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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Language: | English |
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Cambridge University Press (CUP)
1978
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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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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 |
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Cambridge University Press |
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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 |
_version_ |
1802646346612604928 |