^carmitg janb Ifatror. LIBRARY Uiiiversity of Illmois. # CI.ASS. ’VOi;uMK. W Books are n0»t to be 'taken from theiLibrary. & ^ Accession No. Return this book on or before the Latest Date stamped below. A charge is made on all overdue books. U. of I. Library IJtL i o jj^ij yUL t} 805 7-S Digitized by the Internet Archive in 2017 with funding from University of Illinois Urbana-Champaign Alternates https://archive.org/details/introductiontogeOOhinr Ricordiamoci in grazia, che il cercar la costituzione del mondo e dc’ maggiori e de’ pin nobili problcmi, che sieno in natura. Galileo Galilei. Gj. II., Sistemi. LAVOISIER. EXPERIMENTUM CRUCIS. INTRODUCTION TO GENERAL CHEMISTRY. A GRADED COURSE OF ONE HUNDRED LECTURES BY GUSTAVUS DETLEF HINRICHS, M.D., LL.D. HONORARY AND CORRESPONDING MEMBER OF SCIENTIFIC SOCIETIES IN FRANCE, GERMANY AND THE UNITED STATES) PROFESSOR OF CHEMISTRY, ST. LOUIS COLLEGE OF PHARMACY. WITH AX ATLAS OF EIGHTY PLATES, REPRESENTING CHEMISTS, INSTITUTIONS, PRIME MATERIALS, CRYSTALS, DIAGRAMS AND APPARATUS) AND ILLUSTRATIONS IN THE TEXT. ST. LOUIS, MO., U. S. CARL GUSTAV HINRICHS, PUBLISHER. NEW YORK AND LEIPZIG, LEMCKE AND BUECHNER. London, H. Grevel & Co. Paris, H. Le Soudier. 1897. Entered According to Act of Congress, in the year 1897. by Gustavus Hinrichs, In the Office of the Librarian of Congress, at Washington. ALL RIGHTS RESERVED BY THE AETHOR. PHOTO-ENGRAVINGS BY SANDERS ENGRAVING CO., ST. LOUIS, MO. PRINTED BY R. P. STUDLEY & CO., ST. LOUIS, MO. S'vt> p , , V TO Charles Friedel, MEMBER OF THE INSTITUTE OF FRANCE, PROFESSOR OF THE FACULTY OF SCIENCES. CONSERVATOR OF THE M I N ER A LOGI C A L MUSEUM OF THE NATIONAL SCHOOL OF MINES. OF PARIS. THIS VOLUME IS DEDICATED BY The Author MONSIEUR CHARLES FRIEDEL, MEMBRE DE L’ INSTITUT, Paris, France. My Dear Sir : The Introduction to General Chemistry here- with most respectfully dedicated to you, is intended to give the student a first view of the broad field of science that has been enriched by your researches, and to serve as a supplement to existing treatises of our science. To you, the form of a crystal, the synthesis of a mineral and the formation of a new series of organic compounds have been chemical problems of equal importance. Hence the solution of every single problem by your hands has enriched chem- istry with a new principle as broad as the horizon of your mind. Thus, when you made the ancient dwarfs of the mountain speak, the crystal revealed to you its true composition. Upon this you built an organic chemistry of the deep, of which that of air and sun is like the spirit. Your official trusts have been as broad as your chemical work. The magnificent collection of / minerals at the Ecole des Mines, and Organic Chemistry at the Sorbonne, have been equally benefitted by that breadth of mind which the specialist cannot even understand. I Your recent establishment of Les Actualites Chimiques makes all chemists of the world your debtors. The Great Chemist of the North first sacrificed his time to such a task, eighty years ago. For a while, his creation was continued in another country, by the kindred minds of a Liebig and a Woehler. But with modern Byzantinism, the Jahresberichte have depreciated in character even more than they have increased in bulk. You happily have found a form in which the thought of Berzelius arises to new life for the good of science. That your Colleague, Professor Schuetzen- berger of the College de France, under your presi- dency, has delivered a Lecture on work of mine to the chemists of Paris, at the Sorbonne, and that you have opened your new Review with a full report thereof, is acknowledged as a great distinction with gratitude by THF AUTHOR. St. Louis, Mo., U. S., March 15, 1897. A ^^'Z^'^-r — e^c^ Je me suis propose d’embrasser, dans ma publication, la science tout entiere; mon livre sera complet, quand au but; il ne sera elementaire que par le choix des methodes. FRANCOIS ARAGO, Astr.-pop. T. I., 1854, PREFACE. This work embodies the experience of nearly forty years behind the Lecture Table. I have addressed fully ten thousand students in the aggregate. For a century, our chemical text- books have been modelled on one pattern. They all begin with general principles that require advanced knowledge to be understood. The student is first directed to observe that which he cannot see, and to comprehend that which it took old chemists centuries to learn. At the same time, that which is common and of great practical importance, is withheld till late in the course or entirely omitted. Many gases that were of special interest a century ago, are still made prominent, though of no significance at present, while the instructive and useful gasometric processes are given no place. A reformation seems necessary. It has been attempted in this book. The entire science is presented in a strictly graded course. The principal points are determined in the order of their historic growth. The discovery of oxygen is not presented until its necessity can be understood ; it comes as the dramatic event that it actually was in history. The atomic theory comes last, and is here carried to completion. The real authors of chemistry are the chemists that created the science. Hence the portraits of the makers pre- cede their work. The other parts of the Atlas are equally essentfal. The pictorial representation of the prime materials we would like to have increased largely. 11 The present is the Lecture Course exclusively. It is supplemented by a Laboratory Course, the guide for which it is our intention to issue in another year. The lecture is not the place for details on processes and apparatus. It is as impossible to teach as it is to learn such details in the lecture hall. At the laboratory stand such knowledge is acquired almost without an effort. The plates of apparatus are largely suggestive of what is presented at each lecture. The experiments are sufficiently indicated in the text. Neither apparatus, nor experiment, should ever be introduced simply for show or amusement. They are means to an end, namely the establishment of chemical facts and principles. This book does not aim to be a systematic treatise on compounds. Of such books there are enough. The best by far is the Traite of Troost, (11th edit., Paris, 1895); it is a masterpiece of completeness and condensation ; it gives a maximum of chemistry in a minimum of space. The selection of topics, and their order of succession, has been to me a matter of much study and consideration for many years. The text has also been most carefully written and re-written. It has been my constant aim to make the text concise and clear. Each lecture deals with a single, definite topic. It is treated as a subject by itself. The best French writers have been my models of style. But the work is before the reader and the student, respectfully submit it to their consideration. Si GCiESTiox: In a first course it is advisable to omit the more difficult quantitative inorganic part (Lectures 38 to 51) till Lecture 80 in organic chemistrv has been heard. After that, and perhaps a review, the more difficult quantative parts can be taken with greatest advantage. CONTENTS. TEXT OF ONE HUNDRED LECTURES. INORGANIC CHEMISTRY I. Chemic.vl Agencies: I, Chemistry and A 1 Kemi. 2, Weight and Measure. 3, Solids and Fluids. 4, Fusing and Boiling. 3, Furnace and Blowpipe. II. Metals .\xi) Minerals: 6, Metals, old and new. 7, Calcination and Reduction. 8, Alloys and Amalgams. 9, Ores and Cleavage. 10, Crystal Gems. II, Crystal Stones. 12, Rocks and Veins. 13, Salts and Spirits. 14^ Solution and Crystallization. 15, Crystal Description. III. Chemical Reactions : 16, Marble and Fixed Air. 17, Zinc and Inflammable Air. 18, Substitution by Solution. 19^ Solution of Silver and Gold. 20^ Re- duction in the Wet Way. 21^ Sulphur and Sulphides. 22, Hydrogen Sulphide and the Metals. 23, Iodine and Iodides. 24^ Acidimetry and Alkalimetry. 25, Neutralization and Caloration. 26, Flux and Glass. 27, Metals and Radicals. 28, Chemical Reactions. IV. Combustion: 29, Combustion and Phlogiston. 30^ Combustion and Oxygen. 31, Oxide and Radical. 32^ Analysis of the Air. 33^ Nitrogen, Phosphorus and Argon. V. Electrolysis : 34, Battery and Dynamo. 35, Qualitative Electrolysis. 36, Applied Electrolysis. 37, Equivalent and Electricity. VI. Chemical Formulae: 38, Equivalent and Volume. 39, Equivalent and Heat. 40, Atoms and Molecules. 41, Elements and Compounds. 42, Allotropy and Isomery. 43, Binaries and Ternaries. 44, Formula and Compound. \TI. Chemical Analysis: Quantitative: 45, Purity and Strength. 46, The Analytical Balance. 47, Specific Gravity Methods. 48, Analysis by Dissocia- tion. 49, Gasometric Analysis. 50, Volumetric Analvsis. 51, Gravimetric Analysis. Qualitative: 52, Spectrum Analysis. 53, Dry Way Analysis. 54, Wet Way Analysis of Bases. 55, W'et Way Analysis of Acids. 56, Recognition of Specimens. 13 ORGANIC CHEMISTRY. VIII. Organic Prime Materials: \"egetable: 57, Organic Prime Materials. 58, Sugar and Wine. 59, Fats apd Oils. 60, Flower and Fragrance. 61, Indigo and Madder. 62, Balsam and Resin. 63, Vegetable Acids. 64, Vege- table Bases. 65, Neutral Principles. 66, Starch and briber. Animal: 67, Milk and Butter. 68, Flesh and Blood. 69, Bone and Sinew. 70, Animal and Plant. 71, Fermentation and Life. Fossil: 72, Petroleum and Coal. 73, Gas and Tar. 74, Phenol and Aniline. 75, Bone Oil and Wood Spirits. IX. Chemical Transformations: 76, Starch, Sugar and Glucose. 77, Alcohol and Ethers. 78, Fats and Soaps. 79, Nitro-Glycerin and Gun-Cotton. 80, Chloracetic Acid and Chloral. X. Chemical Constitution: 81, Proximate and Ultimate Analysis. 82, Empirical and Molecular Formulae. 83, Radical and Structural Formulae. 84, Polymeric and Isomeric Compounds. 85, Right- and Left-Handed Compounds. 86, Tetrahedron and Benzol Ring. 87, Alcoholic Compounds. 88, Aromatic Compounds. 89, Complex Compounds. 90, Organic Synthesis. XI. Atom-Mechanics : 91, The Atom World. 92, Prismatic Atoms and Boiling. 93, Atom Linkage and Fusing. 94, Atom Volume. 95, Isomeric Atoms. 96, Atomic Rotation. 97, Atomic Libr2Ption. 98, Atomic Crystals. 99, Atomic Weights. 100, The Atomic Composition of the Elements. ERRATA. LECT. 24. Sect. 5: For 5 cc read 50 cc; for 7 in line 5 read 31; Sect. 12, line i, for proportion read preparation. LECT. 25. S. 6, L.3: for ammonia read ammonium; S. 10, L. 6: from calcium, read for cal- cium. LECT. 32. S. 2, L. 5: For hydrometer, read hygrometer. LECT. 33. S. 10, L. 2: Raleigh, read Rayleigh. LECT. 37. S. ii, L. 7 : The — ous, read the anomalous. LECT. 40. S.7, L.4: ForNa27 read Na 23. LECT. 49. S. ii, L. 9: For 2 Ca O Cl = 183, read Ca (O Cl)2 = 143; L. 10, for 7.629 read 5.96. LECT. 51. S. 9, L. 3: Indicated read indicator. LECT. 60. S. 9, L. 6: Add B 160. LECT. 84. S. 2, L. 3: terrible read terribly. LECT. 86. S. 3, L. 5, admir- able read admirably. 14 IHE STUDENTS ATLAS I. Chemists and Institutions; Chemists: 17. In Old Kenii. — A Modern Temple of Chemistry (Leipzig). iS, (hilileo Galilei. 19, Lavoisier. 20, 1 luvghens. 21, Bovle. 22, Berzelius. 23, Liebig. 24, Bunsen. 25, Dumas. 26, Faraday. 27. Berthelot. 28, Ilaidinger. 29. Padre Secchi. 30, Lemery : \’an llelmont. 31, Pasteur; Volta. 32, Berthollet; Dalton. 33, Richter: Stas. 34, Mitscherlich : Hofmann. 35, Kirchhoff; Kekule. 36, Claude Bernard; Moissan. 37, Chevreul; Court of the Institut. Institutions: 38, Palace of the Institute of P'rance; Ante-room of the x\cademy of Sciences. 39, Meeting Room of the Academy; The Institute of PTance, see pp. 37, 38, 39, 42. 39, Balance Room at Breteuil (International Bureau of Weights and Measures). 4O; Chemical Lecture Halls; Gratz^ Paris. 41, Chemical Laboratories; Giessen; Leipzig. 42, Chemical Research Library: Secretary Berthelot’s Room in the Palace of the Institute. 43, A page from the Saint Mark Manuscript. H. Prime Materials: 44, Galileo's Moons of Jupiter: Meteorite P'ield in Iowa. 45^ Amana Meteorites, Hinrichs’ Collections. 46, Gems (models). 47, Veins. 48, Coal: Gold. 49, Vanilla; Milk. 50, Sea Salt: Rock Salt. 51, Cryolite; Marble. 52, Cinchona: Magnetite. HI. The Crystal World: 53, Microphotographs of Snow Crystals; Alexandrite Crystals, Siberia. 54, Cubical Crystals, Rome de P Isle. 55, Calcite Crystals, Hauy. 56, Beryl; Corundum. 57, Hematite. 58, Magnetite. 59, Cuprite: Garnet. 60, Zircon. 61, Topaz. 62, Topaz; Alex- andrite. 63, Pyroxene. 64, Orthoclase; Anorthite. 65, Quartz; Calcite. 66, 67, The Principal Crystal P'orms, according to Von Kobell. 68, Blackboard Sketches of Common Crystals, and Student’s Goniometer. 69, Sulphur Crystals (with their axes). IV. Diagrams : 70, Solubility in Water, Gay-Lussac. 71, Solubility in Water, Etard. 72, Spectra of the Light Metals, Bunsen and Kirchhoff. 73, Chemical Reactions, Dry Way and Wet Way. 74, Boiling and Fusing Points of Paraffins. 75, Boiling Points of Acids, Alcohol, etc., (log. a). 76, Terminal Substitution, complex. 77, Terminal Substitution, simple. 78, Boiling Point of Isomeric Ethers. 79, Stas’ Determination of Silver Nitrate. 80, Ilinrichs’ System of the Elements, showing their Composition. V. Supplement: 385, Cleopatra’s Chrysopoeia, Berthelot; Chemical Valence, Ilinrichs’, 1867. 386, Weight and Measure. 387, Gasometric Apparatus. 388, Gas Manipulation. 389, Distilling and Extracting Apparatus; Professor’s Stand, Chemical Laboratory, St. Louis College of Pharmacy. 390, Micrographs of Ferments. 391, Ilinrichs’ Chemical Elements, 1867. 392, The Dodecahedron; The Pyritohedron. Hauy, Origin of Secondary Forms. 393, Daubree. 394, Structure and Properties. The Paraffins. 395, Structure and Libration. Benzol. 396-7. Ilinrichs’ System of the Elements, 1867 and 1897. 398, Origin of the Periodic Law.” Atomic Weights, Diamond Standard. 399^ Half a page from Hinrichs’ Programme der Atom Mechanik, 1867. 400, A Look-Out to the Old Pastures (67, i). Portraits in the Text: Agricola. Daubree. Lavoisier in Prison under the Reign of Terror (full page). Priestly. Scheele. Woehler. IN OLD KEMI. THE STUDENT’S ATLAS. I. Chemists and Institutions. A MODERN TEMPLE OF CHEMISTRY 17 GALILEO GALILEI. 18 LAVOISIER. 19 HUYGHENS. 20 BOYLE. 21 BERZELIUS. LIEBiG. BUNSEN 24 DUMAS, FARADAY. BERTHELOT. 27 HAIDINGER. 28 P. SECCHI. 29 LEMERY. VAN HELMONT. 30 PASTEUR, VOLTA. 31 BERTHOLLET. DALTON. 82 RICHTER. STAS. 33 MITSCHERLICH. HOFMANN. :u KIRCHHOFF. KEKULE. 85 CLAUDE BERNARD. MOISSAN. ISOLATING FLUORINE IN THE SCHOOL OF PHARMACY, PARIS. :U) COURT OF THE INSTITUTE. CHEVREUL, AT THE AGE OF ONE HUNDRED YEARS. 87 PALACE OF THE INSTITUTE. ANTEROOM OF THE ACADEMY. 38 MEETING ROOM OF THE ACADEMY. LECTURE BY LEMERY, PARIS, 1680. 40 LIEBIG’S LABORATORY, GIESSEN. IN KOLBE’S LABORATORY, LEIPZIG 41 V*ffi Xu t A- 4 ' t -trl t “TH jjlH \ nni m e r K E t juuVi uu *>4 1 i{*n t nr ; c { V^f|sXXOjJLlCt'TtL)W<^ 1 ^ 0 to"<^ajJ 4 - H C CTJJUU NMC 4 >l?VCU<|>l^ '.'• 0 'XJ C, CE^Nhhh Xj* p c K Kf 0 Mfl C<{>iUNONJLmA.I&PC ^ Ytc|>a.f-Hju jsj nXfk-tj ft c Xj’Ht"Try'.peiccr, 2 xHpc ^ Ai:{>p 3 b^j'vM 4 >afCcj 5 c|*’x^^Kot ^ EjJULHCC-riX'BtUK* 5 EAxci''rH^flC ^ V> Y* C 0 C LOV pNHJUJL 0 1 KiiCisrxjuyi VfdKOTjXa^ h 4 a jLt.xxxr^xx| y c 0 Y- ^ ^ rv“p P ^ JLjn. p-v mi ^ JL^rrp Y-pwH juUL r\rjoX^ Y'COICOI^X gjJL? rVf ft CJCEt«iJY"JlUMCC v ^ * I 0 fCU'c t-ru Pt ^XiAKoCK-^ntpoc-^ ^ K^t.n^'pv-rH ? ^ KXIC l-TH f OY^Pt M HJlUL ^ MH JULA- * ’ * juuj b Xj nr rn jlldTm b 2^.0 *x*aLXKdC ju-OTs.! BJXDnrp mhjl-Ul juLi X 1 B :?vo c K e ic Arr juu H 0 c tCJJCt-rHfOl 5 KJLit tTHPt nr-m 'OLPAi. 9 'V^j 7 \Konr"rrt tBJ\X S ^ g HX£C l VK Pot ^CIKA^i-aMd-r ^ ^KOttceKi-TLU^oe j, of PNfv'KHM'trj.rt Kijvj 0 M Azjrrry 0 Ni tow -d- B ^ i^i low W T-O W ‘.V f p*Y^p W HJlUL f i! 2 ui j» o nr TTtnpA-X.o m ^ Ci:^H P dnr lot, ^ Bac JLcb p r f p\H h 40 M ALCHEMISTIC SIGNS OF THE METALS. SAINT MARK MANUSCRIPT. FROM BERTHELOT. 48 GALILEO SHOWING THE MOONS OF JUPITER TO THE SENATORS OF VENICE. THE STUDENT’S ATLAS. THE GREAT IOWA METEOR, FEBRUARY 12, 1875. 44 45 AMANA METEORITES. Hinrichs’ Collections. GEMS. 46 VEINS, FREIBERG, SAXONY. ONE-FIFTIETH NATURAL SIZE. 47 COAL MINING, FRANCE. EPINAC. GOLD MINING, TRANSVAAL ZULU MINERS. 48 VANILLA. JARDIN DES PLANTES, PARIS. MILK. CENTRAL PLATEAU, FRANCE. 49 SEA SALT. FRANCE. BOURG DE BATZ, BRITTANY. ROCK SALT QUARRY, SPAIN. CORDONNA VALLEY, PYRENEES. 50 CRYOLITE, GREENLAND. ARKSUT FJORD. MARBLE, ITALY. MONTE ALTISSIMO. 51 CINCHONA, PERU. BARK GATHERING. MAGNETITE QUARRIES, ELBA. CAPE CALAMITA- r)2 MICROPHOTOGRAPHS OF SNOW STARS. THE STUDENT’S ATLAS. III. The Crystal World. ALEXANDRITE CRYSTALS. SIBERIA. 58 I.e CviiEim lHexaedre et ses Afocii/iaih’oiu 54 ROME DE LISLE. 1’aJITIF. 1)E RAlS(miST>:MKNT 55 RENE-JUST HAUY. TAF Ig 56 BERYL. CORUNDUM. 57 HEMATITE. HEMATITE. TAP XLX 58 MAGNETITE, MAGNETITE, 59 CUPRITE, GARNET, TJF XlVIll 60 ZIRCON. ZIRCON. T/IF XKXMll (a) TAF XXXV/fl (if 61 TOPAZ. TOPAZ. TAF XXWUl (f) 62 TOPAZ. ALEXANDRITE. 63 PYROXENE. PYROXENE. 64 ORTHOCLASE. ANORTHITE. < 2 3 4 > 6 7 16 17 IS <9 20 < 2 3 4 5 6 7 8 9 40 H 12 13 G5 6G 67 CRYSTAL DESCRIPTION, 69 THE STUDENT’S ATLAS. IV. Diagrams. 70 71 SPECTRA OF THE LIGHT METALS. 0 10 20 30 40 50 60 70 80 90 100 110 120 130 140 150 ICO 170 blau violet Spcctraltafol nacli Kirclihoff und Bunsen, CHEMICAL REACTIONS. DRY WAY. VVET WAY. 74 BOILING AND FUSING POINTS OF PARAFFINS. BOILING POINTS OF ACIDS, ALCOHOLS, Etc, 76 TERMINAL SUBSTITUTION, COMPLEX. uhstitutLOTi terminale ( i TERMINAL SUBSTITUTION, SIMPLE. 78 BOILING POINT OF ISOMERIC ETHERS. nitrate - STas, 79 STAS’ DETERMINATION OF SILVER NITRATE. 80 1. CHEMISTRY AND AL KEMI. 1. Chemistry treats of the changes of matter. It was first practiced by the inhabitants of Kern or Kemi (Egypt). The very name of our science thus proclaims its ancient origin. Atlas, p. 17. To understand this definition fully implies to have studied the SCIENCE and practiced the ART of Chemistry. Here it must therefore suffice to explain the words used in the definition. 2. MATTER is that which constitutes all things. We all know some metals, stones and ores, representing the inani- mate kingdom of nature. Flowers and fruits are vegetable, milk, blood, meat and bone are animal things. Chemistry deals with the changes of matter from all three kingdoms of nature. Nor is Chemistry restricted to materials of this earth ; the material of the sun and the stars has been successfully investigated during the last forty years. 3. Motion and division of matter are called PHYSICAL processes ; they do not affect the nature of the material itself. The power to produce such motion or division may be great, as witnessed on our railways and in our mills. The immense ball, thrown several miles from the modern cannon, does not change its material nature in this act of motion; however, the charge of powder has disappeared, it has undergone a chemical change. 