The Relationship between the Visco-Elastic and Structural Properties of Fine-Grained Snow

New and felt-like snow was sieved and sintered at a constant temperature in order to produce homogeneous samples of fine, rounded-grain snow with a density in the range 270–340 kg m −3 . The structure of single samples was changed in stages by non-destructive uniaxial compression. This deformation,...

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Published in:Journal of Glaciology
Main Author: Kry, P. R.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1975
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000021985
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021985
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spelling crcambridgeupr:10.1017/s0022143000021985 2024-04-07T07:53:41+00:00 The Relationship between the Visco-Elastic and Structural Properties of Fine-Grained Snow Kry, P. R. 1975 http://dx.doi.org/10.1017/s0022143000021985 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021985 en eng Cambridge University Press (CUP) Journal of Glaciology volume 14, issue 72, page 479-500 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1975 crcambridgeupr https://doi.org/10.1017/s0022143000021985 2024-03-08T00:35:21Z New and felt-like snow was sieved and sintered at a constant temperature in order to produce homogeneous samples of fine, rounded-grain snow with a density in the range 270–340 kg m −3 . The structure of single samples was changed in stages by non-destructive uniaxial compression. This deformation, which amounted to 30%, took place within 8 hours (thus limiting temperature metamorphism). At each stage the Young’s modulus was measured quasi-statically and the creep behaviour under constant uniaxial compression was recorded. Stereological analysis of sections from the samples provided mean values for both grain-bond and grain properties. The Young’s modulus increased with density slightly more strongly than linearly, whereas the low-stress viscosity in unconfined compression increased nearly exponentially for densities less than 380 kg m −3 . The maximum densification resulted in a 15-fold increase in the measured visco-elastic properties. However, the number of grain bonds per unit mass increased linearly by a factor in the range 1.5 to 2 while the average grain-bond size remained constant. It is concluded that only a fraction of the grain bonds in a snow sample transmit an applied stress, and that the new grain bonds formed during the deformation of a snow sample determine the visco-elastic properties of snow. The hypothesis that chains, defined as series of stress-bearing grains, are the basic units of snow structure is developed. Semi-quantitative calculations developed from the chain concept explain the observed variations in the visco-elastic properties. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 14 72 479 500
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Kry, P. R.
The Relationship between the Visco-Elastic and Structural Properties of Fine-Grained Snow
topic_facet Earth-Surface Processes
description New and felt-like snow was sieved and sintered at a constant temperature in order to produce homogeneous samples of fine, rounded-grain snow with a density in the range 270–340 kg m −3 . The structure of single samples was changed in stages by non-destructive uniaxial compression. This deformation, which amounted to 30%, took place within 8 hours (thus limiting temperature metamorphism). At each stage the Young’s modulus was measured quasi-statically and the creep behaviour under constant uniaxial compression was recorded. Stereological analysis of sections from the samples provided mean values for both grain-bond and grain properties. The Young’s modulus increased with density slightly more strongly than linearly, whereas the low-stress viscosity in unconfined compression increased nearly exponentially for densities less than 380 kg m −3 . The maximum densification resulted in a 15-fold increase in the measured visco-elastic properties. However, the number of grain bonds per unit mass increased linearly by a factor in the range 1.5 to 2 while the average grain-bond size remained constant. It is concluded that only a fraction of the grain bonds in a snow sample transmit an applied stress, and that the new grain bonds formed during the deformation of a snow sample determine the visco-elastic properties of snow. The hypothesis that chains, defined as series of stress-bearing grains, are the basic units of snow structure is developed. Semi-quantitative calculations developed from the chain concept explain the observed variations in the visco-elastic properties.
format Article in Journal/Newspaper
author Kry, P. R.
author_facet Kry, P. R.
author_sort Kry, P. R.
title The Relationship between the Visco-Elastic and Structural Properties of Fine-Grained Snow
title_short The Relationship between the Visco-Elastic and Structural Properties of Fine-Grained Snow
title_full The Relationship between the Visco-Elastic and Structural Properties of Fine-Grained Snow
title_fullStr The Relationship between the Visco-Elastic and Structural Properties of Fine-Grained Snow
title_full_unstemmed The Relationship between the Visco-Elastic and Structural Properties of Fine-Grained Snow
title_sort relationship between the visco-elastic and structural properties of fine-grained snow
publisher Cambridge University Press (CUP)
publishDate 1975
url http://dx.doi.org/10.1017/s0022143000021985
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021985
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 14, issue 72, page 479-500
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000021985
container_title Journal of Glaciology
container_volume 14
container_issue 72
container_start_page 479
op_container_end_page 500
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