 0.01 to 0.75 per
cent. whilst in coarse copper it may amount to 2 or even 3 per cent. To
determine it, dissolve 5, 10, or 20 grams of the copper (according to the
amount of arsenic present) in 18 c.c., 35 c.c., or 70 c.c. of nitric acid, and an
equal volume of water. Boil off the nitrous fumes, dilute to 100 c.c. and
neutralise with soda; add 1.5 or 2 grams of carbonate of soda dissolved in a
little water, and boil. Filter (washing is unnecessary) and dissolve back into
the flask with a little dilute hydrochloric acid; add 30 c.c. of dilute ammonia
and 25 c.c. of "magnesia mixture," and allow to stand overnight. The whole
of the arsenic is precipitated as ammonic-magnesic arsenate in one hour, but
added. Acid Solution. Acid Solution.
5 milligrams 8 milligrams 0.03 milligrams
10 " 11 " 0.03 "
15 " 17 " 12.00 "
Bismuth.—Nearly all samples of copper contain bismuth, but only in small
quantities. It is best determined colorimetrically as described under
Bismuth. The method of concentrating and preparing the solution for
colorimetric assay is as follows. Dissolve 10 grams of copper in nitric acid,
as in the other determinations; neutralise with soda; add 1 or 1.5 grams of
bicarbonate of soda and boil for ten minutes; filter, dissolve the precipitate
in hot dilute sulphuric acid; add sulphurous acid and potassium iodide in
excess, and boil till free from iodine. Filter and dilute to 500 c.c. Take 50
c.c. of the yellow solution for the determination. A few c.c. of a dilute
solution of sulphurous acid (1 in 100) will prevent the liberation of iodine.
The following experiments test the method of separation. Ten grams of
copper were treated as above and precipitated with 1.5 gram of "soda;" the
precipitate contained 0.6 milligram of bismuth (= 0.006 per cent.). The
filtrate treated with another 1.5 gram of "soda" gave a precipitate which was
free from bismuth. To the filtrate from this was added 1.0 milligram of
bismuth, and another fraction was precipitated with 1.5 gram of "soda." In
this precipitate was found 1.0 milligram of bismuth. To the filtrate another
milligram of bismuth was added and the separation with "soda" repeated.
The bismuth was separated from this precipitate with ammonic carbonate
before determination, and 0.9 milligram was found.
Arsenic.—The proportion of arsenic in copper varies from 0.01 to 0.75 per
cent. whilst in coarse copper it may amount to 2 or even 3 per cent. To
determine it, dissolve 5, 10, or 20 grams of the copper (according to the
amount of arsenic present) in 18 c.c., 35 c.c., or 70 c.c. of nitric acid, and an
equal volume of water. Boil off the nitrous fumes, dilute to 100 c.c. and
neutralise with soda; add 1.5 or 2 grams of carbonate of soda dissolved in a
little water, and boil. Filter (washing is unnecessary) and dissolve back into
the flask with a little dilute hydrochloric acid; add 30 c.c. of dilute ammonia
and 25 c.c. of "magnesia mixture," and allow to stand overnight. The whole
of the arsenic is precipitated as ammonic-magnesic arsenate in one hour, but
Page 270
it is advisable to leave it longer. The precipitate may be dried and weighed,
or, better, titrated with uranium acetate. (See Arsenic.) To test this method
of separation 10 grams of pure copper were taken and 0.200 gram of arsenic
dissolved with it. The arsenic was determined by titration with uranium
acetate, and 0.200 gram was found. Two other similar experiments with
0.080 and 0.010 gram of arsenic added, gave 0.079 and 0.012 gram
respectively.
Antimony or bismuth may be present without interfering with the titration.
With 0.100 gram of antimony and 0.100 gram of arsenic, 0.100 gram of
arsenic was found; and in another case, with 0.100 gram of bismuth and
0.060 gram of arsenic, 0.060 gram was found. In these experiments the
antimony and bismuth were present in the assay solution when titrated. For
a gravimetric determination they would require to be removed before
precipitating with "magnesia mixture."
Phosphorus, if present, counts as arsenic in the proportion of 1 to 2.4; but,
except in the case of coarse coppers, it is always absent.
Iron, if present, interferes by forming a white flocculent precipitate of ferric
arsenate after the addition of the sodium acetate and preliminary to the
titration. Each milligram of iron abstracts, in this way, 1.3 milligrams of
arsenic.
Iron.—Refined coppers carry traces of iron, varying from 0.001 to 0.01 per
cent. It is best determined during the arsenic estimation. The precipitate of
the ammonic-magnesic arsenate will contain the whole of the iron as ferric
hydrate. On dissolving in hydrochloric acid, neutralising with ammonia,
adding 5 c.c. of sodic acetate, diluting, and boiling, it reappears as a white
precipitate of ferric arsenate. It is filtered off (the arsenic being estimated in
the filtrate), dissolved in warm hydrochloric acid, and determined
colorimetrically as described under Iron. A series of experiments testing the
separation is there given.
Phosphorus.—Refined coppers do not carry phosphorus, although it may
be present in "coarse copper" up to 1 per cent. or more. In such samples the
following method is adopted for the estimation of both phosphorus and
arsenic. Dissolve 10 grams of copper and 0.1, 0.2, or 0.3 gram of iron wire
(according to the amount of arsenic and phosphorus present) in 35 c.c. of
or, better, titrated with uranium acetate. (See Arsenic.) To test this method
of separation 10 grams of pure copper were taken and 0.200 gram of arsenic
dissolved with it. The arsenic was determined by titration with uranium
acetate, and 0.200 gram was found. Two other similar experiments with
0.080 and 0.010 gram of arsenic added, gave 0.079 and 0.012 gram
respectively.
Antimony or bismuth may be present without interfering with the titration.
With 0.100 gram of antimony and 0.100 gram of arsenic, 0.100 gram of
arsenic was found; and in another case, with 0.100 gram of bismuth and
0.060 gram of arsenic, 0.060 gram was found. In these experiments the
antimony and bismuth were present in the assay solution when titrated. For
a gravimetric determination they would require to be removed before
precipitating with "magnesia mixture."
Phosphorus, if present, counts as arsenic in the proportion of 1 to 2.4; but,
except in the case of coarse coppers, it is always absent.
Iron, if present, interferes by forming a white flocculent precipitate of ferric
arsenate after the addition of the sodium acetate and preliminary to the
titration. Each milligram of iron abstracts, in this way, 1.3 milligrams of
arsenic.
Iron.—Refined coppers carry traces of iron, varying from 0.001 to 0.01 per
cent. It is best determined during the arsenic estimation. The precipitate of
the ammonic-magnesic arsenate will contain the whole of the iron as ferric
hydrate. On dissolving in hydrochloric acid, neutralising with ammonia,
adding 5 c.c. of sodic acetate, diluting, and boiling, it reappears as a white
precipitate of ferric arsenate. It is filtered off (the arsenic being estimated in
the filtrate), dissolved in warm hydrochloric acid, and determined
colorimetrically as described under Iron. A series of experiments testing the
separation is there given.
Phosphorus.—Refined coppers do not carry phosphorus, although it may
be present in "coarse copper" up to 1 per cent. or more. In such samples the
following method is adopted for the estimation of both phosphorus and
arsenic. Dissolve 10 grams of copper and 0.1, 0.2, or 0.3 gram of iron wire
(according to the amount of arsenic and phosphorus present) in 35 c.c. of
Page 271
nitric acid and an equal volume of water. Add soda till the free acid is
nearly neutralised. Next add a strong solution of sodium acetate, until the
solution ceases to darken on further addition, then dilute with water to half
a litre. The solution is best contained in a large beaker; it is next heated to
the boiling point, and at once removed and allowed to settle. If the
precipitate is light coloured it is evidence that sufficient iron has not been
added, or, if it is green, from basic copper salts, it shows that the solution
was not sufficiently acid. In either case start afresh. Filter off the precipitate
and wash with hot water containing a little sodium acetate, dissolve it off
the filter with hot dilute hydrochloric acid, add ammonia in excess, and pass
sulphuretted hydrogen for five minutes. Warm at about 70° C. for a quarter
of an hour. Filter. The clear yellow filtrate contains the arsenic and
phosphorus. Add dilute sulphuric acid in excess; filter off the yellow
precipitate of sulphide of arsenic, dissolve it in nitric acid, and titrate with
uranium acetate, as described under Arsenic.
The filtrate from the sulphide of arsenic is rendered alkaline with ammonia
and "magnesia mixture" added. The solution is stirred, and allowed to stand
overnight. The precipitate of ammonic-magnesic phosphate is filtered off,
dissolved, and titrated with uranium acetate, using the same standard
solution as is used in the arsenic assay: 0.5 gram of arsenic equals 0.207
gram of phosphorus.
Copper.—The method of determining this has been described under
Electrolytic Assay.
In the method of concentration by fractional precipitation with sodic
carbonate (which is adopted in most of these determinations) the precipitate
will contain all the bismuth, iron, and alumina; the arsenic and phosphorus
as cupric arsenate and phosphate; and the greater part of the lead, antimony,
and silver. The nickel and cobalt, and the sulphur as sulphuric acid, will
remain in solution with the greater part of the copper.
PRACTICAL EXERCISES.
1. According to a wet assay 2 grams of a certain ore contained 0.3650 gram
of copper. What would you expect the dry assay produce to be?
nearly neutralised. Next add a strong solution of sodium acetate, until the
solution ceases to darken on further addition, then dilute with water to half
a litre. The solution is best contained in a large beaker; it is next heated to
the boiling point, and at once removed and allowed to settle. If the
precipitate is light coloured it is evidence that sufficient iron has not been
added, or, if it is green, from basic copper salts, it shows that the solution
was not sufficiently acid. In either case start afresh. Filter off the precipitate
and wash with hot water containing a little sodium acetate, dissolve it off
the filter with hot dilute hydrochloric acid, add ammonia in excess, and pass
sulphuretted hydrogen for five minutes. Warm at about 70° C. for a quarter
of an hour. Filter. The clear yellow filtrate contains the arsenic and
phosphorus. Add dilute sulphuric acid in excess; filter off the yellow
precipitate of sulphide of arsenic, dissolve it in nitric acid, and titrate with
uranium acetate, as described under Arsenic.
The filtrate from the sulphide of arsenic is rendered alkaline with ammonia
and "magnesia mixture" added. The solution is stirred, and allowed to stand
overnight. The precipitate of ammonic-magnesic phosphate is filtered off,
dissolved, and titrated with uranium acetate, using the same standard
solution as is used in the arsenic assay: 0.5 gram of arsenic equals 0.207
gram of phosphorus.
Copper.—The method of determining this has been described under
Electrolytic Assay.
In the method of concentration by fractional precipitation with sodic
carbonate (which is adopted in most of these determinations) the precipitate
will contain all the bismuth, iron, and alumina; the arsenic and phosphorus
as cupric arsenate and phosphate; and the greater part of the lead, antimony,
and silver. The nickel and cobalt, and the sulphur as sulphuric acid, will
remain in solution with the greater part of the copper.
PRACTICAL EXERCISES.
1. According to a wet assay 2 grams of a certain ore contained 0.3650 gram
of copper. What would you expect the dry assay produce to be?
Page 272
2. A standard solution is made by dissolving 25 grams of potassic cyanide
and diluting to a litre. Assuming the salt to be 98 per cent. real cyanide,
what would 100 c.c. of the solution be equivalent to in grams of copper?
3. How would you make a solution of "hypo" of such strength that 100 c.c.
shall equal 0.633 gram of copper?
4. What weight of ore, containing 17.0 per cent. of copper, would you take
in order to get about 0.5 gram of copper in solution for electrolysis?
5. The solution of copper in nitric acid is effected by the following reaction:
—
3Cu + 8HNO3 = 3Cu(NO3)2 + 4H2O + 2NO.
What volume of nitric acid will be required to dissolve 1 gram of copper?
LEAD.
The chief ore of lead is galena, a sulphide of lead, common in most mining
districts, and frequently associated with blende and copper-pyrites. It
always carries more or less silver; so that in the assay of the ore a silver
determination is always necessary. Carbonate (cerussite), sulphate
(anglesite), and phosphate (pyromorphite) of lead also occur as ores, but in
much smaller quantities.
Lead ores are easily concentrated (owing to their high specific gravity, &c.)
by mechanical operations, so that the mineral matter sent to the smelter is
comparatively pure.
Lead is readily soluble in dilute nitric acid. The addition of sulphuric acid to
this solution throws down heavy, white, and insoluble lead sulphate.
Galena is soluble in hot hydrochloric acid, sulphuretted hydrogen being
evolved; but the action is retarded by the separation of the sparingly soluble
lead chloride. If a rod of zinc is placed in this solution, metallic lead is
precipitated on it as a spongy mass, the lead chloride being decomposed as
fast as it is formed. The opening up of the ore is thus easily effected, the
sulphur going off as sulphuretted hydrogen, and the lead remaining in a
and diluting to a litre. Assuming the salt to be 98 per cent. real cyanide,
what would 100 c.c. of the solution be equivalent to in grams of copper?
3. How would you make a solution of "hypo" of such strength that 100 c.c.
shall equal 0.633 gram of copper?
4. What weight of ore, containing 17.0 per cent. of copper, would you take
in order to get about 0.5 gram of copper in solution for electrolysis?
5. The solution of copper in nitric acid is effected by the following reaction:
—
3Cu + 8HNO3 = 3Cu(NO3)2 + 4H2O + 2NO.
What volume of nitric acid will be required to dissolve 1 gram of copper?
LEAD.
The chief ore of lead is galena, a sulphide of lead, common in most mining
districts, and frequently associated with blende and copper-pyrites. It
always carries more or less silver; so that in the assay of the ore a silver
determination is always necessary. Carbonate (cerussite), sulphate
(anglesite), and phosphate (pyromorphite) of lead also occur as ores, but in
much smaller quantities.
Lead ores are easily concentrated (owing to their high specific gravity, &c.)
by mechanical operations, so that the mineral matter sent to the smelter is
comparatively pure.
Lead is readily soluble in dilute nitric acid. The addition of sulphuric acid to
this solution throws down heavy, white, and insoluble lead sulphate.
Galena is soluble in hot hydrochloric acid, sulphuretted hydrogen being
evolved; but the action is retarded by the separation of the sparingly soluble
lead chloride. If a rod of zinc is placed in this solution, metallic lead is
precipitated on it as a spongy mass, the lead chloride being decomposed as
fast as it is formed. The opening up of the ore is thus easily effected, the
sulphur going off as sulphuretted hydrogen, and the lead remaining in a
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form easily soluble in dilute nitric acid. Galena itself is readily attacked by
nitric acid, part of the lead going into solution, and the rest remaining as
insoluble lead sulphate. The sulphate is due to the oxidation of the sulphur
by nitric acid; its amount will vary with the quantity and concentration of
the acid used. Sulphate of lead is soluble in solutions of ammonium or
sodium acetate; or it may be converted into carbonate by boiling with
carbonate of soda. The carbonate, after washing off the sulphate of soda,
dissolves easily in nitric acid. The precipitation of lead from acid solutions
with sulphuric acid, and the solubility of the precipitate in ammonium
acetate, distinguishes it from all other metals. The addition of potassium
chromate to the acetate solution reprecipitates the lead as a yellow
chromate.
DRY ASSAY.
The dry assay of lead is largely used, but it is only applicable to rich or
concentrated ores, and even with these only gives approximate results. Both
lead and lead sulphide are sensibly volatile at a moderately-high
temperature; hence it is necessary to obtain a slag which is easily fusible.
As a reducing agent iron is almost always used, and this is added either in
the form of an iron rod, or the crucible itself is made of this metal. The flux
used is carbonate of soda.
When a clay crucible is used, the method of working is as follows:—Weigh
up 25 grams of the dry and powdered ore, mix with an equal weight of
"soda" and 2 grams of tartar; place in a crucible (E. Battersea round), and
then insert a piece of iron rod about half an inch in diameter, and of such a
length that it will just allow the crucible to be covered. The rod should be
pushed down so as to touch the bottom of the crucible, and the mixture
should be covered with a sprinkling of borax. Place in a furnace heated to,
but not above, redness, and cover the crucible. In about twenty minutes the
charge will be fused: the fusion is complete when bubbles of gas are no
longer being evolved; and then, but not till then, the iron is withdrawn, any
adhering buttons of lead being washed off by dipping the rod a few times in
the slag. Cover the crucible, leave it for a minute or two, and then pour.
Detach the slag, when cold, by hammering. The weight of the button
nitric acid, part of the lead going into solution, and the rest remaining as
insoluble lead sulphate. The sulphate is due to the oxidation of the sulphur
by nitric acid; its amount will vary with the quantity and concentration of
the acid used. Sulphate of lead is soluble in solutions of ammonium or
sodium acetate; or it may be converted into carbonate by boiling with
carbonate of soda. The carbonate, after washing off the sulphate of soda,
dissolves easily in nitric acid. The precipitation of lead from acid solutions
with sulphuric acid, and the solubility of the precipitate in ammonium
acetate, distinguishes it from all other metals. The addition of potassium
chromate to the acetate solution reprecipitates the lead as a yellow
chromate.
DRY ASSAY.
The dry assay of lead is largely used, but it is only applicable to rich or
concentrated ores, and even with these only gives approximate results. Both
lead and lead sulphide are sensibly volatile at a moderately-high
temperature; hence it is necessary to obtain a slag which is easily fusible.
As a reducing agent iron is almost always used, and this is added either in
the form of an iron rod, or the crucible itself is made of this metal. The flux
used is carbonate of soda.
When a clay crucible is used, the method of working is as follows:—Weigh
up 25 grams of the dry and powdered ore, mix with an equal weight of
"soda" and 2 grams of tartar; place in a crucible (E. Battersea round), and
then insert a piece of iron rod about half an inch in diameter, and of such a
length that it will just allow the crucible to be covered. The rod should be
pushed down so as to touch the bottom of the crucible, and the mixture
should be covered with a sprinkling of borax. Place in a furnace heated to,
but not above, redness, and cover the crucible. In about twenty minutes the
charge will be fused: the fusion is complete when bubbles of gas are no
longer being evolved; and then, but not till then, the iron is withdrawn, any
adhering buttons of lead being washed off by dipping the rod a few times in
the slag. Cover the crucible, leave it for a minute or two, and then pour.
Detach the slag, when cold, by hammering. The weight of the button
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multiplied by 4 gives the percentage. The commoner errors of students in
working the process are too high a temperature and too quick a withdrawal.
A sample of ore treated in this manner gave on duplicate assay 17.5 and
17.6 grams of lead, equalling 70.0 and 70.4 per cent. respectively. By wet
assay the sample gave 73.3 per cent. Using an iron crucible, the results will
be 1 per cent. or so higher. The crucible must be made of wrought iron; and,
if it has been previously used, should be cleaned by heating to dull redness
and scraping the scale off with a stirrer. Take 30 grams of the ore, mix with
30 grams of "soda" and 3 grams of tartar; put the mixture in the crucible,
and cover with a sprinkling of borax; heat for about twenty minutes at not
too high a temperature, and then scrape down the slag adhering to the side
with a stirrer. Leave in the furnace till action has ceased. Before pouring,
tap the pot gently, and then tilt it so as to make the slag wash over the part
of the crucible along which the charge is to be poured. Pour; and, when
cold, clean and weigh the button of metal. A crucible may be used from ten
to twenty times.
These assays are for ores containing the lead chiefly as sulphide. For
oxidised ores, charcoal or tartar is employed as the reducing agent. The
student may practise on red lead as follows:—Take 30 grams of red lead;
mix with 10 grams each of borax and "soda" and about 1.5 gram of
powdered charcoal; place in a small clay crucible with a cover (C. Battersea
round), fuse at a gentle heat, and pour when action ceases. This assay will
only take a few minutes.
Where lead is present as phosphate (as in the case of pyromorphite), or
mixed with phosphates (as sometimes happens), carbonate of soda is a
suitable flux; but the phosphate of soda which is formed makes a thick
tenacious slag, which is very apt to be carried out of the pot by the escaping
gas. A wide-mouthed clay pot is taken and a little fluor spar added. For the
assay of pyromorphite the following charge may be used:—Ore, 20 grams;
"soda," 25 grams; tartar, 7 grams; and fluor spar, 5 grams; and 2 grams of
borax as a cover. This will melt down in about ten minutes, and should be
poured as soon as tranquil.
WET ASSAY.
working the process are too high a temperature and too quick a withdrawal.
A sample of ore treated in this manner gave on duplicate assay 17.5 and
17.6 grams of lead, equalling 70.0 and 70.4 per cent. respectively. By wet
assay the sample gave 73.3 per cent. Using an iron crucible, the results will
be 1 per cent. or so higher. The crucible must be made of wrought iron; and,
if it has been previously used, should be cleaned by heating to dull redness
and scraping the scale off with a stirrer. Take 30 grams of the ore, mix with
30 grams of "soda" and 3 grams of tartar; put the mixture in the crucible,
and cover with a sprinkling of borax; heat for about twenty minutes at not
too high a temperature, and then scrape down the slag adhering to the side
with a stirrer. Leave in the furnace till action has ceased. Before pouring,
tap the pot gently, and then tilt it so as to make the slag wash over the part
of the crucible along which the charge is to be poured. Pour; and, when
cold, clean and weigh the button of metal. A crucible may be used from ten
to twenty times.
These assays are for ores containing the lead chiefly as sulphide. For
oxidised ores, charcoal or tartar is employed as the reducing agent. The
student may practise on red lead as follows:—Take 30 grams of red lead;
mix with 10 grams each of borax and "soda" and about 1.5 gram of
powdered charcoal; place in a small clay crucible with a cover (C. Battersea
round), fuse at a gentle heat, and pour when action ceases. This assay will
only take a few minutes.
Where lead is present as phosphate (as in the case of pyromorphite), or
mixed with phosphates (as sometimes happens), carbonate of soda is a
suitable flux; but the phosphate of soda which is formed makes a thick
tenacious slag, which is very apt to be carried out of the pot by the escaping
gas. A wide-mouthed clay pot is taken and a little fluor spar added. For the
assay of pyromorphite the following charge may be used:—Ore, 20 grams;
"soda," 25 grams; tartar, 7 grams; and fluor spar, 5 grams; and 2 grams of
borax as a cover. This will melt down in about ten minutes, and should be
poured as soon as tranquil.
WET ASSAY.
Page 275
In the case of galena the best method of getting the lead into solution is to
treat with hydrochloric acid and zinc. Put 1 gram of the ore in an
evaporating dish 4 inches across, and cover with 10 c.c. of dilute
hydrochloric acid. Heat till the evolution of sulphuretted hydrogen becomes
sluggish, and then drop in a piece of zinc rod. If the solution effervesces too
strongly, dilute it. Continue the heating until the sulphide is seen to be all
dissolved; when the lead is all precipitated, pour off the liquid and wash
twice with cold water. Peel off the precipitated lead with the help of a glass
rod, and then clean the zinc. Cover the lead with 20 c.c. of water and 5 c.c.
of dilute nitric acid, and heat gently till dissolved; all the lead will be in
solution, and, when filtered off from the gangue, will be ready for a
gravimetric determination. For volumetric work this filtering is
unnecessary.
The chief objection to this method is that commercial zinc carries
considerable quantities of lead. Although this can be determined and
allowed for, the correction required is in most cases too large to be
satisfactory. The following method is applicable in all cases, but is more
troublesome:—Treat 1 gram of the ore with 10 c.c. of dilute nitric acid in an
evaporating dish covered with a clock-glass, and evaporate till nearly dry.
Take up with 50 c.c. of water, and add 10 c.c. of dilute sulphuric acid. Filter.
The residue contains the lead as sulphate, together with the insoluble matter
of the ore and globules of sulphur. Warm with a solution of ammonium
acetate, and filter. The lead will be in the filtrate, and is recovered in a state
fit for direct gravimetric estimation by the addition of dilute sulphuric acid.
If the volumetric method is to be used, the lead sulphate should be
dissolved out with a solution of sodium acetate instead of with the
ammonium salt solution.
GRAVIMETRIC DETERMINATION.
The lead is separated and precipitated as sulphate, as already described. The
solution must be allowed to stand, and the clear liquid be decanted through
a filter. Transfer the precipitate, and wash with very dilute sulphuric acid (1
or 2 c.c. in 100 c.c. of water). The acid must be completely removed with
one or two washes with cold water, and then with alcohol. The volume of
liquid required for washing is small, as the precipitate is dense and easily
treat with hydrochloric acid and zinc. Put 1 gram of the ore in an
evaporating dish 4 inches across, and cover with 10 c.c. of dilute
hydrochloric acid. Heat till the evolution of sulphuretted hydrogen becomes
sluggish, and then drop in a piece of zinc rod. If the solution effervesces too
strongly, dilute it. Continue the heating until the sulphide is seen to be all
dissolved; when the lead is all precipitated, pour off the liquid and wash
twice with cold water. Peel off the precipitated lead with the help of a glass
rod, and then clean the zinc. Cover the lead with 20 c.c. of water and 5 c.c.
of dilute nitric acid, and heat gently till dissolved; all the lead will be in
solution, and, when filtered off from the gangue, will be ready for a
gravimetric determination. For volumetric work this filtering is
unnecessary.
The chief objection to this method is that commercial zinc carries
considerable quantities of lead. Although this can be determined and
allowed for, the correction required is in most cases too large to be
satisfactory. The following method is applicable in all cases, but is more
troublesome:—Treat 1 gram of the ore with 10 c.c. of dilute nitric acid in an
evaporating dish covered with a clock-glass, and evaporate till nearly dry.
Take up with 50 c.c. of water, and add 10 c.c. of dilute sulphuric acid. Filter.
The residue contains the lead as sulphate, together with the insoluble matter
of the ore and globules of sulphur. Warm with a solution of ammonium
acetate, and filter. The lead will be in the filtrate, and is recovered in a state
fit for direct gravimetric estimation by the addition of dilute sulphuric acid.
If the volumetric method is to be used, the lead sulphate should be
dissolved out with a solution of sodium acetate instead of with the
ammonium salt solution.
GRAVIMETRIC DETERMINATION.
The lead is separated and precipitated as sulphate, as already described. The
solution must be allowed to stand, and the clear liquid be decanted through
a filter. Transfer the precipitate, and wash with very dilute sulphuric acid (1
or 2 c.c. in 100 c.c. of water). The acid must be completely removed with
one or two washes with cold water, and then with alcohol. The volume of
liquid required for washing is small, as the precipitate is dense and easily
Page 276
cleaned; but the washing must be carefully done, since if any acid remains
it will, on drying, char the paper, and render the subsequent work
troublesome. Dry, transfer to a watch-glass, and burn the filter paper,
collecting its ash in a weighed porcelain crucible. The filter paper must be
freed as much as possible from the lead sulphate before burning, and the
ash treated with a drop or two of nitric and sulphuric acids. Transfer the
lead sulphate to the crucible; ignite gently, keeping the temperature below
redness; cool, and weigh. The precipitate will contain 73.6 per cent. of lead
oxide or 68.3 per cent. of lead.
Determination of Lead in Commercial Zinc.—Take 10 grams of zinc,
and treat (without heating) with 60 c.c. of dilute hydrochloric acid. When
the zinc is nearly all dissolved, decant off the clear liquid, and dissolve the
residue in 2 c.c. of dilute nitric acid. Evaporate till most of the acid is
removed; dilute to 20 or 30 c.c. with water, and add 10 c.c. of dilute
sulphuric acid. Filter off, and weigh the lead sulphate. Ten grams treated in
this way gave—0.1610 gram of lead sulphate, equivalent to 1.10 per cent.
of lead.
VOLUMETRIC METHOD.
This is based upon the reaction between chromate of potash and soluble
lead salts in neutral solutions, whereby an insoluble yellow chromate of
lead is produced.[60] An excess of the chromate is required to complete the
reaction, so that the point at which an indicator shows the presence of
undecomposed chromate cannot be satisfactorily taken as the finish.
Therefore an excess of the standard chromate must be run in, and such
excess determined.
Chromate of lead is not precipitated from strong nitric acid solutions, and
only incompletely from dilute ones. Acids generally are detrimental to the
precipitation, and must be neutralised before titrating. If the lead is present
as sulphate in sodic acetate solution, it is well to render it distinctly alkaline
with ammonia.
Lead chromate precipitated in the cold is a lemon-yellow, light precipitate,
very difficult to filter: on heating to 40° C. the colour becomes orange; at
60° C. it assumes a deeper hue, and becomes flocculent; and at a boiling
it will, on drying, char the paper, and render the subsequent work
troublesome. Dry, transfer to a watch-glass, and burn the filter paper,
collecting its ash in a weighed porcelain crucible. The filter paper must be
freed as much as possible from the lead sulphate before burning, and the
ash treated with a drop or two of nitric and sulphuric acids. Transfer the
lead sulphate to the crucible; ignite gently, keeping the temperature below
redness; cool, and weigh. The precipitate will contain 73.6 per cent. of lead
oxide or 68.3 per cent. of lead.
Determination of Lead in Commercial Zinc.—Take 10 grams of zinc,
and treat (without heating) with 60 c.c. of dilute hydrochloric acid. When
the zinc is nearly all dissolved, decant off the clear liquid, and dissolve the
residue in 2 c.c. of dilute nitric acid. Evaporate till most of the acid is
removed; dilute to 20 or 30 c.c. with water, and add 10 c.c. of dilute
sulphuric acid. Filter off, and weigh the lead sulphate. Ten grams treated in
this way gave—0.1610 gram of lead sulphate, equivalent to 1.10 per cent.
of lead.
VOLUMETRIC METHOD.
This is based upon the reaction between chromate of potash and soluble
lead salts in neutral solutions, whereby an insoluble yellow chromate of
lead is produced.[60] An excess of the chromate is required to complete the
reaction, so that the point at which an indicator shows the presence of
undecomposed chromate cannot be satisfactorily taken as the finish.
Therefore an excess of the standard chromate must be run in, and such
excess determined.
Chromate of lead is not precipitated from strong nitric acid solutions, and
only incompletely from dilute ones. Acids generally are detrimental to the
precipitation, and must be neutralised before titrating. If the lead is present
as sulphate in sodic acetate solution, it is well to render it distinctly alkaline
with ammonia.
Lead chromate precipitated in the cold is a lemon-yellow, light precipitate,
very difficult to filter: on heating to 40° C. the colour becomes orange; at
60° C. it assumes a deeper hue, and becomes flocculent; and at a boiling
Page 277
temperature it still further darkens and settles readily. These changes in
colour are not due to any chemical change, as will be seen by testing the
filtrate for chromium or lead: this is an advantage to the assay, since it is
only at the higher temperature that the precipitate can be easily filtered. The
lead is not completely precipitated, but the amount remaining in solution is
only 2 or 3 milligrams, which is just sufficient to give a dark coloration
with sulphuretted hydrogen.
The standard chromate of potash solution is made by dissolving 7.13 grams
of bichromate of potash and 2.0 grams of caustic soda in water, and diluting
to 1 litre; or 9.40 grams of the neutral chromate (K2CrO4) may be dissolved
and diluted to 1 litre: 100 c.c. will be equivalent to 1.000 gram of lead.
Standard Lead Solution.—16 grams of nitrate of lead (Pb(NO3)2) are
dissolved in water and diluted to 1 litre; 100 c.c. will contain 1.000 gram of
lead.
Acetate of Soda Solution.—250 grams of the crystallised salt (NaAc.3H2O)
are dissolved, and diluted to 1 litre. Use 40 c.c. for each assay.
In the titration the assay solution should measure 150 to 200 c.c., and
should be boiling or nearly so. It is best contained in a pint flask, and the
standard chromate solution used with an ordinary burette. Run in the
chromate solution in a steady stream until the whole of the lead has been
precipitated. The amount required for this may be calculated: for example, 1
gram of an 80 per cent. ore would require 80 c.c. A little of the assay may
be filtered off, and if it does not show a yellow colour in the filtrate run in 2
c.c. more of the standard solution and continue this addition till a colour is
shown. After this run in another c.c. to ensure an excess, dilute to 250 c.c.,
and heat to boiling; allow to settle for three or four minutes, filter off 50 c.c.
into a Nessler glass, and determine the excess of chromate colorimetrically.
The excess found in the 50 c.c. must, of course, be multiplied by five, and
then be deducted from the quantity of chromate originally run into the assay
solution. The quantity to be deducted should not exceed 3 c.c. Where a
number of determinations are made the colorimetric estimation is facilitated
by using a series of standard phials similar to those described under the
Electrolytic Copper Assay. The determination is rendered sharper and less
liable to error by the addition of a few drops of acetic acid to convert the
colour are not due to any chemical change, as will be seen by testing the
filtrate for chromium or lead: this is an advantage to the assay, since it is
only at the higher temperature that the precipitate can be easily filtered. The
lead is not completely precipitated, but the amount remaining in solution is
only 2 or 3 milligrams, which is just sufficient to give a dark coloration
with sulphuretted hydrogen.
The standard chromate of potash solution is made by dissolving 7.13 grams
of bichromate of potash and 2.0 grams of caustic soda in water, and diluting
to 1 litre; or 9.40 grams of the neutral chromate (K2CrO4) may be dissolved
and diluted to 1 litre: 100 c.c. will be equivalent to 1.000 gram of lead.
Standard Lead Solution.—16 grams of nitrate of lead (Pb(NO3)2) are
dissolved in water and diluted to 1 litre; 100 c.c. will contain 1.000 gram of
lead.
Acetate of Soda Solution.—250 grams of the crystallised salt (NaAc.3H2O)
are dissolved, and diluted to 1 litre. Use 40 c.c. for each assay.
In the titration the assay solution should measure 150 to 200 c.c., and
should be boiling or nearly so. It is best contained in a pint flask, and the
standard chromate solution used with an ordinary burette. Run in the
chromate solution in a steady stream until the whole of the lead has been
precipitated. The amount required for this may be calculated: for example, 1
gram of an 80 per cent. ore would require 80 c.c. A little of the assay may
be filtered off, and if it does not show a yellow colour in the filtrate run in 2
c.c. more of the standard solution and continue this addition till a colour is
shown. After this run in another c.c. to ensure an excess, dilute to 250 c.c.,
and heat to boiling; allow to settle for three or four minutes, filter off 50 c.c.
into a Nessler glass, and determine the excess of chromate colorimetrically.
The excess found in the 50 c.c. must, of course, be multiplied by five, and
then be deducted from the quantity of chromate originally run into the assay
solution. The quantity to be deducted should not exceed 3 c.c. Where a
number of determinations are made the colorimetric estimation is facilitated
by using a series of standard phials similar to those described under the
Electrolytic Copper Assay. The determination is rendered sharper and less
liable to error by the addition of a few drops of acetic acid to convert the
Page 278
chromate into bichromate. The same chromate solution must be used in this
determination as was used in the precipitation.
In standardising the chromate solution, the standard lead nitrate solution is
used. A quantity containing about as much lead as the assay is supposed to
contain is measured off, rendered alkaline with dilute ammonia, and then
neutralised with acetic acid, using a small piece of litmus paper dropped
into the solution as indicator. Then dilute, boil, and titrate. When the lead in
the assay has been separated as sulphate and dissolved in sodic acetate, less
chromate is apparently required, and in this case it will be necessary to
precipitate the lead in the standard with an equivalent of sodic sulphate and
redissolve in sodic acetate just as in the assay. In these solutions (although
there is considerable chromate in excess) a further addition of 5 or 6 c.c. of
the chromate solution will cause a further precipitate. The following
experiments show the effect of variation in the conditions of the assay:—
Effect of Varying Temperature.—Twenty c.c. of lead nitrate solution and
10 grams of sodium acetate were used; diluted to 200 c.c., heated to the
desired temperature, and titrated. The results were:—
Temperature 15° 30° 50° 100°
"Chromate" required 19.8 c.c. 19.5 c.c. 19.3 c.c. 19.2 c.c.
The first two of these filtered badly, the precipitate coming through the
filter; the last was very satisfactory in the working.
Effect of Varying Bulk.—Using 20 c.c. of lead nitrate, and 10 grams of
sodium acetate as before, diluting to the required bulk, heating to boiling,
and titrating, the results were:—
Bulk 100.0c.c. 200.0 c.c. 500.0c.c. 1000.0 c.c.
"Chromate" required 19.6 " 19.3 " 19.4 " 19.4 "
Effect of Varying Acetic Acid.—Since the experiments are carried out in
the presence of sodic acetate, acetic acid is the only acid whose effect need
be considered. Working as before, but with 200 c.c. bulk and varying
amounts of the acid, the results were:—
Acid present — 10.0c.c. 20.0c.c. 40.0c.c.
determination as was used in the precipitation.
In standardising the chromate solution, the standard lead nitrate solution is
used. A quantity containing about as much lead as the assay is supposed to
contain is measured off, rendered alkaline with dilute ammonia, and then
neutralised with acetic acid, using a small piece of litmus paper dropped
into the solution as indicator. Then dilute, boil, and titrate. When the lead in
the assay has been separated as sulphate and dissolved in sodic acetate, less
chromate is apparently required, and in this case it will be necessary to
precipitate the lead in the standard with an equivalent of sodic sulphate and
redissolve in sodic acetate just as in the assay. In these solutions (although
there is considerable chromate in excess) a further addition of 5 or 6 c.c. of
the chromate solution will cause a further precipitate. The following
experiments show the effect of variation in the conditions of the assay:—
Effect of Varying Temperature.—Twenty c.c. of lead nitrate solution and
10 grams of sodium acetate were used; diluted to 200 c.c., heated to the
desired temperature, and titrated. The results were:—
Temperature 15° 30° 50° 100°
"Chromate" required 19.8 c.c. 19.5 c.c. 19.3 c.c. 19.2 c.c.
The first two of these filtered badly, the precipitate coming through the
filter; the last was very satisfactory in the working.
Effect of Varying Bulk.—Using 20 c.c. of lead nitrate, and 10 grams of
sodium acetate as before, diluting to the required bulk, heating to boiling,
and titrating, the results were:—
Bulk 100.0c.c. 200.0 c.c. 500.0c.c. 1000.0 c.c.
"Chromate" required 19.6 " 19.3 " 19.4 " 19.4 "
Effect of Varying Acetic Acid.—Since the experiments are carried out in
the presence of sodic acetate, acetic acid is the only acid whose effect need
be considered. Working as before, but with 200 c.c. bulk and varying
amounts of the acid, the results were:—
Acid present — 10.0c.c. 20.0c.c. 40.0c.c.
Page 279
"Chromate" required 19.7 c.c. 19.1" 18.5" 17.3"
These experiments show that only slight quantities of acid are admissible.
Effect of Varying Sodium Acetate.—With the same conditions as before,
but with varying weights of sodium acetate, the results were:—
Sodium acetate present — 5 grams 10 grams 25 grams 50 grams
"Chromate" required 19.7 c.c. 19.6 c.c. 19.6 c.c. 18.8 c.c. 17.8 c.c.
These experiments show that excessive quantities of sodium acetate must
be avoided. Ammonium acetate interferes to a greater extent, and if both
acetic acid and this salt are present, each exerts its disturbing influence.
With 10 grams of ammonium acetate, 19.4 c.c. of the chromate solution
were required instead of 19.7 c.c. in the absence of this salt; with 10 grams
of the acetate and 10 c.c. of acetic acid, only 18.6 c.c. were required.
Effect of Foreign Salts.—As already stated, sulphates interfere. Twenty
c.c. of the lead nitrate solution were taken, precipitated with sulphate of
soda, and the precipitate dissolved in 10 grams of sodium acetate and
titrated as before. Duplicate experiments required 18.6 c.c. and 18.7 c.c. of
the chromate solution. A similar experiment with 40 c.c. of lead nitrate
required 37.4 c.c. of chromate. If the sulphate had not been present, the
results would have been 19.7 c.c. and 39.4 c.c. respectively.
Effect of Varying Lead.—In these experiments the conditions were as
before, but with varying amounts of lead.
Lead nitrate solution present 10.0 c.c. 20.0c.c. 50.0 c.c. 100.0c.c.
Chromate solution required. 9.4 " 19.7" 48.8 " 98.2 "
Determination of Lead in Galena.—Weigh up 1 gram of the powdered
and dried ore, and boil in an evaporating dish with 10 c.c. of dilute
hydrochloric acid. When the action becomes sluggish, dilute with an equal
bulk of water, and add a weighed piece of zinc rod about 1 inch long and
quarter-inch across. Keep up a moderate action by warming till the ore is
seen to be completely attacked and the lead precipitated. Decant off the
solution, wash once, strip off the lead, wash and weigh the remaining zinc.
Dissolve the lead in 5 c.c. of dilute nitric acid, and 5 c.c. of water with the
These experiments show that only slight quantities of acid are admissible.
Effect of Varying Sodium Acetate.—With the same conditions as before,
but with varying weights of sodium acetate, the results were:—
Sodium acetate present — 5 grams 10 grams 25 grams 50 grams
"Chromate" required 19.7 c.c. 19.6 c.c. 19.6 c.c. 18.8 c.c. 17.8 c.c.
These experiments show that excessive quantities of sodium acetate must
be avoided. Ammonium acetate interferes to a greater extent, and if both
acetic acid and this salt are present, each exerts its disturbing influence.
With 10 grams of ammonium acetate, 19.4 c.c. of the chromate solution
were required instead of 19.7 c.c. in the absence of this salt; with 10 grams
of the acetate and 10 c.c. of acetic acid, only 18.6 c.c. were required.
Effect of Foreign Salts.—As already stated, sulphates interfere. Twenty
c.c. of the lead nitrate solution were taken, precipitated with sulphate of
soda, and the precipitate dissolved in 10 grams of sodium acetate and
titrated as before. Duplicate experiments required 18.6 c.c. and 18.7 c.c. of
the chromate solution. A similar experiment with 40 c.c. of lead nitrate
required 37.4 c.c. of chromate. If the sulphate had not been present, the
results would have been 19.7 c.c. and 39.4 c.c. respectively.
Effect of Varying Lead.—In these experiments the conditions were as
before, but with varying amounts of lead.
Lead nitrate solution present 10.0 c.c. 20.0c.c. 50.0 c.c. 100.0c.c.
Chromate solution required. 9.4 " 19.7" 48.8 " 98.2 "
Determination of Lead in Galena.—Weigh up 1 gram of the powdered
and dried ore, and boil in an evaporating dish with 10 c.c. of dilute
hydrochloric acid. When the action becomes sluggish, dilute with an equal
bulk of water, and add a weighed piece of zinc rod about 1 inch long and
quarter-inch across. Keep up a moderate action by warming till the ore is
seen to be completely attacked and the lead precipitated. Decant off the
solution, wash once, strip off the lead, wash and weigh the remaining zinc.
Dissolve the lead in 5 c.c. of dilute nitric acid, and 5 c.c. of water with the
Page 280
aid of heat. Dilute and transfer to a pint flask; add a slight excess of dilute
ammonia, and render faintly acid with acetic acid. Dilute to 150 c.c., heat to
boiling, and run in the standard chromate in slight excess, noting the
amount required, and make up to 250 c.c. with water. Boil the solution,
allow to settle for a minute or so, filter off 50 c.c., and determine the excess
of chromate colorimetrically. As an example, 1 gram of an impure galena
was precipitated with 75 c.c. of standard chromate (100 c.c. = 1.020 gram
lead). The excess found in 50 c.c. was 0.3 c.c., which, multiplied by 5, gives
1.5 c.c. as the excess in the whole solution. The remaining 73.5 c.c. of
"chromate" required by the assay, are equivalent to 0.7497 gram of lead.
The zinc used up weighed 1.5 grams, and contained 0.0165 gram of lead.
Thus we get—
Lead in the assay 0.7497 gram
Lead from the zinc 0.0165 "
———
∴ Lead in the galena 0.7332 "
Equivalent to 73.3 per cent.
Another sample, in which the galena was accompanied with a large quantity
of pyrites, gave the following results:—Three grams were treated with 30
c.c. of dilute hydrochloric acid and a rod of zinc. The zinc and lead were
carefully transferred to another vessel, the zinc cleaned, and the lead
(dissolved in 5 c.c. of dilute nitric acid and 20 c.c. of water) treated as
before.
14.5 c.c. of the chromate were required = 0.1479 gram lead
Lead in 2 grams of zinc = 0.0220 "
———
∴ Lead in 3 grams of the ore = 0.1259 "
Equivalent to 4.20 per cent.
The same ore gave by separation of the lead with sulphuretted hydrogen,
and conversion into sulphate, 4.16 per cent.
ammonia, and render faintly acid with acetic acid. Dilute to 150 c.c., heat to
boiling, and run in the standard chromate in slight excess, noting the
amount required, and make up to 250 c.c. with water. Boil the solution,
allow to settle for a minute or so, filter off 50 c.c., and determine the excess
of chromate colorimetrically. As an example, 1 gram of an impure galena
was precipitated with 75 c.c. of standard chromate (100 c.c. = 1.020 gram
lead). The excess found in 50 c.c. was 0.3 c.c., which, multiplied by 5, gives
1.5 c.c. as the excess in the whole solution. The remaining 73.5 c.c. of
"chromate" required by the assay, are equivalent to 0.7497 gram of lead.
The zinc used up weighed 1.5 grams, and contained 0.0165 gram of lead.
Thus we get—
Lead in the assay 0.7497 gram
Lead from the zinc 0.0165 "
———
∴ Lead in the galena 0.7332 "
Equivalent to 73.3 per cent.
Another sample, in which the galena was accompanied with a large quantity
of pyrites, gave the following results:—Three grams were treated with 30
c.c. of dilute hydrochloric acid and a rod of zinc. The zinc and lead were
carefully transferred to another vessel, the zinc cleaned, and the lead
(dissolved in 5 c.c. of dilute nitric acid and 20 c.c. of water) treated as
before.
14.5 c.c. of the chromate were required = 0.1479 gram lead
Lead in 2 grams of zinc = 0.0220 "
———
∴ Lead in 3 grams of the ore = 0.1259 "
Equivalent to 4.20 per cent.
The same ore gave by separation of the lead with sulphuretted hydrogen,
and conversion into sulphate, 4.16 per cent.
Page 281
With fairly pure ores, free from sulphate, the assay may be made more
quickly as follows: Dissolve 1 gram of the finely powdered ore by boiling
gently with 40 c.c. of dilute hydrochloric acid for 15 minutes; cool; add a
few drops of permanganate; neutralise with ammonia, add acetic acid and a
little sodium acetate. Titrate with standard chromate.
COLORIMETRIC PROCESS.
This is based upon the brown coloration produced in very dilute solutions
of lead by the action of a solution of sulphuretted hydrogen. The quantity of
lead in the 50 c.c. of the assay solution must not much exceed 0.5
milligram, nor be less than 0.01. The sulphuretted hydrogen is used in the
form of a solution, and is not bubbled through the assay. The principle of
working is the same as previously described.
Standard Lead Solution.—Each c.c. of this should contain 0.1 milligram of
lead. It is made by diluting 10 c.c. of the solution of lead nitrate, described
under the volumetric process, to 1 litre.
Sulphuretted hydrogen water is made by passing a current of the washed
gas into water till the latter is saturated.
Five c.c. of the sulphuretted hydrogen water are put into a Nessler tube, the
measured portion of the assay solution added, and the whole diluted with
water to the 50 c.c. mark. Into the standard Nessler tube the same amount of
the sulphuretted hydrogen water is put, and diluted to nearly 50 c.c. The
standard lead solution is then run in till the tints are equal. The assay
solution must not contain much free acid, and if the conditions will allow it,
may with advantage be rendered alkaline with ammonia. The chief cause of
disturbance is the precipitation of lead sulphide forming a black turbid
solution instead of a brown clear one. This may be caused by using hot
solutions or an excess of acid. Other metals precipitable by sulphuretted
hydrogen must be absent as well as strong oxidising agents.
Effect of Varying Temperature.—The effect of increased temperature is to
change the colour from brown to black, and to render the estimation
difficult.
quickly as follows: Dissolve 1 gram of the finely powdered ore by boiling
gently with 40 c.c. of dilute hydrochloric acid for 15 minutes; cool; add a
few drops of permanganate; neutralise with ammonia, add acetic acid and a
little sodium acetate. Titrate with standard chromate.
COLORIMETRIC PROCESS.
This is based upon the brown coloration produced in very dilute solutions
of lead by the action of a solution of sulphuretted hydrogen. The quantity of
lead in the 50 c.c. of the assay solution must not much exceed 0.5
milligram, nor be less than 0.01. The sulphuretted hydrogen is used in the
form of a solution, and is not bubbled through the assay. The principle of
working is the same as previously described.
Standard Lead Solution.—Each c.c. of this should contain 0.1 milligram of
lead. It is made by diluting 10 c.c. of the solution of lead nitrate, described
under the volumetric process, to 1 litre.
Sulphuretted hydrogen water is made by passing a current of the washed
gas into water till the latter is saturated.
Five c.c. of the sulphuretted hydrogen water are put into a Nessler tube, the
measured portion of the assay solution added, and the whole diluted with
water to the 50 c.c. mark. Into the standard Nessler tube the same amount of
the sulphuretted hydrogen water is put, and diluted to nearly 50 c.c. The
standard lead solution is then run in till the tints are equal. The assay
solution must not contain much free acid, and if the conditions will allow it,
may with advantage be rendered alkaline with ammonia. The chief cause of
disturbance is the precipitation of lead sulphide forming a black turbid
solution instead of a brown clear one. This may be caused by using hot
solutions or an excess of acid. Other metals precipitable by sulphuretted
hydrogen must be absent as well as strong oxidising agents.
Effect of Varying Temperature.—The effect of increased temperature is to
change the colour from brown to black, and to render the estimation
difficult.
Page 282
1c.c. at 15° C. showed the colour of 0.5c.c. at 60° C.
2 " " " " 1.5 " at 60° C.
3 " " " " 5.0 " at 50° C.
Effect of Varying Time.—The colour becomes lighter on standing: 2 c.c.
on standing 10, 20, and 40 minutes became equal in colour to 1.7 c.c.
Effect of Acids and Ammonia.—Two c.c. of the solution with 2 c.c. of
dilute hydrochloric acid became cloudy and equivalent to about 2.5 c.c.;
and a similar result was got with 2 c.c. of dilute sulphuric acid. With 2 c.c.
of dilute ammonia the solution became somewhat darker, or equal to 2.3
c.c.; but gave a very clear solution easy to compare.
Determination of Lead in Commercial Zinc.—Dissolve 0.1 gram of the
metal in 1 c.c. of dilute nitric acid evaporates till a solid separates out, dilute
to 100 c.c. with water, and take 20 c.c. for assay. A sample treated in this
way required 2.4 c.c.; this multiplied by 5 gives 12.0 c.c., equivalent to 1.2
milligram of lead, or 1.2 per cent. By gravimetric assay the sample gave
1.10 per cent.
PRACTICAL EXERCISES.
1. Thirty grams of galena gave on dry assay 21 grams of lead; and this, on
cupellation, gave 15 milligrams of silver. Calculate the results in per cents.
of lead and in ounces of silver to the ton of ore.
2. How many ounces of silver to the ton would be contained in the lead got
from this ore if the loss in smelting is equal to that of the assay?
3. Having given you a sample of white lead freed from oil by washing with
ether, how would you proceed to determine the percentage of lead in it?
THALLIUM.
Thallium is a rare metal, found in small quantities in some varieties of iron
and copper pyrites, and in some lithia micas. It resembles lead in
appearance. Its compounds resemble the salts of the alkalies in some
respects; and, in others, those of the heavy metals.
2 " " " " 1.5 " at 60° C.
3 " " " " 5.0 " at 50° C.
Effect of Varying Time.—The colour becomes lighter on standing: 2 c.c.
on standing 10, 20, and 40 minutes became equal in colour to 1.7 c.c.
Effect of Acids and Ammonia.—Two c.c. of the solution with 2 c.c. of
dilute hydrochloric acid became cloudy and equivalent to about 2.5 c.c.;
and a similar result was got with 2 c.c. of dilute sulphuric acid. With 2 c.c.
of dilute ammonia the solution became somewhat darker, or equal to 2.3
c.c.; but gave a very clear solution easy to compare.
Determination of Lead in Commercial Zinc.—Dissolve 0.1 gram of the
metal in 1 c.c. of dilute nitric acid evaporates till a solid separates out, dilute
to 100 c.c. with water, and take 20 c.c. for assay. A sample treated in this
way required 2.4 c.c.; this multiplied by 5 gives 12.0 c.c., equivalent to 1.2
milligram of lead, or 1.2 per cent. By gravimetric assay the sample gave
1.10 per cent.
PRACTICAL EXERCISES.
1. Thirty grams of galena gave on dry assay 21 grams of lead; and this, on
cupellation, gave 15 milligrams of silver. Calculate the results in per cents.
of lead and in ounces of silver to the ton of ore.
2. How many ounces of silver to the ton would be contained in the lead got
from this ore if the loss in smelting is equal to that of the assay?
3. Having given you a sample of white lead freed from oil by washing with
ether, how would you proceed to determine the percentage of lead in it?
THALLIUM.
Thallium is a rare metal, found in small quantities in some varieties of iron
and copper pyrites, and in some lithia micas. It resembles lead in
appearance. Its compounds resemble the salts of the alkalies in some
respects; and, in others, those of the heavy metals.
Page 283
It is detected by the green colour which its salts impart to the flame. This,
when examined with the spectroscope, shows only one bright green line.
It is separated and estimated by dissolving in aqua regia; converting into
sulphate by evaporation with sulphuric acid; separating the second group of
metals with sulphuretted hydrogen in the acid solution, boiling off the
excess of the gas; nearly neutralising with carbonate of soda; and
precipitating the thallium with an excess of potassic iodide. On allowing the
liquid to stand for some time a bright yellow precipitate of thallous iodide
separates out. This is collected on a weighed filter; washed with cold water,
finishing off with alcohol; dried at 100° C., and weighed. The precipitate is
thallous iodide TlI, and contains 61.6 per cent. of thallium.
BISMUTH.
Bismuth is nearly always found in nature in the metallic state; but
occasionally it is met with as sulphide in bismuthine and as carbonate in
bismutite. It is also found in some comparatively rare minerals, such as
tetradymite, combined with tellurium, and associated with gold. In minute
quantities it is widely distributed: it is a common constituent of most copper
ores; hence it finds its way into refined copper, which is seldom free from
it. It is occasionally met with in silver in sufficient quantity to interfere with
the working qualities of that metal.
Bismuth compounds are used in medicine and in the manufacture of alloys.
Bismuth possesses many useful properties. It has considerable commercial
value, and sells at a high price.
The metal is brittle, breaks with a highly crystalline fracture, and has a
characteristic reddish-yellow colour. It is almost insoluble in hydrochloric,
but readily dissolves in nitric, acid; and gives, if the acid is in excess, a
clear solution. Bismuth salts have a strong tendency to separate out as
insoluble basic compounds; this is more especially true of the chloride
which, on diluting with a large volume of water, becomes milky; the whole
of the bismuth separating out. The nitrate, carbonate, and hydrate yield the
oxide (Bi2O3) on ignition. This oxide closely resembles litharge. It
combines with silica, forming fluid slags; and at a red heat is liquid enough
to be absorbed by a cupel; in fact, bismuth may take the place of lead in
when examined with the spectroscope, shows only one bright green line.
It is separated and estimated by dissolving in aqua regia; converting into
sulphate by evaporation with sulphuric acid; separating the second group of
metals with sulphuretted hydrogen in the acid solution, boiling off the
excess of the gas; nearly neutralising with carbonate of soda; and
precipitating the thallium with an excess of potassic iodide. On allowing the
liquid to stand for some time a bright yellow precipitate of thallous iodide
separates out. This is collected on a weighed filter; washed with cold water,
finishing off with alcohol; dried at 100° C., and weighed. The precipitate is
thallous iodide TlI, and contains 61.6 per cent. of thallium.
BISMUTH.
Bismuth is nearly always found in nature in the metallic state; but
occasionally it is met with as sulphide in bismuthine and as carbonate in
bismutite. It is also found in some comparatively rare minerals, such as
tetradymite, combined with tellurium, and associated with gold. In minute
quantities it is widely distributed: it is a common constituent of most copper
ores; hence it finds its way into refined copper, which is seldom free from
it. It is occasionally met with in silver in sufficient quantity to interfere with
the working qualities of that metal.
Bismuth compounds are used in medicine and in the manufacture of alloys.
Bismuth possesses many useful properties. It has considerable commercial
value, and sells at a high price.
The metal is brittle, breaks with a highly crystalline fracture, and has a
characteristic reddish-yellow colour. It is almost insoluble in hydrochloric,
but readily dissolves in nitric, acid; and gives, if the acid is in excess, a
clear solution. Bismuth salts have a strong tendency to separate out as
insoluble basic compounds; this is more especially true of the chloride
which, on diluting with a large volume of water, becomes milky; the whole
of the bismuth separating out. The nitrate, carbonate, and hydrate yield the
oxide (Bi2O3) on ignition. This oxide closely resembles litharge. It
combines with silica, forming fluid slags; and at a red heat is liquid enough
to be absorbed by a cupel; in fact, bismuth may take the place of lead in
Page 284
cupellation. The metal itself is easily fusible, and may be separated from its
ores by liquation.
The assay of bismuth by wet methods presents little difficulty, and is fairly
accurate. The price of the metal is such that only methods which yield good
results should be adopted; and, since bismuth is volatile at the temperature
of the furnace, and is found mixed with ores not easy to flux, as also with
metals which are not easily separated by the dry method, the dry assay can
only be considered as having a qualitative value.
DRY ASSAY.
By Liquation.—This is adapted to ores containing the bismuth as metal.
Take 20 grams of the powdered ore and place in a crucible with a perforated
bottom, put this crucible into another of about the same size and lute the
joint. Lute on a cover, place in the furnace and heat to redness. The bismuth
melts readily and drains into the lower crucible from which, when cold, it is
taken and weighed.
By Fusion.—For fairly pure ores the process is as follows:—Take 20 grams
of the ore and mix with 20 grams of fusion mixture, 10 grams of salt and 5
or 10 grams of potassium cyanide; place in a crucible, cover, and fuse at a
moderate temperature for about fifteen minutes; pour; when cold detach the
metal and weigh.
For coppery ores in which the metals are present as sulphides use the fluxes
just given with 2 grams of charcoal (instead of the cyanide) and a little
sulphur.
For coppery ores in which the metals are present as oxides, mix 20 grams of
the ore with 10 grams of fusion mixture, 4 grams of salt, 4 grams of sulphur
and 2 grams of charcoal; and fuse.
A considerable percentage of bismuth is lost in these assays; it is stated as
being nearly 8 per cent. of the metal present.
WET METHODS.
ores by liquation.
The assay of bismuth by wet methods presents little difficulty, and is fairly
accurate. The price of the metal is such that only methods which yield good
results should be adopted; and, since bismuth is volatile at the temperature
of the furnace, and is found mixed with ores not easy to flux, as also with
metals which are not easily separated by the dry method, the dry assay can
only be considered as having a qualitative value.
DRY ASSAY.
By Liquation.—This is adapted to ores containing the bismuth as metal.
Take 20 grams of the powdered ore and place in a crucible with a perforated
bottom, put this crucible into another of about the same size and lute the
joint. Lute on a cover, place in the furnace and heat to redness. The bismuth
melts readily and drains into the lower crucible from which, when cold, it is
taken and weighed.
By Fusion.—For fairly pure ores the process is as follows:—Take 20 grams
of the ore and mix with 20 grams of fusion mixture, 10 grams of salt and 5
or 10 grams of potassium cyanide; place in a crucible, cover, and fuse at a
moderate temperature for about fifteen minutes; pour; when cold detach the
metal and weigh.
For coppery ores in which the metals are present as sulphides use the fluxes
just given with 2 grams of charcoal (instead of the cyanide) and a little
sulphur.
For coppery ores in which the metals are present as oxides, mix 20 grams of
the ore with 10 grams of fusion mixture, 4 grams of salt, 4 grams of sulphur
and 2 grams of charcoal; and fuse.
A considerable percentage of bismuth is lost in these assays; it is stated as
being nearly 8 per cent. of the metal present.
WET METHODS.
Page 285
Detection.—Bismuth is detected by dissolving the substance in nitric or
hydrochloric acid and precipitating the diluted solution with sulphuretted
hydrogen. The precipitated sulphides, after digesting with soda and
washing, are dissolved in nitric acid and the solution boiled with
ammonium carbonate. The precipitate is washed and then warmed with
dilute sulphuric acid. The solution will contain the bismuth. Add a solution
of potassium iodide in excess, and boil; a yellow or dark brown solution
proves that bismuth is present. Another good test for small quantities of
bismuth is to add tartaric acid to the solution to be tested, and then to make
it alkaline with potash. Add a few c.c. of Schneider's liquid,[61] and heat. A
brownish-black colour is produced by as little as one part of bismuth in
200,000 of solution. The test is not applicable in the presence of mercury,
copper, or manganese.
Compounds of bismuth fused with cyanide of potassium in a Berlin crucible
readily give a globule of bismuth which is recognised by its appearance and
fracture.
Solution and Separation.—The solution of bismuth compounds presents
no difficulty. They are soluble in nitric acid or aqua regia, and, provided the
solution is sufficiently acid, they remain dissolved. In separating it from
other metals the solution is made up to about 100 c.c. and treated with a
current of sulphuretted hydrogen. The bismuth comes down in a tolerably
strong acid solution. The sulphide is decanted on to a filter and washed. It is
next digested with ammonic sulphide; or, better (especially when other
metals are present), dissolved in nitric acid, and treated with an excess of
ammonia and a current of sulphuretted hydrogen. The precipitate is filtered
off and evaporated to dryness with nitric acid. It is taken up with a few
drops of sulphuric acid and a little water; and warmed and filtered, if
necessary. The filtrate is nearly neutralised with ammonia; ammonium
carbonate added in slight excess; and the liquid heated to boiling and
filtered. The bismuth will be contained in the precipitate with perhaps traces
of lead, antimony, tin, or sometimes iron from incomplete separation or
washing. When only traces of a precipitate are got it must be tested. The
bismuth precipitate is readily soluble in dilute nitric acid.
GRAVIMETRIC DETERMINATION.
hydrochloric acid and precipitating the diluted solution with sulphuretted
hydrogen. The precipitated sulphides, after digesting with soda and
washing, are dissolved in nitric acid and the solution boiled with
ammonium carbonate. The precipitate is washed and then warmed with
dilute sulphuric acid. The solution will contain the bismuth. Add a solution
of potassium iodide in excess, and boil; a yellow or dark brown solution
proves that bismuth is present. Another good test for small quantities of
bismuth is to add tartaric acid to the solution to be tested, and then to make
it alkaline with potash. Add a few c.c. of Schneider's liquid,[61] and heat. A
brownish-black colour is produced by as little as one part of bismuth in
200,000 of solution. The test is not applicable in the presence of mercury,
copper, or manganese.
Compounds of bismuth fused with cyanide of potassium in a Berlin crucible
readily give a globule of bismuth which is recognised by its appearance and
fracture.
Solution and Separation.—The solution of bismuth compounds presents
no difficulty. They are soluble in nitric acid or aqua regia, and, provided the
solution is sufficiently acid, they remain dissolved. In separating it from
other metals the solution is made up to about 100 c.c. and treated with a
current of sulphuretted hydrogen. The bismuth comes down in a tolerably
strong acid solution. The sulphide is decanted on to a filter and washed. It is
next digested with ammonic sulphide; or, better (especially when other
metals are present), dissolved in nitric acid, and treated with an excess of
ammonia and a current of sulphuretted hydrogen. The precipitate is filtered
off and evaporated to dryness with nitric acid. It is taken up with a few
drops of sulphuric acid and a little water; and warmed and filtered, if
necessary. The filtrate is nearly neutralised with ammonia; ammonium
carbonate added in slight excess; and the liquid heated to boiling and
filtered. The bismuth will be contained in the precipitate with perhaps traces
of lead, antimony, tin, or sometimes iron from incomplete separation or
washing. When only traces of a precipitate are got it must be tested. The
bismuth precipitate is readily soluble in dilute nitric acid.
GRAVIMETRIC DETERMINATION.
Page 286
The bismuth having been separated and dissolved in nitric acid[62] is
precipitated (after dilution) by the addition of carbonate of ammonium in
slight excess, and boiling. The precipitate is filtered off, washed with hot
water, dried, ignited, and weighed. The ignition should be performed
carefully at not above a low red heat. The oxide which is formed has, at this
temperature, a dark yellow or brown colour, and becomes yellow on
cooling. It is bismuthic oxide (Bi2O3) and contains 89.65 per cent. of
bismuth. Fusion with potassium cyanide at a temperature just sufficient to
melt the salt reduces it to the metal which falls to the bottom and runs into a
globule. The button of metal may be weighed, but it often sticks tenaciously
to the bottom of the crucible. The precipitation with ammonic carbonate
must not be made in a sulphate or chloride solution; since basic compounds
would then be thrown down, and the result on weighing would either be too
low (because of the volatilisation of the chloride), or too high (because of
the retention of sulphuric acid).
Bismuth compounds in a nitric acid solution are readily decomposed by the
electric current, but the deposited bismuth is not coherent. It comes down in
shaggy tufts which are difficult to wash and easy to oxidise.
VOLUMETRIC ASSAY.
There are two methods which have been proposed; one based on the
precipitation as chromate and the estimation of the chromic acid; and the
other on the precipitation as oxalate and subsequent titration with
permanganate of potash. These offer little advantage over the easy
gravimetric determination.
COLORIMETRIC METHOD.
Bismuth iodide dissolves in excess of potassium iodide, forming a yellow-
coloured solution, indistinguishable in colour from that given by iodine.
The colour, however, is not removed by boiling or by sulphurous acid.
Since none of the commoner metals give such a colour, and free iodine is
easily separated by boiling, this method is specially suited for small
determinations of bismuth.
precipitated (after dilution) by the addition of carbonate of ammonium in
slight excess, and boiling. The precipitate is filtered off, washed with hot
water, dried, ignited, and weighed. The ignition should be performed
carefully at not above a low red heat. The oxide which is formed has, at this
temperature, a dark yellow or brown colour, and becomes yellow on
cooling. It is bismuthic oxide (Bi2O3) and contains 89.65 per cent. of
bismuth. Fusion with potassium cyanide at a temperature just sufficient to
melt the salt reduces it to the metal which falls to the bottom and runs into a
globule. The button of metal may be weighed, but it often sticks tenaciously
to the bottom of the crucible. The precipitation with ammonic carbonate
must not be made in a sulphate or chloride solution; since basic compounds
would then be thrown down, and the result on weighing would either be too
low (because of the volatilisation of the chloride), or too high (because of
the retention of sulphuric acid).
Bismuth compounds in a nitric acid solution are readily decomposed by the
electric current, but the deposited bismuth is not coherent. It comes down in
shaggy tufts which are difficult to wash and easy to oxidise.
VOLUMETRIC ASSAY.
There are two methods which have been proposed; one based on the
precipitation as chromate and the estimation of the chromic acid; and the
other on the precipitation as oxalate and subsequent titration with
permanganate of potash. These offer little advantage over the easy
gravimetric determination.
COLORIMETRIC METHOD.
Bismuth iodide dissolves in excess of potassium iodide, forming a yellow-
coloured solution, indistinguishable in colour from that given by iodine.
The colour, however, is not removed by boiling or by sulphurous acid.
Since none of the commoner metals give such a colour, and free iodine is
easily separated by boiling, this method is specially suited for small
determinations of bismuth.
Page 287
It requires a solution of bismuth, made by dissolving 0.1 gram of bismuth in
a drop or so of nitric acid, evaporating with a little sulphuric acid and
diluting with water to 1 litre. 1 c.c. will contain 0.1 milligram of bismuth.
And a solution of sulphurous acid, made by diluting 10 c.c. of the
commercial acid to 1 litre with water.
The determination is made in the usual way: 50 c.c. of the prepared
solution, which should not carry more than 0.75 milligram nor less than
0.01 milligram of bismuth, are placed in a Nessler tube and the colour
compared with that observed in a similar tube containing water and
potassium iodide on adding the standard solution of bismuth.
The assay solution is prepared by separating the bismuth with sulphuretted
hydrogen, boiling the precipitate with nitric acid, and evaporating with
sulphuric acid. Take up with water, add 10 or 20 c.c. of solution of
potassium iodide, boil off any iodine liberated, dilute, filter, and make up to
100 c.c. According to the depth of colour take 10, 20, or 50 c.c. and transfer
to the Nessler tube. Add a few c.c. of the solution of sulphurous acid. Into
the other Nessler tube put as much potassium iodide solution as is contained
in the assay tube, with sulphurous acid and water to within a few c.c. of the
bulk. Then add the standard bismuth solution till the tints are equal.
The student must be careful not to confuse the colour of the bismuth iodide
with that of free iodine. If the yellow colour is removed by boiling and
returns on standing it is due altogether to iodine; if it is lessened by the
addition of a few drops of the dilute sulphurous acid, it is in part due to it.
Hence the necessity of having a little free sulphurous acid in each tube. A
strong solution must not be used, since it liberates iodine from potassium
iodide.
The following experiments illustrate the effect of variation in the conditions
of the assay:—
Effect of Varying Temperature.—At a higher temperature the colour is
somewhat lessened.
1.0 c.c. at 15° C. showed the colour of 0.8 c.c. at 70° C.
2.5 " " " 2.0 "
5.0 " " " 5.0 "
a drop or so of nitric acid, evaporating with a little sulphuric acid and
diluting with water to 1 litre. 1 c.c. will contain 0.1 milligram of bismuth.
And a solution of sulphurous acid, made by diluting 10 c.c. of the
commercial acid to 1 litre with water.
The determination is made in the usual way: 50 c.c. of the prepared
solution, which should not carry more than 0.75 milligram nor less than
0.01 milligram of bismuth, are placed in a Nessler tube and the colour
compared with that observed in a similar tube containing water and
potassium iodide on adding the standard solution of bismuth.
The assay solution is prepared by separating the bismuth with sulphuretted
hydrogen, boiling the precipitate with nitric acid, and evaporating with
sulphuric acid. Take up with water, add 10 or 20 c.c. of solution of
potassium iodide, boil off any iodine liberated, dilute, filter, and make up to
100 c.c. According to the depth of colour take 10, 20, or 50 c.c. and transfer
to the Nessler tube. Add a few c.c. of the solution of sulphurous acid. Into
the other Nessler tube put as much potassium iodide solution as is contained
in the assay tube, with sulphurous acid and water to within a few c.c. of the
bulk. Then add the standard bismuth solution till the tints are equal.
The student must be careful not to confuse the colour of the bismuth iodide
with that of free iodine. If the yellow colour is removed by boiling and
returns on standing it is due altogether to iodine; if it is lessened by the
addition of a few drops of the dilute sulphurous acid, it is in part due to it.
Hence the necessity of having a little free sulphurous acid in each tube. A
strong solution must not be used, since it liberates iodine from potassium
iodide.
The following experiments illustrate the effect of variation in the conditions
of the assay:—
Effect of Varying Temperature.—At a higher temperature the colour is
somewhat lessened.
1.0 c.c. at 15° C. showed the colour of 0.8 c.c. at 70° C.
2.5 " " " 2.0 "
5.0 " " " 5.0 "
Page 288
Effect of Free Acid.—
2.5c.c. with 5 c.c. of nitric acid equalled 2.5 c.c.
5.0 " " sulphuric acid " 5.0 "
Hydrochloric acid almost completely removes the colour, which, however,
is restored by the addition of a few crystals of potassium iodide.
Effect of Alkalies.—Ammonia, soda, or potash destroys the colour, but it is
restored on acidifying with nitric or sulphuric acid.
Effect of Ammonic Salts.—The following table shows the results after
addition of ammonic salts:—
C.c. With 10 grams With 10 grams With 10 grams
present. Ammonic Nitrate. Ammonic Sulphate. Ammonic Chloride.
1.0 c.c. 0.9 c.c. 1.1 c.c. —
2.5 " 2.5 " 2.7 " —
5.0 " 5.0 " 5.5 " —
Ammonic chloride, like hydrochloric acid, removes the colour, which may
be restored on the addition of more potassium iodide. Nitrates and sulphates
do not thus interfere.
Effect of Foreign Salts.—Sodic hyposulphite almost completely removes
the colour. Copper salts liberate iodine; but when this has been removed by
boiling and the cuprous iodide has been filtered off there is no further
interference. Dilute solutions of lead salts give no colour.
PRACTICAL EXERCISES.
1. A fusible alloy is made up of 8 parts of bismuth, 5 of lead, and 3 of tin.
What weight of oxide of bismuth, Bi2O3, would you get on the analysis of 1
gram of it?
2. What weight of bismuth can be got from 2 grams of the subnitrate
BiONO3.H2O?
2.5c.c. with 5 c.c. of nitric acid equalled 2.5 c.c.
5.0 " " sulphuric acid " 5.0 "
Hydrochloric acid almost completely removes the colour, which, however,
is restored by the addition of a few crystals of potassium iodide.
Effect of Alkalies.—Ammonia, soda, or potash destroys the colour, but it is
restored on acidifying with nitric or sulphuric acid.
Effect of Ammonic Salts.—The following table shows the results after
addition of ammonic salts:—
C.c. With 10 grams With 10 grams With 10 grams
present. Ammonic Nitrate. Ammonic Sulphate. Ammonic Chloride.
1.0 c.c. 0.9 c.c. 1.1 c.c. —
2.5 " 2.5 " 2.7 " —
5.0 " 5.0 " 5.5 " —
Ammonic chloride, like hydrochloric acid, removes the colour, which may
be restored on the addition of more potassium iodide. Nitrates and sulphates
do not thus interfere.
Effect of Foreign Salts.—Sodic hyposulphite almost completely removes
the colour. Copper salts liberate iodine; but when this has been removed by
boiling and the cuprous iodide has been filtered off there is no further
interference. Dilute solutions of lead salts give no colour.
PRACTICAL EXERCISES.
1. A fusible alloy is made up of 8 parts of bismuth, 5 of lead, and 3 of tin.
What weight of oxide of bismuth, Bi2O3, would you get on the analysis of 1
gram of it?
2. What weight of bismuth can be got from 2 grams of the subnitrate
BiONO3.H2O?
Page 289
3. How would you detect and separate arsenic, lead, and copper in a sample
of bismuth?
ANTIMONY.
Antimony occurs in the native state, but is rare; its common ore is
antimonite, the sulphide (Sb2S3). Jamesonite and other sulphides of lead
and antimony are frequently met with. Sulphide of antimony is also a
constituent of fahlerz and of many silver ores.
Antimonite occurs generally in fibrous masses, has a lead-like metallic
lustre, is easily cut with a knife, and melts in the flame of a candle.
Antimony itself has a very crystalline fracture, is brittle, and has a bluish-
white colour. It is used in the preparation of alloys with lead and tin for the
manufacture of type-metal. It is readily fusible, and imparts hardness and
the property of taking a sharp cast to its alloys. It is practically insoluble in
hydrochloric acid. On boiling with strong nitric acid it is converted into
antimonic oxide (Sb2O5), which is a powder almost insoluble in this acid or
in water, but which may be got into solution with difficulty by the
prolonged action of hydrochloric and tartaric acids. Antimonic oxide is
converted on ignition into the tetroxide (Sb2O4) with loss of oxygen.
Antimony forms two series of salts, antimonious and antimonic; and
advantage is taken of this in its determination volumetrically. Either
sulphide of antimony yields antimonious chloride on boiling with
hydrochloric acid, sulphuretted hydrogen being given off; and, in the case
of antimonic sulphide, sulphur is deposited. Antimonious is converted into
antimonic chloride by treatment with permanganate of potash in an acid
solution. Antimonic chloride and potassium iodide react, forming
antimonious chloride and free iodine. This latter may be got rid of by
boiling. Sulphide of antimony is separated from the ore by liquation; this
regulus is met with in commerce as "crude antimony."
DRY ASSAY.
An approximate determination of the amount of sulphide of antimony in an
ore may be made by fusing and liquating in a luted double crucible in the
of bismuth?
ANTIMONY.
Antimony occurs in the native state, but is rare; its common ore is
antimonite, the sulphide (Sb2S3). Jamesonite and other sulphides of lead
and antimony are frequently met with. Sulphide of antimony is also a
constituent of fahlerz and of many silver ores.
Antimonite occurs generally in fibrous masses, has a lead-like metallic
lustre, is easily cut with a knife, and melts in the flame of a candle.
Antimony itself has a very crystalline fracture, is brittle, and has a bluish-
white colour. It is used in the preparation of alloys with lead and tin for the
manufacture of type-metal. It is readily fusible, and imparts hardness and
the property of taking a sharp cast to its alloys. It is practically insoluble in
hydrochloric acid. On boiling with strong nitric acid it is converted into
antimonic oxide (Sb2O5), which is a powder almost insoluble in this acid or
in water, but which may be got into solution with difficulty by the
prolonged action of hydrochloric and tartaric acids. Antimonic oxide is
converted on ignition into the tetroxide (Sb2O4) with loss of oxygen.
Antimony forms two series of salts, antimonious and antimonic; and
advantage is taken of this in its determination volumetrically. Either
sulphide of antimony yields antimonious chloride on boiling with
hydrochloric acid, sulphuretted hydrogen being given off; and, in the case
of antimonic sulphide, sulphur is deposited. Antimonious is converted into
antimonic chloride by treatment with permanganate of potash in an acid
solution. Antimonic chloride and potassium iodide react, forming
antimonious chloride and free iodine. This latter may be got rid of by
boiling. Sulphide of antimony is separated from the ore by liquation; this
regulus is met with in commerce as "crude antimony."
DRY ASSAY.
An approximate determination of the amount of sulphide of antimony in an
ore may be made by fusing and liquating in a luted double crucible in the
Page 290
manner described under bismuth. This is unsatisfactory. The determination
of metallic antimony in an ore is made either by fusion with potassium
cyanide or by fusion with iron, as in the galena assay. Both methods yield
poor results; and, where iron is used, it must be added in quantity only
sufficient for desulphurising; this amounts to about 40 per cent. in pure
ores. If the iron is in excess it alloys with the reduced antimony. If, on the
other hand, it is insufficient, the metal will contain sulphur; or sulphide of
antimony will be lost in the slag.
The following note, for which we are indebted to Mr. Bedford McNeill,
A.R.S.M., gives a description of the method adopted in the commercial
valuation of a parcel of antimony ore:—
The antimony smelter, when he wishes to determine the value of any parcel
of ore—usually the sulphide—that may be offered for sale, practically has
recourse to the smelting operation. That is, a quantity of 2 or 3 cwts. taken
by his sampler having been obtained, he treats it under the immediate
supervision of the foreman smelter as if it formed part of the ore in process
of daily reduction at his works. He thus determines by actual trial the output
which it may fairly be anticipated will be yielded by the bulk, and upon the
result of this trial or assay, and the knowledge gained of the actual
behaviour of the ore under treatment, he bases his tender, knowing that,
should he secure the parcel, he may confidently expect a similar return.
Briefly, the process consists of the three ordinary operations of—
(a) Singling or removing most of the antimony from the ore;
(b) Doubling;
(c) Refining or "starring."
But in the assay sufficient information is generally given by the first two of
these.
A new pot having been taken and made hot in the furnace, 40 or 45 lbs. of
the ore is weighed in (the mineral from the necessities of sampling not
exceeding walnut size); 1 to 3 lbs. of salt cake is now added to render the
separation of the resulting sulphide of iron more easy, as also to assist in the
fusion of the gangue; 20 to 25 lbs. of tin-plate scrap, beaten more or less
into ball shape, is weighed, placed on the top of the ore and salt cake, and
of metallic antimony in an ore is made either by fusion with potassium
cyanide or by fusion with iron, as in the galena assay. Both methods yield
poor results; and, where iron is used, it must be added in quantity only
sufficient for desulphurising; this amounts to about 40 per cent. in pure
ores. If the iron is in excess it alloys with the reduced antimony. If, on the
other hand, it is insufficient, the metal will contain sulphur; or sulphide of
antimony will be lost in the slag.
The following note, for which we are indebted to Mr. Bedford McNeill,
A.R.S.M., gives a description of the method adopted in the commercial
valuation of a parcel of antimony ore:—
The antimony smelter, when he wishes to determine the value of any parcel
of ore—usually the sulphide—that may be offered for sale, practically has
recourse to the smelting operation. That is, a quantity of 2 or 3 cwts. taken
by his sampler having been obtained, he treats it under the immediate
supervision of the foreman smelter as if it formed part of the ore in process
of daily reduction at his works. He thus determines by actual trial the output
which it may fairly be anticipated will be yielded by the bulk, and upon the
result of this trial or assay, and the knowledge gained of the actual
behaviour of the ore under treatment, he bases his tender, knowing that,
should he secure the parcel, he may confidently expect a similar return.
Briefly, the process consists of the three ordinary operations of—
(a) Singling or removing most of the antimony from the ore;
(b) Doubling;
(c) Refining or "starring."
But in the assay sufficient information is generally given by the first two of
these.
A new pot having been taken and made hot in the furnace, 40 or 45 lbs. of
the ore is weighed in (the mineral from the necessities of sampling not
exceeding walnut size); 1 to 3 lbs. of salt cake is now added to render the
separation of the resulting sulphide of iron more easy, as also to assist in the
fusion of the gangue; 20 to 25 lbs. of tin-plate scrap, beaten more or less
into ball shape, is weighed, placed on the top of the ore and salt cake, and
Page 291
the whole brought to a state of fusion. The foreman from time to time takes
notice of the behaviour of the ore under the working conditions. Ores that
manifest a tendency to "boil" or "froth " require the admixture of other
more sluggish mineral in order to render their reduction economically
practicable.
After 1-1/4 to 1-1/2 hours (the time depending mainly on the temperature),
the contents of the crucible are usually in a state of tranquil fusion. The pot
is now lifted from the fire, and its contents transferred to a conical iron
mould, the empty pot being immediately put back into the fire, and the
latter "mended" with sufficient coke for another run. The conical mould
(when dealing with a "strange" ore, and the possibility of insufficient iron
being present to satisfy the sulphur contents) is wiped inside with clay
previous to pouring in the molten charge. Otherwise the mould itself will be
attacked, and the contents after solidifying will require to be chiselled out
piecemeal.
A further 40 lbs. of the ore is now charged into the crucible with iron as
above; but before this second charge is ready to be drawn an inspection of
the first may suggest the addition of either 3 or 5 lbs. more iron, or 5 or 10
lbs. more ore.
It is a good fault rather to aim at an excess of iron as tending to clean the
ore from antimony, any of the latter that (from an insufficiency of iron) may
be left in the slag from the first process being irretrievably lost; whereas, if
the iron be in excess, that which is combined with the crude antimony
resulting from the first process is easily got rid of by adding 3 to 5 lbs. or so
of ore in the second process.
This latter, as practised for the determination of the value of a parcel of ore,
consists in selecting two of the best quality singles, resulting from perhaps
four or five trials as above, and running them down with a few pounds of
salt cake, or a mixture of salt cake with American potash, and (as is
generally necessary) a small addition of ore.
Upon the final result (confirmed perhaps on another pair of singles, and,
judging from the total weight or output of the metal as calculated from the
ore used in "singling," plus any added in the "doubling," the crystalline
notice of the behaviour of the ore under the working conditions. Ores that
manifest a tendency to "boil" or "froth " require the admixture of other
more sluggish mineral in order to render their reduction economically
practicable.
After 1-1/4 to 1-1/2 hours (the time depending mainly on the temperature),
the contents of the crucible are usually in a state of tranquil fusion. The pot
is now lifted from the fire, and its contents transferred to a conical iron
mould, the empty pot being immediately put back into the fire, and the
latter "mended" with sufficient coke for another run. The conical mould
(when dealing with a "strange" ore, and the possibility of insufficient iron
being present to satisfy the sulphur contents) is wiped inside with clay
previous to pouring in the molten charge. Otherwise the mould itself will be
attacked, and the contents after solidifying will require to be chiselled out
piecemeal.
A further 40 lbs. of the ore is now charged into the crucible with iron as
above; but before this second charge is ready to be drawn an inspection of
the first may suggest the addition of either 3 or 5 lbs. more iron, or 5 or 10
lbs. more ore.
It is a good fault rather to aim at an excess of iron as tending to clean the
ore from antimony, any of the latter that (from an insufficiency of iron) may
be left in the slag from the first process being irretrievably lost; whereas, if
the iron be in excess, that which is combined with the crude antimony
resulting from the first process is easily got rid of by adding 3 to 5 lbs. or so
of ore in the second process.
This latter, as practised for the determination of the value of a parcel of ore,
consists in selecting two of the best quality singles, resulting from perhaps
four or five trials as above, and running them down with a few pounds of
salt cake, or a mixture of salt cake with American potash, and (as is
generally necessary) a small addition of ore.
Upon the final result (confirmed perhaps on another pair of singles, and,
judging from the total weight or output of the metal as calculated from the
ore used in "singling," plus any added in the "doubling," the crystalline
Page 292
fracture and face of the metal, its colour, etc.) the price to be offered for the
parcel of ore is fixed.
WET METHODS.
Detection.—The antimony, if any, being got into solution by treating the
ore with hydrochloric acid or aqua regia may be detected by evaporating
with hydrochloric acid, diluting, and filtering into the cover of a platinum
crucible or (better) a platinum dish. A small lump of zinc is then added, and,
if antimony is present, the dish will in a minute or so be stained black with a
deposit of metallic antimony. This stain is removed by nitric, but not by
hydrochloric, acid. The reaction is delicate and characteristic; arsenic under
like conditions is evolved as arseniuretted hydrogen, and tin is deposited as
metal on the zinc.
Solution.—Ores, &c., containing antimony are best opened up by boiling
with hydrochloric acid or aqua regia; treatment with nitric acid should be
avoided wherever possible, since it forms antimonic acid, which is
subsequently dissolved only with difficulty. Salts of antimony in solution
have a tendency to form insoluble basic salts; so that care must be exercised
in diluting. Compounds such as antimonite which are soluble in
hydrochloric should be dissolved at once in that acid.
Separation.—To the solution add potash in excess and a little free sulphur,
and pass a current of sulphuretted hydrogen for some minutes; allow to
digest for an hour or so on a hot plate; filter; and wash the residue.
Acidulate the filtrate with hydrochloric acid: the precipitate will contain the
antimony (as Sb2S5), and possibly arsenic or tin. The precipitate is
transferred to a beaker and boiled with hydrochloric acid; the solution is
filtered off and diluted. Add a few crystals of tartaric acid, and pass a
current of sulphuretted hydrogen for some time. The first flocculent
precipitate will become denser, and render the filtering more easy. Transfer
the precipitate (after washing free from chlorides) to a Berlin dish, and treat
cautiously with fuming nitric acid. The action of this acid on the sulphide is
very violent. Evaporate and ignite, transfer to a silver dish, and fuse with
four or five times its weight of caustic soda, cool and extract with a little
water, then add an equal volume of alcohol, and allow to stand overnight.
parcel of ore is fixed.
WET METHODS.
Detection.—The antimony, if any, being got into solution by treating the
ore with hydrochloric acid or aqua regia may be detected by evaporating
with hydrochloric acid, diluting, and filtering into the cover of a platinum
crucible or (better) a platinum dish. A small lump of zinc is then added, and,
if antimony is present, the dish will in a minute or so be stained black with a
deposit of metallic antimony. This stain is removed by nitric, but not by
hydrochloric, acid. The reaction is delicate and characteristic; arsenic under
like conditions is evolved as arseniuretted hydrogen, and tin is deposited as
metal on the zinc.
Solution.—Ores, &c., containing antimony are best opened up by boiling
with hydrochloric acid or aqua regia; treatment with nitric acid should be
avoided wherever possible, since it forms antimonic acid, which is
subsequently dissolved only with difficulty. Salts of antimony in solution
have a tendency to form insoluble basic salts; so that care must be exercised
in diluting. Compounds such as antimonite which are soluble in
hydrochloric should be dissolved at once in that acid.
Separation.—To the solution add potash in excess and a little free sulphur,
and pass a current of sulphuretted hydrogen for some minutes; allow to
digest for an hour or so on a hot plate; filter; and wash the residue.
Acidulate the filtrate with hydrochloric acid: the precipitate will contain the
antimony (as Sb2S5), and possibly arsenic or tin. The precipitate is
transferred to a beaker and boiled with hydrochloric acid; the solution is
filtered off and diluted. Add a few crystals of tartaric acid, and pass a
current of sulphuretted hydrogen for some time. The first flocculent
precipitate will become denser, and render the filtering more easy. Transfer
the precipitate (after washing free from chlorides) to a Berlin dish, and treat
cautiously with fuming nitric acid. The action of this acid on the sulphide is
very violent. Evaporate and ignite, transfer to a silver dish, and fuse with
four or five times its weight of caustic soda, cool and extract with a little
water, then add an equal volume of alcohol, and allow to stand overnight.
Page 293
Filter, wash with dilute alcohol. (The filtrate will contain the tin.) The
residue contains the antimony as antimonate of soda, and is dissolved off
the filter with hot dilute hydrochloric, with the help of a little tartaric, acid.
The filtrate is now ready for the gravimetric determination.
GRAVIMETRIC ASSAY.
Pass a current of sulphuretted hydrogen through the solution containing the
antimony to which a little tartaric acid has been previously added. Pass the
gas till the precipitate becomes dense, and the antimony is all down. The
solution must not be too strongly acid. Filter off the precipitate, wash with
hot water, dry in the water oven, transfer to a weighed porcelain dish, and
cautiously treat with fuming nitric acid. Continue the action on the water
bath till the sulphur and antimony are completely oxidised. Evaporate;
ignite, gently at first, then strongly over the blast; cool, and weigh. The
residue is a white infusible powder, and consists of antimony tetroxide,
Sb2O4, containing 78.94 per cent. of the metal.
Determination of Antimony as Bigallate.—What appears to be a very
good method has been worked out by M.A. Guyard, and is described in
Crookes' Select Methods, p. 398.
The antimony must be in solution as antimonious chloride, and must not be
accompanied by an excess of hydrochloric acid. To ensure these conditions,
the solution is treated with potassium iodide until no more iodine is
evolved, and is then evaporated to remove the excess of hydrochloric acid.
To the concentrated, and nearly neutral, solution a freshly-prepared solution
of gallic acid is added in slight excess. A bulky white precipitate is formed
that settles rapidly. The solution is diluted with hot water and washed by
decantation. Then the precipitate is collected on a weighed double filter,
washed once or twice with hot water, and dried at 100° C. The dried
substance is antimony bigallate, and contains 40.85 per cent. of antimony. It
should be completely soluble in ammonium sulphide. The solution in which
the antimony is precipitated need not be quite free from other metals.
VOLUMETRIC METHOD.
residue contains the antimony as antimonate of soda, and is dissolved off
the filter with hot dilute hydrochloric, with the help of a little tartaric, acid.
The filtrate is now ready for the gravimetric determination.
GRAVIMETRIC ASSAY.
Pass a current of sulphuretted hydrogen through the solution containing the
antimony to which a little tartaric acid has been previously added. Pass the
gas till the precipitate becomes dense, and the antimony is all down. The
solution must not be too strongly acid. Filter off the precipitate, wash with
hot water, dry in the water oven, transfer to a weighed porcelain dish, and
cautiously treat with fuming nitric acid. Continue the action on the water
bath till the sulphur and antimony are completely oxidised. Evaporate;
ignite, gently at first, then strongly over the blast; cool, and weigh. The
residue is a white infusible powder, and consists of antimony tetroxide,
Sb2O4, containing 78.94 per cent. of the metal.
Determination of Antimony as Bigallate.—What appears to be a very
good method has been worked out by M.A. Guyard, and is described in
Crookes' Select Methods, p. 398.
The antimony must be in solution as antimonious chloride, and must not be
accompanied by an excess of hydrochloric acid. To ensure these conditions,
the solution is treated with potassium iodide until no more iodine is
evolved, and is then evaporated to remove the excess of hydrochloric acid.
To the concentrated, and nearly neutral, solution a freshly-prepared solution
of gallic acid is added in slight excess. A bulky white precipitate is formed
that settles rapidly. The solution is diluted with hot water and washed by
decantation. Then the precipitate is collected on a weighed double filter,
washed once or twice with hot water, and dried at 100° C. The dried
substance is antimony bigallate, and contains 40.85 per cent. of antimony. It
should be completely soluble in ammonium sulphide. The solution in which
the antimony is precipitated need not be quite free from other metals.
VOLUMETRIC METHOD.
Page 294
This is based on the reduction of antimonic chloride (SbCl5) to antimonious
(SbCl3) by the action of potassium iodide in strong hydrochloric acid
solution.[63] Iodine is at the same time liberated, and the amount of
antimony reduced is got at by titrating with sodium hyposulphite, which
measures the iodine set free.
The standard solution of sodium hyposulphite is made by dissolving 41.32
grams of the salt (Na2S2O3.5H2O) in water, and diluting to 1 litre. One
hundred c.c. will be equivalent to about 1 gram of antimony.
It is standardised with the help of a solution of antimony made as follows:
—Weigh up 5 grams of powdered antimony, transfer to a flask, and cover
with 50 c.c. of hydrochloric acid; boil, and add nitric acid (5 or 10 drops at
a time) until the metal is dissolved. Allow the action of the nitric acid to
cease before adding more. Boil down to a small bulk, add 250 c.c. of
hydrochloric acid, and dilute to nearly 1 litre. Warm until any precipitate
which has formed is redissolved; allow to cool slowly, and run in from a
pipette a weak solution of permanganate until a faint brown colour is
produced. Dilute to exactly 1 litre; 100 c.c. contain 0.5 gram of antimony as
antimonic chloride.
In standardising, take 50 c.c. of the antimony solution, and transfer to a
flask; add 2 grams of potassium iodide crystals, and when dissolved, after
standing a few minutes, run in the solution of "hypo" from an ordinary
burette until the greater part of the iodine has been reduced. Add a few
drops of starch solution, and continue the addition of the "hypo" until the
muddy-green colour changes to a clear brownish-yellow. The solution must
be shaken after each addition of the "hypo."
In determining antimony in ore, weigh up 0.5 to 1 gram, and dissolve in
hydrochloric acid with, if necessary, the help of chlorate of potash. The
antimony is separated as sulphide, redissolved in hydrochloric acid, and
oxidised with a crystal of chlorate of potash. Chlorine is boiled off, and the
solution diluted with an equal bulk of water. To the clear cold solution
potassium iodide is added, and after a few minutes the liberated iodine is
titrated with "hypo," as already described. The method only yields
satisfactory results when the standard and assay are carried out alike.
(SbCl3) by the action of potassium iodide in strong hydrochloric acid
solution.[63] Iodine is at the same time liberated, and the amount of
antimony reduced is got at by titrating with sodium hyposulphite, which
measures the iodine set free.
The standard solution of sodium hyposulphite is made by dissolving 41.32
grams of the salt (Na2S2O3.5H2O) in water, and diluting to 1 litre. One
hundred c.c. will be equivalent to about 1 gram of antimony.
It is standardised with the help of a solution of antimony made as follows:
—Weigh up 5 grams of powdered antimony, transfer to a flask, and cover
with 50 c.c. of hydrochloric acid; boil, and add nitric acid (5 or 10 drops at
a time) until the metal is dissolved. Allow the action of the nitric acid to
cease before adding more. Boil down to a small bulk, add 250 c.c. of
hydrochloric acid, and dilute to nearly 1 litre. Warm until any precipitate
which has formed is redissolved; allow to cool slowly, and run in from a
pipette a weak solution of permanganate until a faint brown colour is
produced. Dilute to exactly 1 litre; 100 c.c. contain 0.5 gram of antimony as
antimonic chloride.
In standardising, take 50 c.c. of the antimony solution, and transfer to a
flask; add 2 grams of potassium iodide crystals, and when dissolved, after
standing a few minutes, run in the solution of "hypo" from an ordinary
burette until the greater part of the iodine has been reduced. Add a few
drops of starch solution, and continue the addition of the "hypo" until the
muddy-green colour changes to a clear brownish-yellow. The solution must
be shaken after each addition of the "hypo."
In determining antimony in ore, weigh up 0.5 to 1 gram, and dissolve in
hydrochloric acid with, if necessary, the help of chlorate of potash. The
antimony is separated as sulphide, redissolved in hydrochloric acid, and
oxidised with a crystal of chlorate of potash. Chlorine is boiled off, and the
solution diluted with an equal bulk of water. To the clear cold solution
potassium iodide is added, and after a few minutes the liberated iodine is
titrated with "hypo," as already described. The method only yields
satisfactory results when the standard and assay are carried out alike.
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FOOTNOTES:
[50] "Modern American Methods of Copper Smelting" (Dr. Peters).
[51] "Journal of the Society of Chemical Industry," vol. v. No. 2.
[52] Lead when present is precipitated on the spiral in the form of a dark powder
of dioxide (PbO2). Manganese is also thrown down on the spiral as dioxide
(MnO2), the solution at the same time becomes violet from the formation of
permanganic acid.
[53] See the method given under Examination of Commercial Copper.
[54] CuSO4 + 4KCy = 2KCy.CuCy2 + K2SO4.
[55] 2CuSO4 + 3KCy + Am2O = Cu2Cy2 + Am2SO4 + K2SO4 + KCyO.
[56] 2CuSO4 + 4KI = Cn2I2 + 2I + 2K2SO4.
[57] 2Na2S2O3 + 2I = 2NaI + Na2S4O6.
[58] For further information, see Appendix B., and a paper by J.W.
Westmoreland, Journal of the Society of Chemical Industry, vol. v. p. 48.
[59]
3Cu2O + 6AgNO3 + 3H2O
= 2Cu2H3O3NO3 + 2Cu(NO3)2 + 6Ag.
(Insoluble basic salt.)
[60] K2CrO4 + Pb(NO3)2 = PbCrO4 + 2KNO3
[61] Made by dissolving 12 grams of tartaric acid and 4 grams of stannous
chloride in water, and adding potash solution till it is alkaline. The solution
should remain clear on heating to 60° or 70° C.
[62] It must be remembered that arsenate of bismuth is completely insoluble in
this acid.
[63] SbCl5 + 2KI = I2 + SbCl3 + 2KCl.
[50] "Modern American Methods of Copper Smelting" (Dr. Peters).
[51] "Journal of the Society of Chemical Industry," vol. v. No. 2.
[52] Lead when present is precipitated on the spiral in the form of a dark powder
of dioxide (PbO2). Manganese is also thrown down on the spiral as dioxide
(MnO2), the solution at the same time becomes violet from the formation of
permanganic acid.
[53] See the method given under Examination of Commercial Copper.
[54] CuSO4 + 4KCy = 2KCy.CuCy2 + K2SO4.
[55] 2CuSO4 + 3KCy + Am2O = Cu2Cy2 + Am2SO4 + K2SO4 + KCyO.
[56] 2CuSO4 + 4KI = Cn2I2 + 2I + 2K2SO4.
[57] 2Na2S2O3 + 2I = 2NaI + Na2S4O6.
[58] For further information, see Appendix B., and a paper by J.W.
Westmoreland, Journal of the Society of Chemical Industry, vol. v. p. 48.
[59]
3Cu2O + 6AgNO3 + 3H2O
= 2Cu2H3O3NO3 + 2Cu(NO3)2 + 6Ag.
(Insoluble basic salt.)
[60] K2CrO4 + Pb(NO3)2 = PbCrO4 + 2KNO3
[61] Made by dissolving 12 grams of tartaric acid and 4 grams of stannous
chloride in water, and adding potash solution till it is alkaline. The solution
should remain clear on heating to 60° or 70° C.
[62] It must be remembered that arsenate of bismuth is completely insoluble in
this acid.
[63] SbCl5 + 2KI = I2 + SbCl3 + 2KCl.
Page 296
CHAPTER XI.
IRON—NICKEL—COBALT—ZINC—CADMIUM.
IRON.
Iron rusts or oxidises very readily, and, consequently, is rarely found in the
metallic state in nature; such native iron as is found being generally of
meteoric origin or imbedded in basalt and other igneous rocks. It chiefly
occurs as oxide, as in magnetite, hæmatite, and in the brown iron ores and
ochres. Chalybite, which is carbonate of iron, is an ore of great importance.
Iron is found combined with sulphur in pyrrhotine and pyrites, and together
with arsenic in mispickel. It is a common constituent of most rocks,
imparting to them a green, black, or brown colour; and is present, either as
an essential part or as an impurity, in most substances.
The chemistry of iron is somewhat complicated by the existence of two
oxides, each of which gives rise to a well-marked series of compounds.
Those derived from the lower oxide, known as ferrous salts, are generally
pale and greenish. Ferric salts are derived from the higher oxide, and are
generally red, brown, or yellow. The existence of these two well-marked
families of salts renders the assay of iron comparatively easy, for the
quantity of iron present in a solution can be readily measured by the amount
of oxidising or reducing agent required to convert it from the one state into
the other—that is, from ferrous to ferric, or from ferric to ferrous, as the
case may be.
In the red and brown iron ores and ochres ferric iron is present; in chalybite
the iron is in the ferrous state; and in magnetite it is present in both forms.
Traces of iron in the ferrous state may be found (even in the presence of
much ferric iron) by either of the following tests:—
1. Ferricyanide of potassium gives a blue precipitate or green
coloration; with ferric salts a brown colour only is produced.
IRON—NICKEL—COBALT—ZINC—CADMIUM.
IRON.
Iron rusts or oxidises very readily, and, consequently, is rarely found in the
metallic state in nature; such native iron as is found being generally of
meteoric origin or imbedded in basalt and other igneous rocks. It chiefly
occurs as oxide, as in magnetite, hæmatite, and in the brown iron ores and
ochres. Chalybite, which is carbonate of iron, is an ore of great importance.
Iron is found combined with sulphur in pyrrhotine and pyrites, and together
with arsenic in mispickel. It is a common constituent of most rocks,
imparting to them a green, black, or brown colour; and is present, either as
an essential part or as an impurity, in most substances.
The chemistry of iron is somewhat complicated by the existence of two
oxides, each of which gives rise to a well-marked series of compounds.
Those derived from the lower oxide, known as ferrous salts, are generally
pale and greenish. Ferric salts are derived from the higher oxide, and are
generally red, brown, or yellow. The existence of these two well-marked
families of salts renders the assay of iron comparatively easy, for the
quantity of iron present in a solution can be readily measured by the amount
of oxidising or reducing agent required to convert it from the one state into
the other—that is, from ferrous to ferric, or from ferric to ferrous, as the
case may be.
In the red and brown iron ores and ochres ferric iron is present; in chalybite
the iron is in the ferrous state; and in magnetite it is present in both forms.
Traces of iron in the ferrous state may be found (even in the presence of
much ferric iron) by either of the following tests:—
1. Ferricyanide of potassium gives a blue precipitate or green
coloration; with ferric salts a brown colour only is produced.
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2. A solution of permanganate of potassium is decolorised by a
ferrous salt, but not by a ferric one.
Traces of ferric iron can be detected (even in the presence of much ferrous
iron) by the following tests:—
(1) By the brown or yellow colour of the solution, especially
when hot.
(2) By giving a pink or red coloration with sulphocyanide of
potassium.
Substances containing oxide of iron yield the whole of the iron as metal
when fused at a high temperature with charcoal and suitable fluxes. The
metal, however, will contain varying proportions of carbon and other
impurities, and its weight can only afford a rough knowledge of the
proportion of the metal in the ore. There are two or three methods of dry
assay for iron, but they are not only inexact, but more troublesome than the
wet methods, and need not be further considered. Chalybite and the
hydrated oxides dissolve very readily in hydrochloric acid; hæmatite and
magnetite dissolve with rather more difficulty. Iron itself, when soft, is
easily soluble in dilute hydrochloric, or sulphuric, acid. Pyrites, mispickel,
&c., are insoluble in hydrochloric acid, but they are readily attacked by
nitric acid. Certain minerals, such as chrome iron ore, titaniferous iron ore,
and some silicates containing iron, remain in the residue insoluble in acids.
Some of these yield their iron when attacked with strong sulphuric acid, or
when fused with the acid sulphate of potash. Generally, however, it is better
in such stubborn cases to fuse with carbonate of soda, and then attack the
"melt" with hydrochloric acid.
When nitric acid, or the fusion method, has been used, the metal will be in
solution in the ferric state, no matter in what condition it existed in the ore.
But with dilute hydrochloric or sulphuric acid it will retain its former
degree of oxidation. Hydrochloric acid, for example, with chalybite (ferrous
carbonate) will give a solution of ferrous chloride; with hæmatite (ferric
oxide) it will yield ferric chloride; and with magnetite (ferrous and ferric
oxides) a mixture of ferrous and ferric chlorides. Metallic iron yields
solutions of ferrous salts. It is convenient to speak of the iron in a ferrous
salt as ferrous iron, and when in the ferric state as ferric iron. Frequently it
ferrous salt, but not by a ferric one.
Traces of ferric iron can be detected (even in the presence of much ferrous
iron) by the following tests:—
(1) By the brown or yellow colour of the solution, especially
when hot.
(2) By giving a pink or red coloration with sulphocyanide of
potassium.
Substances containing oxide of iron yield the whole of the iron as metal
when fused at a high temperature with charcoal and suitable fluxes. The
metal, however, will contain varying proportions of carbon and other
impurities, and its weight can only afford a rough knowledge of the
proportion of the metal in the ore. There are two or three methods of dry
assay for iron, but they are not only inexact, but more troublesome than the
wet methods, and need not be further considered. Chalybite and the
hydrated oxides dissolve very readily in hydrochloric acid; hæmatite and
magnetite dissolve with rather more difficulty. Iron itself, when soft, is
easily soluble in dilute hydrochloric, or sulphuric, acid. Pyrites, mispickel,
&c., are insoluble in hydrochloric acid, but they are readily attacked by
nitric acid. Certain minerals, such as chrome iron ore, titaniferous iron ore,
and some silicates containing iron, remain in the residue insoluble in acids.
Some of these yield their iron when attacked with strong sulphuric acid, or
when fused with the acid sulphate of potash. Generally, however, it is better
in such stubborn cases to fuse with carbonate of soda, and then attack the
"melt" with hydrochloric acid.
When nitric acid, or the fusion method, has been used, the metal will be in
solution in the ferric state, no matter in what condition it existed in the ore.
But with dilute hydrochloric or sulphuric acid it will retain its former
degree of oxidation. Hydrochloric acid, for example, with chalybite (ferrous
carbonate) will give a solution of ferrous chloride; with hæmatite (ferric
oxide) it will yield ferric chloride; and with magnetite (ferrous and ferric
oxides) a mixture of ferrous and ferric chlorides. Metallic iron yields
solutions of ferrous salts. It is convenient to speak of the iron in a ferrous
salt as ferrous iron, and when in the ferric state as ferric iron. Frequently it
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is required to determine how much of the iron exists in an ore in each
condition. In such cases it is necessary to keep off the air whilst dissolving;
the operation should, therefore, be performed in an atmosphere of carbonic
acid.
Separation.—The separation of the iron from the other substances is as
follows:—Silica is removed by evaporating the acid solution, and taking up
with acid, as described under Silica; the whole of the iron will be in
solution. The metals of Groups I. and II. are removed by passing
sulphuretted hydrogen, and at the same time the iron will be reduced to the
ferrous state. The solution should be filtered into a 16 oz. flask, boiled to
get rid of the gas, and treated (whilst boiling) with a few drops of nitric
acid, in order to convert the whole of the iron into the ferric state. When this
condition is arrived at, an additional drop of nitric acid causes no dark
coloration. The boiling must be continued to remove nitrous fumes. Next
add caustic soda solution until the colour of the solution changes from
yellow to red. The solution must be free from a precipitate; if the soda be
incautiously added a permanent precipitate will be formed, in which case it
must be redissolved with hydrochloric acid, and soda again, but more
cautiously, added. After cooling, a solution of sodium acetate is added until
the colour of the solution is no longer darkened. The solution, diluted to
two-thirds of the flaskful with water, is heated to boiling. Long-continued
boiling must be avoided. The precipitate is filtered quickly through a large
filter, and washed with hot water containing a little acetate of soda.
The precipitate will contain all the iron and may also contain alumina,
chromium, titanium, as well as phosphoric, and, perhaps, arsenic acids.[64]
Dissolve the precipitate off the filter with dilute sulphuric acid, avoiding
excess, add tartaric acid and then ammonia in excess. Pass sulphuretted
hydrogen, warm, and allow the precipitate to settle. Filter and wash with
water containing a little ammonic sulphide.
GRAVIMETRIC METHOD.
Dissolve the precipitate in dilute hydrochloric acid; peroxidise with a few
drops of nitric acid and boil, dilute to about 200 c.c., add ammonia (with
constant stirring) till the liquid smells of it, and heat to boiling. Wash as
condition. In such cases it is necessary to keep off the air whilst dissolving;
the operation should, therefore, be performed in an atmosphere of carbonic
acid.
Separation.—The separation of the iron from the other substances is as
follows:—Silica is removed by evaporating the acid solution, and taking up
with acid, as described under Silica; the whole of the iron will be in
solution. The metals of Groups I. and II. are removed by passing
sulphuretted hydrogen, and at the same time the iron will be reduced to the
ferrous state. The solution should be filtered into a 16 oz. flask, boiled to
get rid of the gas, and treated (whilst boiling) with a few drops of nitric
acid, in order to convert the whole of the iron into the ferric state. When this
condition is arrived at, an additional drop of nitric acid causes no dark
coloration. The boiling must be continued to remove nitrous fumes. Next
add caustic soda solution until the colour of the solution changes from
yellow to red. The solution must be free from a precipitate; if the soda be
incautiously added a permanent precipitate will be formed, in which case it
must be redissolved with hydrochloric acid, and soda again, but more
cautiously, added. After cooling, a solution of sodium acetate is added until
the colour of the solution is no longer darkened. The solution, diluted to
two-thirds of the flaskful with water, is heated to boiling. Long-continued
boiling must be avoided. The precipitate is filtered quickly through a large
filter, and washed with hot water containing a little acetate of soda.
The precipitate will contain all the iron and may also contain alumina,
chromium, titanium, as well as phosphoric, and, perhaps, arsenic acids.[64]
Dissolve the precipitate off the filter with dilute sulphuric acid, avoiding
excess, add tartaric acid and then ammonia in excess. Pass sulphuretted
hydrogen, warm, and allow the precipitate to settle. Filter and wash with
water containing a little ammonic sulphide.
GRAVIMETRIC METHOD.
Dissolve the precipitate in dilute hydrochloric acid; peroxidise with a few
drops of nitric acid and boil, dilute to about 200 c.c., add ammonia (with
constant stirring) till the liquid smells of it, and heat to boiling. Wash as
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much as possible by decantation with hot water. Transfer to the filter, and
wash till the filtrate gives no indication of soluble salts coming through.
The filtrate must be colourless and clear. The wet precipitate is very bulky,
of a dark-brown colour and readily soluble in dilute acids, but insoluble in
ammonia and dilute alkalies. When thrown down from a solution containing
other metals it is very apt to carry portions of these with it, even when they
are by themselves very soluble in ammoniacal solutions. It must be dried
and ignited, the filter paper being burnt separately and its ash added. When
further ignition ceases to cause a loss of weight, the residue is ferric oxide
(Fe2O3), which contains 70 per cent. of iron. The weight of iron therefore
can be calculated by multiplying the weight of oxide obtained by 0.7.
The presence of ammonic chloride causes loss of iron during the ignition,
and organic matter causes an apparent loss by reducing the iron to a lower
state of oxidation. When the iron in the solution much exceeds 0.2 gram the
volumetric determination is generally adopted, as the bulkiness of the
precipitate of ferric hydrate makes the gravimetric method very
inconvenient.
VOLUMETRIC METHODS.
As already explained these are based on the measurement of the volume of
a reagent required to bring the whole of the iron from the ferrous to the
ferric state (oxidation), or from the ferric to the ferrous (reduction). Ferrous
compounds are converted into ferric by the action of an oxidising agent in
the presence of an acid. Either permanganate or bichromate of potash is
generally used for this purpose.[65]
Ferric compounds are reduced to ferrous by the action of:—
(1) Stannous chloride;
(2) Sulphuretted hydrogen;
(3) Sodium sulphite; or
(4) Zinc.[66]
The processes, then, may be divided into two kinds, one based on oxidation
and the other on reduction. In each case the titration must be preceded by an
wash till the filtrate gives no indication of soluble salts coming through.
The filtrate must be colourless and clear. The wet precipitate is very bulky,
of a dark-brown colour and readily soluble in dilute acids, but insoluble in
ammonia and dilute alkalies. When thrown down from a solution containing
other metals it is very apt to carry portions of these with it, even when they
are by themselves very soluble in ammoniacal solutions. It must be dried
and ignited, the filter paper being burnt separately and its ash added. When
further ignition ceases to cause a loss of weight, the residue is ferric oxide
(Fe2O3), which contains 70 per cent. of iron. The weight of iron therefore
can be calculated by multiplying the weight of oxide obtained by 0.7.
The presence of ammonic chloride causes loss of iron during the ignition,
and organic matter causes an apparent loss by reducing the iron to a lower
state of oxidation. When the iron in the solution much exceeds 0.2 gram the
volumetric determination is generally adopted, as the bulkiness of the
precipitate of ferric hydrate makes the gravimetric method very
inconvenient.
VOLUMETRIC METHODS.
As already explained these are based on the measurement of the volume of
a reagent required to bring the whole of the iron from the ferrous to the
ferric state (oxidation), or from the ferric to the ferrous (reduction). Ferrous
compounds are converted into ferric by the action of an oxidising agent in
the presence of an acid. Either permanganate or bichromate of potash is
generally used for this purpose.[65]
Ferric compounds are reduced to ferrous by the action of:—
(1) Stannous chloride;
(2) Sulphuretted hydrogen;
(3) Sodium sulphite; or
(4) Zinc.[66]
The processes, then, may be divided into two kinds, one based on oxidation
and the other on reduction. In each case the titration must be preceded by an
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exact preparation of the solution to be assayed in order that the iron may be
in the right state of oxidation.
PERMANGANATE AND BICHROMATE METHODS.
These consist of three operations:—
(1) Solution of the ore;
(2) Reduction of the iron to the ferrous state; and
(3) Titration.
Solution.—The only point to be noticed concerning the first operation (in
addition to those already mentioned) is that nitric acid must be absent. If
nitric acid has been used, evaporate to dryness, of course without previous
dilution; add hydrochloric or sulphuric acid, and boil for five or ten
minutes. Dilute with water to about 100 c.c., and warm until solution is
complete.
The reduction is performed by either of the following methods:—
1. With Stannous Chloride.—Fill a burette with a solution of stannous
chloride,[67] and cautiously run the liquid into the hot assay solution (in
which the iron is present as chloride) until the colour is discharged. A large
excess of the stannous chloride must be avoided. Then add 5 c.c. of a 2-1/2
per cent. solution of mercuric chloride, this will cause a white precipitate
(or a grey one if too large an excess of the stannous chloride has been
added). Boil till the solution clears, cool, dilute, and titrate.
2. With Sulphuretted Hydrogen.—Cool the solution and pass through it a
current of washed sulphuretted hydrogen till the liquid smells strongly of
the gas after withdrawal and shaking. A white precipitate of sulphur will be
formed, this will not interfere with the subsequent titration provided it is
precipitated in the cold. If, however, the precipitate is coloured (showing
the presence of the second group metals), or if the precipitation has been
carried out in a hot solution, it should be filtered off. Boil the solution until
the sulphuretted hydrogen is driven off; this may be tested by holding a
strip of filter paper dipped in lead acetate solution in the steam issuing from
the flask. The presence of sulphuretted hydrogen should be looked for
in the right state of oxidation.
PERMANGANATE AND BICHROMATE METHODS.
These consist of three operations:—
(1) Solution of the ore;
(2) Reduction of the iron to the ferrous state; and
(3) Titration.
Solution.—The only point to be noticed concerning the first operation (in
addition to those already mentioned) is that nitric acid must be absent. If
nitric acid has been used, evaporate to dryness, of course without previous
dilution; add hydrochloric or sulphuric acid, and boil for five or ten
minutes. Dilute with water to about 100 c.c., and warm until solution is
complete.
The reduction is performed by either of the following methods:—
1. With Stannous Chloride.—Fill a burette with a solution of stannous
chloride,[67] and cautiously run the liquid into the hot assay solution (in
which the iron is present as chloride) until the colour is discharged. A large
excess of the stannous chloride must be avoided. Then add 5 c.c. of a 2-1/2
per cent. solution of mercuric chloride, this will cause a white precipitate
(or a grey one if too large an excess of the stannous chloride has been
added). Boil till the solution clears, cool, dilute, and titrate.
2. With Sulphuretted Hydrogen.—Cool the solution and pass through it a
current of washed sulphuretted hydrogen till the liquid smells strongly of
the gas after withdrawal and shaking. A white precipitate of sulphur will be
formed, this will not interfere with the subsequent titration provided it is
precipitated in the cold. If, however, the precipitate is coloured (showing
the presence of the second group metals), or if the precipitation has been
carried out in a hot solution, it should be filtered off. Boil the solution until
the sulphuretted hydrogen is driven off; this may be tested by holding a
strip of filter paper dipped in lead acetate solution in the steam issuing from
the flask. The presence of sulphuretted hydrogen should be looked for
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rather than its absence. It is well to continue the boiling for a few minutes
after the gas has been driven off. Cool and titrate.
3. With Sodium Sulphite.—Add ammonia (a few drops at a time) until the
precipitate first formed redissolves with difficulty. If a permanent
precipitate is formed, redissolve with a few drops of acid. To the warm
solution add from 2 to 3 grams of sodium sulphite crystals. The solution
will become strongly coloured, but the colour will fade away on standing
for a few minutes in a warm place. When the colour is quite removed, add
20 c.c. of dilute sulphuric acid, and boil until the steam is quite free from
the odour of sulphurous acid. Cool and titrate.
4. With Zinc.—Add about 10 grams of granulated zinc; if the hydrogen
comes off violently add water; if, on the other hand, the action is very slow,
add sufficient dilute sulphuric acid to keep up a brisk effervescence. The
reduction is hastened by warming, and is complete when the solution is
quite colourless and a drop of the liquid tested with sulphocyanate of
potassium gives no reaction for ferric iron. Filter through "glass wool" or
quick filtering paper. The zinc should be still giving off gas rapidly,
indicating a freely acid solution; if not, acid must be added. Wash with
water rendered acid. Cool and titrate.
With regard to the relative advantages of the different methods they may be
roughly summed up as follows:—The stannous chloride method has the
advantage of immediately reducing the ferric iron whether in hot or cold
solution and under varied conditions in regard to acidity, but has the
disadvantage of similarly reducing salts of copper and antimony, which, in a
subsequent titration, count as iron. Moreover, there is no convenient method
of eliminating any large excess of the reagent that may have been used; and,
consequently, it either leaves too much to the judgment of the operator, or
entails as much care as a titration. Students generally get good results by
this method.
The sulphuretted hydrogen method also has the advantage of quick
reduction under varying conditions, and the further one of adding nothing
objectionable to the solution; in fact it removes certain impurities. The
disadvantages are the necessity for boiling off the excess of the gas, and of
filtering off the precipitated sulphur, although this last is not necessary if
after the gas has been driven off. Cool and titrate.
3. With Sodium Sulphite.—Add ammonia (a few drops at a time) until the
precipitate first formed redissolves with difficulty. If a permanent
precipitate is formed, redissolve with a few drops of acid. To the warm
solution add from 2 to 3 grams of sodium sulphite crystals. The solution
will become strongly coloured, but the colour will fade away on standing
for a few minutes in a warm place. When the colour is quite removed, add
20 c.c. of dilute sulphuric acid, and boil until the steam is quite free from
the odour of sulphurous acid. Cool and titrate.
4. With Zinc.—Add about 10 grams of granulated zinc; if the hydrogen
comes off violently add water; if, on the other hand, the action is very slow,
add sufficient dilute sulphuric acid to keep up a brisk effervescence. The
reduction is hastened by warming, and is complete when the solution is
quite colourless and a drop of the liquid tested with sulphocyanate of
potassium gives no reaction for ferric iron. Filter through "glass wool" or
quick filtering paper. The zinc should be still giving off gas rapidly,
indicating a freely acid solution; if not, acid must be added. Wash with
water rendered acid. Cool and titrate.
With regard to the relative advantages of the different methods they may be
roughly summed up as follows:—The stannous chloride method has the
advantage of immediately reducing the ferric iron whether in hot or cold
solution and under varied conditions in regard to acidity, but has the
disadvantage of similarly reducing salts of copper and antimony, which, in a
subsequent titration, count as iron. Moreover, there is no convenient method
of eliminating any large excess of the reagent that may have been used; and,
consequently, it either leaves too much to the judgment of the operator, or
entails as much care as a titration. Students generally get good results by
this method.
The sulphuretted hydrogen method also has the advantage of quick
reduction under varying conditions, and the further one of adding nothing
objectionable to the solution; in fact it removes certain impurities. The
disadvantages are the necessity for boiling off the excess of the gas, and of
filtering off the precipitated sulphur, although this last is not necessary if
Page 302
precipitated cold. The tendency with students is to get high results. The
sodium sulphite method has the advantages of being clean and neat, and of
requiring no nitration. On the other hand it requires practice in obtaining the
best conditions for complete reduction; and, as with sulphuretted hydrogen,
there is the necessity for boiling off the gas, while there is no simple and
delicate test for the residual sulphurous acid. In addition, if an excess of
sodium sulphite has been used and enough acid not subsequently added, the
excess will count as iron. Students generally get low results by this method.
The advantages of the zinc method are, that it is easily worked and that the
excess of zinc is readily removed by simply filtering. The disadvantages are
the slowness[68] with which the last portions of ferric iron are reduced, the
danger of loss by effervescence, the precipitation of basic salts, and,
perhaps, of iron, and the loading of the solution with salts of zinc, which in
the titration with bichromate have a prejudicial effect. The tendency in the
hands of students is to get variable results, sometimes low and sometimes
high.
Generally speaking, the sulphuretted hydrogen and sodium sulphite
methods are to be preferred. Carefully worked each method will yield good
results.
The titration may be done with a standard solution of (1) permanganate of
potash, or (2) bichromate of potash.
1. With Permanganate of Potash.—Prepare a standard solution by
dissolving 2.82 grams of the salt and diluting to one litre. The strength of
this should be 100 c.c. = 0.5 gram of iron, but it varies slightly, and should
be determined (and afterwards checked every two or three weeks) by
weighing up 0.2 gram of iron wire, dissolving in 10 c.c. of dilute sulphuric
acid, diluting to about 100 c.c., and titrating.
The standard solution must be put in a burette with a glass stopcock, as it
attacks india-rubber. The assay should be contained in a pint flask, and be
cooled before titrating. The standard solution must be run in until a pinkish
tinge permeates the whole solution; this must be taken as the finishing
point. When certain interfering bodies are present this colour quickly fades,
but the fading must be ignored. With pure solutions the colour is fairly
sodium sulphite method has the advantages of being clean and neat, and of
requiring no nitration. On the other hand it requires practice in obtaining the
best conditions for complete reduction; and, as with sulphuretted hydrogen,
there is the necessity for boiling off the gas, while there is no simple and
delicate test for the residual sulphurous acid. In addition, if an excess of
sodium sulphite has been used and enough acid not subsequently added, the
excess will count as iron. Students generally get low results by this method.
The advantages of the zinc method are, that it is easily worked and that the
excess of zinc is readily removed by simply filtering. The disadvantages are
the slowness[68] with which the last portions of ferric iron are reduced, the
danger of loss by effervescence, the precipitation of basic salts, and,
perhaps, of iron, and the loading of the solution with salts of zinc, which in
the titration with bichromate have a prejudicial effect. The tendency in the
hands of students is to get variable results, sometimes low and sometimes
high.
Generally speaking, the sulphuretted hydrogen and sodium sulphite
methods are to be preferred. Carefully worked each method will yield good
results.
The titration may be done with a standard solution of (1) permanganate of
potash, or (2) bichromate of potash.
1. With Permanganate of Potash.—Prepare a standard solution by
dissolving 2.82 grams of the salt and diluting to one litre. The strength of
this should be 100 c.c. = 0.5 gram of iron, but it varies slightly, and should
be determined (and afterwards checked every two or three weeks) by
weighing up 0.2 gram of iron wire, dissolving in 10 c.c. of dilute sulphuric
acid, diluting to about 100 c.c., and titrating.
The standard solution must be put in a burette with a glass stopcock, as it
attacks india-rubber. The assay should be contained in a pint flask, and be
cooled before titrating. The standard solution must be run in until a pinkish
tinge permeates the whole solution; this must be taken as the finishing
point. When certain interfering bodies are present this colour quickly fades,
but the fading must be ignored. With pure solutions the colour is fairly
Page 303
permanent, and a single drop of the potassium permanganate solution is
sufficient to determine the finishing point.
2. With Bichromate of Potash.—Prepare a standard solution by dissolving
4.39 grams of the powdered and dried salt in water, and diluting to 1 litre.
This solution is permanent, its strength is determined by dissolving 0.2
gram of iron wire in 10 c.c. of dilute sulphuric acid, diluting to about a
quarter of a litre, and titrating.
Also prepare a test solution by dissolving 0.1 gram of ferricyanide of
potassium in 100 c.c. of water. This solution does not keep well and must be
freshly prepared.
An ordinary burette is used. The assay is best contained in a glazed
earthenware dish, and may be titrated hot or cold. To determine the
finishing point, place a series of drops of the ferricyanide solution on a dry
white glazed plate. The drops should be of about the same size and be
placed in lines at fairly equal distances. The bichromate is run in, in a
steady stream, the assay solution being continuously stirred until the
reaction is sensibly slackened. Then bring a drop of the assay with the
stirrer in contact with one of the test drops on the plate. The standard can be
safely run in 1 c.c. at a time, so long as the test drop shows signs of a
precipitate. When only a coloration is produced run in cautiously a few
drops at a time so long as two drops of the assay gives with the test a colour
which is even faintly greener than two drops of the assay solution placed
alongside. The finishing point is decided and practically permanent,
although it demands a little practice to recognise it. The titration with
permanganate of potassium has the advantage of a more distinct finishing
point and easier mode of working; its application, however, is somewhat
limited by the disturbing effects of hydrochloric acid. The bichromate
method has the advantage of a standard solution which does not alter in
strength, and the further one of being but little affected by altering
conditions of assay. Hydrochloric acid has practically no effect on it. Both
methods give accurate results and are good examples of volumetric
methods.
The following results illustrate the extent to which the methods may be
relied on; and the influence which the various conditions of experiment
sufficient to determine the finishing point.
2. With Bichromate of Potash.—Prepare a standard solution by dissolving
4.39 grams of the powdered and dried salt in water, and diluting to 1 litre.
This solution is permanent, its strength is determined by dissolving 0.2
gram of iron wire in 10 c.c. of dilute sulphuric acid, diluting to about a
quarter of a litre, and titrating.
Also prepare a test solution by dissolving 0.1 gram of ferricyanide of
potassium in 100 c.c. of water. This solution does not keep well and must be
freshly prepared.
An ordinary burette is used. The assay is best contained in a glazed
earthenware dish, and may be titrated hot or cold. To determine the
finishing point, place a series of drops of the ferricyanide solution on a dry
white glazed plate. The drops should be of about the same size and be
placed in lines at fairly equal distances. The bichromate is run in, in a
steady stream, the assay solution being continuously stirred until the
reaction is sensibly slackened. Then bring a drop of the assay with the
stirrer in contact with one of the test drops on the plate. The standard can be
safely run in 1 c.c. at a time, so long as the test drop shows signs of a
precipitate. When only a coloration is produced run in cautiously a few
drops at a time so long as two drops of the assay gives with the test a colour
which is even faintly greener than two drops of the assay solution placed
alongside. The finishing point is decided and practically permanent,
although it demands a little practice to recognise it. The titration with
permanganate of potassium has the advantage of a more distinct finishing
point and easier mode of working; its application, however, is somewhat
limited by the disturbing effects of hydrochloric acid. The bichromate
method has the advantage of a standard solution which does not alter in
strength, and the further one of being but little affected by altering
conditions of assay. Hydrochloric acid has practically no effect on it. Both
methods give accurate results and are good examples of volumetric
methods.
The following results illustrate the extent to which the methods may be
relied on; and the influence which the various conditions of experiment
Page 304
have on the assay.
Solutions of ferrous sulphate and of ferrous chloride were made containing
0.5 gram of iron in each 100 c.c., thus corresponding to the standard
solutions of permanganate and bichromate of potassium. These last were
prepared in the way already described. The solution of ferrous sulphate was
made by dissolving 5.01 grams of iron wire in 100 c.c. of dilute sulphuric
acid and diluting to 1 litre. A similar solution may be made by dissolving
24.82 grams of pure ferrous sulphate crystals in water, adding 100 c.c. of
dilute sulphuric acid, and diluting to 1 litre.
Rate of Oxidation by Exposure to Air.—This is an important
consideration, and if the rate were at all rapid would have a serious
influence on the manner of working, since exclusion of air in the various
operations would be troublesome. 20 c.c. of the solution of ferrous sulphate
were taken in each experiment, acidified with 10 c.c. of dilute sulphuric
acid, and diluted to 100 c.c. The solution was exposed, cold, in an open
beaker for varying lengths of time, and titrated with permanganate of
potassium.
Time exposed 1 hour 1 day 2 days 3 days
c.c. required 19.2 19.1 19.0 19.0
These results show that the atmospheric oxidation in cold solutions is
unimportant. With boiling solutions the results are somewhat different; a
solution which at the outset required 20 c.c. of permanganate of potassium,
after boiling for an hour in an open beaker (without any precautions to
prevent oxidation), water being added from time to time to replace that lost
by evaporation, required 19.2 c.c. If the solution be evaporated to dryness
the oxidising power of concentrated sulphuric acid comes into play, so that
very little ferrous iron will be left. A solution evaporated in this way
required only 2.2 c.c. of permanganate of potassium.
Effect of Varying Temperature.—In these experiments the bulk was in
each case 100 c.c., and 10 c.c. of dilute sulphuric acid were present. The
permanganate required by
1c.c. of ferrous sulphate was, at 15° 1.0 c.c., and at 70° 1.1 c.c.
Solutions of ferrous sulphate and of ferrous chloride were made containing
0.5 gram of iron in each 100 c.c., thus corresponding to the standard
solutions of permanganate and bichromate of potassium. These last were
prepared in the way already described. The solution of ferrous sulphate was
made by dissolving 5.01 grams of iron wire in 100 c.c. of dilute sulphuric
acid and diluting to 1 litre. A similar solution may be made by dissolving
24.82 grams of pure ferrous sulphate crystals in water, adding 100 c.c. of
dilute sulphuric acid, and diluting to 1 litre.
Rate of Oxidation by Exposure to Air.—This is an important
consideration, and if the rate were at all rapid would have a serious
influence on the manner of working, since exclusion of air in the various
operations would be troublesome. 20 c.c. of the solution of ferrous sulphate
were taken in each experiment, acidified with 10 c.c. of dilute sulphuric
acid, and diluted to 100 c.c. The solution was exposed, cold, in an open
beaker for varying lengths of time, and titrated with permanganate of
potassium.
Time exposed 1 hour 1 day 2 days 3 days
c.c. required 19.2 19.1 19.0 19.0
These results show that the atmospheric oxidation in cold solutions is
unimportant. With boiling solutions the results are somewhat different; a
solution which at the outset required 20 c.c. of permanganate of potassium,
after boiling for an hour in an open beaker (without any precautions to
prevent oxidation), water being added from time to time to replace that lost
by evaporation, required 19.2 c.c. If the solution be evaporated to dryness
the oxidising power of concentrated sulphuric acid comes into play, so that
very little ferrous iron will be left. A solution evaporated in this way
required only 2.2 c.c. of permanganate of potassium.
Effect of Varying Temperature.—In these experiments the bulk was in
each case 100 c.c., and 10 c.c. of dilute sulphuric acid were present. The
permanganate required by
1c.c. of ferrous sulphate was, at 15° 1.0 c.c., and at 70° 1.1 c.c.
Page 305
10 " " " 9.7 " 9.8 "
100 " " " 97.7 " 96.8 "
The lower result with the 100 c.c. may be due to oxidation from exposure.
Effect of Varying Bulk.—The following experiments show that
considerable variations in bulk have no practical effect. In each case 20 c.c.
of ferrous sulphate solution and 10 c.c. of dilute acid were used.
Bulk of assay 30c.c. 100 c.c. 500c.c. 1000 c.c.
Permanganate required 20.0" 20.0 " 20.2" 20.5 "
Effect of Free Sulphuric Acid.—Free acid is necessary for these assays; if
there is an insufficiency, the assay solution, instead of immediately
decolorising the permanganate, assumes a brown colour. The addition of 10
c.c. of dilute sulphuric acid suffices to meet requirements and keep the
assay clear throughout. The following experiments show that a considerable
excess of acid may be used without in the least affecting the results. In each
case 20 c.c. of ferrous sulphate were used.
Dilute sulphuric acid 1.0 c.c. 5.0 c.c. 10.0c.c. 20.0c.c. 50.0c.c. 100.0c.c.
Permanganate required 19.3" 19.3" 19.3" 19.3" 19.3" 19.3 "
Effect of Foreign Salts.—When the assay has been reduced with zinc
varying quantities of salts of this metal pass into solution, the amount
depending on the quantity of acid and iron present. Salts of sodium or
ammonium may similarly be introduced. It is essential to know by
experiment that these salts do not exert any effect on the titration. The
following series of experiments show that as much as 50 grams of zinc
sulphate may be present without interfering.
Zinc sulphate present 0 gram 1 gram 10 grams 50 grams
Permanganate required 19.3 c.c. 19.3 c.c. 19.3 c.c. 19.3 c.c.
Magnesium, sodium, and ammonium salts, are equally without effect.
Ammonic sulphate present 0 gram 1 gram 10 grams
Permanganate required 19.3 c.c. 19.2 c.c. 19.3 c.c.
100 " " " 97.7 " 96.8 "
The lower result with the 100 c.c. may be due to oxidation from exposure.
Effect of Varying Bulk.—The following experiments show that
considerable variations in bulk have no practical effect. In each case 20 c.c.
of ferrous sulphate solution and 10 c.c. of dilute acid were used.
Bulk of assay 30c.c. 100 c.c. 500c.c. 1000 c.c.
Permanganate required 20.0" 20.0 " 20.2" 20.5 "
Effect of Free Sulphuric Acid.—Free acid is necessary for these assays; if
there is an insufficiency, the assay solution, instead of immediately
decolorising the permanganate, assumes a brown colour. The addition of 10
c.c. of dilute sulphuric acid suffices to meet requirements and keep the
assay clear throughout. The following experiments show that a considerable
excess of acid may be used without in the least affecting the results. In each
case 20 c.c. of ferrous sulphate were used.
Dilute sulphuric acid 1.0 c.c. 5.0 c.c. 10.0c.c. 20.0c.c. 50.0c.c. 100.0c.c.
Permanganate required 19.3" 19.3" 19.3" 19.3" 19.3" 19.3 "
Effect of Foreign Salts.—When the assay has been reduced with zinc
varying quantities of salts of this metal pass into solution, the amount
depending on the quantity of acid and iron present. Salts of sodium or
ammonium may similarly be introduced. It is essential to know by
experiment that these salts do not exert any effect on the titration. The
following series of experiments show that as much as 50 grams of zinc
sulphate may be present without interfering.
Zinc sulphate present 0 gram 1 gram 10 grams 50 grams
Permanganate required 19.3 c.c. 19.3 c.c. 19.3 c.c. 19.3 c.c.
Magnesium, sodium, and ammonium salts, are equally without effect.
Ammonic sulphate present 0 gram 1 gram 10 grams
Permanganate required 19.3 c.c. 19.2 c.c. 19.3 c.c.
Page 306
Sodic sulphate present 0 gram 1 gram 10 grams
Permanganate required 19.3 c.c. 19.3 c.c. 19.3 c.c.
Magnesic sulphate present 0 gram 1 gram 10 grams
Permanganate required 19.3 c.c. 19.3 c.c. 19.3 c.c.
Effect of Varying Amounts of Iron.—It is important to know within what
limits the quantity of iron in an assay may safely vary from that used in
standardising. In the following experiments the conditions as to bulk,
acidity, and mode of working were the same as before:—
Ferrous sulphate solution taken 1 c.c. 10 c.c. 20 c.c. 50 c.c. 100 c.c.
Permanganate required 1.0" 9.7" 19.6 " 48.9 " 97.7"
The ferrous sulphate solution is here a little weaker than that of the
permanganate of potassium, but the results show that the permanganate
required is proportional to the iron present.
Titrations in Hydrochloric Solutions.—These are less satisfactory than
those in sulphuric solutions, since an excess of hydrochloric acid
decomposes permanganate of potassium, evolving chlorine, and since the
finishing point is indicated, not by the persistence of the pink colour of the
permanganate, but by a brown coloration probably due to perchloride of
manganese. Nevertheless, if the solution contains only from 5 to 10 per
cent. of free hydrochloric acid (sp. g. 1.16) the results are the same as those
obtained in a sulphuric acid solution. Equal weights (0.1 gram) of the same
iron wire required exactly the same quantity of the permanganate of
potassium solution (20 c.c.) whether the iron was dissolved in dilute
sulphuric or dilute hydrochloric acid. The following series of experiments
are on the same plan as those given above with sulphuric acid solutions. A
solution of ferrous chloride was made by dissolving 5.01 grams of iron wire
in 50 c.c. of dilute hydrochloric acid and diluting to 1 litre. The dilute
hydrochloric acid was made by mixing equal volumes of the acid (sp. g.
1.16) and water.
Rate of Atmospheric Oxidation.—20 c.c. of the ferrous chloride solution
were acidified with 10 c.c. of the dilute hydrochloric acid and diluted to 100
c.c. This solution was exposed cold in open beakers.
Permanganate required 19.3 c.c. 19.3 c.c. 19.3 c.c.
Magnesic sulphate present 0 gram 1 gram 10 grams
Permanganate required 19.3 c.c. 19.3 c.c. 19.3 c.c.
Effect of Varying Amounts of Iron.—It is important to know within what
limits the quantity of iron in an assay may safely vary from that used in
standardising. In the following experiments the conditions as to bulk,
acidity, and mode of working were the same as before:—
Ferrous sulphate solution taken 1 c.c. 10 c.c. 20 c.c. 50 c.c. 100 c.c.
Permanganate required 1.0" 9.7" 19.6 " 48.9 " 97.7"
The ferrous sulphate solution is here a little weaker than that of the
permanganate of potassium, but the results show that the permanganate
required is proportional to the iron present.
Titrations in Hydrochloric Solutions.—These are less satisfactory than
those in sulphuric solutions, since an excess of hydrochloric acid
decomposes permanganate of potassium, evolving chlorine, and since the
finishing point is indicated, not by the persistence of the pink colour of the
permanganate, but by a brown coloration probably due to perchloride of
manganese. Nevertheless, if the solution contains only from 5 to 10 per
cent. of free hydrochloric acid (sp. g. 1.16) the results are the same as those
obtained in a sulphuric acid solution. Equal weights (0.1 gram) of the same
iron wire required exactly the same quantity of the permanganate of
potassium solution (20 c.c.) whether the iron was dissolved in dilute
sulphuric or dilute hydrochloric acid. The following series of experiments
are on the same plan as those given above with sulphuric acid solutions. A
solution of ferrous chloride was made by dissolving 5.01 grams of iron wire
in 50 c.c. of dilute hydrochloric acid and diluting to 1 litre. The dilute
hydrochloric acid was made by mixing equal volumes of the acid (sp. g.
1.16) and water.
Rate of Atmospheric Oxidation.—20 c.c. of the ferrous chloride solution
were acidified with 10 c.c. of the dilute hydrochloric acid and diluted to 100
c.c. This solution was exposed cold in open beakers.
Page 307
Time exposed — 1 hour 1 day 2 days 3 days
Permanganate required 19.6 c.c. 19.6 c.c. 19.5 c.c. 19.4 c.c. 19.5 c.c.
Similar solutions boiled required, before boiling, 20 c.c.; after boiling for
one hour, replacing the water as it evaporated, 19.3 c.c.; and after
evaporation to a paste and redissolving, 17.0 c.c.
Effect of Varying Temperature.—Solutions similar to the last were titrated
and gave the following results:—
Temperature 15° 30° 50° 70°
Permanganate required 19.8 c.c. 19.6 c.c. 19.5 c.c. 19.4 c.c.
Effect of Varying Bulk.—As before, 20 c.c. of the iron solution, and 10
c.c. of the dilute acid were diluted to the required volumes and titrated.
Bulk 30 c.c. 100 c.c. 500 c.c. 1000 c.c.
Permanganate required 20.4 " 20.3 " 20.8 " 21.5 "
The variation due to difference in bulk here, although only equal to an
excess of 0.7 milligram of iron for each 100 c.c. of dilution, are about three
times as great as those observed in a sulphuric acid solution.
Effect of Free Hydrochloric Acid.—In these experiments 20 c.c. of the
ferrous chloride solution were used with varying quantities of acid, the bulk
of the assay in each case being 100 c.c.
Dilute acid present 5 c.c. 10 c.c. 50 c.c. 100 c.c.
Permanganate required 20.2 " 20.2 " 20.5 " 21.0 "
The last had a very indistinct finishing point, the brown coloration being
very evanescent. The effect of the acid is modified by the presence of
alkaline and other sulphates, but not by sulphuric acid. Repeating the last
experiment we got—
Without further addition 21.0c.c.
With 100 c.c. of dilute sulphuric acid 22.0"
" 10 grams ammonic sulphate 20.5"
Permanganate required 19.6 c.c. 19.6 c.c. 19.5 c.c. 19.4 c.c. 19.5 c.c.
Similar solutions boiled required, before boiling, 20 c.c.; after boiling for
one hour, replacing the water as it evaporated, 19.3 c.c.; and after
evaporation to a paste and redissolving, 17.0 c.c.
Effect of Varying Temperature.—Solutions similar to the last were titrated
and gave the following results:—
Temperature 15° 30° 50° 70°
Permanganate required 19.8 c.c. 19.6 c.c. 19.5 c.c. 19.4 c.c.
Effect of Varying Bulk.—As before, 20 c.c. of the iron solution, and 10
c.c. of the dilute acid were diluted to the required volumes and titrated.
Bulk 30 c.c. 100 c.c. 500 c.c. 1000 c.c.
Permanganate required 20.4 " 20.3 " 20.8 " 21.5 "
The variation due to difference in bulk here, although only equal to an
excess of 0.7 milligram of iron for each 100 c.c. of dilution, are about three
times as great as those observed in a sulphuric acid solution.
Effect of Free Hydrochloric Acid.—In these experiments 20 c.c. of the
ferrous chloride solution were used with varying quantities of acid, the bulk
of the assay in each case being 100 c.c.
Dilute acid present 5 c.c. 10 c.c. 50 c.c. 100 c.c.
Permanganate required 20.2 " 20.2 " 20.5 " 21.0 "
The last had a very indistinct finishing point, the brown coloration being
very evanescent. The effect of the acid is modified by the presence of
alkaline and other sulphates, but not by sulphuric acid. Repeating the last
experiment we got—
Without further addition 21.0c.c.
With 100 c.c. of dilute sulphuric acid 22.0"
" 10 grams ammonic sulphate 20.5"
Page 308
" 10 " sodic sulphate 20.0"
" 10 " magnesium sulphate 20.4"
" 10 " manganese sulphate 20.2"
The results with these salts, in counteracting the interference of the acid,
however, were not a complete success, since the end-reactions were all
indistinct, with the exception, perhaps, of that with the manganese sulphate.
Effect of Varying Amounts of Iron.—In these experiments the bulk of the
assay was 100 c.c., and 10 c.c. of acid were present.
Ferrous chloride used 1 c.c. 10 c.c. 20 c.c. 50 c.c. 100 c.c.
Permanganate required 1.1 " 10.3 " 20.3 " 50.4 " 100.1 "
In making himself familiar with the permanganate of potassium titration,
the student should practise by working out a series of experiments similar to
the above, varying his conditions one at a time so as to be certain of the
cause of any variation in his results. He may then proceed to experiment on
the various methods of reduction.
A solution of ferric chloride is made by dissolving 5.01 grams of iron wire
in 50 c.c. of hydrochloric acid (sp. g. 1.16), and running from a burette
nitric acid diluted with an equal volume of water into the boiling iron
solution, until the liquid changes from a black to a reddish-yellow. About
4.5 c.c. of the nitric acid will be required, and the finishing point is marked
by a brisk effervescence. The solution of iron should be contained in an
evaporating dish, and boiled briskly, with constant stirring. There should be
no excess of nitric acid. Boil down to about half its bulk; then cool, and
dilute to one litre with water. Twenty c.c. of this solution diluted to 100 c.c.
with water, and acidified with 10 c.c. of dilute hydrochloric acid, should not
decolorise any of the permanganate of potassium solution; this shows the
absence of ferrous salts. And 20 c.c. of the same solution, boiled with 20
c.c. of the ferrous sulphate solution, should not decrease the quantity of
"permanganate" required for the titration of the ferrous sulphate added. In a
series of experiments on the various methods of reduction, the following
results were got. The modes of working were those already described.
" 10 " magnesium sulphate 20.4"
" 10 " manganese sulphate 20.2"
The results with these salts, in counteracting the interference of the acid,
however, were not a complete success, since the end-reactions were all
indistinct, with the exception, perhaps, of that with the manganese sulphate.
Effect of Varying Amounts of Iron.—In these experiments the bulk of the
assay was 100 c.c., and 10 c.c. of acid were present.
Ferrous chloride used 1 c.c. 10 c.c. 20 c.c. 50 c.c. 100 c.c.
Permanganate required 1.1 " 10.3 " 20.3 " 50.4 " 100.1 "
In making himself familiar with the permanganate of potassium titration,
the student should practise by working out a series of experiments similar to
the above, varying his conditions one at a time so as to be certain of the
cause of any variation in his results. He may then proceed to experiment on
the various methods of reduction.
A solution of ferric chloride is made by dissolving 5.01 grams of iron wire
in 50 c.c. of hydrochloric acid (sp. g. 1.16), and running from a burette
nitric acid diluted with an equal volume of water into the boiling iron
solution, until the liquid changes from a black to a reddish-yellow. About
4.5 c.c. of the nitric acid will be required, and the finishing point is marked
by a brisk effervescence. The solution of iron should be contained in an
evaporating dish, and boiled briskly, with constant stirring. There should be
no excess of nitric acid. Boil down to about half its bulk; then cool, and
dilute to one litre with water. Twenty c.c. of this solution diluted to 100 c.c.
with water, and acidified with 10 c.c. of dilute hydrochloric acid, should not
decolorise any of the permanganate of potassium solution; this shows the
absence of ferrous salts. And 20 c.c. of the same solution, boiled with 20
c.c. of the ferrous sulphate solution, should not decrease the quantity of
"permanganate" required for the titration of the ferrous sulphate added. In a
series of experiments on the various methods of reduction, the following
results were got. The modes of working were those already described.
Page 309
(1) With Stannous Chloride.—Twenty c.c. of the ferric chloride solution
required, after reduction with stannous chloride, 20 c.c. of "permanganate."
Fifty c.c. of a solution of ferrous chloride, which required on titration 49.8
c.c. of "permanganate," required for re-titration (after subsequent reduction
with stannous chloride) 50 c.c. of the permanganate solution.
(2) With Sulphuretted Hydrogen.—Two experiments with this gas, using in
each 20 c.c. of the ferric chloride solution, and 10 c.c. of hydrochloric acid,
required (after reduction) 20.2 c.c. and 20.1 c.c. of "permanganate."
Repeating the experiments by passing the gas through a nearly boiling
solution, but in other respects working in the same way, 21.3 c.c. and 21.6
c.c. of the permanganate solution were required. The sulphur was not
filtered off in any of these. In another experiment, in which 50 c.c. of the
ferrous sulphate solution were titrated with "permanganate," 48 c.c. of the
latter were required. The titrated solution was next reduced with
sulphuretted hydrogen, brought to the same bulk as before, and again
titrated; 47.9 c.c. of the permanganate of potassium solution were required.
(3) With Sodium Sulphite.—Twenty c.c. of the ferric chloride solution,
reduced with sodium sulphite, required 19.9 c.c. of "permanganate." In one
experiment 50 c.c. of the ferrous sulphate solution were titrated with
"permanganate"; 49.3 c.c. of the last-mentioned solution were required. The
titrated solution was reduced with sodium sulphite, and again titrated; it
required 49.2 c.c. of the permanganate of potassium solution.
(4) With Zinc.—Twenty c.c. of the ferric chloride solution, reduced with
zinc and titrated, required 20.8 c.c. of "permanganate." Fifty c.c. of a
solution of ferrous sulphate which required 49.7 c.c. of "permanganate,"
required for re-titration, after reduction with zinc, 49.7 c.c.
The student should next practise the titration with bichromate, which is
more especially valuable in the estimation of hydrochloric acid solutions.
The following experiments are on the same plan as those already given. In
each experiment (except when otherwise stated) there were present 20 c.c.
of the ferrous chloride solution, and 10 c.c. of dilute hydrochloric acid, and
the bulk was 300 c.c.
Effect of Varying Temperature.—The quantities of the bichromate of
potassium solution required were as follows:—
required, after reduction with stannous chloride, 20 c.c. of "permanganate."
Fifty c.c. of a solution of ferrous chloride, which required on titration 49.8
c.c. of "permanganate," required for re-titration (after subsequent reduction
with stannous chloride) 50 c.c. of the permanganate solution.
(2) With Sulphuretted Hydrogen.—Two experiments with this gas, using in
each 20 c.c. of the ferric chloride solution, and 10 c.c. of hydrochloric acid,
required (after reduction) 20.2 c.c. and 20.1 c.c. of "permanganate."
Repeating the experiments by passing the gas through a nearly boiling
solution, but in other respects working in the same way, 21.3 c.c. and 21.6
c.c. of the permanganate solution were required. The sulphur was not
filtered off in any of these. In another experiment, in which 50 c.c. of the
ferrous sulphate solution were titrated with "permanganate," 48 c.c. of the
latter were required. The titrated solution was next reduced with
sulphuretted hydrogen, brought to the same bulk as before, and again
titrated; 47.9 c.c. of the permanganate of potassium solution were required.
(3) With Sodium Sulphite.—Twenty c.c. of the ferric chloride solution,
reduced with sodium sulphite, required 19.9 c.c. of "permanganate." In one
experiment 50 c.c. of the ferrous sulphate solution were titrated with
"permanganate"; 49.3 c.c. of the last-mentioned solution were required. The
titrated solution was reduced with sodium sulphite, and again titrated; it
required 49.2 c.c. of the permanganate of potassium solution.
(4) With Zinc.—Twenty c.c. of the ferric chloride solution, reduced with
zinc and titrated, required 20.8 c.c. of "permanganate." Fifty c.c. of a
solution of ferrous sulphate which required 49.7 c.c. of "permanganate,"
required for re-titration, after reduction with zinc, 49.7 c.c.
The student should next practise the titration with bichromate, which is
more especially valuable in the estimation of hydrochloric acid solutions.
The following experiments are on the same plan as those already given. In
each experiment (except when otherwise stated) there were present 20 c.c.
of the ferrous chloride solution, and 10 c.c. of dilute hydrochloric acid, and
the bulk was 300 c.c.
Effect of Varying Temperature.—The quantities of the bichromate of
potassium solution required were as follows:—
Page 310
Temperature 15° 30° 70° 100°
Bichromate required 20.2 c.c. 20.3 c.c. 20.3 c.c. 20.4 c.c.
Effect of Varying Bulk.—
Bulk 50 c.c. 100 c.c. 200 c.c. 500 c.c. 1000 c.c.
Bichromate required 20.4 " 20.4 " 20.4 " 20.5 " 20.8 "
Effect of Varying Acid.—In these, variable quantities of dilute
hydrochloric acid were used.
Acid present 10 c.c. 50 c.c. 100 c.c.
Bichromate required 20.3 " 20.3 " 20.2 "
Effect of Foreign Salts.—The effect of the addition of 10 grams of
crystallized zinc sulphate was to decrease the quantity of "bichromate"
required from 20.3 c.c. to 20.1 c.c., but the colour produced with the test-
drop was very slight at 18.5 c.c., and with incautious work the finishing
point might have been taken anywhere between these extremes. Zinc should
not be used as a reducing agent preliminary to a "bichromate" titration. Ten
grams of ammonic sulphate had the effect of rendering the finishing point
faint for about 0.5 c.c. before the titration was finished, but there was no
doubt about the finishing point when allowed to stand for a minute. The
student should note that a titration is not completed if a colour is developed
on standing for five or ten minutes. Ten grams of sodic sulphate had no
effect; 20.3 c.c. were required.
Effect of Varying Iron.—The results are proportional, as will be seen from
the following details:—
Ferrous chloride present 1.0 c.c. 10.0 c.c. 20.0 c.c. 50.0 c.c. 100.0 c.c.
Bichromate required 1.0 " 10.2 " 20.3 " 51.0 " 102.3 "
The student may now apply these titrations to actual assays of minerals. The
following examples will illustrate the mode of working and of calculating
the results:—
Bichromate required 20.2 c.c. 20.3 c.c. 20.3 c.c. 20.4 c.c.
Effect of Varying Bulk.—
Bulk 50 c.c. 100 c.c. 200 c.c. 500 c.c. 1000 c.c.
Bichromate required 20.4 " 20.4 " 20.4 " 20.5 " 20.8 "
Effect of Varying Acid.—In these, variable quantities of dilute
hydrochloric acid were used.
Acid present 10 c.c. 50 c.c. 100 c.c.
Bichromate required 20.3 " 20.3 " 20.2 "
Effect of Foreign Salts.—The effect of the addition of 10 grams of
crystallized zinc sulphate was to decrease the quantity of "bichromate"
required from 20.3 c.c. to 20.1 c.c., but the colour produced with the test-
drop was very slight at 18.5 c.c., and with incautious work the finishing
point might have been taken anywhere between these extremes. Zinc should
not be used as a reducing agent preliminary to a "bichromate" titration. Ten
grams of ammonic sulphate had the effect of rendering the finishing point
faint for about 0.5 c.c. before the titration was finished, but there was no
doubt about the finishing point when allowed to stand for a minute. The
student should note that a titration is not completed if a colour is developed
on standing for five or ten minutes. Ten grams of sodic sulphate had no
effect; 20.3 c.c. were required.
Effect of Varying Iron.—The results are proportional, as will be seen from
the following details:—
Ferrous chloride present 1.0 c.c. 10.0 c.c. 20.0 c.c. 50.0 c.c. 100.0 c.c.
Bichromate required 1.0 " 10.2 " 20.3 " 51.0 " 102.3 "
The student may now apply these titrations to actual assays of minerals. The
following examples will illustrate the mode of working and of calculating
the results:—
Page 311
Determination of Iron in Chalybite.—Weigh up 1 gram of the dry
powdered ore, and dissolve in 10 c.c. of dilute sulphuric acid and an equal
volume of water with the aid of heat. Avoid evaporating to dryness. Dilute
and titrate. The result will give the percentage of iron existing in the ore in
the ferrous state. Some ferric iron may be present. If it is wished to
determine this also, add (in dissolving another portion) 10 c.c. of dilute
hydrochloric acid to the sulphuric acid already ordered, and reduce the
resulting solution before titrating. By dissolving and titrating (without
previous reduction) one has a measure of the ferrous iron present; by
dissolving, reducing, and then titrating, one can measure the total iron; and
as the iron exists in only two conditions, the total iron, less the ferrous iron,
is the measure of the ferric iron.
Determination of Iron in Brown or Red Ores or Magnetite.—Weigh up
0.5 gram of the ore (powdered and dried at 100° C.), and dissolve in from
10 to 20 c.c. of strong hydrochloric acid, boiling until all is dissolved, or
until no coloured particles are left. Dilute, reduce, and titrate.
Determination of Iron in Pyrites.—Weigh up 1 gram of the dry powdered
ore, and place in a beaker. Cover with 10 c.c. of strong sulphuric acid, mix
well by shaking, and place on the hot plate without further handling for an
hour or so until the action has ceased. Allow to cool, and dilute to 100 c.c.
Warm until solution is complete. Reduce and titrate.
Determination of Iron in Substances Insoluble in Acids.—Weigh up 1
gram of the ore, mix with 5 or 6 grams of carbonate of soda and 0.5 gram of
nitre by rubbing in a small mortar, and transfer to a platinum crucible. Clean
out the mortar by rubbing up another gram or so of soda, and add this to the
contents of the crucible as a cover. Fuse till tranquil. Cool. Extract with
water. If the ore carries much silica, evaporate to dryness with hydrochloric
acid to separate it. Re-dissolve in hydrochloric acid, and separate the iron
by precipitating with ammonia and filtering. If only a small quantity of
silica is present, the aqueous extract of the "melt" must be filtered, and the
insoluble residue washed and dissolved in dilute hydrochloric acid. Reduce
and titrate.
A convenient method of at once separating iron from a solution and
reducing it, is to add ammonia, pass sulphuretted hydrogen through it, filter,
powdered ore, and dissolve in 10 c.c. of dilute sulphuric acid and an equal
volume of water with the aid of heat. Avoid evaporating to dryness. Dilute
and titrate. The result will give the percentage of iron existing in the ore in
the ferrous state. Some ferric iron may be present. If it is wished to
determine this also, add (in dissolving another portion) 10 c.c. of dilute
hydrochloric acid to the sulphuric acid already ordered, and reduce the
resulting solution before titrating. By dissolving and titrating (without
previous reduction) one has a measure of the ferrous iron present; by
dissolving, reducing, and then titrating, one can measure the total iron; and
as the iron exists in only two conditions, the total iron, less the ferrous iron,
is the measure of the ferric iron.
Determination of Iron in Brown or Red Ores or Magnetite.—Weigh up
0.5 gram of the ore (powdered and dried at 100° C.), and dissolve in from
10 to 20 c.c. of strong hydrochloric acid, boiling until all is dissolved, or
until no coloured particles are left. Dilute, reduce, and titrate.
Determination of Iron in Pyrites.—Weigh up 1 gram of the dry powdered
ore, and place in a beaker. Cover with 10 c.c. of strong sulphuric acid, mix
well by shaking, and place on the hot plate without further handling for an
hour or so until the action has ceased. Allow to cool, and dilute to 100 c.c.
