A Theoretical Consideration of the Strength of Snow
Abstract A consideration of possible expressions for the number and size of bonds intersected by a potential failure surface leads to the following expression for the strength of snow, σ f , which is age-hardening at a constant porosity n : where σ i is the strength of ice, t f is the time at failur...
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Language: | English |
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Cambridge University Press (CUP)
1966
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Online Access: | http://dx.doi.org/10.1017/s0022143000019146 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019146 |
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crcambridgeupr:10.1017/s0022143000019146 2024-03-03T08:46:05+00:00 A Theoretical Consideration of the Strength of Snow Ballard, G. E. H. Feldt, E. D. 1966 http://dx.doi.org/10.1017/s0022143000019146 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019146 en eng Cambridge University Press (CUP) Journal of Glaciology volume 6, issue 43, page 159-170 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1966 crcambridgeupr https://doi.org/10.1017/s0022143000019146 2024-02-08T08:37:11Z Abstract A consideration of possible expressions for the number and size of bonds intersected by a potential failure surface leads to the following expression for the strength of snow, σ f , which is age-hardening at a constant porosity n : where σ i is the strength of ice, t f is the time at failure, α is a parameter specifically related to the mechanism of bonding, and ω is a temperature-dependent parameter. Allowing t f to become infinite provides the envelope of maximum strength for fully age-hardened snow at any porosity n . Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 6 43 159 170 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Ballard, G. E. H. Feldt, E. D. A Theoretical Consideration of the Strength of Snow |
topic_facet |
Earth-Surface Processes |
description |
Abstract A consideration of possible expressions for the number and size of bonds intersected by a potential failure surface leads to the following expression for the strength of snow, σ f , which is age-hardening at a constant porosity n : where σ i is the strength of ice, t f is the time at failure, α is a parameter specifically related to the mechanism of bonding, and ω is a temperature-dependent parameter. Allowing t f to become infinite provides the envelope of maximum strength for fully age-hardened snow at any porosity n . |
format |
Article in Journal/Newspaper |
author |
Ballard, G. E. H. Feldt, E. D. |
author_facet |
Ballard, G. E. H. Feldt, E. D. |
author_sort |
Ballard, G. E. H. |
title |
A Theoretical Consideration of the Strength of Snow |
title_short |
A Theoretical Consideration of the Strength of Snow |
title_full |
A Theoretical Consideration of the Strength of Snow |
title_fullStr |
A Theoretical Consideration of the Strength of Snow |
title_full_unstemmed |
A Theoretical Consideration of the Strength of Snow |
title_sort |
theoretical consideration of the strength of snow |
publisher |
Cambridge University Press (CUP) |
publishDate |
1966 |
url |
http://dx.doi.org/10.1017/s0022143000019146 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019146 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 6, issue 43, page 159-170 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000019146 |
container_title |
Journal of Glaciology |
container_volume |
6 |
container_issue |
43 |
container_start_page |
159 |
op_container_end_page |
170 |
_version_ |
1792501975780163584 |