Plane-Strain Compressive Strength of Columnar-Grained and Granular-Snow Ice

Abstract An ice cover impinging on a long straight structure is assumed to be under a condition of plane strain. A technique is described for performing plane-strain compression tests, and results are presented for the strain-rate dependence of strength. The plane-strain compressive strength of ice...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Frederking, R.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1977
Subjects:
Online Access:http://dx.doi.org/10.1017/s002214300002116x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300002116X
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spelling crcambridgeupr:10.1017/s002214300002116x 2024-03-03T08:46:08+00:00 Plane-Strain Compressive Strength of Columnar-Grained and Granular-Snow Ice Frederking, R. 1977 http://dx.doi.org/10.1017/s002214300002116x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300002116X en eng Cambridge University Press (CUP) Journal of Glaciology volume 18, issue 80, page 505-516 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1977 crcambridgeupr https://doi.org/10.1017/s002214300002116x 2024-02-08T08:36:10Z Abstract An ice cover impinging on a long straight structure is assumed to be under a condition of plane strain. A technique is described for performing plane-strain compression tests, and results are presented for the strain-rate dependence of strength. The plane-strain compressive strength of ice having anisotropic structure (columnar-grained ice) is at least two and a half times the uniaxial compressive strength, whereas the plane-strain compressive strength of ice having an isotropic structure (granular-snow ice) is at most 25% greater than the uniaxial case. The greater plane-strain compressive strength of columnar grained ice when the loading and confining directions are in the plane of the ice cover, can be attributed to its anisotropic structure, which leads to a different failure mechanism for the plane-strain case. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 18 80 505 516
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Frederking, R.
Plane-Strain Compressive Strength of Columnar-Grained and Granular-Snow Ice
topic_facet Earth-Surface Processes
description Abstract An ice cover impinging on a long straight structure is assumed to be under a condition of plane strain. A technique is described for performing plane-strain compression tests, and results are presented for the strain-rate dependence of strength. The plane-strain compressive strength of ice having anisotropic structure (columnar-grained ice) is at least two and a half times the uniaxial compressive strength, whereas the plane-strain compressive strength of ice having an isotropic structure (granular-snow ice) is at most 25% greater than the uniaxial case. The greater plane-strain compressive strength of columnar grained ice when the loading and confining directions are in the plane of the ice cover, can be attributed to its anisotropic structure, which leads to a different failure mechanism for the plane-strain case.
format Article in Journal/Newspaper
author Frederking, R.
author_facet Frederking, R.
author_sort Frederking, R.
title Plane-Strain Compressive Strength of Columnar-Grained and Granular-Snow Ice
title_short Plane-Strain Compressive Strength of Columnar-Grained and Granular-Snow Ice
title_full Plane-Strain Compressive Strength of Columnar-Grained and Granular-Snow Ice
title_fullStr Plane-Strain Compressive Strength of Columnar-Grained and Granular-Snow Ice
title_full_unstemmed Plane-Strain Compressive Strength of Columnar-Grained and Granular-Snow Ice
title_sort plane-strain compressive strength of columnar-grained and granular-snow ice
publisher Cambridge University Press (CUP)
publishDate 1977
url http://dx.doi.org/10.1017/s002214300002116x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300002116X
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 18, issue 80, page 505-516
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s002214300002116x
container_title Journal of Glaciology
container_volume 18
container_issue 80
container_start_page 505
op_container_end_page 516
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