Warm until solution is complete. Reduce and titrate.
Determination of Iron in Substances Insoluble in Acids.—Weigh up 1
gram of the ore, mix with 5 or 6 grams of carbonate of soda and 0.5 gram of
nitre by rubbing in a small mortar, and transfer to a platinum crucible. Clean
out the mortar by rubbing up another gram or so of soda, and add this to the
contents of the crucible as a cover. Fuse till tranquil. Cool. Extract with
water. If the ore carries much silica, evaporate to dryness with hydrochloric
acid to separate it. Re-dissolve in hydrochloric acid, and separate the iron
by precipitating with ammonia and filtering. If only a small quantity of
silica is present, the aqueous extract of the "melt" must be filtered, and the
insoluble residue washed and dissolved in dilute hydrochloric acid. Reduce
and titrate.
A convenient method of at once separating iron from a solution and
reducing it, is to add ammonia, pass sulphuretted hydrogen through it, filter,
Page 312
and dissolve the precipitate in dilute sulphuric acid. The solution, when
boiled free from sulphuretted hydrogen, is ready for titrating.
STANNOUS CHLORIDE PROCESS.
The colour imparted to hot hydrochloric acid solutions by a trace of a ferric
compound is so strong, and the reducing action of stannous chloride is so
rapid, that a method of titration is based upon the quantity of a standard
solution of stannous chloride required to completely decolorise a solution
containing ferric iron. This method is more especially adapted for the assay
of liquors containing much ferric iron and of those oxidised ores which are
completely soluble in hydrochloric acid. It must be remembered, however,
that it only measures the ferric iron present, and when (as is generally the
case) the total iron is wanted, it is well to calcine the weighed portion of ore
previous to solution in order to get the whole of the iron into the higher
state of oxidation, since many ores which are generally supposed to contain
only ferric iron carry a considerable percentage of ferrous.
The stannous chloride solution is made by dissolving 20 grams of the
commercial salt (SnCl2.2H2O) in 100 c.c. of water with the help of 20 c.c.
of dilute hydrochloric acid, and diluting to a litre. The solution may be
slightly opalescent, but should show no signs of a precipitate. The strength
of this is about equivalent to 1 gram of iron for each 100 c.c. of the solution,
but it is apt to lessen on standing, taking up oxygen from the air, forming
stannic chloride. A larger proportion of hydrochloric acid than is ordered
above would remove the opalescence, but at the same time increase this
tendency to atmospheric oxidation, as the following experiments show. The
stannous chloride solution (20 c.c.) was mixed with varying amounts of
strong hydrochloric acid (sp. g. 1.16), diluted to 100 c.c., and exposed in
open beakers for varying lengths of time; and the residual stannous chloride
measured by titration with permanganate. The quantities required were as
follows:—
Time Exposed. 50 per cent. Acid. 10 per cent. Acid. 1 per cent. Acid.
1 hour 33.2 c.c. 34.4 c.c. 34.5 c.c.
1 day 5.0 " 24.0 " 27.6 "
2 days 3.0 " 14.5 " 21.3 "
boiled free from sulphuretted hydrogen, is ready for titrating.
STANNOUS CHLORIDE PROCESS.
The colour imparted to hot hydrochloric acid solutions by a trace of a ferric
compound is so strong, and the reducing action of stannous chloride is so
rapid, that a method of titration is based upon the quantity of a standard
solution of stannous chloride required to completely decolorise a solution
containing ferric iron. This method is more especially adapted for the assay
of liquors containing much ferric iron and of those oxidised ores which are
completely soluble in hydrochloric acid. It must be remembered, however,
that it only measures the ferric iron present, and when (as is generally the
case) the total iron is wanted, it is well to calcine the weighed portion of ore
previous to solution in order to get the whole of the iron into the higher
state of oxidation, since many ores which are generally supposed to contain
only ferric iron carry a considerable percentage of ferrous.
The stannous chloride solution is made by dissolving 20 grams of the
commercial salt (SnCl2.2H2O) in 100 c.c. of water with the help of 20 c.c.
of dilute hydrochloric acid, and diluting to a litre. The solution may be
slightly opalescent, but should show no signs of a precipitate. The strength
of this is about equivalent to 1 gram of iron for each 100 c.c. of the solution,
but it is apt to lessen on standing, taking up oxygen from the air, forming
stannic chloride. A larger proportion of hydrochloric acid than is ordered
above would remove the opalescence, but at the same time increase this
tendency to atmospheric oxidation, as the following experiments show. The
stannous chloride solution (20 c.c.) was mixed with varying amounts of
strong hydrochloric acid (sp. g. 1.16), diluted to 100 c.c., and exposed in
open beakers for varying lengths of time; and the residual stannous chloride
measured by titration with permanganate. The quantities required were as
follows:—
Time Exposed. 50 per cent. Acid. 10 per cent. Acid. 1 per cent. Acid.
1 hour 33.2 c.c. 34.4 c.c. 34.5 c.c.
1 day 5.0 " 24.0 " 27.6 "
2 days 3.0 " 14.5 " 21.3 "
Page 313
These indicate very clearly the increased susceptibility to oxidation in
strongly acid solutions.
A standard solution of ferric chloride is prepared in the same manner as that
described under the experiments on the methods of reduction; but it should
be of twice the strength, so that 100 c.c. may contain 1 gram of iron. This
solution is used for standardising the stannous chloride when required; and
must be carefully prepared; and tested for the presence of nitric acid.
The titration is more limited in its application than either of the oxidising
processes because of the restrictions as to bulk, quality and quantity of free
acid present, and other conditions of the solution to be assayed. The
following experiments show the conditions necessary for a successful
titration.
Effect of Varying Temperature.—Twenty c.c. of ferric chloride solution
with 20 c.c. of strong hydrochloric acid, diluted to 50 c.c., gave the
following results when titrated:—
Temperature 15° 30° 70° 100°
Stannous chloride required 22.8 c.c. 22.0 c.c. 22.1 c.c. 22.0 c.c.
The finishing point, however, is more distinct the hotter the solution; so that
it is best in all cases to run the standard into the boiling solution.
Effect of Varying Bulk.—Solutions containing the same quantity of iron
and acid as the last, but diluted to various bulks, and titrated while boiling,
gave the following results:—
Bulk 30 c.c. 100 c.c. 500 c.c.
Stannous chloride required 21.5 " 21.7 " 24.3 "
Effect of Varying Quantities of Hydrochloric Acid.—In these
experiments the bulk before titration was 50 c.c. except in the last, in which
it was 70 c.c. With less than 5 c.c. of strong hydrochloric acid the finishing
point is indistinct and prolonged.
Strong hydrochloric acid present 5 c.c. 10 c.c. 20 c.c. 30 c.c. 50 c.c.
Stannous chloride required 21.1 " 21.1 " 21.2 " 21.8 " 22.2 "
strongly acid solutions.
A standard solution of ferric chloride is prepared in the same manner as that
described under the experiments on the methods of reduction; but it should
be of twice the strength, so that 100 c.c. may contain 1 gram of iron. This
solution is used for standardising the stannous chloride when required; and
must be carefully prepared; and tested for the presence of nitric acid.
The titration is more limited in its application than either of the oxidising
processes because of the restrictions as to bulk, quality and quantity of free
acid present, and other conditions of the solution to be assayed. The
following experiments show the conditions necessary for a successful
titration.
Effect of Varying Temperature.—Twenty c.c. of ferric chloride solution
with 20 c.c. of strong hydrochloric acid, diluted to 50 c.c., gave the
following results when titrated:—
Temperature 15° 30° 70° 100°
Stannous chloride required 22.8 c.c. 22.0 c.c. 22.1 c.c. 22.0 c.c.
The finishing point, however, is more distinct the hotter the solution; so that
it is best in all cases to run the standard into the boiling solution.
Effect of Varying Bulk.—Solutions containing the same quantity of iron
and acid as the last, but diluted to various bulks, and titrated while boiling,
gave the following results:—
Bulk 30 c.c. 100 c.c. 500 c.c.
Stannous chloride required 21.5 " 21.7 " 24.3 "
Effect of Varying Quantities of Hydrochloric Acid.—In these
experiments the bulk before titration was 50 c.c. except in the last, in which
it was 70 c.c. With less than 5 c.c. of strong hydrochloric acid the finishing
point is indistinct and prolonged.
Strong hydrochloric acid present 5 c.c. 10 c.c. 20 c.c. 30 c.c. 50 c.c.
Stannous chloride required 21.1 " 21.1 " 21.2 " 21.8 " 22.2 "
Page 314
Effect of Free Sulphuric Acid.—In these experiments 20 c.c. of
hydrochloric acid were present, and the bulk was 50 c.c.
Strong sulphuric acid present — c.c. 3 c.c. 5 c.c. 10 c.c.
Stannous chloride required 21.6 " 22.3 " 22.9 " 23.1 "
This interference of strong sulphuric acid may be completely counteracted
by somewhat modifying the mode of working. Another experiment, like the
last of this series, required 21.6 c.c.
Effect of Foreign Salts.—Experiments in which 10 grams of various salts
were added showed them to be without effect. The results were as follows:
—
Salt present — AmCl Am2SO4 MgCl2
Stannous chloride required 21.6 c.c. 21.6 c.c. 21.6 c.c. 21.6 c.c.
Salt present CaCl2 FeCl2 Al2Cl6
Stannous chloride required 21.8 c.c. 21.6 c.c. 21.6 c.c.
Effect of Varying Iron.—Titrating a solution (with 20 c.c. of hydrochloric
acid) measuring 50 c.c., and kept boiling, the quantity of stannous chloride
solution required is practically proportional to the iron present.
Ferric chloride added 1 c.c. 10 c.c. 20 c.c. 50 c.c. 100 c.c.
Stannous chloride required 1.1 " 10.5 " 20.6 " 51.4 " 102.6 "
The student, having practised some of the above experiments, may proceed
to the assay of an iron ore.
Determination of Iron in Brown Iron Ore.—Weigh up 1 gram of the
dried and powdered ore, calcine in the cover of a platinum crucible, and
dissolve up in an evaporating dish[69] with 20 c.c. of strong hydrochloric
acid. When solution is complete, dilute to 50 c.c. after replacing any acid
that may have been evaporated. Boil, and run in the stannous chloride
solution until the colour is faintly yellow; boil again, and continue the
addition of the stannous chloride solution, stirring continuously until the
solution appears colourless. Note the quantity of the stannous chloride
solution required. Suppose this to be 59 c.c. Take 60 c.c. of the standard
hydrochloric acid were present, and the bulk was 50 c.c.
Strong sulphuric acid present — c.c. 3 c.c. 5 c.c. 10 c.c.
Stannous chloride required 21.6 " 22.3 " 22.9 " 23.1 "
This interference of strong sulphuric acid may be completely counteracted
by somewhat modifying the mode of working. Another experiment, like the
last of this series, required 21.6 c.c.
Effect of Foreign Salts.—Experiments in which 10 grams of various salts
were added showed them to be without effect. The results were as follows:
—
Salt present — AmCl Am2SO4 MgCl2
Stannous chloride required 21.6 c.c. 21.6 c.c. 21.6 c.c. 21.6 c.c.
Salt present CaCl2 FeCl2 Al2Cl6
Stannous chloride required 21.8 c.c. 21.6 c.c. 21.6 c.c.
Effect of Varying Iron.—Titrating a solution (with 20 c.c. of hydrochloric
acid) measuring 50 c.c., and kept boiling, the quantity of stannous chloride
solution required is practically proportional to the iron present.
Ferric chloride added 1 c.c. 10 c.c. 20 c.c. 50 c.c. 100 c.c.
Stannous chloride required 1.1 " 10.5 " 20.6 " 51.4 " 102.6 "
The student, having practised some of the above experiments, may proceed
to the assay of an iron ore.
Determination of Iron in Brown Iron Ore.—Weigh up 1 gram of the
dried and powdered ore, calcine in the cover of a platinum crucible, and
dissolve up in an evaporating dish[69] with 20 c.c. of strong hydrochloric
acid. When solution is complete, dilute to 50 c.c. after replacing any acid
that may have been evaporated. Boil, and run in the stannous chloride
solution until the colour is faintly yellow; boil again, and continue the
addition of the stannous chloride solution, stirring continuously until the
solution appears colourless. Note the quantity of the stannous chloride
solution required. Suppose this to be 59 c.c. Take 60 c.c. of the standard
Page 315
ferric chloride solution, add 20 c.c. of hydrochloric acid, boil and titrate in
the same way as before. Suppose this to require 61 c.c. Then as 61 is
equivalent to 60 of the iron solution, 59 is equivalent to 58.13.[70] This
gives the percentage. It is not necessary to standardise the stannous chloride
solution in this way with each sample assayed, the ratio 61: 60 would serve
for a whole batch of samples; but the standardising should be repeated at
least once each day.
COLORIMETRIC METHOD.
This method is valuable for the determination of small quantities of iron
present as impurities in other metals or ores. It is based on the red
coloration developed by the action of potassic sulphocyanate on acid
solutions of ferric salts.
Standard Ferric Chloride Solution.—Take 1 c.c. of the ferric chloride
solution used for standardising the stannous chloride solution, add 2 c.c. of
dilute hydrochloric acid, and dilute to 1 litre with water. 1 c.c. = 0.01
milligram.
Solution of Potassic Sulphocyanate.—Dissolve 60 grams of the salt in
water, and dilute to a litre. It should be colourless. Use 10 c.c. for each test.
The quantity of the substance to be weighed for the assay should not
contain more than a milligram of iron; consequently, if the ore contain more
than 0.1 per cent. of that metal, less than a gram of it must be taken.
The method is as follows:—Weigh up 1 gram of the substance and dissolve
in a suitable acid; dilute; and add permanganate of potash solution until
tinted. Boil for some time and dilute to 100 c.c. Take a couple of Nessler
tubes, holding over 100 c.c., but marked at 50 c.c.; label them "1" and "2";
and into each put 10 c.c. of the potassic sulphocyanate solution and 2 c.c. of
dilute hydrochloric acid. The solutions should be colourless. To "1" add 10
c.c. of the assay solution, and dilute to the 50 c.c. mark. To the other add
water, but only to within 5 or 10 c.c. of this mark. Now run in the standard
ferric chloride solution from a small burette, 1 c.c. at a time, stirring after
each addition till the colour is nearly equal to that of the assay (No. 1). At
this stage bring the solution to the same level by diluting, and make a
the same way as before. Suppose this to require 61 c.c. Then as 61 is
equivalent to 60 of the iron solution, 59 is equivalent to 58.13.[70] This
gives the percentage. It is not necessary to standardise the stannous chloride
solution in this way with each sample assayed, the ratio 61: 60 would serve
for a whole batch of samples; but the standardising should be repeated at
least once each day.
COLORIMETRIC METHOD.
This method is valuable for the determination of small quantities of iron
present as impurities in other metals or ores. It is based on the red
coloration developed by the action of potassic sulphocyanate on acid
solutions of ferric salts.
Standard Ferric Chloride Solution.—Take 1 c.c. of the ferric chloride
solution used for standardising the stannous chloride solution, add 2 c.c. of
dilute hydrochloric acid, and dilute to 1 litre with water. 1 c.c. = 0.01
milligram.
Solution of Potassic Sulphocyanate.—Dissolve 60 grams of the salt in
water, and dilute to a litre. It should be colourless. Use 10 c.c. for each test.
The quantity of the substance to be weighed for the assay should not
contain more than a milligram of iron; consequently, if the ore contain more
than 0.1 per cent. of that metal, less than a gram of it must be taken.
The method is as follows:—Weigh up 1 gram of the substance and dissolve
in a suitable acid; dilute; and add permanganate of potash solution until
tinted. Boil for some time and dilute to 100 c.c. Take a couple of Nessler
tubes, holding over 100 c.c., but marked at 50 c.c.; label them "1" and "2";
and into each put 10 c.c. of the potassic sulphocyanate solution and 2 c.c. of
dilute hydrochloric acid. The solutions should be colourless. To "1" add 10
c.c. of the assay solution, and dilute to the 50 c.c. mark. To the other add
water, but only to within 5 or 10 c.c. of this mark. Now run in the standard
ferric chloride solution from a small burette, 1 c.c. at a time, stirring after
each addition till the colour is nearly equal to that of the assay (No. 1). At
this stage bring the solution to the same level by diluting, and make a
Page 316
further addition of the standard ferric chloride solution till the colours
correspond. The amount of iron will be the same in each tube; that in the
standard may be known by reading off the volume from the burette and
multiplying by 0.01 milligram.
If the 10 c.c. of the assay solution gave a colour requiring more than 5 or 6
c.c. of the standard ferric chloride solution, repeat the determination, taking
a smaller proportion.
The effect of varying conditions on the assay will be seen from the
following experiments:—
Effect of Varying Temperature.—The effect of increase of temperature is
to lessen the colour; in fact, by boiling, the colour can be entirely removed.
All assays are best carried out in the cold.
1 c.c. at 15° would only show the colour of 0.75 c.c. at 45°
2 " " " 1.75 "
5 " " " 4.0 "
Effect of Time.—The effect of increase of time is to increase the colour, as
will be seen from the following experiments:—
2c.c. on standing 10 minutes became equal to 2.25c.c.
2 " 20 " 2.75"
2 " 40 " 3.00"
Effect of Free Acid.—If no acid at all be present, the sulphocyanate of
potassium solution removes the colour it first produces, so that a certain
amount of acid is necessary to develop the colour. The use of a large excess
has a tendency to increase the colour produced.
5 c.c. nitric acid (sp. g. 1.4) read 3.7 c.c. instead of 2 c.c. with the dilute
acid.
5 c.c. sulphuric acid (sp. g. 1.32) read 2.2 c.c. instead of 2 c.c. with the
dilute acid.
correspond. The amount of iron will be the same in each tube; that in the
standard may be known by reading off the volume from the burette and
multiplying by 0.01 milligram.
If the 10 c.c. of the assay solution gave a colour requiring more than 5 or 6
c.c. of the standard ferric chloride solution, repeat the determination, taking
a smaller proportion.
The effect of varying conditions on the assay will be seen from the
following experiments:—
Effect of Varying Temperature.—The effect of increase of temperature is
to lessen the colour; in fact, by boiling, the colour can be entirely removed.
All assays are best carried out in the cold.
1 c.c. at 15° would only show the colour of 0.75 c.c. at 45°
2 " " " 1.75 "
5 " " " 4.0 "
Effect of Time.—The effect of increase of time is to increase the colour, as
will be seen from the following experiments:—
2c.c. on standing 10 minutes became equal to 2.25c.c.
2 " 20 " 2.75"
2 " 40 " 3.00"
Effect of Free Acid.—If no acid at all be present, the sulphocyanate of
potassium solution removes the colour it first produces, so that a certain
amount of acid is necessary to develop the colour. The use of a large excess
has a tendency to increase the colour produced.
5 c.c. nitric acid (sp. g. 1.4) read 3.7 c.c. instead of 2 c.c. with the dilute
acid.
5 c.c. sulphuric acid (sp. g. 1.32) read 2.2 c.c. instead of 2 c.c. with the
dilute acid.
Page 317
5 c.c. hydrochloric acid (sp. g. 1.16) read 2.5 c.c. instead of 2 c.c. with the
dilute acid.
Effect of Foreign Metals.—Lead, mercury, cadmium, bismuth, arsenic, tin,
antimony, nickel, cobalt, manganese, aluminium, zinc, strontium, barium,
calcium, magnesium, sodium, or potassium, when separately present in
quantities of from 100 to 200 times the weight of iron present, do not
interfere if they have previously been brought to their highest oxidised
condition by boiling with nitric acid or by treating with permanganate.
Arsenic and phosphoric acids interfere unless an excess of free hydrochloric
or other acid is present. Oxalic acid (but not tartaric acid) in minute
quantities destroys the colour. Nitrous acid strikes a red colour with the
sulphocyanate of potassium; consequently, when nitric acid has been used
in excess, high results may be obtained. Copper and some other metals
interfere, so that in most cases it is advisable to concentrate the iron before
estimating it. A blank experiment should always be made with the reagents
used in order to determine the iron, if any, introduced during the solution,
&c., of the substance assayed.
Determination of Iron in Metallic Copper.—This may be most
conveniently done during the estimation of the arsenic. The small quantity
of white flocculent precipitate which may be observed in the acetic acid
solution before titrating, contains the whole of the iron as ferric arsenate. It
should be filtered off, dissolved in 10 c.c. of dilute hydrochloric acid, and
diluted to 100 c.c.; 10 c.c. of this may be taken for the estimation. For
example: 10 grams of copper were taken, and the iron estimated; 3.0 c.c. of
standard ferric chloride solution were used, equivalent to 0.03 milligram of
iron; this multiplied by 10 (because only 1/10th of the sample was taken)
gives 0.3 milligram as the iron in 10 grams of copper. This equals 0.003 per
cent.
In a series of experiments with this method working on 10-gram lots of
copper, to which known quantities of iron had been added, the following
were the results:—
Iron present 0.015% 0.070% 0.100% 0.495%
Iron found 0.015" 0.061" 0.087" 0.522"
dilute acid.
Effect of Foreign Metals.—Lead, mercury, cadmium, bismuth, arsenic, tin,
antimony, nickel, cobalt, manganese, aluminium, zinc, strontium, barium,
calcium, magnesium, sodium, or potassium, when separately present in
quantities of from 100 to 200 times the weight of iron present, do not
interfere if they have previously been brought to their highest oxidised
condition by boiling with nitric acid or by treating with permanganate.
Arsenic and phosphoric acids interfere unless an excess of free hydrochloric
or other acid is present. Oxalic acid (but not tartaric acid) in minute
quantities destroys the colour. Nitrous acid strikes a red colour with the
sulphocyanate of potassium; consequently, when nitric acid has been used
in excess, high results may be obtained. Copper and some other metals
interfere, so that in most cases it is advisable to concentrate the iron before
estimating it. A blank experiment should always be made with the reagents
used in order to determine the iron, if any, introduced during the solution,
&c., of the substance assayed.
Determination of Iron in Metallic Copper.—This may be most
conveniently done during the estimation of the arsenic. The small quantity
of white flocculent precipitate which may be observed in the acetic acid
solution before titrating, contains the whole of the iron as ferric arsenate. It
should be filtered off, dissolved in 10 c.c. of dilute hydrochloric acid, and
diluted to 100 c.c.; 10 c.c. of this may be taken for the estimation. For
example: 10 grams of copper were taken, and the iron estimated; 3.0 c.c. of
standard ferric chloride solution were used, equivalent to 0.03 milligram of
iron; this multiplied by 10 (because only 1/10th of the sample was taken)
gives 0.3 milligram as the iron in 10 grams of copper. This equals 0.003 per
cent.
In a series of experiments with this method working on 10-gram lots of
copper, to which known quantities of iron had been added, the following
were the results:—
Iron present 0.015% 0.070% 0.100% 0.495%
Iron found 0.015" 0.061" 0.087" 0.522"
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When no arsenic is present in the copper, the iron can be separated by
fractionally precipitating with sodic carbonate, dissolving in ammonia, and
filtering off the ferric hydrate. Coppers generally carry more iron the less
arsenic they contain.
Determination of Iron in Metallic Zinc.—Dissolve 1 gram of zinc in 10
c.c. of dilute hydrochloric acid, adding a drop or two of nitric acid towards
the end to effect complete solution. Boil, dilute, and tint with the
permanganate of potassium solution; boil till colourless, and dilute to 100
c.c. Take 10 c.c. for the determination. Make a blank experiment by boiling
10 c.c. of dilute hydrochloric acid with a drop or two of nitric acid; add a
similar quantity of the permanganate of potassium solution, boiling, &c., as
before. The quantity of iron in zinc varies from less than 0.005 to more than
2.0 per cent. When 1 gram is taken and worked as above, each c.c. of ferric
chloride solution required indicates 0.01 per cent. of iron.
Determination of Iron in Metallic Tin.—Cover 1 gram of tin with 5 c.c.
of hydrochloric acid, add 1 c.c. of nitric acid, and evaporate to dryness.
Take up with 2 c.c. of dilute hydrochloric acid, add 10 c.c. of the potassic
sulphocyanate solution, and make up to 50 c.c. Probably the colour
developed will be brown instead of red owing to the presence of copper; in
this case, add to the standard as much copper as the assay is known to
contain (which must have previously been determined; see Copper); the
titration is then carried out in the usual way.
Or the iron may be separated from the copper in the tin by the following
process:—Dissolve 5 grams of metal in 30 c.c. of hydrochloric acid and 5
c.c. of nitric acid, and evaporate to dryness. Take up with 5 c.c. of dilute
hydrochloric acid, add 10 grams of potash dissolved in 30 c.c. of water, and
warm till the tin is dissolved. Pass sulphuretted hydrogen, boil, cool, and
filter. The iron and copper will be in the precipitate. They are separated in
the ordinary manner.
PRACTICAL EXERCISES.
1. Calculate from the following determinations the percentages of ferrous,
ferric, and total iron in the sample of ore used.
fractionally precipitating with sodic carbonate, dissolving in ammonia, and
filtering off the ferric hydrate. Coppers generally carry more iron the less
arsenic they contain.
Determination of Iron in Metallic Zinc.—Dissolve 1 gram of zinc in 10
c.c. of dilute hydrochloric acid, adding a drop or two of nitric acid towards
the end to effect complete solution. Boil, dilute, and tint with the
permanganate of potassium solution; boil till colourless, and dilute to 100
c.c. Take 10 c.c. for the determination. Make a blank experiment by boiling
10 c.c. of dilute hydrochloric acid with a drop or two of nitric acid; add a
similar quantity of the permanganate of potassium solution, boiling, &c., as
before. The quantity of iron in zinc varies from less than 0.005 to more than
2.0 per cent. When 1 gram is taken and worked as above, each c.c. of ferric
chloride solution required indicates 0.01 per cent. of iron.
Determination of Iron in Metallic Tin.—Cover 1 gram of tin with 5 c.c.
of hydrochloric acid, add 1 c.c. of nitric acid, and evaporate to dryness.
Take up with 2 c.c. of dilute hydrochloric acid, add 10 c.c. of the potassic
sulphocyanate solution, and make up to 50 c.c. Probably the colour
developed will be brown instead of red owing to the presence of copper; in
this case, add to the standard as much copper as the assay is known to
contain (which must have previously been determined; see Copper); the
titration is then carried out in the usual way.
Or the iron may be separated from the copper in the tin by the following
process:—Dissolve 5 grams of metal in 30 c.c. of hydrochloric acid and 5
c.c. of nitric acid, and evaporate to dryness. Take up with 5 c.c. of dilute
hydrochloric acid, add 10 grams of potash dissolved in 30 c.c. of water, and
warm till the tin is dissolved. Pass sulphuretted hydrogen, boil, cool, and
filter. The iron and copper will be in the precipitate. They are separated in
the ordinary manner.
PRACTICAL EXERCISES.
1. Calculate from the following determinations the percentages of ferrous,
ferric, and total iron in the sample of ore used.
Page 319
1 gram of ore dissolved and titrated required 26.7 c.c. of bichromate of
potassium solution.
1 gram of ore dissolved, reduced, and titrated required 43.5 c.c. of
bichromate of potassium solution.
Standard = 1.014.
2. One gram of an ore contained 0.307 gram of ferrous iron and 0.655 gram
of total iron. The iron existing as oxide, what are the percentages of ferrous
oxide (FeO) and ferric oxide (Fe2O3) in the ore?
3. One gram of brown iron ore dissolved in hydrochloric acid required 59.2
c.c. of stannous chloride (standard = 0.930). Another gram dissolved in acid
and titrated with "permanganate" required 8.2 c.c. (standard = 0.4951).
Calculate the percentages of ferrous, ferric, and total iron.
4. Another gram of the same ore, roasted, dissolved and titrated with
stannous chloride, required 63.5 c.c. To what extent does this result confirm
the others?
5. Two grams of a metal were dissolved and diluted to 100 c.c. Five c.c.
were taken for a colorimetric determination, and required 4.5 c.c. of the
standard ferric chloride solution. What is the percentage of iron in the
metal?
NICKEL.
Nickel and cobalt are closely related in their chemical properties, and may
best be considered together. Nickel is the commoner of the two, and is met
with in commerce alloyed with copper and zinc as German silver; as also in
the coinage of the United States and on the Continent. It is used for plating
polished iron and steel goods, forming a coating little liable to rust and
taking a good polish. The ores of nickel are not very common. Kupfernickel
and chloanthite are arsenides of nickel with, generally, more or less iron and
cobalt. Noumeite and garnierite are hydrated silicates of nickel and
magnesia. The chief sources of nickel are these silicates, which are found in
large quantity in New Caledonia; and a pyrites found in Norway, containing
three or four per cent. of the metal. In smaller quantities it is more widely
potassium solution.
1 gram of ore dissolved, reduced, and titrated required 43.5 c.c. of
bichromate of potassium solution.
Standard = 1.014.
2. One gram of an ore contained 0.307 gram of ferrous iron and 0.655 gram
of total iron. The iron existing as oxide, what are the percentages of ferrous
oxide (FeO) and ferric oxide (Fe2O3) in the ore?
3. One gram of brown iron ore dissolved in hydrochloric acid required 59.2
c.c. of stannous chloride (standard = 0.930). Another gram dissolved in acid
and titrated with "permanganate" required 8.2 c.c. (standard = 0.4951).
Calculate the percentages of ferrous, ferric, and total iron.
4. Another gram of the same ore, roasted, dissolved and titrated with
stannous chloride, required 63.5 c.c. To what extent does this result confirm
the others?
5. Two grams of a metal were dissolved and diluted to 100 c.c. Five c.c.
were taken for a colorimetric determination, and required 4.5 c.c. of the
standard ferric chloride solution. What is the percentage of iron in the
metal?
NICKEL.
Nickel and cobalt are closely related in their chemical properties, and may
best be considered together. Nickel is the commoner of the two, and is met
with in commerce alloyed with copper and zinc as German silver; as also in
the coinage of the United States and on the Continent. It is used for plating
polished iron and steel goods, forming a coating little liable to rust and
taking a good polish. The ores of nickel are not very common. Kupfernickel
and chloanthite are arsenides of nickel with, generally, more or less iron and
cobalt. Noumeite and garnierite are hydrated silicates of nickel and
magnesia. The chief sources of nickel are these silicates, which are found in
large quantity in New Caledonia; and a pyrites found in Norway, containing
three or four per cent. of the metal. In smaller quantities it is more widely
Page 320
distributed, being frequently met with in copper ores; consequently,
commercial copper is rarely free from it.
Nickel is readily soluble in moderately concentrated nitric acid. Its salts are
mostly green, and soluble in excess of ammonia, forming blue solutions; in
these respects it resembles copper. The acid solutions, however, are not
precipitated by sulphuretted hydrogen, although in alkaline solutions a
black sulphide is formed which is insoluble in dilute hydrochloric acid. If
the sulphide is formed in a solution containing much free ammonia, the
precipitation is incomplete, some sulphide remaining in the solution and
colouring it dark brown. These reactions serve to distinguish and separate
nickel from other metals, except cobalt. If the separated sulphide be heated
in a borax bead, the colour obtained will be a sherry brown in the outer
flame, and grey or colourless in the inner flame if nickel only is present. In
the presence of cobalt these colours are masked by the intense and
characteristic blue yielded in both flames by that metal.
DRY ASSAY.
The dry assay of nickel (cobalt being at the same time determined) is based
on the formation of a speise which will carry the cobalt, nickel, copper, and
some of the iron of the ore in combination with arsenic. A speise of this
kind, fused and exposed at a red heat to air, first loses arsenide of iron by
oxidation. It is only when the iron has been oxidised that the arsenide of
cobalt begins to be attacked; and when the removal of the cobalt is
complete, the nickel commences to pass into the slag, the copper being left
till last. The changes are rendered evident by fusion in contact with borax.
The process is as follows:—Weigh up 5 grams of the ore, and calcine
thoroughly on a roasting dish in the muffle. Rub up with some anthracite,
and re-roast. Mix intimately with from 3 to 5 grams of metallic arsenic, and
heat in a small covered clay crucible at dull redness in a muffle until no
more fumes of arsenic come off (about 15 minutes). Take out the crucible,
and inject a mixture of 20 grams of carbonate of soda, 5 grams of flour, and
2 grams of fused borax. Place in the wind furnace, and raise the temperature
gradually until the charge is in a state of tranquil fusion. Pour; when cold,
detach the button of speise, and weigh.
commercial copper is rarely free from it.
Nickel is readily soluble in moderately concentrated nitric acid. Its salts are
mostly green, and soluble in excess of ammonia, forming blue solutions; in
these respects it resembles copper. The acid solutions, however, are not
precipitated by sulphuretted hydrogen, although in alkaline solutions a
black sulphide is formed which is insoluble in dilute hydrochloric acid. If
the sulphide is formed in a solution containing much free ammonia, the
precipitation is incomplete, some sulphide remaining in the solution and
colouring it dark brown. These reactions serve to distinguish and separate
nickel from other metals, except cobalt. If the separated sulphide be heated
in a borax bead, the colour obtained will be a sherry brown in the outer
flame, and grey or colourless in the inner flame if nickel only is present. In
the presence of cobalt these colours are masked by the intense and
characteristic blue yielded in both flames by that metal.
DRY ASSAY.
The dry assay of nickel (cobalt being at the same time determined) is based
on the formation of a speise which will carry the cobalt, nickel, copper, and
some of the iron of the ore in combination with arsenic. A speise of this
kind, fused and exposed at a red heat to air, first loses arsenide of iron by
oxidation. It is only when the iron has been oxidised that the arsenide of
cobalt begins to be attacked; and when the removal of the cobalt is
complete, the nickel commences to pass into the slag, the copper being left
till last. The changes are rendered evident by fusion in contact with borax.
The process is as follows:—Weigh up 5 grams of the ore, and calcine
thoroughly on a roasting dish in the muffle. Rub up with some anthracite,
and re-roast. Mix intimately with from 3 to 5 grams of metallic arsenic, and
heat in a small covered clay crucible at dull redness in a muffle until no
more fumes of arsenic come off (about 15 minutes). Take out the crucible,
and inject a mixture of 20 grams of carbonate of soda, 5 grams of flour, and
2 grams of fused borax. Place in the wind furnace, and raise the temperature
gradually until the charge is in a state of tranquil fusion. Pour; when cold,
detach the button of speise, and weigh.
Page 321
Weigh out carefully a portion of about 1 gram of it. Place a shallow clay
dish in the muffle, and heat it to bright redness; then add about 1.5 gram of
borax glass wrapped in a piece of tissue paper; when this has fused, drop
the piece of speise into it. Close the muffle until the speise has melted,
which should be almost at once. The arsenide of iron will oxidise first, and
when this has ceased the surface of the button brightens. Remove it from
the muffle, and quench in water as soon as the button has solidified. The
borax should be coloured slightly blue. Weigh: the loss is the arsenide of
iron. Repeat the operation with the weighed button on another dish, using
rather less borax. Continue the scorification until a film, green when cold,
floating on the surface of the button shows that the nickel is beginning to
oxidise. Cool, separate, and weigh the button as before. The loss is the
arsenide of cobalt.
If copper is absent, the speise is now arsenide of nickel.
The weight of nickel corresponding to the arsenide got is calculated by
multiplying by 0.607; and, similarly, the weight of the cobalt is ascertained
by multiplying the loss in the last scorification by 0.615.[71] It must be
remembered that the nickel and cobalt so obtained are derived from a
fraction only of the speise yielded by the ore taken, so that the results must
be multiplied by the weight of the whole of the speise, and divided by the
weight of the fragment used in the determination. As an example, suppose 5
grams of ore gave 3.3 grams of speise, and 1.1 gram of this gave 0.8 gram
of nickel arsenide. Then—
dish in the muffle, and heat it to bright redness; then add about 1.5 gram of
borax glass wrapped in a piece of tissue paper; when this has fused, drop
the piece of speise into it. Close the muffle until the speise has melted,
which should be almost at once. The arsenide of iron will oxidise first, and
when this has ceased the surface of the button brightens. Remove it from
the muffle, and quench in water as soon as the button has solidified. The
borax should be coloured slightly blue. Weigh: the loss is the arsenide of
iron. Repeat the operation with the weighed button on another dish, using
rather less borax. Continue the scorification until a film, green when cold,
floating on the surface of the button shows that the nickel is beginning to
oxidise. Cool, separate, and weigh the button as before. The loss is the
arsenide of cobalt.
If copper is absent, the speise is now arsenide of nickel.
The weight of nickel corresponding to the arsenide got is calculated by
multiplying by 0.607; and, similarly, the weight of the cobalt is ascertained
by multiplying the loss in the last scorification by 0.615.[71] It must be
remembered that the nickel and cobalt so obtained are derived from a
fraction only of the speise yielded by the ore taken, so that the results must
be multiplied by the weight of the whole of the speise, and divided by the
weight of the fragment used in the determination. As an example, suppose 5
grams of ore gave 3.3 grams of speise, and 1.1 gram of this gave 0.8 gram
of nickel arsenide. Then—
Page 322
0.8×0.607 = 0.4856gram of nickel
0.4856×3.3/1.1 = 1.456gram of nickel
And this being obtained from 5 grams of ore is equivalent to 29.12 per cent.
When copper is also present, weigh up accurately about 0.5 gram of gold,
and place it on the scorifier with the button of nickel and copper arsenide,
using borax as before. Scorify until the button shows the bluish-green
colour of a fused gold-copper alloy. Then cool, and weigh the button of
copper and gold. The increase in weight of the gold button gives the copper
as metal. The weight of the copper multiplied by 1.395 is the weight of the
copper arsenide (Cu3As) present. The difference will be the nickel arsenide.
The student should enter the weighings in his book as follows:
Ore taken —grams
Speise got —"
Speise taken —grams
Arsenides ofcobalt, nickel, and copper —"
" nickel and copper —"
Gold added —"
Gold and copper got —"
Showing Cobalt —per cent.
Nickel —"
Copper —"
WET METHODS.
Solution and Separation.—Two or three grams of a rich ore, or 5 to 10
grams if poor, are taken for the assay. If much arsenic is present (as is
usually the case), the ore must be calcined before attacking with acids.
Transfer to a flask; and boil, first with hydrochloric acid until the oxides are
dissolved, and then with the help of nitric acid, until nothing metalliferous
is left. Dilute, nearly neutralise with soda, and separate the iron as basic
acetate,[72] as described in page 233. Through the filtrate pass sulphuretted
hydrogen till saturated. Allow to settle (best overnight), filter, and wash.
0.4856×3.3/1.1 = 1.456gram of nickel
And this being obtained from 5 grams of ore is equivalent to 29.12 per cent.
When copper is also present, weigh up accurately about 0.5 gram of gold,
and place it on the scorifier with the button of nickel and copper arsenide,
using borax as before. Scorify until the button shows the bluish-green
colour of a fused gold-copper alloy. Then cool, and weigh the button of
copper and gold. The increase in weight of the gold button gives the copper
as metal. The weight of the copper multiplied by 1.395 is the weight of the
copper arsenide (Cu3As) present. The difference will be the nickel arsenide.
The student should enter the weighings in his book as follows:
Ore taken —grams
Speise got —"
Speise taken —grams
Arsenides ofcobalt, nickel, and copper —"
" nickel and copper —"
Gold added —"
Gold and copper got —"
Showing Cobalt —per cent.
Nickel —"
Copper —"
WET METHODS.
Solution and Separation.—Two or three grams of a rich ore, or 5 to 10
grams if poor, are taken for the assay. If much arsenic is present (as is
usually the case), the ore must be calcined before attacking with acids.
Transfer to a flask; and boil, first with hydrochloric acid until the oxides are
dissolved, and then with the help of nitric acid, until nothing metalliferous
is left. Dilute, nearly neutralise with soda, and separate the iron as basic
acetate,[72] as described in page 233. Through the filtrate pass sulphuretted
hydrogen till saturated. Allow to settle (best overnight), filter, and wash.
Page 323
Transfer the precipitate to a beaker, and dissolve in nitric acid. Dilute with
water, pass sulphuretted hydrogen, and filter off the precipitate, if any. Boil
off the gas, add ammonia until a precipitate is formed, and then acidify
somewhat strongly with acetic acid. Pass sulphuretted hydrogen in a slow
stream until any white precipitate of zinc sulphide, there may be, begins to
darken. Filter; to the filtrate add ammonia, and pass sulphuretted hydrogen.
The precipitate will contain the nickel and cobalt as sulphides.
Where small quantities of nickel and cobalt are present, and an approximate
determination is sufficient, they can be concentrated as follows:—Remove
the copper, &c., by passing sulphuretted hydrogen through the acid solution
and filtering; add ammonia to the filtrate, and again pass sulphuretted
hydrogen; then heat nearly to boiling, and filter. Dissolve the precipitate off
the filter with dilute hydrochloric acid; the residue will contain nearly all
the nickel and cobalt as sulphides.
Separation of Nickel and Cobalt.—Dissolve the sulphides separated as
above in nitric acid; render alkaline with a solution of potash, then acidify
with acetic acid; add a concentrated solution of nitrite of potash. The liquid
after this addition must have an acid reaction. Allow to stand for 24 hours in
a warm place. Filter off the yellow precipitate of nitrite of potash and
cobalt, and wash with a 10 per cent. solution of acetate of potash. The
cobalt is determined in the precipitate in the way described under Cobalt.
The nickel is separated from the solution by boiling with sodic hydrate,
filtering, and dissolving the precipitate in nitric acid. The solution will
contain the nickel.
GRAVIMETRIC DETERMINATION.
The solution, which contains the nickel free from other metals, is heated,
and a solution of sodic hydrate added in slight excess. The precipitate is
filtered off, washed with boiling water, dried, ignited at a red heat, and
weighed when cold. The ignited substance is nickel oxide (NiO), and
contains 78.67 per cent. of nickel. The oxide is a green powder, readily and
completely soluble in hydrochloric acid, and without action on litmus paper.
It is very easily reduced by ignition in hydrogen to metallic nickel.
water, pass sulphuretted hydrogen, and filter off the precipitate, if any. Boil
off the gas, add ammonia until a precipitate is formed, and then acidify
somewhat strongly with acetic acid. Pass sulphuretted hydrogen in a slow
stream until any white precipitate of zinc sulphide, there may be, begins to
darken. Filter; to the filtrate add ammonia, and pass sulphuretted hydrogen.
The precipitate will contain the nickel and cobalt as sulphides.
Where small quantities of nickel and cobalt are present, and an approximate
determination is sufficient, they can be concentrated as follows:—Remove
the copper, &c., by passing sulphuretted hydrogen through the acid solution
and filtering; add ammonia to the filtrate, and again pass sulphuretted
hydrogen; then heat nearly to boiling, and filter. Dissolve the precipitate off
the filter with dilute hydrochloric acid; the residue will contain nearly all
the nickel and cobalt as sulphides.
Separation of Nickel and Cobalt.—Dissolve the sulphides separated as
above in nitric acid; render alkaline with a solution of potash, then acidify
with acetic acid; add a concentrated solution of nitrite of potash. The liquid
after this addition must have an acid reaction. Allow to stand for 24 hours in
a warm place. Filter off the yellow precipitate of nitrite of potash and
cobalt, and wash with a 10 per cent. solution of acetate of potash. The
cobalt is determined in the precipitate in the way described under Cobalt.
The nickel is separated from the solution by boiling with sodic hydrate,
filtering, and dissolving the precipitate in nitric acid. The solution will
contain the nickel.
GRAVIMETRIC DETERMINATION.
The solution, which contains the nickel free from other metals, is heated,
and a solution of sodic hydrate added in slight excess. The precipitate is
filtered off, washed with boiling water, dried, ignited at a red heat, and
weighed when cold. The ignited substance is nickel oxide (NiO), and
contains 78.67 per cent. of nickel. The oxide is a green powder, readily and
completely soluble in hydrochloric acid, and without action on litmus paper.
It is very easily reduced by ignition in hydrogen to metallic nickel.
Page 324
Nickel is also determined by electrolysis, as follows:—The nitric acid
solution is rendered strongly ammoniacal, and placed under the electrolytic
apparatus used for the copper assay. Three cells (fig. 56), however, must be
used, coupled up for intensity, that is, with the zinc of one connected with
the copper of the next. The electrolysis is allowed to go on overnight, and in
the morning the nickel will be deposited as a bright and coherent film. A
portion of the solution is drawn off with a pipette; if it smells of ammonia,
has no blue colour, and gives no precipitate with ammonic sulphide, the
separation is complete. Wash the cylinder containing the deposited metal,
first with water and then with alcohol, as in the copper assay. Dry in the
water oven, and weigh. The increase in weight is metallic nickel.
As an example:—There was taken 1 gram of a nickel alloy used for
coinage. It was dissolved in 10 c.c. of nitric acid, and diluted to 100 c.c.
with water. The copper was then precipitated by electrolysis. It weighed
0.734 gram. The solution, after electrolysis, was treated with sulphuretted
hydrogen, and the remaining copper was thrown down as sulphide, and
estimated colorimetrically. This amounted to 3-1/2 milligrams. The filtrate
was evaporated, treated with ammonia, warmed, and filtered. The ferric
hydrate was dissolved in dilute acid, and reprecipitated, dried, ignited, and
weighed. Its weight was 0.0310 gram. The two filtrates were mixed, and
reduced in bulk to about 50 c.c.; a considerable excess of ammonia was
added, and the nickel precipitated by electrolysis. It weighed 0.2434 gram.
These quantities are equivalent to:
solution is rendered strongly ammoniacal, and placed under the electrolytic
apparatus used for the copper assay. Three cells (fig. 56), however, must be
used, coupled up for intensity, that is, with the zinc of one connected with
the copper of the next. The electrolysis is allowed to go on overnight, and in
the morning the nickel will be deposited as a bright and coherent film. A
portion of the solution is drawn off with a pipette; if it smells of ammonia,
has no blue colour, and gives no precipitate with ammonic sulphide, the
separation is complete. Wash the cylinder containing the deposited metal,
first with water and then with alcohol, as in the copper assay. Dry in the
water oven, and weigh. The increase in weight is metallic nickel.
As an example:—There was taken 1 gram of a nickel alloy used for
coinage. It was dissolved in 10 c.c. of nitric acid, and diluted to 100 c.c.
with water. The copper was then precipitated by electrolysis. It weighed
0.734 gram. The solution, after electrolysis, was treated with sulphuretted
hydrogen, and the remaining copper was thrown down as sulphide, and
estimated colorimetrically. This amounted to 3-1/2 milligrams. The filtrate
was evaporated, treated with ammonia, warmed, and filtered. The ferric
hydrate was dissolved in dilute acid, and reprecipitated, dried, ignited, and
weighed. Its weight was 0.0310 gram. The two filtrates were mixed, and
reduced in bulk to about 50 c.c.; a considerable excess of ammonia was
added, and the nickel precipitated by electrolysis. It weighed 0.2434 gram.
These quantities are equivalent to:
Page 325
Copper 73.75 per cent.
Nickel 24.34 "
Iron 2.17 "
———
100.26
VOLUMETRIC DETERMINATION.
An alkaline solution of potassium cyanide, to which a little potassium
iodide has been added, can be assayed for its strength in cyanide by titrating
with a standard solution of silver nitrate. Nickel interferes with this assay,
doing the work of its equivalent of silver; and the quantity of nickel present
can be calculated from the amount of its interference in the titration. A
volumetric assay for nickel is based on this. It has the disadvantage of all
indirect titrations in that it requires two standard solutions. On the other
hand it gives good results even under unfavourable conditions, and is
applicable in the presence of much zinc. Small quantities of cobalt will
count as so much nickel, but larger quantities make the assay unworkable.
Some of the other metals—lead for example—have no appreciable effect;
but practically the solution demands a preliminary treatment which would
result in their removal. Nevertheless it is a very satisfactory method and
makes the determination of nickel quick and comparatively easy in most
cases.
The standard solution of silver nitrate is made by dissolving 14.48 grams of
recrystallised silver nitrate in distilled water and diluting to 1 litre: 100 c.c.
of this solution are equivalent to 0.25 gram of nickel.[73]
The standard solution of potassium cyanide should be made so as to be
exactly equal to the silver nitrate solution. This can be done as follows:
Weigh up 12 grams of good potassium cyanide (95 per cent.), dissolve in
water, add 50 c.c. of a 10 per cent. solution of sodium hydrate and dilute to
1 litre. Fill one burette with this and another with the solution of silver
nitrate. Run 50 c.c. of the cyanide into a flask; add a few drops of potassium
iodide solution and titrate with the standard silver nitrate until there is a
distinct permanent yellowish turbidity. The titration is more fully described
under Cyanide, p. 165. The cyanide solution will be found rather stronger
Nickel 24.34 "
Iron 2.17 "
———
100.26
VOLUMETRIC DETERMINATION.
An alkaline solution of potassium cyanide, to which a little potassium
iodide has been added, can be assayed for its strength in cyanide by titrating
with a standard solution of silver nitrate. Nickel interferes with this assay,
doing the work of its equivalent of silver; and the quantity of nickel present
can be calculated from the amount of its interference in the titration. A
volumetric assay for nickel is based on this. It has the disadvantage of all
indirect titrations in that it requires two standard solutions. On the other
hand it gives good results even under unfavourable conditions, and is
applicable in the presence of much zinc. Small quantities of cobalt will
count as so much nickel, but larger quantities make the assay unworkable.
Some of the other metals—lead for example—have no appreciable effect;
but practically the solution demands a preliminary treatment which would
result in their removal. Nevertheless it is a very satisfactory method and
makes the determination of nickel quick and comparatively easy in most
cases.
The standard solution of silver nitrate is made by dissolving 14.48 grams of
recrystallised silver nitrate in distilled water and diluting to 1 litre: 100 c.c.
of this solution are equivalent to 0.25 gram of nickel.[73]
The standard solution of potassium cyanide should be made so as to be
exactly equal to the silver nitrate solution. This can be done as follows:
Weigh up 12 grams of good potassium cyanide (95 per cent.), dissolve in
water, add 50 c.c. of a 10 per cent. solution of sodium hydrate and dilute to
1 litre. Fill one burette with this and another with the solution of silver
nitrate. Run 50 c.c. of the cyanide into a flask; add a few drops of potassium
iodide solution and titrate with the standard silver nitrate until there is a
distinct permanent yellowish turbidity. The titration is more fully described
under Cyanide, p. 165. The cyanide solution will be found rather stronger
Page 326
than the silver nitrate; dilute it so as to get the two solutions of equal value.
For example, 51.3 c.c. of silver nitrate may have been required: then add
1.3 c.c. of water to each 50 c.c. of the cyanide solution remaining. If the full
950 c.c. are available, then add to them 24.7 c.c. of water. After mixing,
take another 50 c.c. and titrate with the silver nitrate; the two solutions
should now be exactly equal. The cyanide solution, being strongly alkaline
with soda, keeps very well; but its strength should be checked from time to
time by titrating with silver nitrate; should there be any slight inequality in
the strengths of the two solutions it is easily allowed for in the calculations.
The titration.—The solution, containing not much more than 0.1 gram of
nickel, and free from the interfering metals, must be cooled. It is next
neutralised and then made strongly alkaline with a solution of soda
(NaHO); an excess of 20 or 30 c.c. suffices. This will produce a precipitate.
The cyanide solution is now run in from a burette until the solution clears,
after which an excess of about 20 c.c. is added. It is well to use some round
number of c.c. to simplify the calculation. Add a few drops of potassium
iodide solution, and run in the standard solution of silver nitrate from a
burette. This should be done a little at a time, though somewhat rapidly, and
with constant shaking, till a permanent yellow precipitate appears. If the
addition of the cyanide did not result in a perfectly clear solution, this is
because something besides nickel is present. The residue may be filtered
off, though with a little practice the finishing-point may be detected with
certainty in the presence of a small precipitate. If the student has the
slightest doubt about a finish he should run in another 5 c.c. of the cyanide
and again finish with silver nitrate. The second result will be the same as
the first. For example, if 40 c.c. of cyanide and 30 c.c. of silver nitrate were
required at the first titration, then the 45 c.c. of cyanide in the second
titration will require 35 c.c. of silver nitrate. The difference between the
quantities of the two solutions used in each case will be 10 c.c. It is this
difference in the readings of the two burettes which measures the quantity
of nickel present. Each c.c. of the difference is equal to .0025 gram of
nickel. But if the cyanide solution is not exactly equal in strength to the
silver nitrate, the quantity of cyanide used should be calculated to its
equivalent in silver nitrate before making the subtraction.
The following experimental results illustrate the accuracy of the assay and
the effect upon it of varying conditions. A solution containing 1 gram of
For example, 51.3 c.c. of silver nitrate may have been required: then add
1.3 c.c. of water to each 50 c.c. of the cyanide solution remaining. If the full
950 c.c. are available, then add to them 24.7 c.c. of water. After mixing,
take another 50 c.c. and titrate with the silver nitrate; the two solutions
should now be exactly equal. The cyanide solution, being strongly alkaline
with soda, keeps very well; but its strength should be checked from time to
time by titrating with silver nitrate; should there be any slight inequality in
the strengths of the two solutions it is easily allowed for in the calculations.
The titration.—The solution, containing not much more than 0.1 gram of
nickel, and free from the interfering metals, must be cooled. It is next
neutralised and then made strongly alkaline with a solution of soda
(NaHO); an excess of 20 or 30 c.c. suffices. This will produce a precipitate.
The cyanide solution is now run in from a burette until the solution clears,
after which an excess of about 20 c.c. is added. It is well to use some round
number of c.c. to simplify the calculation. Add a few drops of potassium
iodide solution, and run in the standard solution of silver nitrate from a
burette. This should be done a little at a time, though somewhat rapidly, and
with constant shaking, till a permanent yellow precipitate appears. If the
addition of the cyanide did not result in a perfectly clear solution, this is
because something besides nickel is present. The residue may be filtered
off, though with a little practice the finishing-point may be detected with
certainty in the presence of a small precipitate. If the student has the
slightest doubt about a finish he should run in another 5 c.c. of the cyanide
and again finish with silver nitrate. The second result will be the same as
the first. For example, if 40 c.c. of cyanide and 30 c.c. of silver nitrate were
required at the first titration, then the 45 c.c. of cyanide in the second
titration will require 35 c.c. of silver nitrate. The difference between the
quantities of the two solutions used in each case will be 10 c.c. It is this
difference in the readings of the two burettes which measures the quantity
of nickel present. Each c.c. of the difference is equal to .0025 gram of
nickel. But if the cyanide solution is not exactly equal in strength to the
silver nitrate, the quantity of cyanide used should be calculated to its
equivalent in silver nitrate before making the subtraction.
The following experimental results illustrate the accuracy of the assay and
the effect upon it of varying conditions. A solution containing 1 gram of
Page 327
nickel sulphate (NiSO4.6H2O) in 100 c.c. was used. By a separate assay the
sulphate was found to contain 22.25 per cent. of nickel. For the sake of
simplicity the results of the experiments are stated in weights of nickel in
grams.
Effect of varying excess of Cyanide Solution.—In each experiment there
was 20 c.c. of the nickel solution, equal to .0445 gram of nickel. There were
also 10 c.c. of soda solution, 3 or 4 drops of potassium iodide and sufficient
water to bring the bulk to 100 c.c. before titrating.
Cyanide in excess 6 c.c. 4 c.c. 8 c.c. 12 c.c. 25 c.c.
Nickel found .0434 .0436.0440.0442 .0444
Although the difference between the highest and lowest of these results is
only 1 milligram, their meaning is quite obvious. The excess of cyanide
should not be less than 20 c.c.
Effect of varying the quantity of Soda.—There were two series of
experiments, one with 2 c.c. of nickel solution (= .0044 gram of nickel), the
other with 20 c.c. The conditions were as before, except that the quantity of
soda was varied.
Soda added 5 c.c. 15 c.c. 30 c.c.
Nickel found, 1st series .0037.0042 .0045
" " 2nd series .0444.0444 .0442
These show that the presence of much soda, though it has only a small
effect, is beneficial rather than otherwise. Ammonia has a bad effect, if
present in anything like the same quantities.
Effect of varying the Nickel.—In experiments with 10, 20, and 40 c.c. of
the nickel solution, the results were:—
Nickel present .0222.0445.0890
Nickel found .0220.0442.0884
Effect of Zinc.—In these experiments 20 c.c. of nickel solution (= .0445
gram of nickel), 10 c.c. of soda, 6 drops of potassium iodide and water to
sulphate was found to contain 22.25 per cent. of nickel. For the sake of
simplicity the results of the experiments are stated in weights of nickel in
grams.
Effect of varying excess of Cyanide Solution.—In each experiment there
was 20 c.c. of the nickel solution, equal to .0445 gram of nickel. There were
also 10 c.c. of soda solution, 3 or 4 drops of potassium iodide and sufficient
water to bring the bulk to 100 c.c. before titrating.
Cyanide in excess 6 c.c. 4 c.c. 8 c.c. 12 c.c. 25 c.c.
Nickel found .0434 .0436.0440.0442 .0444
Although the difference between the highest and lowest of these results is
only 1 milligram, their meaning is quite obvious. The excess of cyanide
should not be less than 20 c.c.
Effect of varying the quantity of Soda.—There were two series of
experiments, one with 2 c.c. of nickel solution (= .0044 gram of nickel), the
other with 20 c.c. The conditions were as before, except that the quantity of
soda was varied.
Soda added 5 c.c. 15 c.c. 30 c.c.
Nickel found, 1st series .0037.0042 .0045
" " 2nd series .0444.0444 .0442
These show that the presence of much soda, though it has only a small
effect, is beneficial rather than otherwise. Ammonia has a bad effect, if
present in anything like the same quantities.
Effect of varying the Nickel.—In experiments with 10, 20, and 40 c.c. of
the nickel solution, the results were:—
Nickel present .0222.0445.0890
Nickel found .0220.0442.0884
Effect of Zinc.—In these experiments 20 c.c. of nickel solution (= .0445
gram of nickel), 10 c.c. of soda, 6 drops of potassium iodide and water to
Page 328
100 c.c. were used. The excess of cyanide was purposely kept at from 10 to
15 c.c., which is hardly sufficient.
Zinc added 0 .25 gram. .5 gram.
Nickel found .0442 .0440 .0407
On increasing the excess of cyanide to over 20 c.c. and doubling the
quantity of soda, the experiment with 0.5 gram of zinc gave 0.441 gram of
nickel. Hence the titration is satisfactory in the presence of zinc provided
that not fewer than 20 or 30 c.c. of soda are used, and that the excess of
cyanide is such that not fewer than 20 or 30 c.c. of silver nitrate are required
in the titration. Moreover, these precautions should be taken whether zinc is
present or not.
Effect of other Metals.—If metals of the first and second groups are
present they should be removed by passing sulphuretted hydrogen and
filtering. If iron is present it must be removed, since ferrous salts use up
much cyanide, forming ferrocyanides, and ferric salts yield ferric hydrate,
which obscures the end reaction. Hence the sulphuretted hydrogen must be
boiled off and the iron removed as basic ferric acetate by the method
described on p. 233. If the precipitate is bulky it should be dissolved in a
little dilute acid, neutralised and again precipitated as basic acetate. The
nickel will be in the two filtrates. In the absence of manganese and cobalt
the titration may be made without further separation.
Manganese does not directly interfere, but the precipitated hydrate, which
rapidly darkens through atmospheric oxidation, obscures the end reaction. It
may be removed by passing sulphuretted hydrogen through the filtrate from
the acetate separation: sulphides of nickel, cobalt and zinc will be
precipitated, whilst manganese remains in solution: the addition of more
sodium acetate may assist the precipitation. The precipitate must be filtered
off and dissolved in nitric acid: the solution should be evaporated to
dryness. The filtrate may retain a little nickel; if so, add ammonia till
alkaline, then acidify with acetic acid and again filter; any small precipitate
obtained here should be added to that first obtained.
It is only when cobalt is present that any further separation is required.
Cobalt hydrate takes up oxygen from the air, and on adding potassium
15 c.c., which is hardly sufficient.
Zinc added 0 .25 gram. .5 gram.
Nickel found .0442 .0440 .0407
On increasing the excess of cyanide to over 20 c.c. and doubling the
quantity of soda, the experiment with 0.5 gram of zinc gave 0.441 gram of
nickel. Hence the titration is satisfactory in the presence of zinc provided
that not fewer than 20 or 30 c.c. of soda are used, and that the excess of
cyanide is such that not fewer than 20 or 30 c.c. of silver nitrate are required
in the titration. Moreover, these precautions should be taken whether zinc is
present or not.
Effect of other Metals.—If metals of the first and second groups are
present they should be removed by passing sulphuretted hydrogen and
filtering. If iron is present it must be removed, since ferrous salts use up
much cyanide, forming ferrocyanides, and ferric salts yield ferric hydrate,
which obscures the end reaction. Hence the sulphuretted hydrogen must be
boiled off and the iron removed as basic ferric acetate by the method
described on p. 233. If the precipitate is bulky it should be dissolved in a
little dilute acid, neutralised and again precipitated as basic acetate. The
nickel will be in the two filtrates. In the absence of manganese and cobalt
the titration may be made without further separation.
Manganese does not directly interfere, but the precipitated hydrate, which
rapidly darkens through atmospheric oxidation, obscures the end reaction. It
may be removed by passing sulphuretted hydrogen through the filtrate from
the acetate separation: sulphides of nickel, cobalt and zinc will be
precipitated, whilst manganese remains in solution: the addition of more
sodium acetate may assist the precipitation. The precipitate must be filtered
off and dissolved in nitric acid: the solution should be evaporated to
dryness. The filtrate may retain a little nickel; if so, add ammonia till
alkaline, then acidify with acetic acid and again filter; any small precipitate
obtained here should be added to that first obtained.
It is only when cobalt is present that any further separation is required.
Cobalt hydrate takes up oxygen from the air, and on adding potassium
Page 329
cyanide some may refuse to dissolve; and the solution itself acquires a
brown colour, which becomes deeper on standing. At this stage the cobalt is
easily separated. The solution containing the nickel and cobalt with no great
excess of acid, is made alkaline by adding 20 c.c. of soda exactly as in
preparing for a titration. So, too, the solution of cyanide is added so as to
have an excess of 20 or 30 c.c.; the solution may have a brown colour, but if
it is not quite clear it must be filtered. Then warm (boiling is not needed)
and add from 50 to 100 c.c. of bromine water. This throws down all the
nickel as black peroxide in a condition easy to filter. Filter it off and wash
with water. The precipitate can be dissolved off the filter with the greatest
ease by a little warm sulphurous acid. The filtrate and washings, boiled till
free from sulphurous acid, yield the nickel as sulphate in a clean condition.
Determination of Nickel in Nickel Sulphate Crystals.—Take 0.5 gram of
the salt, dissolve in 50 c.c. of water and add 25 c.c. of solution of soda. Run
in from a burette, say, 60 c.c. "cyanide." Add a few drops of potassium
iodide and titrate back with "silver nitrate." Suppose 15.5 c.c. of the latter is
required. Then 15.5 c.c. subtracted from 60 c.c. leaves 44.5 c.c., and since
100 c.c. = 0.25 gram of nickel, 44.5 c.c. will equal 0.11125 gram of nickel.
This in 0.5 gram of the salt equals 22.25 per cent.
Determination of Nickel in German Silver.—Weigh up 0.5 gram of the
alloy, and dissolve in a dish with 5 or 10 c.c. of dilute nitric acid. Add 5 c.c.
of dilute sulphuric acid and evaporate till all the nitric acid is removed.
Cool, take up with 50 c.c. of water, and when dissolved pass sulphuretted
hydrogen through the solution. Filter off the precipitate and wash with
water containing sulphuretted hydrogen and dilute sulphuric acid. Boil
down the filtrate and washings to get rid of the excess of the gas; add some
nitric acid and continue the boiling. Cool, neutralise the excess of acid with
soda, add 1 gram of sodium acetate and boil. Filter off the precipitate which
contains the iron. The filtrate, cooled and rendered alkaline with soda, is
ready for the titration.
COBALT
Occurs less abundantly than nickel. Its chief ores are smaltite and cobaltite,
which are arsenides of cobalt, with more or less iron, nickel, and copper. It
brown colour, which becomes deeper on standing. At this stage the cobalt is
easily separated. The solution containing the nickel and cobalt with no great
excess of acid, is made alkaline by adding 20 c.c. of soda exactly as in
preparing for a titration. So, too, the solution of cyanide is added so as to
have an excess of 20 or 30 c.c.; the solution may have a brown colour, but if
it is not quite clear it must be filtered. Then warm (boiling is not needed)
and add from 50 to 100 c.c. of bromine water. This throws down all the
nickel as black peroxide in a condition easy to filter. Filter it off and wash
with water. The precipitate can be dissolved off the filter with the greatest
ease by a little warm sulphurous acid. The filtrate and washings, boiled till
free from sulphurous acid, yield the nickel as sulphate in a clean condition.
Determination of Nickel in Nickel Sulphate Crystals.—Take 0.5 gram of
the salt, dissolve in 50 c.c. of water and add 25 c.c. of solution of soda. Run
in from a burette, say, 60 c.c. "cyanide." Add a few drops of potassium
iodide and titrate back with "silver nitrate." Suppose 15.5 c.c. of the latter is
required. Then 15.5 c.c. subtracted from 60 c.c. leaves 44.5 c.c., and since
100 c.c. = 0.25 gram of nickel, 44.5 c.c. will equal 0.11125 gram of nickel.
This in 0.5 gram of the salt equals 22.25 per cent.
Determination of Nickel in German Silver.—Weigh up 0.5 gram of the
alloy, and dissolve in a dish with 5 or 10 c.c. of dilute nitric acid. Add 5 c.c.
of dilute sulphuric acid and evaporate till all the nitric acid is removed.
Cool, take up with 50 c.c. of water, and when dissolved pass sulphuretted
hydrogen through the solution. Filter off the precipitate and wash with
water containing sulphuretted hydrogen and dilute sulphuric acid. Boil
down the filtrate and washings to get rid of the excess of the gas; add some
nitric acid and continue the boiling. Cool, neutralise the excess of acid with
soda, add 1 gram of sodium acetate and boil. Filter off the precipitate which
contains the iron. The filtrate, cooled and rendered alkaline with soda, is
ready for the titration.
COBALT
Occurs less abundantly than nickel. Its chief ores are smaltite and cobaltite,
which are arsenides of cobalt, with more or less iron, nickel, and copper. It
Page 330
also occurs as arseniate in erythrine, and as oxide in asbolan or earthy
cobalt, which is essentially a wad carrying cobalt.
It is mainly used in the manufacture of smalts for imparting a blue colour to
glass and enamels. The oxide of cobalt forms coloured compounds with
many other metallic oxides. With oxide of zinc it forms "Rinman's green";
with aluminia, a blue; with magnesia, a pink. This property is taken
advantage of in the detection of substances before the blow-pipe.
The compounds of cobalt in most of their properties closely resemble those
of nickel, and the remarks as to solution and separation given for the latter
metal apply here. Solutions of cobalt are pink, whilst those of nickel are
green.
The detection of cobalt, even in very small quantity, is rendered easy by the
strong blue colour which it gives to the borax bead, both in the oxidising
and in the reducing flame. It is concentrated from the ore in the same way
as nickel, and should be separated from that metal by means of potassic
nitrite in the way described. The dry assay of cobalt has been given under
Nickel.
GRAVIMETRIC METHOD.
The yellow precipitate from the potassium nitrite, after being washed with
the acetate of potash, is washed with alcohol, dried, transferred to a
weighed porcelain crucible, and cautiously ignited with an excess of strong
sulphuric acid. The heat must not be sufficient to decompose the sulphate of
cobalt, which decomposition is indicated by a blackening of the substance
at the edges. The salt bears a low red heat without breaking up. If
blackening has occurred, moisten with sulphuric acid, and ignite again.
Cool and weigh. The substance is a mixture of the sulphates of cobalt and
potash (2CoSO4 + 3K2SO4), and contains 14.17 per cent. of cobalt.
Cobalt is also gravimetrically determined, like nickel, by electrolysis, or by
precipitation with sodic hydrate. In the latter case, the ignited oxide will be
somewhat uncertain in composition, owing to its containing an excess of
oxygen. Consequently, it is better to reduce it by igniting at a red heat in a
current of hydrogen and to weigh it as metallic cobalt.
cobalt, which is essentially a wad carrying cobalt.
It is mainly used in the manufacture of smalts for imparting a blue colour to
glass and enamels. The oxide of cobalt forms coloured compounds with
many other metallic oxides. With oxide of zinc it forms "Rinman's green";
with aluminia, a blue; with magnesia, a pink. This property is taken
advantage of in the detection of substances before the blow-pipe.
The compounds of cobalt in most of their properties closely resemble those
of nickel, and the remarks as to solution and separation given for the latter
metal apply here. Solutions of cobalt are pink, whilst those of nickel are
green.
The detection of cobalt, even in very small quantity, is rendered easy by the
strong blue colour which it gives to the borax bead, both in the oxidising
and in the reducing flame. It is concentrated from the ore in the same way
as nickel, and should be separated from that metal by means of potassic
nitrite in the way described. The dry assay of cobalt has been given under
Nickel.
GRAVIMETRIC METHOD.
The yellow precipitate from the potassium nitrite, after being washed with
the acetate of potash, is washed with alcohol, dried, transferred to a
weighed porcelain crucible, and cautiously ignited with an excess of strong
sulphuric acid. The heat must not be sufficient to decompose the sulphate of
cobalt, which decomposition is indicated by a blackening of the substance
at the edges. The salt bears a low red heat without breaking up. If
blackening has occurred, moisten with sulphuric acid, and ignite again.
Cool and weigh. The substance is a mixture of the sulphates of cobalt and
potash (2CoSO4 + 3K2SO4), and contains 14.17 per cent. of cobalt.
Cobalt is also gravimetrically determined, like nickel, by electrolysis, or by
precipitation with sodic hydrate. In the latter case, the ignited oxide will be
somewhat uncertain in composition, owing to its containing an excess of
oxygen. Consequently, it is better to reduce it by igniting at a red heat in a
current of hydrogen and to weigh it as metallic cobalt.
Page 331
PRACTICAL EXERCISES.
1. In the dry assay of an ore containing cobalt, nickel, and copper, the
following results were obtained. Calculate the percentages. Ore taken, 5
grams. Speise formed, 0.99 gram. Speise taken. 0.99 gram. Arsenides of
cobalt, nickel, and copper got, 0.75 gram. Arsenide of nickel and copper
got, 0.54 gram. Gold added, 0.5 gram. Gold and copper got, 0.61 gram.
2. Calculate the percentage composition of the following compounds:
Co2As, Ni2As, and Cu2As.
3. A sample of mispickel contains 7 per cent. cobalt. What weight of the
mixed sulphates of potash and cobalt will be obtained in a gravimetric
determination on 1 gram of the ore?
4. 0.3157 gram of metal was deposited by the electrolysis of a nickel and
cobalt solution. On dissolving in nitric acid and determining the cobalt
0.2563 gram of potassium and cobalt sulphates were got. Find the weights
of cobalt and nickel present in the deposit.
5. What should be the percentage composition of pure cobaltite, its formula
being CoAsS?
ZINC.
Zinc occurs in nature most commonly as sulphide (blende); it also occurs as
carbonate (calamine) and silicate (smithsonite). Each of these is sufficiently
abundant to be a source of the metal.
The metal is known in commerce as "spelter" when in ingots, and as sheet
zinc when rolled. It is chiefly used in the form of alloys with copper, which
are known as brasses. It is also used in the form of a thin film, to protect
iron goods from rusting—galvanised iron.
Ores of zinc, more especially blende, are met with in most lead, copper,
gold, and silver mines, in larger or small quantities scattered through the
lodes. Those ores which generally come under the notice of the assayer are
fairly rich in zinc; but alloys and metallurgical products contain it in very
varying proportions.
1. In the dry assay of an ore containing cobalt, nickel, and copper, the
following results were obtained. Calculate the percentages. Ore taken, 5
grams. Speise formed, 0.99 gram. Speise taken. 0.99 gram. Arsenides of
cobalt, nickel, and copper got, 0.75 gram. Arsenide of nickel and copper
got, 0.54 gram. Gold added, 0.5 gram. Gold and copper got, 0.61 gram.
2. Calculate the percentage composition of the following compounds:
Co2As, Ni2As, and Cu2As.
3. A sample of mispickel contains 7 per cent. cobalt. What weight of the
mixed sulphates of potash and cobalt will be obtained in a gravimetric
determination on 1 gram of the ore?
4. 0.3157 gram of metal was deposited by the electrolysis of a nickel and
cobalt solution. On dissolving in nitric acid and determining the cobalt
0.2563 gram of potassium and cobalt sulphates were got. Find the weights
of cobalt and nickel present in the deposit.
5. What should be the percentage composition of pure cobaltite, its formula
being CoAsS?
ZINC.
Zinc occurs in nature most commonly as sulphide (blende); it also occurs as
carbonate (calamine) and silicate (smithsonite). Each of these is sufficiently
abundant to be a source of the metal.
The metal is known in commerce as "spelter" when in ingots, and as sheet
zinc when rolled. It is chiefly used in the form of alloys with copper, which
are known as brasses. It is also used in the form of a thin film, to protect
iron goods from rusting—galvanised iron.
Ores of zinc, more especially blende, are met with in most lead, copper,
gold, and silver mines, in larger or small quantities scattered through the
lodes. Those ores which generally come under the notice of the assayer are
fairly rich in zinc; but alloys and metallurgical products contain it in very
varying proportions.
Page 332
Zinc itself is readily soluble in dilute acids; any residue which is left after
boiling with dilute hydrochloric or sulphuric acid consists simply of the
impurities of the metal; this is generally lead.
All zinc compounds are either soluble in, or are decomposed by, boiling
with acids, the zinc going into solution. Zinc forms only one series of salts,
and these are colourless. Their chief characteristic is solubility in an
alkaline solution, from which sulphuretted hydrogen produces a white
precipitate of zinc sulphide. Zinc is detected by dissolving the substance in
hydrochloric or nitric acid, boiling, and adding sodic hydrate in excess,
filtering, and adding ammonic sulphide to the filtrate. The precipitate
contains the zinc, which can be dissolved out by boiling with dilute
sulphuric acid, and detected by the formation of a white precipitate on the
addition of potassic ferrocyanide.
The dry assay of zinc can only be made indirectly, and is unsatisfactory.
Zinc is volatile, and at the temperature of its reduction is a gas. It is
impracticable to condense the vapour so as to weigh the metal,
consequently its amount is determined by loss. The following method gives
approximate results: Take 10 grams of the dried and powdered ore and
roast, first at a low temperature and afterwards at a higher one, with the
help of carbonate of ammonia to decompose the sulphates formed; cool and
weigh. The metals will be present as oxides. Mix with 2 grams of powdered
charcoal and charge into a black-lead crucible heated to whiteness, cover
loosely, and leave in the furnace for about a quarter of an hour. Uncover and
calcine the residue, cool and weigh. The loss in weight multiplied by 8.03
gives the percentage of zinc in the ore.
WET METHODS.
Solution and separation may be effected as follows: Treat 1 or 3 grams of
the substance with 10 or 30 c.c. of hydrochloric acid or aqua regia;
evaporate to dryness; take up with 10 c.c. of hydrochloric acid and dilute to
100 c.c.; heat nearly to boiling; saturate with sulphuretted hydrogen; filter,
and wash with water acidulated with hydrochloric acid. Boil off the
sulphuretted hydrogen and peroxidise with a few drops of nitric acid. Cool;
add caustic soda till nearly, but not quite, neutralised, and separate the iron
boiling with dilute hydrochloric or sulphuric acid consists simply of the
impurities of the metal; this is generally lead.
All zinc compounds are either soluble in, or are decomposed by, boiling
with acids, the zinc going into solution. Zinc forms only one series of salts,
and these are colourless. Their chief characteristic is solubility in an
alkaline solution, from which sulphuretted hydrogen produces a white
precipitate of zinc sulphide. Zinc is detected by dissolving the substance in
hydrochloric or nitric acid, boiling, and adding sodic hydrate in excess,
filtering, and adding ammonic sulphide to the filtrate. The precipitate
contains the zinc, which can be dissolved out by boiling with dilute
sulphuric acid, and detected by the formation of a white precipitate on the
addition of potassic ferrocyanide.
The dry assay of zinc can only be made indirectly, and is unsatisfactory.
Zinc is volatile, and at the temperature of its reduction is a gas. It is
impracticable to condense the vapour so as to weigh the metal,
consequently its amount is determined by loss. The following method gives
approximate results: Take 10 grams of the dried and powdered ore and
roast, first at a low temperature and afterwards at a higher one, with the
help of carbonate of ammonia to decompose the sulphates formed; cool and
weigh. The metals will be present as oxides. Mix with 2 grams of powdered
charcoal and charge into a black-lead crucible heated to whiteness, cover
loosely, and leave in the furnace for about a quarter of an hour. Uncover and
calcine the residue, cool and weigh. The loss in weight multiplied by 8.03
gives the percentage of zinc in the ore.
WET METHODS.
Solution and separation may be effected as follows: Treat 1 or 3 grams of
the substance with 10 or 30 c.c. of hydrochloric acid or aqua regia;
evaporate to dryness; take up with 10 c.c. of hydrochloric acid and dilute to
100 c.c.; heat nearly to boiling; saturate with sulphuretted hydrogen; filter,
and wash with water acidulated with hydrochloric acid. Boil off the
sulphuretted hydrogen and peroxidise with a few drops of nitric acid. Cool;
add caustic soda till nearly, but not quite, neutralised, and separate the iron
Page 333
as basic acetate by the method described under Iron. To the filtrate add
ammonia till alkaline, and pass sulphuretted hydrogen. Allow to settle and
decant on to a filter. Dissolve off the precipitate from the filter with hot
dilute hydrochloric acid. The solution will contain the zinc, together with
any manganese the ore contained, and, perhaps, traces of nickel and cobalt.
If the zinc is to be determined volumetrically, and manganese is present,
this latter is separated with carbonate of ammonia, as described further on;
but if a gravimetric method is used, and only small quantities of manganese
are present, it is better to proceed as if it were absent, and to subsequently
determine its amount, which should be deducted.
GRAVIMETRIC DETERMINATION.
The solution containing the zinc is contained in an evaporating dish, and
freed from sulphuretted hydrogen by boiling, and, if necessary, from an
excess of acid by evaporation. The evaporating dish must be a large one.
Cautiously add sodium carbonate to the hot, moderately dilute solution,
until the liquid is distinctly alkaline, and boil. Allow the precipitate to settle,
decant on to a filter, and wash with hot water. Dry, transfer to a porcelain
crucible (cleaning the paper as much as possible), add the ash, ignite, and
weigh. The substance weighed is oxide of zinc, which contains 80.26 per
cent. of the metal. It is a white powder, becoming yellow when heated. It
must not show an alkaline reaction when moistened. If it contains
manganese this metal will be present as sesquioxide (Mn2O3). Its amount
can be determined by dissolving in dilute acid and boiling with an excess of
sodic hydrate. The oxide of manganese will be precipitated, and can be
ignited and weighed. Its weight multiplied by 1.035 must be deducted from
the weight of oxide of zinc previously obtained. The results yielded by the
gravimetric determination are likely to be high, since the basic carbonate of
zinc frequently carries down with it more or less soda which is difficult to
wash off.
VOLUMETRIC DETERMINATION
This method is based on the facts that zinc salts in an acid solution
decompose potassium ferrocyanide, forming a white insoluble zinc
ammonia till alkaline, and pass sulphuretted hydrogen. Allow to settle and
decant on to a filter. Dissolve off the precipitate from the filter with hot
dilute hydrochloric acid. The solution will contain the zinc, together with
any manganese the ore contained, and, perhaps, traces of nickel and cobalt.
If the zinc is to be determined volumetrically, and manganese is present,
this latter is separated with carbonate of ammonia, as described further on;
but if a gravimetric method is used, and only small quantities of manganese
are present, it is better to proceed as if it were absent, and to subsequently
determine its amount, which should be deducted.
GRAVIMETRIC DETERMINATION.
The solution containing the zinc is contained in an evaporating dish, and
freed from sulphuretted hydrogen by boiling, and, if necessary, from an
excess of acid by evaporation. The evaporating dish must be a large one.
Cautiously add sodium carbonate to the hot, moderately dilute solution,
until the liquid is distinctly alkaline, and boil. Allow the precipitate to settle,
decant on to a filter, and wash with hot water. Dry, transfer to a porcelain
crucible (cleaning the paper as much as possible), add the ash, ignite, and
weigh. The substance weighed is oxide of zinc, which contains 80.26 per
cent. of the metal. It is a white powder, becoming yellow when heated. It
must not show an alkaline reaction when moistened. If it contains
manganese this metal will be present as sesquioxide (Mn2O3). Its amount
can be determined by dissolving in dilute acid and boiling with an excess of
sodic hydrate. The oxide of manganese will be precipitated, and can be
ignited and weighed. Its weight multiplied by 1.035 must be deducted from
the weight of oxide of zinc previously obtained. The results yielded by the
gravimetric determination are likely to be high, since the basic carbonate of
zinc frequently carries down with it more or less soda which is difficult to
wash off.
VOLUMETRIC DETERMINATION
This method is based on the facts that zinc salts in an acid solution
decompose potassium ferrocyanide, forming a white insoluble zinc
Page 334
compound; and that an excess of the ferrocyanide can be detected by the
brown coloration it strikes with uranium acetate. The method resembles in
its working the bichromate iron assay. The standard solution of potassium
ferrocyanide is run into a hot hydrochloric acid solution of the zinc until a
drop of the latter brought in contact with a drop of the indicator (uranium
acetate) on a white plate strikes a brown colour. The quantity of zinc in the
solution must be approximately known; run in a little less of the
ferrocyanide than is expected will be necessary; test a drop or two of the
assay, and then run in, one or two c.c. at a time, until the brown colour is
obtained. Add 5 c.c. of a standard zinc solution, equivalent in strength to the
standard "ferrocyanide," re-titrate, and finish off cautiously. Of course 5 c.c.
must be deducted from the reading on the burette. The precipitate of zinc
ferrocyanide formed in the assay solution is white; but if traces of iron are
present, it becomes bluish. If the quantity of ferrocyanide required is known
within a few c.c., the finishing point is exactly determined in the first
titration without any addition of the standard zinc solution. Unfortunately
this titration serves simply to replace the gravimetric determination, and
does not, as many volumetric processes do, lessen the necessity for a
complete separation of any other metals which are present. Most metals
give precipitates with ferrocyanide of potassium in acid solutions. If the
conditions are held to, the titration is a fairly good one, and differences in
the results of an assay will be due to error in the separation. Ferric hydrate
precipitated in a fairly strong solution of zinc will carry with it perceptible
quantities of that metal. Similarly, large quantities of copper precipitated as
sulphide by means of sulphuretted hydrogen will carry zinc with it, except
under certain nicely drawn conditions. When much copper is present it is
best separated in a nitric acid solution by electrolysis. The titration of the
zinc takes less time, and, with ordinary working, is more trustworthy than
the gravimetric method.
The standard ferrocyanide solution is made by dissolving 43.2 grams of
potassium ferrocyanide (K4FeCy6.3H2O) in water, and diluting to a litre.
One hundred c.c. are equal to 1 gram of zinc.
The standard zinc solution is made by dissolving 10 grams of pure zinc in
50 c.c. of hydrochloric acid and 100 or 200 c.c. of water, and diluting to 1
litre, or by dissolving 44.15 grams of zinc sulphate (ZnSO4.7H2O) in water
brown coloration it strikes with uranium acetate. The method resembles in
its working the bichromate iron assay. The standard solution of potassium
ferrocyanide is run into a hot hydrochloric acid solution of the zinc until a
drop of the latter brought in contact with a drop of the indicator (uranium
acetate) on a white plate strikes a brown colour. The quantity of zinc in the
solution must be approximately known; run in a little less of the
ferrocyanide than is expected will be necessary; test a drop or two of the
assay, and then run in, one or two c.c. at a time, until the brown colour is
obtained. Add 5 c.c. of a standard zinc solution, equivalent in strength to the
standard "ferrocyanide," re-titrate, and finish off cautiously. Of course 5 c.c.
must be deducted from the reading on the burette. The precipitate of zinc
ferrocyanide formed in the assay solution is white; but if traces of iron are
present, it becomes bluish. If the quantity of ferrocyanide required is known
within a few c.c., the finishing point is exactly determined in the first
titration without any addition of the standard zinc solution. Unfortunately
this titration serves simply to replace the gravimetric determination, and
does not, as many volumetric processes do, lessen the necessity for a
complete separation of any other metals which are present. Most metals
give precipitates with ferrocyanide of potassium in acid solutions. If the
conditions are held to, the titration is a fairly good one, and differences in
the results of an assay will be due to error in the separation. Ferric hydrate
precipitated in a fairly strong solution of zinc will carry with it perceptible
quantities of that metal. Similarly, large quantities of copper precipitated as
sulphide by means of sulphuretted hydrogen will carry zinc with it, except
under certain nicely drawn conditions. When much copper is present it is
best separated in a nitric acid solution by electrolysis. The titration of the
zinc takes less time, and, with ordinary working, is more trustworthy than
the gravimetric method.
The standard ferrocyanide solution is made by dissolving 43.2 grams of
potassium ferrocyanide (K4FeCy6.3H2O) in water, and diluting to a litre.
One hundred c.c. are equal to 1 gram of zinc.
The standard zinc solution is made by dissolving 10 grams of pure zinc in
50 c.c. of hydrochloric acid and 100 or 200 c.c. of water, and diluting to 1
litre, or by dissolving 44.15 grams of zinc sulphate (ZnSO4.7H2O) in water
Page 335
with 30 c.c. of hydrochloric acid, and diluting to 1 litre. One hundred c.c.
will contain 1 gram of zinc.
The uranium acetate solution is made by dissolving 0.2 gram of the salt in
100 c.c. of water.
To standardise the "ferrocyanide" measure off 50 c.c. of the standard zinc
solution into a 10 oz. beaker, dilute to 100 c.c., and heat to about 50° C. (not
to boiling). Run in 47 or 48 c.c. of the "ferrocyanide" solution from an
ordinary burette, and finish off cautiously. Fifty divided by the quantity of
"ferrocyanide" solution required gives the standard.
In assaying ores, &c., take such quantity as shall contain from 0.1 to 1 gram
of zinc, separate the zinc as sulphide, as already directed. Dissolve the
sulphide off the filter with hot dilute hydrochloric acid, which is best done
by a stream from a wash bottle. Evaporate the filtrate to a paste, add 5 c.c.
of dilute hydrochloric acid, dilute to 100 c.c. or 150 c.c., heat to about 50°
C., and titrate. Manganese, if present, counts as so much zinc, and must be
specially separated, since it is not removed by the method already given.
The following method will effect its removal. To the hydrochloric acid
solution of the zinc and manganese add sodium acetate in large excess and
pass sulphuretted hydrogen freely. Allow to settle, filter off the zinc
sulphide and wash with sulphuretted hydrogen water. The precipitate, freed
from manganese, is then dissolved in hydrochloric acid and titrated.
The following experiments show the effect of variation in the conditions of
the assay:—
Effect of Varying Temperature.—Using 20 c.c. of the standard zinc
solution, 5 c.c. of dilute hydrochloric acid, and diluting to 100 c.c.
Temperature 15° C. 30° C. 70° C. 100° C.
"Ferrocyanide" required 20.6 c.c. 20.3 c.c. 20.3 c.c. 20.3 c.c.
The solution can be heated to boiling before titrating without interfering
with the result; but it is more convenient to work with the solution at about
50° C. Cold solutions must not be used.
will contain 1 gram of zinc.
The uranium acetate solution is made by dissolving 0.2 gram of the salt in
100 c.c. of water.
To standardise the "ferrocyanide" measure off 50 c.c. of the standard zinc
solution into a 10 oz. beaker, dilute to 100 c.c., and heat to about 50° C. (not
to boiling). Run in 47 or 48 c.c. of the "ferrocyanide" solution from an
ordinary burette, and finish off cautiously. Fifty divided by the quantity of
"ferrocyanide" solution required gives the standard.
In assaying ores, &c., take such quantity as shall contain from 0.1 to 1 gram
of zinc, separate the zinc as sulphide, as already directed. Dissolve the
sulphide off the filter with hot dilute hydrochloric acid, which is best done
by a stream from a wash bottle. Evaporate the filtrate to a paste, add 5 c.c.
of dilute hydrochloric acid, dilute to 100 c.c. or 150 c.c., heat to about 50°
C., and titrate. Manganese, if present, counts as so much zinc, and must be
specially separated, since it is not removed by the method already given.
The following method will effect its removal. To the hydrochloric acid
solution of the zinc and manganese add sodium acetate in large excess and
pass sulphuretted hydrogen freely. Allow to settle, filter off the zinc
sulphide and wash with sulphuretted hydrogen water. The precipitate, freed
from manganese, is then dissolved in hydrochloric acid and titrated.
The following experiments show the effect of variation in the conditions of
the assay:—
Effect of Varying Temperature.—Using 20 c.c. of the standard zinc
solution, 5 c.c. of dilute hydrochloric acid, and diluting to 100 c.c.
Temperature 15° C. 30° C. 70° C. 100° C.
"Ferrocyanide" required 20.6 c.c. 20.3 c.c. 20.3 c.c. 20.3 c.c.
The solution can be heated to boiling before titrating without interfering
with the result; but it is more convenient to work with the solution at about
50° C. Cold solutions must not be used.
Page 336
Effect of Varying Bulk.—These were all titrated at about 50° C., and were
like the last, but with varying bulk.
Bulk 25.0 c.c. 50.0c.c. 100.0 c.c. 200.0c.c.
"Ferrocyanide" required 20.2 " 20.4" 20.3 " 20.4 "
Any ordinary variation in bulk has no effect.
Effect of Varying Hydrochloric Acid.— With 100 c.c. bulk and varying
dilute hydrochloric acid the results were:—
Acid added 0.0 c.c. 1.0 c.c. 5.0 c.c. 10.0c.c. 20.0c.c.
"Ferrocyanide" required 24.4 " 20.2" 20.3" 20.3" 20.7"
Effect of Foreign Salts.—The experiments were carried out under the same
conditions as the others. Five grams each of the following salts were added:
—
Ammonic Ammonic Sodium Sodium
Salt added
chloride. sulphate. chloride. sulphate.
"Ferrocyanide"
20.3 c.c. 20.5 c.c. 20.6 c.c. 20.4 c.c.
required
Potassium Magnesium
Salt added Nil.
Nitrate. sulphate.
"Ferrocyanide"
20.2 c.c. 20.4 c.c. 20.4 c.c.
required
In a series of experiments in which foreign metals were present to the extent
of 0.050 gram in each, with 20 c.c. of zinc solution and 5 c.c. of dilute
hydrochloric acid, those in which copper sulphate, ferrous sulphate, and
ferric chloride were used, gave (as might be expected) so strongly coloured
precipitates that the end reaction could not be recognised. The other results
were:—
"Ferrocyanide"
required.
nothing
With 20.3 c.c.
added.
like the last, but with varying bulk.
Bulk 25.0 c.c. 50.0c.c. 100.0 c.c. 200.0c.c.
"Ferrocyanide" required 20.2 " 20.4" 20.3 " 20.4 "
Any ordinary variation in bulk has no effect.
Effect of Varying Hydrochloric Acid.— With 100 c.c. bulk and varying
dilute hydrochloric acid the results were:—
Acid added 0.0 c.c. 1.0 c.c. 5.0 c.c. 10.0c.c. 20.0c.c.
"Ferrocyanide" required 24.4 " 20.2" 20.3" 20.3" 20.7"
Effect of Foreign Salts.—The experiments were carried out under the same
conditions as the others. Five grams each of the following salts were added:
—
Ammonic Ammonic Sodium Sodium
Salt added
chloride. sulphate. chloride. sulphate.
"Ferrocyanide"
20.3 c.c. 20.5 c.c. 20.6 c.c. 20.4 c.c.
required
Potassium Magnesium
Salt added Nil.
Nitrate. sulphate.
"Ferrocyanide"
20.2 c.c. 20.4 c.c. 20.4 c.c.
required
In a series of experiments in which foreign metals were present to the extent
of 0.050 gram in each, with 20 c.c. of zinc solution and 5 c.c. of dilute
hydrochloric acid, those in which copper sulphate, ferrous sulphate, and
ferric chloride were used, gave (as might be expected) so strongly coloured
precipitates that the end reaction could not be recognised. The other results
were:—
"Ferrocyanide"
required.
nothing
With 20.3 c.c.
added.
Page 337
" 0.050 gram lead (as chloride) 20.9 "
manganese (as
" 0.050 " 25.5 "
sulphate)
" 0.050 " cadmium (as sulphate) 23.5 "
" 0.050 " nickel (as sulphate) 26.2 "
Effect of Varying Zinc.—These were titrated under the usual conditions,
and gave the following results:—
Zinc added 1.0 c.c. 10.0 c.c. 20.0 c.c. 50.0 c.c. 100.0 c.c.
"Ferrocyanide" required 1.1 " 10.2 " 20.3 " 50.6 " 101.0 "
Determination of Zinc in a Sample of Brass.—Take the solution from
which the copper has been separated by electrolysis and pass sulphuretted
hydrogen until the remaining traces of copper and the lead are precipitated,
filter, boil the solution free from sulphuretted hydrogen, put in a piece of
litmus paper, and add sodic hydrate solution in slight excess; add 10 c.c. of
dilute hydrochloric acid (which should render the solution acid and clear);
warm, and titrate.
A sample of 0.5 gram of brass treated in this manner required 16.4 c.c. of
"ferrocyanide" (standard 100 c.c. = 0.9909 zinc), which equals 0.1625 gram
of zinc or 32.5 per cent.
Determination of Zinc in Blende.—Dissolve 1 gram of the dried and
powdered sample in 25 c.c. of nitric acid with the help of two or three
grams of potassium chlorate dissolved in the acid. Evaporate to complete
dryness, taking care to avoid spirting. Add 7 grams of powdered ammonium
chloride, 15 c.c. of strong ammonia and 25 c.c. of boiling water; boil for
one minute and see that the residue is all softened. Filter through a small
filter, and wash thoroughly with small quantities of a hot one per cent.
solution of ammonium chloride. Add 25 c.c. of hydrochloric acid to the
filtrate. Place in the solution some clean lead foil, say 10 or 20 square
inches. Boil gently until the solution has been colourless for three or four
minutes. Filter, wash with a little hot water; and titrate with standard
ferrocyanide.
manganese (as
" 0.050 " 25.5 "
sulphate)
" 0.050 " cadmium (as sulphate) 23.5 "
" 0.050 " nickel (as sulphate) 26.2 "
Effect of Varying Zinc.—These were titrated under the usual conditions,
and gave the following results:—
Zinc added 1.0 c.c. 10.0 c.c. 20.0 c.c. 50.0 c.c. 100.0 c.c.
"Ferrocyanide" required 1.1 " 10.2 " 20.3 " 50.6 " 101.0 "
Determination of Zinc in a Sample of Brass.—Take the solution from
which the copper has been separated by electrolysis and pass sulphuretted
hydrogen until the remaining traces of copper and the lead are precipitated,
filter, boil the solution free from sulphuretted hydrogen, put in a piece of
litmus paper, and add sodic hydrate solution in slight excess; add 10 c.c. of
dilute hydrochloric acid (which should render the solution acid and clear);
warm, and titrate.
A sample of 0.5 gram of brass treated in this manner required 16.4 c.c. of
"ferrocyanide" (standard 100 c.c. = 0.9909 zinc), which equals 0.1625 gram
of zinc or 32.5 per cent.
Determination of Zinc in Blende.—Dissolve 1 gram of the dried and
powdered sample in 25 c.c. of nitric acid with the help of two or three
grams of potassium chlorate dissolved in the acid. Evaporate to complete
dryness, taking care to avoid spirting. Add 7 grams of powdered ammonium
chloride, 15 c.c. of strong ammonia and 25 c.c. of boiling water; boil for
one minute and see that the residue is all softened. Filter through a small
filter, and wash thoroughly with small quantities of a hot one per cent.
solution of ammonium chloride. Add 25 c.c. of hydrochloric acid to the
filtrate. Place in the solution some clean lead foil, say 10 or 20 square
inches. Boil gently until the solution has been colourless for three or four
minutes. Filter, wash with a little hot water; and titrate with standard
ferrocyanide.
Page 338
Determination of Zinc in Silver Precipitate.—This precipitate contains
lead sulphate, silver, copper, iron, zinc, lime, &c. Weigh up 5 grams of the
sample, and extract with 30 c.c. of dilute sulphuric acid with the aid of heat.
Separate the copper with sulphuretted hydrogen, peroxidise the iron with a
drop or two of nitric acid, and separate as acetate. Render the filtrate
ammoniacal, pass sulphuretted hydrogen; warm, and filter. Dissolve the
precipitated zinc sulphide in dilute hydrochloric acid, evaporate, dilute, and
titrate. Silver precipitates carry about 2.5 per cent. of zinc.
GASOMETRIC METHOD.
Metallic zinc is readily soluble in dilute hydrochloric or sulphuric acid,
hydrogen being at the same time evolved.[74] The volume of the hydrogen
evolved is obviously a measure of the amount of zinc present in the metallic
state. The speed with which the reaction goes on (even in the cold) and the
insolubility of hydrogen renders this method of assay a convenient one. It is
especially applicable to the determination of the proportion of zinc in zinc
dust. The apparatus described in the chapter on gasometric method is used.
The method of working is as follows: Fill the two burettes with cold water
to a little above the zero mark, place in the bottle about 0.25 gram of the
substance to be determined, and in the inner phial or test tube 5 c.c. of
dilute sulphuric acid; cork the apparatus tightly and allow to stand for a few
minutes; then bring the water to the same level in the two burettes by
running out through the clip at the bottom. Read off the level of the liquid in
the graduated burette. Turn the bottle over sufficiently to spill the acid over
the zinc, and then run water out of the apparatus so as to keep the liquid in
the two burettes at the same level, taking care not to run it out more quickly
than the hydrogen is being generated. When the volume of gas ceases to
increase, read off the level of the liquid, deduct the reading which was
started with; the difference gives the volume of hydrogen evolved. At the
same time read off the volume of air in the "volume corrector," which must
be fixed alongside the gas burettes. Make the correction. For example: A
piece of zinc weighing 0.2835 gram was found to give 99.9 c.c. of gas at a
time when the corrector read 104 c.c.[75] Then the corrected volume is
104 : 100 :: 99.9 : x.
x = 96.0 c.c.
lead sulphate, silver, copper, iron, zinc, lime, &c. Weigh up 5 grams of the
sample, and extract with 30 c.c. of dilute sulphuric acid with the aid of heat.
Separate the copper with sulphuretted hydrogen, peroxidise the iron with a
drop or two of nitric acid, and separate as acetate. Render the filtrate
ammoniacal, pass sulphuretted hydrogen; warm, and filter. Dissolve the
precipitated zinc sulphide in dilute hydrochloric acid, evaporate, dilute, and
titrate. Silver precipitates carry about 2.5 per cent. of zinc.
GASOMETRIC METHOD.
Metallic zinc is readily soluble in dilute hydrochloric or sulphuric acid,
hydrogen being at the same time evolved.[74] The volume of the hydrogen
evolved is obviously a measure of the amount of zinc present in the metallic
state. The speed with which the reaction goes on (even in the cold) and the
insolubility of hydrogen renders this method of assay a convenient one. It is
especially applicable to the determination of the proportion of zinc in zinc
dust. The apparatus described in the chapter on gasometric method is used.
The method of working is as follows: Fill the two burettes with cold water
to a little above the zero mark, place in the bottle about 0.25 gram of the
substance to be determined, and in the inner phial or test tube 5 c.c. of
dilute sulphuric acid; cork the apparatus tightly and allow to stand for a few
minutes; then bring the water to the same level in the two burettes by
running out through the clip at the bottom. Read off the level of the liquid in
the graduated burette. Turn the bottle over sufficiently to spill the acid over
the zinc, and then run water out of the apparatus so as to keep the liquid in
the two burettes at the same level, taking care not to run it out more quickly
than the hydrogen is being generated. When the volume of gas ceases to
increase, read off the level of the liquid, deduct the reading which was
started with; the difference gives the volume of hydrogen evolved. At the
same time read off the volume of air in the "volume corrector," which must
be fixed alongside the gas burettes. Make the correction. For example: A
piece of zinc weighing 0.2835 gram was found to give 99.9 c.c. of gas at a
time when the corrector read 104 c.c.[75] Then the corrected volume is
104 : 100 :: 99.9 : x.
x = 96.0 c.c.
Page 339
100 c.c. of hydrogen at 0° C. and 760 mm. is equivalent to 0.2912 gram of
zinc; therefore the quantity of zinc found is
100 : 96 :: 0.2912 : x.
x = 0.2795 gram of zinc.
This being contained in 0.2835 gram of metal is equivalent to 98.5 per cent.
As an example of a determination in which reducing the volume of
liberated hydrogen to 0° C. and 760 mm. is avoided, the following may be
taken:—
0.2315 gram of pure zinc gave 82.1 c.c. of gas;
and the volume of air in the corrector was 103.6 c.c.
0.2835 gram of the assay gave 99.9 c.c. of gas;
and the volume of air in the corrector was 104.0 c.c.;
104 : 103.6 :: 99.9 : x.
x = 99.5 c.c.
This is the volume of gas got in the assay if measured under the same
conditions as the standard,
82.1 : 99.5 :: 0.2315 : x.
x = 0.2806.
Then 0.2835 : 0.2806 :: 100: x.
x = 98.9 per cent.
As these assays can be made quickly, it is well for the sake of greater
accuracy to make them in duplicate, and to take the mean of the readings.
One set of standardisings will do for any number of assays. The student
must carefully avoid unnecessary handling of the bottle in which the zinc is
dissolved.
Colorimetric Method.—Zinc salts being colourless, there is no
colorimetric determination.
EXAMINATION OF COMMERCIAL ZINC.
zinc; therefore the quantity of zinc found is
100 : 96 :: 0.2912 : x.
x = 0.2795 gram of zinc.
This being contained in 0.2835 gram of metal is equivalent to 98.5 per cent.
As an example of a determination in which reducing the volume of
liberated hydrogen to 0° C. and 760 mm. is avoided, the following may be
taken:—
0.2315 gram of pure zinc gave 82.1 c.c. of gas;
and the volume of air in the corrector was 103.6 c.c.
0.2835 gram of the assay gave 99.9 c.c. of gas;
and the volume of air in the corrector was 104.0 c.c.;
104 : 103.6 :: 99.9 : x.
x = 99.5 c.c.
This is the volume of gas got in the assay if measured under the same
conditions as the standard,
82.1 : 99.5 :: 0.2315 : x.
x = 0.2806.
Then 0.2835 : 0.2806 :: 100: x.
x = 98.9 per cent.
As these assays can be made quickly, it is well for the sake of greater
accuracy to make them in duplicate, and to take the mean of the readings.
One set of standardisings will do for any number of assays. The student
must carefully avoid unnecessary handling of the bottle in which the zinc is
dissolved.
Colorimetric Method.—Zinc salts being colourless, there is no
colorimetric determination.
EXAMINATION OF COMMERCIAL ZINC.
Page 340
Take 20 grams of zinc, and dissolve them in dilute nitric acid; boil, allow to
settle; filter; wash, dry; ignite the precipitate, if any, and weigh as oxide of
tin. Examine this for arsenic.
Lead.—Add ammonia and carbonate of ammonia to the liquid, and boil,
filter off the precipitate, wash with hot water. Digest the precipitate with
dilute sulphuric acid; filter, wash, and weigh the sulphate of lead.
Iron.—To the filtrate from the sulphate of lead add ammonia, and pass
sulphuretted hydrogen; digest, and filter. (Save the filtrate.) Dissolve the
precipitate in hydrochloric acid, oxidise with nitric acid, and precipitate
with ammonia. Wash, ignite, and weigh as ferric oxide. Calculate to iron.
Arsenic.—To the filtrate from the sulphide of iron add hydrochloric acid in
slight excess; filter off, and wash the precipitate. Rinse it back into the
beaker, dissolve in nitric acid, filter from the sulphur, and add ammonia, in
excess, and magnesia mixture. Filter off the ammonic-magnesic arsenate,
and wash with dilute ammonia. Dry, ignite with nitric acid, and weigh as
magnesic pyrarsenate. Calculate to arsenic, and add to that found with the
tin.
Copper.—To the filtrate from the ammonia and ammonic carbonate add
sulphuric acid in small excess, and pass sulphuretted hydrogen. Allow to
settle, filter, and wash. Rinse the precipitate into a beaker, boil with dilute
sulphuric acid, and filter. (Save the filtrate.) Dry, burn the paper with the
precipitate, treat with a drop or two of nitric acid, ignite, and weigh as
copper oxide. Calculate to copper.
Cadmium.—To the filtrate from the sulphide of copper add ammonia, so as
to nearly neutralise the excess of acid, and pass sulphuretted hydrogen.
Collect and weigh the precipitate as cadmium sulphide, as described under
Cadmium.
PRACTICAL EXERCISES.
1. What weight of hydrogen will be evolved in dissolving 1 gram of zinc in
dilute sulphuric acid?
settle; filter; wash, dry; ignite the precipitate, if any, and weigh as oxide of
tin. Examine this for arsenic.
Lead.—Add ammonia and carbonate of ammonia to the liquid, and boil,
filter off the precipitate, wash with hot water. Digest the precipitate with
dilute sulphuric acid; filter, wash, and weigh the sulphate of lead.
Iron.—To the filtrate from the sulphate of lead add ammonia, and pass
sulphuretted hydrogen; digest, and filter. (Save the filtrate.) Dissolve the
precipitate in hydrochloric acid, oxidise with nitric acid, and precipitate
with ammonia. Wash, ignite, and weigh as ferric oxide. Calculate to iron.
Arsenic.—To the filtrate from the sulphide of iron add hydrochloric acid in
slight excess; filter off, and wash the precipitate. Rinse it back into the
beaker, dissolve in nitric acid, filter from the sulphur, and add ammonia, in
excess, and magnesia mixture. Filter off the ammonic-magnesic arsenate,
and wash with dilute ammonia. Dry, ignite with nitric acid, and weigh as
magnesic pyrarsenate. Calculate to arsenic, and add to that found with the
tin.
Copper.—To the filtrate from the ammonia and ammonic carbonate add
sulphuric acid in small excess, and pass sulphuretted hydrogen. Allow to
settle, filter, and wash. Rinse the precipitate into a beaker, boil with dilute
sulphuric acid, and filter. (Save the filtrate.) Dry, burn the paper with the
precipitate, treat with a drop or two of nitric acid, ignite, and weigh as
copper oxide. Calculate to copper.
Cadmium.—To the filtrate from the sulphide of copper add ammonia, so as
to nearly neutralise the excess of acid, and pass sulphuretted hydrogen.
Collect and weigh the precipitate as cadmium sulphide, as described under
Cadmium.
PRACTICAL EXERCISES.
1. What weight of hydrogen will be evolved in dissolving 1 gram of zinc in
dilute sulphuric acid?
Page 341
2. How many c.c. would this quantity of hydrogen measure at 0° C. and 760
m.m.? (1 litre weighs 0.0896 gram).
3. 0.23 gram of zinc are found to give 77.9 c.c. of hydrogen. In another
experiment under the same conditions 80.2 c.c. are got. What weight of zinc
was used for the second experiment?
4. A sample of blende is found to contain 55 per cent. of zinc. What
percentage of zinc sulphide did the sample contain?
5. How much metallic lead would be precipitated from a solution of lead
acetate by 1 gram of zinc?
CADMIUM.
Cadmium occurs in nature as cadmium sulphide in greenockite, CdS, which
is very rare. It is widely diffused in calamine, blende, and other zinc ores,
forming, in some cases, as much as 2 or 3 per cent. of the ore. Oxide of
cadmium forms the "brown blaze" of the zinc smelters.
Sulphide of cadmium is used as a pigment (cadmium yellow); and the metal
and some of its salts are useful reagents.
The salts of cadmium closely resemble those of zinc. The hydrate, however,
is insoluble in excess of potash, and the sulphide is insoluble in dilute acids.
It forms only one series of salts.
Cadmium is detected by giving with sulphuretted hydrogen in solutions, not
too strongly acid, a yellow precipitate, which is insoluble in solutions of the
alkalies, alkaline sulphides, or cyanide of potassium.
Solution and Separation.—Substances containing cadmium are soluble in
acids. The solution is evaporated to dryness (to render any silica that may
be present insoluble) and taken up with 10 c.c. of dilute hydrochloric acid.
Dilute to 100 c.c., and pass sulphuretted hydrogen. Filter, digest the
precipitate with soda, wash, and boil with dilute sulphuric acid. Filter; the
filtrate contains the cadmium and, possibly, a small quantity of zinc, from
which it is best separated by reprecipitating with sulphuretted hydrogen.
m.m.? (1 litre weighs 0.0896 gram).
3. 0.23 gram of zinc are found to give 77.9 c.c. of hydrogen. In another
experiment under the same conditions 80.2 c.c. are got. What weight of zinc
was used for the second experiment?
4. A sample of blende is found to contain 55 per cent. of zinc. What
percentage of zinc sulphide did the sample contain?
5. How much metallic lead would be precipitated from a solution of lead
acetate by 1 gram of zinc?
CADMIUM.
Cadmium occurs in nature as cadmium sulphide in greenockite, CdS, which
is very rare. It is widely diffused in calamine, blende, and other zinc ores,
forming, in some cases, as much as 2 or 3 per cent. of the ore. Oxide of
cadmium forms the "brown blaze" of the zinc smelters.
Sulphide of cadmium is used as a pigment (cadmium yellow); and the metal
and some of its salts are useful reagents.
The salts of cadmium closely resemble those of zinc. The hydrate, however,
is insoluble in excess of potash, and the sulphide is insoluble in dilute acids.
It forms only one series of salts.
Cadmium is detected by giving with sulphuretted hydrogen in solutions, not
too strongly acid, a yellow precipitate, which is insoluble in solutions of the
alkalies, alkaline sulphides, or cyanide of potassium.
Solution and Separation.—Substances containing cadmium are soluble in
acids. The solution is evaporated to dryness (to render any silica that may
be present insoluble) and taken up with 10 c.c. of dilute hydrochloric acid.
Dilute to 100 c.c., and pass sulphuretted hydrogen. Filter, digest the
precipitate with soda, wash, and boil with dilute sulphuric acid. Filter; the
filtrate contains the cadmium and, possibly, a small quantity of zinc, from
which it is best separated by reprecipitating with sulphuretted hydrogen.
Page 342
GRAVIMETRIC DETERMINATION.
The solution containing the cadmium freed from the other metals is
precipitated with sulphuretted hydrogen in a moderately-acid solution. The
precipitate is collected on a weighed filter, and washed, first with an acid
solution of sulphuretted hydrogen, and afterwards with water. It is dried at
100° C. and weighed. If free sulphur is suspected to be present, extract with
bisulphide of carbon, and again weigh. The residue is cadmium sulphide,
which contains 77.78 per cent. of cadmium. It is a yellow powder insoluble
in solutions of the alkalies, alkaline sulphides, or cyanide of potassium. It
dissolves readily in acid. It cannot be ignited in a current of hydrogen
without loss.
VOLUMETRIC METHOD.
The solution containing the cadmium is concentrated by evaporation, and
mixed with an excess of oxalic acid and alcohol. The precipitate is filtered,
washed with alcohol, dissolved in hot hydrochloric acid, and titrated with
permanganate of potassium.
FOOTNOTES:
[64] When chromium is present some of the iron may escape precipitation but it
can be recovered from the solution by means of ammonic sulphide.
[65]
(1) 10FeSO4 + 2KMnO4 + 8H2SO4 = 5Fe2(SO4)3 + 2MnSO4 + K2SO4 +
8H2O. (2) 6FeCl2 + K2Cr2O7 + 14HCl = 3Fe2Cl6 + Cr2Cl6 + 2KCl + 7H2O.
[66]
(1) Fe2Cl6 + SnCl2 = 2FeCl2 + SnCl4.
(2) Fe2Cl6 + SH2 = 2FeCl2 + 2HCl + S.
(3) Fe2Cl6 + Na2SO3 + H2O = 2FeCl2 + Na2SO4 + 2HCl.
(4) Fe2Cl6 + Zn = 2FeCl2 + ZnCl2.
[67] 20 grams of stannous chloride and 20 c.c. of dilute hydrochloric acid are
diluted to one litre.
The solution containing the cadmium freed from the other metals is
precipitated with sulphuretted hydrogen in a moderately-acid solution. The
precipitate is collected on a weighed filter, and washed, first with an acid
solution of sulphuretted hydrogen, and afterwards with water. It is dried at
100° C. and weighed. If free sulphur is suspected to be present, extract with
bisulphide of carbon, and again weigh. The residue is cadmium sulphide,
which contains 77.78 per cent. of cadmium. It is a yellow powder insoluble
in solutions of the alkalies, alkaline sulphides, or cyanide of potassium. It
dissolves readily in acid. It cannot be ignited in a current of hydrogen
without loss.
VOLUMETRIC METHOD.
The solution containing the cadmium is concentrated by evaporation, and
mixed with an excess of oxalic acid and alcohol. The precipitate is filtered,
washed with alcohol, dissolved in hot hydrochloric acid, and titrated with
permanganate of potassium.
FOOTNOTES:
[64] When chromium is present some of the iron may escape precipitation but it
can be recovered from the solution by means of ammonic sulphide.
[65]
(1) 10FeSO4 + 2KMnO4 + 8H2SO4 = 5Fe2(SO4)3 + 2MnSO4 + K2SO4 +
8H2O. (2) 6FeCl2 + K2Cr2O7 + 14HCl = 3Fe2Cl6 + Cr2Cl6 + 2KCl + 7H2O.
[66]
(1) Fe2Cl6 + SnCl2 = 2FeCl2 + SnCl4.
(2) Fe2Cl6 + SH2 = 2FeCl2 + 2HCl + S.
(3) Fe2Cl6 + Na2SO3 + H2O = 2FeCl2 + Na2SO4 + 2HCl.
(4) Fe2Cl6 + Zn = 2FeCl2 + ZnCl2.
[67] 20 grams of stannous chloride and 20 c.c. of dilute hydrochloric acid are
diluted to one litre.
Page 343
[68] The maximum reducing effect of zinc is obtained by exposing as large a
surface as possible of the metal in a hot concentrated solution containing but
little free acid (Thorpe).
[69] About 5 inches in diameter.
[70] 61: 60:: 59: 58.13.
The iron in the ore is, then, the same in amount as that in 58.13 c.c. of the ferric
chloride solution; and since 100 c.c. of the latter contain 1 gram of iron, 58.13
c.c. of the same contains 0.5813 gram of iron; and, further, if 1 gram of ore
carries this amount of iron, 100 grams of ore will obviously give 58.13 grams of
iron.
[71] These compounds are Ni2As and Co2As.
[72] With large quantities of iron the ferric precipitate should be re-dissolved
and re-precipitated. The filtrate must be added to the original filtrate.
[73]
4KCy + NiSO4 = K2NiCy4 + K2SO4
2KCy + AgNO3 = KAgCy2 + KNO3
∴ 2AgNO3 = Ni
[74] Zn + H2SO4 = H2 + ZnSO4.
[75] These 104 c.c. are equivalent to 100 c.c. of dry air at 0° C. and 760 mm.
surface as possible of the metal in a hot concentrated solution containing but
little free acid (Thorpe).
[69] About 5 inches in diameter.
[70] 61: 60:: 59: 58.13.
The iron in the ore is, then, the same in amount as that in 58.13 c.c. of the ferric
chloride solution; and since 100 c.c. of the latter contain 1 gram of iron, 58.13
c.c. of the same contains 0.5813 gram of iron; and, further, if 1 gram of ore
carries this amount of iron, 100 grams of ore will obviously give 58.13 grams of
iron.
[71] These compounds are Ni2As and Co2As.
[72] With large quantities of iron the ferric precipitate should be re-dissolved
and re-precipitated. The filtrate must be added to the original filtrate.
[73]
4KCy + NiSO4 = K2NiCy4 + K2SO4
2KCy + AgNO3 = KAgCy2 + KNO3
∴ 2AgNO3 = Ni
[74] Zn + H2SO4 = H2 + ZnSO4.
[75] These 104 c.c. are equivalent to 100 c.c. of dry air at 0° C. and 760 mm.
Page 344
CHAPTER XII.
TIN—TUNGSTEN—TITANIUM.
TIN.
Tin occurs in nature as cassiterite (containing from 90 to 95 per cent. of
oxide of tin), which mineral is the source from which the whole of the tin of
commerce is derived. Tin also occurs as sulphide combined with sulphides
of copper and iron in the mineral stannine or bell-metal ore. It is a
constituent of certain rare minerals, such as tantalite.
The methods of assaying tin in actual use are remarkable when compared
with those of other metals. The more strictly chemical methods are rendered
troublesome by the oxide being insoluble in acids, resembling in this
respect the gangue with which it is associated. Moreover, it is not readily
decomposed by fusion with alkalies. The oxide has first to be reduced to
metal before the tin can be dissolved. The reduction may be performed by
fusing with potassic cyanide, by heating to moderate redness in a current of
hydrogen or coal gas, or by heating to a higher temperature with carbon.
The reduced metal is only slowly dissolved by hydrochloric acid, and
although it is readily soluble in aqua regia, the solution cannot be
evaporated or freed from the excess of acids, by boiling, without loss of tin,
because of the volatility of stannic chloride. There has long been a difficulty
in getting a quick wet method.
The process of assaying tin ores adopted in the mines of Cornwall is a
mechanical one known as "vanning," the object of which is to find the
percentage of "black tin," which, it is well to remember, is not pure
cassiterite, much less pure oxide of tin. Tin ore, as taken from the lode,
contains from 2 to 5 per cent. of cassiterite, and is mainly made up of
quartz, felspar, chlorite, schorl, and other stony minerals, together with
more or less mispickel, iron and copper pyrites, oxide of iron, and wolfram.
The cassiterite has a specific gravity (6.4 to 7.1) considerably higher than
that of the vein-stuff (2.5 to 3.0), and is concentrated by a series of
TIN—TUNGSTEN—TITANIUM.
TIN.
Tin occurs in nature as cassiterite (containing from 90 to 95 per cent. of
oxide of tin), which mineral is the source from which the whole of the tin of
commerce is derived. Tin also occurs as sulphide combined with sulphides
of copper and iron in the mineral stannine or bell-metal ore. It is a
constituent of certain rare minerals, such as tantalite.
The methods of assaying tin in actual use are remarkable when compared
with those of other metals. The more strictly chemical methods are rendered
troublesome by the oxide being insoluble in acids, resembling in this
respect the gangue with which it is associated. Moreover, it is not readily
decomposed by fusion with alkalies. The oxide has first to be reduced to
metal before the tin can be dissolved. The reduction may be performed by
fusing with potassic cyanide, by heating to moderate redness in a current of
hydrogen or coal gas, or by heating to a higher temperature with carbon.
The reduced metal is only slowly dissolved by hydrochloric acid, and
although it is readily soluble in aqua regia, the solution cannot be
evaporated or freed from the excess of acids, by boiling, without loss of tin,
because of the volatility of stannic chloride. There has long been a difficulty
in getting a quick wet method.
The process of assaying tin ores adopted in the mines of Cornwall is a
mechanical one known as "vanning," the object of which is to find the
percentage of "black tin," which, it is well to remember, is not pure
cassiterite, much less pure oxide of tin. Tin ore, as taken from the lode,
contains from 2 to 5 per cent. of cassiterite, and is mainly made up of
quartz, felspar, chlorite, schorl, and other stony minerals, together with
more or less mispickel, iron and copper pyrites, oxide of iron, and wolfram.
The cassiterite has a specific gravity (6.4 to 7.1) considerably higher than
that of the vein-stuff (2.5 to 3.0), and is concentrated by a series of
Page 345
washings till it is free from the lighter material. Those minerals which have
a specific gravity approaching that of the cassiterite are not completely
removed. The mispickel and copper and iron pyrites are converted into
oxides by roasting, and are in great part removed by a subsequent washing.
The concentrated product is known as "black tin," and in this condition is
sold to the smelter. The chief foreign matters in the black tin are silica,
oxides of iron and copper, and wolfram, with traces of manganese and
niobic acid; and in certain stream ores there may be as much as 6 or 7 per
cent. of titaniferous iron. The black tin from the mines contains from 5 to 12
per cent. of water, and is sold and assayed wet. A series of typical samples
of black tin ranged as follows:—
Source of Material. Percentage of Metal in Dry Ore. Specific Gravity.
Good mine ore 72.0 6.39
Inferior do. 71.5 6.64
Titaniferous stream ore 67.0 6.39
Mine ore with wolfram 64.5 6.67
Ore from stream works 58.5 5.99
It will be seen from these figures that black tin is a very variable substance;
and that the specific gravity is largely influenced by the impurities; hence, it
is only an indication of the percentage of metal when the same kind of ore
is dealt with.
As already pointed out, the object of vanning is to determine the proportion
of black tin in the lode stuff. The relation between the actual content in
oxide of tin and the produce got by vanning has been tested on several
occasions with results which show a fair degree of approximation.
The following are some published results of assays of the same batch of
ore. The vanning results were obtained by a Cornish vanner of recognised
ability, and the wet assays by two London firms of the highest standing:—
Vanning results:
(Average) 91 lbs. of "black tin."
Wet Assay results:
A 83.7 lbs. of stannic oxide.
a specific gravity approaching that of the cassiterite are not completely
removed. The mispickel and copper and iron pyrites are converted into
oxides by roasting, and are in great part removed by a subsequent washing.
The concentrated product is known as "black tin," and in this condition is
sold to the smelter. The chief foreign matters in the black tin are silica,
oxides of iron and copper, and wolfram, with traces of manganese and
niobic acid; and in certain stream ores there may be as much as 6 or 7 per
cent. of titaniferous iron. The black tin from the mines contains from 5 to 12
per cent. of water, and is sold and assayed wet. A series of typical samples
of black tin ranged as follows:—
Source of Material. Percentage of Metal in Dry Ore. Specific Gravity.
Good mine ore 72.0 6.39
Inferior do. 71.5 6.64
Titaniferous stream ore 67.0 6.39
Mine ore with wolfram 64.5 6.67
Ore from stream works 58.5 5.99
It will be seen from these figures that black tin is a very variable substance;
and that the specific gravity is largely influenced by the impurities; hence, it
is only an indication of the percentage of metal when the same kind of ore
is dealt with.
As already pointed out, the object of vanning is to determine the proportion
of black tin in the lode stuff. The relation between the actual content in
oxide of tin and the produce got by vanning has been tested on several
occasions with results which show a fair degree of approximation.
The following are some published results of assays of the same batch of
ore. The vanning results were obtained by a Cornish vanner of recognised
ability, and the wet assays by two London firms of the highest standing:—
Vanning results:
(Average) 91 lbs. of "black tin."
Wet Assay results:
A 83.7 lbs. of stannic oxide.
Page 346
B 79.7 lbs. "
The vanner reported his black tin as containing 70 per cent. of tin. This will
bring his result, if calculated as stannic oxide, to 80.9 lbs. to the ton; which
agrees with the others.
According to our experience the "van" assay agrees fairly well with the
"wet" one, if the black tin is assumed to contain 92.5 per cent. of stannic
oxide (SnO2).
Vanners are, as a rule, skilful men, and show remarkable dexterity in
separating the black tin, with the help of their apparatus, which consists
simply of a shovel and a kieve of water. An account of the process is given
below. But different vanners, all good men, will get different results
working on material new to them. The black tin weighed by the vanner is
supposed to correspond in quality with the black tin returned from the
floors of the mine for which he is assaying, but this differs materially in
different mines with the nature of the gangue. The process leaves too much
to the judgment of the vanner. It is more than probable that in practice the
returns from the dressing-floors check the assayer, instead of, as should
properly be the case, the assayer checking the returns. It is only when this
last is done that any control is had over the system of dressing. A correct
assay of this ore is a matter of some importance, because of the high price
of the metal.
The method of assaying the black tin is a dry one, and consists of mixing it
with "culm," and submitting it in a black-lead crucible to the highest
temperature of a wind furnace. The sample is taken wet as it arrives at the
smelting house, and is assayed direct. The product of the assay is examined,
and a deduction of a considerable percentage is very properly made for
impurities, since the assay really determines the percentage, not merely of
tin, but of the bodies present which are reducible at a white heat. The
judgment as to how much is to be deducted is assisted partly by an
examination of the metal got from the assay, and partly by the experience
acquired in smelting similar ores. The produce, which is that of the impure
tin, is stated in parts in twenty; thus a produce of 14 is equivalent to 70 per
cent., or to 14 cwt. per ton.
The vanner reported his black tin as containing 70 per cent. of tin. This will
bring his result, if calculated as stannic oxide, to 80.9 lbs. to the ton; which
agrees with the others.
According to our experience the "van" assay agrees fairly well with the
"wet" one, if the black tin is assumed to contain 92.5 per cent. of stannic
oxide (SnO2).
Vanners are, as a rule, skilful men, and show remarkable dexterity in
separating the black tin, with the help of their apparatus, which consists
simply of a shovel and a kieve of water. An account of the process is given
below. But different vanners, all good men, will get different results
working on material new to them. The black tin weighed by the vanner is
supposed to correspond in quality with the black tin returned from the
floors of the mine for which he is assaying, but this differs materially in
different mines with the nature of the gangue. The process leaves too much
to the judgment of the vanner. It is more than probable that in practice the
returns from the dressing-floors check the assayer, instead of, as should
properly be the case, the assayer checking the returns. It is only when this
last is done that any control is had over the system of dressing. A correct
assay of this ore is a matter of some importance, because of the high price
of the metal.
The method of assaying the black tin is a dry one, and consists of mixing it
with "culm," and submitting it in a black-lead crucible to the highest
temperature of a wind furnace. The sample is taken wet as it arrives at the
smelting house, and is assayed direct. The product of the assay is examined,
and a deduction of a considerable percentage is very properly made for
impurities, since the assay really determines the percentage, not merely of
tin, but of the bodies present which are reducible at a white heat. The
judgment as to how much is to be deducted is assisted partly by an
examination of the metal got from the assay, and partly by the experience
acquired in smelting similar ores. The produce, which is that of the impure
tin, is stated in parts in twenty; thus a produce of 14 is equivalent to 70 per
cent., or to 14 cwt. per ton.
Page 347
MECHANICAL SEPARATION.—VANNING.
This process, which has already been referred to, is carried out as follows:
—After sampling the ore in the ordinary way, a quantity (varying with its
richness) is weighed out. Special weights are generally used. The standard
weight, marked 200, weighs about an ounce; with poor ores this quantity is
taken for an assay, but with richer ores 100 or even 50 is sufficient. The unit
of weight has no special name, but the parts in 200 are spoken of as the
produce; thus, if 200 of ore were taken and 9.5 of black tin were separated,
the produce would be 9-1/2: obviously half the "produce" will give the
percentage. The weighed portion of the ore is placed on the vanning shovel.
The vanner stands in front of a tub of water (kieve) and allows 30 or 40 c.c.
of water to flow on to the ore. He then raises the shovel a little above the
surface of the water, and, holding it nearly horizontal, briskly rotates the
water by imparting to the shovel a slight circular motion, passing into an
elliptical one (front to back). This causes the finer mud to be suspended in
the liquid, which is then run off, leaving the body of the ore in the centre of
the shovel. This is repeated until the water after standing a moment is fairly
clear. About half as much water as before is brought on; then, with a motion
which is similar to the previous one, but with a jerk added in one direction,
the heavier minerals are thrown up, and the stony matter brought back. The
jerk is produced just as the wave of water is returning. The descending
This process, which has already been referred to, is carried out as follows:
—After sampling the ore in the ordinary way, a quantity (varying with its
richness) is weighed out. Special weights are generally used. The standard
weight, marked 200, weighs about an ounce; with poor ores this quantity is
taken for an assay, but with richer ores 100 or even 50 is sufficient. The unit
of weight has no special name, but the parts in 200 are spoken of as the
produce; thus, if 200 of ore were taken and 9.5 of black tin were separated,
the produce would be 9-1/2: obviously half the "produce" will give the
percentage. The weighed portion of the ore is placed on the vanning shovel.
The vanner stands in front of a tub of water (kieve) and allows 30 or 40 c.c.
of water to flow on to the ore. He then raises the shovel a little above the
surface of the water, and, holding it nearly horizontal, briskly rotates the
water by imparting to the shovel a slight circular motion, passing into an
elliptical one (front to back). This causes the finer mud to be suspended in
the liquid, which is then run off, leaving the body of the ore in the centre of
the shovel. This is repeated until the water after standing a moment is fairly
clear. About half as much water as before is brought on; then, with a motion
which is similar to the previous one, but with a jerk added in one direction,
the heavier minerals are thrown up, and the stony matter brought back. The
jerk is produced just as the wave of water is returning. The descending
Page 348
wave of water draws with it the bulkier and lighter particles of the ore,
whilst the heavier matter lying on the bottom is scarcely affected by it. The
jerky motion, however, carries it to the front of the shovel. The lighter stuff
is washed off, and the residue dried by holding the shovel over the furnace.
It now corresponds, more or less, to the stuff which on the mine is sent to
the calciner. It is swept from the shovel into a scoop, and transferred to a
hot crucible; in which it is calcined until free from sulphur. Some vanners
calcine their samples before commencing to van. The calcined ore is shaken
out of the crucible on to the shovel; rubbed up with a hammer; and washed
(as at first) to get rid of the finer and lighter "waste." The separating
motions are again gone through; and the "head" of the best of the black tin
is thrown well up on one side of the shovel in the form of a crescent, so as
to leave room on the shovel to work with the "tailings." The quantity of
water used is kept low, to prevent this "crop" tin from being washed back
again. The tailings are then crushed to free the tin from adherent oxide of
iron; and again washed to throw up the remaining tin ore. As this tin is
finely divided, it is more difficult to bring it up, so that a vigorous and rapid
motion is required. The tailings are now washed off, and the whole of the
black tin is brought into the centre of the shovel. It requires two or three
washings more to free it from the waste it contains. Very small quantities of
water are used. The purity of the black tin can be seen by its appearance on
the shovel. The cleaned ore is dried as before, freed from particles of iron
with the aid of a magnet, and weighed. The weighings are carried to 1/8th
of the unit used. The following example illustrates the method of
calculation adopted on the mine. A parcel of 1 ton 2 cwt. 3 qrs. of tin ore
with a produce of 45 (equal to 22-1/2 per cent.) contains 5 cwt. 0 qrs. 12
lbs. of black tin. This result is obtained as follows:—
ton cwt. qrs.
1 2 3
9 }
----------------- }
10 4 3 } equivalent to multiplying by 45.
5 }
---------------- }
5.1 3 3 strike off the first figure to the right.
4 multiply by 4 to reduce to quarters.
---------
4 12
whilst the heavier matter lying on the bottom is scarcely affected by it. The
jerky motion, however, carries it to the front of the shovel. The lighter stuff
is washed off, and the residue dried by holding the shovel over the furnace.
It now corresponds, more or less, to the stuff which on the mine is sent to
the calciner. It is swept from the shovel into a scoop, and transferred to a
hot crucible; in which it is calcined until free from sulphur. Some vanners
calcine their samples before commencing to van. The calcined ore is shaken
out of the crucible on to the shovel; rubbed up with a hammer; and washed
(as at first) to get rid of the finer and lighter "waste." The separating
motions are again gone through; and the "head" of the best of the black tin
is thrown well up on one side of the shovel in the form of a crescent, so as
to leave room on the shovel to work with the "tailings." The quantity of
water used is kept low, to prevent this "crop" tin from being washed back
again. The tailings are then crushed to free the tin from adherent oxide of
iron; and again washed to throw up the remaining tin ore. As this tin is
finely divided, it is more difficult to bring it up, so that a vigorous and rapid
motion is required. The tailings are now washed off, and the whole of the
black tin is brought into the centre of the shovel. It requires two or three
washings more to free it from the waste it contains. Very small quantities of
water are used. The purity of the black tin can be seen by its appearance on
the shovel. The cleaned ore is dried as before, freed from particles of iron
with the aid of a magnet, and weighed. The weighings are carried to 1/8th
of the unit used. The following example illustrates the method of
calculation adopted on the mine. A parcel of 1 ton 2 cwt. 3 qrs. of tin ore
with a produce of 45 (equal to 22-1/2 per cent.) contains 5 cwt. 0 qrs. 12
lbs. of black tin. This result is obtained as follows:—
ton cwt. qrs.
1 2 3
9 }
----------------- }
10 4 3 } equivalent to multiplying by 45.
5 }
---------------- }
5.1 3 3 strike off the first figure to the right.
4 multiply by 4 to reduce to quarters.
---------
4 12
Page 349
3
---------
4 15
28 multiply by 28 to reduce to pounds.
-----
112
15
-----
12.7 strike off the first figure to the right.
Similarly, a parcel of 20 tons 10 cwt. with a produce of 9-1/2 contains 19
cwt. 1 qr. 25 lbs. of black tin. For the following information, as well as for
much of that already given about vanning, we are indebted to Captain
Reynolds, of Cook's Kitchen Mine. "To have a complete set of tools for all
vanning purposes, it will be necessary to get the following:—A vanning
shovel 14 inches long and 13 inches wide, weighing not over 2-3/4 pounds.
It is made of hammered sheet iron of the shape shown in fig. 57. It must
have a light wooden handle (preferably of deal) 3 feet long. A bruising
hammer, weighing 2-1/2 pounds, with a handle 1 foot long. A pair of tongs
(furnace) 2-1/2 feet long, made of 1/2-inch round iron. And a set of ordinary
clay crucibles for calcining. There ought to be two sets of scales and
weights: the first should be confined to weighing the powdered tin stuff,
and the second ought to be a much higher class one, for weighing the black
tin obtained. The furnace for roasting the sample should be 10 inches square
and 12 inches deep, with the fire-bars at the bottom three-quarters of an
inch apart. The water-box for vanning in should be at least 4 feet long, 2
feet 6 inches wide, and 8 inches deep."
DRY METHODS.
For the following description of the process adopted in Cornwall we are
indebted to Mr. A.K. Barnett, F.G.S., of Chyandour.
Cornish Method.—Tin Ore Assay.—The ore to be smelted or assayed
should be concentrated to say not less than 50 per cent. of metallic tin;
though to obtain satisfactory results it should be brought nearer 70 per cent.,
as with ore containing less than 40 to 50 per cent. of metal there will be a
considerable loss both in the assaying and in the smelting. If the ore to be
operated on does not contain this quantity of metal, then the sample (if
---------
4 15
28 multiply by 28 to reduce to pounds.
-----
112
15
-----
12.7 strike off the first figure to the right.
Similarly, a parcel of 20 tons 10 cwt. with a produce of 9-1/2 contains 19
cwt. 1 qr. 25 lbs. of black tin. For the following information, as well as for
much of that already given about vanning, we are indebted to Captain
Reynolds, of Cook's Kitchen Mine. "To have a complete set of tools for all
vanning purposes, it will be necessary to get the following:—A vanning
shovel 14 inches long and 13 inches wide, weighing not over 2-3/4 pounds.
It is made of hammered sheet iron of the shape shown in fig. 57. It must
have a light wooden handle (preferably of deal) 3 feet long. A bruising
hammer, weighing 2-1/2 pounds, with a handle 1 foot long. A pair of tongs
(furnace) 2-1/2 feet long, made of 1/2-inch round iron. And a set of ordinary
clay crucibles for calcining. There ought to be two sets of scales and
weights: the first should be confined to weighing the powdered tin stuff,
and the second ought to be a much higher class one, for weighing the black
tin obtained. The furnace for roasting the sample should be 10 inches square
and 12 inches deep, with the fire-bars at the bottom three-quarters of an
inch apart. The water-box for vanning in should be at least 4 feet long, 2
feet 6 inches wide, and 8 inches deep."
DRY METHODS.
For the following description of the process adopted in Cornwall we are
indebted to Mr. A.K. Barnett, F.G.S., of Chyandour.
Cornish Method.—Tin Ore Assay.—The ore to be smelted or assayed
should be concentrated to say not less than 50 per cent. of metallic tin;
though to obtain satisfactory results it should be brought nearer 70 per cent.,
as with ore containing less than 40 to 50 per cent. of metal there will be a
considerable loss both in the assaying and in the smelting. If the ore to be
operated on does not contain this quantity of metal, then the sample (if
Page 350
coarse) must be reduced to a fine state, the gangue being removed by
vanning, and the ore saved for the fire assay.
The method adopted for the determination of tin in the ore is as follows:—
About 2-1/2 ounces troy (1200 grains, or about 80 grams) of the ore to be
assayed is weighed out and mixed on a flat copper pan (shaped with a long
lip) with one-fifth of its weight (240 grains, or 15.5 grams) of powdered
culm (anthracite). The mixture of ore and culm is either transferred to a
black-lead crucible before the latter is put into the furnace, or, as some
prefer, it is carefully swept into a crucible which has been imbedded in the
fire. Some assayers cover their pots with a flat cover placed loosely on,
while others leave the mixture in the open pot. The furnace, which has been
previously fired to a strong heat, is then covered, and the sample is
subjected to a sharp fire for a period of from twelve to twenty minutes. No
definite time can be stated, as, besides the strength of the fire, the quality
and condition of the ore, and the impurities associated with it, greatly
affects the time required for the complete reduction of the ore. As soon as
the mixture in the crucible has settled down to a uniform white heat, and
any very slight ebullition which may have taken place has subsided, the
crucible is gently shaken, removed from the fire (the culm-ash or slag
which covers the metal being carefully drawn aside with an iron scraper),
and the metal is poured quickly into an iron ingot-mould, which is usually
placed on a copper pan to save the culm-slag and the adherent metal which
comes out with it. The crucible is then carefully scraped, and the scrapings,
together with the contents of the mould and pan, are transferred to a mortar.
There the ingot of tin is freed from slag and then taken to the scales. The
rest, after being finely powdered, is passed through a sieve. The flattened
particles of tin which remain on the sieve are weighed with the ingot (the
lump, as it is called); whilst the siftings are vanned on a shovel, and (the
slag being washed off) the fine tin is collected, dried, and weighed with the
rest: the whole gives the produce or percentage of metal in the ore. The
results of the assays are expressed in cwts. of metal in the ton of ore. The
percentage is rarely given and never used in Cornwall. Thus—"13-1/2
Produce" would mean that the assay yielded results at the rate of 13-1/2
cwts. of metal for one ton of the ore. Some assayers use a little powdered
fluor-spar to assist the fusion of refractory slags. A small quantity of borax
will also occasionally be of service for ores containing silica in excess of
vanning, and the ore saved for the fire assay.
The method adopted for the determination of tin in the ore is as follows:—
About 2-1/2 ounces troy (1200 grains, or about 80 grams) of the ore to be
assayed is weighed out and mixed on a flat copper pan (shaped with a long
lip) with one-fifth of its weight (240 grains, or 15.5 grams) of powdered
culm (anthracite). The mixture of ore and culm is either transferred to a
black-lead crucible before the latter is put into the furnace, or, as some
prefer, it is carefully swept into a crucible which has been imbedded in the
fire. Some assayers cover their pots with a flat cover placed loosely on,
while others leave the mixture in the open pot. The furnace, which has been
previously fired to a strong heat, is then covered, and the sample is
subjected to a sharp fire for a period of from twelve to twenty minutes. No
definite time can be stated, as, besides the strength of the fire, the quality
and condition of the ore, and the impurities associated with it, greatly
affects the time required for the complete reduction of the ore. As soon as
the mixture in the crucible has settled down to a uniform white heat, and
any very slight ebullition which may have taken place has subsided, the
crucible is gently shaken, removed from the fire (the culm-ash or slag
which covers the metal being carefully drawn aside with an iron scraper),
and the metal is poured quickly into an iron ingot-mould, which is usually
placed on a copper pan to save the culm-slag and the adherent metal which
comes out with it. The crucible is then carefully scraped, and the scrapings,
together with the contents of the mould and pan, are transferred to a mortar.
There the ingot of tin is freed from slag and then taken to the scales. The
rest, after being finely powdered, is passed through a sieve. The flattened
particles of tin which remain on the sieve are weighed with the ingot (the
lump, as it is called); whilst the siftings are vanned on a shovel, and (the
slag being washed off) the fine tin is collected, dried, and weighed with the
rest: the whole gives the produce or percentage of metal in the ore. The
results of the assays are expressed in cwts. of metal in the ton of ore. The
percentage is rarely given and never used in Cornwall. Thus—"13-1/2
Produce" would mean that the assay yielded results at the rate of 13-1/2
cwts. of metal for one ton of the ore. Some assayers use a little powdered
fluor-spar to assist the fusion of refractory slags. A small quantity of borax
will also occasionally be of service for ores containing silica in excess of
Page 351
any iron that may be present. The borax renders the slag more fusible, and
assists the formation of a larger lump (with less fine tin in the slag) than
would be obtained by the use of culm alone.
The quality and the percentage of pure tin in the metal will vary
considerably, according to the impurities that are associated with the ore to
be assayed.
The crude lump is then remelted in a small iron ladle at as low a
temperature as possible, and the fused metal is poured into a shallow trench
about 4 inches long by 3/4 of an inch wide cut in a block of white marble.
The metal will be silvery-white if the temperature employed be correct; if
too hot, the surface will show a yellow, red, or blue colour (according to the
heat employed); in such case the metal should be remelted at a lower
temperature. If the metal on cooling remains perfectly clear and bright, then
it may be assumed that the tin is of good quality and commercially pure. A
crystallised or frosted appearance of the metal indicates the presence of
some alloy, say of iron, copper, zinc, lead, antimony, &c. The assayer who
has had much practice can readily distinguish the metal or metals that are
associated with the ore by noting the appearance of the tin on cooling; and
can fairly judge the quantity of impurity present by the amount of the
crystallisation or stain.
Whilst the foregoing method of assaying cannot lay claim to scientific
accuracy, it is by no means so imperfect as some writers would have us
believe, who state that a loss of 5 to 10 per cent. arises in the operation. It is
certainly the most ready and expeditious mode of determining the
commercial value of a parcel of tin ore, which, after all, is the main object
of all assaying operations.
The difficulty which beginners find in obtaining satisfactory results, and
any loss of metal which those not accustomed to the process may incur, will
invariably occur in the vanning of the powdered slag for the fine tin, the rest
of the operations being easy of execution, and requiring only the ordinary
care necessary for all metallurgical work.
There is no doubt that if low percentage ores containing silica are assayed
in this manner, low results are obtained, as it is impossible to reduce the
whole of the tin in the presence of free silica; with this class of ores, care
assists the formation of a larger lump (with less fine tin in the slag) than
would be obtained by the use of culm alone.
The quality and the percentage of pure tin in the metal will vary
considerably, according to the impurities that are associated with the ore to
be assayed.
The crude lump is then remelted in a small iron ladle at as low a
temperature as possible, and the fused metal is poured into a shallow trench
about 4 inches long by 3/4 of an inch wide cut in a block of white marble.
The metal will be silvery-white if the temperature employed be correct; if
too hot, the surface will show a yellow, red, or blue colour (according to the
heat employed); in such case the metal should be remelted at a lower
temperature. If the metal on cooling remains perfectly clear and bright, then
it may be assumed that the tin is of good quality and commercially pure. A
crystallised or frosted appearance of the metal indicates the presence of
some alloy, say of iron, copper, zinc, lead, antimony, &c. The assayer who
has had much practice can readily distinguish the metal or metals that are
associated with the ore by noting the appearance of the tin on cooling; and
can fairly judge the quantity of impurity present by the amount of the
crystallisation or stain.
Whilst the foregoing method of assaying cannot lay claim to scientific
accuracy, it is by no means so imperfect as some writers would have us
believe, who state that a loss of 5 to 10 per cent. arises in the operation. It is
certainly the most ready and expeditious mode of determining the
commercial value of a parcel of tin ore, which, after all, is the main object
of all assaying operations.
The difficulty which beginners find in obtaining satisfactory results, and
any loss of metal which those not accustomed to the process may incur, will
invariably occur in the vanning of the powdered slag for the fine tin, the rest
of the operations being easy of execution, and requiring only the ordinary
care necessary for all metallurgical work.
There is no doubt that if low percentage ores containing silica are assayed
in this manner, low results are obtained, as it is impossible to reduce the
whole of the tin in the presence of free silica; with this class of ores, care
Page 352
should be taken to remove some of the silica by preliminary vanning, or
some flux should be added which will combine with the silica, and so
prevent its entering into combination with the tin. Low quality tin ores
containing iron, copper, lead, zinc, antimony, etc., combined with arsenic,
sulphur, or oxygen, will give very much higher results than the actual
percentage of tin in the sample. The other metals (being readily reduced in
the presence of tin) alloy with it, and give a hard lump difficult to fuse in
the iron ladle; where the quantity of foreign metals is large, the metal can
only be melted to a stiff pasty mass; so that (in determining the value of a
ton of tin ore, or even reporting on the percentage of tin it contains) not
only must the weight of the assay be the basis for calculation, but the
quality and character of the metal obtained must also be considered. Thus
two ores of tin might be assayed both yielding a similar produce, say 13-1/2
(67-1/2 per cent.), and yet one might contain 5 per cent. less tin than the
other.
If it be required to obtain the pure metal from tin ores containing the ores of
other metals associated with them, the latter must be removed by digesting
in strong hydrochloric acid, and washing. The assay may then be conducted
in the usual way, and a fairly pure lump will be obtained.
If wolfram be present in any appreciable quantity in the ore, it considerably
reduces the proportion of lump, and at the same time it increases the fine tin
(or prillion, as it is termed) in the assay. This may be got rid of by boiling in
aqua regia, and dissolving out the tungstic acid which has been liberated by
means of ammonia.
It will be seen that this method of assaying tin has its advantages and its
drawbacks. It is quickly performed; with ores of good quality it gives
results not to be excelled by any other process; and it gives the smelter the
actual alloy and quality of metal he may expect to get in the smelting of the
ore, which no other mode of assaying will do: against which may be set the
skill required to obtain accurate results with the vanning shovel; the loss of
metal in poor ores containing an excess of silica; and the high results from
ores containing a large quantity of metallic impurities.
Cyanide Method.—Weigh up 20 grams of the ore and dry it on a scoop
over the Bunsen flame. When dry, weigh, and calculate the percentage of
some flux should be added which will combine with the silica, and so
prevent its entering into combination with the tin. Low quality tin ores
containing iron, copper, lead, zinc, antimony, etc., combined with arsenic,
sulphur, or oxygen, will give very much higher results than the actual
percentage of tin in the sample. The other metals (being readily reduced in
the presence of tin) alloy with it, and give a hard lump difficult to fuse in
the iron ladle; where the quantity of foreign metals is large, the metal can
only be melted to a stiff pasty mass; so that (in determining the value of a
ton of tin ore, or even reporting on the percentage of tin it contains) not
only must the weight of the assay be the basis for calculation, but the
quality and character of the metal obtained must also be considered. Thus
two ores of tin might be assayed both yielding a similar produce, say 13-1/2
(67-1/2 per cent.), and yet one might contain 5 per cent. less tin than the
other.
If it be required to obtain the pure metal from tin ores containing the ores of
other metals associated with them, the latter must be removed by digesting
in strong hydrochloric acid, and washing. The assay may then be conducted
in the usual way, and a fairly pure lump will be obtained.
If wolfram be present in any appreciable quantity in the ore, it considerably
reduces the proportion of lump, and at the same time it increases the fine tin
(or prillion, as it is termed) in the assay. This may be got rid of by boiling in
aqua regia, and dissolving out the tungstic acid which has been liberated by
means of ammonia.
It will be seen that this method of assaying tin has its advantages and its
drawbacks. It is quickly performed; with ores of good quality it gives
results not to be excelled by any other process; and it gives the smelter the
actual alloy and quality of metal he may expect to get in the smelting of the
ore, which no other mode of assaying will do: against which may be set the
skill required to obtain accurate results with the vanning shovel; the loss of
metal in poor ores containing an excess of silica; and the high results from
ores containing a large quantity of metallic impurities.
Cyanide Method.—Weigh up 20 grams of the ore and dry it on a scoop
over the Bunsen flame. When dry, weigh, and calculate the percentage of
Page 353
water from the loss in weight. Transfer the dried ore to an evaporating dish,
and cover with 30 c.c. of hydrochloric acid; boil for 10 or 12 minutes, and
then add 5 c.c. of nitric acid and boil again. Dilute with water, and filter.
Transfer the filter and its contents to an E Battersea crucible, and calcine it
for a few minutes. Cool, and weigh the residue. The loss equals the oxides
soluble in acid. Transfer the residue to the crucible and mix it with its own
weight of cyanide of potassium; add a similar amount of "cyanide" as a
cover. Place in the furnace, and when the charge has attained the
temperature of the furnace (in from 3 to 6 minutes), remove it at once; tap
the pot vigorously several times, and then pour its contents quietly into a
mould. Dissolve the slag in water, clean, dry, and weigh the button of tin.
WET METHODS.
Detection.—Tin ore is detected by its insolubility in acids, high specific
gravity, and characteristic appearance in water. The powder is separated
from the lighter gangue by washing. It is fused in a Berlin crucible with five
times its weight of potassic cyanide at a moderately high temperature in a
muffle, or over the blowpipe. The slag is washed off with water, and the
metallic buttons or residue treated with hydrochloric acid (not aqua regia),
for some time. One portion of the solution strikes a purple colour with
chloride of gold, another portion gives a white or grey precipitate or
cloudiness with mercuric chloride. These reactions are characteristic of tin
as stannous chloride.
Metallic tin treated with nitric acid becomes converted into a white
insoluble powder (metastannic acid). Aqua regia dissolves tin readily,
forming stannic chloride, and in this solution the metal is detected by
precipitation with sulphuretted hydrogen, which gives a yellow precipitate.
Tin in solution as stannic or stannous chloride is precipitated as metal by
means of zinc.
The fact that tin forms two well-defined series of compounds is taken
advantage of in assaying (just as in the case of iron), by determining how
much of an oxidising agent is required to convert it from the stannous into
the stannic state. For example, on the addition of a solution of
permanganate of potash to a solution of stannous chloride the oxidation
and cover with 30 c.c. of hydrochloric acid; boil for 10 or 12 minutes, and
then add 5 c.c. of nitric acid and boil again. Dilute with water, and filter.
Transfer the filter and its contents to an E Battersea crucible, and calcine it
for a few minutes. Cool, and weigh the residue. The loss equals the oxides
soluble in acid. Transfer the residue to the crucible and mix it with its own
weight of cyanide of potassium; add a similar amount of "cyanide" as a
cover. Place in the furnace, and when the charge has attained the
temperature of the furnace (in from 3 to 6 minutes), remove it at once; tap
the pot vigorously several times, and then pour its contents quietly into a
mould. Dissolve the slag in water, clean, dry, and weigh the button of tin.
WET METHODS.
Detection.—Tin ore is detected by its insolubility in acids, high specific
gravity, and characteristic appearance in water. The powder is separated
from the lighter gangue by washing. It is fused in a Berlin crucible with five
times its weight of potassic cyanide at a moderately high temperature in a
muffle, or over the blowpipe. The slag is washed off with water, and the
metallic buttons or residue treated with hydrochloric acid (not aqua regia),
for some time. One portion of the solution strikes a purple colour with
chloride of gold, another portion gives a white or grey precipitate or
cloudiness with mercuric chloride. These reactions are characteristic of tin
as stannous chloride.
Metallic tin treated with nitric acid becomes converted into a white
insoluble powder (metastannic acid). Aqua regia dissolves tin readily,
forming stannic chloride, and in this solution the metal is detected by
precipitation with sulphuretted hydrogen, which gives a yellow precipitate.
Tin in solution as stannic or stannous chloride is precipitated as metal by
means of zinc.
The fact that tin forms two well-defined series of compounds is taken
advantage of in assaying (just as in the case of iron), by determining how
much of an oxidising agent is required to convert it from the stannous into
the stannic state. For example, on the addition of a solution of
permanganate of potash to a solution of stannous chloride the oxidation
Page 354
goes on rapidly, and the finishing point is sharp and distinct; but acid
solutions of stannous chloride quickly take up oxygen from that dissolved
in the water used and from the air. Unfortunately, there is no obvious sign
that such oxidation has taken place, except that (fatal to the assay) a smaller
volume of the permanganate is required. Great care is required with such
solutions, both before and during titration. The addition of an excess of
ferric chloride to the stannous solution, as soon as the whole of the tin has
been dissolved, will lessen this liability to oxidation.
Separation.—If the tin is present in an alloy, the substance is boiled in an
evaporating dish with dilute nitric acid until the whole of the material is
attacked. Evaporate nearly to dryness, dilute, boil for a few minutes, and
filter off the white insoluble residue. Under certain circumstances this
residue will be nearly free from other metals, in which case it is ignited and
weighed. If not known to be pure it must be ignited, reduced in a current of
hydrogen, and treated as subsequently described.
When the tin is present as insoluble oxide in an ore, the substance is finely
powdered, and from 1 to 5 grams of it (according to its richness) boiled
with 30 c.c. of hydrochloric acid in an evaporating dish till the oxide of iron
is seen to be dissolved. Then add 1 c.c. of nitric acid (or more if much
pyrites, &c., is present) and continue the boiling till these are decomposed;
dilute and filter off, washing first with dilute acid and afterwards with a
little dilute ammonia, dry, ignite, and place in a combustion tube (together
with the filter-ash) and heat to redness for about thirty minutes in a current
of dried hydrogen.
The oxide of tin is placed in a porcelain boat (fig. 58), which is then
introduced into a piece of combustion tube. The latter, wrapped in a piece of
wire gauze, is supported on a couple of iron rings, and heated by one or two
Bunsen burners in a furnace fitted up with loose fire-brick tiles, as shown in
fig. 59.
solutions of stannous chloride quickly take up oxygen from that dissolved
in the water used and from the air. Unfortunately, there is no obvious sign
that such oxidation has taken place, except that (fatal to the assay) a smaller
volume of the permanganate is required. Great care is required with such
solutions, both before and during titration. The addition of an excess of
ferric chloride to the stannous solution, as soon as the whole of the tin has
been dissolved, will lessen this liability to oxidation.
Separation.—If the tin is present in an alloy, the substance is boiled in an
evaporating dish with dilute nitric acid until the whole of the material is
attacked. Evaporate nearly to dryness, dilute, boil for a few minutes, and
filter off the white insoluble residue. Under certain circumstances this
residue will be nearly free from other metals, in which case it is ignited and
weighed. If not known to be pure it must be ignited, reduced in a current of
hydrogen, and treated as subsequently described.
When the tin is present as insoluble oxide in an ore, the substance is finely
powdered, and from 1 to 5 grams of it (according to its richness) boiled
with 30 c.c. of hydrochloric acid in an evaporating dish till the oxide of iron
is seen to be dissolved. Then add 1 c.c. of nitric acid (or more if much
pyrites, &c., is present) and continue the boiling till these are decomposed;
dilute and filter off, washing first with dilute acid and afterwards with a
little dilute ammonia, dry, ignite, and place in a combustion tube (together
with the filter-ash) and heat to redness for about thirty minutes in a current
of dried hydrogen.
The oxide of tin is placed in a porcelain boat (fig. 58), which is then
introduced into a piece of combustion tube. The latter, wrapped in a piece of
wire gauze, is supported on a couple of iron rings, and heated by one or two
Bunsen burners in a furnace fitted up with loose fire-brick tiles, as shown in
fig. 59.
Page 355
When the reduction is complete the tube is allowed to cool; the boat is
removed and the tin dissolved. Add a rod of zinc to the freely-acid hot
solution, and in a few minutes decant through a filter and wash with water,
after having removed the zinc. Wash the precipitated metal back into the
beaker, and dissolve in 10 c.c. of dilute nitric acid, evaporate off the excess
of acid; dilute, boil, and filter. Wash, dry, ignite strongly in a porcelain
crucible, and weigh.
In the absence of antimony the above separation works very well, but if this
metal is present in quantity the metals precipitated on the zinc must be
covered with hydrochloric acid and treated with a few drops of nitric. It is
then warmed with iron wire until no more of the latter dissolves. The
antimony is precipitated as metal, and the tin remains in solution as
stannous chloride. The antimony is filtered off, and may be washed with
alcohol, and weighed, whilst the tin in the filtrate is precipitated with zinc,
and treated as already described.
GRAVIMETRIC METHOD.
If the tin is not already in the metallic state it is reduced to this condition by
the method given (precipitation by zinc). Treat the finely-divided metal
(washed free from chlorides) in a four-inch evaporating dish with 10 c.c. of
dilute nitric acid, cover with a clock-glass, and apply a gentle heat until the
precipitate appears of a white colour and the metal is completely attacked.
Evaporate nearly to dryness on a water-bath; then add 50 c.c. of water, heat
to boiling, and filter. Wash with hot water, dry, transfer to a weighed
porcelain crucible, add the filter-ash, ignite strongly, and weigh. The
precipitate after ignition is stannic oxide (SnO2). It is a yellowish-white
powder (darker whilst hot), insoluble in acids, and contains 78.67 per cent.
of tin. Cold dilute nitric acid dissolves tin to a clear solution, which
removed and the tin dissolved. Add a rod of zinc to the freely-acid hot
solution, and in a few minutes decant through a filter and wash with water,
after having removed the zinc. Wash the precipitated metal back into the
beaker, and dissolve in 10 c.c. of dilute nitric acid, evaporate off the excess
of acid; dilute, boil, and filter. Wash, dry, ignite strongly in a porcelain
crucible, and weigh.
In the absence of antimony the above separation works very well, but if this
metal is present in quantity the metals precipitated on the zinc must be
covered with hydrochloric acid and treated with a few drops of nitric. It is
then warmed with iron wire until no more of the latter dissolves. The
antimony is precipitated as metal, and the tin remains in solution as
stannous chloride. The antimony is filtered off, and may be washed with
alcohol, and weighed, whilst the tin in the filtrate is precipitated with zinc,
and treated as already described.
GRAVIMETRIC METHOD.
If the tin is not already in the metallic state it is reduced to this condition by
the method given (precipitation by zinc). Treat the finely-divided metal
(washed free from chlorides) in a four-inch evaporating dish with 10 c.c. of
dilute nitric acid, cover with a clock-glass, and apply a gentle heat until the
precipitate appears of a white colour and the metal is completely attacked.
