THE PRINCIPLES OF CHEMISTRY
George Kamensky translation
By D. MENDELÉEFF TRANSLATED FROM THE RUSSIAN (SIXTH EDITION) BY GEORGE KAMENSKY, A.R.S.M. OF THE IMPERIAL MINT, ST PETERSBURG: MEMBER OF THE RUSSIAN PHYSICO-CHEMICAL SOCIETY EDITED BY T. A. LAWSON, B.Sc. Ph.D. EXAMINER IN COAL-TAR PRODUCTS TO THE CITY AND GUILDS OF LONDON INSTITUTE FELLOW OF THE INSTITUTE OF CHEMISTRY IN TWO VOLUMES VOLUME II. LONGMANS, GREEN, AND CO 39 PATERNOSTER ROW, LONDON NEW YORK AND BOMBAY 1897 All rights reserved
Table III.
The periodic dependence of the composition of the simplest compounds and properties of the simple bodies upon the atomic weights of the elements.
Molecular composition of the higher hydrogen and metallo-organic compounds Atomic weights of the elements Composition of the saline compounds, X=Cl Peroxides Lower hydrogen compounds Simple bodies
Sp. gr. Sp. vol. Melting point
Br, (NO3), ½O, ½(SO4), OH, (OM)=Z, where M=K
½Ca, ⅓Al, &c.
E=CH3, C2H5, &c. Form RX RX2 RX3 RX4 RX5 RX6 RX7 RX8
Oxides R2O RO R2O3 RO2 R2O5 RO3 R2O7 RO4
[1] [2] [3] [4] [5] [6] [7] [8] [9] [10] [11] [12] [13] [14] [15] [16] [17] [18] [19]
HH H 1,005 (mean) HX or H2O H2O2 — *0·05 20 -250°?
Li 7·02 (Stas) LiX — — 0·59 11·9 180°
Be 9·1 (Nilson Pettersson) — BX2 — BeH 1·64 5·5 900°?
BE3 — — B 11·0 (Ramsay Ashton) — — BX3 — — 2·5 4·4 1,300°?
CH4 C2H6 C2H4 C2H2 C 12·0 (Roscoe) — CO — COZ2 C2O5* — *1·9 6·3 2,600°?
NH3 N2H4 — N 14·04 (Stas) N2O NO NOZ NO2 NO2Z N2O6* N3H *0·6 23 -203°
OH2 — O 16 (conventional) — OX2 O3 — *0·9 18 -230°?
— FH F 19·0 (Christiansen) FZ — — — ?1·0 19 ?
NaE Na 23·04 (Stas) NaX NaO Na2H 0·98 23·5 96°
MgE2 — Mg 24·3 (Burton) — MgX2 — MgH 1·74 14 500°
AlE3 — — Al 27·1 (Mallet) — — AlX3 — — 2·6 11 600°
SiH4 Si2E6 — — Si 28·4 (Thorpe Young) — — — SiOZ2 — — 2·3 12 1,300°?
PH3 P2H4 — P 31·0 (v. d. Plaats) — — PX3 — POZ3 — P2H 2·2 14 44°
SH2 — S 32·06 (Stas) — SX2 — SOZ2 — SO2Z2 S2O7 — 2·07 15 114°
ClH Cl 35·45 (Stas) ClZ — ClOZ — ClO2Z — ClO3Z — — *1·3 27 -75°
K 39·15 (Stas) KX KO2 K2H 0·87 45 58°
Ca 40·0 (Dumas) — CaX2 CaO2 CaH 1·56 26 800°
Sc 44·0 (Nilson) — — ScX3 — — ?2·5 ?18 1,200°?
Ti 48·1 (Thorpe) — TiX2 TiX3 TiX4 TiO3 — 3·6 13 2,500°?
V 51·2 (Roscoe) — VO VOX — VOZ3 — — — 5·5 9 3,000°?
Cr 52·1 (Rawson) — CrX2 CrX3 CrO2 — CrO2Z2 Cr2O7 — 6·7 7·7 2,000°?
