Pressure Waves in Snow

Abstract A dynamic constitutive law is used to study the response of medium-density snow to shock waves. The results show good correlation between theory and experiment, except for low-intensity shocks which produce small permanent density changes. In this case the validity of the data is questioned...

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Published in:Journal of Glaciology
Main Author: Brown, R. L.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1980
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000010327
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000010327
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spelling crcambridgeupr:10.1017/s0022143000010327 2024-03-03T08:45:58+00:00 Pressure Waves in Snow Brown, R. L. 1980 http://dx.doi.org/10.1017/s0022143000010327 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000010327 en eng Cambridge University Press (CUP) Journal of Glaciology volume 25, issue 91, page 99-108 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1980 crcambridgeupr https://doi.org/10.1017/s0022143000010327 2024-02-08T08:41:37Z Abstract A dynamic constitutive law is used to study the response of medium-density snow to shock waves. The results show good correlation between theory and experiment, except for low-intensity shocks which produce small permanent density changes. In this case the validity of the data is questioned, although further experimental work is needed to settle this question. The results of this work also partially explain why snow is so effective in absorbing energy associated with stress waves. This is felt to be due to the work-hardening characteristics of snow. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 25 91 99 108
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Brown, R. L.
Pressure Waves in Snow
topic_facet Earth-Surface Processes
description Abstract A dynamic constitutive law is used to study the response of medium-density snow to shock waves. The results show good correlation between theory and experiment, except for low-intensity shocks which produce small permanent density changes. In this case the validity of the data is questioned, although further experimental work is needed to settle this question. The results of this work also partially explain why snow is so effective in absorbing energy associated with stress waves. This is felt to be due to the work-hardening characteristics of snow.
format Article in Journal/Newspaper
author Brown, R. L.
author_facet Brown, R. L.
author_sort Brown, R. L.
title Pressure Waves in Snow
title_short Pressure Waves in Snow
title_full Pressure Waves in Snow
title_fullStr Pressure Waves in Snow
title_full_unstemmed Pressure Waves in Snow
title_sort pressure waves in snow
publisher Cambridge University Press (CUP)
publishDate 1980
url http://dx.doi.org/10.1017/s0022143000010327
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000010327
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 25, issue 91, page 99-108
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000010327
container_title Journal of Glaciology
container_volume 25
container_issue 91
container_start_page 99
op_container_end_page 108
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