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Quantum mechanical calculations of the vibrational spectra of quartz- and rutile-type GeO2
Authors:Reinhard Kaindl  Daniel M T?bbens  Simon Penner  Thomas Bielz  Soipatta Soisuwan  Bernhard Kl?tzer
Institution:(1) Institute of Mineralogy and Petrography, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria;(2) Present address: Helmholtz-Zentrum Berlin, Hahn-Meitner-Platz 1, 14109 Berlin, Germany;(3) Institute of Physical Chemistry, University of Innsbruck, Innrain 52a, 6020 Innsbruck, Austria;(4) Department of Chemical Engineering, Burapha University, Chonburi, 20131, Thailand;(5) Materials-Institute of Surface Technologies and Photonics, JOANNEUM RESEARCH Forschungsges.mbH, Leobner Stra?e 94, 8712 Niklasdorf, Austria
Abstract:Heat-treatment and stepwise cooling of as-delivered, water-containing quartz-type GeO2 powder resulted in transformation into a water-free form. A rutile-type modification could be prepared by impregnation of the quartz-type phase with RbOH solutions, drying and annealing. Raman- and FTIR-absorption spectra of quartz- and rutile-type GeO2 were measured and compared to quantum-mechanical ab initio calculations based on a hybrid functional using the Perdew–Burke–Ernzerhof correlation functional with 16.7% Hartree–Fock exchange density functional. Maximum and mean deviations between measured spectral bands and assigned vibrational modes are 14 and ±8 cm−1 for the quartz-type and 30 and ±13 cm−1 for the rutile-type polymorphic form. Water is incorporated into GeO4 entities of quartz-type GeO2; a water-free and structurally stable form can be prepared by a heating up to 1,425 K, tempering at 1,323 K and stepwise cooling. Spectral bands not explained by the calculations suggest defects and distortions in both quartz- and rutile-type structures, in case of the quartz-type one by incomplete transformation into an ideal structure after removing the water, whereas the rutile-type modification most probably incorporates Rb during its synthesis.
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