4. But if that ball be left exposed to the air, the water or the earth, it will gradually be changed into a brownish, non- coherent mass,' which we call rust. Smaller and thinner iron things are quite rapidly changed to rust throughout. Objects of copper turn green under like conditions. Gold remains unchanged. The change of limestone to lime in the kiln is also a radical one, practiced from time immemorial to make mortar. Such are chemical CHANGES of matter. 82 LECTURE 1. 5. Organic matter, that is vegetable and animal substance, chars when heated while the air is partly excluded. Inflam- mable materials pass off during this process. A specially offensive odor is noted when animal matters are charred. Thus it is generally easy to distinguish mineral, vegetable and animal materials by a simple CHEMICAL TEST. 6. All nature is one boundless CHEMICAL LABORATORY, and the most skillful of all chemists are the plants and animals. From the same soil, water and air, and by the power of the same sunbeam, PLANTS produce not only their diverse materials such as wood, leaf, flower and fruit in general, but each kind of plant produces some more valuable chemical specialty, such as the fragrance of the rose, differing from that of the lily; the potency of the poppy, differing from that of the conium. Atlas, p. 49. 7. In a like manner, every animal is a most wonderful CHEMICAL FACTORY. The beginner should be impressed with such primary fact as the chemical change of grass and water into milk. Surely, grass, water and air are the only raw materials accessible to the cow in her pasture. And what a remarkable chemical product is the milk produced, containing butter, cheese, sugar, and mineral salts dissolved and sus- pended in water! Atlas, p. 49. 8. Seeing the INFINITE DIVERSITY of organic matter pro- duced from the identical simple raw materials of soil, water and air, we can understand that profound thinkers, twenty five centuries ago, considered all matter essentially one in kind. For about a century this idea has been generally derided by chemists. It does not seem to us that the ancient sages were greatly in error. 9. But if all matter be essentially one, it seems possible that any material might be made by art if only sufficient knowledge had been acquired. Hence ancient chemists (ALCHEMISTS) endeavored to make gold from common metals, and tried to produce an elixir to give health and prolong life. CHEMISTRY AND AL KEMI. 8:j Working to realize these high ideals, they laid the foundations of CHEMICAL ART AND SCIENCE, the two equally important parts of CHEMISTRY. The science we present in the lecture hall, the art we practice in the laboratory. Atlas pp. 40, 41. 10. Chemical science has ever enabled chemical art indi- rectly to make gold, and thus to REALIZE THE IDEAL OF THE ALCHEMIST. Clay was converted into costly porcelain; coal tar was changed into the colors of the rainbow, and apparently worthless ores are now yielding gold by the million dollars in Transvaal and in Colorado. Atlas, p. 48. 11. Chemistry is also approaching the second ideal of its founders. The active remedial principles have been extracted from many plants, and even new remedies have been pro- duced by direct synthesis, the chemist imitating the work done by the living cell! Moreover, practical hygiene is main- ly chemical. Surely, Chemistry does give health and pro- long life. 12. Until it shall be deemed proper to deride Columbus for having discovered America while he sought the Indies, we will not join those who deride the early workers in Kemi for having held ideals too high to be fully realized in three thousand years. In Chemistry, as everywhere else, the highest ideals are the best; the distant star is a better guide than the near ignis fatuus. Sic itur ad astra. Notes. Deeming it essential to keep the text as brief and clear as possible, collateral and explanatory matter, aiding in the understanding of the topic presented, is appended in the form of short notes, precisely as explanations are given at the lectures, but not considered as part of the subject itself, once that being understood. The notes will be prefaced by a numeral referring to the paragraph for which they are intended. I. Chemistry, in English, is commonly pronounced Kem-istry; sig- nifying knowledge pertaining to Kemi. Chemistry is called Kemi in Danish, Chemie in German and Chimie in French. 6. Among the various plants represented in the cut as growing in a glass-house of the Jardin des Plantes at Paris, the climbing Vanilla will 84 LECTURE 2. be noticed, showing flower and the valued fruit, also numerous pendent air roots. 7. These Chemical factories (cows) are exceedingly numerous and their product aggregates millions a year in every country. When no longer wanted for milk production, these factories are let alone, and pro- duce meats and fats, hides and bones, all prime materials of the highest importance. England imports for 40 million dollars butter alone a year. 10. The new cyanide process with reduction by electrolysis makes it possible to work low grade ores profitably. The Zulus do the mechani- cal work of drilling, shown p. 48; dynamite does the rest. The Trans- vaal gold deposit is not a vein, but a stratum, the onl}' stratified gold deposit in the world. 2. WEIGHT AND MEASURE. 1. Any body or thing occupies some definite amount of space, called its bulk, measure or VOLUME. It also exerts some definite amount of pressure upon its support; this pres- sure is called its WEIGHT. Weight and measure are the only two general properties which matter possesses. 2. By adopting convenient UNITS, both weight and volume can be expressed by numbers. The standard units are the KILOGRAMME and the METER. Exact copies thereof are made at the International Bureau of Weights and Measures, in the Pavilion Breteuil at Saint-Cloud, in southwestern Paris. This Bureau is jointly maintained by over twenty countries, including the United States and Great Britain. Atlas, p. 39, shows the Balance Hall of this Bureau. 3. The metrical standards were adopted in France a cen- tury ago, to secure natural units and uniformity; even towns having distinct units at that time. The meter was intended to be the ten -millionth partmf the earth’s quadrant passing through Paris. The kilogramme was intended to be the pres- sure of a tenth -meter cube of water at its greatest density. 4. Modern determinations have shown that the quadrant really is about 10.001.900 meters and that the kilogramme exceeds the defined amount by something less than one ten- WEIGHT AND MEASURE. 85 thousandth part. The actual material STANDARDS, made a century ago are, however, retained unchanged by the Interna- tional Commission; the original definition being sufficiently complied with for practical purposes. 5. The system of numeration in universal use being DECIMAL, the units of weight and measure must also be divided and multiplied by tens to avoid useless reductions. The sub-multiples are distinguished by Latin prefixes (deci, centi, mini), while the multiples are designated by greek pre- fixes (deka, hecto, kilo). The mega is used for very large (million) and the micro for equally small (millionth) values. Thus the micrometer or micron (/^) being the thousandth of a millimeter, is the usual unit for microscopic objects. 6. THE BALANCE is the instrument for weighing. It con- sists of a light, rigid beam, resting by means of a transverse edge on a hard smooth plane. Two smaller edges at the ends of the beam support like planes to which the pans are attached. The distances from the outer to the central edge (the arms) must be equal. In good (prescription) balances, edges and planes are of hardened steel ; in the analytical balance, the planes are of agate ; in the best balances, the edges are also made of agate. 7. Weights are made in sets, containing one 5, one 2 and two 1 for each digit, except the last, for which commonly two 2 and one 1 are given to complete the 10 and allow a check. f;rom one gramme up, the weights are usually turned brass; for subdivisions of the gramme, platinum foil is used. Each single weight is fitted to its special place in the box holding the set. Chemical weights must be handled by forceps only, never touched with the fingers. 8. In WEIGHING, the body is placed on the left pan, and weights' are applied in the order of their magnitude on the right pan. By a simple mechanism, the beam is brought into action only for an instant to see whether the weights on the pan are too heavy or insufficient. Below the centigramme. LECTURE 2. the beam is permitted to oscillate, the balance case being closed to prevent air currents. If the oscillations of the pointer are equal on both sides, the weighing is completed. 9. Balances and weights obtained from reputable makers will stand all TESTS warranted by the price paid. All details about these matters belong to the course in practical chemistry. The balance being the most sensitive and accurate instru- ment of all, the chemist checks his volume measures by weighing them empty and filled with water up to mark. Every cubic centimeter (cc) should correspond to a gramme (gr.) 10. For the ready measurement of volumes the chemist uses sets of glass vessels accurately graduated (BURETTES and CYLINDERS) or provided with a mark filled up to which they hold a definite amount (FLASKS and PIPETTES). Graduated cylinders with ground glass stoppers are also called MIXING JARS. The burettes are either provided with a rubber tube and spring clamp (Mohr’s), or with a perforated ground glass stopper (Geissler’s) for use with corrosive liquids. 11. Common experience shows that bodies differ greatly in density; lead is heavy, chalk is light, cork even lighter than water. The SPECIFIC GRAVITY (G) of a substance is the weight, in grammes, of one cubic centimeter thereof. The specific gravity, carefully determined, is an important characteristic of matter, enabling us to distinguish otherwise similar bodies. Thus one cc of lead weighs 11.35 gr. ; or lead is character- ized by its G being 11.35. 12. To determine the specific gravity of any body, ascer- tain its weight (w) in grammes and measure its volume (v) in cubic centimeters; dividing the volume into the weight, we evidently obtain the weight of one cubic centimeter, that is the value of G. This process applies to all bodies; the special methods of measuring vary with the nature of the body. A ten gramme flask holds 7.91 gr. of absolute alcohol; hence G is 0.794 for this liquid. 3. SOLIDS AND FLUIDS. 1. Matter presents itself in three distinct forms, namely as solid, liquid and gas. These forms are also called the three STATES OF AGGREGATION. Ice, wood, iron, copper, are solids; water, oil, alcohol, are liquids. The most common gas is atmospheric air. 2. Hold any SOLID body in varying positions, especially in reference to the vertical, and no change in either shape (form) or bulk (volume) of the solid will be noticed. That is, solid bodies possess a form and volume of their own. In other words, the volume and form of a solid are fixed (constant) quantities. 3. A LIQUID contained in any glass vessel, handled in the same way, will exhibit in all positions a free surface which is plain and level, otherwise it will conform to the shape of the containing vessel. If the volume of the liquid is measured at the beginning and at the close of such experiment, it will be ^ found to have remained unchanged. Thus liquids have a fixed volume, but no form of their own. 4. The FREE SURFACE of the liquid shows near the walls of the containing vessel a curved surface ; concave for water, convex for mercury in glass vessels. If a tube be inserted, the liquid will rise or sink so much the more as the tube is more narrow or hair like (capillary). Hence the cause of this deviation from the plane surface is called CAPILLARITY. 5. Only vessels sufficiently wide will show the true plane and level free surface of the liquid. To FILL TO MARK or read the volume on a graduation, the eye should be brought exactly in the height of this surface. If the vessel be too narrow, the lower (for mercury the upper) curved surface should be tangent to the mark of capacity or graduation. 6. The free surface of the same liquid contained in two VESSELS, COMMUNICATING by means of a sufficiently wide tube, stand always in the same level, however the position of LECTURE 3. the vessels may be changed. This is readily seen by using the burette with reservoir, or our gas burette open, and with any liquid, including mercury. 7. If the exit tube of the gas burette be closed, the free surface of the liquid in the burette and reservoir will no longer be in the same level; it will stand low in the burette if the reservoir is raised, and vice versa. Consequently the AIR in the burette resists the pressure of the liquid in the reservoir, and expands when the reservoir is lowered ; it is a substance or body. 8. Thus the air in the closed gas burette has neither volume nor form of its own ; its form is that of the containing vessel, and its volume is dependent on the pressure to which it is subjected. Such a body is called a GAS. Liquids and gases flowing freely from one vessel to another, are also designated by one term FLUID. A liquid is a fluid of fixed volume; a gas is a fluid of variable volume. 9. A gas may be handled almost as readily as a liquid, by means of the pneumatic trough, flasks and cylinders. The PNEUMATIC TROUGH is simply a wide vessel containing a liquid (water, mercury) in which cylinders, flasks, etc., can be filled with the liquid and inverted; they will remain filled, and receive and retain gas from any other vessel or delivery tube. A few experiments make this familiar. See also plate of gas apparatus. 10. A gas burette filled with mercury and provided with a stop -cock at the top can be used as BAROMETER and as a mercurial air pump. By raising the reservoir, fill the burette to a little above the stop -cock, then shut this. Now lower the reservoir. The burette will remain filled with mercury so long as the surface of the mercury is not more than 76 cm lower than the stop- cock. If lowered more, the VACUUM will appear in the burette, and the column of mercury will remain invariably 76 cm. This corresponds to Torricelli’s experiment (1642). SOLIDS AND FLUIDS. 89 11. To use the burette as mercury AIR PUMP, its stop-cock must be perforated lengthwise and connected with the receiver to be exhausted. By a simple turn of the stop-cock, the burette can now be closed (A), or communicate with the air (B) or with the receiver (C). In position (B), fill the burette with mercury, by raising the reservoir; then close (A) and lower reservoir 76 cm; now. connect with receiver (C) ; then turn to B, raise reservoir and drive out air. Continue these operations, and the air in the receiver will rapidly be reduced in amount. 12. If the burette be equal to the capacity of the receiver, the amount of air withdrawn at each complete motion is one half, leakages neglected. Ten motions would reduce it to the thousandth part of the original. If a U tube with perforated stoppers and a capacity of from 50 to 100 cc be exhausted, it will show a loss in weight of over one milligram per cubic centimeter. This evidently is (approximately) the WEIGHT OF THE AIR. Notes 3. Before filling the vessel, film it. that is, move a small amount of the liquid around in the vessel so as to cover the inside with a film of that liquid; then let run and drip out all that will flow. If the vessel was not filmed, the volume of the liquid used in the experiment would apparently have diminished slightly. 4. FUSING AND BOILING. 1. Solid ICE brought into a warm room melts or fuses, being converted into liquid WATER. The latter, heated in a flask, soon begins to boil; while condensed vapor (liquid drops) issue at the top, the flask above the water looks as if it con- tained air, that is the true STEAM, water in the gaseous state. Solid' IODINE is also readily melted and converted into beautiful violet vapor. The corresponding experiment with SULPHUR requires care, the vapors burning with explosive violence. 90 LECTURE 4. 2. In general, a fusible solid, upon heating, will melt, and a volatile liquid will boil. By decreasing the heat, the vapor will again liquefy (condense), and the liquid will solidify (frequently crystallize). Thus the state of aggregation of a substance depends not only on the nature of that substance, but essentially also on the temperature to which the substance is exposed. 3. Heat does not change gases, except in bulk. Grasp the receiver of our gas burette firmly with the hand, and the motion of the liquid will show. that the air EXPANDED. With- drawing the hand, the air returns to exactly its original volume. This apparatus accordingly is a sensitive AIR THERMOMETER. With porcelain and platinum receivers, it permits the determi- nation of very high and also very low degrees of heat. Com- mon thermometers contain mercury or alcohol. 4. Inserting the bulb of such a thermometer into crushed ice, the thermometer will first fall rapidly, then more gradually, and finally remain perfectly stationary or fixed, so long as a reasonably large amount of ice remains. This FIXED POINT of temperature at which ice melts is called the freezing point, and marked zero. In the same manner, boiling of water is found to take place at a fixed point, called the boiling point, which is marked 100. 5. The interval (volume in burette or in thermometer tube) is divided into 100 equal parts, called DEGREES of tempera- ture. For air thermometers this division is continued indefinitely upwards and downwards. 6. If the reservoir be a 100 cc pipette melted off at the mark, and connected by narrow tube with (mercury) gas burette, and the reading of the burette be taken while the reservoir (bulb) is packed in melting ice and also when sur- rounded by steam of boiling water, the EXPANSION will be found equal to 36 cc. Accordingly it is 0.36 cc per degree for 100 cc. Gay-Lussac. FUSING AND BOILING. 91 7. In the same manner, the FUSING POINT (F) of any solid is that fixed degree of temperature at which the solid changes to a liquid; so long as any notable amount of solid is left, the thermometer will remain stationary. If the crucible with the molten mass is set aside to cool, the crust broken and the remaining liquid poured out, the wall will often be found studded with beautiful crystals. Examples: Sulphur; Bismuth. 8. When heating a volatile liquid in a flask provided with a thermometer, the temperature will first rapidly rise, then gradually become stationary, when the liquid will begin to boil, forming bubbles of gas throughout its mass. This fixed temperature is the BOILING POINT (B) of the liquid. When the vapors of the liquid are inflammable, the flask must be connected with a condenser. EVAPORATION is the forma- tion of vapor at the surface of the liquid only. 9. A CONDENSER consists of an inner tube through which the vapors pass from the bulb or flask to the receiver, sur- rounded by an outer tube through which a current of cold water is kept flowing in the opposite direction of the flow of the vapors. Accordingly,' the chance of their condensation in- creases as they pass on. The Liebig condenser is the most common form in use. Atlas, p. 23. 