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 methods which have been most commonly used are those based on a
determination of the ratio R₂O₃ : R₂(SO₄)₃, and these are of two kinds,
the synthetic and the analytical. The first, in which a known weight of
the oxide is converted into the sulphate, has been most used for the
most strongly basic oxides, since with these it is difficult to remove
the last traces of sulphuric anhydride from the oxide by heat. The
oxides are best obtained from the oxalates, which are precipitated from
an acid solution of the nitrates, washed thoroughly with water, alcohol
and ether in succession, dried, and ignited in a tarred platinum
crucible. The oxide is best dissolved in dilute hydrochloric or nitric
acid on the waterbath, a slight excess of sulphuric acid being added
only when a clear solution has been obtained; the liquid is then heated
gradually to 300°, and finally in the electric furnace at 450°-550°
until constant in weight. If sulphuric acid be added directly to the
weighed oxide, particles of the latter may become completely coated with
the insoluble sulphate, and so escape the action of the acid.
In the analytical method, a known weight of sulphate is ignited to the
oxide, and weighed as such. This method is most suitable for the less
basic members of the yttria earths, of which the sulphates can be
completely decomposed without difficulty at a red heat. By the use of
the microbalance, a sufficiently accurate determination can be carried
out by either of these methods in little more than half an hour, as the
chemical changes are exceedingly rapid where only small quantities are
employed, and no time is required to allow the vessels and solids to
cool. Using the microbalance, Brill[192] has carried out a series of
experiments to determine the limits of temperature within which the
various steps of the process should be carried out. He finds that a
temperature of 400°-550° is required to decompose the last traces of
acid sulphate, and give the pure neutral sulphate. Between the
temperatures of 850° and 950°, basic salts are formed, from which the
last trace of sulphuric anhydride is expelled at 900°-1150°; the precise
temperature required in each case depends, of course, on the basic
strength of the oxide in question.
[192] _Zeitsch. anorg. Chem._ 1905, ~47~, 464.
The determination of equivalents by means of the ratio R₂O₃ : R₂(C₂O₄)₃,
has been brought to a high degree of accuracy by Brauner.[193] A weighed
quantity of the carefully prepared oxalate is ignited, with suitable
precautions, to the oxide, in a tarred platinum crucible. A second
weighed specimen of the same oxalate preparation is dissolved in dilute
sulphuric acid, and titrated at 60° with permanganate, which is
standardised against pure ammonium oxalate.
[193] _Ibid._ 1903, ~34~, 103, 207.
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