Mechanical behaviour and structure of snow under uniaxial tensile stress

Abstract The mechanical behaviour of snow was studied at — 10°C under uniaxial tensile stress in a range of cross-head speed 6.8 × 10 –8 to 3.1 × 10 –4 ms –1 and snow density 240-470 kg m –3 .It was found from the resisting force-deformation curves that the snow was deformed in two different ways: n...

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Published in:Journal of Glaciology
Main Author: Narita, Hidek
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1980
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000010819
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000010819
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spelling crcambridgeupr:10.1017/s0022143000010819 2024-09-15T18:15:37+00:00 Mechanical behaviour and structure of snow under uniaxial tensile stress Narita, Hidek 1980 http://dx.doi.org/10.1017/s0022143000010819 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000010819 en eng Cambridge University Press (CUP) Journal of Glaciology volume 26, issue 94, page 275-282 ISSN 0022-1430 1727-5652 journal-article 1980 crcambridgeupr https://doi.org/10.1017/s0022143000010819 2024-08-28T04:03:41Z Abstract The mechanical behaviour of snow was studied at — 10°C under uniaxial tensile stress in a range of cross-head speed 6.8 × 10 –8 to 3.1 × 10 –4 ms –1 and snow density 240-470 kg m –3 .It was found from the resisting force-deformation curves that the snow was deformed in two different ways: namely, brittle and ductile deformation at high and low strain-rates, respectively. The critical strain-rate dividing the two deformation modes was found to depend on the density of snow. In ductile deformation, many small cracks appeared throughout the entire specimen. Their features were observed by making thin sections and they were compared with small cracks formed in natural snow on a mountain slope. The maximum strength of snow was found to depend on strain-rate: at strain-rates above about 10 –5 s –1 , the maximum strength increased with decreasing strain-rate but below 10 –5 s –1 it decreased with decreasing strain-rate. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 26 94 275 282
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract The mechanical behaviour of snow was studied at — 10°C under uniaxial tensile stress in a range of cross-head speed 6.8 × 10 –8 to 3.1 × 10 –4 ms –1 and snow density 240-470 kg m –3 .It was found from the resisting force-deformation curves that the snow was deformed in two different ways: namely, brittle and ductile deformation at high and low strain-rates, respectively. The critical strain-rate dividing the two deformation modes was found to depend on the density of snow. In ductile deformation, many small cracks appeared throughout the entire specimen. Their features were observed by making thin sections and they were compared with small cracks formed in natural snow on a mountain slope. The maximum strength of snow was found to depend on strain-rate: at strain-rates above about 10 –5 s –1 , the maximum strength increased with decreasing strain-rate but below 10 –5 s –1 it decreased with decreasing strain-rate.
format Article in Journal/Newspaper
author Narita, Hidek
spellingShingle Narita, Hidek
Mechanical behaviour and structure of snow under uniaxial tensile stress
author_facet Narita, Hidek
author_sort Narita, Hidek
title Mechanical behaviour and structure of snow under uniaxial tensile stress
title_short Mechanical behaviour and structure of snow under uniaxial tensile stress
title_full Mechanical behaviour and structure of snow under uniaxial tensile stress
title_fullStr Mechanical behaviour and structure of snow under uniaxial tensile stress
title_full_unstemmed Mechanical behaviour and structure of snow under uniaxial tensile stress
title_sort mechanical behaviour and structure of snow under uniaxial tensile stress
publisher Cambridge University Press (CUP)
publishDate 1980
url http://dx.doi.org/10.1017/s0022143000010819
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000010819
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 26, issue 94, page 275-282
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000010819
container_title Journal of Glaciology
container_volume 26
container_issue 94
container_start_page 275
op_container_end_page 282
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