Mn 55·1 (Marignac) — MnX2 MnX3 MnO2 — MnO2Z2 MnO3Z — — 7·5 7·3 1,500°
Fe 56·0 (Dumas) — FeX2 FeX3 — — FeO2Z2 — FenH* 7·8 7·2 1,450°
Co 58·9 (Zimmermann) — CoX2 CoX3 CoO2 — — 8·6 6·8 1,400°
Ni 59·4 (Winkler) — NiX2 NiX3 — NinH 8·7 6·8 1,350°
Cu 63·6 (Richards) CuX CuX2 Cu2O5* CuH 8·8 7·2 1,054°
ZnE2 — Zn 65·3 (Marignac) — ZnX2 ZnO2 — 7·1 9·2 418°
GaE3 — — Ga 69·9 (Boisbaudran) — — GaX3 — — 5·96 11·7 30°
GeE4 — — — Ge 72·3 (Winkler) — GaX2 — GaX4 — — 5·47 13·2 900°
AsH3 — — As 75·0 (Dumas) — AsS AsX3 AsS2 AsO2Z — As4H* 5·65 13·3 500°
SeH2 — Se 79·0[A] (Pettersson) — — — SeOZ2 — SeO2Z2 — — 4·8 16 217°
BrH Br 79·95 (Stas) BrZ — BrOZ — BrO2Z — BrO3Z — — 3·1 26 -7°
Rb 85·5 (Godeffroy) RbX RbO Rb2H* 1·5 57 39°
Sr 87·6 (Dumas) — SrX2 SrO2 SrH 2·5 35 600°?
Y 89 (Clève) — — YX3 — — *3·4 *26 1,000°?
Zr 90·6 (Bailey) — — — ZrX4 — Zr4nH* 4·1 2·2 1,500°?
Nb 94 (Marignac) — — NbX3 — NbO2Z — NbnH* 7·1 13 1,800°?
Mo 96·1 (Maas) — — MoX3 MoX4 — MoO2Z2 Mo2O7 — 8·6 11 2,200°?
Unknown metal (eka-manganese, Em = 99). EmO3Z — — — — —
Ru 101·7 (Joly) — RuX2 RuX3 RuX4 — RuO2Z2 — RuO4 — RunH* 12·2 8·4 2,000°?
Rh 102·7 (Seubert) — RhX2 RhX3 RhX4 — RhO2Z2 — RhnH* 12·1 8·6 1,900°?
Pd 106·4 (Keller Smith) PdX PdX2 — PdX4 — Pd2H 11·4 8·3 1,500°
Ag 107·92 (Stas) AgX AgO — 10·5 10·3 950°
CdE2 — Cd 112·1 (Lorimer Smith) — CdX2 CdO2 — 8·6 13 320°
InE3 — — In 113·6 (Winkler) — InX2 InX3 — — 7·4 14 176°
SnE4 — — — Sn 119·1 (Classen) — SnX2 — SnX4 SnO3 — 7·2 16 232°
SbH3 — — Sb 120·4 (Schneider) — — SbX3 — SbO2Z — — 6·7 18 432°
TeH2 — Te 125·1 (Brauner) — — — TeOZ2 — — 6·4 20 455°
IH I 126·85 (Stas) IZ — IZ3 — IO2Z — IO3Z — — 4·9 26 114°
Cs 132·7 (Godeffroy) CsX — Cs2H* 2·37 56 27°
Ba 137·4 (Richards) — BaX2 BaO2 BaH 3·76 36 ?
La 138·2 (Brauner) — — LaX3 — — 6·1 23 ?
Ce 140·2 (Brauner) — — CeX3 CeX4 — — 6·6 21 700°?
Little known Di = 142.1 and Yb = 173.2, and over 15 unknown elements.
Ta 182·7 (Marignac) — — — — TaO2Z — TanH* 10·4 18 ?
W 184·0 (Waddel) — — — WX4 — WO2Z2 W2O7 — 19·1 9·6 2,600°
Unknown element.
Os 191·6 (Seubert) — — OsX3 OsX4 — OsO2Z2 — OsO4 — — 22·5 8·5 2,700°?
Ir 193·3 (Joly) — — IrX3 IrX4 — IrO2Z2 — IrnH* 22·4 8·6 2,000°
Pt 196·0 (Dittmar McArthur) — PtX2 — PtX4 — PtnH* 21·4 9·2 1,775°
Au 197·5 (Dittmar McArthur) AuX — AuX3 — — 19·3 10 1,045°
HgE2 — Hg 200·5 (Erdmann Mar.) HgX HgX2 — — 13·6 15 -39°
TlE3 — — Tl 204·1 (Crookes) TlX — TlX3 — — 11·8 17 294°
PbE4 — — — Pb 206·90 (Stas) — PbX2 — PbOZ2 — — 11·3 18 328°
BiE3 — — Bi 208·9 (Classen) — — BiX3 — BiO2 — — 9·8 21 269°
Five unknown elements.
Th 232·4 (Krüss Nilson) — — — ThX4 — — 11·1 21 ?