Evaporate nearly to dryness on a water-bath; then add 50 c.c. of water, heat
to boiling, and filter. Wash with hot water, dry, transfer to a weighed
porcelain crucible, add the filter-ash, ignite strongly, and weigh. The
precipitate after ignition is stannic oxide (SnO2). It is a yellowish-white
powder (darker whilst hot), insoluble in acids, and contains 78.67 per cent.
of tin. Cold dilute nitric acid dissolves tin to a clear solution, which
Page 356
becomes a white enamel-like jelly on heating; this (filtered off, washed, and
dried) forms an opal-like substance, which is converted on ignition into
stannic oxide with evolution of nitrous fumes. Stannic oxide when ignited
with chlorides is more or less completely converted into stannic chloride,
which volatilises. The presence of chlorides during the evaporation with
nitric acid causes a similar loss.
Determination of Tin in an Alloy.—(Bronze.)—Take 2 grams, and attack
with 20 c.c. of dilute nitric acid in a covered beaker with the aid of heat.
Boil till the bulk is reduced by one-half, dilute with 50 c.c. of water, allow
to settle for a few minutes, and filter; wash well first with water acidulated
with a little nitric acid, and afterwards with water; dry, ignite, and weigh as
stannic oxide.
Determination of Tin in Tin Ore.—Treat 5 grams of the dried and finely-
powdered ore with 30 c.c. of hydrochloric acid in a four-inch evaporating
dish. After the soluble oxides have been dissolved add 1 or 2 c.c. of nitric
acid, boil off nitrous fumes, dilute, and filter. Dry the filter, transfer the
cleaned ore to a piece of combustion tube ten or twelve inches long and
narrowed at one end. Pass a current of hydrogen through the tube and heat
to redness for 30 minutes; cool whilst the gas is still passing. Dissolve in 20
c.c. of dilute hydrochloric acid and keep the solution tinted with
permanganate of potassium. When the colour of the permanganate becomes
permanent dilute to a bulk of 50 c.c. with water, filter, and wash. Heat; add
a rod of zinc weighing about 3 grams; allow to stand for a few minutes;
decant through a filter; and wash, removing the remaining zinc and
returning the tin to the beaker. Treat with 5 c.c. of dilute nitric acid, boil for
some time, take up with water, filter, wash, dry, ignite, and weigh as stannic
oxide.
VOLUMETRIC METHOD.
Titration with Solution of Permanganate of Potassium.—This titration
may be made either directly on the solution of stannous chloride (prepared
by dissolving the precipitated metal in hydrochloric acid), or indirectly, on a
solution of ferrous chloride (produced by the reducing action of the
precipitated metal on ferric chloride). The standard solution of
dried) forms an opal-like substance, which is converted on ignition into
stannic oxide with evolution of nitrous fumes. Stannic oxide when ignited
with chlorides is more or less completely converted into stannic chloride,
which volatilises. The presence of chlorides during the evaporation with
nitric acid causes a similar loss.
Determination of Tin in an Alloy.—(Bronze.)—Take 2 grams, and attack
with 20 c.c. of dilute nitric acid in a covered beaker with the aid of heat.
Boil till the bulk is reduced by one-half, dilute with 50 c.c. of water, allow
to settle for a few minutes, and filter; wash well first with water acidulated
with a little nitric acid, and afterwards with water; dry, ignite, and weigh as
stannic oxide.
Determination of Tin in Tin Ore.—Treat 5 grams of the dried and finely-
powdered ore with 30 c.c. of hydrochloric acid in a four-inch evaporating
dish. After the soluble oxides have been dissolved add 1 or 2 c.c. of nitric
acid, boil off nitrous fumes, dilute, and filter. Dry the filter, transfer the
cleaned ore to a piece of combustion tube ten or twelve inches long and
narrowed at one end. Pass a current of hydrogen through the tube and heat
to redness for 30 minutes; cool whilst the gas is still passing. Dissolve in 20
c.c. of dilute hydrochloric acid and keep the solution tinted with
permanganate of potassium. When the colour of the permanganate becomes
permanent dilute to a bulk of 50 c.c. with water, filter, and wash. Heat; add
a rod of zinc weighing about 3 grams; allow to stand for a few minutes;
decant through a filter; and wash, removing the remaining zinc and
returning the tin to the beaker. Treat with 5 c.c. of dilute nitric acid, boil for
some time, take up with water, filter, wash, dry, ignite, and weigh as stannic
oxide.
VOLUMETRIC METHOD.
Titration with Solution of Permanganate of Potassium.—This titration
may be made either directly on the solution of stannous chloride (prepared
by dissolving the precipitated metal in hydrochloric acid), or indirectly, on a
solution of ferrous chloride (produced by the reducing action of the
precipitated metal on ferric chloride). The standard solution of
Page 357
permanganate of potassium is made by dissolving 5.356 grams of the salt in
water and diluting to one litre. 100 c.c. are equivalent to 1.00 gram of tin.
The precipitated tin is transferred to a flask; and dissolved in 10 c.c.
hydrochloric acid, with the aid of heat and in an atmosphere of carbonic
acid. The acid and metal are placed in the flask; which is then filled with the
gas, and stopped with a cork provided with a rubber valve. When solution is
complete the flask is again filled with carbonic acid. Fifty c.c. of water
freed from air and saturated with carbonic acid are then added. This water is
made by adding a gram of bicarbonate of soda and 2 c.c. of hydrochloric
acid to 100 c.c. of water: the effervescence sweeps out the dissolved
oxygen. The permanganate of potassium solution is then run in from a stop-
cock burette in the usual way until a faint pink tinge is obtained.
The following experiments show the effect of variations in the conditions of
the assay. A solution of stannous chloride equivalent in strength to the
"permanganate" was made by dissolving 19.06 grams of the crystallised salt
(SnCl2.2H2O.) in 50 c.c. of water and 10 c.c. of hydrochloric acid and
diluting to 1 litre with water freed from dissolved oxygen. 100 c.c. contain
1 gram of tin. In the first experiments tap water was used and no
precautions were taken for excluding air. Except when otherwise stated, 20
c.c. of the stannous chloride were used in each experiment with 10 c.c. of
hydrochloric acid, and were diluted to 100 c.c. with water before titration.
Effect of Varying Hydrochloric Acid.
Acid added 1.0 c.c. 10.0c.c. 20.0c.c. 50.0 c.c.
"Permanganate" required 18.8" 18.9" 18.8" 18.8 "
The only effect of the increase in quantity of acid was to give the brown of
perchloride of manganese instead of the pink of permanganic acid to mark
the finishing point.
Effect of Varying Temperature.
Temperature 15° C. 50° C. 70° C. 100° C.
"Permanganate" required 18.8 c.c. 18.7 c.c. 18.6 c.c. 18.4 c.c.
water and diluting to one litre. 100 c.c. are equivalent to 1.00 gram of tin.
The precipitated tin is transferred to a flask; and dissolved in 10 c.c.
hydrochloric acid, with the aid of heat and in an atmosphere of carbonic
acid. The acid and metal are placed in the flask; which is then filled with the
gas, and stopped with a cork provided with a rubber valve. When solution is
complete the flask is again filled with carbonic acid. Fifty c.c. of water
freed from air and saturated with carbonic acid are then added. This water is
made by adding a gram of bicarbonate of soda and 2 c.c. of hydrochloric
acid to 100 c.c. of water: the effervescence sweeps out the dissolved
oxygen. The permanganate of potassium solution is then run in from a stop-
cock burette in the usual way until a faint pink tinge is obtained.
The following experiments show the effect of variations in the conditions of
the assay. A solution of stannous chloride equivalent in strength to the
"permanganate" was made by dissolving 19.06 grams of the crystallised salt
(SnCl2.2H2O.) in 50 c.c. of water and 10 c.c. of hydrochloric acid and
diluting to 1 litre with water freed from dissolved oxygen. 100 c.c. contain
1 gram of tin. In the first experiments tap water was used and no
precautions were taken for excluding air. Except when otherwise stated, 20
c.c. of the stannous chloride were used in each experiment with 10 c.c. of
hydrochloric acid, and were diluted to 100 c.c. with water before titration.
Effect of Varying Hydrochloric Acid.
Acid added 1.0 c.c. 10.0c.c. 20.0c.c. 50.0 c.c.
"Permanganate" required 18.8" 18.9" 18.8" 18.8 "
The only effect of the increase in quantity of acid was to give the brown of
perchloride of manganese instead of the pink of permanganic acid to mark
the finishing point.
Effect of Varying Temperature.
Temperature 15° C. 50° C. 70° C. 100° C.
"Permanganate" required 18.8 c.c. 18.7 c.c. 18.6 c.c. 18.4 c.c.
Page 358
Rate of Atmospheric Oxidation.—Solutions ready for titration were
exposed to air at the ordinary temperature for varying lengths of time and
then titrated.
Time exposed 0 min. 5 min. 10 min. 20 min. 60 min.
"Permanganate" required 18.8 c.c. 18.8 c.c. 18.8 c.c. 18.8 c.c. 18.6 c.c.
It is best to titrate at once, although the loss by oxidation is only small after
one hour's exposure.
Effect of Varying Tin.
Stannous chloride added 1.0c.c. 10.0c.c. 20.0c.c. 50.0c.c. 100.0c.c.
"Permanganate" required 0.7" 8.8 " 18.0" 47.4" 95.4 "
Effect of Varying Bulk.
Bulk 50.0 c.c. 100.0c.c. 200.0c.c. 500.0c.c.
"Permanganate" required. 9.0 " 18.3 " 17.4 " 15.1 "
The two last series show an interference, which is due to the oxygen
dissolved in the water, as may be seen from the following similar
experiments, which were, however, performed with water freed from
oxygen and in which the titrations were effected in an atmosphere of
carbonic acid.
Effect of Varying Tin.—A new solution of stannous chloride was used.
Stannous chloride added 1.0c.c. 10.0c.c. 20.0c.c. 50.0c.c. 100.0c.c.
"Permanganate" required 1.0" 10.0" 19.8" 49.6" 99.3 "
Effect of Varying Bulk.
Bulk 30.0c.c. 50.0c.c. 100.0c.c. 200.0c.c. 500.0c.c.
"Permanganate" required 19.8" 19.8" 19.8 " 19.8 " 19.8 "
It will be seen that in working under these conditions the results are
proportional and the method satisfactory.
exposed to air at the ordinary temperature for varying lengths of time and
then titrated.
Time exposed 0 min. 5 min. 10 min. 20 min. 60 min.
"Permanganate" required 18.8 c.c. 18.8 c.c. 18.8 c.c. 18.8 c.c. 18.6 c.c.
It is best to titrate at once, although the loss by oxidation is only small after
one hour's exposure.
Effect of Varying Tin.
Stannous chloride added 1.0c.c. 10.0c.c. 20.0c.c. 50.0c.c. 100.0c.c.
"Permanganate" required 0.7" 8.8 " 18.0" 47.4" 95.4 "
Effect of Varying Bulk.
Bulk 50.0 c.c. 100.0c.c. 200.0c.c. 500.0c.c.
"Permanganate" required. 9.0 " 18.3 " 17.4 " 15.1 "
The two last series show an interference, which is due to the oxygen
dissolved in the water, as may be seen from the following similar
experiments, which were, however, performed with water freed from
oxygen and in which the titrations were effected in an atmosphere of
carbonic acid.
Effect of Varying Tin.—A new solution of stannous chloride was used.
Stannous chloride added 1.0c.c. 10.0c.c. 20.0c.c. 50.0c.c. 100.0c.c.
"Permanganate" required 1.0" 10.0" 19.8" 49.6" 99.3 "
Effect of Varying Bulk.
Bulk 30.0c.c. 50.0c.c. 100.0c.c. 200.0c.c. 500.0c.c.
"Permanganate" required 19.8" 19.8" 19.8 " 19.8 " 19.8 "
It will be seen that in working under these conditions the results are
proportional and the method satisfactory.
Page 359
Examination of Tin Phosphide.—(Phosphor Tin.)—This substance is used
in the manufacture of "phosphor bronze" and similar alloys. It is a
crystalline, imperfectly-malleable, metallic substance. It is soluble in
hydrochloric acid with effervescence; phosphoretted hydrogen, which
inflames on the addition of a drop or two of nitric acid, being evolved. It is
attacked by nitric acid, yielding a white powder of stannic phosphate; this is
not easily decomposed by ammonium sulphide or readily soluble in
hydrochloric acid.
"Phosphor-tin" is made up only of tin and phosphorus. For the estimation
weigh up 1 gram. Place in a weighed Berlin dish; and cover with 10 c.c. of
nitric acid and 3 or 4 c.c. of water. Let the reaction proceed (under a clock-
glass) on the water-bath till complete. Remove the glass; evaporate to
dryness, and ignite, at first gently over a Bunsen burner, and afterwards in
the muffle at a red heat. Cool in the desiccator, and weigh as quickly as
possible when cold. The substance contains the tin as stannic oxide, SnO2,
and the phosphorus as phosphoric oxide, P2O5. The increase in weight on
the gram of substance taken gives the weight of the oxygen taken up by the
phosphorus and tin, and since 1 gram of tin takes up only 0.271 gram of
oxygen, and 1 gram of phosphorus takes up 1.29 gram, the proportion of tin
to phosphorus can be calculated from the increase in weight. For example, 1
gram of a sample gave 1.3410 gram of mixed oxides, which is 0.070 gram
in excess of that which would be got with pure tin. If the substance was all
phosphorus the excess would be 1.0190 gram; consequently the proportion
of phosphorus in the substance is 0.070 / 1.019, or 6.87 per cent. The tin is
calculated by difference, 93.13 per cent.
Another method of separating and determining the phosphorus is as
follows:—Take 1 gram of the substance and add to it 15 c.c. of hot aqua
regia. Boil till dissolved, dilute, and precipitate the tin with sulphuretted
hydrogen. To the filtrate add ammonia and "magnesia mixture." Filter; wash
the precipitate with dilute ammonia; dry, ignite, and weigh as magnesic
pyrophosphate. Calculate the phosphorus, and take the tin by difference.
A sample of phosphor tin gave—
Tin 93.1 per cent. (by difference)
Phosphorus 6.9 "
in the manufacture of "phosphor bronze" and similar alloys. It is a
crystalline, imperfectly-malleable, metallic substance. It is soluble in
hydrochloric acid with effervescence; phosphoretted hydrogen, which
inflames on the addition of a drop or two of nitric acid, being evolved. It is
attacked by nitric acid, yielding a white powder of stannic phosphate; this is
not easily decomposed by ammonium sulphide or readily soluble in
hydrochloric acid.
"Phosphor-tin" is made up only of tin and phosphorus. For the estimation
weigh up 1 gram. Place in a weighed Berlin dish; and cover with 10 c.c. of
nitric acid and 3 or 4 c.c. of water. Let the reaction proceed (under a clock-
glass) on the water-bath till complete. Remove the glass; evaporate to
dryness, and ignite, at first gently over a Bunsen burner, and afterwards in
the muffle at a red heat. Cool in the desiccator, and weigh as quickly as
possible when cold. The substance contains the tin as stannic oxide, SnO2,
and the phosphorus as phosphoric oxide, P2O5. The increase in weight on
the gram of substance taken gives the weight of the oxygen taken up by the
phosphorus and tin, and since 1 gram of tin takes up only 0.271 gram of
oxygen, and 1 gram of phosphorus takes up 1.29 gram, the proportion of tin
to phosphorus can be calculated from the increase in weight. For example, 1
gram of a sample gave 1.3410 gram of mixed oxides, which is 0.070 gram
in excess of that which would be got with pure tin. If the substance was all
phosphorus the excess would be 1.0190 gram; consequently the proportion
of phosphorus in the substance is 0.070 / 1.019, or 6.87 per cent. The tin is
calculated by difference, 93.13 per cent.
Another method of separating and determining the phosphorus is as
follows:—Take 1 gram of the substance and add to it 15 c.c. of hot aqua
regia. Boil till dissolved, dilute, and precipitate the tin with sulphuretted
hydrogen. To the filtrate add ammonia and "magnesia mixture." Filter; wash
the precipitate with dilute ammonia; dry, ignite, and weigh as magnesic
pyrophosphate. Calculate the phosphorus, and take the tin by difference.
A sample of phosphor tin gave—
Tin 93.1 per cent. (by difference)
Phosphorus 6.9 "
Page 360
——-
100.0
Tin Arsenide.—This is met with in tin-smelting; it closely resembles the
phosphide, but the crystals have a duller grey appearance. It contains simply
tin and arsenic. The determination is made by treating 1 gram of the
substance with nitric acid and weighing the mixed oxides of tin and arsenic
in the same manner as in the case of the phosphide. One gram of arsenic
will give 1.533 gram of arsenic oxide, As2O5; consequently the excess of
weight of the mixed oxides over 1.271 gram must be divided by 0.262; the
result multiplied by 100 gives the percentage of arsenic. In consequence of
the higher atomic weight of arsenic the results by this method are not so
close as with the phosphide. Each milligram of excess weight (over 1.271)
represents 0.38 per cent. of arsenic, As. Both in this and in the
corresponding phosphide determination care must be taken to avoid
absorption of moisture, by allowing the oxides to cool in a desiccator and
weighing quickly.
The percentage of arsenic is better determined as follows:—Weigh up 1
gram of the substance, dissolve in aqua regia, dilute, and pass sulphuretted
hydrogen. Render alkaline with ammonia, and add ammonium sulphide till
the precipitate is dissolved. Add "magnesia mixture." Filter off the
precipitate, wash with dilute ammonia, ignite with a few drops of nitric
acid, and weigh as magnesic pyrarsenate. Calculate the arsenic and take the
tin by difference. A sample treated in this way gave—
Tin 96.8 per cent. by difference
Arsenic 3.2 "
——-
100.0
Examination of Black Tin.—Dry the ore, and reduce it to a fine powder.
Weigh up 2 grams, and boil with 20 c.c. of hydrochloric acid and 2 c.c. of
nitric for ten or fifteen minutes. Filter, and reserve the filtrate.
Tungstic Acid.—Digest the residue with about 50 c.c. of water and a few
c.c. of dilute ammonia for a few minutes, and filter; collect the filtrate in a
100.0
Tin Arsenide.—This is met with in tin-smelting; it closely resembles the
phosphide, but the crystals have a duller grey appearance. It contains simply
tin and arsenic. The determination is made by treating 1 gram of the
substance with nitric acid and weighing the mixed oxides of tin and arsenic
in the same manner as in the case of the phosphide. One gram of arsenic
will give 1.533 gram of arsenic oxide, As2O5; consequently the excess of
weight of the mixed oxides over 1.271 gram must be divided by 0.262; the
result multiplied by 100 gives the percentage of arsenic. In consequence of
the higher atomic weight of arsenic the results by this method are not so
close as with the phosphide. Each milligram of excess weight (over 1.271)
represents 0.38 per cent. of arsenic, As. Both in this and in the
corresponding phosphide determination care must be taken to avoid
absorption of moisture, by allowing the oxides to cool in a desiccator and
weighing quickly.
The percentage of arsenic is better determined as follows:—Weigh up 1
gram of the substance, dissolve in aqua regia, dilute, and pass sulphuretted
hydrogen. Render alkaline with ammonia, and add ammonium sulphide till
the precipitate is dissolved. Add "magnesia mixture." Filter off the
precipitate, wash with dilute ammonia, ignite with a few drops of nitric
acid, and weigh as magnesic pyrarsenate. Calculate the arsenic and take the
tin by difference. A sample treated in this way gave—
Tin 96.8 per cent. by difference
Arsenic 3.2 "
——-
100.0
Examination of Black Tin.—Dry the ore, and reduce it to a fine powder.
Weigh up 2 grams, and boil with 20 c.c. of hydrochloric acid and 2 c.c. of
nitric for ten or fifteen minutes. Filter, and reserve the filtrate.
Tungstic Acid.—Digest the residue with about 50 c.c. of water and a few
c.c. of dilute ammonia for a few minutes, and filter; collect the filtrate in a
Page 361
weighed porcelain dish, evaporate to dryness, ignite, and weigh as tungstic
acid, WO3.
Stannic Oxide.—Dry, ignite, and weigh the insoluble residue. Transfer to a
porcelain boat, and reduce in a current of hydrogen at a red heat for half an
hour. Allow to cool whilst the hydrogen is still passing. Transfer the boat to
a beaker, and dissolve up the tin in 10 c.c. of hydrochloric acid and a c.c. or
so of nitric. Wash out the combustion tube with some acid and add the
washing to the contents of the beaker. Warm gently, dilute with water, and
filter. Collect, dry, ignite, and weigh the insoluble residue. Through the
filtrate pass a rapid current of sulphuretted hydrogen, allow to settle, and
filter. Wash the precipitate with hot water, dry, calcine gently; ignite with
ammonium carbonate, and weigh as stannic oxide, SnO2. The insoluble
residue will in most cases retain some tin. Fuse it with fusion mixture, take
up with hydrochloric acid, filter, pass sulphuretted hydrogen through the
filtrate, collect and wash the sulphide of tin. Ignite and weigh as stannic
oxide, and add it to that previously obtained.
Copper.—Pass sulphuretted hydrogen through the acid filtrate obtained in
the first cleaning of the ore, collect the precipitate, and wash first with soda
solution and then with hot water. Dry, ignite, and weigh as cupric oxide,
CuO. Mix the filtrate with that from the main portion of the sulphide of tin.
Ferric Oxide.—Boil off the sulphuretted hydrogen from the mixed filtrates
and peroxidise with nitric acid. Add ammonia in slight excess, boil, filter,
dry, ignite, and weigh the precipitate as ferric oxide. This will be practically
pure, but the iron in it must be determined by dissolving and titrating. The
filtrate from the iron may contain zinc, lime, and magnesia, but rarely in
quantities sufficient to be determined.
Silica, &c.—-The silica may be calculated from the weight of the residue
insoluble in acid, after the reduction of the tin in hydrogen, by deducting
from it the weight of the oxide of tin subsequently found. Or it may be
determined as follows:—The insoluble portion is fused with fusion mixture,
and taken up with hydrochloric acid, as already described. On filtering, the
filter will retain a portion of the silica. The rest is recovered, after the
removal of the stannous sulphide, by evaporating to dryness, taking up with
hydrochloric acid, and filtering through the same filter. It is washed, dried,
acid, WO3.
Stannic Oxide.—Dry, ignite, and weigh the insoluble residue. Transfer to a
porcelain boat, and reduce in a current of hydrogen at a red heat for half an
hour. Allow to cool whilst the hydrogen is still passing. Transfer the boat to
a beaker, and dissolve up the tin in 10 c.c. of hydrochloric acid and a c.c. or
so of nitric. Wash out the combustion tube with some acid and add the
washing to the contents of the beaker. Warm gently, dilute with water, and
filter. Collect, dry, ignite, and weigh the insoluble residue. Through the
filtrate pass a rapid current of sulphuretted hydrogen, allow to settle, and
filter. Wash the precipitate with hot water, dry, calcine gently; ignite with
ammonium carbonate, and weigh as stannic oxide, SnO2. The insoluble
residue will in most cases retain some tin. Fuse it with fusion mixture, take
up with hydrochloric acid, filter, pass sulphuretted hydrogen through the
filtrate, collect and wash the sulphide of tin. Ignite and weigh as stannic
oxide, and add it to that previously obtained.
Copper.—Pass sulphuretted hydrogen through the acid filtrate obtained in
the first cleaning of the ore, collect the precipitate, and wash first with soda
solution and then with hot water. Dry, ignite, and weigh as cupric oxide,
CuO. Mix the filtrate with that from the main portion of the sulphide of tin.
Ferric Oxide.—Boil off the sulphuretted hydrogen from the mixed filtrates
and peroxidise with nitric acid. Add ammonia in slight excess, boil, filter,
dry, ignite, and weigh the precipitate as ferric oxide. This will be practically
pure, but the iron in it must be determined by dissolving and titrating. The
filtrate from the iron may contain zinc, lime, and magnesia, but rarely in
quantities sufficient to be determined.
Silica, &c.—-The silica may be calculated from the weight of the residue
insoluble in acid, after the reduction of the tin in hydrogen, by deducting
from it the weight of the oxide of tin subsequently found. Or it may be
determined as follows:—The insoluble portion is fused with fusion mixture,
and taken up with hydrochloric acid, as already described. On filtering, the
filter will retain a portion of the silica. The rest is recovered, after the
removal of the stannous sulphide, by evaporating to dryness, taking up with
hydrochloric acid, and filtering through the same filter. It is washed, dried,
Page 362
ignited, and weighed as silica. The filtrate from the silica is boiled with a
little nitric acid and precipitated with ammonia. The precipitate is collected,
washed, ignited, and weighed as ferric oxide and alumina (but it frequently
contains oxide of titanium). When the last is present it is determined by
fusing with bisulphate of potash and extracting with cold water. The
solution is nearly neutralised with ammonia, charged with sulphurous acid,
and boiled. The precipitate is collected, washed, dried, ignited, and weighed
as oxide of titanium, TiO2. The difference between this weight and that of
the combined oxides gives the ferric oxide and alumina. The filtrate from
the mixed oxides is examined for lime and magnesia.
Sulphur.—Rub up 5 grams of the ore with 5 grams of nitre, transfer to a
porcelain dish, and fuse over a Bunsen burner for fifteen minutes. When
cold, extract with water, and determine the sulphur volumetrically with
standard barium chloride. The sulphur may be present as sulphide or
sulphate.
Arsenic.—Take 5 grams, and evaporate with nitric acid; dilute, add
ammonia, pass sulphuretted hydrogen, and filter.
To the filtrate add "magnesia mixture." Collect the precipitate, ignite with
nitric acid, and weigh as magnesic pyrarsenate.
The following may be taken as an example of the composition of an impure
black tin:—
Tungstic acid 1.8%
Stannic oxide 79.0
Silica 2.6
Titanic oxide 0.8
Copper oxide 0.9
Ferric oxide 13.4
Sulphur 0.4
Arsenic 0.3
——
99.2
little nitric acid and precipitated with ammonia. The precipitate is collected,
washed, ignited, and weighed as ferric oxide and alumina (but it frequently
contains oxide of titanium). When the last is present it is determined by
fusing with bisulphate of potash and extracting with cold water. The
solution is nearly neutralised with ammonia, charged with sulphurous acid,
and boiled. The precipitate is collected, washed, dried, ignited, and weighed
as oxide of titanium, TiO2. The difference between this weight and that of
the combined oxides gives the ferric oxide and alumina. The filtrate from
the mixed oxides is examined for lime and magnesia.
Sulphur.—Rub up 5 grams of the ore with 5 grams of nitre, transfer to a
porcelain dish, and fuse over a Bunsen burner for fifteen minutes. When
cold, extract with water, and determine the sulphur volumetrically with
standard barium chloride. The sulphur may be present as sulphide or
sulphate.
Arsenic.—Take 5 grams, and evaporate with nitric acid; dilute, add
ammonia, pass sulphuretted hydrogen, and filter.
To the filtrate add "magnesia mixture." Collect the precipitate, ignite with
nitric acid, and weigh as magnesic pyrarsenate.
The following may be taken as an example of the composition of an impure
black tin:—
Tungstic acid 1.8%
Stannic oxide 79.0
Silica 2.6
Titanic oxide 0.8
Copper oxide 0.9
Ferric oxide 13.4
Sulphur 0.4
Arsenic 0.3
——
99.2
Page 363
Examination of Hardhead.—In the smelting of tin ores a quantity of
speise, known as "hardhead," is produced. It is essentially an arsenide of
iron, carrying a considerable quantity of tin. Much of this last is present in
the form of small buttons of metal distributed through the mass. The buttons
can be seen on careful inspection, and become evident on powdering.
In assaying the substance, a variation in the usual method of sampling is
required, because of the quantity of metal present which cannot be
powdered. After powdering as finely as possible, the coarse particles are
sifted off and weighed. The weight of the powder is also taken. The method
of working is best illustrated by an example. A sample of hardhead weighed
155.1 grams, and gave 21.0 grams of coarse particles, equivalent to 13.5 per
cent. of the whole. The fine portion weighed 134 grams, which is equivalent
to 86.5 per cent.
Thirteen and a half grams of the coarse material were dissolved in aqua
regia, and diluted with water to 1 litre. Ten c.c. of this contain 0.135 gram
of the metallic portion, which is the amount contained in 1 gram of the
original hardhead. If, in a determination, 1 gram of the substance is wanted,
weigh up 0.865 gram of the powdered portion, and add to it 10 c.c. of the
solution. It will be seen that these together make up 1 gram of the original
sample. The solution of the metallic portion must be saved until the analysis
is finished.
Tin and Copper.—Weigh up the portion of the powdered stuff equivalent
to 1 gram of the sample. Transfer to a flask, and cover with 10 c.c. of the
solution of the metallic portion and 10 c.c. of aqua regia. Boil gently till
oxidation is complete and the nitric acid for the greater part driven off.
Dilute to 100 c.c. with water, and pass sulphuretted hydrogen for some
time. Filter, wash with hot water, and rinse through the funnel back into the
flask. Digest with yellow sodium sulphide until only a light, flocculent,
black precipitate is left. Filter this off, wash with hot water, dry, calcine,
treat with a little nitric acid, ignite, and weigh as copper oxide, CuO. The
weight multiplied by 0.7983 gives the weight of copper.
The filtrate containing the tin is rendered acid with hydrochloric acid, and
filtered. The precipitate is rinsed into a half-pint beaker, covered with 20
c.c. of hydrochloric acid, and boiled down to about 20 c.c. The solution is
speise, known as "hardhead," is produced. It is essentially an arsenide of
iron, carrying a considerable quantity of tin. Much of this last is present in
the form of small buttons of metal distributed through the mass. The buttons
can be seen on careful inspection, and become evident on powdering.
In assaying the substance, a variation in the usual method of sampling is
required, because of the quantity of metal present which cannot be
powdered. After powdering as finely as possible, the coarse particles are
sifted off and weighed. The weight of the powder is also taken. The method
of working is best illustrated by an example. A sample of hardhead weighed
155.1 grams, and gave 21.0 grams of coarse particles, equivalent to 13.5 per
cent. of the whole. The fine portion weighed 134 grams, which is equivalent
to 86.5 per cent.
Thirteen and a half grams of the coarse material were dissolved in aqua
regia, and diluted with water to 1 litre. Ten c.c. of this contain 0.135 gram
of the metallic portion, which is the amount contained in 1 gram of the
original hardhead. If, in a determination, 1 gram of the substance is wanted,
weigh up 0.865 gram of the powdered portion, and add to it 10 c.c. of the
solution. It will be seen that these together make up 1 gram of the original
sample. The solution of the metallic portion must be saved until the analysis
is finished.
Tin and Copper.—Weigh up the portion of the powdered stuff equivalent
to 1 gram of the sample. Transfer to a flask, and cover with 10 c.c. of the
solution of the metallic portion and 10 c.c. of aqua regia. Boil gently till
oxidation is complete and the nitric acid for the greater part driven off.
Dilute to 100 c.c. with water, and pass sulphuretted hydrogen for some
time. Filter, wash with hot water, and rinse through the funnel back into the
flask. Digest with yellow sodium sulphide until only a light, flocculent,
black precipitate is left. Filter this off, wash with hot water, dry, calcine,
treat with a little nitric acid, ignite, and weigh as copper oxide, CuO. The
weight multiplied by 0.7983 gives the weight of copper.
The filtrate containing the tin is rendered acid with hydrochloric acid, and
filtered. The precipitate is rinsed into a half-pint beaker, covered with 20
c.c. of hydrochloric acid, and boiled down to about 20 c.c. The solution is
Page 364
filtered off from the sulphur and sulphide of arsenic, which, after washing
with hot water, is transferred to a flask labelled "arsenic." A strip of sheet
zinc (2 in. by 1 in.) is placed in the solution. The evolution of hydrogen
should be brisk. In five or ten minutes decant off a few c.c. of the liquid,
and test with sulphuretted hydrogen for tin. If no yellowish precipitate is
formed, decant off the rest of the liquid, and wash the precipitated metal
with hot water two or three times by decantation. The metal should be in a
lump; if there are any floating particles they must be made to sink by
compression with a glass rod. Transfer the washed metal to an evaporating
dish 3 or 4 in. across, and cover with a few c.c. of hot water. Add nitric acid
drop by drop till the tin is completely attacked. Evaporate nearly to dryness,
and add a drop or two more of nitric acid and 20 c.c. of water. Boil and
filter. Wash with hot water, dry, ignite, and weigh as stannic oxide, SnO2.
Calculate to metallic tin by multiplying by 0.7867.[76]
The filtrate from the first treatment with sulphuretted hydrogen will
probably no longer smell of the gas. Warm and pass the gas for a few
minutes longer. Filter off any precipitate of sulphide of arsenic, and transfer
it to the flask for "arsenic." Boil the filtrate (ignoring any signs of a further
precipitation of arsenic) with a few c.c. of nitric acid, and separate the iron
as basic acetate. Wash; reserve the filtrate for cobalt.
Iron.—Rinse back the "basic acetate," precipitate into the flask, add
ammonia, dilute with water to about 100 c.c., and pass sulphuretted
hydrogen for a few minutes. Filter, and wash with hot water. Collect the
filtrate in the flask labelled "arsenic." Boil the precipitate with dilute
sulphuric acid, filter, and titrate the filtrate with the permanganate of
potassium solution after boiling off the sulphuretted hydrogen. Report the
result as iron. The sulphuric acid will not effect complete solution, a light
black residue will remain, chiefly sulphur; this must be rinsed into the
filtrate from the acetate separation. It contains cobalt.
Cobalt.—The filtrate from the acetate separation will have a pink colour.
Render it ammoniacal and pass sulphuretted hydrogen. Collect the
precipitate on a filter, dry, and ignite. Dissolve in hydrochloric acid, and
evaporate nearly to dryness with an excess of nitric acid. Dilute with 10 or
20 c.c. of water and add potash solution in slight excess. Add acetic acid
until the solution is acid and the precipitate is quite dissolved. Add 20 or 30
with hot water, is transferred to a flask labelled "arsenic." A strip of sheet
zinc (2 in. by 1 in.) is placed in the solution. The evolution of hydrogen
should be brisk. In five or ten minutes decant off a few c.c. of the liquid,
and test with sulphuretted hydrogen for tin. If no yellowish precipitate is
formed, decant off the rest of the liquid, and wash the precipitated metal
with hot water two or three times by decantation. The metal should be in a
lump; if there are any floating particles they must be made to sink by
compression with a glass rod. Transfer the washed metal to an evaporating
dish 3 or 4 in. across, and cover with a few c.c. of hot water. Add nitric acid
drop by drop till the tin is completely attacked. Evaporate nearly to dryness,
and add a drop or two more of nitric acid and 20 c.c. of water. Boil and
filter. Wash with hot water, dry, ignite, and weigh as stannic oxide, SnO2.
Calculate to metallic tin by multiplying by 0.7867.[76]
The filtrate from the first treatment with sulphuretted hydrogen will
probably no longer smell of the gas. Warm and pass the gas for a few
minutes longer. Filter off any precipitate of sulphide of arsenic, and transfer
it to the flask for "arsenic." Boil the filtrate (ignoring any signs of a further
precipitation of arsenic) with a few c.c. of nitric acid, and separate the iron
as basic acetate. Wash; reserve the filtrate for cobalt.
Iron.—Rinse back the "basic acetate," precipitate into the flask, add
ammonia, dilute with water to about 100 c.c., and pass sulphuretted
hydrogen for a few minutes. Filter, and wash with hot water. Collect the
filtrate in the flask labelled "arsenic." Boil the precipitate with dilute
sulphuric acid, filter, and titrate the filtrate with the permanganate of
potassium solution after boiling off the sulphuretted hydrogen. Report the
result as iron. The sulphuric acid will not effect complete solution, a light
black residue will remain, chiefly sulphur; this must be rinsed into the
filtrate from the acetate separation. It contains cobalt.
Cobalt.—The filtrate from the acetate separation will have a pink colour.
Render it ammoniacal and pass sulphuretted hydrogen. Collect the
precipitate on a filter, dry, and ignite. Dissolve in hydrochloric acid, and
evaporate nearly to dryness with an excess of nitric acid. Dilute with 10 or
20 c.c. of water and add potash solution in slight excess. Add acetic acid
until the solution is acid and the precipitate is quite dissolved. Add 20 or 30
Page 365
c.c. of a strong solution of potassium nitrite, and determine the cobalt, as
described on pp. 254, 256. Boil the filtrate from the cobalt, precipitate with
hydrochloric acid, render ammoniacal, and test for zinc, nickel, and
manganese.
The remainder of the tin will be contained in the flask labelled "arsenic."
Acidify with hydrochloric acid and filter. Rinse into a beaker, and evaporate
to a small bulk with 10 c.c. of nitric acid. Dilute and filter. Dry the
precipitate, consisting of stannic arsenate (2SnO2.As2O5), ignite, and
weigh. Calculate the tin it contains by multiplying by 0.4453, and add to
that already found.
Arsenic.—This is determined in a separate portion. Weigh up a portion of
the powder equivalent to 1 gram of the hardhead, place in a pint flask, and
boil with 10 c.c. of nitric acid. When action has ceased add 10 c.c. of the
solution of the metallic portion and then hydrochloric acid (a few drops at a
time) till solution is complete. Warm gently in dissolving, but do not boil.
Dilute to about 100 c.c., render alkaline with ammonia, and add 20 c.c. of
yellow ammonium sulphide. Digest at a gentle heat for about thirty minutes,
filter, and wash. Add 50 c.c. of magnesia mixture, shake well, allow to
stand for an hour, filter, and wash with dilute ammonia. The precipitate is
dissolved and then titrated with uranium acetate, or it is evaporated with
nitric acid, ignited, and weighed as pyrarsenate of magnesia. Calculate the
result to arsenic, As.
Sulphur.—Weigh up a portion of the powder equivalent to 2 or 3 grams of
the hardhead. Rub up in a mortar with 5 grams of nitre and fuse in a
porcelain dish for ten minutes. Extract with water, add 20 or 30 c.c. (as the
case may be) of the solution of the "metallics." Add 10 grams of sodic
acetate, and ferric chloride until the precipitate turns brown; dilute with
water to half a litre, boil, and titrate with standard baric chloride, as
described under Sulphur. Report as sulphur.
A sample of hardhead examined in this way gave—
Sulphur 3.00%
Arsenic 27.10
Tin 22.2
described on pp. 254, 256. Boil the filtrate from the cobalt, precipitate with
hydrochloric acid, render ammoniacal, and test for zinc, nickel, and
manganese.
The remainder of the tin will be contained in the flask labelled "arsenic."
Acidify with hydrochloric acid and filter. Rinse into a beaker, and evaporate
to a small bulk with 10 c.c. of nitric acid. Dilute and filter. Dry the
precipitate, consisting of stannic arsenate (2SnO2.As2O5), ignite, and
weigh. Calculate the tin it contains by multiplying by 0.4453, and add to
that already found.
Arsenic.—This is determined in a separate portion. Weigh up a portion of
the powder equivalent to 1 gram of the hardhead, place in a pint flask, and
boil with 10 c.c. of nitric acid. When action has ceased add 10 c.c. of the
solution of the metallic portion and then hydrochloric acid (a few drops at a
time) till solution is complete. Warm gently in dissolving, but do not boil.
Dilute to about 100 c.c., render alkaline with ammonia, and add 20 c.c. of
yellow ammonium sulphide. Digest at a gentle heat for about thirty minutes,
filter, and wash. Add 50 c.c. of magnesia mixture, shake well, allow to
stand for an hour, filter, and wash with dilute ammonia. The precipitate is
dissolved and then titrated with uranium acetate, or it is evaporated with
nitric acid, ignited, and weighed as pyrarsenate of magnesia. Calculate the
result to arsenic, As.
Sulphur.—Weigh up a portion of the powder equivalent to 2 or 3 grams of
the hardhead. Rub up in a mortar with 5 grams of nitre and fuse in a
porcelain dish for ten minutes. Extract with water, add 20 or 30 c.c. (as the
case may be) of the solution of the "metallics." Add 10 grams of sodic
acetate, and ferric chloride until the precipitate turns brown; dilute with
water to half a litre, boil, and titrate with standard baric chloride, as
described under Sulphur. Report as sulphur.
A sample of hardhead examined in this way gave—
Sulphur 3.00%
Arsenic 27.10
Tin 22.2
Page 366
Copper 1.64
Iron 43.2
Cobalt 2.6
———
99.74
Examination of Tin Slags.—In tin smelting works the term "slag" is
applied to the unfused portion of the charge. It is made up of unburnt
anthracite and small lumps of slag proper together with some buttons of
metallic tin. This is rarely, if ever, assayed. The slag proper (or, as it is
generally called, "glass") is a silicate of iron, alumina, and lime, containing
from 3 to 7 per cent. of tin. It is thus examined:—The sample after bruising
on an iron plate, is reduced to a very fine powder by grinding in an agate
mortar. In this state it is in most cases readily decomposed by hydrochloric
acid.
Determination of Tin.—Where the percentage of tin only is required, take
2 grams of the powdered slag and well mix with it 20 c.c. of hydrochloric
acid, and heat to boiling. Add 1 c.c. of nitric acid, allow to stand for fifteen
minutes, dilute with water, and filter. Pass a rapid current of sulphuretted
hydrogen for some time. Allow to settle, and filter. The precipitate, after
washing with hot water, is dried, and gently calcined until the greater part of
the sulphur is burnt off. It is then strongly ignited in the muffle (or over the
blowpipe) with the addition of a small lump of ammonic carbonate. The
residue is weighed as stannic oxide (SnO2); and is calculated to metallic tin
by multiplying by 0.787. The percentage on the slag is calculated in the
usual way.
The tin is always best determined in the examination of slags by a separate
assay carried out in this way. The determination of the other constituents is
thus made:—
Silica.—Take 2 grams of the powdered slag and cover them, in a small
evaporating dish, with 20 c.c. of hydrochloric acid; mix well by stirring
with a glass rod; and evaporate to dryness. If (as is generally the case)
tungsten is present the solution will be blue. Take up with 20 c.c. of
hydrochloric acid. Add 1 c.c. of nitric acid; and reduce by boiling to about
half the bulk. Add about 20 c.c. of water, boil, and filter. Wash the residue
Iron 43.2
Cobalt 2.6
———
99.74
Examination of Tin Slags.—In tin smelting works the term "slag" is
applied to the unfused portion of the charge. It is made up of unburnt
anthracite and small lumps of slag proper together with some buttons of
metallic tin. This is rarely, if ever, assayed. The slag proper (or, as it is
generally called, "glass") is a silicate of iron, alumina, and lime, containing
from 3 to 7 per cent. of tin. It is thus examined:—The sample after bruising
on an iron plate, is reduced to a very fine powder by grinding in an agate
mortar. In this state it is in most cases readily decomposed by hydrochloric
acid.
Determination of Tin.—Where the percentage of tin only is required, take
2 grams of the powdered slag and well mix with it 20 c.c. of hydrochloric
acid, and heat to boiling. Add 1 c.c. of nitric acid, allow to stand for fifteen
minutes, dilute with water, and filter. Pass a rapid current of sulphuretted
hydrogen for some time. Allow to settle, and filter. The precipitate, after
washing with hot water, is dried, and gently calcined until the greater part of
the sulphur is burnt off. It is then strongly ignited in the muffle (or over the
blowpipe) with the addition of a small lump of ammonic carbonate. The
residue is weighed as stannic oxide (SnO2); and is calculated to metallic tin
by multiplying by 0.787. The percentage on the slag is calculated in the
usual way.
The tin is always best determined in the examination of slags by a separate
assay carried out in this way. The determination of the other constituents is
thus made:—
Silica.—Take 2 grams of the powdered slag and cover them, in a small
evaporating dish, with 20 c.c. of hydrochloric acid; mix well by stirring
with a glass rod; and evaporate to dryness. If (as is generally the case)
tungsten is present the solution will be blue. Take up with 20 c.c. of
hydrochloric acid. Add 1 c.c. of nitric acid; and reduce by boiling to about
half the bulk. Add about 20 c.c. of water, boil, and filter. Wash the residue
Page 367
with hot dilute hydrochloric acid. It consists of silica with the tungstic acid.
Wash it back into the dish; and digest with 5 or 10 c.c. of a cold solution of
ammonic carbonate. Filter; and collect the filtrate and washings in a
weighed porcelain dish. Dry the residue, ignite strongly, and weigh as silica,
SiO2. In certain exceptional cases this may contain some unaltered
cassiterite, which is easily recognised by its appearance.
Tungsten.—The ammonic carbonate filtrate from the silica is evaporated to
dryness, ignited strongly over the blowpipe, and weighed. The residue is
tungstic acid, WO3. The tungsten may be conveniently reported in this
form, although it is probably present as a lower oxide.
Tin.—The acid filtrate from the silica and tungstic acid is treated with
sulphuretted hydrogen. The sulphide of tin is filtered off. Since the
percentage of tin has been already determined, this precipitate may be
neglected; or may be treated in the same way as the previous one, so as to
check the result. Since some stannic chloride will have been lost in the
evaporation, a low result may be expected. The tin should be reported as
stannous oxide; and is calculated by multiplying the percentage of tin by
1.136.
The filtrate from the tin is boiled rapidly down to remove sulphuretted
hydrogen; and then peroxidised with 1 or 2 c.c. of nitric acid. It is cooled,
transferred to a graduated flask, and diluted with water to 200 c.c.
Ferrous Oxide and Alumina.—Half the filtrate from the tin (that is, 100
c.c.) is taken, nearly neutralised with soda, and treated with sodium acetate.
The basic acetate precipitate obtained on boiling is filtered off and washed.
Reserve the filtrate. The precipitate is dissolved off the filter with hot dilute
hydrochloric acid; and the solution thus formed is treated with a slight
excess of ammonia, and boiled. The precipitate is filtered off, washed with
hot water, dried, ignited, and weighed as mixed ferric oxide and alumina.
The ignited precipitate is then dissolved with sulphuric and hydrochloric
acids; and the iron determined in the solution by titration with the solution
of stannous chloride. The iron found is calculated to and reported as ferrous
oxide, FeO (factor = 1.286). To find the alumina, which is best estimated by
difference, multiply the iron by 1.428 to get the weight of ferric oxide, and
deduct this from the weight of alumina and ferric oxide found. This, of
Wash it back into the dish; and digest with 5 or 10 c.c. of a cold solution of
ammonic carbonate. Filter; and collect the filtrate and washings in a
weighed porcelain dish. Dry the residue, ignite strongly, and weigh as silica,
SiO2. In certain exceptional cases this may contain some unaltered
cassiterite, which is easily recognised by its appearance.
Tungsten.—The ammonic carbonate filtrate from the silica is evaporated to
dryness, ignited strongly over the blowpipe, and weighed. The residue is
tungstic acid, WO3. The tungsten may be conveniently reported in this
form, although it is probably present as a lower oxide.
Tin.—The acid filtrate from the silica and tungstic acid is treated with
sulphuretted hydrogen. The sulphide of tin is filtered off. Since the
percentage of tin has been already determined, this precipitate may be
neglected; or may be treated in the same way as the previous one, so as to
check the result. Since some stannic chloride will have been lost in the
evaporation, a low result may be expected. The tin should be reported as
stannous oxide; and is calculated by multiplying the percentage of tin by
1.136.
The filtrate from the tin is boiled rapidly down to remove sulphuretted
hydrogen; and then peroxidised with 1 or 2 c.c. of nitric acid. It is cooled,
transferred to a graduated flask, and diluted with water to 200 c.c.
Ferrous Oxide and Alumina.—Half the filtrate from the tin (that is, 100
c.c.) is taken, nearly neutralised with soda, and treated with sodium acetate.
The basic acetate precipitate obtained on boiling is filtered off and washed.
Reserve the filtrate. The precipitate is dissolved off the filter with hot dilute
hydrochloric acid; and the solution thus formed is treated with a slight
excess of ammonia, and boiled. The precipitate is filtered off, washed with
hot water, dried, ignited, and weighed as mixed ferric oxide and alumina.
The ignited precipitate is then dissolved with sulphuric and hydrochloric
acids; and the iron determined in the solution by titration with the solution
of stannous chloride. The iron found is calculated to and reported as ferrous
oxide, FeO (factor = 1.286). To find the alumina, which is best estimated by
difference, multiply the iron by 1.428 to get the weight of ferric oxide, and
deduct this from the weight of alumina and ferric oxide found. This, of
Page 368
course, gives the alumina. A direct determination may be made by removing
the tin from the titrated solution with sulphuretted hydrogen, filtering,
nearly neutralising with ammonia, and boiling with a few grams of
hyposulphite of soda. The precipitate, filtered, washed, and ignited, is the
alumina, which is weighed. The direct determination gives a slightly low
result.
Oxides of Zinc and Manganese.—These are determined in the filtrate
from the basic acetate precipitate by rendering alkaline with ammonia, and
passing a current of sulphuretted hydrogen. Generally a small, but decided,
precipitate of alumina comes down, together with sulphides of any zinc or
manganese which is present. The precipitate is allowed to settle, dried,
ignited, and weighed. The metals are separately determined in it; and the
residue is counted as alumina, and added to that already found. The mixed
precipitate amounts to from 1 to 2 per cent. of the sample.
Lime.—The filtrate from the last is treated with ammonic oxalate, boiled
for a few minutes, allowed to settle, and filtered. The precipitate is washed
with hot water; dried; ignited; and weighed as carbonate, after gentle
ignition; or as lime, after strong ignition in the muffle.
Magnesia.—The filtrate from the lime is treated with sodic phosphate and
ammonia. It is well mixed by stirring, and allowed to stand overnight. The
precipitate is washed with dilute ammonia, dried, ignited, and weighed as
pyrophosphate.
Soda and Potash.—These are determined in the remaining half of the
filtrate from the tin. The solution is rendered ammoniacal with ammonia;
and treated, first with sulphuretted hydrogen, and then with ammonium
oxalate. The precipitate is filtered off and rejected. The filtrate is evaporated
in a small porcelain dish over a Bunsen burner, or on the sand bath; and
towards the close (or earlier if the evaporation is not proceeding well) nitric
acid is added. The evaporation is carried to dryness; and the residue heated
nearly to redness. The residue, which consists of magnesia with carbonates
and chlorides of the alkalies, is extracted with water; and filtered. The
filtrate is evaporated with hydrochloric acid in a weighed platinum dish,
ignited gently, and weighed. This gives the weight of the mixed chlorides of
the tin from the titrated solution with sulphuretted hydrogen, filtering,
nearly neutralising with ammonia, and boiling with a few grams of
hyposulphite of soda. The precipitate, filtered, washed, and ignited, is the
alumina, which is weighed. The direct determination gives a slightly low
result.
Oxides of Zinc and Manganese.—These are determined in the filtrate
from the basic acetate precipitate by rendering alkaline with ammonia, and
passing a current of sulphuretted hydrogen. Generally a small, but decided,
precipitate of alumina comes down, together with sulphides of any zinc or
manganese which is present. The precipitate is allowed to settle, dried,
ignited, and weighed. The metals are separately determined in it; and the
residue is counted as alumina, and added to that already found. The mixed
precipitate amounts to from 1 to 2 per cent. of the sample.
Lime.—The filtrate from the last is treated with ammonic oxalate, boiled
for a few minutes, allowed to settle, and filtered. The precipitate is washed
with hot water; dried; ignited; and weighed as carbonate, after gentle
ignition; or as lime, after strong ignition in the muffle.
Magnesia.—The filtrate from the lime is treated with sodic phosphate and
ammonia. It is well mixed by stirring, and allowed to stand overnight. The
precipitate is washed with dilute ammonia, dried, ignited, and weighed as
pyrophosphate.
Soda and Potash.—These are determined in the remaining half of the
filtrate from the tin. The solution is rendered ammoniacal with ammonia;
and treated, first with sulphuretted hydrogen, and then with ammonium
oxalate. The precipitate is filtered off and rejected. The filtrate is evaporated
in a small porcelain dish over a Bunsen burner, or on the sand bath; and
towards the close (or earlier if the evaporation is not proceeding well) nitric
acid is added. The evaporation is carried to dryness; and the residue heated
nearly to redness. The residue, which consists of magnesia with carbonates
and chlorides of the alkalies, is extracted with water; and filtered. The
filtrate is evaporated with hydrochloric acid in a weighed platinum dish,
ignited gently, and weighed. This gives the weight of the mixed chlorides of
Page 369
sodium and potassium; which are then separated and determined as
described under Potash.
It must be remembered when calculating the percentage that (with the
exception of the silica, tungstic acid, and tin) the determinations have been
made on 1 gram of the sample.
The following analysis will illustrate the composition of such a slag:—
Tungstic acid 1.3%
Silica 39.4
Stannous oxide 8.1
Ferrous oxide 26.2
Alumina 14.8
Oxide of manganese traces
Lime 7.9
Magnesia 0.5
Alkalies calculated as soda 1.7
———
99.9
TITANIUM.
Titanium only occurs as a mineral in its oxidised state, or as titanic oxide
(TiO2). It is a substance which has little commercial value, and is generally
recognised as one of the rare bodies; although, in small quantities, it is
widely disseminated. It occurs in granite, basalt, and other igneous rocks in
quantities up to as much as 1 per cent. It is also met with in clays and iron
ores, and in river sands, in which it is often associated with stream tin. The
proper minerals of titanium are rutile (TiO2), titaniferous iron (titanate of
iron), and sphene (titanate and silicate of lime).
The oxide of titanium (like cassiterite and quartz) is undecomposed by
hydrochloric or nitric acid; so that it is generally found in the residue
insoluble in acids. The titanates, however, are attacked, and a portion of the
titanium dissolves; so that it must be looked for in both the filtrate and
described under Potash.
It must be remembered when calculating the percentage that (with the
exception of the silica, tungstic acid, and tin) the determinations have been
made on 1 gram of the sample.
The following analysis will illustrate the composition of such a slag:—
Tungstic acid 1.3%
Silica 39.4
Stannous oxide 8.1
Ferrous oxide 26.2
Alumina 14.8
Oxide of manganese traces
Lime 7.9
Magnesia 0.5
Alkalies calculated as soda 1.7
———
99.9
TITANIUM.
Titanium only occurs as a mineral in its oxidised state, or as titanic oxide
(TiO2). It is a substance which has little commercial value, and is generally
recognised as one of the rare bodies; although, in small quantities, it is
widely disseminated. It occurs in granite, basalt, and other igneous rocks in
quantities up to as much as 1 per cent. It is also met with in clays and iron
ores, and in river sands, in which it is often associated with stream tin. The
proper minerals of titanium are rutile (TiO2), titaniferous iron (titanate of
iron), and sphene (titanate and silicate of lime).
The oxide of titanium (like cassiterite and quartz) is undecomposed by
hydrochloric or nitric acid; so that it is generally found in the residue
insoluble in acids. The titanates, however, are attacked, and a portion of the
titanium dissolves; so that it must be looked for in both the filtrate and
Page 370
residue. Oxide of titanium in its native form, or after ignition, may be made
soluble by fusing the finely-divided substance with fusion mixture in a
platinum dish. The resulting titanate is dissolved out of the "melt" by cold
hydrochloric acid.
The method most commonly used is fusion with bisulphate of potash. This
renders the oxide of titanium soluble in cold water. The process is as
follows:—The substance is extracted with hydrochloric and nitric acids, and
the solution reserved for further treatment; the residue is dried, moistened
with sulphuric acid, and evaporated once or twice to dryness with
hydrofluoric acid. It is then fused with bisulphate of potash, and the "melt"
extracted with cold water until all soluble matter is removed. The solution is
filtered. The residue may consist of unremoved silica, and oxides of
tantalum, niobium, and, perhaps, chromium. On the prolonged boiling of
the filtrate, the oxide of titanium (and oxide of zirconium, if any) is
precipitated.
Any titanium dissolved by the first extraction with acids is recovered in the
following way:—Sulphuretted hydrogen is passed into the acid solution,
and any precipitate that may be formed is filtered off. The filtrate is
oxidised, and the iron, aluminium, and titanium are separated as basic
acetates (see under Iron). The precipitate is dried and fused with bisulphate
of potash. The "melt" is extracted with cold water, filtered if necessary, and
the solution rendered first faintly alkaline with ammonia, then very slightly
acid with sulphuric acid. 30 or 40 c.c. of a saturated solution of sulphurous
acid is added, and the oxide of titanium precipitated by prolonged boiling. It
is filtered off, added to the precipitate previously got, ignited with ammonic
carbonate towards the end, and then weighed.
Detection.—Titanium is detected in an insoluble residue by fusing the
residue for some time in a bead of microcosmic salt. In the reducing flame
it gives a violet colour, which becomes reddish-brown if much iron is
present. In the oxidising flame it gives a colourless or whitish bead. It is
best detected in acid solutions by the deep brown or iodine colour
developed on adding hydroxyl. A solution of this can be prepared by
pouring peroxide of barium (BaO2) diffused in water into dilute
hydrochloric acid (a little at a time), and keeping the acid in excess.
soluble by fusing the finely-divided substance with fusion mixture in a
platinum dish. The resulting titanate is dissolved out of the "melt" by cold
hydrochloric acid.
The method most commonly used is fusion with bisulphate of potash. This
renders the oxide of titanium soluble in cold water. The process is as
follows:—The substance is extracted with hydrochloric and nitric acids, and
the solution reserved for further treatment; the residue is dried, moistened
with sulphuric acid, and evaporated once or twice to dryness with
hydrofluoric acid. It is then fused with bisulphate of potash, and the "melt"
extracted with cold water until all soluble matter is removed. The solution is
filtered. The residue may consist of unremoved silica, and oxides of
tantalum, niobium, and, perhaps, chromium. On the prolonged boiling of
the filtrate, the oxide of titanium (and oxide of zirconium, if any) is
precipitated.
Any titanium dissolved by the first extraction with acids is recovered in the
following way:—Sulphuretted hydrogen is passed into the acid solution,
and any precipitate that may be formed is filtered off. The filtrate is
oxidised, and the iron, aluminium, and titanium are separated as basic
acetates (see under Iron). The precipitate is dried and fused with bisulphate
of potash. The "melt" is extracted with cold water, filtered if necessary, and
the solution rendered first faintly alkaline with ammonia, then very slightly
acid with sulphuric acid. 30 or 40 c.c. of a saturated solution of sulphurous
acid is added, and the oxide of titanium precipitated by prolonged boiling. It
is filtered off, added to the precipitate previously got, ignited with ammonic
carbonate towards the end, and then weighed.
Detection.—Titanium is detected in an insoluble residue by fusing the
residue for some time in a bead of microcosmic salt. In the reducing flame
it gives a violet colour, which becomes reddish-brown if much iron is
present. In the oxidising flame it gives a colourless or whitish bead. It is
best detected in acid solutions by the deep brown or iodine colour
developed on adding hydroxyl. A solution of this can be prepared by
pouring peroxide of barium (BaO2) diffused in water into dilute
hydrochloric acid (a little at a time), and keeping the acid in excess.
Page 371
Separation.—In the usual course of an analytical separation the hydrate of
titanium will be thrown down with ferric hydrate, &c., on the addition of
ammonic chloride and ammonia. It is best separated from this precipitate by
fusion with bisulphate of potash, as already described, but it must be
remembered that the presence of much mineral acid prevents complete
precipitation when the solution is boiled. Further, if phosphates are present,
the precipitate will contain phosphoric oxide; it may be freed from this by
fusion with sodium carbonate. A very good method of separating titanium
from iron is to add tartaric acid and ammonia to the solution, and then
precipitate the iron (as sulphide) with sulphuretted hydrogen. The filtrate
contains the titanium, which is recovered by evaporating and igniting. It
may be separated from zirconia by the action of sodium carbonate, which
precipitates both; but when concentrated, redissolves the zirconia. The
separation from large quantities of silica is best effected by evaporating
with hydrofluoric acid, which volatilises the silicon; but sulphuric acid must
be present, otherwise some titanium also will be lost, as may be seen from
the following experiments,[77] in which oxide of titanium (pure, ignited)
was evaporated to dryness with a quantity of hydrofluoric acid known by
experiment to be sufficient to volatilise 1 gram of silica.
Without sulphuric acid, 0.0466 gram of titanic oxide left 0.0340 gram,
showing a loss of about 25 per cent.
With sulphuric acid the following results were obtained:—
Oxide taken. Left after Evaporation and Ignition.
0.0340 gram 0.0340 gram
0.0414 " 0.0413 "
0.0520 " 0.0520 "
0.0352 " 0.0352 "
GRAVIMETRIC DETERMINATION.
The titanic hydrate thrown down by ammonia (or on boiling the solution
from the bisulphate) is collected, washed, dried, ignited strongly with the
addition of a little ammonic carbonate, and weighed. The substance is
titanic oxide (TiO2), and is generally reported as such. It contains 60.98 per
titanium will be thrown down with ferric hydrate, &c., on the addition of
ammonic chloride and ammonia. It is best separated from this precipitate by
fusion with bisulphate of potash, as already described, but it must be
remembered that the presence of much mineral acid prevents complete
precipitation when the solution is boiled. Further, if phosphates are present,
the precipitate will contain phosphoric oxide; it may be freed from this by
fusion with sodium carbonate. A very good method of separating titanium
from iron is to add tartaric acid and ammonia to the solution, and then
precipitate the iron (as sulphide) with sulphuretted hydrogen. The filtrate
contains the titanium, which is recovered by evaporating and igniting. It
may be separated from zirconia by the action of sodium carbonate, which
precipitates both; but when concentrated, redissolves the zirconia. The
separation from large quantities of silica is best effected by evaporating
with hydrofluoric acid, which volatilises the silicon; but sulphuric acid must
be present, otherwise some titanium also will be lost, as may be seen from
the following experiments,[77] in which oxide of titanium (pure, ignited)
was evaporated to dryness with a quantity of hydrofluoric acid known by
experiment to be sufficient to volatilise 1 gram of silica.
Without sulphuric acid, 0.0466 gram of titanic oxide left 0.0340 gram,
showing a loss of about 25 per cent.
With sulphuric acid the following results were obtained:—
Oxide taken. Left after Evaporation and Ignition.
0.0340 gram 0.0340 gram
0.0414 " 0.0413 "
0.0520 " 0.0520 "
0.0352 " 0.0352 "
GRAVIMETRIC DETERMINATION.
The titanic hydrate thrown down by ammonia (or on boiling the solution
from the bisulphate) is collected, washed, dried, ignited strongly with the
addition of a little ammonic carbonate, and weighed. The substance is
titanic oxide (TiO2), and is generally reported as such. It contains 60.98 per
Page 372
cent. of titanium. It should be white, if pure (Holland), white, yellow, or
brown (Fresenius), or black (Tidy).
VOLUMETRIC METHOD.
A method has been proposed based on the reduction of titanic oxide by zinc
in hydrochloric acid solutions to the sesquioxide. The reduction is marked
by the development of a violet or green colour, the former with chlorides
and the latter when fluorides are present. The quantity of titanium reduced
is measured by titrating with permanganate of potassium solution. The
water used must be free from dissolved oxygen.
TUNGSTEN AND TUNGSTATES.
Tungsten occurs in nature only in the oxidised state, or as tungstic acid
(WO3), either free, as in wolframine, or combined with oxides of
manganese and iron, as in wolfram, or with lime, as in scheelite. Wolfram
occurs associated with tin ores, the value of which is consequently lowered.
Both wolfram and scheelite are of considerable importance as a source of
tungstic acid for the manufacture of sodium tungstate, which is used as a
mordant and for some other purposes, and as a source of metallic tungsten,
which is used in steel-making.
The tungsten minerals have a high specific gravity (6 to 7.5). On treatment
with hydrochloric acid or aqua regia they are decomposed; the yellow
tungstic acid separates and remains insoluble.
Tungsten itself is insoluble in nitric acid or aqua regia; but is converted into
tungstic acid (WO3) by prolonged and strong ignition in air. Alloys
containing tungsten leave tungstic acid after treatment with nitric acid or
aqua regia. Tungstic acid may be got into solution after fusion with alkalies
or alkaline carbonates. This solution gives with hydrochloric acid a white
precipitate of tungstic acid, which becomes yellow on boiling, but the
separation is not complete. Fusion with bisulphate of potash gives a residue,
which does not dissolve in water, but is soluble in ammonic carbonate. For
the assay of minerals containing tungsten these reactions are only
brown (Fresenius), or black (Tidy).
VOLUMETRIC METHOD.
A method has been proposed based on the reduction of titanic oxide by zinc
in hydrochloric acid solutions to the sesquioxide. The reduction is marked
by the development of a violet or green colour, the former with chlorides
and the latter when fluorides are present. The quantity of titanium reduced
is measured by titrating with permanganate of potassium solution. The
water used must be free from dissolved oxygen.
TUNGSTEN AND TUNGSTATES.
Tungsten occurs in nature only in the oxidised state, or as tungstic acid
(WO3), either free, as in wolframine, or combined with oxides of
manganese and iron, as in wolfram, or with lime, as in scheelite. Wolfram
occurs associated with tin ores, the value of which is consequently lowered.
Both wolfram and scheelite are of considerable importance as a source of
tungstic acid for the manufacture of sodium tungstate, which is used as a
mordant and for some other purposes, and as a source of metallic tungsten,
which is used in steel-making.
The tungsten minerals have a high specific gravity (6 to 7.5). On treatment
with hydrochloric acid or aqua regia they are decomposed; the yellow
tungstic acid separates and remains insoluble.
Tungsten itself is insoluble in nitric acid or aqua regia; but is converted into
tungstic acid (WO3) by prolonged and strong ignition in air. Alloys
containing tungsten leave tungstic acid after treatment with nitric acid or
aqua regia. Tungstic acid may be got into solution after fusion with alkalies
or alkaline carbonates. This solution gives with hydrochloric acid a white
precipitate of tungstic acid, which becomes yellow on boiling, but the
separation is not complete. Fusion with bisulphate of potash gives a residue,
which does not dissolve in water, but is soluble in ammonic carbonate. For
the assay of minerals containing tungsten these reactions are only
Page 373
occasionally taken advantage of for testing or purifying the separated
tungstic acid.
Detection.—The minerals are easily recognised by their physical
characters, and the yellow tungstic acid separated by boiling with acids is
the best test for its presence; this, after decanting and washing, immediately
dissolves in a few drops of dilute ammonia. A solution of tungstate
acidulated with hydrochloric acid becomes intensely blue on the addition of
stannous chloride and warming. Fused in a bead of microcosmic salt it
gives a clear blue colour (reddish-brown if iron is also present) in the
reducing flame, but is colourless in the oxidising flame.
Solution and Separation.—The decomposition and solution of natural
tungstates is difficult to effect owing to the separation of tungstic acid; the
method of treatment is as follows:—Boil the finely-powdered substance
with hydrochloric acid or aqua regia till it apparently ceases to be attacked;
dilute, filter, and wash with dilute hydrochloric acid. Cover with dilute
ammonia, and filter the solution, which contains ammonic tungstate, into an
evaporating dish. Treat the residue again with acid, and again dissolve out
the separated tungstic acid with ammonia, and repeat this operation until
decomposition is complete. By this means there will be obtained—(1) a
solution containing tungstate of ammonia; (2) an insoluble residue with
silicates, and oxides of tin, niobium, tantalum, &c.; and (3) an acid solution
containing the soluble bases. The tungstate of ammonia requires simple
evaporation on the water-bath and gentle ignition in order to cause the
tungstic acid to be left in an almost pure state; possibly, it may carry a little
silica.
GRAVIMETRIC DETERMINATION.
The tungstic acid is dissolved, and separated as ammonic tungstate, and,
after evaporation, is gently ignited, the heat being increased towards the
end. The residual tungstic acid is fixed, so that when the ammonia has been
driven off it may be strongly heated without loss. It is a dark yellow or
brown powder whilst hot, which becomes a light yellow on cooling. If any
reduction has taken place it will be more or less greenish. It is weighed
when cold, and is the trioxide or "tungstic acid" (WO3), which contains
tungstic acid.
Detection.—The minerals are easily recognised by their physical
characters, and the yellow tungstic acid separated by boiling with acids is
the best test for its presence; this, after decanting and washing, immediately
dissolves in a few drops of dilute ammonia. A solution of tungstate
acidulated with hydrochloric acid becomes intensely blue on the addition of
stannous chloride and warming. Fused in a bead of microcosmic salt it
gives a clear blue colour (reddish-brown if iron is also present) in the
reducing flame, but is colourless in the oxidising flame.
Solution and Separation.—The decomposition and solution of natural
tungstates is difficult to effect owing to the separation of tungstic acid; the
method of treatment is as follows:—Boil the finely-powdered substance
with hydrochloric acid or aqua regia till it apparently ceases to be attacked;
dilute, filter, and wash with dilute hydrochloric acid. Cover with dilute
ammonia, and filter the solution, which contains ammonic tungstate, into an
evaporating dish. Treat the residue again with acid, and again dissolve out
the separated tungstic acid with ammonia, and repeat this operation until
decomposition is complete. By this means there will be obtained—(1) a
solution containing tungstate of ammonia; (2) an insoluble residue with
silicates, and oxides of tin, niobium, tantalum, &c.; and (3) an acid solution
containing the soluble bases. The tungstate of ammonia requires simple
evaporation on the water-bath and gentle ignition in order to cause the
tungstic acid to be left in an almost pure state; possibly, it may carry a little
silica.
GRAVIMETRIC DETERMINATION.
The tungstic acid is dissolved, and separated as ammonic tungstate, and,
after evaporation, is gently ignited, the heat being increased towards the
end. The residual tungstic acid is fixed, so that when the ammonia has been
driven off it may be strongly heated without loss. It is a dark yellow or
brown powder whilst hot, which becomes a light yellow on cooling. If any
reduction has taken place it will be more or less greenish. It is weighed
when cold, and is the trioxide or "tungstic acid" (WO3), which contains
Page 374
79.31 per cent. of tungsten. After its weight has been taken its purity is
checked by fusing with hydric potassic sulphate, extracting with water, and
treating the residue with ammonic carbonate. Any silica present will be left
undissolved; it should be separated and weighed, and its weight deducted
from that of the tungstic acid found.
Determination of Tungstic Acid in Wolfram.—Take 2 grams of the
finely-powdered sample and boil with 50 c.c. of hydrochloric acid for half
an hour, adding 5 c.c. of nitric acid towards the end. Allow to stand
overnight and boil again for 15 or 20 minutes; dilute with an equal volume
of water, and filter. Wash with dilute hydrochloric acid, dissolve in a few
c.c. of warm dilute ammonia, and dilute to 200 c.c. with distilled water;
allow to settle, and filter. Evaporate in a weighed dish, ignite, and weigh.
The following analysis will illustrate the composition of a sample of
Cornish wolfram as brought into the market:—
Tungstic acid 50.1%
Cassiterite 10.9
Ferrous oxide 24.6
Manganous oxide 5.4
Niobic oxide, alumina, &c. 3.5
Silica 1.2
Copper oxide 2.7
Zinc oxide 0.22
Arsenic 0.51
Sulphur 0.20
———
99.33
NIOBIC AND TANTALIC OXIDES.
These oxides are commonly met with in samples of wolfram and tinstone,
especially niobic. They are probably present in the form of columbite, a
niobate of iron and manganese; and tantalite, a tantalate of the same metals.
checked by fusing with hydric potassic sulphate, extracting with water, and
treating the residue with ammonic carbonate. Any silica present will be left
undissolved; it should be separated and weighed, and its weight deducted
from that of the tungstic acid found.
Determination of Tungstic Acid in Wolfram.—Take 2 grams of the
finely-powdered sample and boil with 50 c.c. of hydrochloric acid for half
an hour, adding 5 c.c. of nitric acid towards the end. Allow to stand
overnight and boil again for 15 or 20 minutes; dilute with an equal volume
of water, and filter. Wash with dilute hydrochloric acid, dissolve in a few
c.c. of warm dilute ammonia, and dilute to 200 c.c. with distilled water;
allow to settle, and filter. Evaporate in a weighed dish, ignite, and weigh.
The following analysis will illustrate the composition of a sample of
Cornish wolfram as brought into the market:—
Tungstic acid 50.1%
Cassiterite 10.9
Ferrous oxide 24.6
Manganous oxide 5.4
Niobic oxide, alumina, &c. 3.5
Silica 1.2
Copper oxide 2.7
Zinc oxide 0.22
Arsenic 0.51
Sulphur 0.20
———
99.33
NIOBIC AND TANTALIC OXIDES.
These oxides are commonly met with in samples of wolfram and tinstone,
especially niobic. They are probably present in the form of columbite, a
niobate of iron and manganese; and tantalite, a tantalate of the same metals.
Page 375
On boiling with hydrochloric acid they are both liberated, and remain for
the greater part (all the niobic) in the insoluble residue with the tungstic
acid. On removing the latter with dilute ammonia they remain as a white
insoluble precipitate, very prone to run through the filter on washing. They
may be dissolved in hydrofluoric acid either at once or after fusion with
bisulphate of potash, and extraction with cold water. To the solution in
hydrofluoric acid gradually add a boiling solution of acid potassium
fluoride (HF, KF.). Potassic fluotantalate (soluble in 200 parts of water)
separates out first, and afterwards potassic fluoniobate (soluble in 12 parts
of water). The separated salts (after heating with sulphuric acid and washing
out the potassium sulphate formed) are ignited with ammonic carbonate,
and weighed as tantalic oxide (Ta2O5) and niobic oxide (Nb2O5)
respectively.
They are both white powders. The oxide of niobium dissolved in a bead of
microcosmic salt gives a bluish colour in the reducing flame. The oxide of
tantalum dissolves in the bead, but gives no colour.
the greater part (all the niobic) in the insoluble residue with the tungstic
acid. On removing the latter with dilute ammonia they remain as a white
insoluble precipitate, very prone to run through the filter on washing. They
may be dissolved in hydrofluoric acid either at once or after fusion with
bisulphate of potash, and extraction with cold water. To the solution in
hydrofluoric acid gradually add a boiling solution of acid potassium
fluoride (HF, KF.). Potassic fluotantalate (soluble in 200 parts of water)
separates out first, and afterwards potassic fluoniobate (soluble in 12 parts
of water). The separated salts (after heating with sulphuric acid and washing
out the potassium sulphate formed) are ignited with ammonic carbonate,
and weighed as tantalic oxide (Ta2O5) and niobic oxide (Nb2O5)
respectively.
They are both white powders. The oxide of niobium dissolved in a bead of
microcosmic salt gives a bluish colour in the reducing flame. The oxide of
tantalum dissolves in the bead, but gives no colour.
Page 376
FOOTNOTES:
[76] This will give almost the whole of the tin; a further portion will be got in
subsequent work, and must be added to this result.
[77] Published by P. Holland, in the Chemical News, vol. lix. p. 27.
[76] This will give almost the whole of the tin; a further portion will be got in
subsequent work, and must be added to this result.
[77] Published by P. Holland, in the Chemical News, vol. lix. p. 27.
Page 377
CHAPTER XIII.
MANGANESE, CHROMIUM, &c.
MANGANESE.
Manganese occurs mainly as black oxide (MnO2) in the mineral pyrolusite;
and, in a less pure form, in psilomelane and wad. The value of the ore
depends rather on the percentage of available oxygen than on the proportion
of metal present. The results of assays are generally reported as so much per
cent. of the dioxide (MnO2). In smaller quantities it is very widely
distributed. Manganese itself has a value for steel-making; or, rather, for the
making of spiegeleisen and ferro-manganese, which are used in the
Bessemer and Siemens processes. For this purpose the percentage of the
metal (Mn) is required. Consequently the minerals of manganese may be
considered in two aspects—(1) as a source of oxygen; and (2) as a source of
manganese. These will require separate consideration.
The black oxide is mainly used in the preparation of chlorine, liberation of
which it brings about when treated with hot hydrochloric acid, or with a
mixture of common salt and sulphuric acid. The quantity of chlorine which
is obtained depends upon the proportion of dioxide present;[78] and in
assaying may either be measured by its equivalent of iodine liberated, or by
the oxidising effect on an acid solution of ferrous sulphate. When the ore
also carries substances which have a reducing effect (such as ferrous
compounds), such assays will give, not the total dioxide (MnO2), but less,
by the amount required to oxidise these impurities; and this is exactly what
is required in valuing such an ore for commercial purposes. Manganese
compounds are characterised by the readiness with which they may be
converted into highly-oxidised bodies. Solution of manganese in
hydrochloric acid, rendered alkaline with ammonia, yields a clear solution,
[79]
which rapidly takes up oxygen from the air, forming a brown precipitate
of the oxide (Mn2O3). The addition of bromine or chlorine to such a
MANGANESE, CHROMIUM, &c.
MANGANESE.
Manganese occurs mainly as black oxide (MnO2) in the mineral pyrolusite;
and, in a less pure form, in psilomelane and wad. The value of the ore
depends rather on the percentage of available oxygen than on the proportion
of metal present. The results of assays are generally reported as so much per
cent. of the dioxide (MnO2). In smaller quantities it is very widely
distributed. Manganese itself has a value for steel-making; or, rather, for the
making of spiegeleisen and ferro-manganese, which are used in the
Bessemer and Siemens processes. For this purpose the percentage of the
metal (Mn) is required. Consequently the minerals of manganese may be
considered in two aspects—(1) as a source of oxygen; and (2) as a source of
manganese. These will require separate consideration.
The black oxide is mainly used in the preparation of chlorine, liberation of
which it brings about when treated with hot hydrochloric acid, or with a
mixture of common salt and sulphuric acid. The quantity of chlorine which
is obtained depends upon the proportion of dioxide present;[78] and in
assaying may either be measured by its equivalent of iodine liberated, or by
the oxidising effect on an acid solution of ferrous sulphate. When the ore
also carries substances which have a reducing effect (such as ferrous
compounds), such assays will give, not the total dioxide (MnO2), but less,
by the amount required to oxidise these impurities; and this is exactly what
is required in valuing such an ore for commercial purposes. Manganese
compounds are characterised by the readiness with which they may be
converted into highly-oxidised bodies. Solution of manganese in
hydrochloric acid, rendered alkaline with ammonia, yields a clear solution,
[79]
which rapidly takes up oxygen from the air, forming a brown precipitate
of the oxide (Mn2O3). The addition of bromine or chlorine to such a
Page 378
solution determines the precipitation of a still higher oxide (approximately
MnO2). On treating a compound containing manganese with nitric acid and
dioxide of lead (PbO2), the oxidation is carried still further, a purple-
coloured solution of permanganic acid (HMnO4 or H2O.Mn2O7) being
formed. On fusing minerals containing (even traces of) manganese with
sodium carbonate in an open crucible, a green "melt" is obtained which
owes its colour to sodium manganate (Na2MnO4 or Na2O.MnO3). This salt
is soluble in water, forming a green solution; which, when rendered acid,
rapidly changes into the permanganate with the characteristic purple colour.
Permanganate of potash is a salt much used in assaying, with some
properties of which the student will have already become familiar.
Compounds of manganese, on boiling with strong hydrochloric acid, yield
manganous chloride[80] (MnCl2).
The properties given above serve for the detection of manganese; the higher
oxides are distinguished by causing the evolution of chlorine (with its
peculiarly suffocating smell) when acted on with hydrochloric acid; while
the green "melt," with sodium carbonate, can be relied on for the
recognition of manganese itself. There is no dry assay of manganese ores.
WET METHODS.
Strong hydrochloric acid is the best solvent for ores of manganese; but
where the proportion of dioxide (MnO2) is required, the solution is effected
during the assay. The ore should be in a very fine state of division before
treatment with acids.
The separation of manganese from other metals is thus effected: Ignite, in
order to destroy any organic matter which may be present; dissolve in
hydrochloric acid, and evaporate to dryness, to separate silica. Take up with
hydrochloric acid, dilute, pass sulphuretted hydrogen, and filter. Boil off the
excess of gas, peroxidise the iron with a drop or two of nitric acid, and
separate the iron as basic acetate (as described under Iron).[81] If the iron
precipitate is bulky, it is dissolved in a little hydrochloric acid,
reprecipitated, and the filtrate added to the original one. Neutralise with
soda, and add bromine in excess; heat gradually to boiling, allow to settle,
MnO2). On treating a compound containing manganese with nitric acid and
dioxide of lead (PbO2), the oxidation is carried still further, a purple-
coloured solution of permanganic acid (HMnO4 or H2O.Mn2O7) being
formed. On fusing minerals containing (even traces of) manganese with
sodium carbonate in an open crucible, a green "melt" is obtained which
owes its colour to sodium manganate (Na2MnO4 or Na2O.MnO3). This salt
is soluble in water, forming a green solution; which, when rendered acid,
rapidly changes into the permanganate with the characteristic purple colour.
Permanganate of potash is a salt much used in assaying, with some
properties of which the student will have already become familiar.
Compounds of manganese, on boiling with strong hydrochloric acid, yield
manganous chloride[80] (MnCl2).
The properties given above serve for the detection of manganese; the higher
oxides are distinguished by causing the evolution of chlorine (with its
peculiarly suffocating smell) when acted on with hydrochloric acid; while
the green "melt," with sodium carbonate, can be relied on for the
recognition of manganese itself. There is no dry assay of manganese ores.
WET METHODS.
Strong hydrochloric acid is the best solvent for ores of manganese; but
where the proportion of dioxide (MnO2) is required, the solution is effected
during the assay. The ore should be in a very fine state of division before
treatment with acids.
The separation of manganese from other metals is thus effected: Ignite, in
order to destroy any organic matter which may be present; dissolve in
hydrochloric acid, and evaporate to dryness, to separate silica. Take up with
hydrochloric acid, dilute, pass sulphuretted hydrogen, and filter. Boil off the
excess of gas, peroxidise the iron with a drop or two of nitric acid, and
separate the iron as basic acetate (as described under Iron).[81] If the iron
precipitate is bulky, it is dissolved in a little hydrochloric acid,
reprecipitated, and the filtrate added to the original one. Neutralise with
soda, and add bromine in excess; heat gradually to boiling, allow to settle,
Page 379
and filter. The precipitate is impure dioxide of manganese (containing
alkalies and, possibly, cobalt or nickel).
GRAVIMETRIC DETERMINATION.
Dissolve the precipitate in hydrochloric acid, and boil; add a slight excess
of carbonate of soda, warm, and filter. Wash with hot water, dry, carefully
ignite in an open Berlin crucible, and weigh. The substance is the brown
oxide (Mn3O4), and contains 72.05 per cent. of manganese. If the
percentage of dioxide is required it may be calculated by multiplying the
percentage of manganese by 1.582. It must be borne in mind that the
manganese should never be calculated to dioxide except when it is known
to exist in the ore only in that form.
VOLUMETRIC METHODS.
The two methods are based on the oxidising effect of manganese dioxide;
and if the metal does not already exist in this form it will require a
preliminary treatment to convert it. The following method due to Mr. J.
Pattinson[82] effects this: A quantity of the ore containing not more than .25
grams of the metal (Mn), is dissolved in hydrochloric acid in a pint beaker,
and, if necessary, 3 or 4 c.c. of nitric acid are added to peroxidise the iron,
and ferric chloride is added if required, so that there may be at least as
much iron as manganese. Calcium carbonate is added till the solution is
slightly red; and next the redness is removed by the cautious addition of
acid; 30 c.c. of zinc chloride solution (containing 15 grams of zinc per litre)
are added, the liquid is brought to boil and diluted to about 300 c.c. with
boiling water; 60 c.c. of a solution of bleaching powder (33 grams to the
litre and filtered), rendered slightly greenish by acid, are then run in and are
followed by 3 grams of calcium carbonate suspended in 15 c.c. of boiling
water. During effervescence the beaker is covered, the precipitate is stirred,
and 2 c.c. of methylated spirit are mixed in. The precipitate is collected on a
large filter, washed with cold water, and then with hot, till free from
chlorine, which is tested for with starch and potassium iodide. The acid
ferrous sulphate solution (presently described) is then measured into the
beaker, and the precipitate, still in the paper, added; more acid is added (if
alkalies and, possibly, cobalt or nickel).
GRAVIMETRIC DETERMINATION.
Dissolve the precipitate in hydrochloric acid, and boil; add a slight excess
of carbonate of soda, warm, and filter. Wash with hot water, dry, carefully
ignite in an open Berlin crucible, and weigh. The substance is the brown
oxide (Mn3O4), and contains 72.05 per cent. of manganese. If the
percentage of dioxide is required it may be calculated by multiplying the
percentage of manganese by 1.582. It must be borne in mind that the
manganese should never be calculated to dioxide except when it is known
to exist in the ore only in that form.
VOLUMETRIC METHODS.
The two methods are based on the oxidising effect of manganese dioxide;
and if the metal does not already exist in this form it will require a
preliminary treatment to convert it. The following method due to Mr. J.
Pattinson[82] effects this: A quantity of the ore containing not more than .25
grams of the metal (Mn), is dissolved in hydrochloric acid in a pint beaker,
and, if necessary, 3 or 4 c.c. of nitric acid are added to peroxidise the iron,
and ferric chloride is added if required, so that there may be at least as
much iron as manganese. Calcium carbonate is added till the solution is
slightly red; and next the redness is removed by the cautious addition of
acid; 30 c.c. of zinc chloride solution (containing 15 grams of zinc per litre)
are added, the liquid is brought to boil and diluted to about 300 c.c. with
boiling water; 60 c.c. of a solution of bleaching powder (33 grams to the
litre and filtered), rendered slightly greenish by acid, are then run in and are
followed by 3 grams of calcium carbonate suspended in 15 c.c. of boiling
water. During effervescence the beaker is covered, the precipitate is stirred,
and 2 c.c. of methylated spirit are mixed in. The precipitate is collected on a
large filter, washed with cold water, and then with hot, till free from
chlorine, which is tested for with starch and potassium iodide. The acid
ferrous sulphate solution (presently described) is then measured into the
beaker, and the precipitate, still in the paper, added; more acid is added (if
Page 380
necessary), and the solution is diluted and titrated. In place of bleaching
powder solution, 90 c.c. of bromine water (containing 22 grams per litre)
may be used.
FERROUS SULPHATE ASSAY.
This method, which is the one commonly used, is based on the
determination of the amount of ferrous iron oxidised by a known weight of
the ore. It is known that 87 parts of the dioxide will oxidise 112 parts of
ferrous iron;[83] therefore 1 gram will oxidise 1.287 gram of ferrous iron, or
1 gram of ferrous iron oxidised will be equivalent to 0.7768 gram of the
dioxide. The finely-divided substance containing the dioxide is digested in a
solution of a known quantity of iron in sulphuric acid. The iron, of course,
must be in excess, which excess is determined when the ore is dissolved by
titrating with standard permanganate or bichromate of potash solution. The
assay resolves itself into one for the determination of ferrous iron, for which
the standard solutions and method of working described under Iron are
used.
The assay is as follows:—For rich ores, 2 grams of clean soft iron wire are
treated, in a pint flask, with 100 c.c. of dilute sulphuric acid and warmed till
dissolved. Carefully sample the ore, and in one portion determine the
"moisture at 100° C.;" grind the rest in a Wedgwood mortar with a little
pure alcohol until free from grit. This reduces the substance to a finely-
divided state and assists solution. Evaporate off the alcohol and dry at 100°
C., mix well, and keep in a weighing-bottle. Weigh up 2 grams and add
them to the solution of iron in the flask; carefully wash it all down into the
acid liquid. On rotating the flask the ore will rapidly dissolve, but gentle
heat may be used towards the end to complete the solution. When the
residue is clean and sandy-looking, and free from black particles, the flask
is cooled, and the residual ferrous iron is determined by titration with
"permanganate." The iron thus found, deducted from the 2 grams taken, will
give the amount of iron peroxidised by the dioxide contained in the 2 grams
of ore. This divided by 2 and multiplied by 77.68 will give the percentage
of dioxide in the sample, or multiplied by 49.41 will give that of metallic
manganese.
powder solution, 90 c.c. of bromine water (containing 22 grams per litre)
may be used.
FERROUS SULPHATE ASSAY.
This method, which is the one commonly used, is based on the
determination of the amount of ferrous iron oxidised by a known weight of
the ore. It is known that 87 parts of the dioxide will oxidise 112 parts of
ferrous iron;[83] therefore 1 gram will oxidise 1.287 gram of ferrous iron, or
1 gram of ferrous iron oxidised will be equivalent to 0.7768 gram of the
dioxide. The finely-divided substance containing the dioxide is digested in a
solution of a known quantity of iron in sulphuric acid. The iron, of course,
must be in excess, which excess is determined when the ore is dissolved by
titrating with standard permanganate or bichromate of potash solution. The
assay resolves itself into one for the determination of ferrous iron, for which
the standard solutions and method of working described under Iron are
used.
The assay is as follows:—For rich ores, 2 grams of clean soft iron wire are
treated, in a pint flask, with 100 c.c. of dilute sulphuric acid and warmed till
dissolved. Carefully sample the ore, and in one portion determine the
"moisture at 100° C.;" grind the rest in a Wedgwood mortar with a little
pure alcohol until free from grit. This reduces the substance to a finely-
divided state and assists solution. Evaporate off the alcohol and dry at 100°
C., mix well, and keep in a weighing-bottle. Weigh up 2 grams and add
them to the solution of iron in the flask; carefully wash it all down into the
acid liquid. On rotating the flask the ore will rapidly dissolve, but gentle
heat may be used towards the end to complete the solution. When the
residue is clean and sandy-looking, and free from black particles, the flask
is cooled, and the residual ferrous iron is determined by titration with
"permanganate." The iron thus found, deducted from the 2 grams taken, will
give the amount of iron peroxidised by the dioxide contained in the 2 grams
of ore. This divided by 2 and multiplied by 77.68 will give the percentage
of dioxide in the sample, or multiplied by 49.41 will give that of metallic
manganese.
Page 381
When the quantity of manganese or of the dioxide to be determined is
small, it is not necessary to use 2 grams of iron; 1 gram, or even less, may
be taken. The iron may be used in the form of a standard solution of ferrous
sulphate and portions measured off, thus saving the labour of weighing.
Determination of Dioxide in a Manganese Ore.—Weigh up 1 or 2 grams
of the finely-powdered ore[84] and an equal weight of pure iron wire,
dissolve the wire in 50 or 100 c.c. of dilute sulphuric acid, and, when
solution is complete, add the ore and warm till it too is dissolved. Cool and
titrate the remaining ferrous iron with the permanganate or bichromate of
potassium solution.
For example, 0.7560 gram of pyrolusite and 1.000 gram of iron were taken
and treated as above; 13.9 c.c. of "permanganate" (standard 100 c.c. =
0.4920 gram iron) were required; this indicates that 0.0684 gram of iron
was left unoxidised by the ore. The iron oxidised, then, was 0.9316 gram
(1.000 - 0.0684); multiplying this by 0.7768, we find that 0.7237 gram is
the quantity of manganese dioxide which was present. This is equivalent to
95.77 per cent.;
0.7560 : 0.7237 :: 100 : 95.77.
IODINE METHOD.
It has been already stated that when dioxide of manganese is boiled with
strong hydrochloric acid chlorine is given off, and that the amount of
chlorine so liberated is a measure of the dioxide present. If the chlorine is
passed into a solution of potassium iodide, an equivalent of iodine will be
set free.[85] This is apparently a very indirect way of determining how much
of the dioxide is present; but the reactions are very sharp, and the final
determination of the iodine is an easy one.
small, it is not necessary to use 2 grams of iron; 1 gram, or even less, may
be taken. The iron may be used in the form of a standard solution of ferrous
sulphate and portions measured off, thus saving the labour of weighing.
Determination of Dioxide in a Manganese Ore.—Weigh up 1 or 2 grams
of the finely-powdered ore[84] and an equal weight of pure iron wire,
dissolve the wire in 50 or 100 c.c. of dilute sulphuric acid, and, when
solution is complete, add the ore and warm till it too is dissolved. Cool and
titrate the remaining ferrous iron with the permanganate or bichromate of
potassium solution.
For example, 0.7560 gram of pyrolusite and 1.000 gram of iron were taken
and treated as above; 13.9 c.c. of "permanganate" (standard 100 c.c. =
0.4920 gram iron) were required; this indicates that 0.0684 gram of iron
was left unoxidised by the ore. The iron oxidised, then, was 0.9316 gram
(1.000 - 0.0684); multiplying this by 0.7768, we find that 0.7237 gram is
the quantity of manganese dioxide which was present. This is equivalent to
95.77 per cent.;
0.7560 : 0.7237 :: 100 : 95.77.
IODINE METHOD.
It has been already stated that when dioxide of manganese is boiled with
strong hydrochloric acid chlorine is given off, and that the amount of
chlorine so liberated is a measure of the dioxide present. If the chlorine is
passed into a solution of potassium iodide, an equivalent of iodine will be
set free.[85] This is apparently a very indirect way of determining how much
of the dioxide is present; but the reactions are very sharp, and the final
determination of the iodine is an easy one.
Page 382
The finely-powdered sample of dioxide is placed in a small flask provided
with an exit tube leading into a solution of potassic iodide (fig. 60). On
adding hydrochloric acid and boiling, the chlorine evolved is driven into the
iodide solution and there absorbed; the boiling is continued till the steam
and hydrochloric acid fumes have driven the last portions of the chlorine
out of the flask and into the solution. In this experiment there is a strong
tendency for the iodide solution to rush back into the flask. This tendency is
overcome by avoiding draughts and regulating the heat; or by placing a
lump of magnesite in the flask, which acts by evolving carbonic acid and so
producing a steady outward pressure. When the distillation is finished the
tube containing the iodine is detached and washed out into a beaker. If the
solution is strongly acid it should be almost neutralised by the cautious
addition of dilute ammonia. If crystals of iodine have separated, potassium
iodide must be added in quantity sufficient to dissolve them. The condenser
must be kept cool whilst the chlorine is passing into it.
The solution, transferred to a beaker, is titrated with a standard solution of
sodic hyposulphite (100 c.c. = 1.27 gram iodine or 0.435 gram of dioxide of
manganese). In titrating, the solution should be cold, or not warmer than
30° C. The bulk may vary from 100 to 200 c.c.; but it is best always to work
with the same volume. The "hypo" is run in with constant agitation until the
brown colour has been reduced to a light yellow; 5 c.c. of starch solution
with an exit tube leading into a solution of potassic iodide (fig. 60). On
adding hydrochloric acid and boiling, the chlorine evolved is driven into the
iodide solution and there absorbed; the boiling is continued till the steam
and hydrochloric acid fumes have driven the last portions of the chlorine
out of the flask and into the solution. In this experiment there is a strong
tendency for the iodide solution to rush back into the flask. This tendency is
overcome by avoiding draughts and regulating the heat; or by placing a
lump of magnesite in the flask, which acts by evolving carbonic acid and so
producing a steady outward pressure. When the distillation is finished the
tube containing the iodine is detached and washed out into a beaker. If the
solution is strongly acid it should be almost neutralised by the cautious
addition of dilute ammonia. If crystals of iodine have separated, potassium
iodide must be added in quantity sufficient to dissolve them. The condenser
must be kept cool whilst the chlorine is passing into it.
The solution, transferred to a beaker, is titrated with a standard solution of
sodic hyposulphite (100 c.c. = 1.27 gram iodine or 0.435 gram of dioxide of
manganese). In titrating, the solution should be cold, or not warmer than
30° C. The bulk may vary from 100 to 200 c.c.; but it is best always to work
with the same volume. The "hypo" is run in with constant agitation until the
brown colour has been reduced to a light yellow; 5 c.c. of starch solution
Page 383
are then added and the titration cautiously continued until the end is
reached; the finish is indicated by a change from blue to colourless.
The assay solution may be acidified with acetic, sulphuric, or hydrochloric
acid before titrating with "hypo;" but it must be only faintly so. An excess
of acid may be nearly neutralised with ammonia without interference, but
excess of alkali is fatal. Bicarbonate of soda must not be used in excess; it is
best to avoid it altogether. The assay solution should be titrated at once, as it
weakens on standing; and the "hypo" solution should be standardised every
two or three days, as its strength is not constant.
The standard solution of hyposulphite of soda is made by dissolving 25
grams of the salt (Na2S2O3.5H2O) in water and diluting to 1 litre. 100 c.c.
are equivalent to 1.27 gram of iodine.
This solution is standardised by weighing, in a small beaker, about half a
gram of iodine, to which is added a crystal or two of potassium iodide and a
few drops of water. When dissolved, the solution is diluted to 100 c.c., and
titrated in the manner described. The starch solution is made in the manner
described under the iodide copper assay. 5 c.c. are used for each titration.
In determining the effects of variations in the condition of the assay a
solution of iodine was used, which was equivalent in strength to the "hypo"
solution. It was made by dissolving 12.7 grams of iodine with 25 grams of
potassium iodide in a little water and diluting to 1 litre. 100 c.c. of this
solution were found (at the time of the experiments) to be equivalent to
102.0 c.c. of the "hypo."
Effect of Varying Temperature.—The bulk of the solution was 100 c.c.;
20 c.c. of iodine were taken, and 5 c.c. of starch solution were added
towards the end as indicator. These conditions are also those of the other
experiments, except where otherwise stated. Iodine being volatile, it is to be
expected that with hot solutions low results will be obtained.
Temperature 15° 20° 40° 60° 80°
"Hypo" required 20.4 c.c. 20.4 c.c. 20.1 c.c. 19.2 c.c. 15.5 c.c.
These show that the temperature should not much exceed 20°.
reached; the finish is indicated by a change from blue to colourless.
The assay solution may be acidified with acetic, sulphuric, or hydrochloric
acid before titrating with "hypo;" but it must be only faintly so. An excess
of acid may be nearly neutralised with ammonia without interference, but
excess of alkali is fatal. Bicarbonate of soda must not be used in excess; it is
best to avoid it altogether. The assay solution should be titrated at once, as it
weakens on standing; and the "hypo" solution should be standardised every
two or three days, as its strength is not constant.
The standard solution of hyposulphite of soda is made by dissolving 25
grams of the salt (Na2S2O3.5H2O) in water and diluting to 1 litre. 100 c.c.
are equivalent to 1.27 gram of iodine.
This solution is standardised by weighing, in a small beaker, about half a
gram of iodine, to which is added a crystal or two of potassium iodide and a
few drops of water. When dissolved, the solution is diluted to 100 c.c., and
titrated in the manner described. The starch solution is made in the manner
described under the iodide copper assay. 5 c.c. are used for each titration.
In determining the effects of variations in the condition of the assay a
solution of iodine was used, which was equivalent in strength to the "hypo"
solution. It was made by dissolving 12.7 grams of iodine with 25 grams of
potassium iodide in a little water and diluting to 1 litre. 100 c.c. of this
solution were found (at the time of the experiments) to be equivalent to
102.0 c.c. of the "hypo."
Effect of Varying Temperature.—The bulk of the solution was 100 c.c.;
20 c.c. of iodine were taken, and 5 c.c. of starch solution were added
towards the end as indicator. These conditions are also those of the other
experiments, except where otherwise stated. Iodine being volatile, it is to be
expected that with hot solutions low results will be obtained.
Temperature 15° 20° 40° 60° 80°
"Hypo" required 20.4 c.c. 20.4 c.c. 20.1 c.c. 19.2 c.c. 15.5 c.c.
These show that the temperature should not much exceed 20°.
Page 384
Effect of Exposure of the Iodine Solution.—Twenty c.c. of the iodine
were diluted to 100 c.c., and exposed for varying lengths of time in open
beakers at the ordinary temperature, and then titrated.
Time exposed — 1 day 2 days 3 days
"Hypo" required 20.4 c.c. 16.1 c.c. 13.6 c.c. 9.4 c.c.
Effect of Varying Bulk.—These experiments were carried out in the usual
way, bulk only varying.
Bulk 100.0 c.c. 200.0c.c. 300.0 c.c. 500.0 c.c.
"Hypo" required 20.4 " 20.4 " 20.4 " 20.4 "
Effect of Varying Acid.—These experiments were under the usual
conditions, the bulk being 100 c.c. The results were—
Acetic acid — 1.5 c.c. 30.0c.c.
"Hypo" required 20.4 c.c. 20.7 " 20.7"
Hydrochloric acid — 1.5 c.c. 15.0c.c.
"Hypo" required 20.4 c.c. 20.6 " 20.9"
Sulphuric acid — 0.5 c.c. 20.0c.c.
"Hypo" required 20.4 c.c. 20.7 " 15.2 "[86]
Nitric acid — 0.5 c.c. 10.0c.c.
"Hypo" required 20.4 c.c. 21.5 " could not be titrated.
In the application of this titration to the assay of manganese ores,
hydrochloric and hydriodic acids are the only ones likely to be present.
Effect of Alkalies.—On theoretical grounds the presence of these is known
to be inadmissible. A solution rendered faintly alkaline with ammonia
required only 11.2 c.c. of "hypo;" and another, with 0.5 gram of caustic
soda, required 4.0 c.c. instead of 20.4 c.c. as in neutral solutions.
Effect of nearly Neutralising Hydrochloric Acid Solutions with
Ammonia.—Provided care is taken not to add excess of ammonia, this has
a good effect, counteracting the interference of excess of acid. Thus 20 c.c.
of iodine (as before) required 20.4 c.c. of "hypo;" with 15 c.c. of
were diluted to 100 c.c., and exposed for varying lengths of time in open
beakers at the ordinary temperature, and then titrated.
Time exposed — 1 day 2 days 3 days
"Hypo" required 20.4 c.c. 16.1 c.c. 13.6 c.c. 9.4 c.c.
Effect of Varying Bulk.—These experiments were carried out in the usual
way, bulk only varying.
Bulk 100.0 c.c. 200.0c.c. 300.0 c.c. 500.0 c.c.
"Hypo" required 20.4 " 20.4 " 20.4 " 20.4 "
Effect of Varying Acid.—These experiments were under the usual
conditions, the bulk being 100 c.c. The results were—
Acetic acid — 1.5 c.c. 30.0c.c.
"Hypo" required 20.4 c.c. 20.7 " 20.7"
Hydrochloric acid — 1.5 c.c. 15.0c.c.
"Hypo" required 20.4 c.c. 20.6 " 20.9"
Sulphuric acid — 0.5 c.c. 20.0c.c.
"Hypo" required 20.4 c.c. 20.7 " 15.2 "[86]
Nitric acid — 0.5 c.c. 10.0c.c.
"Hypo" required 20.4 c.c. 21.5 " could not be titrated.
In the application of this titration to the assay of manganese ores,
hydrochloric and hydriodic acids are the only ones likely to be present.
Effect of Alkalies.—On theoretical grounds the presence of these is known
to be inadmissible. A solution rendered faintly alkaline with ammonia
required only 11.2 c.c. of "hypo;" and another, with 0.5 gram of caustic
soda, required 4.0 c.c. instead of 20.4 c.c. as in neutral solutions.
Effect of nearly Neutralising Hydrochloric Acid Solutions with
Ammonia.—Provided care is taken not to add excess of ammonia, this has
a good effect, counteracting the interference of excess of acid. Thus 20 c.c.
of iodine (as before) required 20.4 c.c. of "hypo;" with 15 c.c. of
Page 385
hydrochloric acid 20.7 c.c. were required, but with 15 c.c. of acid, nearly
neutralised with dilute ammonia 20.4 c.c. were used.
Effect of the Addition of Starch.—The addition of varying quantities of
starch has no effect, provided it is added when the titration is nearly
finished, as the following experiments show:—
Starch added 1.0 c.c. 5.0 c.c. 10.0c.c. 50.0c.c.
"Hypo" required 20.4 " 20.4" 20.4" 20.5"
But if the starch is added before the titration, the results are liable to error.
Starch added 1.0 c.c. 50.0c.c.
"Hypo" required 20.4" 24.0"
The starch should be used fresh, and is best made on the day it is used; after
four days the finishing point is not so good.
Effect of Varying Potassium Iodide.—An excess of iodide is always
required to keep the iodine in solution; a larger excess has little effect.
Iodide added — 1 gram 20 grams
"Hypo" required 20.4 c.c. 20.5 c.c. 20.6 c.c.
The 20 c.c. of iodine used, itself contained 0.5 gram of potassium iodide.
Effect of Foreign Salts.—
Bicarbonate of soda added — 0.5 gram1.5 gram 5.0 grams
"Hypo" required 20.4 c.c. 18.2 c.c. 17.1 c.c. 16.0 c.c.
The solution obviously must be free from bicarbonate of soda. This should
be remembered, since when titrating arsenic assays with iodine it must be
present; and students must avoid confounding the two titrations.
In some other experiments, in which 10 grams each of the salts were taken,
the following results were obtained:—
Salt added — AmCl AmNO3 Am2SO4
neutralised with dilute ammonia 20.4 c.c. were used.
Effect of the Addition of Starch.—The addition of varying quantities of
starch has no effect, provided it is added when the titration is nearly
finished, as the following experiments show:—
Starch added 1.0 c.c. 5.0 c.c. 10.0c.c. 50.0c.c.
"Hypo" required 20.4 " 20.4" 20.4" 20.5"
But if the starch is added before the titration, the results are liable to error.
Starch added 1.0 c.c. 50.0c.c.
"Hypo" required 20.4" 24.0"
The starch should be used fresh, and is best made on the day it is used; after
four days the finishing point is not so good.
Effect of Varying Potassium Iodide.—An excess of iodide is always
required to keep the iodine in solution; a larger excess has little effect.
Iodide added — 1 gram 20 grams
"Hypo" required 20.4 c.c. 20.5 c.c. 20.6 c.c.
The 20 c.c. of iodine used, itself contained 0.5 gram of potassium iodide.
Effect of Foreign Salts.—
Bicarbonate of soda added — 0.5 gram1.5 gram 5.0 grams
"Hypo" required 20.4 c.c. 18.2 c.c. 17.1 c.c. 16.0 c.c.
The solution obviously must be free from bicarbonate of soda. This should
be remembered, since when titrating arsenic assays with iodine it must be
present; and students must avoid confounding the two titrations.
In some other experiments, in which 10 grams each of the salts were taken,
the following results were obtained:—
Salt added — AmCl AmNO3 Am2SO4
Page 386
"Hypo" required 20.4 c.c. 20.5 c.c. 20.3 c.c. 20.2 c.c.
Salt added NaCl NaNO3 Na2SO4
"Hypo" required 20.3 c.c. 20.4 c.c. 20.4 c.c.
Effect of Varying Iodine.—
Iodine added 1.0c.c. 10.0c.c. 20.0c.c. 50.0c.c. 100.0c.c.
"Hypo" required 1.3" 10.2" 20.4" 51.0" 102.0"
Determination of Dioxide in a Manganese Ore.—Weigh up 0.25 to 0.3
gram of the powdered ore; place in a flask, cover with 10 c.c. of
hydrochloric acid, and close the flask with a paraffined cork, and bulbs (as
shown in fig. 60), having previously charged the bulb with 5 grams of
potassium iodide in strong solution. Heat the flask, and boil cautiously for
about fifteen minutes. Wash the contents of the bulbs into a large beaker,
nearly (but not quite) neutralise with dilute ammonia, and titrate with the
standard "hypo."
As an example, 0.2675 gram of pyrolusite was taken, and required 60.3 c.c.
of standard "hypo" (100 c.c. equal 1.185 gram iodine, or 0.4042 gram
MnO2), which equals 0.2437 gram of the dioxide or 91.1 per cent.
COLORIMETRIC METHOD.
When compounds of manganese free from chlorides are boiled with nitric
acid and dioxide of lead,[87] the manganese is converted into permanganic
acid, which is soluble and tints the solution violet. The depth of colour
depends on the amount of manganese present, and this should not much
exceed 10 milligrams. A quantity of substance containing not more than this
amount of manganese should be boiled for a few minutes with 25 c.c. of a
solution containing 5 c.c. of nitric acid, and 10 or 20 c.c. of dilute sulphuric
acid, with 2 or 3 grams of lead dioxide. Filter through asbestos, wash by
decantation with dilute sulphuric acid, make up with distilled water[88] to a
definite bulk, and take a measured portion for the colorimetric
determination.
Salt added NaCl NaNO3 Na2SO4
"Hypo" required 20.3 c.c. 20.4 c.c. 20.4 c.c.
Effect of Varying Iodine.—
Iodine added 1.0c.c. 10.0c.c. 20.0c.c. 50.0c.c. 100.0c.c.
"Hypo" required 1.3" 10.2" 20.4" 51.0" 102.0"
Determination of Dioxide in a Manganese Ore.—Weigh up 0.25 to 0.3
gram of the powdered ore; place in a flask, cover with 10 c.c. of
hydrochloric acid, and close the flask with a paraffined cork, and bulbs (as
shown in fig. 60), having previously charged the bulb with 5 grams of
potassium iodide in strong solution. Heat the flask, and boil cautiously for
about fifteen minutes. Wash the contents of the bulbs into a large beaker,
nearly (but not quite) neutralise with dilute ammonia, and titrate with the
standard "hypo."
As an example, 0.2675 gram of pyrolusite was taken, and required 60.3 c.c.
of standard "hypo" (100 c.c. equal 1.185 gram iodine, or 0.4042 gram
MnO2), which equals 0.2437 gram of the dioxide or 91.1 per cent.
COLORIMETRIC METHOD.
When compounds of manganese free from chlorides are boiled with nitric
acid and dioxide of lead,[87] the manganese is converted into permanganic
acid, which is soluble and tints the solution violet. The depth of colour
depends on the amount of manganese present, and this should not much
exceed 10 milligrams. A quantity of substance containing not more than this
amount of manganese should be boiled for a few minutes with 25 c.c. of a
solution containing 5 c.c. of nitric acid, and 10 or 20 c.c. of dilute sulphuric
acid, with 2 or 3 grams of lead dioxide. Filter through asbestos, wash by
decantation with dilute sulphuric acid, make up with distilled water[88] to a
definite bulk, and take a measured portion for the colorimetric
determination.
Page 387
The standard solution of manganese is made by dissolving 0.1435 gram of
permanganate of potash (KMnO4) in a little water acidulated with nitric
acid, and diluting to 1 litre. One c.c. will contain 0.05 milligram of
manganese.
PRACTICAL EXERCISES.
1. What percentage of manganese (Mn) is contained in permanganate of
potash (KMnO4)?
2. Ten c.c. of a solution of permanganate of potash is found to oxidise 10
c.c. of an acid solution of ferrous sulphate. The manganese is determined in
the titrated solution by precipitation as dioxide and titrating. How much of
the ferrous solution will be oxidised in the second titration?
3. What weight of potassium iodide would be just sufficient to absorb the
chlorine evolved by 0.5 gram of pure dioxide of manganese?
4. What weight of iron must be dissolved up so as to have an excess of 0.25
gram after oxidation by 1 gram of pure dioxide?
5. What weight of the brown oxide, Mn2O4 will be left on igniting 1 gram
of the pure dioxide?
CHROMIUM.
Chromium occurs in nature chiefly as chromite or chrome iron ore
(FeO2Cr2O3, with more or less MgO and Al2O3), which is the chief ore. It is
a constituent of some silicates, and is frequently met with in very small
quantities in iron ores. It occurs as chromate in crocoisite (PbCrO4), and
some other rare minerals.
The metal is used in steel-making. Steel containing about 0.5 per cent. of it
is rendered very hard; but its chief value is in its salts, the chromates. These
are highly-coloured compounds, generally red or yellow. Some of the
insoluble chromates are used as pigments; chromate of lead or chrome-
yellow is the most important. The soluble chromates, those of soda and
permanganate of potash (KMnO4) in a little water acidulated with nitric
acid, and diluting to 1 litre. One c.c. will contain 0.05 milligram of
manganese.
PRACTICAL EXERCISES.
1. What percentage of manganese (Mn) is contained in permanganate of
potash (KMnO4)?
2. Ten c.c. of a solution of permanganate of potash is found to oxidise 10
c.c. of an acid solution of ferrous sulphate. The manganese is determined in
the titrated solution by precipitation as dioxide and titrating. How much of
the ferrous solution will be oxidised in the second titration?
3. What weight of potassium iodide would be just sufficient to absorb the
chlorine evolved by 0.5 gram of pure dioxide of manganese?
4. What weight of iron must be dissolved up so as to have an excess of 0.25
gram after oxidation by 1 gram of pure dioxide?
5. What weight of the brown oxide, Mn2O4 will be left on igniting 1 gram
of the pure dioxide?
CHROMIUM.
Chromium occurs in nature chiefly as chromite or chrome iron ore
(FeO2Cr2O3, with more or less MgO and Al2O3), which is the chief ore. It is
a constituent of some silicates, and is frequently met with in very small
quantities in iron ores. It occurs as chromate in crocoisite (PbCrO4), and
some other rare minerals.
The metal is used in steel-making. Steel containing about 0.5 per cent. of it
is rendered very hard; but its chief value is in its salts, the chromates. These
are highly-coloured compounds, generally red or yellow. Some of the
insoluble chromates are used as pigments; chromate of lead or chrome-
yellow is the most important. The soluble chromates, those of soda and
Page 388
potash, are valuable chemicals, and are largely used in the preparation of
pigments, dyeing and tanning, and as oxidising agents.
Chromium forms two important classes of compounds—chromic salts,
corresponding to the oxide Cr2O3, and chromates, which contain the
trioxide CrO3. Solutions of chromic salts are green, whilst those of the
chromates are yellow. Chromates are reduced to chromic salts by the action
of most reducing agents in the presence of an acid; and this property is used
in assaying for the volumetric determination of ferrous iron, &c. The
chromates in solution are more stable than other similar oxidising agents,
and consequently are generally used in the laboratory as one of the standard
oxidising agents for volumetric analysis. They have the disadvantage of
requiring an outside indicator. Bichromate of potash (K2Cr2O7) is the salt
generally used for this purpose.
Chromic salts are oxidised to chromate by fusion with "fusion mixture" and
nitre, or by treating with chlorine in an alkaline solution.
Chromic salts closely resemble those of ferric iron, and in the ordinary
course of analysis chromic hydrate (green) is precipitated together with
ferric hydrate, alumina, &c., on the addition of ammonic chloride and
ammonia. The ignited oxide, Cr2O3, however, is not reduced on heating to
redness in a current of hydrogen.
Detection.—Chromium is detected by fusing the powdered substance with
"fusion mixture" and nitre. The melt is extracted with water and filtered.
The filtrate is acidified with acetic acid, and treated with a few drops of a
solution of lead acetate. A yellow precipitate indicates chromium.
Substances containing chromium impart a green colour to the borax bead in
both flames. Small quantities of chromate in neutral solution can be found
by the dark or violet-red colouration imparted thereto on boiling with a
dilute decoction of logwood.
Solution and Separation.—Chromates and chromic salts are generally
soluble in water or dilute acids. Chrome iron ore, however, and ignited
chromic oxide are insoluble; and the former presents considerable difficulty
on attempting to open up by the usual methods. A large number of mixtures
have been tried in order to get all the chromium in a soluble form. Among
pigments, dyeing and tanning, and as oxidising agents.
Chromium forms two important classes of compounds—chromic salts,
corresponding to the oxide Cr2O3, and chromates, which contain the
trioxide CrO3. Solutions of chromic salts are green, whilst those of the
chromates are yellow. Chromates are reduced to chromic salts by the action
of most reducing agents in the presence of an acid; and this property is used
in assaying for the volumetric determination of ferrous iron, &c. The
chromates in solution are more stable than other similar oxidising agents,
and consequently are generally used in the laboratory as one of the standard
oxidising agents for volumetric analysis. They have the disadvantage of
requiring an outside indicator. Bichromate of potash (K2Cr2O7) is the salt
generally used for this purpose.
Chromic salts are oxidised to chromate by fusion with "fusion mixture" and
nitre, or by treating with chlorine in an alkaline solution.
Chromic salts closely resemble those of ferric iron, and in the ordinary
course of analysis chromic hydrate (green) is precipitated together with
ferric hydrate, alumina, &c., on the addition of ammonic chloride and
ammonia. The ignited oxide, Cr2O3, however, is not reduced on heating to
redness in a current of hydrogen.
Detection.—Chromium is detected by fusing the powdered substance with
"fusion mixture" and nitre. The melt is extracted with water and filtered.
The filtrate is acidified with acetic acid, and treated with a few drops of a
solution of lead acetate. A yellow precipitate indicates chromium.
Substances containing chromium impart a green colour to the borax bead in
both flames. Small quantities of chromate in neutral solution can be found
by the dark or violet-red colouration imparted thereto on boiling with a
dilute decoction of logwood.
Solution and Separation.—Chromates and chromic salts are generally
soluble in water or dilute acids. Chrome iron ore, however, and ignited
chromic oxide are insoluble; and the former presents considerable difficulty
on attempting to open up by the usual methods. A large number of mixtures
have been tried in order to get all the chromium in a soluble form. Among
Page 389
these are the following. One part of the very finely-powdered ore is fused
with any of these mixtures.
(1) 10 parts of bisulphate of potash.
(2) 5 parts of bisulphate of potash and 5 parts of potassium fluoride.
(3) 5 parts of hydric potassic fluoride.
(4) 12 parts of bisulphate of potash; and, afterwards, with 6 parts of
carbonate of soda and 6 parts of nitre.
(5) 8 parts of borax; afterwards, with carbonate of soda till it ceases
to effervesce; then, with 3 parts of carbonate of soda and 3 of
nitre.
(6) 4 parts of borax and 6 parts of fusion mixture.
(7) 12 parts of caustic potash.
(8) 10 parts of caustic soda and 30 of magnesia.
(9) 5 parts of caustic soda and 3 of magnesia.
(10) 2 parts of carbonate of soda and 1 of lime.
(11) 6 parts of soda-lime and 2 of chlorate of potash.
(12) Sodium peroxide.
Of these, numbers 1, 2, and 3 yield the chromium in a form soluble in dilute
acids, as chromic salt. The rest in a form soluble in water, as potassium or
sodium chromate.
On boiling an insoluble chromium compound with chlorate of potash and
nitric acid, the chromium passes into solution as chromate. This method,
however, does not answer for chrome iron ore. In the fusion methods the
ore must be very finely powdered, well mixed with the fluxes, and
subjected to a prolonged fusion in a platinum vessel at a high temperature.
Undecomposed particles require re-fusion.
The aqueous extract containing the chromate is ready for volumetric work,
except in those cases where nitre has been used. For gravimetric work the
solution is acidified with hydrochloric acid, then mixed with ammonia in
slight excess, boiled, and filtered. The filtrate is acidified with hydrochloric
acid, and treated with sulphuretted hydrogen, warmed, rendered slightly
alkaline with ammonia, and the gas again passed. The chromium is
precipitated as chromic hydrate mixed with sulphur from the reduction with
with any of these mixtures.
(1) 10 parts of bisulphate of potash.
(2) 5 parts of bisulphate of potash and 5 parts of potassium fluoride.
(3) 5 parts of hydric potassic fluoride.
(4) 12 parts of bisulphate of potash; and, afterwards, with 6 parts of
carbonate of soda and 6 parts of nitre.
(5) 8 parts of borax; afterwards, with carbonate of soda till it ceases
to effervesce; then, with 3 parts of carbonate of soda and 3 of
nitre.
(6) 4 parts of borax and 6 parts of fusion mixture.
(7) 12 parts of caustic potash.
(8) 10 parts of caustic soda and 30 of magnesia.
(9) 5 parts of caustic soda and 3 of magnesia.
(10) 2 parts of carbonate of soda and 1 of lime.
(11) 6 parts of soda-lime and 2 of chlorate of potash.
(12) Sodium peroxide.
Of these, numbers 1, 2, and 3 yield the chromium in a form soluble in dilute
acids, as chromic salt. The rest in a form soluble in water, as potassium or
sodium chromate.
On boiling an insoluble chromium compound with chlorate of potash and
nitric acid, the chromium passes into solution as chromate. This method,
however, does not answer for chrome iron ore. In the fusion methods the
ore must be very finely powdered, well mixed with the fluxes, and
subjected to a prolonged fusion in a platinum vessel at a high temperature.
Undecomposed particles require re-fusion.
The aqueous extract containing the chromate is ready for volumetric work,
except in those cases where nitre has been used. For gravimetric work the
solution is acidified with hydrochloric acid, then mixed with ammonia in
slight excess, boiled, and filtered. The filtrate is acidified with hydrochloric
acid, and treated with sulphuretted hydrogen, warmed, rendered slightly
alkaline with ammonia, and the gas again passed. The chromium is
precipitated as chromic hydrate mixed with sulphur from the reduction with
Page 390
sulphuretted hydrogen. It is filtered off, washed with hot water, and ignited.
It is weighed as chromic oxide.
GRAVIMETRIC DETERMINATION.
The solution containing the chromium, freed from other metals and earths
and in the form of (green) chromic salt, is heated to boiling. If any chromate
is present reduce it with sodium sulphite or sulphuretted hydrogen. Add
ammonia in slight excess, boil till the liquid is free from a red tint, and
allow to settle for a few minutes. Filter, wash with hot water, dry, and ignite
strongly in a loosely-covered crucible. Cool, and weigh. The substance is
chromic oxide, Cr2O3, and contains 68.62 per cent. of chromium. It is a
dark-green powder insoluble in acids.
When, as is generally the case, the chromium exists altogether as chromate
(phosphates and arsenates being absent) it is best to proceed as follows:—
Render the solution acid with acetic acid, then add sodium acetate to the
solution and heat nearly to boiling; next treat with a slight excess of acetate
of lead, and boil. Allow to settle, and filter. Wash the precipitate with hot
water, dry in the water-oven or at a low temperature. Transfer the
precipitate to a weighed Berlin crucible, burn the filter separately, ignite
below redness, cool in the desiccator, and weigh. The substance is lead
chromate, PbCrO4, and contains 16.1 per cent. of chromium, or 23.53 per
cent. of chromic oxide (Cr2O3).
VOLUMETRIC METHOD.
This is based on the oxidation of ferrous iron by the solution containing the
chromium as chromate. A known weight of iron (0.5, 1, or 1.5 gram,
according to the quantity of chromate) is dissolved in 50 c.c. of dilute
sulphuric acid. The solution containing the chromate is added, and the
remaining ferrous iron titrated with the permanganate or bichromate of
potassium solution, as described under Iron. The iron thus found is
deducted from that taken, and the difference gives the iron oxidised by the
chromate. This multiplied by 0.3101 gives the chromium, Cr, and when
multiplied by 0.4529 gives the chromic oxide, Cr2O3.
It is weighed as chromic oxide.
GRAVIMETRIC DETERMINATION.
The solution containing the chromium, freed from other metals and earths
and in the form of (green) chromic salt, is heated to boiling. If any chromate
is present reduce it with sodium sulphite or sulphuretted hydrogen. Add
ammonia in slight excess, boil till the liquid is free from a red tint, and
allow to settle for a few minutes. Filter, wash with hot water, dry, and ignite
strongly in a loosely-covered crucible. Cool, and weigh. The substance is
chromic oxide, Cr2O3, and contains 68.62 per cent. of chromium. It is a
dark-green powder insoluble in acids.
When, as is generally the case, the chromium exists altogether as chromate
(phosphates and arsenates being absent) it is best to proceed as follows:—
Render the solution acid with acetic acid, then add sodium acetate to the
solution and heat nearly to boiling; next treat with a slight excess of acetate
of lead, and boil. Allow to settle, and filter. Wash the precipitate with hot
water, dry in the water-oven or at a low temperature. Transfer the
precipitate to a weighed Berlin crucible, burn the filter separately, ignite
below redness, cool in the desiccator, and weigh. The substance is lead
chromate, PbCrO4, and contains 16.1 per cent. of chromium, or 23.53 per
cent. of chromic oxide (Cr2O3).
VOLUMETRIC METHOD.
This is based on the oxidation of ferrous iron by the solution containing the
chromium as chromate. A known weight of iron (0.5, 1, or 1.5 gram,
according to the quantity of chromate) is dissolved in 50 c.c. of dilute
sulphuric acid. The solution containing the chromate is added, and the
remaining ferrous iron titrated with the permanganate or bichromate of
potassium solution, as described under Iron. The iron thus found is
deducted from that taken, and the difference gives the iron oxidised by the
chromate. This multiplied by 0.3101 gives the chromium, Cr, and when
multiplied by 0.4529 gives the chromic oxide, Cr2O3.
Page 391
COLORIMETRIC METHOD.
Small quantities of chromium may be determined, after conversion into
chromate, colorimetrically. The solution, which should not contain more
than a few milligrams in 100 c.c., is acidified with acetic acid and compared
against an equal volume of water rendered acid with acetic acid and tinted
with a standard bichromate of potassium solution. This standard bichromate
is made by dissolving 2.827 grams of the salt in water and diluting to 1 litre.
One c.c. will contain 1 milligram of chromium, Cr. The manner of working
this assay is the same as that adopted in the other colorimetric processes.
Determination of Chromium in Steel.[89]—Weigh up 2.4 grams, dissolve
in hydrochloric acid, and evaporate to dryness. Fuse with sodium carbonate
and nitre, extract with water, and make up to 301 c.c. Take 250 c.c. of the
clear liquor, boil with hydrochloric acid, add sodium phosphate, and then
ammonia in slight excess. Heat till clear. Filter off the precipitate, dissolve
it in hydrochloric acid, and evaporate to dryness. Take up with a little acid,
filter, and precipitate with a slight excess of ammonia. Wash, ignite, and
weigh as chromium phosphate (3Cr2O3,2P2O5), which contains 42.2 per
cent. of chromium.
VANADIUM.
Vanadium occurs in certain rare minerals, such as vanadinite
(3Pb3(VO4)2.PbCl2), a vanadate of lead; mottramite, a vanadate of copper
and lead; and dechenite, a vanadate of lead and zinc. It is occasionally
found in iron and copper ores and in the slags from them. In Spanish
copper-precipitates it is found along with chromium, and is probably
derived from the iron used for precipitating. The vanadates, like the
chromates, are coloured compounds, generally yellow or red. On reduction,
blue solutions are got. In their general reactions vanadates resemble
phosphates.
Vanadium is detected by the red colouration produced by passing
sulphuretted hydrogen into ammoniacal solutions for some time. On adding
an acid to the filtered solution a brown precipitate of the sulphide is
Small quantities of chromium may be determined, after conversion into
chromate, colorimetrically. The solution, which should not contain more
than a few milligrams in 100 c.c., is acidified with acetic acid and compared
against an equal volume of water rendered acid with acetic acid and tinted
with a standard bichromate of potassium solution. This standard bichromate
is made by dissolving 2.827 grams of the salt in water and diluting to 1 litre.
One c.c. will contain 1 milligram of chromium, Cr. The manner of working
this assay is the same as that adopted in the other colorimetric processes.
Determination of Chromium in Steel.[89]—Weigh up 2.4 grams, dissolve
in hydrochloric acid, and evaporate to dryness. Fuse with sodium carbonate
and nitre, extract with water, and make up to 301 c.c. Take 250 c.c. of the
clear liquor, boil with hydrochloric acid, add sodium phosphate, and then
ammonia in slight excess. Heat till clear. Filter off the precipitate, dissolve
it in hydrochloric acid, and evaporate to dryness. Take up with a little acid,
filter, and precipitate with a slight excess of ammonia. Wash, ignite, and
weigh as chromium phosphate (3Cr2O3,2P2O5), which contains 42.2 per
cent. of chromium.
VANADIUM.
Vanadium occurs in certain rare minerals, such as vanadinite
(3Pb3(VO4)2.PbCl2), a vanadate of lead; mottramite, a vanadate of copper
and lead; and dechenite, a vanadate of lead and zinc. It is occasionally
found in iron and copper ores and in the slags from them. In Spanish
copper-precipitates it is found along with chromium, and is probably
derived from the iron used for precipitating. The vanadates, like the
chromates, are coloured compounds, generally yellow or red. On reduction,
blue solutions are got. In their general reactions vanadates resemble
phosphates.
Vanadium is detected by the red colouration produced by passing
sulphuretted hydrogen into ammoniacal solutions for some time. On adding
an acid to the filtered solution a brown precipitate of the sulphide is
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produced. This gives with borax a colourless bead in the oxidising, and a
green one in the reducing, flame.
It is separated by fusing the ore with potassic nitrate, extracting with water
and precipitating with baric chloride. The precipitate is boiled with dilute
sulphuric acid, filtered, neutralised with ammonia, and saturated with
ammonic chloride. Ammonium vanadate separates out. It is filtered off,
ignited, and weighed as vanadic oxide, V2O5, containing 56.18 per cent. of
vanadium.
MOLYBDENUM.
Molybdenum occurs in nature chiefly as molybdenite (MoS2); it also occurs
in wulfenite, a molybdate of lead (PbMoO4), and in molybdic ochre
(MoO3).
Molybdate of ammonia is an important reagent in the determination of
phosphates, the manufacture of which compound is the chief purpose to
which molybdenum is applied.
Iron and copper ores frequently contain molybdenum, sometimes in
quantity; consequently it is met with in slags and pig-iron.
Molybdenum forms several series of salts. In those corresponding to the
lower oxides it is basic; but the trioxide (MoO3) is the acid oxide which
forms a series of salts called the molybdates. All molybdenum compounds
are converted into the trioxide by boiling with nitric acid. The trioxide is a
white powder readily dissolved by ammonia. It fuses at a red heat, and
volatilises freely in contact with air. It is slightly soluble in water.
Molybdates are easily reduced, with the production of coloured solutions,
by most reducing agents. Sulphuretted hydrogen first produces a blue tint,
and then precipitates a brown sulphide. The precipitation as sulphide is only
complete on prolonged treatment; a green colour indicates that some
molybdenum still remains in solution. The precipitated sulphide is soluble
in ammonium sulphide.
green one in the reducing, flame.
It is separated by fusing the ore with potassic nitrate, extracting with water
and precipitating with baric chloride. The precipitate is boiled with dilute
sulphuric acid, filtered, neutralised with ammonia, and saturated with
ammonic chloride. Ammonium vanadate separates out. It is filtered off,
ignited, and weighed as vanadic oxide, V2O5, containing 56.18 per cent. of
vanadium.
MOLYBDENUM.
Molybdenum occurs in nature chiefly as molybdenite (MoS2); it also occurs
in wulfenite, a molybdate of lead (PbMoO4), and in molybdic ochre
(MoO3).
Molybdate of ammonia is an important reagent in the determination of
phosphates, the manufacture of which compound is the chief purpose to
which molybdenum is applied.
Iron and copper ores frequently contain molybdenum, sometimes in
quantity; consequently it is met with in slags and pig-iron.
Molybdenum forms several series of salts. In those corresponding to the
lower oxides it is basic; but the trioxide (MoO3) is the acid oxide which
forms a series of salts called the molybdates. All molybdenum compounds
are converted into the trioxide by boiling with nitric acid. The trioxide is a
white powder readily dissolved by ammonia. It fuses at a red heat, and
volatilises freely in contact with air. It is slightly soluble in water.
Molybdates are easily reduced, with the production of coloured solutions,
by most reducing agents. Sulphuretted hydrogen first produces a blue tint,
and then precipitates a brown sulphide. The precipitation as sulphide is only
complete on prolonged treatment; a green colour indicates that some
molybdenum still remains in solution. The precipitated sulphide is soluble
in ammonium sulphide.
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Detection.—Molybdenum is detected by its behaviour with sulphuretted
hydrogen. Molybdenite can only be mistaken for graphite, from which it is
easily distinguished by yielding sulphur dioxide on roasting, and by giving,
on charcoal, a yellowish white incrustation, which becomes blue on
touching it for a moment with the reducing flame. The borax-bead is
colourless in the oxidising, and dark-brown in the reducing, flame.
GRAVIMETRIC DETERMINATION.
The solution containing the molybdate is neutralised and treated with an
excess of mercurous nitrate. The precipitate is allowed to settle for some
time, filtered, and washed with a dilute solution of mercurous nitrate. Then
it is dried, transferred to a weighed Berlin crucible containing ignited oxide
of lead, mixed, ignited, and weighed. The increase in weight gives the
amount of trioxide, MoO3. This contains 66.7 per cent. of molybdenum.
URANIUM.
Uranium occurs chiefly as pitchblende, which is an impure oxide (U3O8). It
is also found as sulphate in uranochre, johannite, &c.; and as phosphate in
the uranites, torbernite (hydrated phosphate of uranium and copper), and
autunite (hydrated phosphate of uranium and lime). It also occurs in some
rarer minerals.
The oxide is used for colouring glass; and the nitrate and acetate are used as
reagents. "Uranium yellow," used for enamel painting, is sodium uranate.
The uranates, in which the oxide of uranium acts as an acid, are mostly
insoluble and of secondary importance.
Uranium forms two families of salts, uranous and uranic; corresponding to
the oxides UO2 and UO3 respectively. The former are generally green and
the latter yellow. Uranous salts are converted into uranic by boiling with
nitric acid or other oxidising agents. Uranic salts, on the other hand, are
easily reduced by sulphuretted hydrogen, stannous chloride or zinc. This
property is made use of in determining the quantity of uranium in pure
solutions by titrating with permanganate of potassium solution as in the
case with iron.
hydrogen. Molybdenite can only be mistaken for graphite, from which it is
easily distinguished by yielding sulphur dioxide on roasting, and by giving,
on charcoal, a yellowish white incrustation, which becomes blue on
touching it for a moment with the reducing flame. The borax-bead is
colourless in the oxidising, and dark-brown in the reducing, flame.
GRAVIMETRIC DETERMINATION.
The solution containing the molybdate is neutralised and treated with an
excess of mercurous nitrate. The precipitate is allowed to settle for some
time, filtered, and washed with a dilute solution of mercurous nitrate. Then
it is dried, transferred to a weighed Berlin crucible containing ignited oxide
of lead, mixed, ignited, and weighed. The increase in weight gives the
amount of trioxide, MoO3. This contains 66.7 per cent. of molybdenum.
URANIUM.
Uranium occurs chiefly as pitchblende, which is an impure oxide (U3O8). It
is also found as sulphate in uranochre, johannite, &c.; and as phosphate in
the uranites, torbernite (hydrated phosphate of uranium and copper), and
autunite (hydrated phosphate of uranium and lime). It also occurs in some
rarer minerals.
The oxide is used for colouring glass; and the nitrate and acetate are used as
reagents. "Uranium yellow," used for enamel painting, is sodium uranate.
The uranates, in which the oxide of uranium acts as an acid, are mostly
insoluble and of secondary importance.
Uranium forms two families of salts, uranous and uranic; corresponding to
the oxides UO2 and UO3 respectively. The former are generally green and
the latter yellow. Uranous salts are converted into uranic by boiling with
nitric acid or other oxidising agents. Uranic salts, on the other hand, are
easily reduced by sulphuretted hydrogen, stannous chloride or zinc. This
property is made use of in determining the quantity of uranium in pure
solutions by titrating with permanganate of potassium solution as in the
case with iron.
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Detection.—The most characteristic reaction of the uranium compounds is
their behaviour in the presence of alkaline carbonates in which they are
freely soluble; even ammonium sulphide will not precipitate uranium from
these solutions. On neutralising the carbonate with an acid a uranate of the
alkali is precipitated. Ammonia or sodic hydrate (free from carbonates) give
yellow precipitates, which are insoluble in excess of the reagent, but are
soluble in acids. Ferrocyanide of potassium gives a reddish-brown
precipitate. Uranium colours the borax-bead yellowish-green in the
oxidising, and green in the reducing, flame.
Solution and Separation.—The compounds of uranium are soluble in
acids. Powder the substance and evaporate with an excess of nitric acid.
Take up with hydrochloric acid, dilute, pass sulphuretted hydrogen, and
filter. Peroxidise the filtrate with a little nitric acid, add an excess of
ammonic carbonate and some ammonium sulphide, and filter. Render the
solution acid, boil; and precipitate the uranium by means of ammonia. Filter
off, and wash it with dilute ammonic chloride. Ignite, and weigh as
protosesqui-oxide, U3O8.
GRAVIMETRIC DETERMINATION.
The solution containing the uranium free from other metals is, if required,
first peroxidised by boiling with nitric acid. Ammonia in slight excess is
added to the nearly-boiling solution. A yellow precipitate is formed, which
is filtered off hot and washed with a dilute solution of ammonium chloride.
The precipitate is dried and ignited; and weighed as U3O8, which contains
84.8 per cent. of uranium.
VOLUMETRIC METHOD.
This is based on the precipitation of uranium as phosphate from acetic acid
solutions and the recognition of complete precipitation by testing with
potassic ferrocyanide; it is the converse of the process for the volumetric
determination of phosphate.
The standard solution of phosphate is prepared by dissolving 29.835 grams
of hydric sodic phosphate (Na2HPO4.12H2O) in water and diluting to 1
their behaviour in the presence of alkaline carbonates in which they are
freely soluble; even ammonium sulphide will not precipitate uranium from
these solutions. On neutralising the carbonate with an acid a uranate of the
alkali is precipitated. Ammonia or sodic hydrate (free from carbonates) give
yellow precipitates, which are insoluble in excess of the reagent, but are
soluble in acids. Ferrocyanide of potassium gives a reddish-brown
precipitate. Uranium colours the borax-bead yellowish-green in the
oxidising, and green in the reducing, flame.
Solution and Separation.—The compounds of uranium are soluble in
acids. Powder the substance and evaporate with an excess of nitric acid.
Take up with hydrochloric acid, dilute, pass sulphuretted hydrogen, and
filter. Peroxidise the filtrate with a little nitric acid, add an excess of
ammonic carbonate and some ammonium sulphide, and filter. Render the
solution acid, boil; and precipitate the uranium by means of ammonia. Filter
off, and wash it with dilute ammonic chloride. Ignite, and weigh as
protosesqui-oxide, U3O8.
GRAVIMETRIC DETERMINATION.
The solution containing the uranium free from other metals is, if required,
first peroxidised by boiling with nitric acid. Ammonia in slight excess is
added to the nearly-boiling solution. A yellow precipitate is formed, which
is filtered off hot and washed with a dilute solution of ammonium chloride.
The precipitate is dried and ignited; and weighed as U3O8, which contains
84.8 per cent. of uranium.
VOLUMETRIC METHOD.
This is based on the precipitation of uranium as phosphate from acetic acid
solutions and the recognition of complete precipitation by testing with
potassic ferrocyanide; it is the converse of the process for the volumetric
determination of phosphate.
The standard solution of phosphate is prepared by dissolving 29.835 grams
of hydric sodic phosphate (Na2HPO4.12H2O) in water and diluting to 1
Page 395
litre. 100 c.c. will be equivalent to 2 grams of uranium.
Take 1 gram of the sample (or, if poor in uranium, 2 grams) and separate the
uranium as described. Dissolve the precipitate in nitric acid and evaporate
to a small bulk, add 2 grams of sodium acetate, dilute with water to 100
c.c., and boil. Titrate the boiling solution with the sodium phosphate till it
ceases to give a brown colouration with potassium ferrocyanide. Calculate
the percentage in the usual way.
FOOTNOTES:
[78] MnO2 + 4HCl = MnCl2 + Cl2 + 2H2O.
[79] Provided a sufficiency of ammonic chloride is present.
[80] With some silicates, &c., a preliminary fusion with sodium carbonate will
be necessary.
[81] Instead of sodium acetate, ammonium succinate can be used.
[82] Journ. Soc. Chem. Industry, vol. x. p. 333.
[83] MnO2 + 2FeSO4 + 2H2SO4 = Fe2(SO4)3 + MnSO4 + 2H2O.
[84] If the ore is very rich, a smaller quantity (0.75 or 1.5 gram) must be taken;
otherwise the iron will be insufficient.
[85]
MnO2 + 4HCl = MnCl2 + 2H2O + Cl2.
Cl2 + 2KI = 2KCl + I2.
[86] Iodine probably lost by volatilisation.
[87] Obtained as a brown powder by digesting red lead with nitric acid and
filtering.
[88] The water for dilution and the dilute sulphuric acid used for washing should
be previously tested, to see they have no reducing action, with dilute
permanganate of potassium solution.
[89] Arnold and Hardy, Chemical News, vol. lvii. p. 153.
Take 1 gram of the sample (or, if poor in uranium, 2 grams) and separate the
uranium as described. Dissolve the precipitate in nitric acid and evaporate
to a small bulk, add 2 grams of sodium acetate, dilute with water to 100
c.c., and boil. Titrate the boiling solution with the sodium phosphate till it
ceases to give a brown colouration with potassium ferrocyanide. Calculate
the percentage in the usual way.
FOOTNOTES:
[78] MnO2 + 4HCl = MnCl2 + Cl2 + 2H2O.
[79] Provided a sufficiency of ammonic chloride is present.
[80] With some silicates, &c., a preliminary fusion with sodium carbonate will
be necessary.
[81] Instead of sodium acetate, ammonium succinate can be used.
[82] Journ. Soc. Chem. Industry, vol. x. p. 333.
[83] MnO2 + 2FeSO4 + 2H2SO4 = Fe2(SO4)3 + MnSO4 + 2H2O.
[84] If the ore is very rich, a smaller quantity (0.75 or 1.5 gram) must be taken;
otherwise the iron will be insufficient.
[85]
MnO2 + 4HCl = MnCl2 + 2H2O + Cl2.
Cl2 + 2KI = 2KCl + I2.
[86] Iodine probably lost by volatilisation.
[87] Obtained as a brown powder by digesting red lead with nitric acid and
filtering.
[88] The water for dilution and the dilute sulphuric acid used for washing should
be previously tested, to see they have no reducing action, with dilute
permanganate of potassium solution.
[89] Arnold and Hardy, Chemical News, vol. lvii. p. 153.
Page 396
CHAPTER XIV.
EARTHS, ALKALINE EARTHS, ALKALIES.
ALUMINA.
Alumina, the oxide of aluminium (Al2O3), is found in nature fairly pure in
the mineral corundum; transparent and coloured varieties of which form the
gems sapphire and ruby. A coarser compact variety contaminated with oxide
of iron constitutes emery. Compounded with silica, alumina forms the base
of clays and many rock-forming minerals. China clay (or kaolin) is used as
a source of alumina. Bauxite, hydrated alumina, is also used for the same
purpose—that is, for the preparation of sulphate of alumina. The mineral
cryolite is a fluoride of aluminium and sodium.
Corundum is characterised by a high specific gravity (4.0) and extreme
hardness. By these it is distinguished from felspar and similar minerals,
which it somewhat resembles in general appearance.
Aluminium is used for a variety of small purposes: it is white, light, and
very tenacious; but owing to the difficulty of its reduction it is expensive.
Aluminium forms one series of salts which closely resemble those of ferric
iron. It forms an interesting series of double sulphates, known as the alums.
Common potash alum is Al2(SO4)3,K2SO4,24H2O.
Detection.—Alumina is not precipitated from its acid solution by
sulphuretted hydrogen, but it is thrown down by ammonia (with the other
earths) as a white hydrate, soluble in soda and insoluble in ammonic
carbonate. Filtered off and ignited, it assumes, after treatment with nitrate of
cobalt before the blowpipe, a blue colour which is characteristic. With
natural compounds containing metallic oxides this colour is masked. It is
more satisfactory to make a separation in the wet way and to test the ignited
oxide.
EARTHS, ALKALINE EARTHS, ALKALIES.
ALUMINA.
Alumina, the oxide of aluminium (Al2O3), is found in nature fairly pure in
the mineral corundum; transparent and coloured varieties of which form the
gems sapphire and ruby. A coarser compact variety contaminated with oxide
of iron constitutes emery. Compounded with silica, alumina forms the base
of clays and many rock-forming minerals. China clay (or kaolin) is used as
a source of alumina. Bauxite, hydrated alumina, is also used for the same
purpose—that is, for the preparation of sulphate of alumina. The mineral
cryolite is a fluoride of aluminium and sodium.
Corundum is characterised by a high specific gravity (4.0) and extreme
hardness. By these it is distinguished from felspar and similar minerals,
which it somewhat resembles in general appearance.
Aluminium is used for a variety of small purposes: it is white, light, and
very tenacious; but owing to the difficulty of its reduction it is expensive.
Aluminium forms one series of salts which closely resemble those of ferric
iron. It forms an interesting series of double sulphates, known as the alums.
Common potash alum is Al2(SO4)3,K2SO4,24H2O.
Detection.—Alumina is not precipitated from its acid solution by
sulphuretted hydrogen, but it is thrown down by ammonia (with the other
earths) as a white hydrate, soluble in soda and insoluble in ammonic
carbonate. Filtered off and ignited, it assumes, after treatment with nitrate of
cobalt before the blowpipe, a blue colour which is characteristic. With
natural compounds containing metallic oxides this colour is masked. It is
more satisfactory to make a separation in the wet way and to test the ignited
oxide.
Page 397
Separation and Solution.—If the substance is insoluble in hydrochloric
acid it is finely powdered and fused with "fusion mixture" with the help, in
the case of corundum (which is very refractory) of a little caustic soda or
potash. The method of working is the same as that described for opening up
silicates. See under Silica. Corundum cannot be powdered in Wedgwood, or
even agate, mortars; since it rapidly wears these away and becomes
contaminated with their powder. It is best to use a hard steel mortar and to
extract the metallic particles from the bruised sample with a magnet or
dilute acid.
When the substance has been completely attacked and dissolved, it is
evaporated to dryness with an excess of hydrochloric acid on the water-bath
to render any silica present insoluble. The residue is extracted with
hydrochloric acid and freed from the second group of metals by means of
sulphuretted hydrogen. The filtrate from this (after removing the
sulphuretted hydrogen by boiling) is nearly neutralised, and treated with 8
or 10 grams of hyposulphite of soda[90] in solution. It is then boiled till the
sulphurous oxide is driven off. The precipitate is filtered off, ignited, and
weighed as alumina.
It is sometimes more convenient to proceed as follows:—After boiling off
the sulphuretted hydrogen peroxidise the iron with a little nitric acid, add a
solution of ammonic chloride, and then ammonia in very slight excess; boil,
filter, wash, ignite, and weigh the oxides. These generally consist of ferric
oxide and alumina. It is a common practice to determine the iron, calculate
it to ferric oxide, and so to estimate the alumina indirectly. This may be
done either by igniting in a current of hydrogen and estimating the iron by
the weight of oxygen lost; or, by dissolving with sulphuric and hydrochloric
acids, and determining the iron volumetrically. It should be borne in mind
that these oxides will also contain any phosphoric oxide that happened to be
in the mineral.
In general analyses of samples containing alumina, it may be contained in
both the soluble and insoluble portions. In these cases it is better to fuse the
sample with "fusion mixture" before treatment with acids. The alumina in
the fused mass will exist in a state soluble in acids.
GRAVIMETRIC DETERMINATION.
acid it is finely powdered and fused with "fusion mixture" with the help, in
the case of corundum (which is very refractory) of a little caustic soda or
potash. The method of working is the same as that described for opening up
silicates. See under Silica. Corundum cannot be powdered in Wedgwood, or
even agate, mortars; since it rapidly wears these away and becomes
contaminated with their powder. It is best to use a hard steel mortar and to
extract the metallic particles from the bruised sample with a magnet or
dilute acid.
When the substance has been completely attacked and dissolved, it is
evaporated to dryness with an excess of hydrochloric acid on the water-bath
to render any silica present insoluble. The residue is extracted with
hydrochloric acid and freed from the second group of metals by means of
sulphuretted hydrogen. The filtrate from this (after removing the
sulphuretted hydrogen by boiling) is nearly neutralised, and treated with 8
or 10 grams of hyposulphite of soda[90] in solution. It is then boiled till the
sulphurous oxide is driven off. The precipitate is filtered off, ignited, and
weighed as alumina.
It is sometimes more convenient to proceed as follows:—After boiling off
the sulphuretted hydrogen peroxidise the iron with a little nitric acid, add a
solution of ammonic chloride, and then ammonia in very slight excess; boil,
filter, wash, ignite, and weigh the oxides. These generally consist of ferric
oxide and alumina. It is a common practice to determine the iron, calculate
it to ferric oxide, and so to estimate the alumina indirectly. This may be
done either by igniting in a current of hydrogen and estimating the iron by
the weight of oxygen lost; or, by dissolving with sulphuric and hydrochloric
acids, and determining the iron volumetrically. It should be borne in mind
that these oxides will also contain any phosphoric oxide that happened to be
in the mineral.
In general analyses of samples containing alumina, it may be contained in
both the soluble and insoluble portions. In these cases it is better to fuse the
sample with "fusion mixture" before treatment with acids. The alumina in
the fused mass will exist in a state soluble in acids.
GRAVIMETRIC DETERMINATION.
Page 398
Solutions containing alumina free from the other metals are diluted to a
convenient bulk and heated nearly to boiling. Add chloride of ammonium,
and then ammonia in slight excess; boil, allow to settle, filter, and wash
with hot water. Dry the precipitate, and ignite in a platinum or porcelain
crucible at the strongest heat. Cool, and weigh. The substance is alumina,
Al2O3, which contains 52.94 per cent. of aluminium. It is only in special
cases, such as the analysis of metals and alloys, that it is reported as
aluminium. The percentage of alumina is generally given.
Ignited alumina is difficultly soluble in acids; it is not reduced by hydrogen
at a red heat. Ignited with ammonium chloride portions are volatilised.
Direct Determination of Alumina in the Presence of Iron.—The iron and
alumina are precipitated as hydrates by ammonia. The precipitate is
dissolved in hydrochloric acid and the iron reduced to the ferrous state. It is
then added to a hot solution of potash or soda. The solution is boiled till the
precipitate settles readily, filtered, and washed with hot water. The alumina
is contained in the filtrate, which is acidified with hydrochloric acid and the
alumina precipitated therefrom as hydrate with ammonia, as just described.
Determination of Alumina in the Presence of Phosphates and Iron.—
For details, see a paper by R.T. Thomson in the "Journal of the Society of
Chemical Industry," v. p. 152. The principles of the method are as follows:
—If the substance does not already contain sufficient phosphoric oxide to
saturate the alumina, some phosphate is added. The iron is reduced to the
ferrous state and phosphate of alumina precipitated in an acetic acid
solution. It is purified by reprecipitation, ignited, and weighed as phosphate
(Al2O3,P2O5), which contains 41.8 per cent. of alumina, Al2O3.
EXAMINATION OF CLAYS.
Moisture.—Take 5 grams of the carefully-prepared sample and dry in the
water-oven till the weight is constant.
Loss on Ignition.—Weigh up 2 grams of the sample used for the moisture
determination, and ignite in a platinum-crucible to redness, cool, and weigh.
convenient bulk and heated nearly to boiling. Add chloride of ammonium,
and then ammonia in slight excess; boil, allow to settle, filter, and wash
with hot water. Dry the precipitate, and ignite in a platinum or porcelain
crucible at the strongest heat. Cool, and weigh. The substance is alumina,
Al2O3, which contains 52.94 per cent. of aluminium. It is only in special
cases, such as the analysis of metals and alloys, that it is reported as
aluminium. The percentage of alumina is generally given.
Ignited alumina is difficultly soluble in acids; it is not reduced by hydrogen
at a red heat. Ignited with ammonium chloride portions are volatilised.
Direct Determination of Alumina in the Presence of Iron.—The iron and
alumina are precipitated as hydrates by ammonia. The precipitate is
dissolved in hydrochloric acid and the iron reduced to the ferrous state. It is
then added to a hot solution of potash or soda. The solution is boiled till the
precipitate settles readily, filtered, and washed with hot water. The alumina
is contained in the filtrate, which is acidified with hydrochloric acid and the
alumina precipitated therefrom as hydrate with ammonia, as just described.
Determination of Alumina in the Presence of Phosphates and Iron.—
For details, see a paper by R.T. Thomson in the "Journal of the Society of
Chemical Industry," v. p. 152. The principles of the method are as follows:
—If the substance does not already contain sufficient phosphoric oxide to
saturate the alumina, some phosphate is added. The iron is reduced to the
ferrous state and phosphate of alumina precipitated in an acetic acid
solution. It is purified by reprecipitation, ignited, and weighed as phosphate
(Al2O3,P2O5), which contains 41.8 per cent. of alumina, Al2O3.
EXAMINATION OF CLAYS.
Moisture.—Take 5 grams of the carefully-prepared sample and dry in the
water-oven till the weight is constant.
Loss on Ignition.—Weigh up 2 grams of the sample used for the moisture
determination, and ignite in a platinum-crucible to redness, cool, and weigh.
Page 399
Silica and Insoluble Silicates.—Weigh up another 2 grams of the dried
sample, and place them in a platinum dish; moisten with water, and cover
with 20 c.c. of sulphuric acid. Evaporate and heat gently to drive off the
greater portion of the free acid. Allow to cool; and repeat the operation.
Extract by boiling with dilute hydrochloric acid, filter, wash, dry, ignite, and
weigh. The quantity of insoluble silicates is determined by dissolving out
the separated silica with a strong boiling solution of sodium carbonate. The
residue (washed, dried, and ignited) is weighed, and reported as "sand."
Alumina and Ferrous Oxide.—To the filtrate from the silica add "soda"
solution till nearly neutral, and then sodium acetate. Boil and filter off the
precipitate. Reserve the filtrate. Dissolve the precipitate in hydrochloric
acid, and dilute to exactly 200 c.c. Divide into two parts of 100 c.c. each. In
one determine the iron by reducing and titrating in the way described under
volumetric iron. Calculate the percentage as ferrous oxide, unless there are
reasons to the contrary, also calculate its weight as ferric oxide. To the other
portion add ammonia in slight excess, and boil. Filter, wash with hot water,
dry, ignite, and weigh as mixed alumina and ferric oxide. The weight of the
ferric oxide has already been determined in the first portion: deduct it, and
the difference is the weight of alumina.
Lime.—To the reserved filtrate, concentrated by evaporation, add
ammonium oxalate and ammonia; boil, filter, ignite strongly, and weigh as
lime.
Magnesia is separated from the filtrate by adding sodium phosphate. It is
weighed as magnesium pyrophosphate.
Potash and Soda.—These are determined in a fresh portion of the sample
by Lawrence Smith's method, as described on page 333.
THORIA.
This is an oxide of thorium, ThO2. It is only found in a few rare minerals. It
is a heavy oxide, having, when strongly ignited, a specific gravity of 9.2. In
the ordinary course of analysis it will be separated and weighed as alumina.
It is separated from this and other earths by the following method. The
solution in hydrochloric acid is nearly neutralised and then boiled with
sample, and place them in a platinum dish; moisten with water, and cover
with 20 c.c. of sulphuric acid. Evaporate and heat gently to drive off the
greater portion of the free acid. Allow to cool; and repeat the operation.
Extract by boiling with dilute hydrochloric acid, filter, wash, dry, ignite, and
weigh. The quantity of insoluble silicates is determined by dissolving out
the separated silica with a strong boiling solution of sodium carbonate. The
residue (washed, dried, and ignited) is weighed, and reported as "sand."
Alumina and Ferrous Oxide.—To the filtrate from the silica add "soda"
solution till nearly neutral, and then sodium acetate. Boil and filter off the
precipitate. Reserve the filtrate. Dissolve the precipitate in hydrochloric
acid, and dilute to exactly 200 c.c. Divide into two parts of 100 c.c. each. In
one determine the iron by reducing and titrating in the way described under
volumetric iron. Calculate the percentage as ferrous oxide, unless there are
reasons to the contrary, also calculate its weight as ferric oxide. To the other
portion add ammonia in slight excess, and boil. Filter, wash with hot water,
dry, ignite, and weigh as mixed alumina and ferric oxide. The weight of the
ferric oxide has already been determined in the first portion: deduct it, and
the difference is the weight of alumina.
Lime.—To the reserved filtrate, concentrated by evaporation, add
ammonium oxalate and ammonia; boil, filter, ignite strongly, and weigh as
lime.
Magnesia is separated from the filtrate by adding sodium phosphate. It is
weighed as magnesium pyrophosphate.
Potash and Soda.—These are determined in a fresh portion of the sample
by Lawrence Smith's method, as described on page 333.
THORIA.
This is an oxide of thorium, ThO2. It is only found in a few rare minerals. It
is a heavy oxide, having, when strongly ignited, a specific gravity of 9.2. In
the ordinary course of analysis it will be separated and weighed as alumina.
It is separated from this and other earths by the following method. The
solution in hydrochloric acid is nearly neutralised and then boiled with
Page 400
sodium hyposulphite. The thoria will be in the precipitate. It is dissolved,
and the solution heated with ammonium oxalate in excess. The precipitate is
thorium oxalate, which is washed with hot water, dried, and ignited. It is
then weighed as thoria, ThO2. Thoria which has been ignited is not readily
soluble in acids.
ZIRCONIA.
The oxide of zirconium, ZrO2, is found in the mineral zircon, a silicate of
zirconia, ZrSiO4. When heated intensely it becomes very luminous, and is
used on this account for incandescent lights.
In the ordinary course it is thrown down by ammonia with the other earths,
from which it is thus separated:—The hydrates precipitated in the cold, and
washed with cold water, are dissolved in hydrochloric acid, nearly
neutralised with soda, and precipitated by boiling with hyposulphite of
soda. Dissolve; and from the hydrochloric acid solution precipitate the
thoria (if any) with ammonium oxalate. To the filtrate add carbonate of
ammonia, which will precipitate any titanium present. The zirconia will be
in solution, and is recovered by precipitating with potassium sulphate, or by
evaporating the solution and igniting. It is separated from alumina by taking
advantage of its insolubility in potassic hydrate.
It is estimated in zircons in the following way:—The powdered substance is
fused with bisulphate of potash, and extracted with dilute sulphuric acid.
The residue is fused with caustic soda and extracted with water. The portion
not dissolved, consisting of zirconate of soda, is dissolved in hydrochloric
acid. The solution is diluted, filtered if necessary, and treated with ammonia
in excess. The precipitate is filtered off, washed with hot water, dried,
ignited, and weighed as zirconia, ZrO2. This is a white powder, which is
insoluble in acids; even in hydrofluoric acid it is only slightly attacked.
CERIUM.
Cerium occurs as silicate (together with the oxides of lanthanum,
didymium, iron and calcium) in the mineral cerite, which is its chief source.
and the solution heated with ammonium oxalate in excess. The precipitate is
thorium oxalate, which is washed with hot water, dried, and ignited. It is
then weighed as thoria, ThO2. Thoria which has been ignited is not readily
soluble in acids.
ZIRCONIA.
The oxide of zirconium, ZrO2, is found in the mineral zircon, a silicate of
zirconia, ZrSiO4. When heated intensely it becomes very luminous, and is
used on this account for incandescent lights.
