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 _phthalates_ of the yttrium group have been found to be very
valuable for purposes of separation by Meyer and Wuorinen.[172] The
salts are readily obtained in solution by shaking together cold aqueous
suspensions of the rare earth hydroxides, and phthalic acid; the clear
solutions when warmed become cloudy, the organic salts hydrolysing very
easily, with separation of the hydroxides. The most positive elements
naturally remain longest in the solution, the weakly basic oxides
accumulating in the first precipitates.
[172] _Zeitsch. anorg. Chem._ 1913, ~80~, 7.
An organic compound which has proved very useful in the treatment of
the rare earths is acetylacetone, CH₃.CO.CH₂.CO.CH₃.[173] In its enolic
form, this substance forms salts with metals, which in the case of the
rare earth elements are especially characterised by the ease with which
they may be obtained, and their high crystallising power. They may be
prepared by double decomposition of neutral solutions of rare earth
salts with ammonium acetylacetone, and crystallise readily from dilute
alcohol. They have been used by Urbain in the fractionation of the
yttrium group, and for determination of molecular weights by the boiling
point method; Biltz[174] has shown that in solution they generally have
the double formula R₂(C₅H₇O₂)₆.
[173] Urbain, _Bull. Soc. chim._ 1897, [iii.], ~17~, 98; Urbain and
Budischofsky, _Compt. rend._ 1897, ~124~, 618; Biltz and Clinch,
_Zeitsch. anorg. Chem._ 1904, ~40~, 218.
[174] _Annalen_, 1904, ~331~, 334.
THE RARE EARTH ELEMENTS, AND THE PERIODIC CLASSIFICATION
At the time of the introduction of the periodic classification the rare
earth elements were generally believed to be divalent. This belief,
which has persisted until quite recently,[175] was based chiefly on the
electropositive character of the metals, and their general chemical
resemblance to the elements of the alkaline earths; the isomorphism of
the tungstates of calcium and the cerium elements, and of the molybdates
of lead and the cerium elements, also supports this view. The physical
evidence in favour of Mendelejeff’s view, however, is quite
overwhelming; the specific heats of the metals, the equivalent
conductivities of the chlorides, and molecular weight determinations by
means of vapour densities and the boiling point method, prove beyond
doubt that the elements are in fact trivalent.
[175] See Wyrouboff, _Bull. Soc. franc. Min._ 1896, ~19~, 219;
Wyrouboff and Verneuil, _Compt. rend._ 1897, ~124~, 1230 and 1300;
_ibid._, 1899, ~128~, 1573; etc.
In deciding in favour of the trivalent nature of the rare earth metals,
Mendelejeff was influenced chiefly by the fact that there was no room in
the table for divalent elements with the equivalent weights then
assigned to the cerium and yttrium elements. At that time, only the six
oxides obtained by Mosander were known; of these the accepted
equivalents and atomic weights were as follows:
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