Elastic Constants of Ice by Brillouin Spectroscopy
Abstract Brillouin spectroscopy has been used to measure the adiabatic elastic constants of laboratory-grown pure monocrystalline ice Ih at – 3°C. The values obtained were (in units of 10 8 N/m 2 ): c 11 = 136.96 ±0.60, c 12 = 69.66± 0.45, c 13 = 56.28±0.31, c 33 = 147.02±0.68, c 44 = 29.59±0.15. Co...
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Cambridge University Press (CUP)
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Online Access: | http://dx.doi.org/10.1017/s0022143000010376 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000010376 |
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crcambridgeupr:10.1017/s0022143000010376 2024-03-03T08:45:59+00:00 Elastic Constants of Ice by Brillouin Spectroscopy Gammon, P. H. Kiefte, H. Clouter, M. J. 1980 http://dx.doi.org/10.1017/s0022143000010376 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000010376 en eng Cambridge University Press (CUP) Journal of Glaciology volume 25, issue 91, page 159-168 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1980 crcambridgeupr https://doi.org/10.1017/s0022143000010376 2024-02-08T08:41:37Z Abstract Brillouin spectroscopy has been used to measure the adiabatic elastic constants of laboratory-grown pure monocrystalline ice Ih at – 3°C. The values obtained were (in units of 10 8 N/m 2 ): c 11 = 136.96 ±0.60, c 12 = 69.66± 0.45, c 13 = 56.28±0.31, c 33 = 147.02±0.68, c 44 = 29.59±0.15. Comparison of these values with ultrasonic measurements quoted in the literature reveals no significant acoustic dispersion in ice over frequencies ranging to 10 10 Hz. However, the results suggest that the elastic constants of ice may depend on the precise crystal quality and age of a given sample. The low experimental error in the values obtained, along with the inherent versatility of the method, indicate that Brillouin spectroscopy is an effective technique for systematically investigating the elastic properties of ice samples formed under natural conditions. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 25 91 159 168 |
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Open Polar |
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Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Gammon, P. H. Kiefte, H. Clouter, M. J. Elastic Constants of Ice by Brillouin Spectroscopy |
topic_facet |
Earth-Surface Processes |
description |
Abstract Brillouin spectroscopy has been used to measure the adiabatic elastic constants of laboratory-grown pure monocrystalline ice Ih at – 3°C. The values obtained were (in units of 10 8 N/m 2 ): c 11 = 136.96 ±0.60, c 12 = 69.66± 0.45, c 13 = 56.28±0.31, c 33 = 147.02±0.68, c 44 = 29.59±0.15. Comparison of these values with ultrasonic measurements quoted in the literature reveals no significant acoustic dispersion in ice over frequencies ranging to 10 10 Hz. However, the results suggest that the elastic constants of ice may depend on the precise crystal quality and age of a given sample. The low experimental error in the values obtained, along with the inherent versatility of the method, indicate that Brillouin spectroscopy is an effective technique for systematically investigating the elastic properties of ice samples formed under natural conditions. |
format |
Article in Journal/Newspaper |
author |
Gammon, P. H. Kiefte, H. Clouter, M. J. |
author_facet |
Gammon, P. H. Kiefte, H. Clouter, M. J. |
author_sort |
Gammon, P. H. |
title |
Elastic Constants of Ice by Brillouin Spectroscopy |
title_short |
Elastic Constants of Ice by Brillouin Spectroscopy |
title_full |
Elastic Constants of Ice by Brillouin Spectroscopy |
title_fullStr |
Elastic Constants of Ice by Brillouin Spectroscopy |
title_full_unstemmed |
Elastic Constants of Ice by Brillouin Spectroscopy |
title_sort |
elastic constants of ice by brillouin spectroscopy |
publisher |
Cambridge University Press (CUP) |
publishDate |
1980 |
url |
http://dx.doi.org/10.1017/s0022143000010376 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000010376 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 25, issue 91, page 159-168 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000010376 |
container_title |
Journal of Glaciology |
container_volume |
25 |
container_issue |
91 |
container_start_page |
159 |
op_container_end_page |
168 |
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1792501730720612352 |