In the ordinary course it is thrown down by ammonia with the other earths,
from which it is thus separated:—The hydrates precipitated in the cold, and
washed with cold water, are dissolved in hydrochloric acid, nearly
neutralised with soda, and precipitated by boiling with hyposulphite of
soda. Dissolve; and from the hydrochloric acid solution precipitate the
thoria (if any) with ammonium oxalate. To the filtrate add carbonate of
ammonia, which will precipitate any titanium present. The zirconia will be
in solution, and is recovered by precipitating with potassium sulphate, or by
evaporating the solution and igniting. It is separated from alumina by taking
advantage of its insolubility in potassic hydrate.
It is estimated in zircons in the following way:—The powdered substance is
fused with bisulphate of potash, and extracted with dilute sulphuric acid.
The residue is fused with caustic soda and extracted with water. The portion
not dissolved, consisting of zirconate of soda, is dissolved in hydrochloric
acid. The solution is diluted, filtered if necessary, and treated with ammonia
in excess. The precipitate is filtered off, washed with hot water, dried,
ignited, and weighed as zirconia, ZrO2. This is a white powder, which is
insoluble in acids; even in hydrofluoric acid it is only slightly attacked.
CERIUM.
Cerium occurs as silicate (together with the oxides of lanthanum,
didymium, iron and calcium) in the mineral cerite, which is its chief source.
Page 401
It also occurs as phosphate in monazite, and as fluoride in fluocerite. The
oxalate is used in medicine. Cerium forms two classes of salts
corresponding to the oxides, cerous oxide (Ce2O3) and ceric oxide (CeO2).
Compounds of cerium with volatile acids yield dioxide on ignition; and
this, on solution in hydrochloric acid, yields cerous chloride and chlorine.
In the ordinary course cerium is thrown down along with alumina and the
other earths by ammonia. It is separated by dissolving the hydrates in
hydrochloric acid, and oxidizing with chlorine water. On treating with
oxalic acid, cerium, lanthanum, and didymium are precipitated as oxalates,
which on ignition are converted into oxides. These are soluble in acids.
Their solution in hydrochloric acid is nearly neutralised; acetate of soda is
then added, and an excess of sodium hypochlorite. On boiling, the cerium is
precipitated as dioxide, which is filtered off, ignited, and weighed.
Cerium is detected by giving with borax a bead which is yellow in the
oxidising, and colourless in the reducing flame. Traces of cerium
compounds boiled with dioxide of lead and nitric acid will give a yellow
solution.
LANTHANUM AND DIDYMIUM
occur together with cerium in cerite, and are separated with that metal as
oxalates, as described under Cerium.
Didymium salts have a rose or violet colour, and impart (when in sufficient
quantity) the same colour to the borax bead. Solutions have a characteristic
absorption-spectrum.
The separation of lanthanum and didymium in the solution from which the
cerium has been precipitated is effected by precipitating them together as
oxalates, igniting, and dissolving in dilute nitric acid. This solution is then
evaporated to dryness and ignited, for a few minutes, just below redness. A
subnitrate of didymium is formed, and remains as an insoluble residue on
extracting with hot water. The separated salts are treated with ammonia and
ignited, and weighed as oxides (La2O3 and Di2O3).
YTTRIA.
oxalate is used in medicine. Cerium forms two classes of salts
corresponding to the oxides, cerous oxide (Ce2O3) and ceric oxide (CeO2).
Compounds of cerium with volatile acids yield dioxide on ignition; and
this, on solution in hydrochloric acid, yields cerous chloride and chlorine.
In the ordinary course cerium is thrown down along with alumina and the
other earths by ammonia. It is separated by dissolving the hydrates in
hydrochloric acid, and oxidizing with chlorine water. On treating with
oxalic acid, cerium, lanthanum, and didymium are precipitated as oxalates,
which on ignition are converted into oxides. These are soluble in acids.
Their solution in hydrochloric acid is nearly neutralised; acetate of soda is
then added, and an excess of sodium hypochlorite. On boiling, the cerium is
precipitated as dioxide, which is filtered off, ignited, and weighed.
Cerium is detected by giving with borax a bead which is yellow in the
oxidising, and colourless in the reducing flame. Traces of cerium
compounds boiled with dioxide of lead and nitric acid will give a yellow
solution.
LANTHANUM AND DIDYMIUM
occur together with cerium in cerite, and are separated with that metal as
oxalates, as described under Cerium.
Didymium salts have a rose or violet colour, and impart (when in sufficient
quantity) the same colour to the borax bead. Solutions have a characteristic
absorption-spectrum.
The separation of lanthanum and didymium in the solution from which the
cerium has been precipitated is effected by precipitating them together as
oxalates, igniting, and dissolving in dilute nitric acid. This solution is then
evaporated to dryness and ignited, for a few minutes, just below redness. A
subnitrate of didymium is formed, and remains as an insoluble residue on
extracting with hot water. The separated salts are treated with ammonia and
ignited, and weighed as oxides (La2O3 and Di2O3).
YTTRIA.
Page 402
Yttria is found in gadolinite and some other rare minerals. It is precipitated
along with the other earths by ammonia. It is distinguished by the
insolubility of its hydrate in potash, by the insolubility of its oxalate in
oxalic acid, and by not being precipitated by hyposulphite of soda or
potassium sulphate. Further, it is precipitated by potash in the presence of
tartaric acid as an insoluble tartrate. This reaction distinguishes the
members of the yttria group from most of the other earths. The other
members of the group closely resemble it, and amongst them are erbia,
terbia, ytterbia, scandia, &c.
BERYLLIA.
The oxide of beryllium, BeO (also known as glucina), occurs in nature
mainly as silicate. Beryl, the green transparent variety of which is the
emerald, is the best known of these. It is a silicate of alumina and beryllia.
[91]
Some other minerals in which it occurs are phenakite, euclase, and
chrysoberyl.
In the ordinary course of analysis, beryllia will be precipitated with
alumina, &c., by ammonic hydrate. It is distinguished by the solubility of
its hydrate in ammonic carbonate, by not being precipitated by boiling with
sodium hyposulphite, and by not being precipitated by ammonic sulphide
from an ammonic carbonate solution.
The analysis of silicates containing beryllia is thus effected. The finely
powdered substance is fused with twice its weight of potassium carbonate;
and the "melt" is extracted with water, and evaporated with a slight excess
of sulphuric acid to render the silica insoluble. Treat with water, filter, and
evaporate the filtrate until a crust is formed. Potash alum crystallises out.
The liquor is poured off into a warm strong solution of ammonium
carbonate. Ferric hydrate and alumina will be precipitated. They are filtered
off, re-dissolved, and again precipitated in ammonic carbonate solution; the
combined filtrates are boiled for some time, and acidified slightly with
hydrochloric acid. The carbon dioxide is boiled off, and the beryllia is then
precipitated as hydrate with ammonia. The hydrate is washed with hot
water, dried, ignited, and weighed as beryllia, BeO.
along with the other earths by ammonia. It is distinguished by the
insolubility of its hydrate in potash, by the insolubility of its oxalate in
oxalic acid, and by not being precipitated by hyposulphite of soda or
potassium sulphate. Further, it is precipitated by potash in the presence of
tartaric acid as an insoluble tartrate. This reaction distinguishes the
members of the yttria group from most of the other earths. The other
members of the group closely resemble it, and amongst them are erbia,
terbia, ytterbia, scandia, &c.
BERYLLIA.
The oxide of beryllium, BeO (also known as glucina), occurs in nature
mainly as silicate. Beryl, the green transparent variety of which is the
emerald, is the best known of these. It is a silicate of alumina and beryllia.
[91]
Some other minerals in which it occurs are phenakite, euclase, and
chrysoberyl.
In the ordinary course of analysis, beryllia will be precipitated with
alumina, &c., by ammonic hydrate. It is distinguished by the solubility of
its hydrate in ammonic carbonate, by not being precipitated by boiling with
sodium hyposulphite, and by not being precipitated by ammonic sulphide
from an ammonic carbonate solution.
The analysis of silicates containing beryllia is thus effected. The finely
powdered substance is fused with twice its weight of potassium carbonate;
and the "melt" is extracted with water, and evaporated with a slight excess
of sulphuric acid to render the silica insoluble. Treat with water, filter, and
evaporate the filtrate until a crust is formed. Potash alum crystallises out.
The liquor is poured off into a warm strong solution of ammonium
carbonate. Ferric hydrate and alumina will be precipitated. They are filtered
off, re-dissolved, and again precipitated in ammonic carbonate solution; the
combined filtrates are boiled for some time, and acidified slightly with
hydrochloric acid. The carbon dioxide is boiled off, and the beryllia is then
precipitated as hydrate with ammonia. The hydrate is washed with hot
water, dried, ignited, and weighed as beryllia, BeO.
Page 403
Beryllia has a specific gravity of 3.08. It is white, infusible, and insoluble in
water. After ignition, it is insoluble in acids, except sulphuric, but is
rendered soluble by fusion with alkalies.
Beryllia, in a solution of carbonate of ammonia, is precipitated as carbonate
on boiling in proportion as the carbonate of ammonia is volatilised. The
hydrate is dissolved by a boiling solution of ammonic chloride, ammonia
being evolved.
THE ALKALINE EARTHS.
LIME.
Lime is an oxide of calcium, CaO. It occurs abundantly in nature, but only
in a state of combination. The carbonate (CaCO3), found as limestone,
chalk, and other rocks, and as the minerals calcite and arragonite, is the
most commonly occurring compound. The hydrated sulphate, gypsum
(CaSO4.2H2O), is common, and is used in making "plaster of Paris."
Anhydrite (CaSO4) also occurs in rock masses, and is often associated with
rock salt. Phosphate of lime, in the forms of apatite, phosphorite, coprolite,
&c., is largely mined. Lime is a component of most natural silicates.
Calcium also occurs, combined with fluorine, in the mineral fluor (CaF2). In
most of these the acid is the important part of the mineral; it is only the
carbonate which is used as a source of lime.
Lime, in addition to its use in mortars and cements, is valuable as a flux in
metallurgical operations, and as a base in chemical work on a large scale. A
mixture of lime and magnesia is used in the manufacture of basic fire-
bricks.
Carbonate of lime on ignition, especially when in contact with reducing
substances, loses carbonic acid, and becomes lime. This is known as
"quicklime"; on treatment with water it becomes hot, expands, and falls to a
powder of "slaked lime" or calcium hydrate (CaH2O2). The hydrate is
slightly soluble in water (0.1368 gram in 100 c.c.), forming an alkaline
solution known as lime-water. Calcium hydrate is more generally used
suspended in water as "milk of lime."
water. After ignition, it is insoluble in acids, except sulphuric, but is
rendered soluble by fusion with alkalies.
Beryllia, in a solution of carbonate of ammonia, is precipitated as carbonate
on boiling in proportion as the carbonate of ammonia is volatilised. The
hydrate is dissolved by a boiling solution of ammonic chloride, ammonia
being evolved.
THE ALKALINE EARTHS.
LIME.
Lime is an oxide of calcium, CaO. It occurs abundantly in nature, but only
in a state of combination. The carbonate (CaCO3), found as limestone,
chalk, and other rocks, and as the minerals calcite and arragonite, is the
most commonly occurring compound. The hydrated sulphate, gypsum
(CaSO4.2H2O), is common, and is used in making "plaster of Paris."
Anhydrite (CaSO4) also occurs in rock masses, and is often associated with
rock salt. Phosphate of lime, in the forms of apatite, phosphorite, coprolite,
&c., is largely mined. Lime is a component of most natural silicates.
Calcium also occurs, combined with fluorine, in the mineral fluor (CaF2). In
most of these the acid is the important part of the mineral; it is only the
carbonate which is used as a source of lime.
Lime, in addition to its use in mortars and cements, is valuable as a flux in
metallurgical operations, and as a base in chemical work on a large scale. A
mixture of lime and magnesia is used in the manufacture of basic fire-
bricks.
Carbonate of lime on ignition, especially when in contact with reducing
substances, loses carbonic acid, and becomes lime. This is known as
"quicklime"; on treatment with water it becomes hot, expands, and falls to a
powder of "slaked lime" or calcium hydrate (CaH2O2). The hydrate is
slightly soluble in water (0.1368 gram in 100 c.c.), forming an alkaline
solution known as lime-water. Calcium hydrate is more generally used
suspended in water as "milk of lime."
Page 404
As a flux it is used either as limestone or as quicklime. Silica forms with
lime a compound, calcium silicate, which is not very fusible; but when
alumina and other oxides are present, as in clays and in most rocky
substances, the addition of lime gives a very fusible slag.
Detection.—Calcium is detected by the reddish colour which its salts
impart to the flame. It is best to moisten with hydrochloric acid (or, in the
case of some silicates, to treat with ammonium fluoride) before bringing the
substance into the flame. When seen through a spectroscope, it shows a
large number of lines, of which a green and an orange are most intense and
characteristic. Calcium is detected in solution (after removal of the metals
by treatment with sulphuretted hydrogen and ammonium sulphide) by
boiling with ammonium oxalate and ammonia. The lime is completely
thrown down as a white precipitate. Lime is distinguished from the other
alkaline earths by forming a sulphate insoluble in dilute alcohol, but
completely soluble in a boiling solution of ammonium sulphate.
Lime compounds are for the most part soluble in water or in dilute
hydrochloric acid. Calcium fluoride must be first converted into sulphate by
evaporation in a platinum dish with sulphuric acid. Insoluble silicates are
opened up by fusion with "fusion mixture," as described under Silica.
Separation.—The separation of lime is effected by evaporating with
hydrochloric acid, to separate silica; and by treating with sulphuretted
hydrogen, to remove the second group of metals. If the substance contains
much iron, the solution is next oxidised by boiling with a little nitric acid;
and the iron, alumina, &c., are removed as basic acetates. The filtrate is
treated with ammonia and sulphuretted hydrogen, and allowed to settle. The
filtrate from this is heated to boiling, treated with a solution of ammonium
oxalate in excess, boiled for five or ten minutes, allowed to settle for half an
hour, and filtered. The precipitate contains all the lime as calcium oxalate.
GRAVIMETRIC DETERMINATION.
The precipitate of calcium oxalate is washed with hot water, dried,
transferred to a weighed platinum crucible, and ignited at a temperature not
above incipient redness. This ignition converts the oxalate into carbonate,
with evolution of carbonic oxide, which burns at the mouth of the crucible
lime a compound, calcium silicate, which is not very fusible; but when
alumina and other oxides are present, as in clays and in most rocky
substances, the addition of lime gives a very fusible slag.
Detection.—Calcium is detected by the reddish colour which its salts
impart to the flame. It is best to moisten with hydrochloric acid (or, in the
case of some silicates, to treat with ammonium fluoride) before bringing the
substance into the flame. When seen through a spectroscope, it shows a
large number of lines, of which a green and an orange are most intense and
characteristic. Calcium is detected in solution (after removal of the metals
by treatment with sulphuretted hydrogen and ammonium sulphide) by
boiling with ammonium oxalate and ammonia. The lime is completely
thrown down as a white precipitate. Lime is distinguished from the other
alkaline earths by forming a sulphate insoluble in dilute alcohol, but
completely soluble in a boiling solution of ammonium sulphate.
Lime compounds are for the most part soluble in water or in dilute
hydrochloric acid. Calcium fluoride must be first converted into sulphate by
evaporation in a platinum dish with sulphuric acid. Insoluble silicates are
opened up by fusion with "fusion mixture," as described under Silica.
Separation.—The separation of lime is effected by evaporating with
hydrochloric acid, to separate silica; and by treating with sulphuretted
hydrogen, to remove the second group of metals. If the substance contains
much iron, the solution is next oxidised by boiling with a little nitric acid;
and the iron, alumina, &c., are removed as basic acetates. The filtrate is
treated with ammonia and sulphuretted hydrogen, and allowed to settle. The
filtrate from this is heated to boiling, treated with a solution of ammonium
oxalate in excess, boiled for five or ten minutes, allowed to settle for half an
hour, and filtered. The precipitate contains all the lime as calcium oxalate.
GRAVIMETRIC DETERMINATION.
The precipitate of calcium oxalate is washed with hot water, dried,
transferred to a weighed platinum crucible, and ignited at a temperature not
above incipient redness. This ignition converts the oxalate into carbonate,
with evolution of carbonic oxide, which burns at the mouth of the crucible
Page 405
with a blue flame.[92] Generally a small quantity of the carbonate is at the
same time converted into lime. To reconvert it into carbonate, moisten with
a few drops of ammonic carbonate solution, and dry in a water-oven. Heat
gently over a Bunsen burner, cool, and weigh. The substance is calcium
carbonate (CaCO3), and contains 56 per cent. of lime (CaO). It is a white
powder, and should show no alkaline reaction with moistened litmus-paper.
Where the precipitate is small, it is better to ignite strongly over the
blowpipe, and weigh directly as lime. With larger quantities, and when
many determinations have to be made, it is easier to make the determination
volumetrically.
VOLUMETRIC METHODS.
These are carried out either by dissolving the oxalate at once in dilute
sulphuric acid, and titrating with permanganate of potassium solution; or by
calcining it to a mixture of lime and carbonate, and determining its
neutralising power with the standard solutions of acid and alkali.
Titration with Permanganate of Potassium Solution.—This solution is
made by dissolving 5.643 grams of the salt in water, and by diluting to 1
litre; 100 c.c. are equivalent to 0.5 gram of lime. The solution is
standardised by titrating a quantity of oxalic acid about equivalent to the
lime present in the assay; 0.5 gram of lime is equivalent to 1.125 gram of
crystallised oxalic acid. The standardising may be done with iron. The
standard found for iron multiplied by 0.5 gives that for lime.
The process is as follows:—The calcium oxalate (having been precipitated
and washed, as in the gravimetric process) is washed through the funnel
into a flask with hot dilute sulphuric acid, boiled till dissolved, diluted to
200 c.c. with water, and heated to about 80° C. The standard solution of
"permanganate" is then run in, (not too quickly, and with constant shaking)
until a permanent pink tinge is produced. The c.c. used multiplied by the
standard, and divided by the weight of the substance taken, will give the
percentage of lime.
Estimation of Lime by Alkalimetry.—The methods of determining the
amount of an alkali or base by means of a standard acid solution, or,
same time converted into lime. To reconvert it into carbonate, moisten with
a few drops of ammonic carbonate solution, and dry in a water-oven. Heat
gently over a Bunsen burner, cool, and weigh. The substance is calcium
carbonate (CaCO3), and contains 56 per cent. of lime (CaO). It is a white
powder, and should show no alkaline reaction with moistened litmus-paper.
Where the precipitate is small, it is better to ignite strongly over the
blowpipe, and weigh directly as lime. With larger quantities, and when
many determinations have to be made, it is easier to make the determination
volumetrically.
VOLUMETRIC METHODS.
These are carried out either by dissolving the oxalate at once in dilute
sulphuric acid, and titrating with permanganate of potassium solution; or by
calcining it to a mixture of lime and carbonate, and determining its
neutralising power with the standard solutions of acid and alkali.
Titration with Permanganate of Potassium Solution.—This solution is
made by dissolving 5.643 grams of the salt in water, and by diluting to 1
litre; 100 c.c. are equivalent to 0.5 gram of lime. The solution is
standardised by titrating a quantity of oxalic acid about equivalent to the
lime present in the assay; 0.5 gram of lime is equivalent to 1.125 gram of
crystallised oxalic acid. The standardising may be done with iron. The
standard found for iron multiplied by 0.5 gives that for lime.
The process is as follows:—The calcium oxalate (having been precipitated
and washed, as in the gravimetric process) is washed through the funnel
into a flask with hot dilute sulphuric acid, boiled till dissolved, diluted to
200 c.c. with water, and heated to about 80° C. The standard solution of
"permanganate" is then run in, (not too quickly, and with constant shaking)
until a permanent pink tinge is produced. The c.c. used multiplied by the
standard, and divided by the weight of the substance taken, will give the
percentage of lime.
Estimation of Lime by Alkalimetry.—The methods of determining the
amount of an alkali or base by means of a standard acid solution, or,
Page 406
conversely, of determining an acid by means of a standard alkaline solution,
are so closely related that they are best considered under one head. The
same standard solution is applicable for many purposes, and, consequently,
it is convenient to make it of such strength that one litre of it shall equal an
equivalent in grams of any of the substances to be determined. Such
solutions are termed normal. For example, a solution of hydrochloric acid
(HCl = 36.5) containing 36.5 grams of real acid per litre, would be normal
and of equivalent strength to a solution containing either 17 grams of
ammonia (NH3 = 17) or 40 grams of sodic hydrate (NaHO = 40) per litre. It
will be seen in these cases that the normal solution contains the molecular
weight in grams per litre; and, if solutions of these strengths be made, it will
be found that they possess equal neutralising value.
If, now, a solution containing 98 grams of sulphuric acid (H2SO4 = 98) per
litre be made, it will be found to have twice the strength of the above
solution, that is, 100 c.c. of the soda would only require 50 c.c. of the acid
to neutralise it. The reason for this will be seen on inspecting the equations:
—
NaHO + HCl = NaCl + H2O.
2NaHO + H2SO4 = Na2SO4 + 2H2O.
Acids like sulphuric acid are termed bibasic, and their equivalent is only
half the molecular weight. Thus, a normal solution of sulphuric acid would
contain 49 grams (98/2) of real acid per litre. Similarly, lime and most of
the bases are bibasic, as may be seen from the following equations; hence
their equivalent will be half the molecular weight.
2HCl + CaO = CaCl2 + H2O.
2HCl + MgO = MgCl2 + H2O.
The standard normal solution of hydrochloric acid is made by diluting 100
c.c. of the strong acid to one litre with water. This will be approximately
normal. In order to determine its exact strength, weigh up 3 grams of
recently ignited pure sodium carbonate or of the ignited bicarbonate.
Transfer to a flask and dissolve in 200 c.c. of water; when dissolved, cool,
tint faintly yellow with a few drops of a solution of methyl orange, and run
in the standard "acid " from a burette till the yellow changes to a pink. Read
are so closely related that they are best considered under one head. The
same standard solution is applicable for many purposes, and, consequently,
it is convenient to make it of such strength that one litre of it shall equal an
equivalent in grams of any of the substances to be determined. Such
solutions are termed normal. For example, a solution of hydrochloric acid
(HCl = 36.5) containing 36.5 grams of real acid per litre, would be normal
and of equivalent strength to a solution containing either 17 grams of
ammonia (NH3 = 17) or 40 grams of sodic hydrate (NaHO = 40) per litre. It
will be seen in these cases that the normal solution contains the molecular
weight in grams per litre; and, if solutions of these strengths be made, it will
be found that they possess equal neutralising value.
If, now, a solution containing 98 grams of sulphuric acid (H2SO4 = 98) per
litre be made, it will be found to have twice the strength of the above
solution, that is, 100 c.c. of the soda would only require 50 c.c. of the acid
to neutralise it. The reason for this will be seen on inspecting the equations:
—
NaHO + HCl = NaCl + H2O.
2NaHO + H2SO4 = Na2SO4 + 2H2O.
Acids like sulphuric acid are termed bibasic, and their equivalent is only
half the molecular weight. Thus, a normal solution of sulphuric acid would
contain 49 grams (98/2) of real acid per litre. Similarly, lime and most of
the bases are bibasic, as may be seen from the following equations; hence
their equivalent will be half the molecular weight.
2HCl + CaO = CaCl2 + H2O.
2HCl + MgO = MgCl2 + H2O.
The standard normal solution of hydrochloric acid is made by diluting 100
c.c. of the strong acid to one litre with water. This will be approximately
normal. In order to determine its exact strength, weigh up 3 grams of
recently ignited pure sodium carbonate or of the ignited bicarbonate.
Transfer to a flask and dissolve in 200 c.c. of water; when dissolved, cool,
tint faintly yellow with a few drops of a solution of methyl orange, and run
in the standard "acid " from a burette till the yellow changes to a pink. Read
Page 407
off the number of c.c. used, and calculate to how much sodium carbonate
100 c.c. of the "acid" are equivalent. If the "acid" is strictly normal, this will
be 5.3 grams. It will probably be equivalent to more than this. Now
calculate how much strictly normal "acid" would be equivalent to the
standard found. For example: suppose the standard found is 5.5 gram of
sodium carbonate, then—
5.3 : 5.5 :: 100 : x
(where x is the quantity of normal "acid" required).
x = 103.8 c.c.
To get the "acid" of normal strength, we should then add 3.8 c.c. of water to
each 100 c.c. of the standard solution remaining. Suppose there were left
930 c.c. of the approximate "acid," 35.3 c.c. of water must be added and
mixed. It should then be checked by another titration with pure sodium
carbonate.
The standard solution of semi-normal "alkali." The best alkali for general
purposes is ammonia, but, since it is volatile (especially in strong
solutions), it is best to make it of half the usual strength, or semi-normal.
One litre of this will contain 8.5 grams of ammonia (NH3), and 100 c.c. of it
will just neutralise 50 c.c. of the normal "acid." Take 100 c.c. of dilute
ammonia and dilute with water to one litre. Run into a flask 50 c.c. of the
standard "acid," tint with methyl orange, and run in from a burette the
solution of ammonia till neutralised. Less than 100 c.c. will probably be
used. Suppose 95 c.c. were required, there should have been 100, hence
there is a deficiency of five. Then, for each 95 c.c. of standard "ammonia"
left, add 5 c.c. of water, and mix well. 100 c.c. will now be equivalent to 50
c.c. of the "acid."
As an example of the application of this method, we may take the
determination of lime in limestone, marble, and similar substances.
Determination of Lime in Limestone.—Weigh up 1 gram of the dried
sample, and dissolve in 25 c.c. of normal acid, cool, dilute to 100 c.c., and
titrate with the semi-normal solution of alkali (using methyl-orange as an
indicator). Divide the c.c. of alkali used by 2, subtract from 25, and
multiply by 0.028 to find the weight of lime. This method is not applicable
100 c.c. of the "acid" are equivalent. If the "acid" is strictly normal, this will
be 5.3 grams. It will probably be equivalent to more than this. Now
calculate how much strictly normal "acid" would be equivalent to the
standard found. For example: suppose the standard found is 5.5 gram of
sodium carbonate, then—
5.3 : 5.5 :: 100 : x
(where x is the quantity of normal "acid" required).
x = 103.8 c.c.
To get the "acid" of normal strength, we should then add 3.8 c.c. of water to
each 100 c.c. of the standard solution remaining. Suppose there were left
930 c.c. of the approximate "acid," 35.3 c.c. of water must be added and
mixed. It should then be checked by another titration with pure sodium
carbonate.
The standard solution of semi-normal "alkali." The best alkali for general
purposes is ammonia, but, since it is volatile (especially in strong
solutions), it is best to make it of half the usual strength, or semi-normal.
One litre of this will contain 8.5 grams of ammonia (NH3), and 100 c.c. of it
will just neutralise 50 c.c. of the normal "acid." Take 100 c.c. of dilute
ammonia and dilute with water to one litre. Run into a flask 50 c.c. of the
standard "acid," tint with methyl orange, and run in from a burette the
solution of ammonia till neutralised. Less than 100 c.c. will probably be
used. Suppose 95 c.c. were required, there should have been 100, hence
there is a deficiency of five. Then, for each 95 c.c. of standard "ammonia"
left, add 5 c.c. of water, and mix well. 100 c.c. will now be equivalent to 50
c.c. of the "acid."
As an example of the application of this method, we may take the
determination of lime in limestone, marble, and similar substances.
Determination of Lime in Limestone.—Weigh up 1 gram of the dried
sample, and dissolve in 25 c.c. of normal acid, cool, dilute to 100 c.c., and
titrate with the semi-normal solution of alkali (using methyl-orange as an
indicator). Divide the c.c. of alkali used by 2, subtract from 25, and
multiply by 0.028 to find the weight of lime. This method is not applicable
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in the presence of other carbonates or oxides, unless the weight of these
substances be afterwards determined and due correction be made.
STRONTIA.
Strontia, the oxide of strontium (SrO), occurs in nature as sulphate, in the
mineral celestine (SrSO4), and as carbonate in strontianite (SrCO3). It is
found in small quantities in limestones, chalk, &c.
Strontia is used in sugar-refining, and for the preparation of coloured lights.
Detection.—It is detected by the crimson colour which its compounds
(when moistened with hydrochloric acid) impart to the flame. The spectrum
shows a large number of lines, of which a red, an orange, and a blue are
most characteristic.
It resembles lime in many of its compounds, but is distinguished by the
insolubility of its sulphate in a boiling solution of ammonium sulphate, and
by the insolubility of its nitrate in alcohol. From baryta, which it also
resembles, it is distinguished by not yielding an insoluble chromate in an
acetic acid solution, by the solubility of its chloride in alcohol, and by the
fact that its sulphate is converted into carbonate on boiling with a solution
formed of 3 parts of potassium carbonate and 1 of potassium sulphate.
It is got into solution in the same manner as lime. The sulphate should be
fused with "fusion mixture," extracted with water, and thoroughly washed.
The residue will contain the strontia as carbonate, which is readily soluble
in dilute hydrochloric or nitric acid.
Separation.—It is separated (after removal of the silica and metals, as
described under Lime) by adding ammonia and ammonia carbonate, and
allowing to stand for some hours in a warm place. In the absence of baryta
or lime it is filtered off, and weighed as strontium carbonate, which contains
70.17 per cent. of strontia. It is separated from baryta by dissolving in a
little hydrochloric acid, adding ammonia in excess, and then acidifying with
acetic acid, and precipitating the baryta with potassium bichromate, as
described under Baryta. The strontia is precipitated from the filtrate by
boiling for some time with a strong solution of ammonic sulphate and a
substances be afterwards determined and due correction be made.
STRONTIA.
Strontia, the oxide of strontium (SrO), occurs in nature as sulphate, in the
mineral celestine (SrSO4), and as carbonate in strontianite (SrCO3). It is
found in small quantities in limestones, chalk, &c.
Strontia is used in sugar-refining, and for the preparation of coloured lights.
Detection.—It is detected by the crimson colour which its compounds
(when moistened with hydrochloric acid) impart to the flame. The spectrum
shows a large number of lines, of which a red, an orange, and a blue are
most characteristic.
It resembles lime in many of its compounds, but is distinguished by the
insolubility of its sulphate in a boiling solution of ammonium sulphate, and
by the insolubility of its nitrate in alcohol. From baryta, which it also
resembles, it is distinguished by not yielding an insoluble chromate in an
acetic acid solution, by the solubility of its chloride in alcohol, and by the
fact that its sulphate is converted into carbonate on boiling with a solution
formed of 3 parts of potassium carbonate and 1 of potassium sulphate.
It is got into solution in the same manner as lime. The sulphate should be
fused with "fusion mixture," extracted with water, and thoroughly washed.
The residue will contain the strontia as carbonate, which is readily soluble
in dilute hydrochloric or nitric acid.
Separation.—It is separated (after removal of the silica and metals, as
described under Lime) by adding ammonia and ammonia carbonate, and
allowing to stand for some hours in a warm place. In the absence of baryta
or lime it is filtered off, and weighed as strontium carbonate, which contains
70.17 per cent. of strontia. It is separated from baryta by dissolving in a
little hydrochloric acid, adding ammonia in excess, and then acidifying with
acetic acid, and precipitating the baryta with potassium bichromate, as
described under Baryta. The strontia is precipitated from the filtrate by
boiling for some time with a strong solution of ammonic sulphate and a
Page 409
little ammonia. Fifty parts of ammonic sulphate are required for each part of
strontia or lime present. The precipitate is filtered off, and washed first with
a solution of ammonic sulphate, and then with alcohol. It is dried, ignited
and weighed as strontium sulphate.
GRAVIMETRIC DETERMINATION.
The determination of strontia in pure solutions is best made by adding
sulphuric acid in excess and alcohol in volume equal to that of the solution.
Allow to stand overnight, filter, wash with dilute alcohol, dry, ignite at a red
heat, and weigh as sulphate (SrSO4). This contains 56.4 per cent. of strontia
(SrO); or 47.7 per cent. of strontium.
BARYTA.
Baryta, oxide of barium (BaO), commonly occurs in combination with
sulphuric oxide in the mineral barytes or heavy spar (BaSO4), and in
combination with carbon dioxide in witherite (BaCO3). These minerals are
not unfrequently found in large quantity (associated with galena and other
metallic sulphides) in lodes. Small isolated crystals of these are frequently
found in mining districts. Barium is a constituent of certain mineral waters.
The minerals are recognised by their high specific gravity and their
crystalline form.
Compounds of barium are often used by the assayer, more especially the
chloride and hydrate. The salts are, with the exception of the sulphate,
generally soluble in water or hydrochloric acid. In such solutions sulphuric
acid produces a white precipitate of baric sulphate, which is practically
insoluble in all acids.
The dioxide (BaO2) is used for the preparation of oxygen. On strong
ignition it gives up oxygen, and is converted into baryta (BaO), which, at a
lower temperature, takes up oxygen from the air, re-forming the dioxide.
Detection.—Barium is detected by the green colour its salts, especially the
chloride, give to the flame. This, viewed through the spectroscope, shows a
complicated spectrum, of which two lines in the green are most easily
strontia or lime present. The precipitate is filtered off, and washed first with
a solution of ammonic sulphate, and then with alcohol. It is dried, ignited
and weighed as strontium sulphate.
GRAVIMETRIC DETERMINATION.
The determination of strontia in pure solutions is best made by adding
sulphuric acid in excess and alcohol in volume equal to that of the solution.
Allow to stand overnight, filter, wash with dilute alcohol, dry, ignite at a red
heat, and weigh as sulphate (SrSO4). This contains 56.4 per cent. of strontia
(SrO); or 47.7 per cent. of strontium.
BARYTA.
Baryta, oxide of barium (BaO), commonly occurs in combination with
sulphuric oxide in the mineral barytes or heavy spar (BaSO4), and in
combination with carbon dioxide in witherite (BaCO3). These minerals are
not unfrequently found in large quantity (associated with galena and other
metallic sulphides) in lodes. Small isolated crystals of these are frequently
found in mining districts. Barium is a constituent of certain mineral waters.
The minerals are recognised by their high specific gravity and their
crystalline form.
Compounds of barium are often used by the assayer, more especially the
chloride and hydrate. The salts are, with the exception of the sulphate,
generally soluble in water or hydrochloric acid. In such solutions sulphuric
acid produces a white precipitate of baric sulphate, which is practically
insoluble in all acids.
The dioxide (BaO2) is used for the preparation of oxygen. On strong
ignition it gives up oxygen, and is converted into baryta (BaO), which, at a
lower temperature, takes up oxygen from the air, re-forming the dioxide.
Detection.—Barium is detected by the green colour its salts, especially the
chloride, give to the flame. This, viewed through the spectroscope, shows a
complicated spectrum, of which two lines in the green are most easily
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recognised and characteristic. The salts of barium give no precipitate with
sulphuretted hydrogen in either acid or alkaline solution, but with sulphuric
acid they at once give a precipitate, which is insoluble in acetate of soda. In
solutions rendered faintly acid with acetic acid, they give a yellow
precipitate with bichromate of potash. These reactions are characteristic of
barium.
Baryta is got into solution in the manner described under Lime; but in the
case of the sulphate the substance is fused with three or four times its
weight of "fusion mixture." The "melt" is extracted with water, washed, and
the residue dissolved in dilute hydrochloric acid.
Separation.—The separation is thus effected:—The solution in
hydrochloric acid is evaporated to dryness, re-dissolved in hot dilute
hydrochloric acid, and sulphuric acid is added to the solution till no further
precipitate is formed. The precipitate is filtered off, and digested with a
solution of ammonium acetate or of sodium hyposulphite at 50° or 60° C. to
dissolve out any lead sulphate. The residue is filtered off, washed, dried,
and ignited. The ignited substance is mixed with four or five times its
weight of "fusion mixture," and fused in a platinum-dish over the blowpipe
for a few minutes. When cold, it is extracted with cold water, filtered, and
washed. The residue is dissolved in dilute hydrochloric acid, and (if
necessary) filtered. The solution contains the barium as baric chloride
mixed, perhaps, with salts of strontium or lime. To separate these, ammonia
is added till the solution is alkaline, and then acetic acid in slight excess.
Chromate of baryta is then thrown down, by the addition of bichromate of
potash, as a yellow precipitate. It is allowed to settle, filtered and washed
with a solution of acetate or of nitrate of ammonia. It is dried, ignited
gently, and weighed. It is BaCrO4, and contains 60.47 per cent. of baryta.
GRAVIMETRIC DETERMINATION.
The gravimetric determination of baryta, when lime and strontia are absent,
is as follows:—The solution, if it contains much free acid, is nearly
neutralised with ammonia, and then diluted to 100 or 200 c.c. It is heated to
boiling, and dilute sulphuric acid is added till no further precipitation takes
place. The precipitate is allowed to settle for a few minutes, decanted
sulphuretted hydrogen in either acid or alkaline solution, but with sulphuric
acid they at once give a precipitate, which is insoluble in acetate of soda. In
solutions rendered faintly acid with acetic acid, they give a yellow
precipitate with bichromate of potash. These reactions are characteristic of
barium.
Baryta is got into solution in the manner described under Lime; but in the
case of the sulphate the substance is fused with three or four times its
weight of "fusion mixture." The "melt" is extracted with water, washed, and
the residue dissolved in dilute hydrochloric acid.
Separation.—The separation is thus effected:—The solution in
hydrochloric acid is evaporated to dryness, re-dissolved in hot dilute
hydrochloric acid, and sulphuric acid is added to the solution till no further
precipitate is formed. The precipitate is filtered off, and digested with a
solution of ammonium acetate or of sodium hyposulphite at 50° or 60° C. to
dissolve out any lead sulphate. The residue is filtered off, washed, dried,
and ignited. The ignited substance is mixed with four or five times its
weight of "fusion mixture," and fused in a platinum-dish over the blowpipe
for a few minutes. When cold, it is extracted with cold water, filtered, and
washed. The residue is dissolved in dilute hydrochloric acid, and (if
necessary) filtered. The solution contains the barium as baric chloride
mixed, perhaps, with salts of strontium or lime. To separate these, ammonia
is added till the solution is alkaline, and then acetic acid in slight excess.
Chromate of baryta is then thrown down, by the addition of bichromate of
potash, as a yellow precipitate. It is allowed to settle, filtered and washed
with a solution of acetate or of nitrate of ammonia. It is dried, ignited
gently, and weighed. It is BaCrO4, and contains 60.47 per cent. of baryta.
GRAVIMETRIC DETERMINATION.
The gravimetric determination of baryta, when lime and strontia are absent,
is as follows:—The solution, if it contains much free acid, is nearly
neutralised with ammonia, and then diluted to 100 or 200 c.c. It is heated to
boiling, and dilute sulphuric acid is added till no further precipitation takes
place. The precipitate is allowed to settle for a few minutes, decanted
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through a filter, and washed with hot water; and, afterwards, dried,
transferred to a porcelain crucible, and strongly ignited in the muffle or over
the blowpipe for a few minutes. It is then cooled, and weighed as sulphate
of baryta (BaSO4). It contains 65.67 per cent. of baryta (BaO).
In determining the baryta in minerals which are soluble in acid, it is
precipitated direct from the hydrochloric acid solution (nearly neutralised
with ammonia) by means of sulphuric acid. The precipitated baric sulphate
is digested with a solution of ammonic acetate; and filtered, washed,
ignited, and weighed.
VOLUMETRIC DETERMINATION.
The principle and mode of working of this is the same as that given under
the Sulphur Assay; but using a standard solution of sulphuric acid instead of
one of barium chloride. The standard solution of sulphuric acid is made to
contain 32.02 grams of sulphuric acid (H2SO4), or an equivalent of a
soluble alkaline sulphate, per litre. 100 c.c. will be equal to 5 grams of
baryta.
Five grams of the substance are taken, and the baryta they contain
converted into carbonate (if necessary). The carbonate is dissolved in dilute
hydrochloric acid. Ten grams of sodium acetate are added, and the solution,
diluted to 500 c.c., is boiled, and titrated in the manner described.
Lead salts must be absent in the titration, and so must strontia and lime.
Ferrous salts should be peroxidised by means of permanganate or chlorate
of potash. Other salts do not interfere.
MAGNESIA.
Magnesia, the oxide of magnesium (MgO) occurs in nature in the rare
mineral periclase (MgO); and hydrated, as brucite (MgH2O2). As carbonate
it occurs in large quantity as magnesite (MgCO3), which is the chief source
of magnesia. Mixed with carbonate of lime, it forms magnesian limestone
and dolomite. It is present in larger or smaller quantity in most silicates; and
the minerals, serpentine, talc, steatite and meerschaum are essentially
transferred to a porcelain crucible, and strongly ignited in the muffle or over
the blowpipe for a few minutes. It is then cooled, and weighed as sulphate
of baryta (BaSO4). It contains 65.67 per cent. of baryta (BaO).
In determining the baryta in minerals which are soluble in acid, it is
precipitated direct from the hydrochloric acid solution (nearly neutralised
with ammonia) by means of sulphuric acid. The precipitated baric sulphate
is digested with a solution of ammonic acetate; and filtered, washed,
ignited, and weighed.
VOLUMETRIC DETERMINATION.
The principle and mode of working of this is the same as that given under
the Sulphur Assay; but using a standard solution of sulphuric acid instead of
one of barium chloride. The standard solution of sulphuric acid is made to
contain 32.02 grams of sulphuric acid (H2SO4), or an equivalent of a
soluble alkaline sulphate, per litre. 100 c.c. will be equal to 5 grams of
baryta.
Five grams of the substance are taken, and the baryta they contain
converted into carbonate (if necessary). The carbonate is dissolved in dilute
hydrochloric acid. Ten grams of sodium acetate are added, and the solution,
diluted to 500 c.c., is boiled, and titrated in the manner described.
Lead salts must be absent in the titration, and so must strontia and lime.
Ferrous salts should be peroxidised by means of permanganate or chlorate
of potash. Other salts do not interfere.
MAGNESIA.
Magnesia, the oxide of magnesium (MgO) occurs in nature in the rare
mineral periclase (MgO); and hydrated, as brucite (MgH2O2). As carbonate
it occurs in large quantity as magnesite (MgCO3), which is the chief source
of magnesia. Mixed with carbonate of lime, it forms magnesian limestone
and dolomite. It is present in larger or smaller quantity in most silicates; and
the minerals, serpentine, talc, steatite and meerschaum are essentially
Page 412
hydrated silicates of magnesia. Soluble magnesian salts occur in many
natural waters; more especially the sulphate and the chloride. Kieserite
(MgSO4.H2O) occurs in quantity at Stassfurt, and is used in the
manufacture of Epsom salts.
Detection.—Magnesia is best detected in the wet way. Its compounds give
no colour to the flame, and the only characteristic dry reaction is its
yielding a pink mass when ignited before the blowpipe (after treatment with
a solution of cobalt nitrate). In solution, it is recognised by giving no
precipitate with ammonia or ammonic carbonate in the presence of
ammonic chloride, and by giving a white crystalline precipitate on adding
sodium phosphate or arsenate to the ammoniacal solution.
Magnesia differs from the other alkaline earths by the solubility of its
sulphate in water.
Magnesia is dissolved by boiling with moderately strong acids; the
insoluble compounds are fused with "fusion mixture," and treated as
described under Silicates.
Separation.—It is separated by evaporating the acid solution to dryness to
render silica insoluble, and by taking up with dilute hydrochloric acid. The
solution is freed from the second group of metals by means of sulphuretted
hydrogen, and the iron, alumina, &c., are removed with ammonic chloride,
ammonia, and ammonic sulphide. The somewhat diluted filtrate is treated,
first, with ammonia, and then with carbonate of ammonia in slight excess. It
is allowed to stand for an hour in a warm place, and then filtered. The
magnesia is precipitated from the filtrate by the addition of an excess of
sodium phosphate and ammonia. It is allowed to stand overnight, filtered,
and washed with dilute ammonia. The precipitate contains the magnesia as
ammonic-magnesic phosphate.
In cases where it is not desirable to introduce sodium salts or phosphoric
acid into the assay solution, the following method is adopted. The solution
(freed from the other alkaline earths by ammonium carbonate) is evaporated
in a small porcelain dish with nitric acid. The residue (after removing the
ammonic salts by ignition) is taken up with a little water and a few crystals
of oxalic acid, transferred to a platinum dish, evaporated to dryness, and
ignited. The residue is extracted with small quantities of boiling water and
natural waters; more especially the sulphate and the chloride. Kieserite
(MgSO4.H2O) occurs in quantity at Stassfurt, and is used in the
manufacture of Epsom salts.
Detection.—Magnesia is best detected in the wet way. Its compounds give
no colour to the flame, and the only characteristic dry reaction is its
yielding a pink mass when ignited before the blowpipe (after treatment with
a solution of cobalt nitrate). In solution, it is recognised by giving no
precipitate with ammonia or ammonic carbonate in the presence of
ammonic chloride, and by giving a white crystalline precipitate on adding
sodium phosphate or arsenate to the ammoniacal solution.
Magnesia differs from the other alkaline earths by the solubility of its
sulphate in water.
Magnesia is dissolved by boiling with moderately strong acids; the
insoluble compounds are fused with "fusion mixture," and treated as
described under Silicates.
Separation.—It is separated by evaporating the acid solution to dryness to
render silica insoluble, and by taking up with dilute hydrochloric acid. The
solution is freed from the second group of metals by means of sulphuretted
hydrogen, and the iron, alumina, &c., are removed with ammonic chloride,
ammonia, and ammonic sulphide. The somewhat diluted filtrate is treated,
first, with ammonia, and then with carbonate of ammonia in slight excess. It
is allowed to stand for an hour in a warm place, and then filtered. The
magnesia is precipitated from the filtrate by the addition of an excess of
sodium phosphate and ammonia. It is allowed to stand overnight, filtered,
and washed with dilute ammonia. The precipitate contains the magnesia as
ammonic-magnesic phosphate.
In cases where it is not desirable to introduce sodium salts or phosphoric
acid into the assay solution, the following method is adopted. The solution
(freed from the other alkaline earths by ammonium carbonate) is evaporated
in a small porcelain dish with nitric acid. The residue (after removing the
ammonic salts by ignition) is taken up with a little water and a few crystals
of oxalic acid, transferred to a platinum dish, evaporated to dryness, and
ignited. The residue is extracted with small quantities of boiling water and
Page 413
filtered off; while the insoluble magnesia is washed. The filtrate contains
the alkalies. The residue is ignited, and weighed as magnesia. It is MgO.
GRAVIMETRIC DETERMINATION.
The solution containing the magnesia is mixed with chloride of ammonium
and ammonia in excess. If a precipitate should form, more ammonic
chloride is required. Add sodium phosphate solution in excess, stir and
allow to stand overnight. Filter and wash the precipitate with dilute
ammonia. Dry, transfer to a platinum or porcelain crucible, and ignite
(finally at intense redness); cool, and weigh. The substance is magnesic
pyrophosphate (Mg2P2O7), and contains 36.04 per cent. of magnesia.
VOLUMETRIC METHOD.
The magnesia having been precipitated as ammonic-magnesic phosphate,
which is the usual separation, its weight can be determined volumetrically
by the method of titration described under Phosphates.
The same standard solution of uranium acetate is used. Its standard for
magnesia is got by multiplying the standard for phosphoric oxide by
0.5493. For example, if one hundred c.c. are equivalent to 0.5 gram of
phosphoric oxide, they will be equivalent to (0.5 × .5493) 0.2746 gram of
magnesia. The method of working and the conditions of the titration are the
same as for the phosphate titration. The quantity of substance taken for
assay must not contain more than 0.1 or 0.2 gram of magnesia. After
precipitating as ammonic-magnesic phosphate with sodium phosphate, and
well washing with ammonia, it is dissolved in dilute hydrochloric acid,
neutralised with ammonia, and sodic acetate and acetic acid are added in the
usual quantity. The solution is boiled and titrated.
EXAMINATION OF A LIMESTONE.
Silica and Insoluble Silicates.—Take one gram of the dried sample and
dissolve it in 10 c.c. of dilute hydrochloric acid; filter; wash, dry, and ignite
the residue.
the alkalies. The residue is ignited, and weighed as magnesia. It is MgO.
GRAVIMETRIC DETERMINATION.
The solution containing the magnesia is mixed with chloride of ammonium
and ammonia in excess. If a precipitate should form, more ammonic
chloride is required. Add sodium phosphate solution in excess, stir and
allow to stand overnight. Filter and wash the precipitate with dilute
ammonia. Dry, transfer to a platinum or porcelain crucible, and ignite
(finally at intense redness); cool, and weigh. The substance is magnesic
pyrophosphate (Mg2P2O7), and contains 36.04 per cent. of magnesia.
VOLUMETRIC METHOD.
The magnesia having been precipitated as ammonic-magnesic phosphate,
which is the usual separation, its weight can be determined volumetrically
by the method of titration described under Phosphates.
The same standard solution of uranium acetate is used. Its standard for
magnesia is got by multiplying the standard for phosphoric oxide by
0.5493. For example, if one hundred c.c. are equivalent to 0.5 gram of
phosphoric oxide, they will be equivalent to (0.5 × .5493) 0.2746 gram of
magnesia. The method of working and the conditions of the titration are the
same as for the phosphate titration. The quantity of substance taken for
assay must not contain more than 0.1 or 0.2 gram of magnesia. After
precipitating as ammonic-magnesic phosphate with sodium phosphate, and
well washing with ammonia, it is dissolved in dilute hydrochloric acid,
neutralised with ammonia, and sodic acetate and acetic acid are added in the
usual quantity. The solution is boiled and titrated.
EXAMINATION OF A LIMESTONE.
Silica and Insoluble Silicates.—Take one gram of the dried sample and
dissolve it in 10 c.c. of dilute hydrochloric acid; filter; wash, dry, and ignite
the residue.
Page 414
Organic Matter.—If the residue insoluble in hydrochloric acid shows the
presence of organic matter, it must be collected on a weighed filter and
dried at 100°. On weighing, it gives the combined weights of organic and
insoluble matter. The latter is determined by igniting and weighing again.
The organic matter is calculated by difference.
Lime.—Where but little magnesia is present, this is determined by titration
with standard acid. Take one gram, and dissolve it in 25 c.c. of normal
hydrochloric acid. Tint with methyl-orange and titrate with semi-normal
ammonia. Divide the quantity of ammonia used by 2, deduct this from 25,
and multiply the remainder by 2.8. This gives the percentage of lime.
Where magnesia is present, the same method is adopted, and the magnesia
(which is separately determined) is afterwards deducted. The percentage of
magnesia found is multiplied by 1.4, and the result is deducted from the
apparent percentage of lime got by titrating.
Magnesia.—Dissolve 2 grams of the limestone in hydrochloric acid, and
separate the lime with ammonia and ammonium oxalate. The filtrate is
treated with sodium phosphate, and the magnesia is weighed as
pyrophosphate, or titrated with uranium acetate.
Iron.—Dissolve 2 grams in hydrochloric acid, reduce, and titrate with
standard permanganate of potassium solution. This gives the total iron. The
ferrous iron is determined by dissolving another 2 grams in hydrochloric
acid and at once titrating with the permanganate of potassium solution.
Manganese.—Dissolve 20 grams in hydrochloric acid, nearly neutralise
with soda, add sodium acetate, boil, and filter. To the filtrate add bromine;
boil, and determine the manganese in the precipitate. See page 300.
Phosphoric Oxide.—This is determined by dissolving the ferric acetate
precipitate from the manganese separation in hydrochloric acid, adding
ammonia in excess, and passing sulphuretted hydrogen. Filter and add to
the filtrate "magnesia mixture." The precipitate is collected, washed with
ammonia, ignited, and weighed as pyrophosphate.
THE ALKALIES.
presence of organic matter, it must be collected on a weighed filter and
dried at 100°. On weighing, it gives the combined weights of organic and
insoluble matter. The latter is determined by igniting and weighing again.
The organic matter is calculated by difference.
Lime.—Where but little magnesia is present, this is determined by titration
with standard acid. Take one gram, and dissolve it in 25 c.c. of normal
hydrochloric acid. Tint with methyl-orange and titrate with semi-normal
ammonia. Divide the quantity of ammonia used by 2, deduct this from 25,
and multiply the remainder by 2.8. This gives the percentage of lime.
Where magnesia is present, the same method is adopted, and the magnesia
(which is separately determined) is afterwards deducted. The percentage of
magnesia found is multiplied by 1.4, and the result is deducted from the
apparent percentage of lime got by titrating.
Magnesia.—Dissolve 2 grams of the limestone in hydrochloric acid, and
separate the lime with ammonia and ammonium oxalate. The filtrate is
treated with sodium phosphate, and the magnesia is weighed as
pyrophosphate, or titrated with uranium acetate.
Iron.—Dissolve 2 grams in hydrochloric acid, reduce, and titrate with
standard permanganate of potassium solution. This gives the total iron. The
ferrous iron is determined by dissolving another 2 grams in hydrochloric
acid and at once titrating with the permanganate of potassium solution.
Manganese.—Dissolve 20 grams in hydrochloric acid, nearly neutralise
with soda, add sodium acetate, boil, and filter. To the filtrate add bromine;
boil, and determine the manganese in the precipitate. See page 300.
Phosphoric Oxide.—This is determined by dissolving the ferric acetate
precipitate from the manganese separation in hydrochloric acid, adding
ammonia in excess, and passing sulphuretted hydrogen. Filter and add to
the filtrate "magnesia mixture." The precipitate is collected, washed with
ammonia, ignited, and weighed as pyrophosphate.
THE ALKALIES.
Page 415
The oxides of sodium, potassium, lithium, cæsium, and rubidium and
ammonia are grouped under this head. Of these cæsia and rubidia are rare,
and lithia comparatively so. They are easily distinguished by their spectra.
They are characterised by the solubility of almost all their salts in water,
and, consequently, are found in the solutions from which the earths and
oxides of the metals have been separated by the usual group re-agents.
The solution from which the other substances have been separated is
evaporated to dryness, and the product ignited to remove the ammonic salts
added for the purpose of separation. The residue contains the alkali metals
generally, as chlorides or sulphates. Before determining the quantities of the
particular alkali metals present, it is best to convert them altogether, either
into chloride or sulphate, and to take the weight of the mixed salts. It is
generally more convenient to weigh them as chlorides. They are converted
into this form, if none of the stronger acids are present, by simply
evaporating with an excess of hydrochloric acid. Nitrates are converted into
chlorides by this treatment. When sulphates or phosphates are present, the
substance is dissolved in a little water, and the sulphuric or phosphoric acid
precipitated with a slight excess of acetate of lead in the presence of
alcohol. The solution is filtered, and the excess of lead precipitated with
sulphuretted hydrogen. The filtrate from this is evaporated to dryness with
an excess of hydrochloric acid, and the residue, consisting of the mixed
chlorides, is gently ignited and weighed. In many cases (such as the
analysis of slags and of some natural silicates where the percentage of
alkalies is small) the percentage of soda and potash (which most commonly
occur) need not be separately determined. It is sufficient to report the
proportion of mixed alkalies; which is thus ascertained:—Dissolve the
ignited and weighed chlorides in 100 c.c. of distilled water, and titrate with
the standard solution of silver nitrate (using potassic chromate as indicator)
in the manner described under Chlorine. The c.c. of silver nitrate used gives
the weight in milligrams of the chlorine present. Multiply this by 0.775, and
deduct the product from the weight of the mixed chlorides. This will give
the combined weight of the alkalies (Na2O and K2O) present. For example,
0.0266 gram of mixed chlorides required on titrating 14.2 c.c. of silver
nitrate, which is equivalent to 0.0142 gram of chlorine. This multiplied by
0.775 gives 0.0110 to be deducted from the weight of the mixed chlorides.
ammonia are grouped under this head. Of these cæsia and rubidia are rare,
and lithia comparatively so. They are easily distinguished by their spectra.
They are characterised by the solubility of almost all their salts in water,
and, consequently, are found in the solutions from which the earths and
oxides of the metals have been separated by the usual group re-agents.
The solution from which the other substances have been separated is
evaporated to dryness, and the product ignited to remove the ammonic salts
added for the purpose of separation. The residue contains the alkali metals
generally, as chlorides or sulphates. Before determining the quantities of the
particular alkali metals present, it is best to convert them altogether, either
into chloride or sulphate, and to take the weight of the mixed salts. It is
generally more convenient to weigh them as chlorides. They are converted
into this form, if none of the stronger acids are present, by simply
evaporating with an excess of hydrochloric acid. Nitrates are converted into
chlorides by this treatment. When sulphates or phosphates are present, the
substance is dissolved in a little water, and the sulphuric or phosphoric acid
precipitated with a slight excess of acetate of lead in the presence of
alcohol. The solution is filtered, and the excess of lead precipitated with
sulphuretted hydrogen. The filtrate from this is evaporated to dryness with
an excess of hydrochloric acid, and the residue, consisting of the mixed
chlorides, is gently ignited and weighed. In many cases (such as the
analysis of slags and of some natural silicates where the percentage of
alkalies is small) the percentage of soda and potash (which most commonly
occur) need not be separately determined. It is sufficient to report the
proportion of mixed alkalies; which is thus ascertained:—Dissolve the
ignited and weighed chlorides in 100 c.c. of distilled water, and titrate with
the standard solution of silver nitrate (using potassic chromate as indicator)
in the manner described under Chlorine. The c.c. of silver nitrate used gives
the weight in milligrams of the chlorine present. Multiply this by 0.775, and
deduct the product from the weight of the mixed chlorides. This will give
the combined weight of the alkalies (Na2O and K2O) present. For example,
0.0266 gram of mixed chlorides required on titrating 14.2 c.c. of silver
nitrate, which is equivalent to 0.0142 gram of chlorine. This multiplied by
0.775 gives 0.0110 to be deducted from the weight of the mixed chlorides.
Page 416
Mixed chlorides 0.0266 gram
Deduction 0.0110 "
———
Mixed alkalies 0.0156 "
Assuming this to have been got from 1 gram of a rock, it would amount to
1.56 per cent. of "potash and soda."
The relative proportions of the potash and soda can be ascertained from the
same determination. Sodium and potassium chlorides have the following
composition:—
Sodium 39.38 Potassium 52.46
Chlorine 60.62 Chlorine 47.54
——— ———
100.00 100.00
The percentage of chlorine in the mixed chlorides is calculated. It
necessarily falls somewhere between 47.5 and 60.6 per cent., and
approaches the one or the other of these numbers as the proportion of the
sodium or potassium preponderates. Each per cent. of chlorine in excess of
47.5 represents 7.63 per cent. of sodium chloride in the mixed chlorides.
The percentage of potash and soda in the substance can be calculated in the
usual way. Sodium chloride multiplied by 0.5302 gives its equivalent of
soda (Na2O), and potassium chloride multiplied by 0.6317 gives its
equivalent of potash (K2O).
The weight of sodium chloride in the mixed chlorides is also calculated
thus:—Take the same example for illustration. Multiply the chlorine found
by 2.103. This gives—
(0.0142×2.103) = 0.02987.
From the product deduct the weight of the mixed chlorides found—
Product 0.02987
Mixed chlorides 0.02660
———
Deduction 0.0110 "
———
Mixed alkalies 0.0156 "
Assuming this to have been got from 1 gram of a rock, it would amount to
1.56 per cent. of "potash and soda."
The relative proportions of the potash and soda can be ascertained from the
same determination. Sodium and potassium chlorides have the following
composition:—
Sodium 39.38 Potassium 52.46
Chlorine 60.62 Chlorine 47.54
——— ———
100.00 100.00
The percentage of chlorine in the mixed chlorides is calculated. It
necessarily falls somewhere between 47.5 and 60.6 per cent., and
approaches the one or the other of these numbers as the proportion of the
sodium or potassium preponderates. Each per cent. of chlorine in excess of
47.5 represents 7.63 per cent. of sodium chloride in the mixed chlorides.
The percentage of potash and soda in the substance can be calculated in the
usual way. Sodium chloride multiplied by 0.5302 gives its equivalent of
soda (Na2O), and potassium chloride multiplied by 0.6317 gives its
equivalent of potash (K2O).
The weight of sodium chloride in the mixed chlorides is also calculated
thus:—Take the same example for illustration. Multiply the chlorine found
by 2.103. This gives—
(0.0142×2.103) = 0.02987.
From the product deduct the weight of the mixed chlorides found—
Product 0.02987
Mixed chlorides 0.02660
———
Page 417
Difference 0.00327
The difference multiplied by 3.6288 gives the weight of sodium chloride in
the mixture. In this case it equals 0.0118 gram. The potassium chloride is
indicated by the difference between this and the weight of the mixed
chlorides. It equals 0.0148 gram. We have now got—
Sodium chloride 0.0118 gram
Potassium chloride 0.0148 "
from 1 gram of the rock taken. Multiplying these by their factors we have
(Soda = 0.0118×0.5302; Potash 0.0148×0.6317)—
Soda = 0.625 per cent.
Potash = 0.935 "
Concentration of the Alkalies.—With the exception of magnesia, all the
other bases are separated from the alkalies in the ordinary course of work
without the addition of any re-agent which cannot be removed by simple
evaporation and ignition. Consequently, with substances soluble in acids,
successive treatment of the solution with sulphuretted hydrogen, ammonia,
ammonic sulphide, and ammonic carbonate, filtering, where necessary, will
yield a filtrate containing the whole of the alkalies with ammonic salts and,
perhaps, magnesia.
The filtrate is evaporated in a small porcelain dish, with the addition of
nitric acid towards the finish. It is carried to dryness and ignited. The
residue is taken up with a little water, treated with a few crystals of oxalic
acid, and again evaporated and ignited. The alkaline salts are extracted with
water, and filtered from the magnesia into a weighed platinum dish. The
solution is then evaporated with an excess of hydrochloric acid, ignited at a
low red heat, and weighed. The residue consists of the mixed alkaline
chlorides.
For substances (such as most silicates and similar bodies) not completely
decomposed by acids, Lawrence Smith's method is generally used. This is
as follows:—Take from 0.5 to 1 gram of the finely powdered mineral, and
mix, by rubbing in the mortar, with an equal weight of ammonium chloride.
The difference multiplied by 3.6288 gives the weight of sodium chloride in
the mixture. In this case it equals 0.0118 gram. The potassium chloride is
indicated by the difference between this and the weight of the mixed
chlorides. It equals 0.0148 gram. We have now got—
Sodium chloride 0.0118 gram
Potassium chloride 0.0148 "
from 1 gram of the rock taken. Multiplying these by their factors we have
(Soda = 0.0118×0.5302; Potash 0.0148×0.6317)—
Soda = 0.625 per cent.
Potash = 0.935 "
Concentration of the Alkalies.—With the exception of magnesia, all the
other bases are separated from the alkalies in the ordinary course of work
without the addition of any re-agent which cannot be removed by simple
evaporation and ignition. Consequently, with substances soluble in acids,
successive treatment of the solution with sulphuretted hydrogen, ammonia,
ammonic sulphide, and ammonic carbonate, filtering, where necessary, will
yield a filtrate containing the whole of the alkalies with ammonic salts and,
perhaps, magnesia.
The filtrate is evaporated in a small porcelain dish, with the addition of
nitric acid towards the finish. It is carried to dryness and ignited. The
residue is taken up with a little water, treated with a few crystals of oxalic
acid, and again evaporated and ignited. The alkaline salts are extracted with
water, and filtered from the magnesia into a weighed platinum dish. The
solution is then evaporated with an excess of hydrochloric acid, ignited at a
low red heat, and weighed. The residue consists of the mixed alkaline
chlorides.
For substances (such as most silicates and similar bodies) not completely
decomposed by acids, Lawrence Smith's method is generally used. This is
as follows:—Take from 0.5 to 1 gram of the finely powdered mineral, and
mix, by rubbing in the mortar, with an equal weight of ammonium chloride.
Page 418
Then mix with eight times as much pure calcium carbonate, using a part of
it to rinse out the mortar. Transfer to a platinum crucible, and heat gently
over a Bunsen burner until the ammonic chloride is decomposed (five or ten
minutes). Raise the heat to redness, and continue at this temperature for
about three quarters of an hour. The crucible must be kept covered. Cool,
and turn out the mass into a 4-inch evaporating dish; wash the crucible and
cover with distilled water, and add the washings to the dish; dilute to 60 or
80 c.c., and heat to boiling. Filter and wash. Add to the filtrate about 1.5
gram of ammonium carbonate; evaporate to about 40 c.c., and add a little
more ammonic carbonate and some ammonia. Filter into a weighed
platinum dish, and evaporate to dryness. Heat gently, to drive off the
ammonic chloride, and ignite to a little below redness. Cool and weigh. The
residue consists of the mixed alkaline chlorides.
Separation of the Alkali-Metals from each other.—Sodium and lithium
are separated from the other alkali-metals by taking advantage of the
solubility of their chlorides in the presence of platinic chloride; and from
one another by the formation of an almost insoluble lithic phosphate on
boiling with a solution of sodium phosphate in a slightly alkaline solution.
Cæsium, rubidium, and potassium yield precipitates with platinic chloride,
which are somewhat soluble, and must be precipitated from concentrated
solutions. Cæsium and rubidium are separated from potassium by fractional
precipitation with platinum chloride. Their platino-chlorides, being less
soluble than that of potassium, are precipitated first. One hundred parts of
boiling water dissolve 5.18 of the potassium platino-chloride, 0.634 of the
rubidium salt, and 0.377 of the corresponding cæsium compound. The
separation of lithium, cæsium, and rubidium is seldom called for, owing to
their rarity. The details of the separation of potassium from sodium are
described under Potassium. Ammonia compounds are sharply marked off
from the rest by their volatility, and it is always assumed that they have
been removed by ignition; if left in the solution, they would count as
potassium compounds. They will be considered under Ammonia.
SODIUM.
Sodium is the commonest of the alkali metals. It is found in nature chiefly
combined with chlorine as "common salt" (NaCl). This mineral is the
it to rinse out the mortar. Transfer to a platinum crucible, and heat gently
over a Bunsen burner until the ammonic chloride is decomposed (five or ten
minutes). Raise the heat to redness, and continue at this temperature for
about three quarters of an hour. The crucible must be kept covered. Cool,
and turn out the mass into a 4-inch evaporating dish; wash the crucible and
cover with distilled water, and add the washings to the dish; dilute to 60 or
80 c.c., and heat to boiling. Filter and wash. Add to the filtrate about 1.5
gram of ammonium carbonate; evaporate to about 40 c.c., and add a little
more ammonic carbonate and some ammonia. Filter into a weighed
platinum dish, and evaporate to dryness. Heat gently, to drive off the
ammonic chloride, and ignite to a little below redness. Cool and weigh. The
residue consists of the mixed alkaline chlorides.
Separation of the Alkali-Metals from each other.—Sodium and lithium
are separated from the other alkali-metals by taking advantage of the
solubility of their chlorides in the presence of platinic chloride; and from
one another by the formation of an almost insoluble lithic phosphate on
boiling with a solution of sodium phosphate in a slightly alkaline solution.
Cæsium, rubidium, and potassium yield precipitates with platinic chloride,
which are somewhat soluble, and must be precipitated from concentrated
solutions. Cæsium and rubidium are separated from potassium by fractional
precipitation with platinum chloride. Their platino-chlorides, being less
soluble than that of potassium, are precipitated first. One hundred parts of
boiling water dissolve 5.18 of the potassium platino-chloride, 0.634 of the
rubidium salt, and 0.377 of the corresponding cæsium compound. The
separation of lithium, cæsium, and rubidium is seldom called for, owing to
their rarity. The details of the separation of potassium from sodium are
described under Potassium. Ammonia compounds are sharply marked off
from the rest by their volatility, and it is always assumed that they have
been removed by ignition; if left in the solution, they would count as
potassium compounds. They will be considered under Ammonia.
SODIUM.
Sodium is the commonest of the alkali metals. It is found in nature chiefly
combined with chlorine as "common salt" (NaCl). This mineral is the
Page 419
source from which the various compounds of sodium in use are prepared.
Sodium occurs abundantly as nitrate (NaNO3) in Chili saltpetre, and as
silicate in various minerals, such as albite (or soda-felspar).
It occurs as fluoride in cryolite (Na3AlF6), and as carbonate in natron, &c.
Sulphates are also found. Sodium is very widely diffused, few substances
being free from it.
The detection of sodium is easy and certain, owing to the strong yellow
colour its salts impart to the flame; this, when viewed by the spectroscope,
shows a single yellow line.[93] The extreme delicacy of this test limits its
value, because of the wide diffusion of sodium salts. It is more satisfactory
to separate the chloride, which may be recognised by its taste, flame
coloration, fusibility, and negative action with reagents. The chloride
dissolved in a few drops of water gives with potassium metantimoniate, a
white precipitate of the corresponding sodium salt.
Sodium salts are dissolved out from most compounds on treatment with
water or dilute acids. Insoluble silicates are decomposed and the alkali
rendered soluble by Lawrence Smith's method, which has just been
described. The separation of the sodium from the mixed chlorides is
effected in the following way:—The chlorides are dissolved in a little water
and the potassium separated as platino-chloride. The soluble sodium
platino-chloride, with the excess of platinum, is boiled, mixed with
sulphuric acid, evaporated to dryness, and ignited. On extracting with water,
filtering, evaporating, and igniting, sodium sulphate is left, and is weighed
as such.
It is more usual, and quite as satisfactory, to calculate the weight of the
sodium chloride by difference from that of the mixed chlorides, by
subtracting that of the potassium chloride, which is separately determined.
For example, 1 gram of a rock gave—Mixed chlorides, 0.0266 gram, and
0.0486 gram of potassic platino-chloride. This last is equivalent to 0.0149
gram of potassium chloride.
Mixed chlorides found 0.0266
Deduct potassium chloride 0.0149
———
Sodium occurs abundantly as nitrate (NaNO3) in Chili saltpetre, and as
silicate in various minerals, such as albite (or soda-felspar).
It occurs as fluoride in cryolite (Na3AlF6), and as carbonate in natron, &c.
Sulphates are also found. Sodium is very widely diffused, few substances
being free from it.
The detection of sodium is easy and certain, owing to the strong yellow
colour its salts impart to the flame; this, when viewed by the spectroscope,
shows a single yellow line.[93] The extreme delicacy of this test limits its
value, because of the wide diffusion of sodium salts. It is more satisfactory
to separate the chloride, which may be recognised by its taste, flame
coloration, fusibility, and negative action with reagents. The chloride
dissolved in a few drops of water gives with potassium metantimoniate, a
white precipitate of the corresponding sodium salt.
Sodium salts are dissolved out from most compounds on treatment with
water or dilute acids. Insoluble silicates are decomposed and the alkali
rendered soluble by Lawrence Smith's method, which has just been
described. The separation of the sodium from the mixed chlorides is
effected in the following way:—The chlorides are dissolved in a little water
and the potassium separated as platino-chloride. The soluble sodium
platino-chloride, with the excess of platinum, is boiled, mixed with
sulphuric acid, evaporated to dryness, and ignited. On extracting with water,
filtering, evaporating, and igniting, sodium sulphate is left, and is weighed
as such.
It is more usual, and quite as satisfactory, to calculate the weight of the
sodium chloride by difference from that of the mixed chlorides, by
subtracting that of the potassium chloride, which is separately determined.
For example, 1 gram of a rock gave—Mixed chlorides, 0.0266 gram, and
0.0486 gram of potassic platino-chloride. This last is equivalent to 0.0149
gram of potassium chloride.
Mixed chlorides found 0.0266
Deduct potassium chloride 0.0149
———
Page 420
Leaves sodium chloride 0.0117
The weight of sodium chloride found, multiplied by 0.5302, gives the
weight of the soda (Na2O).
GRAVIMETRIC DETERMINATION.
The solution, which must contain no other metal than sodium, is evaporated
in a weighed platinum crucible or dish. Towards the finish an excess, not
too great, of sulphuric acid is added, and the evaporation is continued under
a loosely fitting cover. The residue is ignited over the blowpipe, a fragment
of ammonic carbonate being added towards the end, when fumes of
sulphuric acid cease to be evolved. This ensures the removal of the excess
of acid. The crucible is cooled in the desiccator, and weighed. The
substance is sulphate of soda (Na2SO4), and contains 43.66 per cent. of
soda (Na2O), or 32.38 per cent. of sodium (Na).
VOLUMETRIC METHODS.
There are various methods used for the different compounds of sodium.
There is no one method of general application. Thus with "common salt"
the chlorine is determined volumetrically; and the sodium, after deducting
for the other impurities, is estimated by difference.
With sodic carbonate and caustic soda, a given weight of the sample is
titrated with standard acid, and the equivalent of soda estimated from the
alkalinity of the solution.
With sodium sulphate, a modification of the same method is used. To a
solution of 3.55 grams of the salt contained in a half-litre flask, 250 c.c. of a
solution of baryta water is added. The volume is made up to 500 c.c. with
water. The solution is mixed and filtered. Half of the filtrate is measured
off, treated with a current of carbonic acid, and then boiled. It is transferred
to a half-litre flask, diluted to the mark, shaken up, and filtered. 250 c.c. of
the filtrate, representing a quarter of the sample taken, is then titrated with
standard acid. The standard acid is made by diluting 250 c.c. of the normal
acid to 1 litre. The c.c. of acid used multiplied by 2 gives the percentage. A
The weight of sodium chloride found, multiplied by 0.5302, gives the
weight of the soda (Na2O).
GRAVIMETRIC DETERMINATION.
The solution, which must contain no other metal than sodium, is evaporated
in a weighed platinum crucible or dish. Towards the finish an excess, not
too great, of sulphuric acid is added, and the evaporation is continued under
a loosely fitting cover. The residue is ignited over the blowpipe, a fragment
of ammonic carbonate being added towards the end, when fumes of
sulphuric acid cease to be evolved. This ensures the removal of the excess
of acid. The crucible is cooled in the desiccator, and weighed. The
substance is sulphate of soda (Na2SO4), and contains 43.66 per cent. of
soda (Na2O), or 32.38 per cent. of sodium (Na).
VOLUMETRIC METHODS.
There are various methods used for the different compounds of sodium.
There is no one method of general application. Thus with "common salt"
the chlorine is determined volumetrically; and the sodium, after deducting
for the other impurities, is estimated by difference.
With sodic carbonate and caustic soda, a given weight of the sample is
titrated with standard acid, and the equivalent of soda estimated from the
alkalinity of the solution.
With sodium sulphate, a modification of the same method is used. To a
solution of 3.55 grams of the salt contained in a half-litre flask, 250 c.c. of a
solution of baryta water is added. The volume is made up to 500 c.c. with
water. The solution is mixed and filtered. Half of the filtrate is measured
off, treated with a current of carbonic acid, and then boiled. It is transferred
to a half-litre flask, diluted to the mark, shaken up, and filtered. 250 c.c. of
the filtrate, representing a quarter of the sample taken, is then titrated with
standard acid. The standard acid is made by diluting 250 c.c. of the normal
acid to 1 litre. The c.c. of acid used multiplied by 2 gives the percentage. A
Page 421
correction must be made to counteract the effect of impurities in the baryta
as well as errors inherent in the process. This is small, and its amount is
determined by an experiment with 3.55 grams of pure sodium sulphate.
EXAMINATION OF COMMON SALT.
Moisture.—Powder and weigh up 10 grams of the sample into a platinum
dish. Dry in a water oven for an hour, and afterwards heat to bare redness
over a Bunsen burner. Cool, and weigh. The loss gives the water.
Chlorine.—Weigh up two separate lots of 1 gram each; dissolve in 100 c.c.
of water, and determine the chlorine by titrating with the standard silver
nitrate solution, using chromate of potash as indicator. See Chlorine.
Insoluble Matter.—Dissolve 10 grams of the salt in water with the help of
a little hydrochloric acid. Filter off the sediment, wash, ignite, and weigh.
This residue is chiefly sand. Dilute the nitrate to 500 c.c.
Lime.—Take 250 c.c. of the filtrate, render ammoniacal and add
ammonium oxalate; wash, dry, and ignite the precipitate. Weigh as lime
(CaO).
Magnesia.—To the filtrate from the lime add phosphate of soda. Allow to
stand overnight, filter, wash with dilute ammonia, dry, ignite, and weigh as
pyrophosphate.
Sulphuric Oxide.—To the remaining 250 c.c. of the filtrate from the
"insoluble," add an excess of barium chloride. Collect, wash, dry, ignite,
and weigh the barium sulphate.
Sodium.—It is estimated by difference.
The following may be taken as an example:—
Moisture 0.35
Insoluble matter 0.40
Lime 0.40
Magnesia 0.05
Sulphuric oxide 0.60
as well as errors inherent in the process. This is small, and its amount is
determined by an experiment with 3.55 grams of pure sodium sulphate.
EXAMINATION OF COMMON SALT.
Moisture.—Powder and weigh up 10 grams of the sample into a platinum
dish. Dry in a water oven for an hour, and afterwards heat to bare redness
over a Bunsen burner. Cool, and weigh. The loss gives the water.
Chlorine.—Weigh up two separate lots of 1 gram each; dissolve in 100 c.c.
of water, and determine the chlorine by titrating with the standard silver
nitrate solution, using chromate of potash as indicator. See Chlorine.
Insoluble Matter.—Dissolve 10 grams of the salt in water with the help of
a little hydrochloric acid. Filter off the sediment, wash, ignite, and weigh.
This residue is chiefly sand. Dilute the nitrate to 500 c.c.
Lime.—Take 250 c.c. of the filtrate, render ammoniacal and add
ammonium oxalate; wash, dry, and ignite the precipitate. Weigh as lime
(CaO).
Magnesia.—To the filtrate from the lime add phosphate of soda. Allow to
stand overnight, filter, wash with dilute ammonia, dry, ignite, and weigh as
pyrophosphate.
Sulphuric Oxide.—To the remaining 250 c.c. of the filtrate from the
"insoluble," add an excess of barium chloride. Collect, wash, dry, ignite,
and weigh the barium sulphate.
Sodium.—It is estimated by difference.
The following may be taken as an example:—
Moisture 0.35
Insoluble matter 0.40
Lime 0.40
Magnesia 0.05
Sulphuric oxide 0.60
Page 422
Chlorine 59.60
Sodium 38.60
———
100.00
POTASSIUM.
Potassium occurs in nature as chloride, in the mineral sylvine (KCl), and
more abundantly combined with magnesium chloride, in earnallite
(KCl.MgCl2.6H2O). It occurs as nitrate in nitre (KNO3), and as silicate in
many minerals, such as orthoclase (or potash-felspar) and muscovite (or
potash-mica).
Potassium compounds are detected by the characteristic violet colour they
impart to the flame. The presence of sodium salts masks this tint, but the
interference can be neutralised by viewing the flame through a piece of blue
glass. Viewed through the spectroscope, it shows a characteristic line in the
red and another in the violet. These, however, are not so easy to recognise
or obtain as the sodium one. Concentrated solutions of potassium salts give
a yellow crystalline precipitate with platinum chloride, and a white
crystalline one with the acid tartrate of soda. For these tests the solution is
best neutral. These tests are only applicable in the absence of compounds
other than those of potassium and sodium.
GRAVIMETRIC DETERMINATION.
This process serves for its separation from sodium. Take 1 gram of the
sample and dissolve it in an evaporating dish with 50 c.c. of water. Acidify
with hydrochloric acid in quantity sufficient (if the metals are present as
chlorides) to make it acid, or, if other acids are present, in at least such
quantity as will provide the equivalent of chlorine. Add 3 grams of
platinum, in solution as platinum chloride, and evaporate on a water-bath to
a stiff paste, but not to dryness. Moisten with a few drops of platinic
chloride solution without breaking up the paste by stirring. Cover with 20
c.c. of strong alcohol, and wash the crystals as much as possible by rotating
the dish. Allow to settle for a few moments, and decant through a filter.
Sodium 38.60
———
100.00
POTASSIUM.
Potassium occurs in nature as chloride, in the mineral sylvine (KCl), and
more abundantly combined with magnesium chloride, in earnallite
(KCl.MgCl2.6H2O). It occurs as nitrate in nitre (KNO3), and as silicate in
many minerals, such as orthoclase (or potash-felspar) and muscovite (or
potash-mica).
Potassium compounds are detected by the characteristic violet colour they
impart to the flame. The presence of sodium salts masks this tint, but the
interference can be neutralised by viewing the flame through a piece of blue
glass. Viewed through the spectroscope, it shows a characteristic line in the
red and another in the violet. These, however, are not so easy to recognise
or obtain as the sodium one. Concentrated solutions of potassium salts give
a yellow crystalline precipitate with platinum chloride, and a white
crystalline one with the acid tartrate of soda. For these tests the solution is
best neutral. These tests are only applicable in the absence of compounds
other than those of potassium and sodium.
GRAVIMETRIC DETERMINATION.
This process serves for its separation from sodium. Take 1 gram of the
sample and dissolve it in an evaporating dish with 50 c.c. of water. Acidify
with hydrochloric acid in quantity sufficient (if the metals are present as
chlorides) to make it acid, or, if other acids are present, in at least such
quantity as will provide the equivalent of chlorine. Add 3 grams of
platinum, in solution as platinum chloride, and evaporate on a water-bath to
a stiff paste, but not to dryness. Moisten with a few drops of platinic
chloride solution without breaking up the paste by stirring. Cover with 20
c.c. of strong alcohol, and wash the crystals as much as possible by rotating
the dish. Allow to settle for a few moments, and decant through a filter.
Page 423
Wash in the same way two or three times until the colour of the filtrate
shows that the excess of the platinum chloride used is removed. Wash the
precipitate on to the filter with a jet of alcohol from the wash-bottle; clean
the filter-paper, using as little alcohol as possible. Dry in the water-oven for
an hour. Brush the precipitate into a weighed dish, and weigh it. It is
potassium platino-chloride (K2PtCl6), and contains 16.03 per cent. of
potassium, or 30.56 per cent. of potassium chloride (KCl), which is
equivalent to 19.3 per cent. of potash (K2O).
If the filter-paper is not free from precipitate, burn it and weigh separately.
The excess of weight over that of the ash will be due to platinum and
potassic chloride (Pt and 2KCl). This multiplied by 1.413 will give the
weight of the potassic platino-chloride from which it was formed. It must be
added to the weight of the main precipitate.
The mixed alkaline chlorides obtained in the usual course of analysis are
treated in this manner; the quantity of platinum added must be about three
times as much as the mixed chlorides weigh.
VOLUMETRIC METHODS.
These are the same as with soda.
Examination of Commercial Carbonate of Potash.—The impurities to be
determined are moisture, silica, and insoluble matter, chlorine, sulphuric
oxide, and oxide of iron. These determinations are made in the ways
described under the examination of common salt.
The potassium is determined by converting it into chloride and
precipitating with platinum chloride, &c., as just described.
Available Alkali.—Weigh up 23.5 grams of the sample, dissolve in water,
and make up to 500 c.c. Take 50 c.c., tint with methyl orange, and titrate
with the normal solution of acid. The c.c. of acid used multiplied by 2 gives
the percentage of available alkali calculated as potash (K2O).
Soda.—This is calculated indirectly in the following way:—Deduct from
the potassium found the quantity required for combination with the chlorine
shows that the excess of the platinum chloride used is removed. Wash the
precipitate on to the filter with a jet of alcohol from the wash-bottle; clean
the filter-paper, using as little alcohol as possible. Dry in the water-oven for
an hour. Brush the precipitate into a weighed dish, and weigh it. It is
potassium platino-chloride (K2PtCl6), and contains 16.03 per cent. of
potassium, or 30.56 per cent. of potassium chloride (KCl), which is
equivalent to 19.3 per cent. of potash (K2O).
If the filter-paper is not free from precipitate, burn it and weigh separately.
The excess of weight over that of the ash will be due to platinum and
potassic chloride (Pt and 2KCl). This multiplied by 1.413 will give the
weight of the potassic platino-chloride from which it was formed. It must be
added to the weight of the main precipitate.
The mixed alkaline chlorides obtained in the usual course of analysis are
treated in this manner; the quantity of platinum added must be about three
times as much as the mixed chlorides weigh.
VOLUMETRIC METHODS.
These are the same as with soda.
Examination of Commercial Carbonate of Potash.—The impurities to be
determined are moisture, silica, and insoluble matter, chlorine, sulphuric
oxide, and oxide of iron. These determinations are made in the ways
described under the examination of common salt.
The potassium is determined by converting it into chloride and
precipitating with platinum chloride, &c., as just described.
Available Alkali.—Weigh up 23.5 grams of the sample, dissolve in water,
and make up to 500 c.c. Take 50 c.c., tint with methyl orange, and titrate
with the normal solution of acid. The c.c. of acid used multiplied by 2 gives
the percentage of available alkali calculated as potash (K2O).
Soda.—This is calculated indirectly in the following way:—Deduct from
the potassium found the quantity required for combination with the chlorine
Page 424
and sulphuric oxide present, and calculate the remainder to potash (K2O).
The apparent surplus excess of available alkali is the measure of the soda
present.
Carbon Dioxide.—The c.c. of acid used in the available alkali
determination, multiplied by 2.2 and divided by 2.35, gives the percentage
of carbon dioxide.
LITHIUM.
Lithia, the oxide of lithium (Li2O), occurs in quantities of 3 or 4 per cent. in
various silicates, such as lepidolite (or lithia-mica), spodumene, and
petalite. It also occurs as phosphate in triphyline. It is a constituent of the
water of certain mineral springs. A spring at Wheal Clifford contained as
much as 0.372 gram of lithium chloride per litre. In small quantities, lithia
is very widely diffused.
The Detection of lithia is rendered easy by the spectroscope; its spectrum
shows a red line lying about midway between the yellow sodium line and
the red one of potassium. It also shows a faint yellow line. The colour of the
flame (a crimson) is characteristic.
The reactions of the lithium compounds lie between those of the alkalies
and of the alkaline earths. Solutions are not precipitated by tartaric acid nor
by platinic chloride. The oxide is slowly soluble in water. The carbonate is
not freely soluble. Lithia is completely precipitated by sodic phosphate,
especially in hot alkaline solutions.
In its determination the mixed alkaline chlorides obtained in the separation
of the alkalies are dissolved in water, a solution of soda is added in slight
excess, and the lithia precipitated with sodic phosphate. Before filtering, it
is evaporated to dryness and extracted with hot water rendered slightly
ammoniacal. The residue is transferred to a filter, dried, ignited, and
weighed. The precipitate is lithium phosphate (3Li2O, P2O5), and contains
38.8 per cent. of lithia. The separation of lithia from magnesia is not given
by the usual authorities. Wohler recommends evaporating the solution to
dryness with carbonate of soda. On extracting the residue with water, the
lithia dissolves out and is determined in the filtrate. One hundred parts of
The apparent surplus excess of available alkali is the measure of the soda
present.
Carbon Dioxide.—The c.c. of acid used in the available alkali
determination, multiplied by 2.2 and divided by 2.35, gives the percentage
of carbon dioxide.
LITHIUM.
Lithia, the oxide of lithium (Li2O), occurs in quantities of 3 or 4 per cent. in
various silicates, such as lepidolite (or lithia-mica), spodumene, and
petalite. It also occurs as phosphate in triphyline. It is a constituent of the
water of certain mineral springs. A spring at Wheal Clifford contained as
much as 0.372 gram of lithium chloride per litre. In small quantities, lithia
is very widely diffused.
The Detection of lithia is rendered easy by the spectroscope; its spectrum
shows a red line lying about midway between the yellow sodium line and
the red one of potassium. It also shows a faint yellow line. The colour of the
flame (a crimson) is characteristic.
The reactions of the lithium compounds lie between those of the alkalies
and of the alkaline earths. Solutions are not precipitated by tartaric acid nor
by platinic chloride. The oxide is slowly soluble in water. The carbonate is
not freely soluble. Lithia is completely precipitated by sodic phosphate,
especially in hot alkaline solutions.
In its determination the mixed alkaline chlorides obtained in the separation
of the alkalies are dissolved in water, a solution of soda is added in slight
excess, and the lithia precipitated with sodic phosphate. Before filtering, it
is evaporated to dryness and extracted with hot water rendered slightly
ammoniacal. The residue is transferred to a filter, dried, ignited, and
weighed. The precipitate is lithium phosphate (3Li2O, P2O5), and contains
38.8 per cent. of lithia. The separation of lithia from magnesia is not given
by the usual authorities. Wohler recommends evaporating the solution to
dryness with carbonate of soda. On extracting the residue with water, the
lithia dissolves out and is determined in the filtrate. One hundred parts of
Page 425
water dissolve, at the ordinary temperature, 0.769 parts of lithium carbonate
(Li2CO3); the basic magnesia compound is almost insoluble in the absence
of carbon dioxide and ammonium salts.
CAESIUM.
The oxide of caesium, caesia (Cs2O), is found associated with lithia in
lepidolite, &c., and, together with rubidium, in many mineral waters. The
mineral pollux is essentially a silicate of alumina and caesia; it contains
34.0 per cent. of the latter oxide.
Caesium is best detected by the spectroscope, its spectrum being
characterised by two lines in the blue and one in the red; the latter is about
midway between the lithium and sodium lines.
If not detected by the spectroscope, or specially looked for, caesia would, in
the ordinary course of work, be separated with the potash and weighed as
potassium platino-chloride.
Caesia is separated from all the other alkalies by adding to the acid solution
of the mixed chlorides a strongly acid cold solution of antimonious
chloride. The acid used must be hydrochloric. The caesium is precipitated
as a white crystalline precipitate (CsCl.SbCl3), which is filtered off, and
washed, when cold, with strong hydrochloric acid; since it is decomposed
by water or on warming. The precipitate is washed into a beaker, and
treated with sulphuretted hydrogen; after filtering off the sulphide of
antimony, the solution leaves, on evaporation, the caesium as chloride.
RUBIDIUM.
Rubidium occurs widely diffused in nature, but in very small quantities. It is
generally associated with caesium.
It is detected by the spectroscope, which shows two violet lines and two
dark red ones. Like caesium, it is precipitated with platinic chloride, and in
the ordinary course of work would be weighed as potassium. It is separated
(Li2CO3); the basic magnesia compound is almost insoluble in the absence
of carbon dioxide and ammonium salts.
CAESIUM.
The oxide of caesium, caesia (Cs2O), is found associated with lithia in
lepidolite, &c., and, together with rubidium, in many mineral waters. The
mineral pollux is essentially a silicate of alumina and caesia; it contains
34.0 per cent. of the latter oxide.
Caesium is best detected by the spectroscope, its spectrum being
characterised by two lines in the blue and one in the red; the latter is about
midway between the lithium and sodium lines.
If not detected by the spectroscope, or specially looked for, caesia would, in
the ordinary course of work, be separated with the potash and weighed as
potassium platino-chloride.
Caesia is separated from all the other alkalies by adding to the acid solution
of the mixed chlorides a strongly acid cold solution of antimonious
chloride. The acid used must be hydrochloric. The caesium is precipitated
as a white crystalline precipitate (CsCl.SbCl3), which is filtered off, and
washed, when cold, with strong hydrochloric acid; since it is decomposed
by water or on warming. The precipitate is washed into a beaker, and
treated with sulphuretted hydrogen; after filtering off the sulphide of
antimony, the solution leaves, on evaporation, the caesium as chloride.
RUBIDIUM.
Rubidium occurs widely diffused in nature, but in very small quantities. It is
generally associated with caesium.
It is detected by the spectroscope, which shows two violet lines and two
dark red ones. Like caesium, it is precipitated with platinic chloride, and in
the ordinary course of work would be weighed as potassium. It is separated
Page 426
from potassium by fractional precipitation with platinic chloride. Rubidium
platino-chloride is much less soluble than the potassium salt.
AMMONIUM.
It is usual to look upon the salts of ammonia as containing a compound
radical (NH4 = Am), which resembles in many respects the metals of the
alkalies. Ammonium occurs in nature as chloride in sal ammoniac (AmCl),
as sulphate in mascagnine (Am2SO4), as phosphate in struvite
(AmMgPO4.12H2O). Minerals containing ammonium are rare, and are
chiefly found either in volcanic districts or associated with guano.
Ammonia and ammonium sulphide occur in the waters of certain Tuscan
lagoons, which are largely worked for the boracic acid they contain. The
crude boracic acid from this source contains from 5 to 10 per cent. of
ammonium salts. It is from these that the purer forms of ammonium
compounds of commerce known as "from volcanic ammonia" are derived.
But the bulk of the ammonia of commerce is prepared from the ammoniacal
liquors obtained as bye-products in the working of certain forms of blast
furnaces and coke ovens, and more especially in gas-making.
Ammonia hardly comes within the objects of assaying; but it is largely used
in the laboratory, and the assayer is not unfrequently called on to determine
it. Ammonium salts are mostly soluble in water. In strong solutions they
give a yellow precipitate of ammonium platino-chloride on the addition of
chloride of platinum; and with the acid tartrate of soda yield a white
precipitate of hydric ammonic tartrate. These reactions are similar to those
produced with potassium compounds.
Heated with a base, such as lime or sodic hydrate, ammonium salts are
decomposed, yielding ammonia gas (NH3), which is readily soluble in
water. The solution of this substance is known as ammonic hydrate or
"ammonia."
They are volatilised on ignition; either with, or without, decomposition
according to the acid present. This fact is of importance in analytical work;
since it allows of the use of alkaline solutions and reagents which leave
nothing behind on heating. It must be remembered, however, that, although
platino-chloride is much less soluble than the potassium salt.
AMMONIUM.
It is usual to look upon the salts of ammonia as containing a compound
radical (NH4 = Am), which resembles in many respects the metals of the
alkalies. Ammonium occurs in nature as chloride in sal ammoniac (AmCl),
as sulphate in mascagnine (Am2SO4), as phosphate in struvite
(AmMgPO4.12H2O). Minerals containing ammonium are rare, and are
chiefly found either in volcanic districts or associated with guano.
Ammonia and ammonium sulphide occur in the waters of certain Tuscan
lagoons, which are largely worked for the boracic acid they contain. The
crude boracic acid from this source contains from 5 to 10 per cent. of
ammonium salts. It is from these that the purer forms of ammonium
compounds of commerce known as "from volcanic ammonia" are derived.
But the bulk of the ammonia of commerce is prepared from the ammoniacal
liquors obtained as bye-products in the working of certain forms of blast
furnaces and coke ovens, and more especially in gas-making.
Ammonia hardly comes within the objects of assaying; but it is largely used
in the laboratory, and the assayer is not unfrequently called on to determine
it. Ammonium salts are mostly soluble in water. In strong solutions they
give a yellow precipitate of ammonium platino-chloride on the addition of
chloride of platinum; and with the acid tartrate of soda yield a white
precipitate of hydric ammonic tartrate. These reactions are similar to those
produced with potassium compounds.
Heated with a base, such as lime or sodic hydrate, ammonium salts are
decomposed, yielding ammonia gas (NH3), which is readily soluble in
water. The solution of this substance is known as ammonic hydrate or
"ammonia."
They are volatilised on ignition; either with, or without, decomposition
according to the acid present. This fact is of importance in analytical work;
since it allows of the use of alkaline solutions and reagents which leave
nothing behind on heating. It must be remembered, however, that, although
Page 427
ammonic chloride is volatile, it cannot be volatilised in the presence of
substances which form volatile chlorides without loss of the latter. For
example: ferric oxide and alumina are thus lost, volatilising as chlorides;
and there are some other compounds (notably ammonic magnesic arsenate)
which on heating to redness suffer reduction. The presence of ammonic
chloride in such cases must be avoided.
Detection.—Compounds of ammonium are detected by their evolving
ammonia when mixed or heated with any of the stronger bases. The
ammonia is recognised by its odour, by its alkaline reaction with litmus
paper, and by yielding white fumes, when brought in contact with fuming
acid. In consequence of the use of ammonium salts and ammonia as
reagents, it is necessary to make a special test for and determination of
ammonium.[94] In the ordinary course of work it will be "lost on ignition."
The determination presents little difficulty, and is based on the method used
for its detection.
Solution and Separation.—Although ammonium salts are soluble in water,
there is no necessity for dissolving them. The compound containing the
ammonia is boiled with an alkaline solution; and the liberated ammonia
condensed and collected. The substance is weighed out into a flask of about
200 c.c. capacity. The flask is closed with a rubber cork perforated to carry
substances which form volatile chlorides without loss of the latter. For
example: ferric oxide and alumina are thus lost, volatilising as chlorides;
and there are some other compounds (notably ammonic magnesic arsenate)
which on heating to redness suffer reduction. The presence of ammonic
chloride in such cases must be avoided.
Detection.—Compounds of ammonium are detected by their evolving
ammonia when mixed or heated with any of the stronger bases. The
ammonia is recognised by its odour, by its alkaline reaction with litmus
paper, and by yielding white fumes, when brought in contact with fuming
acid. In consequence of the use of ammonium salts and ammonia as
reagents, it is necessary to make a special test for and determination of
ammonium.[94] In the ordinary course of work it will be "lost on ignition."
The determination presents little difficulty, and is based on the method used
for its detection.
Solution and Separation.—Although ammonium salts are soluble in water,
there is no necessity for dissolving them. The compound containing the
ammonia is boiled with an alkaline solution; and the liberated ammonia
condensed and collected. The substance is weighed out into a flask of about
200 c.c. capacity. The flask is closed with a rubber cork perforated to carry
Page 428
a 20 c.c. pipette and a bulb exit tube. The latter is connected with a receiver,
which is a small flask containing dilute hydrochloric acid (fig. 61). The
flask containing the substance is corked, and the greater part of the soda
solution is run in from the pipette. The solution is then boiled. The
ammonia volatilises, and is carried over into the hydrochloric acid, with
which it combines to form ammonic chloride. The distillation is carried on
gently until the bulk of the liquid is driven over. The ammonia in the
receiver will be mixed only with the excess of hydrochloric acid. This
separation is used in all determinations.
GRAVIMETRIC DETERMINATION.
The contents of the flask are transferred to a weighed platinum dish, and
evaporated on the water-bath. It is dried until the weight is constant. The
chloride of ammonium remains as a white mass which, after cooling in a
desiccator, is weighed. It contains 33.72 per cent. of ammonium (NH4), or
31.85 per cent. of ammonia (NH3). On heating over the Bunsen burner it is
completely volatilised, leaving no residue.
VOLUMETRIC DETERMINATION.
Weigh up 1.7 gram of the substance and place it in the flask. Measure off 50
c.c. of the normal solution of acid, place them in the receiver, and dilute
with an equal volume of water. Run in through the pipette (by opening the
clip) 20 c.c. of a strong solution of soda, boil until the ammonia has passed
over, and then aspirate a current of air through the apparatus. Disconnect
the receiver, and tint its contents with methyl orange. Titrate the residual
acid with a semi-normal solution of alkali. Divide the c.c. of the "alkali"
solution used by 2, and deduct from the 50 c.c. The difference will give the
number of c.c. of the normal acid solution neutralised by the ammonia
distilled over. Each c.c. of "acid" so neutralised, represents 1 per cent. of
ammonia in the sample. If the results are to be reported as ammonium, 1.8
gram of the sample is taken instead of 1.7 gram.
COLORIMETRIC DETERMINATION.
which is a small flask containing dilute hydrochloric acid (fig. 61). The
flask containing the substance is corked, and the greater part of the soda
solution is run in from the pipette. The solution is then boiled. The
ammonia volatilises, and is carried over into the hydrochloric acid, with
which it combines to form ammonic chloride. The distillation is carried on
gently until the bulk of the liquid is driven over. The ammonia in the
receiver will be mixed only with the excess of hydrochloric acid. This
separation is used in all determinations.
GRAVIMETRIC DETERMINATION.
The contents of the flask are transferred to a weighed platinum dish, and
evaporated on the water-bath. It is dried until the weight is constant. The
chloride of ammonium remains as a white mass which, after cooling in a
desiccator, is weighed. It contains 33.72 per cent. of ammonium (NH4), or
31.85 per cent. of ammonia (NH3). On heating over the Bunsen burner it is
completely volatilised, leaving no residue.
VOLUMETRIC DETERMINATION.
Weigh up 1.7 gram of the substance and place it in the flask. Measure off 50
c.c. of the normal solution of acid, place them in the receiver, and dilute
with an equal volume of water. Run in through the pipette (by opening the
clip) 20 c.c. of a strong solution of soda, boil until the ammonia has passed
over, and then aspirate a current of air through the apparatus. Disconnect
the receiver, and tint its contents with methyl orange. Titrate the residual
acid with a semi-normal solution of alkali. Divide the c.c. of the "alkali"
solution used by 2, and deduct from the 50 c.c. The difference will give the
number of c.c. of the normal acid solution neutralised by the ammonia
distilled over. Each c.c. of "acid" so neutralised, represents 1 per cent. of
ammonia in the sample. If the results are to be reported as ammonium, 1.8
gram of the sample is taken instead of 1.7 gram.
COLORIMETRIC DETERMINATION.
Page 429
This is effected by means of "Nessler's" reagent, which strikes a brown
colour with traces of ammonia, even with a few hundredths of a milligram
in 100 c.c. of liquid. With larger quantities of ammonia the reagent gives a
precipitate. This reagent is a strongly alkaline solution of potassic mercuric
iodide; and is thus made:—
Nessler's solution: Dissolve 17 grams of mercuric chloride in 300 c.c. of
water; and add the solution to one of 35 grams of potassium iodide in 100
c.c. of water until a permanent precipitate is produced. Both solutions must
be cold. Then make up to a litre by adding a 20 per cent. solution of potash.
Add more of the mercuric chloride (a little at a time) until a permanent
precipitate is again formed. Allow to settle, decant, and use the clear liquor.
Four or five c.c. are used for each 100 c.c. of liquid to be tested.
A Standard Solution of Ammonia is made by dissolving 0.315 gram of
ammonic chloride in water, and diluting to 100 c.c. Ten c.c. of this are taken
and diluted to 1 litre. One c.c. contains 0.01 milligram of ammonia (NH3).
In working, the solution containing the ammonia is diluted to a definite
volume, and to such an extent that 50 c.c. of it shall not contain more than
0.02 or 0.03 milligram of ammonia. Fifty c.c. of it are transferred to a
Nessler glass and mixed with 2 c.c. of Nessler's reagent. The colour is
noted, and an estimate made as to the amount of ammonia it indicates. A
measured quantity of the standard ammonia, judged to contain about as
much ammonia as that in the assay, is then put into another Nessler glass. It
is diluted to 50 c.c. with water, and mixed with 2 c.c. of "Nessler." After
standing a minute or two, the colours in the two glasses are compared. If the
tints are equal, the assay is finished; but if the standard is weaker or
stronger than the assay, another standard, containing more or less ammonia,
as the case may be, must be prepared and compared with the assay. Two
such experiments will generally be sufficient; but, if not, a third must be
made. The addition of more standard ammonia to the solution to which the
"Nessler" has already been added does not give a satisfactory result.
When the ammonia in 50 c.c. has been determined, that in the whole
solution is ascertained by a suitable multiplication. By 10, for example, if
the bulk was 500 c.c., or by 20 if it was a litre.
colour with traces of ammonia, even with a few hundredths of a milligram
in 100 c.c. of liquid. With larger quantities of ammonia the reagent gives a
precipitate. This reagent is a strongly alkaline solution of potassic mercuric
iodide; and is thus made:—
Nessler's solution: Dissolve 17 grams of mercuric chloride in 300 c.c. of
water; and add the solution to one of 35 grams of potassium iodide in 100
c.c. of water until a permanent precipitate is produced. Both solutions must
be cold. Then make up to a litre by adding a 20 per cent. solution of potash.
Add more of the mercuric chloride (a little at a time) until a permanent
precipitate is again formed. Allow to settle, decant, and use the clear liquor.
Four or five c.c. are used for each 100 c.c. of liquid to be tested.
A Standard Solution of Ammonia is made by dissolving 0.315 gram of
ammonic chloride in water, and diluting to 100 c.c. Ten c.c. of this are taken
and diluted to 1 litre. One c.c. contains 0.01 milligram of ammonia (NH3).
In working, the solution containing the ammonia is diluted to a definite
volume, and to such an extent that 50 c.c. of it shall not contain more than
0.02 or 0.03 milligram of ammonia. Fifty c.c. of it are transferred to a
Nessler glass and mixed with 2 c.c. of Nessler's reagent. The colour is
noted, and an estimate made as to the amount of ammonia it indicates. A
measured quantity of the standard ammonia, judged to contain about as
much ammonia as that in the assay, is then put into another Nessler glass. It
is diluted to 50 c.c. with water, and mixed with 2 c.c. of "Nessler." After
standing a minute or two, the colours in the two glasses are compared. If the
tints are equal, the assay is finished; but if the standard is weaker or
stronger than the assay, another standard, containing more or less ammonia,
as the case may be, must be prepared and compared with the assay. Two
such experiments will generally be sufficient; but, if not, a third must be
made. The addition of more standard ammonia to the solution to which the
"Nessler" has already been added does not give a satisfactory result.
When the ammonia in 50 c.c. has been determined, that in the whole
solution is ascertained by a suitable multiplication. By 10, for example, if
the bulk was 500 c.c., or by 20 if it was a litre.
Page 430
Distilled water is used throughout. It must be free from ammonia; and is
best prepared by distilling an ammonia-free spring water.
FOOTNOTES:
[90] Al2Cl6 + 3Na2S2O3 + 3H2O = Al2(HO)6 + 6NaCl + 3S + 3SO2
[91] 3BeO,Al2O3,6SiO2
[92] CaC2O4 = CaCO3+CO.
[93] Resolved into two with a powerful spectroscope.
[94] Ammonium compounds are frequently produced when dissolving metals in
nitric acid; or when nitrates are heated in the presence of the metals.
best prepared by distilling an ammonia-free spring water.
FOOTNOTES:
[90] Al2Cl6 + 3Na2S2O3 + 3H2O = Al2(HO)6 + 6NaCl + 3S + 3SO2
[91] 3BeO,Al2O3,6SiO2
[92] CaC2O4 = CaCO3+CO.
[93] Resolved into two with a powerful spectroscope.
[94] Ammonium compounds are frequently produced when dissolving metals in
nitric acid; or when nitrates are heated in the presence of the metals.
Page 431
PART III—NON-METALS.
Page 432
CHAPTER XV.
OXYGEN AND OXIDES.—THE HALOGENS.
OXYGEN.
Oxygen occurs in nature in the free state, forming 23 per cent. by weight, or
21 per cent. by volume of the atmosphere; but, since it is a gas, its presence
is easily overlooked and its importance underestimated. Except in the
examination of furnace-gases, &c., the assayer is not often called upon to
determine its quantity, but it forms one of his most useful reagents, and
there are many cases where he cannot afford to disregard its presence. It
occurs not only in the air, but also dissolved in water; ordinary waters
containing on an average 0.00085 per cent. by weight, or 0.85 parts per
100,000.
Chemically, it is characterised by its power of combining, especially at high
temperatures, with the other elements, forming an important class of
compounds called oxides. This combination, when rapid, is accompanied by
the evolution of light and heat; hence oxygen is generally called the
supporter of combustion. This property is taken advantage of in the
operation of calcining, scorifying, cupelling, &c. The importance of a free
access of air in all such work is seen when it is remembered that 1 litre of
air contains 0.2975 gram of oxygen, and this quantity will only oxidise
0.1115 gram of carbon, 0.2975 gram of sulphur, or 3.849 grams of lead.
Oxidation takes place at the ordinary temperature with many substances.
Examples of such action are seen in the weathering of pyrites, rusting of
iron, and (in the assay office) the weakening of solutions of many reducing
agents.
For methods of determining the percentage of oxygen in gases, for technical
purposes, the student is referred to Winkler & Lunge's "Technical Gas
Analysis."
OXYGEN AND OXIDES.—THE HALOGENS.
OXYGEN.
Oxygen occurs in nature in the free state, forming 23 per cent. by weight, or
21 per cent. by volume of the atmosphere; but, since it is a gas, its presence
is easily overlooked and its importance underestimated. Except in the
examination of furnace-gases, &c., the assayer is not often called upon to
determine its quantity, but it forms one of his most useful reagents, and
there are many cases where he cannot afford to disregard its presence. It
occurs not only in the air, but also dissolved in water; ordinary waters
containing on an average 0.00085 per cent. by weight, or 0.85 parts per
100,000.
Chemically, it is characterised by its power of combining, especially at high
temperatures, with the other elements, forming an important class of
compounds called oxides. This combination, when rapid, is accompanied by
the evolution of light and heat; hence oxygen is generally called the
supporter of combustion. This property is taken advantage of in the
operation of calcining, scorifying, cupelling, &c. The importance of a free
access of air in all such work is seen when it is remembered that 1 litre of
air contains 0.2975 gram of oxygen, and this quantity will only oxidise
0.1115 gram of carbon, 0.2975 gram of sulphur, or 3.849 grams of lead.
Oxidation takes place at the ordinary temperature with many substances.
Examples of such action are seen in the weathering of pyrites, rusting of
iron, and (in the assay office) the weakening of solutions of many reducing
agents.
For methods of determining the percentage of oxygen in gases, for technical
purposes, the student is referred to Winkler & Lunge's "Technical Gas
Analysis."
Page 433
OXIDES.
Oxides are abundant in nature, almost all the commonly occurring bodies
being oxidised. Water (H2O) contains 88.8 per cent. of oxygen; silica, lime,
alumina, magnesia, and the other earths are oxides, and the oxides of the
heavier metals are in many cases important ores; as, for example, cassiterite
(SnO2), hæmatite (Fe2O3), magnetite (Fe3O4), and pyrolusite (MnO2). In
fact, the last-named mineral owes its value to the excess of oxygen it
contains, and may be regarded as an ore of oxygen rather than of
manganese.
Most of the metals, when heated to redness in contact with air, lose their
metallic lustre and become coated with, or (if the heating be prolonged)
altogether converted into, oxide. This oxide was formerly termed a "calx,"
and has long been known to weigh more than the metal from which it was
obtained. For example, one part by weight of tin becomes, on calcining,
1.271 parts of oxide (putty powder). The student will do well to try the
following experiments:—Take 20 grams of tin and heat them in a muffle on
a scorifier, scraping back the dross as it forms, and continuing the operation
until the whole of the metal is burnt to a white powder and ceases to
increase in weight.[95] Take care to avoid loss, and, when cold, weigh the
oxide formed. The oxide should weigh 25.42 grams, which increase in
weight is due to the oxygen absorbed from the air and combined with the
metal. It can be calculated from this experiment (if there has been no loss)
that oxide of tin contains 21.33 per cent. of oxygen and 78.67 per cent. of
tin. Oxidation is performed with greater convenience by wet methods, using
reagents, such as nitric acid, which contain a large proportion of oxygen
loosely held. Such reagents are termed oxidising agents. Besides nitric acid,
permanganate of potash, bichromate of potash, and peroxide of hydrogen
are largely used for this purpose. One c.c. of nitric acid contains as much
oxygen as 2.56 litres of air, and the greater part of this is available for
oxidising purposes. Try the following experiment:—Take 2 grams of tin and
cover in a weighed Berlin dish with 20 c.c. of dilute nitric acid, heat till
decomposed, evaporate to dryness, ignite, and weigh. The 2 grams of tin
should yield 2.542 grams of oxide. The increase in weight will be
proportionally the same as in the previous experiment by calcination, and is
due to oxygen, which in this case has been derived from the nitric acid.
Oxides are abundant in nature, almost all the commonly occurring bodies
being oxidised. Water (H2O) contains 88.8 per cent. of oxygen; silica, lime,
alumina, magnesia, and the other earths are oxides, and the oxides of the
heavier metals are in many cases important ores; as, for example, cassiterite
(SnO2), hæmatite (Fe2O3), magnetite (Fe3O4), and pyrolusite (MnO2). In
fact, the last-named mineral owes its value to the excess of oxygen it
contains, and may be regarded as an ore of oxygen rather than of
manganese.
Most of the metals, when heated to redness in contact with air, lose their
metallic lustre and become coated with, or (if the heating be prolonged)
altogether converted into, oxide. This oxide was formerly termed a "calx,"
and has long been known to weigh more than the metal from which it was
obtained. For example, one part by weight of tin becomes, on calcining,
1.271 parts of oxide (putty powder). The student will do well to try the
following experiments:—Take 20 grams of tin and heat them in a muffle on
a scorifier, scraping back the dross as it forms, and continuing the operation
until the whole of the metal is burnt to a white powder and ceases to
increase in weight.[95] Take care to avoid loss, and, when cold, weigh the
oxide formed. The oxide should weigh 25.42 grams, which increase in
weight is due to the oxygen absorbed from the air and combined with the
metal. It can be calculated from this experiment (if there has been no loss)
that oxide of tin contains 21.33 per cent. of oxygen and 78.67 per cent. of
tin. Oxidation is performed with greater convenience by wet methods, using
reagents, such as nitric acid, which contain a large proportion of oxygen
loosely held. Such reagents are termed oxidising agents. Besides nitric acid,
permanganate of potash, bichromate of potash, and peroxide of hydrogen
are largely used for this purpose. One c.c. of nitric acid contains as much
oxygen as 2.56 litres of air, and the greater part of this is available for
oxidising purposes. Try the following experiment:—Take 2 grams of tin and
cover in a weighed Berlin dish with 20 c.c. of dilute nitric acid, heat till
decomposed, evaporate to dryness, ignite, and weigh. The 2 grams of tin
should yield 2.542 grams of oxide. The increase in weight will be
proportionally the same as in the previous experiment by calcination, and is
due to oxygen, which in this case has been derived from the nitric acid.
Page 434
The percentage of oxygen in this oxide of tin (or in any of the oxides of the
heavier metals) may be directly determined by heating such oxides in a
current of hydrogen, and collecting and weighing the water formed.
It is found by experiment that 88.86 parts by weight of oxygen, combining
with 11.14 parts of hydrogen, form 100 parts of water; so that from the
weight of water formed it is easy to calculate the amount of oxygen the
oxide contained.
heavier metals) may be directly determined by heating such oxides in a
current of hydrogen, and collecting and weighing the water formed.
It is found by experiment that 88.86 parts by weight of oxygen, combining
with 11.14 parts of hydrogen, form 100 parts of water; so that from the
weight of water formed it is easy to calculate the amount of oxygen the
oxide contained.
Page 435
Take 1 gram of the dried and powdered oxide and place it in a warm dry
combustion tube. Place the tube in a furnace, and connect at one end with a
hydrogen apparatus provided with a sulphuric acid bulb for drying the gas,
and at the other with a weighed sulphuric acid tube for collecting the water
formed. The apparatus required is shown in fig. 62. Pass hydrogen through
the apparatus, and, when the air has been cleared out, light the furnace.
Continue the heat and current of hydrogen for half an hour (or longer, if
necessary). Allow to cool. Draw a current of dry air through the weighed
tube. Weigh. The increase in weight gives the amount of water formed, and
this, multiplied by 0.8886, gives the weight of the oxygen. The percentage
of oxygen thus determined should be compared with that got by the
oxidation of the metal. It will be practically the same. The following results
can be taken as examples:—
Twenty grams of tin, calcined as described, gave 25.37 grams of oxide.
Two grams of tin, oxidised with nitric acid and ignited, gave 2.551 grams of
oxide.
One gram of the oxide of tin, on reduction in a current of hydrogen, gave
0.2360 gram of water (equivalent to 0.2098 gram of oxygen), and left
0.7900 gram of metal.
Ten grams of ferrous sulphate gave, on strong ignition, 2.898 grams of
ferric oxide (Fe2O3)[96] instead of 2.877.
The student should similarly determine the percentage of oxygen in oxides
of copper and iron. The former oxide may be prepared by dissolving 5
grams of copper in 50 c.c. of dilute nitric acid, evaporating to dryness, and
strongly igniting the residue. The oxide of iron may be made by weighing
up 10 grams of powdered ferrous sulphate (= to 2.014 grams of iron) and
combustion tube. Place the tube in a furnace, and connect at one end with a
hydrogen apparatus provided with a sulphuric acid bulb for drying the gas,
and at the other with a weighed sulphuric acid tube for collecting the water
formed. The apparatus required is shown in fig. 62. Pass hydrogen through
the apparatus, and, when the air has been cleared out, light the furnace.
Continue the heat and current of hydrogen for half an hour (or longer, if
necessary). Allow to cool. Draw a current of dry air through the weighed
tube. Weigh. The increase in weight gives the amount of water formed, and
this, multiplied by 0.8886, gives the weight of the oxygen. The percentage
of oxygen thus determined should be compared with that got by the
oxidation of the metal. It will be practically the same. The following results
can be taken as examples:—
Twenty grams of tin, calcined as described, gave 25.37 grams of oxide.
Two grams of tin, oxidised with nitric acid and ignited, gave 2.551 grams of
oxide.
One gram of the oxide of tin, on reduction in a current of hydrogen, gave
0.2360 gram of water (equivalent to 0.2098 gram of oxygen), and left
0.7900 gram of metal.
Ten grams of ferrous sulphate gave, on strong ignition, 2.898 grams of
ferric oxide (Fe2O3)[96] instead of 2.877.
The student should similarly determine the percentage of oxygen in oxides
of copper and iron. The former oxide may be prepared by dissolving 5
grams of copper in 50 c.c. of dilute nitric acid, evaporating to dryness, and
strongly igniting the residue. The oxide of iron may be made by weighing
up 10 grams of powdered ferrous sulphate (= to 2.014 grams of iron) and
Page 436
heating, at first gently, to drive off the water, and then at a red heat, until
completely decomposed. The weight of oxide, in each case, should be
determined; and the percentage of oxygen calculated. Compare the figures
arrived at with those calculated from the formula of the oxides, CuO and
Fe2O3.
It would be found in a more extended series of experiments that the same
metal will, under certain conditions, form two or more oxides differing
among themselves in the amount of oxygen they contain. These oxides are
distinguished from one another by such names as "higher" and "lower
oxides," "peroxides," "protoxides," "dioxides," &c.
The oxides may be conveniently classified under three heads:—
(1) Those that are reduced to metal by heat alone, such as the oxides of
mercury, silver, platinum, gold, &c.;
(2) Those which are reduced by hydrogen at a red heat, which includes the
oxides of the heavy metals;
(3) Those which are not reduced by these means, good examples of which
are silica, alumina, the alkalies, and the alkaline earths.
Another important classification is into acid, basic and neutral oxides. The
oxides of the non-metallic elements, such as sulphur, carbon, phosphorus,
&c., are, as a rule, acid; and the more oxygen they contain, the more
distinctly acid they are. The oxides of the metals are nearly all basic; and, as
a rule, the less oxygen they contain, the more distinctly basic they are.
The basic oxides, which are soluble in acids, give rise to the formation of
salts when dissolved therein. During the solution, water is formed, but no
gas is evolved. The oxide dissolved in each case neutralizes an equivalent
of the acid used for solution.[97] The basic properties of many of these can
be taken advantage of for their determination. This is done in the case of
soda, potash, lime, &c., by finding the quantity of acid required to
neutralize a given weight of the substance.
There are some oxides which, under certain conditions, are acid to one
substance (a stronger base) and basic to another (a stronger acid). For
example, the oxides of lead and of tin, as also alumina, dissolve in caustic
completely decomposed. The weight of oxide, in each case, should be
determined; and the percentage of oxygen calculated. Compare the figures
arrived at with those calculated from the formula of the oxides, CuO and
Fe2O3.
It would be found in a more extended series of experiments that the same
metal will, under certain conditions, form two or more oxides differing
among themselves in the amount of oxygen they contain. These oxides are
distinguished from one another by such names as "higher" and "lower
oxides," "peroxides," "protoxides," "dioxides," &c.
The oxides may be conveniently classified under three heads:—
(1) Those that are reduced to metal by heat alone, such as the oxides of
mercury, silver, platinum, gold, &c.;
(2) Those which are reduced by hydrogen at a red heat, which includes the
oxides of the heavy metals;
(3) Those which are not reduced by these means, good examples of which
are silica, alumina, the alkalies, and the alkaline earths.
Another important classification is into acid, basic and neutral oxides. The
oxides of the non-metallic elements, such as sulphur, carbon, phosphorus,
&c., are, as a rule, acid; and the more oxygen they contain, the more
distinctly acid they are. The oxides of the metals are nearly all basic; and, as
a rule, the less oxygen they contain, the more distinctly basic they are.
The basic oxides, which are soluble in acids, give rise to the formation of
salts when dissolved therein. During the solution, water is formed, but no
gas is evolved. The oxide dissolved in each case neutralizes an equivalent
of the acid used for solution.[97] The basic properties of many of these can
be taken advantage of for their determination. This is done in the case of
soda, potash, lime, &c., by finding the quantity of acid required to
neutralize a given weight of the substance.
There are some oxides which, under certain conditions, are acid to one
substance (a stronger base) and basic to another (a stronger acid). For
example, the oxides of lead and of tin, as also alumina, dissolve in caustic
Page 437
soda, acting as acids; whilst, on the other hand, they combine with sulphuric
or hydrochloric acid, playing the part of bases.
The oxides known as "earths," when ignited, are many of them insoluble in
acids, although easily dissolved before ignition.
It is common in complete analyses of minerals to meet with cases in which
the sum total of the elements found falls short of the amount of ore taken;
and here oxygen must be looked for. For example, this occurs in the case of
a mixture of pyrites with oxide of iron, or in a mixture of sulphides and
sulphates. The state in which the elements are present, and the percentage
(say of sulphides and sulphates) can in many cases be determined; but this
is not always required. When the difference between the sum total and the
elements found is small, it is reported as "oxygen and loss." When,
however, it is considerable, the oxygen may be reported as such; and its
amount be either determined directly in the way already described, or
calculated from the best determination that can be made of the relative
amounts of oxides, sulphides, sulphates, &c., present. Such cases require a
careful qualitative analysis to find out that the substance is present; and then
the separation of each constituent is made as strictly as possible. These
remarks apply especially to ores of the heavy metals. The separation of the
constituents is effected with suitable solvents applied in proper order. The
soluble sulphates, for example, are extracted with water; the oxides by the
dilute acids or alkalies in which they are known to be soluble. The oxygen
in the sulphates and oxides thus obtained is estimated by determining the
sulphur and metals in the solutions, and calculating the amount of oxygen
with which they combine. The metals of the earths and alkalies are almost
invariably present as oxides, and are reported as such; except it is known
that they are present in some other form, such as fluoride or chloride. Thus,
silica, alumina, lime, water, &c., appear in an analysis; even in those cases
where "oxygen and loss" is also mentioned. As an example of such a report,
take the following analysis of Spanish pyrites:—
Sulphur 49.00
Iron 43.55
Copper 3.20
Arsenic 0.47
Lead 0.93
or hydrochloric acid, playing the part of bases.
The oxides known as "earths," when ignited, are many of them insoluble in
acids, although easily dissolved before ignition.
It is common in complete analyses of minerals to meet with cases in which
the sum total of the elements found falls short of the amount of ore taken;
and here oxygen must be looked for. For example, this occurs in the case of
a mixture of pyrites with oxide of iron, or in a mixture of sulphides and
sulphates. The state in which the elements are present, and the percentage
(say of sulphides and sulphates) can in many cases be determined; but this
is not always required. When the difference between the sum total and the
elements found is small, it is reported as "oxygen and loss." When,
however, it is considerable, the oxygen may be reported as such; and its
amount be either determined directly in the way already described, or
calculated from the best determination that can be made of the relative
amounts of oxides, sulphides, sulphates, &c., present. Such cases require a
careful qualitative analysis to find out that the substance is present; and then
the separation of each constituent is made as strictly as possible. These
remarks apply especially to ores of the heavy metals. The separation of the
constituents is effected with suitable solvents applied in proper order. The
soluble sulphates, for example, are extracted with water; the oxides by the
dilute acids or alkalies in which they are known to be soluble. The oxygen
in the sulphates and oxides thus obtained is estimated by determining the
sulphur and metals in the solutions, and calculating the amount of oxygen
with which they combine. The metals of the earths and alkalies are almost
invariably present as oxides, and are reported as such; except it is known
that they are present in some other form, such as fluoride or chloride. Thus,
silica, alumina, lime, water, &c., appear in an analysis; even in those cases
where "oxygen and loss" is also mentioned. As an example of such a report,
take the following analysis of Spanish pyrites:—
Sulphur 49.00
Iron 43.55
Copper 3.20
Arsenic 0.47
Lead 0.93
Page 438
Zinc 0.35
Lime 0.10
Silica, &c. 0.63
Water 0.70
Oxygen and loss 1.07
———
100.00
The following example will illustrate the mode of calculating and reporting.
A mineral, occurring as blue crystals soluble in water, and found on testing
to be a mixed sulphate of iron and copper, gave on analysis the following
results:—
Water 44.51 per cent.
Sulphuric oxide 28.82 "
Copper 8.44 "
Ferrous iron 11.81 "
Ferric iron 0.38 "
Zinc 0.28 "
———
94.24
There is here a deficiency of 5.76 per cent. due to oxygen. Nothing else
could be found, and it is known that in the sulphates the metals exist as
oxides. By multiplying the weight of the copper by 1.252, the weight of
copper oxide (CuO) will be ascertained; in this case it equals 10.57 per cent.
The ferrous iron multiplied by 1.286 will give the ferrous oxide (FeO); in
this case 15.19 per cent. The ferric iron multiplied by 1.428 will give the
ferric oxide (Fe2O3); in this case 0.54 per cent. The zinc multiplied by 1.246
will give the zinc oxide (ZnO); in this case it equals 0.35 per cent. The
analysis will be reported as—
Water 44.51
Sulphuric oxide 28.82
Copper oxide 10.57equal to copper 8.44%
Ferrous oxide 15.19
Lime 0.10
Silica, &c. 0.63
Water 0.70
Oxygen and loss 1.07
———
100.00
The following example will illustrate the mode of calculating and reporting.
A mineral, occurring as blue crystals soluble in water, and found on testing
to be a mixed sulphate of iron and copper, gave on analysis the following
results:—
Water 44.51 per cent.
Sulphuric oxide 28.82 "
Copper 8.44 "
Ferrous iron 11.81 "
Ferric iron 0.38 "
Zinc 0.28 "
———
94.24
There is here a deficiency of 5.76 per cent. due to oxygen. Nothing else
could be found, and it is known that in the sulphates the metals exist as
oxides. By multiplying the weight of the copper by 1.252, the weight of
copper oxide (CuO) will be ascertained; in this case it equals 10.57 per cent.
The ferrous iron multiplied by 1.286 will give the ferrous oxide (FeO); in
this case 15.19 per cent. The ferric iron multiplied by 1.428 will give the
ferric oxide (Fe2O3); in this case 0.54 per cent. The zinc multiplied by 1.246
will give the zinc oxide (ZnO); in this case it equals 0.35 per cent. The
analysis will be reported as—
Water 44.51
Sulphuric oxide 28.82
Copper oxide 10.57equal to copper 8.44%
Ferrous oxide 15.19
Page 439
Ferric oxide 0.54
Zinc oxide 0.35
———
99.98
The following (A) is an analysis of a sample of South American copper ore,
which will serve as a further illustration. The analysis showed the presence
of 6.89 per cent. of ferrous oxide, and some oxide of copper.
The analysis (B) is that of an ore from the same mine after an imperfect
roasting. It will be seen that the carbonates have been converted into
sulphates. If the total sulphur simply had been determined, and the sulphate
overlooked, the "oxygen and loss" would have been 5.65 per cent., an
amount which would obviously require an explanation.
A. B.
Water 0.25 0.59
Organic matter 0.54 —
Sulphur 29.50 21.33
Copper 10.92 9.80 {Copper 9.57
{Copper oxide 0.28
Iron 32.09 39.73 {Iron 34.32
{Ferric oxide 7.73
Lead 0.35 0.12
Zinc 0.86 0.69
Cobalt 0.06 0.11
Lime 5.25 7.69
Magnesia 2.33 2.55
Sulphuric oxide 1.00 5.30
Carbon dioxide 8.87 —
"Insoluble silicates" 5.12 8.38
Oxygen and loss 2.86 2.47
———Potash 0.15
100.00 Soda 1.09
———
Zinc oxide 0.35
———
99.98
The following (A) is an analysis of a sample of South American copper ore,
which will serve as a further illustration. The analysis showed the presence
of 6.89 per cent. of ferrous oxide, and some oxide of copper.
The analysis (B) is that of an ore from the same mine after an imperfect
roasting. It will be seen that the carbonates have been converted into
sulphates. If the total sulphur simply had been determined, and the sulphate
overlooked, the "oxygen and loss" would have been 5.65 per cent., an
amount which would obviously require an explanation.
A. B.
Water 0.25 0.59
Organic matter 0.54 —
Sulphur 29.50 21.33
Copper 10.92 9.80 {Copper 9.57
{Copper oxide 0.28
Iron 32.09 39.73 {Iron 34.32
{Ferric oxide 7.73
Lead 0.35 0.12
Zinc 0.86 0.69
Cobalt 0.06 0.11
Lime 5.25 7.69
Magnesia 2.33 2.55
Sulphuric oxide 1.00 5.30
Carbon dioxide 8.87 —
"Insoluble silicates" 5.12 8.38
Oxygen and loss 2.86 2.47
———Potash 0.15
100.00 Soda 1.09
———
Page 440
100.00
WATER.
Water occurs in minerals in two forms, free and combined. The term
"moisture" ought, strictly, to be limited to the first, although, as has already
been explained, it is more convenient in assaying to apply the term to all
water which is driven off on drying at 100° C. The combined water is really
a part of the mineral itself, although it may be driven off at a high
temperature, which varies with the base. In some cases a prolonged red heat
is required; whilst with crystallised salts it is sometimes given off at the
ordinary temperatures. This latter phenomenon, known as efflorescence, is
mostly confined to artificial salts.
The determination of the combined water may often be made by simply
igniting the substance from which the moisture has been removed. The
quantity of water may be determined, either indirectly by the loss, or
directly by collecting it in a calcium chloride tube, and weighing. In some
cases, in which the loss on ignition does not give simply the proportion of
combined water, it can be seen from the analysis to what else the loss is
due; and, after a proper deduction, the amount of water can be estimated.
For example, 1 gram of crystallised iron sulphate was found to contain on
analysis 0.2877 gram of sulphuric oxide; and on igniting another gram,
0.2877 gram of ferric oxide was left. As the salt is known to be made up of
ferrous oxide, sulphuric oxide, and combined water, the combined water
can be thus calculated: 0.2877 gram of ferric oxide is equal to 0.2589 gram
of ferrous oxide,[98] and consequently, the loss on ignition has been
diminished by 0.0288 gram, which is the weight of oxygen absorbed by the
ferrous oxide during calcining. The loss on ignition was 0.7123 gram, to
which must be added 0.0288 gram; hence 0.7411 gram is the weight of the
combined sulphuric oxide and water present. Deducting the weight of
sulphuric oxide found, 0.2877 gram, there is left for combined water 0.4534
gram. The composition of 1 gram of the dry salt is then:—
Water 0.4534
Sulphuric oxide 0.2877
Ferrous oxide 0.2589
WATER.
Water occurs in minerals in two forms, free and combined. The term
"moisture" ought, strictly, to be limited to the first, although, as has already
been explained, it is more convenient in assaying to apply the term to all
water which is driven off on drying at 100° C. The combined water is really
a part of the mineral itself, although it may be driven off at a high
temperature, which varies with the base. In some cases a prolonged red heat
is required; whilst with crystallised salts it is sometimes given off at the
ordinary temperatures. This latter phenomenon, known as efflorescence, is
mostly confined to artificial salts.
The determination of the combined water may often be made by simply
igniting the substance from which the moisture has been removed. The
quantity of water may be determined, either indirectly by the loss, or
directly by collecting it in a calcium chloride tube, and weighing. In some
cases, in which the loss on ignition does not give simply the proportion of
combined water, it can be seen from the analysis to what else the loss is
due; and, after a proper deduction, the amount of water can be estimated.
For example, 1 gram of crystallised iron sulphate was found to contain on
analysis 0.2877 gram of sulphuric oxide; and on igniting another gram,
0.2877 gram of ferric oxide was left. As the salt is known to be made up of
ferrous oxide, sulphuric oxide, and combined water, the combined water
can be thus calculated: 0.2877 gram of ferric oxide is equal to 0.2589 gram
of ferrous oxide,[98] and consequently, the loss on ignition has been
diminished by 0.0288 gram, which is the weight of oxygen absorbed by the
ferrous oxide during calcining. The loss on ignition was 0.7123 gram, to
which must be added 0.0288 gram; hence 0.7411 gram is the weight of the
combined sulphuric oxide and water present. Deducting the weight of
sulphuric oxide found, 0.2877 gram, there is left for combined water 0.4534
gram. The composition of 1 gram of the dry salt is then:—
Water 0.4534
Sulphuric oxide 0.2877
Ferrous oxide 0.2589
Page 441
———
1.0000
The following is another example:—A sample of malachite lost on ignition
28.47 per cent., leaving a residue which was found on analysis to be made
up of oxide of copper (equal to 70.16 per cent. on the mineral), and silica
and oxide of iron (equal to 1.37 per cent.). Carbon dioxide and water (but
nothing else) was found to be present, and the carbon dioxide amounted to
19.64 per cent.; deducting this from the loss on ignition, we have 8.82 as
the percentage of water present. The analysis was then reported as follows:
—
Cupric oxide 70.16 equal to 56.0% copper.
Silica and ferric oxide 1.37
Carbon dioxide 19.64
Water 8.82
———
99.99
Direct Determination of Combined Water.—Transfer about 3 grams of
the substance to a piece of combustion tube (8 or 10 inches long), attached
(as in fig. 63) at one end to a U-tube containing sulphuric acid, and at the
other end to a calcium chloride tube. The last is weighed previous to the
determination. The tube should be warmed to ensure complete dryness, and
must be free from a misty appearance. Aspirate a current of air through the
apparatus, heat the mineral by means of a Bunsen burner, cautiously at first,
and afterwards to redness (if necessary). The water is driven off and
1.0000
The following is another example:—A sample of malachite lost on ignition
28.47 per cent., leaving a residue which was found on analysis to be made
up of oxide of copper (equal to 70.16 per cent. on the mineral), and silica
and oxide of iron (equal to 1.37 per cent.). Carbon dioxide and water (but
nothing else) was found to be present, and the carbon dioxide amounted to
19.64 per cent.; deducting this from the loss on ignition, we have 8.82 as
the percentage of water present. The analysis was then reported as follows:
—
Cupric oxide 70.16 equal to 56.0% copper.
Silica and ferric oxide 1.37
Carbon dioxide 19.64
Water 8.82
———
99.99
Direct Determination of Combined Water.—Transfer about 3 grams of
the substance to a piece of combustion tube (8 or 10 inches long), attached
(as in fig. 63) at one end to a U-tube containing sulphuric acid, and at the
other end to a calcium chloride tube. The last is weighed previous to the
determination. The tube should be warmed to ensure complete dryness, and
must be free from a misty appearance. Aspirate a current of air through the
apparatus, heat the mineral by means of a Bunsen burner, cautiously at first,
and afterwards to redness (if necessary). The water is driven off and
Page 442
condenses in the calcium chloride tube, which is afterwards cooled and
weighed. The increase in weight is due to the water. If the substance gives
off acid products on heating, it is previously mixed with some dry oxide of
lead or pure calcined magnesia.
EXAMINATION OF WATERS.
The assayer is occasionally called on to test water for the purpose of
ascertaining the nature and quantity of the salts contained in it, and whether
it is or is not fit for technical and drinking purposes.
In mineral districts the water is generally of exceptional character, being
more or less charged, not only with earthy salts, but also frequently with
those of the metals. Distilled water is only used by assayers in certain
exceptional cases, so that by many it would be classed among the rarer
oxides. Water of ordinary purity will do for most purposes, but the nature
and quantity of the impurities must be known.
The following determinations are of chief importance:—
Total Solids at 100° C.—Where simply the amount is required, take 100
c.c. and evaporate on the water-bath in a weighed dish; then dry in the
water-oven, and weigh.
Total Solids Ignited.—The above residue is very gently ignited (keeping
the heat well below redness), and again weighed. A larger loss than 4 or 5
parts per 100,000 on the water requires an explanation.
Chlorine.—Take 100 c.c. of the water in a porcelain dish, add 2 c.c. of a 5
per cent. solution of neutral potassic chromate, and titrate with a neutral
standard solution of nitrate of silver, made by dissolving 4.789 grams of
crystallised silver nitrate in distilled water, and diluting to 1 litre. The
addition of the nitrate of silver is continued until the yellow of the solution
assumes a reddish tint. The reaction is very sharp. Each c.c. of nitrate of
silver used is equal to 1 part by weight of chlorine in 100,000 of water. At
inland places this rarely amounts to more than 1 in 100,000; but near the sea
it may amount to 3 or 5. More than this requires explanation, and generally
indicates sewage pollution.
weighed. The increase in weight is due to the water. If the substance gives
off acid products on heating, it is previously mixed with some dry oxide of
lead or pure calcined magnesia.
EXAMINATION OF WATERS.
The assayer is occasionally called on to test water for the purpose of
ascertaining the nature and quantity of the salts contained in it, and whether
it is or is not fit for technical and drinking purposes.
In mineral districts the water is generally of exceptional character, being
more or less charged, not only with earthy salts, but also frequently with
those of the metals. Distilled water is only used by assayers in certain
exceptional cases, so that by many it would be classed among the rarer
oxides. Water of ordinary purity will do for most purposes, but the nature
and quantity of the impurities must be known.
The following determinations are of chief importance:—
Total Solids at 100° C.—Where simply the amount is required, take 100
c.c. and evaporate on the water-bath in a weighed dish; then dry in the
water-oven, and weigh.
Total Solids Ignited.—The above residue is very gently ignited (keeping
the heat well below redness), and again weighed. A larger loss than 4 or 5
parts per 100,000 on the water requires an explanation.
Chlorine.—Take 100 c.c. of the water in a porcelain dish, add 2 c.c. of a 5
per cent. solution of neutral potassic chromate, and titrate with a neutral
standard solution of nitrate of silver, made by dissolving 4.789 grams of
crystallised silver nitrate in distilled water, and diluting to 1 litre. The
addition of the nitrate of silver is continued until the yellow of the solution
assumes a reddish tint. The reaction is very sharp. Each c.c. of nitrate of
silver used is equal to 1 part by weight of chlorine in 100,000 of water. At
inland places this rarely amounts to more than 1 in 100,000; but near the sea
it may amount to 3 or 5. More than this requires explanation, and generally
indicates sewage pollution.
Page 443
Nitric Pentoxide (N2O5).—It is more generally reported under the heading,
"nitrogen as nitrates." Take 250 c.c. of the water and evaporate to 2 or 3
c.c.; acidulate with a few drops of dilute sulphuric acid, and transfer to a
nitrometer (using strong sulphuric acid to wash in the last traces). The
sulphuric acid must be added to at least twice the bulk of the liquid. Shake
up with mercury. The mercury rapidly flours, and nitric oxide is given off
(if any nitrate is present). The volume of the nitric oxide (corrected to
normal temperature and pressure), multiplied by 0.25, gives the parts of
nitrogen per 100,000; or, multiplied by 0.965, will give the nitric pentoxide
in parts per 100,000. In well and spring waters the nitrogen may amount to
0.3 or 0.4 parts per 100,000; or in richly cultivated districts 0.7 or 0.8 parts
per 100,000. An excess of nitrates is a suspicious feature, and is generally
due to previous contamination.
Ammonia.—Take 500 c.c. of the water and place them in a retort
connected with a Liebig's condenser. Add a drop or two of a solution of
carbonate of soda and distil over 100 c.c.; collect another 50 c.c. separately.
Determine the ammonia in the distillate colorimetrically (with Nessler's
solution, as described under Ammonia) and compare with a standard
solution of ammonic chloride containing 0.0315 gram of ammonic chloride
in 1 litre of water. One c.c. contains 0.01 milligram of ammonia. The
second distillate will show little, if any, ammonia in ordinary cases. The
amounts found in both distillates are added together, and expressed in parts
per 100,000.
Waters (other than rain and tank waters) which contain more than 0.003 per
100,000 are suspicious.
Organic Matter.—The organic matter cannot be determined directly; but
for ordinary purposes it may be measured by the amount of permanganate
of potassium which it reduces, or by the amount of ammonia which it
evolves on boiling with an alkaline permanganate of potassium solution.
A. Albuminoid Ammonia.—To the residue left after distilling the ammonia
add 50 c.c. of a solution made by dissolving 200 grams of potash and 8
grams of potassium permanganate in 1100 c.c. of water, and rapidly boiling
till the volume is reduced to 1 litre (this should be kept in a well stoppered
bottle, and be occasionally tested to see that it is free from ammonia).
"nitrogen as nitrates." Take 250 c.c. of the water and evaporate to 2 or 3
c.c.; acidulate with a few drops of dilute sulphuric acid, and transfer to a
nitrometer (using strong sulphuric acid to wash in the last traces). The
sulphuric acid must be added to at least twice the bulk of the liquid. Shake
up with mercury. The mercury rapidly flours, and nitric oxide is given off
(if any nitrate is present). The volume of the nitric oxide (corrected to
normal temperature and pressure), multiplied by 0.25, gives the parts of
nitrogen per 100,000; or, multiplied by 0.965, will give the nitric pentoxide
in parts per 100,000. In well and spring waters the nitrogen may amount to
0.3 or 0.4 parts per 100,000; or in richly cultivated districts 0.7 or 0.8 parts
per 100,000. An excess of nitrates is a suspicious feature, and is generally
due to previous contamination.
Ammonia.—Take 500 c.c. of the water and place them in a retort
connected with a Liebig's condenser. Add a drop or two of a solution of
carbonate of soda and distil over 100 c.c.; collect another 50 c.c. separately.
Determine the ammonia in the distillate colorimetrically (with Nessler's
solution, as described under Ammonia) and compare with a standard
solution of ammonic chloride containing 0.0315 gram of ammonic chloride
in 1 litre of water. One c.c. contains 0.01 milligram of ammonia. The
second distillate will show little, if any, ammonia in ordinary cases. The
amounts found in both distillates are added together, and expressed in parts
per 100,000.
Waters (other than rain and tank waters) which contain more than 0.003 per
100,000 are suspicious.
Organic Matter.—The organic matter cannot be determined directly; but
for ordinary purposes it may be measured by the amount of permanganate
of potassium which it reduces, or by the amount of ammonia which it
evolves on boiling with an alkaline permanganate of potassium solution.
A. Albuminoid Ammonia.—To the residue left after distilling the ammonia
add 50 c.c. of a solution made by dissolving 200 grams of potash and 8
grams of potassium permanganate in 1100 c.c. of water, and rapidly boiling
till the volume is reduced to 1 litre (this should be kept in a well stoppered
bottle, and be occasionally tested to see that it is free from ammonia).
Page 444
Continue the distillation, collecting 50 c.c. at a time, until the distillate is
free from ammonia. Three or four fractions are generally sufficient.
Determine the ammonia colorimetrically as before. If the total albuminoid
ammonia does not exceed 0.005 in 100,000, the water may be regarded as
clean as regards organic matter; if it amounts to more than 0.015, it is dirty.
B. Oxygen Consumed.—A standard solution of permanganate of potash is
made by dissolving 0.395 gram of the salt in water and diluting to 1 litre.
Each c.c. equals 0.1 milligram of available oxygen. The following are also
required:—1. A solution of sodium hyposulphite containing 1 gram of the
salt (Na2S2O3.5H2O) in 1 litre of water. 2. Dilute sulphuric acid, made by
adding one part of the acid to three of water, and titrating with the
permanganate solution till a faint pink persists after warming for several
hours. 3. Starch paste. 4. Potassium iodide solution.
Take 250 c.c. of the water in a stoppered bottle, add 10 c.c. of sulphuric acid
and 10 c.c. of the permanganate, and allow to stand in a warm place for four
hours. Then add a few drops of the solution of potassium iodide, and titrate
the liberated iodine with "hypo," using starch paste towards the end as an
indicator. To standardise the hyposulphite, take 250 c.c. of water and 10 c.c.
of sulphuric acid, and a few drops of potassium iodide; then run in 10 c.c.
of the "permanganate" solution, and again titrate; about 30 c.c. of the
"hypo" will be used. The difference in the two titrations, divided by the last
and multiplied by 10, will give the c.c. of permanganate solution used in
oxidising the organic matter in the 250 c.c. of water. Each c.c. represents
0.04 parts of oxygen in 100,000.
Metals.—These may for the most part be estimated colorimetrically.
Lead.—Take 100 c.c. of the water in a Nessler tube, and add 10 c.c. of
sulphuretted hydrogen water, and compare the tint, if any, against a standard
lead solution, as described under Colorimetric Lead. Report in parts per
100,000.
Copper.—Proceed as with the last-mentioned metal; but, if lead is also
present, boil down 500 c.c. to about 50 c.c., then add ammonia, filter, and
estimate the copper in the blue solution, as described under Colorimetric
Copper.
free from ammonia. Three or four fractions are generally sufficient.
Determine the ammonia colorimetrically as before. If the total albuminoid
ammonia does not exceed 0.005 in 100,000, the water may be regarded as
clean as regards organic matter; if it amounts to more than 0.015, it is dirty.
B. Oxygen Consumed.—A standard solution of permanganate of potash is
made by dissolving 0.395 gram of the salt in water and diluting to 1 litre.
Each c.c. equals 0.1 milligram of available oxygen. The following are also
required:—1. A solution of sodium hyposulphite containing 1 gram of the
salt (Na2S2O3.5H2O) in 1 litre of water. 2. Dilute sulphuric acid, made by
adding one part of the acid to three of water, and titrating with the
permanganate solution till a faint pink persists after warming for several
hours. 3. Starch paste. 4. Potassium iodide solution.
Take 250 c.c. of the water in a stoppered bottle, add 10 c.c. of sulphuric acid
and 10 c.c. of the permanganate, and allow to stand in a warm place for four
hours. Then add a few drops of the solution of potassium iodide, and titrate
the liberated iodine with "hypo," using starch paste towards the end as an
indicator. To standardise the hyposulphite, take 250 c.c. of water and 10 c.c.
of sulphuric acid, and a few drops of potassium iodide; then run in 10 c.c.
of the "permanganate" solution, and again titrate; about 30 c.c. of the
"hypo" will be used. The difference in the two titrations, divided by the last
and multiplied by 10, will give the c.c. of permanganate solution used in
oxidising the organic matter in the 250 c.c. of water. Each c.c. represents
0.04 parts of oxygen in 100,000.
Metals.—These may for the most part be estimated colorimetrically.
Lead.—Take 100 c.c. of the water in a Nessler tube, and add 10 c.c. of
sulphuretted hydrogen water, and compare the tint, if any, against a standard
lead solution, as described under Colorimetric Lead. Report in parts per
100,000.
Copper.—Proceed as with the last-mentioned metal; but, if lead is also
present, boil down 500 c.c. to about 50 c.c., then add ammonia, filter, and
estimate the copper in the blue solution, as described under Colorimetric
Copper.
Page 445
Iron.—Take 50 c.c., or a smaller quantity (if necessary), dilute up to the
mark with distilled water, and determine with potassium sulphocyanate, as
described under Colorimetric Iron.
Zinc.—Zinc is the only other metal likely to be present; and, since it cannot
be determined colorimetrically, it must be separately estimated during the
examination of the "total solids."
Examination of "Total Solids."—Evaporate 500 c.c. to dryness with a
drop or two of hydrochloric acid. Take up with hydrochloric acid, filter,
ignite, and weigh the residue as "silica." To the filtrate add a little ammonic
chloride and ammonia, boil and filter, ignite, and weigh the precipitate as
"oxide of iron and alumina." Collect the filtrate in a small flask, add a few
drops of ammonium sulphide or pass sulphuretted hydrogen, cork the flask,
and allow to stand overnight; filter, wash, and determine the zinc
gravimetrically as oxide of zinc. If copper or lead were present, they should
have been previously removed with sulphuretted hydrogen in the acid
solution. To the filtrate add ammonic oxalate and ammonia, boil for some
time, allow to stand, filter, wash, ignite, and weigh as "lime." Evaporate the
filtrate with nitric acid, and ignite. Take up with a few drops of dilute
hydrochloric acid, add baric hydrate in excess, evaporate, and extract with
water. The residue contains the magnesia; boil with dilute sulphuric acid,
filter, precipitate it with phosphate of soda and ammonia, and weigh as
pyrophosphate. The aqueous extract contains the alkalies with the excess of
barium. Add sulphuric acid in slight excess, filter, evaporate, and ignite
strongly. The residue consists of the sulphates of the alkalies (which are
separately determined, as described under Potash).
Sulphuric Oxide (SO3).—Take 200 c.c. and boil to a small bulk with a
little hydrochloric acid, filter (if necessary), add baric chloride solution in
slight excess to the hot solution, filter, ignite, and weigh as baric sulphate.
Carbon Dioxide (free).—Carbon dioxide exists in waters in two forms,
free and combined. The latter generally occurs as bicarbonate, although on
analysis it is more convenient to consider it as carbonate, and to count the
excess of carbon dioxide with the free. The method is as follows:—To
determine the free carbon dioxide, take 100 c.c. of the water, place them in
a flask with 3 c.c. of a strong solution of calcium chloride and 2 c.c. of a
mark with distilled water, and determine with potassium sulphocyanate, as
described under Colorimetric Iron.
Zinc.—Zinc is the only other metal likely to be present; and, since it cannot
be determined colorimetrically, it must be separately estimated during the
examination of the "total solids."
Examination of "Total Solids."—Evaporate 500 c.c. to dryness with a
drop or two of hydrochloric acid. Take up with hydrochloric acid, filter,
ignite, and weigh the residue as "silica." To the filtrate add a little ammonic
chloride and ammonia, boil and filter, ignite, and weigh the precipitate as
"oxide of iron and alumina." Collect the filtrate in a small flask, add a few
drops of ammonium sulphide or pass sulphuretted hydrogen, cork the flask,
and allow to stand overnight; filter, wash, and determine the zinc
gravimetrically as oxide of zinc. If copper or lead were present, they should
have been previously removed with sulphuretted hydrogen in the acid
solution. To the filtrate add ammonic oxalate and ammonia, boil for some
time, allow to stand, filter, wash, ignite, and weigh as "lime." Evaporate the
filtrate with nitric acid, and ignite. Take up with a few drops of dilute
hydrochloric acid, add baric hydrate in excess, evaporate, and extract with
water. The residue contains the magnesia; boil with dilute sulphuric acid,
filter, precipitate it with phosphate of soda and ammonia, and weigh as
pyrophosphate. The aqueous extract contains the alkalies with the excess of
barium. Add sulphuric acid in slight excess, filter, evaporate, and ignite
strongly. The residue consists of the sulphates of the alkalies (which are
separately determined, as described under Potash).
Sulphuric Oxide (SO3).—Take 200 c.c. and boil to a small bulk with a
little hydrochloric acid, filter (if necessary), add baric chloride solution in
slight excess to the hot solution, filter, ignite, and weigh as baric sulphate.
Carbon Dioxide (free).—Carbon dioxide exists in waters in two forms,
free and combined. The latter generally occurs as bicarbonate, although on
analysis it is more convenient to consider it as carbonate, and to count the
excess of carbon dioxide with the free. The method is as follows:—To
determine the free carbon dioxide, take 100 c.c. of the water, place them in
a flask with 3 c.c. of a strong solution of calcium chloride and 2 c.c. of a
Page 446
solution of ammonic chloride, next add 50 c.c. of lime-water. The strength
of the lime-water must be known. Make up to 200 c.c. with distilled water,
stop the flask, and allow the precipitate to settle. Take out 100 c.c. of the
clear solution with a pipette, and titrate with the standard solution of acid.
[99]
The number of c.c. required, multiplied by two, and deducted from that
required for the 50 c.c. of lime-water, and then multiplied by 0.0045, will
give the carbon dioxide present other than as normal carbonates.
Carbon Dioxide combined as normal carbonate.—100 c.c. of the water are
tinted with phenacetolin or lacmoid; then heated to near boiling, and titrated
with standard acid. The number of c.c. used, multiplied by 0.0045, will give
the weight in grams of the combined carbon dioxide.
Free Acid.—In some waters (especially those from mining districts) there
will be no carbonates. On the contrary, there may be free mineral acid or
acid salts. In these cases it is necessary to determine the amount of acid
(other than carbon dioxide) present in excess of that required to form
normal salts. This is done in the following way:—Make an ammoniacal
copper solution by taking 13 grams of copper sulphate (CuSO4.5H2O),
dissolving in water, adding solution of ammonia until the precipitate first
formed has nearly dissolved, and diluting to 1 litre. Allow to settle, and
decant off the clear liquid. The strength of this solution is determined by
titrating against 10 or 20 c.c. of the standard solution of sulphuric acid (100
c.c. = 1 gram H2SO4). The finishing point is reached as soon as the solution
becomes turbid from precipitated cupric hydrate. At first, as each drop falls
into the acid solution, the ammonia and cupric hydrate combine with the
free acid to form ammonic and cupric sulphates; but as soon as the free acid
is used up, the ammonia in the next drop not only precipitates an equivalent
of cupric hydrate from the solution, but also throws down that carried by
itself. This method is applicable in the presence of metallic sulphates other
than ferric. The standardising and titration should be made under the same
conditions. Since sulphuric acid and sulphates are predominant in waters of
this kind, it is most convenient to report the acidity of the water as
equivalent to so much sulphuric acid.
Dissolved Oxygen.—For the gasometric method of analysing for dissolved
oxygen, and for the Schützenberger's volumetric method, the student is
referred to Sutton's "Volumetric Analysis." The following is an easy method
of the lime-water must be known. Make up to 200 c.c. with distilled water,
stop the flask, and allow the precipitate to settle. Take out 100 c.c. of the
clear solution with a pipette, and titrate with the standard solution of acid.
[99]
The number of c.c. required, multiplied by two, and deducted from that
required for the 50 c.c. of lime-water, and then multiplied by 0.0045, will
give the carbon dioxide present other than as normal carbonates.
Carbon Dioxide combined as normal carbonate.—100 c.c. of the water are
tinted with phenacetolin or lacmoid; then heated to near boiling, and titrated
with standard acid. The number of c.c. used, multiplied by 0.0045, will give
the weight in grams of the combined carbon dioxide.
Free Acid.—In some waters (especially those from mining districts) there
will be no carbonates. On the contrary, there may be free mineral acid or
acid salts. In these cases it is necessary to determine the amount of acid
(other than carbon dioxide) present in excess of that required to form
normal salts. This is done in the following way:—Make an ammoniacal
copper solution by taking 13 grams of copper sulphate (CuSO4.5H2O),
dissolving in water, adding solution of ammonia until the precipitate first
formed has nearly dissolved, and diluting to 1 litre. Allow to settle, and
decant off the clear liquid. The strength of this solution is determined by
titrating against 10 or 20 c.c. of the standard solution of sulphuric acid (100
c.c. = 1 gram H2SO4). The finishing point is reached as soon as the solution
becomes turbid from precipitated cupric hydrate. At first, as each drop falls
into the acid solution, the ammonia and cupric hydrate combine with the
free acid to form ammonic and cupric sulphates; but as soon as the free acid
is used up, the ammonia in the next drop not only precipitates an equivalent
of cupric hydrate from the solution, but also throws down that carried by
itself. This method is applicable in the presence of metallic sulphates other
than ferric. The standardising and titration should be made under the same
conditions. Since sulphuric acid and sulphates are predominant in waters of
this kind, it is most convenient to report the acidity of the water as
equivalent to so much sulphuric acid.
Dissolved Oxygen.—For the gasometric method of analysing for dissolved
oxygen, and for the Schützenberger's volumetric method, the student is
referred to Sutton's "Volumetric Analysis." The following is an easy method
Page 447
of estimating the free oxygen in a water:—Take 20 c.c. of a stannous
chloride solution (about 20 grams of the salt with 10 c.c. of hydrochloric
acid to the litre); add 10 c.c. of hydrochloric acid, and titrate in an
atmosphere of carbon dioxide with standard permanganate of potassium
solution (made by dissolving 1.975 gram of the salt in 1 litre of water: 1 c.c.
equals 0.5 milligram of oxygen). A similar titration is made with the
addition of 100 c.c. of the water to be tested. Less permanganate will be
required in the second titration, according to the amount of oxygen in the
water; and the difference, multiplied by 0.5, will give the weight of the
oxygen in milligrams. Small quantities of nitrates do not interfere.
In reporting the results of the analysis, it is customary to combine the acids
and bases found on some such principle as the following:—The sulphuric
oxide is calculated as combined with the potash, and reported as potassic
sulphate (K2SO4); the balance of the sulphuric oxide is then apportioned to
the soda, and reported as sulphate of soda (Na2SO4); if any is still left, it is
reported as calcium sulphate (CaSO4), and after that as magnesic sulphate
(MgSO4). When the sulphuric oxide has been satisfied, the chlorine is
distributed, taking the bases in the same order, then the nitric pentoxide, and
lastly the carbon dioxide. But any method for thus combining the bases and
acids must be arbitrary and inaccurate. It is extremely improbable that any
simple statement can represent the manner in which the bases and acids are
distributed whilst in solution; and, since different chemists are not agreed as
to any one system, it is better to give up the attempt, and simply state the
results of the analysis. This has only one inconvenience. The bases are
represented as oxides; and, since some of them are present as chlorides, the
sum total of the analysis will be in excess of the actual amount present by
the weight of the oxygen equivalent to the chlorine present as chloride. The
following is an example of such a statement:—
Parts per 100,000.
Total solids, dried at 100° C. 28.73
Chlorine 1.70
Nitrogen as nitrate 0.03
Ammonia 0.001
Albuminoid ammonia 0.004
chloride solution (about 20 grams of the salt with 10 c.c. of hydrochloric
acid to the litre); add 10 c.c. of hydrochloric acid, and titrate in an
atmosphere of carbon dioxide with standard permanganate of potassium
solution (made by dissolving 1.975 gram of the salt in 1 litre of water: 1 c.c.
equals 0.5 milligram of oxygen). A similar titration is made with the
addition of 100 c.c. of the water to be tested. Less permanganate will be
required in the second titration, according to the amount of oxygen in the
water; and the difference, multiplied by 0.5, will give the weight of the
oxygen in milligrams. Small quantities of nitrates do not interfere.