10. This entire process, comprising the change of liquid into vapor, followed by the condensation of the vapor to a liquid, is called DISTILLATION. All non-volatile matters will remain in the flask; hence distillation enables the chemist to separate the volatile from the non-volatile matters. If the vapors condense to a solid, the operation is called SUBLIMATION. Example: Iodine. If the thermometer remains stationary, it marks the boiling point (B) of the pure liquid. If the thermometer is not sta- tionary, the substance is a mixture. 11. In such cases, the process of FRACTIONAL DISTILLA- TION will separate these different substances and yield nearly 92 LECTURE 5. pure materials. The portions or fractions of the distillate, pas- sing over between definite degrees of temperature, are kept separately; these fractions are again run through the distilling apparatus in succession, always removing the new fractions when the same limits of temperature are obtained. After four or more such runs, the fractions often pass over without change in temperature, and thus represent single substances. 12. These two fixed points F and B are most CHARAC- TERISTIC numbers for a given substance, often readily distin- guishing otherwise closely resembling materials; hence they form, together with G, the most important part of the scien- tific description of a given substance. If the material has no such fixed points, it is thereby proved to be impure, and should be subjected to fractioning, to separate it into its prin- cipal ingredients. 5. FURNACE AND BLOWPIPE. 1. HEAT not only produces the 'physical changes of volume and state of aggregation, but it also is one of the common causes of CHEMICAL CHANGES. Inversely, the latter often produce heat. This is especially the case in the general pro- cess of COMBUSTION, a chemical action of combustible and air. When either combustible or air is withdrawn, com- bustion ceases. 2. WOOD is the oldest combustible used; it produces first a flame or blaze, and when the volatile combustible material is burnt, the intensely glowing coals remain. Such a fire is too unsteady for most chemical purposes. Hence, wood first is charred, by slowly burning with limited supply of air, and the resulting CHARCOAL is used. It was the only com- bustible of the early chemists. 3. In modern days, combustible liquids and gases have come into general use in laboratories. In the days of Berzelius, ALCOHOL was used, especially in the excellent lamp with FURNACE AND BLOWPIPE. 93 double draft, constructed by him. For many years, illumi- nating gas — the volatile part of bituminous coal— has been accessible nearly everywhere; it is the best combustible for most laboratory purposes. Where gas cannot be had, gaso- line is frequently used. Atlas, p. 22. 4. An ordinary gas flame is brightly luminous, but not very hot; a cool vessel held over it will be soiled with soot. For heating purposes, a gas flame evidently needs a more abundant supply of air. In the BUNSEN BURNER, this object is per- fectly attained, by surrounding the small gas jet with a wide air tube or chimney, open below. Such a burner gives a tall, steady, almost invisible flame, very hot and depositing no soot. Glass tubes are bent and drawn easily in this flame. Atlas, p. 24. 5. The Bunsen Burner is used in all laboratories the world over, singly for ordinary work, grouped into FURNACES for heating larger forms of apparatus, such as tubes and crucibles. These furnaces are provided with fire clay slabs, disks, wide tubes, to support or encase the vessel, so that the heat may be concentrated upon the vessel and not dissipated to the surroundings. Example: The so-called combustion furnace for elementary analysis 6. The highest degree of heat can only be obtained by burning a large amount of gas completely by means of a correspondingly large supply of air. Accordingly, the gas tap must be large, and the air must be forced by a bellows into the center of the flame. Glass is readily fused in Glassbiowers in ancient Egypt SUCh SL BLAST FLAME, and platinum crucibles are brought to white heat almost instantly. Forms of blast and blast furnaces are very numerous, many makes being most excellent. 7. By means of the chemical BLOWPIPE, all the effects of furnaces may be obtained on a small scale; it is truly a 94 LECTURE 5. miniature furnace. After a little careful practice, an intensely hot flame may be maintained steadily and on a minute sample produce almost instantly the varied effects of furnaces. The chemical blowpipe was pefected by Swedish chemists of last century and became universal through BERZELIUS. Atlas, P..22. 8. The main difficulty in using the blowpipe consists in keeping up a steady flame independent of the regular work of the lungs. TO INHALE AND BLOW at the same time seems impossible; but it is quite easily done, if the respiratory out- let be rigidly limited to the nose (which was specially made for that) while the cheeks fully distended, by their elasticity keep up the flow of the small amount of air required for the blowpipe. 9. Where much blowpipe work is to be done, the inner tube of a so-called COMPOUND BLOWPIPE may be connected with foot bellows, while the outer tube is connected with the gas tap. With such an apparatus, blowpipe work may be exhibited to a class during lectures. 10. In every good blowpipe flame THREE REGIONS are dis- tinguished. At the luminous, bluish point the heat is greatest; it is the FUSING POINT (borax beads, flame colorations). Beyond that point is the OUTER FLAME, assisting combus- tion and producing calcination of metals; within is the INNER FLAME, in which the calx may be reduced again to the metallic state. Example: Lead, supported on charcoal ; flame colora- tions of nitre or salt; borax beads with copper or cobalt calx. 11. As SUPPORT for substances while being heated, glass, porcelain, platinum and carbon, are most generally used for experimental purposes. Fireclay and bone ash are also em- ployed. The best chemical glass is the so-called Bohemian glass, which is light, hard and difficultly fusible; when heated in a Bunsen flame, it is not quick to color it, and first tinges it purple only. Tubes of such glass are most useful. METALS, OLD AND NEW. 95 12. Porcelain in the form of dishes, crucibles and tubes, will stand a higher heat than glass. Platinum vessels and carbon (charcoal and graphite) are used at the highest temperatures. For blowpipe work, hard glass tubing, platinum wire and foil, and good charcoal are all that is required. The properties recognized by blowpipe work are commonly called PYRO- GNOSTIC PROPERTIES (Berzelius). Note. — In this lecture, as in all others, the objects referred to are abundantly exhibited, and the operations mentioned, are pi'oduced before the class. Thus work on glass (especially tubing) and metals v is exhibited; flame colorations and beads are shown. The manganese bead is amethyst in the outer, colorless in the inner flame. 6. METALS, OLD AND NEW. 1. Two substances have attracted the attention of man in the earliest times, and continue to busy his thoughts to-day. The one is and ever has been most precious to him, so that he is willing to accept a small portion thereof as reward for his labors. The other first was his heaven-sent weapon, has become the tool of his hand and mind; he even endeavors with it to build higher than Babel. 2. GOLD is the one of these bodies. Hardly any rich gold deposit is left in the long inhabited countries, but history and myth show they were once as rich in gold, as California and Australia in the middle of this century. Gold has the brilliant luster (metallic) in a high degree; its color is yellow- .ish; its density almost twenty times that of water; when struck a blow, it yields (is malleable). Fire does not change it; it is rare, it cannot be overlooked or mistaken. It is gold. 3. Primitive man also found another metal (luster, mal- leable, heavy), in large lumps, grey in color. We have record of early falls from heaven of such masses of malleable IRON 9G LECTURE 6. at Aegos Potamos on the Bosphorus. Such METEORITES are represented on ancient medals and coins. In the time of Homer iron was prized with gold. Many large meteoric iron masses have been found in Mexico, near the Texas border; also in Southeast Africa, where the natives worked them into tools. (J. Herschel). Atlas, pp. 44, 45. 4. To-day, THE WORLD produces 175 tons' of GOLD a year (49 in U. S., 46 Australia, 15 Transvaal, 40 Russia in 1890; now Transvaal much more). In the same year (1890) the total production of IRON was 27 million tons, (U. S. 10, England 8, Germany 5, France 2). This enormous increase in the production of iron is directly due to chemical progress. The price in Germany was (1890) down to 12 dollars a ton. 5. THE UNITED STATES produced, in 1895, 71 tons of GOLD worth 47 million dollars, and 9.5 million tons of IRON worth 105 million dollars. Accordingly, the ratio of the weights of iron and gold possessing equal value is 60,000 to 1. With the progress of smelting this ratio has been rapidly in- creasing during the ages, and is bound to increase still more. 6. In addition to these two METALS, the ancients knew only five other bodies possessing metallic luster and mallea- bility; namely silver, copper, tin, lead and mercury. For almost two thousand years these SEVEN METALS were com- pared to the seven planets and designated by the planetary signs: Gold, Sun; silver. Moon; quicksilver. Mercury; cop- per, Venus; iron. Mars; tin, Jupiter; lead, Saturn. Terms in common use still remind us of this comparison. Atlas, p. 43. 7. Chemists now designate the metals by the CHEMICAL SYMBOLS introduced by BERZELIUS and consisting of the first and the characteristic letters of their latin (or latinized) name. Thus gold (aurum). An; silver (argentum), Ag; quicksilver (hydrargyrum), Hg; copper (cuprum), Cu; iron (ferrum), Fe; tin (stannum), Sn; lead (plumbum), Pb. In a like manner, sulphur is represented by S, Carbon by C, and Iodine by lo. Atlas, p. 22. METALS, OLD AND NEW. 97 • 8. The seven old metals remain even to-day THE GREAT METALS in the economic life of nations. Thus the United States produced in 1895 in all 270.5 million dollars in metals, of which iron 105.2; silver 60.8; gold 47.0; copper 38.7; lead 10.7; zinc 6.3; mercury 1.3 million dollars. Here we have the big seven of old, with the exception of tin, replaced by the modern zinc. 9. These seven old metals are easily DISTINGUISHED. Mercury is a heavy liquid, silvery white. Tin and lead are readily fusible; color and gravity distinguish them: Sn, white, 7.2; lead, bluish-gray, 11.4. The three most lustrous and malleable metals melt in the blowpipe flame, and are dis- tinguished by color and gravity: Cu, red, 8.8; Ag, white, 10.5; Au, yellow, 19.4. Iron is infusible in the blowpipe flame, grayish- white, and has G 7.8; it is also magnetic. 10. Zinc (Zn) was known to ALCHEMISTS in the 15th cen- tury; it is a metal, but malleable only at a moderate range of temperature (100 to 130 degrees); melts at 415, G 6.9; boils 940. The readily fusible and quite volatile metals Ar- senic (As), Antimony, (Stibium, Sb) and Bismuth (Bi) are so brittle that they can be pulverized; color and gravity will distinguish them : As, corroding black, 5.7 ; Sb, is white, 6.7 ; Bi, reddish-white, 9.8. Probably at some temperature these will show malleability. 11. DURING LAST CENTURY the very heavy (21.5) white metal Platinum (Pt), infusible in the blowpipe flame, was found in Brazil. The lighter (11.4) companion Palladium (Pd) was distinguished by Wollaston, 1803. Nickel (Ni) and Cobalt (Co) are rare companions of iron, equally infusible in the blowpipe flame, almost equally magnetic, but heavier (8.8) and whiter; Ni corrodes green, Co pinkish-red. Manga- nese (Mn) and chromium (Cr) also resemble iron, but are not yet used as metals. 12. Near the beginning of the present century a number of LIGHT METALS (G less than 5) were discovered; the follow- 98 LECTURE 6. ing have lately come into use. Aluminium (Al) quite white, like silver, has F 625, G 2.56, and does not corrode in dry air. Magnesium (Mg), grayish -white, F 420, G 1.75; burns most brilliantly to a white ash when lit by a match. Finally the silver white metals sodium (Natrium, Na) and potassium (Kalium, Ka) cannot be kept in air, are lighter than water, in contact with which they burn. Notes 3. — The great Iowa Meteor (10:20 P. M., February 12, 1875) was seen throughout the territory extending from St. Louis to St. Paul and from Chicago to Omaha. Its explosion was heard over the ten thousand square miles of Iowa shaded on the map, p. 44. The meteorites fell in Iowa County, Iowa, scattered over an elliptic area extending nearly ten miles from southeast to northwest, and almost three miles across at the widest. The greatest stones (all containing over ten per cent of native nickelliferous iron in granular form) fell between the seven towns of the Amana Colony; hence the name Amana Meteorites. I made seven collections, aggregating over five hundred pounds; four of these groups are well shown on page 45 of the Atlas. The two largest (Nos. 22 and 33) were not my own property, but en- trusted to me for study and protection. The largest stone weighs seven- ty five lbs. (No. 33) ; the smallest two oz. (No. 32). The following specimens, arranged in decreasing order of weight, were presented by the author to the principal mineralogical museums of Europe: No. i, Paris (5 kilos, nearly); 2, London; ii, St. Petersburg; 4, Vienna; 13, Brussels; 5, Copenhagen; 14, Harlem; 6, Berlin; 15, Paris (second specimen, over 2 kilos) ; 7, Christiania; 8, Stockholm ; 16, Munich; and No. 9, Lausanne (i kilo). The specific gravity ranged from 3.45 to 3.50. Meteorites, entering our atmosphere from space beyond, are the only cosmical substances accessible to the chemist; hence their extra- ordinary importance. They range from pure nickelliferous irons to STONES almost destitute of metallic iron. The oldest collection of meteorites is at Vienna. It was mainly de- veloped by Haidinger (p. 28), and is now again rapidly growing under Br^zina. It contains 500 distinct localities, of which 320 are stones; the total weight is three tons and a half. The collection of meteorites at the Museum of the Jardin des Plantes at Paris was greatly developed under the care of the eminent Daubree, and is now in charge of Meunier. The grand collection of the British Museum at London is in charge of Fletcher. The London collection is the richest, because of the vast ex- METALS, OLD AND NEW. 1)9 tent of the empire in which the sun never sets, and because English intelligence is ever ready to part with British gold to secure prime ma- terials for science. Thus they possess the largest meteoric iron from Cranbourne, Australia, weighing ten tons; and their gold secured the most remarkable Estherville meteorite (May lo, 1879) from this land of millionaires. However, this meteorite was drawn up from its wet hiding place for my study, before it left this country. 7. CALCINATION AND REDUCTION. 1. GOLD heated on charcoal, in the fusing point of the blowpipe flame, will promptly melt to a metallic globule, but suffer no other change. When cold, it retains the globular form, has all its original properties, and lost nothing in weight. It has been TRIED BY FIRE. (1 Pet. 1.7; Rev. 3, 18). It remains the king of metals; a metallic globule obtained by the blowpipe is still called a regulus, and pure metals are called reguline, as of old. 2. Silver melts like gold, but loses slightly in weight; a small amount of a metallic calx is deposited as a reddish IN- CRUSTATION on the charcoal. Heat this incrustation for an instant with a good, steady, inner flame, and minute, brilliant white silver globules will appear. The calx has been reduced again to reguline silver. Mercury completely volatilizes in the blowpipe flame. 3. Copper melts like gold and silver. The globule re- mains red in the inner flame, tinging that flame green, while in the outer flame the globule turns black on the surface. This copper ash, scraped off, gives reguline copper in the inner flame. Most other metals are much more readily CALCINED, and correspondingly more difficultly REDUCED. 4. Exposing a fragment of LEAD on charcoal to the blow- pipe flame, it melts almost instantly, boils, and burns with a bluish flame to a calx or ash (Litharge) which forms quite a 100 LECTURE 7. large yellowish, incrustation on the charcoal. If the outer flame is used for some time, the incrustation will be reddish (red lead), and all metallic lead will be calcined. 5. This lead incrustation, heated in the inner flame, almost instantly yields a multitude of minute globules of metallic lead (reguli), readily recognized as such by color, softness and malleability. Thus lead is readily calcined in the outer, and reduced in the inner flame. This change from metal to calx, and reduction from calx to regulus, may be repeated any number of times. 6. Lead containing some silver will leave that silver as a pure regulus, while the lead is calcinated in the outer blowpipe flame. In this manner much of the silver has been extracted from argentiferous lead from time immemorial ; the process is called CUPELLATION. The name litharge (lith-argyros, silver stone) still in use points to the antiquity of this process. On a porous support (bone ash cupel) it works better than on charcoal, the melted calx soaking into the cupel. 7. TIN heated on charcoal in the outer flame melts and forms a white incrustation due to its calcination. This in- crustation can be reduced to a regulus, especially after mixing the calx with a little soda and borax. Aiding reduction to the metallic state, soda alone or with borax, is spoken of as a REDUCING FLUX. 8. A fragment of ZINC is so promptly calcinated in the outer flame that its fusion is usually not noticed. It burns with a brilliant green flame and deposits a large incrustation which (as well as the RESIDUE of calx left where the metal was) is infusible, yellow while hot, and turns white on cooling. This change in color can be indefinitely renewed by repeated heating. 9. MAGNESIUM burns with extreme brilliancy, leaving a pure white, infusible residue of calx. ALUMINIUM burns also, but much less readily; its calx is also white and infusible. CALCINATION AND REDUCTION. 101 These white infusible masses cannot be reduced by the blowpipe, but are readily distinguished by igniting them after the addition of a drop of COBALT SOLUTION. The calx from aluminium will become deep blue, that from magnesium pale rose, while zinc calx treated in this way becomes green. 