Tensile strain and fracture of snow

Abstract Measurements over several hours of the tensile strain of snow have been carried out, and the strain-rate e can be expressed in terms of stress σ, elapsed time t, and (Celsius) snow temperature T as . It is evident from this expression that a creep fracture does not happen without either an...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Watanabe, Zempachi
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1980
Subjects:
Earth-Surface Processes
Journal of Glaciology
Online Access:http://dx.doi.org/10.1017/s0022143000010790
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000010790
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spelling crcambridgeupr:10.1017/s0022143000010790 2024-03-03T08:46:05+00:00 Tensile strain and fracture of snow Watanabe, Zempachi 1980 http://dx.doi.org/10.1017/s0022143000010790 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000010790 en eng Cambridge University Press (CUP) Journal of Glaciology volume 26, issue 94, page 255-262 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1980 crcambridgeupr https://doi.org/10.1017/s0022143000010790 2024-02-08T08:47:47Z Abstract Measurements over several hours of the tensile strain of snow have been carried out, and the strain-rate e can be expressed in terms of stress σ, elapsed time t, and (Celsius) snow temperature T as . It is evident from this expression that a creep fracture does not happen without either an increase of stress or a rise of temperature. We observed the phenomenon of creep fracture of snow by these two methods. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 26 94 255 262
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Watanabe, Zempachi
Tensile strain and fracture of snow
topic_facet Earth-Surface Processes
description Abstract Measurements over several hours of the tensile strain of snow have been carried out, and the strain-rate e can be expressed in terms of stress σ, elapsed time t, and (Celsius) snow temperature T as . It is evident from this expression that a creep fracture does not happen without either an increase of stress or a rise of temperature. We observed the phenomenon of creep fracture of snow by these two methods.
format Article in Journal/Newspaper
author Watanabe, Zempachi
author_facet Watanabe, Zempachi
author_sort Watanabe, Zempachi
title Tensile strain and fracture of snow
title_short Tensile strain and fracture of snow
title_full Tensile strain and fracture of snow
title_fullStr Tensile strain and fracture of snow
title_full_unstemmed Tensile strain and fracture of snow
title_sort tensile strain and fracture of snow
publisher Cambridge University Press (CUP)
publishDate 1980
url http://dx.doi.org/10.1017/s0022143000010790
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000010790
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 26, issue 94, page 255-262
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000010790
container_title Journal of Glaciology
container_volume 26
container_issue 94
container_start_page 255
op_container_end_page 262
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