The Rare Earths: Their Occurrence, Chemistry, and TechnologyLevy, Stanley Isaac
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The Rare Earths: Their Occurrence, Chemistry, and Technology
Levy, Stanley Isaac
Rare earths
~The Emission Spectra: Spark Spectra.~--The factors which tend to limit
the value of the absorption spectra for analytical purposes, for the
most part disappear when the emission spectra are employed. In the case
of the spark spectra, indeed, great differences are observed according
to the conditions and method of experiment; but the arc spectra are
practically invariable under all conditions, and hence they constitute
the ultimate test in all cases. The spark spectra are observed when one
terminal--the cathode--of an induction coil is embedded in the oxides to
be examined, and the discharge then passed. The discharge is also
frequently passed between platinum poles partly immersed in a strong
solution of a salt of the element under examination; a form of apparatus
very suitable for this method of observation has been described by Sir
W. Crookes.[186] The spectra so obtained are in a high degree
characteristic, but they vary very considerably with the form and
dimensions of the coil, the length and cross-section of the wires, the
potential difference employed, and so on. An entirely new spectrum also
is obtained in many cases by mere reversal of the current; under these
conditions, a phosphorescent appearance is observed, the spectrum of
which--reversed spark spectrum of de Boisbaudran--has been found in many
cases to resemble the cathode luminescence spectra of Crookes.
[186] _Proc. Roy. Soc._, 1903, ~72~, 295.
~The Arc Spectra.~--The final criterion of purity in the examination of
a rare earth element is in almost all cases the arc spectrum. Since for
some of the elements, especially in the yttrium group, the entire
spectrum has not yet been accurately mapped out, spectra are generally
observed frequently throughout the course of a fractionation; by this
means, the separation can be followed by the disappearance of some
lines, and the appearing or strengthening of others, and such
examinations have led occasionally to the discovery of new elements
(see, for example, under Separation of ytterbium earths, p. 205). Such
determinations, however, require much time and extensive and complicated
apparatus.
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