10. The metals As, Sb, Bi burn readily and leave an ash. The most volatile ARSENIC, emitting the odor of garlic, dis- appears, leaving but a slight white incrustation far away from the sample. ANTIMONY melts to a globule and burns with a white smoke, rising straight up from the sample when the flame is withdrawn ; when the burning globule is dropped on the table, it breaks into many small globules, each leaving a white trail of the calx. BISMUTH gives a yellow incrustation. When reduced, both antimony and bismuth are brittle, dis- tinguishing them from tin and lead. 11. IRON heated in the outer flame gives a black residue, no incrustation; when again exposed to the inner flame (best with soda) only gray, MAGNETIC grains or spangles are ob- tained. COBALT and NICKEL act in a like manner. They are however readily distinguished by fusing a little of the calx into a borax bead. Iron will make the bead yellowish in the outer, colorless in the inner flame; nickel gives a brownish bead, and with cobalt the bead shows a splendid deep blue color. The chromium beads are green, those containing manganese are amethyst in the outer, colorless in the inner flame. 12. The light metals SODIUM and POTASSIUM should not be burnt in the blowpipe flame; it would be very dangerous. They leave white, fusible residues, coloring the flame yellow (Na) or purple (Ka). Thus all metals may be readily distinguished in a few in- stants by the blowpipe, even if they are calcinated or otherwise combined. These fire-tests or PYROGNOSTIC CHARACTERS of the metals, should be familiar to all who wish to study chemistry. They are the most ready and distinct means for the recognition of the metals under all conditions. 8. ALLOYS AND AMALGAMS. 1. The different metals can be melted together in various proportions forming ALLOYS, several of which have been in common use from time immemorial, such as bronze and brass. If one of the metals is mercury, the alloy is called an AMALGAM. 2. The readily fusible white metals are very soluble in mercury. Lead, antimony, bismuth and even silver, dissolve so readily and abundantly in mercury as to cool the mass, over 20 degrees (down to 16 below zero) . The tin amalgam is used as a coating on glass for mirrors. Iron is insoluble in mercury; so are the other metals infusible before the blowpipe, like platinum. Accordingly, mercury is shipped in iron flasks, each holding 35 kilos. 3. Gold is about as soluble in mercury as silver. The GOLD AMALGAM is solid at common temperatures, and can be separated by wringing out the chamois into which the mercury and amalgam has been poured; the mercury will run through, the solid amalgam remaining. The amalgam loses about one third of its weight on heating, or contains two parts of gold to one of mercury. 4. The bulk of all the mercury produced (about 4000 tons a year) is used for the EXTRACTION of GOLD and SILVER. Gold sand is concentrated by washing, the lighter materials being removed farthest. When sufficiently concentrated, the remaining heavy material is treated with mercury, which dis- solves the gold. The excess of mercury is separated as above from the gold alloy, which then by heat is freed from the mercury. 5. SOLDER, for tin ware, is an alloy of equal parts of tin and lead, melted together in an iron ladle. It melts at about 190 degrees, which is 40 degrees below the fusing point of tin, the most fusible of the two ingredients. In general, the alloys are more fusible than their constituents. ALLOYS AND AMALGAMS. 103 6. The most important of all alloys in the history of man- kind is BRONZE, containing about one part of tin to nine of copper. In ancient days it was smelted direct from a mixture of copper and tin ores, or by adding tin ore to melted copper. By slow cooling it hardens, by sudden cooling it becomes mal- leable (contrast with steel). 7. The ancients, from the Egyptians to the Romans, made WEAPONS, TOOLS and ORNAMENTS of bronze. Until recently, canons were made of bronze ; now it is used for statuary, bells, medals and ornamental work. The copper is first melted, then the tin added in reasonable excess, to allow for loss by combustion. 8. BRASS (yellow) is an alloy of two parts of copper with one of zinc. It can be cast, hammered, rolled and drawn and thus is most readily shaped into any form. It was used before zinc was known, by adding the mineral cadmia (a zinc ore) to molten copper. By adding an amount of nickel equal to that of zinc to the brass, German silver results. 9. TYPE METAL consists of lead about 4 and antimony 1 part, with some tin. It is very readily fusible, and expands upon solidification (as does water on freezing), thus filling the form exactly to the minutest detail. Very fusible alloys contain bismuth. Thus Darcet’s Metal, melting in the steam over boiling water, consists of bismuth 8, lead 5, tin 3 parts; it melts at 94 degrees. 10. The most characteristic modern alloy is ALUMINIUM BRONZE (copper 9, aluminium 1 part), which is very light and resembles gold in appearance. Ferroaluminium contains 9 iron to 1 aluminium; it is much stronger than the above. 11. Native gold generally contains some silver. Australian gold averages 7 per cent., Californian gold averages 12 per cent, of silver, and is light yellow. VVith about 20 per cent, it is called Electron, the ASEM of the ancient Egyptians. From this, pure gold or pure silver was obtained at will. The 104 LECTURE 9. alloys seemed to show that metals were variable and thus gave some encouragement to the alchemists. 12. When the Egyptians had learned to separate silver from gold, they dropped Asem from their list of metals. Their method of separation, described in the Leyden papyri, is essentially the same dry way process used till the present. The active agents were calcined green vitriol and salt, as in the ROYAL CEMENT of the alchemists. 9. ORES AND CLEAVAGE. 1. ORES ARE MINERALS FROM WHICH METALS CAN BE PROFITABLY OBTAINED. Every student in chemistry should know at least the principal ores from which already the ancients and the alchemists extracted the metals; he should be able to recognize them at sight and by handling them. To .help him do so is the object of this lesson. 2. Ores are generally distinguished from other minerals by a HIGH GRAVITY (4 and over) associated with LOW HARD- NESS. Very few have a hardness equal to glass (de- gree 5) , that is, able to scratch glass and be equally scratched by it. Many have the hard- ness of copper (3) only. METALLIC LUSTER is fre- quent; in that case, the color is constant and therefore specific. If the luster is not metallic, the color is gen- erally variable. 3. THE BLOWPIPE will promptly reveal the presence and nature of the metal in the ore. It will also show whether the ore is a sulphide or not; the former emit the odor of burning AGRICOLA. ORES AND CLEAVAGE. 105 sulphur while heated. This test may be made by simply heating the mineral in an open glass tube, held slanting in the Bunsen flame. Some sulphides also yield a sublimate of white arsenic and give the odor of garlic. 4. Accordingly, the ORES are readily DISTINGUISHED as sulphides and free from sulphur. The last are either native metals or calxes. The first are either simple sulphides or con- tain arsenic also. We will give the principal distinctive prop- erties for each of the common ores. 5. NATIVE METALS are distinguished by their luster and malleability (flattening under the blow of a hammer) . They give no odor of either sulphur or arsenic before the blowpipe. Gravity and color distinguish them one from the other. G 17 to 19: Au, yellow; Pt, white; 11, Pd, white; 10, Ag, white; Bi, reddish gray and rather brittle; 8.5, Cu, red; 8, Fe, white, only in meteorites. 6. The CALXES are without metallic luster, either dull or sub-metallic. HARD enough to scratch glass (over 5) readily, are: G 6, CASSITERITE, brown, and brownish streak (streak is the color of the powder, or trace on rough porcelain), con- tains Sn; G 5, contain Fe; streak: Black, MAGNETITE; red, HEMATITE. 7. Calxes not hard enough to scratch glass, but scratching copper readily, are quite numerous, and have all a specific gravity of about 4. Hence they are to be distinguished by color (first named) and streak (second) : red, orange, LlMONlTE (Fe) ; red, brownish-red, CUPRITE (Cu) ; reddish, orange, ZINCITE (Zn) ; grayish, white, SMITHSONITE (Zn) ; brownish, gray, SlDERlTE (Fe); green, green, MALACHITE (Cu). GARNIERITE, the modern nickel ore, is green and harder than Malachite; blackish-gray, black, PYROLUSITE (Mn). 8. SULPHIDES HARD enough to scratch glass readily, but resisting the knife, have all marked metallic luster and there- fore are easily distinguished by their color. Yellow, PYRITE 106 LECTURE 9. (Fe, no As). The following contain arsenic and are distin- guished by their color and gravity: Gray, (6) ARSENO- PYRITE; white (8), LEUCOPYRITE, and red (7.5) NlCCO- LITE (copper nickel, the old nickel ore). 9. SULPHIDES, NOT HARD enough to scratch glass, readily yielding to the knife edge, have either brilliant metallic luster or not. By their gravity and color they are readily distin- guished as follows; the metal they yield before the blowpipe being added. Brilliant metallic luster; gravity : 7.5, GALE- NITE, gray, Pb; 5, TETRAHEDRITE, gray, much As, some Ag; 4.5 STIBNITE, blackish -gray, Sb; 4, CHALCOPYRITE (copper pyrite), brass-yellow, Cu. Without metallic luster; gravity: 9, CINNABAR, red, Hg; 4, SPHALERITE, blackish to yellow, Zn; 3.5 ORPIMENT, yellow. As; 3, REALGAR, red. As. GRAPHITE (C) and SULPHUR (S) are readily dis- tinguished from sulphides. 10. Almost every specimen of galenite shows many plane, brilliantly reflecting surfaces. If struck by a hammer, it will break according to such plane surfaces only, with extreme readiness; we say it has perfect CLEAVAGE. There will be seen three such cleavage planes, mutually under a right angle. This is most characteristic of gale’nite. Magnetite shows four cleavage planes; fine specimens of Sphalerite even six. Orpi- ment has one cleavage only, according to which it will split into thin foli«. Pyrite is entirely destitute of cleavage. 11. Choice specimens, taken from the walls of some cavity, where the substances were free to grow, show beautiful geometrical forms, all bounded by plane surfaces only. Such specimens are CRYSTALS. Galenite, corresponding to its cleavages, shows cubes, often with the corners equally cut off (truncated) ; p. 66, fig. 2. Magnetite and Cuprite show octahedrae; p. 58, 59. Tetrahedrite shows modifications of half-octahedrae, or tetrahedrse ; p. 66, figs. 16, 9. ITematite, especially from Elba, shows splendid six and twelve sided forms (Elba Roses), p. 57. ORES AND CLEAVAGE. 107 12. Pyrite quite frequently is crystallized. Its simplest and most common form is the cube, bounded by six equal squares (p. 66, fig. 1). Upon inspection these squares are usually found to be striated parallel to one side. Examining the three squares meeting at one corner, these striations will be found parallel to the three edges meeting at that corner, (p. 54, figs. 17 to 19). In many cases the edges are beveled, and finally show the so-called Pyritohedron (p. 66, fig. 21) bounded by twelve five sided faces. Note. The portrait of Georg Agricola has been inserted in the text of this lecture. Agricola was called the father of mineralogy by Werner, a century ago. He was born March 24, 1494 at Glauchau, Saxony, and died in November, 1555, at Chemnitz, Saxony. He settled in the new mining town Joachimsthal, Bohemia, and studied everything pertaining to the rich silver veins which made that town and region flourish. His works on metals and mining are the first which have appeared during modern times; they are noted for thoroughness and accuracy. The portrait is a copy of Schrauf’s, (Vienna 1894) which is a reduction from Sambucus, Antwerp, 1574, plate 38. 10. CRYSTAL GEMS. 1. The old egyptian list of metals contains blue (chesteb) and green (mafek) gems immediately after Gold (nub), Asem and Silver (hat), and followed by bronze (chomt), iron (men) and lead (taht). The Egyptians were familiar with the fact that copper tints fluxes blue and green; but they distin- guished the genuine gems easily from the artificial by their hardness. Moses also was familiar with true gems. (Exod. 28). — Gems are sold by the CARAT which is one-fifth of a gramme. 2. THE TRUE GEMS (p. 46) are crystals. of exceeding hardness. To be prized as jewels they must also be trans- parent and either absolutely colorless or finely colored. Hence, good instructive specimens are obtainable for study 108 LECTURE 10. at reasonable rates, while the price of the same materials fit for the lapidary may be beyond reach. Gems do not differ much in specific gravity; accordingly, this property is of little value in distinguishing them. 3. The gem crystals are generally well formed, and their DEGREE of SYMMETRY may be recognized without much dif- ficulty. If the same face, as to inclination and position towards the direction of a more or less marked corner or prism, occurs twice only, the crystal is called rhombic, (pp. 61, 62) ; if thrice, rhombohedral, p. 57; if four times, quadratic, (p. 60), and if six times, hexagonal, (Beryl, p. 56). If the same crystal, held in two different positions, shows both rhombohe- dral and quadratic symmetry, it is called tesseral (pp. 58, 59). (For mono-and tri-clinic, see note). 4. The degree of HARDNESS of quartz is called 7 ; that of topaz 8, of corundum 9 and of the diamond 10. The most precious gems possess the hardness 8 and over; namely topaz 8, spinel 8, chrysoberyl 8i, ruby and sapphire 9, diamond 10. Below these we have the emerald 7f, zircon 7j, turmaline 7i and the “poor man’s gems” garnet and quartz 7. 5. These gems are also CHEMICALLY divisible into the same two groups. All of lower hardness, including topaz, fail to dissolve in a bead of microcosmic salt in the blowpipe flame, precisely as do glass and other silicates ; to that extent they are natural glasses, crystalized. But the harder gems, spinel, chrysoberyl and corundum (sapphire and ruby) do dissolve, and are not glass-like (silicates). The diamond stands, entirely by itself; it is combustible under special conditions. 6. Quartz crystals (p. 65) are quite abundant, and very often perfectly transparent (rock crystal) ; if purple, amethyst, if dark wine yellow, smoky quartz. Its hardness is taken as the standard 7. Gravity 2.7 ; no cleavage. Symmetry rhombohedral; commonly a regular six-sided prism, r, striated crosswise (Figs. 6, 7) dominates, terminated by the three CRYSTAL GEMS. lOJ) rhombohedral faces, P, usually alternating with a second smaller set of rhombohedral faces, Z. A little experience will enable any one to recognize the constancy of crystal form in the apparently infinite variety of appearances and linear dimensions. 7. The GARNET (p. 59) is recognized by its form, being generally a dodecahedron (bounded by twelve equal rhombs, d), inclined under a right angle over the long diagonal, and forming a rhombohedron of 120 degrees at the three sided corners. Garnets show many colors; the pyrope, used in jewelry, is deep red. TURMALINE crystals have a dominant prism, striated lengthwise, surmounted by rhombohedral faces; usually only one termination shows, the crystals breaking readily cross- wise. Colors varied, often in belts or zones. 8. The Zircon (p. 60) is noted for quadratic symmetry only; fine transparent brownish and orange crystals are used under the name of hyacinth. BERYLS (p. 56) are quite common and very large, forming regular six-sided prisms, terminating in a base at right angles thereto, and show cleavage after this plane. Fine beryls are always small and prized as AQUAMARINES when blueish ; when bright green, they are the most valuable EMERALD. 9. The TOPAZ (pp. 61, 62; also p. 67, Fig. 43) forms a rhombic prism (M, 1), striated lengthwise, and possessing perfect cleavage crosswise (i. e. basal, P) ; the crystals show generally only one termination, the basal plane with the domes f and y and the pyramid i. Yellowish colors are most common. The shade of color and especially the character or habitus of the crystals are peculiar to each principal locality, so that the expert can tell from the habitus and color whether the topaz came from Brazil, Saxony, Siberia or Japan. 10. SPINEL is tesseral, the octahedron (bounded by eight equal equilateral triangles, p. 58, fig. 1) dominating. CHRY- SOBERYL (p. 62, Alexandrite) is rhombic; but its prism (119.8 110 LECTURE 10. degs.) is so nearly hexagonal (120 degs.) that it gener- ally occurs in six-sided stellar combinations. A Russian vari- ety, known as ALEXANDRITE, is emerald green in reflected, deep red in transmitted light, thus showing the Russian colors. Transparent specimens thereof form very valuable gems. Atlas, p. 53. 11. CORUNDUM (p. 56) is exceeded in hardness by the diamond only, so that it readily, is distinguished from all other bodies. It crystallizes in rhombohedral forms, usually showing a double pyramid, terminated by a base, o. It shows perfect cleavage according to its base and a rhombohedron, R. Transparent crystals of corundum are next to the diamond in value; when blue they are called SAPPHIRE, when red RUBY. Good rubies have been made by Fremy. Impure corundum, containing hematite, is called emery, and used for grinding and polishing steel. 12. The DIAMOND is the hardest of all bodies; it crystal- lizes in octahedrae (p. 66, fig. 9) variously modified (figs. 11, 12), and has four cleavage planes parallel to the faces of the octahedron. Imperfect diamonds, unfit for jewelry, are called bort. Black pebbles of diamond hardness are called carbonado and used for rock drills. The price of good diamonds increases approximately as the square of the number of carats. Dia- monds have been made by Moissan (p. 36). Notes — 2. The cost of gems varies greatly according to quality. The following extract from the price list of a New York dealer is for ^^fair to good gems, neither poor nor the best.” The price is given in dollars per carat; the order is that of our description. Quartz: rock crystal 3-1; amethyst 'ii,— i ; garnet ^-2 ; turmaline 2-12; zircon 2-8; beryl, golden and aquamarines 1-8; emerald 10-80; topaz i-5 ; spinel 8-48; chrysoberyl 3-16; alexandrite 24-96. Corundum : sapphire 3-24 ; ruby 8-96. Diamond 50-150. 