In reporting the results of the analysis, it is customary to combine the acids
and bases found on some such principle as the following:—The sulphuric
oxide is calculated as combined with the potash, and reported as potassic
sulphate (K2SO4); the balance of the sulphuric oxide is then apportioned to
the soda, and reported as sulphate of soda (Na2SO4); if any is still left, it is
reported as calcium sulphate (CaSO4), and after that as magnesic sulphate
(MgSO4). When the sulphuric oxide has been satisfied, the chlorine is
distributed, taking the bases in the same order, then the nitric pentoxide, and
lastly the carbon dioxide. But any method for thus combining the bases and
acids must be arbitrary and inaccurate. It is extremely improbable that any
simple statement can represent the manner in which the bases and acids are
distributed whilst in solution; and, since different chemists are not agreed as
to any one system, it is better to give up the attempt, and simply state the
results of the analysis. This has only one inconvenience. The bases are
represented as oxides; and, since some of them are present as chlorides, the
sum total of the analysis will be in excess of the actual amount present by
the weight of the oxygen equivalent to the chlorine present as chloride. The
following is an example of such a statement:—
Parts per 100,000.
Total solids, dried at 100° C. 28.73
Chlorine 1.70
Nitrogen as nitrate 0.03
Ammonia 0.001
Albuminoid ammonia 0.004
Page 448
"Oxygen consumed" in 4 hours 0.01
The solids were made up as under:—
Per 100,000 of the Water.
Potash 0.38
Soda 2.01
Magnesia 1.44
Lime 10.55
Ferric oxide 0.01
Silica 0.30
Sulphuric oxide 3.69
Nitrogen pentoxide 0.11
Carbon dioxide 8.38
Chlorine 1.70
Volatile and organic matter 0.66
———
29.23
Less oxygen equivalent to chlorine found 0.39
———
28.84
For the preparation of distilled water, the apparatus shown in fig. 64 is
convenient for laboratory use. It consists of a copper retort heated by a ring
gas-burner, and connected with a worm-condenser.
The solids were made up as under:—
Per 100,000 of the Water.
Potash 0.38
Soda 2.01
Magnesia 1.44
Lime 10.55
Ferric oxide 0.01
Silica 0.30
Sulphuric oxide 3.69
Nitrogen pentoxide 0.11
Carbon dioxide 8.38
Chlorine 1.70
Volatile and organic matter 0.66
———
29.23
Less oxygen equivalent to chlorine found 0.39
———
28.84
For the preparation of distilled water, the apparatus shown in fig. 64 is
convenient for laboratory use. It consists of a copper retort heated by a ring
gas-burner, and connected with a worm-condenser.
Page 449
PRACTICAL EXERCISE.
A mineral, on analysis, gave the following results:—Water, 44.94 per cent.;
sulphuric oxide, 28.72 per cent.; ferrous iron, 13.92 per cent.; ferric iron,
0.35 per cent.; copper, 6.1 per cent. The mineral was soluble in water, and
showed nothing else on testing. How would you report the analysis?
Calculate the formula for the salt.
THE HALOGENS.
There is a group of closely allied elements to which the name halogen (salt-
producer) has been given. It comprises chlorine, bromine, iodine, and
fluorine. These elements combine directly with metals, forming as many
series of salts (chlorides, bromides, iodides, and fluorides), corresponding
to the respective oxides, but differing in their formulæ by having two atoms
of the halogen in the place of one atom of oxygen. For example, ferrous
oxide is FeO and ferrous chloride is FeCl2, and, again, ferric oxide is
Fe2O3, whilst ferric chloride is Fe2Cl6. These salts differ from the
carbonates, nitrates, &c., in containing no oxygen. Consequently, it is
incorrect to speak of such compounds as chloride of potash, fluoride of
lime, &c., since potash and lime are oxides. It is important to bear this in
mind in reporting analyses in which determinations have been made, say, of
A mineral, on analysis, gave the following results:—Water, 44.94 per cent.;
sulphuric oxide, 28.72 per cent.; ferrous iron, 13.92 per cent.; ferric iron,
0.35 per cent.; copper, 6.1 per cent. The mineral was soluble in water, and
showed nothing else on testing. How would you report the analysis?
Calculate the formula for the salt.
THE HALOGENS.
There is a group of closely allied elements to which the name halogen (salt-
producer) has been given. It comprises chlorine, bromine, iodine, and
fluorine. These elements combine directly with metals, forming as many
series of salts (chlorides, bromides, iodides, and fluorides), corresponding
to the respective oxides, but differing in their formulæ by having two atoms
of the halogen in the place of one atom of oxygen. For example, ferrous
oxide is FeO and ferrous chloride is FeCl2, and, again, ferric oxide is
Fe2O3, whilst ferric chloride is Fe2Cl6. These salts differ from the
carbonates, nitrates, &c., in containing no oxygen. Consequently, it is
incorrect to speak of such compounds as chloride of potash, fluoride of
lime, &c., since potash and lime are oxides. It is important to bear this in
mind in reporting analyses in which determinations have been made, say, of
Page 450
chlorine, magnesia, and potash, or of fluorine, silica, and alumina. It is
necessary in all such cases to deduct from the total an amount of oxygen
equivalent to the halogen found, except, of course, where the base has been
determined and recorded as metal. Compounds containing oxides and
fluorides, &c., do not lend themselves to the method of determining the
halogen by difference. For example, topaz, which, according to Dana, has
the formula Al2SiO4F2, would yield in the ordinary course of analysis—
Alumina 55.4%
Silica 32.6
Fluorine 20.6
———
108.6
The oxygen equivalent to 20.6 per cent. fluorine may be found by
multiplying the percentage of fluorine by 0.421; it is 8.7 per cent., and must
be deducted. The analysis would then be reported thus:—
Alumina 55.4%
Silica 32.6
Fluorine 20.6
———
108.6
Less oxygen equivalent to fluorine 8.7
———
99.9
Take as an illustration the following actual analysis by F.W. Clarke and J.S.
Diller:—
Alumina 57.38%
Silica 31.92
Fluorine 16.99
Potash 0.15
Soda 1.33
Water 0.20
necessary in all such cases to deduct from the total an amount of oxygen
equivalent to the halogen found, except, of course, where the base has been
determined and recorded as metal. Compounds containing oxides and
fluorides, &c., do not lend themselves to the method of determining the
halogen by difference. For example, topaz, which, according to Dana, has
the formula Al2SiO4F2, would yield in the ordinary course of analysis—
Alumina 55.4%
Silica 32.6
Fluorine 20.6
———
108.6
The oxygen equivalent to 20.6 per cent. fluorine may be found by
multiplying the percentage of fluorine by 0.421; it is 8.7 per cent., and must
be deducted. The analysis would then be reported thus:—
Alumina 55.4%
Silica 32.6
Fluorine 20.6
———
108.6
Less oxygen equivalent to fluorine 8.7
———
99.9
Take as an illustration the following actual analysis by F.W. Clarke and J.S.
Diller:—
Alumina 57.38%
Silica 31.92
Fluorine 16.99
Potash 0.15
Soda 1.33
Water 0.20
Page 451
———
107.97
Deduct oxygen equivalent 7.16
———
100.81
In calculating the factor for the "oxygen equivalent," divide the weight of
one atom of oxygen (16) by the weight of two atoms of the halogen; for
example, with chlorine it would be 16/71 or 0.2253; with bromine, 16/160
or 0.1000; with iodine, 16/254 or 0.063; and with fluorine, 16/38 or 0.421.
CHLORINE AND CHLORIDES.
Chlorine occurs in nature chiefly combined with sodium, as halite or rock
salt (NaCl). With potassium it forms sylvine (KCl), and, together with
magnesium, carnallite (KCl.MgCl2.6H2O). Of the metalliferous minerals
containing chlorine, kerargyrite, or horn silver (AgCl), and atacamite, an
oxychloride of copper (CuCl2.3Cu(HO)2.) are the most important. Apatite
(phosphate of lime) and pyromorphite (phosphate of lead) contain a
considerable amount of it. Chlorine is a gas of a greenish colour, possessing
a characteristic odour, and moderately soluble in water. It does not occur
native, and is generally prepared by the action of an oxidising agent on
hydrochloric acid. It combines directly with metals at the ordinary
temperature (even with platinum and gold), forming chlorides, which
(except in the case of silver) are soluble.
It is important in metallurgy, because of the extensive use of it in extracting
gold by "chloridising" processes. It is also used in refining gold.
Detection.—Compounds containing the oxides of chlorine are not found in
nature, because of the readiness with which they lose oxygen. By reduction
they yield a chloride; the form in which chlorine is met with in minerals. In
testing, the compound supposed to contain a chloride is boiled with water,
or, in some cases, dilute nitric acid. To the clear solution containing nitric
acid a few drops of nitrate of silver solution are added. If, on shaking, a
white curdy precipitate, soluble in ammonia, separates out, it is sufficiently
satisfactory evidence of the presence of chlorides.
107.97
Deduct oxygen equivalent 7.16
———
100.81
In calculating the factor for the "oxygen equivalent," divide the weight of
one atom of oxygen (16) by the weight of two atoms of the halogen; for
example, with chlorine it would be 16/71 or 0.2253; with bromine, 16/160
or 0.1000; with iodine, 16/254 or 0.063; and with fluorine, 16/38 or 0.421.
CHLORINE AND CHLORIDES.
Chlorine occurs in nature chiefly combined with sodium, as halite or rock
salt (NaCl). With potassium it forms sylvine (KCl), and, together with
magnesium, carnallite (KCl.MgCl2.6H2O). Of the metalliferous minerals
containing chlorine, kerargyrite, or horn silver (AgCl), and atacamite, an
oxychloride of copper (CuCl2.3Cu(HO)2.) are the most important. Apatite
(phosphate of lime) and pyromorphite (phosphate of lead) contain a
considerable amount of it. Chlorine is a gas of a greenish colour, possessing
a characteristic odour, and moderately soluble in water. It does not occur
native, and is generally prepared by the action of an oxidising agent on
hydrochloric acid. It combines directly with metals at the ordinary
temperature (even with platinum and gold), forming chlorides, which
(except in the case of silver) are soluble.
It is important in metallurgy, because of the extensive use of it in extracting
gold by "chloridising" processes. It is also used in refining gold.
Detection.—Compounds containing the oxides of chlorine are not found in
nature, because of the readiness with which they lose oxygen. By reduction
they yield a chloride; the form in which chlorine is met with in minerals. In
testing, the compound supposed to contain a chloride is boiled with water,
or, in some cases, dilute nitric acid. To the clear solution containing nitric
acid a few drops of nitrate of silver solution are added. If, on shaking, a
white curdy precipitate, soluble in ammonia, separates out, it is sufficiently
satisfactory evidence of the presence of chlorides.
Page 452
Solution and Separation.—The chlorides are generally soluble in water,
and are got into solution by extracting with warm dilute nitric acid. Or, if
insoluble, the substance is fused with carbonate of soda, extracted with
water, and the filtrate acidified with nitric acid. For the determination, it is
not necessary to obtain the solution of the chloride free from other acids or
metals. If tin, antimony, mercury, or platinum is present, it is best to
separate by means of sulphuretted hydrogen. The chloride is determined in
the solution after removal of the excess of the gas. Where traces of
chlorides are being looked for, a blank experiment is made to determine the
quantity introduced with the reagents. One hundred c.c. of ordinary water
contains from 1 to 3 milligrams of chlorine. On the addition of nitrate of
silver to the nitric acid solution, chloride of silver separates out. This is free
from other substances, except, perhaps, bromide and iodide.
GRAVIMETRIC DETERMINATION.
Freely mix the solution containing the chloride with dilute nitric acid, filter
(if necessary), and treat with nitrate of silver. Heat nearly to boiling, and,
when the precipitate has settled, filter, and wash with hot distilled water.
Dry, and transfer to a weighed Berlin crucible. Burn the filter-paper
separately, and convert any reduced silver into chloride by alternate
treatment with drops of nitric and of hydrochloric acid. Add the main
portion to this, and heat cautiously till the edges of the mass show signs of
fusing (about 260°). Cool in the desiccator and weigh. The substance is
chloride of silver (AgCl), and contains 24.73 per cent. of chlorine.
The precipitated chloride is filtered and washed as soon as possible after
settling, since on exposure to light it becomes purple, and loses a small
amount of chlorine.
VOLUMETRIC METHOD.
There are several volumetric methods; but that based on the precipitation of
silver chloride in neutral solution, by means of a standard solution of silver
nitrate (using potassium chromate as indicator), is preferred. Silver
chromate is a red-coloured salt; and, when silver nitrate is added to a
solution containing both chloride and chromate, the development of the red
and are got into solution by extracting with warm dilute nitric acid. Or, if
insoluble, the substance is fused with carbonate of soda, extracted with
water, and the filtrate acidified with nitric acid. For the determination, it is
not necessary to obtain the solution of the chloride free from other acids or
metals. If tin, antimony, mercury, or platinum is present, it is best to
separate by means of sulphuretted hydrogen. The chloride is determined in
the solution after removal of the excess of the gas. Where traces of
chlorides are being looked for, a blank experiment is made to determine the
quantity introduced with the reagents. One hundred c.c. of ordinary water
contains from 1 to 3 milligrams of chlorine. On the addition of nitrate of
silver to the nitric acid solution, chloride of silver separates out. This is free
from other substances, except, perhaps, bromide and iodide.
GRAVIMETRIC DETERMINATION.
Freely mix the solution containing the chloride with dilute nitric acid, filter
(if necessary), and treat with nitrate of silver. Heat nearly to boiling, and,
when the precipitate has settled, filter, and wash with hot distilled water.
Dry, and transfer to a weighed Berlin crucible. Burn the filter-paper
separately, and convert any reduced silver into chloride by alternate
treatment with drops of nitric and of hydrochloric acid. Add the main
portion to this, and heat cautiously till the edges of the mass show signs of
fusing (about 260°). Cool in the desiccator and weigh. The substance is
chloride of silver (AgCl), and contains 24.73 per cent. of chlorine.
The precipitated chloride is filtered and washed as soon as possible after
settling, since on exposure to light it becomes purple, and loses a small
amount of chlorine.
VOLUMETRIC METHOD.
There are several volumetric methods; but that based on the precipitation of
silver chloride in neutral solution, by means of a standard solution of silver
nitrate (using potassium chromate as indicator), is preferred. Silver
chromate is a red-coloured salt; and, when silver nitrate is added to a
solution containing both chloride and chromate, the development of the red
Page 453
colour marks off sharply the point at which the chloride is used up. Silver
chromate is decomposed and consequently decolorised by solution of any
chloride. The solution for this method must be neutral, since free acid
prevents the formation of the red silver chromate. If not already neutral, it is
neutralised by titrating cautiously with a solution of soda. In a neutral
solution, other substances (such as phosphates and arsenates) also yield a
precipitate with a solution of nitrate of silver; and will count as chloride if
they are not removed.
The Standard Solution of Nitrate of Silver is made by dissolving 23.94
grams of the salt (AgNO3) in distilled water, and diluting to 1 litre; 100 c.c.
are equal to 0.5 gram of chlorine.
The indicator is made by adding silver nitrate to a strong neutral solution of
yellow chromate of potash (K2CrO4), till a permanent red precipitate is
formed. The solution is allowed to settle, and the clear liquid decanted into
a stoppered bottle labelled "chromate indicator for chlorine."
Standardise the silver nitrate by weighing up 0.5 gram of pure sodium
chloride (or potassium chloride). Transfer to a flask and dissolve in distilled
water; dilute to 100 c.c. Fill an ordinary burette with the standard silver
solution, and (after adjusting) run into the flask a quantity sufficient to
throw down the greater part of the chlorine. Add a few drops of the
chromate indicator and continue the addition of the silver nitrate until the
yellow colour of the solution becomes permanently tinted red, after
shaking. This shows that the chlorine is all precipitated, and that the
chromate is beginning to come down. The further addition of a couple of
drops of the silver solution will cause a marked difference in the tint. Read
off the quantity run in, and calculate the standard. One gram of sodium
chloride contains 0.6062 gram of chlorine; and 1 gram of potassium
chloride contains 0.4754 gram.
For the determination of small quantities of chloride (a few milligrams), the
same method is used; but the standard solution is diluted so that each c.c. is
equal to 1 milligram of chlorine; and the chromate indicator is added before
titrating. The standard solution is made by measuring off 200 c.c. of the
solution described above, and diluting with distilled water to 1 litre.
chromate is decomposed and consequently decolorised by solution of any
chloride. The solution for this method must be neutral, since free acid
prevents the formation of the red silver chromate. If not already neutral, it is
neutralised by titrating cautiously with a solution of soda. In a neutral
solution, other substances (such as phosphates and arsenates) also yield a
precipitate with a solution of nitrate of silver; and will count as chloride if
they are not removed.
The Standard Solution of Nitrate of Silver is made by dissolving 23.94
grams of the salt (AgNO3) in distilled water, and diluting to 1 litre; 100 c.c.
are equal to 0.5 gram of chlorine.
The indicator is made by adding silver nitrate to a strong neutral solution of
yellow chromate of potash (K2CrO4), till a permanent red precipitate is
formed. The solution is allowed to settle, and the clear liquid decanted into
a stoppered bottle labelled "chromate indicator for chlorine."
Standardise the silver nitrate by weighing up 0.5 gram of pure sodium
chloride (or potassium chloride). Transfer to a flask and dissolve in distilled
water; dilute to 100 c.c. Fill an ordinary burette with the standard silver
solution, and (after adjusting) run into the flask a quantity sufficient to
throw down the greater part of the chlorine. Add a few drops of the
chromate indicator and continue the addition of the silver nitrate until the
yellow colour of the solution becomes permanently tinted red, after
shaking. This shows that the chlorine is all precipitated, and that the
chromate is beginning to come down. The further addition of a couple of
drops of the silver solution will cause a marked difference in the tint. Read
off the quantity run in, and calculate the standard. One gram of sodium
chloride contains 0.6062 gram of chlorine; and 1 gram of potassium
chloride contains 0.4754 gram.
For the determination of small quantities of chloride (a few milligrams), the
same method is used; but the standard solution is diluted so that each c.c. is
equal to 1 milligram of chlorine; and the chromate indicator is added before
titrating. The standard solution is made by measuring off 200 c.c. of the
solution described above, and diluting with distilled water to 1 litre.
Page 454
BROMINE AND BROMIDES.
Bromine closely resembles chlorine in the nature of its compounds. It does
not occur free in nature, but is occasionally found in combination with
silver as bromargyrite (AgBr) and, together with chloride, in embolite. It
mainly occurs as alkaline bromides in certain natural waters. Nearly all the
bromine of commerce is derived from the mother liquors of salt-works—
i.e., the liquors from which the common salt has been crystallised out.
Bromine combines directly with the metals, forming a series of salts—the
bromides. In ordinary work they are separated with, and (except when
specially tested for) counted as, chlorides. They are detected by adding
chlorine water to the suspected solution and shaking up with carbon
bisulphide. Bromine colours the latter brown.
IODINE AND IODIDES.
Iodine does not occur in nature in the free state; and iodides are rare,
iodargyrite or iodide of silver (AgI) being the only one which ranks as a
mineral species. Iodates are found associated with Chili saltpetre, which is
an important source of the element.
Iodine and Iodides are largely used in the laboratory, and have already been
frequently referred to. It is used as an oxidising agent in a similar manner as
permanganate and bichromate of potash, especially in the determinations of
copper, arsenic, antimony, and manganese.
Iodine is not readily soluble in water; but dissolves easily in a concentrated
solution of potassium iodide. Its solutions are strongly coloured; a drop of a
dilute solution colours a large volume of water decidedly yellow; on the
addition of starch paste, this becomes blue. The delicacy of this reaction is
taken advantage of in titrations to determine when free iodine is present.
The blue colour may be alternately developed and removed by the addition
of iodine (or an oxidising agent) and hyposulphite of soda (or some other
reducing agent). In decolorising, the solution changes from blue or black to
colourless or pale yellow according to circumstances. Sometimes the
solution, instead of remaining colourless, gradually develops a blue which
recurs in spite of the further addition of the reducing agent. In these cases
Bromine closely resembles chlorine in the nature of its compounds. It does
not occur free in nature, but is occasionally found in combination with
silver as bromargyrite (AgBr) and, together with chloride, in embolite. It
mainly occurs as alkaline bromides in certain natural waters. Nearly all the
bromine of commerce is derived from the mother liquors of salt-works—
i.e., the liquors from which the common salt has been crystallised out.
Bromine combines directly with the metals, forming a series of salts—the
bromides. In ordinary work they are separated with, and (except when
specially tested for) counted as, chlorides. They are detected by adding
chlorine water to the suspected solution and shaking up with carbon
bisulphide. Bromine colours the latter brown.
IODINE AND IODIDES.
Iodine does not occur in nature in the free state; and iodides are rare,
iodargyrite or iodide of silver (AgI) being the only one which ranks as a
mineral species. Iodates are found associated with Chili saltpetre, which is
an important source of the element.
Iodine and Iodides are largely used in the laboratory, and have already been
frequently referred to. It is used as an oxidising agent in a similar manner as
permanganate and bichromate of potash, especially in the determinations of
copper, arsenic, antimony, and manganese.
Iodine is not readily soluble in water; but dissolves easily in a concentrated
solution of potassium iodide. Its solutions are strongly coloured; a drop of a
dilute solution colours a large volume of water decidedly yellow; on the
addition of starch paste, this becomes blue. The delicacy of this reaction is
taken advantage of in titrations to determine when free iodine is present.
The blue colour may be alternately developed and removed by the addition
of iodine (or an oxidising agent) and hyposulphite of soda (or some other
reducing agent). In decolorising, the solution changes from blue or black to
colourless or pale yellow according to circumstances. Sometimes the
solution, instead of remaining colourless, gradually develops a blue which
recurs in spite of the further addition of the reducing agent. In these cases
Page 455
the conditions of the assay have been departed from, or (and this is more
often the case) there is some substance present capable of liberating iodine.
Iodine forms a series of salts—the iodides—resembling in many respects
the chlorides. These can be obtained by direct combination of the metals
with iodine.
Detection.—Free iodine is best recognised by the violet vapours evolved
from the solution on heating, and by the blue or black colour which it
strikes on the addition of starch paste. Iodides are detected by boiling with
strong solutions of ferric sulphate or chloride. Iodine is liberated, distilled
over, and collected. Chlorine also liberates iodine from iodides; and this
reaction is frequently made use of in assaying. A process based on this is
described under Manganese. All substances which liberate chlorine on
boiling with hydrochloric acid (dioxides, bichromates, permanganates, &c.)
are determined in a similar way.
Solution and Separation.—Most iodides are soluble in water or dilute
acids. The separation is effected by distilling the substance with solution of
ferric sulphate, and collecting the vapour in a dilute solution of sulphurous
acid or arsenite of soda. On the completion of the distillation, the iodine
will be in the distillate as iodide; and the gravimetric determination is made
on this.
GRAVIMETRIC DETERMINATION.
To the solution containing the iodine, as iodide, and which is free from
chlorides (and bromides), add a little dilute nitric acid and nitrate of silver
till no further precipitate is produced. Filter off, wash with hot water, and
dry. Clean the filter-paper as much as possible, and burn it. Collect the ash
in a weighed porcelain crucible, add the main portion, and heat to incipient
fusion; cool, and weigh. The substance is silver iodide, and contains 54.03
per cent. of iodine.
VOLUMETRIC METHOD.
often the case) there is some substance present capable of liberating iodine.
Iodine forms a series of salts—the iodides—resembling in many respects
the chlorides. These can be obtained by direct combination of the metals
with iodine.
Detection.—Free iodine is best recognised by the violet vapours evolved
from the solution on heating, and by the blue or black colour which it
strikes on the addition of starch paste. Iodides are detected by boiling with
strong solutions of ferric sulphate or chloride. Iodine is liberated, distilled
over, and collected. Chlorine also liberates iodine from iodides; and this
reaction is frequently made use of in assaying. A process based on this is
described under Manganese. All substances which liberate chlorine on
boiling with hydrochloric acid (dioxides, bichromates, permanganates, &c.)
are determined in a similar way.
Solution and Separation.—Most iodides are soluble in water or dilute
acids. The separation is effected by distilling the substance with solution of
ferric sulphate, and collecting the vapour in a dilute solution of sulphurous
acid or arsenite of soda. On the completion of the distillation, the iodine
will be in the distillate as iodide; and the gravimetric determination is made
on this.
GRAVIMETRIC DETERMINATION.
To the solution containing the iodine, as iodide, and which is free from
chlorides (and bromides), add a little dilute nitric acid and nitrate of silver
till no further precipitate is produced. Filter off, wash with hot water, and
dry. Clean the filter-paper as much as possible, and burn it. Collect the ash
in a weighed porcelain crucible, add the main portion, and heat to incipient
fusion; cool, and weigh. The substance is silver iodide, and contains 54.03
per cent. of iodine.
VOLUMETRIC METHOD.
Page 456
This is for the titration of free iodine, and is practically that which is
described under Manganese. The substance to be determined is distilled
with ferric sulphate, and the iodine is collected in a solution of potassium
iodide, in which it readily dissolves. If flaky crystals separate out in the
receiver, more potassium iodide crystals are added. When the distillation is
finished, the receiver is disconnected, and its contents washed out into a
beaker and titrated with "hypo." The standard solution of "hypo" is made by
dissolving 19.58 grams of hyposulphite of soda (Na2S2O3.5H2O) in water
and diluting to 1 litre; 100 c.c. are equal to 1 gram of iodine. To standardise
the solution, weigh up 0.25 gram of pure iodine in a small beaker. Add 2 or
3 crystals of potassium iodide; cover with water; and, when dissolved,
dilute to 50 or 100 c.c. Titrate, and calculate the standard.
FLUORINE AND FLUORIDES.
Fluorine is frequently met with as calcium fluoride or fluor-spar (CaF2). It
occurs less abundantly as cryolite (Na3AlF6), a fluoride of aluminium and
sodium, which is used in glass-making. Certain other rarer fluorides are
occasionally met with. Fluorine is also found in apatite, and in some
silicates, such as topaz, tourmaline, micas, &c.
Hydrofluoric acid is used for etching glass and opening up silicates. It
attacks silica, forming fluoride of silicon (SiF4), which is volatile. Silica is
by this means eliminated from other oxides, which, in the presence of
sulphuric acid, are fixed. The commercial acid is seldom pure, and
generally weak; and the acid itself is dangerously obnoxious. The use of
ammonium fluoride (or sodium fluoride) and a mineral acid is more
convenient. Determinations of this kind are made in platinum dishes
enclosed in lead or copper vessels in a well-ventilated place. Fluor-spar is
useful as a flux in dry assaying; it renders slags, which would otherwise be
pasty, quite fluid. Fluorides generally are fusible, and impart fusibility to
substances with which they form weak compounds. Their fluxing action
does not depend on the removal of silicon as fluoride.
Detection.—Fluorides in small quantity are easily overlooked unless
specially sought for. In larger amounts they are recognised by the property
hydrofluoric acid has of etching glass. A watch-glass is warmed, and a layer
described under Manganese. The substance to be determined is distilled
with ferric sulphate, and the iodine is collected in a solution of potassium
iodide, in which it readily dissolves. If flaky crystals separate out in the
receiver, more potassium iodide crystals are added. When the distillation is
finished, the receiver is disconnected, and its contents washed out into a
beaker and titrated with "hypo." The standard solution of "hypo" is made by
dissolving 19.58 grams of hyposulphite of soda (Na2S2O3.5H2O) in water
and diluting to 1 litre; 100 c.c. are equal to 1 gram of iodine. To standardise
the solution, weigh up 0.25 gram of pure iodine in a small beaker. Add 2 or
3 crystals of potassium iodide; cover with water; and, when dissolved,
dilute to 50 or 100 c.c. Titrate, and calculate the standard.
FLUORINE AND FLUORIDES.
Fluorine is frequently met with as calcium fluoride or fluor-spar (CaF2). It
occurs less abundantly as cryolite (Na3AlF6), a fluoride of aluminium and
sodium, which is used in glass-making. Certain other rarer fluorides are
occasionally met with. Fluorine is also found in apatite, and in some
silicates, such as topaz, tourmaline, micas, &c.
Hydrofluoric acid is used for etching glass and opening up silicates. It
attacks silica, forming fluoride of silicon (SiF4), which is volatile. Silica is
by this means eliminated from other oxides, which, in the presence of
sulphuric acid, are fixed. The commercial acid is seldom pure, and
generally weak; and the acid itself is dangerously obnoxious. The use of
ammonium fluoride (or sodium fluoride) and a mineral acid is more
convenient. Determinations of this kind are made in platinum dishes
enclosed in lead or copper vessels in a well-ventilated place. Fluor-spar is
useful as a flux in dry assaying; it renders slags, which would otherwise be
pasty, quite fluid. Fluorides generally are fusible, and impart fusibility to
substances with which they form weak compounds. Their fluxing action
does not depend on the removal of silicon as fluoride.
Detection.—Fluorides in small quantity are easily overlooked unless
specially sought for. In larger amounts they are recognised by the property
hydrofluoric acid has of etching glass. A watch-glass is warmed, and a layer
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of wax is melted over the convex side. When cold, some lines are engraved
on the waxed surface with any sharp-pointed instrument. The substance to
be tested is powdered; and moistened, in a platinum dish, with sulphuric
acid. The watch-glass is filled with cold water and supported over the dish.
The dish is then carefully warmed, but not sufficiently to melt the wax.
After a minute or two, the glass is taken off, and the wax removed. If the
substance contained fluorine, the characters will be found permanently
etched on the glass. An equally good, but more rapid, test is to mix the
powdered substance with some silica, and to heat the mixture in a test tube
with sulphuric acid. Silicon fluoride is evolved, and, if a moistened glass
rod is held in the tube, it becomes coated with a white deposit of silica,
formed by the decomposition of the silicon fluoride by the water. This is
also used as a test for silica; but in this case the substance is mixed with a
fluoride, and the experiment must obviously be carried out in a platinum
vessel.
Separation and Determination.—The determination of fluorine is
difficult. In the case of fluorides free from silicates (such as fluor-spar), it is
determined indirectly by decomposing a weighed portion with sulphuric
acid, evaporating, igniting, and weighing the residual sulphate. The increase
in weight multiplied by 0.655 gives the weight of fluorine.
In the presence of silica this method does not answer, because of the
volatilisation of silicon fluoride. In these cases Wöhler adopted the
following plan, which resembles that for the indirect determination of
carbon dioxide. Mix the weighed substance in a small flask with powdered
silica and sulphuric acid. The mouth of the flask is closed with a cork
carrying a tube which is filled, the first half with calcium chloride and the
second half with pumice coated with dried copper sulphate. The apparatus
is weighed quickly, and then warmed till decomposition is complete. A
current of dry air is aspirated for a minute or two; and the apparatus again
weighed. The loss in weight gives that of the silicon fluoride (SiF4), which,
multiplied by 0.7307, gives the weight of fluorine.
Fresenius uses the same reaction; but collects and weighs the silicon
fluoride. The finely powdered and dried substance is mixed with ten or
fifteen times its weight of ignited and powdered silica. The mixture is
introduced into a small dry flask connected on one side with a series of
on the waxed surface with any sharp-pointed instrument. The substance to
be tested is powdered; and moistened, in a platinum dish, with sulphuric
acid. The watch-glass is filled with cold water and supported over the dish.
The dish is then carefully warmed, but not sufficiently to melt the wax.
After a minute or two, the glass is taken off, and the wax removed. If the
substance contained fluorine, the characters will be found permanently
etched on the glass. An equally good, but more rapid, test is to mix the
powdered substance with some silica, and to heat the mixture in a test tube
with sulphuric acid. Silicon fluoride is evolved, and, if a moistened glass
rod is held in the tube, it becomes coated with a white deposit of silica,
formed by the decomposition of the silicon fluoride by the water. This is
also used as a test for silica; but in this case the substance is mixed with a
fluoride, and the experiment must obviously be carried out in a platinum
vessel.
Separation and Determination.—The determination of fluorine is
difficult. In the case of fluorides free from silicates (such as fluor-spar), it is
determined indirectly by decomposing a weighed portion with sulphuric
acid, evaporating, igniting, and weighing the residual sulphate. The increase
in weight multiplied by 0.655 gives the weight of fluorine.
In the presence of silica this method does not answer, because of the
volatilisation of silicon fluoride. In these cases Wöhler adopted the
following plan, which resembles that for the indirect determination of
carbon dioxide. Mix the weighed substance in a small flask with powdered
silica and sulphuric acid. The mouth of the flask is closed with a cork
carrying a tube which is filled, the first half with calcium chloride and the
second half with pumice coated with dried copper sulphate. The apparatus
is weighed quickly, and then warmed till decomposition is complete. A
current of dry air is aspirated for a minute or two; and the apparatus again
weighed. The loss in weight gives that of the silicon fluoride (SiF4), which,
multiplied by 0.7307, gives the weight of fluorine.
Fresenius uses the same reaction; but collects and weighs the silicon
fluoride. The finely powdered and dried substance is mixed with ten or
fifteen times its weight of ignited and powdered silica. The mixture is
introduced into a small dry flask connected on one side with a series of
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drying-tubes, and on the other with an empty tube (to condense any
sulphuric acid). To this last is joined a drying-tube containing chloride of
calcium and anhydrous copper sulphate. This is directly connected with a
series of three weighed tubes in which the fluoride of silicon is collected.
The last of these is joined to another drying-tube. The first weighed tube
contains pumice and cotton wool, moistened with water; the second tube
contains soda-lime as well as (in the upper half of the second limb) fused
calcium chloride between plugs of wool; the third tube is filled half with
soda-lime and half with fused calcium chloride. The distilling-flask
containing the substance mixed with silica is charged with 40 or 50 c.c. of
sulphuric acid, and placed on the hot plate. Alongside it is placed a similar
dry flask containing a thermometer, and the temperature in this is kept at
150° or 160° C. A current of air is sent through the tubes during the
operation, which takes from one to three hours for from 0.1 to 1 gram of the
substance. A correction is made by deducting 0.001 gram for every hour the
dried air has been passed through. The increase in weight of the three tubes
gives the weight of the silicon fluoride.
Penfield uses a similar arrangement, but passes his silicon fluoride into an
alcoholic solution of potassium chloride. Silica and potassium silico-
fluoride are precipitated, and hydrochloric acid is set free.[100] The acid thus
liberated is titrated, with a standard solution of alkali, in the alcoholic
solution, and from the amount of free acid found the fluorine is calculated.
The weight of hydrochloric acid (HCl) found, multiplied by 1.562, gives the
weight of the fluorine. With this method of working, fewer U-tubes are
required. The exit tube from the flask is bent so as to form a small V, which
is kept cool in water; this is directly connected with the U-tube containing
the alcoholic solution of potassium chloride. The flask with the assay is
heated for about two hours, and a current of dry air is aspirated throughout
the determination. Fluoride of silicon is a gas not easily condensed to a
liquid: but is immediately decomposed by water or moist air.
FOOTNOTES:
[95] This will require two or three hours to thoroughly complete. It is best to
powder the oxide first produced, and recalcine.
[96] No magnetic oxide was formed.
sulphuric acid). To this last is joined a drying-tube containing chloride of
calcium and anhydrous copper sulphate. This is directly connected with a
series of three weighed tubes in which the fluoride of silicon is collected.
The last of these is joined to another drying-tube. The first weighed tube
contains pumice and cotton wool, moistened with water; the second tube
contains soda-lime as well as (in the upper half of the second limb) fused
calcium chloride between plugs of wool; the third tube is filled half with
soda-lime and half with fused calcium chloride. The distilling-flask
containing the substance mixed with silica is charged with 40 or 50 c.c. of
sulphuric acid, and placed on the hot plate. Alongside it is placed a similar
dry flask containing a thermometer, and the temperature in this is kept at
150° or 160° C. A current of air is sent through the tubes during the
operation, which takes from one to three hours for from 0.1 to 1 gram of the
substance. A correction is made by deducting 0.001 gram for every hour the
dried air has been passed through. The increase in weight of the three tubes
gives the weight of the silicon fluoride.
Penfield uses a similar arrangement, but passes his silicon fluoride into an
alcoholic solution of potassium chloride. Silica and potassium silico-
fluoride are precipitated, and hydrochloric acid is set free.[100] The acid thus
liberated is titrated, with a standard solution of alkali, in the alcoholic
solution, and from the amount of free acid found the fluorine is calculated.
The weight of hydrochloric acid (HCl) found, multiplied by 1.562, gives the
weight of the fluorine. With this method of working, fewer U-tubes are
required. The exit tube from the flask is bent so as to form a small V, which
is kept cool in water; this is directly connected with the U-tube containing
the alcoholic solution of potassium chloride. The flask with the assay is
heated for about two hours, and a current of dry air is aspirated throughout
the determination. Fluoride of silicon is a gas not easily condensed to a
liquid: but is immediately decomposed by water or moist air.
FOOTNOTES:
[95] This will require two or three hours to thoroughly complete. It is best to
powder the oxide first produced, and recalcine.
[96] No magnetic oxide was formed.
Page 459
[97] For example:—
CaO + 2HCl = CaCl2 + H2O.
PbO + H2SO4 = PbSO4 + H2O.
MgO + 2HNO3 = Mg(NO3)2 + H2O.
Al2O3 + 6HCl = Al2Cl6 + 3H2O.
Fe2O3 + 3H2SO4 = Fe2(SO4)3 + 3H2O.
[98] Fe2O3: 2FeO:: 0.2877: 0.2589.
[99] 100 c.c. contain 1 gram of sulphuric acid.
[100] 3SiF4 + 4KCl + 2H2O = 2K2SiF6 + SiO2 + 4HCl.
CaO + 2HCl = CaCl2 + H2O.
PbO + H2SO4 = PbSO4 + H2O.
MgO + 2HNO3 = Mg(NO3)2 + H2O.
Al2O3 + 6HCl = Al2Cl6 + 3H2O.
Fe2O3 + 3H2SO4 = Fe2(SO4)3 + 3H2O.
[98] Fe2O3: 2FeO:: 0.2877: 0.2589.
[99] 100 c.c. contain 1 gram of sulphuric acid.
[100] 3SiF4 + 4KCl + 2H2O = 2K2SiF6 + SiO2 + 4HCl.
Page 460
CHAPTER XVI.
SULPHUR AND SULPHATES.
Sulphur occurs native in volcanic districts, and is mined in Sicily, Italy, and
California in considerable quantities. Combined with metals (sulphides), it
is common in all mineral districts. Iron pyrites (FeS2) is the most abundant
source of this element. Sulphates, such as gypsum, are fairly common, but
have no value so far as the sulphur in them is concerned. In coal it exists as
an impurity, occurring partly as a constituent of organic compounds.
Sulphur, whether free or combined with metals, forms, on burning,
sulphurous oxide (SO2), which by the action of oxidising agents and water
is converted into sulphuric acid. It forms two oxides, sulphurous (SO2) and
sulphuric (SO3), which combine with bases to form sulphites and sulphates.
Sulphites are of little importance to the assayer, and are converted into
sulphates by the action of nitric acid and other oxidising agents.
The native sulphides, when acted on with hydrochloric acid, give off
sulphuretted hydrogen; with nitric acid or aqua regia, sulphates are formed,
and more or less sulphur separated.
Sulphur is detected in sulphides by the irritating odour of sulphurous oxide
given off on roasting, by the evolution of sulphuretted hydrogen when
treated with hydrochloric acid, or by a white precipitate of barium sulphate
formed when barium chloride is added to the aqua regia solution.
Dry Assay.—There is no method of general application. Free or native
sulphur may be volatilised, condensed, and weighed, but pyrites only gives
up a portion of its sulphur when heated in a closed vessel, while most
sulphides, and all sulphates, give up none at all.
In the determination of sulphur in brimstone, 10 grams of the substance are
taken, placed in a small porcelain dish, heated over a Bunsen burner in a
well-ventilated place, and ignited. When the sulphur has been completely
SULPHUR AND SULPHATES.
Sulphur occurs native in volcanic districts, and is mined in Sicily, Italy, and
California in considerable quantities. Combined with metals (sulphides), it
is common in all mineral districts. Iron pyrites (FeS2) is the most abundant
source of this element. Sulphates, such as gypsum, are fairly common, but
have no value so far as the sulphur in them is concerned. In coal it exists as
an impurity, occurring partly as a constituent of organic compounds.
Sulphur, whether free or combined with metals, forms, on burning,
sulphurous oxide (SO2), which by the action of oxidising agents and water
is converted into sulphuric acid. It forms two oxides, sulphurous (SO2) and
sulphuric (SO3), which combine with bases to form sulphites and sulphates.
Sulphites are of little importance to the assayer, and are converted into
sulphates by the action of nitric acid and other oxidising agents.
The native sulphides, when acted on with hydrochloric acid, give off
sulphuretted hydrogen; with nitric acid or aqua regia, sulphates are formed,
and more or less sulphur separated.
Sulphur is detected in sulphides by the irritating odour of sulphurous oxide
given off on roasting, by the evolution of sulphuretted hydrogen when
treated with hydrochloric acid, or by a white precipitate of barium sulphate
formed when barium chloride is added to the aqua regia solution.
Dry Assay.—There is no method of general application. Free or native
sulphur may be volatilised, condensed, and weighed, but pyrites only gives
up a portion of its sulphur when heated in a closed vessel, while most
sulphides, and all sulphates, give up none at all.
In the determination of sulphur in brimstone, 10 grams of the substance are
taken, placed in a small porcelain dish, heated over a Bunsen burner in a
well-ventilated place, and ignited. When the sulphur has been completely
Page 461
burnt off, the residue (which consists chiefly of sand) is collected and
weighed. In a separate portion the moisture and arsenic are determined; the
amounts of these are deducted from the loss in the first experiment. The
difference, multiplied by 10, gives the percentage of sulphur.
WET METHODS.
Solution.—All sulphates, excepting those of lead, barium, strontium, and
lime, are soluble in water or dilute acid. All sulphides, except cinnabar, are
converted into sulphates by the action of nitric acid at a gentle heat; or,
better, by the action of a mixture of three volumes of nitric acid and one
volume of hydrochloric acid. This last attacks cinnabar as well. With most
substances it is difficult to convert the whole of the sulphur into sulphuric
acid. The sulphur separates out at first as a dark spongy mass, which (on
continued treatment) changes to light-coloured flakes. When the solution
becomes concentrated and the temperature rises sufficiently, the sulphur
fuses into one or more honey-coloured globules which, owing to the small
surface they oppose to the acid, are very slowly oxidised. It is not desirable
to assist the formation of these globules; therefore, the temperature is kept
as low as possible, and strong nitric acid is used. When such globules form,
it is best to allow the solution to cool, when the globules will solidify. They
can then be filtered off and picked out from the insoluble residue, dried,
weighed, ignited, and again weighed, the loss being counted as sulphur.
With iron pyrites this difficulty seldom occurs.
Metallic sulphides when fused with an excess of nitre are completely
oxidised. If the ore is rich in sulphur, some inert body (such as sodium
chloride, or, better, sodium carbonate) is added to dilute the action. With
pure sulphur, the action is so energetic as to cause an explosion, so that care
should be taken. With burnt ores (incompletely calcined pyrites), there is
sufficient oxide of iron present to prevent too rapid action.
These fusions with nitre are best conducted in a platinum dish covered with
a piece of platinum foil. The ore is ground with the nitre to ensure complete
mixing. The heat need not be excessive, so that a single Bunsen burner
placed beneath the dish will suffice; if the bottom of the dish is seen to be
red-hot, it is sufficient. On cooling and extracting with water, the sulphur
weighed. In a separate portion the moisture and arsenic are determined; the
amounts of these are deducted from the loss in the first experiment. The
difference, multiplied by 10, gives the percentage of sulphur.
WET METHODS.
Solution.—All sulphates, excepting those of lead, barium, strontium, and
lime, are soluble in water or dilute acid. All sulphides, except cinnabar, are
converted into sulphates by the action of nitric acid at a gentle heat; or,
better, by the action of a mixture of three volumes of nitric acid and one
volume of hydrochloric acid. This last attacks cinnabar as well. With most
substances it is difficult to convert the whole of the sulphur into sulphuric
acid. The sulphur separates out at first as a dark spongy mass, which (on
continued treatment) changes to light-coloured flakes. When the solution
becomes concentrated and the temperature rises sufficiently, the sulphur
fuses into one or more honey-coloured globules which, owing to the small
surface they oppose to the acid, are very slowly oxidised. It is not desirable
to assist the formation of these globules; therefore, the temperature is kept
as low as possible, and strong nitric acid is used. When such globules form,
it is best to allow the solution to cool, when the globules will solidify. They
can then be filtered off and picked out from the insoluble residue, dried,
weighed, ignited, and again weighed, the loss being counted as sulphur.
With iron pyrites this difficulty seldom occurs.
Metallic sulphides when fused with an excess of nitre are completely
oxidised. If the ore is rich in sulphur, some inert body (such as sodium
chloride, or, better, sodium carbonate) is added to dilute the action. With
pure sulphur, the action is so energetic as to cause an explosion, so that care
should be taken. With burnt ores (incompletely calcined pyrites), there is
sufficient oxide of iron present to prevent too rapid action.
These fusions with nitre are best conducted in a platinum dish covered with
a piece of platinum foil. The ore is ground with the nitre to ensure complete
mixing. The heat need not be excessive, so that a single Bunsen burner
placed beneath the dish will suffice; if the bottom of the dish is seen to be
red-hot, it is sufficient. On cooling and extracting with water, the sulphur
Page 462
will pass into solution as potassium sulphate, which is then filtered off from
the insoluble oxides of iron, copper, &c. The filtrate, after having been
treated with a large excess of hydrochloric acid, evaporated to dryness, and
re-dissolved in water, is ready for the determination.
Lead sulphate may be dissolved by boiling with ammonium acetate. The
insoluble sulphates of barium, strontium, and lime, are decomposed by
fusing with 4 or 5 times their weight of "fusion mixture." The alkaline
sulphates are then dissolved out with water, and filtered off from the
insoluble residue. The filtrate is rendered acid with hydrochloric acid.
Separation.—The determination of the sulphuric acid in these solutions by
precipitation with barium chloride also serves as a separation; but in hot
acid solutions containing copper, and more especially iron salts, the baric
sulphate has a strong tendency to carry down amounts of those bodies,
varying, no doubt, with the conditions of the precipitation. Boiling
hydrochloric acid fails to completely extract them. Moreover, the use of hot
concentrated hydrochloric acid causes a loss by dissolving barium sulphate.
Nitric acid and nitrates must be decomposed by prolonged boiling and
evaporation with hydrochloric acid. The iron may be removed by adding a
slight excess of ammonia to the faintly acid solution, filtering off, and
washing the precipitated ferric hydrate with hot water. By slightly
acidulating the filtrate with hydrochloric acid, it will be rendered ready for
the determination.
GRAVIMETRIC METHOD.
This assay is one of those which strikingly shows the necessity of getting
the assay solution under proper conditions, in order to obtain satisfactory
results. The method has been repeatedly investigated, and the conclusion
arrived at, "that it can be correct only by accident." Yet there are many
chemists who get good results, and place considerable faith in its accuracy.
This can only be due to differences in the manner of working. It is generally
understood that nitric acid or nitrates must be absent; and our experience
fully confirms this. Precipitations in nitrate solutions are worthless, as the
following experiments show. In each experiment the bulk of the solution
was 150 c.c. The solutions contained 10 grams of nitre, were freely acid
the insoluble oxides of iron, copper, &c. The filtrate, after having been
treated with a large excess of hydrochloric acid, evaporated to dryness, and
re-dissolved in water, is ready for the determination.
Lead sulphate may be dissolved by boiling with ammonium acetate. The
insoluble sulphates of barium, strontium, and lime, are decomposed by
fusing with 4 or 5 times their weight of "fusion mixture." The alkaline
sulphates are then dissolved out with water, and filtered off from the
insoluble residue. The filtrate is rendered acid with hydrochloric acid.
Separation.—The determination of the sulphuric acid in these solutions by
precipitation with barium chloride also serves as a separation; but in hot
acid solutions containing copper, and more especially iron salts, the baric
sulphate has a strong tendency to carry down amounts of those bodies,
varying, no doubt, with the conditions of the precipitation. Boiling
hydrochloric acid fails to completely extract them. Moreover, the use of hot
concentrated hydrochloric acid causes a loss by dissolving barium sulphate.
Nitric acid and nitrates must be decomposed by prolonged boiling and
evaporation with hydrochloric acid. The iron may be removed by adding a
slight excess of ammonia to the faintly acid solution, filtering off, and
washing the precipitated ferric hydrate with hot water. By slightly
acidulating the filtrate with hydrochloric acid, it will be rendered ready for
the determination.
GRAVIMETRIC METHOD.
This assay is one of those which strikingly shows the necessity of getting
the assay solution under proper conditions, in order to obtain satisfactory
results. The method has been repeatedly investigated, and the conclusion
arrived at, "that it can be correct only by accident." Yet there are many
chemists who get good results, and place considerable faith in its accuracy.
This can only be due to differences in the manner of working. It is generally
understood that nitric acid or nitrates must be absent; and our experience
fully confirms this. Precipitations in nitrate solutions are worthless, as the
following experiments show. In each experiment the bulk of the solution
was 150 c.c. The solutions contained 10 grams of nitre, were freely acid
Page 463
with hydrochloric acid, and were precipitated (while boiling) with slight
excess of baric chloride.
Sulphuric acid taken 0.020gram0.050gram 0.100gram
" found 0.019" 0.047" 0.098"
" taken 0.500" 1.004" 1.000"
" found 0.526" 1.126" 1.126"
All the precipitates were boiled with hydrochloric acid, and thoroughly
washed before weighing. The results of some other experiments on this
subject are given under "sulphur" in the "examination of commercial
copper," page 207.
The solution having been obtained free from nitrates and chlorates (and
containing but little free hydrochloric acid), is largely diluted, heated to
boiling, and precipitated with a moderate excess of a solution of chloride of
barium (8 parts of the crystallized barium chloride are sufficient for 1 of
sulphur). It is allowed to settle for half-an-hour, and then decanted through
a filter. The precipitate is shaken up with boiling water, rendered slightly
acid, filtered, washed, dried, ignited, and weighed. The ignited precipitate,
when pure, is white, and is not decomposed at a red heat; it is barium
sulphate (BaSO4), and contains 13.73 per cent. of sulphur, or 34.33 per
cent. of sulphuric oxide (SO3).
Determination of Sulphur in Pyrites.—Weigh up half a gram of the dried
and powdered sample, and treat with 10 c.c. of a mixture of 3 volumes of
nitric acid and 1 volume of hydrochloric acid, occasionally heating.
Evaporate to dryness, treat with 5 c.c. of hydrochloric acid, and again
evaporate; take up with 1 c.c. of hydrochloric acid and 100 c.c. of hot water,
filter through a small filter, and wash. The residue may contain sulphates of
lead, barium, or lime; it must be separately examined, if the total sulphur is
wanted. The filtrate is heated, and rendered slightly alkaline with ammonia.
Filter off the precipitated ferric hydrate through a quick filter, and wash
with hot water. If necessary, evaporate the bulk to about 200 c.c., render
faintly acid with hydrochloric acid, and add 20 c.c. of solution of barium
chloride; allow to stand for half-an-hour, and decant through a filter. Wash
excess of baric chloride.
Sulphuric acid taken 0.020gram0.050gram 0.100gram
" found 0.019" 0.047" 0.098"
" taken 0.500" 1.004" 1.000"
" found 0.526" 1.126" 1.126"
All the precipitates were boiled with hydrochloric acid, and thoroughly
washed before weighing. The results of some other experiments on this
subject are given under "sulphur" in the "examination of commercial
copper," page 207.
The solution having been obtained free from nitrates and chlorates (and
containing but little free hydrochloric acid), is largely diluted, heated to
boiling, and precipitated with a moderate excess of a solution of chloride of
barium (8 parts of the crystallized barium chloride are sufficient for 1 of
sulphur). It is allowed to settle for half-an-hour, and then decanted through
a filter. The precipitate is shaken up with boiling water, rendered slightly
acid, filtered, washed, dried, ignited, and weighed. The ignited precipitate,
when pure, is white, and is not decomposed at a red heat; it is barium
sulphate (BaSO4), and contains 13.73 per cent. of sulphur, or 34.33 per
cent. of sulphuric oxide (SO3).
Determination of Sulphur in Pyrites.—Weigh up half a gram of the dried
and powdered sample, and treat with 10 c.c. of a mixture of 3 volumes of
nitric acid and 1 volume of hydrochloric acid, occasionally heating.
Evaporate to dryness, treat with 5 c.c. of hydrochloric acid, and again
evaporate; take up with 1 c.c. of hydrochloric acid and 100 c.c. of hot water,
filter through a small filter, and wash. The residue may contain sulphates of
lead, barium, or lime; it must be separately examined, if the total sulphur is
wanted. The filtrate is heated, and rendered slightly alkaline with ammonia.
Filter off the precipitated ferric hydrate through a quick filter, and wash
with hot water. If necessary, evaporate the bulk to about 200 c.c., render
faintly acid with hydrochloric acid, and add 20 c.c. of solution of barium
chloride; allow to stand for half-an-hour, and decant through a filter. Wash
Page 464
with hot water, dry, ignite, and weigh. Pure pyrites contains 53.33 per cent.
of sulphur.
VOLUMETRIC METHOD.
This is based upon the easy conversion of all sulphur compounds into
sulphates by fusion with nitre or by oxidation with nitric acid; and on the
determination of the sulphate formed by titration in an acetic acid solution
with baric chloride.[101] The finishing point is determined by filtering off
portions of the assay solution, and testing with sulphuric acid. A slight
excess of baric chloride will cause a precipitate.
The process may be divided into—(1) the preparation of the solution, and
(2) the titration.
Preparation of the Solution.—Weigh up from 1 to 5 grams of the dried
and powdered substance, and mix intimately with 4 grams of powdered
nitre; clean out the mortar with another gram of nitre, and add this as a
cover. Heat in a platinum crucible for fifteen minutes at a low temperature;
cool, and extract with water in an evaporating-dish about 9 inches across,
and holding 700 or 800 c.c. Add 10 grams of sodium acetate and 10 c.c. of
acetic acid, and dilute to half a litre. Boil. The solution is ready for titrating.
Substances which lose sulphur on heating (such as pyrites) are thus treated:
—Weigh up 1 gram, and evaporate nearly to dryness with 10 c.c. each of
nitric and hydrochloric acids. Take up with 10 c.c. of hydrochloric acid, and
again boil down to a small bulk; dilute and transfer to a 9-inch evaporating-
dish; add 10 grams of sodium acetate and 5 c.c. of acetic acid, dilute to half
a litre, and boil. The solution is ready for titrating. Sulphates may be
dissolved up in the dish itself with the help of a c.c. or so of hydrochloric
acid; sodium acetate and acetic acid are then added; and, after dilution and
boiling, the solutions are at once titrated.
The solution before titration must contain no free mineral acid, but 5 or 10
c.c. of acetic acid should be present. It must contain 10 grams of sodium
acetate, or sufficient to convert any free mineral acid into its corresponding
sodic salt; or, if chlorides, nitrates or sulphates of the metals are present,
sufficient to decompose them. If a precipitation occurs, as is the case with
ferric salts, &c., the solution is titrated with the precipitate in it.
of sulphur.
VOLUMETRIC METHOD.
This is based upon the easy conversion of all sulphur compounds into
sulphates by fusion with nitre or by oxidation with nitric acid; and on the
determination of the sulphate formed by titration in an acetic acid solution
with baric chloride.[101] The finishing point is determined by filtering off
portions of the assay solution, and testing with sulphuric acid. A slight
excess of baric chloride will cause a precipitate.
The process may be divided into—(1) the preparation of the solution, and
(2) the titration.
Preparation of the Solution.—Weigh up from 1 to 5 grams of the dried
and powdered substance, and mix intimately with 4 grams of powdered
nitre; clean out the mortar with another gram of nitre, and add this as a
cover. Heat in a platinum crucible for fifteen minutes at a low temperature;
cool, and extract with water in an evaporating-dish about 9 inches across,
and holding 700 or 800 c.c. Add 10 grams of sodium acetate and 10 c.c. of
acetic acid, and dilute to half a litre. Boil. The solution is ready for titrating.
Substances which lose sulphur on heating (such as pyrites) are thus treated:
—Weigh up 1 gram, and evaporate nearly to dryness with 10 c.c. each of
nitric and hydrochloric acids. Take up with 10 c.c. of hydrochloric acid, and
again boil down to a small bulk; dilute and transfer to a 9-inch evaporating-
dish; add 10 grams of sodium acetate and 5 c.c. of acetic acid, dilute to half
a litre, and boil. The solution is ready for titrating. Sulphates may be
dissolved up in the dish itself with the help of a c.c. or so of hydrochloric
acid; sodium acetate and acetic acid are then added; and, after dilution and
boiling, the solutions are at once titrated.
The solution before titration must contain no free mineral acid, but 5 or 10
c.c. of acetic acid should be present. It must contain 10 grams of sodium
acetate, or sufficient to convert any free mineral acid into its corresponding
sodic salt; or, if chlorides, nitrates or sulphates of the metals are present,
sufficient to decompose them. If a precipitation occurs, as is the case with
ferric salts, &c., the solution is titrated with the precipitate in it.
Page 465
The Titration.—The standard solution of barium chloride is made by
dissolving 76.25 grams of the crystallized salt (BaCl2.2H2O) in distilled
water, and diluting to 1 litre. 100 c.c. will equal 1 gram of sulphur. As
indicator, use dilute sulphuric acid. The strength of the solution may be
checked by the titration of 5 grams of ferrous sulphate (oxidized with
permanganate of potassium or a few drops of nitric acid), which should
require 57.5 c.c. of the barium chloride solution; or any pure sulphate of
known composition can be used; anhydrous salts should be preferred.
Fill an ordinary 100 c.c. burette with the solution of barium chloride. The
evaporating dish containing the assay solution is placed on a round burner
(as shown in fig. 65), and the solution is kept steadily boiling. An ordinary
Bunsen-burner flame will cause bumping, and should not be used. Run in
the standard solution in quantity known to be insufficient; then withdraw a
portion of about 2 c.c., with a pipette, and filter through a fine filter-paper
into a test tube. Run in another 0.5 c.c. of the standard solution, and
withdraw and filter into a test tube another portion of 2 c.c.; and continue
this operation until half-a-dozen or more portions have been drawn off. The
test tubes should be arranged in order in a stand resting on a piece of paper,
so that each test tube representing 0.5 c.c. of the standard baric chloride
may have its value recorded beneath it (fig. 66). Add to each test tube 3
drops of dilute sulphuric acid; that which shows the first appearance of a
precipitate marks the point at which the titration is complete. Suppose, for
example, that the test tube marked 48.5 c.c. shows no precipitate, while that
at 49.0 c.c. shows one, it is evident that the finishing point lies between
these readings. With a little practice, one can judge from the appearance of
the precipitate in the 49 c.c. tube, whether 1/4 c.c. should be deducted or
not.
dissolving 76.25 grams of the crystallized salt (BaCl2.2H2O) in distilled
water, and diluting to 1 litre. 100 c.c. will equal 1 gram of sulphur. As
indicator, use dilute sulphuric acid. The strength of the solution may be
checked by the titration of 5 grams of ferrous sulphate (oxidized with
permanganate of potassium or a few drops of nitric acid), which should
require 57.5 c.c. of the barium chloride solution; or any pure sulphate of
known composition can be used; anhydrous salts should be preferred.
Fill an ordinary 100 c.c. burette with the solution of barium chloride. The
evaporating dish containing the assay solution is placed on a round burner
(as shown in fig. 65), and the solution is kept steadily boiling. An ordinary
Bunsen-burner flame will cause bumping, and should not be used. Run in
the standard solution in quantity known to be insufficient; then withdraw a
portion of about 2 c.c., with a pipette, and filter through a fine filter-paper
into a test tube. Run in another 0.5 c.c. of the standard solution, and
withdraw and filter into a test tube another portion of 2 c.c.; and continue
this operation until half-a-dozen or more portions have been drawn off. The
test tubes should be arranged in order in a stand resting on a piece of paper,
so that each test tube representing 0.5 c.c. of the standard baric chloride
may have its value recorded beneath it (fig. 66). Add to each test tube 3
drops of dilute sulphuric acid; that which shows the first appearance of a
precipitate marks the point at which the titration is complete. Suppose, for
example, that the test tube marked 48.5 c.c. shows no precipitate, while that
at 49.0 c.c. shows one, it is evident that the finishing point lies between
these readings. With a little practice, one can judge from the appearance of
the precipitate in the 49 c.c. tube, whether 1/4 c.c. should be deducted or
not.
Page 466
It is better to add dilute sulphuric acid, and to watch for the appearance of a
precipitate in the test tube, than to add baric chloride and to look for its non-
appearance; besides, baric chloride is much less likely to be present in a test
tube as impurity than sulphates are. In this way the chance of error from
what are termed "accidental causes" is diminished.
The following experiments show the effect of variation in the conditions of
titration:—
Make a standard solution of sulphuric acid by diluting 43.65 grams of
sulphuric acid (sp. g. 1.6165) to 1 litre: 100 c.c. will contain 1 gram of
sulphur. An equivalent solution may be made by dissolving 100.62 grams of
sodium sulphate crystals (Na2SO4.10H2O), or 86.88 grams of ferrous
sulphate (FeSO4.7H2O), in water (oxidising the latter), and diluting to 1
litre.
The order in which these experiments are given is that in which they were
made in an investigation into the conditions under which the titration could
most accurately be effected.
Effect of Hydrochloric and Nitric Acids.—The titrations were performed
in the manner already described, but sodic acetate and acetic acid were
absent. Twenty c.c. of the standard solution of sulphuric acid were used.
Hydrochloric acid present 0.0 c.c. 1.0 c.c. 2.0 c.c. 5.0 c.c.
"Baric chloride" required 20.0" 20.0" 19.7 " 12.5 "
Nitric acid present 0.0 c.c. 1.0 c.c. 2.0 c.c. 5.0 c.c.
"Baric chloride" required 20.0" 19.5" 18.0 " 10.0 "
precipitate in the test tube, than to add baric chloride and to look for its non-
appearance; besides, baric chloride is much less likely to be present in a test
tube as impurity than sulphates are. In this way the chance of error from
what are termed "accidental causes" is diminished.
The following experiments show the effect of variation in the conditions of
titration:—
Make a standard solution of sulphuric acid by diluting 43.65 grams of
sulphuric acid (sp. g. 1.6165) to 1 litre: 100 c.c. will contain 1 gram of
sulphur. An equivalent solution may be made by dissolving 100.62 grams of
sodium sulphate crystals (Na2SO4.10H2O), or 86.88 grams of ferrous
sulphate (FeSO4.7H2O), in water (oxidising the latter), and diluting to 1
litre.
The order in which these experiments are given is that in which they were
made in an investigation into the conditions under which the titration could
most accurately be effected.
Effect of Hydrochloric and Nitric Acids.—The titrations were performed
in the manner already described, but sodic acetate and acetic acid were
absent. Twenty c.c. of the standard solution of sulphuric acid were used.
Hydrochloric acid present 0.0 c.c. 1.0 c.c. 2.0 c.c. 5.0 c.c.
"Baric chloride" required 20.0" 20.0" 19.7 " 12.5 "
Nitric acid present 0.0 c.c. 1.0 c.c. 2.0 c.c. 5.0 c.c.
"Baric chloride" required 20.0" 19.5" 18.0 " 10.0 "
Page 467
These show clearly the interference of free mineral acids, although very
dilute hydrochloric acid (1 c.c. in 500 of water) has no effect.
Effect of Acetic and Citric Acids.—A similar series of experiments with
these acids gave the following results:—
Acetic acid present 0.0 c.c. 5.0 c.c. 50.0 c.c. 100.0 c.c.
"Baric chloride" required20.0" 20.0 " 20.0 " 20.0"
Citric acid present 0 gram 1 gram 5 grams
"Baric chloride" required20.0 c.c. 20.0 c.c. 20.0 c.c.
These acids do not interfere.
Effect of Sodic Acetate and Acetic Acid.—In each of these experiments 5
c.c. of acetic acid was present.
Sodium acetate added 0 gram 1 gram 10 grams 50 grams
"Baric chloride" required 20.0 c.c. 20.0 c.c. 20.0 c.c. 20.0 c.c.
As sodic acetate and acetic acid did not interfere, it became desirable to
make some experiments on the finishing point. The first object sought for
was the smallest amount of the standard baric chloride in 500 c.c. of water,
required to give an indication when tested in the manner already described.
Baric Chloride
Conditions of Assay Solution.
required.
Water only 0.05 c.c.
With 10 grams of sodium acetate and 5 c.c. of
0.05 "
acetic acid
The same with 5 grams of nitre 0.10 "
Like the last, but with 5 grams of salt instead of
0.10 "
nitre
These show that as small an amount of baric chloride solution as is equal to
only 0.000002 gram of sulphur in the 2 c.c. of solution tested yields a
decided precipitate on the addition of 3 drops of sulphuric acid.
dilute hydrochloric acid (1 c.c. in 500 of water) has no effect.
Effect of Acetic and Citric Acids.—A similar series of experiments with
these acids gave the following results:—
Acetic acid present 0.0 c.c. 5.0 c.c. 50.0 c.c. 100.0 c.c.
"Baric chloride" required20.0" 20.0 " 20.0 " 20.0"
Citric acid present 0 gram 1 gram 5 grams
"Baric chloride" required20.0 c.c. 20.0 c.c. 20.0 c.c.
These acids do not interfere.
Effect of Sodic Acetate and Acetic Acid.—In each of these experiments 5
c.c. of acetic acid was present.
Sodium acetate added 0 gram 1 gram 10 grams 50 grams
"Baric chloride" required 20.0 c.c. 20.0 c.c. 20.0 c.c. 20.0 c.c.
As sodic acetate and acetic acid did not interfere, it became desirable to
make some experiments on the finishing point. The first object sought for
was the smallest amount of the standard baric chloride in 500 c.c. of water,
required to give an indication when tested in the manner already described.
Baric Chloride
Conditions of Assay Solution.
required.
Water only 0.05 c.c.
With 10 grams of sodium acetate and 5 c.c. of
0.05 "
acetic acid
The same with 5 grams of nitre 0.10 "
Like the last, but with 5 grams of salt instead of
0.10 "
nitre
These show that as small an amount of baric chloride solution as is equal to
only 0.000002 gram of sulphur in the 2 c.c. of solution tested yields a
decided precipitate on the addition of 3 drops of sulphuric acid.
Page 468
To determine whether the same finishing point is obtained on testing the
filtered portions in the test tubes with baric chloride as is obtained on
testing with sulphuric acid, a titration was made with 20 c.c. of standard
solution of sulphuric acid, together with the usual quantities of sodic acetate
and acetic acid; and two lots of 2 c.c. each were filtered into two sets of test
tubes after each addition of the standard baric chloride. To one series 3
drops of baric chloride solution were added, and to the other 3 drops of
sulphuric acid. The results were—
"Baric Chloride" With Dilute Sulphuric With Baric Chloride
added. Acid. Solution.
19.5 c.c. Clear Cloudy
19.75 " Clear Cloudy
20.0 " Finished Finished
20.25 " Cloudy Clear
20.5 " Cloudy Clear
The two methods of testing give the same result. But this balance is
disturbed in the presence of much nitre, the indications with baric chloride
being disturbed by an opalescence for some c.c. beyond the finishing point.
In solutions containing free hydrochloric or nitric acid, a precipitate is
obtained with either baric chloride or sulphuric acid.
Effect of Varying Sulphur.—In these and the subsequent experiments the
titrations were performed in the presence of 10 grams of sodic acetate and
10 c.c. of acetic acid in the manner already described.
Standard sulphuric acid used 5.0 c.c. 10.0 c.c. 20.0 c.c. 50.0 c.c. 100.0 c.c.
"Baric chloride" required 5.0 " 10.0 " 20.0 " 50.0 " 100.0 "
Effect of Varying Temperature.—With 5 c.c. of standard sulphuric acid
titrated at 15° C., 5 c.c. of baric chloride were required; but with larger
quantities the results were altogether unsatisfactory when titrated cold.
Effect of Varying Bulk.—
Bulk 100.0 c.c. 200.0 c.c. 500.0 c.c. 1000.0 c.c.
"Baric chloride" required 20.0 " 20.0 " 20.0 " 20.5 "
filtered portions in the test tubes with baric chloride as is obtained on
testing with sulphuric acid, a titration was made with 20 c.c. of standard
solution of sulphuric acid, together with the usual quantities of sodic acetate
and acetic acid; and two lots of 2 c.c. each were filtered into two sets of test
tubes after each addition of the standard baric chloride. To one series 3
drops of baric chloride solution were added, and to the other 3 drops of
sulphuric acid. The results were—
"Baric Chloride" With Dilute Sulphuric With Baric Chloride
added. Acid. Solution.
19.5 c.c. Clear Cloudy
19.75 " Clear Cloudy
20.0 " Finished Finished
20.25 " Cloudy Clear
20.5 " Cloudy Clear
The two methods of testing give the same result. But this balance is
disturbed in the presence of much nitre, the indications with baric chloride
being disturbed by an opalescence for some c.c. beyond the finishing point.
In solutions containing free hydrochloric or nitric acid, a precipitate is
obtained with either baric chloride or sulphuric acid.
Effect of Varying Sulphur.—In these and the subsequent experiments the
titrations were performed in the presence of 10 grams of sodic acetate and
10 c.c. of acetic acid in the manner already described.
Standard sulphuric acid used 5.0 c.c. 10.0 c.c. 20.0 c.c. 50.0 c.c. 100.0 c.c.
"Baric chloride" required 5.0 " 10.0 " 20.0 " 50.0 " 100.0 "
Effect of Varying Temperature.—With 5 c.c. of standard sulphuric acid
titrated at 15° C., 5 c.c. of baric chloride were required; but with larger
quantities the results were altogether unsatisfactory when titrated cold.
Effect of Varying Bulk.—
Bulk 100.0 c.c. 200.0 c.c. 500.0 c.c. 1000.0 c.c.
"Baric chloride" required 20.0 " 20.0 " 20.0 " 20.5 "
Page 469
Considerable variation in bulk has no effect, but 500 c.c. is the most
convenient volume to work with. It is well to occasionally replace the water
boiled off during titration.
Effect of Foreign Salts.—In all these experiments 20 c.c. of "sulphuric
acid" were used, and the titration was performed in the ordinary way.
Sodic chloride added 0 gram 5 grams 10 grams
"Baric chloride" required 20.0 c.c. 20.0 c.c. 19.7 c.c.
Ammonic chloride added 0 gram 5 grams 10 grams
"Baric chloride" required 20.0 c.c. 20.0 c.c. 19.5 c.c.
Calcic chloride added 0 gram 1 gram 2 grams 5 grams
"Baric chloride" required 20.0 c.c. 20.0 c.c. 19.2 c.c. 19.0 c.c.
Zinc chloride added 0 gram 1 gram 3 grams 5 grams
"Baric chloride" required 20.0 c.c. 20.0 c.c. 20.0 c.c. 20.0 c.c.
Ferrous chloride added 0 gram 1 gram 3 grams 5 grams
"Baric chloride" required 20.0 c.c. 19.7 c.c. 19.5 c.c. 19.0 c.c.
Ferric chloride added 0 gram 1 gram 3 grams 5 grams
"Baric chloride" required 20.0 c.c. 20.0 c.c. 20.0 c.c. 20.0 c.c.
Copper chloride added 0 gram 1 gram 3 grams 5 grams
"Baric chloride" required 20.0 c.c. 20.0 c.c. 20.0 c.c. 20.0 c.c.
Potassic Nitrate added 0 gram 1 gram 5 grams 10 grams
"Baric chloride" required 20.0 c.c. 20.0 c.c. 20.0 c.c. 19.0 c.c.
Potassic Nitrite added 0 gram 1 gram 5 grams
"Baric chloride" required 20.0 c.c. 20.0 c.c. 20.0 c.c.
Sodic phosphate added 0 gram 1 gram
"Baric chloride" required 20.0 c.c. 22.5 c.c.
Sodic arsenate added 0 gram 1 gram
"Baric chloride" required 20.0 c.c. 20.5 c.c.
In the absence of ferric salts, phosphates and arsenates count as sulphur.
In two series of experiments for determining the effect of varying amounts
of sulphur in the form of ferrous sulphate, we obtained the following
results:—In the first series the assay solution was prepared in the manner
we have described for Pyrites; and in the second series, by fusion with nitre.
convenient volume to work with. It is well to occasionally replace the water
boiled off during titration.
Effect of Foreign Salts.—In all these experiments 20 c.c. of "sulphuric
acid" were used, and the titration was performed in the ordinary way.
Sodic chloride added 0 gram 5 grams 10 grams
"Baric chloride" required 20.0 c.c. 20.0 c.c. 19.7 c.c.
Ammonic chloride added 0 gram 5 grams 10 grams
"Baric chloride" required 20.0 c.c. 20.0 c.c. 19.5 c.c.
Calcic chloride added 0 gram 1 gram 2 grams 5 grams
"Baric chloride" required 20.0 c.c. 20.0 c.c. 19.2 c.c. 19.0 c.c.
Zinc chloride added 0 gram 1 gram 3 grams 5 grams
"Baric chloride" required 20.0 c.c. 20.0 c.c. 20.0 c.c. 20.0 c.c.
Ferrous chloride added 0 gram 1 gram 3 grams 5 grams
"Baric chloride" required 20.0 c.c. 19.7 c.c. 19.5 c.c. 19.0 c.c.
Ferric chloride added 0 gram 1 gram 3 grams 5 grams
"Baric chloride" required 20.0 c.c. 20.0 c.c. 20.0 c.c. 20.0 c.c.
Copper chloride added 0 gram 1 gram 3 grams 5 grams
"Baric chloride" required 20.0 c.c. 20.0 c.c. 20.0 c.c. 20.0 c.c.
Potassic Nitrate added 0 gram 1 gram 5 grams 10 grams
"Baric chloride" required 20.0 c.c. 20.0 c.c. 20.0 c.c. 19.0 c.c.
Potassic Nitrite added 0 gram 1 gram 5 grams
"Baric chloride" required 20.0 c.c. 20.0 c.c. 20.0 c.c.
Sodic phosphate added 0 gram 1 gram
"Baric chloride" required 20.0 c.c. 22.5 c.c.
Sodic arsenate added 0 gram 1 gram
"Baric chloride" required 20.0 c.c. 20.5 c.c.
In the absence of ferric salts, phosphates and arsenates count as sulphur.
In two series of experiments for determining the effect of varying amounts
of sulphur in the form of ferrous sulphate, we obtained the following
results:—In the first series the assay solution was prepared in the manner
we have described for Pyrites; and in the second series, by fusion with nitre.
Page 470
Sulphur added 0.050 gram0.100 gram0.200 gram
"Baric chloride" required (1) 5.0 c.c. 10.0 c.c. 20.0 c.c.
" " (2) 4.7 " 10.0 " 20.0 "
Sulphur added 0.500 gram1.000 gram
"Baric chloride" required (1) 50.0 c.c. 100.0 c.c.
" " (2) 50.0 " 100.0 "
More than 5 grams of nitre must not be used in an assay; and, since the
requisite amount of nitre considerably exceeds that sufficient to oxidise the
sulphur, not more than 0.5 gram of unoxidised sulphur should be present in
the portion of the sample weighed up for determination. When the amount
of sulphur present is not known within reasonable limits, the test portions
may be tried with a drop of baric chloride solution instead of sulphuric acid,
so that the diminishing quantity of precipitate may give warning of an
approach to the finishing point.
Determination of Sulphur in Blende.—Weigh up 1 gram of dried and
powdered blende, and mix and fuse with 5 grams of nitre in the manner
described. Place the dish and its contents in the titrating-dish, extract with
water, add 10 grams of sodium acetate and 10 c.c. of acetic acid, remove
and wash the platinum-dish, and dilute to 500 c.c.; boil and titrate. In the
example, duplicate determinations required (a) 32.0 c.c., (b) 32.25 c.c.,
giving an average of 32.1 per cent. of sulphur.
Determination of Sulphur in Chalcopyrite (Yellow Copper Ore).—Take
1 gram of the finely-powdered sample, and 5 grams of nitre. Sprinkle a little
of the nitre in a small Wedgwood mortar, place the ore on it, and cover with
2 or 3 grams more of the nitre. Rub up together, and transfer to a small
porcelain dish; clean out the mortar with the rest of the nitre, and add to the
contents of the dish. Cover with a piece of platinum foil, and heat gently
with a Bunsen burner till the nitre melts and the stuff shows signs of
deflagrating; remove the heat, and allow the action to go on by itself for a
minute or so, then heat over the Bunsen burner for 10 minutes. Cool;
transfer the whole to the titrating-dish; boil with 500 c.c. of water; remove
the small dish and foil; add sodic acetate and acetic acid, and titrate.
For example, 1 gram required 34.5 c.c. of "barium chloride" (standard =
1.005 gram S), which is equivalent to 34.7 per cent. sulphur. The theoretical
"Baric chloride" required (1) 5.0 c.c. 10.0 c.c. 20.0 c.c.
" " (2) 4.7 " 10.0 " 20.0 "
Sulphur added 0.500 gram1.000 gram
"Baric chloride" required (1) 50.0 c.c. 100.0 c.c.
" " (2) 50.0 " 100.0 "
More than 5 grams of nitre must not be used in an assay; and, since the
requisite amount of nitre considerably exceeds that sufficient to oxidise the
sulphur, not more than 0.5 gram of unoxidised sulphur should be present in
the portion of the sample weighed up for determination. When the amount
of sulphur present is not known within reasonable limits, the test portions
may be tried with a drop of baric chloride solution instead of sulphuric acid,
so that the diminishing quantity of precipitate may give warning of an
approach to the finishing point.
Determination of Sulphur in Blende.—Weigh up 1 gram of dried and
powdered blende, and mix and fuse with 5 grams of nitre in the manner
described. Place the dish and its contents in the titrating-dish, extract with
water, add 10 grams of sodium acetate and 10 c.c. of acetic acid, remove
and wash the platinum-dish, and dilute to 500 c.c.; boil and titrate. In the
example, duplicate determinations required (a) 32.0 c.c., (b) 32.25 c.c.,
giving an average of 32.1 per cent. of sulphur.
Determination of Sulphur in Chalcopyrite (Yellow Copper Ore).—Take
1 gram of the finely-powdered sample, and 5 grams of nitre. Sprinkle a little
of the nitre in a small Wedgwood mortar, place the ore on it, and cover with
2 or 3 grams more of the nitre. Rub up together, and transfer to a small
porcelain dish; clean out the mortar with the rest of the nitre, and add to the
contents of the dish. Cover with a piece of platinum foil, and heat gently
with a Bunsen burner till the nitre melts and the stuff shows signs of
deflagrating; remove the heat, and allow the action to go on by itself for a
minute or so, then heat over the Bunsen burner for 10 minutes. Cool;
transfer the whole to the titrating-dish; boil with 500 c.c. of water; remove
the small dish and foil; add sodic acetate and acetic acid, and titrate.
For example, 1 gram required 34.5 c.c. of "barium chloride" (standard =
1.005 gram S), which is equivalent to 34.7 per cent. sulphur. The theoretical
Page 471
percentage is 34.8.
Determination of Sulphur in Chalcocite (Grey Copper Ore).—Proceed as
in the last experiment but, since the action with nitre is more moderate, no
special precautions need be taken on heating. A platinum dish may be used.
An example which was heated for 30 minutes required 20.5 c.c. of the
barium chloride solution. This is equivalent to 20.6 per cent. of sulphur. The
theoretical yield is 20.2 per cent.
Determination of Sulphur in Pyrites.—Take 1 gram of the finely-
powdered sample, cover with 10 c.c. of nitric acid, and, when action has
ceased, evaporate to a small bulk. Add 3 or 4 c.c. of hydrochloric acid, and
again evaporate to a paste. Take up with 1 or 2 c.c. of dilute hydrochloric
acid, dilute with water, transfer to a titrating-dish, add 10 grams of sodic
acetate and 5 c.c. of acetic acid, and dilute with water to 500 c.c. Boil and
titrate.
An example with 1 gram of a pure crystallized pyrites required 52.7 c.c. of
the barium chloride solution, which is equivalent to 53.0 per cent. of
sulphur. Theory requires 53.3 per cent. of sulphur.
Determination of Sulphur in Mispickel.—Take 1 gram of the powdered
ore and evaporate with 10 c.c. of nitric acid, and take up with 3 or 4 c.c. of
hydrochloric acid. If any globules of sulphur remain, again evaporate with
nitric acid. Dilute, and transfer to the titrating-dish. Add 10 grams of sodic
acetate, dilute with water, boil, and titrate. The mispickel carries (according
to theory) exactly sufficient iron to precipitate the arsenic as ferric arsenate
in an acetic acid solution, so no more iron need be added. The ferric
arsenate will separate out as a yellowish-white flocculent precipitate.
An example required, in duplicate experiment, 18.5 c.c. and 18.7 c.c. of
barium chloride, equivalent to 18.7 per cent. of sulphur. The formula,
FeS2.FeAs2, requires 19.6 percent., but the sulphur generally varies
considerably from this amount.
Determination of Sulphur in Burnt Ores.—Take 5 grams of the dried and
powdered ore, and rub up with 4 grams of nitre; transfer to the platinum-
dish; clean out the mortar with another gram of nitre, and add this as a
Determination of Sulphur in Chalcocite (Grey Copper Ore).—Proceed as
in the last experiment but, since the action with nitre is more moderate, no
special precautions need be taken on heating. A platinum dish may be used.
An example which was heated for 30 minutes required 20.5 c.c. of the
barium chloride solution. This is equivalent to 20.6 per cent. of sulphur. The
theoretical yield is 20.2 per cent.
Determination of Sulphur in Pyrites.—Take 1 gram of the finely-
powdered sample, cover with 10 c.c. of nitric acid, and, when action has
ceased, evaporate to a small bulk. Add 3 or 4 c.c. of hydrochloric acid, and
again evaporate to a paste. Take up with 1 or 2 c.c. of dilute hydrochloric
acid, dilute with water, transfer to a titrating-dish, add 10 grams of sodic
acetate and 5 c.c. of acetic acid, and dilute with water to 500 c.c. Boil and
titrate.
An example with 1 gram of a pure crystallized pyrites required 52.7 c.c. of
the barium chloride solution, which is equivalent to 53.0 per cent. of
sulphur. Theory requires 53.3 per cent. of sulphur.
Determination of Sulphur in Mispickel.—Take 1 gram of the powdered
ore and evaporate with 10 c.c. of nitric acid, and take up with 3 or 4 c.c. of
hydrochloric acid. If any globules of sulphur remain, again evaporate with
nitric acid. Dilute, and transfer to the titrating-dish. Add 10 grams of sodic
acetate, dilute with water, boil, and titrate. The mispickel carries (according
to theory) exactly sufficient iron to precipitate the arsenic as ferric arsenate
in an acetic acid solution, so no more iron need be added. The ferric
arsenate will separate out as a yellowish-white flocculent precipitate.
An example required, in duplicate experiment, 18.5 c.c. and 18.7 c.c. of
barium chloride, equivalent to 18.7 per cent. of sulphur. The formula,
FeS2.FeAs2, requires 19.6 percent., but the sulphur generally varies
considerably from this amount.
Determination of Sulphur in Burnt Ores.—Take 5 grams of the dried and
powdered ore, and rub up with 4 grams of nitre; transfer to the platinum-
dish; clean out the mortar with another gram of nitre, and add this as a
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cover. Heat, and extract with water as before; add the sodium acetate and
acetic acid; and titrate. Burnt ores carry from 2.5 to 5 per cent. of sulphur. A
series of four determinations gave:—
"Baric Chloride" Required. Percentage of Sulphur. Gravimetric Results.
12.6 c.c. 2.52 % 2.45 %
29.9 " 5.98 " 5.84 "
18.1 " 3.62 " 3.53 "
22.0 " 4.40 " 4.43 "
For ores carrying less than 1 per cent. of sulphur, take 10 grams for the
assay.
Determination of Sulphuric Oxide (SO3) in Sulphates.—When the
sulphur exists in the sample received by the assayer in an oxidised state as
sulphate, it is usual to report it in terms of sulphuric oxide (SO3). In this
case, the metal must also be reported as oxide. For example, an analysis of
copper sulphate would be thus reported:—
Oxide of copper (CuO) 31.8 %
Sulphuric oxide (SO3) 32.1 "
Water 36.1 "
———
100.0
The percentage of sulphur multiplied by 2.5 gives the percentage of
sulphuric oxide. Thus a sample of copper sulphate containing 12.85 per
cent. of sulphur will contain 12.85 × 2.5 or 32.12 per cent. of sulphuric
oxide.
In minerals and metallurgical products, it is common to find the sulphur in
both conditions—i.e., as sulphate and sulphide. Generally in these the
percentage of sulphur only is wanted; but this will depend entirely on
commercial requirements, and not on the fancy of the assayer. Soluble
sulphates are determined separately by extracting with small quantities of
cold water, so as to avoid the separation of basic sulphates, or, if the
sulphides present are not at the same time attacked, by dilute hydrochloric
acetic acid; and titrate. Burnt ores carry from 2.5 to 5 per cent. of sulphur. A
series of four determinations gave:—
"Baric Chloride" Required. Percentage of Sulphur. Gravimetric Results.
12.6 c.c. 2.52 % 2.45 %
29.9 " 5.98 " 5.84 "
18.1 " 3.62 " 3.53 "
22.0 " 4.40 " 4.43 "
For ores carrying less than 1 per cent. of sulphur, take 10 grams for the
assay.
Determination of Sulphuric Oxide (SO3) in Sulphates.—When the
sulphur exists in the sample received by the assayer in an oxidised state as
sulphate, it is usual to report it in terms of sulphuric oxide (SO3). In this
case, the metal must also be reported as oxide. For example, an analysis of
copper sulphate would be thus reported:—
Oxide of copper (CuO) 31.8 %
Sulphuric oxide (SO3) 32.1 "
Water 36.1 "
———
100.0
The percentage of sulphur multiplied by 2.5 gives the percentage of
sulphuric oxide. Thus a sample of copper sulphate containing 12.85 per
cent. of sulphur will contain 12.85 × 2.5 or 32.12 per cent. of sulphuric
oxide.
In minerals and metallurgical products, it is common to find the sulphur in
both conditions—i.e., as sulphate and sulphide. Generally in these the
percentage of sulphur only is wanted; but this will depend entirely on
commercial requirements, and not on the fancy of the assayer. Soluble
sulphates are determined separately by extracting with small quantities of
cold water, so as to avoid the separation of basic sulphates, or, if the
sulphides present are not at the same time attacked, by dilute hydrochloric
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acid. Lead sulphate may be extracted by boiling with ammonic acetate;
whilst barium, strontium, and, perhaps, calcium sulphate, will be mainly
found in the residue insoluble in acids.
Weigh up from 2 to 5 grams of the material according to the amount of
sulphur judged to be present, and dissolve them in the titrating-dish with 1
c.c. of hydrochloric acid and 50 c.c. of water. Add 10 grams of sodic
acetate, and 10 c.c. of acetic acid; dilute, boil, and titrate. In the case of
ferric salts, half the quantity of acetic acid will be better, as then the ferric
iron will be precipitated, and a colourless solution will be left, in which the
end reaction is more readily distinguished.
Determined in this way, 5 gram samples of the following salts gave the
results indicated below:—
Salt. "Barium Chloride" Required. Sulphuric Oxide.
Copper sulphate 64.25 c.c. 32.12 %
Magnesium sulphate 65.25 " 32.62 "
Zinc sulphate 56.25 " 28.12 "
Ferrous sulphate 58.25 " 29.12 "
Sodium sulphate 51.25 " 25.60 "
Determination of Sulphuric Oxide in Barytes (Heavy spar).—Fuse 2
grams of the powdered mineral with 5 grams of "fusion mixture" for five
minutes; and, when cold, extract with water. Filter, acidulate the filtrate
with an excess of 10 c.c. of acetic acid, dilute, boil, and titrate. For example,
a transparent crystallised sample required 27.0 c.c. of barium chloride,
which is equivalent to 13.6 per cent. of sulphur, or 34.0 per cent. of
sulphuric oxide. Theory requires 34.3 per cent. of the latter. Since both
carbonate of soda and potash are liable to contain sulphates, a blank
determination should be made on 5 grams of the "fusion mixture," and the
amount found be deducted from that got in the assay.
PRACTICAL EXERCISES.
1. The price of sulphur in an ore being 4-1/2d. per unit in the northern
markets, what would be the price of a ton of ore containing 49 per cent. of
whilst barium, strontium, and, perhaps, calcium sulphate, will be mainly
found in the residue insoluble in acids.
Weigh up from 2 to 5 grams of the material according to the amount of
sulphur judged to be present, and dissolve them in the titrating-dish with 1
c.c. of hydrochloric acid and 50 c.c. of water. Add 10 grams of sodic
acetate, and 10 c.c. of acetic acid; dilute, boil, and titrate. In the case of
ferric salts, half the quantity of acetic acid will be better, as then the ferric
iron will be precipitated, and a colourless solution will be left, in which the
end reaction is more readily distinguished.
Determined in this way, 5 gram samples of the following salts gave the
results indicated below:—
Salt. "Barium Chloride" Required. Sulphuric Oxide.
Copper sulphate 64.25 c.c. 32.12 %
Magnesium sulphate 65.25 " 32.62 "
Zinc sulphate 56.25 " 28.12 "
Ferrous sulphate 58.25 " 29.12 "
Sodium sulphate 51.25 " 25.60 "
Determination of Sulphuric Oxide in Barytes (Heavy spar).—Fuse 2
grams of the powdered mineral with 5 grams of "fusion mixture" for five
minutes; and, when cold, extract with water. Filter, acidulate the filtrate
with an excess of 10 c.c. of acetic acid, dilute, boil, and titrate. For example,
a transparent crystallised sample required 27.0 c.c. of barium chloride,
which is equivalent to 13.6 per cent. of sulphur, or 34.0 per cent. of
sulphuric oxide. Theory requires 34.3 per cent. of the latter. Since both
carbonate of soda and potash are liable to contain sulphates, a blank
determination should be made on 5 grams of the "fusion mixture," and the
amount found be deducted from that got in the assay.
PRACTICAL EXERCISES.
1. The price of sulphur in an ore being 4-1/2d. per unit in the northern
markets, what would be the price of a ton of ore containing 49 per cent. of
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sulphur? What would be the effect on the price of an error of 0.25 per cent.
in the assay?
2. Pyrites carries 50 per cent. of sulphur, and on calcining yields 70 per
cent. of its weight of burnt ore. Supposing the burnt ore carries 3.5 per cent.
of sulphur, what proportion of the sulphur will have been removed in the
calcining?
3. How would blende compare with pyrites as a source of sulphur for
sulphuric acid making?
4. How would you determine the percentage of sulphuric oxide in a sample
of gypsum? What is sulphuric oxide, and what relation does it bear to
sulphur?
5. A mineral contains 20.7 per cent. of water, 32.4 per cent. of lime, and
18.6 per cent. of sulphur. What is its probable composition? What
experiment would you try to determine the accuracy of your conclusion?
SELENIUM
occurs in nature combined with copper, mercury, and lead, in certain rare
minerals. In small quantities it is found in many ores. It is detected in
solution by the red precipitate produced on boiling the acid solution with
sodium sulphite. This reaction is used for its determination.
Solution.—The solution is effected by boiling with nitric acid or aqua
regia, or by fusing with nitre. To separate the selenium, the solution is
evaporated with an excess of hydrochloric acid and a little sodium or
potassium chloride. This destroys any nitric acid that may be present, and
reduces selenic acid (H2SeO4) to selenious (H2SeO3). The solution is
diluted with water, and treated with a solution of sulphite of soda. It is
warmed, and at last boiled. The selenium separates as a red precipitate,
which (on boiling) becomes denser and black. It is collected on a weighed
filter, washed with hot water, dried at 100° C., and weighed as pure
selenium.
Selenium can be precipitated with sulphuretted hydrogen as a sulphide,
which is readily soluble in ammonium sulphide. This sulphide may be
in the assay?
2. Pyrites carries 50 per cent. of sulphur, and on calcining yields 70 per
cent. of its weight of burnt ore. Supposing the burnt ore carries 3.5 per cent.
of sulphur, what proportion of the sulphur will have been removed in the
calcining?
3. How would blende compare with pyrites as a source of sulphur for
sulphuric acid making?
4. How would you determine the percentage of sulphuric oxide in a sample
of gypsum? What is sulphuric oxide, and what relation does it bear to
sulphur?
5. A mineral contains 20.7 per cent. of water, 32.4 per cent. of lime, and
18.6 per cent. of sulphur. What is its probable composition? What
experiment would you try to determine the accuracy of your conclusion?
SELENIUM
occurs in nature combined with copper, mercury, and lead, in certain rare
minerals. In small quantities it is found in many ores. It is detected in
solution by the red precipitate produced on boiling the acid solution with
sodium sulphite. This reaction is used for its determination.
Solution.—The solution is effected by boiling with nitric acid or aqua
regia, or by fusing with nitre. To separate the selenium, the solution is
evaporated with an excess of hydrochloric acid and a little sodium or
potassium chloride. This destroys any nitric acid that may be present, and
reduces selenic acid (H2SeO4) to selenious (H2SeO3). The solution is
diluted with water, and treated with a solution of sulphite of soda. It is
warmed, and at last boiled. The selenium separates as a red precipitate,
which (on boiling) becomes denser and black. It is collected on a weighed
filter, washed with hot water, dried at 100° C., and weighed as pure
selenium.
Selenium can be precipitated with sulphuretted hydrogen as a sulphide,
which is readily soluble in ammonium sulphide. This sulphide may be
Page 475
oxidised with hydrochloric acid and chlorate of potash; and the selenium
separated in the manner described.
TELLURIUM.
Tellurium occurs in nature, native, and in combination with gold, silver,
bismuth and lead. It is sometimes met with in assaying gold ores. It may be
detected by the purple colour it imparts to strong sulphuric acid when
dissolved in the cold, and by the black precipitate of metallic tellurium
which its solutions yield on treatment with a reducing agent. Telluric acid is
reduced to tellurous (with evolution of chlorine) on boiling with
hydrochloric acid.
Solution is effected by boiling with aqua regia, or by fusing with nitre and
sodium carbonate.
Separation.—Tellurium closely resembles selenium in its reactions. It is
separated and determined in the same way. Like it, it forms a sulphide
soluble in ammonium sulphide. It is distinguished from selenium by the
insolubility, in a solution of cyanide of potassium, of the metal precipitated
by sodium sulphite; whereas selenium dissolves, forming a soluble potassic
seleno-cyanide.[102]
For the determination, solution is effected by fusing with nitre and sodium
carbonate, dissolving out the tellurate of potash with water, and boiling with
hydrochloric acid. Tellurous compounds are formed, with evolution of
chlorine; and the solution, on treating with a reducing agent (such as
sulphurous acid or stannous chloride), yields metallic tellurium; which is
washed, dried at 100° C., and weighed.
FOOTNOTES:
[101] BaCl2 + Na2SO4 = BaSO4 + 2NaCl.
[102] Se + KCy = KCySe.
separated in the manner described.
TELLURIUM.
Tellurium occurs in nature, native, and in combination with gold, silver,
bismuth and lead. It is sometimes met with in assaying gold ores. It may be
detected by the purple colour it imparts to strong sulphuric acid when
dissolved in the cold, and by the black precipitate of metallic tellurium
which its solutions yield on treatment with a reducing agent. Telluric acid is
reduced to tellurous (with evolution of chlorine) on boiling with
hydrochloric acid.
Solution is effected by boiling with aqua regia, or by fusing with nitre and
sodium carbonate.
Separation.—Tellurium closely resembles selenium in its reactions. It is
separated and determined in the same way. Like it, it forms a sulphide
soluble in ammonium sulphide. It is distinguished from selenium by the
insolubility, in a solution of cyanide of potassium, of the metal precipitated
by sodium sulphite; whereas selenium dissolves, forming a soluble potassic
seleno-cyanide.[102]
For the determination, solution is effected by fusing with nitre and sodium
carbonate, dissolving out the tellurate of potash with water, and boiling with
hydrochloric acid. Tellurous compounds are formed, with evolution of
chlorine; and the solution, on treating with a reducing agent (such as
sulphurous acid or stannous chloride), yields metallic tellurium; which is
washed, dried at 100° C., and weighed.
FOOTNOTES:
[101] BaCl2 + Na2SO4 = BaSO4 + 2NaCl.
[102] Se + KCy = KCySe.
Page 476
Page 477
CHAPTER XVII.
ARSENIC, PHOSPHORUS, NITROGEN.
ARSENIC.
The chief source of the arsenic of commerce is arsenical pyrites, or
mispickel, which contains about 45 per cent. of arsenic (As). Arsenic also
occurs as a constituent of several comparatively rare minerals; and, as an
impurity, it is very widely distributed. White arsenic is an oxide of arsenic,
and is obtained by roasting arsenical ores, and refining the material (crude
arsenic), which condenses in the flues. Arsenic itself is volatile, and many
of its compounds have the same property. It forms two well-defined series
of salts, corresponding to the oxides: arsenious oxide (As2O3), and arsenic
oxide (As2O5). These combine with bases to form arsenites and arsenates
respectively. Boiling with nitric acid converts the lower into the higher
oxide; and powerful reducing-agents, such as cuprous chloride, have the
opposite effect.
Arsenic may be detected by dissolving the substance in hydrochloric acid,
or in aqua regia (avoiding an excess of nitric acid), and adding a little of
this solution to the contents of a small flask in which hydrogen is being
made by the action of zinc and hydrochloric acid. The ignited jet of
hydrogen assumes a blue colour if arsenic is present, and a cold porcelain
dish held in the flame (fig. 67) becomes coated with a dark deposit of
metallic arsenic. Antimony produces a similar effect, but is distinguished by
the insolubility of its deposit in a cold solution of bleaching-powder.
ARSENIC, PHOSPHORUS, NITROGEN.
ARSENIC.
The chief source of the arsenic of commerce is arsenical pyrites, or
mispickel, which contains about 45 per cent. of arsenic (As). Arsenic also
occurs as a constituent of several comparatively rare minerals; and, as an
impurity, it is very widely distributed. White arsenic is an oxide of arsenic,
and is obtained by roasting arsenical ores, and refining the material (crude
arsenic), which condenses in the flues. Arsenic itself is volatile, and many
of its compounds have the same property. It forms two well-defined series
of salts, corresponding to the oxides: arsenious oxide (As2O3), and arsenic
oxide (As2O5). These combine with bases to form arsenites and arsenates
respectively. Boiling with nitric acid converts the lower into the higher
oxide; and powerful reducing-agents, such as cuprous chloride, have the
opposite effect.
Arsenic may be detected by dissolving the substance in hydrochloric acid,
or in aqua regia (avoiding an excess of nitric acid), and adding a little of
this solution to the contents of a small flask in which hydrogen is being
made by the action of zinc and hydrochloric acid. The ignited jet of
hydrogen assumes a blue colour if arsenic is present, and a cold porcelain
dish held in the flame (fig. 67) becomes coated with a dark deposit of
metallic arsenic. Antimony produces a similar effect, but is distinguished by
the insolubility of its deposit in a cold solution of bleaching-powder.
Page 478
Arsenites are distinguished by the volatility of the chloride; by decolorising
a solution of permanganate of potassium, and by immediately giving a
yellow precipitate with sulphuretted hydrogen. Arsenates are distinguished
(after converting into soda salts by boiling with carbonate of soda and
neutralising) by giving with nitrate of silver a red precipitate, and with
"magnesia mixture" a white crystalline one.
Dry Assay.—There is no dry assay which is trustworthy. The following
method is sometimes used to find the proportion of arsenious oxide in
"crude arsenic":—Weigh up 5 grams of the dried sample, and place them in
a clean dry test-tube about 6 inches long. Tie a small filter-paper over the
mouth of the tube, so as to prevent air-currents. Heat the tube cautiously so
as to sublime off the white arsenic into the upper part of the tube. Cut off
the bottom of the test-tube by wetting whilst hot. Scrape out the arsenic and
weigh it. The weight gives an approximate idea of the quantity, and the
colour of the quality, of the white arsenic obtainable from the sample. Some
workers (sellers) weigh the residue, and determine the white arsenic by
difference. In determining the percentage of moisture in these samples, the
substance is dried on a water-bath or in a water-oven.
WET METHODS.
a solution of permanganate of potassium, and by immediately giving a
yellow precipitate with sulphuretted hydrogen. Arsenates are distinguished
(after converting into soda salts by boiling with carbonate of soda and
neutralising) by giving with nitrate of silver a red precipitate, and with
"magnesia mixture" a white crystalline one.
Dry Assay.—There is no dry assay which is trustworthy. The following
method is sometimes used to find the proportion of arsenious oxide in
"crude arsenic":—Weigh up 5 grams of the dried sample, and place them in
a clean dry test-tube about 6 inches long. Tie a small filter-paper over the
mouth of the tube, so as to prevent air-currents. Heat the tube cautiously so
as to sublime off the white arsenic into the upper part of the tube. Cut off
the bottom of the test-tube by wetting whilst hot. Scrape out the arsenic and
weigh it. The weight gives an approximate idea of the quantity, and the
colour of the quality, of the white arsenic obtainable from the sample. Some
workers (sellers) weigh the residue, and determine the white arsenic by
difference. In determining the percentage of moisture in these samples, the
substance is dried on a water-bath or in a water-oven.
WET METHODS.
Page 479
Solution.—Where, as in crude arsenic, the substance is arsenious oxide
(As2O3) mixed with impurities, the arsenic is best got into solution by
warming with caustic soda, and neutralising the excess with hydrochloric
acid; it will be present as sodium arsenite. Metals and alloys are acted on by
means of nitric acid; or the arsenic may be at the same time dissolved and
separated by distilling with a strongly-acid solution of ferric chloride, in the
way described under Volumetric Methods.
With minerals, mattes, &c., solution is thus effected:—The finely-powdered
substance is mixed (in a large platinum or porcelain crucible) with from six
to ten times its weight of a mixture of equal parts of carbonate of soda and
nitre. The mass is then heated gradually to fusion, and kept for a few
minutes in that state. When cold, it is extracted with warm water, and
filtered from the insoluble residue. The solution, acidified with nitric acid
and boiled, contains the arsenic as sodium arsenate. With mispickel, and
those substances which easily give off arsenic on heating, the substance is
first treated with nitric acid, evaporated to dryness, and then the residue is
treated in the way just described.
When the arsenic is present as arsenite or arsenide, distillation with an acid
solution of ferric chloride will give the whole of the arsenic in the distillate
free from any metal except, perhaps, tin as stannic chloride. With arsenates,
dissolve the substance in acid and then add an excess of soda. Pass
sulphuretted hydrogen into the solution; warm, and filter. Acidulate the
filtrate, and pass sulphuretted hydrogen. Decant off the liquid through a
filter, and digest the precipitate with ammonic carbonate; filter, and re-
precipitate with hydrochloric acid and sulphuretted hydrogen. Allow to
stand in a warm place, and filter off the yellow sulphide of arsenic. Wash it
into a beaker, clean the filter-paper (if necessary) with a drop or two of
dilute ammonia; evaporate with 10 c.c. of dilute nitric acid to a small bulk;
dilute; and filter off the globules of sulphur. The filtrate contains the arsenic
as arsenic acid.
GRAVIMETRIC METHOD.
Having got the arsenic into solution as arsenic acid, and in a volume not
much exceeding 50 c.c., add about 20 c.c. of dilute ammonia and 20 c.c. of
(As2O3) mixed with impurities, the arsenic is best got into solution by
warming with caustic soda, and neutralising the excess with hydrochloric
acid; it will be present as sodium arsenite. Metals and alloys are acted on by
means of nitric acid; or the arsenic may be at the same time dissolved and
separated by distilling with a strongly-acid solution of ferric chloride, in the
way described under Volumetric Methods.
With minerals, mattes, &c., solution is thus effected:—The finely-powdered
substance is mixed (in a large platinum or porcelain crucible) with from six
to ten times its weight of a mixture of equal parts of carbonate of soda and
nitre. The mass is then heated gradually to fusion, and kept for a few
minutes in that state. When cold, it is extracted with warm water, and
filtered from the insoluble residue. The solution, acidified with nitric acid
and boiled, contains the arsenic as sodium arsenate. With mispickel, and
those substances which easily give off arsenic on heating, the substance is
first treated with nitric acid, evaporated to dryness, and then the residue is
treated in the way just described.
When the arsenic is present as arsenite or arsenide, distillation with an acid
solution of ferric chloride will give the whole of the arsenic in the distillate
free from any metal except, perhaps, tin as stannic chloride. With arsenates,
dissolve the substance in acid and then add an excess of soda. Pass
sulphuretted hydrogen into the solution; warm, and filter. Acidulate the
filtrate, and pass sulphuretted hydrogen. Decant off the liquid through a
filter, and digest the precipitate with ammonic carbonate; filter, and re-
precipitate with hydrochloric acid and sulphuretted hydrogen. Allow to
stand in a warm place, and filter off the yellow sulphide of arsenic. Wash it
into a beaker, clean the filter-paper (if necessary) with a drop or two of
dilute ammonia; evaporate with 10 c.c. of dilute nitric acid to a small bulk;
dilute; and filter off the globules of sulphur. The filtrate contains the arsenic
as arsenic acid.
GRAVIMETRIC METHOD.
Having got the arsenic into solution as arsenic acid, and in a volume not
much exceeding 50 c.c., add about 20 c.c. of dilute ammonia and 20 c.c. of
Page 480
"magnesia mixture." Stir with a glass rod, and allow to settle overnight.
Filter, and wash with dilute ammonia, avoiding the use of large quantities of
wash water. Dry, transfer the precipitate to a Berlin crucible, and clean the
filter-paper thoroughly. Burn this paper carefully and completely; and add
the ash to the contents of the crucible, together with 4 or 5 drops of nitric
acid. Evaporate with a Bunsen burner, and slowly ignite, finishing off with
the blow-pipe or muffle. Cool, and weigh. The ignited precipitate is
pyrarsenate of magnesia (Mg2As2O7), and contains 48.4 per cent. of arsenic
(As).
Instead of igniting the precipitate with nitric acid, it may be collected on a
weighed filter-paper, dried at 100° C., and weighed as ammonic-magnesic
arsenate (2AmMgAsO4.H2O), which contains 39.5 per cent. of arsenic. The
results in this case are likely to be a little higher. The drying is very tedious,
and is likely to leave behind more water than is allowed for in the formula.
In a series of determinations in which the arsenic was weighed in both
forms, the results were:—
Ammonic-magnesic Arsenic in Magnesium Arsenic in
Arsenate in grams. grams. Pyrarsenate in grams. grams.
0.0080 0.0032 0.0065 0.0031
0.0400 0.0158 0.0330 0.0160
0.0799 0.0316 0.0633 0.0306
0.1600 0.0632 0.1287 0.0623
0.4000 0.1580 0.3205 0.1551
0.7990 0.3156 0.6435 0.3114
VOLUMETRIC METHODS.
There are two methods: one for determining the arsenic in the lower, and
the other in the higher state of oxidation. In the first-mentioned method this
is done by titrating with a standard solution of iodine; and in the latter with
a solution of uranium acetate. Where the arsenic already exists as arsenious
oxide, or where it is most conveniently separated by distillation as arsenious
chloride, the iodine method should be used; but when the arsenic is
Filter, and wash with dilute ammonia, avoiding the use of large quantities of
wash water. Dry, transfer the precipitate to a Berlin crucible, and clean the
filter-paper thoroughly. Burn this paper carefully and completely; and add
the ash to the contents of the crucible, together with 4 or 5 drops of nitric
acid. Evaporate with a Bunsen burner, and slowly ignite, finishing off with
the blow-pipe or muffle. Cool, and weigh. The ignited precipitate is
pyrarsenate of magnesia (Mg2As2O7), and contains 48.4 per cent. of arsenic
(As).
Instead of igniting the precipitate with nitric acid, it may be collected on a
weighed filter-paper, dried at 100° C., and weighed as ammonic-magnesic
arsenate (2AmMgAsO4.H2O), which contains 39.5 per cent. of arsenic. The
results in this case are likely to be a little higher. The drying is very tedious,
and is likely to leave behind more water than is allowed for in the formula.
In a series of determinations in which the arsenic was weighed in both
forms, the results were:—
Ammonic-magnesic Arsenic in Magnesium Arsenic in
Arsenate in grams. grams. Pyrarsenate in grams. grams.
0.0080 0.0032 0.0065 0.0031
0.0400 0.0158 0.0330 0.0160
0.0799 0.0316 0.0633 0.0306
0.1600 0.0632 0.1287 0.0623
0.4000 0.1580 0.3205 0.1551
0.7990 0.3156 0.6435 0.3114
VOLUMETRIC METHODS.
There are two methods: one for determining the arsenic in the lower, and
the other in the higher state of oxidation. In the first-mentioned method this
is done by titrating with a standard solution of iodine; and in the latter with
a solution of uranium acetate. Where the arsenic already exists as arsenious
oxide, or where it is most conveniently separated by distillation as arsenious
chloride, the iodine method should be used; but when the arsenic is
Page 481
separated as ammonic-magnesic arsenate or as sulphide, the uranium
acetate titration should be adopted.
IODINE PROCESS.
This is based on the fact that sodium arsenite in a solution containing an
excess of bicarbonate of soda is indirectly oxidised by iodine to sodium
arsenate,[103] and that an excess of iodine may be recognised by the blue
colour it strikes with starch. The process is divided into two parts—(1) the
preparation of the solution, and (2) the titration.
Preparation of the Solution.—For substances like crude arsenic, in which
the arsenic is present as arsenious oxide, the method is as follows:—Take a
portion which shall contain from 0.25 to 0.5 gram of the oxide, place in a
beaker, and cover with 10 c.c. of sodic hydrate solution; warm till
dissolved, put a small piece of litmus paper in the solution, and render acid
with dilute hydrochloric acid. Add 2 grams of bicarbonate of soda in
solution, filter (if necessary), and dilute to 100 c.c. The solution is now
ready for titrating.
Where the arsenic has to be separated as arsenious chloride, the process is
as follows:[104]—Weigh up 1 gram of the finely-powdered ore (metals
acetate titration should be adopted.
IODINE PROCESS.
This is based on the fact that sodium arsenite in a solution containing an
excess of bicarbonate of soda is indirectly oxidised by iodine to sodium
arsenate,[103] and that an excess of iodine may be recognised by the blue
colour it strikes with starch. The process is divided into two parts—(1) the
preparation of the solution, and (2) the titration.
Preparation of the Solution.—For substances like crude arsenic, in which
the arsenic is present as arsenious oxide, the method is as follows:—Take a
portion which shall contain from 0.25 to 0.5 gram of the oxide, place in a
beaker, and cover with 10 c.c. of sodic hydrate solution; warm till
dissolved, put a small piece of litmus paper in the solution, and render acid
with dilute hydrochloric acid. Add 2 grams of bicarbonate of soda in
solution, filter (if necessary), and dilute to 100 c.c. The solution is now
ready for titrating.
Where the arsenic has to be separated as arsenious chloride, the process is
as follows:[104]—Weigh up 1 gram of the finely-powdered ore (metals
Page 482
should be hammered out into a thin foil or be used as filings), and place in a
16-ounce flask provided with a well-fitting cork, and connected with a U-
tube, as shown in the drawing (fig. 68). The U-tube should contain 2 or 3
c.c. of water, and is cooled by being placed in a jar or large beaker of cold
water. The water used for cooling should be renewed for each assay.
Pour on the assay in the flask 50 c.c. of a "ferric chloride mixture," made by
dissolving 600 grams of calcium chloride and 300 grams of ferric chloride
in 600 c.c. of hydrochloric acid, and making up to 1 litre with water.
Firmly cork up the apparatus, and boil over a small Bunsen-burner flame
for fifteen or twenty minutes, but avoid evaporating to dryness. Disconnect
the flask, and pour away its contents at once to prevent breakage of the
flask by their solidification. The arsenic will be condensed in the U-tube,
together with the greater part of the hydrochloric acid; transfer the distillate
to a beaker washing out the tube two or three times with water; add a small
piece of litmus paper; neutralise with ammonia; render faintly acid with
dilute hydrochloric acid; add 2 grams of bicarbonate of soda in solution;
and dilute to 250 c.c. The solution is now ready for titrating.
The arsenic comes over in the early part of the distillation, as will be seen
from the following experiment, made on 1 gram of copper precipitate; in
which experiment the distillate was collected in separate portions at equal
intervals, and the arsenic in each portion determined:—
Time Distilling. Iodine Required. Equivalent to Arsenic in the Distillate.
5 minutes 12.0 c.c. 0.0450 gram
5" 0.17 " 0.0005 "
5" 0.0 "
5" 0.0 "
To dryness 0.0 "
The volume of each distillate was about 5 c.c.
In this operation the metals are converted into chlorides by the action of
ferric chloride, which gives up a part of its chlorine, and becomes reduced
to the ferrous salt. The calcium chloride does not enter into the chemical
reaction, but raises the temperature at which the solution boils, and is
16-ounce flask provided with a well-fitting cork, and connected with a U-
tube, as shown in the drawing (fig. 68). The U-tube should contain 2 or 3
c.c. of water, and is cooled by being placed in a jar or large beaker of cold
water. The water used for cooling should be renewed for each assay.
Pour on the assay in the flask 50 c.c. of a "ferric chloride mixture," made by
dissolving 600 grams of calcium chloride and 300 grams of ferric chloride
in 600 c.c. of hydrochloric acid, and making up to 1 litre with water.
Firmly cork up the apparatus, and boil over a small Bunsen-burner flame
for fifteen or twenty minutes, but avoid evaporating to dryness. Disconnect
the flask, and pour away its contents at once to prevent breakage of the
flask by their solidification. The arsenic will be condensed in the U-tube,
together with the greater part of the hydrochloric acid; transfer the distillate
to a beaker washing out the tube two or three times with water; add a small
piece of litmus paper; neutralise with ammonia; render faintly acid with
dilute hydrochloric acid; add 2 grams of bicarbonate of soda in solution;
and dilute to 250 c.c. The solution is now ready for titrating.
The arsenic comes over in the early part of the distillation, as will be seen
from the following experiment, made on 1 gram of copper precipitate; in
which experiment the distillate was collected in separate portions at equal
intervals, and the arsenic in each portion determined:—
Time Distilling. Iodine Required. Equivalent to Arsenic in the Distillate.
5 minutes 12.0 c.c. 0.0450 gram
5" 0.17 " 0.0005 "
5" 0.0 "
5" 0.0 "
To dryness 0.0 "
The volume of each distillate was about 5 c.c.
In this operation the metals are converted into chlorides by the action of
ferric chloride, which gives up a part of its chlorine, and becomes reduced
to the ferrous salt. The calcium chloride does not enter into the chemical
reaction, but raises the temperature at which the solution boils, and is
Page 483
essential for the completion of the distillation.[105] Two experiments with
material containing 3.48 per cent. of arsenic gave—(1) with ferric chloride
alone, 2.74 per cent.; and (2) with the addition of calcium chloride, 3.48 per
cent.
It is always necessary to make a blank determination with 1 gram of
electrotype copper, to find out the amount of arsenic in the ferric chloride
mixture.[106] Unfortunately, a correction is always required. This amounts to
about 0.15 per cent. of arsenic on each assay, even when the mixture has
been purified; and this constitutes the weakness of the method, since, in
some cases, the correction is as much as, or even greater than, the
percentage to be determined.
The acid distillate containing the arsenious chloride may be left for an hour
or so without much fear of oxidation; but it is safer to neutralise and then to
add the bicarbonate of soda, as the following experiments show. Several
portions of a solution, each having a bulk of 100 c.c., were exposed for
varying lengths of time, and the arsenic in each determined.
Acid Solutions. Neutralised Solutions.
Time
"Iodine" Required. Arsenic "Iodine"Required. Arsenic
Exposed.
Found. Found.
18.2 c.c. = 0.0136
— 18.1 c.c. = 0.0136 gram
gram
1 hour 18.2 " = 0.0136 " 18.2 " = 0.0136 "
2 hours 17.7 " = 0.0133 " 18.0 " = 0.0135 "
4 " 17.5 " = 0.0131 " 18.4 " = 0.0138 "
5 " 17.0 " = 0.0127 " 18.3 " = 0.0137 "
The Titration.—Make a standard solution of iodine by weighing up in a
beaker 16.933 grams of iodine and 30 grams of potassium iodide in
crystals; add a few c.c. of water, and, when dissolved, dilute to 1 litre: 100
c.c. will equal 0.500 gram of arsenic.
A solution of starch similar to that used in the iodide-copper assay will be
required. Use 2 c.c. for each assay. Variations in the quantity of starch used
do not interfere; but the solution must be freshly prepared, as after seven or
eight days it becomes useless.
material containing 3.48 per cent. of arsenic gave—(1) with ferric chloride
alone, 2.74 per cent.; and (2) with the addition of calcium chloride, 3.48 per
cent.
It is always necessary to make a blank determination with 1 gram of
electrotype copper, to find out the amount of arsenic in the ferric chloride
mixture.[106] Unfortunately, a correction is always required. This amounts to
about 0.15 per cent. of arsenic on each assay, even when the mixture has
been purified; and this constitutes the weakness of the method, since, in
some cases, the correction is as much as, or even greater than, the
percentage to be determined.
The acid distillate containing the arsenious chloride may be left for an hour
or so without much fear of oxidation; but it is safer to neutralise and then to
add the bicarbonate of soda, as the following experiments show. Several
portions of a solution, each having a bulk of 100 c.c., were exposed for
varying lengths of time, and the arsenic in each determined.
Acid Solutions. Neutralised Solutions.
Time
"Iodine" Required. Arsenic "Iodine"Required. Arsenic
Exposed.
Found. Found.
18.2 c.c. = 0.0136
— 18.1 c.c. = 0.0136 gram
gram
1 hour 18.2 " = 0.0136 " 18.2 " = 0.0136 "
2 hours 17.7 " = 0.0133 " 18.0 " = 0.0135 "
4 " 17.5 " = 0.0131 " 18.4 " = 0.0138 "
5 " 17.0 " = 0.0127 " 18.3 " = 0.0137 "
The Titration.—Make a standard solution of iodine by weighing up in a
beaker 16.933 grams of iodine and 30 grams of potassium iodide in
crystals; add a few c.c. of water, and, when dissolved, dilute to 1 litre: 100
c.c. will equal 0.500 gram of arsenic.
A solution of starch similar to that used in the iodide-copper assay will be
required. Use 2 c.c. for each assay. Variations in the quantity of starch used
do not interfere; but the solution must be freshly prepared, as after seven or
eight days it becomes useless.
Page 484
To standardise the iodine solution, weigh up 0.3 gram of white arsenic;
dissolve in caustic soda; neutralise; after acidulating, add 2 grams of
bicarbonate of soda and 2 c.c. of the starch solution, and dilute to 200 c.c.
with cold water. Fill a burette having a glass stop-cock with the iodine
solution, and run it into the solution of arsenic, rapidly at first, and then
more cautiously, till a final drop produces a blue colour throughout the
solution. Calculate the standard in the usual way. White arsenic contains
75.76 per cent. of arsenic.
The following experiments show the effect of variation in the conditions of
the titration:—
Make a solution of arsenic by dissolving 6.60 grams of white arsenic in 100
c.c. of sodic hydrate solution; render slightly acid with hydrochloric acid;
add 10 grains of bicarbonate of soda, and dilute to 1 litre: 100 c.c. will
contain 0.50 gram of arsenic.
Effect of Varying Temperature.—The reaction goes on very quickly in the
cold, and, since there is no occasion for heating, all titrations should
therefore be carried out cold.
Effect of Varying Bulk.—In these experiments, 20 c.c. of arsenic solution
were taken, 2 grams of bicarbonate of soda and 2 c.c. of starch solution
added, and water supplied to the required bulk. The results were:—
Bulk 50.0 c.c. 100.0 c.c. 250.0 c.c. 500.0 c.c.
"Iodine" required 20.0 " 20.0 " 20.0 " 20.0 "
Considerable variation in bulk does not interfere.
Effect of Varying Bicarbonate of Soda.—This salt must be present in each
titration in considerable excess, to prevent the interference of free acid. The
bicarbonate must be dissolved without heating, as neutral carbonates should
be avoided.
Bicarbonate added1 gram 2 grams 5 grams 10 grams
"Iodine" required 20.1 c.c. 20.0 c.c. 20.1 c.c. 20.0 c.c.
dissolve in caustic soda; neutralise; after acidulating, add 2 grams of
bicarbonate of soda and 2 c.c. of the starch solution, and dilute to 200 c.c.
with cold water. Fill a burette having a glass stop-cock with the iodine
solution, and run it into the solution of arsenic, rapidly at first, and then
more cautiously, till a final drop produces a blue colour throughout the
solution. Calculate the standard in the usual way. White arsenic contains
75.76 per cent. of arsenic.
The following experiments show the effect of variation in the conditions of
the titration:—
Make a solution of arsenic by dissolving 6.60 grams of white arsenic in 100
c.c. of sodic hydrate solution; render slightly acid with hydrochloric acid;
add 10 grains of bicarbonate of soda, and dilute to 1 litre: 100 c.c. will
contain 0.50 gram of arsenic.
Effect of Varying Temperature.—The reaction goes on very quickly in the
cold, and, since there is no occasion for heating, all titrations should
therefore be carried out cold.
Effect of Varying Bulk.—In these experiments, 20 c.c. of arsenic solution
were taken, 2 grams of bicarbonate of soda and 2 c.c. of starch solution
added, and water supplied to the required bulk. The results were:—
Bulk 50.0 c.c. 100.0 c.c. 250.0 c.c. 500.0 c.c.
"Iodine" required 20.0 " 20.0 " 20.0 " 20.0 "
Considerable variation in bulk does not interfere.
Effect of Varying Bicarbonate of Soda.—This salt must be present in each
titration in considerable excess, to prevent the interference of free acid. The
bicarbonate must be dissolved without heating, as neutral carbonates should
be avoided.
Bicarbonate added1 gram 2 grams 5 grams 10 grams
"Iodine" required 20.1 c.c. 20.0 c.c. 20.1 c.c. 20.0 c.c.
Page 485
These results show that large variation in the quantity of bicarbonate has no
effect.
Effect of Free Acid.—In these experiments, the arsenic taken, the starch,
and the bulk were as before, but no bicarbonate was added. In one case the
solution was rendered acid with 5 c.c. of acetic acid, and in the other with 5
c.c. of hydrochloric acid; in both cases the interference was strongly
marked, and no satisfactory finishing point could be obtained. This was
much more marked with the hydrochloric acid.
Effect of Foreign Salts.—The process for getting the arsenic into solution
will exclude all metals except tin, but the solution will be charged with
sodium or ammonium salts in the process of neutralising, so that it is only
necessary to see if these cause any interference. The alkaline hydrates,
including ammonia, are plainly inadmissible, since no free iodine can exist
in their presence. Monocarbonates similarly interfere, but to a much less
extent; hence the necessity for rendering the assay distinctly acid before
adding the bicarbonate of soda.
With 20 c.c. of arsenic solution; and with bulk, soda, and starch as before,
the results obtained were:—
"Iodine" required.
With 20 grams of ammonic chloride 20.0 c.c.
" 20 grams of sodium chloride 20.0 "
" 20 grams of sodium acetate 20.0 "
" 0.050 gram of tin, as stannic chloride 19.6 "
Without any addition 20.0 "
The interference of the stannic salt is probably mechanical, the precipitate
carrying down some arsenious acid.
Effect of Varying Arsenic.—With bulk, starch, and soda as before, but
with varying arsenic, the results were:—
Arsenic added 1.0 c.c. 10.0 c.c. 20.0 c.c. 50.0 c.c. 100.0 c.c.
"Iodine" required 1.1 " 9.9 " 20.0 " 50.0 " 100.0 "
effect.
Effect of Free Acid.—In these experiments, the arsenic taken, the starch,
and the bulk were as before, but no bicarbonate was added. In one case the
solution was rendered acid with 5 c.c. of acetic acid, and in the other with 5
c.c. of hydrochloric acid; in both cases the interference was strongly
marked, and no satisfactory finishing point could be obtained. This was
much more marked with the hydrochloric acid.
Effect of Foreign Salts.—The process for getting the arsenic into solution
will exclude all metals except tin, but the solution will be charged with
sodium or ammonium salts in the process of neutralising, so that it is only
necessary to see if these cause any interference. The alkaline hydrates,
including ammonia, are plainly inadmissible, since no free iodine can exist
in their presence. Monocarbonates similarly interfere, but to a much less
extent; hence the necessity for rendering the assay distinctly acid before
adding the bicarbonate of soda.
With 20 c.c. of arsenic solution; and with bulk, soda, and starch as before,
the results obtained were:—
"Iodine" required.
With 20 grams of ammonic chloride 20.0 c.c.
" 20 grams of sodium chloride 20.0 "
" 20 grams of sodium acetate 20.0 "
" 0.050 gram of tin, as stannic chloride 19.6 "
Without any addition 20.0 "
The interference of the stannic salt is probably mechanical, the precipitate
carrying down some arsenious acid.
Effect of Varying Arsenic.—With bulk, starch, and soda as before, but
with varying arsenic, the results were:—
Arsenic added 1.0 c.c. 10.0 c.c. 20.0 c.c. 50.0 c.c. 100.0 c.c.
"Iodine" required 1.1 " 9.9 " 20.0 " 50.0 " 100.0 "
Page 486
Determination of Arsenic in Metallic Copper.—Put 1 gram of the copper
filings, freed from particles of the file with a magnet, into a 16-oz.-flask;
and distil with the ferric chloride mixture, as above described. Neutralise
the distillate; acidify; add bicarbonate of soda and starch; dilute; and titrate
with the standard solution of iodine.[107] Make a blank determination with 1
gram of electrotype copper, proceeding exactly as with the assay; and
deduct the amount of arsenic found in this experiment from that previously
obtained.
Working in this way on a copper containing 0.38 per cent. of arsenic and
0.80 per cent. of antimony, 0.38 per cent. of arsenic was found.
Determination of White Arsenic in Crude Arsenic.—Weigh out 1 gram
of the dried and powdered substance (or 0.5 gram if rich), and digest with
10 c.c. of a 10 per cent. solution of soda; dilute to about 50 c.c., and filter.
Render faintly acid with hydrochloric acid, and filter (if necessary); add 2
or 3 grams of bicarbonate of soda in solution, then 5 c.c. of starch, and
titrate the cold solution with the standard solution of iodine.
The following is an example:—
1 gram of crude arsenic required 53.7 c.c. "Iodine;"
100 c.c. "Iodine" = 0.6000 gram white arsenic;
100 : 53.7 :: 0.6 : 0.3222, or 32.2 per cent.
With the test-tube method of dry assaying, this same sample gave results
varying from 33 to 35 per cent. of white arsenic, which (judging from its
appearance) was impure.
URANIC ACETATE PROCESS.
This may be looked upon as an alternative to the gravimetric method. It is
applicable in all cases where the arsenic exists in solution as arsenic acid or
as arsenate of soda. The process may be considered in two parts: (1) the
preparation of the solution, and (2) the titration.
Preparation of the Solution.—If the arsenic has been separated as
sulphide, it is sufficient to attack it with 10 or 15 c.c. of nitric acid, and to
filings, freed from particles of the file with a magnet, into a 16-oz.-flask;
and distil with the ferric chloride mixture, as above described. Neutralise
the distillate; acidify; add bicarbonate of soda and starch; dilute; and titrate
with the standard solution of iodine.[107] Make a blank determination with 1
gram of electrotype copper, proceeding exactly as with the assay; and
deduct the amount of arsenic found in this experiment from that previously
obtained.
Working in this way on a copper containing 0.38 per cent. of arsenic and
0.80 per cent. of antimony, 0.38 per cent. of arsenic was found.
Determination of White Arsenic in Crude Arsenic.—Weigh out 1 gram
of the dried and powdered substance (or 0.5 gram if rich), and digest with
10 c.c. of a 10 per cent. solution of soda; dilute to about 50 c.c., and filter.
Render faintly acid with hydrochloric acid, and filter (if necessary); add 2
or 3 grams of bicarbonate of soda in solution, then 5 c.c. of starch, and
titrate the cold solution with the standard solution of iodine.
The following is an example:—
1 gram of crude arsenic required 53.7 c.c. "Iodine;"
100 c.c. "Iodine" = 0.6000 gram white arsenic;
100 : 53.7 :: 0.6 : 0.3222, or 32.2 per cent.
With the test-tube method of dry assaying, this same sample gave results
varying from 33 to 35 per cent. of white arsenic, which (judging from its
appearance) was impure.
URANIC ACETATE PROCESS.
This may be looked upon as an alternative to the gravimetric method. It is
applicable in all cases where the arsenic exists in solution as arsenic acid or
as arsenate of soda. The process may be considered in two parts: (1) the
preparation of the solution, and (2) the titration.
Preparation of the Solution.—If the arsenic has been separated as
sulphide, it is sufficient to attack it with 10 or 15 c.c. of nitric acid, and to
Page 487
heat gently till dissolved, avoiding too high a temperature at first.
Afterwards continue the heat till the separated sulphur runs into globules,
and the bulk of the acid has been reduced to 3 or 4 c.c. Dilute with 20 or 30
c.c. of water; put in a piece of litmus paper; and add dilute ammonia until
just alkaline. Then add 5 c.c. of the sodium acetate and acetic acid solution
(which should make the solution distinctly acid); dilute to 150 c.c., and heat
to boiling. The solution is ready for titrating.
When the arsenic exists in a nitric acid solution mixed with much copper, it
is separated in the way described under Examination of Commercial Copper
(Arsenic and Phosphorus), pages 208, 209.
If the arsenic has been separated as ammonium-magnesium arsenate, and
phosphates are known to be absent; dissolve the precipitate (after filtering,
but without washing) in dilute hydrochloric acid. Add dilute ammonia till a
slight precipitate is formed, and then 5 c.c. of the sodium acetate and acetic
acid solution; dilute to 150 c.c., and heat to boiling. Titrate.
If phosphates are present (which will always be the case if they were
present in the original substance, and no separation with sulphuretted
hydrogen has been made), the phosphorus will count in the subsequent
titration as arsenic (one part of phosphorus counting as 2.4 parts of arsenic).
It will be necessary to dissolve the mixed arsenate and phosphate of
magnesia in hydrochloric acid. Add about four or five times as much iron
(as ferric chloride) as the combined phosphorus and arsenic present will
unite with, and separate by the "basic acetate" process as described under
Phosphorus in the Examination of Commercial Copper, page 209.
Obviously, when phosphates are present, it is easier to separate the arsenic
as sulphide than to precipitate it with the "magnesia mixture."
The Titration.—The standard solution of uranium acetate is made by
dissolving 34.1 grams of the salt (with the help of 25 c.c. of acetic acid) in
water; and diluting to 1 litre. The water and acid are added a little at a time,
and warmed till solution is effected; then cooled, and diluted to the required
volume: 100 c.c. will equal 0.50 gram of arsenic.
The sodic acetate and acetic acid solution is made by dissolving 100 grams
of sodic acetate in 500 c.c. of acetic acid, and diluting with water to 1 litre.
Five c.c. are used for each assay.
Afterwards continue the heat till the separated sulphur runs into globules,
and the bulk of the acid has been reduced to 3 or 4 c.c. Dilute with 20 or 30
c.c. of water; put in a piece of litmus paper; and add dilute ammonia until
just alkaline. Then add 5 c.c. of the sodium acetate and acetic acid solution
(which should make the solution distinctly acid); dilute to 150 c.c., and heat
to boiling. The solution is ready for titrating.
When the arsenic exists in a nitric acid solution mixed with much copper, it
is separated in the way described under Examination of Commercial Copper
(Arsenic and Phosphorus), pages 208, 209.
If the arsenic has been separated as ammonium-magnesium arsenate, and
phosphates are known to be absent; dissolve the precipitate (after filtering,
but without washing) in dilute hydrochloric acid. Add dilute ammonia till a
slight precipitate is formed, and then 5 c.c. of the sodium acetate and acetic
acid solution; dilute to 150 c.c., and heat to boiling. Titrate.
If phosphates are present (which will always be the case if they were
present in the original substance, and no separation with sulphuretted
hydrogen has been made), the phosphorus will count in the subsequent
titration as arsenic (one part of phosphorus counting as 2.4 parts of arsenic).
It will be necessary to dissolve the mixed arsenate and phosphate of
magnesia in hydrochloric acid. Add about four or five times as much iron
(as ferric chloride) as the combined phosphorus and arsenic present will
unite with, and separate by the "basic acetate" process as described under
Phosphorus in the Examination of Commercial Copper, page 209.
Obviously, when phosphates are present, it is easier to separate the arsenic
as sulphide than to precipitate it with the "magnesia mixture."
The Titration.—The standard solution of uranium acetate is made by
dissolving 34.1 grams of the salt (with the help of 25 c.c. of acetic acid) in
water; and diluting to 1 litre. The water and acid are added a little at a time,
and warmed till solution is effected; then cooled, and diluted to the required
volume: 100 c.c. will equal 0.50 gram of arsenic.
The sodic acetate and acetic acid solution is made by dissolving 100 grams
of sodic acetate in 500 c.c. of acetic acid, and diluting with water to 1 litre.
Five c.c. are used for each assay.
Page 488
The solution of potassic ferrocyanide used as indicator is made by
dissolving 10 grams of the salt in 100 c.c. of water.
To standardise the solution of uranium acetate, weigh up a quantity of white
arsenic (As2O3) which shall be about equivalent to the arsenic contained in
the assay (0.1 or 0.2 gram); transfer to a flask, and dissolve in 10 c.c. of
nitric acid with the aid of heat. Evaporate to a small bulk (taking care to
avoid the presence of hydrochloric acid); dilute with water; add a small
piece of litmus paper; render faintly alkaline with ammonia; then add 5 c.c.
of the sodic acetate mixture; dilute to 150 c.c.; and heat to boiling.
Fill an ordinary burette with the uranium acetate solution, and run into the
assay a quantity known to be insufficient. Again heat for a minute or two.
Arrange a series of drops of the solution of ferrocyanide of potassium on a
porcelain slab, and, with the help of a glass rod, bring a drop of the assay
solution in contact with one of these. If no colour is produced, run in the
uranium acetate, 1 c.c. at a time, testing after each addition, till a brown
colour is developed. It is best to overdo the assay, and to count back. It is
not necessary to filter off a portion of the assay before testing with the
"ferrocyanide," since the precipitate (uranic arsenate) has no effect.
The following experiments show the effect of variation in the conditions of
titration. Make a solution of arsenic acid by dissolving 4.95 grams of
arsenious acid (As2O3) in a covered beaker with 35 c.c. of nitric acid;
evaporate down to 7 or 8 c.c.; and dilute with water to 1 litre: 100 c.c. will
contain 0.375 gram of arsenic. Use 20 c.c. for each experiment.
Effect of Varying Temperature.—It is generally recommended to titrate
the boiling solution, since it is possible that the precipitation is only
complete on boiling. Low results are obtained in a cold solution, the
apparent excess of uranium acetate striking a colour at once; on boiling,
however, it ceases to do so; consequently, the solution should always be
boiled directly before testing.
In four experiments made in the way described, but with 20 c.c. of a
solution of arsenic acid stronger than that given (100 c.c. = 0.5 gram As),
the results at varying temperatures were:—
dissolving 10 grams of the salt in 100 c.c. of water.
To standardise the solution of uranium acetate, weigh up a quantity of white
arsenic (As2O3) which shall be about equivalent to the arsenic contained in
the assay (0.1 or 0.2 gram); transfer to a flask, and dissolve in 10 c.c. of
nitric acid with the aid of heat. Evaporate to a small bulk (taking care to
avoid the presence of hydrochloric acid); dilute with water; add a small
piece of litmus paper; render faintly alkaline with ammonia; then add 5 c.c.
of the sodic acetate mixture; dilute to 150 c.c.; and heat to boiling.
Fill an ordinary burette with the uranium acetate solution, and run into the
assay a quantity known to be insufficient. Again heat for a minute or two.
Arrange a series of drops of the solution of ferrocyanide of potassium on a
porcelain slab, and, with the help of a glass rod, bring a drop of the assay
solution in contact with one of these. If no colour is produced, run in the
uranium acetate, 1 c.c. at a time, testing after each addition, till a brown
colour is developed. It is best to overdo the assay, and to count back. It is
not necessary to filter off a portion of the assay before testing with the
"ferrocyanide," since the precipitate (uranic arsenate) has no effect.
The following experiments show the effect of variation in the conditions of
titration. Make a solution of arsenic acid by dissolving 4.95 grams of
arsenious acid (As2O3) in a covered beaker with 35 c.c. of nitric acid;
evaporate down to 7 or 8 c.c.; and dilute with water to 1 litre: 100 c.c. will
contain 0.375 gram of arsenic. Use 20 c.c. for each experiment.
Effect of Varying Temperature.—It is generally recommended to titrate
the boiling solution, since it is possible that the precipitation is only
complete on boiling. Low results are obtained in a cold solution, the
apparent excess of uranium acetate striking a colour at once; on boiling,
however, it ceases to do so; consequently, the solution should always be
boiled directly before testing.
In four experiments made in the way described, but with 20 c.c. of a
solution of arsenic acid stronger than that given (100 c.c. = 0.5 gram As),
the results at varying temperatures were:—
Page 489
Temperature 15° C. 30° C. 70° C. 100° C.
"Uranium" required 18.0 c.c. 18.5 c.c. 18.5 c.c. 18.7 c.c.
Effect of Varying Bulk.—These experiments were like those last mentioned, but
were titrated boiling, and the volume was varied:—
Bulk 50.0 c.c. 100.0 c.c. 200.0 c.c. 300.0 c.c.
"Uranium" required 14.0 " 14.0 " 14.5 " 15.0 "
Considerable variations in bulk are to be avoided.
Effect of Varying Sodium Acetate.—These experiments were carried out like
those last noticed, but the bulk was 150 c.c., and varying amounts of sodic acetate
were added in excess of the quantity used in the experiments previously described:
—
Sodic acetate added 0 gram 1 gram 10 grams 20 grams
"Uranium" required 14.5 c.c. 14.5 c.c. 16.0 c.c. 18.0 c.c.
It is evidently important that the quantity of this salt present in each titration be
measured out, so as to avoid variation.
Effect of Varying the Sodium Acetate and Acetic Acid Solution.—Acetic Acid
also affects the results, but in the opposite direction, by preventing the precipitation
of uranium arsenate. With varying volumes of the solution now under notice, the
results were:—
Solution added 0.0 c.c. 5.0 c.c. 10.0 c.c. 15.0 c.c.
"Uranium" required 14.5 " 14.5 " 14.5 " 14.0 "
Solution added 20.0 " 30.0 " 40.0 " 50.0 "
"Uranium" required 13.2 " 10.0 " 6.0 " 2.0 "
These show that the quantity ordered (5 c.c.) must be adhered to.
Effect of Foreign Salts.—In these experiments, 10 grams of the salt (the effect of
which it was desired to determine) were added to a solution in other respects
resembling those previously used:—
Ammonic Ammonic Ammonic Magnesium
Salt added
sulphate nitrate chloride sulphate
"Uranium"
15.5 c.c. 15.5 c.c. 15.3 c.c. 15.3 c.c.
required
"Uranium" required 18.0 c.c. 18.5 c.c. 18.5 c.c. 18.7 c.c.
Effect of Varying Bulk.—These experiments were like those last mentioned, but
were titrated boiling, and the volume was varied:—
Bulk 50.0 c.c. 100.0 c.c. 200.0 c.c. 300.0 c.c.
"Uranium" required 14.0 " 14.0 " 14.5 " 15.0 "
Considerable variations in bulk are to be avoided.
Effect of Varying Sodium Acetate.—These experiments were carried out like
those last noticed, but the bulk was 150 c.c., and varying amounts of sodic acetate
were added in excess of the quantity used in the experiments previously described:
—
Sodic acetate added 0 gram 1 gram 10 grams 20 grams
"Uranium" required 14.5 c.c. 14.5 c.c. 16.0 c.c. 18.0 c.c.
It is evidently important that the quantity of this salt present in each titration be
measured out, so as to avoid variation.
Effect of Varying the Sodium Acetate and Acetic Acid Solution.—Acetic Acid
also affects the results, but in the opposite direction, by preventing the precipitation
of uranium arsenate. With varying volumes of the solution now under notice, the
results were:—
Solution added 0.0 c.c. 5.0 c.c. 10.0 c.c. 15.0 c.c.
"Uranium" required 14.5 " 14.5 " 14.5 " 14.0 "
Solution added 20.0 " 30.0 " 40.0 " 50.0 "
"Uranium" required 13.2 " 10.0 " 6.0 " 2.0 "
These show that the quantity ordered (5 c.c.) must be adhered to.
Effect of Foreign Salts.—In these experiments, 10 grams of the salt (the effect of
which it was desired to determine) were added to a solution in other respects
resembling those previously used:—
Ammonic Ammonic Ammonic Magnesium
Salt added
sulphate nitrate chloride sulphate
"Uranium"
15.5 c.c. 15.5 c.c. 15.3 c.c. 15.3 c.c.
required
Page 490
Without any addition, 15.0 c.c. were required; and in another experiment, in which
30 grams of ammonic salts were present, 15.6 c.c. of uranium solution were
required. Such variations in the amount of ammonic salts as occur in ordinary
working are unimportant.
Phosphates, of course, interfere. In fact, the uranium acetate solution can be
standardised by titrating with a known weight of phosphate, and calculating its
equivalent of arsenic. Thus, in an experiment with 0.6 gram of hydric sodic
phosphate (Na2HPO4.12H2O), equivalent to 0.05195 gram of phosphorus, or
0.1256 gram of arsenic, 23.25 c.c. of a solution of uranium acetate were required.
The same solution standardised with white arsenic gave a standard of which 100
c.c. = 0.5333 gram arsenic. On this standard the 0.6 gram of sodic phosphate
should have required 23.5 c.c.
Experiments in which 0.1 gram of bismuth and 0.1 gram of antimony were present
with 0.1 gram of arsenic, showed no interference on the titration. Ferric or aluminic
salts would remove their equivalent of arsenic, and, consequently, must be
removed before titrating.
Effect of Varying Arsenic.—Varying amounts of metallic arsenic were weighed
up and dissolved in nitric acid, &c., and titrated:—
Arsenic taken 0.010 gram0.050 gram 0.100 gram0.200 gram
Arsenic found 0.010 " 0.050 " 0.100 " 0.197 "
These experiments show that the method yields good results within these limits.
Determination of Arsenic in Mispickel.—Weigh up 1 gram of the dried and
powdered ore, and evaporate to near dryness with 20 c.c. of dilute nitric acid. Make
up to 100 c.c. with water, and pass sulphuretted hydrogen to reduce the ferric iron
to the ferrous state, then add 20 c.c. of dilute ammonia, and again pass sulphuretted
hydrogen. Warm, filter, and evaporate the filtrate to drive off the excess of
ammonia; then add 10 c.c. of nitric acid, and boil down till the sulphide of arsenic
at first precipitated is dissolved; neutralise; add 5 c.c. of sodium acetate and acetic
acid solution; transfer to a pint flask, boil, and titrate.
For example, an impure sample of ore required, in duplicate assay of half a gram
each, when treated in the above-mentioned way, 39.6 and 39.5 c.c. of the uranium
acetate solution (100 c.c. = 0.537 gram of arsenic), equivalent to 0.2114 gram of
arsenic, or 42.3 per cent.
An alternative method is as follows. Powder the ore very finely and weigh up .5
gram. Place in a 2-3/4 inch berlin dish and add strong nitric acid, one drop at a time
30 grams of ammonic salts were present, 15.6 c.c. of uranium solution were
required. Such variations in the amount of ammonic salts as occur in ordinary
working are unimportant.
Phosphates, of course, interfere. In fact, the uranium acetate solution can be
standardised by titrating with a known weight of phosphate, and calculating its
equivalent of arsenic. Thus, in an experiment with 0.6 gram of hydric sodic
phosphate (Na2HPO4.12H2O), equivalent to 0.05195 gram of phosphorus, or
0.1256 gram of arsenic, 23.25 c.c. of a solution of uranium acetate were required.
The same solution standardised with white arsenic gave a standard of which 100
c.c. = 0.5333 gram arsenic. On this standard the 0.6 gram of sodic phosphate
should have required 23.5 c.c.
Experiments in which 0.1 gram of bismuth and 0.1 gram of antimony were present
with 0.1 gram of arsenic, showed no interference on the titration. Ferric or aluminic
salts would remove their equivalent of arsenic, and, consequently, must be
removed before titrating.
Effect of Varying Arsenic.—Varying amounts of metallic arsenic were weighed
up and dissolved in nitric acid, &c., and titrated:—
Arsenic taken 0.010 gram0.050 gram 0.100 gram0.200 gram
Arsenic found 0.010 " 0.050 " 0.100 " 0.197 "
These experiments show that the method yields good results within these limits.
Determination of Arsenic in Mispickel.—Weigh up 1 gram of the dried and
powdered ore, and evaporate to near dryness with 20 c.c. of dilute nitric acid. Make
up to 100 c.c. with water, and pass sulphuretted hydrogen to reduce the ferric iron
to the ferrous state, then add 20 c.c. of dilute ammonia, and again pass sulphuretted
hydrogen. Warm, filter, and evaporate the filtrate to drive off the excess of
ammonia; then add 10 c.c. of nitric acid, and boil down till the sulphide of arsenic
at first precipitated is dissolved; neutralise; add 5 c.c. of sodium acetate and acetic
acid solution; transfer to a pint flask, boil, and titrate.
For example, an impure sample of ore required, in duplicate assay of half a gram
each, when treated in the above-mentioned way, 39.6 and 39.5 c.c. of the uranium
acetate solution (100 c.c. = 0.537 gram of arsenic), equivalent to 0.2114 gram of
arsenic, or 42.3 per cent.
An alternative method is as follows. Powder the ore very finely and weigh up .5
gram. Place in a 2-3/4 inch berlin dish and add strong nitric acid, one drop at a time
Page 491
until the action ceases; with care there need be no very violent reaction. Dry over a
water bath. Cover with 2 grams of nitre and over this spread 5 grams of a mixture
of equal parts of nitre and carbonate of soda. Fuse in a muffle or over a large gentle
blow-pipe flame for 4 or 5 minutes. This will spoil the dish. Allow to cool and boil
out in a larger dish with 100 c.c. of water. Filter and wash into an 8 oz. flask.
Acidify the liquor with nitric and boil down to about 100 c.c. The acid should not
be in too large excess, but an excess is needed to destroy nitrites. Neutralise with
soda or ammonia. Add 5 c.c. of the mixture of sodium acetate and acetic acid.
Titrate with uranium acetate.
Determination of Arsenic (As) in Crude Arsenic.—The method given under the
iodine titration simply determines that portion of the arsenic which is present in the
substance as arsenious oxide or white arsenic. The following method will give the
total arsenic in the sample. It would be incorrect to report this as so much per cent.
of arsenious oxide, although it may be reported as so much per cent. of arsenic
equivalent to so much per cent. of white arsenic, thus:—
Arsenic 30.0 per cent.
Equivalent to white arsenic 39.6 "
The equivalent of white arsenic is calculated by multiplying the percentage of
arsenic by 1.32. The method of determining the percentage of arsenic is as follows:
—-Boil 1 gram of the sample with 10 c.c. of nitric acid. When the bulk of the
solution has been reduced to one-half, and red fumes are no longer evolved, dilute
with a little water, and filter into a flask. Neutralise the filtrate, add 5 c.c. of sodic
acetate solution, boil and filter. The precipitate (ferric arsenate) is transferred to a
small beaker, treated with 5 c.c. of dilute ammonia, and sulphuretted hydrogen
passed through it. The iron sulphide is filtered off, and the filtrate evaporated with
an excess of nitric acid. When the solution is clear, it is neutralised, and 1 or 2 c.c.
of sodic acetate solution having been added, is then mixed with the first filtrate.
The solution is boiled and titrated.
A sample treated in this way required 49.2 c.c. of the uranium acetate solution (100
c.c. = 0.537 gram of arsenic), equivalent to 26.4 per cent.
Determination of Arsenic in Brimstone.—Take 10 grams of the substance, and
powder in a mortar; rub up with 10 c.c. of dilute ammonia and a little water; rinse
into a pint flask; pass a current of sulphuretted hydrogen; and warm on a hot plate
for a few minutes. Filter, acidulate the filtrate with sulphuric acid; filter off the
precipitate; attack it with 10 c.c. of nitric acid; and proceed as in the other
determinations.
water bath. Cover with 2 grams of nitre and over this spread 5 grams of a mixture
of equal parts of nitre and carbonate of soda. Fuse in a muffle or over a large gentle
blow-pipe flame for 4 or 5 minutes. This will spoil the dish. Allow to cool and boil
out in a larger dish with 100 c.c. of water. Filter and wash into an 8 oz. flask.
Acidify the liquor with nitric and boil down to about 100 c.c. The acid should not
be in too large excess, but an excess is needed to destroy nitrites. Neutralise with
soda or ammonia. Add 5 c.c. of the mixture of sodium acetate and acetic acid.
Titrate with uranium acetate.
Determination of Arsenic (As) in Crude Arsenic.—The method given under the
iodine titration simply determines that portion of the arsenic which is present in the
substance as arsenious oxide or white arsenic. The following method will give the
total arsenic in the sample. It would be incorrect to report this as so much per cent.
of arsenious oxide, although it may be reported as so much per cent. of arsenic
equivalent to so much per cent. of white arsenic, thus:—
Arsenic 30.0 per cent.
Equivalent to white arsenic 39.6 "
The equivalent of white arsenic is calculated by multiplying the percentage of
arsenic by 1.32. The method of determining the percentage of arsenic is as follows:
—-Boil 1 gram of the sample with 10 c.c. of nitric acid. When the bulk of the
solution has been reduced to one-half, and red fumes are no longer evolved, dilute
with a little water, and filter into a flask. Neutralise the filtrate, add 5 c.c. of sodic
acetate solution, boil and filter. The precipitate (ferric arsenate) is transferred to a
small beaker, treated with 5 c.c. of dilute ammonia, and sulphuretted hydrogen
passed through it. The iron sulphide is filtered off, and the filtrate evaporated with
an excess of nitric acid. When the solution is clear, it is neutralised, and 1 or 2 c.c.
of sodic acetate solution having been added, is then mixed with the first filtrate.
The solution is boiled and titrated.
A sample treated in this way required 49.2 c.c. of the uranium acetate solution (100
c.c. = 0.537 gram of arsenic), equivalent to 26.4 per cent.
Determination of Arsenic in Brimstone.—Take 10 grams of the substance, and
powder in a mortar; rub up with 10 c.c. of dilute ammonia and a little water; rinse
into a pint flask; pass a current of sulphuretted hydrogen; and warm on a hot plate
for a few minutes. Filter, acidulate the filtrate with sulphuric acid; filter off the
precipitate; attack it with 10 c.c. of nitric acid; and proceed as in the other
determinations.
Page 492
PRACTICAL EXERCISES.
1. Mispickel contains 45.0 per cent. of arsenic, to how much white arsenic will this
be equivalent?
2. How would you make a standard solution of iodine so that 100 c.c. shall be
equivalent to 1 gram of white arsenic?
3. What weight of arsenic is contained in 1 gram of pyrarsenate of magnesia, and
what weight of ammonic-magnesic arsenate would it be equivalent to?
4. The residue, after heating 10 grams of crude arsenic, weighed 0.62 gram. What
information does this give as to the composition of the substance? If another 10
grams of the substance, heated on a water-bath, lost 0.43 gram, what conclusions
would you draw, and how would you report your results?
5. If a sample of copper contained 0.5 per cent. of arsenic, and 1 gram of it were
taken for an assay, how much standard uranium acetate solution would be required
in the titration?
PHOSPHORUS AND PHOSPHATES.
Phosphorus rarely occurs among minerals except in its highest oxidized state,
phosphoric oxide (P2O5), in which it occurs abundantly as "rock phosphate," a
variety of apatite which is mainly phosphate of lime. Phosphates of most of the
metallic oxides are found. Phosphoric oxide in small quantities is widely diffused,
and is a constituent of most rocks. Its presence in varying amounts in iron ores is a
matter of importance, since it affects the quality of the iron obtainable from them.
Phosphorus occurs in alloys in the unoxidized state. It is directly combined with
the metal, forming a phosphide. In this manner it occurs in meteoric iron. The alloy
phosphor-bronze is made up of copper, tin, zinc, and phosphorus.
Phosphates are mined in large quantities for the use of manure manufacturers, and
for making phosphorus.
Phosphorus and arsenic closely resemble each other in their chemical properties,
more especially those which the assayer makes use of for their determination.
Phosphorus forms several series of salts; but the phosphates are the only ones
which need be considered. Pyrophosphate of magnesia, which is the form in which
phosphoric oxide is generally weighed, differs from the ordinary phosphate in the
proportion of base to acid. Metaphosphates differ in the same way. If these are
1. Mispickel contains 45.0 per cent. of arsenic, to how much white arsenic will this
be equivalent?
2. How would you make a standard solution of iodine so that 100 c.c. shall be
equivalent to 1 gram of white arsenic?
3. What weight of arsenic is contained in 1 gram of pyrarsenate of magnesia, and
what weight of ammonic-magnesic arsenate would it be equivalent to?
4. The residue, after heating 10 grams of crude arsenic, weighed 0.62 gram. What
information does this give as to the composition of the substance? If another 10
grams of the substance, heated on a water-bath, lost 0.43 gram, what conclusions
would you draw, and how would you report your results?
5. If a sample of copper contained 0.5 per cent. of arsenic, and 1 gram of it were
taken for an assay, how much standard uranium acetate solution would be required
in the titration?
PHOSPHORUS AND PHOSPHATES.
Phosphorus rarely occurs among minerals except in its highest oxidized state,
phosphoric oxide (P2O5), in which it occurs abundantly as "rock phosphate," a
variety of apatite which is mainly phosphate of lime. Phosphates of most of the
metallic oxides are found. Phosphoric oxide in small quantities is widely diffused,
and is a constituent of most rocks. Its presence in varying amounts in iron ores is a
matter of importance, since it affects the quality of the iron obtainable from them.
Phosphorus occurs in alloys in the unoxidized state. It is directly combined with
the metal, forming a phosphide. In this manner it occurs in meteoric iron. The alloy
phosphor-bronze is made up of copper, tin, zinc, and phosphorus.
Phosphates are mined in large quantities for the use of manure manufacturers, and
for making phosphorus.
Phosphorus and arsenic closely resemble each other in their chemical properties,
more especially those which the assayer makes use of for their determination.
Phosphorus forms several series of salts; but the phosphates are the only ones
which need be considered. Pyrophosphate of magnesia, which is the form in which
phosphoric oxide is generally weighed, differs from the ordinary phosphate in the
proportion of base to acid. Metaphosphates differ in the same way. If these are
Page 493
present, it must be remembered they act differently with some reagents from the
ordinary phosphates, which are called orthophosphates. They are, however, all
convertible into orthophosphates by some means which will remove their base,
such as fusion with alkaline carbonates, boiling with strong acids, &c.[108]
Phosphides are converted into phosphates by the action of nitric acid or other
oxidizing agents. Dilute acids, when they act on the substance, evolve
phosphuretted hydrogen (PH3). The student should be on his guard against losing
phosphorus in this manner.
There is no dry assay for phosphorus. All assays for it are made either
gravimetrically or volumetrically.
The separation of phosphoric oxide is made as follows:—The ore or metal is
dissolved in acid and evaporated, to render the silica insoluble. It is taken up with
hydrochloric acid, diluted with water, and treated with sulphuretted hydrogen. The
filtrate is boiled, to get rid of the excess of gas, and treated with nitric acid, to
peroxidize the iron present. If the iron is not present in more than sufficient
quantity to form ferric phosphate with all the phosphorus present, some ferric
chloride is added. The iron is then separated as basic acetate. The precipitate will
contain the phosphorus, together with any arsenic acid not reduced by the
sulphuretted hydrogen. The precipitate should have a decided brown colour. The
precipitate is washed, transferred to a flask, and treated first with ammonia, and
then with a current of sulphuretted hydrogen. The filtrate from this (acidulated with
hydrochloric acid, and, if necessary, filtered) contains the phosphorus as
phosphoric acid. This method is not applicable in the presence of alumina,
chromium, titanium, or tin, if the solution is effected with nitric acid. The
precipitate obtained by the action of nitric acid on tin retains any phosphoric or
arsenic oxide that may be present.
A method of separation more generally applicable and more convenient to work is
based on the precipitation of a yellow phospho-molybdate of ammonia,[109] by the
action of an excess of ammonic molybdate upon a solution of a phosphate in nitric
acid. Dissolve the substance by treatment with acid, and evaporate to dryness. Take
up with 10 c.c. of nitric acid, and add 20 grams of ammonic nitrate, together with a
little water. Next put in the solution of ammonium molybdate solution in the
proportion of about 50 c.c. for each 0.1 gram of phosphoric oxide judged to be
present. Warm to about 80° C., and allow to stand for an hour. Filter, and wash
with a 10 per cent. solution of ammonic nitrate. It is not necessary that the whole
of the precipitate be placed on the filter; but the beaker must be completely
cleaned. Dissolve the precipitate off the filter with dilute ammonia, and run the
solution into the original beaker. Run in from a burette, slowly and with stirring,
ordinary phosphates, which are called orthophosphates. They are, however, all
convertible into orthophosphates by some means which will remove their base,
such as fusion with alkaline carbonates, boiling with strong acids, &c.[108]
Phosphides are converted into phosphates by the action of nitric acid or other
oxidizing agents. Dilute acids, when they act on the substance, evolve
phosphuretted hydrogen (PH3). The student should be on his guard against losing
phosphorus in this manner.
There is no dry assay for phosphorus. All assays for it are made either
gravimetrically or volumetrically.
