Effect of Hydrostatic Pressure on Velocity of Shear Deformation of Single Ice Crystals
Apparatus was built for deforming ice crystals under hydrostatic pressures up to 350 atmospheres. Single crystals were placed in the mounts in such a way that the deformation occurred by gliding on the basal glide plane. It was found that the shear strain rate increased as the pressure was increased...
Published in: | Journal of Glaciology |
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Language: | English |
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Cambridge University Press (CUP)
1958
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Online Access: | http://dx.doi.org/10.1017/s0022143000023911 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023911 |
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crcambridgeupr:10.1017/s0022143000023911 2024-03-03T08:46:03+00:00 Effect of Hydrostatic Pressure on Velocity of Shear Deformation of Single Ice Crystals Rigsby, George P. 1958 http://dx.doi.org/10.1017/s0022143000023911 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023911 en eng Cambridge University Press (CUP) Journal of Glaciology volume 3, issue 24, page 271-278 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1958 crcambridgeupr https://doi.org/10.1017/s0022143000023911 2024-02-08T08:36:10Z Apparatus was built for deforming ice crystals under hydrostatic pressures up to 350 atmospheres. Single crystals were placed in the mounts in such a way that the deformation occurred by gliding on the basal glide plane. It was found that the shear strain rate increased as the pressure was increased at constant temperature, but that the rate is practically independent of hydrostatic pressure when the difference between the ice temperature and the melting temperature is kept constant. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 3 24 271 278 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Rigsby, George P. Effect of Hydrostatic Pressure on Velocity of Shear Deformation of Single Ice Crystals |
topic_facet |
Earth-Surface Processes |
description |
Apparatus was built for deforming ice crystals under hydrostatic pressures up to 350 atmospheres. Single crystals were placed in the mounts in such a way that the deformation occurred by gliding on the basal glide plane. It was found that the shear strain rate increased as the pressure was increased at constant temperature, but that the rate is practically independent of hydrostatic pressure when the difference between the ice temperature and the melting temperature is kept constant. |
format |
Article in Journal/Newspaper |
author |
Rigsby, George P. |
author_facet |
Rigsby, George P. |
author_sort |
Rigsby, George P. |
title |
Effect of Hydrostatic Pressure on Velocity of Shear Deformation of Single Ice Crystals |
title_short |
Effect of Hydrostatic Pressure on Velocity of Shear Deformation of Single Ice Crystals |
title_full |
Effect of Hydrostatic Pressure on Velocity of Shear Deformation of Single Ice Crystals |
title_fullStr |
Effect of Hydrostatic Pressure on Velocity of Shear Deformation of Single Ice Crystals |
title_full_unstemmed |
Effect of Hydrostatic Pressure on Velocity of Shear Deformation of Single Ice Crystals |
title_sort |
effect of hydrostatic pressure on velocity of shear deformation of single ice crystals |
publisher |
Cambridge University Press (CUP) |
publishDate |
1958 |
url |
http://dx.doi.org/10.1017/s0022143000023911 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023911 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 3, issue 24, page 271-278 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000023911 |
container_title |
Journal of Glaciology |
container_volume |
3 |
container_issue |
24 |
container_start_page |
271 |
op_container_end_page |
278 |
_version_ |
1792501874416418816 |