3. The important subject of Crystal Symmetry can only be ap- proached by the beginner when aided by a good atlas of crystal forms. For that reason 18 plates of the admirable atlas of Nikolai von Kokscha- CRYSTAL GEMS. Ill row^ accompanying his great work: Materialien zur Mineralogie Russ- lands, have been added in good photo reductions. In most cases each form is represented first in perspective and' right helow in horizontal projection; the first is marked bv the number, the second by the same number and the word bis ” (twice, second). This second figure shows the symmetry undisturbed by perspective, and should be specially studied. Each face is generally designated by a letter. In addition to the five degrees of symmetry specified, two lower forms exist, namely: moxoclinic, having only symmetry right and left, in pyroxene, p. 63 and orthoclase p. 64; and finally triclinic, having no symmetry whatever, or being asj'mmetric, see Lepolith (really anorthite) p. 64. 9. Good specimens of topaz for the study of rhombic crystal form are comparitively cheap; the basal cleavage avoids the possibility of mistakes. The three plates copied from Kokscharow show some of the finest topaz crystals in their true form, each face exactly as it is developed. The scale of our plates is almost one-half of the original; exactly 0.44 or nine-twentieths. See pages 61, 62, where the plates are designated by the letters a, d and f at the right hand top. On page 61 (a and d) figures 58, 59 and 67 represent (half size) splendid topaz crystals from Nertschinsk, Siberia ("Vol. Ill, p. 207). They are transparent, dark wine yellow. The crystal fig. 59 weighs 1.6 kilograms. On page 62 (f) is given (fig. 76) the horizontal projection (half natural size) of the finest and largest topaz crystal yet obtained. It is 28 cm high, 16 and 12 cm across, and weighs 10.2 kilograms. Von Kokscharow (III 378) says: a topaz crystal of so extraordinary size and beauty as has never been seen before. This crystal belongs to the greatest rarities of the mineral kingdom, on account of its extraordinary magni- tude, perfection of crystallization, fine color (dark wine yellow) and transparency.” It was found in the Nertschinsk region, in the mountains near the Urulga river, Transbaikalia, Siberia; was presented to Emperor Alexander II in i860, and is deposited in the Mineralogical Museum of the Mining Institute of St. Petersburg. 10. The group of Alexandrite crystals represented (p. 53) is one of the most magnificent specimens of native crystals (v. Kokscharow, Vol. IV, p. 62). The group contains 22 large and finely formed twin crystals; the group is 25 cm long, 14 cm high and ii cm wide, and weighs over 5 kilograms. The Gems. Page 46, shows the common crystal form of the following: I, diamond; 2, sapphire; 3, ruby; 4, amethyst; 5, emerald; 6, garnet; 7, aquamarine; 8, topaz; 9, peridot or olivine, chrysolite; 10, rock crystal; II, turmaline. This plate is a half-tone reduction from the fine colored plate V of Simonin, Les pierres, Paris, 1869. 11. CRYSTAL STONES. 1. THE RECOGNITION OF ANY MATERIAL by means of its physical properties is a habit that must be cultivated by every one who would study chemistry successfully. Incident- ally the student becomes practically acquainted with a number of those minerals on which the chemist depends for his ma- terials — and even for the very ideal of chemical individuality. 2. The following dozen STONES should be so familiar to every student that he can recognize them promptly in any of their varied forms. As a group they are not as hard as the gems, nor as heavy as the ores. H 6 and G 4, are the limits. The dozen selected are the most important practically, and the best marked physically and crystallographically. Good speci- mens can be had at comparatively little outlay; many can be collected. 3. To recognize a substance, its properties should be observed in a DEFINITE ORDER. First (by sight) luster, then color and streak; next (by handling), hardness and by mere lifting an estimate of the specific gravity is obtained. Then the specimen — if not a crystal — should be broken by a blow; that will reveal fracture or cleavage; in the latter case, the number, relative position and degree. Finally, if crystal faces visible, they should be examined with a view to determine the symmetry of the crystal. In that case, cleavage planes are often revealed by existing cracks. 4. The last five of the minerals selected are SILICATES, that is, they leave an insoluble silica skeleton in the micro- cosmic bead (10, 5); they are among the most common constituents of the hard rocks, such as granites. The others are not silicates. The first alone is soluble, its taste reveals its nature, salt; the merest trifle of it tinges the blowpipe flame persistantly and intensely yellow (Na). The next five tinge the flame orange, appearing siskin -green through a green glass; they contain calcium (Ca). The heaviest tinges the flame yellowish green; it contains the metal barium (Ba). CRYSTAL STONES. 113 5. TABULAR STONES— VIEW OF THE PROPERTIES OF A DOZEN No. Name. n. G. Cleavage. Crystal Synimetrj’. I. Halite, 2 2.2 3 pfct., 90 degs. Tesseral. 2. Gypsum, 2 2-3 I em.,.2 pfct.. Monoclinic. 3 * Calcite, 3 2.6 3 perfect, 105 degs. Rhombohedral. 4 - Aragonite, 3 h 2.9 I imperfect. Rhombic. 5 * Fluorite, 4 3-1 4 perfect, octah. Tesseral. 6. Apatite, 5 3-1 I imperfect. Hexagonal. 7 ' Barite, 3 4-5 I pfct., 2 less so. Rhombic. S. Mica. 2 2.9 I eminent. Six-sided. 9 * Amphibole, 3 -^ 2 pfct., nearly 120 degs. Monoclinic. lO. Pyroxene, 3-3 2 pfct., nearly 90 degs. Monoclinic. II. Feldspar, 6 2-5 2 pfct., nearly 90 degs. Mono ortriclin. 12. Quartz, 7 2.7 no cleavage. Rhombohedral. 6. All of these stones are destitute of metallic LUSTER, that property being peculiar to metals and ores. The luster is dull or vitreous according to the perfection of the specimen. If ONE CLEAVAGE eminent, so perfect that it can be split into thin leaves (Nos. 2,8) the luster will appear pearly, which is noted even on the best cleavage of feldspar (No. 11.) 7. These minerals are generally colorless or white; but as they have no metallic luster, their COLOR VARIES according to impurities admixed, whether organic or inorganic. Thus Halite (Rock Salt) and Fluorite (Fluorspar) show beautiful colors: yellow, red, green, blue, mostly due to organic matter, destroyed by ignition. Pyroxene (augite) and amphibole (hornblende) are generally green to black, from iron silicates. Quartz and calcite show also most of the colors of the rainbow. 8. Contact with the tongue reveals the only SOLUBLE mineral in the list, HALITE. Hardness 2, indentable by the finger nail, singles out gypsum and mica. Of these two, only GYPSUM occurs massive and fibrous; when foliaceous, its folia are flexible, but not elastic, while MICA always is folia- ceous and elastic as well as flexible. [CRYOLITE from Greenland, has greater gravity (3) and is insoluble in water; otherwise it might be mistaken by hardness and cleavage for poor specimens of rock salt. See p. 51.] 114 LECTURE 11. 9. Copper hardness (3) gives the three species Calcite, Barite and ARAGONITE (p. 67, fig. 55). This latter is very rare, almost destitute of cleavage, while the other two possess perfect cleavages. BARITE is readily distinguished by its high gravity, which has given it the common name Heavy Spar. By cleavage it yields right rhombic tablets of 101.7 degs. The lighter is CALCITE or calcareous spar, the most common of all minerals, which will receive special study further on. It effervesces with vinegar. 10. FLUORITE (Fluorspar) and APATITE (p. 67, fig. 37) are not scratched by copper. Fluorite generally shows its cleavages readily, while apatite practically has no cleavage. The four cleavages of Fluorite equally developed yield a tetra- hedron (p. 66, fig. 16) ; splitting off the corners also, the regular octahedron (fig. 9) results. Fluorspar crystallizes beautifully (figs. 1, 5, 7, 14, etc.) and shows many fine colors; it is the ERZBLUME (ore blossom) of the old miners, ac- companying valuable ores. 11. The silicate stones are easily distinguished by hard- ness and cleavage combined. One eminent cleavage, MICA (isinglass) ; no cleavage, QUARTZ, if hardness 7 (good file). Hardness below this, but the specimen scratching glass quite readily, showing two cleavages under a right angle: FELD- SPAR (p. 64: Orthoclase and Anorthite, here called Lepolith) which is reddish or whiteish, except in the bright green Amazone stone. AUGITE (Pyroxene, p. 63) and HORN- BLENDE are not as hard, but heavier, blackish and greenish colors prevailing; only if showing cleavage, can they be dis- tinguished, except that fibrous varieties are hornblende. 12. Calcite (p. 65) exhibits a thousand modifications (secondary forms) of its rhombohedron, P, of 105.1 degrees, according to which all are broken up by the cleavage planes parallel to the three faces of the rhombohedron meeting in one corner (HAUY, p. 55). The most common secondary forms are the Scalenohedra (r, figs. 15 to 21, Dogtooth Spar) ; next thereto the hexagonal prism, c, and the obtuse rhombohedron. CRYSTAL STONES. 115 g (Nailhead Spar). Marble is crystalline (saccharine marble) ; variegated marble may be massive. Limestone is the most common form. The most perfectly transparent cleavage pieces come from Iceland (Iceland Spar) ; next in perfection are the spars from Lampasas, Texas. 12. ROCKS AND VEINS. 1. Limestone generally is stratified, forming banks or strata of varying thickness, apparently deposited in a primeval sea. The strata have since, in many places, been tilted and broken. Extensive deposits of limestone occur, hundreds of feet in thickness, and for hundreds of miles in extent. They furnish locally fine building stone and material for burning lime. 2. Many LIMESTONES are quite hard, some even crystal- line; but ah effervesce readily with vinegar. The beautiful white MARBLE of Carrara has been quarried for statuary and ornamental work since the days of the Romans, (p. 51). The Greeks obtained a superior, more fine grained marble for their statuary and monumental buildings from the island of Paros. Gypsum also forms valuable rock deposits; easily dis- tinguished by yielding to the finger nail and not effervescing with vinegar. 3. SANDSTONES consist of grains of sand (irregular frag- ments of quartz) held together by some stony cement, often calcareous and effervescing with vinegar. These stones are also stratified, but less extended than the limestones; they vary exceedingly in their characters, as to color, grain and durability of the cement. Many localities offer excellent building stones (Strasburg Munster). The building stones quarried in the United States during 1895 had a value of 35 million dollars. 4. CLAY like deposits form extended strata, differing in consistency from moist, plastic clays to shales and slates (for 116 LECTURE 12. roofing). When heated to redness, clays lose their water, shrink and become hard (brick, pottery.) In a bright white- heat most ordinary clays will show signs of fusion ; the purest clays (white, free from iron, lime, etc.) resist furnace heat, are called fire clay, and serve for crucibles, finer pottery, to porce- lain. All these clay rocks contain aluminium for they will (after removing iron, etc.) give the blue cobalt reaction (7.9). 5. These common stratified rocks — limestones, sandstones and shales — are resting upon and at times tilted up by the the two principal crystalline siliceous rocks, the graystones (granites) and the GREENSTONES (hornblendic and basaltic rocks). In granite the three constituent minerals (mica, feldspar and quartz) may be distinguished without much diffi- culty. The greenstones are heavier, containing more iron. 6. During great convulsions, the rocks, whether stratified or not, have been cracked, deep fissures running nearly paral- lel have been made. In the course of time, nature has healed these wounds, filled up these crevasses in various ways, by materials drawn from the adjacent rocks (the country) or from the depths. Such filled up deep crevasses are called veins (p. 47), especially if they contain ores with the other minerals or veinstones (gangue). 7. The true veins extend indefinitely downwards; their direction on the ground is called their strike, their inclination, dip. The most common veinstones are quartz, calcite, fluorite and barite. These gangues, as well as the associated ores, are often quite symmetrically distributed across the vein, that is, if from the left the order of minerals be a, b, c, d, it will be the same from the right side of vein. See p. 47. 8. If, after a set of. veins has formed, like convulsions take place again, another set of cracks may result, leading to an- other set of veins with other gangue and other ores, CROSS- ING the first and older ones, which thereby may have been greatly displaced. (See right side, p. 47). At Ehrenfried- ersdorf, a set of silver veins run from north to south, while the tin veins run from east to* west. ROCKS AND VEINS. 117 9. The discovery of rich veins in a new country is a matter of luck. The crowd drawn by the story makes a careful and extended search (prospecting) and is followed by the general settler. In a few years, the treasure found, has added a rich and populous state to civilization. The words California, Colorado, Australia, Transvaal, all tell the same story. In Antiquity, similar effects of mining are recorded. 10. One of the most remarkable stratified rocks is stone coal, H 2, G 1.5 and less, black combustible (p. 48). Anthra- cite (hard coal) gives no volatile matter (bitumen) when heated in a tube; the other coals give up to 50 per cent, bitumen, and burn with a luminous flame. Asphaltum and Petroleum are essentially natural bitumens, with but little fixed carbon. Stone coal supplies our industries with heat and power; largely replacing the slave labor of earlier civiliza- tions. The United States produced 265 million dollars worth of mineral combustibles in 1895 — as much as their total pro- duction of metals. 11. Iron ores also occur as rock deposits. The magnetite (p. 52) and hematite deposits of Elba formed the center of metallurgy of Antiquity. We have' corresponding deposits in Missouri (Iron Mountain, Pilot Knob) and especially on Lake Superior (Marquette Region). In parts of England, iron ore, coal and flux occur in neighboring strata, greatly favoring the smelting of the iron. 12. Salt is obtained by the evaporation of sea water (France, p. 50, top) ; from salt springs (Michigan, New York) ; and above all as rock-salt. The Stassfurth rock-salt deposit is over three thousand feet thick. That at Vilisca — over one thousand feet thick— has been mined for centuries. At Cor- donna, Spain (p. 50), rock-salt is q.uarried from a deposit reaching over five hundred feet above ground. These deposits are aijsociated with gypsum and other salts of sea water, proving them to be the result of evaporation of bays of a primeval ocean, or inland lakes (Dead Sea, Great Salt Lake). 13. SALTS AND SPIRITS. 1. The ancients distinguished a number of substances re- sembling rock-salt in appearance, solubility, and marked by some peculiar taste ; the term SALT has been used to designate all materials of this kind. The most important salts have been in use for two thousand years ; surely, every student of chemistry should be able to recognize them. 2. Already the Hebrews used two very soluble salts effer- vescing with vinegar. Neter (to effervesce) was found in lakes of northern Africa, and is permanent in air; we call it SODA. The other, borith, was obtained by lixiviating wood ashes; it is our very deliquescent POTASH. Both of these substances are non volatile or fixed. A very volatile salt of this kind (spiritus urinse) was at an early day obtained from putrid urine; we call it Ammonium Carbonate, and obtain it from stone coal (gas works refuse, tar water). 3. ALUM is a styptic salt. When heated in a tube it gives off much water and leaves a light, white, ash -like residue, called burnt alum. Accordingly, the ancients said alum con- sists of water and earth. The old VITRIOLS (glass-like) are similar salts, styptic, but heavier and yielding much less water; the one is pale GREEN and gives iron before the blowpipe, while the other is deep BLUE and yields copper.. Pyrites weathering give green vitriol, while blue vitriol results from the weathering of copper pyrites (9. 8). 4. Our nitre or SALTPETRE (sal petr«) was found as crusts on rocks in caves of Asia Minor; it is distinguished from the preceding salts by violently deflagrating on glowing charcoal, showing its leading character of supporting combus- tion. BORAX on the contrary, melts quietly to a colorless drop or bead; it readily dissolves metallic ashes, forming characteristic colors therewith. It is also a most useful flux in smelting. SALTS AND SPIRITS. 119 5. Limestone when burnt leaves quick LIME, which heats up greatly with water; yielding slacked lime which is slightly soluble in water (Limewater) and very CAUSTIC (corrosive to the skin and organic tissue). While limestones effervesce with vinegar, slacked lime does not. Concentrated solutions of the effervescent soluble salts (2) yield with slacked lime, upon decantation, the most caustic liquids known, the CAUS- TIC ALKALIES. 6. Sal ammoniac first came from Egypt in fibrous cakes., already described by Dioscorides; the crude salt of to-day has the same characteristic fibrous structure. When warmed with slacked lime, pungent spirits of ammonia are abundantly produced and readily taken up by water, giving our Aqua Ammoniae, the volatile alkali. 7. The ancient chemists studied the properties of all ma- terials at high temperatures. They distinguished the very volatile substances as we do. The volatile principle collected in a distilling apparatus they termed SPIRIT, independent of the special property, which might be acid, like vinegar, neutral, like water, or alkaline, like ammonia. Litmus turns red with acids, blue with alkalies, and remains unchanged (blue or red) with neutral substances. 8. VINEGAR (acetum) is the only acid known to the ancients; it resulted from light wines exposed to air, turning sour (vin aigre, french). We have used it to recognize lime- stone, marble, soda, by the effervescence it produces. Vine- gar dissolves lead, yielding SUGAR OF LEAD, readily soluble in water. Such a solution gives an abundant white precipi- tate with vitriol and alum solutions, even when much extra vinegar has been added. None of the other salts show this behaviour ( reaction ) . 9. Alum mixed with nitre and heated gives the strongly acid SPIRITS OF NITRE, our nitric acid — the “first water” of the alchemists. This corrosive liquid stains the skin and wood yellow, and dissolves copper readily, while abundant and 120 LECTURE 13. » very noxious red fumes (rutilant vapors) pass off. Silver also dissolves in this acid, leaving white transparent crystals — lunar caustic, lapis infernalis — our SILVER NITRATE. 