The separation of phosphoric oxide is made as follows:—The ore or metal is
dissolved in acid and evaporated, to render the silica insoluble. It is taken up with
hydrochloric acid, diluted with water, and treated with sulphuretted hydrogen. The
filtrate is boiled, to get rid of the excess of gas, and treated with nitric acid, to
peroxidize the iron present. If the iron is not present in more than sufficient
quantity to form ferric phosphate with all the phosphorus present, some ferric
chloride is added. The iron is then separated as basic acetate. The precipitate will
contain the phosphorus, together with any arsenic acid not reduced by the
sulphuretted hydrogen. The precipitate should have a decided brown colour. The
precipitate is washed, transferred to a flask, and treated first with ammonia, and
then with a current of sulphuretted hydrogen. The filtrate from this (acidulated with
hydrochloric acid, and, if necessary, filtered) contains the phosphorus as
phosphoric acid. This method is not applicable in the presence of alumina,
chromium, titanium, or tin, if the solution is effected with nitric acid. The
precipitate obtained by the action of nitric acid on tin retains any phosphoric or
arsenic oxide that may be present.
A method of separation more generally applicable and more convenient to work is
based on the precipitation of a yellow phospho-molybdate of ammonia,[109] by the
action of an excess of ammonic molybdate upon a solution of a phosphate in nitric
acid. Dissolve the substance by treatment with acid, and evaporate to dryness. Take
up with 10 c.c. of nitric acid, and add 20 grams of ammonic nitrate, together with a
little water. Next put in the solution of ammonium molybdate solution in the
proportion of about 50 c.c. for each 0.1 gram of phosphoric oxide judged to be
present. Warm to about 80° C., and allow to stand for an hour. Filter, and wash
with a 10 per cent. solution of ammonic nitrate. It is not necessary that the whole
of the precipitate be placed on the filter; but the beaker must be completely
cleaned. Dissolve the precipitate off the filter with dilute ammonia, and run the
solution into the original beaker. Run in from a burette, slowly and with stirring,
Page 494
"magnesia mixture," using about 15 c.c. for each 0.1 gram of phosphoric oxide.
Allow to stand for one hour. The white crystalline precipitate contains the
phosphorus as ammonium-magnesium phosphate.
Phosphate of lead is decomposed by sulphuric acid; the lead is converted into the
insoluble lead sulphate, and the phosphoric acid is dissolved. Phosphate of copper
and phosphate of iron may be treated with sulphuretted hydrogen; the former in an
acid, and the latter in an alkaline, solution. Phosphate of alumina is generally
weighed without separation of the alumina, since this requires a fusion. In all cases
the aim is to get the phosphoric oxide either free, or combined with some metal
whose phosphate is soluble in ammonia.
Joulie's method of separation is as follows:—One to ten grams of the sample are
treated with hydrochloric acid, and evaporated to dryness with the addition (if any
pyrites is present) of a little nitric acid. The residue is taken up with hydrochloric
acid, cooled, transferred to a graduated flask, and diluted to the mark. It is then
shaken up, filtered through a dry filter, and a measured portion (containing about
0.05 gram of phosphoric acid) transferred to a small beaker. Ten c.c. of a citric-acid
solution of magnesia[110] is added, and then an excess of ammonia. If an immediate
precipitate is formed, a fresh portion must be measured out and treated with 20 c.c.
of the citrate of magnesia solution and with ammonia as before. The beaker is put
aside for from two to twelve hours. The precipitate is then filtered off and washed
with weak ammonia; it contains the phosphorus as ammonium-magnesium
phosphate.
GRAVIMETRIC DETERMINATION.
If the phosphate is not already in the form of ammonic-magnesic phosphate, it is
converted into this by the addition to its solution of an excess of ammonia and
"magnesia mixture." In order to get the precipitate pure, the "magnesia mixture" is
run in gradually (by drops) from a burette, with constant stirring. A white
crystalline precipitate at once falls, if much phosphorus is present; but, if there is
only a small quantity, it may be an hour or two before it shows itself. The solution
is best allowed to rest for twelve or fifteen hours (overnight) before filtering. The
presence of tartaric acid should be avoided; and the appearance of the precipitate
should be crystalline. The solution is decanted through a filter, and the precipitate
washed with dilute ammonia, using as little as may be necessary. The precipitate is
dried, transferred to a weighed Berlin or platinum crucible; the filter-paper is
carefully burnt, and its ash added to the precipitate, which is then ignited, at first
gently over a Bunsen burner, and then more strongly over the blowpipe or in the
Allow to stand for one hour. The white crystalline precipitate contains the
phosphorus as ammonium-magnesium phosphate.
Phosphate of lead is decomposed by sulphuric acid; the lead is converted into the
insoluble lead sulphate, and the phosphoric acid is dissolved. Phosphate of copper
and phosphate of iron may be treated with sulphuretted hydrogen; the former in an
acid, and the latter in an alkaline, solution. Phosphate of alumina is generally
weighed without separation of the alumina, since this requires a fusion. In all cases
the aim is to get the phosphoric oxide either free, or combined with some metal
whose phosphate is soluble in ammonia.
Joulie's method of separation is as follows:—One to ten grams of the sample are
treated with hydrochloric acid, and evaporated to dryness with the addition (if any
pyrites is present) of a little nitric acid. The residue is taken up with hydrochloric
acid, cooled, transferred to a graduated flask, and diluted to the mark. It is then
shaken up, filtered through a dry filter, and a measured portion (containing about
0.05 gram of phosphoric acid) transferred to a small beaker. Ten c.c. of a citric-acid
solution of magnesia[110] is added, and then an excess of ammonia. If an immediate
precipitate is formed, a fresh portion must be measured out and treated with 20 c.c.
of the citrate of magnesia solution and with ammonia as before. The beaker is put
aside for from two to twelve hours. The precipitate is then filtered off and washed
with weak ammonia; it contains the phosphorus as ammonium-magnesium
phosphate.
GRAVIMETRIC DETERMINATION.
If the phosphate is not already in the form of ammonic-magnesic phosphate, it is
converted into this by the addition to its solution of an excess of ammonia and
"magnesia mixture." In order to get the precipitate pure, the "magnesia mixture" is
run in gradually (by drops) from a burette, with constant stirring. A white
crystalline precipitate at once falls, if much phosphorus is present; but, if there is
only a small quantity, it may be an hour or two before it shows itself. The solution
is best allowed to rest for twelve or fifteen hours (overnight) before filtering. The
presence of tartaric acid should be avoided; and the appearance of the precipitate
should be crystalline. The solution is decanted through a filter, and the precipitate
washed with dilute ammonia, using as little as may be necessary. The precipitate is
dried, transferred to a weighed Berlin or platinum crucible; the filter-paper is
carefully burnt, and its ash added to the precipitate, which is then ignited, at first
gently over a Bunsen burner, and then more strongly over the blowpipe or in the
Page 495
muffle. The residue is a white mass of magnesium pyrophosphate containing 27.92
per cent. of phosphorus, or 63.96 per cent. of phosphoric oxide.
VOLUMETRIC METHOD.
Instead of separating and weighing this compound, the phosphoric oxide in it can
be determined by titration. In many cases the ore may be dissolved and
immediately titrated without previous separation. It is better, however, to carry the
separation so far as to get phosphoric acid, an alkaline phosphate, or the magnesia
precipitate. It may then be prepared for titration in the following way:—The
precipitate in the last case (without much washing) is dissolved in a little
hydrochloric acid, and the solution in any case rendered fairly acid. Dilute
ammonia is added till it is just alkaline, and then 5 c.c. of the sodic acetate and
acetic acid mixture (as described under the Arsenic Assay). This should yield a
clear distinctly-acid solution. It is diluted to 100 or 150 c.c., heated to boiling, and
titrated with the uranium acetate solution, using that of potassic ferrocyanide as
indicator.
The standard solution required is made by dissolving 35 grams of uranium acetate
in water with the aid of 25 c.c. of acetic acid, and diluting to 1 litre.
An equivalent solution of phosphoric oxide is made by dissolving 25.21 grams of
crystallised hydric disodic phosphate (HNa2PO4.12H2O) in water, and making up
to 1 litre. 100 c.c. will contain 0.5 gram of phosphoric oxide (P2O5), or 0.2183
gram of phosphorus. In making this solution, transparent crystals only must be
used. The uranium acetate solution is only approximately equivalent to this, so that
its exact standard must be determined.
Sodic Acetate and Acetic Acid Solution.—It is the same as that described under
Arsenic.[111] Use 5 c.c. for each assay.
The following experiments show the effect of variation in the conditions of the
titration:—
Effect of Varying Temperature.—The solution should be titrated while boiling.
This is especially necessary for the last few c.c. in order to get a decided and fixed
finishing point.
Temperature 15° C. 30° C. 70° C. 100° C.
"Uranium" required 18.0 c.c. 19.2 c.c. 19.0 c.c. 18.9 c.c.
Effect of Varying Bulk.—
per cent. of phosphorus, or 63.96 per cent. of phosphoric oxide.
VOLUMETRIC METHOD.
Instead of separating and weighing this compound, the phosphoric oxide in it can
be determined by titration. In many cases the ore may be dissolved and
immediately titrated without previous separation. It is better, however, to carry the
separation so far as to get phosphoric acid, an alkaline phosphate, or the magnesia
precipitate. It may then be prepared for titration in the following way:—The
precipitate in the last case (without much washing) is dissolved in a little
hydrochloric acid, and the solution in any case rendered fairly acid. Dilute
ammonia is added till it is just alkaline, and then 5 c.c. of the sodic acetate and
acetic acid mixture (as described under the Arsenic Assay). This should yield a
clear distinctly-acid solution. It is diluted to 100 or 150 c.c., heated to boiling, and
titrated with the uranium acetate solution, using that of potassic ferrocyanide as
indicator.
The standard solution required is made by dissolving 35 grams of uranium acetate
in water with the aid of 25 c.c. of acetic acid, and diluting to 1 litre.
An equivalent solution of phosphoric oxide is made by dissolving 25.21 grams of
crystallised hydric disodic phosphate (HNa2PO4.12H2O) in water, and making up
to 1 litre. 100 c.c. will contain 0.5 gram of phosphoric oxide (P2O5), or 0.2183
gram of phosphorus. In making this solution, transparent crystals only must be
used. The uranium acetate solution is only approximately equivalent to this, so that
its exact standard must be determined.
Sodic Acetate and Acetic Acid Solution.—It is the same as that described under
Arsenic.[111] Use 5 c.c. for each assay.
The following experiments show the effect of variation in the conditions of the
titration:—
Effect of Varying Temperature.—The solution should be titrated while boiling.
This is especially necessary for the last few c.c. in order to get a decided and fixed
finishing point.
Temperature 15° C. 30° C. 70° C. 100° C.
"Uranium" required 18.0 c.c. 19.2 c.c. 19.0 c.c. 18.9 c.c.
Effect of Varying Bulk.—
Page 496
Bulk 50.0 c.c. 100.0 c.c. 200.0 c.c. 300.0 c.c.
"Uranium" required 18.8 " 18.9 " 19.0 " 19.3 "
Variation in bulk affects the results; therefore, a constant bulk should be adhered
to.
Effect of Varying Sodium Acetate and Acetic Acid Solution.—
Sodium acetate and acetic acid solution 0.0 c.c. 1.0 c.c. 5.0 c.c. 10.0 c.c. 20.0 c.c.
"Uranium" required 18.9 " 18.9 " 19.0 " 18.8 " 17.5 "
As in the titration with arsenates, an excess is dangerous to the assay; a definite
quantity (5 c.c.) should, therefore, be used.
Effect of Foreign Salts.—Besides the sodium acetate, &c., added, the only salts
likely to be present are those of ammonia and magnesia. In three experiments, in
one of which no foreign salts were introduced, while in the other two 5 grams of
ammonic chloride and of magnesium sulphate respectively were added, there were
required:—
With ammonic chloride 18.8 c.c. "Uranium" solution
With magnesium sulphate 19.0 " "
Without foreign salts 18.9 " "
Effect of Varying Phosphate.—
"Phosphate" solution added 10.0 c.c. 20.0 c.c. 50.0 c.c. 100.0 c.c.
"Uranium" required 9.8 " 18.9 " 47.6 " 94.5 "
The quantity of phosphoric oxide in the assay solution for the conditions of
titration should not be much less than 0.05 gram. For smaller quantities the
uranium solution should be diluted to half its strength, and the assay solution
concentrated by reducing its bulk to 50 c.c. and using 2.5 c.c. of the sodium acetate
and acetic acid solution.
Determination of Phosphoric Oxide in Apatite.—Weigh up 0.5 gram of the dried
and powdered sample, and dissolve it in 5 c.c. of hydrochloric acid. Evaporate to a
paste, add 5 c.c. of the sodic acetate and acetic acid solution, dilute to 100 c.c. with
water, boil, and titrate with uranium acetate solution.
In an example, 0.5 gram of apatite required 37.4 c.c. of uranium acetate solution
(standard equal to 0.5291 gram of phosphoric oxide). The sample therefore
"Uranium" required 18.8 " 18.9 " 19.0 " 19.3 "
Variation in bulk affects the results; therefore, a constant bulk should be adhered
to.
Effect of Varying Sodium Acetate and Acetic Acid Solution.—
Sodium acetate and acetic acid solution 0.0 c.c. 1.0 c.c. 5.0 c.c. 10.0 c.c. 20.0 c.c.
"Uranium" required 18.9 " 18.9 " 19.0 " 18.8 " 17.5 "
As in the titration with arsenates, an excess is dangerous to the assay; a definite
quantity (5 c.c.) should, therefore, be used.
Effect of Foreign Salts.—Besides the sodium acetate, &c., added, the only salts
likely to be present are those of ammonia and magnesia. In three experiments, in
one of which no foreign salts were introduced, while in the other two 5 grams of
ammonic chloride and of magnesium sulphate respectively were added, there were
required:—
With ammonic chloride 18.8 c.c. "Uranium" solution
With magnesium sulphate 19.0 " "
Without foreign salts 18.9 " "
Effect of Varying Phosphate.—
"Phosphate" solution added 10.0 c.c. 20.0 c.c. 50.0 c.c. 100.0 c.c.
"Uranium" required 9.8 " 18.9 " 47.6 " 94.5 "
The quantity of phosphoric oxide in the assay solution for the conditions of
titration should not be much less than 0.05 gram. For smaller quantities the
uranium solution should be diluted to half its strength, and the assay solution
concentrated by reducing its bulk to 50 c.c. and using 2.5 c.c. of the sodium acetate
and acetic acid solution.
Determination of Phosphoric Oxide in Apatite.—Weigh up 0.5 gram of the dried
and powdered sample, and dissolve it in 5 c.c. of hydrochloric acid. Evaporate to a
paste, add 5 c.c. of the sodic acetate and acetic acid solution, dilute to 100 c.c. with
water, boil, and titrate with uranium acetate solution.
In an example, 0.5 gram of apatite required 37.4 c.c. of uranium acetate solution
(standard equal to 0.5291 gram of phosphoric oxide). The sample therefore
Page 497
contained 0.1979 gram of P2O5, equal to 39.58 per cent.
Determination of Phosphoric Oxide in an Iron Ore.—Take 10 grams, boil with
50 c.c. of hydrochloric acid, and evaporate to a paste; take up with 10 c.c. of dilute
hydrochloric acid, and dilute with water to 400 c.c. Pass sulphuretted hydrogen for
nearly a quarter of an hour; warm, and filter. Boil off the excess of gas; cool, add
ammonia till nearly neutral, and then a few drops of ferric chloride solution, and 4
or 5 grams of sodium acetate, with a drop or two of acetic acid. Boil and filter.
Dissolve the precipitate in hot dilute hydrochloric acid, and add citro-magnesia
mixture and ammonia; allow to stand overnight; filter, ignite, and weigh.
In an example, 10 grams of ore gave 28.5 milligrams of magnesic pyrophosphate,
which is equivalent to 0.18 per cent. of phosphoric oxide.
Determination of Phosphorus in Iron.—Take from 2 to 10 grams (according to
the amount of phosphorus present), and dissolve in aqua regia, keeping the nitric
acid in excess; evaporate to dryness and take up with hydrochloric acid, boil,
dilute, and filter. Add 10 c.c. of nitric acid, nearly neutralise with ammonia, render
acid with 3 or 4 c.c. of nitric acid, and add 10 or 20 c.c. of ammonic molybdate
solution. Heat for some time, allow to settle, filter, and wash the precipitate with a
solution of ammonic nitrate. Dissolve the precipitate in dilute ammonia, nearly
neutralise with dilute hydrochloric acid, and add first "magnesia mixture," and then
ammonia; allow to stand overnight; filter, wash with dilute ammonia, dry, ignite,
and weigh as magnesic pyrophosphate. Calculate to phosphorus.
PRACTICAL EXERCISES.
1. Ten grams of an iron yielded 12 milligrams of pyrophosphate of magnesia. What
percentage of phosphorus did the metal contain?
2. Ten grams of an iron ore gave 12 milligrams of pyrophosphate. What percentage
of phosphoric oxide did it contain?
3. What weight of apatite 3Ca3(PO4)2.CaClF would require 50 c.c. of standard
uranium solution (100 c.c. equal to 0.5 gram of P2O5)?
4. You have reason to believe that a precipitate which has been weighed as
magnetic pyrophosphate contains some arsenate. How would you determine the
amount of phosphate really present?
5. Twenty c.c. of a solution of sodic phosphate containing 0.100 gram of P2O5 was
found to require a solution containing 0.700 gram of hydrated uranium acetate in a
Determination of Phosphoric Oxide in an Iron Ore.—Take 10 grams, boil with
50 c.c. of hydrochloric acid, and evaporate to a paste; take up with 10 c.c. of dilute
hydrochloric acid, and dilute with water to 400 c.c. Pass sulphuretted hydrogen for
nearly a quarter of an hour; warm, and filter. Boil off the excess of gas; cool, add
ammonia till nearly neutral, and then a few drops of ferric chloride solution, and 4
or 5 grams of sodium acetate, with a drop or two of acetic acid. Boil and filter.
Dissolve the precipitate in hot dilute hydrochloric acid, and add citro-magnesia
mixture and ammonia; allow to stand overnight; filter, ignite, and weigh.
In an example, 10 grams of ore gave 28.5 milligrams of magnesic pyrophosphate,
which is equivalent to 0.18 per cent. of phosphoric oxide.
Determination of Phosphorus in Iron.—Take from 2 to 10 grams (according to
the amount of phosphorus present), and dissolve in aqua regia, keeping the nitric
acid in excess; evaporate to dryness and take up with hydrochloric acid, boil,
dilute, and filter. Add 10 c.c. of nitric acid, nearly neutralise with ammonia, render
acid with 3 or 4 c.c. of nitric acid, and add 10 or 20 c.c. of ammonic molybdate
solution. Heat for some time, allow to settle, filter, and wash the precipitate with a
solution of ammonic nitrate. Dissolve the precipitate in dilute ammonia, nearly
neutralise with dilute hydrochloric acid, and add first "magnesia mixture," and then
ammonia; allow to stand overnight; filter, wash with dilute ammonia, dry, ignite,
and weigh as magnesic pyrophosphate. Calculate to phosphorus.
PRACTICAL EXERCISES.
1. Ten grams of an iron yielded 12 milligrams of pyrophosphate of magnesia. What
percentage of phosphorus did the metal contain?
2. Ten grams of an iron ore gave 12 milligrams of pyrophosphate. What percentage
of phosphoric oxide did it contain?
3. What weight of apatite 3Ca3(PO4)2.CaClF would require 50 c.c. of standard
uranium solution (100 c.c. equal to 0.5 gram of P2O5)?
4. You have reason to believe that a precipitate which has been weighed as
magnetic pyrophosphate contains some arsenate. How would you determine the
amount of phosphate really present?
5. Twenty c.c. of a solution of sodic phosphate containing 0.100 gram of P2O5 was
found to require a solution containing 0.700 gram of hydrated uranium acetate in a
Page 498
titration. The precipitate contains 80.09 per cent. uranium oxide and 19.91 per cent.
of phosphoric oxide. What percentage of uranium oxide was contained in the
uranic acetate?
NITROGEN AND NITRATES.
Nitrogen occurs in nature in the free state, and forms about four-fifths of the
atmosphere. In combination, as nitrate, it is found in nitre (KNO3), and Chili
saltpetre (NaNO3), minerals which have a commercial importance. The latter
occurs in beds, and is extensively worked for use as a manure and in the
preparation of nitric acid.
Nitrogen is mainly characterised by negative properties, although many of its
compounds are very energetic bodies. It is a gas, present everywhere, but so
inactive that the assayer can always afford to ignore its presence, and, except in
testing furnace gases, &c., he is never called on to determine its quantity.
The nitrates are an important class of salts, and may be looked on as compounds of
the bases with nitric pentoxide (N2O5). They are, with the exception of a few basic
compounds, soluble in water, and are remarkable for the ease with which they give
up their oxygen. The alkaline nitrates fuse readily, and lose oxygen with
effervescence forming nitrites; while at a higher temperature they yield more
oxygen and lose their nitrogen, either as a lower oxide or as nitrogen. The nitrates
of the metals, on heating, leave the oxide of the metal. It is as yielders of oxygen
that nitrates are so largely used in the manufacture of explosives. Gunpowder
contains from 65 to 75 per cent. of potassium nitrate (nitre).
Nitrates are best detected and determined by their yielding nitric oxide when
treated with sulphuric acid and a suitable reducing agent, such as ferrous sulphate,
mercury, or copper. Nitric oxide is a colourless gas very slightly soluble in water. It
combines at once with oxygen, on mixing with the air, to form brown "nitrous
fumes," and dissolves in a solution of ferrous sulphate, producing a characteristic
blackish-brown colour. It is this colour which affords the best and most easily-
applied test for nitrates. The substance suspected to contain nitrates is dissolved in
about 1 c.c. of water, and treated with an equal volume of strong sulphuric acid.
After cooling, a solution of ferrous sulphate is poured on its surface, so as to form
a layer resting on it. On standing, a brown or black ring is developed where the
liquids join, if any nitrate or nitrite is present. Nitrites are distinguished from
nitrates by effervescing and yielding brown fumes when treated with a little dilute
sulphuric acid.
of phosphoric oxide. What percentage of uranium oxide was contained in the
uranic acetate?
NITROGEN AND NITRATES.
Nitrogen occurs in nature in the free state, and forms about four-fifths of the
atmosphere. In combination, as nitrate, it is found in nitre (KNO3), and Chili
saltpetre (NaNO3), minerals which have a commercial importance. The latter
occurs in beds, and is extensively worked for use as a manure and in the
preparation of nitric acid.
Nitrogen is mainly characterised by negative properties, although many of its
compounds are very energetic bodies. It is a gas, present everywhere, but so
inactive that the assayer can always afford to ignore its presence, and, except in
testing furnace gases, &c., he is never called on to determine its quantity.
The nitrates are an important class of salts, and may be looked on as compounds of
the bases with nitric pentoxide (N2O5). They are, with the exception of a few basic
compounds, soluble in water, and are remarkable for the ease with which they give
up their oxygen. The alkaline nitrates fuse readily, and lose oxygen with
effervescence forming nitrites; while at a higher temperature they yield more
oxygen and lose their nitrogen, either as a lower oxide or as nitrogen. The nitrates
of the metals, on heating, leave the oxide of the metal. It is as yielders of oxygen
that nitrates are so largely used in the manufacture of explosives. Gunpowder
contains from 65 to 75 per cent. of potassium nitrate (nitre).
Nitrates are best detected and determined by their yielding nitric oxide when
treated with sulphuric acid and a suitable reducing agent, such as ferrous sulphate,
mercury, or copper. Nitric oxide is a colourless gas very slightly soluble in water. It
combines at once with oxygen, on mixing with the air, to form brown "nitrous
fumes," and dissolves in a solution of ferrous sulphate, producing a characteristic
blackish-brown colour. It is this colour which affords the best and most easily-
applied test for nitrates. The substance suspected to contain nitrates is dissolved in
about 1 c.c. of water, and treated with an equal volume of strong sulphuric acid.
After cooling, a solution of ferrous sulphate is poured on its surface, so as to form
a layer resting on it. On standing, a brown or black ring is developed where the
liquids join, if any nitrate or nitrite is present. Nitrites are distinguished from
nitrates by effervescing and yielding brown fumes when treated with a little dilute
sulphuric acid.
Page 499
The separation of nitrates is in many cases difficult. Generally, on treating the
substance with water, the nitrate will be in the solution, and is filtered off from any
insoluble matter. In the exceptional cases it is got into solution by treating with a
boiling solution of sodium carbonate; the nitrate will contain it as an alkaline
nitrate.
Since, however, in their determination, nitrates are never separated and weighed as
such, the difficulty of separating them has little importance. Usually, the
determination can be made on the original aqueous solution, and it is never
necessary to do more than remove any special substance which has a bad effect;
and this is easily done by the usual reagents.
GRAVIMETRIC DETERMINATION.
It follows from what has been said that there is no direct gravimetric determination.
The percentage of nitrogen pentoxide (N2O5) in a comparatively pure nitrate is
sometimes determined indirectly in the following way:—Place in a platinum-
crucible 4 or 5 grams of powdered and cleaned quartz. Ignite, cool in a desiccator,
and weigh with the cover. Mix 1 gram of the dried and powdered salt with the
quartz in the crucible by stirring with a stout platinum-wire. Cover the crucible,
and heat in a Bunsen-burner flame at scarcely visible redness for half-an-hour.
Cool and weigh. The loss in weight gives the amount of nitrogen pentoxide.
Sulphates and chlorides in moderate quantity do not interfere. The following is an
example of the process:—
Crucible and sand 26.6485 grams
Nitre taken 1.0000 "
————
27.6485 "
Weight after ignition 27.1160 "
————
Loss on ignition 0.5325 "
This is equal to 53.25 per cent. of nitrogen pentoxide.
VOLUMETRIC DETERMINATION.
This is based on the oxidising action of nitric acid, or of nitrates in acid solutions
on ferrous salts. The pentoxide (N2O5) of the nitrate is reduced to nitric oxide
(NO), so that 336 parts of iron peroxidised represent 108 parts of nitric pentoxide
substance with water, the nitrate will be in the solution, and is filtered off from any
insoluble matter. In the exceptional cases it is got into solution by treating with a
boiling solution of sodium carbonate; the nitrate will contain it as an alkaline
nitrate.
Since, however, in their determination, nitrates are never separated and weighed as
such, the difficulty of separating them has little importance. Usually, the
determination can be made on the original aqueous solution, and it is never
necessary to do more than remove any special substance which has a bad effect;
and this is easily done by the usual reagents.
GRAVIMETRIC DETERMINATION.
It follows from what has been said that there is no direct gravimetric determination.
The percentage of nitrogen pentoxide (N2O5) in a comparatively pure nitrate is
sometimes determined indirectly in the following way:—Place in a platinum-
crucible 4 or 5 grams of powdered and cleaned quartz. Ignite, cool in a desiccator,
and weigh with the cover. Mix 1 gram of the dried and powdered salt with the
quartz in the crucible by stirring with a stout platinum-wire. Cover the crucible,
and heat in a Bunsen-burner flame at scarcely visible redness for half-an-hour.
Cool and weigh. The loss in weight gives the amount of nitrogen pentoxide.
Sulphates and chlorides in moderate quantity do not interfere. The following is an
example of the process:—
Crucible and sand 26.6485 grams
Nitre taken 1.0000 "
————
27.6485 "
Weight after ignition 27.1160 "
————
Loss on ignition 0.5325 "
This is equal to 53.25 per cent. of nitrogen pentoxide.
VOLUMETRIC DETERMINATION.
This is based on the oxidising action of nitric acid, or of nitrates in acid solutions
on ferrous salts. The pentoxide (N2O5) of the nitrate is reduced to nitric oxide
(NO), so that 336 parts of iron peroxidised represent 108 parts of nitric pentoxide
Page 500
as oxidising agent.[112] The quantity of iron peroxidised is determined by taking a
known quantity of ferrous salt, oxidizing with a weighed sample of nitrate, and
then determining the residual ferrous iron by titration with bichromate or
permanganate of potassium solution. The difference between the ferrous iron taken
and that found, gives the amount oxidized by the nitrate. The speed with which
nitric oxide takes up oxygen from the air, and thus becomes capable of oxidising
more iron, renders some precautions necessary; ferrous chloride should, therefore,
be used, since it is easier to expel nitric oxide (by boiling) from solutions of a
chloride than it is from those of a sulphate. The process is as follows:—Dissolve 2
grams of thin soft iron wire in 50 c.c. of hydrochloric acid in a flask provided with
an arrangement for maintaining an atmosphere of carbon dioxide. When the iron
has dissolved, allow the solution to cool, and add 0.5 gram of the nitrate. Heat
gently for a few minutes, and then boil until the nitric oxide is expelled. An
atmosphere of carbon dioxide must be kept up. Dilute with water, and titrate the
residual iron with standard solution of bichromate of potassium. The standard
"bichromate" is made by dissolving 17.5 grams of the salt (K2Cr2O7) in water, and
diluting to 1 litre: 100 c.c. equal 2 grams of iron. Deduct the weight of iron found
from the 2 grams originally taken, and multiply by 0.3214. This gives the weight of
the pentoxide in the sample. In an example, 0.5 gram of nitre was taken, and 59.4
c.c. of the "bichromate" solution were required. The 59.4 c.c. thus used are
equivalent to 1.198 gram of iron. This leaves 0.822 gram as the quantity oxidised
by the nitre, which, multiplied by 0.3214, gives 0.2642 gram for the nitrogen
pentoxide, or 52.8 per cent.
GASOMETRIC METHOD.
This is based upon the measurement of the nitric oxide evolved on shaking up a
weighed quantity of the nitrate with sulphuric acid over mercury in a nitrometer.
Each c.c. of nitric oxide obtained, when reduced to normal temperature and
pressure, is equivalent to:—
0.627milligram of nitrogen.
1.343 " of nitric oxide.
2.418 " of nitric pentoxide.
2.820 " of nitric acid.
3.805 " of sodium nitrate.
4.523 " of potassium nitrate.
In working on substances not rich in nitrates, an ordinary nitrometer (fig. 69) is
used; but in the assay of sodium nitrate, nitroglycerine, &c., an instrument
known quantity of ferrous salt, oxidizing with a weighed sample of nitrate, and
then determining the residual ferrous iron by titration with bichromate or
permanganate of potassium solution. The difference between the ferrous iron taken
and that found, gives the amount oxidized by the nitrate. The speed with which
nitric oxide takes up oxygen from the air, and thus becomes capable of oxidising
more iron, renders some precautions necessary; ferrous chloride should, therefore,
be used, since it is easier to expel nitric oxide (by boiling) from solutions of a
chloride than it is from those of a sulphate. The process is as follows:—Dissolve 2
grams of thin soft iron wire in 50 c.c. of hydrochloric acid in a flask provided with
an arrangement for maintaining an atmosphere of carbon dioxide. When the iron
has dissolved, allow the solution to cool, and add 0.5 gram of the nitrate. Heat
gently for a few minutes, and then boil until the nitric oxide is expelled. An
atmosphere of carbon dioxide must be kept up. Dilute with water, and titrate the
residual iron with standard solution of bichromate of potassium. The standard
"bichromate" is made by dissolving 17.5 grams of the salt (K2Cr2O7) in water, and
diluting to 1 litre: 100 c.c. equal 2 grams of iron. Deduct the weight of iron found
from the 2 grams originally taken, and multiply by 0.3214. This gives the weight of
the pentoxide in the sample. In an example, 0.5 gram of nitre was taken, and 59.4
c.c. of the "bichromate" solution were required. The 59.4 c.c. thus used are
equivalent to 1.198 gram of iron. This leaves 0.822 gram as the quantity oxidised
by the nitre, which, multiplied by 0.3214, gives 0.2642 gram for the nitrogen
pentoxide, or 52.8 per cent.
GASOMETRIC METHOD.
This is based upon the measurement of the nitric oxide evolved on shaking up a
weighed quantity of the nitrate with sulphuric acid over mercury in a nitrometer.
Each c.c. of nitric oxide obtained, when reduced to normal temperature and
pressure, is equivalent to:—
0.627milligram of nitrogen.
1.343 " of nitric oxide.
2.418 " of nitric pentoxide.
2.820 " of nitric acid.
3.805 " of sodium nitrate.
4.523 " of potassium nitrate.
In working on substances not rich in nitrates, an ordinary nitrometer (fig. 69) is
used; but in the assay of sodium nitrate, nitroglycerine, &c., an instrument
Page 501
provided with a bulb having a capacity of 100 c.c. is employed.
The plan of working is as follows:—The "measuring tube" is filled with mercury
until it reaches up into the tap, and the levelling-tube is placed so that it contains an
inch or two of mercury. If the nitrate is in solution, 2 or 3 c.c. of the liquid (dilute
liquids are brought to this bulk by evaporation) are measured into the cup. The
levelling-tube is lowered a little, and the tap cautiously opened until all but the last
drop of the liquid has run in. The cup is then rinsed with 2 or 3 c.c. of sulphuric
acid, which is run in in the same way, and the operation is repeated with another lot
of acid. The measuring-tube is now taken from the clamp, and shaken for two or
three minutes, until no more gas is given off. It is replaced, and the mercury-level
in the two tubes adjusted. Then it is allowed to stand until the froth has subsided,
and the gas has cooled to the temperature of the room. The volume of the gas is
then read off. In adjusting the level, account must be taken of the sulphuric acid in
the measuring-tube; this is allowed for by having the mercury higher in the other
tube by, say, 1 mm. for each 6.5 mm. of sulphuric acid, or it is counterpoised by an
equal height of sulphuric acid in the levelling-tube, in which case the two mercury-
levels are made to correspond. On opening the tap after reading off the volume,
there should be no change in the level of the mercury. If it should rise or fall a
The plan of working is as follows:—The "measuring tube" is filled with mercury
until it reaches up into the tap, and the levelling-tube is placed so that it contains an
inch or two of mercury. If the nitrate is in solution, 2 or 3 c.c. of the liquid (dilute
liquids are brought to this bulk by evaporation) are measured into the cup. The
levelling-tube is lowered a little, and the tap cautiously opened until all but the last
drop of the liquid has run in. The cup is then rinsed with 2 or 3 c.c. of sulphuric
acid, which is run in in the same way, and the operation is repeated with another lot
of acid. The measuring-tube is now taken from the clamp, and shaken for two or
three minutes, until no more gas is given off. It is replaced, and the mercury-level
in the two tubes adjusted. Then it is allowed to stand until the froth has subsided,
and the gas has cooled to the temperature of the room. The volume of the gas is
then read off. In adjusting the level, account must be taken of the sulphuric acid in
the measuring-tube; this is allowed for by having the mercury higher in the other
tube by, say, 1 mm. for each 6.5 mm. of sulphuric acid, or it is counterpoised by an
equal height of sulphuric acid in the levelling-tube, in which case the two mercury-
levels are made to correspond. On opening the tap after reading off the volume,
there should be no change in the level of the mercury. If it should rise or fall a
Page 502
little, a slight increase or decrease (say 0.1 c.c.) is made to the volume previously
read off.
In working with nitrate of soda, &c., in the bulb nitrometer, it is necessary to take a
quantity of the substance which will yield more than 100 and less than 150 c.c. of
the gas.
FOOTNOTES:
[103] Na3AsO3 + H2O + 2I = Na3AsO4 + 2HI. The acid is at once neutralised.
[104] Mr. Thomas Gibb is the originator of this ingenious process.
[105] By taking hold of the water present, it may prevent the dissociation of arsenious
chloride.
[106] It is difficult to get ferric chloride free from arsenic; but the following treatment
will remove 80 or 90 per cent. of the arsenic contained in the commercial material:—
Dissolve 2 or 3 lbs. of ferric chloride with the smallest amount of water that will effect
solution with the addition of 100 c.c. of hydrochloric acid; add a solution of sulphurous
acid in quantity sufficient to reduce 2 or 3 per cent. of the iron to the ferrous state; allow
to stand a week; and then boil, to remove the hydrochloric acid added. Nitric acid, which
is prejudicial, is also removed by this treatment.
[107] When the amount of arsenic to be estimated is small (as in refined coppers), it is
better to use a weaker solution of iodine. This is made by diluting 200 c.c. of the
standard solution with water to 1 litre. Each c.c. will equal 0.1 per cent., if 1 gram of the
metal has been taken for the assay.
[108] The constitution of these phosphates may be thus illustrated—
Magnesic meta-phosphate MgO.P2O5.
Magnesic pyro-phosphate 2MgO.P2O5.
Magnesic ortho-phosphate 3MgO.P2O5.
[109] The composition of which is—
MoO2 90.74,
P2O5 3.14,
(NH4)2O 3.57,
H2O 2.55=100.00.
[110] This is made by adding 27 grams of magnesium carbonate (a little at a time) to a
solution of 270 grams of citric acid in 350 c.c. of warm water; and, when dissolved,
adding 400 c.c. of dilute ammonia, and making up the bulk to 1 litre; 20 c.c. of the
solution is sufficient for 0.1 gram of P2O5, although more will be required if much iron
or alumina is present.
[111] For the details of the titration, the student is referred to the same place.
[112] N2O5 + 6FeO = 3Fe2O3 + 2NO.
read off.
In working with nitrate of soda, &c., in the bulb nitrometer, it is necessary to take a
quantity of the substance which will yield more than 100 and less than 150 c.c. of
the gas.
FOOTNOTES:
[103] Na3AsO3 + H2O + 2I = Na3AsO4 + 2HI. The acid is at once neutralised.
[104] Mr. Thomas Gibb is the originator of this ingenious process.
[105] By taking hold of the water present, it may prevent the dissociation of arsenious
chloride.
[106] It is difficult to get ferric chloride free from arsenic; but the following treatment
will remove 80 or 90 per cent. of the arsenic contained in the commercial material:—
Dissolve 2 or 3 lbs. of ferric chloride with the smallest amount of water that will effect
solution with the addition of 100 c.c. of hydrochloric acid; add a solution of sulphurous
acid in quantity sufficient to reduce 2 or 3 per cent. of the iron to the ferrous state; allow
to stand a week; and then boil, to remove the hydrochloric acid added. Nitric acid, which
is prejudicial, is also removed by this treatment.
[107] When the amount of arsenic to be estimated is small (as in refined coppers), it is
better to use a weaker solution of iodine. This is made by diluting 200 c.c. of the
standard solution with water to 1 litre. Each c.c. will equal 0.1 per cent., if 1 gram of the
metal has been taken for the assay.
[108] The constitution of these phosphates may be thus illustrated—
Magnesic meta-phosphate MgO.P2O5.
Magnesic pyro-phosphate 2MgO.P2O5.
Magnesic ortho-phosphate 3MgO.P2O5.
[109] The composition of which is—
MoO2 90.74,
P2O5 3.14,
(NH4)2O 3.57,
H2O 2.55=100.00.
[110] This is made by adding 27 grams of magnesium carbonate (a little at a time) to a
solution of 270 grams of citric acid in 350 c.c. of warm water; and, when dissolved,
adding 400 c.c. of dilute ammonia, and making up the bulk to 1 litre; 20 c.c. of the
solution is sufficient for 0.1 gram of P2O5, although more will be required if much iron
or alumina is present.
[111] For the details of the titration, the student is referred to the same place.
[112] N2O5 + 6FeO = 3Fe2O3 + 2NO.
Page 503
Page 504
CHAPTER XVIII.
SILICON, CARBON, BORON.
SILICON AND SILICATES.
In assaying, more especially products direct from the mine, there is always found,
when the rock is siliceous, a quantity of white sandy-looking substance, insoluble
in acids, which is sometimes accompanied by a light gelatinous material very
difficult to filter. This is variously described as "insoluble," "sand," "insoluble
silicates," "gangue," or "rocky matter." It may be pure quartz; but oftener it is
mixed with silicates from the rock containing the mineral. Some silicates, but not
many, are completely decomposed by boiling with hydrochloric acid or aqua regia;
and others are partly so, they yield a gelatinous precipitate of silica which greatly
interferes with the filtering. It is a common practice with assayers to carry the first
attack of the sample with acids to dryness, and to take up with a fresh portion of
acid. By this means the separated silica becomes granular and insoluble, and
capable of being filtered off and washed with comparative ease.
This residue may be ignited and weighed; and be reported as so much per cent. of
"silica and silicates insoluble in acids." Unless specially wanted, a determination of
its constituents need not be made. When required, the analysis is best made on the
ignited residue, and separately reported as "analysis of the insoluble portion."
Silicon only occurs in nature in the oxidised state; but the oxide generally known
as silica (SiO2) is common, being represented by the abundant minerals—quartz,
flint, &c. Silica, combined with alumina, lime, oxide of iron, magnesia and the
alkalies, forms a large number of rock-forming minerals. Most rock masses, other
than limestones, contain over 50 per cent. of silica. The following are analyses of
some of the commoner silicates; but it must be noted that these minerals often
show great variation in composition. This is more especially true of chlorite,
schorl, hornblende and augite.
Ferric Ferrous Fluorine,
Silica, Alumina, Lime, Magnesia, Potash, Soda,
Oxide, Oxide,
SiO2. Al2O3. CaO. MgO. K2O. Na2O. Water
Fe2O3. FeO. &c.
Potash-
65.2 18.2 0.2 — — — 14.7 1.5
felspar
SILICON, CARBON, BORON.
SILICON AND SILICATES.
In assaying, more especially products direct from the mine, there is always found,
when the rock is siliceous, a quantity of white sandy-looking substance, insoluble
in acids, which is sometimes accompanied by a light gelatinous material very
difficult to filter. This is variously described as "insoluble," "sand," "insoluble
silicates," "gangue," or "rocky matter." It may be pure quartz; but oftener it is
mixed with silicates from the rock containing the mineral. Some silicates, but not
many, are completely decomposed by boiling with hydrochloric acid or aqua regia;
and others are partly so, they yield a gelatinous precipitate of silica which greatly
interferes with the filtering. It is a common practice with assayers to carry the first
attack of the sample with acids to dryness, and to take up with a fresh portion of
acid. By this means the separated silica becomes granular and insoluble, and
capable of being filtered off and washed with comparative ease.
This residue may be ignited and weighed; and be reported as so much per cent. of
"silica and silicates insoluble in acids." Unless specially wanted, a determination of
its constituents need not be made. When required, the analysis is best made on the
ignited residue, and separately reported as "analysis of the insoluble portion."
Silicon only occurs in nature in the oxidised state; but the oxide generally known
as silica (SiO2) is common, being represented by the abundant minerals—quartz,
flint, &c. Silica, combined with alumina, lime, oxide of iron, magnesia and the
alkalies, forms a large number of rock-forming minerals. Most rock masses, other
than limestones, contain over 50 per cent. of silica. The following are analyses of
some of the commoner silicates; but it must be noted that these minerals often
show great variation in composition. This is more especially true of chlorite,
schorl, hornblende and augite.
Ferric Ferrous Fluorine,
Silica, Alumina, Lime, Magnesia, Potash, Soda,
Oxide, Oxide,
SiO2. Al2O3. CaO. MgO. K2O. Na2O. Water
Fe2O3. FeO. &c.
Potash-
65.2 18.2 0.2 — — — 14.7 1.5
felspar
Page 505
Soda-
67.0 19.2 — 0.3 1.2 1.8 2.2 7.2
felspar
Lime-
43.3 35.4 — 1.3 17.4 0.35 0.5 0.9
felspar
F (0.8)
Potash- H 2O
45.7 33.7 3.1 — — 1.1 7.5 2.8
mica
(4.9)
Magnesia-
39.1 15.4 7.1 — — 23.6 7.5 2.6 F (0.7)
mica
Hornblende 40.6 14.3 5.8 7.2 12.5 14.0 1.5 1.6
MnO
Augite 50.0 3.7 2.4 6.6 22.8 13.5 — —
(0.1)
Almandine MnO
39.7 19.7 — 39.7 — — — —
(Garnet) (1.8)
Chlorite H 2O
32.1 18.5 — — — 36.7 — —
(Peach) (12.1)
B2O3
Schorl 37.0 33.1 9.3 6.2 0.5 2.6 0.7 1.4 (7.7)
F (1.5)
H 2O
China-clay 46.7 39.6 — — — — — —
(13.4)
H 2O
Talc 61.7 — — 1.7 — 31.7 — —
(3.8)
H 2O
Serpentine 42.9 — — 3.8 — 40.5 — —
(12.6)
Olivine 39.3 — — 14.8 — 45.8 — —
Silicon, from a chemical point of view, is an interesting body. It combines with
iron to form a silicide; and is present in this condition in cast iron. Only in the case
of the analysis of this and similar substances is the assayer called on to report the
percentage of silicon. Silicon is readily converted into silica by the action of
oxidizing agents. Silica forms only one series of salts—the silicates—which have
in many cases a complex constitution; thus there are a large number of double
silicates, which vary among themselves, not only in the relation of base to acid
(which is the essential difference), but also in the ratio of the bases between
themselves (which varies with almost every specimen).
Silica is detected by heating the substance with a fluoride and sulphuric acid in a
platinum-crucible. On holding a rod, moistened with a drop of water, over the
67.0 19.2 — 0.3 1.2 1.8 2.2 7.2
felspar
Lime-
43.3 35.4 — 1.3 17.4 0.35 0.5 0.9
felspar
F (0.8)
Potash- H 2O
45.7 33.7 3.1 — — 1.1 7.5 2.8
mica
(4.9)
Magnesia-
39.1 15.4 7.1 — — 23.6 7.5 2.6 F (0.7)
mica
Hornblende 40.6 14.3 5.8 7.2 12.5 14.0 1.5 1.6
MnO
Augite 50.0 3.7 2.4 6.6 22.8 13.5 — —
(0.1)
Almandine MnO
39.7 19.7 — 39.7 — — — —
(Garnet) (1.8)
Chlorite H 2O
32.1 18.5 — — — 36.7 — —
(Peach) (12.1)
B2O3
Schorl 37.0 33.1 9.3 6.2 0.5 2.6 0.7 1.4 (7.7)
F (1.5)
H 2O
China-clay 46.7 39.6 — — — — — —
(13.4)
H 2O
Talc 61.7 — — 1.7 — 31.7 — —
(3.8)
H 2O
Serpentine 42.9 — — 3.8 — 40.5 — —
(12.6)
Olivine 39.3 — — 14.8 — 45.8 — —
Silicon, from a chemical point of view, is an interesting body. It combines with
iron to form a silicide; and is present in this condition in cast iron. Only in the case
of the analysis of this and similar substances is the assayer called on to report the
percentage of silicon. Silicon is readily converted into silica by the action of
oxidizing agents. Silica forms only one series of salts—the silicates—which have
in many cases a complex constitution; thus there are a large number of double
silicates, which vary among themselves, not only in the relation of base to acid
(which is the essential difference), but also in the ratio of the bases between
themselves (which varies with almost every specimen).
Silica is detected by heating the substance with a fluoride and sulphuric acid in a
platinum-crucible. On holding a rod, moistened with a drop of water, over the
Page 506
escaping fumes, the white crust of silica formed on the drop of water shows its
presence. The insolubility of a fragment of the mineral in a bead of microcosmic
salt, is also a very good test; the fragment, on prolonged heating, does not lose its
angular form.
There is no dry assay for this substance, nor volumetric method; when the
determination is required, it is carried out gravimetrically and, generally, by the
following plan.
If the sample contains oxides, sulphides, &c., in any quantity, these are first
dissolved out by treatment with acid, evaporated to dryness, taken up with
hydrochloric acid, and filtered. The dried residue is treated in the same way as the
silicates. Some silicates are completely decomposed by such treatment; but it saves
time (unless one is sure that no undecomposable silicate is present) to treat these in
the same way as the others. On the other hand, there are some silicates which are
only attacked with difficulty even by fusion with alkaline carbonates; consequently,
it is always well to have the substance reduced to the finest state of division by
careful powdering, as this greatly assists the subsequent action. With very hard
silicates, the grinding away of the mortar in this operation will be perceptible; the
foreign matter thus introduced must not be ignored. Previously igniting the
substance sometimes assists the powdering; but it is best to use a steel mortar. The
particles of steel can be removed by a magnet, or, where the nature of the substance
will allow it, by boiling with a little dilute hydrochloric acid.
The dried and powdered material is intimately mixed with four times its weight of
"fusion mixture" in a platinum-crucible or dish. It is then moderately heated over a
Bunsen burner, and afterwards more strongly fused over a blast, or enclosed in a
clay crucible in the wind-furnace. The action is continued until the fused mass is
perfectly tranquil. With very refractory substances, the action must be long
continued at a high temperature. When sufficiently cold, the crucible is examined
to see that no particles of foreign matter are adhering to its outer surface. It is then
transferred to a five- or six-inch evaporating-dish, where its contents are acted
upon with warm water for some time. The "melt" will slowly dissolve, but the
solution should be hastened by keeping the liquid moderately acid with
hydrochloric acid. When the "melt" has dissolved, clean and remove the platinum-
dish, and evaporate the solution to a paste. Continue the evaporation to dryness on
a water-bath (not on the hot plate), and whilst drying stir with a glass rod, feeling at
the bottom of the dish for any unfused particles, which, if present, can be detected
by their grittiness. If there is much grit, it will be necessary to repeat the assay; but
with a small quantity it will only be necessary to refuse the grit and silica after
ignition.
presence. The insolubility of a fragment of the mineral in a bead of microcosmic
salt, is also a very good test; the fragment, on prolonged heating, does not lose its
angular form.
There is no dry assay for this substance, nor volumetric method; when the
determination is required, it is carried out gravimetrically and, generally, by the
following plan.
If the sample contains oxides, sulphides, &c., in any quantity, these are first
dissolved out by treatment with acid, evaporated to dryness, taken up with
hydrochloric acid, and filtered. The dried residue is treated in the same way as the
silicates. Some silicates are completely decomposed by such treatment; but it saves
time (unless one is sure that no undecomposable silicate is present) to treat these in
the same way as the others. On the other hand, there are some silicates which are
only attacked with difficulty even by fusion with alkaline carbonates; consequently,
it is always well to have the substance reduced to the finest state of division by
careful powdering, as this greatly assists the subsequent action. With very hard
silicates, the grinding away of the mortar in this operation will be perceptible; the
foreign matter thus introduced must not be ignored. Previously igniting the
substance sometimes assists the powdering; but it is best to use a steel mortar. The
particles of steel can be removed by a magnet, or, where the nature of the substance
will allow it, by boiling with a little dilute hydrochloric acid.
The dried and powdered material is intimately mixed with four times its weight of
"fusion mixture" in a platinum-crucible or dish. It is then moderately heated over a
Bunsen burner, and afterwards more strongly fused over a blast, or enclosed in a
clay crucible in the wind-furnace. The action is continued until the fused mass is
perfectly tranquil. With very refractory substances, the action must be long
continued at a high temperature. When sufficiently cold, the crucible is examined
to see that no particles of foreign matter are adhering to its outer surface. It is then
transferred to a five- or six-inch evaporating-dish, where its contents are acted
upon with warm water for some time. The "melt" will slowly dissolve, but the
solution should be hastened by keeping the liquid moderately acid with
hydrochloric acid. When the "melt" has dissolved, clean and remove the platinum-
dish, and evaporate the solution to a paste. Continue the evaporation to dryness on
a water-bath (not on the hot plate), and whilst drying stir with a glass rod, feeling at
the bottom of the dish for any unfused particles, which, if present, can be detected
by their grittiness. If there is much grit, it will be necessary to repeat the assay; but
with a small quantity it will only be necessary to refuse the grit and silica after
ignition.
Page 507
During solution of the "melt" and evaporation (which may be carried on together),
a clear solution will not be obtained, a flocculent silica will separate out, and
towards the end of the evaporation the mass will get gelatinous. The drying of the
jelly must be finished on the water-bath; first, because at this temperature the silica
is rendered insoluble in hydrochloric acid, whilst the solubility of the alumina,
iron, &c., is unaffected, which would not be the case at a much higher temperature;
and second, because the gelatinous residue requires very cautious drying to prevent
loss from spirting.
When dry, the substance is moistened, and heated with strong hydrochloric acid,
and the sides of the dish are washed down with water. The silica is washed by
decantation two or three times with hydrochloric acid and hot water, before being
thrown on to the filter. The filtrate is again evaporated to dryness, taken up with a
little hydrochloric acid and water and again filtered. The residue on the filter is
silica. The two lots of silica are washed free from chlorides with hot water, dried
on an air-bath, transferred to a platinum-crucible, ignited gently at first, at last
strongly over the blast or in a muffle, cooled in a desiccator, and weighed.
The white powdery precipitate is silica (SiO2), and its weight, multiplied by 100,
and divided by the weight of ore taken, gives the percentage of silica in the sample.
Where the percentage of silicon is wanted, which is very rarely the case, it is got by
multiplying this result by 0.4667. It is always necessary to examine the purity of
the body weighed as silica. This is done by re-fusing the material weighed, and re-
determining the silica in it; or, better, by mixing a weighed portion in a platinum-
dish with a little strong sulphuric acid, covering with hydrofluoric acid, and
evaporating. In the latter case, the silica will be converted into fluoride, which will
be driven off, and the impurities will be left behind as sulphates of barium,
phosphate and oxide of tin, titanium, &c. This must be weighed and deducted from
the weight of the silica. In a complete examination of a silicate it should be treated
with the precipitate containing alumina, ferric oxide, &c.
EXAMINATION OF SILICATES.
The student interested in the analysis of rocks and rock-forming minerals is
advised to consult a valuable paper by Dr. W.F. Hillebrand in the Bulletin of the
United States Geological Survey, No. 148, to which I am very largely indebted in
the revision of the following pages.
Moisture.—Five grams of the powdered sample is dried between watch-glasses in
the water-oven for two hours, or till its weight is constant; and the loss is reported
a clear solution will not be obtained, a flocculent silica will separate out, and
towards the end of the evaporation the mass will get gelatinous. The drying of the
jelly must be finished on the water-bath; first, because at this temperature the silica
is rendered insoluble in hydrochloric acid, whilst the solubility of the alumina,
iron, &c., is unaffected, which would not be the case at a much higher temperature;
and second, because the gelatinous residue requires very cautious drying to prevent
loss from spirting.
When dry, the substance is moistened, and heated with strong hydrochloric acid,
and the sides of the dish are washed down with water. The silica is washed by
decantation two or three times with hydrochloric acid and hot water, before being
thrown on to the filter. The filtrate is again evaporated to dryness, taken up with a
little hydrochloric acid and water and again filtered. The residue on the filter is
silica. The two lots of silica are washed free from chlorides with hot water, dried
on an air-bath, transferred to a platinum-crucible, ignited gently at first, at last
strongly over the blast or in a muffle, cooled in a desiccator, and weighed.
The white powdery precipitate is silica (SiO2), and its weight, multiplied by 100,
and divided by the weight of ore taken, gives the percentage of silica in the sample.
Where the percentage of silicon is wanted, which is very rarely the case, it is got by
multiplying this result by 0.4667. It is always necessary to examine the purity of
the body weighed as silica. This is done by re-fusing the material weighed, and re-
determining the silica in it; or, better, by mixing a weighed portion in a platinum-
dish with a little strong sulphuric acid, covering with hydrofluoric acid, and
evaporating. In the latter case, the silica will be converted into fluoride, which will
be driven off, and the impurities will be left behind as sulphates of barium,
phosphate and oxide of tin, titanium, &c. This must be weighed and deducted from
the weight of the silica. In a complete examination of a silicate it should be treated
with the precipitate containing alumina, ferric oxide, &c.
EXAMINATION OF SILICATES.
The student interested in the analysis of rocks and rock-forming minerals is
advised to consult a valuable paper by Dr. W.F. Hillebrand in the Bulletin of the
United States Geological Survey, No. 148, to which I am very largely indebted in
the revision of the following pages.
Moisture.—Five grams of the powdered sample is dried between watch-glasses in
the water-oven for two hours, or till its weight is constant; and the loss is reported
Page 508
as water lost at 100° C. The rest of the determinations are made on this dried
mineral.
Combined Water, &c.—Weigh up 1 gram of the substance, and ignite over the
blowpipe for some time in a platinum-crucible, cool in a desiccator, and weigh.
Record the loss as "loss on ignition," not as "combined water."
Silica.—The ignition should have been performed in an oxidising atmosphere in a
muffle or over a slanting blowpipe flame; this will ensure the oxidation of any
pyrites or other sulphide present, which if unoxidised would injure the crucible in
the next operation. The ignited residue is mixed with 6 or 7 grams of anhydrous
sodium carbonate. This reagent should be the purest obtainable, but its purity
should be checked, or rather its impurities should be determined by running a
"check" or "blank" assay with 10 grams of it through the stages of the analysis; the
impurities will be chiefly silica, alumina and lime, and altogether they ought not to
exceed 1 milligram. The crucible with the mixture is heated at first gently over a
Bunsen and afterwards more strongly in an oxidising atmosphere in a muffle or
over the blowpipe. The fused mass is allowed to cool in the crucible, and is then
dissolved out in a basin with water and a small excess of hydrochloric acid. After
the removal and cleaning of the crucible, the liquor is evaporated almost to
dryness. Dr. Hillebrand advises stopping short of complete dryness. The residue is
taken up with a little hydrochloric acid and water and filtered and washed. The
liquor, including the washings, is again evaporated and taken up with water and a
little acid. Usually about 1 per cent. of silica will be thus recovered. It is to be
filtered off and washed and added to the main silica. The filtrate is reserved. The
silica, thoroughly washed, is dried and ignited at a high temperature for twenty or
thirty minutes. It is then weighed in a platinum crucible. After weighing it is
treated with hydrofluoric acid and a little sulphuric, carefully evaporated and
ignited strongly. The residue, which in extreme cases may amount to 2 or 3 per
cent. of the rock, is weighed and deducted from the weight of the impure silica. It
is retained in the crucible.
Alumina, &c.—The filtrate from silica is treated by the basic acetate method. That
is, it is first treated by a cautious addition of a solution of soda, almost to the point
of producing a precipitate, in order to neutralise the excess of acid; 2 or 3 grams of
sodium acetate are added, and the whole boiled for a minute or so. The precipitate
is filtered off and washed only slightly. Save the filtrate. The precipitate is
dissolved in hydrochloric, or, perhaps better, in nitric acid; and is reprecipitated by
adding an excess of ammonia and boiling. The precipitate is filtered and washed
with water containing 2 per cent. of ammonium nitrate. Both filtrates are
evaporated separately to a small bulk, a drop or two of ammonia being added to the
second towards the finish. They are next filtered into a 6 or 8-ounce flask through a
mineral.
Combined Water, &c.—Weigh up 1 gram of the substance, and ignite over the
blowpipe for some time in a platinum-crucible, cool in a desiccator, and weigh.
Record the loss as "loss on ignition," not as "combined water."
Silica.—The ignition should have been performed in an oxidising atmosphere in a
muffle or over a slanting blowpipe flame; this will ensure the oxidation of any
pyrites or other sulphide present, which if unoxidised would injure the crucible in
the next operation. The ignited residue is mixed with 6 or 7 grams of anhydrous
sodium carbonate. This reagent should be the purest obtainable, but its purity
should be checked, or rather its impurities should be determined by running a
"check" or "blank" assay with 10 grams of it through the stages of the analysis; the
impurities will be chiefly silica, alumina and lime, and altogether they ought not to
exceed 1 milligram. The crucible with the mixture is heated at first gently over a
Bunsen and afterwards more strongly in an oxidising atmosphere in a muffle or
over the blowpipe. The fused mass is allowed to cool in the crucible, and is then
dissolved out in a basin with water and a small excess of hydrochloric acid. After
the removal and cleaning of the crucible, the liquor is evaporated almost to
dryness. Dr. Hillebrand advises stopping short of complete dryness. The residue is
taken up with a little hydrochloric acid and water and filtered and washed. The
liquor, including the washings, is again evaporated and taken up with water and a
little acid. Usually about 1 per cent. of silica will be thus recovered. It is to be
filtered off and washed and added to the main silica. The filtrate is reserved. The
silica, thoroughly washed, is dried and ignited at a high temperature for twenty or
thirty minutes. It is then weighed in a platinum crucible. After weighing it is
treated with hydrofluoric acid and a little sulphuric, carefully evaporated and
ignited strongly. The residue, which in extreme cases may amount to 2 or 3 per
cent. of the rock, is weighed and deducted from the weight of the impure silica. It
is retained in the crucible.
Alumina, &c.—The filtrate from silica is treated by the basic acetate method. That
is, it is first treated by a cautious addition of a solution of soda, almost to the point
of producing a precipitate, in order to neutralise the excess of acid; 2 or 3 grams of
sodium acetate are added, and the whole boiled for a minute or so. The precipitate
is filtered off and washed only slightly. Save the filtrate. The precipitate is
dissolved in hydrochloric, or, perhaps better, in nitric acid; and is reprecipitated by
adding an excess of ammonia and boiling. The precipitate is filtered and washed
with water containing 2 per cent. of ammonium nitrate. Both filtrates are
evaporated separately to a small bulk, a drop or two of ammonia being added to the
second towards the finish. They are next filtered into a 6 or 8-ounce flask through a
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small filter, the second filtrate coming after, and serving in a manner as wash water
for the first[113]. The two washed alumina precipitates are dried and placed in the
platinum crucible containing the residue from silica after treatment with
hydrofluoric acid. They are then ignited in an oxidising atmosphere at a high
temperature for about 10 minutes. The weight, including that of the residue from
the silica, is noted as that of "alumina, &c."
The weighed oxides are next fused with bisulphate of potash for some hours. The
bisulphate should have been first fused, apart, until the effervescence from the
escape of steam has stopped. The melt is dissolved out with cold water and dilute
sulphuric acid, and any insoluble residue is filtered off, washed, ignited and
weighed. The filtrate is reserved for determinations of iron and titanium. The
residue, after weighing, may be treated with hydrofluoric and sulphuric acids for
any silica,[114] which would be determined by loss. It may be tested for barium
sulphate by treatment with hot strong sulphuric acid; in which this salt dissolves,
but is again insoluble (and so comes out as a white precipitate) on diluting with
cold water; the acid also must be cold before adding the water. The filtrate
containing the iron is reduced with sulphuretted hydrogen, boiled till free from that
gas, filtered and titrated with a standard solution of permanganate of potassium.
The iron found is calculated to ferric oxide by dividing by .7. The iron solution
after titration serves for the determination of titanium oxide (TiO2). This is done
colorimetrically, by adding peroxide of hydrogen free from hydrofluoric acid, and
comparing the brown colour produced with that produced by the addition of a
standard solution of titanium to an equal volume of water containing sulphuric
acid.[115] The alumina is determined by difference. From the weight of the
combined precipitate which has been recorded as "Alumina, &c.," deduct (1) the
residue, insoluble, after fusion with bisulphate; (2) the ferric oxide; (3) the titanium
oxide; and (4) the phosphoric oxide (P2O5), the amount of which is subsequently
determined in a separate portion. This gives the alumina.
Manganous oxide, &c.—The filtrate from the "alumina, &c." contained in a 6 or
8-ounce flask, which it nearly fills, is made slightly alkaline with ammonia and
treated with a small excess of ammonium sulphide; the flask is then corked and
placed on one side for some time (a day or so) so that the manganese sulphide may
separate. The precipitate is filtered off and washed with water containing
ammonium chloride and a few drops of ammonium sulphide. The filtrate is
reserved for lime, &c. The precipitate is digested with sulphuretted hydrogen
water, to which one-fifth of its volume of strong hydrochloric acid has been added;
this dissolves the sulphides of zinc and manganese; any black residue should be
tested for copper and perhaps nickel. The solution is evaporated to dryness, taken
up with a little water and treated with a small excess of solution of carbonate of
for the first[113]. The two washed alumina precipitates are dried and placed in the
platinum crucible containing the residue from silica after treatment with
hydrofluoric acid. They are then ignited in an oxidising atmosphere at a high
temperature for about 10 minutes. The weight, including that of the residue from
the silica, is noted as that of "alumina, &c."
The weighed oxides are next fused with bisulphate of potash for some hours. The
bisulphate should have been first fused, apart, until the effervescence from the
escape of steam has stopped. The melt is dissolved out with cold water and dilute
sulphuric acid, and any insoluble residue is filtered off, washed, ignited and
weighed. The filtrate is reserved for determinations of iron and titanium. The
residue, after weighing, may be treated with hydrofluoric and sulphuric acids for
any silica,[114] which would be determined by loss. It may be tested for barium
sulphate by treatment with hot strong sulphuric acid; in which this salt dissolves,
but is again insoluble (and so comes out as a white precipitate) on diluting with
cold water; the acid also must be cold before adding the water. The filtrate
containing the iron is reduced with sulphuretted hydrogen, boiled till free from that
gas, filtered and titrated with a standard solution of permanganate of potassium.
The iron found is calculated to ferric oxide by dividing by .7. The iron solution
after titration serves for the determination of titanium oxide (TiO2). This is done
colorimetrically, by adding peroxide of hydrogen free from hydrofluoric acid, and
comparing the brown colour produced with that produced by the addition of a
standard solution of titanium to an equal volume of water containing sulphuric
acid.[115] The alumina is determined by difference. From the weight of the
combined precipitate which has been recorded as "Alumina, &c.," deduct (1) the
residue, insoluble, after fusion with bisulphate; (2) the ferric oxide; (3) the titanium
oxide; and (4) the phosphoric oxide (P2O5), the amount of which is subsequently
determined in a separate portion. This gives the alumina.
Manganous oxide, &c.—The filtrate from the "alumina, &c." contained in a 6 or
8-ounce flask, which it nearly fills, is made slightly alkaline with ammonia and
treated with a small excess of ammonium sulphide; the flask is then corked and
placed on one side for some time (a day or so) so that the manganese sulphide may
separate. The precipitate is filtered off and washed with water containing
ammonium chloride and a few drops of ammonium sulphide. The filtrate is
reserved for lime, &c. The precipitate is digested with sulphuretted hydrogen
water, to which one-fifth of its volume of strong hydrochloric acid has been added;
this dissolves the sulphides of zinc and manganese; any black residue should be
tested for copper and perhaps nickel. The solution is evaporated to dryness, taken
up with a little water and treated with a small excess of solution of carbonate of
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soda. It is boiled and again evaporated, washed out with hot water and filtered on
to a small filter, dried, ignited, and weighed as Mn3O4. It is calculated to MnO. It
may contain, and should be tested for oxide of zinc, which, if present, must be
deducted. If the dish becomes stained during evaporation, take up with a few drops
of hydrochloric and sulphurous acids, evaporate, and then treat with carbonate of
soda.
Lime, &c.—The filtrate from the manganese sulphide is boiled, and without
cooling, treated with ammonium oxalate in solution, which also should be heated
to boiling. The liquid is filtered off and reserved for magnesia. The precipitate is
dissolved in very little hydrochloric acid and reprecipitated by adding ammonium
oxalate and ammonia to the boiling solution. The filtrate and washings from this
are reserved for magnesia. The precipitate is either dissolved in dilute sulphuric
and titrated with permanganate of potash as described under Lime (p. 322); or it is
ignited and weighed as oxide. In this last case it may be examined for barium and
strontium, the former of which will rarely be present.
Magnesia.—The filtrate from the first lime precipitate is treated with sodium
phosphate and ammonia, and allowed to stand overnight. It is then filtered. The
precipitate is dissolved in hydrochloric acid; the solution is filtered into the beaker
containing the solution from the second lime precipitate. Ammonia and sodium
phosphate are again added, and the precipitate, after standing, is filtered off,
washed with water containing ammonia; it is then dried, ignited and weighed as
magnesium pyrophosphate. This is calculated into magnesia.
Potash and Soda.—Weigh out .5 gram of the dried ore, and mix with an equal
quantity of ammonic chloride; and to the mixture add gradually 4 grams of calcium
carbonate ("precipitated"). Introduce into a platinum-crucible and cover loosely.
Heat, at first, gently; and then at a red heat for from forty to sixty minutes. Transfer
to a porcelain dish, and digest with 60 or 80 c.c. of water; warm and filter: to the
filtrate add ammonic carbonate and ammonia, and filter; evaporate the filtrate to
dryness, adding a few drops more of ammonic carbonate towards the end; when
dry, heat gently, and then raise the temperature to a little below redness. Dissolve
in a small quantity of water, add a drop of ammonic carbonate, and filter through a
small filter into a weighed platinum dish. Evaporate, ignite gently, and weigh. The
residue contains the soda and potash of the mineral as chlorides.
To determine the proportion of potassium, dissolve this residue in a little water, add
platinum chloride in excess, evaporate to a paste, extract with alcohol, decant
through a small weighed filter, wash with alcohol, and dry at 100° C. Weigh. The
to a small filter, dried, ignited, and weighed as Mn3O4. It is calculated to MnO. It
may contain, and should be tested for oxide of zinc, which, if present, must be
deducted. If the dish becomes stained during evaporation, take up with a few drops
of hydrochloric and sulphurous acids, evaporate, and then treat with carbonate of
soda.
Lime, &c.—The filtrate from the manganese sulphide is boiled, and without
cooling, treated with ammonium oxalate in solution, which also should be heated
to boiling. The liquid is filtered off and reserved for magnesia. The precipitate is
dissolved in very little hydrochloric acid and reprecipitated by adding ammonium
oxalate and ammonia to the boiling solution. The filtrate and washings from this
are reserved for magnesia. The precipitate is either dissolved in dilute sulphuric
and titrated with permanganate of potash as described under Lime (p. 322); or it is
ignited and weighed as oxide. In this last case it may be examined for barium and
strontium, the former of which will rarely be present.
Magnesia.—The filtrate from the first lime precipitate is treated with sodium
phosphate and ammonia, and allowed to stand overnight. It is then filtered. The
precipitate is dissolved in hydrochloric acid; the solution is filtered into the beaker
containing the solution from the second lime precipitate. Ammonia and sodium
phosphate are again added, and the precipitate, after standing, is filtered off,
washed with water containing ammonia; it is then dried, ignited and weighed as
magnesium pyrophosphate. This is calculated into magnesia.
Potash and Soda.—Weigh out .5 gram of the dried ore, and mix with an equal
quantity of ammonic chloride; and to the mixture add gradually 4 grams of calcium
carbonate ("precipitated"). Introduce into a platinum-crucible and cover loosely.
Heat, at first, gently; and then at a red heat for from forty to sixty minutes. Transfer
to a porcelain dish, and digest with 60 or 80 c.c. of water; warm and filter: to the
filtrate add ammonic carbonate and ammonia, and filter; evaporate the filtrate to
dryness, adding a few drops more of ammonic carbonate towards the end; when
dry, heat gently, and then raise the temperature to a little below redness. Dissolve
in a small quantity of water, add a drop of ammonic carbonate, and filter through a
small filter into a weighed platinum dish. Evaporate, ignite gently, and weigh. The
residue contains the soda and potash of the mineral as chlorides.
To determine the proportion of potassium, dissolve this residue in a little water, add
platinum chloride in excess, evaporate to a paste, extract with alcohol, decant
through a small weighed filter, wash with alcohol, and dry at 100° C. Weigh. The
Page 511
substance is potassium platinic chloride (2KCl.PtCl4). Its weight, multiplied by
0.1941, will give the weight of potash (K2O).
To find the proportion of soda, multiply the weight of the potassium platinic
chloride by 0.306; this gives the weight of potassium chloride. Deduct this from
the weight of the mixed chlorides first got; the difference will be the sodium
chloride, which weight, multiplied by 0.53, will give the weight of soda (Na2O).
Ferrous Oxide.—When a qualitative test shows both ferric and ferrous oxide to be
present, the proportion of the ferrous oxide must be separately determined. The
finely ground mineral mixed with dilute sulphuric acid is treated on a water bath
with hydrofluoric acid. Solution is best effected in an atmosphere of carbonic acid.
In about an hour the decomposition is complete, and the solution is diluted with
cold water, and titrated with the solution of bichromate or of permanganate of
potassium. The iron found is multiplied by 1.286, and reported as ferrous oxide. To
find the proportion of ferric oxide, the ferrous iron found is multiplied by 1.428,
and this is deducted from the weight of ferric oxide obtained by precipitation with
ammonia. The ammonia precipitate contains the whole of the iron as ferric oxide;
hence the necessity for calculating the ferrous oxide as ferric, and deducting it.
Phosphoric Oxide (P2O5).—Weigh up 5 grams of the finely-divided and dry
sample, and digest with 10 or 20 c.c. of nitric acid; evaporate to dryness on the
water-bath; take up with a little dilute nitric acid; dilute with water; and filter. Add
a few grams of ammonic nitrate and 10 c.c. of ammonium molybdate solution, heat
nearly to boiling, and allow to settle; filter off, and wash the yellow precipitate.
Dissolve with dilute ammonia, add "magnesia mixture," and allow to stand
overnight. Filter, wash with dilute ammonia, dry, ignite, and weigh as
pyrophosphate of magnesia. The weight, multiplied by 0.6396, gives the weight of
phosphoric oxide.
Soluble Silica.—Some silicates are acted on by hydrochloric acid, and leave on
evaporation a residue; which, when the soluble salts have been washed out,
consists generally of the separated silica with perhaps quartz and unattacked
silicates. It should be ignited, weighed and boiled with a solution containing less
than 10 per cent. of caustic soda: this dissolves the separated silica. The liquor is
diluted, rendered faintly acid, and filtered. The residue is washed, ignited and
weighed. The loss gives the soluble silica.
Estimation of Silica in Slags (Ferrous silicates).—Take 1 gram of the powdered
slag, treat with aqua regia, evaporate to dryness, extract with hydrochloric acid,
filter, dry, ignite, and fuse the ignited residue with "fusion mixture," then separate
and weigh the silica in the usual way. Slags are for the most part decomposed by
0.1941, will give the weight of potash (K2O).
To find the proportion of soda, multiply the weight of the potassium platinic
chloride by 0.306; this gives the weight of potassium chloride. Deduct this from
the weight of the mixed chlorides first got; the difference will be the sodium
chloride, which weight, multiplied by 0.53, will give the weight of soda (Na2O).
Ferrous Oxide.—When a qualitative test shows both ferric and ferrous oxide to be
present, the proportion of the ferrous oxide must be separately determined. The
finely ground mineral mixed with dilute sulphuric acid is treated on a water bath
with hydrofluoric acid. Solution is best effected in an atmosphere of carbonic acid.
In about an hour the decomposition is complete, and the solution is diluted with
cold water, and titrated with the solution of bichromate or of permanganate of
potassium. The iron found is multiplied by 1.286, and reported as ferrous oxide. To
find the proportion of ferric oxide, the ferrous iron found is multiplied by 1.428,
and this is deducted from the weight of ferric oxide obtained by precipitation with
ammonia. The ammonia precipitate contains the whole of the iron as ferric oxide;
hence the necessity for calculating the ferrous oxide as ferric, and deducting it.
Phosphoric Oxide (P2O5).—Weigh up 5 grams of the finely-divided and dry
sample, and digest with 10 or 20 c.c. of nitric acid; evaporate to dryness on the
water-bath; take up with a little dilute nitric acid; dilute with water; and filter. Add
a few grams of ammonic nitrate and 10 c.c. of ammonium molybdate solution, heat
nearly to boiling, and allow to settle; filter off, and wash the yellow precipitate.
Dissolve with dilute ammonia, add "magnesia mixture," and allow to stand
overnight. Filter, wash with dilute ammonia, dry, ignite, and weigh as
pyrophosphate of magnesia. The weight, multiplied by 0.6396, gives the weight of
phosphoric oxide.
Soluble Silica.—Some silicates are acted on by hydrochloric acid, and leave on
evaporation a residue; which, when the soluble salts have been washed out,
consists generally of the separated silica with perhaps quartz and unattacked
silicates. It should be ignited, weighed and boiled with a solution containing less
than 10 per cent. of caustic soda: this dissolves the separated silica. The liquor is
diluted, rendered faintly acid, and filtered. The residue is washed, ignited and
weighed. The loss gives the soluble silica.
Estimation of Silica in Slags (Ferrous silicates).—Take 1 gram of the powdered
slag, treat with aqua regia, evaporate to dryness, extract with hydrochloric acid,
filter, dry, ignite, and fuse the ignited residue with "fusion mixture," then separate
and weigh the silica in the usual way. Slags are for the most part decomposed by
Page 512
boiling with aqua regia, but it will be found more convenient and accurate to first
extract with acids and then to treat the residue as an insoluble silicate.
Estimation of "Silica and Insoluble Silicates" in an Ore.—Take 2 grams of the
powdered mineral, evaporate with nitric acid (if sulphides are present), treat the
dried residue (or the original substance if sulphides are absent) with 10 or 20 c.c. of
hydrochloric acid; again evaporate to dryness, take up with dilute hydrochloric
acid, filter, wash, ignite, and weigh.
Estimation of Silicon in Iron.—Place 2 grams of the metal (borings or filings) in
a four-inch evaporating dish, and dissolve (with aid of heat) in 25 c.c. of dilute
nitric acid. Evaporate to complete dryness, take up with 20 c.c. of hydrochloric
acid, and allow to digest for one hour. Boil down to a small bulk, dilute with a 5
per cent. solution of hydrochloric acid, boil, and filter. Wash with acid and water,
dry, ignite in a platinum crucible, and weigh the SiO2. This, multiplied by 0.4673,
gives the weight of the silicon. The percentage is calculated in the usual way.
PRACTICAL EXERCISES.
1. A certain rock is a mixture of 70 per cent. of quartz, 25 per cent. of potash-
felspar, and 5 per cent. of potash-mica. What per cent. of silica will it contain?
2. Two grams of a mixture of silica and cassiterite left, after reduction in hydrogen,
1.78 grams. Assuming all the oxide of tin to have been reduced, what will be the
percentage of silica?
3. The formula of a compound is 2FeO.SiO2. What percentage of silica will it
contain?
4. Two grams of a sample of cast-iron gave 0.025 gram of silica. Find the
percentage of silicon in the metal.
5. What weights of quartz and marble (CaCO3) would you take to make 30 grams
of a slag having the formula CaO.SiO2?
CARBON AND CARBONATES.
Carbon compounds enter so largely into the structure of organised bodies that their
chemistry is generally considered apart from that of the other elements under the
head of Organic Chemistry. Carbon occurs, however, among minerals not only in
the oxidised state (as carbonates), but also in the elementary form (as in diamond
extract with acids and then to treat the residue as an insoluble silicate.
Estimation of "Silica and Insoluble Silicates" in an Ore.—Take 2 grams of the
powdered mineral, evaporate with nitric acid (if sulphides are present), treat the
dried residue (or the original substance if sulphides are absent) with 10 or 20 c.c. of
hydrochloric acid; again evaporate to dryness, take up with dilute hydrochloric
acid, filter, wash, ignite, and weigh.
Estimation of Silicon in Iron.—Place 2 grams of the metal (borings or filings) in
a four-inch evaporating dish, and dissolve (with aid of heat) in 25 c.c. of dilute
nitric acid. Evaporate to complete dryness, take up with 20 c.c. of hydrochloric
acid, and allow to digest for one hour. Boil down to a small bulk, dilute with a 5
per cent. solution of hydrochloric acid, boil, and filter. Wash with acid and water,
dry, ignite in a platinum crucible, and weigh the SiO2. This, multiplied by 0.4673,
gives the weight of the silicon. The percentage is calculated in the usual way.
PRACTICAL EXERCISES.
1. A certain rock is a mixture of 70 per cent. of quartz, 25 per cent. of potash-
felspar, and 5 per cent. of potash-mica. What per cent. of silica will it contain?
2. Two grams of a mixture of silica and cassiterite left, after reduction in hydrogen,
1.78 grams. Assuming all the oxide of tin to have been reduced, what will be the
percentage of silica?
3. The formula of a compound is 2FeO.SiO2. What percentage of silica will it
contain?
4. Two grams of a sample of cast-iron gave 0.025 gram of silica. Find the
percentage of silicon in the metal.
5. What weights of quartz and marble (CaCO3) would you take to make 30 grams
of a slag having the formula CaO.SiO2?
CARBON AND CARBONATES.
Carbon compounds enter so largely into the structure of organised bodies that their
chemistry is generally considered apart from that of the other elements under the
head of Organic Chemistry. Carbon occurs, however, among minerals not only in
the oxidised state (as carbonates), but also in the elementary form (as in diamond
Page 513
and graphite), and combined with hydrogen, oxygen, &c. (as in petroleums,
bitumens, lignites, shales, and coals). In small quantities "organic matter" is widely
diffused in minerals and rocks. In shales and clays it may amount to as much as 10
or 20 per cent. (mainly as bituminous and coaly matters).
The assayer has only to take account of the organic matter when it is of
commercial importance, so that in assays it is generally included under "loss on
ignition."
In coals, shales, lignites, &c., the carbon compounds are, on heating, split up into
oils and similar compounds. The products of distillation may be classified as water,
gas, tars, coke, and ash. The assay of these bodies generally resolves itself into a
distillation, and, in the case of the shales, an examination of the distillates for the
useful oils, paraffin, creosote, &c., contained in them.
Elementary carbon is found in nature in three different forms, but these all re-act
chemically in the same way. They combine with oxygen to form the dioxide.[116]
The weight of oxygen required to burn a given weight of any form of carbon is the
same, and the resulting product from all three has the same characteristic
properties. Carbon dioxide is the common oxide of carbon. A lower oxide exists,
but on burning it is converted into the dioxide. Wherever the oxidation of carbon
takes place, if there is sufficient oxygen, carbon dioxide (carbonic acid) is formed;
this re-action is the one used for the determination of carbon in bodies generally.
The dioxide has acid properties, and combines with lime and other bases forming a
series of salts called carbonates.
The carbon-compounds (other than carbonates, which will be subsequently
considered) occurring in minerals are generally characterised by their sparing
solubility in acids. The diamond is distinguished from other crystals by its
hardness, lustre, and specific gravity. It may be subjected to a red heat without
being apparently affected, but at a higher temperature it slowly burns away.
Graphite, also, burns slowly, but at a lower temperature. The other bodies (coals,
shales, &c.) differ considerably among themselves in the temperature at which they
commence to burn. Some, such as anthracite, burn with little or no flame, but most
give off gases, which burn with a luminous flame. They deflagrate when sprinkled
on fused nitre, forming carbonate of potash. In making this test the student must
remember that sulphur and, in fact, all oxidisable bodies similarly deflagrate, but it
is only in the case of carbon compounds that carbonate of potash is formed. Carbon
unites with iron and some of the metals to form carbides; combined carbon of this
kind is detected by the odour of the carburetted hydrogen evolved when the metal
is treated with hydrochloric acid; for example, on dissolving steel in acid.
bitumens, lignites, shales, and coals). In small quantities "organic matter" is widely
diffused in minerals and rocks. In shales and clays it may amount to as much as 10
or 20 per cent. (mainly as bituminous and coaly matters).
The assayer has only to take account of the organic matter when it is of
commercial importance, so that in assays it is generally included under "loss on
ignition."
In coals, shales, lignites, &c., the carbon compounds are, on heating, split up into
oils and similar compounds. The products of distillation may be classified as water,
gas, tars, coke, and ash. The assay of these bodies generally resolves itself into a
distillation, and, in the case of the shales, an examination of the distillates for the
useful oils, paraffin, creosote, &c., contained in them.
Elementary carbon is found in nature in three different forms, but these all re-act
chemically in the same way. They combine with oxygen to form the dioxide.[116]
The weight of oxygen required to burn a given weight of any form of carbon is the
same, and the resulting product from all three has the same characteristic
properties. Carbon dioxide is the common oxide of carbon. A lower oxide exists,
but on burning it is converted into the dioxide. Wherever the oxidation of carbon
takes place, if there is sufficient oxygen, carbon dioxide (carbonic acid) is formed;
this re-action is the one used for the determination of carbon in bodies generally.
The dioxide has acid properties, and combines with lime and other bases forming a
series of salts called carbonates.
The carbon-compounds (other than carbonates, which will be subsequently
considered) occurring in minerals are generally characterised by their sparing
solubility in acids. The diamond is distinguished from other crystals by its
hardness, lustre, and specific gravity. It may be subjected to a red heat without
being apparently affected, but at a higher temperature it slowly burns away.
Graphite, also, burns slowly, but at a lower temperature. The other bodies (coals,
shales, &c.) differ considerably among themselves in the temperature at which they
commence to burn. Some, such as anthracite, burn with little or no flame, but most
give off gases, which burn with a luminous flame. They deflagrate when sprinkled
on fused nitre, forming carbonate of potash. In making this test the student must
remember that sulphur and, in fact, all oxidisable bodies similarly deflagrate, but it
is only in the case of carbon compounds that carbonate of potash is formed. Carbon
unites with iron and some of the metals to form carbides; combined carbon of this
kind is detected by the odour of the carburetted hydrogen evolved when the metal
is treated with hydrochloric acid; for example, on dissolving steel in acid.
Page 514
The natural carbon compounds, although, speaking generally, insoluble in
hydrochloric or nitric acids, are more or less attacked by aqua regia. The assayer
seldom requires these compounds to be in solution. The presence of "organic
matter"[117] interferes with most of the reactions which are used for the
determination of the metals. Consequently, in such cases, it should be removed by
calcination unless it is known that its presence will not interfere. When calcination
is not admissible it may be destroyed by heating with strong sulphuric acid and
bichromate or permanganate of potash or by fusion with nitre.
Carbon may be separated from other substances by conversion into carbon dioxide
by burning. In most cases substances soluble in acids are first removed, and the
insoluble residue dried, weighed, and then calcined or burned in a current of air.
The quantity of "organic matter" may be determined indirectly by the loss the
substance undergoes, but it is better to determine the "organic carbon" by confining
the calcination in a tube, and collecting and weighing the carbon dioxide formed.
Each gram of carbon dioxide is equivalent to 0.2727 gram of carbon.
Instead of a current of oxygen or air, oxide of copper may be more conveniently
used. The operation is as follows:—Take a clean and dry piece of combustion tube
drawn out and closed at one end, as shown in the figure (fig. 70), and about
eighteen inches long. Fit it with a perforated cork connected with a U-tube
hydrochloric or nitric acids, are more or less attacked by aqua regia. The assayer
seldom requires these compounds to be in solution. The presence of "organic
matter"[117] interferes with most of the reactions which are used for the
determination of the metals. Consequently, in such cases, it should be removed by
calcination unless it is known that its presence will not interfere. When calcination
is not admissible it may be destroyed by heating with strong sulphuric acid and
bichromate or permanganate of potash or by fusion with nitre.
Carbon may be separated from other substances by conversion into carbon dioxide
by burning. In most cases substances soluble in acids are first removed, and the
insoluble residue dried, weighed, and then calcined or burned in a current of air.
The quantity of "organic matter" may be determined indirectly by the loss the
substance undergoes, but it is better to determine the "organic carbon" by confining
the calcination in a tube, and collecting and weighing the carbon dioxide formed.
Each gram of carbon dioxide is equivalent to 0.2727 gram of carbon.
Instead of a current of oxygen or air, oxide of copper may be more conveniently
used. The operation is as follows:—Take a clean and dry piece of combustion tube
drawn out and closed at one end, as shown in the figure (fig. 70), and about
eighteen inches long. Fit it with a perforated cork connected with a U-tube
Page 515
(containing freshly-fused calcium chloride in coarse grains) and a set of potash
bulbs (fig. 71) (containing a strong solution of potash), the exit of which last is
provided with a small tube containing calcium chloride or a stick of potash. Both
the U-tube and bulbs should have a loop of fine wire, by which they may be
suspended on the hook of the balance for convenience in weighing. They must both
be weighed before the combustion is commenced; to prevent absorption of
moisture during weighing, &c., the ends are plugged with pieces of tube and glass
rod.
Fill the combustion tube to a depth of about eight inches with some copper oxide,
which has been recently ignited and cooled in a close vessel. Put in the weighed
portion for assay and a little fresh copper oxide, and mix in the tube by means of an
iron wire shaped at the end after the manner of a corkscrew. Put in some more
oxide of copper, and clean the stirrer in it. Close loosely with a plug of recently
ignited asbestos, place in the furnace, and connect the U-tube and bulbs in the way
shown in the sketch (fig. 72).
See that the joints are tight, and then commence the combustion by lighting the
burners nearest the U-tube; make the first three or four inches red hot, and
gradually extend the heat backwards the length of the tube, but avoid too rapid a
disengagement of gas. When gas ceases to come off, open the pointed end of the
tube and draw a current of dried air through the apparatus.
The carbon dioxide is absorbed in the potash bulbs, and their increase in weight
multiplied 0.2727 gives the amount of carbon in the substance taken.
The increase in weight in the calcium chloride tube will be due to the water formed
by the oxidation of the combined hydrogen. If this last is required the increase in
weight multiplied by 0.111 gives its amount.
COALS.
bulbs (fig. 71) (containing a strong solution of potash), the exit of which last is
provided with a small tube containing calcium chloride or a stick of potash. Both
the U-tube and bulbs should have a loop of fine wire, by which they may be
suspended on the hook of the balance for convenience in weighing. They must both
be weighed before the combustion is commenced; to prevent absorption of
moisture during weighing, &c., the ends are plugged with pieces of tube and glass
rod.
Fill the combustion tube to a depth of about eight inches with some copper oxide,
which has been recently ignited and cooled in a close vessel. Put in the weighed
portion for assay and a little fresh copper oxide, and mix in the tube by means of an
iron wire shaped at the end after the manner of a corkscrew. Put in some more
oxide of copper, and clean the stirrer in it. Close loosely with a plug of recently
ignited asbestos, place in the furnace, and connect the U-tube and bulbs in the way
shown in the sketch (fig. 72).
See that the joints are tight, and then commence the combustion by lighting the
burners nearest the U-tube; make the first three or four inches red hot, and
gradually extend the heat backwards the length of the tube, but avoid too rapid a
disengagement of gas. When gas ceases to come off, open the pointed end of the
tube and draw a current of dried air through the apparatus.
The carbon dioxide is absorbed in the potash bulbs, and their increase in weight
multiplied 0.2727 gives the amount of carbon in the substance taken.
The increase in weight in the calcium chloride tube will be due to the water formed
by the oxidation of the combined hydrogen. If this last is required the increase in
weight multiplied by 0.111 gives its amount.
COALS.
Page 516
The determination of the actual carbon in coals and shales is seldom called for; if
required, it would be performed in the way just described.[118] The ordinary assay
of a sample of coal involves the following determinations—moisture, volatile
matter, fixed carbon, ash, and sulphur. These are thus carried out:—
Determination of Moisture.—Take 3 grams of the powdered sample and dry in a
water-bath for an hour or so. The loss is reported as moisture. Coals carry from 1 to
2 per cent. If the drying is carried too far, coals gain a little in weight owing to
oxidation, so that it is not advisable to extend it over more than one or two hours.
Determination of Volatile Matter.—This determination is an approximate one,
and it is only when working under the same conditions with regard to time, amount
of coal taken, and degree of heat used, that concordant results can be arrived at. It
is a matter of importance whether the coal has been previously dried before heating
or not, since a difference of 2 per cent. may be got by working on the dried or
undried sample. Take 2 grams of the powdered, but undried, sample of coal, place
in a weighed platinum crucible, and support this over a good Bunsen burner by
means of a thin platinum-wire triangle. The heat is continued until no further
quantity of gas comes off and burns at the mouth. This takes only a few minutes.
The cover is tightly fitted on, and when cold the crucible is weighed. The loss in
weight, after deducting the moisture, gives the "volatile matter," and the residue
consists of "fixed carbon" and "ash."
Determination of Ash.—The coke produced in the last operation is turned out into
a porcelain dish and ignited over a Bunsen burner till the residue is free from
particles of carbon. Calcination is hastened by stirring with a platinum wire. The
operation may be done in a muffle, but this gives results a few tenths of a per cent.
too low. The dish is cooled in a dessicator, and weighed. The increase in weight
gives the amount of "ash," and the difference between this and the weight of the
coke gives the "fixed carbon."
The assay is reported as follows:—
Moisture at 100° C. __per cent.
Volatile matter __ "
Fixed carbon __ "
Ash __ "
contains sulphur __ per cent.
Determination of Sulphur.—The sulphur exists in the coal partly in organic
combination, partly as metallic sulphide (iron pyrites, marcasite, &c.), and,
perhaps, as sulphate. So that the sulphur determination must be separately reported,
required, it would be performed in the way just described.[118] The ordinary assay
of a sample of coal involves the following determinations—moisture, volatile
matter, fixed carbon, ash, and sulphur. These are thus carried out:—
Determination of Moisture.—Take 3 grams of the powdered sample and dry in a
water-bath for an hour or so. The loss is reported as moisture. Coals carry from 1 to
2 per cent. If the drying is carried too far, coals gain a little in weight owing to
oxidation, so that it is not advisable to extend it over more than one or two hours.
Determination of Volatile Matter.—This determination is an approximate one,
and it is only when working under the same conditions with regard to time, amount
of coal taken, and degree of heat used, that concordant results can be arrived at. It
is a matter of importance whether the coal has been previously dried before heating
or not, since a difference of 2 per cent. may be got by working on the dried or
undried sample. Take 2 grams of the powdered, but undried, sample of coal, place
in a weighed platinum crucible, and support this over a good Bunsen burner by
means of a thin platinum-wire triangle. The heat is continued until no further
quantity of gas comes off and burns at the mouth. This takes only a few minutes.
The cover is tightly fitted on, and when cold the crucible is weighed. The loss in
weight, after deducting the moisture, gives the "volatile matter," and the residue
consists of "fixed carbon" and "ash."
Determination of Ash.—The coke produced in the last operation is turned out into
a porcelain dish and ignited over a Bunsen burner till the residue is free from
particles of carbon. Calcination is hastened by stirring with a platinum wire. The
operation may be done in a muffle, but this gives results a few tenths of a per cent.
too low. The dish is cooled in a dessicator, and weighed. The increase in weight
gives the amount of "ash," and the difference between this and the weight of the
coke gives the "fixed carbon."
The assay is reported as follows:—
Moisture at 100° C. __per cent.
Volatile matter __ "
Fixed carbon __ "
Ash __ "
contains sulphur __ per cent.
Determination of Sulphur.—The sulphur exists in the coal partly in organic
combination, partly as metallic sulphide (iron pyrites, marcasite, &c.), and,
perhaps, as sulphate. So that the sulphur determination must be separately reported,
Page 517
since a portion will go off with the volatile matter, and the remainder would be
retained and weighed with the coke.
The sulphur is thus determined:—Take 1 gram of the coal and mix with 1.5 gram
of a mixture of 2 parts of calcined magnesia and 1 part of carbonate of soda, and
heat in a platinum crucible for one hour or until oxidation is complete. Turn out the
mass and extract it with water and bromine, filter, acidulate with hydrochloric acid,
boil off the bromine, and precipitate with baric chloride (estimating gravimetrically
as given under Sulphur). Another method is as follows:—Take 1 gram of the coal
and drop it gradually from a sheet of note paper on to 5 grams of fused nitre
contained in a platinum dish. Extract with water, acidify with acetic acid, and
estimate volumetrically as described under Sulphur.
Calorific Effect of Coals.—The heat-giving value of a coal is best expressed in
the number of pounds of water, previously heated to the boiling point, which it will
convert into steam. This is generally termed its evaporative-power. It may be
determined by means of the calorimeter (fig. 73). This consists of a glass cylinder
marked to hold 29.010 grains of water. The instrument consists of a perforated
copper stand, provided with a socket and three springs. The socket holds a copper
cylinder which is charged with 30 grains of the dried coal mixed with 300 grains of
a mixture of 3 parts of potassium chlorate and 1 part of nitre. The charge is well
retained and weighed with the coke.
The sulphur is thus determined:—Take 1 gram of the coal and mix with 1.5 gram
of a mixture of 2 parts of calcined magnesia and 1 part of carbonate of soda, and
heat in a platinum crucible for one hour or until oxidation is complete. Turn out the
mass and extract it with water and bromine, filter, acidulate with hydrochloric acid,
boil off the bromine, and precipitate with baric chloride (estimating gravimetrically
as given under Sulphur). Another method is as follows:—Take 1 gram of the coal
and drop it gradually from a sheet of note paper on to 5 grams of fused nitre
contained in a platinum dish. Extract with water, acidify with acetic acid, and
estimate volumetrically as described under Sulphur.
Calorific Effect of Coals.—The heat-giving value of a coal is best expressed in
the number of pounds of water, previously heated to the boiling point, which it will
convert into steam. This is generally termed its evaporative-power. It may be
determined by means of the calorimeter (fig. 73). This consists of a glass cylinder
marked to hold 29.010 grains of water. The instrument consists of a perforated
copper stand, provided with a socket and three springs. The socket holds a copper
cylinder which is charged with 30 grains of the dried coal mixed with 300 grains of
a mixture of 3 parts of potassium chlorate and 1 part of nitre. The charge is well
Page 518
packed in the cylinder and provided with a small fuse of cotton saturated with
nitre. Fill the glass cylinder to its mark with water and take the temperature with a
thermometer marked in degrees Fahrenheit. Ignite the fuse and immediately cover
with the outer copper cylinder (extinguisher-fashion), which will be held in its
place by the springs. The stop-cock should be closed before this is done. Place the
apparatus quickly in the cylinder of water. When the action is over open the stop-
cock and agitate the water by raising and lowering the instrument a few times.
Again take the temperature. The rise in temperature, plus 10 per cent. for the heat
used in warming the apparatus and lost by radiation, gives the evaporative-power.
The following is an example:—
Temperature before experiment67.0° F.
Temperature after " 79.0° "
————
Rise 12.0° "
+ 1/10th 1.2° "
————
Gives 13.2° "
One pound of the coal will evaporate 13.2 pounds of water.
SHALES, ETC.
The assay of these is carried out in the same way as that of coals, but the volatile
matters are separately examined, and, in consequence, a larger quantity of material
must be used. For the moisture, volatile matter, fixed carbon and ash, the
determinations are the same, but a special distillation must be made to obtain a
sufficient quantity of the volatile products for subsequent examination. Take 500 or
1000 grams of the well-sampled and powdered shale, and introduce into a cast-iron
retort as shown in fig. 74. Lute the joint with fire-clay, place the cover on, and bolt
it down. The bolts should have a covering of fire-clay to protect them from the
action of the fire. Place the retort in a wind furnace, supporting it on a brick, and
pack well around with coke. Build up the furnace around and over the retort with
loose fire-bricks, and heat gradually.
nitre. Fill the glass cylinder to its mark with water and take the temperature with a
thermometer marked in degrees Fahrenheit. Ignite the fuse and immediately cover
with the outer copper cylinder (extinguisher-fashion), which will be held in its
place by the springs. The stop-cock should be closed before this is done. Place the
apparatus quickly in the cylinder of water. When the action is over open the stop-
cock and agitate the water by raising and lowering the instrument a few times.
Again take the temperature. The rise in temperature, plus 10 per cent. for the heat
used in warming the apparatus and lost by radiation, gives the evaporative-power.
The following is an example:—
Temperature before experiment67.0° F.
Temperature after " 79.0° "
————
Rise 12.0° "
+ 1/10th 1.2° "
————
Gives 13.2° "
One pound of the coal will evaporate 13.2 pounds of water.
SHALES, ETC.
The assay of these is carried out in the same way as that of coals, but the volatile
matters are separately examined, and, in consequence, a larger quantity of material
must be used. For the moisture, volatile matter, fixed carbon and ash, the
determinations are the same, but a special distillation must be made to obtain a
sufficient quantity of the volatile products for subsequent examination. Take 500 or
1000 grams of the well-sampled and powdered shale, and introduce into a cast-iron
retort as shown in fig. 74. Lute the joint with fire-clay, place the cover on, and bolt
it down. The bolts should have a covering of fire-clay to protect them from the
action of the fire. Place the retort in a wind furnace, supporting it on a brick, and
pack well around with coke. Build up the furnace around and over the retort with
loose fire-bricks, and heat gradually.
Page 519
As soon as water begins to drip, the tube of the retort is cooled by wrapping a wet
cloth around it, and keeping wet with water. The water is kept from running into
the receiver by a ring of damp fire-clay. A quantity of gas first comes over and will
be lost, afterwards water and oily matters. The retort must be red hot at the close of
the distillation, and when nothing more distils off, which occurs in about two or
three hours, the wet cloth is removed, and the tube heated with a Bunsen burner to
drive forward the matter condensed in it into the receiver, and thus to clean the
tube. It can be seen when the tube is clean by looking up through it into the red-hot
retort. The receiver is then removed, and the retort, taken from the furnace, is
allowed to cool. When cold it is opened, and the fixed carbon and ash weighed, as
a check on the smaller assay.
The distillate of water and oil is warmed, and will separate into two layers, the
upper one of which is oil, and the lower water. These are measured, and if the
specific gravity of the oil is taken, its weight may be calculated. If the two liquids
do not separate well, the water may be filtered off, after cooling, through a damped
filter. The separation is, however, best effected in a separator (fig. 75). The liquids
are poured into this, allowed to settle, and the lower layer drained off. The volume
of the water is measured and its weight calculated in per cents. on the amount of
shale taken.
cloth around it, and keeping wet with water. The water is kept from running into
the receiver by a ring of damp fire-clay. A quantity of gas first comes over and will
be lost, afterwards water and oily matters. The retort must be red hot at the close of
the distillation, and when nothing more distils off, which occurs in about two or
three hours, the wet cloth is removed, and the tube heated with a Bunsen burner to
drive forward the matter condensed in it into the receiver, and thus to clean the
tube. It can be seen when the tube is clean by looking up through it into the red-hot
retort. The receiver is then removed, and the retort, taken from the furnace, is
allowed to cool. When cold it is opened, and the fixed carbon and ash weighed, as
a check on the smaller assay.
The distillate of water and oil is warmed, and will separate into two layers, the
upper one of which is oil, and the lower water. These are measured, and if the
specific gravity of the oil is taken, its weight may be calculated. If the two liquids
do not separate well, the water may be filtered off, after cooling, through a damped
filter. The separation is, however, best effected in a separator (fig. 75). The liquids
are poured into this, allowed to settle, and the lower layer drained off. The volume
of the water is measured and its weight calculated in per cents. on the amount of
shale taken.
Page 520
Examination of the Oil.—A sufficient quantity of the oil must be got, so that if
one distillation does not yield enough, the requisite quantity must be obtained by
making two or more distillations. The oils are mixed, and the mixture, after having
had its volume and specific gravity ascertained, is placed in a copper retort, and re-
distilled with the aid of a current of steam. The residue in the retort is coke.
The distillate is separated from the water by means of the separator, and shaken for
ten minutes with one-twentieth of its bulk of sulphuric acid (sp. g. 1.70). The
temperature should not be allowed to rise above 40°. Allow to stand, and run off
the "acid tar."
The oil is now shaken up with from 10 c.c. to 20 c.c. of sodic hydrate solution (sp.
g. 1.3), allowed to stand, warmed for half-an-hour, and the "soda-tar" run off.
On mixing this soda-tar with dilute acid, the "crude shale oil creosote" separates,
and is measured off.
The purified oil is next re-distilled in fractions, which come over in the following
order:—"Naphtha," "light oil," "heavy oil," and "still bottoms." For the first
product, which is only got from certain shales, the receiver is changed when the
distillate has a specific gravity of 0.78. For the second product the process is
continued till a drop of the distillate, caught as it falls from the neck of the retort on
a cold spatula, shows signs of solidifying. This is "crude light oil."
one distillation does not yield enough, the requisite quantity must be obtained by
making two or more distillations. The oils are mixed, and the mixture, after having
had its volume and specific gravity ascertained, is placed in a copper retort, and re-
distilled with the aid of a current of steam. The residue in the retort is coke.
The distillate is separated from the water by means of the separator, and shaken for
ten minutes with one-twentieth of its bulk of sulphuric acid (sp. g. 1.70). The
temperature should not be allowed to rise above 40°. Allow to stand, and run off
the "acid tar."
The oil is now shaken up with from 10 c.c. to 20 c.c. of sodic hydrate solution (sp.
g. 1.3), allowed to stand, warmed for half-an-hour, and the "soda-tar" run off.
On mixing this soda-tar with dilute acid, the "crude shale oil creosote" separates,
and is measured off.
The purified oil is next re-distilled in fractions, which come over in the following
order:—"Naphtha," "light oil," "heavy oil," and "still bottoms." For the first
product, which is only got from certain shales, the receiver is changed when the
distillate has a specific gravity of 0.78. For the second product the process is
continued till a drop of the distillate, caught as it falls from the neck of the retort on
a cold spatula, shows signs of solidifying. This is "crude light oil."
Page 521
The receiver is changed, and the "heavy oil" comes over; towards the end a thick
brown or yellow viscid product is got. The receiver is again changed, and the
distillation carried to dryness.
The "crude light oil" is washed cold with 2 per cent. of sulphuric acid
(concentrated), and afterwards with excess of soda. Thus purified it is again
distilled to dryness, three fractions being collected as before. Naphtha, which is
added to the main portion, and measured; "light oil," which is also measured; and
"heavy oil," which is added to that got in the first distillation. This last is poured
into a flat-bottom capsule, and allowed to cool slowly. The temperature may with
advantage be carried below freezing-point. The cooled cake is pressed between
folds of linen, and the paraffin scale detached and weighed.
The results may be reported thus:—
Naphtha, sp. g. ——
Light oil, sp. g. ——
Heavy oil, sp. g.——
Paraffin scale ——
Coke, &c. ——
The results are calculated in per cents. on the oil taken. Some workers take their
fractions at each rise of 50° C. The composition of average shale, as given by
Mills, is as follows:—Specific gravity, 1.877; moisture, 2.54.
Gas }
Volatile matter, water, ammonia } 23.53
Oil }
Fixed carbon 12.69
Ash 63.74
_____
99.96
The ash is made up of silica, 55.6; ferric oxide, 12.2; alumina, 22.14; lime, 1.5;
sulphur, 0.9; soluble salts (containing 0.92 per cent. sulphuric oxide), 8.3.
Total sulphur in shale 1.8per cent.
" " in ash 1.3 "
For further information on these assays, and for the assay of petroleums, bitumens,
&c., the student is referred to Allen's "Commercial Organic Analysis," Vol. II.
brown or yellow viscid product is got. The receiver is again changed, and the
distillation carried to dryness.
The "crude light oil" is washed cold with 2 per cent. of sulphuric acid
(concentrated), and afterwards with excess of soda. Thus purified it is again
distilled to dryness, three fractions being collected as before. Naphtha, which is
added to the main portion, and measured; "light oil," which is also measured; and
"heavy oil," which is added to that got in the first distillation. This last is poured
into a flat-bottom capsule, and allowed to cool slowly. The temperature may with
advantage be carried below freezing-point. The cooled cake is pressed between
folds of linen, and the paraffin scale detached and weighed.
The results may be reported thus:—
Naphtha, sp. g. ——
Light oil, sp. g. ——
Heavy oil, sp. g.——
Paraffin scale ——
Coke, &c. ——
The results are calculated in per cents. on the oil taken. Some workers take their
fractions at each rise of 50° C. The composition of average shale, as given by
Mills, is as follows:—Specific gravity, 1.877; moisture, 2.54.
Gas }
Volatile matter, water, ammonia } 23.53
Oil }
Fixed carbon 12.69
Ash 63.74
_____
99.96
The ash is made up of silica, 55.6; ferric oxide, 12.2; alumina, 22.14; lime, 1.5;
sulphur, 0.9; soluble salts (containing 0.92 per cent. sulphuric oxide), 8.3.
Total sulphur in shale 1.8per cent.
" " in ash 1.3 "
For further information on these assays, and for the assay of petroleums, bitumens,
&c., the student is referred to Allen's "Commercial Organic Analysis," Vol. II.
Page 522
Determination of Organic Carbon in a Limestone.—Take 1 or 2 grams and
dissolve with a very slight excess of dilute hydrochloric acid, evaporate to dryness,
and determine the carbon in the residue by combustion with copper oxide.
Estimation of Carbon in a Sample of Graphite (Black-lead).—Weigh up 1 or 2
grams in a dish and calcine in the muffle till the carbon is burnt off. Weigh the
residue, and calculate the carbon by difference.
Determination of Carbon in Iron.—The carbon exists in two states—free
(graphite) and combined. The following process estimates the total carbon:—The
carbon existing as graphite may be separately estimated in another portion by the
dissolve with a very slight excess of dilute hydrochloric acid, evaporate to dryness,
and determine the carbon in the residue by combustion with copper oxide.
Estimation of Carbon in a Sample of Graphite (Black-lead).—Weigh up 1 or 2
grams in a dish and calcine in the muffle till the carbon is burnt off. Weigh the
residue, and calculate the carbon by difference.
Determination of Carbon in Iron.—The carbon exists in two states—free
(graphite) and combined. The following process estimates the total carbon:—The
carbon existing as graphite may be separately estimated in another portion by the
Page 523
same process, but using hydrochloric acid to dissolve the iron instead of the copper
solution:—Weigh up 2 grams of the iron (or a larger quantity if very poor in
carbon), and attack it with 30 grams of ammonic-cupric chloride[119] dissolved in
100 c.c. of water. Let the reaction proceed for a quarter-of-an-hour, and then warm
until the copper is dissolved. Allow to settle, and filter through a filtering-tube.
This is a piece of combustion tube drawn out and narrowed at one end, as shown in
fig. 76. The narrow part is blocked with a pea of baked clay, and on this is placed
half-an-inch of silica sand (previously calcined to remove organic matter), then a
small plug of asbestos, and then a quarter-of-an-inch of sand. The tube is connected
with a pump working at a gentle pressure, and the solution is filtered through the
tube with the aid of a small funnel (fig. 77). The residue is washed, first with dilute
hydrochloric acid, and then with distilled water. The tube is dried by aspirating air
through it, and gently warming with a Bunsen burner. The tube is then placed in a
small combustion-furnace, and connected with calcium chloride and potash bulbs,
as shown in fig. 78. The potash bulb to the right of the figure must be weighed. A
slow stream of air is drawn through the apparatus, and the heat gradually raised; in
from thirty minutes to one hour the combustion will be complete. The potash bulbs
are then disconnected and weighed, and the increase multiplied by 0.2727 gives the
weight of carbon.
CARBONATES.
Carbon dioxide, which is formed by the complete oxidation of carbon, is a gas with
a sweetish odour and taste, having a strong affinity for alkalies, and forming a
series of compounds termed carbonates. The gas itself occurs in nature, and is
sometimes met with in quantity in mining. The carbonates occur largely in nature,
forming mountain masses of limestone, &c. Carbonates of many of the metals,
such as carbonate of lead (cerussite), carbonate of iron (chalybite), carbonates of
copper (malachite and chessylite), and carbonate of magnesia (magnesite), are
common.
All the carbonates (those of the alkalies and alkaline earths excepted) are
completely decomposed on ignition into the oxide of the metal and carbon dioxide;
but the temperature required for this decomposition varies with the nature of the
base. All carbonates are soluble with effervescence in dilute acids; some, such as
chalybite and magnesite, require the aid of heat. The alkaline carbonates are
soluble in water; the rest, with the exception of the bicarbonates, are insoluble
therein.
Carbonates are recognised by their effervescence with acids—a stream of bubbles
of gas are given off which collect in the tube, and possess the property of
solution:—Weigh up 2 grams of the iron (or a larger quantity if very poor in
carbon), and attack it with 30 grams of ammonic-cupric chloride[119] dissolved in
100 c.c. of water. Let the reaction proceed for a quarter-of-an-hour, and then warm
until the copper is dissolved. Allow to settle, and filter through a filtering-tube.
This is a piece of combustion tube drawn out and narrowed at one end, as shown in
fig. 76. The narrow part is blocked with a pea of baked clay, and on this is placed
half-an-inch of silica sand (previously calcined to remove organic matter), then a
small plug of asbestos, and then a quarter-of-an-inch of sand. The tube is connected
with a pump working at a gentle pressure, and the solution is filtered through the
tube with the aid of a small funnel (fig. 77). The residue is washed, first with dilute
hydrochloric acid, and then with distilled water. The tube is dried by aspirating air
through it, and gently warming with a Bunsen burner. The tube is then placed in a
small combustion-furnace, and connected with calcium chloride and potash bulbs,
as shown in fig. 78. The potash bulb to the right of the figure must be weighed. A
slow stream of air is drawn through the apparatus, and the heat gradually raised; in
from thirty minutes to one hour the combustion will be complete. The potash bulbs
are then disconnected and weighed, and the increase multiplied by 0.2727 gives the
weight of carbon.
CARBONATES.
Carbon dioxide, which is formed by the complete oxidation of carbon, is a gas with
a sweetish odour and taste, having a strong affinity for alkalies, and forming a
series of compounds termed carbonates. The gas itself occurs in nature, and is
sometimes met with in quantity in mining. The carbonates occur largely in nature,
forming mountain masses of limestone, &c. Carbonates of many of the metals,
such as carbonate of lead (cerussite), carbonate of iron (chalybite), carbonates of
copper (malachite and chessylite), and carbonate of magnesia (magnesite), are
common.
All the carbonates (those of the alkalies and alkaline earths excepted) are
completely decomposed on ignition into the oxide of the metal and carbon dioxide;
but the temperature required for this decomposition varies with the nature of the
base. All carbonates are soluble with effervescence in dilute acids; some, such as
chalybite and magnesite, require the aid of heat. The alkaline carbonates are
soluble in water; the rest, with the exception of the bicarbonates, are insoluble
therein.
Carbonates are recognised by their effervescence with acids—a stream of bubbles
of gas are given off which collect in the tube, and possess the property of
Page 524
extinguishing a lighted match. The most characteristic test for the gas is a white
precipitate, which is produced by passing it into lime or baryta-water, or into a
solution of subacetate of lead.
The expulsion of carbon dioxide by the stronger acids serves for the separation of
this body from the other acids and bases.
Dry Assay.—There is no dry assay in use. Any method which may be adopted will
necessarily be applicable only to special compounds.
WET METHODS.
There are several methods in use which leave little to be desired either in speed or
accuracy. We will give (1) a gravimetric method in which the estimation may be
made directly by weighing the carbonic acid, or, indirectly, by estimating the
carbon dioxide from the loss; (2) a volumetric one, by which an indirect
determination is made of the gas; and (3) a gasometric method, in which the
volume of carbon dioxide given off is measured, and its weight deducted.
precipitate, which is produced by passing it into lime or baryta-water, or into a
solution of subacetate of lead.
The expulsion of carbon dioxide by the stronger acids serves for the separation of
this body from the other acids and bases.
Dry Assay.—There is no dry assay in use. Any method which may be adopted will
necessarily be applicable only to special compounds.
WET METHODS.
There are several methods in use which leave little to be desired either in speed or
accuracy. We will give (1) a gravimetric method in which the estimation may be
made directly by weighing the carbonic acid, or, indirectly, by estimating the
carbon dioxide from the loss; (2) a volumetric one, by which an indirect
determination is made of the gas; and (3) a gasometric method, in which the
volume of carbon dioxide given off is measured, and its weight deducted.
Page 525
Direct Gravimetric Method.—Fit up the apparatus shown in the diagram (fig.
79). The various tubes are supported by a fixed rod with nails and wire loops, and
connected by short lengths of rubber-tubing. The first tube contains soda-lime. The
small flask is fitted with a rubber-stopper perforated with two holes, through one of
which passes the tube of a pipette holding 25 or 30 c.c. This pipette is to contain
the acid. The substance to be determined is weighed out into the flask. The second
tube contains strong sulphuric acid; the third, pumice stone, saturated with copper
sulphate solution, and dried until nearly white (at 200° C.); the fourth contains
recently fused calcium chloride; and the fifth, which is the weighed tube in which
the carbonic acid is absorbed, contains calcium chloride and soda-lime,[120] as
shown in fig. 80. The sixth also contains calcium chloride and soda-lime; its object
is to prevent the access of moisture and carbonic acid to the weighed tube from this
direction; it is connected with an aspirator.
Having weighed the U-tube and got the apparatus in order, weigh up 1, 2, or 5
grams of the substance and place in the flask. Fill the pipette with dilute acid, close
the clamp, and cork the flask. Then see that the apparatus is tight. Open the clamp
and allow from 10 to 20 c.c. of the acid to run on to the assay. Carbonic acid will
be evolved and will be driven through the tubes. The gas should bubble through the
sulphuric acid in a moderate and regular stream. When the effervescence slackens
the clamp is opened and the greater part of the remaining acid run in. When the
effervescence has ceased the clamp is opened to its full extent and a current of air
drawn through with an aspirator. A gentle heat is applied to the flask; but it should
not be prolonged or carried to boiling. After the removal of the heat a gentle
current of air is drawn through the apparatus for 30 or 40 minutes. The weighed U-
tube, which in the early part of the operation will have become warm if much
carbonic acid was present, will by this time be cold. It is disconnected, plugged,
and weighed. The increase in weight is due to the carbon dioxide of the sample.
Example.—Ore taken 1 gram.
Weight of tube, before 42.6525 grams
" " after 43.0940 "
———-
Increase equals CO2 0.4415 "
79). The various tubes are supported by a fixed rod with nails and wire loops, and
connected by short lengths of rubber-tubing. The first tube contains soda-lime. The
small flask is fitted with a rubber-stopper perforated with two holes, through one of
which passes the tube of a pipette holding 25 or 30 c.c. This pipette is to contain
the acid. The substance to be determined is weighed out into the flask. The second
tube contains strong sulphuric acid; the third, pumice stone, saturated with copper
sulphate solution, and dried until nearly white (at 200° C.); the fourth contains
recently fused calcium chloride; and the fifth, which is the weighed tube in which
the carbonic acid is absorbed, contains calcium chloride and soda-lime,[120] as
shown in fig. 80. The sixth also contains calcium chloride and soda-lime; its object
is to prevent the access of moisture and carbonic acid to the weighed tube from this
direction; it is connected with an aspirator.
Having weighed the U-tube and got the apparatus in order, weigh up 1, 2, or 5
grams of the substance and place in the flask. Fill the pipette with dilute acid, close
the clamp, and cork the flask. Then see that the apparatus is tight. Open the clamp
and allow from 10 to 20 c.c. of the acid to run on to the assay. Carbonic acid will
be evolved and will be driven through the tubes. The gas should bubble through the
sulphuric acid in a moderate and regular stream. When the effervescence slackens
the clamp is opened and the greater part of the remaining acid run in. When the
effervescence has ceased the clamp is opened to its full extent and a current of air
drawn through with an aspirator. A gentle heat is applied to the flask; but it should
not be prolonged or carried to boiling. After the removal of the heat a gentle
current of air is drawn through the apparatus for 30 or 40 minutes. The weighed U-
tube, which in the early part of the operation will have become warm if much
carbonic acid was present, will by this time be cold. It is disconnected, plugged,
and weighed. The increase in weight is due to the carbon dioxide of the sample.
Example.—Ore taken 1 gram.
Weight of tube, before 42.6525 grams
" " after 43.0940 "
———-
Increase equals CO2 0.4415 "
Page 526
Indirect Gravimetric, or Determination by Loss.—Take a Geissler's carbonic-
acid apparatus (fig. 81) and place in the double bulb some strong sulphuric acid.
Put into the other bulb, the stopcock being closed, 3 or 4 c.c. of nitric acid diluted
with water. Leave the apparatus in the balance-box for a few minutes and weigh.
Introduce into the flask (through A) about 1 gram of the powdered substance and
again weigh to find the exact amount added. Allow the acid to run gradually on to
the carbonate, and when solution is complete, heat and aspirate. Cool and again
weigh; the loss in weight is the carbonic acid.
For Example:—
Weightof apparatus and acids 85.494 grams
" " marble 86.879 "
———
Equal to marble taken 1.385 "
Weightof apparatus and marble 86.879 grams
" " minus carbonic acid 86.2692 "
———
Equal to carbonic acid 0.6098 "
acid apparatus (fig. 81) and place in the double bulb some strong sulphuric acid.
Put into the other bulb, the stopcock being closed, 3 or 4 c.c. of nitric acid diluted
with water. Leave the apparatus in the balance-box for a few minutes and weigh.
Introduce into the flask (through A) about 1 gram of the powdered substance and
again weigh to find the exact amount added. Allow the acid to run gradually on to
the carbonate, and when solution is complete, heat and aspirate. Cool and again
weigh; the loss in weight is the carbonic acid.
For Example:—
Weightof apparatus and acids 85.494 grams
" " marble 86.879 "
———
Equal to marble taken 1.385 "
Weightof apparatus and marble 86.879 grams
" " minus carbonic acid 86.2692 "
———
Equal to carbonic acid 0.6098 "
Page 527
1.385 : 100 :: 0.6098 : x
x = 44.03 per cent.
The substance contains 44.03 per cent. of carbonic acid; a duplicate experiment
gave 43.73 per cent.
This method is quicker, but less exact, than the direct gravimetric determination.
VOLUMETRIC METHOD.
This, which is of somewhat limited application, is based upon the determination of
the quantity of acid required to decompose the carbonate. It consists in adding to a
weighed quantity of the mineral a known amount of standard solution of acid
which is in excess of that required to effect the decomposition. The quantity of
residual acid is then determined by titrating with standard solution of alkali. This
method has been described under Lime.
GASOMETRIC METHOD.
This method is the quickest of all, and the least troublesome after the apparatus has
been once prepared. It yields fairly accurate results when worked in the manner
described below; but if greater precautions are taken the results are exact. It
depends on the measurement of the volume of gas given off on treating the
weighed sample with acid. The apparatus described, page 52, is used. Weigh out a
portion of the mineral which shall contain not more than 0.15 gram of carbonic
acid (or 0.4 gram of carbonate of lime) and put it in the bottle. Put in the inner tube
10 c.c. of dilute hydrochloric acid (1—1), cork tightly, and read off the level of the
liquid in the burette after adjusting the pressure. Turn the acid over on to the
mineral. Run out the water so as to keep the level in the two burettes the same.
When effervescence has ceased, rotate the contents of the bottle; finally, adjust the
level in the burettes and read off the volume. The increase in volume is due to the
evolved carbon dioxide. At the same time read off the "volume corrector."
Some of the carbon dioxide remains dissolved in the acid in the generating bottle,
and the quantity thus dissolved will depend on the amount of carbonate as well as
on the amount of acid present. Consequently, a measured quantity of acid should
be used in each assay and a comparative experiment made with a known weight of
pure carbonate of lime which will yield about the same volume of gas. The number
of c.c. of gas got in the assay multiplied by 4.7 will give the number of milligrams
of pure carbonate of lime that must be taken for the standard. With ordinary work
the error rarely exceeds half a c.c.
x = 44.03 per cent.
The substance contains 44.03 per cent. of carbonic acid; a duplicate experiment
gave 43.73 per cent.
This method is quicker, but less exact, than the direct gravimetric determination.
VOLUMETRIC METHOD.
This, which is of somewhat limited application, is based upon the determination of
the quantity of acid required to decompose the carbonate. It consists in adding to a
weighed quantity of the mineral a known amount of standard solution of acid
which is in excess of that required to effect the decomposition. The quantity of
residual acid is then determined by titrating with standard solution of alkali. This
method has been described under Lime.
GASOMETRIC METHOD.
This method is the quickest of all, and the least troublesome after the apparatus has
been once prepared. It yields fairly accurate results when worked in the manner
described below; but if greater precautions are taken the results are exact. It
depends on the measurement of the volume of gas given off on treating the
weighed sample with acid. The apparatus described, page 52, is used. Weigh out a
portion of the mineral which shall contain not more than 0.15 gram of carbonic
acid (or 0.4 gram of carbonate of lime) and put it in the bottle. Put in the inner tube
10 c.c. of dilute hydrochloric acid (1—1), cork tightly, and read off the level of the
liquid in the burette after adjusting the pressure. Turn the acid over on to the
mineral. Run out the water so as to keep the level in the two burettes the same.
When effervescence has ceased, rotate the contents of the bottle; finally, adjust the
level in the burettes and read off the volume. The increase in volume is due to the
evolved carbon dioxide. At the same time read off the "volume corrector."
Some of the carbon dioxide remains dissolved in the acid in the generating bottle,
and the quantity thus dissolved will depend on the amount of carbonate as well as
on the amount of acid present. Consequently, a measured quantity of acid should
be used in each assay and a comparative experiment made with a known weight of
pure carbonate of lime which will yield about the same volume of gas. The number
of c.c. of gas got in the assay multiplied by 4.7 will give the number of milligrams
of pure carbonate of lime that must be taken for the standard. With ordinary work
the error rarely exceeds half a c.c.
Page 528
The following example will illustrate the calculations:—
One gram of a mineral was taken, and yielded 49.0 c.c. of gas. The "volume
corrector" reading was 100.4 c.c.
0.2405 gram of pure carbonate of lime was then taken, and treated in the same
way; 50.5 c.c. of gas were got. The volume corrector still read 100.4 c.c.
0.2405 gram of carbonate of lime is equivalent to 0.1058 gram of carbon dioxide;
then,
50.5 : 49.0 :: 0.1058 : x
x = 10.26 per cent.
Estimation of Carbonic Acid in the Air of Mines.—According to a series of
analyses by Angus Smith, the proportion of carbonic acid in the air of underground
workings varied from 0.04 to 2.7 per cent. by volume. In places where men are
working the proportion ought not to reach 0.25 per cent.
A simple method of determining whether a sample of air reaches this limit (0.25
per cent.) is described by Dr. C. Le Neve Foster in the "Proceedings of the Mining
Association and Institute of Cornwall" for 1888. The apparatus used is an ordinary
corked 8-ounce medicine bottle. This is filled with the air to be examined by
sucking out its contents with a piece of rubber-tube. Half-an-ounce of dilute lime-
water[121] (tinted with phenolphthalein) is poured in. If, on corking the bottle and
shaking, the colour is not discharged, the air contains less than 0.25 per cent. of
carbon dioxide. "If the colour fades slowly, and does not finally vanish till after a
great deal of shaking, it may be assumed that the percentage of carbon dioxide
does not greatly exceed one quarter; whereas, if the disappearance is rapid after a
very few shakes, the contrary, of course, is the case." The dilute lime-water is
measured out and carried in ordinary half-ounce phials. This method does not
pretend to great accuracy, but as a method of distinguishing between good and bad
air it is very convenient, and will be found useful.
For determining the actual proportion in the air the following plan is adopted:—
Take a bottle which will hold about 50 ounces, and measure its capacity; fill the
bottle with the air to be examined, pour in 100 c.c. of lime-water, and shake up for
some time; add phenolphthalein, and titrate the remaining calcium hydrate with
standard solution of oxalic acid.
The solution of oxalic acid is made by dissolving 2.25 grams of re-crystallised
oxalic acid (H2C2O4.2H2O) in water and diluting to 1 litre. One c.c. = 0.001 gram
of lime (CaO), or 0.0007857 gram of carbon dioxide.
One gram of a mineral was taken, and yielded 49.0 c.c. of gas. The "volume
corrector" reading was 100.4 c.c.
0.2405 gram of pure carbonate of lime was then taken, and treated in the same
way; 50.5 c.c. of gas were got. The volume corrector still read 100.4 c.c.
0.2405 gram of carbonate of lime is equivalent to 0.1058 gram of carbon dioxide;
then,
50.5 : 49.0 :: 0.1058 : x
x = 10.26 per cent.
Estimation of Carbonic Acid in the Air of Mines.—According to a series of
analyses by Angus Smith, the proportion of carbonic acid in the air of underground
workings varied from 0.04 to 2.7 per cent. by volume. In places where men are
working the proportion ought not to reach 0.25 per cent.
A simple method of determining whether a sample of air reaches this limit (0.25
per cent.) is described by Dr. C. Le Neve Foster in the "Proceedings of the Mining
Association and Institute of Cornwall" for 1888. The apparatus used is an ordinary
corked 8-ounce medicine bottle. This is filled with the air to be examined by
sucking out its contents with a piece of rubber-tube. Half-an-ounce of dilute lime-
water[121] (tinted with phenolphthalein) is poured in. If, on corking the bottle and
shaking, the colour is not discharged, the air contains less than 0.25 per cent. of
carbon dioxide. "If the colour fades slowly, and does not finally vanish till after a
great deal of shaking, it may be assumed that the percentage of carbon dioxide
does not greatly exceed one quarter; whereas, if the disappearance is rapid after a
very few shakes, the contrary, of course, is the case." The dilute lime-water is
measured out and carried in ordinary half-ounce phials. This method does not
pretend to great accuracy, but as a method of distinguishing between good and bad
air it is very convenient, and will be found useful.
For determining the actual proportion in the air the following plan is adopted:—
Take a bottle which will hold about 50 ounces, and measure its capacity; fill the
bottle with the air to be examined, pour in 100 c.c. of lime-water, and shake up for
some time; add phenolphthalein, and titrate the remaining calcium hydrate with
standard solution of oxalic acid.
The solution of oxalic acid is made by dissolving 2.25 grams of re-crystallised
oxalic acid (H2C2O4.2H2O) in water and diluting to 1 litre. One c.c. = 0.001 gram
of lime (CaO), or 0.0007857 gram of carbon dioxide.
Page 529
Take 100 c.c. of the same lime-water, to which add the same amount of
phenolphthalein as before. Titrate. The difference between the two readings gives
the amount of "acid" equivalent to the lime-water neutralised by the carbon
dioxide. The number of c.c. thus used up, when multiplied by 0.3989, gives the
number of c.c. of carbon dioxide (at 0° C. and 760 mm.) in the volume of air taken.
This volume, which is that of the bottle less 100 c.c., must in accurate work be
reduced to the normal temperature and pressure.[122] The percentage by volume can
then be calculated.
PRACTICAL EXERCISES.
1. In a gasometric determination 71.3 c.c. of gas were obtained from 0.2055 gram
of mineral. The "volume corrector" reading was 102.2 c.c. 0.3445 gram of pure
carbonate of lime gave 74.1 c.c. The "volume corrector" reading was 100.6. What
is the percentage of carbon dioxide in the substance?
2. What volume of dry gas at 0° C. and 760 m.m. pressure should be obtained from
0.3445 gram of carbonate of lime? 1 c.c. of CO2 under these conditions weighs
1.97 milligrams.
3. A sample of coal is reported on as follows:—
Specific gravity 1.315
Moisture 1.001
Volatile matter 35.484
Fixed carbon 50.172
Ash 12.028
———
100.000
What is there about this requiring explanation?
4. Calculate the percentage of carbonic acid in a mineral from the following data:
—
Weightof apparatus and acids 87.0888grams
" " " plus mineral 88.8858"
" " " after loss of carbonic acid 88.1000"
5. A sample of pig iron contains 1.43 per cent. of "combined" and 2.02 per cent. of
"free" carbon. Taking 2 grams of it for each determination, what weight of CO2
phenolphthalein as before. Titrate. The difference between the two readings gives
the amount of "acid" equivalent to the lime-water neutralised by the carbon
dioxide. The number of c.c. thus used up, when multiplied by 0.3989, gives the
number of c.c. of carbon dioxide (at 0° C. and 760 mm.) in the volume of air taken.
This volume, which is that of the bottle less 100 c.c., must in accurate work be
reduced to the normal temperature and pressure.[122] The percentage by volume can
then be calculated.
PRACTICAL EXERCISES.
1. In a gasometric determination 71.3 c.c. of gas were obtained from 0.2055 gram
of mineral. The "volume corrector" reading was 102.2 c.c. 0.3445 gram of pure
carbonate of lime gave 74.1 c.c. The "volume corrector" reading was 100.6. What
is the percentage of carbon dioxide in the substance?
2. What volume of dry gas at 0° C. and 760 m.m. pressure should be obtained from
0.3445 gram of carbonate of lime? 1 c.c. of CO2 under these conditions weighs
1.97 milligrams.
3. A sample of coal is reported on as follows:—
Specific gravity 1.315
Moisture 1.001
Volatile matter 35.484
Fixed carbon 50.172
Ash 12.028
———
100.000
What is there about this requiring explanation?
4. Calculate the percentage of carbonic acid in a mineral from the following data:
—
Weightof apparatus and acids 87.0888grams
" " " plus mineral 88.8858"
" " " after loss of carbonic acid 88.1000"
5. A sample of pig iron contains 1.43 per cent. of "combined" and 2.02 per cent. of
"free" carbon. Taking 2 grams of it for each determination, what weight of CO2
Page 530
will be got on burning the residue from solution in ammonium cupric chloride, and
what from the residue after solution in hydrochloric acid?
BORON AND BORATES.
Boron occurs in nature as boric acid or sassoline (H3BO3); borax or tincal
(Na2B4O7.10H2O); ulexite or boronatrocalcite (2CaB4O7.Na2B4O7); borocalcite
(CaB4O7.4H2O); boracite, 2Mg3B8O15.MgCl2, and some other minerals. Boric acid
is also a constituent of certain silicates, such as tourmaline, axinite, and datholite.
The natural borates are used in the preparation of borax, which is largely employed
as a preservative agent, for fluxing, and for other purposes.
There is only one series of boron compounds which have any importance. These
are the borates in which the trioxide (B2O3) acts the part of a weak acid. The
addition of any acid liberates boric acid, which separates out in cold solutions as a
crystalline precipitate. Boric acid is soluble in alcohol and in hot water. On
evaporating these solutions it is volatilised, although the anhydrous oxide is "fixed"
at a red heat. The borates are mostly fusible compounds, and are soluble in acids
and in solutions of ammonic salts.
Detection.—Boron in small quantities will escape detection unless specially
looked for, but there is no difficulty in detecting its presence. Heated in the
Bunsen-burner flame with "Turner's test," it gives an evanescent yellowish-green
colour, due to fluoride of boron (BF3). "Turner's test" is a mixture of 5 parts of
bisulphate of potash and 1 part of fluor spar. Boric acid itself imparts a
characteristic green colour to the flame, which gives a spectrum made up of four
well-marked and equidistant lines, three in the green and one in the blue. Solutions
of boric acid give with "turmeric paper," which has been dipped into it and dried, a
characteristic red tint. This is a very delicate test, but in trying it a blank
experiment should be carried out alongside with a solution made up of the same re-
agents which have been used in liberating the boric acid in the sample.
Solution and Separation.—The solution presents no difficulty, but the separation
is troublesome. The best method is that of Gooch; who, if necessary, first fuses
with carbonate of soda, and after the removal of chlorides and fluorides (by nitrate
of silver or a lime salt), evaporates the aqueous extract with nitric or acetic acid to
dryness in a retort and, subsequently, with repeated doses of 10 c.c. each of methyl
alcohol. The distillate contains the boron as boric acid. Half a gram of the trioxide
(B2O3) is completely carried over by two evaporations, each with 10 c.c. of the
what from the residue after solution in hydrochloric acid?
BORON AND BORATES.
Boron occurs in nature as boric acid or sassoline (H3BO3); borax or tincal
(Na2B4O7.10H2O); ulexite or boronatrocalcite (2CaB4O7.Na2B4O7); borocalcite
(CaB4O7.4H2O); boracite, 2Mg3B8O15.MgCl2, and some other minerals. Boric acid
is also a constituent of certain silicates, such as tourmaline, axinite, and datholite.
The natural borates are used in the preparation of borax, which is largely employed
as a preservative agent, for fluxing, and for other purposes.
There is only one series of boron compounds which have any importance. These
are the borates in which the trioxide (B2O3) acts the part of a weak acid. The
addition of any acid liberates boric acid, which separates out in cold solutions as a
crystalline precipitate. Boric acid is soluble in alcohol and in hot water. On
evaporating these solutions it is volatilised, although the anhydrous oxide is "fixed"
at a red heat. The borates are mostly fusible compounds, and are soluble in acids
and in solutions of ammonic salts.
Detection.—Boron in small quantities will escape detection unless specially
looked for, but there is no difficulty in detecting its presence. Heated in the
Bunsen-burner flame with "Turner's test," it gives an evanescent yellowish-green
colour, due to fluoride of boron (BF3). "Turner's test" is a mixture of 5 parts of
bisulphate of potash and 1 part of fluor spar. Boric acid itself imparts a
characteristic green colour to the flame, which gives a spectrum made up of four
well-marked and equidistant lines, three in the green and one in the blue. Solutions
of boric acid give with "turmeric paper," which has been dipped into it and dried, a
characteristic red tint. This is a very delicate test, but in trying it a blank
experiment should be carried out alongside with a solution made up of the same re-
agents which have been used in liberating the boric acid in the sample.
Solution and Separation.—The solution presents no difficulty, but the separation
is troublesome. The best method is that of Gooch; who, if necessary, first fuses
with carbonate of soda, and after the removal of chlorides and fluorides (by nitrate
of silver or a lime salt), evaporates the aqueous extract with nitric or acetic acid to
dryness in a retort and, subsequently, with repeated doses of 10 c.c. each of methyl
alcohol. The distillate contains the boron as boric acid. Half a gram of the trioxide
(B2O3) is completely carried over by two evaporations, each with 10 c.c. of the
Page 531
alcohol; but if water or foreign salts are present, more than this is required. In
ordinary cases six such evaporations are sufficient for 0.2 gram of the oxide.[123]
GRAVIMETRIC DETERMINATION.
Before the introduction of Gooch's process it was usual to determine the boron
trioxide "by difference." If the alcoholic distillate containing the boric acid is
digested with about 1 gram (a known weight) of lime for ten or fifteen minutes, the
alcohol can be evaporated off without danger of loss. Either calcium nitrate or
acetate (which will be formed at the same time) yields lime upon subsequent
ignition. Consequently, the increase in weight, after ignition, upon that of the lime
taken gives the amount of boron trioxide present. The trioxide contains 31.4 per
cent. of boron (B). Since magnesia does not form a soluble hydrate it cannot
satisfactorily be used instead of lime.
The apparatus required is shown in fig. 82. It consists of a small retort or
evaporating vessel made out of a pipette of 200 c.c. capacity. This is heated by
means of a paraffin-bath at 130° or 140° C. It is connected with an upright
condenser, at the lower end of which is a small flask which serves as a receiver.
The quantity of the borate taken should contain not more than 0.2 gram of the
trioxide. Insoluble compounds are "dissolved in nitric acid at once, or, if necessary,
first fused with sodium carbonate." With soluble and alkaline borates sufficient
ordinary cases six such evaporations are sufficient for 0.2 gram of the oxide.[123]
GRAVIMETRIC DETERMINATION.
Before the introduction of Gooch's process it was usual to determine the boron
trioxide "by difference." If the alcoholic distillate containing the boric acid is
digested with about 1 gram (a known weight) of lime for ten or fifteen minutes, the
alcohol can be evaporated off without danger of loss. Either calcium nitrate or
acetate (which will be formed at the same time) yields lime upon subsequent
ignition. Consequently, the increase in weight, after ignition, upon that of the lime
taken gives the amount of boron trioxide present. The trioxide contains 31.4 per
cent. of boron (B). Since magnesia does not form a soluble hydrate it cannot
satisfactorily be used instead of lime.
The apparatus required is shown in fig. 82. It consists of a small retort or
evaporating vessel made out of a pipette of 200 c.c. capacity. This is heated by
means of a paraffin-bath at 130° or 140° C. It is connected with an upright
condenser, at the lower end of which is a small flask which serves as a receiver.
The quantity of the borate taken should contain not more than 0.2 gram of the
trioxide. Insoluble compounds are "dissolved in nitric acid at once, or, if necessary,
first fused with sodium carbonate." With soluble and alkaline borates sufficient
Page 532
nitric acid is added to render it faintly acid. The solution is then introduced into the
retort.
"The lime, to retain the boric acid in the distillate, is ignited in the crucible in
which the evaporation of the distillate is to be made subsequently." It is then cooled
in the desiccator for ten minutes, and weighed. The lime is transferred to the
receiving flask and slaked with a little water. The retort is lowered into the bath so
that "only the rear dips below the surface." The evaporation is carried to dryness,
the retort being lowered further into the bath as the evaporation proceeds. Ten c.c.
of methyl alcohol are introduced upon the residue, and the evaporation again
started. Six such portions of alcohol are thus distilled and 2 c.c. of water are
introduced and evaporated between the second and third, as also between the
fourth and fifth distillations. If acetic acid is used instead of nitric in the first
instance this addition of water is unnecessary.
The distillate is evaporated in the crucible ignited over the blowpipe, cooled in the
desiccator for ten minutes and weighed. The increase in weight gives the boron
trioxide. The results tend to be from 1 to 2 milligrams too high.
VOLUMETRIC METHOD.
This method is applicable to the indirect determination of boric acid in borax and
similar compounds. It is based on the measurement of the quantity of normal
solution of acid required to replace the boric acid, and, consequently, is rather a
measure of the soda present. The process is an alkalimetric one, and is carried out
as follows:—Weigh up 3 grams of the sample and dissolve in water. Tint with
methyl orange, and run in from an ordinary burette normal solution of sulphuric
acid until a pink tint is got. 100 c.c. of the normal solution of acid are equal to 7.0
grams of boron trioxide (B2O3), or 10.1 grams of anhydrous borax (Na2B4O7).
Examination of Borax.—In addition to the determination just given, the following
determinations are also required:—
Water.—Take about 2 grams and heat to tranquil fusion in a platinum crucible.
Count the loss in weight as water.
Sulphuric Oxide.—Take 2 grams, dissolve in water, acidify with hydrochloric
acid, filter, and precipitate with barium chloride. Wash the precipitate, ignite, and
weigh as barium sulphate (see Sulphur).
Chlorine.—Take 2 grams, dissolve in water, acidify with nitric acid, filter, and add
silver nitrate. Collect, wash, and weigh the precipitate as silver chloride.
retort.
"The lime, to retain the boric acid in the distillate, is ignited in the crucible in
which the evaporation of the distillate is to be made subsequently." It is then cooled
in the desiccator for ten minutes, and weighed. The lime is transferred to the
receiving flask and slaked with a little water. The retort is lowered into the bath so
that "only the rear dips below the surface." The evaporation is carried to dryness,
the retort being lowered further into the bath as the evaporation proceeds. Ten c.c.
of methyl alcohol are introduced upon the residue, and the evaporation again
started. Six such portions of alcohol are thus distilled and 2 c.c. of water are
introduced and evaporated between the second and third, as also between the
fourth and fifth distillations. If acetic acid is used instead of nitric in the first
instance this addition of water is unnecessary.
The distillate is evaporated in the crucible ignited over the blowpipe, cooled in the
desiccator for ten minutes and weighed. The increase in weight gives the boron
trioxide. The results tend to be from 1 to 2 milligrams too high.
VOLUMETRIC METHOD.
This method is applicable to the indirect determination of boric acid in borax and
similar compounds. It is based on the measurement of the quantity of normal
solution of acid required to replace the boric acid, and, consequently, is rather a
measure of the soda present. The process is an alkalimetric one, and is carried out
as follows:—Weigh up 3 grams of the sample and dissolve in water. Tint with
methyl orange, and run in from an ordinary burette normal solution of sulphuric
acid until a pink tint is got. 100 c.c. of the normal solution of acid are equal to 7.0
grams of boron trioxide (B2O3), or 10.1 grams of anhydrous borax (Na2B4O7).
Examination of Borax.—In addition to the determination just given, the following
determinations are also required:—
Water.—Take about 2 grams and heat to tranquil fusion in a platinum crucible.
Count the loss in weight as water.
Sulphuric Oxide.—Take 2 grams, dissolve in water, acidify with hydrochloric
acid, filter, and precipitate with barium chloride. Wash the precipitate, ignite, and
weigh as barium sulphate (see Sulphur).
Chlorine.—Take 2 grams, dissolve in water, acidify with nitric acid, filter, and add
silver nitrate. Collect, wash, and weigh the precipitate as silver chloride.
Page 533
Alumina.—Take 5 or 10 grams, dissolve in water, boil, add ammonia in slight
excess, and filter off the precipitate when it has settled. Wash with hot water,
ignite, and weigh as alumina (Al2O3).
FOOTNOTES:
[113] If the dishes show a manganese stain, wash them out with a few drops of
hydrochloric and sulphurous acids. Pass the acid liquor through the same small filter but
collect the liquor apart. Make ammoniacal and again pass through the filter, this time
collecting the liquid with the main filtrate.
[114] This rarely amounts to more than 1 milligram.
[115] To make this, dissolve 1 gram of titanium oxide by fusing for some time with an
excess of bisulphate of potash and dissolve out with cold water and sulphuric acid.
Dilute to 1 litre, having previously added not less than 50 c.c. of strong sulphuric acid: 1
c.c. will contain .01 gram of TiO2. For the assay take 10 c.c. of this, add 2 c.c. of
peroxide of hydrogen and dilute to 100 c.c. Run this from a burette into the flask until
the colour equals that of the assay. Each c.c. equals 1 milligram of TiO2. Fluorides must
be absent.
[116] C + O2 = CO2
[117] For example, soluble organic acids formed by partial oxidation with nitric acid.
[118] For coals, and other bodies containing sulphur, chromate of lead should be used
instead of oxide of copper; and the temperature should be limited to dull redness.
[119] This may be prepared by dissolving 534 grams of ammonium chloride and 854
grams of crystallized cupric chloride (CuCl2.2H2O) in hot water and crystallizing.
[120] Soda-lime is made by dissolving 100 grams of "soda" in water, and carefully
slaking 200 grams of lime with it. Evaporate to dryness in an iron dish and ignite at a
low red heat in a crucible. Use the small lumps.
[121] Made by diluting 1 part by measure of saturated lime-water up to 10 with recently
boiled distilled water.
[122] See under Gasometric Assays.
[123] See "A Method for the Separation and Estimation of Boric Acid," by F.A. Gooch,
Chemical News, January 7, 1887.
excess, and filter off the precipitate when it has settled. Wash with hot water,
ignite, and weigh as alumina (Al2O3).
FOOTNOTES:
[113] If the dishes show a manganese stain, wash them out with a few drops of
hydrochloric and sulphurous acids. Pass the acid liquor through the same small filter but
collect the liquor apart. Make ammoniacal and again pass through the filter, this time
collecting the liquid with the main filtrate.
[114] This rarely amounts to more than 1 milligram.
[115] To make this, dissolve 1 gram of titanium oxide by fusing for some time with an
excess of bisulphate of potash and dissolve out with cold water and sulphuric acid.
Dilute to 1 litre, having previously added not less than 50 c.c. of strong sulphuric acid: 1
c.c. will contain .01 gram of TiO2. For the assay take 10 c.c. of this, add 2 c.c. of
peroxide of hydrogen and dilute to 100 c.c. Run this from a burette into the flask until
the colour equals that of the assay. Each c.c. equals 1 milligram of TiO2. Fluorides must
be absent.
[116] C + O2 = CO2
[117] For example, soluble organic acids formed by partial oxidation with nitric acid.
[118] For coals, and other bodies containing sulphur, chromate of lead should be used
instead of oxide of copper; and the temperature should be limited to dull redness.
[119] This may be prepared by dissolving 534 grams of ammonium chloride and 854
grams of crystallized cupric chloride (CuCl2.2H2O) in hot water and crystallizing.
[120] Soda-lime is made by dissolving 100 grams of "soda" in water, and carefully
slaking 200 grams of lime with it. Evaporate to dryness in an iron dish and ignite at a
low red heat in a crucible. Use the small lumps.
[121] Made by diluting 1 part by measure of saturated lime-water up to 10 with recently
boiled distilled water.
[122] See under Gasometric Assays.
[123] See "A Method for the Separation and Estimation of Boric Acid," by F.A. Gooch,
Chemical News, January 7, 1887.
Page 534
APPENDIX A.
Table of Atomic Weights and other Constants.
Symbols. Names. Atomic Weights. Specific Gravity. Melting Points. C.
Ag Silver 107.9 10.5 1000°
Al Aluminium 27.0 2.7 700°
As Arsenic 75.0 5.9
Au Gold 197.3 19.2 1200°
B Boron 11.0 2.7
Ba Barium 137.0 4.0
Be Beryllium 9.0 2.1
Bi Bismuth 208.9 9.8 270°
Br Bromine 80.0 3.2 -25°
C Carbon 12.0
Ca Calcium 40.0 1.6
Cd Cadmium 112.0 8.6 315°
Ce Cerium 140.2 6.7
Cl Chlorine 35.5
Co Cobalt 59.0 8.5
Cr Chromium 52.1 7.3
Cs Caesium 132.9 1.9 25°
Cu Copper 63.4 8.9 1090°
Di Didymium 142.3 6.5
Er Erbium 166.3
F Fluorine 19.0
Fe Iron 56.0 7.8
Ga Gallium 69.0 5.9 30°
Ge Germanium 72.3
H Hydrogen 1.0
Hg Mercury 200.0 13.6 -40°
I Iodine 126.8 4.9 106°
In Indium 113.7 7.4 175°
Ir Iridium 193.1 22.4
K Potassium 39.1 0.86 62.5°
Table of Atomic Weights and other Constants.
Symbols. Names. Atomic Weights. Specific Gravity. Melting Points. C.
Ag Silver 107.9 10.5 1000°
Al Aluminium 27.0 2.7 700°
As Arsenic 75.0 5.9
Au Gold 197.3 19.2 1200°
B Boron 11.0 2.7
Ba Barium 137.0 4.0
Be Beryllium 9.0 2.1
Bi Bismuth 208.9 9.8 270°
Br Bromine 80.0 3.2 -25°
C Carbon 12.0
Ca Calcium 40.0 1.6
Cd Cadmium 112.0 8.6 315°
Ce Cerium 140.2 6.7
Cl Chlorine 35.5
Co Cobalt 59.0 8.5
Cr Chromium 52.1 7.3
Cs Caesium 132.9 1.9 25°
Cu Copper 63.4 8.9 1090°
Di Didymium 142.3 6.5
Er Erbium 166.3
F Fluorine 19.0
Fe Iron 56.0 7.8
Ga Gallium 69.0 5.9 30°
Ge Germanium 72.3
H Hydrogen 1.0
Hg Mercury 200.0 13.6 -40°
I Iodine 126.8 4.9 106°
In Indium 113.7 7.4 175°
Ir Iridium 193.1 22.4
K Potassium 39.1 0.86 62.5°
Page 535
La Lanthanum 138.2 6.1
Table of Atomic Weights and other Constants.—continued.
Symbols. Names. Atomic Weights. Specific Gravity. Melting Points. C.
Li Lithium 7.0 0.59 180°
Mg Magnesium 24.3 1.7
Mn Manganese 55.0 8.0
Mo Molybdenum 96.0 8.6
N Nitrogen 14.0
Na Sodium 23.0 0.97 95.6°
Nb Niobium 94.0 4.1
Ni Nickel 58.7 8.9
O Oxygen 16.0
Os Osmium 191.7 22.4
P Phosphorus 31.0 1.8 44°
Pb Lead 206.9 11.4 334°
Pd Palladium 106.6 11.4 1350°
Pt Platinum 195.0 21.5 2000°
Rb Rubidium 85.5 1.5 38.5°
Rh Rhodium 103.5 12.1
Ru Ruthenium 101.6 11.4
S Sulphur 32.0 2.0 115°
Sb Antimony 120.0 6.7 425°
Se Selenium 79.0 4.8 100°
Si Silicon 28.4 2.0
Sn Tin 119.0 7.3 235°
Sr Strontium 87.6 2.5
Ta Tantalum 182.6
Te Tellurium 125.0 6.2 480°
Th Thorium 232.6 7.8
Ti Titanium 48.0 5.3
Tl Thallium 204.2 11.9 294°
U Uranium 239.6 18.4
V Vanadium 51.4 5.5
W Tungsten 184.0 19.1
Y Yttrium 89.1
Table of Atomic Weights and other Constants.—continued.
Symbols. Names. Atomic Weights. Specific Gravity. Melting Points. C.
Li Lithium 7.0 0.59 180°
Mg Magnesium 24.3 1.7
Mn Manganese 55.0 8.0
Mo Molybdenum 96.0 8.6
N Nitrogen 14.0
Na Sodium 23.0 0.97 95.6°
Nb Niobium 94.0 4.1
Ni Nickel 58.7 8.9
O Oxygen 16.0
Os Osmium 191.7 22.4
P Phosphorus 31.0 1.8 44°
Pb Lead 206.9 11.4 334°
Pd Palladium 106.6 11.4 1350°
Pt Platinum 195.0 21.5 2000°
Rb Rubidium 85.5 1.5 38.5°
Rh Rhodium 103.5 12.1
Ru Ruthenium 101.6 11.4
S Sulphur 32.0 2.0 115°
Sb Antimony 120.0 6.7 425°
Se Selenium 79.0 4.8 100°
Si Silicon 28.4 2.0
Sn Tin 119.0 7.3 235°
Sr Strontium 87.6 2.5
Ta Tantalum 182.6
Te Tellurium 125.0 6.2 480°
Th Thorium 232.6 7.8
Ti Titanium 48.0 5.3
Tl Thallium 204.2 11.9 294°
U Uranium 239.6 18.4
V Vanadium 51.4 5.5
W Tungsten 184.0 19.1
Y Yttrium 89.1
Page 536
Yb Ytterbium 173.0
Zn Zinc 65.3 6.9 423°
Zr Zirconium 90.6 4.1
The atomic weights in this table are in accord with the numbers given by F.W.
Clarke (Dec. 6, 1890), chief chemist of the United States Geological Survey.
Zn Zinc 65.3 6.9 423°
Zr Zirconium 90.6 4.1
The atomic weights in this table are in accord with the numbers given by F.W.
Clarke (Dec. 6, 1890), chief chemist of the United States Geological Survey.
Page 537
Table for Converting Degrees of the
Centigrade Thermometer into Degrees of
Fahrenheit's Scale.
Nitric Acid.
Table showing the percentage, by Weight, of Real Acid (HNO3) in Aqueous
Solutions of Nitric Acid of different Specific Gravities. Temperature, 15° C.
1.530100.0 1.40566.0 1.20533.0
1.52799.0 1.40065.0 1.19832.0
1.52498.0 1.39564.0 1.19231.0
1.52097.0 1.39063.0 1.18530.0
1.51696.0 1.38662.0 1.17929.0
1.51395.0 1.38061.0 1.17228.0
1.50994.0 1.37460.0 1.16627.0
Centigrade Thermometer into Degrees of
Fahrenheit's Scale.
Nitric Acid.
Table showing the percentage, by Weight, of Real Acid (HNO3) in Aqueous
Solutions of Nitric Acid of different Specific Gravities. Temperature, 15° C.
1.530100.0 1.40566.0 1.20533.0
1.52799.0 1.40065.0 1.19832.0
1.52498.0 1.39564.0 1.19231.0
1.52097.0 1.39063.0 1.18530.0
1.51696.0 1.38662.0 1.17929.0
1.51395.0 1.38061.0 1.17228.0
1.50994.0 1.37460.0 1.16627.0
Page 538
1.50693.0 1.36859.0 1.15926.0
1.50392.0 1.36358.0 1.15225.0
1.49991.0 1.35857.0 1.14524.0
1.49590.0 1.35356.0 1.13823.0
1.49289.0 1.34655.0 1.13222.0
1.48888.0 1.34154.0 1.12621.0
1.48587.0 1.33553.0 1.12020.0
1.48286.0 1.32952.0 1.114 19.0
1.47885.0 1.32351.0 1.10818.0
1.47484.0 1.31750.0 1.10217.0
1.47083.0 1.311 49.0 1.09616.0
1.46782.0 1.30448.0 1.08915.0
1.46381.0 1.29847.0 1.08314.0
1.46080.0 1.29146.0 1.07713.0
1.45679.0 1.28445.0 1.07112.0
1.45278.0 1.27744.0 1.06511.0
1.44977.0 1.27043.0 1.06010.0
1.44576.0 1.26442.0 1.0539.0
1.44275.0 1.25741.0 1.0478.0
1.43874.0 1.25140.0 1.0417.0
1.43573.0 1.24439.0 1.0346.0
1.43172.0 1.23838.0 1.0285.0
1.42771.0 1.23237.0 1.0224.0
1.42370.0 1.22536.0 1.0163.0
1.41869.0 1.21835.0 1.0102.0
1.41468.0 1.21234.0 1.0041.0
1.41067.0
Hydrochloric Acid.
Table showing the percentage, by Weight, of Real Acid (HCl) in Aqueous
Solutions of Hydrochloric Acid of different Specific Gravities. Temperature,
15° C.
1.50392.0 1.36358.0 1.15225.0
1.49991.0 1.35857.0 1.14524.0
1.49590.0 1.35356.0 1.13823.0
1.49289.0 1.34655.0 1.13222.0
1.48888.0 1.34154.0 1.12621.0
1.48587.0 1.33553.0 1.12020.0
1.48286.0 1.32952.0 1.114 19.0
1.47885.0 1.32351.0 1.10818.0
1.47484.0 1.31750.0 1.10217.0
1.47083.0 1.311 49.0 1.09616.0
1.46782.0 1.30448.0 1.08915.0
1.46381.0 1.29847.0 1.08314.0
1.46080.0 1.29146.0 1.07713.0
1.45679.0 1.28445.0 1.07112.0
1.45278.0 1.27744.0 1.06511.0
1.44977.0 1.27043.0 1.06010.0
1.44576.0 1.26442.0 1.0539.0
1.44275.0 1.25741.0 1.0478.0
1.43874.0 1.25140.0 1.0417.0
1.43573.0 1.24439.0 1.0346.0
1.43172.0 1.23838.0 1.0285.0
1.42771.0 1.23237.0 1.0224.0
1.42370.0 1.22536.0 1.0163.0
1.41869.0 1.21835.0 1.0102.0
1.41468.0 1.21234.0 1.0041.0
1.41067.0
Hydrochloric Acid.
Table showing the percentage, by Weight, of Real Acid (HCl) in Aqueous
Solutions of Hydrochloric Acid of different Specific Gravities. Temperature,
15° C.
Page 539
1.200040.78 1.141028.54 1.079816.31
1.198240.37 1.138928.13 1.077815.90
1.196439.96 1.136927.72 1.075815.49
1.194639.55 1.134927.32 1.073815.08
1.192839.14 1.132826.91 1.071814.68
1.191038.74 1.130826.50 1.069714.27
1.189338.33 1.128726.10 1.067713.86
1.187537.92 1.126725.69 1.065713.45
1.185737.51 1.124725.28 1.063713.05
1.184637.11 1.122624.87 1.061712.64
1.182236.70 1.120624.46 1.059712.23
1.180236.29 1.1185 24.06 1.057711.82
1.178235.88 1.1164 23.65 1.055711.41
1.176235.47 1.1143 23.24 1.053711.01
1.174135.07 1.1123 22.83 1.051710.60
1.172134.66 1.1102 22.43 1.049710.19
1.170134.25 1.108222.02 1.04779.78
1.168133.84 1.106121.61 1.04579.38
1.166133.43 1.104121.20 1.04378.97
1.164133.03 1.102020.79 1.04178.56
1.162032.62 1.100020.39 1.03978.15
1.159932.21 1.098019.98 1.03777.75
1.157831.80 1.096019.57 1.03577.34
1.155731.40 1.093919.16 1.03376.93
1.153630.99 1.091918.76 1.03186.52
1.151530.58 1.089918.35 1.02986.11
1.149430.17 1.087917.94 1.02795.51
1.147329.76 1.085917.53 1.02595.30
1.145229.36 1.083817.12 1.02394.89
1.143128.95 1.081816.72 1.02004.01
AMMONIA.