Unknown element.
U 239·3 (Zimmermann) — — — UO2 — UO2X2 — UO4 — — 18·7 13 2,400°?
Columns 1, 2, 3, and 4 give the molecular composition of the hydrogen and metallo-organic compounds, exhibiting the most characteristic forms assumed by the elements. The first column contains only those which correspond to the form RX4, the second column those of the form RX3, the third of the form RX2, and the fourth of the form RX, so that the periodicity stands out clearly (see Column 16).
Column 5 contains the symbols of all the more or less well-known elements, placed according to the order of the magnitude of their atomic weights.
Column 6 contains the atomic weights of the elements according to the most trustworthy determinations. The names of the investigators are given in parenthesis. The atomic weight of oxygen, taken as 16, forms the basis upon which these atomic weights were calculated. Some of these have been recalculated by me on the basis of Stas's most trustworthy data (see Chapter XXIV. and the numbers given by Stas in the table, where they are taken according to van der Plaats and Thomsen's calculations).
Columns 7–14 contain the composition of the saline compounds of the elements, placed according to their forms, RX, RX2 to RX8 (in the 14th column). If the element R has a metallic character like H, Li, Be, &c., then X represents Cl, NO3, ½ SO4, &c., haloid radicles, or (OH) if a perfect hydrate is formed (alkali, aqueous base), or ½ O, ½ S, &c. when an anhydrous oxide, sulphide, &c. is formed. For instance, NaCl, Mg(NO3)2, Al2(SO4)3, correspond to NaX, MgX2, and AlX3; so also Na(OH), Mg(OH)2, Al(OH)3, Na2O, MgO, Al2O3, &c. But if the element, like C or N, be of a metalloid or acid character, X must be regarded as (OH) in the formation of hydrates; (OM) in the formation of salts, where M is the equivalent of a metal, ½ O in the formation of an anhydride, and Cl in the formation of a chloranhydride; and in this case (i.e. in the acid compounds) Z is put in the place of X; for example, the formulæ COZ2, NO2Z, MNO2Z, FeO2Z2, and IZ3 correspond to CO(NaO)2 = Na2CO3, COCl2, CO2, NO2(NaO) = NaNO3, NO2Cl, NO2(OH) = HNO3; MnO3(OK) = KMnO4, ICl, &c.
The 15th column gives the compositions of the peroxides of the elements, taking them as anhydrous. An asterisk (*) is attached to those of which the composition has not been well established, and a dash (—) shows that for a given element no peroxides have yet been obtained. The peroxides contain more oxygen than the higher saline oxides of the same elements, are powerfully oxidising, and easily give peroxide of hydrogen. This latter circumstance necessitates their being referred to the type of peroxide of hydrogen, if bases and acids are referred to the type of water (see Chapter XV., Note 7 and 11 bis).
The 16th column gives the composition of the lower hydrogen compounds like N3H and Na2H. They may often be regarded as alloys of hydrogen, which is frequently disengaged by them at a comparatively moderate temperature. They differ greatly in their nature from the hydrogen compounds given in columns 1–4 (see Note 12).
Column 17 gives the specific gravity of the elements in a solid and a liquid state. An asterisk (*) is placed by those which can either only be assumed from analogy (for example, the sp. gr. of fluorine and hydrogen, which have not been obtained in a liquid state), or which vary very rapidly with a variation of temperature and pressure (like oxygen and nitrogen), or physical state (for instance, carbon in passing from the state of charcoal to graphite and diamond). But as the sp. gr. in general varies with the temperature, mechanical condition, &c., the figures given, although chosen from the most trustworthy sources, can only be regarded as approximate, and not as absolutely true. They clearly show a certain periodicity; for instance, the sp. gr. diminishes from Al on both sides (Al, Mg, Na, with decreasing atomic weight; and Al, Si, P, S, Cl, with increasing atomic weight, it also diminishes on both sides from Cu, Ru, and Os.)
The same remarks refer to the figures in the 18th column, which gives the so-called atomic volumes of the simple bodies, or the quotient of their atomic weight and specific gravity. For Na, K, Rb, and Cs the atomic volume is greatest among the neighbouring elements. For Ni, Pd, and Os it is least, and this indicates the periodicity of this property of the simple bodies.
The last (19th) column gives the melting points of the simple bodies. Here also a periodicity is seen, i.e. a maximum and minimum value between which there are intermediate values, as we see, for instance, in the series Cl, K, Ca, Sc, and Ti, or in the series Cr, Mn, Fe, Co, Ni, Cu, Zn, Ga, and Ge.