10. Alum and salt (murias) heated in the same manner yield the less corrosive SPIRITS OF SALT, our muriatic acid. It is easily distinguished from the preceding acids by giving a white, curdy precipitate with silver nitrate; which precipitate is readily dissolved by aqua ammonia. Accordingly, silver is insoluble in muriatic acid. 11. Mixing both salt and nitre with alum, heat drives off the most corrosive acid, AQUA REGIA, so called because it dissolves even gold, the king of metals. These acids were quite generally used by chemists in the days of Geber, more than a thousand years ago. Aqua regia was called the “second water” by the later alchemists. 12. Intensely heating alum (or any vitriol) alone (or with dried, pure clay) we obtain SPIRITS OF VITRIOL, oui sulphuric acid, or oil of vitriol. It chars most organic materials (wood), and gives the same white precipitate with sugar of lead which we‘ obtained with alum and vitriol solutions. At present, the term spirit is restricted to the distillate from wine and similar liquids; our alcohol is spirits of wine, spiritus vini. Notes. Section ii is in accordance with current information, accept- ing the works of Geber as they exist in latin to be genuine, due to the arab Djaber (eighth century). But Berthelot has published the original text in arabic and finds (Comptes Rendus, T. ii6, p. 1 166-1171; 1S93) that the latin works accepted for centuries as the translation thereof, are works of European chemists of much later date; that the arabs did not add to the chemistry of the Greek school. Consequently, that “ thous- and years ago ” will have to be cut in two, leaving say half a thousand years. 14. SOLUTION AND CRYSTALLIZATION. 1. THE OCEAN is the greatest residual solution on the globe. The taste of its water reveals the presence of common and bitter salts. By evaporation sea-salt is obtained there- from. The great (rock) salt deposits have undoubtedly been formed in bays periodically in narrow communication with the ocean (12, 12; Atlas, p. 50). Seawater contains 3j percent, of salts, varying slightly in different regions. Forchhammer^ 1864. 2. SOLUTION is the conversion of a solid into a liquid by means of a liquid. The liquid used is called the solvent, the liquid resulting is called the solution. The word solution thus is used both for the operation and the result. A solution is saturated, when in contact (aided by repeated shaking) with the finely pulverized solid, it does not take up any more thereof. Concentrated is a solution approximating saturation; dilute when remote from it. Water is the most common sol- vent; alcohol, ether, and other volatile liquids are also used. 3. THE SOLUBILITY of a solid is the weight thereof dis- solved to a saturated solution by a unit of weight of solvent (Gay-Lussac, 1819). It may also be defined as the weight of the solid contained in a unit of weight of the saturated so- lution (Etard, 1894). For practical purposes, the STRENGTH OF ANY SOLUTION (whether saturated or not) is usually given by stating the weight of solid per unit of volume of the solution; that is in milligrammes per cubic centimeter or grammes per Liter. 4. THE SOLUBILITY INCREASES WITH THE TEMPERA- TURE, as shown by the diagrams, p. 70. For alum, nitre and blue vitriol dissolved in water, the increase is very rapid, the Gay-Lussac curves rising steeply. Salt shows but a very slight change in solubility. The Etard lines, p. 71, are straight, or consist of several straight lines, the last section 122 LECTURE 14. (except for sulphates) running to the melting point. All chemistry in the WET WAY is but an application of the facts of solubility. 5. When a given solid is divided, the surface increases rapidly, while the weight remains unchanged. As solution can only take place at the surface of the solid in contact with the solvent, it follows that PULVERIZATION must greatly accelerate solution. Solids are first broken with hammer and anvil, then crushed in a diamond mortar (steel socket with steel pestle), and finally ground thoroughly fine in appropriate mortars (porcelain, agate). 6. WARMING the finely pulverized solid with a reasonable excess of solvent will effect rapid solution of all that is soluble. Any insoluble impurities will remain in the solid state. They can be removed by DECANTATION after the solution has been standing undisturbed to permit the solids to settle; or better and more rapidly, they are removed by FILTRATION through a porous insoluble solid, usually filter paper, supported in a funnel of 60 degrees aperture. 7. A hot, concentrated solution set aside will COOL slowly, and generally soon show the growth of beautiful CRYSTALS, the solubility diminishing as the temperature sinks. With an almost boiling saturated solution of nitre, a half dozen con- secutive crops of bulky masses of silky crystals may be ob- tained by as many consecutive decantations, showing most strikingly the enormous decrease of solubility of nitre upon cooling. 8. While the gradual cooling of a hot, concentrated solu- tion gives rapidly large groups of crystals, the most perfect crystals are generally obtained from saturated solutions by SPONTANEOUS EVAPORATION, in crystallizing basins and dishes of glass or porcelain. On a small scale, watch glasses answer admirably. For work with the magnifier and the MICROSCOPE, a drop of solution on the microscope slide is -sufficient. Creeping is avoided by a line drawn with paraffin. SOLUTION AND CRYSTALLIZATION. 123 9. By careful work a COLLECTION OF CRYSTALS of the more common substances may thus be obtained. The best crystals are comparatively small, and require a magnifier for close study. A trifle of wax, rolled on the head of a pin, serves to support the crystal. The pin stuck into the cork of a speci- men tube mounts and protects the crystal quite nicely. A paper strip as wide as the cork is long, around the tube, forms the proper label. 10. The study of this subject is very much facilitated by procuring at drug stores a few LARGER CRYSTALS that can be picked out from a drawerful of blue vitriol, alum, nitre, yellow prussiate of potash, potassium sulphate, and the like. Rock- candy, in large crystal groups on strings, is also obtainable at candy stores. A few native crystals from dealers in minerals will greatly add to the value of the collection. 11. The operations of solution, filtration and crystallization are employed not only in the laboratory, but in chemical works to obtain pure products from impure raw materials (REFINING). Many of these raw materials are transported from hot or desert regions to Europe and the United States to be refined; salt- peter from India, borax from the dead valley of Arizona (for- merly from Thibet to Venice), Chili saltpeter from South America, raw sugar from the tropics. Alum and blue vitriol works are among the oldest establishments producing pure •chemicals. 12. Most soluble substances are associated not only with insoluble materials removable by filtration, but also with substances merely differing in solubility. The less soluble will crystallize first, the most soluble last; so that by setting .aside of the first crop of crystals, and decanting before the substance wanted is all deposited, very pure materials are ob- tained. This process of FRACTIONAL CRYSTALLIZATION is one of the most simple and effective means for obtaining pure chemical individual substances. 15. CRYSTAL DESCRIPTION. 1. Magnificent specimens of CRYSTALS are found IN' MINERALOGICAL MUSEUMS— and beautiful, though smaller, crystals of the most varied kind are MADE IN THE LABO- RATORIES. But their forms seem bewildering; no two crystals; of the same substance appear to be exactly alike. 2. The ancients were familiar with the large quartz crystals- of the Alps and the splendid blue vitriol crystals made in Spain. Pliny speaks of both; the former he considers ice (KRYSTALLOS, in Greek) so hard frozen that heat cannot thaw it (Hist. Nat. 37, 9), the latter he believes to be a glass vitrum, hence our word vitriol (Hist. Nat. 34, 11). It is only in modern days that the characteristic, fixed features in this form of crystals have been discovered. Accordingly we now can describe a crystal in such a way that its form can be identified and recognized by that description. 3. The Dane STEEN (or Steno) discovered (1669 in Italy) that while the linear dimensions of the six-sided quartz crys- tals varied infinitely (see p. 65) the angles between adjacent faces of that prism (rr) are constant, always exactly 120 degrees. Crystallographically, as to these INTER-FACIAL ANGLES, the quartz prism therefore is a REGULAR hexagon of 120 degrees. ROME DE LTSLE (p. 54) and especially HAUY (p. 55) have laid the foundation of crystallography upon this law of Steno. 4. A CRYSTAL IS A POLYHEDRON FORMED SPON- TANEOUSLY. This is the best and most simple definition that can be given. Its expresses the two fundamental facts, that crystals are bounded by plane surfaces called faces, and form without external influences, the substance being left en- tirely to itself. The line of intersection of two faces is called an EDGE. The point where three or more faces meet is- called a CORNER. CRYSTAL DESCRIPTION. 125 5. Three or more faces having their edges parallel consti- tute a ZONE or PRISM. This prism is limited or cut off by ■one or more faces. If one face, it is called the BASE— right if at right angles to the. edges, oblique if not. If the prism is cut off by two faces under an angle, as the roof on a house, these faces are called a DOME, also right or inclined, accord- ing as the ridge is perpendicular or not to the edges of the prism. If limited by three or more faces, the prism is said to be surmounted by PYRAMID. 6. The general appearance of a crystal is distinguished as TABULAR or PRISMATIC, according as two dimensions or one only predominates. If a corner or edge is replaced by a face, it is said to be TRUNCATED. If an edge is replaced by two faces, it is BEVELLED. The general predominance of a par- ticular set of forms is called the HABITUS, and depends on the special conditions under which the crystals grew. See 10, 9. 7. The interfacial angle of »a crystal can be determined . with sufficient accuracy for all purposes of identification by my diagram GONIOMETER (p. 68) for student’s use. Hold the edge of the crystal so that it appears as a point, and the two faces as lines — then the edge will be vertical to the paper goniometer, and it will be easy to find the angle most nearly identic with the interfacial angle concerned. 8. The crystal is held mounted on a pin or by means of forceps, and the eye may, for small crystals, be assisted by a magnifying glass of low power, that is, if long focus. Both large and small crystals are readily measured in this manner. After some practice, the nearest degree can be ascertained, though in description the TENTH of a degree will be stated for reference. Thus calcite is about 105 degrees; exactly 105.1 degrees. 9. BLUE VITRIOL (p. 68) crystals show the dominant zones MT 123.2, PT 127.7 and MP 109.2. In the first zone the faces n, I, r replace edges, so that Tr 110.2, Tn 148.8, Mr 126.7. Also Pn 120.8 and Pr 103.4. 126 LECTURE 15. Special characters: Crystals tabular after M; face T looks rectangular; face N is frequently striated parallel to edge MT ; and face P in coarse crystals shows curved projections due to disturbed rapid growth. These forms are evidently triclinic, destitute of symmetry; 10, 3, note. 10. Nitre (p. 68) forms right prisms, M M'b, very nearly hexagonal; MM' 119.4, Mb 120.3. The right dome D meas- ures 109.8 and Db 125.1. Crystals often tabular after b. ALUM is octahedral (O) with corners (hexahedron, H) and edges (dodecahedron, D) truncated. OO 109.5, OH 125.3, OD 144.7, and HH 90.0, DD 120.0 Crystals commonly grow resting on a face of the octahedron, and thus show rhombo- hedral appearance, the three D forming a rhombohedron of 120 and the three H one of 90 degrees. 11. THE FERROUS SALT (hydrated ammonio-ferrous sulphate) forms tabular crystals, the oblique base P dominat- ing and striated. The prism MM' about 109, and MP=M'P about 105 degrees. The characteristic triangular truncatures q form Pq about 155 degrees. These crystals form very readily by mixing strong. solutions of ammonium sulphate and of ferrous sulphate (green vitriol) ; even a drop each on the microscope slide will suffice. This double salt is permanent in air; green vitriol is not. 12. The ferrous (pale green) solution may be replaced by nickel (deep green), cobalt (pink), manganese (pale rose), copper (deep blue), or the colorless solution of magnesium, zinc or cadmium sulphates. In all cases, these solutions will, with ammonium sulphate solution, give crystals of the same general form and nearly the same angles; such compounds are called ISOMORPHOUS. The habitus may be more prismatic or more tabular, according as MM' or P dominates. Isomor- phism was discovered by ElLHARD MlTSCHERLlCH (1794- 1863) ; portrait p. 34. 16. MARBLE AND FIXED AIR. 1. CALCITE in all its natural varieties, down to the common limestone, has the property of promptly effervescing with vine- gar ; a drop of vinegar placed on the specimen produces the ap- parent boiling up (11,9). In a test tube this shows better; in large cylinders and flask the phenomenon becomes very strik- ing. It is also advisable to take a common mineral acid, like muriatic or nitric acid instead of vinegar. Sulphuric acid cannot be used, giving a precipitate with lime solution. 2. TO STUDY THE GAS set free in this effervescence, it is necessary to produce it in quantity and to collect it. The most convenient generator is Kipp’s, because it will yield the gas exactly as it is required. The upper compartment is charged with clean fragments of marble as large as can be in- troduced through the tubulature. The acid is dilute muriatic, 3 water to 1 acid. We remove the lower glass stopper, re- place it by a rubber stopper (well tied or wired) connected with rubber tube, as shown. Then the pressure can be promptly released at the close of the working hours. 3. THE GAS is drawn by slightly turning the delivery stopcock. It may be collected in cylinders over the pneu- matic trough or in empty gas washing bottles; best the Drechsler form made entirely of glass. A series of such cylindrical washing bottles may be connected by rubber tubes and thus the different reactions of the gas shown at one view. These cylindrical bottles are easily detached by the ground joint, so that the reagents can be introduced at any time. 4. COLOR, ODOR, TESTS. The gas collected over the water or in the washing cylinders cannot be distinguished by sight from the air surrounding the apparatus — it is colorless. Nor has the escaping gas been recognized by odor — it is odor- less. In a wash bottle containing blue litmus, a wine red tint 128 LECTURE 16. is produced as the gas passes through— it is soluble in water, and that solution is an acid. In another cylinder, lime water becomes turbid (white precipitate), which increases in amount, finally diminishes again, and dissolves. 5. This solution, exposed to the air in a shallow vessel, gradually deposits microscopic rhombohedral crystals, exactly of the same form as the calcite rhombohedron of 105 degrees. They effervesce with acids, give the orange tint to the blow- pipe flame, exactly as calcite; they are ARTIFICIAL CALCITE. They show beautiful colors in the polarizing microscope. 6. THE GAS IS decidedly HEAVIER THAN atmospheric AIR; for it can be poured out of one vessel into another, exactly like water. A little lime water in the lower vessel becomes turbid, especially after shaking. A burning taper at the bottom of the lower cylinder will be extinguished, as the gas is poured into that cylinder — the same as if the taper were lowered into a vessel filled with the gas. The gas does NOT SUPPORT COMBUSTION. 7. PROPERTIES. The gas set free by an acid acting on calcite thus is colorless, odorless, heavier than air, does not support combustion; it is soluble in water, forming an acid, makes lime water turbid, an excess redissolves the precipitate, .and from that solution the original calcite deposits in perfect rhombohedral crystals. This gas is evidently contained (fixed) in all forms of calcite; it was called FIXED AIR by Black of Edinburgh (1755), who first most thoroughly studied it. 8. This gas was first produced by VAN HELMONT (1577- 1644), who introduced the term GAS; really spirit, ghost (engl.), ghoast (dutch), geist (german)-, gast (anglo-saxon). He called it gas sylvestre (spiritus sylvestris) or wild, savage gas, because he was unable to tame and control it, so as to collect and handle it. (See portrait, p. 30). Since Black, it has been called carbonic acid — but the dry gas itself has no acid properties. Then it was called carbonic anhydride, and MARBLE AND FIXED AIR. 129 now it is quite learnedly called carbon dioxide! Bergman (1774) called it acidum aereum. 9. BURNING CHARCOAL in a current of air, the product of combustion will show all the properties of fixed air; hence, fixed air contains carbon. In this experiment the charcoal is heated in a tube of Bohemian glass connected with the Drechslers, which are attached to an aspirator, producing the current of air. Air exhaled shows like properties; so does air from fermenting grape juice. 10. Fixed air has been LIQUEFIED to a limpid, colorless liquid by cold and pressure (Faraday, 1823); but no amount of pressure will liquefy it above 31 degrees. That is, above 31 degrees it is a true, non -liquefiable gas; below 31 degrees it is a condensable vapor. This limiting temperature be- tween vapor and true gas is called the CRITICAL TEMPERA- TURE. The pressure sufficient to liquefy it at that temperature is 73 atmospheres. At — 78 degrees, fixed air CRYSTALLIZES to white, snow-like masses (Thilorier, 1835). 11. LIQUID FIXED AIR (liquid carbonic acid) is now pro- duced in chemical works and sold in steel cylinders to various industries. The solution of fixed air in water, made strong by using from 2 to 5 atmospheres pressure, is used as a refresh- ing beverage (soda water) ; it is also produced in the portable fire-extinguishers and chemical fire engines. Many natural spring waters are also stron'gly carbonated, that is, impregnated with fixed air. 12. RAIN DROPS ABSORB FIXED AIR while falling, and while sinking through the soil. Reaching the rocks below, the water will slowly dissolve limestone, become hard — de- positing kettle stone when boiled. Such rock-water, reaching fissures or cavities, will lose its fixed air and deposit the lime- stone it. held in solution as calcite, often finely crystallized. Thus chemical changes (METAMORPHOSES) are going on in the depths of the earth. 17. ZINC AND INFLAMMABLE AIR. 1. Iron is insoluble in water; iron pipes are used for water conduits in cities. But if to the water standing over scrap iron, oil of vitriol be gradually added, effervescence will promptly start up; an inflammable gas of unpleasant odor will escape in abundance. Paracelsus (1493-1541) has first described this quaintly: Air rises and bursts forth like a wind. BOYLE (1626-1691) first collected this gas. See portrait p. 21. 