1.198240.37 1.138928.13 1.077815.90
1.196439.96 1.136927.72 1.075815.49
1.194639.55 1.134927.32 1.073815.08
1.192839.14 1.132826.91 1.071814.68
1.191038.74 1.130826.50 1.069714.27
1.189338.33 1.128726.10 1.067713.86
1.187537.92 1.126725.69 1.065713.45
1.185737.51 1.124725.28 1.063713.05
1.184637.11 1.122624.87 1.061712.64
1.182236.70 1.120624.46 1.059712.23
1.180236.29 1.1185 24.06 1.057711.82
1.178235.88 1.1164 23.65 1.055711.41
1.176235.47 1.1143 23.24 1.053711.01
1.174135.07 1.1123 22.83 1.051710.60
1.172134.66 1.1102 22.43 1.049710.19
1.170134.25 1.108222.02 1.04779.78
1.168133.84 1.106121.61 1.04579.38
1.166133.43 1.104121.20 1.04378.97
1.164133.03 1.102020.79 1.04178.56
1.162032.62 1.100020.39 1.03978.15
1.159932.21 1.098019.98 1.03777.75
1.157831.80 1.096019.57 1.03577.34
1.155731.40 1.093919.16 1.03376.93
1.153630.99 1.091918.76 1.03186.52
1.151530.58 1.089918.35 1.02986.11
1.149430.17 1.087917.94 1.02795.51
1.147329.76 1.085917.53 1.02595.30
1.145229.36 1.083817.12 1.02394.89
1.143128.95 1.081816.72 1.02004.01
AMMONIA.
Page 540
Table showing the percentage, by Weight, of Real Ammonia (NH3) in
Aqueous Solutions of Ammonia of different Specific Gravities. Temperature,
14° C.
0.884436.0 0.914523.6 0.953411.6
0.885235.6 0.915623.2 0.954911.2
0.886035.2 0.916822.8 0.956310.8
0.886834.8 0.918022.4 0.957810.4
0.887734.4 0.919122.0 0.959310.0
0.888534.0 0.920321.6 0.96089.6
0.889433.6 0.921521.2 0.96239.2
0.890333.2 0.922720.8 0.96398.8
0.8911 32.8 0.923920.4 0.96548.4
0.892032.4 0.925120.0 0.96708.0
0.892932.0 0.926419.6 0.96857.6
0.893831.6 0.927719.2 0.97017.2
0.894831.2 0.928918.8 0.97176.8
0.895730.8 0.930218.4 0.97336.4
0.896730.4 0.931418.0 0.97496.0
0.897630.0 0.932717.6 0.97655.6
0.898629.6 0.934017.2 0.97815.2
0.899629.2 0.935316.8 0.97904.8
0.900628.8 0.936616.4 0.98074.6
0.901628.4 0.938016.0 0.98234.2
0.902628.0 0.939315.6 0.98393.8
0.903627.6 0.940715.2 0.98553.4
0.904727.2 0.942014.8 0.98733.0
0.905726.8 0.943414.4 0.98902.6
0.906826.4 0.944914.0 0.99072.2
0.907826.0 0.946313.6 0.99241.8
0.908925.6 0.947713.2 0.99411.4
0.910025.2 0.949112.8 0.99591.0
0.9111 24.8 0.950512.4 0.99750.6
0.912224.4 0.952012.0 0.99910.2
Aqueous Solutions of Ammonia of different Specific Gravities. Temperature,
14° C.
0.884436.0 0.914523.6 0.953411.6
0.885235.6 0.915623.2 0.954911.2
0.886035.2 0.916822.8 0.956310.8
0.886834.8 0.918022.4 0.957810.4
0.887734.4 0.919122.0 0.959310.0
0.888534.0 0.920321.6 0.96089.6
0.889433.6 0.921521.2 0.96239.2
0.890333.2 0.922720.8 0.96398.8
0.8911 32.8 0.923920.4 0.96548.4
0.892032.4 0.925120.0 0.96708.0
0.892932.0 0.926419.6 0.96857.6
0.893831.6 0.927719.2 0.97017.2
0.894831.2 0.928918.8 0.97176.8
0.895730.8 0.930218.4 0.97336.4
0.896730.4 0.931418.0 0.97496.0
0.897630.0 0.932717.6 0.97655.6
0.898629.6 0.934017.2 0.97815.2
0.899629.2 0.935316.8 0.97904.8
0.900628.8 0.936616.4 0.98074.6
0.901628.4 0.938016.0 0.98234.2
0.902628.0 0.939315.6 0.98393.8
0.903627.6 0.940715.2 0.98553.4
0.904727.2 0.942014.8 0.98733.0
0.905726.8 0.943414.4 0.98902.6
0.906826.4 0.944914.0 0.99072.2
0.907826.0 0.946313.6 0.99241.8
0.908925.6 0.947713.2 0.99411.4
0.910025.2 0.949112.8 0.99591.0
0.9111 24.8 0.950512.4 0.99750.6
0.912224.4 0.952012.0 0.99910.2
Page 541
0.913324.0
SULPHURIC ACID.
Table showing the percentage, by Weight, of Real Acid (H2SO4) in Aqueous
Solutions of Sulphuric Acid of varying Specific Gravity. Temperature, 15°
C.
1.838100.0 1.56866.0 1.24733.0
1.84099.0 1.55765.0 1.23932.0
1.84198.0 1.54564.0 1.23131.0
1.84197.0 1.53463.0 1.22330.0
1.84096.0 1.52362.0 1.21529.0
1.83895.0 1.51261.0 1.20628.0
1.83694.0 1.50160.0 1.19827.0
1.83493.0 1.49059.0 1.19026.0
1.83192.0 1.48058.0 1.18225.0
1.82791.0 1.46957.0 1.17424.0
1.82290.0 1.45856.0 1.16723.0
1.81689.0 1.44855.0 1.15922.0
1.80988.0 1.43854.0 1.15121.0
1.80287.0 1.42853.0 1.14420.0
1.79486.0 1.41852.0 1.13619.0
1.78685.0 1.40851.0 1.12918.0
1.77784.0 1.39850.0 1.12117.0
1.76783.0 1.38849.0 1.113 16.0
1.75682.0 1.37948.0 1.10615.0
1.74581.0 1.37047.0 1.09814.0
1.73480.0 1.36146.0 1.09113.0
1.72279.0 1.35145.0 1.08312.0
1.71078.0 1.34244.0 1.07511.0
1.69877.0 1.33343.0 1.06810.0
1.68676.0 1.32442.0 1.0619.0
1.67575.0 1.31541.0 1.0538.0
SULPHURIC ACID.
Table showing the percentage, by Weight, of Real Acid (H2SO4) in Aqueous
Solutions of Sulphuric Acid of varying Specific Gravity. Temperature, 15°
C.
1.838100.0 1.56866.0 1.24733.0
1.84099.0 1.55765.0 1.23932.0
1.84198.0 1.54564.0 1.23131.0
1.84197.0 1.53463.0 1.22330.0
1.84096.0 1.52362.0 1.21529.0
1.83895.0 1.51261.0 1.20628.0
1.83694.0 1.50160.0 1.19827.0
1.83493.0 1.49059.0 1.19026.0
1.83192.0 1.48058.0 1.18225.0
1.82791.0 1.46957.0 1.17424.0
1.82290.0 1.45856.0 1.16723.0
1.81689.0 1.44855.0 1.15922.0
1.80988.0 1.43854.0 1.15121.0
1.80287.0 1.42853.0 1.14420.0
1.79486.0 1.41852.0 1.13619.0
1.78685.0 1.40851.0 1.12918.0
1.77784.0 1.39850.0 1.12117.0
1.76783.0 1.38849.0 1.113 16.0
1.75682.0 1.37948.0 1.10615.0
1.74581.0 1.37047.0 1.09814.0
1.73480.0 1.36146.0 1.09113.0
1.72279.0 1.35145.0 1.08312.0
1.71078.0 1.34244.0 1.07511.0
1.69877.0 1.33343.0 1.06810.0
1.68676.0 1.32442.0 1.0619.0
1.67575.0 1.31541.0 1.0538.0
Page 542
1.66374.0 1.30640.0 1.0467.0
1.65173.0 1.29739.0 1.0396.0
1.63972.0 1.28938.0 1.0325.0
1.62771.0 1.28137.0 1.0254.0
1.61570.0 1.27236.0 1.0193.0
1.60469.0 1.26435.0 1.0132.0
1.59268.0 1.25634.0 1.0061.0
1.58067.0
1.65173.0 1.29739.0 1.0396.0
1.63972.0 1.28938.0 1.0325.0
1.62771.0 1.28137.0 1.0254.0
1.61570.0 1.27236.0 1.0193.0
1.60469.0 1.26435.0 1.0132.0
1.59268.0 1.25634.0 1.0061.0
1.58067.0
Page 543
APPENDIX B.
ESTIMATION OF SMALL QUANTITIES OF GOLD.[124]
In the case of small buttons of gold the weight can be determined more
easily and accurately by measuring with the help of a microscope than by
the actual use of a balance. Moreover, the method of measurement is
applicable to the determination of quantities of gold too minute to affect
even the most delicate balance.
For quantities of gold of from .5 to .005 milligram a microscope with 1/2
inch objective and B eyepiece is suitable. The measurements are made with
the help of a scale engraved (or, better, photographed) on a circular piece of
glass which rests on the diaphragm of the eyepiece. This scale and the
object upon the stage can be easily brought into focus at the same time. The
button of gold obtained by cupelling is loosened from the cupel by gently
touching with the moistened point of a knife; it generally adheres to the
knife, and is then transferred to a glass slide. The slide is placed on the
stage of the microscope, illuminated from below; and the button is brought
into focus, and so placed that it apparently coincides with the scale. The
diameters in two or three directions (avoiding the flattened surface) are then
read off: the different directions being got by rotating the eyepiece. The
mean diameter is taken. The weight of the button is arrived at by comparing
with the mean diameter of a standard prill of gold of known weight. The
weights are in the proportion of the cubes of the diameters. For example,
suppose a prill has been obtained which measures 12.5 divisions of the
scale, and that a standard prill weighing 0.1 milligram measures 11.1
divisions. The weight will be calculated as follows:
11.13 : 12.53 :: 0.1 : x
0.1×12.5×12.5×12.5
x = —————————— = 0.143 milligram.
11.1×11.1×11.1
ESTIMATION OF SMALL QUANTITIES OF GOLD.[124]
In the case of small buttons of gold the weight can be determined more
easily and accurately by measuring with the help of a microscope than by
the actual use of a balance. Moreover, the method of measurement is
applicable to the determination of quantities of gold too minute to affect
even the most delicate balance.
For quantities of gold of from .5 to .005 milligram a microscope with 1/2
inch objective and B eyepiece is suitable. The measurements are made with
the help of a scale engraved (or, better, photographed) on a circular piece of
glass which rests on the diaphragm of the eyepiece. This scale and the
object upon the stage can be easily brought into focus at the same time. The
button of gold obtained by cupelling is loosened from the cupel by gently
touching with the moistened point of a knife; it generally adheres to the
knife, and is then transferred to a glass slide. The slide is placed on the
stage of the microscope, illuminated from below; and the button is brought
into focus, and so placed that it apparently coincides with the scale. The
diameters in two or three directions (avoiding the flattened surface) are then
read off: the different directions being got by rotating the eyepiece. The
mean diameter is taken. The weight of the button is arrived at by comparing
with the mean diameter of a standard prill of gold of known weight. The
weights are in the proportion of the cubes of the diameters. For example,
suppose a prill has been obtained which measures 12.5 divisions of the
scale, and that a standard prill weighing 0.1 milligram measures 11.1
divisions. The weight will be calculated as follows:
11.13 : 12.53 :: 0.1 : x
0.1×12.5×12.5×12.5
x = —————————— = 0.143 milligram.
11.1×11.1×11.1
Page 544
The calculations are simplified by the use of a table of cubes. The standard
prills used in the comparison should not differ much in size from the prills
to be determined. They are prepared by alloying known weights of gold and
lead, so as to get an alloy of known composition, say one per cent. gold.
Portions of the alloy containing the weight of gold required (say 0.1
milligram) are then weighed off and cupelled on small smooth cupels, made
with the finest bone-ash. Care must be taken to remove the cupels as soon
as cupellation has finished. Several standard prills of the same size should
be made at the same time, and their mean diameter calculated. The lead for
making the gold-lead alloy is prepared from litharge purified by reducing
from it about 10 per cent. of its lead by fusion with a suitable proportion of
flour; the purified litharge is powdered, mixed with sufficient flour and
reduced to metal.
In determining the gold contained in small buttons of silver-gold alloy
obtained in assaying (and in which the silver is almost sure to be in excess
of that required for parting), transfer the button from the cupel to a small
clean porcelain crucible; pour on it a drop or two of nitric acid (diluted with
half its bulk of water), and heat gently and cautiously until action has
ceased. If the residual gold is broken up, move the crucible so as to bring
the particles together, so that they may cohere. Wash three or four times
with distilled water, about half filling the crucible each time and decanting
off against the finger. Dry the crucible in a warm place; and when dry, but
whilst still black, take the gold up on a small piece of pure lead. Half a
grain of lead is sufficient, and it is best to hold it on the point of a blunt
penknife, and press it on the gold in the crucible. The latter generally
adheres. Transfer to a small smooth cupel and place in the muffle. When the
cupellation has finished, the button of gold is measured as already
described.
PRACTICAL NOTES ON THE IODIDE PROCESS OF COPPER
ASSAYING.
For the following remarks and experiments we are indebted to Mr. J.W.
Westmoreland, who has had considerable experience with the process.
Having dissolved the ore he converts the metals into sulphates by
evaporating with sulphuric acid. The copper is then separated as
prills used in the comparison should not differ much in size from the prills
to be determined. They are prepared by alloying known weights of gold and
lead, so as to get an alloy of known composition, say one per cent. gold.
Portions of the alloy containing the weight of gold required (say 0.1
milligram) are then weighed off and cupelled on small smooth cupels, made
with the finest bone-ash. Care must be taken to remove the cupels as soon
as cupellation has finished. Several standard prills of the same size should
be made at the same time, and their mean diameter calculated. The lead for
making the gold-lead alloy is prepared from litharge purified by reducing
from it about 10 per cent. of its lead by fusion with a suitable proportion of
flour; the purified litharge is powdered, mixed with sufficient flour and
reduced to metal.
In determining the gold contained in small buttons of silver-gold alloy
obtained in assaying (and in which the silver is almost sure to be in excess
of that required for parting), transfer the button from the cupel to a small
clean porcelain crucible; pour on it a drop or two of nitric acid (diluted with
half its bulk of water), and heat gently and cautiously until action has
ceased. If the residual gold is broken up, move the crucible so as to bring
the particles together, so that they may cohere. Wash three or four times
with distilled water, about half filling the crucible each time and decanting
off against the finger. Dry the crucible in a warm place; and when dry, but
whilst still black, take the gold up on a small piece of pure lead. Half a
grain of lead is sufficient, and it is best to hold it on the point of a blunt
penknife, and press it on the gold in the crucible. The latter generally
adheres. Transfer to a small smooth cupel and place in the muffle. When the
cupellation has finished, the button of gold is measured as already
described.
PRACTICAL NOTES ON THE IODIDE PROCESS OF COPPER
ASSAYING.
For the following remarks and experiments we are indebted to Mr. J.W.
Westmoreland, who has had considerable experience with the process.
Having dissolved the ore he converts the metals into sulphates by
evaporating with sulphuric acid. The copper is then separated as
Page 545
subsulphide by means of hyposulphite of soda, and the precipitate is
washed, dried, and calcined. The resulting oxide of copper is then dissolved
in nitric acid; and to the concentrated solution, a saturated solution of
carbonate of soda is added in sufficient quantity to throw down a
considerable proportion of the copper. Acetic acid is added to dissolve the
precipitate, and when this is effected more of the acid is poured on so as to
render the solution strongly acid. To this potassium iodide crystals are
added in the proportion of ten parts of iodide to each one part of copper
supposed to be present. The solution is then titrated with "hypo" as usual.
For the examination of technical products experiments made in sulphuric
acid solutions have no value, since arsenic acid, which is generally present
to a greater or less extent, affects the end reaction. In such solutions
bismuth may also interfere.
The solution best suited for the assay is one containing acetate of soda and
free acetic acid. The presence of acetate of soda counteracts the interference
of arsenic and of bismuth.
The return of the blue colour after titration is due to the excessive dilution
of the assay, or to an insufficiency of potassium iodide, or to the presence of
nitrous fumes. The interference of an excess of sodium acetate is avoided
by adding more iodide crystals to the extent of doubling the usual amount.
The interference of lead can be avoided by the addition of sulphuric acid or
of phosphate of soda to the acid solution containing the copper, and before
neutralising with carbonate of soda. The end reaction is, however, with care
distinguishable without this addition. The following experiments, each
containing .0648 gram of lead, were made by him in illustration:
Copper taken. Reagent added. Copper found. End reaction.
.2092 gram — .2077 gram fairly satisfactory
.2101 " — .2092 " "
.2167 " sulphuric acid .2152 " "
.2117 " " .2108 " "
.2109 " phosphate of soda .2092 " good, colourless
.2205 " " .2174 " rather yellow
washed, dried, and calcined. The resulting oxide of copper is then dissolved
in nitric acid; and to the concentrated solution, a saturated solution of
carbonate of soda is added in sufficient quantity to throw down a
considerable proportion of the copper. Acetic acid is added to dissolve the
precipitate, and when this is effected more of the acid is poured on so as to
render the solution strongly acid. To this potassium iodide crystals are
added in the proportion of ten parts of iodide to each one part of copper
supposed to be present. The solution is then titrated with "hypo" as usual.
For the examination of technical products experiments made in sulphuric
acid solutions have no value, since arsenic acid, which is generally present
to a greater or less extent, affects the end reaction. In such solutions
bismuth may also interfere.
The solution best suited for the assay is one containing acetate of soda and
free acetic acid. The presence of acetate of soda counteracts the interference
of arsenic and of bismuth.
The return of the blue colour after titration is due to the excessive dilution
of the assay, or to an insufficiency of potassium iodide, or to the presence of
nitrous fumes. The interference of an excess of sodium acetate is avoided
by adding more iodide crystals to the extent of doubling the usual amount.
The interference of lead can be avoided by the addition of sulphuric acid or
of phosphate of soda to the acid solution containing the copper, and before
neutralising with carbonate of soda. The end reaction is, however, with care
distinguishable without this addition. The following experiments, each
containing .0648 gram of lead, were made by him in illustration:
Copper taken. Reagent added. Copper found. End reaction.
.2092 gram — .2077 gram fairly satisfactory
.2101 " — .2092 " "
.2167 " sulphuric acid .2152 " "
.2117 " " .2108 " "
.2109 " phosphate of soda .2092 " good, colourless
.2205 " " .2174 " rather yellow
Page 546
Effect of Sodium Acetate.—Each solution contained .3343 gram of copper.
a.b.c. d. e. f. g.
grams. grams. grams. grams. grams.
"Acetate" added — 16.2 16.2 16.2 16.2
"Iodide" added 3.5 3.5 7.0 3.5 7.0
Copper found .3343 .3324 .3351 .3269 .3356
In these experiments, except with the excessive quantities of acetate of soda
and the insufficiency of potassium iodide in the cases of d and f, there was
no difficulty with the after-blueing.
METHOD OF SEPARATING COBALT AND NICKEL.
The following method of separating and estimating cobalt and nickel has
been described by Mr. James Hope,[125] with whom it has been in daily use
for several years with completely satisfactory results.
The quantity of ore taken should contain about .5 gram of the mixed metals.
It is dissolved in hydrochloric acid or aqua regia, and the solution
evaporated to dryness. The residue is taken up with dilute hydrochloric acid
and hot water. The solution is filtered off from the silica, freed from second
group metals by treatment with sulphuretted hydrogen and filtered, and
after oxidation with nitric acid is separated from iron and alumina by the
basic acetate method (page 233). The precipitate is redissolved in a little
hydrochloric acid, and again precipitated by sodium acetate. The two
filtrates are mixed and treated with a little acetic acid, and the cobalt and
nickel are then precipitated as sulphides by a current of sulphuretted
hydrogen. The precipitate is filtered off, washed, dried, and calcined, and
the resulting oxides are weighed to get an idea as to the quantity of the two
metals present.
The calcined precipitate is dissolved in a small covered beaker in aqua regia
with the help of a few drops of bromine to remove any separated sulphur,
and the solution evaporated to dryness with a few drops of sulphuric acid.
The residue is dissolved in hot water, diluted to about 50 c.c., and heated to
boiling. About 2 grams (four times the quantity of mixed metals present) of
a.b.c. d. e. f. g.
grams. grams. grams. grams. grams.
"Acetate" added — 16.2 16.2 16.2 16.2
"Iodide" added 3.5 3.5 7.0 3.5 7.0
Copper found .3343 .3324 .3351 .3269 .3356
In these experiments, except with the excessive quantities of acetate of soda
and the insufficiency of potassium iodide in the cases of d and f, there was
no difficulty with the after-blueing.
METHOD OF SEPARATING COBALT AND NICKEL.
The following method of separating and estimating cobalt and nickel has
been described by Mr. James Hope,[125] with whom it has been in daily use
for several years with completely satisfactory results.
The quantity of ore taken should contain about .5 gram of the mixed metals.
It is dissolved in hydrochloric acid or aqua regia, and the solution
evaporated to dryness. The residue is taken up with dilute hydrochloric acid
and hot water. The solution is filtered off from the silica, freed from second
group metals by treatment with sulphuretted hydrogen and filtered, and
after oxidation with nitric acid is separated from iron and alumina by the
basic acetate method (page 233). The precipitate is redissolved in a little
hydrochloric acid, and again precipitated by sodium acetate. The two
filtrates are mixed and treated with a little acetic acid, and the cobalt and
nickel are then precipitated as sulphides by a current of sulphuretted
hydrogen. The precipitate is filtered off, washed, dried, and calcined, and
the resulting oxides are weighed to get an idea as to the quantity of the two
metals present.
The calcined precipitate is dissolved in a small covered beaker in aqua regia
with the help of a few drops of bromine to remove any separated sulphur,
and the solution evaporated to dryness with a few drops of sulphuric acid.
The residue is dissolved in hot water, diluted to about 50 c.c., and heated to
boiling. About 2 grams (four times the quantity of mixed metals present) of
Page 547
ammonium phosphate (AmH2PO4) are weighed off, dissolved in the
smallest possible quantity of water, and boiled for a minute or two with a
few c.c. of dilute sulphuric acid. This is added to the boiling-hot solution of
cobalt and nickel, which is then treated cautiously with dilute ammonia
until the precipitate partially dissolves. The addition of the ammonia is
continued drop by drop with constant stirring, until the cobalt comes down
as a pink precipitate of ammonium cobalt phosphate (AmCoPO4). The
beaker is placed on the top of a water bath with occasional stirring for five
or ten minutes. The blue liquid containing the nickel is decanted through a
small filter and the precipitate is dissolved with a few drops of dilute
sulphuric acid. The resulting solution is treated with a small excess of
ammonium phosphate and the cobalt again precipitated by the cautious
addition of ammonia exactly as before. The precipitate containing the whole
of the cobalt is filtered off and washed with small quantities of hot water.
The filtrate is added to the previous one containing the greater part of the
nickel.
The ammonium cobalt phosphate is dried, transferred to a platinum
crucible, and ignited over a Bunsen flame for fifteen or twenty minutes. A
purple coloured cobalt pyrophosphate (Co2P2O7) is thus formed, and is
weighed. It contains 40.3 per cent. of cobalt.
The mixed filtrates containing the nickel are placed in a tall beaker, and
dilated if necessary to about 200 c.c. Ten c.c. of strong ammonia are added,
and the solution, heated to 70° C., is ready for electrolysis. A battery of two
1-1/2 pint Bunsen cells is used. This is found capable of depositing from .15
to .20 gram of nickel per hour, and from two to three hours is generally
sufficient for the electrolysis. The electrode with the deposited nickel is
washed with distilled water, afterwards with alcohol as described under
copper, and is then dried and weighed.
The following results obtained with this method by Mr. Hope illustrate the
accuracy of the method. They were obtained by working on solutions
containing known weights of the two metals:
Taken. Found.
Cobalt. Nickel. Cobalt. Nickel.
.1236 gram .1155 gram .1242 gram.1155 gram
smallest possible quantity of water, and boiled for a minute or two with a
few c.c. of dilute sulphuric acid. This is added to the boiling-hot solution of
cobalt and nickel, which is then treated cautiously with dilute ammonia
until the precipitate partially dissolves. The addition of the ammonia is
continued drop by drop with constant stirring, until the cobalt comes down
as a pink precipitate of ammonium cobalt phosphate (AmCoPO4). The
beaker is placed on the top of a water bath with occasional stirring for five
or ten minutes. The blue liquid containing the nickel is decanted through a
small filter and the precipitate is dissolved with a few drops of dilute
sulphuric acid. The resulting solution is treated with a small excess of
ammonium phosphate and the cobalt again precipitated by the cautious
addition of ammonia exactly as before. The precipitate containing the whole
of the cobalt is filtered off and washed with small quantities of hot water.
The filtrate is added to the previous one containing the greater part of the
nickel.
The ammonium cobalt phosphate is dried, transferred to a platinum
crucible, and ignited over a Bunsen flame for fifteen or twenty minutes. A
purple coloured cobalt pyrophosphate (Co2P2O7) is thus formed, and is
weighed. It contains 40.3 per cent. of cobalt.
The mixed filtrates containing the nickel are placed in a tall beaker, and
dilated if necessary to about 200 c.c. Ten c.c. of strong ammonia are added,
and the solution, heated to 70° C., is ready for electrolysis. A battery of two
1-1/2 pint Bunsen cells is used. This is found capable of depositing from .15
to .20 gram of nickel per hour, and from two to three hours is generally
sufficient for the electrolysis. The electrode with the deposited nickel is
washed with distilled water, afterwards with alcohol as described under
copper, and is then dried and weighed.
The following results obtained with this method by Mr. Hope illustrate the
accuracy of the method. They were obtained by working on solutions
containing known weights of the two metals:
Taken. Found.
Cobalt. Nickel. Cobalt. Nickel.
.1236 gram .1155 gram .1242 gram.1155 gram
Page 548
.1236 " .0577 " .1232 " .0575 "
.2472 " .0577 " .2449 " .0585 "
.3708 " .0577 " .3701 " .0580 "
.0618 " .3465 " .0619 " .3454 "
.0618 " .2310 " .0625 " .2295 "
.0618 " .1155 " .0621 " .1155 "
FOOTNOTES:
[124] For fuller information see a paper on "The Estimation of Minute
Quantities of Gold," by Dr. George Tate; read before the Liverpool Polytechnic
Society, Nov. 1889.
[125] Journal of the Society of Chemical Industry, No 4, vol. ix. April 30, 1890.
.2472 " .0577 " .2449 " .0585 "
.3708 " .0577 " .3701 " .0580 "
.0618 " .3465 " .0619 " .3454 "
.0618 " .2310 " .0625 " .2295 "
.0618 " .1155 " .0621 " .1155 "
FOOTNOTES:
[124] For fuller information see a paper on "The Estimation of Minute
Quantities of Gold," by Dr. George Tate; read before the Liverpool Polytechnic
Society, Nov. 1889.
[125] Journal of the Society of Chemical Industry, No 4, vol. ix. April 30, 1890.
Page 549
APPENDIX C.
A LECTURE ON THE THEORY OF SAMPLING.
The problem of the sampler is essentially the same as that of the student of
statistics. One aims at getting a small parcel of ore, the other a number of
data, but each hopes to obtain what shall represent a true average applicable
to a much larger mass of material. Ignoring the mechanical part of the
problems, the sampling errors of the one and the deviations from the
average of the other are the same thing.
It may be doubted whether many not specially trained in the study of
statistics could answer such a question as the following:—Seven hundred
thousand men being employed, there are, in a given year, one thousand
deaths from accident. Assuming the conditions to remain unaltered, within
what limits could one foretell the number of deaths by accident in any other
year?
On the other hand, there is a widespread belief in the efficacy of what is
called the law of averages. Even the ordinary newspaper reader is
accustomed to look on the national death-rate or birth-rate as a thing
capable of being stated with accuracy to one or two places of decimals, and
he knows that the annual number of suicides is practically constant.
If a man played whist often and kept a record of the number of trumps n
each hand, he would find fortune treated him quite fairly; in a year's play
the average number would deviate very little from the theoretical average,
i.e., one-quarter of thirteen. And a knowledge of this truth is useful, and that
not merely in keeping ejaculations in due restraint. But every good player
knows more than this: he has a sense of what variations in the number of
trumps may reasonably be expected. For example, he will be prepared to
risk something on neither of his opponents having more than five trumps,
and will accept it as a practical certainty that no one has more than eight.
Much of what is known as good judgment is based on a proper estimate of
deviations from the average. The question has an important bearing on
A LECTURE ON THE THEORY OF SAMPLING.
The problem of the sampler is essentially the same as that of the student of
statistics. One aims at getting a small parcel of ore, the other a number of
data, but each hopes to obtain what shall represent a true average applicable
to a much larger mass of material. Ignoring the mechanical part of the
problems, the sampling errors of the one and the deviations from the
average of the other are the same thing.
It may be doubted whether many not specially trained in the study of
statistics could answer such a question as the following:—Seven hundred
thousand men being employed, there are, in a given year, one thousand
deaths from accident. Assuming the conditions to remain unaltered, within
what limits could one foretell the number of deaths by accident in any other
year?
On the other hand, there is a widespread belief in the efficacy of what is
called the law of averages. Even the ordinary newspaper reader is
accustomed to look on the national death-rate or birth-rate as a thing
capable of being stated with accuracy to one or two places of decimals, and
he knows that the annual number of suicides is practically constant.
If a man played whist often and kept a record of the number of trumps n
each hand, he would find fortune treated him quite fairly; in a year's play
the average number would deviate very little from the theoretical average,
i.e., one-quarter of thirteen. And a knowledge of this truth is useful, and that
not merely in keeping ejaculations in due restraint. But every good player
knows more than this: he has a sense of what variations in the number of
trumps may reasonably be expected. For example, he will be prepared to
risk something on neither of his opponents having more than five trumps,
and will accept it as a practical certainty that no one has more than eight.
Much of what is known as good judgment is based on a proper estimate of
deviations from the average. The question has an important bearing on
Page 550
sampling, as may be seen from the fact that shuffling and dealing at cards
are but modifications of the well-known mixing and quartering of the
sampler.
Because of this bearing on sampling and for other reasons, I became many
years ago much interested in the question, and gave to its solution perhaps
more labour than it was worth. In books on Medical Statistics the answer to
the question is stated in a mathematical formula, called Poisson's formula,
which, in a modified form, I shall give further on. But this did not satisfy
me, because I wanted to learn what a reasonably safe limit of error actually
meant, and this could be best learnt by experiment; so with the help of some
friends I went in for a thorough course of penny-tossing.
Tossing a penny twenty times, an average result would be ten heads and ten
tails. To find the deviations from this, we tossed two hundred twenties, i.e.,
four thousand times. Of the two hundred, thirty-three gave the exact
average, viz.:—10 heads; sixty-four gave an error of one, viz.:—9 or 11
heads; forty-nine, an error of two; twenty-six, an error of three; twenty, an
error of four; eight gave an error of five, and this limit was not exceeded.
From these we may say that six is a reasonably safe limit of error. Ninety-
seven cases, say one-half, gave an error not exceeding one; and the mean
error is 1.8.
In other words, in twenty tosses you will not get more than 16 nor less than
4 heads; you are as likely as not to get 9, 10, or 11 heads; and lastly, if you
lost in twenty throws all heads or tails over 10 your average loss would be
1.8 penny, or say roughly 2d. on the twenty throws.
It was necessary to compare these with another series containing a larger
average, say that of 100 heads in 200 throws. I confess the labour of tossing
pennies two hundred at a time was little to our taste. So from a bag of
pennies borrowed from the bank, we weighed out samples containing two
hundred, and for an evening we were busy counting heads and tails in these.
The heads in sixty samples ranged from 80 to 114. One hundred heads
occurred seven times. The extent and frequency of the errors is shown in the
table.
Error. No. of Times. Error.No. of Times. Error.No. of Times.
are but modifications of the well-known mixing and quartering of the
sampler.
Because of this bearing on sampling and for other reasons, I became many
years ago much interested in the question, and gave to its solution perhaps
more labour than it was worth. In books on Medical Statistics the answer to
the question is stated in a mathematical formula, called Poisson's formula,
which, in a modified form, I shall give further on. But this did not satisfy
me, because I wanted to learn what a reasonably safe limit of error actually
meant, and this could be best learnt by experiment; so with the help of some
friends I went in for a thorough course of penny-tossing.
Tossing a penny twenty times, an average result would be ten heads and ten
tails. To find the deviations from this, we tossed two hundred twenties, i.e.,
four thousand times. Of the two hundred, thirty-three gave the exact
average, viz.:—10 heads; sixty-four gave an error of one, viz.:—9 or 11
heads; forty-nine, an error of two; twenty-six, an error of three; twenty, an
error of four; eight gave an error of five, and this limit was not exceeded.
From these we may say that six is a reasonably safe limit of error. Ninety-
seven cases, say one-half, gave an error not exceeding one; and the mean
error is 1.8.
In other words, in twenty tosses you will not get more than 16 nor less than
4 heads; you are as likely as not to get 9, 10, or 11 heads; and lastly, if you
lost in twenty throws all heads or tails over 10 your average loss would be
1.8 penny, or say roughly 2d. on the twenty throws.
It was necessary to compare these with another series containing a larger
average, say that of 100 heads in 200 throws. I confess the labour of tossing
pennies two hundred at a time was little to our taste. So from a bag of
pennies borrowed from the bank, we weighed out samples containing two
hundred, and for an evening we were busy counting heads and tails in these.
The heads in sixty samples ranged from 80 to 114. One hundred heads
occurred seven times. The extent and frequency of the errors is shown in the
table.
Error. No. of Times. Error.No. of Times. Error.No. of Times.
Page 551
1 8 6 3 11 1
2 5 7 3 14 3
3 6 8 3 15 1
4 3 9 7 18 2
5 6 10 1 20 1
We may call the limit of error 21. Twenty-nine results out of sixty, say one-
half, had an error not exceeding 4; and the mean error is 5.6. In comparing
these with the series 10 in 20 we must, working by rule, divide not by 10
but by 3.16, the square root of 10; for if we multiply an average by any
number[126] the error is also multiplied but only by the square root of the
number. The error varies as the square root of the number. Now
21/3.16 = 6.6 = limit of error for 10 in 20.
5.6/3.16 = 1.8 = mean error " " "
4/3.16 = 1.2 = probable error " " "
It will be seen that these calculated results agree fairly well with those
actually obtained. The rule by which these calculations are made is
important and will bear further illustration. To calculate the number of
heads in 3200 throws, we have to find the limit of error on a true average of
1600 in 3200. This being 16 times the average of 100 in 200, the
corresponding errors must be multiplied by 4. This gives
21×4 = 84 = limit of error.
5.6×4 = 22.4 = mean error.
4×4 = 16 = probable error.
The results I have actually obtained with these large numbers are hardly
enough to base much on, but have a value by way of confirmation.
Expecting 1600 heads, the actual numbers were 1560, 1596, 1643, 1557,
1591, 1605, 1615, 1545.
It will be seen that exactly half are within the probable error; but this,
considering the small number of results, must be more or less of an
accident; it is more to the point they are all well within the limits of error.
2 5 7 3 14 3
3 6 8 3 15 1
4 3 9 7 18 2
5 6 10 1 20 1
We may call the limit of error 21. Twenty-nine results out of sixty, say one-
half, had an error not exceeding 4; and the mean error is 5.6. In comparing
these with the series 10 in 20 we must, working by rule, divide not by 10
but by 3.16, the square root of 10; for if we multiply an average by any
number[126] the error is also multiplied but only by the square root of the
number. The error varies as the square root of the number. Now
21/3.16 = 6.6 = limit of error for 10 in 20.
5.6/3.16 = 1.8 = mean error " " "
4/3.16 = 1.2 = probable error " " "
It will be seen that these calculated results agree fairly well with those
actually obtained. The rule by which these calculations are made is
important and will bear further illustration. To calculate the number of
heads in 3200 throws, we have to find the limit of error on a true average of
1600 in 3200. This being 16 times the average of 100 in 200, the
corresponding errors must be multiplied by 4. This gives
21×4 = 84 = limit of error.
5.6×4 = 22.4 = mean error.
4×4 = 16 = probable error.
The results I have actually obtained with these large numbers are hardly
enough to base much on, but have a value by way of confirmation.
Expecting 1600 heads, the actual numbers were 1560, 1596, 1643, 1557,
1591, 1605, 1615, 1545.
It will be seen that exactly half are within the probable error; but this,
considering the small number of results, must be more or less of an
accident; it is more to the point they are all well within the limits of error.
Page 552
I have a large number of other results which with a single exception are all
in accord with those given; and this exception only just overstepped the
limits. It was like a case of nine trumps, which though in a sense possible, is
very unlikely to happen in any one's experience.
But even now we are not quite in a position to answer the question with
which we started. If you refer to it you will see that we are face to face with
this problem: the limit of variation on the 1000 who died would be say 70,
[127]
ignoring decimals. But if we calculate on the number who did not die,
viz.—699,000,[128] we shall get a variation 26 times as great as this. But it
is evident the variation must be the same in each case. I submitted this kind
of problem also to the test of experiment, the results of which gave me great
faith in Poisson's formula.
Imagine two hundred pennies in a bag all heads up. Any shaking will spoil
this arrangement and give a certain proportion of tails. And, further, the
probable effect of shaking and turning will be to reduce the preponderance
of heads or tails whichever may be in excess. This of course is the reason
why we are so unlikely to get more than 120 of them in either position.
But if the two hundred pennies are increased to 20,000 by adding pennies
which have tails on both sides, then the shaking or mixing would be less
effective. We should still expect as an average result to get the 100 heads
but in 20,000 instead of 200. The variation will be 28 or 29 on the 100
instead of 20. And this is a better limit in such cases. Taking 28 as the limit
of error on 100 instances and proportionally increasing the others so that
the mean error becomes 7.8 and the probable error 5.6, we may now
calculate the answer without gross mistake.
The probable variation on the 1000 deaths by accident will be 18, the mean
variation will be 24.6, and the limits of variation 88.5. One such table
showing in five years a mean number of deaths of about 1120 per annum
gives an annual deviation of about 50 up or down of this. It will be seen at
once that an improvement of 30 or 40 in any one year would be without
meaning, but that an improvement of from 100 to 200 would indicate some
change for the better in the circumstances of the industry. Before applying
these principles to the elucidation of some of the problems of sampling it
in accord with those given; and this exception only just overstepped the
limits. It was like a case of nine trumps, which though in a sense possible, is
very unlikely to happen in any one's experience.
But even now we are not quite in a position to answer the question with
which we started. If you refer to it you will see that we are face to face with
this problem: the limit of variation on the 1000 who died would be say 70,
[127]
ignoring decimals. But if we calculate on the number who did not die,
viz.—699,000,[128] we shall get a variation 26 times as great as this. But it
is evident the variation must be the same in each case. I submitted this kind
of problem also to the test of experiment, the results of which gave me great
faith in Poisson's formula.
Imagine two hundred pennies in a bag all heads up. Any shaking will spoil
this arrangement and give a certain proportion of tails. And, further, the
probable effect of shaking and turning will be to reduce the preponderance
of heads or tails whichever may be in excess. This of course is the reason
why we are so unlikely to get more than 120 of them in either position.
But if the two hundred pennies are increased to 20,000 by adding pennies
which have tails on both sides, then the shaking or mixing would be less
effective. We should still expect as an average result to get the 100 heads
but in 20,000 instead of 200. The variation will be 28 or 29 on the 100
instead of 20. And this is a better limit in such cases. Taking 28 as the limit
of error on 100 instances and proportionally increasing the others so that
the mean error becomes 7.8 and the probable error 5.6, we may now
calculate the answer without gross mistake.
The probable variation on the 1000 deaths by accident will be 18, the mean
variation will be 24.6, and the limits of variation 88.5. One such table
showing in five years a mean number of deaths of about 1120 per annum
gives an annual deviation of about 50 up or down of this. It will be seen at
once that an improvement of 30 or 40 in any one year would be without
meaning, but that an improvement of from 100 to 200 would indicate some
change for the better in the circumstances of the industry. Before applying
these principles to the elucidation of some of the problems of sampling it
Page 553
will be well to give Poisson's formula (in a modified form) and to illustrate
its working.
Let x equal the number of cases of one sort, y the cases of the other sort, and
z the total. In the example, z will be the 700,000 engaged in the industry; x
will be the 1000 killed by accidents, and y will be the 699,000 who did not
so die. The limit of deviation or error calculated by Poisson's formula will
be the square root of 8xy/z. Replacing x, y and z by the figures of the
example we get the square root of (8×1000×699000)/700,000, which works
out to the square root of 7988.57, or 89.3. Which means that we may
reasonably expect the number of deaths not to vary from 1000 by more than
89, i.e., they will be between 1090 and 910. It will be seen that this number
is in very satisfactory agreement with 88.5 given by the rougher calculation
based on my own experiments.
To come to the question of sampling. Consider a powder of uniform
fineness and fine enough to pass through an 80 sieve. For purposes of
calculation this may be assumed to be made up of particles of about one-
eighth of a millimetre across (say roughly 1/200 of an inch); cubed, this
gives the content as about 1/500 (strictly 1/512) of a cubic m.m. Now one
cubic m.m. of water weighs 1 milligram; therefore 500 such particles if they
have the specific gravity of water weigh 1 milligram, and otherwise weigh 1
milligram multiplied by the sp. gr.: 500 particles of ruby silver (Pyrargyrite)
[129]
will weigh 5.8 milligrams and will contain nearly 3.5 milligrams of
silver.
Now suppose a portion of 3.2667 grams (1/10 Assay Ton) of silver ore to
contain 500 such particles of ruby silver and no other material carrying
silver: such an ore would contain 35 ozs. of silver to the ton. But the limits
of variation on 500 particles would be 28[130] multiplied by the square root
of 5, or 62 particles. Thus the limit of sampling error would amount to just
one-eighth of the silver present, or say to rather more than 4 ozs. to the ton;
the mean sampling error would be rather more than a quarter of this, or say
about 1.3 ozs. to the ton.
On the other hand, if one took for the assay a charge six times greater (say
about 20 grams), the number of particles would be 3000 and the limits of
variation would be 28 multiplied by the square root of 30, or 153 particles,
its working.
Let x equal the number of cases of one sort, y the cases of the other sort, and
z the total. In the example, z will be the 700,000 engaged in the industry; x
will be the 1000 killed by accidents, and y will be the 699,000 who did not
so die. The limit of deviation or error calculated by Poisson's formula will
be the square root of 8xy/z. Replacing x, y and z by the figures of the
example we get the square root of (8×1000×699000)/700,000, which works
out to the square root of 7988.57, or 89.3. Which means that we may
reasonably expect the number of deaths not to vary from 1000 by more than
89, i.e., they will be between 1090 and 910. It will be seen that this number
is in very satisfactory agreement with 88.5 given by the rougher calculation
based on my own experiments.
To come to the question of sampling. Consider a powder of uniform
fineness and fine enough to pass through an 80 sieve. For purposes of
calculation this may be assumed to be made up of particles of about one-
eighth of a millimetre across (say roughly 1/200 of an inch); cubed, this
gives the content as about 1/500 (strictly 1/512) of a cubic m.m. Now one
cubic m.m. of water weighs 1 milligram; therefore 500 such particles if they
have the specific gravity of water weigh 1 milligram, and otherwise weigh 1
milligram multiplied by the sp. gr.: 500 particles of ruby silver (Pyrargyrite)
[129]
will weigh 5.8 milligrams and will contain nearly 3.5 milligrams of
silver.
Now suppose a portion of 3.2667 grams (1/10 Assay Ton) of silver ore to
contain 500 such particles of ruby silver and no other material carrying
silver: such an ore would contain 35 ozs. of silver to the ton. But the limits
of variation on 500 particles would be 28[130] multiplied by the square root
of 5, or 62 particles. Thus the limit of sampling error would amount to just
one-eighth of the silver present, or say to rather more than 4 ozs. to the ton;
the mean sampling error would be rather more than a quarter of this, or say
about 1.3 ozs. to the ton.
On the other hand, if one took for the assay a charge six times greater (say
about 20 grams), the number of particles would be 3000 and the limits of
variation would be 28 multiplied by the square root of 30, or 153 particles,
Page 554
which is very closely 1/20 of the silver present, or say 1.75 ozs. to the ton,
whilst the mean error would amount to about .5 ozs. to the ton.
To work these examples by Poisson's formula let us assume the gangue to
have a mean sp. gr. of 3. Then 500 particles would weigh 3 milligrams; and
3.2609[131] grams would contain 543,500 particles. There would be then
500 of ruby silver and 543,500 of gangue, together 544,000, and the
formula gives the square root of (8×500×543500)/544000, which works out
to 63 particles as against 62 by the other method.
A practical conclusion from this is of course that either the ore must be
powdered more finely or a larger portion than 3 grams must be taken for the
assay. Moreover, it is evident that on such an ore no small sample must be
taken containing less than several million particles.
Consider now a copper ore of the same uniform fineness containing
particles of copper pyrites (sp. gr. 4) of which 1000 particles will weigh 8
milligrams, mixed with gangue of which 1000 particles weigh 6 milligrams.
If one gram of such ore contain .5 gram of copper pyrites (= .1725 gram
copper) and .5 gram of gangue, these will contain 62,500 and say 83,500
particles respectively. Altogether 146,000 particles. With Poisson's formula
this gives the limit of sampling error as the square root of
(8×62500×83500)/146000 or 521 particles. But a variation of 521 on
62,500 is a variation of .83 per cent. The percentage of copper in the ore is
17.25 per cent., and .83 per cent. of this is .14 per cent. The limits of
sampling error, therefore, are 17.11 per cent. and 17.39 per cent. Again, it
must be remembered that the mean sampling error would be a little over
one-quarter of this, or say from 17.2 per cent. to 17.3 per cent. The practical
conclusion is that a powder of this degree of fineness is not fine enough. In
the last place let us consider a similar iron ore containing 90 per cent. of
hæmatite (sp. gr. 5) and 10 per cent. of gangue (sp. gr. 3), 1 gram of such
ore will contain 90,000 particles of hæmatite weighing .9 gram and
containing .63 gram of iron with say 16,500 particles of gangue weighing .1
gram. Altogether 106,500 particles.
Poisson's formula then gives the limits of variation as the square root of
(8×90000×16500)/106500 or 334 particles. But 334 on 90,000 is 0.23 on
63.0, which is the percentage of iron present. The limits of sampling error
whilst the mean error would amount to about .5 ozs. to the ton.
To work these examples by Poisson's formula let us assume the gangue to
have a mean sp. gr. of 3. Then 500 particles would weigh 3 milligrams; and
3.2609[131] grams would contain 543,500 particles. There would be then
500 of ruby silver and 543,500 of gangue, together 544,000, and the
formula gives the square root of (8×500×543500)/544000, which works out
to 63 particles as against 62 by the other method.
A practical conclusion from this is of course that either the ore must be
powdered more finely or a larger portion than 3 grams must be taken for the
assay. Moreover, it is evident that on such an ore no small sample must be
taken containing less than several million particles.
Consider now a copper ore of the same uniform fineness containing
particles of copper pyrites (sp. gr. 4) of which 1000 particles will weigh 8
milligrams, mixed with gangue of which 1000 particles weigh 6 milligrams.
If one gram of such ore contain .5 gram of copper pyrites (= .1725 gram
copper) and .5 gram of gangue, these will contain 62,500 and say 83,500
particles respectively. Altogether 146,000 particles. With Poisson's formula
this gives the limit of sampling error as the square root of
(8×62500×83500)/146000 or 521 particles. But a variation of 521 on
62,500 is a variation of .83 per cent. The percentage of copper in the ore is
17.25 per cent., and .83 per cent. of this is .14 per cent. The limits of
sampling error, therefore, are 17.11 per cent. and 17.39 per cent. Again, it
must be remembered that the mean sampling error would be a little over
one-quarter of this, or say from 17.2 per cent. to 17.3 per cent. The practical
conclusion is that a powder of this degree of fineness is not fine enough. In
the last place let us consider a similar iron ore containing 90 per cent. of
hæmatite (sp. gr. 5) and 10 per cent. of gangue (sp. gr. 3), 1 gram of such
ore will contain 90,000 particles of hæmatite weighing .9 gram and
containing .63 gram of iron with say 16,500 particles of gangue weighing .1
gram. Altogether 106,500 particles.
Poisson's formula then gives the limits of variation as the square root of
(8×90000×16500)/106500 or 334 particles. But 334 on 90,000 is 0.23 on
63.0, which is the percentage of iron present. The limits of sampling error
Page 555
then are 62.77 per cent. and 63.23 per cent. and the mean variation is from
62.94 per cent. to 63.06 per cent.
These examples are worthy of careful consideration, and it must be
remembered that the calculations are made on the assumption that the ore is
made up of uniform particles of mineral of such fineness as would pass
easily through an 80 sieve, but which does not pretend to represent with
great exactness the fineness of the powdered ore customary in practice.
They show that having passed through such a sieve is no proof of sufficient
powdering, not that all ores powdered and so sifted are unfit for assaying.
This last would be an absurd and illogical conclusion.
If an ore be powdered to a fairly fine sand and then be passed through a
series of sieves, say a 40, 60, and 80, in such a state that little or none
remains on the first, but the others retain a large proportion; then of that
which comes through the 80 sieve, perhaps two-thirds by weight may be
even coarser than the powder I have used in the example. Of the rest most
may be of about half this diameter; the weight of the really fine powder
may be quite inconsiderable. On the other hand, if the grinding be
continued until, on sifting, little or nothing that is powderable remains on
the sieves; then in the sifted product the proportions will be very different.
This last, of course, is the only right way of powdering. Also it is evident
that so much depends on the manner of powdering that nothing precise can
be stated as to the average coarseness of the powder. Suppose, however, by
good powdering a product is obtained which may be represented by a
uniform powder with particles 1/20th of a millimetre in diameter (say
roughly 1/500 inch). Compared with the previous powder, the diameter has
been divided by 2.5; their number, therefore, in any given weight has been
increased by the cube of 2.5, which is 15.6. But the value of a sample varies
as the square root of the number of particles. Hence the reduction in size
and consequent increase in number has made the sample nearly four times
better than before; and it will be seen that this brings the sampling error
within tolerable limits.
There are one or two words of warning which should be given. In the first
place, using a 90 sieve instead of an 80 must not be too much relied on; the
powder I took in the example would pass through it. It is a question of good
powdering rather than of fine sifting. In the second place, a set of, say half-
62.94 per cent. to 63.06 per cent.
These examples are worthy of careful consideration, and it must be
remembered that the calculations are made on the assumption that the ore is
made up of uniform particles of mineral of such fineness as would pass
easily through an 80 sieve, but which does not pretend to represent with
great exactness the fineness of the powdered ore customary in practice.
They show that having passed through such a sieve is no proof of sufficient
powdering, not that all ores powdered and so sifted are unfit for assaying.
This last would be an absurd and illogical conclusion.
If an ore be powdered to a fairly fine sand and then be passed through a
series of sieves, say a 40, 60, and 80, in such a state that little or none
remains on the first, but the others retain a large proportion; then of that
which comes through the 80 sieve, perhaps two-thirds by weight may be
even coarser than the powder I have used in the example. Of the rest most
may be of about half this diameter; the weight of the really fine powder
may be quite inconsiderable. On the other hand, if the grinding be
continued until, on sifting, little or nothing that is powderable remains on
the sieves; then in the sifted product the proportions will be very different.
This last, of course, is the only right way of powdering. Also it is evident
that so much depends on the manner of powdering that nothing precise can
be stated as to the average coarseness of the powder. Suppose, however, by
good powdering a product is obtained which may be represented by a
uniform powder with particles 1/20th of a millimetre in diameter (say
roughly 1/500 inch). Compared with the previous powder, the diameter has
been divided by 2.5; their number, therefore, in any given weight has been
increased by the cube of 2.5, which is 15.6. But the value of a sample varies
as the square root of the number of particles. Hence the reduction in size
and consequent increase in number has made the sample nearly four times
better than before; and it will be seen that this brings the sampling error
within tolerable limits.
There are one or two words of warning which should be given. In the first
place, using a 90 sieve instead of an 80 must not be too much relied on; the
powder I took in the example would pass through it. It is a question of good
powdering rather than of fine sifting. In the second place, a set of, say half-
Page 556
a-dozen, assays concordant within 1 oz. where the theory gives 4 ozs. as the
limit of error does not upset the theory: the theory itself states this as likely.
It is the error you may get in one or two assays out of a hundred, not the
error you are likely to get in any one assay, which is considered under the
heading "limit of error."
Accepting the result just arrived at that a portion of 1 gram may be safely
taken for an assay if the particles are 1-20th of a millimetre in diameter, the
further question remains as to what weight of the original sample must be
reduced to this degree of fineness. This may be answered on the principle
that the same degree of excellence should be aimed at in each of a series of
samplings. This principle is illustrated in the table on page 2.[** PP: page
reference]
A fine sand, such as would pass a 40 sieve but be retained on a 60 sieve,
would be fairly represented by particles one-quarter of a millimetre in
diameter. This being five times coarser, to contain the same number of
particles must be 125 times (the cube of 5) as heavy; therefore 125 grams of
it can be taken with the same degree of safety as 1 gram of the finer powder.
Of such a sand about this weight should be taken and reduced to the finer
powder. If the ore were in coarse sand, say in particles 1 millimetre in
diameter, this would be four times as coarse as that last considered, and we
should have to take 64 times as much of it: 64 times 125 grams is 8 kilos, or
say roughly from 15 to 20 lbs. This should be crushed to the finer size and
mixed; then from 100 to 150 grams should be taken and ground to the finest
powder.
There is, however, a reason why, on the coarser stuff, a smaller proportion
may safely be used. This becomes more evident if we consider a still
coarser sample. A heap of ore in stones about 2 inches across would be 50
times coarser than the sand, and an equivalent sample would need to be
125,000 times heavier; this would amount to about 1000 tons. Experienced
samplers would say that under such conditions so large a sample was hardly
necessary.
This is because I have assumed in the calculations that the grains of copper
pyrites, for example, were all copper pyrites and the particles of gangue
were free from copper. This would be true or nearly so for the very fine
limit of error does not upset the theory: the theory itself states this as likely.
It is the error you may get in one or two assays out of a hundred, not the
error you are likely to get in any one assay, which is considered under the
heading "limit of error."
Accepting the result just arrived at that a portion of 1 gram may be safely
taken for an assay if the particles are 1-20th of a millimetre in diameter, the
further question remains as to what weight of the original sample must be
reduced to this degree of fineness. This may be answered on the principle
that the same degree of excellence should be aimed at in each of a series of
samplings. This principle is illustrated in the table on page 2.[** PP: page
reference]
A fine sand, such as would pass a 40 sieve but be retained on a 60 sieve,
would be fairly represented by particles one-quarter of a millimetre in
diameter. This being five times coarser, to contain the same number of
particles must be 125 times (the cube of 5) as heavy; therefore 125 grams of
it can be taken with the same degree of safety as 1 gram of the finer powder.
Of such a sand about this weight should be taken and reduced to the finer
powder. If the ore were in coarse sand, say in particles 1 millimetre in
diameter, this would be four times as coarse as that last considered, and we
should have to take 64 times as much of it: 64 times 125 grams is 8 kilos, or
say roughly from 15 to 20 lbs. This should be crushed to the finer size and
mixed; then from 100 to 150 grams should be taken and ground to the finest
powder.
There is, however, a reason why, on the coarser stuff, a smaller proportion
may safely be used. This becomes more evident if we consider a still
coarser sample. A heap of ore in stones about 2 inches across would be 50
times coarser than the sand, and an equivalent sample would need to be
125,000 times heavier; this would amount to about 1000 tons. Experienced
samplers would say that under such conditions so large a sample was hardly
necessary.
This is because I have assumed in the calculations that the grains of copper
pyrites, for example, were all copper pyrites and the particles of gangue
were free from copper. This would be true or nearly so for the very fine
Page 557
powder, but far from true in the case of the ore heap. In the heap probably
few of the stones would be pure ore and still fewer would be free from
copper. The stones would differ among themselves in their copper contents
only within certain comparatively narrow limits. And it is evident that, if
replacing one stone by another, instead of resulting in the gain or loss of all
the copper one or other contained, merely affected the result to one-tenth of
this amount, then a sample of 1-100th of the weight (say 10 tons) would be
equally safe.
It should be remembered, however, that while the man who samples on a
large scale can safely and properly reduce the size of his samples on this
account, yet the principle is one which counts less and less as the stuff
becomes more finely divided, and ought to be ignored in the working down
of the smaller samples which come to the assayer.
FOOTNOTES:
[126] The 10 in 20 multiplied by 10 = 100 in 200.
[127] Multiply the errors for 100 by the square root of 10.
[128] Multiply the errors for 100 by the square root of 6990.
[129] Sp. Gr. 5.8. Silver 60 per cent.
[130] Taking 28 as the limit of variation on 100.
[131] The weight of the ore less the weight of ruby silver in it.
few of the stones would be pure ore and still fewer would be free from
copper. The stones would differ among themselves in their copper contents
only within certain comparatively narrow limits. And it is evident that, if
replacing one stone by another, instead of resulting in the gain or loss of all
the copper one or other contained, merely affected the result to one-tenth of
this amount, then a sample of 1-100th of the weight (say 10 tons) would be
equally safe.
It should be remembered, however, that while the man who samples on a
large scale can safely and properly reduce the size of his samples on this
account, yet the principle is one which counts less and less as the stuff
becomes more finely divided, and ought to be ignored in the working down
of the smaller samples which come to the assayer.
FOOTNOTES:
[126] The 10 in 20 multiplied by 10 = 100 in 200.
[127] Multiply the errors for 100 by the square root of 10.
[128] Multiply the errors for 100 by the square root of 6990.
[129] Sp. Gr. 5.8. Silver 60 per cent.
[130] Taking 28 as the limit of variation on 100.
[131] The weight of the ore less the weight of ruby silver in it.
Page 558
INDEX.
Acid measures, 49
Acidimetry, 323
Acidity of ores, 168
Acids, 54
strength of, 54, 75, 436
Air of mines, carbonic acid in, 428
Alkalies, 330
determination of, 331
Lawrence Smith's method for, 333, 412
separation of, 332
Alkalimetry, 323
Alkaline earths, 320
Alumina, 314
determination of, 315
in mineral phosphates, 316
separation of, 314, 316
Amalgamation, 126
Ammonia, detection of, 341
determination of, 342
in natural waters, 353
Antimony, 225
Acid measures, 49
Acidimetry, 323
Acidity of ores, 168
Acids, 54
strength of, 54, 75, 436
Air of mines, carbonic acid in, 428
Alkalies, 330
determination of, 331
Lawrence Smith's method for, 333, 412
separation of, 332
Alkalimetry, 323
Alkaline earths, 320
Alumina, 314
determination of, 315
in mineral phosphates, 316
separation of, 314, 316
Amalgamation, 126
Ammonia, detection of, 341
determination of, 342
in natural waters, 353
Antimony, 225
Page 559
detection of, 227
dry assay for, 226
gravimetric assay, 228
separation of, 228
volumetric assay, 229
Arsenic, 381
detection of, 381
dry assay for, 382
gravimetric assay, 383
in brimstone, 393
in crude arsenic, 388, 393
in mispickel, 125, 392
iodine, assay for, 386
separation by distilling, 384
uranium acetate, assay for, 389
Volhard's method applied to, 124
Assay book, 11
note, 12
results, 7
tons, 13, 131
Assaying, 1
methods, 15
Assays, check, 154
preliminary, 147
Atomic weights, 69
table of, 433
Barium, 326
Baryta, 326
dry assay for, 226
gravimetric assay, 228
separation of, 228
volumetric assay, 229
Arsenic, 381
detection of, 381
dry assay for, 382
gravimetric assay, 383
in brimstone, 393
in crude arsenic, 388, 393
in mispickel, 125, 392
iodine, assay for, 386
separation by distilling, 384
uranium acetate, assay for, 389
Volhard's method applied to, 124
Assay book, 11
note, 12
results, 7
tons, 13, 131
Assaying, 1
methods, 15
Assays, check, 154
preliminary, 147
Atomic weights, 69
table of, 433
Barium, 326
Baryta, 326
Page 560
Barytes, sulphur in, 378
Base bullion, sampling of, 157
Basic acetate separation, 233
Baumé's hydrometer, 77
Beryllia, 319
Bismuth, 220
colorimetric assay, 223
detection of, 221
gravimetric determination of, 222
in commercial copper, 208
separation of, 222
Black tin, 271
an analysis of, 287
assay of, 276
copper in, 204
examination of, 285
separation by vanning, 272
Blank assays, 34
Blende, sulphur in, 375
zinc in, 266
Book, assay, 11
laboratory, 10
sample, 9
Boracic acid. See Boron
Borax, examination of, 431
Base bullion, sampling of, 157
Basic acetate separation, 233
Baumé's hydrometer, 77
Beryllia, 319
Bismuth, 220
colorimetric assay, 223
detection of, 221
gravimetric determination of, 222
in commercial copper, 208
separation of, 222
Black tin, 271
an analysis of, 287
assay of, 276
copper in, 204
examination of, 285
separation by vanning, 272
Blank assays, 34
Blende, sulphur in, 375
zinc in, 266
Book, assay, 11
laboratory, 10
sample, 9
Boracic acid. See Boron
Borax, examination of, 431
Page 561
Boron, 429
direct determination of, 431
Brass, copper in, 194
zinc in, 265
Bromine and bromides, 361
Bronze, copper in, 194
tin in, 281
Burettes, 51
Burnt ore, silver in, 116, 118
sulphur in, 377
Cadmium, 269
gravimetric determination, 269
separation of, 269
Caesium, 339
Calcination, 22, 92, 139, 345
Calcium, 320
detection of, 321
gravimetric determination, 321
separation of, 321
titration with normal acid, 322
titration with permanganate, 322
Calculation of results, 7
Calculations from formulæ, 70
Calorific effect of coal, 419
direct determination of, 431
Brass, copper in, 194
zinc in, 265
Bromine and bromides, 361
Bronze, copper in, 194
tin in, 281
Burettes, 51
Burnt ore, silver in, 116, 118
sulphur in, 377
Cadmium, 269
gravimetric determination, 269
separation of, 269
Caesium, 339
Calcination, 22, 92, 139, 345
Calcium, 320
detection of, 321
gravimetric determination, 321
separation of, 321
titration with normal acid, 322
titration with permanganate, 322
Calculation of results, 7
Calculations from formulæ, 70
Calorific effect of coal, 419
Page 562
Calorimeter, 419
Calx, 345
Carbon, 414
gravimetric determination, 416
in iron or steel, 423
Carbonates, 424
Carbonic acid in the air of mines, 428
Caustic potash = potassium hydroxide, 65
Caustic soda = sodium hydroxide, 66
Cerium, 318
Chalybite, iron in, 243
Charcoal, 21, 94
Check assays for gold, 154
for silver, 104, 113
Chlorine and chlorides, 359
Chromium, 307
gravimetric assay, 309
in chrome iron ore, 308
volumetric assay, 309
Clays, examination of, 316
Coals, 418
Calx, 345
Carbon, 414
gravimetric determination, 416
in iron or steel, 423
Carbonates, 424
Carbonic acid in the air of mines, 428
Caustic potash = potassium hydroxide, 65
Caustic soda = sodium hydroxide, 66
Cerium, 318
Chalybite, iron in, 243
Charcoal, 21, 94
Check assays for gold, 154
for silver, 104, 113
Chlorine and chlorides, 359
Chromium, 307
gravimetric assay, 309
in chrome iron ore, 308
volumetric assay, 309
Clays, examination of, 316
Coals, 418
Page 563
Cobalt, 259
detection of, 259
dry assay for, 251
gravimetric determination, 260
in hardhead, 288
separation from nickel, 442, 254, 258
Coke, 25
Common salt, examination of, 336
Concentrates, assay for gold of, 140
Colorimetric assays, 44
Copper, 175
Copper, bismuth in, 208
colorimetric assay for, 190, 203
commercial, arsenic in, 208, 388
commercial, copper in, 193
commercial, examination of, 205
cyanide assay for, 194
dry assay of, 176
dry assay, loss of, in, 176
electrolytic assay for, 190, 203
gold in, 206
iodide assay for, 199
iron in, 209, 249
lead in, 206
separation of, 183
silver in, 205
sulphur in, 207
Copper ores, solution of, 183
valuation of, 181
detection of, 259
dry assay for, 251
gravimetric determination, 260
in hardhead, 288
separation from nickel, 442, 254, 258
Coke, 25
Common salt, examination of, 336
Concentrates, assay for gold of, 140
Colorimetric assays, 44
Copper, 175
Copper, bismuth in, 208
colorimetric assay for, 190, 203
commercial, arsenic in, 208, 388
commercial, copper in, 193
commercial, examination of, 205
cyanide assay for, 194
dry assay of, 176
dry assay, loss of, in, 176
electrolytic assay for, 190, 203
gold in, 206
iodide assay for, 199
iron in, 209, 249
lead in, 206
separation of, 183
silver in, 205
sulphur in, 207
Copper ores, solution of, 183
valuation of, 181
Page 564
Copper pyrites, copper in, 179, 188, 198, 202
sulphur in, 376
Culm, 22
Cupel, 23, 142
Cupellation, loss, corrections for, 103
loss in gold, 145
loss in silver, 101
of gold lead alloys, 182
of silver lead alloys, 98, 110
temperature of, 143
Cyanicides, 169
Cyanide assay for copper, 194
for nickel, 255
for tin, 278
Cyanides, alkalinity of, 167
assay of, 167
commercial, 160
double, 161
gold-dissolving power, 162
prussic acid, 162
volumetric determination of, 163, 165
Cyanide liquors, alkalinity of, 167
assay of, 164, 165
assay of, for gold, 140
assay of, for zinc, &c., 169
Daniell cells, 185
Didymium, 319
sulphur in, 376
Culm, 22
Cupel, 23, 142
Cupellation, loss, corrections for, 103
loss in gold, 145
loss in silver, 101
of gold lead alloys, 182
of silver lead alloys, 98, 110
temperature of, 143
Cyanicides, 169
Cyanide assay for copper, 194
for nickel, 255
for tin, 278
Cyanides, alkalinity of, 167
assay of, 167
commercial, 160
double, 161
gold-dissolving power, 162
prussic acid, 162
volumetric determination of, 163, 165
Cyanide liquors, alkalinity of, 167
assay of, 164, 165
assay of, for gold, 140
assay of, for zinc, &c., 169
Daniell cells, 185
Didymium, 319
Page 565
Dollars to the ton, 9
Dry assays, 16
Drying, 5, 33
Earths, 314
the alkaline, 320
Electrodes, 187
Electrolysis for copper, 184
for nickel, 254
Equations, 69
Erbia, 319
Ferrous and ferric salts, 231
Filtration, 31
Finishing point, 42
Flasks, graduated, 49
Flatting, 149
Fluorine and fluorides, 363
Fluxes, 16, 93, 136, 138, 140
Formulæ, 68
Dry assays, 16
Drying, 5, 33
Earths, 314
the alkaline, 320
Electrodes, 187
Electrolysis for copper, 184
for nickel, 254
Equations, 69
Erbia, 319
Ferrous and ferric salts, 231
Filtration, 31
Finishing point, 42
Flasks, graduated, 49
Flatting, 149
Fluorine and fluorides, 363
Fluxes, 16, 93, 136, 138, 140
Formulæ, 68
Page 566
Furnaces, 25
Galena, lead in, 217, 218
Gangue, 405
iron in the, 244
Gas-measuring apparatus, 52
Gases, measurement of, 44
Gay-Lussac's assay for silver, 119
assay for silver modified, 123
German silver, copper in, 194
nickel in, 255, 259
Gold, 126
amalgamation of, 126
in cyanide liquor, 140
loss of, in cupellation, 145
loss of, in parting, 154
preparation of, 63
silver in, 157
silver in, after parting, 154
test for, 126
Gold-lead alloys, cupellation of, 142
sampling of, 158
Gold ores assay with cyanide solutions, 141
calcination of, 139
concentrates, 140
fluxing, 136, 138, 140
sampling of, 127
size of assay charges, 127
Galena, lead in, 217, 218
Gangue, 405
iron in the, 244
Gas-measuring apparatus, 52
Gases, measurement of, 44
Gay-Lussac's assay for silver, 119
assay for silver modified, 123
German silver, copper in, 194
nickel in, 255, 259
Gold, 126
amalgamation of, 126
in cyanide liquor, 140
loss of, in cupellation, 145
loss of, in parting, 154
preparation of, 63
silver in, 157
silver in, after parting, 154
test for, 126
Gold-lead alloys, cupellation of, 142
sampling of, 158
Gold ores assay with cyanide solutions, 141
calcination of, 139
concentrates, 140
fluxing, 136, 138, 140
sampling of, 127
size of assay charges, 127
Page 567
tailings, 140
Gold-parting, 150
platinum in, 145, 154, 170, 171
Gold-zinc slimes, 142
Graduated vessels, 49
Gravimetric methods, 15, 27
Halogens, 358
Hardhead, 287
an analysis of, 289
Hot plate, 30
Hydrogen, preparation of, 62
reduction by, 280
Hydrometer, 77
Ignition, 32
in hydrogen, 280
Indicators, 42
Inquartation, 146
Iodine and iodides, 362
Iridium, 171
Iron, 231
Gold-parting, 150
platinum in, 145, 154, 170, 171
Gold-zinc slimes, 142
Graduated vessels, 49
Gravimetric methods, 15, 27
Halogens, 358
Hardhead, 287
an analysis of, 289
Hot plate, 30
Hydrogen, preparation of, 62
reduction by, 280
Hydrometer, 77
Ignition, 32
in hydrogen, 280
Indicators, 42
Inquartation, 146
Iodine and iodides, 362
Iridium, 171
Iron, 231
Page 568
bichromate assay for, 237, 243,
carbon in, 423
colorimetric assay for, 247
ferrous and ferric, 231
gravimetric determination, 233
permanganate assay for, 236, 238
phosphorus in, 399
reduction of ferric solutions, 235, 241
separation of, 232
stannous chloride assay for, 244
volumetric assays for, 234
Iron ores, iron in, 244, 247
phosphates in, 399
Laboratory books, 9
Lanthanum, 319
Lawrence Smith's method for alkalies, 333, 412
Lead, 211
colorimetric assay for, 218
detection of, 211
dry assay for, 211
gravimetric determination of, 213
in commercial copper, 206
in commercial zinc, 214
in galena, 217, 218
separation of, 211, 213
volumetric determination of, 214
Litharge, use of, in dry assays, 20, 93
Lithium, 338
carbon in, 423
colorimetric assay for, 247
ferrous and ferric, 231
gravimetric determination, 233
permanganate assay for, 236, 238
phosphorus in, 399
reduction of ferric solutions, 235, 241
separation of, 232
stannous chloride assay for, 244
volumetric assays for, 234
Iron ores, iron in, 244, 247
phosphates in, 399
Laboratory books, 9
Lanthanum, 319
Lawrence Smith's method for alkalies, 333, 412
Lead, 211
colorimetric assay for, 218
detection of, 211
dry assay for, 211
gravimetric determination of, 213
in commercial copper, 206
in commercial zinc, 214
in galena, 217, 218
separation of, 211, 213
volumetric determination of, 214
Litharge, use of, in dry assays, 20, 93
Lithium, 338
Page 569
Lime, 320
milk of, 321
volumetric assays for, 322
Limestone, examination of, 329
lime in, 324
Limewater, 321
Loths, 9
Magnesia, magnesium, 328
mixture, preparation of, 64
Manganese, 298
colorimetric assay, 306
detection of, 299
gravimetric determination of, 300
separation of, 299
volumetric determination of, 300
Manganese peroxide, ferrous sulphate assay for, 301
iodine assay for, 302
= manganese dioxide, 298
Manganese ore, copper in, 204
manganese in, 300
peroxide in, 302
Matte, 18
Measuring, 49
flasks, 49
gases, 44, 52
gold buttons, 133, 440,
liquids, 49
milk of, 321
volumetric assays for, 322
Limestone, examination of, 329
lime in, 324
Limewater, 321
Loths, 9
Magnesia, magnesium, 328
mixture, preparation of, 64
Manganese, 298
colorimetric assay, 306
detection of, 299
gravimetric determination of, 300
separation of, 299
volumetric determination of, 300
Manganese peroxide, ferrous sulphate assay for, 301
iodine assay for, 302
= manganese dioxide, 298
Manganese ore, copper in, 204
manganese in, 300
peroxide in, 302
Matte, 18
Measuring, 49
flasks, 49
gases, 44, 52
gold buttons, 133, 440,
liquids, 49
Page 570
silver buttons, 106
Mechanical methods, 16
Mercury, 171
dry assay, 172
wet assay, 173
Metallic particles in ores, gold, 129
particles in ores, silver, 108
particles, tin, 278, 287
Micrometer, 133
Microscope, measuring with the, 440, 133
Mispickel, arsenic in, 125, 392
sulphur in, 376
Moisture, 7, 350
Molybdate separation for phosphates, 395
solution, preparation of, 60
Molybdenum, 311
Muffle, 25
Nessler's solution, 342
Nickel, 251
dry assay for, 251
electrolytic assay, 254
gravimetric determination of, 254
in German silver, 255, 259
separation from cobalt, 254, 258, 442
Mechanical methods, 16
Mercury, 171
dry assay, 172
wet assay, 173
Metallic particles in ores, gold, 129
particles in ores, silver, 108
particles, tin, 278, 287
Micrometer, 133
Microscope, measuring with the, 440, 133
Mispickel, arsenic in, 125, 392
sulphur in, 376
Moisture, 7, 350
Molybdate separation for phosphates, 395
solution, preparation of, 60
Molybdenum, 311
Muffle, 25
Nessler's solution, 342
Nickel, 251
dry assay for, 251
electrolytic assay, 254
gravimetric determination of, 254
in German silver, 255, 259
separation from cobalt, 254, 258, 442
Page 571
separation from iron, 258
separation from manganese, 258
separation of, 253
volumetric assay, 255
Niobium, 297
Nitre, 22
use of, in dry assays, 95
Nitrogen and nitrates, 400
Nitrometer, 403
Normal acid, normal solutions, 323
Ores, determining water in, 5, 351
drying, 5
powdering, 4, 109, 130, 448
quantities of, for an assay, 11, 27, 127
sampling, 1, 127, 444
with metallic particles, 3, 108, 129
Osmiridium, 171
Osmium, 171
Ounces to the ton, long, 107
to the ton, short, 132
Oxidation, 345
Oxides, 345
determination of oxygen in, 346
Oxidising agents, 22, 95, 345
separation from manganese, 258
separation of, 253
volumetric assay, 255
Niobium, 297
Nitre, 22
use of, in dry assays, 95
Nitrogen and nitrates, 400
Nitrometer, 403
Normal acid, normal solutions, 323
Ores, determining water in, 5, 351
drying, 5
powdering, 4, 109, 130, 448
quantities of, for an assay, 11, 27, 127
sampling, 1, 127, 444
with metallic particles, 3, 108, 129
Osmiridium, 171
Osmium, 171
Ounces to the ton, long, 107
to the ton, short, 132
Oxidation, 345
Oxides, 345
determination of oxygen in, 346
Oxidising agents, 22, 95, 345
Page 572
effect of nitre, 95
effect of nitric acid, 56
Oxygen, 344
equivalent, 358
in natural waters, 344, 356
in ores, 348
Palladium, 171
Parting, 150
acids, 150
in flasks, 151
in glazed crucibles, 153
in special apparatus, 156
in test tubes, 152
Phosphate, assay of apatite for, 399
assay of iron ore for, 399
Phosphates, gravimetric assay, 396
volumetric assay, 397
Phosphorus and phosphates, 394
in iron, 399
Pipette, 50, 120
Platinum, 170
in gold, 145, 154, 170
Potash, commercial examination of, 338
Potassium, 336
gravimetric determination, 337
effect of nitric acid, 56
Oxygen, 344
equivalent, 358
in natural waters, 344, 356
in ores, 348
Palladium, 171
Parting, 150
acids, 150
in flasks, 151
in glazed crucibles, 153
in special apparatus, 156
in test tubes, 152
Phosphate, assay of apatite for, 399
assay of iron ore for, 399
Phosphates, gravimetric assay, 396
volumetric assay, 397
Phosphorus and phosphates, 394
in iron, 399
Pipette, 50, 120
Platinum, 170
in gold, 145, 154, 170
Potash, commercial examination of, 338
Potassium, 336
gravimetric determination, 337
Page 573
Potassium cyanide, 22, 65, 160
commercial assay of, 167
commercial, purity of, 161
Powdering, 4, 130, 448, 109
Precipitation, 30
Precipitates, drying, 32
igniting, 32, 34
washing, 31
Preliminary assays, 104, 147
Preparation of acids, 54
of other reagents, 59
Prill, 108, 129, 278, 287
Produce, 8
Pyrarsenate of magnesia, 383
Pyrites, iron in, 244
sulphur in, 370, 376
Pyrophosphate of magnesia, 397
Quantity to be taken for an assay, 11, 27, 127
Quartation, 146
Quartering, 2
Reagents, strength of, 54
commercial assay of, 167
commercial, purity of, 161
Powdering, 4, 130, 448, 109
Precipitation, 30
Precipitates, drying, 32
igniting, 32, 34
washing, 31
Preliminary assays, 104, 147
Preparation of acids, 54
of other reagents, 59
Prill, 108, 129, 278, 287
Produce, 8
Pyrarsenate of magnesia, 383
Pyrites, iron in, 244
sulphur in, 370, 376
Pyrophosphate of magnesia, 397
Quantity to be taken for an assay, 11, 27, 127
Quartation, 146
Quartering, 2
Reagents, strength of, 54
Page 574
Red lead for dry assays, 20, 22, 94
Reducing agents, 21, 94
effects of charcoal, &c., 94
effect of mineral sulphides, 95, 97, 98
Reduction by hydrogen, 280
of ferric solutions, 235, 242, 244
Regulus, 18
Report form, 12
Results, calculation of, 7, 13, 16, 38, 107, 131, 132
statement of, 7
Rhodium, 171
Roasting, 22, 345
Rolling, 149
Rubidium, 340
Ruthenium, 171
Sample book, 9
Sampling, 1
effect of powdering on, 449
errors, 447
gold ores, 127
metals, 157
theory of, 444
Reducing agents, 21, 94
effects of charcoal, &c., 94
effect of mineral sulphides, 95, 97, 98
Reduction by hydrogen, 280
of ferric solutions, 235, 242, 244
Regulus, 18
Report form, 12
Results, calculation of, 7, 13, 16, 38, 107, 131, 132
statement of, 7
Rhodium, 171
Roasting, 22, 345
Rolling, 149
Rubidium, 340
Ruthenium, 171
Sample book, 9
Sampling, 1
effect of powdering on, 449
errors, 447
gold ores, 127
metals, 157
theory of, 444
Page 575
Scorification of silver ores, 88
Scorifier, 23, 89
Selenium, 379
Separation, as sulphides, 57
basic acetate, 233
molybdate, 395
Shales, bituminous, 420
Silicon and silicates, 405
in iron, 414
Silica in rocks, 409
in slags, 414
Silicates, alkalies in, 333, 412
beryllia in, 320
examination of, 409
titanium in, 411
Silver, 87
correction for cupellation loss, 103
detection of, 87
Gay-Lussac's assay, 119
Gay-Lussac's assay modified, 123
gravimetric determination of, 117
in bullion, 113
in burnt ore, 116, 118
in copper, 114, 205
in galena, 114
in lead, 113
in oxide of lead, 113
in silver precipitate, 115
loss in cupellation, 101
Scorifier, 23, 89
Selenium, 379
Separation, as sulphides, 57
basic acetate, 233
molybdate, 395
Shales, bituminous, 420
Silicon and silicates, 405
in iron, 414
Silica in rocks, 409
in slags, 414
Silicates, alkalies in, 333, 412
beryllia in, 320
examination of, 409
titanium in, 411
Silver, 87
correction for cupellation loss, 103
detection of, 87
Gay-Lussac's assay, 119
Gay-Lussac's assay modified, 123
gravimetric determination of, 117
in bullion, 113
in burnt ore, 116, 118
in copper, 114, 205
in galena, 114
in lead, 113
in oxide of lead, 113
in silver precipitate, 115
loss in cupellation, 101
Page 576
pure preparation of, 66
Volhard's assay, 121
volumetric methods, 119, 121, 123
Silver lead alloys, cupellation of, 98
sampling of, 157
Silver ore, crucible assay of, 90
metallic particles in, 108
scorification of, 88
Size of assay charges, 11, 27, 127
Slags, 19
Soda-lime, 425
Sodium, 334
Sodium cyanide, 160
Solution, 29
Solutions, normal, 323
standard, 36
Specific gravity, 75, 436
Speise, 19
Standard, 37
solutions, 36
Standardising, 37
Steel, carbon in, 423
chromium in, 310
Volhard's assay, 121
volumetric methods, 119, 121, 123
Silver lead alloys, cupellation of, 98
sampling of, 157
Silver ore, crucible assay of, 90
metallic particles in, 108
scorification of, 88
Size of assay charges, 11, 27, 127
Slags, 19
Soda-lime, 425
Sodium, 334
Sodium cyanide, 160
Solution, 29
Solutions, normal, 323
standard, 36
Specific gravity, 75, 436
Speise, 19
Standard, 37
solutions, 36
Standardising, 37
Steel, carbon in, 423
chromium in, 310
Page 577
manganese in, 300
Stoking, 25, 143
Strength of reagents, 54
Strontium, 324
Sulphates and sulphur, 367
gravimetric determination, 369
volumetric determination, 370
Sulphides, reducing action of, 9, 95
Sulphocyanate assay for silver, 121
Sulphur in blende, 375
in burnt ore, 377
in chalcocite, 376
in coal, 419
in copper, 207
in copper pyrites, 376
in mispickel, 376
in pyrites, 370, 376
Sulphuretted hydrogen, preparation, 57
Surcharge, 154
System in assaying, 28
Table, atomic weights, 433
comparing thermometers, 435
ounces to the long ton, 107
ounces to the short ton, 132
sp. g. ammonia, 438
Stoking, 25, 143
Strength of reagents, 54
Strontium, 324
Sulphates and sulphur, 367
gravimetric determination, 369
volumetric determination, 370
Sulphides, reducing action of, 9, 95
Sulphocyanate assay for silver, 121
Sulphur in blende, 375
in burnt ore, 377
in chalcocite, 376
in coal, 419
in copper, 207
in copper pyrites, 376
in mispickel, 376
in pyrites, 370, 376
Sulphuretted hydrogen, preparation, 57
Surcharge, 154
System in assaying, 28
Table, atomic weights, 433
comparing thermometers, 435
ounces to the long ton, 107
ounces to the short ton, 132
sp. g. ammonia, 438
Page 578
sp. g. hydrochloric acid, 437
sp. g. minerals, 86
sp. g. nitric acid, 436
sp. g. sulphuric acid, 439
sp. g. water, 83
Tantalum, 297
Tartar, 20, 94
Tellurium, 379
improved test for, 150
Thallium, 219
Thorium, 317
Tin, 271 See also Black tin
assay for, by vanning, 273
copper in, 204
Cornish assay, 276
cyanide assay, 278
detection of, 279
gravimetric determination of, 281
iron in, 250
separation of, 280
volumetric assay for, 282
Tin arsenide, 284
Tin phosphide, 284
Tin slag, 290
an analysis of, 292
tin in, 290
Titanium, 292
sp. g. minerals, 86
sp. g. nitric acid, 436
sp. g. sulphuric acid, 439
sp. g. water, 83
Tantalum, 297
Tartar, 20, 94
Tellurium, 379
improved test for, 150
Thallium, 219
Thorium, 317
Tin, 271 See also Black tin
assay for, by vanning, 273
copper in, 204
Cornish assay, 276
cyanide assay, 278
detection of, 279
gravimetric determination of, 281
iron in, 250
separation of, 280
volumetric assay for, 282
Tin arsenide, 284
Tin phosphide, 284
Tin slag, 290
an analysis of, 292
tin in, 290
Titanium, 292
Page 579
detection of, 293
in black tin, 272, 287
in rocks, 411
separation, &c., 294
Titration, 35
indirect, 43, 72
Ton, assay, 13, 131,
long, 2240 lbs. = 32,666.6 oz., 107
short, 2000 lbs = 29,166.6 oz., 132
Tungsten, 295
Tungstic acid, 295
gravimetric determination, 296
in black tin, 285
in wolfram, 296
Uranium, 312
Valuation, of copper ores, 181
Vanadium, 310
Vanning, 273
Volhard's assay applied to arsenic, 124
silver assay, 121
Volume-corrector, 53
Volumetric assay, 35, 38
Water, 7, 350
in black tin, 272, 287
in rocks, 411
separation, &c., 294
Titration, 35
indirect, 43, 72
Ton, assay, 13, 131,
long, 2240 lbs. = 32,666.6 oz., 107
short, 2000 lbs = 29,166.6 oz., 132
Tungsten, 295
Tungstic acid, 295
gravimetric determination, 296
in black tin, 285
in wolfram, 296
Uranium, 312
Valuation, of copper ores, 181
Vanadium, 310
Vanning, 273
Volhard's assay applied to arsenic, 124
silver assay, 121
Volume-corrector, 53
Volumetric assay, 35, 38
Water, 7, 350
Page 580
direct determination of, 351
examination of, 352
expansion of, 83
solids in, 354
Weighing, 47
small gold buttons, 131
Weights, 47
Wolfram, an analysis of, 296
tungstic acid in, 296
Yttria, 319
Zinc, 261
commercial, examination of, 268
commercial, iron in, 249
commercial, lead in, 214
dry assay, 261
gasometric assay, 266
gravimetric determination, 262
in blende, 266
in cyanide liquors, 169
in silver precipitate, 266
separation of, 262
volumetric assay, 263
Zirconia, 317
Printed by Ballantyne, Hanson & Co.
London & Edinburgh.
examination of, 352
expansion of, 83
solids in, 354
Weighing, 47
small gold buttons, 131
Weights, 47
Wolfram, an analysis of, 296
tungstic acid in, 296
Yttria, 319
Zinc, 261
commercial, examination of, 268
commercial, iron in, 249
commercial, lead in, 214
dry assay, 261
gasometric assay, 266
gravimetric determination, 262
in blende, 266
in cyanide liquors, 169
in silver precipitate, 266
separation of, 262
volumetric assay, 263
Zirconia, 317
Printed by Ballantyne, Hanson & Co.
London & Edinburgh.
Page 581
Page 582
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Page 583
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Page 584
Third Edition, Revised, with an Additional Chapter on Foundations.
Numerous Diagrams, Examples, and Tables. Large 8vo. Cloth. 16s.
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BY S. ANGLIN, C.E.,
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THE DESIGN OF STRUCTURES:
A Practical Treatise on the Building of Bridges, Roofs, &c.
BY S. ANGLIN, C.E.,
Master of Engineering, Royal University of Ireland, late Whitworth Scholar, &c.
"Students of Engineering will find this Text-Book invaluable."—Architect.
"The author has certainly succeeded in producing a thoroughly practical
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A PRACTICAL TREATISE ON
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FOR THE USE OF STUDENTS, DRAUGHTSMEN, AND ENGINEERS.
By T. CLAXTON FIDLER, M. INST. C.E.,
Prof. of Engineering, University College, Dundee.
Page 585
General Contents.—Part I.—Elementary Statics. Part II.—General
Principles of Bridge-Construction. Part III.—The Strength of Materials.
Part IV.—The Design of Bridges in Detail.
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By BRYSON CUNNINGHAM, B.E., Assoc.M.Inst.C.E.,
Of the Engineers' Department, Mersey Docks and Harbour Board.
GENERAL CONTENTS.
Historical and Discursive.—Dock Design.—Constructive Appliances.—
Materials.—Dock and Quay Walls.—Entrance Passages and Locks.—
Jetties, Wharves, and Piers.—Dock Gates and Caissons.—Transit Sheds
and Warehouses.—Dock Bridges.—Graving and Repairing Docks.—
Working Equipment of Docks.—Index.
*** The object of the Author has been to deal fully and comprehensively
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and their appanages, not simply as a record of works carried out, but as a
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Principles of Bridge-Construction. Part III.—The Strength of Materials.
Part IV.—The Design of Bridges in Detail.
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At Press. In Large 8vo. Handsome Cloth. With Copious Plates and
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The Principles and Practice of
DOCK ENGINEERING.
By BRYSON CUNNINGHAM, B.E., Assoc.M.Inst.C.E.,
Of the Engineers' Department, Mersey Docks and Harbour Board.
GENERAL CONTENTS.
Historical and Discursive.—Dock Design.—Constructive Appliances.—
Materials.—Dock and Quay Walls.—Entrance Passages and Locks.—
Jetties, Wharves, and Piers.—Dock Gates and Caissons.—Transit Sheds
and Warehouses.—Dock Bridges.—Graving and Repairing Docks.—
Working Equipment of Docks.—Index.
*** The object of the Author has been to deal fully and comprehensively
with the problems arising out of the construction and maintenance of Docks
and their appanages, not simply as a record of works carried out, but as a
treatise on the principles underlying their construction and an investigation
of the mathematical theories involved. It is primarily intended for the
Page 586
student; but it is hoped that the large amount of data and material collected
from various sources, and in many cases contributed specially for this book,
will render it useful to the expert engineer as a work of reference; while, at
the same time, of general interest to directors and others connected with the
management and administration of seaports.
Third Edition. In Two Parts, Published Separately.
A TEXT-BOOK OF
Engineering Drawing and Design
Vol. I.—Practical Geometry, Plane, and Solid. 3s.
VOL. II.—Machine and Engine Drawing and Design. 4s. 6d.
BY
SIDNEY H. WELLS, Wh.Sc.,
A.M.INST.C.E., A.M.INST.MECH.E.,
Principal of the Battersea Polytechnic Institute, and Head of the
Engineering Department therein; formerly of the Engineering Departments
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"A capital text-book, arranged on an EXCELLENT SYSTEM, calculated
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from various sources, and in many cases contributed specially for this book,
will render it useful to the expert engineer as a work of reference; while, at
the same time, of general interest to directors and others connected with the
management and administration of seaports.
Third Edition. In Two Parts, Published Separately.
A TEXT-BOOK OF
Engineering Drawing and Design
Vol. I.—Practical Geometry, Plane, and Solid. 3s.
VOL. II.—Machine and Engine Drawing and Design. 4s. 6d.
BY
SIDNEY H. WELLS, Wh.Sc.,
A.M.INST.C.E., A.M.INST.MECH.E.,
Principal of the Battersea Polytechnic Institute, and Head of the
Engineering Department therein; formerly of the Engineering Departments
of the Yorkshire College, Leeds; and Dulwich College, London.
With many Illustrations, specially prepared for the Work, and numerous
Examples, for the Use of Students in Technical Schools and Colleges.
"A capital text-book, arranged on an EXCELLENT SYSTEM, calculated
to give an intelligent grasp of the subject, and not the mere faculty of
mechanical copying.... Mr. Wells shows how to make complete working
drawings, discussing fully each step in the design."—Electrical Review.
Page 587
"The first book leads easily and naturally towards the second, where the
technical pupil brought into contact with large and more complex
designs."—The Schoolmaster.
Works by BRYAN DONKIN, M. Inst. C.E., M. Inst. Mech. E., &c.
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Development—British, French, and German Gas Engines—Gas Production
for Motive Power—Theory of the Gas Engine—Chemical Composition of
Gas in Gas Engines—Utilisation of Heat—Explosion and Combustion. Oil
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Types: Stirling's, Ericsson's, &c., &c.
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Page 588
In Quarto, Handsome Cloth. With Numerous Plates. 25s.
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General Contents.—Classification of different Types of Boilers—425
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Review.
Page 589
Third Edition, Revised and Enlarged. Pocket-Size, Leather, 12s. 6d.; also
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Boilers, Marine and Land:
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FOR THE USE OF ENGINEERS, SURVEYORS, BOILER-MAKERS,
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FOR THE USE OF ENGINEERS, SURVEYORS, BOILER-MAKERS,
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Page 590
BY JOHN G. LIVERSIDGE,
Engineer, R.N., A.M.I.C.E., Instructor in Applied Mechanics at the Royal Naval College, Greenwich.
Contents.—General Description of Marine Machinery.—The Conditions of
Service and Duties of Engineers of the Royal Navy.—Entry and Conditions
of Service of Engineers of the Leading S.S. Companies.—Raising Steam.—
Duties of a Steaming Watch on Engines and Boilers.—Shutting off Steam.
—Harbour Duties and Watches.—Adjustments and Repairs of Engines.—
Preservation and Repairs of "Tank" Boilers.—The Hull and its Fittings.—
Cleaning and Painting Machinery.—Reciprocating Pumps, Feed Heaters,
and Automatic Feed-Water Regulators.—Evaporators.—Steam Boats.—
Electric Light Machinery.—Hydraulic Machinery.—Air-Compressing
Pumps.—Refrigerating Machines.—Machinery of Destroyers.—The
Management of Water-Tube Boilers.—Regulations for Entry of Assistant
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Engineers, R.N.—Regulations respecting Board of Trade Examinations for
Engineers, &c.
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In Crown 8vo, extra, with Numerous Illustrations. [Shortly.
GAS AND OIL ENGINES:
An Introductory Text-Book on the Theory, Design, Construction, and Testing of Internal
Combustion Engines without Boiler.
FOR THE USE OF STUDENTS.
By Prof. W.H. WATKINSON, Whit. Sch., M. Inst. Mech. E.,
Engineer, R.N., A.M.I.C.E., Instructor in Applied Mechanics at the Royal Naval College, Greenwich.
Contents.—General Description of Marine Machinery.—The Conditions of
Service and Duties of Engineers of the Royal Navy.—Entry and Conditions
of Service of Engineers of the Leading S.S. Companies.—Raising Steam.—
Duties of a Steaming Watch on Engines and Boilers.—Shutting off Steam.
—Harbour Duties and Watches.—Adjustments and Repairs of Engines.—
Preservation and Repairs of "Tank" Boilers.—The Hull and its Fittings.—
Cleaning and Painting Machinery.—Reciprocating Pumps, Feed Heaters,
and Automatic Feed-Water Regulators.—Evaporators.—Steam Boats.—
Electric Light Machinery.—Hydraulic Machinery.—Air-Compressing
Pumps.—Refrigerating Machines.—Machinery of Destroyers.—The
Management of Water-Tube Boilers.—Regulations for Entry of Assistant
Engineers, R.N.—Questions given in Examinations for Promotion of
Engineers, R.N.—Regulations respecting Board of Trade Examinations for
Engineers, &c.
"The contents cannot fail to be appreciated."—The Steamship.
"This very useful book.... Illustrations are of great importance in a work
of this kind, and it is satisfactory to find that special attention has been
given in this respect."—Engineers' Gazette.
In Crown 8vo, extra, with Numerous Illustrations. [Shortly.
GAS AND OIL ENGINES:
An Introductory Text-Book on the Theory, Design, Construction, and Testing of Internal
Combustion Engines without Boiler.
FOR THE USE OF STUDENTS.
By Prof. W.H. WATKINSON, Whit. Sch., M. Inst. Mech. E.,
Page 591
Glasgow and West of Scotland Technical College.
Second Edition, Revised. With numerous Plates reduced from Working
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A MANUAL OF
LOCOMOTIVE ENGINEERING:
A Practical Text-Book for the Use of Engine Builders, Designers and Draughtsmen, Railway
Engineers, and Students.
BY
WILLIAM FRANK PETTIGREW, M. Inst. C.E.
With a Section on American and Continental Engines.
By ALBERT F. RAVENSHEAR, B.Sc.,
Of His Majesty's Patent Office.
Contents.—Historical Introduction, 1763-1863.—Modern Locomotives:
Simple.—Modern Locomotives: Compound.—Primary Consideration in
Locomotive Design.—Cylinders, Steam Chests, and Stuffing Boxes.—
Pistons, Piston Rods, Crossheads, and Slide Bars.—Connecting and
Coupling Rods.—Wheels and Axles, Axle Boxes, Hornblocks, and Bearing
Springs.—Balancing.—Valve Gear.—Slide Valves and Valve Gear Details.
—Framing, Bogies and Axle Trucks, Radial Axle Boxes.—Boilers.—
Smokebox, Blast Pipe, Firebox Fittings.—Boiler Mountings.—Tenders.—
Railway Brakes.—Lubrication.—Consumption of Fuel, Evaporation and
Engine Efficiency.—American Locomotives.—Continental Locomotives.—
Repairs, Running, Inspection, and Renewals.—Three Appendices.—Index.
Second Edition, Revised. With numerous Plates reduced from Working
Drawings and 280 Illustrations in the Text. 21s.
A MANUAL OF
LOCOMOTIVE ENGINEERING:
A Practical Text-Book for the Use of Engine Builders, Designers and Draughtsmen, Railway
Engineers, and Students.
BY
WILLIAM FRANK PETTIGREW, M. Inst. C.E.
With a Section on American and Continental Engines.
By ALBERT F. RAVENSHEAR, B.Sc.,
Of His Majesty's Patent Office.
Contents.—Historical Introduction, 1763-1863.—Modern Locomotives:
Simple.—Modern Locomotives: Compound.—Primary Consideration in
Locomotive Design.—Cylinders, Steam Chests, and Stuffing Boxes.—
Pistons, Piston Rods, Crossheads, and Slide Bars.—Connecting and
Coupling Rods.—Wheels and Axles, Axle Boxes, Hornblocks, and Bearing
Springs.—Balancing.—Valve Gear.—Slide Valves and Valve Gear Details.
—Framing, Bogies and Axle Trucks, Radial Axle Boxes.—Boilers.—
Smokebox, Blast Pipe, Firebox Fittings.—Boiler Mountings.—Tenders.—
Railway Brakes.—Lubrication.—Consumption of Fuel, Evaporation and
Engine Efficiency.—American Locomotives.—Continental Locomotives.—
Repairs, Running, Inspection, and Renewals.—Three Appendices.—Index.
Page 592
"Likely to remain for many years the Standard Work for those wishing to
learn Design."—Engineer.
"A most interesting and valuable addition to the bibliography of the
Locomotive."—Railway Official Gazette.
"We recommend the book as thoroughly practical in its character, and
meriting a place in any collection of ... works on Locomotive
Engineering."—Railway News.
"The work contains all that can be learnt from a book upon such a
subject. It will at once rank as the standard work upon this important
subject."—Railway Magazine.
In Large 8vo. Handsome Cloth. With Plates and Illustrations. 16s.
LIGHT RAILWAYS AT HOME AND ABROAD.
By WILLIAM HENRY COLE, M. Inst. C.E.,
Late Deputy-Manager, North-Western Railway, India.
Contents.—Discussion of the Term "Light Railways."—English Railways,
Rates, and Farmers.—Light Railways in Belgium, France, Italy, other
European Countries, America and the Colonies, India, Ireland.—Road
Transport as an alternative.—The Light Railways Act, 1896.—The
Question of Gauge.—Construction and Working.—Locomotives and
Rolling-Stock.—Light Railways in England, Scotland, and Wales.—
Appendices and Index.
"Mr. W.H. Cole has brought together ... a large amount of valuable
information ... hitherto practically inaccessible to the ordinary reader."—
Times.
"Will remain, for some time yet a Standard Work in everything relating to
Light Railways."—Engineer.
learn Design."—Engineer.
"A most interesting and valuable addition to the bibliography of the
Locomotive."—Railway Official Gazette.
"We recommend the book as thoroughly practical in its character, and
meriting a place in any collection of ... works on Locomotive
Engineering."—Railway News.
"The work contains all that can be learnt from a book upon such a
subject. It will at once rank as the standard work upon this important
subject."—Railway Magazine.
In Large 8vo. Handsome Cloth. With Plates and Illustrations. 16s.
LIGHT RAILWAYS AT HOME AND ABROAD.
By WILLIAM HENRY COLE, M. Inst. C.E.,
Late Deputy-Manager, North-Western Railway, India.
Contents.—Discussion of the Term "Light Railways."—English Railways,
Rates, and Farmers.—Light Railways in Belgium, France, Italy, other
European Countries, America and the Colonies, India, Ireland.—Road
Transport as an alternative.—The Light Railways Act, 1896.—The
Question of Gauge.—Construction and Working.—Locomotives and
Rolling-Stock.—Light Railways in England, Scotland, and Wales.—
Appendices and Index.
"Mr. W.H. Cole has brought together ... a large amount of valuable
information ... hitherto practically inaccessible to the ordinary reader."—
Times.
"Will remain, for some time yet a Standard Work in everything relating to
Light Railways."—Engineer.
Page 593
"The author has extended practical experience that makes the book lucid
and useful. It is exceedingly well done"—Engineering.
"The whole subject is exhaustively and practically considered. The work
can be cordially recommended as indispensable to those whose duty it is to
become acquainted with one of the prime necessities of the immediate
future."—Railway Official Gazette.
"There could be no better book of first reference on its subject. All classes
of Engineers will welcome its appearance."—Scotsman.
Third Edition, Revised and Enlarged. With Numerous Illustrations. Price
8s. 6d.
VALVES AND VALVE-GEARING:
INCLUDING THE CORLISS VALVE AND TRIP GEARS.
BY
CHARLES HURST,
Practical Draughtsman.
"Concise explanations illustrated by 115 very clear diagrams and drawings
and 4 folding-plates ... the book fulfils a valuable function."—Athenæum.
"Mr. Hurst's valves and valve-gearing will prove a very valuable aid, and
tend to the production of Engines of scientific design and economical
working.... Will be largely sought after by Students and Designers.—
Marine Engineer.
"Useful and thoroughly practical. Will undoubtedly be found of GREAT
VALUE to all concerned with the design of Valve-gearing."—Mechanical
World.
and useful. It is exceedingly well done"—Engineering.
"The whole subject is exhaustively and practically considered. The work
can be cordially recommended as indispensable to those whose duty it is to
become acquainted with one of the prime necessities of the immediate
future."—Railway Official Gazette.
"There could be no better book of first reference on its subject. All classes
of Engineers will welcome its appearance."—Scotsman.
Third Edition, Revised and Enlarged. With Numerous Illustrations. Price
8s. 6d.
VALVES AND VALVE-GEARING:
INCLUDING THE CORLISS VALVE AND TRIP GEARS.
BY
CHARLES HURST,
Practical Draughtsman.
"Concise explanations illustrated by 115 very clear diagrams and drawings
and 4 folding-plates ... the book fulfils a valuable function."—Athenæum.
"Mr. Hurst's valves and valve-gearing will prove a very valuable aid, and
tend to the production of Engines of scientific design and economical
working.... Will be largely sought after by Students and Designers.—
Marine Engineer.
"Useful and thoroughly practical. Will undoubtedly be found of GREAT
VALUE to all concerned with the design of Valve-gearing."—Mechanical
World.
Page 594
"Almost every type of valve and its gearing is clearly set forth, and
illustrated in such a way as to be readily understood and practically
applied by either the Engineer, Draughtsman, or Student.... Should prove
both USEFUL and valuable to all Engineers seeking for reliable and
clear information on the subject. Its moderate price brings it within the
reach of all"—Industries and Iron.
"Mr. Hurst's work is admirably suited to the needs of the practical
mechanic.... It is free from any elaborate theoretical discussions, and the
explanations of the various types of valve-gear are accompanied by
diagrams which render them easily understood."—The Scientific
American.
Hints on Steam Engine Design and Construction. By Charles Hurst,
"Author of Valves and Valve Gearing." In Paper Boards, 8vo., Cloth Back.
Illustrated. Price 1s. 6d. net.
Contents.—I. Steam Pipes.—II. Valves.—III. Cylinders.—IV. Air Pumps
and Condensers.—V. Motion Work.—VI. Crank Shafts and Pedestals.—
VII. Valve Gear.—VIII. Lubrication.—IX. Miscellaneous Details—Index.
"A handy volume which every practical young engineer should possess."—
The Model Engineer.
JUST OUT. Strongly Bound in Super Royal 8vo. Cloth Boards.
illustrated in such a way as to be readily understood and practically
applied by either the Engineer, Draughtsman, or Student.... Should prove
both USEFUL and valuable to all Engineers seeking for reliable and
clear information on the subject. Its moderate price brings it within the
reach of all"—Industries and Iron.
"Mr. Hurst's work is admirably suited to the needs of the practical
mechanic.... It is free from any elaborate theoretical discussions, and the
explanations of the various types of valve-gear are accompanied by
diagrams which render them easily understood."—The Scientific
American.
Hints on Steam Engine Design and Construction. By Charles Hurst,
"Author of Valves and Valve Gearing." In Paper Boards, 8vo., Cloth Back.
Illustrated. Price 1s. 6d. net.
Contents.—I. Steam Pipes.—II. Valves.—III. Cylinders.—IV. Air Pumps
and Condensers.—V. Motion Work.—VI. Crank Shafts and Pedestals.—
VII. Valve Gear.—VIII. Lubrication.—IX. Miscellaneous Details—Index.
"A handy volume which every practical young engineer should possess."—
The Model Engineer.
JUST OUT. Strongly Bound in Super Royal 8vo. Cloth Boards.
Page 595
BONUS TABLES:
For Calculating Wages on the Bonus or Premium Systems.
For Engineering, Technical and Allied Trades.
By HENRY A. GOLDING, A.M.Inst.M.E.,
Technical Assistant to Messrs. Bryan Donkin and Clench, Ltd., and
Assistant Lecturer in Mechanical Engineering at the Northampton Institute,
London, E.C.
"The adoption of this system for the payment of workmen has created a
demand for some handy table or series of tables, by means of which the
wages may be easily found without the necessity of any calculations
whatever. With the object of supplying this need, the author has compiled
the following tables, which have been in practical use for some time past at
a large engineering works in London, and have been found of inestimable
value. Not only are they of great value as a 'time saving appliance,' the
computation of the bonus or premiums earned by a number of men taking
only one-tenth the time by the aid of these tables compared with ordinary
calculations, but they possess the additional advantage of being less liable
to error, as there is practically no possibility of a mistake occurring."—
Extract from Preface.
Large 8vo, Handsome Cloth. With Illustrations, Tables, &c. 21s.
Lubrication & Lubricants:
A TREATISE ON THE
THEORY AND PRACTICE OF LUBRICATION
For Calculating Wages on the Bonus or Premium Systems.
For Engineering, Technical and Allied Trades.
By HENRY A. GOLDING, A.M.Inst.M.E.,
Technical Assistant to Messrs. Bryan Donkin and Clench, Ltd., and
Assistant Lecturer in Mechanical Engineering at the Northampton Institute,
London, E.C.
"The adoption of this system for the payment of workmen has created a
demand for some handy table or series of tables, by means of which the
wages may be easily found without the necessity of any calculations
whatever. With the object of supplying this need, the author has compiled
the following tables, which have been in practical use for some time past at
a large engineering works in London, and have been found of inestimable
value. Not only are they of great value as a 'time saving appliance,' the
computation of the bonus or premiums earned by a number of men taking
only one-tenth the time by the aid of these tables compared with ordinary
calculations, but they possess the additional advantage of being less liable
to error, as there is practically no possibility of a mistake occurring."—
Extract from Preface.
Large 8vo, Handsome Cloth. With Illustrations, Tables, &c. 21s.
Lubrication & Lubricants:
A TREATISE ON THE
THEORY AND PRACTICE OF LUBRICATION
Page 596
AND ON THE
NATURE, PROPERTIES, AND TESTING OF LUBRICANTS.
By LEONARD ARCHBUTT, F.I.C., F.C.S.,
Chemist to the Midland Railway Company,
AND
R. MOUNTFORD DEELEY, M.I.M.E., F.G.S.,
Midland Railway Locomotive Works' Manager, Derby.
Contents.—I. Friction of Solids.—II. Liquid Friction or Viscosity, and
Plastic Friction.—III. Superficial Tension.—IV. The Theory of Lubrication.
—V. Lubricants, their Sources, Preparation, and Properties.—VI. Physical
Properties and Methods of Examination of Lubricants.—VII. Chemical
Properties and Methods of Examination of Lubricants.—VIII. The
Systematic Testing of Lubricants by Physical and Chemical Methods.—IX.
The Mechanical Testing of Lubricants.—X. The Design and Lubrication of
Bearings.—XI. The Lubrication of Machinery.—Index.
"Destined to become a classic on the subject."—Industries and Iron.
"Contains practically all that is known on the subject. Deserves the careful
attention of all Engineers."—Railway Official Guide.
Fourth Edition. Very fully Illustrated. Cloth, 4s. 6d.
STEAM-BOILERS: THEIR DEFECTS, MANAGEMENT,
AND CONSTRUCTION.
By R.D. MUNRO,
Chief Engineer of the Scottish Boiler Insurance and Engine Inspection Company.
NATURE, PROPERTIES, AND TESTING OF LUBRICANTS.
By LEONARD ARCHBUTT, F.I.C., F.C.S.,
Chemist to the Midland Railway Company,
AND
R. MOUNTFORD DEELEY, M.I.M.E., F.G.S.,
Midland Railway Locomotive Works' Manager, Derby.
Contents.—I. Friction of Solids.—II. Liquid Friction or Viscosity, and
Plastic Friction.—III. Superficial Tension.—IV. The Theory of Lubrication.
—V. Lubricants, their Sources, Preparation, and Properties.—VI. Physical
Properties and Methods of Examination of Lubricants.—VII. Chemical
Properties and Methods of Examination of Lubricants.—VIII. The
Systematic Testing of Lubricants by Physical and Chemical Methods.—IX.
The Mechanical Testing of Lubricants.—X. The Design and Lubrication of
Bearings.—XI. The Lubrication of Machinery.—Index.
"Destined to become a classic on the subject."—Industries and Iron.
"Contains practically all that is known on the subject. Deserves the careful
attention of all Engineers."—Railway Official Guide.
Fourth Edition. Very fully Illustrated. Cloth, 4s. 6d.
STEAM-BOILERS: THEIR DEFECTS, MANAGEMENT,
AND CONSTRUCTION.
By R.D. MUNRO,
Chief Engineer of the Scottish Boiler Insurance and Engine Inspection Company.
Page 597
General Contents.—I. Explosions caused (1) by Overheating of Plates—
(2) By Defective and Overloaded Safety Valves—(3) By Corrosion, Internal
or External—(4) By Defective Design and Construction (Unsupported Flue
Tubes; Unstrengthened Manholes; Defective Staying; Strength of Rivetted
Joints; Factor of Safety)—II. Construction of Vertical Boilers: Shells—
Crown Plates and Uptake Tubes—Man-Holes, Mud-Holes, and Fire-Holes
—Fireboxes—Mountings—Management—Cleaning—Table of Bursting
Pressures of Steel Boilers—Table of Rivetted Joints—Specifications and
Drawings of Lancashire Boiler for Working Pressures (a) 80 lbs.; (b) 200
lbs. per square inch respectively.
"A valuable companion for workmen and engineers engaged about Steam
Boilers, ought to be carefully studied, and always at hand."—Coll.
Guardian.
"The book is very useful, especially to steam users, artisans, and young
Engineers."—Engineer.
By the same Author.
KITCHEN BOILER EXPLOSIONS:
Why they Occur, and How to Prevent their Occurrence. A Practical
Handbook based on Actual Experiment. With Diagram and Coloured Plate.
Price 3s.
Just Out. In Crown 8vo, Handsome Cloth. With Numerous Illustrations. 5s.
net.
EMERY GRINDING MACHINERY.
A Text-Book of Workshop Practice in General Tool Grinding, and the Design, Construction, and
Application of the Machines Employed.
(2) By Defective and Overloaded Safety Valves—(3) By Corrosion, Internal
or External—(4) By Defective Design and Construction (Unsupported Flue
Tubes; Unstrengthened Manholes; Defective Staying; Strength of Rivetted
Joints; Factor of Safety)—II. Construction of Vertical Boilers: Shells—
Crown Plates and Uptake Tubes—Man-Holes, Mud-Holes, and Fire-Holes
—Fireboxes—Mountings—Management—Cleaning—Table of Bursting
Pressures of Steel Boilers—Table of Rivetted Joints—Specifications and
Drawings of Lancashire Boiler for Working Pressures (a) 80 lbs.; (b) 200
lbs. per square inch respectively.
"A valuable companion for workmen and engineers engaged about Steam
Boilers, ought to be carefully studied, and always at hand."—Coll.
Guardian.
"The book is very useful, especially to steam users, artisans, and young
Engineers."—Engineer.
By the same Author.
KITCHEN BOILER EXPLOSIONS:
Why they Occur, and How to Prevent their Occurrence. A Practical
Handbook based on Actual Experiment. With Diagram and Coloured Plate.
Price 3s.
Just Out. In Crown 8vo, Handsome Cloth. With Numerous Illustrations. 5s.
net.
EMERY GRINDING MACHINERY.
A Text-Book of Workshop Practice in General Tool Grinding, and the Design, Construction, and
Application of the Machines Employed.
Page 598
BY
R.B. HODGSON, A.M. Inst. Mech. E.,
Author of "Machines and Tools Employed in the Working of Sheet Metals."
Introduction.—Tool Grinding.—Emery Wheels.—Mounting Emery
Wheels.—Emery Rings and Cylinders.—Conditions to Ensure Efficient
Working.—Leading Types of Machines.—Concave and Convex Grinding.
—Cup and Cone Machines.—Multiple Grinding.—"Guest" Universal and
Cutter Grinding Machines.—Ward Universal Cutter Grinder.—Press.—Tool
Grinding.—Lathe Centre Grinder.—Polishing.—Index.
"Deals practically with every phase of his subject."—Ironmonger.
Fifth Edition. Folio, strongly half-bound, 21/.
TRAVERSE TABLES:
Computed to Four Places of Decimals for every Minute of Angle up to 100 of Distance.
For the use of Surveyors and Engineers.
BY
RICHARD LLOYD GURDEN,
Authorised Surveyor for the Governments of New South Wales and Victoria.
*** Published with the Concurrence of the Surveyors-General for New South Wales and Victoria.
"Those who have experience in exact Survey-work will best know how to
appreciate the enormous amount of labour represented by this valuable
book. The computations enable the user to ascertain the sines and cosines
for a distance of twelve miles to within half an inch, and this by Reference
To But One Table, in place of the usual Fifteen minute computations
R.B. HODGSON, A.M. Inst. Mech. E.,
Author of "Machines and Tools Employed in the Working of Sheet Metals."
Introduction.—Tool Grinding.—Emery Wheels.—Mounting Emery
Wheels.—Emery Rings and Cylinders.—Conditions to Ensure Efficient
Working.—Leading Types of Machines.—Concave and Convex Grinding.
—Cup and Cone Machines.—Multiple Grinding.—"Guest" Universal and
Cutter Grinding Machines.—Ward Universal Cutter Grinder.—Press.—Tool
Grinding.—Lathe Centre Grinder.—Polishing.—Index.
"Deals practically with every phase of his subject."—Ironmonger.
Fifth Edition. Folio, strongly half-bound, 21/.
TRAVERSE TABLES:
Computed to Four Places of Decimals for every Minute of Angle up to 100 of Distance.
For the use of Surveyors and Engineers.
BY
RICHARD LLOYD GURDEN,
Authorised Surveyor for the Governments of New South Wales and Victoria.
*** Published with the Concurrence of the Surveyors-General for New South Wales and Victoria.
"Those who have experience in exact Survey-work will best know how to
appreciate the enormous amount of labour represented by this valuable
book. The computations enable the user to ascertain the sines and cosines
for a distance of twelve miles to within half an inch, and this by Reference
To But One Table, in place of the usual Fifteen minute computations
Page 599
required. This alone is evidence of the assistance which the Tables ensure to
every user, and as every Surveyor in active practice has felt the want of
such assistance few knowing of their publication will remain without
them."—Engineer.
WORKS BY
ANDREW JAMIESON, M. Inst. C.E., M.I.E.E., F.R.S.E.,
Formerly Professor of Electrical Engineering, The Glasgow and West of Scotland Technical
College.
PROFESSOR JAMIESON'S ADVANCED TEXT-BOOKS.
In Large Crown 8vo. Fully Illustrated.
STEAM AND STEAM-ENGINES (A Text-Book on).
For the Use of Students preparing for Competitive Examinations. With 600
pp., over 200 Illustrations, 6 Folding Plates, and numerous Examination
Papers. Thirteenth Edition, Revised. 8/6.
"Professor Jamieson fascinates the reader by his clearness of conception
and simplicity of expression. His treatment recalls the lecturing of
Faraday."—Athenæum.
"The Best Book yet published for the use of Students."—Engineer.
MAGNETISM AND ELECTRICITY (An Advanced Text-Book on).
For Advanced and "Honours" Students. By Prof. Jamieson, assisted by
David Robertson, B.Sc., Professor of Electrical Engineering in the
every user, and as every Surveyor in active practice has felt the want of
such assistance few knowing of their publication will remain without
them."—Engineer.
WORKS BY
ANDREW JAMIESON, M. Inst. C.E., M.I.E.E., F.R.S.E.,
Formerly Professor of Electrical Engineering, The Glasgow and West of Scotland Technical
College.
PROFESSOR JAMIESON'S ADVANCED TEXT-BOOKS.
In Large Crown 8vo. Fully Illustrated.
STEAM AND STEAM-ENGINES (A Text-Book on).
For the Use of Students preparing for Competitive Examinations. With 600
pp., over 200 Illustrations, 6 Folding Plates, and numerous Examination
Papers. Thirteenth Edition, Revised. 8/6.
"Professor Jamieson fascinates the reader by his clearness of conception
and simplicity of expression. His treatment recalls the lecturing of
Faraday."—Athenæum.
"The Best Book yet published for the use of Students."—Engineer.
MAGNETISM AND ELECTRICITY (An Advanced Text-Book on).
For Advanced and "Honours" Students. By Prof. Jamieson, assisted by
David Robertson, B.Sc., Professor of Electrical Engineering in the
Page 600
Merchant Venturers' Technical College, Bristol. [Shortly.
APPLIED MECHANICS (An Advanced Text-Book on).
Vol. I.—Comprising Part I.: The Principle of Work and its applications; Part
II.: Gearing. Price 7s. 6d. Third Edition.
"Fully maintains the reputation of the Author."—Pract. Engineer.
Vol. II.—Comprising Parts III. to VI.: Motion and Energy; Graphic Statics;
Strength of Materials; Hydraulics and Hydraulic Machinery. Second
Edition. 8s. 6d.
"Well and lucidly written."—The Engineer.
*** Each of the above volumes is complete in itself, and sold separately.
PROFESSOR JAMIESON'S INTRODUCTORY MANUALS.
Crown 8vo. With Illustrations and Examination Papers.
STEAM AND THE STEAM-ENGINE (Elementary Manual of).
For First-Year Students. Ninth Edition, Revised. 3/6.
"Should be in the hands of every engineering apprentice."—Practical
Engineer.
MAGNETISM AND ELECTRICITY (Elementary Manual of).
For First-Year Students. Fifth Edition.. 3/6.
"A capital text-book.... The diagrams are an important feature."—
Schoolmaster.
"A thoroughly trustworthy Text-book. Practical and clear."—Nature.
APPLIED MECHANICS (An Advanced Text-Book on).
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II.: Gearing. Price 7s. 6d. Third Edition.
"Fully maintains the reputation of the Author."—Pract. Engineer.
Vol. II.—Comprising Parts III. to VI.: Motion and Energy; Graphic Statics;
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"Well and lucidly written."—The Engineer.
*** Each of the above volumes is complete in itself, and sold separately.
PROFESSOR JAMIESON'S INTRODUCTORY MANUALS.
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STEAM AND THE STEAM-ENGINE (Elementary Manual of).
For First-Year Students. Ninth Edition, Revised. 3/6.
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MAGNETISM AND ELECTRICITY (Elementary Manual of).
For First-Year Students. Fifth Edition.. 3/6.
"A capital text-book.... The diagrams are an important feature."—
Schoolmaster.
"A thoroughly trustworthy Text-book. Practical and clear."—Nature.
Page 601
APPLIED MECHANICS (Elementary Manual of).
Specially arranged for First-Year Students. Fifth Edition, Revised. 3/6.
"The work has very high qualities, which may be condensed into the one
word 'clear.'"—Science and Art.
In Preparation. 300 pages. Crown 8vo. Profusely Illustrated.
Modern Electric Tramway Traction: A Text-Book of Present-Day
Practice.
For the Use of Electrical Engineering Students and those interested in
Electric Transmission of Power.
By Prof. ANDREW JAMIESON.
A POCKET-BOOK of ELECTRICAL RULES and TABLES.
For the Use of Electricians and Engineers. Pocket Size. Leather, 8s. 6d.
Sixteenth Edition. [See p. 49.
WORKS BY
W.J. MACQUORN RANKINE, LL.D., F.R.S.,
Late Regius Professor of Civil Engineering in the University of Glasgow.
THOROUGHLY REVISED BY
Specially arranged for First-Year Students. Fifth Edition, Revised. 3/6.
"The work has very high qualities, which may be condensed into the one
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In Preparation. 300 pages. Crown 8vo. Profusely Illustrated.
Modern Electric Tramway Traction: A Text-Book of Present-Day
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For the Use of Electrical Engineering Students and those interested in
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By Prof. ANDREW JAMIESON.
A POCKET-BOOK of ELECTRICAL RULES and TABLES.
For the Use of Electricians and Engineers. Pocket Size. Leather, 8s. 6d.
Sixteenth Edition. [See p. 49.
WORKS BY
W.J. MACQUORN RANKINE, LL.D., F.R.S.,
Late Regius Professor of Civil Engineering in the University of Glasgow.
THOROUGHLY REVISED BY
Page 602
W.J. MILLAR, C.E.,
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A MANUAL OF APPLIED MECHANICS: Comprising the Principles of
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A MANUAL OF CIVIL ENGINEERING: Comprising Engineering
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A MANUAL OF THE STEAM-ENGINE AND OTHER PRIME
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Crown 8vo, cloth. Fifteenth Edition. 12s. 6d.
Late Secretary to the Institute of Engineers and Shipbuilders in Scotland.
A MANUAL OF APPLIED MECHANICS: Comprising the Principles of
Statics and Cinematics, and Theory of Structures, Mechanism, and
Machines. With Numerous Diagrams. Crown 8vo, cloth. Sixteenth Edition.
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A MANUAL OF CIVIL ENGINEERING: Comprising Engineering
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A MANUAL OF THE STEAM-ENGINE AND OTHER PRIME
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Donkin, M.Inst.C.E. With Folding Plates and Numerous Illustrations.
Crown 8vo, cloth. Fifteenth Edition. 12s. 6d.
Page 603
USEFUL RULES AND TABLES: For Architects, Builders, Engineers,
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With Memoir by Professor Tait, M.A. Edited by W.J. Millar, C.E. With
fine Portrait on Steel, Plates, and Diagrams.
"No more enduring Memorial of Professor Rankine could be devised than
the publication of these papers in an accessible form.... The Collection is
most valuable on account of the nature of his discoveries, and the beauty
and completeness of his analysis.... The Volume exceeds in importance any
work in the same department published in our time."—Architect.
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MISCELLANEOUS SCIENTIFIC PAPERS.
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With Memoir by Professor Tait, M.A. Edited by W.J. Millar, C.E. With
fine Portrait on Steel, Plates, and Diagrams.
"No more enduring Memorial of Professor Rankine could be devised than
the publication of these papers in an accessible form.... The Collection is
most valuable on account of the nature of his discoveries, and the beauty
and completeness of his analysis.... The Volume exceeds in importance any
work in the same department published in our time."—Architect.
Page 604
SHELTON-BEY (W. Vincent, Foreman to the Imperial
Ottoman Gun Factories, Constantinople):
THE MECHANIC'S GUIDE: A Hand-Book for Engineers and Artizans.
With Copious Tables and Valuable Recipes for Practical Use. Illustrated.
Second Edition. Crown 8vo. Cloth, 7/6.
SECOND EDITION, Revised and Enlarged. In Large 8vo, Handsome cloth,
34s.
HYDRAULIC POWER AND HYDRAULIC MACHINERY.
BY HENRY ROBINSON, M. Inst. C.E., F.G.S.,
FELLOW OF KING'S COLLEGE, LONDON; PROF. OF CIVIL ENGINEERING, KING'S COLLEGE, ETC., ETC.
With numerous Woodcuts, and Sixty-nine Plates.
"A Book of great Professional Usefulness."—Iron.
In Large 8vo, Handsome Cloth. With Frontispiece, several Plates, and over
250 Illustrations. 21s.
THE PRINCIPLES AND CONSTRUCTION OF PUMPING
MACHINERY (STEAM AND WATER PRESSURE).
With Practical Illustrations of Engines and Pumps applied to Mining, Town Water Supply,
Drainage of Lands, &c., also Economy and Efficiency Trials of Pumping Machinery.
By HENRY DAVEY,
Member of the Institution of Civil Engineers, Member of the Institution of Mechanical Engineers, F.G.S., &c.
Ottoman Gun Factories, Constantinople):
THE MECHANIC'S GUIDE: A Hand-Book for Engineers and Artizans.
With Copious Tables and Valuable Recipes for Practical Use. Illustrated.
Second Edition. Crown 8vo. Cloth, 7/6.
SECOND EDITION, Revised and Enlarged. In Large 8vo, Handsome cloth,
34s.
HYDRAULIC POWER AND HYDRAULIC MACHINERY.
BY HENRY ROBINSON, M. Inst. C.E., F.G.S.,
FELLOW OF KING'S COLLEGE, LONDON; PROF. OF CIVIL ENGINEERING, KING'S COLLEGE, ETC., ETC.
With numerous Woodcuts, and Sixty-nine Plates.
"A Book of great Professional Usefulness."—Iron.
In Large 8vo, Handsome Cloth. With Frontispiece, several Plates, and over
250 Illustrations. 21s.
THE PRINCIPLES AND CONSTRUCTION OF PUMPING
MACHINERY (STEAM AND WATER PRESSURE).
With Practical Illustrations of Engines and Pumps applied to Mining, Town Water Supply,
Drainage of Lands, &c., also Economy and Efficiency Trials of Pumping Machinery.
By HENRY DAVEY,
Member of the Institution of Civil Engineers, Member of the Institution of Mechanical Engineers, F.G.S., &c.
Page 605
Contents—Early History of Pumping Engines—Steam Pumping Engines—
Pumps and Pump Valves—General Principles of Non-Rotative Pumping
Engines—The Cornish Engine, Simple and Compound—Types of Mining
Engines—Pit Work—Shaft Sinking—Hydraulic Transmission of Power in
Mines—Valve Gears of Pumping Engines—Water Pressure Pumping
Engines—Water Works Engines—Pumping Engine Economy and Trials of
Pumping Machinery—Centrifugal and other Low-Lift Pumps—Hydraulic
Rams. Pumping Mains, &c.—Index.
"By the 'one' English Engineer who probably knows more about Pumping
Machinery than any other.' ... A volume recording the results of long
experience and study."—The Engineer.
"Undoubtedly the best and most practical treatise on Pumping Machinery
that has yet been published."—Mining Journal.
Royal 8vo, Handsome Cloth. With numerous Illustrations and Tables. 25s.
THE STABILITY OF SHIPS.
BY
SIR EDWARD J. REED, K.C.B., F.R.S., M.P.,
KNIGHT OF THE IMPERIAL ORDERS OF ST. STANILAUS OF RUSSIA; FRANCIS JOSEPH OF AUSTRIA;
MEDJIDIE OF TURKEY; AND RISING SUN OF JAPAN; VICE-PRESIDENT OF THE INSTITUTION OF NAVAL
ARCHITECTS.
In order to render the work complete for the purposes of the Shipbuilder,
whether at home or abroad, the Methods of Calculation introduced by Mr.
F.K. Barnes, Mr. Gray, M. Reech, M. Daymard, and Mr. Benjamin, are all
given separately, illustrated by Tables and worked-out examples. The book
contains more than 200 Diagrams, and is illustrated by a large number of
actual cases, derived from ships of all descriptions.
Pumps and Pump Valves—General Principles of Non-Rotative Pumping
Engines—The Cornish Engine, Simple and Compound—Types of Mining
Engines—Pit Work—Shaft Sinking—Hydraulic Transmission of Power in
Mines—Valve Gears of Pumping Engines—Water Pressure Pumping
Engines—Water Works Engines—Pumping Engine Economy and Trials of
Pumping Machinery—Centrifugal and other Low-Lift Pumps—Hydraulic
Rams. Pumping Mains, &c.—Index.
"By the 'one' English Engineer who probably knows more about Pumping
Machinery than any other.' ... A volume recording the results of long
experience and study."—The Engineer.
"Undoubtedly the best and most practical treatise on Pumping Machinery
that has yet been published."—Mining Journal.
Royal 8vo, Handsome Cloth. With numerous Illustrations and Tables. 25s.
THE STABILITY OF SHIPS.
BY
SIR EDWARD J. REED, K.C.B., F.R.S., M.P.,
KNIGHT OF THE IMPERIAL ORDERS OF ST. STANILAUS OF RUSSIA; FRANCIS JOSEPH OF AUSTRIA;
MEDJIDIE OF TURKEY; AND RISING SUN OF JAPAN; VICE-PRESIDENT OF THE INSTITUTION OF NAVAL
ARCHITECTS.
In order to render the work complete for the purposes of the Shipbuilder,
whether at home or abroad, the Methods of Calculation introduced by Mr.
F.K. Barnes, Mr. Gray, M. Reech, M. Daymard, and Mr. Benjamin, are all
given separately, illustrated by Tables and worked-out examples. The book
contains more than 200 Diagrams, and is illustrated by a large number of
actual cases, derived from ships of all descriptions.
Page 606
"Sir Edward Reed's 'Stability of Ships' is invaluable. The Naval Architect
will find brought together and ready to his hand, a mass of information
which he would otherwise have to seek in an almost endless variety of
publications, and some of which he would possibly not be able to obtain at
all elsewhere."—Steamship.
THE DESIGN AND CONSTRUCTION OF SHIPS.
By John Harvard Biles, M.Inst.N.A.,
Professor of Naval Architecture in the University of Glasgow. [In Preparation.
Second Edition. Illustrated with Plates, Numerous Diagrams, and Figures in
the Text. 18s. net.
STEEL SHIPS: THEIR CONSTRUCTION AND
MAINTENANCE.
A Manual for Shipbuilders, Ship Superintendents, Students, and Marine Engineers.
By THOMAS WALTON, Naval Architect,
AUTHOR OF "KNOW YOUR OWN SHIP."
Contents.—I. Manufacture of Cast Iron, Wrought Iron, and Steel.—
Composition of Iron and Steel, Quality, Strength, Tests, &c. II.
Classification of Steel Ships. III. Considerations in making choice of Type
of Vessel.—Framing of Ships. IV. Strains experienced by Ships.—Methods
of Computing and Comparing Strengths of Ships. V. Construction of Ships.
—Alternative Modes of Construction.—Types of Vessels.—Turret, Self
Trimming, and Trunk Steamers, &c.—Rivets and Rivetting, Workmanship.
will find brought together and ready to his hand, a mass of information
which he would otherwise have to seek in an almost endless variety of
publications, and some of which he would possibly not be able to obtain at
all elsewhere."—Steamship.
THE DESIGN AND CONSTRUCTION OF SHIPS.
By John Harvard Biles, M.Inst.N.A.,
Professor of Naval Architecture in the University of Glasgow. [In Preparation.
Second Edition. Illustrated with Plates, Numerous Diagrams, and Figures in
the Text. 18s. net.
STEEL SHIPS: THEIR CONSTRUCTION AND
MAINTENANCE.
A Manual for Shipbuilders, Ship Superintendents, Students, and Marine Engineers.
By THOMAS WALTON, Naval Architect,
AUTHOR OF "KNOW YOUR OWN SHIP."
Contents.—I. Manufacture of Cast Iron, Wrought Iron, and Steel.—
Composition of Iron and Steel, Quality, Strength, Tests, &c. II.
Classification of Steel Ships. III. Considerations in making choice of Type
of Vessel.—Framing of Ships. IV. Strains experienced by Ships.—Methods
of Computing and Comparing Strengths of Ships. V. Construction of Ships.
—Alternative Modes of Construction.—Types of Vessels.—Turret, Self
Trimming, and Trunk Steamers, &c.—Rivets and Rivetting, Workmanship.
Page 607
VI. Pumping Arrangements. VII. Maintenance.—Prevention of
Deterioration in the Hulls of Ships.—Cement, Paint, &c.—Index.
"So thorough and well written is every chapter in the book that it is difficult
to select any of them as being worthy of exceptional praise. Altogether, the
work is excellent, and will prove of great value to those for whom it is
intended."—The Engineer.
"Mr. Walton has written for the profession of which he is an ornament. His
work will be read and appreciated, no doubt, by every M.I.N.A., and with
great benefit by the majority of them."—Journal of Commerce.
Second Edition, Cloth, 8s. 6d. Leather, for the Pocket, 8s. 6d.
GRIFFIN'S ELECTRICAL PRICE-BOOK: For Electrical, Civil,
Marine, and Borough Engineers, Local Authorities, Architects, Railway
Contractors, &c., &c. Edited by H.J. Dowsing.
"The Electrical Price-Book removes all mystery about the cost of
Electrical Power. By its aid the expense that will be entailed by utilising
electricity on a large or small scale can be discovered."—Architect.
GRIFFIN'S NAUTICAL SERIES,
Edited by EDW. BLACKMORE,
Master Mariner, First Class Trinity House Certificate, Assoc. Inst. N.A.; And Written, mainly, by Sailors for Sailors.
"This admirable series."—Fairplay. "A very useful series."—Nature.
"The volumes of Messrs. Griffin's Nautical Series may well and profitably
be read by all interested in our national maritime progress."—Marine
Engineer.
Deterioration in the Hulls of Ships.—Cement, Paint, &c.—Index.
"So thorough and well written is every chapter in the book that it is difficult
to select any of them as being worthy of exceptional praise. Altogether, the
work is excellent, and will prove of great value to those for whom it is
intended."—The Engineer.
"Mr. Walton has written for the profession of which he is an ornament. His
work will be read and appreciated, no doubt, by every M.I.N.A., and with
great benefit by the majority of them."—Journal of Commerce.
Second Edition, Cloth, 8s. 6d. Leather, for the Pocket, 8s. 6d.
GRIFFIN'S ELECTRICAL PRICE-BOOK: For Electrical, Civil,
Marine, and Borough Engineers, Local Authorities, Architects, Railway
Contractors, &c., &c. Edited by H.J. Dowsing.
"The Electrical Price-Book removes all mystery about the cost of
Electrical Power. By its aid the expense that will be entailed by utilising
electricity on a large or small scale can be discovered."—Architect.
GRIFFIN'S NAUTICAL SERIES,
Edited by EDW. BLACKMORE,
Master Mariner, First Class Trinity House Certificate, Assoc. Inst. N.A.; And Written, mainly, by Sailors for Sailors.
"This admirable series."—Fairplay. "A very useful series."—Nature.
"The volumes of Messrs. Griffin's Nautical Series may well and profitably
be read by all interested in our national maritime progress."—Marine
Engineer.
Page 608
"Every Ship should have the whole Series as a Reference Library.
Handsomely bound, clearly printed and illustrated."—Liverpool Journ.
of Commerce.
The British Mercantile Marine: An Historical Sketch of its Rise and
Development. By the Editor, Capt. Blackmore. 3s. 6d.
"Captain Blackmore's splendid book ... contains paragraphs on every point
of interest to the Merchant Marine. The 243 pages of this book are the most
valuable to the sea captain that have ever been compiled."—Merchant
Service Review.
Elementary Seamanship. By D. Wilson-Barker, Master Mariner,
F.R.S.E., F.R.G.S. With numerous Plates, two in Colours, and Frontispiece.
Third Edition, Thoroughly Revised, Enlarged, and Re-set. With additional
Illustrations. 6s.
"This admirable manual, by Capt. Wilson Barker, of the 'Worcester',
seems to us perfectly designed. "—Athenæum.
Know Your Own Ship: A Simple Explanation of the Stability,
Construction, Tonnage, and Freeboard of Ships. By Thos. Walton, Naval
Architect. With numerous Illustrations and additional Chapters on
Buoyancy, Trim, and Calculations. Sixth Edition, Revised. 7s. 6d.
"Mr. Walton's book will be found very useful."—The Engineer.
Navigation: Theoretical and Practical. By D. Wilson-Barker, Master
Mariner, &c., and William Allingham. Second Edition, Revised. 8s. 6d.
"Precisely the kind of work required for the New Certificates of
competency. Candidates will find it Invaluable."—Dundee Advertiser.
Marine Meteorology: For Officers of the Merchant Navy. By William
Allingham, First Class Honours, Navigation, Science and Art Department.
With Illustrations, Maps, and Diagrams, and facsimile reproduction of log
page. 7s. 6d.
"Quite the best publication on this subject."—Shipping Gazette.
Handsomely bound, clearly printed and illustrated."—Liverpool Journ.
of Commerce.
The British Mercantile Marine: An Historical Sketch of its Rise and
Development. By the Editor, Capt. Blackmore. 3s. 6d.
"Captain Blackmore's splendid book ... contains paragraphs on every point
of interest to the Merchant Marine. The 243 pages of this book are the most
valuable to the sea captain that have ever been compiled."—Merchant
Service Review.
Elementary Seamanship. By D. Wilson-Barker, Master Mariner,
F.R.S.E., F.R.G.S. With numerous Plates, two in Colours, and Frontispiece.
Third Edition, Thoroughly Revised, Enlarged, and Re-set. With additional
Illustrations. 6s.
"This admirable manual, by Capt. Wilson Barker, of the 'Worcester',
seems to us perfectly designed. "—Athenæum.
Know Your Own Ship: A Simple Explanation of the Stability,
Construction, Tonnage, and Freeboard of Ships. By Thos. Walton, Naval
Architect. With numerous Illustrations and additional Chapters on
Buoyancy, Trim, and Calculations. Sixth Edition, Revised. 7s. 6d.
"Mr. Walton's book will be found very useful."—The Engineer.
Navigation: Theoretical and Practical. By D. Wilson-Barker, Master
Mariner, &c., and William Allingham. Second Edition, Revised. 8s. 6d.
"Precisely the kind of work required for the New Certificates of
competency. Candidates will find it Invaluable."—Dundee Advertiser.
Marine Meteorology: For Officers of the Merchant Navy. By William
Allingham, First Class Honours, Navigation, Science and Art Department.
With Illustrations, Maps, and Diagrams, and facsimile reproduction of log
page. 7s. 6d.
"Quite the best publication on this subject."—Shipping Gazette.
Page 609
Latitude and Longitude: How to find them. By W.J. Millar, C.E., late
Sec. to the Inst. of Engineers and Shipbuilders in Scotland. Second Edition,
Revised. 2s.
"Cannot but prove an acquisition to those studying Navigation."—Marine
Engineer.
Practical Mechanics: Applied to the requirements of the Sailor. By Thos.
Mackenzie, Master Mariner, F.R.A.S. Second Edition, Revised. 3s. 6d.
"Well worth the money ... exceedingly helpful."—Shipping World.
Trigonometry: For the Young Sailor, &c. By Rich. C. Buck, of the Thames
Nautical Training College, H.M.S. "Worcester." Second Edition, Revised.
Price 3s. 6d.
"This eminently practical and reliable volume."—Schoolmaster.
Practical Algebra. By Rich. C. Buck. Companion Volume to the above, for
Sailors and others. Price 3s. 6d.
"It is just the book for the young sailor mindful of progress."—Nautical
Magazine.
The Legal Duties of Shipmasters. By Benedict Wm. Ginsburg, M.A.,
LL.D., of the Inner Temple and Northern Circuit; Barrister-at-Law. Second
Edition, Thoroughly Revised and Extended. Price 4s. 6d.
"Invaluable to masters ... We can fully recommend it."—Shipping Gazette.
A Medical and Surgical Help for Shipmasters. Including First Aid at Sea.
By Wm. Johnson Smith, F.R.C.S., Principal Medical Officer, Seamen's
Hospital, Greenwich. Second Edition, Revised. 6s. "Sound, judicious,
really helpful."—The Lancet.
Introductory Volume. Price 3s. 6d.
THE
Sec. to the Inst. of Engineers and Shipbuilders in Scotland. Second Edition,
Revised. 2s.
"Cannot but prove an acquisition to those studying Navigation."—Marine
Engineer.
Practical Mechanics: Applied to the requirements of the Sailor. By Thos.
Mackenzie, Master Mariner, F.R.A.S. Second Edition, Revised. 3s. 6d.
"Well worth the money ... exceedingly helpful."—Shipping World.
Trigonometry: For the Young Sailor, &c. By Rich. C. Buck, of the Thames
Nautical Training College, H.M.S. "Worcester." Second Edition, Revised.
Price 3s. 6d.
"This eminently practical and reliable volume."—Schoolmaster.
Practical Algebra. By Rich. C. Buck. Companion Volume to the above, for
Sailors and others. Price 3s. 6d.
"It is just the book for the young sailor mindful of progress."—Nautical
Magazine.
The Legal Duties of Shipmasters. By Benedict Wm. Ginsburg, M.A.,
LL.D., of the Inner Temple and Northern Circuit; Barrister-at-Law. Second
Edition, Thoroughly Revised and Extended. Price 4s. 6d.
"Invaluable to masters ... We can fully recommend it."—Shipping Gazette.
A Medical and Surgical Help for Shipmasters. Including First Aid at Sea.
By Wm. Johnson Smith, F.R.C.S., Principal Medical Officer, Seamen's
Hospital, Greenwich. Second Edition, Revised. 6s. "Sound, judicious,
really helpful."—The Lancet.
Introductory Volume. Price 3s. 6d.
THE
Page 610
British Mercantile Marine.
By EDWARD BLACKMORE,
MASTER MARINER; ASSOCIATE OF THE INSTITUTION OF NAVAL ARCHITECTS; MEMBER OF THE
INSTITUTION OF ENGINEERS AND SHIPBUILDERS IN SCOTLAND; EDITOR OF GRIFFIN'S "NAUTICAL
SERIES."
General Contents.—Historical: From Early Times to 1486—Progress
under Henry VIII.—To Death of Mary—During Elizabeth's Reign—Up to
the Reign of William III.—The 18th and 19th Centuries—Institution of
Examinations—Rise and Progress of Steam Propulsion—Development of
Free Trade—Shipping Legislation, 1862 to 1875—"Locksley Hall" Case—
Shipmasters' Societies—Loading of Ships—Shipping Legislation, 1884 to
1894—Statistics of Shipping. The Personnel: Shipowners—Officers—
Mariners—Duties and Present Position. Education: A Seaman's Education:
what it should be—Present Means of Education—Hints. Discipline and
Duty—Postscript—The Serious Decrease in the Number of British
Seamen, a Matter demanding the Attention of the Nation.
"Interesting and Instructive ... may be read with profit and enjoyment."—
Glasgow Herald.
"Every Branch of the subject is dealt with in a way which shows that the
writer 'knows the ropes' familiarly."—Scotsman.
"This admirable book ... teems with useful information—Should be in the
hands of every Sailor."—Western Morning News.
Third Edition, Thoroughly Revised, Enlarged, and Re-set. With Additional
Illustrations. Price 6s.
A MANUAL OF ELEMENTARY SEAMANSHIP.
BY
By EDWARD BLACKMORE,
MASTER MARINER; ASSOCIATE OF THE INSTITUTION OF NAVAL ARCHITECTS; MEMBER OF THE
INSTITUTION OF ENGINEERS AND SHIPBUILDERS IN SCOTLAND; EDITOR OF GRIFFIN'S "NAUTICAL
SERIES."
General Contents.—Historical: From Early Times to 1486—Progress
under Henry VIII.—To Death of Mary—During Elizabeth's Reign—Up to
the Reign of William III.—The 18th and 19th Centuries—Institution of
Examinations—Rise and Progress of Steam Propulsion—Development of
Free Trade—Shipping Legislation, 1862 to 1875—"Locksley Hall" Case—
Shipmasters' Societies—Loading of Ships—Shipping Legislation, 1884 to
1894—Statistics of Shipping. The Personnel: Shipowners—Officers—
Mariners—Duties and Present Position. Education: A Seaman's Education:
what it should be—Present Means of Education—Hints. Discipline and
Duty—Postscript—The Serious Decrease in the Number of British
Seamen, a Matter demanding the Attention of the Nation.
"Interesting and Instructive ... may be read with profit and enjoyment."—
Glasgow Herald.
"Every Branch of the subject is dealt with in a way which shows that the
writer 'knows the ropes' familiarly."—Scotsman.
"This admirable book ... teems with useful information—Should be in the
hands of every Sailor."—Western Morning News.
Third Edition, Thoroughly Revised, Enlarged, and Re-set. With Additional
Illustrations. Price 6s.
A MANUAL OF ELEMENTARY SEAMANSHIP.
BY
Page 611
D. WILSON-BARKER, Master Mariner; F.R.S.E., F.R.G.S., &c., &c.;
YOUNGER BROTHER OF THE TRINITY HOUSE.
With Frontispiece, Numerous Plates (Two in Colours), and Illustrations in
the Text.
General Contents.—The Building of a Ship; Parts of Hull, Masts, &c.—
Ropes, Knots, Splicing, &c.—Gear, Lead and Log, &c.—Rigging, Anchors
—Sailmaking—The Sails, &c.—Handling of Boats under Sail—Signals
and Signalling—Rule of the Road—Keeping and Relieving Watch—Points
of Etiquette—Glossary of Sea Terms and Phrases—Index.
*** The volume contains the new rules of the road.
"This admirable manual, by Capt. Wilson-Barker of the 'Worcester,'
seems to us perfectly designed, and holds its place excellently in Griffin's
Nautical Series.' ... Although intended for those who are to become
Officers of the Merchant Navy, it will be found useful by all
yachtsmen."—Athenæum.
*** For complete List of Griffin's Nautical Series, see p. 39.
Second Edition, Revised and Illustrated. Price 3s. 6d.
NAVIGATION:
PRACTICAL AND THEORETICAL
By DAVID WILSON-BARKER, R.N.R, F.R.S.E., &c., &c.,
AND
WILLIAM ALLINGHAM,
FIRST-CLASS HONORS, NAVIGATION, SCIENCE AND ART DEPARTMENT.
YOUNGER BROTHER OF THE TRINITY HOUSE.
With Frontispiece, Numerous Plates (Two in Colours), and Illustrations in
the Text.
General Contents.—The Building of a Ship; Parts of Hull, Masts, &c.—
Ropes, Knots, Splicing, &c.—Gear, Lead and Log, &c.—Rigging, Anchors
—Sailmaking—The Sails, &c.—Handling of Boats under Sail—Signals
and Signalling—Rule of the Road—Keeping and Relieving Watch—Points
of Etiquette—Glossary of Sea Terms and Phrases—Index.
*** The volume contains the new rules of the road.
"This admirable manual, by Capt. Wilson-Barker of the 'Worcester,'
seems to us perfectly designed, and holds its place excellently in Griffin's
Nautical Series.' ... Although intended for those who are to become
Officers of the Merchant Navy, it will be found useful by all
yachtsmen."—Athenæum.
*** For complete List of Griffin's Nautical Series, see p. 39.
Second Edition, Revised and Illustrated. Price 3s. 6d.
NAVIGATION:
PRACTICAL AND THEORETICAL
By DAVID WILSON-BARKER, R.N.R, F.R.S.E., &c., &c.,
AND
WILLIAM ALLINGHAM,
FIRST-CLASS HONORS, NAVIGATION, SCIENCE AND ART DEPARTMENT.
Page 612
With Numerous Illustrations and Examination Questions.
General Contents.—Definitions—Latitude and Longitude—Instruments of
Navigation—Correction of Courses—Plane Sailing—Traverse Sailing—
Day's Work—Parallel Sailing—Middle Latitude Sailing—Mercator's Chart
—Mercator Sailing—Current Sailing—Position by Bearings—Great Circle
Sailing—The Tides—Questions—Appendix: Compass Error—Numerous
Useful Hints, &c.—Index.
"Precisely the kind of work required for the New Certificates of
competency in grades from Second Mate to extra Master.... Candidates will
find it invaluable."—Dundee Advertiser.
"A capital little book ... specially adapted to the New Examinations. The
Authors are Capt. Wilson-Barker (Captain-Superintendent of the Nautical
College, H.M.S. 'Worcester,' who has had great experience in the highest
problems of Navigation), and Mr. Allingham, a well-known writer on the
Science of Navigation and Nautical Astronomy."—Shipping World.
Handsome Cloth. Fully Illustrated. Price 7s. 6d.
MARINE METEOROLOGY, FOR OFFICERS OF THE
MERCHANT NAVY.
By WILLIAM ALLINGHAM,
Joint Author of "Navigation, Theoretical and Practical."
With numerous Plates, Maps, Diagrams, and Illustrations, and a facsimile
Reproduction of a Page from an actual Meteorological Log-Book.
SUMMARY OF CONTENTS.
Introductory.—Instruments Used at Sea for Meteorological Purposes.—
Meteorological Log-Books.—Atmospheric Pressure.—Air Temperatures.—
General Contents.—Definitions—Latitude and Longitude—Instruments of
Navigation—Correction of Courses—Plane Sailing—Traverse Sailing—
Day's Work—Parallel Sailing—Middle Latitude Sailing—Mercator's Chart
—Mercator Sailing—Current Sailing—Position by Bearings—Great Circle
Sailing—The Tides—Questions—Appendix: Compass Error—Numerous
Useful Hints, &c.—Index.
"Precisely the kind of work required for the New Certificates of
competency in grades from Second Mate to extra Master.... Candidates will
find it invaluable."—Dundee Advertiser.
"A capital little book ... specially adapted to the New Examinations. The
Authors are Capt. Wilson-Barker (Captain-Superintendent of the Nautical
College, H.M.S. 'Worcester,' who has had great experience in the highest
problems of Navigation), and Mr. Allingham, a well-known writer on the
Science of Navigation and Nautical Astronomy."—Shipping World.
Handsome Cloth. Fully Illustrated. Price 7s. 6d.
MARINE METEOROLOGY, FOR OFFICERS OF THE
MERCHANT NAVY.
By WILLIAM ALLINGHAM,
Joint Author of "Navigation, Theoretical and Practical."
With numerous Plates, Maps, Diagrams, and Illustrations, and a facsimile
Reproduction of a Page from an actual Meteorological Log-Book.
SUMMARY OF CONTENTS.
Introductory.—Instruments Used at Sea for Meteorological Purposes.—
Meteorological Log-Books.—Atmospheric Pressure.—Air Temperatures.—
Page 613
Sea Temperatures.—Winds.—Wind Force Scales.—History of the Law of
Storms.—Hurricanes, Seasons, and Storm Tracks.—Solution of the Cyclone
Problem.—Ocean Currents.—Icebergs.—Synchronous Charts.—Dew,
Mists, Fogs, and Haze.—Clouds.—Rain, Snow, and Hail.—Mirage,
Rainbows, Coronas, Halos, and Meteors.—Lightning, Corposants, and
Auroras.—Questions.—Appendix.—Index.
"Quite the best publication, AND certainly the most interesting, on this
subject ever presented to Nautical men."—Shipping Gazette.
*** For Complete List of Griffin's Nautical Series, see p. 39.
Second Edition, Revised. With Numerous Illustrations. Price 3s. 6d.
Practical Mechanics: Applied to the Requirements of the Sailor.
By THOS. MACKENZIE,
Master Mariner, F.R.A.S.
General Contents.—Resolution and Composition of Forces—Work done
by Machines and Living Agents—The Mechanical Powers: The Lever;
Derricks as Bent Levers—The Wheel and Axle: Windlass; Ship's Capstan;
Crab Winch—Tackles: the "Old Man"—The Inclined Plane; the Screw—
The Centre of Gravity of a Ship and Cargo—Relative Strength of Rope:
Steel Wire, Manilla, Hemp, Coir—Derricks and Shears—Calculation of the
Cross-breaking Strain of Fir Spar—Centre of Effort of Sails—Hydrostatics:
the Diving-bell; Stability of Floating Bodies; the Ship's Pump, &c.
"This Excellent Book ... contains a LARGE AMOUNT of information."—
Nature.
"Well worth the money ... will be found EXCEEDINGLY HELPFUL."—
Shipping World.
Storms.—Hurricanes, Seasons, and Storm Tracks.—Solution of the Cyclone
Problem.—Ocean Currents.—Icebergs.—Synchronous Charts.—Dew,
Mists, Fogs, and Haze.—Clouds.—Rain, Snow, and Hail.—Mirage,
Rainbows, Coronas, Halos, and Meteors.—Lightning, Corposants, and
Auroras.—Questions.—Appendix.—Index.
"Quite the best publication, AND certainly the most interesting, on this
subject ever presented to Nautical men."—Shipping Gazette.
*** For Complete List of Griffin's Nautical Series, see p. 39.
Second Edition, Revised. With Numerous Illustrations. Price 3s. 6d.
Practical Mechanics: Applied to the Requirements of the Sailor.
By THOS. MACKENZIE,
Master Mariner, F.R.A.S.
General Contents.—Resolution and Composition of Forces—Work done
by Machines and Living Agents—The Mechanical Powers: The Lever;
Derricks as Bent Levers—The Wheel and Axle: Windlass; Ship's Capstan;
Crab Winch—Tackles: the "Old Man"—The Inclined Plane; the Screw—
The Centre of Gravity of a Ship and Cargo—Relative Strength of Rope:
Steel Wire, Manilla, Hemp, Coir—Derricks and Shears—Calculation of the
Cross-breaking Strain of Fir Spar—Centre of Effort of Sails—Hydrostatics:
the Diving-bell; Stability of Floating Bodies; the Ship's Pump, &c.
"This Excellent Book ... contains a LARGE AMOUNT of information."—
Nature.
"Well worth the money ... will be found EXCEEDINGLY HELPFUL."—
Shipping World.
Page 614
"No Ships' Officers' bookcase will henceforth be complete without Captain
Mackenzie's 'Practical Mechanics.' Notwithstanding my many years'
experience at sea, it has told me how much more there is to acquire."—
(Letter to the Publishers from a Master Mariner).
"I must express my thanks to you for the labour and care you have taken in
'Practical Mechanics.' ... It is a life's experience. ... What an amount we
frequently see wasted by rigging purchases without reason and accidents to
spars, &c., &c.! 'Practical Mechanics' would save all this."—(Letter to
the Author from another Master Mariner).
WORKS BY RICHARD C. BUCK,
of the Thames Nautical Training College, H.M.S. 'Worcester.'
A Manual of Trigonometry: With Diagrams, Examples, and
Exercises. Price 3s. 6d.
Second Edition, Revised and Corrected.
*** Mr. Buck's Text-Book has been specially prepared with a view to the
New Examinations of the Board of Trade, in which Trigonometry is an
obligatory subject.
"This eminently practical and reliable volume."—Schoolmaster.
A Manual of Algebra.
Designed to meet the Requirements of Sailors and others. Price 3s. 6d.
*** These elementary works on algebra and trigonometry are written
specially for those who will have little opportunity of consulting a Teacher.
Mackenzie's 'Practical Mechanics.' Notwithstanding my many years'
experience at sea, it has told me how much more there is to acquire."—
(Letter to the Publishers from a Master Mariner).
"I must express my thanks to you for the labour and care you have taken in
'Practical Mechanics.' ... It is a life's experience. ... What an amount we
frequently see wasted by rigging purchases without reason and accidents to
spars, &c., &c.! 'Practical Mechanics' would save all this."—(Letter to
the Author from another Master Mariner).
WORKS BY RICHARD C. BUCK,
of the Thames Nautical Training College, H.M.S. 'Worcester.'
A Manual of Trigonometry: With Diagrams, Examples, and
Exercises. Price 3s. 6d.
Second Edition, Revised and Corrected.
*** Mr. Buck's Text-Book has been specially prepared with a view to the
New Examinations of the Board of Trade, in which Trigonometry is an
obligatory subject.
"This eminently practical and reliable volume."—Schoolmaster.
A Manual of Algebra.
Designed to meet the Requirements of Sailors and others. Price 3s. 6d.
*** These elementary works on algebra and trigonometry are written
specially for those who will have little opportunity of consulting a Teacher.
Page 615
They are books for "self-help." All but the simplest explanations have,
therefore, been avoided, and answers to the Exercises are given. Any
person may readily, by careful study, become master of their contents, and
thus lay the foundation for a further mathematical course, if desired. It is
hoped that to the younger Officers of our Mercantile Marine they will be
found decidedly serviceable. The Examples and Exercises are taken from
the Examination Papers set for the Cadets of the "Worcester."
"Clearly arranged, and well got up.... A first-rate Elementary Algebra."—
Nautical Magazine.
Second Edition, Thoroughly Revised and Extended. In Crown 8vo.
Handsome Cloth. Price 4s. 6d.
THE LEGAL DUTIES OF SHIPMASTERS.
BY
BENEDICT WM. GINSBURG, M.A., LL.D. (Cantab.),
Of the Inner Temple and Northern Circuit; Barrister-at-Law.
General Contents.—The Qualification for the Position of Shipmaster—
The Contract with the Shipowner—The Master's Duty in respect of the
Crew: Engagement; Apprentices; Discipline; Provisions, Accommodation,
and Medical Comforts; Payment of Wages and Discharge—The Master's
Duty in respect of the Passengers—The Master's Financial Responsibilities
—The Master's Duty in respect of the Cargo—The Master's Duty in Case of
Casualty—The Master's Duty to certain Public Authorities—The Master's
Duty in relation to Pilots, Signals, Flags, and Light Dues—The Master's
Duty upon Arrival at the Port of Discharge—Appendices relative to certain
Legal Matters: Board of Trade Certificates, Dietary Scales, Stowage of
Grain Cargoes, Load Line Regulations, Life-saving Appliances, Carriage of
Cattle at Sea, &c., &c.—Copious Index.
therefore, been avoided, and answers to the Exercises are given. Any
person may readily, by careful study, become master of their contents, and
thus lay the foundation for a further mathematical course, if desired. It is
hoped that to the younger Officers of our Mercantile Marine they will be
found decidedly serviceable. The Examples and Exercises are taken from
the Examination Papers set for the Cadets of the "Worcester."
