1150
SENNIKOV et al.
8
×
10–4 vol % in samples 2 and 3 (isotopically
This work was supported by the RF President’s
enriched). The total hydrocarbon content of the isotoꢀ Grants Council (Support to RF’s Leading Scientific
pically enriched samples is seven times lower than that Schools Program, grant no. NShꢀ4701.2008.03) and
of the sample of natural isotopic composition. Isotopic the Presidium of the Russian Academy of Sciences
(
program no. 20, theme 2).
enrichment reduces the content of saturated hydroꢀ
carbons in germanium tetrafluoride by a factor of 10–
5
0. The content of unsaturated hydrocarbons in the
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Using highꢀresolution Fourierꢀtransform IR specꢀ
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than 20 impurity species, in concentrations from 10
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4
1
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compositions. The germanium tetrafluoride samples
were shown to contain C –C hydrocarbons; hydroꢀ
gen, carbon, silicon, and sulfur fluorides; fluorogerꢀ
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The likely sources of these impurities in GeF are
the starting germanium and fluorine and the residual
background) gases in the process equipment. The
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4
(
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nium leads to high SiF and CF concentrations, espeꢀ
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cially in the sample of natural isotopic composition. At
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The isotopic enrichment process alters the qualitaꢀ
tive and quantitative impurity compositions and is, on
the whole, accompanied by a reduction in the concenꢀ
tration of a number of impurities. The smallest numꢀ
ber of impurity species and the lowest impurity conꢀ
centrations are offered by the Geꢀenriched germaꢀ
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to the particular character of the enrichment process.
9
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1
ACKNOWLEDGMENTS
1
2. Ebsworth, E.A.V. and Robiette, A.S., The Infrared
Spectra of Dihalogermanes, Spectrochim. Acta, 1964,
vol. 20, pp. 1639–1642.
We are grateful to L.A. Chuprov and B.A. Andreev
for their assistance in taking the IR spectra.
INORGANIC MATERIALS Vol. 46
No. 10
2010