2. Cavendish (1731-1810) first carefully studied this gas which he called INFLAMMABLE AIR. He found it colorless and odorless (when pure); the lightest of all gases (1765); inflammable, producing water when burning. With air it forms an explosive mixture. Hence, great care is required when handling this gas near any flame; the explosions are violent, so much so that Lemery thought (1675) thunder due to the “ fulminations ” of this gas. 3. TO GENERATE INFLAMMABLE AIR in quantity, charge a Kipp with ordinary granulated zinc and dilute muriatic acid. Collect a cylinder full (100 or 200 cc) over the through, and carry the filled cylinder to a flame — the gas will explode. Let the Kipp be emptied a few times, filling up by closing the stop-cock. Trying another cylinder of the gas now collected, it will burn quietly, without explosion ; this is a sign that the gas is free from air. 4. THE EXTREME LIGHTNESS of the inflammable air is shown by holding a cylinder containing air for a few moments over a cylinder containing the gas, and now trying both at the flame, the gas in both will burn with explosion. Careful determinations have shown that under ordinary conditions (of temperature and pressure) twelve cubic centime- ters of inflammable air weigh one milligramme (0.083 mgr. per cc). ZINC AND INFLAMMABLE AIR. m 5. The gas generated from zinc has not as unpleasant an odor as that generated from iron; it is less impure. TO PURIFY A GAS it must pass slowly through absorption and washing tubes, containing the proper absorbents. If these are in the liquid form, it requires pressure to force the gas through; hence, it is generally preferable to soak fragments of pumice with the absorbent liquids and pack these frag- ments in cylinders. 6. The most effective ABSORBENTS for purifying inflam- mable air are lead and silver solutions (removing the odorous gases), caustic potash solution (removing traces of acids) and concentrated oil of vitriol one of the most effective dryers, being strongly hygroscopic. 7. For such purposes the Drechslers are not applicable. We generally use cylinders of glass, on foot, so they will stand firmly, and provided with a tubulature in a lower division, separated from the main upper parts by a narrow contraction, preventing the fragments of pumice from falling. Connection is made by rubber stopper and glass tubing at the top opening and at the tubulature below. A number of such cylinders are used in series. 8. If the inflammable air is carefully dried so that it will pass through a tube surrounded with fragments of ice without depositing moisture in the same, it can be connected with a small burner (like the microchemical burners) and, after due precautions, the jet may be lit. IT WILL BURN with a pale, very hot flame. A bell glass held over the flame will bedew, and WATER will soon run in drops down into a plate placed to receive it. 9. Since inflammable gas produces or generates water (Greek: hydor) when burning, it was called HYDROGEN by Lavoisier -(p. 19). The chemical symbol of hydrogen is FI. Experience has shown that HYDROGEN IS CLOSELY RE- LATED TO THE METALS, several of which form genuine alloys with it. Palladium absorbs a thousand times its own 132 LECTURE 18. volume of hydrogen (Graham) ; it is used in gas analysis to remove hydrogen from other gases. 10. In recent days, since very low temperatures have been produced on a sufficiently large scale, it has been found (Olszewski, 1895) that the CRITICAL POINT of hydrogen gas is at 234.5 degrees below the freezing point, and that the critical pressure is 20 atmospheres. Below this temperature hydrogen is a vapor, liquefiable by an increase of pressure. 11. Any of the acids can he used instead of muriatic, es- pecially nitric, sulphuric and even acetic. THE METAL§ THAT DISSOLVE more or less readily IN some of these DILUTE ACIDS are, in addition to iron and zinc: Magnesium, aluminium, cadmium, nickel, cobalt, lead. The special con- ditions of solution will be studied in due season. Lead is insoluble in both muriatic and sulphuric acids. 12. In many cases, especially where sulphuric acid has been used, CRYSTALS FORM, in which the blowpipe readily detects the metal originally dissolved. Some of these crys- tals, especially the sulphates, contain water of crystallization, easily driven off by heating the crystals in a glass tube. 18. SUBSTITUTION BY SOLUTION. 1. THE CONTRAST between the solution of marble and metals in ACIDS and salts in WATER must have become apparent. When the salt dissolves in water nothing escapes, and upon evaporation, the original salt is reproduced, fre- quently in crystals. When the metals dissolve in acid, a gas escapes, a new substance forms, no longer the metal, but containing the metal, as proved by means of the blow-pipe. 2. Accordingly we have two different kinds of solution, simple and CHEMICAL SOLUTION, also distinguished as solu- tion and dissolution. The first is largely physical in its nature; the second is entirely chemical, the original sub- SUBSTITUTION BY SOLUTION. 133 stances both disappear and are replaced by two new and totally different substances. Thus we have entered the very center of CHEMISTRY IN THE WET WAY. 3. In the solution of any metal in a dilute acid, HYDRO- GEN GAS is always produced. The solution obtained in many cases — detailed directions belong to practical chemistry — crystallizes, in all cases can be evaporated to dryness, so that the new salt is obtained by itself, free from water and any excess of acid — the last best avoided by having an excess of metal, and decanting the solution. IN THE SALT, the blowpipe readily detects THE METAL used and dissolved. 4. For example, in the preparation of hydrogen gas by means of zinc and dilute sulphuric acid, we obtain the gas and a white crystallized salt containing zinc; this salt is iden- tical with common white vitriol. A solution of this salt gives an abundant white precipitate with lead acetate, precisely as does the acid used; it contains, therefore, the essential or chemical characteristic part of sulphuric acid. Hence, it is termed a sulphate, namely ZINC SULPHATE. 5. The chemical solution considered may now be repre- sented thus: Zinc and sulphuric acid give hydrogen gas and zinc sulphate. Evidently the hydrogen must have formed part of the sulphuric acid. It is known to be metallic in its real nature (17.9). We have here apparently an exchange of metals, hydrogen for zinc; consequently the acid itself must be hydrogen sulphate. In other words, the ACID IS A HYDRO- GEN SALT, exactly as white vitriol is a zinc salt, the salt of a metal. G. The above REACTION— that is chemical action — be- tween the metal and the acid may therefore be written as follows: Zinc and hydrogen sulphate give hydrogen and zinc sulphate. Such a reaction in which any substance A takes the place of any other substance B in any combina- tion, setting free this second B, is called a SUBSTITUTION. The above reaction is the substitution of zinc for the hydrogen of the acid. See blackboard diagram. 134 LECTURE 18. 7. Having studied the qualitative side of this fundamental reaction, we must next try to determine the QUANTITATIVE RELATIONS of the same. The merest trials show that with- out weighing the quantities used, there either remains metal or acid in excess. To obtain the best salt it is generally advisable to have an excess of the metal, decanting the liquid when th^ reaction ceases and setting the liquid aside to crystallize. 8. First, TO DETERMINE THE AMOUNT OF HYDROGEN GAS the latter must be measured in a gas burette. The evo- lution tube is charged with an excess of the acid and the accurately weighed metal— the latter held on the slanting walls of the dry, inclined tube above the acid. When the burette is properly adjusted, the operation is started by simply bringing the evolution tube to a perpendicular. 9. MAGNESIUM ribbon is specially convenient for these determinations. It is found that a cubic centimeter of hydro- gen gas is produced for each milligramme of magnesium used, very nearly. As 12 cc hydrogen gas weigh one milligramme (17.4) THE UNIT OF ONE MILLIGRAMME OF HYDROGEN IS EQUIVALENT TO TWELVE MILLIGRAMMES OF MAGNE- SIUM. 10. Repeating the experiment with zinc we find that it requires nearly 32 mgr. of zinc to give 12 cc gas representing 1 mgr gas, at the same time (under same pressure and tem- perature). For iron the equivalent number is 28. For alum- inium — easiest dissolved in an alkaline liquid (13.5) — the equivalent is found to be 9. Accordingly 1 of hydrogen (by weight) is equivalent to 9 Al, 12 Mg, 28 Fe, 32 Zn (really 31.75). These numbers are called the CHEMICAL EQUIVA- LENTS of the metals. 11. Careful experiments, on a small scale with accurate weighings, show that PER UNIT of weight of metal dissolved in sulphuric acid, THE CRYSTALLIZED SULPHATES WEIGH: For Mg, 10.25; Fe, 4.96; Zn, 4.38; Cd, 2.49. If carefully heated to drive out the water of crystalization, the residual SUBSTITUTION BY SOLUTION. 135 anhydrous sulphates weigh respectively 5.00, 2.71, 2.46 and 1.85 times as much as the metal used. Lead converted into nitrate weighs 1.60, into crystalized acetate (sugar of lead) 1.83 per unit. 12. Careful experiments of this kind also permit the deter- mination of the CHEMICAL EQUIVALENTS OF THE ACIDS themselves. Thus, since 1 Mg gives 5.00 dry sulphate, the equivalent 12 Mg gives 60 Mg S^te, in which the non-metallic matter (the S^te) is 60-12=48. But the acid contains H=1 as metal or instead of the metal. Hence, the chemical equiv- alent of sulphuric acid, H is 49. In a like manner, the equivalent of nitric acid is found to be 63, and thaf of muri- atic acid, 36.5. 19. SOLUTION OF SILVER AND GOLD. 1. Dilute sulphuric or muriatic acids have no effect what- ever on copper, mercury and silver, nor on gold and platinum. All these metals are insoluble in dilute acids. But when heated with CONCENTRATED sulphuric ACID, the first three dissolve, yielding a noxious gas having the odor of burning sulphur; the last two, gold and platinum, remain insoluble even in boiling concentrated sulphuric acid. 2. Very dilute nitric acid, in the cold, has but little action on the first three metals (Cu, Hg, Ag), but when the acid is reasonably strong — say 10 per cent. — it acts quite promptly, especially when moderately heated. While the metals dissolve, a very noxious reddish gas (RUTILANT VAPORS) is produced in abundance. 3. The rutilant vapors invariably make their appearance when strong nitric acid exerts its dissolving influence. When a filter paper or sponge with aqua ammonia is brought near, ABUNDANT WHITE CLOUDS take the place of the noxious vapors, which evidently combine with the ammonia to a white solid. In this way, the solution may be effected in a room not provided with hood. 136 LECTURE 19. 4. Nitric acid (AQUA FORTIS), even when boiled, has no effect on gold nor on platinum; they are insoluble in all ordi- nary single acids. In fact, gold is generally separated from its alloy with silver, by boiling the alloy with concentrated sulphuric acid or with nitric acid under conditions established by long practice; the amount of gold present must be less than one -fourth in the alloy. This accounts for the common name of nitric acid in german: Scheide wasser. Compare this wet way process with the dry way separation, 8, 12. 5. AQUA REGIA (4 muriatic with 1 nitric acid) dissolves gold (foil) readily. Both gold and platinum are dissolved by moderately heating them with this acid in large excess. When all metal dissolved, the excess of acid is driven off, carefully avoiding overheating, as that would decompose the MURIATE obtained (test, 13, 10). Dissolving in water, we have the common solutions of these two metals; muriate of gold and of platinum. 6. The nitrates of copper, mercury and silver are readily obtained in crystal form. Silver nitrate crystallizes generally in rhombic tablets, of almost 130 degrees. Silver and its salts are very sensitive to light and to many gases, and even to dust, so that good, colorless (or white) crystals can only be obtained under specially favorable conditions. 7. The nitrate of mercury obtained varies with the con- ditions under which the metal is dissolved. When at com- mon temperature, acted upon by dilute nitric acid, the resulting nitrate is precipitated abundantly by the muriatic acid or by salt; it is called MERCUROUS NITRATE. When the metal is acted upon by reasonably strong acid on the water bath, the resulting nitrate is not precipitated by muriatic acid or salt; it is called MERCURIC NITRATE. 8. The sulphates of mercury show the same difference. Heating the metal with less than half its weight of concen- trated sulphuric acid gives MERCUROUS sulphate; while heating mercury with twice its weight of concentrated acid until the excess of acid is driven off, gives MERCURIC sul- SOLUTION OF SILVER AND GOLD. 137 phate. The distinction is made as before stated; the mercu- rous solutions are precipitated by muriates. The precipitate is CALOMEL; the other muriate is SUBLIMATE. 9. When trying to dissolve the mercuric sulphate, an abundant yellow precipitate — the TURPETH MINERAL — forms, a so-called basic sulphate, while the balance or acid sulphate passes into solution. By adding about 5 per cent (sulphuric) acid to the water, the entire salt will be dissolved, and no yellow precipitate will form. When it has formed, such addition of acid will redissolve it. 10. If the residue from copper and concentrated acid is taken up in warm water, the resulting solution will deposit the crystals of blue vitriol described (15.9). In this manner ALL METALS HAVE BEEN BROUGHT INTO SOLUTION, excepting the modern light metals potassium and sodium (6.12). Greenish iron solutions in presence of nitric acid become reddish; these are called FERRIC, the original greenish FERROUS. 11. THESE SOFT METALS have to be kept in well stop- pered bottles under pure naphta, and even then their surface soon looks dull and corroded. When freshly cut with a knife the surface looks brilliant white like silver. Thrown on water the metal floats, melts (round globule) and burns with a pur- ple (Ka) flame, finally exploding; hence, the experiment must be made in a deep beaker with but an inch of water. Sodium is less violent; burns with yellow flame. 12. The solution so obtained is strongly alkaline. Evapo- rated to dryness and fused, the CAUSTIC ALKALIES are obtained. Made carefully in a large nickel crucible, the ex- periment yields 1.7-1 of caustic soda, 1.43 of caustic potassa per unit- of metal. It may also be added that a UNIT WEIGHT OF METAL GIVES 1.44 Ag Sate, 1.57 Ag Nate, 1.60 Pb Nate, 3.94 blue vitriol, 1.48 mercuric sulphate; 1.24 mercurous sulphate; 1.18 calomel and 1.35 sublimate. Accordingly, the EQUIVALENT of SILVER is about 108, of lead 104. See 18, 12. 20. REDUCTION IN THE WET WAY. 1. The four solvents used for the solution of the metals are water, dilute acids, concentrated (single) acids and aqua regia. The type metals, soluble in these solvents, are POTASSIUM, ZINC, SILVER and GOLD. To the most soluble group belong Ka, Na, as shown; also Ca, Sr, Ba. Insoluble in water, soluble in dilute acid are: Mg, Al; Zn, Fe, Pb. Requiring a concentrated acid are: Cu, Hg, Ag. Requiring aqua regia: Au, Pt. 2. In each of the four groups, the metals have been enumerated according to their DEGREE OF SOLUBILITY. Thus, experience shows that Mg is clearly the most soluble, Pb the least soluble, of those mentioned in the second group; also Zn more soluble than Fe, but less soluble than Al and Mg. 3. But if into a blue copper solution a piece of iron be thrown, the iron will become covered with red copper and the solution will loose its fine blue color, soon appearing colorless; if exposed for hours to the air, the iron now in the solution will show a rust- like precipitate. Evidently, the more soluble iron has taken the place of the less soluble copper in the solu- tion. We have a substitution of iron for copper. 4. This rule is general. A MORE SOLUBLE METAL WILL TAKE THE PLACE OF ANY LESS SOLUBLE METAL IN A SOLUTION. A gold solution will deposit its gold upon a piece of metallic silver and be changed to a silver solution. This silver solution will surrender to mercury, a mercury solution to copper, the latter to lead, the lead solution to zinc. 5. THIS REDUCTION OF THE METALS IN THE WET WAY finds important applications in the arts as well as in the laboratory. Copper-waters issuing in mining regions are run into large reservoirs, and old iron thrown in; after some weeks this iron seems to have been converted into copper. (Hungary) . REDUCTION IN THE WET WAY. 131) 6. In the laboratories, the most elegant and conclusive TEST FOR METALS IN THE WET WAY is this very reduc- tion by substitution. A drop of the solution to be tested is placed on a microscope slide, and a minute clipping of a more soluble metal (generallyzinc) placed in that drop. Almost instantly the substitution takes place, beautiful crystals of the metal in solution growing as it were out from the zinc, form- ing elegant groupings. 7. Even the alchemists were familiar with these reactions, though some are believed to have considered these simple substitutions evidences of transmutation of copper into silver, of zinc into lead. A dilute lead solution with brass wires and a fragment of zinc, gives the old arbor saturni (LEAD TREE) brilliant crystals of pure lead coating the wires like leaves and branches on a tree. A silver solution with mercury gives arbor dianas, the SILVER TREE, growing up from the mer- cury. 8. By putting a weighed amount of the more soluble metal into an excess of a solution of the less soluble metal, an EQUIVALENT amount of the latter will be precipitated and can be weighed after proper separation and drying. However, for several pairs of metals it is difficult to get accurate results, the metals changing too readily. 9. It is found that the silver precipitated weighs exactly nine times as much as the magnesium used; hence the chemical equivalent of silver is 9 times 12 or 108. For every unit of copper thrown into a silver solution, 3.39 units of the latter are obtained from its nitrate solution, especially if the solution is kept in a cool place. The equivalent of cop- per, therefore is 108, divided by this number, or about 31. G. Silver thrown into -a gold solution gives the equivalent of gold about 66. 10. THE CAUSE of these substitutions is given by the facts of solubility of the several metals taken singly. Thus, copper does not dissolve in dilute sulphuric, while zinc does 140 LECTURE 21. so readily. If copper and zinc together are thrown into the same dilute acid, the zinc will dissolve, the copper not. There can be no question about these facts. Surely, zinc is much more soluble than copper. 