"Clearly arranged, and well got up.... A first-rate Elementary Algebra."—
Nautical Magazine.
Second Edition, Thoroughly Revised and Extended. In Crown 8vo.
Handsome Cloth. Price 4s. 6d.
THE LEGAL DUTIES OF SHIPMASTERS.
BY
BENEDICT WM. GINSBURG, M.A., LL.D. (Cantab.),
Of the Inner Temple and Northern Circuit; Barrister-at-Law.
General Contents.—The Qualification for the Position of Shipmaster—
The Contract with the Shipowner—The Master's Duty in respect of the
Crew: Engagement; Apprentices; Discipline; Provisions, Accommodation,
and Medical Comforts; Payment of Wages and Discharge—The Master's
Duty in respect of the Passengers—The Master's Financial Responsibilities
—The Master's Duty in respect of the Cargo—The Master's Duty in Case of
Casualty—The Master's Duty to certain Public Authorities—The Master's
Duty in relation to Pilots, Signals, Flags, and Light Dues—The Master's
Duty upon Arrival at the Port of Discharge—Appendices relative to certain
Legal Matters: Board of Trade Certificates, Dietary Scales, Stowage of
Grain Cargoes, Load Line Regulations, Life-saving Appliances, Carriage of
Cattle at Sea, &c., &c.—Copious Index.
Page 616
"No intelligent Master should fail to add this to his list of necessary books.
A few lines of it may save a lawyer's fee, besides endless worry."—
Liverpool Journal of Commerce.
"Sensible, plainly written, in CLEAR and non-technical language, and
will be found of much service by the Shipmaster."—British Trade Review.
Second Edition, Revised. With Diagrams. Price 2s.
Latitude and Longitude: How to Find them.
By W.J. MILLAR, C.E.,
Late Secretary to the Inst. of Engineers and Shipbuilders in Scotland.
"Concisely and clearly written ... cannot but prove an acquisition to those
studying Navigation."—Marine Engineer.
"Young Seamen will find it handy and useful, simple and clear."—The
Engineer.
FIRST AID AT SEA.
Second Edition, Revised. With Coloured Plates and Numerous Illustrations, and comprising
the latest Regulations Respecting the Carriage of Medical Stores on Board Ship. Price 6s.
A MEDICAL AND SURGICAL HELP FOR SHIPMASTERS
AND OFFICERS IN THE MERCHANT NAVY.
BY
WM. JOHNSON SMITH, F.R.C.S.,
A few lines of it may save a lawyer's fee, besides endless worry."—
Liverpool Journal of Commerce.
"Sensible, plainly written, in CLEAR and non-technical language, and
will be found of much service by the Shipmaster."—British Trade Review.
Second Edition, Revised. With Diagrams. Price 2s.
Latitude and Longitude: How to Find them.
By W.J. MILLAR, C.E.,
Late Secretary to the Inst. of Engineers and Shipbuilders in Scotland.
"Concisely and clearly written ... cannot but prove an acquisition to those
studying Navigation."—Marine Engineer.
"Young Seamen will find it handy and useful, simple and clear."—The
Engineer.
FIRST AID AT SEA.
Second Edition, Revised. With Coloured Plates and Numerous Illustrations, and comprising
the latest Regulations Respecting the Carriage of Medical Stores on Board Ship. Price 6s.
A MEDICAL AND SURGICAL HELP FOR SHIPMASTERS
AND OFFICERS IN THE MERCHANT NAVY.
BY
WM. JOHNSON SMITH, F.R.C.S.,
Page 617
Principal Medical Officer, Seamen's Hospital, Greenwich.
*** The attention of all interested in our Merchant Navy is requested to this
exceedingly useful and valuable work. It is needless to say that it is the
outcome of many years practical experience amongst Seamen.
"Sound, judicious, really helpful."—The Lancet.
Sixth Edition. Revised, with Chapters on Trim, Buoyancy, and
Calculations. Numerous Illustrations. Handsome Cloth, Crown 8vo. Price
7s. 6d.
KNOW YOUR OWN SHIP.
By THOMAS WALTON, Naval Architect.
SPECIALLY ARRANGED TO SUIT THE REQUIREMENTS OF SHIPS' OFFICERS,
SHIPOWNERS, SUPERINTENDENTS, DRAUGHTSMEN, ENGINEERS, AND OTHERS.
This work explains, in a simple manner, such important subjects as:—
Displacement,
Deadweight,
Tonnage,
Freeboard,
Moments,
Buoyancy,
Strain,
Structure,
Stability,
Rolling,
Ballasting,
Loading,
Shifting Cargoes,
Admission of Water,
*** The attention of all interested in our Merchant Navy is requested to this
exceedingly useful and valuable work. It is needless to say that it is the
outcome of many years practical experience amongst Seamen.
"Sound, judicious, really helpful."—The Lancet.
Sixth Edition. Revised, with Chapters on Trim, Buoyancy, and
Calculations. Numerous Illustrations. Handsome Cloth, Crown 8vo. Price
7s. 6d.
KNOW YOUR OWN SHIP.
By THOMAS WALTON, Naval Architect.
SPECIALLY ARRANGED TO SUIT THE REQUIREMENTS OF SHIPS' OFFICERS,
SHIPOWNERS, SUPERINTENDENTS, DRAUGHTSMEN, ENGINEERS, AND OTHERS.
This work explains, in a simple manner, such important subjects as:—
Displacement,
Deadweight,
Tonnage,
Freeboard,
Moments,
Buoyancy,
Strain,
Structure,
Stability,
Rolling,
Ballasting,
Loading,
Shifting Cargoes,
Admission of Water,
Page 618
Sail Area,
&c., &c.
"The little book will be found exceedingly handy by most officers and
officials connected with shipping.... Mr. Walton's work will obtain lasting
success, because of its unique fitness for those for whom it has been
written."—Shipping World.
"An excellent work, full of solid instruction and invaluable to every
officer of the Mercantile Marine who has his profession at heart."—
Shipping.
"Not one of the 242 pages could well be spared. It will admirably fulfil its
purpose ... useful to ship owners, ship superintendents, ship draughtsmen,
and all interested in shipping."—Liverpool Journal of Commerce.
"A mass of very useful information, accompanied by diagrams and
illustrations, is given in a compact form."—Fairplay.
"We have found no one statement that we could have wished differently
expressed. The matter has, so far as clearness allows, been admirably
condensed, and is simple enough to be understood by every seaman."—
Marine Engineer.
BY THE SAME AUTHOR.
Steel Ships: Their Construction and Maintenance.
(See page 38.)
Fourteenth Edition, Revised. Price 21s.
Demy 8vo, Cloth. With Numerous Illustrations, reduced from Working
Drawings.
&c., &c.
"The little book will be found exceedingly handy by most officers and
officials connected with shipping.... Mr. Walton's work will obtain lasting
success, because of its unique fitness for those for whom it has been
written."—Shipping World.
"An excellent work, full of solid instruction and invaluable to every
officer of the Mercantile Marine who has his profession at heart."—
Shipping.
"Not one of the 242 pages could well be spared. It will admirably fulfil its
purpose ... useful to ship owners, ship superintendents, ship draughtsmen,
and all interested in shipping."—Liverpool Journal of Commerce.
"A mass of very useful information, accompanied by diagrams and
illustrations, is given in a compact form."—Fairplay.
"We have found no one statement that we could have wished differently
expressed. The matter has, so far as clearness allows, been admirably
condensed, and is simple enough to be understood by every seaman."—
Marine Engineer.
BY THE SAME AUTHOR.
Steel Ships: Their Construction and Maintenance.
(See page 38.)
Fourteenth Edition, Revised. Price 21s.
Demy 8vo, Cloth. With Numerous Illustrations, reduced from Working
Drawings.
Page 619
A MANUAL OF MARINE ENGINEERING: COMPRISING
THE DESIGNING, CONSTRUCTION, AND WORKING OF
MARINE MACHINERY.
By A.E. SEATON, M. Inst. C.E., M. Inst. Mech. E., M. Inst. N.A.
General Contents.—Part I.—Principles of Marine Propulsion. Part II.—
Principles of Steam Engineering. Part III.—Details of Marine Engines:
Design and Calculations for Cylinders, Pistons, Valves, Expansion Valves,
&c. Part IV.—Propellers. Part V.—Boilers. Part VI.—Miscellaneous.
*** This Edition includes a Chapter on Water-Tube Boilers, with
Illustrations of the leading Types and the Revised Rules of the Bureau
Veritas.
"In the three-fold capacity of enabling a Student to learn how to design,
construct, and work a Marine Steam-Engine, Mr. Seaton's Manual has no
rival."—Times.
"By far the best Manual in existence.... Gives a complete account of the
methods of solving, with the utmost possible economy, the problems before
the Marine Engineer."—Athenæum.
"The Student, Draughtsman, and Engineer will find this work the most
valuable Handbook of Reference on the Marine Engine now in
existence."—Marine Engineer.
Seventh Edition, Thoroughly Revised. Pocket-Size, Leather. 8s. 6d.
A POCKET-BOOK OF MARINE ENGINEERING RULES
AND TABLES, FOR THE USE OF
Marine Engineers, Naval Architects, Designers, Draughtsmen,
Superintendents and Others.
THE DESIGNING, CONSTRUCTION, AND WORKING OF
MARINE MACHINERY.
By A.E. SEATON, M. Inst. C.E., M. Inst. Mech. E., M. Inst. N.A.
General Contents.—Part I.—Principles of Marine Propulsion. Part II.—
Principles of Steam Engineering. Part III.—Details of Marine Engines:
Design and Calculations for Cylinders, Pistons, Valves, Expansion Valves,
&c. Part IV.—Propellers. Part V.—Boilers. Part VI.—Miscellaneous.
*** This Edition includes a Chapter on Water-Tube Boilers, with
Illustrations of the leading Types and the Revised Rules of the Bureau
Veritas.
"In the three-fold capacity of enabling a Student to learn how to design,
construct, and work a Marine Steam-Engine, Mr. Seaton's Manual has no
rival."—Times.
"By far the best Manual in existence.... Gives a complete account of the
methods of solving, with the utmost possible economy, the problems before
the Marine Engineer."—Athenæum.
"The Student, Draughtsman, and Engineer will find this work the most
valuable Handbook of Reference on the Marine Engine now in
existence."—Marine Engineer.
Seventh Edition, Thoroughly Revised. Pocket-Size, Leather. 8s. 6d.
A POCKET-BOOK OF MARINE ENGINEERING RULES
AND TABLES, FOR THE USE OF
Marine Engineers, Naval Architects, Designers, Draughtsmen,
Superintendents and Others.
Page 620
BY
A.E. SEATON, M.I.C.E., M.I.Mech.E., M.I.N.A.,
AND
H.M. ROUNTHWAITE, M.I.Mech.E., M.I.N.A.
"Admirably fulfils its purpose."—Marine Engineer.
By B. CUNNINGHAM.
DOCKS: THEIR CONSTRUCTION & MAINTENANCE.
(See page 27.)
WORKS BY PROF. ROBERT H. SMITH, Assoc. M.I.C.E., M.I.M.E.,
M.I.El.B., M.I. Min. E., Whit. Sch., M. Ord. Meiji.
THE CALCULUS FOR ENGINEERS AND PHYSICISTS,
Applied to Technical Problems.
WITH EXTENSIVE CLASSIFIED REFERENCE LIST OF INTEGRALS.
By PROF. ROBERT H. SMITH.
ASSISTED BY
A.E. SEATON, M.I.C.E., M.I.Mech.E., M.I.N.A.,
AND
H.M. ROUNTHWAITE, M.I.Mech.E., M.I.N.A.
"Admirably fulfils its purpose."—Marine Engineer.
By B. CUNNINGHAM.
DOCKS: THEIR CONSTRUCTION & MAINTENANCE.
(See page 27.)
WORKS BY PROF. ROBERT H. SMITH, Assoc. M.I.C.E., M.I.M.E.,
M.I.El.B., M.I. Min. E., Whit. Sch., M. Ord. Meiji.
THE CALCULUS FOR ENGINEERS AND PHYSICISTS,
Applied to Technical Problems.
WITH EXTENSIVE CLASSIFIED REFERENCE LIST OF INTEGRALS.
By PROF. ROBERT H. SMITH.
ASSISTED BY
Page 621
R.F. MUIRHEAD, M.A., B.Sc.,
Formerly Clark Fellow of Glasgow University, and Lecturer on Mathematics at Mason College.
In Crown 8vo, extra, with Diagrams and Folding-Plate. 8s. 6d.
"Prof. R.H. Smith's book will be serviceable in rendering a hard road as
easy as practicable for the non-mathematical Student and Engineer."—
Athenæum.
"Interesting diagrams, with practical illustrations of actual occurrence, are
to be found here in abundance. The very complete classified reference
table will prove very useful in saving the time of those who want an
integral in a hurry."—The Engineer.
MEASUREMENT CONVERSIONS
(English and French): 28 GRAPHIC TABLES OR DIAGRAMS.
Showing at a glance the Mutual Conversion of Measurements in
Different Units
Of Lengths, Areas, Volumes, Weights, Stresses, Densities, Quantities of
Work, Horse Powers, Temperatures, &c.
For the use of Engineers, Surveyors, Architects, and Contractors.
In 4to, Boards. 7s. 6d.
*** Prof. Smith's Conversion-Tables form the most unique and
comprehensive collection ever placed before the profession. By their use
much time and labour will be saved, and the chances of error in calculation
Formerly Clark Fellow of Glasgow University, and Lecturer on Mathematics at Mason College.
In Crown 8vo, extra, with Diagrams and Folding-Plate. 8s. 6d.
"Prof. R.H. Smith's book will be serviceable in rendering a hard road as
easy as practicable for the non-mathematical Student and Engineer."—
Athenæum.
"Interesting diagrams, with practical illustrations of actual occurrence, are
to be found here in abundance. The very complete classified reference
table will prove very useful in saving the time of those who want an
integral in a hurry."—The Engineer.
MEASUREMENT CONVERSIONS
(English and French): 28 GRAPHIC TABLES OR DIAGRAMS.
Showing at a glance the Mutual Conversion of Measurements in
Different Units
Of Lengths, Areas, Volumes, Weights, Stresses, Densities, Quantities of
Work, Horse Powers, Temperatures, &c.
For the use of Engineers, Surveyors, Architects, and Contractors.
In 4to, Boards. 7s. 6d.
*** Prof. Smith's Conversion-Tables form the most unique and
comprehensive collection ever placed before the profession. By their use
much time and labour will be saved, and the chances of error in calculation
Page 622
diminished. It is believed that henceforth no Engineer's Office will be
considered complete without them.
"The work is invaluable."—Colliery Guardian.
"Ought to be in every office where even occasional conversions are
required.... Prof. Smith's Tables form very excellent checks on results."—
Electrical Review.
"Prof. Smith deserves the hearty thanks, not only of the Engineer, but of the
Commercial World, for having smoothed the way for the adoption of the
Metric System of Measurement, a subject which is now assuming great
importance as a factor in maintaining our hold upon foreign trade."—The
Machinery Market.
In Large 8vo. Handsome Cloth. 10s. 6d.
CHEMISTRY FOR ENGINEERS.
BY
BERTRAM BLOUNT, F.I.C., F.C.S., A.I.C.E.,
Consulting Chemist to the Crown Agents for the Colonies.
AND
A.G. BLOXAM, F.I.C., F.C.S.,
Consulting Chemist, Head of the Chemistry Department, Goldsmiths' Inst., New Cross.
GENERAL CONTENTS.—Introduction—Chemistry of the Chief Materials
of Construction—Sources of Energy—Chemistry of Steam-raising—
Chemistry of Lubrication and Lubricants—Metallurgical Processes used in
the Winning and Manufacture of Metals.
considered complete without them.
"The work is invaluable."—Colliery Guardian.
"Ought to be in every office where even occasional conversions are
required.... Prof. Smith's Tables form very excellent checks on results."—
Electrical Review.
"Prof. Smith deserves the hearty thanks, not only of the Engineer, but of the
Commercial World, for having smoothed the way for the adoption of the
Metric System of Measurement, a subject which is now assuming great
importance as a factor in maintaining our hold upon foreign trade."—The
Machinery Market.
In Large 8vo. Handsome Cloth. 10s. 6d.
CHEMISTRY FOR ENGINEERS.
BY
BERTRAM BLOUNT, F.I.C., F.C.S., A.I.C.E.,
Consulting Chemist to the Crown Agents for the Colonies.
AND
A.G. BLOXAM, F.I.C., F.C.S.,
Consulting Chemist, Head of the Chemistry Department, Goldsmiths' Inst., New Cross.
GENERAL CONTENTS.—Introduction—Chemistry of the Chief Materials
of Construction—Sources of Energy—Chemistry of Steam-raising—
Chemistry of Lubrication and Lubricants—Metallurgical Processes used in
the Winning and Manufacture of Metals.
Page 623
"The authors have succeeded beyond all expectation, and have produced a
work which should give fresh power to the Engineer and Manufacturer."—
The Times.
"Practical throughout ... an admirable text-book, useful not only to
Students, but to Engineers and Managers of works in preventing waste
and improving processes."—Scotsman.
"A book worthy to take high rank ... treatment of the subject of gaseous
fuel particularly good.... Water gas and its production clearly worked
out.... We warmly recommend the work."—Journal of Gas Lighting.
For Companion Volume by the same Authors, see "Chemistry for
Manufacturers," p. 71.
Works by WALTER R. BROWNE, M.A., M. Inst. C.E.,
Late Fellow of Trinity College, Cambridge.
THE STUDENT'S MECHANICS: An Introduction to the
Study of Force and Motion.
With Diagrams. Crown 8vo. Cloth, 4s. 6d.
"Clear in style and practical in method, 'The Student's Mechanics' is
cordially to be commended from all points of view."—Athenæum.
FOUNDATIONS OF MECHANICS.
Papers reprinted from the Engineer. In Crown 8vo, 1s.
work which should give fresh power to the Engineer and Manufacturer."—
The Times.
"Practical throughout ... an admirable text-book, useful not only to
Students, but to Engineers and Managers of works in preventing waste
and improving processes."—Scotsman.
"A book worthy to take high rank ... treatment of the subject of gaseous
fuel particularly good.... Water gas and its production clearly worked
out.... We warmly recommend the work."—Journal of Gas Lighting.
For Companion Volume by the same Authors, see "Chemistry for
Manufacturers," p. 71.
Works by WALTER R. BROWNE, M.A., M. Inst. C.E.,
Late Fellow of Trinity College, Cambridge.
THE STUDENT'S MECHANICS: An Introduction to the
Study of Force and Motion.
With Diagrams. Crown 8vo. Cloth, 4s. 6d.
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FOUNDATIONS OF MECHANICS.
Papers reprinted from the Engineer. In Crown 8vo, 1s.
Page 624
Demy 8vo, with Numerous Illustrations, 9s.
FUEL AND WATER: A Manual for Users of Steam and Water.
By Prof. FRANZ SCHWACKHÖFER of Vienna, and WALTER R.
BROWNE, M.A., C.E.
General Contents.—Heat and Combustion—Fuel, Varieties of—Firing
Arrangements: Furnace, Flues, Chimney—The Boiler, Choice of—Varieties
—Feed-water Heaters—Steam Pipes—Water: Composition, Purification—
Prevention of Scale, &c., &c.
"The Section on Heat is one of the best and most lucid ever written."—
Engineer.
"Cannot fail to be valuable to thousands using steam power."—Railway
Engineer.
GRIFFINS LOCAL GOVERNMENT HANDBOOKS.
WORKS SUITABLE FOR MUNICIPAL AND COUNTY
ENGINEERS, ANALYSTS, AND OTHERS.
See also Davies' Hygiene, p. 99, and MacLeod's Public Health, p. 110.
Gas Manufacture (The Chemistry of). A Handbook on the Production,
Purification, and Testing of Illuminating Gas, and the Assay of Bye-
Products. By W.J.A. Butterfield, M.A., F.I.C., F.C.S. With Illustrations.
Third Edition, Revised (in preparation). [See page 77.
Water Supply: A Practical Treatise on the Selection of Sources and the
Distribution of Water. By Reginald E. Middleton, M. Inst. C.E., M. Inst.
Mech. E., F.S.I. With Four Plates and Numerous Diagrams. Crown 8vo.
[See page 77.
FUEL AND WATER: A Manual for Users of Steam and Water.
By Prof. FRANZ SCHWACKHÖFER of Vienna, and WALTER R.
BROWNE, M.A., C.E.
General Contents.—Heat and Combustion—Fuel, Varieties of—Firing
Arrangements: Furnace, Flues, Chimney—The Boiler, Choice of—Varieties
—Feed-water Heaters—Steam Pipes—Water: Composition, Purification—
Prevention of Scale, &c., &c.
"The Section on Heat is one of the best and most lucid ever written."—
Engineer.
"Cannot fail to be valuable to thousands using steam power."—Railway
Engineer.
GRIFFINS LOCAL GOVERNMENT HANDBOOKS.
WORKS SUITABLE FOR MUNICIPAL AND COUNTY
ENGINEERS, ANALYSTS, AND OTHERS.
See also Davies' Hygiene, p. 99, and MacLeod's Public Health, p. 110.
Gas Manufacture (The Chemistry of). A Handbook on the Production,
Purification, and Testing of Illuminating Gas, and the Assay of Bye-
Products. By W.J.A. Butterfield, M.A., F.I.C., F.C.S. With Illustrations.
Third Edition, Revised (in preparation). [See page 77.
Water Supply: A Practical Treatise on the Selection of Sources and the
Distribution of Water. By Reginald E. Middleton, M. Inst. C.E., M. Inst.
Mech. E., F.S.I. With Four Plates and Numerous Diagrams. Crown 8vo.
[See page 77.
Page 625
Central Electrical Stations: Their Design, Organisation, and Management.
By C.H. Wordingham, A.K.C., M. Inst. C.E. Price 24s. net.
For details see opposite page.
Sewage Disposal Works: A Guide to the Construction of Works for the
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Santo Crimp, M. Inst. C.E., F.G.S. Second Edition, Revised and Enlarged.
Large 8vo, Handsome Cloth. With 37 Plates. Price 30s. [See page 76.
Trades' Waste: Its Treatment and Utilisation, with Special Reference to the
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Numerous Plates, Diagrams, and Illustrations. 21s. net. [See page 76.
Calcareous Cements: Their Nature, Preparation, and Uses. With some
Remarks upon Cement Testing. By Gilbert Redgrave, Assoc. Inst. C.E.
With Illustrations, Analytical Data, and Appendices on Costs, &c. 8s. 6d.
[See page 76.
Road Making and Maintenance: A Practical Treatise for Engineers,
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Page 626
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page 73.
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ABRIDGED CONTENTS.
Page 627
Introductory.—Central Station Work as a Profession.—As an Investment.—
The Establishment of a Central Station.—Systems of Supply.—Site.—
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Economy.—Coal Handling, Weighing, and Storing.—The Transmission of
Steam.—Generators.—Condensing Appliances.—Switching Gear,
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Feeders.—Testing Mains.—Meters and Appliances.—Standardising and
Testing Laboratory.—Secondary Batteries.—Street Lighting.—Cost.—
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General Principles of Switchgear Design.—Constructional Details.—
Circuit Breakers or Arc Interrupting Devices.—Automatically Operated
Circuit Breakers.—Alternating Reverse Current Devices.—Arrangement of
'Bus Bars, and Apparatus for Parallel Running.—General Arrangement of
Controlling Apparatus for High Tension Systems.—General Arrangement of
Controlling Apparatus for Low Tension Systems.—Examples of Complete
Installations.—Long Distance Transmission Schemes.
The Establishment of a Central Station.—Systems of Supply.—Site.—
Architecture.—Plant.—Boilers.—Systems of Draught and Waste Heat
Economy.—Coal Handling, Weighing, and Storing.—The Transmission of
Steam.—Generators.—Condensing Appliances.—Switching Gear,
Instruments, and Connections.—Distributing Mains.—Insulation,
Resistance, and Cost.—Distributing Networks.—Service Mains and
Feeders.—Testing Mains.—Meters and Appliances.—Standardising and
Testing Laboratory.—Secondary Batteries.—Street Lighting.—Cost.—
General Organisation.—Mains Department.—Installation Department.—
Standardising Department.—Drawing Office.—Clerical Department.—The
Consumer.—Routine and Main Laying.—Index.
"One of the most valuable contributions to Central Station literature we
have had for some time."—Electricity.
ELECTRICITY CONTROL.
A Treatise on Electricity Switchgear and Systems of Transmission.
By LEONARD ANDREWS, M.I.E.E.,
Ex-Member of Council of the Incorporated Municipal Electrical Association; Consulting Electrical Engineer to the
Hastings Corporation, &c., &c.
General Principles of Switchgear Design.—Constructional Details.—
Circuit Breakers or Arc Interrupting Devices.—Automatically Operated
Circuit Breakers.—Alternating Reverse Current Devices.—Arrangement of
'Bus Bars, and Apparatus for Parallel Running.—General Arrangement of
Controlling Apparatus for High Tension Systems.—General Arrangement of
Controlling Apparatus for Low Tension Systems.—Examples of Complete
Installations.—Long Distance Transmission Schemes.
Page 628
Sixteenth Edition, Thoroughly Revised and Enlarged.
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A TEXT-BOOK OF PHYSICS.
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J.H. POYNTING, SC.D., F.R.S.,
Late Fellow of Trinity College, Cambridge; Professor of Physics, Birmingham University.
Page 629
AND
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Page 630
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THE MEAN DENSITY OF THE EARTH: An Essay to which the Adams
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Athenæum.
Griffin's Geological, Prospecting, Mining, and Metallurgical
Publications.
For Works on Chemistry and Chemical Industries see p. 69.
Page 631
PAGE
Geology, Stratigraphical, R. Etheridge, F.R.S., 52
" Physical, Prof. H.G. Seeley, 52
" Practical Aids, Prof. Grenville Cole, 53
" Open Air Studies, " " 19
Griffin's "New Land" Series, Ed. by Prof. Cole, 54
Prospecting for Minerals, S. Herbert Cox, A.R.S.M., 55
Food Supply, Robt. Bruce, 55
New Lands, H.R. Mill, D.Sc., F.R.S.E., 54
Building Construction, Prof. James Lyon, 54
Ore and Stone Mining, Prof. Le Neve Foster, 56
Elementary Mining, " " 56
Coal Mining, H.W. Hughes, F.G.S., 56
Practical Coal Mining, G.L. Kerr, M.Inst.M.E., 58
Elementary " " " 58
Electrical Coal Mining, D. Burns, 58
Mine-Surveying, Bennett H. Brough, A.R.S.M., 57
Blasting and Explosives, O. Guttmann, A.M.I.C.E., 57
Mine Accounts, Prof. J.G. Lawn, 57
Mining Engineers' Pkt.-Bk., E.R. Field, M.Inst.M.M., 60
Petroleum, Redwood and Holloway, 61
A Handbook on Petroleum, J.H. Thomson and Dr. Redwood, 61
The Petroleum Lamp, " " 61
Metallurgical Analysis, Macleod and Walker, 60
Metallurgy (General), Phillips and Bauerman, 60
" (Elementary), Prof. Humboldt Sexton, 66
Getting Gold, J.C.F. Johnson, F.G.S., 58
Gold Seeking in South Africa, Theo Kassner, 59
Cyanide Process, James Park, F.G.S., 59
Cyaniding, Smart and Julian, 59
Electric Smelting, Borchers and McMillan, 67
Electro-Metallurgy, W.G. McMillan, F.I.C., 67
Assaying, J.J. & C. Beringer, 66
Metallurgical Analysis, J.J. Morgan, F.C.S, 66
Geology, Stratigraphical, R. Etheridge, F.R.S., 52
" Physical, Prof. H.G. Seeley, 52
" Practical Aids, Prof. Grenville Cole, 53
" Open Air Studies, " " 19
Griffin's "New Land" Series, Ed. by Prof. Cole, 54
Prospecting for Minerals, S. Herbert Cox, A.R.S.M., 55
Food Supply, Robt. Bruce, 55
New Lands, H.R. Mill, D.Sc., F.R.S.E., 54
Building Construction, Prof. James Lyon, 54
Ore and Stone Mining, Prof. Le Neve Foster, 56
Elementary Mining, " " 56
Coal Mining, H.W. Hughes, F.G.S., 56
Practical Coal Mining, G.L. Kerr, M.Inst.M.E., 58
Elementary " " " 58
Electrical Coal Mining, D. Burns, 58
Mine-Surveying, Bennett H. Brough, A.R.S.M., 57
Blasting and Explosives, O. Guttmann, A.M.I.C.E., 57
Mine Accounts, Prof. J.G. Lawn, 57
Mining Engineers' Pkt.-Bk., E.R. Field, M.Inst.M.M., 60
Petroleum, Redwood and Holloway, 61
A Handbook on Petroleum, J.H. Thomson and Dr. Redwood, 61
The Petroleum Lamp, " " 61
Metallurgical Analysis, Macleod and Walker, 60
Metallurgy (General), Phillips and Bauerman, 60
" (Elementary), Prof. Humboldt Sexton, 66
Getting Gold, J.C.F. Johnson, F.G.S., 58
Gold Seeking in South Africa, Theo Kassner, 59
Cyanide Process, James Park, F.G.S., 59
Cyaniding, Smart and Julian, 59
Electric Smelting, Borchers and McMillan, 67
Electro-Metallurgy, W.G. McMillan, F.I.C., 67
Assaying, J.J. & C. Beringer, 66
Metallurgical Analysis, J.J. Morgan, F.C.S, 66
Page 632
Griffin's Metallurgical Series Ed. by Sir W. Roberts-Austen, 62
Introduction, Sir W. Roberts-Austen, K.C.B.,, 63
Gold, Metallurgy of, Dr. Kirke Rose, A.R.S.M., 63
Lead and Silver, " H.F. Collins, A.R.S.M., 64
Iron, Metallurgy of, Thos. Turner, A.R.S.M., 65
Steel, " F.W. Harbord, 65
Metallurgical Machinery, H.C. Jenkins, A.R.S.M., 64
Goldsmith and Jeweller's Art, Thos. B. Wigley, 68
Precious Stones, Dr. Max Bauer, 68
Demy 8vo, Handsome cloth, 18s.
Physical Geology and Palæontology,
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BY
HARRY GOVIER SEELEY, F.R.S.,
PROFESSOR OF GEOGRAPHY IN KING'S COLLEGE, LONDON.
With Frontispiece in Chromo-Lithography, and Illustrations.
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the "Geological Magazine."
Introduction, Sir W. Roberts-Austen, K.C.B.,, 63
Gold, Metallurgy of, Dr. Kirke Rose, A.R.S.M., 63
Lead and Silver, " H.F. Collins, A.R.S.M., 64
Iron, Metallurgy of, Thos. Turner, A.R.S.M., 65
Steel, " F.W. Harbord, 65
Metallurgical Machinery, H.C. Jenkins, A.R.S.M., 64
Goldsmith and Jeweller's Art, Thos. B. Wigley, 68
Precious Stones, Dr. Max Bauer, 68
Demy 8vo, Handsome cloth, 18s.
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With Frontispiece in Chromo-Lithography, and Illustrations.
"It is impossible to praise too highly the research which Professor Seeley's
'Physical Geology' evidences. It is far more than a Text-book—it is a
Directory to the Student in prosecuting his researches."—Presidential
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F.R.S.
"Professor Seeley maintains in his 'Physical Geology' the high reputation
he already deservedly bears as a Teacher."—Dr. Henry Woodward, F.R.S., in
the "Geological Magazine."
Page 633
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OF THE NATURAL HIST. DEPARTMENT, BRITISH MUSEUM, LATE PALÆONTOLOGIST TO THE
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OPEN-AIR STUDIES IN GEOLOGY:
An Introduction to Geology Out-of-doors.
By PROFESSOR GRENVILLE COLE, M.R.I.A., F.G.S.
Lithology in the English language."—American Journal of Engineering.
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OF THE NATURAL HIST. DEPARTMENT, BRITISH MUSEUM, LATE PALÆONTOLOGIST TO THE
GEOLOGICAL SURVEY OF GREAT BRITAIN, PAST PRESIDENT OF THE GEOLOGICAL SOCIETY, ETC.
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"If Prof. Seeley's volume was remarkable for its originality and the breadth
of its views, Mr. Etheridge fully justifies the assertion made in his preface
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Must take high rank among works of reference."—Athenæum.
OPEN-AIR STUDIES IN GEOLOGY:
An Introduction to Geology Out-of-doors.
By PROFESSOR GRENVILLE COLE, M.R.I.A., F.G.S.
Page 634
For details, see Griffin's Introductory Science Series, p. 85.
Crown 8vo. Handsome Cloth, 2s. 6d.
RESEARCHES ON THE PAST AND PRESENT HISTORY
OF THE EARTH'S ATMOSPHERE.
Including the latest Discoveries and their Practical Applications.
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PART I.—The Earth's Atmosphere in Remote Geological Periods.
PART II.—The Atmosphere of Our Present Period. Appendices; Index.
*** Dr. Phipson's work presents, amidst much which is of interest to the
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connection with Weather Lore, and with Scientific Meteorology.—
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"The book should prove of interest to general readers, as well as to
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By GRENVILLE A.J. COLE, M.R.I.A., F.G.S.,
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See also the two following pages (54, 55), and page 85.
Crown 8vo. Handsome Cloth, 2s. 6d.
RESEARCHES ON THE PAST AND PRESENT HISTORY
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PART I.—The Earth's Atmosphere in Remote Geological Periods.
PART II.—The Atmosphere of Our Present Period. Appendices; Index.
*** Dr. Phipson's work presents, amidst much which is of interest to the
Scientist and the General Reader alike, a short résumé of his discovery of
the origin of Atmospheric Oxygen, the existence of which he attributes
wholly to the action of Solar Radiation upon vegetable life. The book will
be found replete with much that is new, curious, and interesting, both in
connection with Weather Lore, and with Scientific Meteorology.—
Publisher's Note.
"The book should prove of interest to general readers, as well as to
meteorologists and other students of science."—Nature.
By GRENVILLE A.J. COLE, M.R.I.A., F.G.S.,
Professor of Geology in the Royal College of Science for Ireland, and Examiner in the University of London.
See also the two following pages (54, 55), and page 85.
Page 635
AIDS IN PRACTICAL GEOLOGY:
WITH A SECTION ON PALÆONTOLOGY.
By PROFESSOR GRENVILLE COLE, M.R.I.A., F.G.S.
Fourth Edition, Thoroughly Revised. With Frontispiece and Illustrations. Cloth, 10s. 6d.
GENERAL CONTENTS.—
PART I.—Sampling of the Earth's Crust.
PART II.—Examination of Minerals.
PART III.—Examination of Rocks.
PART IV.—Examination of Fossils.
"Prof. Cole treats of the examination of minerals and rocks in a way that
has never been attempted before ... deserving of the highest praise. Here
indeed are 'Aids' innumerable and invaluable. All the directions are given,
with the utmost clearness and precision."—Athenæum.
"That the work deserves its title, that it is full of 'Aids,' and in the highest
degree 'practical,' will be the verdict of all who use it."—Nature.
"This excellent Manual ... will be a very great help.... The Section on the
Examination of Fossils is probably the best of its kind yet published.... Full
of well-digested information from the newest sources and from personal
research."—Annals of Nat. History.
GRIFFINS "NEW LAND" SERIES.
Practical Hand-Books for the Use of Prospectors, Explorers, Settlers,
Colonists, and all Interested in the opening up and Development of New
WITH A SECTION ON PALÆONTOLOGY.
By PROFESSOR GRENVILLE COLE, M.R.I.A., F.G.S.
Fourth Edition, Thoroughly Revised. With Frontispiece and Illustrations. Cloth, 10s. 6d.
GENERAL CONTENTS.—
PART I.—Sampling of the Earth's Crust.
PART II.—Examination of Minerals.
PART III.—Examination of Rocks.
PART IV.—Examination of Fossils.
"Prof. Cole treats of the examination of minerals and rocks in a way that
has never been attempted before ... deserving of the highest praise. Here
indeed are 'Aids' innumerable and invaluable. All the directions are given,
with the utmost clearness and precision."—Athenæum.
"That the work deserves its title, that it is full of 'Aids,' and in the highest
degree 'practical,' will be the verdict of all who use it."—Nature.
"This excellent Manual ... will be a very great help.... The Section on the
Examination of Fossils is probably the best of its kind yet published.... Full
of well-digested information from the newest sources and from personal
research."—Annals of Nat. History.
GRIFFINS "NEW LAND" SERIES.
Practical Hand-Books for the Use of Prospectors, Explorers, Settlers,
Colonists, and all Interested in the opening up and Development of New
Page 636
Lands.
Edited by GRENVILLE A.J. COLE, M.R.I.A., F.G.S.,
Professor of Geology in the Royal College of Science for Ireland, and Examiner in the University of London.
In Crown 8vo. Handsome Cloth. 5s.
With Numerous Maps Specially Drawn and Executed for this Work.
NEW LANDS:
THEIR RESOURCES AND PROSPECTIVE ADVANTAGES.
By HUGH ROBERT MILL, D.Sc., LL.D., F.R.S.E.,
Librarian to the Royal Geographical Society.
Introductory.—The Development of New Lands.—The Dominion of
Canada.—Canada, Eastern Provinces.—Canada, Western Provinces and
Territories.—Newfoundland.—The United States.—Latin America,
Mexico.—Latin America, Temperate Brazil and Chili.—Latin America,
Argentina.—The Falkland Islands.—Victoria.—New South Wales.—
Queensland.—South Australia.—Tasmania.—Western Australia.—New
Zealand.—The Resources of South Africa.—Southern Rhodesia.—Index.
"Painstaking ... complete ... of great practical assistance."—The Field.
"A want admirably supplied.... Has the advantage of being written by a
professed Geographer."—Geographical Journal.
IN PREPARATION.
Edited by GRENVILLE A.J. COLE, M.R.I.A., F.G.S.,
Professor of Geology in the Royal College of Science for Ireland, and Examiner in the University of London.
In Crown 8vo. Handsome Cloth. 5s.
With Numerous Maps Specially Drawn and Executed for this Work.
NEW LANDS:
THEIR RESOURCES AND PROSPECTIVE ADVANTAGES.
By HUGH ROBERT MILL, D.Sc., LL.D., F.R.S.E.,
Librarian to the Royal Geographical Society.
Introductory.—The Development of New Lands.—The Dominion of
Canada.—Canada, Eastern Provinces.—Canada, Western Provinces and
Territories.—Newfoundland.—The United States.—Latin America,
Mexico.—Latin America, Temperate Brazil and Chili.—Latin America,
Argentina.—The Falkland Islands.—Victoria.—New South Wales.—
Queensland.—South Australia.—Tasmania.—Western Australia.—New
Zealand.—The Resources of South Africa.—Southern Rhodesia.—Index.
"Painstaking ... complete ... of great practical assistance."—The Field.
"A want admirably supplied.... Has the advantage of being written by a
professed Geographer."—Geographical Journal.
IN PREPARATION.
Page 637
BUILDING CONSTRUCTION in WOOD, STONE, and CONCRETE.
By James Lyon, M.A., Professor of Engineering in the Royal College of
Science for Ireland; sometime Superintendent of the Engineering
Department in the University of Cambridge; and J. Taylor, A.R.C.S.I.
*** Other Volumes, dealing with subjects of Primary Importance in the
Examination and Utilisation of Lands which have not as yet been fully
developed, are in preparation.
Third Edition, Revised. With Illustrations. Handsome Cloth, 5s.
PROSPECTING FOR MINERALS.
A Practical Handbook for Prospectors, Explorers, Settlers, and all interested in the Opening up
and Development of New Lands.
BY
S. HERBERT COX, Assoc. R.S.M., M. Inst. M.M., F.G.S., &c.
General Contents.—Introduction and Hints on Geology—The
Determination of Minerals: Use of the Blow-pipe, &c.—Rock-forming
Minerals and Non-Metallic Minerals of Commercial Value: Rock Salt,
Borax, Marbles, Lithographic Stone, Quartz and Opal, &c., &c.—Precious
Stones and Gems—Stratified Deposits: Coal and Ores—Mineral Veins and
Lodes—Irregular Deposits—Dynamics of Lodes: Faults, &c.—Alluvial
Deposits—Noble Metals: Gold, Platinum, Silver, &c.—Lead—Mercury—
Copper—Tin—Zinc—Iron—Nickel, &c.—Sulphur, Antimony, Arsenic, &c.
—Combustible Minerals—Petroleum—General Hints on Prospecting—
Glossary—Index.
By James Lyon, M.A., Professor of Engineering in the Royal College of
Science for Ireland; sometime Superintendent of the Engineering
Department in the University of Cambridge; and J. Taylor, A.R.C.S.I.
*** Other Volumes, dealing with subjects of Primary Importance in the
Examination and Utilisation of Lands which have not as yet been fully
developed, are in preparation.
Third Edition, Revised. With Illustrations. Handsome Cloth, 5s.
PROSPECTING FOR MINERALS.
A Practical Handbook for Prospectors, Explorers, Settlers, and all interested in the Opening up
and Development of New Lands.
BY
S. HERBERT COX, Assoc. R.S.M., M. Inst. M.M., F.G.S., &c.
General Contents.—Introduction and Hints on Geology—The
Determination of Minerals: Use of the Blow-pipe, &c.—Rock-forming
Minerals and Non-Metallic Minerals of Commercial Value: Rock Salt,
Borax, Marbles, Lithographic Stone, Quartz and Opal, &c., &c.—Precious
Stones and Gems—Stratified Deposits: Coal and Ores—Mineral Veins and
Lodes—Irregular Deposits—Dynamics of Lodes: Faults, &c.—Alluvial
Deposits—Noble Metals: Gold, Platinum, Silver, &c.—Lead—Mercury—
Copper—Tin—Zinc—Iron—Nickel, &c.—Sulphur, Antimony, Arsenic, &c.
—Combustible Minerals—Petroleum—General Hints on Prospecting—
Glossary—Index.
Page 638
"This admirable little work ... written with scientific accuracy
in a clear and lucid style.... An important addition to technical
literature ... will be of value not only to the Student, but to the
experienced Prospector.... If the succeeding volumes of the New
Land Series are equal in merit to the First, we must congratulate
the Publishers on successfully filling up a gap in existing
literature.—Mining Journal.
"This excellent handbook will prove a perfect Vade-mecum to
those engaged in the practical work of Mining and
Metallurgy."—Times of Africa.
With many Engravings and Photographs. Handsome Cloth, 4s. 6d.
FOOD SUPPLY.
By ROBERT BRUCE, Agricultural Superintendent to the Royal
Dublin Society.
With Appendix on Preserved Foods by C.A. Mitchell, B.A., F.L.C.
General Contents.—Climate and Soil—Drainage and Rotation of Crops—
Seeds and Crops—Vegetables and Fruits—Cattle and Cattle-Breeding—
Sheep and Sheep Rearing—Pigs—Poultry—Horses—The Dairy—The
Farmer's Implements—The Settler's Home.
"Bristles With Information."—Farmers' Gazette.
"The work is one which will appeal to those intending to become farmers at
home or in the Colonies, and who desire to obtain a general idea of the true
principles of farming in all its branches."—Journal of the Royal Colonial
Inst.
"A most readable and valuable book, and merits an extensive sale."—
Scottish Farmer.
in a clear and lucid style.... An important addition to technical
literature ... will be of value not only to the Student, but to the
experienced Prospector.... If the succeeding volumes of the New
Land Series are equal in merit to the First, we must congratulate
the Publishers on successfully filling up a gap in existing
literature.—Mining Journal.
"This excellent handbook will prove a perfect Vade-mecum to
those engaged in the practical work of Mining and
Metallurgy."—Times of Africa.
With many Engravings and Photographs. Handsome Cloth, 4s. 6d.
FOOD SUPPLY.
By ROBERT BRUCE, Agricultural Superintendent to the Royal
Dublin Society.
With Appendix on Preserved Foods by C.A. Mitchell, B.A., F.L.C.
General Contents.—Climate and Soil—Drainage and Rotation of Crops—
Seeds and Crops—Vegetables and Fruits—Cattle and Cattle-Breeding—
Sheep and Sheep Rearing—Pigs—Poultry—Horses—The Dairy—The
Farmer's Implements—The Settler's Home.
"Bristles With Information."—Farmers' Gazette.
"The work is one which will appeal to those intending to become farmers at
home or in the Colonies, and who desire to obtain a general idea of the true
principles of farming in all its branches."—Journal of the Royal Colonial
Inst.
"A most readable and valuable book, and merits an extensive sale."—
Scottish Farmer.
Page 639
"Will prove of service in any part of the world."—Nature.
Fourth Edition, Revised, and brought thoroughly up-to-date by L.H.
Cooke, Instructor in Mine Surveying, Royal College of Science.
With Frontispiece and 716 Illustrations. Price 34s.
ORE & STONE MINING.
BY
C. LE NEVE FOSTER, D.Sc., F.R.S.,
PROFESSOR OF MINING, ROYAL COLLEGE OF SCIENCE; EXAMINER IN MINING TO THE BOARD OF
EDUCATION.
GENERAL CONTENTS.
INTRODUCTION. Mode of Occurrence of Minerals.—Prospecting.—
Boring.—Breaking Ground.—Supporting Excavations.—Exploitation.—
Haulage or Transport.—Hoisting or Winding.—Drainage.—Ventilation.—
Lighting.—Descent and Ascent.—Dressing.—Principles of Employment of
Mining Labour.—Legislation affecting Mines and Quarries.—Condition of
the Miner.—Accidents.—Index.
"Dr. Foster's book was expected to be epoch-making, and it fully justifies
such expectation.... A most admirable account of the mode of occurrence of
practically all known minerals. Probably stands unrivalled for
completeness."—The Mining Journal.
"This epoch-making work ... appeals to men of experience no less than to
students."—Berg- und Hüttenmännische Zeitung.
"This splendid work."—Oesterr. Ztschrft. für Berg- und Hüttenwesen.
Fourth Edition, Revised, and brought thoroughly up-to-date by L.H.
Cooke, Instructor in Mine Surveying, Royal College of Science.
With Frontispiece and 716 Illustrations. Price 34s.
ORE & STONE MINING.
BY
C. LE NEVE FOSTER, D.Sc., F.R.S.,
PROFESSOR OF MINING, ROYAL COLLEGE OF SCIENCE; EXAMINER IN MINING TO THE BOARD OF
EDUCATION.
GENERAL CONTENTS.
INTRODUCTION. Mode of Occurrence of Minerals.—Prospecting.—
Boring.—Breaking Ground.—Supporting Excavations.—Exploitation.—
Haulage or Transport.—Hoisting or Winding.—Drainage.—Ventilation.—
Lighting.—Descent and Ascent.—Dressing.—Principles of Employment of
Mining Labour.—Legislation affecting Mines and Quarries.—Condition of
the Miner.—Accidents.—Index.
"Dr. Foster's book was expected to be epoch-making, and it fully justifies
such expectation.... A most admirable account of the mode of occurrence of
practically all known minerals. Probably stands unrivalled for
completeness."—The Mining Journal.
"This epoch-making work ... appeals to men of experience no less than to
students."—Berg- und Hüttenmännische Zeitung.
"This splendid work."—Oesterr. Ztschrft. für Berg- und Hüttenwesen.
Page 640
ELEMENTARY MINING AND QUARRYING
(An Introductory Text-book).
By Prof. C. Le Neve Foster, F.R.S.
With Illustrations. [At Press.
Fourth Edition, Revised and Greatly Enlarged. With Numerous Additional
Illustrations, mostly reduced from Working Drawings. Price 24s. net.
A TEXT-BOOK OF COAL-MINING:
FOR THE USE OF COLLIERY MANAGERS AND OTHERS ENGAGED IN COAL-MINING.
BY
HERBERT WILLIAM HUGHES, F.G.S.,
Assoc. Royal School of Mines, General Manager of Sandwell Park Colliery.
GENERAL CONTENTS.
Geology.—Search for Coal.—Breaking Ground.—Sinking.—Preliminary
Operations.—Methods of Working.—Haulage.—Winding.—Pumping.—
Ventilation.—Lighting.—Works at Surface.—Preparation of Coal for
Market.—Index.
"Quite the best book of its kind ... as practical in aim as a book can be ...
The illustrations are excellent."—Athenæum.
"We cordially recommend the work."—Colliery Guardian.
"Will soon come to be regarded as the standard work of its kind."—
Birmingham Daily Gazette.
(An Introductory Text-book).
By Prof. C. Le Neve Foster, F.R.S.
With Illustrations. [At Press.
Fourth Edition, Revised and Greatly Enlarged. With Numerous Additional
Illustrations, mostly reduced from Working Drawings. Price 24s. net.
A TEXT-BOOK OF COAL-MINING:
FOR THE USE OF COLLIERY MANAGERS AND OTHERS ENGAGED IN COAL-MINING.
BY
HERBERT WILLIAM HUGHES, F.G.S.,
Assoc. Royal School of Mines, General Manager of Sandwell Park Colliery.
GENERAL CONTENTS.
Geology.—Search for Coal.—Breaking Ground.—Sinking.—Preliminary
Operations.—Methods of Working.—Haulage.—Winding.—Pumping.—
Ventilation.—Lighting.—Works at Surface.—Preparation of Coal for
Market.—Index.
"Quite the best book of its kind ... as practical in aim as a book can be ...
The illustrations are excellent."—Athenæum.
"We cordially recommend the work."—Colliery Guardian.
"Will soon come to be regarded as the standard work of its kind."—
Birmingham Daily Gazette.
Page 641
Tenth Edition, Revised and Enlarged. With Numerous Diagrams.
Cloth, 7s. 6d.
A TREATISE ON MINE-SURVEYING:
For the use of Managers of Mines and Collieries, Students at the Royal School of Mines, &c.
By BENNETT H. BROUGH, F.G.S., Assoc.R.S.M.,
Formerly Instructor of Mine-Surveying, Royal School of Mines.
General Contents.—General Explanations.—Measurement of Distances.
—Miner's Dial.—Variation of the Magnetic-Needle.—Surveying.—German
Dial.—Theodolite.—Traversing Underground.—Surface-Surveys.—
Plotting the Survey.—Calculation of Areas.—Levelling.—Measuring
Distances by Telescope.—Setting-out.—Problems.—Photographic
Surveying.—Appendices.
"Its clearness of style, lucidity of description, and fulness of detail have
long ago won for it a place unique in the literature of this branch of mining
engineering, and the present edition fully maintains the high standard of its
predecessors. To the student, and to the mining engineer alike, its value is
inestimable. The illustrations are excellent."—The Mining Journal.
In Large 8vo. Second Edition. Price 10s. 6d.
Mine Accounts and Mining Book-keeping.
For Students, Managers, Secretaries, and others.
With Examples taken from Actual Practice of Leading Companies.
BY
Cloth, 7s. 6d.
A TREATISE ON MINE-SURVEYING:
For the use of Managers of Mines and Collieries, Students at the Royal School of Mines, &c.
By BENNETT H. BROUGH, F.G.S., Assoc.R.S.M.,
Formerly Instructor of Mine-Surveying, Royal School of Mines.
General Contents.—General Explanations.—Measurement of Distances.
—Miner's Dial.—Variation of the Magnetic-Needle.—Surveying.—German
Dial.—Theodolite.—Traversing Underground.—Surface-Surveys.—
Plotting the Survey.—Calculation of Areas.—Levelling.—Measuring
Distances by Telescope.—Setting-out.—Problems.—Photographic
Surveying.—Appendices.
"Its clearness of style, lucidity of description, and fulness of detail have
long ago won for it a place unique in the literature of this branch of mining
engineering, and the present edition fully maintains the high standard of its
predecessors. To the student, and to the mining engineer alike, its value is
inestimable. The illustrations are excellent."—The Mining Journal.
In Large 8vo. Second Edition. Price 10s. 6d.
Mine Accounts and Mining Book-keeping.
For Students, Managers, Secretaries, and others.
With Examples taken from Actual Practice of Leading Companies.
BY
Page 642
JAMES GUNSON LAWN, Assoc.R.S.M., Assoc. Mem. Inst. C.E.,
F.G.S.,
Professor of Mining at the South African School of Mines.
Edited by C. LE NEVE FOSTER, D.Sc., F.R.S.
General Contents.—Introduction.—Part I. Engagement and Payment of
Workmen.—Part II. Purchases and Sales.—Part III. Working Summaries
and Analyses.—Part IV. Ledger, Balance Sheet, and Company Books.—
Part V. Reports and Statistics.
"It seems impossible to suggest how Mr. Lawn's book could be made more
complete or more valuable, careful, and exhaustive."—Accountants'
Magazine.
In Large 8vo, with Illustrations and Folding-Plates. 10s. 6d.
BLASTING:
AND THE USE OF EXPLOSIVES.
A Handbook for Engineers and others Engaged in Mining, Tunnelling, Quarrying, &c.
By OSCAR GUTTMANN, Assoc. M. Inst. C.E.
Member of the Societies of Civil Engineers and Architects of Vienna and Budapest, Corresponding Member of the Imp. Roy.
Geological Institution of Austria, &c.
"This admirable work."—Colliery Guardian.
"Should prove a vade-mecum to Mining Engineers and all engaged in
practical work."—Iron and Coal Trades Review.
F.G.S.,
Professor of Mining at the South African School of Mines.
Edited by C. LE NEVE FOSTER, D.Sc., F.R.S.
General Contents.—Introduction.—Part I. Engagement and Payment of
Workmen.—Part II. Purchases and Sales.—Part III. Working Summaries
and Analyses.—Part IV. Ledger, Balance Sheet, and Company Books.—
Part V. Reports and Statistics.
"It seems impossible to suggest how Mr. Lawn's book could be made more
complete or more valuable, careful, and exhaustive."—Accountants'
Magazine.
In Large 8vo, with Illustrations and Folding-Plates. 10s. 6d.
BLASTING:
AND THE USE OF EXPLOSIVES.
A Handbook for Engineers and others Engaged in Mining, Tunnelling, Quarrying, &c.
By OSCAR GUTTMANN, Assoc. M. Inst. C.E.
Member of the Societies of Civil Engineers and Architects of Vienna and Budapest, Corresponding Member of the Imp. Roy.
Geological Institution of Austria, &c.
"This admirable work."—Colliery Guardian.
"Should prove a vade-mecum to Mining Engineers and all engaged in
practical work."—Iron and Coal Trades Review.
Page 643
In Crown 8vo. Handsome cloth. With Numerous Illustrations. 6s. net.
ELECTRICAL PRACTICE IN COLLIERIES.
By D. BURNS, M.E., M.Inst.M.E.,
Certificated Colliery Manager, and Lecturer on Mining and Geology to the Glasgow and West of Scotland Technical
College.
Units of Measurement, Conductors, &c.—The Theory of the Dynamo.—
The Dynamo, Details of Construction and Working.—Motors.—Lighting
Installations in Collieries.—Pumping by Electricity.—Electrical Haulage.—
Coal Cutting.—Miscellaneous Applications of Electricity in Mines.—Index.
"A clear and concise introduction to electrical practice in collieries."—
Mining Journal.
Second Edition. Large Crown 8vo. Handsome Cloth. With over 520
Illustrations in the Text. 12s. 6d.
PRACTICAL COAL-MINING:
A MANUAL FOR MANAGERS, UNDER-MANAGERS, COLLIERY ENGINEERS, AND
OTHERS.
With Worked-out Problems on Haulage, Pumping, Ventilation, &c.
By GEORGE L. KERR, M.E., M.Inst.M.E.
"An essentially practical work, and can be confidently recommended. No
department of Coal-Mining has been overlooked."—Engineers' Gazette.
"This book just meets the wants of Students preparing for the Colliery
Managers' Examinations. I have decided to use it for our classes here.... We
ELECTRICAL PRACTICE IN COLLIERIES.
By D. BURNS, M.E., M.Inst.M.E.,
Certificated Colliery Manager, and Lecturer on Mining and Geology to the Glasgow and West of Scotland Technical
College.
Units of Measurement, Conductors, &c.—The Theory of the Dynamo.—
The Dynamo, Details of Construction and Working.—Motors.—Lighting
Installations in Collieries.—Pumping by Electricity.—Electrical Haulage.—
Coal Cutting.—Miscellaneous Applications of Electricity in Mines.—Index.
"A clear and concise introduction to electrical practice in collieries."—
Mining Journal.
Second Edition. Large Crown 8vo. Handsome Cloth. With over 520
Illustrations in the Text. 12s. 6d.
PRACTICAL COAL-MINING:
A MANUAL FOR MANAGERS, UNDER-MANAGERS, COLLIERY ENGINEERS, AND
OTHERS.
With Worked-out Problems on Haulage, Pumping, Ventilation, &c.
By GEORGE L. KERR, M.E., M.Inst.M.E.
"An essentially practical work, and can be confidently recommended. No
department of Coal-Mining has been overlooked."—Engineers' Gazette.
"This book just meets the wants of Students preparing for the Colliery
Managers' Examinations. I have decided to use it for our classes here.... We
Page 644
have, I believe the largest atining class in Great Britain."—The Principal of
a Training College.
ELEMENTARY COAL-MINING:
For the Use of Students, Miners, and others preparing for Examinations. By George L. Kerr,
M.E., M.Inst.M.E., Author of "Practical Coal-Mining." In Crown 8vo. Handsome Cloth. With
200 Illustrations. 3s. 6d.
"An abundance of information conveyed in a popular and attractive form....
Will be of great use to all who are in any way interested in coal mining."—
Scottish Critic.
Second Edition. With Illustrations. Cloth, 3s. 6d.
GETTING GOLD:
A GOLD-MINING HANDBOOK FOR PRACTICAL MEN.
By J.C.F. JOHNSON, F.G.S., A.I.M.E.,
Life Member Australasian Mine-Managers' Association.
General Contents.—Introductory: Prospecting (Alluvial and General)—
Lode or Reef Prospecting—Genesiology of Gold—Auriferous Lodes—
Drifts—Gold Extraction—Lixiviation—Calcination—Motor Power and its
Transmission—Company Formation—Mining Appliances and Methods—
Australasian Mining Regulations.
"Practical from beginning to end ... deals thoroughly with the Prospecting,
Sinking, Crushing, and Extraction of gold."—Brit. Australasian.
a Training College.
ELEMENTARY COAL-MINING:
For the Use of Students, Miners, and others preparing for Examinations. By George L. Kerr,
M.E., M.Inst.M.E., Author of "Practical Coal-Mining." In Crown 8vo. Handsome Cloth. With
200 Illustrations. 3s. 6d.
"An abundance of information conveyed in a popular and attractive form....
Will be of great use to all who are in any way interested in coal mining."—
Scottish Critic.
Second Edition. With Illustrations. Cloth, 3s. 6d.
GETTING GOLD:
A GOLD-MINING HANDBOOK FOR PRACTICAL MEN.
By J.C.F. JOHNSON, F.G.S., A.I.M.E.,
Life Member Australasian Mine-Managers' Association.
General Contents.—Introductory: Prospecting (Alluvial and General)—
Lode or Reef Prospecting—Genesiology of Gold—Auriferous Lodes—
Drifts—Gold Extraction—Lixiviation—Calcination—Motor Power and its
Transmission—Company Formation—Mining Appliances and Methods—
Australasian Mining Regulations.
"Practical from beginning to end ... deals thoroughly with the Prospecting,
Sinking, Crushing, and Extraction of gold."—Brit. Australasian.
Page 645
With Plates and Illustrations. Handsome Cloth. At Press.
THE CYANIDE PROCESS OF GOLD EXTRACTION.
A Text-Book for the Use of Metallurgists and Students at Schools of Mines, &c.
By JAMES PARK, F.G.S., M.Inst.M.M.,
Professor of Mining and Director of the Otago University School of Mines;
late Director Thames School of Mines, and Geological Surveyor and
Mining Geologist to the Government of New Zealand.
Third English Edition. Thoroughly Revised and Greatly Enlarged. With
additional details concerning the Siemens-Halske and other recent
processes.
Contents.—The MacArthur Process.—Chemistry of the Process.—
Laboratory Experiments.—Control Testing and Analysis of Solutions.—
Appliances for Cyanide Extraction.—The Actual Extraction by Cyanide.—
Application of the Process.—Leaching by Agitation.—Zinc Precipitation of
Gold.—The Siemens-Halske Process.—Other Cyanide Processes.—
Antidotes for Cyanide Poisoning.—Cyaniding in New Zealand.
"Mr. Park's book deserves to be ranked as amongst the best of existing
treatises on this subject."—Mining Journal.
At Press. With Numerous Plates, Maps, and Illustrations.
CYANIDING GOLD & SILVER ORES.
A Practical Treatise on the Cyanide Process; its Application, Methods of Working, Design and
Construction of Plant, and Costs.
By H. FORBES JULIAN,
THE CYANIDE PROCESS OF GOLD EXTRACTION.
A Text-Book for the Use of Metallurgists and Students at Schools of Mines, &c.
By JAMES PARK, F.G.S., M.Inst.M.M.,
Professor of Mining and Director of the Otago University School of Mines;
late Director Thames School of Mines, and Geological Surveyor and
Mining Geologist to the Government of New Zealand.
Third English Edition. Thoroughly Revised and Greatly Enlarged. With
additional details concerning the Siemens-Halske and other recent
processes.
Contents.—The MacArthur Process.—Chemistry of the Process.—
Laboratory Experiments.—Control Testing and Analysis of Solutions.—
Appliances for Cyanide Extraction.—The Actual Extraction by Cyanide.—
Application of the Process.—Leaching by Agitation.—Zinc Precipitation of
Gold.—The Siemens-Halske Process.—Other Cyanide Processes.—
Antidotes for Cyanide Poisoning.—Cyaniding in New Zealand.
"Mr. Park's book deserves to be ranked as amongst the best of existing
treatises on this subject."—Mining Journal.
At Press. With Numerous Plates, Maps, and Illustrations.
CYANIDING GOLD & SILVER ORES.
A Practical Treatise on the Cyanide Process; its Application, Methods of Working, Design and
Construction of Plant, and Costs.
By H. FORBES JULIAN,
Page 646
Mining and Metallurgical Engineer; Specialist in Gold: Late Technical Adviser of the Deutsche Gold und Silber Scheide
Anstalt, Frankfort-on-Maine.
And EDGAR SMART, A.M.I.C.E.,
Civil and Metallurgical Engineer.
*** This book deals with the Cyanide Process from Technical, Commercial,
and Scientific points of view. It is adapted for the Use of Directors,
Managers, and Superintendents of Mines and Metallurgical Works, Mining
Engineers, Metallurgists, Chemists, Assayers, Working Cyaniders, and
Students.
In Crown. 8vo. Illustrated. Fancy Cloth Boards. 4s. 6d.
GOLD SEEKING IN SOUTH AFRICA:
A Handbook of Hints for intending Explorers, Prospectors, and Settlers.
By THEO KASSNER,
Mine Manager, Author of the Geological Sketch Map of the De Kaap Gold Fields.
With a Chapter on the Agricultural Prospects of South Africa.
Abstract of Contents—History.—Geology.—Prospecting.—The De Kaap
Goldfields.—Komati and Swaziland.—Cost of Mining, Native Labour, &c.
—Lydenberg Goldfields—Zoutspanberg.—Witwatersrand.—Other
Goldfields.—General Considerations—Conclusions.—Agricultural
Prospects, Tables, Index, &c.
"As fascinating in its way as anything ever penned by Jules Verne. Mr.
Kassner manages to impart his information in a way that enables him to be
understanded even of the dullest."—African Commerce.
Anstalt, Frankfort-on-Maine.
And EDGAR SMART, A.M.I.C.E.,
Civil and Metallurgical Engineer.
*** This book deals with the Cyanide Process from Technical, Commercial,
and Scientific points of view. It is adapted for the Use of Directors,
Managers, and Superintendents of Mines and Metallurgical Works, Mining
Engineers, Metallurgists, Chemists, Assayers, Working Cyaniders, and
Students.
In Crown. 8vo. Illustrated. Fancy Cloth Boards. 4s. 6d.
GOLD SEEKING IN SOUTH AFRICA:
A Handbook of Hints for intending Explorers, Prospectors, and Settlers.
By THEO KASSNER,
Mine Manager, Author of the Geological Sketch Map of the De Kaap Gold Fields.
With a Chapter on the Agricultural Prospects of South Africa.
Abstract of Contents—History.—Geology.—Prospecting.—The De Kaap
Goldfields.—Komati and Swaziland.—Cost of Mining, Native Labour, &c.
—Lydenberg Goldfields—Zoutspanberg.—Witwatersrand.—Other
Goldfields.—General Considerations—Conclusions.—Agricultural
Prospects, Tables, Index, &c.
"As fascinating in its way as anything ever penned by Jules Verne. Mr.
Kassner manages to impart his information in a way that enables him to be
understanded even of the dullest."—African Commerce.
Page 647
At Press. Large 8vo. Handsome Cloth. With Illustrations.
METALLURGICAL ANALYSIS & ASSAYING:
A THREE YEARS' COURSE FOR STUDENTS OF SCHOOLS OF MINES.
By W.A. MACLEOD, B.A., B.Sc., A.O.S.M. (N.Z.),
Formerly Assist.-Director, Thames School of Mines (N.Z.), and Lecturer in Chemistry, University of Tasmania; Director of
Queensland Government School of Mines, Charters Towers;
And CHAS. WALKER, F.C.S.,
Formerly Assist.-Demonstrator in Chemistry, Sydney University; Lecturer in Chemistry and Metallurgy, Charters Towers
School of Mines
Part I.—Qualitative Analysis and Preparation and Properties of Gases.
Part II.—Qualitative and Quantitative Analysis.
Part III.—Assaying, Technical Analysis (Gas, Water, Fuels, Oils, &c.).
*** "The aim of this work is to provide the student with a graded course of
work leading from Simple Quantitative Analysis up to the Technical
Quantitative Methods. It has been specially prepared to meet the
requirements of Schools of Mines, and more especially, of those in the
Colonies, the subject matter having been selected to cover a three years'
laboratory course."—Extract from Author's Preface.
Third Edition. With Folding Plates and Many Illustrations. 36s.
ELEMENTS OF METALLURGY.
A PRACTICAL TREATISE ON THE ART OF EXTRACTING METALS FROM THEIR
ORES.
METALLURGICAL ANALYSIS & ASSAYING:
A THREE YEARS' COURSE FOR STUDENTS OF SCHOOLS OF MINES.
By W.A. MACLEOD, B.A., B.Sc., A.O.S.M. (N.Z.),
Formerly Assist.-Director, Thames School of Mines (N.Z.), and Lecturer in Chemistry, University of Tasmania; Director of
Queensland Government School of Mines, Charters Towers;
And CHAS. WALKER, F.C.S.,
Formerly Assist.-Demonstrator in Chemistry, Sydney University; Lecturer in Chemistry and Metallurgy, Charters Towers
School of Mines
Part I.—Qualitative Analysis and Preparation and Properties of Gases.
Part II.—Qualitative and Quantitative Analysis.
Part III.—Assaying, Technical Analysis (Gas, Water, Fuels, Oils, &c.).
*** "The aim of this work is to provide the student with a graded course of
work leading from Simple Quantitative Analysis up to the Technical
Quantitative Methods. It has been specially prepared to meet the
requirements of Schools of Mines, and more especially, of those in the
Colonies, the subject matter having been selected to cover a three years'
laboratory course."—Extract from Author's Preface.
Third Edition. With Folding Plates and Many Illustrations. 36s.
ELEMENTS OF METALLURGY.
A PRACTICAL TREATISE ON THE ART OF EXTRACTING METALS FROM THEIR
ORES.
Page 648
By J. ARTHUR PHILLIPS, M. Inst. C.E., F.C.S., F.G.S., &c., And H.
BAUERMAN, V.P.G.S.
General Contents.—Refractory Materials.—Fire-Clays.—Fuels, &c.—
Aluminium.—Copper.—Tin.—Antimony.—Arsenic.—Zinc.—Mercury.—
Bismuth.—Lead.—Iron.—Cobalt.—Nickel.—Silver.—Gold.—Platinum.
"Of the Third Edition, we are still able to say that, as a Text-book of
Metallurgy, it is the best with which we are acquainted."—Engineer.
"A work which is equally valuable to the Student as a Text-book, and to the
practical Smelter as a Standard Work of Reference.... The Illustrations are
admirable examples of Wood Engraving."—Chemical News.
THE MINING ENGINEERS' REPORT BOOK AND DIRECTORS'
AND SHAREHOLDERS' GUIDE TO MINING REPORTS. By Edwin R.
Field, M.Inst.M.M. With Notes on the Valuation of Mining Property and
Tabulating Reports, Useful Tables, &c., and provided with detachable blank
pages for MS. Notes.
"An admirably compiled book which Mining Engineers and Managers will
find extremely useful."—Mining Journal.
Second Edition. In Preparation. In Two Volumes, Large 8vo. With
Numerous Maps, Plates, and Illustrations in the Text. Price 45s.
PETROLEUM AND ITS PRODUCTS: A PRACTICAL
TREATISE.
By Dr. BOVERTON REDWOOD, F.R.S.E., F.I.C., Assoc.R.C.S.,
Hon. Corr. Mem. of the Imperial Russian Technical Society; Mem. of the American Chemical Society; Adviser to the Home
Office and to the Corporation of London under the Petroleum Acts, &c., &c.
BAUERMAN, V.P.G.S.
General Contents.—Refractory Materials.—Fire-Clays.—Fuels, &c.—
Aluminium.—Copper.—Tin.—Antimony.—Arsenic.—Zinc.—Mercury.—
Bismuth.—Lead.—Iron.—Cobalt.—Nickel.—Silver.—Gold.—Platinum.
"Of the Third Edition, we are still able to say that, as a Text-book of
Metallurgy, it is the best with which we are acquainted."—Engineer.
"A work which is equally valuable to the Student as a Text-book, and to the
practical Smelter as a Standard Work of Reference.... The Illustrations are
admirable examples of Wood Engraving."—Chemical News.
THE MINING ENGINEERS' REPORT BOOK AND DIRECTORS'
AND SHAREHOLDERS' GUIDE TO MINING REPORTS. By Edwin R.
Field, M.Inst.M.M. With Notes on the Valuation of Mining Property and
Tabulating Reports, Useful Tables, &c., and provided with detachable blank
pages for MS. Notes.
"An admirably compiled book which Mining Engineers and Managers will
find extremely useful."—Mining Journal.
Second Edition. In Preparation. In Two Volumes, Large 8vo. With
Numerous Maps, Plates, and Illustrations in the Text. Price 45s.
PETROLEUM AND ITS PRODUCTS: A PRACTICAL
TREATISE.
By Dr. BOVERTON REDWOOD, F.R.S.E., F.I.C., Assoc.R.C.S.,
Hon. Corr. Mem. of the Imperial Russian Technical Society; Mem. of the American Chemical Society; Adviser to the Home
Office and to the Corporation of London under the Petroleum Acts, &c., &c.
Page 649
Assisted by GEO. T. HOLLOWAY, F.I.C., Assoc. R.C.S., And Numerous Contributors.
General Contents.—I. Historical.—II. Geological and Geographical
Distribution of Petroleum and Natural Gas.—III. Chemical and Physical
Properties.—IV. Origin—V. Production.—VI. Refining.—VII. The Shale
Oil and Allied Industries.—VIII. Transport, Storage, and Distribution.—IX.
Testing.—X. Application and Uses.—XI. Legislation at Home and Abroad.
—XII. Statistics.—Index.
"The MOST COMPREHENSIVE AND CONVENIENT ACCOUNT that
has yet appeared of a gigantic Industry which has made incalculable
additions to the comfort of civilised man."—The Times.
"A splendid contribution to our technical literature."—Chemical News.
With Plates (One Coloured) and Illustrations. Price 8s. 6d. net.
A HANDBOOK ON PETROLEUM.
FOR INSPECTORS UNDER THE PETROLEUM ACTS,
And for those engaged in the Storage, Transport, Distribution, and Industrial Use of Petroleum
and its Products, and of Calcium Carbide. With suggestions on the Construction and Use of
Mineral Oil Lamps.
By CAPTAIN J.H. THOMSON, H.M. Chief Inspector of Explosives,
AND
Dr. BOVERTON REDWOOD,
Author of "Petroleum and its Products."
Contents.—I. Introductory.—II. Sources of Supply.—III. Production.—IV.
Chemical Products, Shale Oil, and Coal Tar.—V. Flash Point and Fire Test.
—VI. Testings.—VII. Existing Legislation relating to Petroleum.—VIII.—
General Contents.—I. Historical.—II. Geological and Geographical
Distribution of Petroleum and Natural Gas.—III. Chemical and Physical
Properties.—IV. Origin—V. Production.—VI. Refining.—VII. The Shale
Oil and Allied Industries.—VIII. Transport, Storage, and Distribution.—IX.
Testing.—X. Application and Uses.—XI. Legislation at Home and Abroad.
—XII. Statistics.—Index.
"The MOST COMPREHENSIVE AND CONVENIENT ACCOUNT that
has yet appeared of a gigantic Industry which has made incalculable
additions to the comfort of civilised man."—The Times.
"A splendid contribution to our technical literature."—Chemical News.
With Plates (One Coloured) and Illustrations. Price 8s. 6d. net.
A HANDBOOK ON PETROLEUM.
FOR INSPECTORS UNDER THE PETROLEUM ACTS,
And for those engaged in the Storage, Transport, Distribution, and Industrial Use of Petroleum
and its Products, and of Calcium Carbide. With suggestions on the Construction and Use of
Mineral Oil Lamps.
By CAPTAIN J.H. THOMSON, H.M. Chief Inspector of Explosives,
AND
Dr. BOVERTON REDWOOD,
Author of "Petroleum and its Products."
Contents.—I. Introductory.—II. Sources of Supply.—III. Production.—IV.
Chemical Products, Shale Oil, and Coal Tar.—V. Flash Point and Fire Test.
—VI. Testings.—VII. Existing Legislation relating to Petroleum.—VIII.—
Page 650
IX.—Precautions Necessary.—X. Petroleum Oil Lamps.—XI. Carbide of
Calcium and Acetylene.—Appendices.—Index.
"A volume that will enrich the world's petroleum literature, and render a
service to the British branch of the industry.... Reliable, indispensable, a
brilliant contribution."—Petroleum.
THE PETROLEUM LAMP: Its Choice and Use. A Guide to the Safe
Employment of Mineral Oil in what is commonly termed the Paraffin
Lamp. By Capt. J.H. Thomson and Dr. Boverton Redwood. Popular
Edition, Illustrated. 1s. net.
"The book contains a great deal of interesting reading, much of which is
thoroughly practical and useful. It is a work which will meet every purpose
for which it has been written."—Petroleum.
Calcium and Acetylene.—Appendices.—Index.
"A volume that will enrich the world's petroleum literature, and render a
service to the British branch of the industry.... Reliable, indispensable, a
brilliant contribution."—Petroleum.
THE PETROLEUM LAMP: Its Choice and Use. A Guide to the Safe
Employment of Mineral Oil in what is commonly termed the Paraffin
Lamp. By Capt. J.H. Thomson and Dr. Boverton Redwood. Popular
Edition, Illustrated. 1s. net.
"The book contains a great deal of interesting reading, much of which is
thoroughly practical and useful. It is a work which will meet every purpose
for which it has been written."—Petroleum.
Page 651
Griffin's Metallurgical Series.
STANDARD WORKS OF REFERENCE
FOR
Metallurgists, Mine-Owners, Assayers, Manufacturers, and all interested in the development of
the Metallurgical Industries.
EDITED BY Sir W. ROBERTS-AUSTEN, K.C.B., D.C.L, F.R.S.
In Large 8vo, Handsome Cloth. With Illustrations.
INTRODUCTION to the STUDY of METALLURGY. By the Editor.
Fifth Edition. 18s. (See p. 63.)
GOLD (The Metallurgy of). By Thos. Kirke Rose, D.Sc., Assoc.R.S.M.,
F.I.C., Chemist and Assayer of the Royal Mint. Fourth Edition. 21s. (See p.
63.)
LEAD AND SILVER (The Metallurgy of). By H.F. Collins,
Assoc.R.S.M., M.Inst.M.M. Part I., Lead, 16s; Part II., Silver, 16s. (See p.
64.)
IRON (The Metallurgy of). By T. Turner, A.R.S.M., F.I.C., F.C.S. Second
Edition, Revised. 16s. (See p. 65.)
STEEL (The Metallurgy of). By F.W. Harbord, Assoc.R.S.M., F.I.C., with
a Section on Mechanical Treatment by J.W. Hall, A.M.Inst, C.E. (See p.
65.) [Ready shortly.
STANDARD WORKS OF REFERENCE
FOR
Metallurgists, Mine-Owners, Assayers, Manufacturers, and all interested in the development of
the Metallurgical Industries.
EDITED BY Sir W. ROBERTS-AUSTEN, K.C.B., D.C.L, F.R.S.
In Large 8vo, Handsome Cloth. With Illustrations.
INTRODUCTION to the STUDY of METALLURGY. By the Editor.
Fifth Edition. 18s. (See p. 63.)
GOLD (The Metallurgy of). By Thos. Kirke Rose, D.Sc., Assoc.R.S.M.,
F.I.C., Chemist and Assayer of the Royal Mint. Fourth Edition. 21s. (See p.
63.)
LEAD AND SILVER (The Metallurgy of). By H.F. Collins,
Assoc.R.S.M., M.Inst.M.M. Part I., Lead, 16s; Part II., Silver, 16s. (See p.
64.)
IRON (The Metallurgy of). By T. Turner, A.R.S.M., F.I.C., F.C.S. Second
Edition, Revised. 16s. (See p. 65.)
STEEL (The Metallurgy of). By F.W. Harbord, Assoc.R.S.M., F.I.C., with
a Section on Mechanical Treatment by J.W. Hall, A.M.Inst, C.E. (See p.
65.) [Ready shortly.
Page 652
Will be Published at Short Intervals.
METALLURGICAL MACHINERY: the Application of Engineering to
Metallurgical Problems. By Henry Charles Jenkins, Wh.Sc., Assoc.R.S.M.,
Assoc.M.Inst.C.E., of the Royal College of Science. (See p. 64).
ALLOYS. By the Editor.
*** Other Volumes in Preparation.
Fifth Edition, thoroughly Revised and considerably Enlarged. Large 8vo,
with numerous Illustrations and Micro-Photographic Plates of different
varieties of Steel. 18s.
An Introduction to the Study of METALLURGY.
BY
Sir W. ROBERTS-AUSTEN, K.C.B., D.C.L., F.R.S., A.R.S.M.,
Late Chemist and Assayer of the Royal Mint, and Professor of Metallurgy in the Royal College of Science.
General Contents.—The Relation of Metallurgy to Chemistry.—Physical
Properties of Metals.—Alloys.—The Thermal Treatment of Metals.—Fuel
and Thermal Measurements.—Materials and Products of Metallurgical
Processes.—Furnaces.—Means of Supplying Air to Furnaces.—Thermo-
Chemistry.—Typical Metallurgical Processes.—The Micro-Structure of
Metals and Alloys.—Economic Considerations.
"No English text-book at all approaches this in the completeness with
which the most modern views on the subject are dealt with. Professor
Austen's volume will be invaluable, not only to the student, but also to
those whose knowledge of the art is far advanced."—Chemical News.
METALLURGICAL MACHINERY: the Application of Engineering to
Metallurgical Problems. By Henry Charles Jenkins, Wh.Sc., Assoc.R.S.M.,
Assoc.M.Inst.C.E., of the Royal College of Science. (See p. 64).
ALLOYS. By the Editor.
*** Other Volumes in Preparation.
Fifth Edition, thoroughly Revised and considerably Enlarged. Large 8vo,
with numerous Illustrations and Micro-Photographic Plates of different
varieties of Steel. 18s.
An Introduction to the Study of METALLURGY.
BY
Sir W. ROBERTS-AUSTEN, K.C.B., D.C.L., F.R.S., A.R.S.M.,
Late Chemist and Assayer of the Royal Mint, and Professor of Metallurgy in the Royal College of Science.
General Contents.—The Relation of Metallurgy to Chemistry.—Physical
Properties of Metals.—Alloys.—The Thermal Treatment of Metals.—Fuel
and Thermal Measurements.—Materials and Products of Metallurgical
Processes.—Furnaces.—Means of Supplying Air to Furnaces.—Thermo-
Chemistry.—Typical Metallurgical Processes.—The Micro-Structure of
Metals and Alloys.—Economic Considerations.
"No English text-book at all approaches this in the completeness with
which the most modern views on the subject are dealt with. Professor
Austen's volume will be invaluable, not only to the student, but also to
those whose knowledge of the art is far advanced."—Chemical News.
Page 653
Fourth Edition, Revised, Considerably Enlarged, and in part Re-written.
Including the most recent Improvements in the Cyanide Process. With
Frontispiece and numerous Illustrations. 21s.
THE METALLURGY OF GOLD.
BY
T. KIRKE ROSE, D.Sc.Lond., Assoc.R.S.M.,
Chemist and Assayer of the Royal Mint.
General Contents.—The Properties of Gold and its Alloys.—Chemistry of
Gold.—Mode of Occurrence and Distribution.—Placer Mining.—Shallow
Deposits.—Deep Placer Mining.—Quartz Crushing in the Stamp Battery.—
Amalgamation.—Other Forms of Crushing and Amalgamating.—
Concentration.—Stamp Battery Practice.—Chlorination: The Preparation of
Ore.—The Vat Process.—The Barrel Process.—Chlorination Practice in
Particular Mills.—The Cyanide Process.—Chemistry of the Process.—
Pyritic Smelting.—The Refining and Parting of Gold Bullion—The Assay
of Gold Ores.—The Assay of Bullion—Economic Considerations.—
Bibliography.
"A comprehensive practical treatise on this important subject."—The
Times.
"The most complete description of the chlorination process which has yet
been published."—Mining Journal.
"Adapted for all who are interested in the Gold Mining Industry, being free
from technicalities as far as possible, but is more particularly of value to
those engaged in the industry."—Cape Times.
Edited by SIR W. ROBERTS-AUSTEN, K.C.B., F.R.S., D.C.L.
Including the most recent Improvements in the Cyanide Process. With
Frontispiece and numerous Illustrations. 21s.
THE METALLURGY OF GOLD.
BY
T. KIRKE ROSE, D.Sc.Lond., Assoc.R.S.M.,
Chemist and Assayer of the Royal Mint.
General Contents.—The Properties of Gold and its Alloys.—Chemistry of
Gold.—Mode of Occurrence and Distribution.—Placer Mining.—Shallow
Deposits.—Deep Placer Mining.—Quartz Crushing in the Stamp Battery.—
Amalgamation.—Other Forms of Crushing and Amalgamating.—
Concentration.—Stamp Battery Practice.—Chlorination: The Preparation of
Ore.—The Vat Process.—The Barrel Process.—Chlorination Practice in
Particular Mills.—The Cyanide Process.—Chemistry of the Process.—
Pyritic Smelting.—The Refining and Parting of Gold Bullion—The Assay
of Gold Ores.—The Assay of Bullion—Economic Considerations.—
Bibliography.
"A comprehensive practical treatise on this important subject."—The
Times.
"The most complete description of the chlorination process which has yet
been published."—Mining Journal.
"Adapted for all who are interested in the Gold Mining Industry, being free
from technicalities as far as possible, but is more particularly of value to
those engaged in the industry."—Cape Times.
Edited by SIR W. ROBERTS-AUSTEN, K.C.B., F.R.S., D.C.L.
Page 654
In Large 8vo. Handsome Cloth. With Illustrations.
In Two Volumes, Each Complete in Itself and Sold Separately.
THE METALLURGY OF LEAD AND SILVER.
By H.F. COLLINS, Assoc.R.S.M., M.Inst.M.M.
Part I.—LEAD:
A Complete and Exhaustive Treatise on the Manufacture of Lead, with
Sections on Smelting and Desilverisation, and Chapters on the Assay and
Analysis of the Materials involved. Price 16s.
Summary of Contents.—Sampling and Assaying Lead and Silver.—
Properties and Compounds of Lead.—Lead Ores.—Lead Smelting.—
Reverberatories.—Lead Smelting in Hearths.—The Roasting of Lead Ores.
—Blast Furnace Smelting; Principles, Practice, and Examples; Products.—
Flue Dust, its Composition, Collection and Treatment.—Costs and Losses,
Purchase of Ores.—Treatment of Zinc, Lead Sulphides, Desilverisation,
Softening and Refining.—The Pattinson Process.—The Parkes Process.—
Cupellation and Refining, &c., &c.
"A thoroughly sound and useful digest. May with every confidence be
recommended."—Mining Journal.
Part II. SILVER.
Comprising Details regarding the Sources and Treatment of Silver Ores,
together with Descriptions of Plant, Machinery, and Processes of
Manufacture, Refining of Bullion, Cost of Working, &c. Price 16s.
In Two Volumes, Each Complete in Itself and Sold Separately.
THE METALLURGY OF LEAD AND SILVER.
By H.F. COLLINS, Assoc.R.S.M., M.Inst.M.M.
Part I.—LEAD:
A Complete and Exhaustive Treatise on the Manufacture of Lead, with
Sections on Smelting and Desilverisation, and Chapters on the Assay and
Analysis of the Materials involved. Price 16s.
Summary of Contents.—Sampling and Assaying Lead and Silver.—
Properties and Compounds of Lead.—Lead Ores.—Lead Smelting.—
Reverberatories.—Lead Smelting in Hearths.—The Roasting of Lead Ores.
—Blast Furnace Smelting; Principles, Practice, and Examples; Products.—
Flue Dust, its Composition, Collection and Treatment.—Costs and Losses,
Purchase of Ores.—Treatment of Zinc, Lead Sulphides, Desilverisation,
Softening and Refining.—The Pattinson Process.—The Parkes Process.—
Cupellation and Refining, &c., &c.
"A thoroughly sound and useful digest. May with every confidence be
recommended."—Mining Journal.
Part II. SILVER.
Comprising Details regarding the Sources and Treatment of Silver Ores,
together with Descriptions of Plant, Machinery, and Processes of
Manufacture, Refining of Bullion, Cost of Working, &c. Price 16s.
Page 655
Summary of Contents.—Properties of Silver and its Principal Compounds.
—Silver Ores.—The Patio Process.—The Kazo, Fondon, Kröhnke, and
Tina Processes.—The Pan Process.—Roast Amalgamation.—Treatment of
Tailings and Concentration.—Retorting, Melting, and Assaying.—
Chloridising-Roasting.—The Augustin, Claudet, and Ziervogel Processes.
—The Hypo-Sulphite Leaching Process.—Refining.—Matte Smelting.—
Pyritic Smelting.—Matte Smelting in Reverberatories.—Silver-Copper
Smelting and Refining.—Index.
"The author has focussed a large amount of valuable information into a
convenient form.... The author has evidently considerable practical
experience, and describes the various processes clearly and well."—Mining
Journal.
IN PREPARATION.
METALLURGICAL MACHINERY:
The Application of Engineering to Metallurgical Problems.
By HENRY CHARLES JENKINS,
Wh.Sc., Assoc.R.S.M., Assoc.M.Inst.C.E.
Ready Shortly. With Numerous Illustrations. Large 8vo. Handsome Cloth.
THE METALLURGY OF STEEL.
By F.W. HARBORD, Assoc.R.S.M., F.I.C.,
Consulting Metallurgist and Analytical Chemist to the Indian Government, Royal Indian Engineering College, Coopers Hill.
—Silver Ores.—The Patio Process.—The Kazo, Fondon, Kröhnke, and
Tina Processes.—The Pan Process.—Roast Amalgamation.—Treatment of
Tailings and Concentration.—Retorting, Melting, and Assaying.—
Chloridising-Roasting.—The Augustin, Claudet, and Ziervogel Processes.
—The Hypo-Sulphite Leaching Process.—Refining.—Matte Smelting.—
Pyritic Smelting.—Matte Smelting in Reverberatories.—Silver-Copper
Smelting and Refining.—Index.
"The author has focussed a large amount of valuable information into a
convenient form.... The author has evidently considerable practical
experience, and describes the various processes clearly and well."—Mining
Journal.
IN PREPARATION.
METALLURGICAL MACHINERY:
The Application of Engineering to Metallurgical Problems.
By HENRY CHARLES JENKINS,
Wh.Sc., Assoc.R.S.M., Assoc.M.Inst.C.E.
Ready Shortly. With Numerous Illustrations. Large 8vo. Handsome Cloth.
THE METALLURGY OF STEEL.
By F.W. HARBORD, Assoc.R.S.M., F.I.C.,
Consulting Metallurgist and Analytical Chemist to the Indian Government, Royal Indian Engineering College, Coopers Hill.
Page 656
With over 40 Plates, 500 Illustrations (comprising nearly 100 Micro-
Sections of Steel), Diagrams of Plant and Machinery, reduced from
Working Drawings, and a Section on Mill Practice.
By J.W. HALL, A.M.Inst.C.E.
Abridged Contents.—The Plant, Machinery, Methods and Chemistry of the
Bessemer and of the Open Hearth Processes (Acid and Basic).—The
Mechanical Treatment of Steel comprising Mill Practice, Plant and
Machinery.—The Influence of Metalloids, Heat Treatment, Special Steels,
Microstructure, Testing, and Specifications.
Second Edition, Revised. Price 16s.
THE METALLURGY OF IRON.
By THOMAS TURNER, Assoc.R.S.M., F.I.C.,
Professor of Metallurgy in the University of Birmingham.
In Large 8vo, Handsome Cloth, With Numerous Illustrations (many from
Photographs).
General Contents.—Early History of Iron.—Modern History of Iron.—The
Age of Steel.—Chief Iron Ores.—Preparation of Iron Ores.—The Blast
Furnace.—The Air used in the Blast Furnace.—Reactions of the Blast
Furnace.—The Fuel used in the Blast Furnace.—Slags and Fluxes of Iron
Smelting.—Properties of Cast Iron.—Foundry Practice.—Wrought Iron.—
Indirect Production of Wrought Iron.—The Puddling Process.—Further
Treatment of Wrought Iron.—Corrosion of Iron and Steel.
"A most valuable summary of knowledge relating to every method and
stage in the manufacture of cast and wrought iron ... rich in chemical
details.... Exhaustive and thoroughly up-to-date."—Bulletin of the
American Iron and Steel Association.
Sections of Steel), Diagrams of Plant and Machinery, reduced from
Working Drawings, and a Section on Mill Practice.
By J.W. HALL, A.M.Inst.C.E.
Abridged Contents.—The Plant, Machinery, Methods and Chemistry of the
Bessemer and of the Open Hearth Processes (Acid and Basic).—The
Mechanical Treatment of Steel comprising Mill Practice, Plant and
Machinery.—The Influence of Metalloids, Heat Treatment, Special Steels,
Microstructure, Testing, and Specifications.
Second Edition, Revised. Price 16s.
THE METALLURGY OF IRON.
By THOMAS TURNER, Assoc.R.S.M., F.I.C.,
Professor of Metallurgy in the University of Birmingham.
In Large 8vo, Handsome Cloth, With Numerous Illustrations (many from
Photographs).
General Contents.—Early History of Iron.—Modern History of Iron.—The
Age of Steel.—Chief Iron Ores.—Preparation of Iron Ores.—The Blast
Furnace.—The Air used in the Blast Furnace.—Reactions of the Blast
Furnace.—The Fuel used in the Blast Furnace.—Slags and Fluxes of Iron
Smelting.—Properties of Cast Iron.—Foundry Practice.—Wrought Iron.—
Indirect Production of Wrought Iron.—The Puddling Process.—Further
Treatment of Wrought Iron.—Corrosion of Iron and Steel.
"A most valuable summary of knowledge relating to every method and
stage in the manufacture of cast and wrought iron ... rich in chemical
details.... Exhaustive and thoroughly up-to-date."—Bulletin of the
American Iron and Steel Association.
Page 657
"This is a delightful book, giving, as it does, reliable information on a
subject becoming every day more elaborate."—Colliery Guardian.
"A thoroughly useful book, which brings the subject up to date. Of great
value to those engaged in the iron industry."—Mining Journal.
*** For Details of Works on Mining, see pages 55-59.
A TEXT-BOOK OF ASSAYING:
For the use of Students, Mine Managers, Assayers, &c.
By J.J. BERINGER, F.I.C., F.C.S.,
Public Analyst for, and Lecturer to the Mining Association of, Cornwall.
And C. BERINGER, F.C.S.,
Late Chief Assayer to the Rio Tinto Copper Company, London.
With numerous Tables and Illustrations. Crown 8vo. Cloth, 10s. 6d. Eighth
Edition.
General Contents.—Part I.—Introductory; Manipulation: Sampling;
Drying; Calculation of Results—Laboratory-books and Reports. Methods:
Dry Gravimetric; Wet Gravimetric—Volumetric Assays: Titrometric,
Colorimetric, Gasometric—Weighing and Measuring—Reagents—
Formulæ, Equations, &c.—Specific Gravity.
Part II.—Metals: Detection and Assay of Silver, Gold, Platinum, Mercury,
Copper, Lead, Thallium, Bismuth, Antimony, Iron, Nickel, Cobalt, Zinc,
Cadmium, Tin, Tungsten, Titanium, Manganese, Chromium, &c.—Earths,
Alkalies.
subject becoming every day more elaborate."—Colliery Guardian.
"A thoroughly useful book, which brings the subject up to date. Of great
value to those engaged in the iron industry."—Mining Journal.
*** For Details of Works on Mining, see pages 55-59.
A TEXT-BOOK OF ASSAYING:
For the use of Students, Mine Managers, Assayers, &c.
By J.J. BERINGER, F.I.C., F.C.S.,
Public Analyst for, and Lecturer to the Mining Association of, Cornwall.
And C. BERINGER, F.C.S.,
Late Chief Assayer to the Rio Tinto Copper Company, London.
With numerous Tables and Illustrations. Crown 8vo. Cloth, 10s. 6d. Eighth
Edition.
General Contents.—Part I.—Introductory; Manipulation: Sampling;
Drying; Calculation of Results—Laboratory-books and Reports. Methods:
Dry Gravimetric; Wet Gravimetric—Volumetric Assays: Titrometric,
Colorimetric, Gasometric—Weighing and Measuring—Reagents—
Formulæ, Equations, &c.—Specific Gravity.
Part II.—Metals: Detection and Assay of Silver, Gold, Platinum, Mercury,
Copper, Lead, Thallium, Bismuth, Antimony, Iron, Nickel, Cobalt, Zinc,
Cadmium, Tin, Tungsten, Titanium, Manganese, Chromium, &c.—Earths,
Alkalies.
Page 658
Part III.—Non-Metals: Oxygen and Oxides; The Halogens—Sulphur and
Sulphates—Arsenic, Phosphorus, Nitrogen—Silicon, Carbon, Boron—
Useful Tables.
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Third Edition, Revised. Handsome Cloth. With Numerous Illustrations. 6s.
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Including the Author's Practical Laboratory Course.
By A. HUMBOLDT SEXTON, F.I.C., F.C.S.,
Professor of Metallurgy in the Glasgow and West of Scotland Technical College.
GENERAL CONTENTS.—Introduction.—Properties of the Metals.—
Combustion.—Fuels.—Refractory Materials.—Furnaces.—Occurrence of
the Metals in Nature.—Preparation of the Ore for the Smelter.—
Metallurgical Processes.—Iron.—Steel.—-Copper.—Lead.—Zinc and Tin.
—Silver.—Gold.—Mercury.—Alloys.—Applications of Electricity to
Metallurgy.—Laboratory Course.
"Just the kind of work for Students commencing the study of Metallurgy, or
for Engineering Students."—Practical Engineer.
"Excellently got-up and well-arranged."—Chemical Trade Journal.
In Large 8vo. Handsome Cloth. Price 4s.
Sulphates—Arsenic, Phosphorus, Nitrogen—Silicon, Carbon, Boron—
Useful Tables.
"A really meritorious work, that may be safely depended upon either for
systematic instruction or for reference."—Nature.
"This work is one of the best of its kind."—Engineer.
Third Edition, Revised. Handsome Cloth. With Numerous Illustrations. 6s.
A TEXT-BOOK OF ELEMENTARY METALLURGY.
Including the Author's Practical Laboratory Course.
By A. HUMBOLDT SEXTON, F.I.C., F.C.S.,
Professor of Metallurgy in the Glasgow and West of Scotland Technical College.
GENERAL CONTENTS.—Introduction.—Properties of the Metals.—
Combustion.—Fuels.—Refractory Materials.—Furnaces.—Occurrence of
the Metals in Nature.—Preparation of the Ore for the Smelter.—
Metallurgical Processes.—Iron.—Steel.—-Copper.—Lead.—Zinc and Tin.
—Silver.—Gold.—Mercury.—Alloys.—Applications of Electricity to
Metallurgy.—Laboratory Course.
"Just the kind of work for Students commencing the study of Metallurgy, or
for Engineering Students."—Practical Engineer.
"Excellently got-up and well-arranged."—Chemical Trade Journal.
In Large 8vo. Handsome Cloth. Price 4s.
Page 659
TABLES FOR QUANTITATIVE METALLURGICAL
ANALYSIS. FOR LABORATORY USE.
ON THE PRINCIPLE OF "GROUP" SEPARATIONS.
By J. JAMES MORGAN, F.C.S., M.S.C.I.
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carried out."—The Engineer.
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precision mark the book out as a highly useful one."—Mining Journal.
Second Edition, Revised, Enlarged, and in part Re-written. With Additional
Sections on Modern Theories of Electrolysis Costs, &c. Price 10s. 6d.
A TREATISE ON ELECTRO-METALLURGY:
Embracing the Application of Electrolysis to the Plating, Depositing, Smelting, and Refining of
various Metals, and to the Reproduction of Printing Surfaces and Art-Work, &c.
BY
WALTER G. McMILLAN, F.I.C., F.C.S.,
Secretary to the Institution of Electrical Engineers; late Lecturer in Metallurgy at Mason College, Birmingham.
With numerous Illustrations. Large Crown 8vo. Cloth.
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manuals hitherto published on Electro-Metallurgy."—Electrical Review.
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ON THE PRINCIPLE OF "GROUP" SEPARATIONS.
By J. JAMES MORGAN, F.C.S., M.S.C.I.
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A TREATISE ON ELECTRO-METALLURGY:
Embracing the Application of Electrolysis to the Plating, Depositing, Smelting, and Refining of
various Metals, and to the Reproduction of Printing Surfaces and Art-Work, &c.
BY
WALTER G. McMILLAN, F.I.C., F.C.S.,
Secretary to the Institution of Electrical Engineers; late Lecturer in Metallurgy at Mason College, Birmingham.
With numerous Illustrations. Large Crown 8vo. Cloth.
"This excellent treatise, ... one of the BEST and MOST COMPLETE
manuals hitherto published on Electro-Metallurgy."—Electrical Review.
"This work will be a standard."—Jeweller.
Page 660
"Any metallurgical process which reduces the cost of production must of
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manual to ALL who are interested in the practical application of
electrolytic processes."—Nature.
In large 8vo. With Numerous Illustrations and Three Folding-Plates. Price
21s.
ELECTRIC SMELTING & REFINING:
A Practical Manual of the Extraction and Treatment of Metals by Electrical Methods.
Being the "Elektro-Metallurgie" of Dr. W. BORCHERS.
Translated from the Second Edition by WALTER G. McMILLAN,
F.I.C., F.C.S
CONTENTS.
Part I.—Alkalies and Alkaline Earth Metals: Magnesium, Lithium,
Beryllium, Sodium, Potassium, Calcium, Strontium, Barium, the Carbides
of the Alkaline Earth Metals.
Part II.—The Earth Metals: Aluminium, Cerium, Lanthanum, Didymium.
Part III.—The Heavy Metals: Copper, Silver, Gold, Zinc and Cadmium,
Mercury, Tin, Lead, Bismuth, Antimony, Chromium, Molybdenum,
Tungsten, Uranium, Manganese, Iron, Nickel, and Cobalt, the Platinum
Group.
"Comprehensive and authoritative ... not only full of valuable
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manual to ALL who are interested in the practical application of
electrolytic processes."—Nature.
In large 8vo. With Numerous Illustrations and Three Folding-Plates. Price
21s.
ELECTRIC SMELTING & REFINING:
A Practical Manual of the Extraction and Treatment of Metals by Electrical Methods.
Being the "Elektro-Metallurgie" of Dr. W. BORCHERS.
Translated from the Second Edition by WALTER G. McMILLAN,
F.I.C., F.C.S
CONTENTS.
Part I.—Alkalies and Alkaline Earth Metals: Magnesium, Lithium,
Beryllium, Sodium, Potassium, Calcium, Strontium, Barium, the Carbides
of the Alkaline Earth Metals.
Part II.—The Earth Metals: Aluminium, Cerium, Lanthanum, Didymium.
Part III.—The Heavy Metals: Copper, Silver, Gold, Zinc and Cadmium,
Mercury, Tin, Lead, Bismuth, Antimony, Chromium, Molybdenum,
Tungsten, Uranium, Manganese, Iron, Nickel, and Cobalt, the Platinum
Group.
"Comprehensive and authoritative ... not only full of valuable
information, but gives evidence of athorough insight into the technical
Page 661
value and possibilities of all the methods discussed."—The Electrician.
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every one interested in the subject. Excellently put into English with
additional matter by Mr. McMillan."—Nature.
"Will be of GREAT SERVICE to the practical man and the Student."—
Electric Smelting.
In Large 4to, Library Style. Beautifully Illustrated with 20 Plates, many in
Colours, and 94 Figures in the Text.
PRECIOUS STONES: Their Properties, Occurrences, and
Uses.
A Treatise for Dealers, Manufacturers, Jewellers, and for all Collectors and others interested in
Gems.
By Dr. MAX BAUER, Professor in the University of Marburg,
Translated by L.J. SPENCER, M.A. (Cantab.), F.G.S.
General Contents.—General Properties of Gems: Their Natural
Characters, Occurrence, Application, and Uses.—Detailed Description of
Particular Gems: The Diamond, Rubies, Sapphires; Emeralds, Tourmalines,
and Opals; Felspars, Amphiboles, Malachite.—Non-mineral Gems: Amber,
&c.—Optical Features, Transparency, Translucency, Opacity, Refraction
and Dispersion, &c.—Appendix: Pearls; Coral.
In Large Crown 8vo. With Numerous Illustrations. 8s. 6d.
The Art of the Goldsmith and Jeweller
"Dr. Borchers' well-known work ... must of necessity be acquired by
every one interested in the subject. Excellently put into English with
additional matter by Mr. McMillan."—Nature.
"Will be of GREAT SERVICE to the practical man and the Student."—
Electric Smelting.
In Large 4to, Library Style. Beautifully Illustrated with 20 Plates, many in
Colours, and 94 Figures in the Text.
PRECIOUS STONES: Their Properties, Occurrences, and
Uses.
A Treatise for Dealers, Manufacturers, Jewellers, and for all Collectors and others interested in
Gems.
By Dr. MAX BAUER, Professor in the University of Marburg,
Translated by L.J. SPENCER, M.A. (Cantab.), F.G.S.
General Contents.—General Properties of Gems: Their Natural
Characters, Occurrence, Application, and Uses.—Detailed Description of
Particular Gems: The Diamond, Rubies, Sapphires; Emeralds, Tourmalines,
and Opals; Felspars, Amphiboles, Malachite.—Non-mineral Gems: Amber,
&c.—Optical Features, Transparency, Translucency, Opacity, Refraction
and Dispersion, &c.—Appendix: Pearls; Coral.
In Large Crown 8vo. With Numerous Illustrations. 8s. 6d.
The Art of the Goldsmith and Jeweller
Page 662
A Manual on the Manipulation of Gold and the Manufacture of Personal Ornaments.
By THOS. B. WIGLEY,
Headmaster of the Jewellers and Silversmiths' Association Technical School, Birmingham.
ASSISTED BY J.H. STANSBIE, B.Sc. (Lond.), F.I.C.,
Lecturer at the Birmingham Municipal Technical School.
General Contents.—Introduction.—The Ancient Goldsmith's Art.—
Metallurgy of Gold.—Prices, &c.—Alloys.—Melting, Rolling, and Slitting
Gold.—The workshop and Tools.—Wire Drawing.—Rings.—Chains and
Insignia.—Antique Jewellery and its Revival.—Etruscan Work.—Precious
Stones.—Cutting.—Polishing and Finishing.—Chasing, Embossing, and
Repoussé Work.—Colouring and Finishing.—Enamelling.—Engraving.—
Moulding and Casting Ornaments, &c.—Fluxes. &c.—Recovery of the
Precious Metals.—Refining and Assaying.—Gilding and Electro
Deposition.—Hall-Marking.—Miscellaneous.—Appendix.
By THOS. B. WIGLEY,
Headmaster of the Jewellers and Silversmiths' Association Technical School, Birmingham.
ASSISTED BY J.H. STANSBIE, B.Sc. (Lond.), F.I.C.,
Lecturer at the Birmingham Municipal Technical School.
General Contents.—Introduction.—The Ancient Goldsmith's Art.—
Metallurgy of Gold.—Prices, &c.—Alloys.—Melting, Rolling, and Slitting
Gold.—The workshop and Tools.—Wire Drawing.—Rings.—Chains and
Insignia.—Antique Jewellery and its Revival.—Etruscan Work.—Precious
Stones.—Cutting.—Polishing and Finishing.—Chasing, Embossing, and
Repoussé Work.—Colouring and Finishing.—Enamelling.—Engraving.—
Moulding and Casting Ornaments, &c.—Fluxes. &c.—Recovery of the
Precious Metals.—Refining and Assaying.—Gilding and Electro
Deposition.—Hall-Marking.—Miscellaneous.—Appendix.
Page 663
PAGE
Inorganic Chemistry, Profs. Dupré and Hake, 70
Quantitative Analysis, Prof. Humboldt Sexton, 70
Qualitative " " " 70
Chemistry for Engineers, Blount and Bloxam, 71
" " Manufacturers, " " 71
Foods, Analysis of, A. Wynter Blyth, 72
Poisons, Detection of, " " 72
Tables for Chemists and
Prof. Castell-Evans, 79
Manufacturers,
Agricultural Chemistry, Prof. J.M.H. Munro, 75
Dairy Chemistry, H. D. Richmond, 73
Milk, E.F. Willoughby, 73
Flesh Foods, C.A. Mitchell, 73
Practical Sanitation, Dr. G. Reid, 78
Sanitary Engineering, F. Wood, 78
Technical Mycology, Lafar and Salter, 74
Ferments, C. Oppenheimer, 74
Brewing, Dr. W.J. Sykes, 75
Sewage Disposal, Santo Crimp, 76
Trades' Waste, W. Naylor, 76
Cements, G.R. Redgrave, 76
Water Supply, R.E. Middleton, 77
Road Making, Thos. Aitken, 79
Gas Manufacture, W. Atkinson Butterfield, 77
Acetylene, Leeds and Butterfield, 77
Fire Risks, Dr. Schwartz, 77
Petroleum, Redwood and Holloway, 61
—— (Handbook), Thomson and Redwood, 61
Oils, Soaps, Candles, Dr. Alder Wright, 81
Lubrication and Lubricants, Archbutt and Deeley, 32
India Rubber, Dr. Carl O. Weber, 81
Painters' Colours, Oils, and
G.H. Hurst, 80
Varnishes,
Inorganic Chemistry, Profs. Dupré and Hake, 70
Quantitative Analysis, Prof. Humboldt Sexton, 70
Qualitative " " " 70
Chemistry for Engineers, Blount and Bloxam, 71
" " Manufacturers, " " 71
Foods, Analysis of, A. Wynter Blyth, 72
Poisons, Detection of, " " 72
Tables for Chemists and
Prof. Castell-Evans, 79
Manufacturers,
Agricultural Chemistry, Prof. J.M.H. Munro, 75
Dairy Chemistry, H. D. Richmond, 73
Milk, E.F. Willoughby, 73
Flesh Foods, C.A. Mitchell, 73
Practical Sanitation, Dr. G. Reid, 78
Sanitary Engineering, F. Wood, 78
Technical Mycology, Lafar and Salter, 74
Ferments, C. Oppenheimer, 74
Brewing, Dr. W.J. Sykes, 75
Sewage Disposal, Santo Crimp, 76
Trades' Waste, W. Naylor, 76
Cements, G.R. Redgrave, 76
Water Supply, R.E. Middleton, 77
Road Making, Thos. Aitken, 79
Gas Manufacture, W. Atkinson Butterfield, 77
Acetylene, Leeds and Butterfield, 77
Fire Risks, Dr. Schwartz, 77
Petroleum, Redwood and Holloway, 61
—— (Handbook), Thomson and Redwood, 61
Oils, Soaps, Candles, Dr. Alder Wright, 81
Lubrication and Lubricants, Archbutt and Deeley, 32
India Rubber, Dr. Carl O. Weber, 81
Painters' Colours, Oils, and
G.H. Hurst, 80
Varnishes,
Page 664
Painters' Laboratory Guide, " " 80
Painting and Decorating, W.J. Pearce, 80
Photography, A. Brothers, 21
Dyeing, Knecht and Rawson, 82
Rawson, Gardner, and
Dictionary of Dyes, 82
Laycock,
Textile Printing, Seymour Rothwell, 83
Textile Fibres of Commerce, W.I. Hannan, 83
Dyeing and Cleaning, G.H. Hurst, 84
Bleaching and Calico-Printing, Geo. Duerr, 84
A SHORT MANUAL OF INORGANIC CHEMISTRY.
BY A. DUPRÉ, Ph.D., F.R.S.,
AND
WILSON HAKE, Ph.D., F.I.C., F.C.S.,
Of the Westminster Hospital Medical School
Third Edition, Revised, Enlarged, and Re-issued. Price 6s. net.
"A well-written, clear and accurate Elementary Manual of Inorganic
Chemistry.... We agree heartily with the system adopted by Drs. Dupré and
Hake. Will Make Experimental Work trebly interesting because
intelligible."—Saturday Review.
"There is no question that, given the perfect grounding of the Student in his
Science, the remainder comes afterwards to him in a manner much more
simple and easily acquired. The work is an example of the advantages of
the Systematic Treatment of a Science over the fragmentary style so
generally followed. By a long way the best of the small Manuals for
Students."—Analyst.
Painting and Decorating, W.J. Pearce, 80
Photography, A. Brothers, 21
Dyeing, Knecht and Rawson, 82
Rawson, Gardner, and
Dictionary of Dyes, 82
Laycock,
Textile Printing, Seymour Rothwell, 83
Textile Fibres of Commerce, W.I. Hannan, 83
Dyeing and Cleaning, G.H. Hurst, 84
Bleaching and Calico-Printing, Geo. Duerr, 84
A SHORT MANUAL OF INORGANIC CHEMISTRY.
BY A. DUPRÉ, Ph.D., F.R.S.,
AND
WILSON HAKE, Ph.D., F.I.C., F.C.S.,
Of the Westminster Hospital Medical School
Third Edition, Revised, Enlarged, and Re-issued. Price 6s. net.
"A well-written, clear and accurate Elementary Manual of Inorganic
Chemistry.... We agree heartily with the system adopted by Drs. Dupré and
Hake. Will Make Experimental Work trebly interesting because
intelligible."—Saturday Review.
"There is no question that, given the perfect grounding of the Student in his
Science, the remainder comes afterwards to him in a manner much more
simple and easily acquired. The work is an example of the advantages of
the Systematic Treatment of a Science over the fragmentary style so
generally followed. By a long way the best of the small Manuals for
Students."—Analyst.
Page 665
LABORATORY HANDBOOKS BY A. HUMBOLDT SEXTON,
Professor of Metallurgy in the Glasgow and West of Scotland Technical College.
OUTLINES OF QUANTITATIVE ANALYSIS.
FOR THE USE OF STUDENTS.
With Illustrations. Fourth Edition. Crown 8vo, Cloth, 3s.
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OUTLINES OF QUALITATIVE ANALYSIS.
FOR THE USE OF STUDENTS.
With Illustrations. Fourth Edition, Revised. Crown 8vo, Cloth, 3s. 6d.
"The work of a thoroughly practical chemist."—British Medical Journal.
"Compiled with great care, and will supply a want."—Journal of Education.
ELEMENTARY METALLURGY:
Including the Author's Practical Laboratory Course. With many Illustrations. [See p. 66.
Third Edition, Revised. Crown 8vo. Cloth, 6s.
Professor of Metallurgy in the Glasgow and West of Scotland Technical College.
OUTLINES OF QUANTITATIVE ANALYSIS.
FOR THE USE OF STUDENTS.
With Illustrations. Fourth Edition. Crown 8vo, Cloth, 3s.
"A compact laboratory guide for beginners was wanted, and the want has
been well supplied.... A good and useful book."—Lancet.
OUTLINES OF QUALITATIVE ANALYSIS.
FOR THE USE OF STUDENTS.
With Illustrations. Fourth Edition, Revised. Crown 8vo, Cloth, 3s. 6d.
"The work of a thoroughly practical chemist."—British Medical Journal.
"Compiled with great care, and will supply a want."—Journal of Education.
ELEMENTARY METALLURGY:
Including the Author's Practical Laboratory Course. With many Illustrations. [See p. 66.
Third Edition, Revised. Crown 8vo. Cloth, 6s.
Page 666
"Just the kind of work for students commencing the study of metallurgy."—
Practical Engineer.
CHEMISTRY FOR ENGINEERS AND MANUFACTURERS.
A PRACTICAL TEXT-BOOK.
BY
BERTRAM BLOUNT, F.I.C., F.C.S.,
Assoc.Inst.C.E., Consulting Chemist to the Crown Agents for the Colonies.
AND
A.G. BLOXAM, F.I.C., F.C.S.,
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VOLUME I. Price 10s. 6d.
CHEMISTRY OF ENGINEERING, BUILDING, AND
METALLURGY.
Practical Engineer.
CHEMISTRY FOR ENGINEERS AND MANUFACTURERS.
A PRACTICAL TEXT-BOOK.
BY
BERTRAM BLOUNT, F.I.C., F.C.S.,
Assoc.Inst.C.E., Consulting Chemist to the Crown Agents for the Colonies.
AND
A.G. BLOXAM, F.I.C., F.C.S.,
Consulting Chemist, Head of the Chemistry Department, Goldsmiths' Inst., New Cross.
In Two Vols., Large 8vo. With Illustrations. Sold Separately.
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CHEMISTRY OF ENGINEERING, BUILDING, AND
METALLURGY.
Page 667
General Content.—INTRODUCTION—Chemistry of the Chief Materials
of Construction—Sources of Energy—Chemistry of Steam-raising—
Chemistry of Lubrication and Lubricants—Metallurgical Processes used in
the Winning and Manufacture of Metals.
"Practical throughout ... an admirable text-book, useful not only to
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THE CHEMISTRY OF MANUFACTURING PROCESSES.
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Brewing and Distilling—Oils, Resins, and Varnishes—Soap and Candles—
Textiles and Bleaching—Colouring Matters, Dyeing, and Printing—Paper
and Pasteboard—Pigments and Paints—Leather, Glue, and Size—
Explosives and Matches—Minor Chemical Manufactures.
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"We confidently recommend this volume as a practical, and not
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Students, but to Engineers and Managers of works in preventing waste
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"Eminently practical."—Glasgow Herald.
"A book worthy of high rank ... its merit is great ... treatment of the subject
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VOLUME II. Price 16s.
THE CHEMISTRY OF MANUFACTURING PROCESSES.
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Brewing and Distilling—Oils, Resins, and Varnishes—Soap and Candles—
Textiles and Bleaching—Colouring Matters, Dyeing, and Printing—Paper
and Pasteboard—Pigments and Paints—Leather, Glue, and Size—
Explosives and Matches—Minor Chemical Manufactures.
"Certainly a good and useful book, constituting a practical guide for
students by affording a clear conception of the numerous processes as a
whole."—Chemical Trade Journal.
"We confidently recommend this volume as a practical, and not
overloaded, text-book, of great value to students."—The Builder.
Page 668
Just Out. Fifth Edition, Thoroughly Revised, Greatly Enlarged and Re-
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FOODS: THEIR COMPOSITION AND ANALYSIS.
By A. WYNTER BLYTH, M.R.C.S., F.I.C., F.C.S.,
Barrister-at-Law, Public Analyst for the County of Devon, and Medical Officer of Health for St. Marylebone.
And M. WYNTER BLYTH, B.A., B.Sc., F.C.S.
General Contents.—History of Adulteration.—Legislation.—Apparatus.
—"Ash."—Sugar.—Confectionery.—Honey.—Treacle.—Jams and
Preserved Fruits.—Starches.—Wheaten-Flour.—Bread.—Oats.—Barley.—
Rye.—Rice.—Maize.—Millet.—Potato.—Peas.—Lentils.—Beans.—Milk.
—Cream.—Butter.—Oleo-Margarine.—Cheese.—Lard.—Tea.—Coffee.—
Cocoa and Chocolate.—Alcohol.—Brandy.—Rum.—Whisky.—Gin.—
Arrack.—Liqueurs.—Absinthe.—Yeast.—-Beer.—Wine.—Vinegar.—
Lemon and Lime Juice.—Mustard.—Pepper.—Sweet and Bitter Almonds.
—Annatto.—Olive Oil.—Water Analysis.—Appendix: Adulteration Acts,
&c.
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Barrister-at-Law, Public Analyst for the County of Devon, and Medical Officer of Health for St. Marylebone.
Page 669
GENERAL CONTENTS.
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CHEMIST TO THE AYLESBURY DAIRY COMPANY.
Contents.—I. Introductory.—The Constituents of Milk. II. The Analysis of
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I.—Historical Introduction. II.—Classification—Statistics—Connection
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less Volatile Poisonous Substances. VI.—Alkaloids and Poisonous
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Appendix: Treatment, by Antidotes or otherwise, of Cases of Poisoning.
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By H. DROOP RICHMOND, F.C.S.,
CHEMIST TO THE AYLESBURY DAIRY COMPANY.
Contents.—I. Introductory.—The Constituents of Milk. II. The Analysis of
Milk. III. Normal Milk: its Adulterations and Alterations, and their
Page 670
Detection. IV. The Chemical Control of the Dairy. V. Biological and
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By C. AINSWORTH MITCHELL, B.A.(Oxon),
Fellow of the Institute of Chemistry; Member of Council, Society of Public Analysts.
With Numerous Tables, Illustrations, and a Coloured Plate.
Page 671
Contents.—Structure and Chemical Composition of Muscular Fibre.—of
Connective Tissue, and Blood.—The Flesh of Different Animals.—The
Examination of Flesh.—Methods of Examining Animal Fat.—The
Preservation of Flesh.—Composition and Analysis of Sausages.—Proteids
of Flesh.—Meat Extracts and Flesh Peptones.—The Cooking of Flesh.—
Poisonous Flesh.—The Animal Parasites of Flesh.—The Bacteriological
Examination of Flesh.—The Extraction and Separation of Ptomaines.—
Index.
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TECHNICAL MYCOLOGY: THE UTILISATION OF
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A Practical Handbook on Fermentation and Fermentative Processes for the Use of Brewers and
Distillers, Analysts, Technical and Agricultural Chemists, and all interested in the Industries
dependent on Fermentation.
By Dr. FRANZ LAFAR,
Professor of Fermentation-Physiology and Bacteriology in the Technical High School, Vienna.
Connective Tissue, and Blood.—The Flesh of Different Animals.—The
Examination of Flesh.—Methods of Examining Animal Fat.—The
Preservation of Flesh.—Composition and Analysis of Sausages.—Proteids
of Flesh.—Meat Extracts and Flesh Peptones.—The Cooking of Flesh.—
Poisonous Flesh.—The Animal Parasites of Flesh.—The Bacteriological
Examination of Flesh.—The Extraction and Separation of Ptomaines.—
Index.
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putrefactive changes, and poisonous or injurious constituents, together with
an account of their causes and effects.—Publishers' Note.
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TECHNICAL MYCOLOGY: THE UTILISATION OF
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A Practical Handbook on Fermentation and Fermentative Processes for the Use of Brewers and
Distillers, Analysts, Technical and Agricultural Chemists, and all interested in the Industries
dependent on Fermentation.
By Dr. FRANZ LAFAR,
Professor of Fermentation-Physiology and Bacteriology in the Technical High School, Vienna.
Page 672
With an Introduction by Dr. EMIL CHR. HANSEN, Principal of the
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Translated by CHARLES T.C. SALTER.
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FERMENTS AND THEIR ACTIONS.
A Text-book on the Chemistry and Physics of Fermentative Changes.
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Of the Physiological Institute at Eilangen.
Carlsberg Laboratory, Copenhagen.
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FERMENTS AND THEIR ACTIONS.
A Text-book on the Chemistry and Physics of Fermentative Changes.
By CARL OPPENHEIMER, Ph.D., M.D.,
Of the Physiological Institute at Eilangen.
Page 673
Translated from the German by C. AINSWORTH MITCHELL, B.A.,
F.I.C., F.C.S.
Abridged Contents.—Introduction.—Definition.—Chemical Nature of
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Physiological Action.—Secretion.—Importance of Ferments to Vital
Action.—Proteolytic Ferments.—Trypsin.—Bacteriolytic and Hæmolytic
Ferments.—Vegetable Ferments.—Coagulating Ferments.—Saccharifying
Ferments.—Diastases.—Polysaccharides.—Enzymes.—Ferments which
decompose Glucosides.—Hydrolytic Ferments.—Lactic Acid Fermentation.
—Alcoholic Fermentation.—Biology of Alcoholic Fermentation.—
Oxydases.—Oxidising Fermentation.—Bibliography.—Index.
The present Translation embodies Notes and Additions to the Work
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THE PRINCIPLES AND PRACTICE OF BREWING.
FOR THE USE OF STUDENTS AND PRACTICAL MEN.
BY
WALTER J. SYKES, M.D., D.P.H., F.I.C.,
EDITOR OF "THE ANALYST."
ABSTRACT OF CONTENTS.
F.I.C., F.C.S.
Abridged Contents.—Introduction.—Definition.—Chemical Nature of
Ferments.—Influence of External Factors.—Mode of Action.—
Physiological Action.—Secretion.—Importance of Ferments to Vital
Action.—Proteolytic Ferments.—Trypsin.—Bacteriolytic and Hæmolytic
Ferments.—Vegetable Ferments.—Coagulating Ferments.—Saccharifying
Ferments.—Diastases.—Polysaccharides.—Enzymes.—Ferments which
decompose Glucosides.—Hydrolytic Ferments.—Lactic Acid Fermentation.
—Alcoholic Fermentation.—Biology of Alcoholic Fermentation.—
Oxydases.—Oxidising Fermentation.—Bibliography.—Index.
The present Translation embodies Notes and Additions to the Work
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THE PRINCIPLES AND PRACTICE OF BREWING.
FOR THE USE OF STUDENTS AND PRACTICAL MEN.
BY
WALTER J. SYKES, M.D., D.P.H., F.I.C.,
EDITOR OF "THE ANALYST."
ABSTRACT OF CONTENTS.
Page 674
I. Physical Principles involved in Brewing Operations.
Chemistry with special reference to the materials used in Brewing.
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Vegetable Biology.
Fermentation.
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Barley and Malting.
Brewery Plant.
Brewing.
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Appendices.
Index.
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Page 675
AGRICULTURAL CHEMISTRY AND ANALYSIS:
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A PRACTICAL HANDBOOK FOR THE USE OF AGRICULTURAL STUDENTS.
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Page 676
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Page 677
CALCAREOUS CEMENTS: THEIR NATURE,
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THE CHEMISTRY OF GAS MANUFACTURE:
Page 678
A Hand-Book on the Production, Purification, and Testing of Illuminating Gas, and the Assay of
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Pipes.—Subsidiary Apparatus.—Burners.—Incandescent Burners.—
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Page 679
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PRACTICAL SANITATION: A HAND-BOOK FOR
SANITARY INSPECTORS AND OTHERS INTERESTED IN
SANITATION.
By GEORGE REID, M.D., D.P.H.,
Fellow, Mem. Council, and Examiner, Sanitary Institute of Great Britain, and Medical Officer to the Staffordshire County
Council.
With an Appendix on Sanitary Law.
Lamps.—Valuation and Analysis of Carbide.
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FIRE AND EXPLOSION RISKS.
A Handbook of the Detection, Investigation, and Prevention of Fires and Explosion.
By Dr. VON SCHWARTZ.
Translated from the Revised German Edition By C.T.C. SALTER.
Abridged General Contents.—Fires and Explosions of a General
Character.—Dangers arising from Sources of Light and Heat.—Dangerous
Gases.—Risks Attending Special Industries.—Materials Employed.—
Agricultural Products.—Fats, Oils, and Resins.—Mineral Oils and Tar.—
Alcohol, &c.—Metals, Oxides, Acids, &c.—Lightning, Ignition
Appliances, Fireworks.
Tenth Edition, Revised. Price 6s.
PRACTICAL SANITATION: A HAND-BOOK FOR
SANITARY INSPECTORS AND OTHERS INTERESTED IN
SANITATION.
By GEORGE REID, M.D., D.P.H.,
Fellow, Mem. Council, and Examiner, Sanitary Institute of Great Britain, and Medical Officer to the Staffordshire County
Council.
With an Appendix on Sanitary Law.
Page 680
By HERBERT MANLEY, M.A., M.B., D.P.H.,
Medical Officer of Health for the County Borough of West Bromwich.
General Contents.—Introduction—Water Supply: Drinking Water,
Pollution of Water—Ventilation and Warming—Principles of Sewage
Removal—Details of Drainage; Refuse Removal and Disposal—Sanitary
and Insanitary Work and Appliances—Details of Plumbers' Work—House
Construction—Infection and Disinfection—Food, Inspection of;
Characteristics of Good Meat; Meat, Milk, Fish, &c., unfit for Human Food
—Appendix: Sanitary Law; Model Bye-Laws, &c.
"Dr. Reid's very useful Manual ... abounds in practical detail."—British
Medical Journal.
"A very useful Handbook, with a very useful Appendix. We recommend it
not only to Sanitary Inspectors, but to Householders and all interested in
Sanitary matters."—Sanitary Record.
COMPANION VOLUME TO REID'S SANITATION.
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Sanitary Engineering: A Practical Manual of Town Drainage
and Sewage and Refuse Disposal.
For Sanitary Authorities, Engineers, Inspectors, Architects, Contractors, and Students.
BY
FRANCIS WOOD, A.M.Inst.C.E., F.G.S.,
Borough Engineer and Surveyor, Fulham; late Borough Engineer, Bacup, Lancs.
GENERAL CONTENTS.
Medical Officer of Health for the County Borough of West Bromwich.
General Contents.—Introduction—Water Supply: Drinking Water,
Pollution of Water—Ventilation and Warming—Principles of Sewage
Removal—Details of Drainage; Refuse Removal and Disposal—Sanitary
and Insanitary Work and Appliances—Details of Plumbers' Work—House
Construction—Infection and Disinfection—Food, Inspection of;
Characteristics of Good Meat; Meat, Milk, Fish, &c., unfit for Human Food
—Appendix: Sanitary Law; Model Bye-Laws, &c.
"Dr. Reid's very useful Manual ... abounds in practical detail."—British
Medical Journal.
"A very useful Handbook, with a very useful Appendix. We recommend it
not only to Sanitary Inspectors, but to Householders and all interested in
Sanitary matters."—Sanitary Record.
COMPANION VOLUME TO REID'S SANITATION.
In Crown 8vo. Handsome Cloth. Profusely Illustrated. 8s. 6d. net.
Sanitary Engineering: A Practical Manual of Town Drainage
and Sewage and Refuse Disposal.
For Sanitary Authorities, Engineers, Inspectors, Architects, Contractors, and Students.
BY
FRANCIS WOOD, A.M.Inst.C.E., F.G.S.,
Borough Engineer and Surveyor, Fulham; late Borough Engineer, Bacup, Lancs.
GENERAL CONTENTS.
Page 681
Introduction.—Hydraulics.—Velocity of Water in Pipes.—Earth Pressures
and Retaining Walls.—Powers.—House Drainage.—Land Drainage.—
Sewers.—Separate System.—Sewage Pumping.—Sewer Ventilation.—
Drainage Areas.—Sewers, Manholes, &c.—Trade Refuse.—Sewage
Disposal Works.—Bacteriolysis.—Sludge Disposal.—Construction and
Cleansing of Sewers.—Refuse Disposal.—Chimneys and Foundations.
"The volume bristles with information which will be greedily read by those
in need of assistance. The book is one that ought to be on the bookshelves
of every practical engineer."—Sanitary Journal.
"A veritable pocket compendium of Sanitary Engineering.... A work which
may, in many respects, be considered as complete ... commendably cautious
... interesting ... suggestive."—Public Health Engineer.
Vol. I. Now Ready. in Half Morocco, 24s.
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PHYSICO-CHEMICAL TABLES
FOR THE USE OF ANALYSTS, PHYSICISTS, CHEMICAL MANUFACTURERS, AND
SCIENTIFIC CHEMISTS.
Volume I.—Chemical Engineering, Physical Chemistry. [Just Out.
Volume II.—Chemical Physics, Pure and Analytical Chemistry.
By JOHN CASTELL-EVANS, F.I.C., F.C.S., Superintendent of the
Chemical Laboratories, and Lecturer on Inorganic Chemistry and
Metallurgy at the Finsbury Technical College.
The Tables may almost claim to be exhaustive, and embody and collate all
the most recent data established by experimentalists at home and abroad.
The volumes will be found invaluable to all engaged in research and
experimental investigation in Chemistry and Physics.
and Retaining Walls.—Powers.—House Drainage.—Land Drainage.—
Sewers.—Separate System.—Sewage Pumping.—Sewer Ventilation.—
Drainage Areas.—Sewers, Manholes, &c.—Trade Refuse.—Sewage
Disposal Works.—Bacteriolysis.—Sludge Disposal.—Construction and
Cleansing of Sewers.—Refuse Disposal.—Chimneys and Foundations.
"The volume bristles with information which will be greedily read by those
in need of assistance. The book is one that ought to be on the bookshelves
of every practical engineer."—Sanitary Journal.
"A veritable pocket compendium of Sanitary Engineering.... A work which
may, in many respects, be considered as complete ... commendably cautious
... interesting ... suggestive."—Public Health Engineer.
Vol. I. Now Ready. in Half Morocco, 24s.
In Two Volumes, each complete in itself.
PHYSICO-CHEMICAL TABLES
FOR THE USE OF ANALYSTS, PHYSICISTS, CHEMICAL MANUFACTURERS, AND
SCIENTIFIC CHEMISTS.
Volume I.—Chemical Engineering, Physical Chemistry. [Just Out.
Volume II.—Chemical Physics, Pure and Analytical Chemistry.
By JOHN CASTELL-EVANS, F.I.C., F.C.S., Superintendent of the
Chemical Laboratories, and Lecturer on Inorganic Chemistry and
Metallurgy at the Finsbury Technical College.
The Tables may almost claim to be exhaustive, and embody and collate all
the most recent data established by experimentalists at home and abroad.
The volumes will be found invaluable to all engaged in research and
experimental investigation in Chemistry and Physics.
Page 682
The Work comprehends as far as possible all rulles and tables required
by the Analyst, Brewer, Distiller, Acid- and Alkali-Manufacturer, &c., &c.;
and also the principal data in Thermo-chemistry, Electro-chemistry, and
the various branches of Chemical Physics. Every possible care has been
taken to ensure perfect accuracy, and to include the results of the most
recent investigations.
In Large 8vo. Handsome Cloth. Beautifully Illustrated. With Plates and
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Road Making and Maintenance:
A PRACTICAL TREATISE FOR ENGINEERS, SURVEYORS, AND OTHERS.
With an Historical Sketch of Ancient and Modern Practice.
By THOS. AITKEN, Assoc.M.Inst.C.E.,
Member of the Association of Municipal and County Engineers; Member of the Sanitary Inst.; Surveyor to the County
Council of Fife, Cupar Division.
WITH NUMEROUS PLATES, DIAGRAMS, AND ILLUSTRATIONS.
Contents.—Historical Sketch.—Resistance of Traction.—Laying out New
Roads.—Earthworks, Drainage, and Retaining Walls.—Road Materials, or
Metal.—Quarrying.—Stone Breaking and Haulage.—Road-Rolling and
Scarifying.—The Construction of New, and the Maintenance of existing
Roads.—Carriage Ways and Foot Ways.
"The Literary style is excellent ... A comprehensive and excellent Modern
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by the Analyst, Brewer, Distiller, Acid- and Alkali-Manufacturer, &c., &c.;
and also the principal data in Thermo-chemistry, Electro-chemistry, and
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taken to ensure perfect accuracy, and to include the results of the most
recent investigations.
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Road Making and Maintenance:
A PRACTICAL TREATISE FOR ENGINEERS, SURVEYORS, AND OTHERS.
With an Historical Sketch of Ancient and Modern Practice.
By THOS. AITKEN, Assoc.M.Inst.C.E.,
Member of the Association of Municipal and County Engineers; Member of the Sanitary Inst.; Surveyor to the County
Council of Fife, Cupar Division.
WITH NUMEROUS PLATES, DIAGRAMS, AND ILLUSTRATIONS.
Contents.—Historical Sketch.—Resistance of Traction.—Laying out New
Roads.—Earthworks, Drainage, and Retaining Walls.—Road Materials, or
Metal.—Quarrying.—Stone Breaking and Haulage.—Road-Rolling and
Scarifying.—The Construction of New, and the Maintenance of existing
Roads.—Carriage Ways and Foot Ways.
"The Literary style is excellent ... A comprehensive and excellent Modern
Book, an up-to-date work ... Should be on the reference shelf of every
Municipal and County Engineer or Surveyor in the United Kingdom, and of
every Colonial Engineer."—The Surveyor.
Page 683
Third Edition, Revised and Enlarged. With Illustrations, 12s. 6d.
Painters' Colours, Oils, & Varnishes:
A PRACTICAL MANUAL.
By GEORGE H. HURST, F.C.S.,
Member of the Society of Chemical Industry; Lecturer on the Technology of Painters' Colours, Oils, and Varnishes, the
Municipal Technical School, Manchester.
General Contents.—Introductory—The Composition, Manufacture,
Assay, and Analysis of Pigments, White, Red, Yellow and Orange, Green,
Blue, Brown, and Black—Lakes—Colour and Paint Machinery—Paint
Vehicles (Oils, Turpentine, &c., &c.)—Driers—Varnishes.
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*** For Mr. Hurst's Garment Dyeing and Cleaning, see p. 84.
In Crown 8vo. Handsome Cloth. With Illustrations. 5s.
THE PAINTER'S LABORATORY GUIDE.
A Student's Handbook of Paints, Colours, and Varnishes.
By GEORGE H. HURST, F.C.S., M.S.C.I.
Abstract of Contents.—Preparation of Pigment Colours.—Chemical
Principles Involved.—Oils and Varnishes.—Properties of Oils and
Varnishes.—Tests and Experiments.—Plants, Methods, and Machinery of
the Paint and Varnish Manufactures.
Painters' Colours, Oils, & Varnishes:
A PRACTICAL MANUAL.
By GEORGE H. HURST, F.C.S.,
Member of the Society of Chemical Industry; Lecturer on the Technology of Painters' Colours, Oils, and Varnishes, the
Municipal Technical School, Manchester.
General Contents.—Introductory—The Composition, Manufacture,
Assay, and Analysis of Pigments, White, Red, Yellow and Orange, Green,
Blue, Brown, and Black—Lakes—Colour and Paint Machinery—Paint
Vehicles (Oils, Turpentine, &c., &c.)—Driers—Varnishes.
"A thoroughly practical book, ... the only English work that satisfactorily
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In Crown 8vo. Handsome Cloth. With Illustrations. 5s.
THE PAINTER'S LABORATORY GUIDE.
A Student's Handbook of Paints, Colours, and Varnishes.
By GEORGE H. HURST, F.C.S., M.S.C.I.
Abstract of Contents.—Preparation of Pigment Colours.—Chemical
Principles Involved.—Oils and Varnishes.—Properties of Oils and
Varnishes.—Tests and Experiments.—Plants, Methods, and Machinery of
the Paint and Varnish Manufactures.
Page 684
This Work has been designed by the Author for the Laboratory of the
Technical School, and of the Paint and Colour Works, and for all interested
or engaged in these industries.
Second Edition, Revised. In Crown 8vo. extra. With Numerous Illustrations
and Plates (some in Colours), including Original Designs. 12s. 6d.
Painting and Decorating:
A Complete Practical Manual for House Painters and Decorators.
By WALTER JOHN PEARCE,
LECTURER AT THE MANCHESTER TECHNICAL SCHOOL FOR HOUSE-PAINTING AND DECORATING.
GENERAL CONTENTS.
Introduction—Workshop and Stores—Plant and Appliances—Brushes and
Tools—Materials: Pigments, Driers, Painters' Oils—Wall Hangings—Paper
Hanging—Colour Mixing—Distempering—Plain Painting—Staining—
Varnish and Varnishing—Imitative Painting—Graining—Marbling—
Gilding—Sign-Writing and Lettering—Decoration: General Principles—
Decoration in Distemper—Painted Decoration—Relievo Decoration—
Colour—Measuring and Estimating—Coach-Painting—Ship-Painting.
"A thoroughly useful book ... good, sound, practical information in a
clear and concise form."—Plumber and Decorator.
"A thoroughly good and reliable text-book.... So full and complete that
it would be difficult to imagine how anything further could be added about
the Painter's craft."—Builders' Journal.
Technical School, and of the Paint and Colour Works, and for all interested
or engaged in these industries.
Second Edition, Revised. In Crown 8vo. extra. With Numerous Illustrations
and Plates (some in Colours), including Original Designs. 12s. 6d.
Painting and Decorating:
A Complete Practical Manual for House Painters and Decorators.
By WALTER JOHN PEARCE,
LECTURER AT THE MANCHESTER TECHNICAL SCHOOL FOR HOUSE-PAINTING AND DECORATING.
GENERAL CONTENTS.
Introduction—Workshop and Stores—Plant and Appliances—Brushes and
Tools—Materials: Pigments, Driers, Painters' Oils—Wall Hangings—Paper
Hanging—Colour Mixing—Distempering—Plain Painting—Staining—
Varnish and Varnishing—Imitative Painting—Graining—Marbling—
Gilding—Sign-Writing and Lettering—Decoration: General Principles—
Decoration in Distemper—Painted Decoration—Relievo Decoration—
Colour—Measuring and Estimating—Coach-Painting—Ship-Painting.
"A thoroughly useful book ... good, sound, practical information in a
clear and concise form."—Plumber and Decorator.
"A thoroughly good and reliable text-book.... So full and complete that
it would be difficult to imagine how anything further could be added about
the Painter's craft."—Builders' Journal.
Page 685
In Large 8vo. Handsome Cloth. With 4 Plates and Several Illustrations. 16s.
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THE CHEMISTRY OF INDIA RUBBER.
A Treatise on the Nature of India Rubber, its Chemical and Physical Examination, and the
Determination and Valuation of India Rubber Substitutes.
Including the Outlines of a Theory on Vulcanisation.
BY
CARL OTTO WEBER, Ph.D.
Abstract of Contents.—Introduction.—The Chemistry of India Rubber.—
The Examination and Valuation of India Rubber.—Examination of India
Rubber Substitutes.—Inorganic Filling Materials.—Vulcanisers and
Sulphur Carriers.—India Rubber Solvents.—Colouring Matters and
Pigment Colours.—Constructive Components of India Rubber Articles.—
Analysis of Manufactured India Rubber.—Sanitary Conditions in India
Rubber Works.—Index.
"Replete with scientific and also with technical interest.... The sub-section
on the physical properties is a complete résumé of every thing known to-
day on the subject."—India-rubber Journal.
New Edition. In Large 8vo. Handsome Cloth. With 144 Illustrations.
OILS, FATS, BUTTERS & WAXES:
THEIR PREPARATION AND PROPERTIES, AND MANUFACTURE THEREFROM OF
CANDLES, SOAPS, AND OTHER PRODUCTS.
BY
net.
THE CHEMISTRY OF INDIA RUBBER.
A Treatise on the Nature of India Rubber, its Chemical and Physical Examination, and the
Determination and Valuation of India Rubber Substitutes.
Including the Outlines of a Theory on Vulcanisation.
BY
CARL OTTO WEBER, Ph.D.
Abstract of Contents.—Introduction.—The Chemistry of India Rubber.—
The Examination and Valuation of India Rubber.—Examination of India
Rubber Substitutes.—Inorganic Filling Materials.—Vulcanisers and
Sulphur Carriers.—India Rubber Solvents.—Colouring Matters and
Pigment Colours.—Constructive Components of India Rubber Articles.—
Analysis of Manufactured India Rubber.—Sanitary Conditions in India
Rubber Works.—Index.
"Replete with scientific and also with technical interest.... The sub-section
on the physical properties is a complete résumé of every thing known to-
day on the subject."—India-rubber Journal.
New Edition. In Large 8vo. Handsome Cloth. With 144 Illustrations.
OILS, FATS, BUTTERS & WAXES:
THEIR PREPARATION AND PROPERTIES, AND MANUFACTURE THEREFROM OF
CANDLES, SOAPS, AND OTHER PRODUCTS.
BY
Page 686
C.R. ALDER WRIGHT, D.Sc., F.R.S.,
Late Lecturer on Chemistry, St. Mary's Hospital Medical School; Examiner in "Soap" to the City and Guilds of London
Institute.
Thoroughly Revised, Enlarged, and in Part Rewritten
By C. AINSWORTH MITCHELL, B.A., F.I.C.
"Dr. Wright's work will be found absolutely indispensable by every
Chemist. Teems with information valuable alike to the Analyst and the
Technical Chemist."—The Analyst.
"Will rank as the Standard English Authority on Oils and Fats for many
years to come."—Industries and Iron.
THE TEXTILE INDUSTRIES.
In Two Large Volumes, 920 pp., with a Supplementary Volume, containing
Specimens of Dyed Fabrics. 45s.
A MANUAL OF DYEING:
FOR THE USE OF PRACTICAL DYERS, MANUFACTURERS, STUDENTS, AND ALL
INTERESTED IN THE ART OF DYEING.
BY
E. KNECHT, Ph.D., F.I.C.,
Head of the Chemistry and Dyeing Department of the Technical College, Manchester; Editor of "The Journal of the
Society of Dyers and Colourists;"
Late Lecturer on Chemistry, St. Mary's Hospital Medical School; Examiner in "Soap" to the City and Guilds of London
Institute.
Thoroughly Revised, Enlarged, and in Part Rewritten
By C. AINSWORTH MITCHELL, B.A., F.I.C.
"Dr. Wright's work will be found absolutely indispensable by every
Chemist. Teems with information valuable alike to the Analyst and the
Technical Chemist."—The Analyst.
"Will rank as the Standard English Authority on Oils and Fats for many
years to come."—Industries and Iron.
THE TEXTILE INDUSTRIES.
In Two Large Volumes, 920 pp., with a Supplementary Volume, containing
Specimens of Dyed Fabrics. 45s.
A MANUAL OF DYEING:
FOR THE USE OF PRACTICAL DYERS, MANUFACTURERS, STUDENTS, AND ALL
INTERESTED IN THE ART OF DYEING.
BY
E. KNECHT, Ph.D., F.I.C.,
Head of the Chemistry and Dyeing Department of the Technical College, Manchester; Editor of "The Journal of the
Society of Dyers and Colourists;"
Page 687
CHR. RAWSON, F.I.C., F.C.S.,
Late Head of the Chemistry and Dyeing Department of the Technical College, Bradford; Member of Council of the Society
of Dyers and Colourists;
And RICHARD LOEWENTHAL, Ph.D.
General Contents.—Chemical Technology of the Textile Fabrics—Water
—Washing and Bleaching—Acids, Alkalies, Mordants—Natural Colouring
Matters—Artificial Organic Colouring Matters—Mineral Colours—
Machinery used in Dyeing—Tinctorial Properties of Colouring Matters—
Analysis and Valuation of Materials used in Dyeing, &c., &c.
"The most valuable and useful work on Dyeing that has yet appeared in
the English language ... likely to be the Standard Work of Reference for
years to come."—Textile Mercury.
"This authoritative and exhaustive work ... the most complete we have yet
seen on the subject."—Textile Manufacturer.
"The most exhaustive and complete work on the subject extant."—Textile
Recorder.
Companion Volume to Knecht & Rawson's "Dyeing." In Large 8vo.
Handsome Cloth, Library Style. 16s. net.
A DICTIONARY OF DYES, MORDANTS, & OTHER
COMPOUNDS USED IN DYEING AND CALICO
PRINTING.
With Formulæ, Properties, and Applications of the various substances described, and concise
directions for their Commercial Valuation. and for the Detection of Adulterants.
Late Head of the Chemistry and Dyeing Department of the Technical College, Bradford; Member of Council of the Society
of Dyers and Colourists;
And RICHARD LOEWENTHAL, Ph.D.
General Contents.—Chemical Technology of the Textile Fabrics—Water
—Washing and Bleaching—Acids, Alkalies, Mordants—Natural Colouring
Matters—Artificial Organic Colouring Matters—Mineral Colours—
Machinery used in Dyeing—Tinctorial Properties of Colouring Matters—
Analysis and Valuation of Materials used in Dyeing, &c., &c.
"The most valuable and useful work on Dyeing that has yet appeared in
the English language ... likely to be the Standard Work of Reference for
years to come."—Textile Mercury.
"This authoritative and exhaustive work ... the most complete we have yet
seen on the subject."—Textile Manufacturer.
"The most exhaustive and complete work on the subject extant."—Textile
Recorder.
Companion Volume to Knecht & Rawson's "Dyeing." In Large 8vo.
Handsome Cloth, Library Style. 16s. net.
A DICTIONARY OF DYES, MORDANTS, & OTHER
COMPOUNDS USED IN DYEING AND CALICO
PRINTING.
With Formulæ, Properties, and Applications of the various substances described, and concise
directions for their Commercial Valuation. and for the Detection of Adulterants.
Page 688
By CHRISTOPHER RAWSON, F.I.C., F.C.S.,
Consulting Chemist to the Behar Indigo Planters' Association: Co-Author of "A Manual of Dyeing;"
WALTER M. GARDNER, F.C.S.,
Head of the Department of Chemistry and Dyeing, Bradford Municipal Technical College; Editor of the "Journ. Soc.
Dyers and Colourists;"
And W.F. LAYCOCK, Ph.D., F.C.S.,
Analytical and Consulting Chemist.
"Turn to the book as one may on any subject, or any substance in
connection with the trade, and a reference is sure to be found. The authors
have apparently left nothing out. Considering the immense amount of
information, the book is a cheap one, and we trust it will be widely
appreciated,"—Textile Mercury.
In Large 8vo, Handsome Cloth, with Numerous Illustrations. 9s. net.
TEXTILE FIBRES OF COMMERCE.
A HANDBOOK OF The Occurrence, Distribution, Preparation, and Industrial Uses of the
Animal, Vegetable, and Mineral Products used in Spinning and Weaving.
By WILLIAM I. HANNAN,
Lecturer on Botany at the Ashton Municipal Technical School, Lecturer on Cotton Spinning at the Chorley Science and
Art School, &c.
With Numerous Photo Engravings from Nature.
*** The subjects discussed in this volume are, in order to facilitate
reference, arranged in alphabetical order under their respective heads. The
work may thus be regarded as a Dictionary of Textile Fibres. A feature of
Consulting Chemist to the Behar Indigo Planters' Association: Co-Author of "A Manual of Dyeing;"
WALTER M. GARDNER, F.C.S.,
Head of the Department of Chemistry and Dyeing, Bradford Municipal Technical College; Editor of the "Journ. Soc.
Dyers and Colourists;"
And W.F. LAYCOCK, Ph.D., F.C.S.,
Analytical and Consulting Chemist.
"Turn to the book as one may on any subject, or any substance in
connection with the trade, and a reference is sure to be found. The authors
have apparently left nothing out. Considering the immense amount of
information, the book is a cheap one, and we trust it will be widely
appreciated,"—Textile Mercury.
In Large 8vo, Handsome Cloth, with Numerous Illustrations. 9s. net.
TEXTILE FIBRES OF COMMERCE.
A HANDBOOK OF The Occurrence, Distribution, Preparation, and Industrial Uses of the
Animal, Vegetable, and Mineral Products used in Spinning and Weaving.
By WILLIAM I. HANNAN,
Lecturer on Botany at the Ashton Municipal Technical School, Lecturer on Cotton Spinning at the Chorley Science and
Art School, &c.
With Numerous Photo Engravings from Nature.
*** The subjects discussed in this volume are, in order to facilitate
reference, arranged in alphabetical order under their respective heads. The
work may thus be regarded as a Dictionary of Textile Fibres. A feature of
Page 689
the work is the wealth of botanical description which accompanies the
Section dealing with Vegetable Fibres.—Publishers' Note.
"Useful Information.... Admirable Illustrations.... The information is not
easily attainable, and in its present convenient form will be valuable."—
Textile Recorder.
TEXTILE PRINTING: A PRACTICAL MANUAL.
Including the Processes Used in the Printing of COTTON, WOOLLEN, SILK, and HALF-
SILK FABRICS.
By C.F. SEYMOUR ROTHWELL, F.C.S.,
Mem. Soc. of Chemical Industries; late Lecturer at the Municipal Technical School, Manchester.
In Large 8vo, with Illustrations and Printed Patterns. Price 21s.
General Contents.—Introduction.—The Machinery Used in Textile
Printing.—Thickeners and Mordants.—The Printing of Cotton Goods.—
The Steam Style.—Colours Produced Directly on the Fibre.—Dyed Styles.
—Padding Style.—Resist and Discharge Styles.—The Printing of
Compound Colourings, &c.—The Printing of Woollen Goods.—The
Printing of Silk Goods.—Practical Recipes for Printing.—Appendix.—
Useful Tables.—Patterns.
"By far the best and most practical book on textile printing which has
yet been brought out, and will long remain the standard work on the subject.
It is essentially practical in character."—Textile Mercury.
"The most practical manual of textile printing which has yet appeared.
We have no hesitation in recommending it."—The Textile Manufacturer.
Section dealing with Vegetable Fibres.—Publishers' Note.
"Useful Information.... Admirable Illustrations.... The information is not
easily attainable, and in its present convenient form will be valuable."—
Textile Recorder.
TEXTILE PRINTING: A PRACTICAL MANUAL.
Including the Processes Used in the Printing of COTTON, WOOLLEN, SILK, and HALF-
SILK FABRICS.
By C.F. SEYMOUR ROTHWELL, F.C.S.,
Mem. Soc. of Chemical Industries; late Lecturer at the Municipal Technical School, Manchester.
In Large 8vo, with Illustrations and Printed Patterns. Price 21s.
General Contents.—Introduction.—The Machinery Used in Textile
Printing.—Thickeners and Mordants.—The Printing of Cotton Goods.—
The Steam Style.—Colours Produced Directly on the Fibre.—Dyed Styles.
—Padding Style.—Resist and Discharge Styles.—The Printing of
Compound Colourings, &c.—The Printing of Woollen Goods.—The
Printing of Silk Goods.—Practical Recipes for Printing.—Appendix.—
Useful Tables.—Patterns.
"By far the best and most practical book on textile printing which has
yet been brought out, and will long remain the standard work on the subject.
It is essentially practical in character."—Textile Mercury.
"The most practical manual of textile printing which has yet appeared.
We have no hesitation in recommending it."—The Textile Manufacturer.
Page 690
Large 8vo. Handsome Cloth. 12s. 6d.
BLEACHING & CALICO-PRINTING.
A Short Manual for Students and Practical Men.
By GEORGE DUERR,
Director of the Bleaching, Dyeing, and Printing Department at the Accrington and Bacup Technical Schools; Chemist and
Colourist at the Irwell Print Works.
Assisted by WILLIAM TURNBULL (of Turnbull & Stockdale,
Limited).
With Illustrations and upwards of One Hundred Dyed and Printed Patterns
designed specially to show various Stages of the Processes described.
GENERAL CONTENTS.—Cotton, Composition of; Bleaching, New
Processes; Printing, Hand-Block; Flat-Press Work; Machine Printing—
Mordants—Styles of Calico-Printing: The Dyed or Madder Style, Resist
Padded Style, Discharge and Extract Style, Chromed or Raised Colours,
Insoluble Colours, &c.—Thickeners—Natural Organic Colouring Matters
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Colours—Coal Tar Colours—Dyeing—Water, Softening of—Theory of
Colours—Weights and Measures, &c.
"When a ready way out of a difficulty is wanted, it is in books like this that
it is found."—Textile Recorder.
"Mr. Duerr's work will be found most useful.... The information given is of
great value.... The Recipes are thoroughly practical."—Textile
Manufacturer.
Second Edition. Revised and Enlarged. With Numerous Illustrations. 4s. 6d.
GARMENT DYEING AND CLEANING.
BLEACHING & CALICO-PRINTING.
A Short Manual for Students and Practical Men.
By GEORGE DUERR,
Director of the Bleaching, Dyeing, and Printing Department at the Accrington and Bacup Technical Schools; Chemist and
Colourist at the Irwell Print Works.
Assisted by WILLIAM TURNBULL (of Turnbull & Stockdale,
Limited).
With Illustrations and upwards of One Hundred Dyed and Printed Patterns
designed specially to show various Stages of the Processes described.
GENERAL CONTENTS.—Cotton, Composition of; Bleaching, New
Processes; Printing, Hand-Block; Flat-Press Work; Machine Printing—
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Insoluble Colours, &c.—Thickeners—Natural Organic Colouring Matters
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GARMENT DYEING AND CLEANING.
Page 691
A Practical Book for Practical Men.
By GEORGE H. HURST, F.C.S.,
Member of the Society of Chemical Industry.
General Contents.—Technology of the Textile Fibres—Garment Cleaning
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Fabrics—Scouring and Dyeing of Skin Rugs and Mats—Cleaning and
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Dyeing—Glossary of Drugs and Chemicals—Useful Tables.
"An up-to-date hand book has long been wanted, and Mr. Hurst has done
nothing more complete than this. An important work, the more so that
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Illustrated by Drawings from Nature by S. Rosamond Praeger, and Photographs by R. Welch.
By GEORGE H. HURST, F.C.S.,
Member of the Society of Chemical Industry.
General Contents.—Technology of the Textile Fibres—Garment Cleaning
—Dyeing of Textile Fabrics—Bleaching—Finishing of Dyed and Cleaned
Fabrics—Scouring and Dyeing of Skin Rugs and Mats—Cleaning and
Dyeing of Feathers—Glove Cleaning and Dyeing—Straw Bleaching and
Dyeing—Glossary of Drugs and Chemicals—Useful Tables.
"An up-to-date hand book has long been wanted, and Mr. Hurst has done
nothing more complete than this. An important work, the more so that
several of the branches of the craft here treated upon are almost entirely
without English Manuals for the guidance of workers. The price brings it
within the reach of all."—Dyer and Calico-Printer.
"Mr. Hurst's work decidedly fills a want ... ought to be in the hands of
every GARMENT DYER and cleaner in the Kingdom"—Textile Mercury.
"Boys could not have a more alluring introduction to scientific pursuits
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By R. LLOYD PRAEGER, B.A., M.R.I.A.
Illustrated by Drawings from Nature by S. Rosamond Praeger, and Photographs by R. Welch.
Page 692
General Contents.—A Daisy-Starred Pasture—Under the Hawthorns—By
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"The fascinating 'Open-Air Studies' of Prof. Cole give the Subject a glow
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the River—Along the Shingle—A Fragrant Hedgerow—A Connemara Bog
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Study in Weeds)—In the Home of the Alpines—A City Rubbish-Heap—
Glossary.
"A fresh and stimulating book ... should take a high place.... The
Illustrations are drawn with much skill."—The Times.
"Beautifully illustrated.... One of the most accurate as well as
interesting books of the kind we have seen."—Athenæum.
"Redolent with the scent of woodland and meadow."—The Standard.
With 12 Full-Page Illustrations from Photographs. Cloth. Second Edition,
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OPEN-AIR STUDIES IN GEOLOGY: An Introduction to
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By GRENVILLE A.J. COLE, F.G.S., M.R.I.A.,
Professor of Geology in the Royal College of Science for Ireland, and Examiner in the University of London.
General Contents.—The Materials of the Earth—A Mountain Hollow—
Down the Valley—Along the Shore—Across the Plains—Dead Volcanoes
—A Granite Highland—The Annals of the Earth—The Surrey Hills—The
Folds of the Mountains.
"The fascinating 'Open-Air Studies' of Prof. Cole give the Subject a glow
animation ... cannot fail to arouse keen interest in geology."—Geological
Magazine.
"A charming book, beautifully illustrated."—Athenæum.
Page 693
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Page 694
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time one of the most generally useful works for the library or the desk."—
The Times.
"British Societies are now well represented in the 'Year-Book of the
Scientific and Learned Societies of Great Britain and Ireland'"—(Art.
"Societies" in New Edition of "Encyclopædia Britannica," vol. xxii.)
Page 695
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all our great Scientific Centres, Museums, and Libraries throughout the
Kingdom, and has become an indispensable book of reference to every one
engaged in Scientific Work.
READY IN OCTOBER EACH YEAR.
Griffin's Metallurgical Series.
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INTRODUCTION TO THE STUDY OF METALLURGY. By Sir W.C.
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Fourth Edition, Thoroughly Revised and Enlarged. 21s. THE
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Royal Mint. Including the most recent Improvements in the Cyanide
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In Two Volumes, each complete in itself.
THE METALLURGY OF LEAD AND SILVER. By H.F. Collins,
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and Desilverisation, and the Assay and Analysis of the Materials Involved.
16s. Part II.—SILVER. Sources and Treatment of Ores, with Descriptions
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Page 696
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GETTING GOLD. A Practical Treatise for Prospectors and Miners. By
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German Edition. With numerous Illustrations and Three Folding Plates. 21s.
Page 697
MINE ACCOUNTS AND MINING BOOKKEEPING. From the Actual
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Page 698
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