The Rare Earths: Their Occurrence, Chemistry, and TechnologyLevy, Stanley Isaac
Science
The Rare Earths: Their Occurrence, Chemistry, and Technology
Levy, Stanley Isaac
Rare earths
In presence of a large excess of alkali carbonate, double carbonates are
formed. The stability as well as the solubility of these compounds
increases in passing from the cerium to the yttrium group, _i.e._ as
the electropositive character becomes weaker. The double carbonates of
the cerium elements are sparingly soluble, and are decomposed by water,
especially on warming; they may, however, be recrystallised from alkali
carbonate solution. The sodium and ammonium double salts are less
soluble than the potassium compounds. The latter have the general
formula R₂(CO₃)₃,K₂CO₃,12H₂O, and are of considerable importance in many
processes of separation. The yttrium elements can be separated from the
cerium metals, and the latter from one another, by taking advantage of
the differences of solubility shown by the potassium double carbonates.
If a concentrated solution of the salts in potassium carbonate solution
be fractionally diluted with water, the cerium elements separate in the
order: lanthanum, praseodymium, cerium, neodymium, and samarium; the
more soluble yttrium compounds remain in the solution. Thorium forms
double alkali carbonates which are very readily soluble in excess of
alkali carbonate; this property is of great importance for the technical
separation of the element.
~Oxalates.~--The oxalates of the rare earth elements are of the greatest
importance, on account of the fact that they are not only insoluble in
water, but are also very sparingly soluble in dilute mineral acids, and
in excess of oxalic acid. They can be completely precipitated even from
strongly acid solutions by addition of sufficient excess of oxalic acid,
or alkali oxalate, and thus afford a means of easily and completely
separating the rare earth group from the commoner elements.
They are thrown down by addition of oxalic acid, or alkali oxalate, as
amorphous precipitates, which rapidly become crystalline, especially if
the solution is warmed. From water at normal temperatures they usually
separate as the decahydrates, R₂(C₂O₄)₃,10H₂O, but hydrates with 7, 9,
and 11 molecules of water of crystallisation are also known. From
strongly acid solutions, mixed oxalo-salts of the general formula
R(C₂O₄)X, where X = Cl, NO₃, HSO₄, etc., may be obtained. These mixed
salts may also be prepared by dissolving the oxalates in concentrated
solutions of the chlorides, nitrates, etc., whilst nitro-sulphates,
R(SO₄)NO₃, have been obtained by recrystallising the sulphates from
strong nitric acid. The tendency to form salts with mixed acid radicles
appears to be general.[166]
[166] See Meyer and Marckwald, _Ber._ 1900, ~33~, 1003; also Matignon,
_Ann. Chim. Phys._ 1906, [viii.], ~8~, 243.
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