11. Now if metallic zinc be thrown info a solution of blue vitriol, we have THE SAME THREE BODIES — zinc, copper and the dilute acid — in the same dish and the same final result ought to be Obtained, a zinc solution with metallic cop- per. Such is actually the case; zinc displaces the copper from its solution because zinc is much more soluble than copper. 12. The common talk about CHEMICAL AFFINITIES of these metals is nothing but reasoning in a circle, and the attempt to hide this false reasoning by the introduction of the high sounding term. If zinc has greater affinity for the acids than the copper, nobody knows of that except by the very experiment which it was attempted to explain. 21. SULPHUR AND SULPHIDES. 1. Sulphur was known to the ancients. Already, Homer speaks of the purifying effects of burning sulphur (fumiga- tion). Its faint blue flame imparts pallor to the face in the dark. Hence, the ancients burnt sulphur at certain religious ceremonies. 2. THE OLD CHEMISTS detected sulphur in many ores which upon heating in the open fire, emit the odor of burning sulphur abundantly (9. 3). These ores generally having me- tallic luster, the ancients smelting metals from them, concluded that sulphur is a constituent of metals themselves. Tb change baser metals to gold seemed to the alchemist to involve simply a removal of sulphur or something like sulphur. 3. SULPHUR continues to be a most important substance to CHEMICAL INDUSTRY. About 400,000 tons, worth 10 SULPHUR AND SULPHIDES. 141 million dollars, of native sulphur are produced yearly in Sicily alone, where 25,000 laborers dig for it. For many purposes the sulphur of ores is also available. Pyrites contain about 50 per cent, of sulphur, and occur in immense deposits (9. 8). 4. Native sulphur is a yellow solid, hardness, and gravity very near 2. Its luster is peculiar, resinous. It is a very poor conductor for heat and electricity, and very brittle. Fine specimens (crystals) are' transparent. It is readily fusi- ble (113 degrees), and on boiling (about 450 degrees) forms a brownish red vapor, which condensed gives flowers of sul- phur as sublimate. Melted sulphur, cast in forms, gives roll- sulphur. At about 200 degrees melted sulphur becomes viscid; above that temperature, it gets limpid again. 5. . Sulphur when absolutely pure has no odor, not being volatile at common temperatures. When heated in the open vessel, it burns with a pale blue flame (250 degrees) far be- low its boiling point; the gas produced is suffocating, of the familiar and characteristic odor of burning sulphur. Sulphur is not soluble in water, but quite soluble in essen- tial oils, from which it crystallizes in the forms exhibited by native sulphur. 6. NATIVE SULPHUR CRYSTALS from Sicily (see p. 69) are very beautiful and often quite large. They are (stable or permanent) rhombic octahedr^; OO' 106.6; sharp edge 85.0; lateral OO" 143.3. Quite generally the sharp corners are truncated by the base P, forming PO 108.4. The sharp edge CB is also frequently truncated by the face q, for which Pq 117.8, Oq 132.5 and mutually over middle edge, qq' 124.4. Finally the edges PO are often truncated by an obtuse octa- hedron 0 , for which Po 134.5. The basal rhomb has 101.8. These faces are readily identified even on small crystals from solution. 7. MELTED SULPHUR CRYSTALLIZES (p. 69) upon cool- ing, forming (unstable) nearly square prisms MM' 90.6, cut off 142 LECTURE 21. obliquely by the base P, so that Pa 95.8, the face a replacing the edge MM'. The lateral corners are often replaced by the triangular faces q, while PM may be truncated by the octa- hedral 0 . Characteristic angles are MP 94.1; Ma 135.3. Pq 135.1; qq' over P 90.3. These dimensions are easily identified. Showing two different crystal forms, sulphur is said to be DIMORPHOUS. 8. SULPHUR melted or as vapor COMBINES WITH many METALS to new bodies, called SULPHIDES. Several of these artificial sulphides are identic with native sulphides. Copper — in foil or turnings — when reached by the vapor of boiling sulphur, burns brightly. The malleable copper used is thus converted into a very brittle blueish black sulphide. 9. Mercury, silver, iron, lead, zine and most other ordinary metals combine in a like manner with sulphur. The coarsely divided metals (filings, turnings, thin foil, etc.) need only be melted with sulphur in a crucible. Melting together equal weights of iron and sulphur gives the BLACK IRON SULPHIDE, very much used in chemical laboratories; it is distinguished as FERROUS SULPHIDE from the native yellow iron sulphide, pyrite (9, 8). Iron filings mixed with flowers of sulphur, and moistened, also give ferrous sulphide — the mixture may even inflame (Lemery’s Volcano) . 10. DUMAS (portrait p. 25) exposed pure silver foil in a combustion tube to the vapors of sulphur, and obtained finely crystallized silver sulphide. He found 1.148 of sulphide per unit of silver used. The increase of 14.8 per cent, of silver (equivalent 108) gives 16 as the chemical EQUIVALENT OF SULPHUR. 11. If fragments of charcoal are heated in a combustion tube while vapors of sulphur are passed over them, a very volatile, highly inflammable liquid is formed, which will con- dense in a cooled receiver. It is called CARBON BISULPHIDE, and is the best solvent for sulphur, taking up nearly half its SULPHUR AND SULPHIDES. 143 weight at common temperatures. From this solution, splendid sulphur crystals can be obtained. 12. GUN POWDER IS A MIXTURE of sulphur, carbon and nitre in the proportion 1: 1: 6. Washing with water removes the nitre, the identity of which will be revealed by its prismatic crystal form, (15, 10). The well dried residue yields sulphur to the bisulphide, from which fine crystals readily deposit, showing the octahedron O, the base P, and frequently the truncature q, all readily identified by the figures given, using a magnifier. Insoluble, black carbon finally remains. Thus the gun powder was ANALYZED, separated into its constitu- ent parts. 22. HYDROGEN SULPHIDE AND METALS. 1. Ferrous sulphide (21.9) covered with almost any diluted acid, gives strong effervescence, both in bulk of gas produced and in odor. The latter is that of rotten eggs. This reaction or chemical process is readily understood. The acid, say H Muriate with Ferrous Sulphide gives HYDROGEN SULPHIDE GAS and Ferrous Muriate remains in the green solution. Rouelle first noticed this gas, which Scheele soon after studied thoroughly. 2. In this reaction, the substances taken, H Mr^te and Fe^us Side, yielding Fe^^s Mr^te and FI S^^® gas, have evidently interchanged their constituents. They are said to have under- gone DOUBLE DECOMPOSITION— in this case by VOLATIL- IZATION, the product being a gas. Such reactions are very common in chemistry. 3. HYDROGEN SULPHIDE GAS is quite soluble in water, to which it imparts a strong and highly characteristic odor. When left exposed to the air, such sulphuretted water soon becomes opalescent, and gradually a white deposit forms — this is finely divided sulphur (white streak, substance yellow). Some springs produce such sulphuretted water in abundance, and are very valuable medicinally. 144 LECTURE 22. 4. Silver coin and ware, especially when moist, turns black when exposed to the gas or the water; lead paint and compounds of lead, bismuth, silver and other metals, also turn promptly brown or black. Accordingly, hydrogen sulphide is a most IMPORTANT REAGENT by means of which heavy metals can be recognized. During working hours, the chemi- ical laboratories keep this gas on tap in a large Kipp genera- tor for constant use. 5. A lead solution of ordinary working strength — say one per cent — is perfectly colorless and transparent. A few bubbles of the hydrogen sulphide gas passed into it almost instantly blackens it, forming an abundant black precipitate of Pb Side, settling soon to the bottom. Even when extremely dilute, a brownish coloration will be produced in lead solution by H Side gas. This gas is the most sensitive reagent known for lead in solution. For this reason, lead solutions are replaced by barium solution as reagent for sulphates (13, 12). 6. The black lead sulphide PRECIPITATE being solid, may be readily separated from the liquid by FILTRATION, and by WASHING, best adding a little hydrogen sulphide to the wash water; drying then removes both water and excess of hydrogen sulphide. This precipitate is not only insoluble in water but also insol- uble in dilute acids (nitric, acetic must be tried for sulphuric and muriatic produce precipitates themselves, 13.8). 7. This reaction evidently again is a double decomposition, for both substances taken interchange constituents. The lead acetate and hydrogen sulphide gas give lead sulphide and hydrogen acetate (acetic acid). But it differs from the pre- ceding case (2) by the product being an insoluble instead of a volatile compound. The present reaction is therefore a DOUBLE DECOMPOSITION BY PRECIPITATION. 8. It is evident that all SULPHIDES INSOLUBLE IN DILUTE ACID will precipitate by sulphide gas in acidified solutions. The corresponding metals which thus may be HYDROGEN SULPHIDE AND METALS. 145 precipitated as sulphides are, in proper groupings: a) Ag Hgous, pb; b, Cu, Hgic. Cd, Bi; c) As, Sb, Sn; d) Au, Pt. They are distinguished a) by precipitate with muriates (their muriates insoluble) ; c and d, the sulphide precipitates soluble in yellow Am Solution of c colorless, d yellowish. 9. YELLOW AMMONIUM SULPHIDE is obtained by satur- ating aqua ammonia with hydrogen sulphide gas, and perhaps dissolving some flowers of sulphur in it. The precipitate is tested while still on the filter, but completely washed with water, so that the washing is entirely free from acid reaction (a drop making no red stain on blue test paper). If the acid were not completely removed, it would decompose the reagent, giving hydrogen sulphide gas and an abundant precipitate of sulphur. 10. The other heavy metals (not precipitated by hydrogen sulphide gas because their sulphides are soluble in dilute acids) do come down when the solution is made ALKALINE by a rea- sonable excess of ammonium hydrate (suificient to give the odor). These metals are f) Zn, Mn, Fe^us, Co and g) Al, Fe’c> Chc- In case of Ferric, the hydrogen sul- phide first makes the solution opalescent (from separation of S) and ferrous, then precipitates this black. H. The two groups f and g are readily distinguished by the latter giving a precipitate by ammonium hydrate after the solution has been treated with an excess (as solvent) of am- monium muriate, while the metals grouped under f do not give a precipitate under these conditions i. e. their HYDRATE is SOLUBLE IN SAL AMMONIAC (or ammonium muriate). 12. THE LIGHT METALS, Ka, Na and Mg, Ca are not pre- cipitated by hydrogen sulphide gas under any conditions, their sulphides being soluble in water. Thus, the metals in solu- tion are almost as readily distinguished by means of hydrogen sulphide gas and a few other reagents as by the blowpipe in the dry way. We shall soon return to this most important subject of CHEMICAL ANALYSIS IN THE WET WAY. 146 LECTURE 22. Note. — The following preliminary tabular exposition of the course IN WET WAY ANALYSIS FOR METALS Comprises only the general reactions determining the groups, and the special features which in these reactions mark the individual members. These are the only reactions sufficiently explained in the preceding. Only one metal is here supposed to be in the solution, which thus contains a simple compound only and is not complex. 1. Solution -f - 11 Mrate — white precipitate — Silver Group I. Pre- cipitate soluble in'much water, Pb ; precipitate soluble in Am Hate. Ag; insol., turning black, Hgous. 2. Solution-j- 11 Sate, white^precipitate. Barium Group, IF. Very dilute solution, no precipitate, Ca; a precipitate forms promptly, Ba, very slowly, Sr. If solution black by H Side, it contains Pb, from r. 3. Acidified (mur) solution, saturated with H Side gas gives a precipitate (other than merely S) . . IH, IV, V. The precipitate washed and treated with yellow Am Side remains insoluble, III; or dis- solves IV, V. III. Copper Group. Original solution blue or green . , Cu. Precipitate first whitish, then yellowish, brownish, finally black . . Hgic; precipitate yellow . . Cd; brown . . Bi. Precipitate soluble in yellow Am Side; original solution color- less, . . IV ; yellow to’brownish . . V. IV. Arsenic Group. — Color of sulphide precipitate yellow, . As ; orange . . Sb; brownish . . Sn. V. Gold Group. — Original solution precipitated brownish by ferrous solution . . Au; yellow by sal ammoniac solution . . Pt. 4. Solution (3) made alkaline with ammonia after adding considerable Am MrMe; a precipitate forms VI or VII. Original solution with excess sal ammoniac, made strongly alka- line with Am Hate, np precipitate, VI; a precipitate VII. VI. Zinc Group. Original solution, deep green, Ni; pink, Co; pale rose, Mn ; pale green, turning rusty, Feo^s; colorless, Zn. Am Side precipitate=white, Zn ; flesh colored, Mn ; black, Feo^s, Ni, Co, distinguished by color of original solution (or dry way borax bead, 6, 1 1). VII. Aluminium Group. Original solution, colorless, A1 ; green, Cr; yellow to orange, Feic. The precipitates have nearly the same colors. 5. If no precipitate obtained : Magnesium group, VIII. Solution with much sal ammoniac, made strongly alkaline with Am Hate; to por- tions of this mixture, add a) Am Cate; a precipitate forms, or at least on adding Am Oxalate . . Ca from H. b) Na pate, white crystalline precipitate . . Mg. HYDROGEN SULPHIDE AND METALS. 147 Original solution or substance, with Ka IDte, odor of ammonia; red paper turned blue . . Am. Flame coloration, persistent and intense yellow . . . Na, purplish, and through blue glass deep reddish . . . Ka. It is understood that the tests are carried on till the substance is found, not beyond (for simple solutions), throughout this course. Thus, if found in reaction i, none of the others is tried; if in 5, reaction gives a precipitate, that ends it. For diagram of this course see p. 73. 23. IODINE AND IODIDES. 1 . Iodine is a solid substance which in many respects re- sembles sulphur, especially in its action on metals. While now in the market of chemicals because of its many applica- tions, it was not known till 1811, when COURTOIS discovered it in ashes from sea weeds. It is mainly obtained from the mother liquors of Chili saltpeter. 2. IODINE is a grayish black solid, sufficiently volatile to make its offensive and characteristic odor perceptible at common temperatures. Its main properties are: G 4.50, F 113 and B 180 degrees. Its vapors have a beautiful deep violet (Greek: iodos) color; hence its name and chemical symbol lo. It is sufficiently soluble in water to tinge it yellow. It is more soluble in alcohol, and abundantly soluble in chloro- form and carbon bisulphide. 3. Both from solution and by sublimation it crystallizes quite readily. On account of its marked volatility, IODINE CRYSTALS are not permanent, but disappear and form again in the containing vessels, according to the changes in tempera- ture. The crystals are rhombic tablets. Compared to the sulphur crystals (p. 69) the angles are OO" 136 and PO 112 degrees. 4. Starch paste is colored deep blue by iodine; the color disappears on heating to about the boiling of water, but promptly re-appears on cooling. This reaction is one of the most delicate or sensitive we have in the wet way. The merest trace of iodine in solution can be revealed by this TEST. One part of iodine in a million of solution will show 148 LECTURE 23. the color with starch paste; in 10 cc of such a solution there is the hundredth part of a milligram of iodine. 5. Passing hydrogen sulphide gas through a solution of iodine in chloroform or bisulphide under water, the intense red color will gradually disappear and the water will become turbid from sulphur. This is evidently a substitution of iodine for sulphur. lo and H Side giving S and H loide. Decant, filter and by gentle heating drive off the excess of H Side, and a strong solution H loide or HYDRIODIC ACID remains. This colorless solution gradually decomposes, setting free iodine, as indicated by the yellow color it assumes. 6. Finely pulverized metallic arsenic thrown into a solution of iodine in bisulphide, combines with the iodine, forming ARSENIC IODIDE, which separates in brick red, brilliant, thin tablets upon the volatilization of the solvent. This As lo^de is readily fusible and volatile; it sublimates without decomposition (Synthesis). 7. Iodine, like sulphur, unites with most metals in the dry way. Heating a glass vessel containing a little mercury, this will deposit, by distillation, in small metallic globules on the inner walls of the vessel. When this has cooled again, heat an equal weight of iodine in the same; as the violet vapors reach the mercury, they combine therewith, forming crystals of MERCURIC IODIDE. 8. Mercuric iodide can be readily moved from one place to another by heat; it will deposit by sublimation on the colder parts of the vessel. At first it forms YELLOW prismatic crystals of 114.5 degress. Gradually it turns BRILLIANT RED; this change may be produced instantly by rubbing the yellow crystals with any hard body (a glass rod). The red crystals are generally tabular, with a pyramid inclined under 1(H). 5 degrees to the base ; hence quadratic (10.3). Mercuric iodide is DIMORPHOUS (21, V). 9. THE SMALLEST TRACE OF MERCURY may be posi- tively IDENTIFIED in the dry way by applying these reactions IODINE AND IODIDES. 149 in a small blowpipe test tube of hard glass, and observing the results with a magnifier and under the microscope. The metal is identified by the distillate consisting of minute white globules, having brilliant metallic luster. The iodide is next formed by synthesis, its colors and crystal forms recognized. This series of tests is important in toxicology. 10. Iron, in the presence of water, combines readil}^ with iodine, forming FERROUS IODIDE, which being freely soluble in water, is purified by simple filtration. See 21.9. With potassium carbonate, Ka C^te, there will form a pre- cipitate containing the iron (as shown by blowpipe) and from the filtrate, permanent CUBICAL CRYSTALS of potassium iodide are obtained. Fe^us loide and Ka give Fe^us c^te (insol) and Ka lo^^^ (sol). By synthesis, the iron takes the iodine, and by double decomposition this is transferred to the potassium. 11. Potassium iodide is the most important soluble iodide; by its means the INSOLUBLE IODIDES are readily obtained as PRECIPITATES from the solution of the metals. Thus Pb loide, yellow; hexagonal tablets readily crystallize from solu- tion in hot' water. FIgic red; first pink, then rose, finally brilliant red; soluble in excess of reagent, Ka lo'^^ to colorless solution. Mercurous solutions give dirty green Hgous loUe as precipitate. Ag lo'^^ is yellowis