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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Published in:Journal of Glaciology
Main Authors: Ballard, G. E. H., Feldt, E. D.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1966
Subjects:
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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spelling 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
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