The Rare Earths: Their Occurrence, Chemistry, and TechnologyLevy, Stanley Isaac
Science
The Rare Earths: Their Occurrence, Chemistry, and Technology
Levy, Stanley Isaac
Rare earths
The _double ceric nitrates_[219] are a large and very important class of
compounds; they are the most stable of the ceric salts. With nitrates of
the monovalent metals, ceric nitrate forms double nitrates of the type
R₂Ce(NO₃)₆; these are deep red hygroscopic substances, crystallising in
the monoclinic system, readily soluble in water and alcohol, but
dissolving only sparingly in nitric acid. The ammonium salt is important
for the separation of cerium. A series of double nitrates with the
nitrates of manganese, magnesium, zinc, nickel, and cobalt has the
general formula RCe(NO₃)₆,8H₂O, but these are much less stable in
solution than the alkali double salts.
[219] Meyer and Jacoby, _loc. cit._
ATOMIC WEIGHT OF CERIUM
No less than twenty-eight separate determinations of the atomic weight
of cerium have been carried out. The earlier determinations are rendered
unreliable by the almost certain presence of other elements, and
Brauner[220] has shown that some of the methods employed in later work
give erroneous results.
[220] _Trans. Chem. Soc._ 1885, ~47~, 879; also _Zeitsch. anorg.
Chem._ 1903, ~34~, 207.
A very careful determination was made by Robinson in 1884.[221] Cerium
oxalate was heated in a stream of dry hydrogen chloride, mixed with
carbon dioxide, and the anhydrous chloride freed from traces of acid in
a vacuum over chalk. The weighed chloride was then dissolved in water,
and titrated with silver nitrate. He obtained the value 140·26;
recalculation from his data with the modern values for silver and
chlorine give 140·19. Brauner points out that this result is too low,
since no account was taken of the solubility of silver chloride in
water. In the following year, Brauner[222] determined the ratio
Ce₂(SO₄)₃ : 2CeO₂, and obtained the atomic weight 140·22. Wyrouboff and
Verneuil[223] in 1897 disputed Brauner’s work, and as a result of
several determinations gave the values 139·21, 139·43, and 139·50; their
determinations, however, varied very considerably, and the work has been
severely criticised by Brauner. In 1903, the latter author and
Batěk[224] obtained the values 140·21 and 140·27 by the sulphate and
oxalate methods respectively; whilst in the same year, using the same
methods, Brauner[225] obtained from three independent series of
determinations the values 140·25, 140·24, and 140·25.
[221] _Proc. Roy. Soc._ 1884, ~37~, 150.
[222] _Loc. cit._
[223] _Compt. rend._ 1897, ~124~, 1300.
[224] _Zeitsch. anorg. Chem._ 1903, ~34~, 103.
[225] _Zeitsch. anorg. Chem._ 1903, ~34~, 207.
The International Atomic Weight Committee have accepted the value 140·25
since 1904.
DETECTION AND ESTIMATION OF CERIUM
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