Origin of the High-Frequency Translational Bands of Ice I

Abstract The translational vibrations of hypothetical ordered forms of ice Ic and ice Ih have been predicted and correlated with the known spectra of the actual disordered phases. The TO–LO splittings have been predicted by assuming that the changes of mean refractive indexes across the translationa...

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Published in:Journal of Glaciology
Main Authors: Klug, D. D., Whalley, E.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1978
Subjects:
Online Access:http://dx.doi.org/10.1017/s002214300003330x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300003330X
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spelling crcambridgeupr:10.1017/s002214300003330x 2024-06-23T07:54:15+00:00 Origin of the High-Frequency Translational Bands of Ice I Klug, D. D. Whalley, E. 1978 http://dx.doi.org/10.1017/s002214300003330x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300003330X en eng Cambridge University Press (CUP) Journal of Glaciology volume 21, issue 85, page 55-63 ISSN 0022-1430 1727-5652 journal-article 1978 crcambridgeupr https://doi.org/10.1017/s002214300003330x 2024-06-12T04:04:33Z Abstract The translational vibrations of hypothetical ordered forms of ice Ic and ice Ih have been predicted and correlated with the known spectra of the actual disordered phases. The TO–LO splittings have been predicted by assuming that the changes of mean refractive indexes across the translational band is the same in all phases, and equal to the known change for ice Ih. Both ordered phases are predicted to have LO components at c. 275 and c. 310 cm -1 . These predicted bands are assumed to be related to the bands at the same frequencies in the disordered phases. These bands are therefore LO components corresponding to the TO translational vibrations. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 21 85 55 63
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract The translational vibrations of hypothetical ordered forms of ice Ic and ice Ih have been predicted and correlated with the known spectra of the actual disordered phases. The TO–LO splittings have been predicted by assuming that the changes of mean refractive indexes across the translational band is the same in all phases, and equal to the known change for ice Ih. Both ordered phases are predicted to have LO components at c. 275 and c. 310 cm -1 . These predicted bands are assumed to be related to the bands at the same frequencies in the disordered phases. These bands are therefore LO components corresponding to the TO translational vibrations.
format Article in Journal/Newspaper
author Klug, D. D.
Whalley, E.
spellingShingle Klug, D. D.
Whalley, E.
Origin of the High-Frequency Translational Bands of Ice I
author_facet Klug, D. D.
Whalley, E.
author_sort Klug, D. D.
title Origin of the High-Frequency Translational Bands of Ice I
title_short Origin of the High-Frequency Translational Bands of Ice I
title_full Origin of the High-Frequency Translational Bands of Ice I
title_fullStr Origin of the High-Frequency Translational Bands of Ice I
title_full_unstemmed Origin of the High-Frequency Translational Bands of Ice I
title_sort origin of the high-frequency translational bands of ice i
publisher Cambridge University Press (CUP)
publishDate 1978
url http://dx.doi.org/10.1017/s002214300003330x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300003330X
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 21, issue 85, page 55-63
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s002214300003330x
container_title Journal of Glaciology
container_volume 21
container_issue 85
container_start_page 55
op_container_end_page 63
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