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...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Rigsby, George P.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1958
Subjects:
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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spelling 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
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