The Role of Stress Concentration in Slab Avalanche Release
Abstract Slab avalanches are shown to be released by brittle fracture. An analogy is drawn in which the snow-pack is considered to be a macroscopic, molecular model of glass. The analogy is examined qualitatively from two viewpoints: the Griffith fracture criterion, and stress concentration theory....
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Cambridge University Press (CUP)
1969
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Online Access: | http://dx.doi.org/10.1017/s0022143000027039 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000027039 |
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crcambridgeupr:10.1017/s0022143000027039 2024-09-15T18:15:39+00:00 The Role of Stress Concentration in Slab Avalanche Release Sommerfeld, R. A. 1969 http://dx.doi.org/10.1017/s0022143000027039 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000027039 en eng Cambridge University Press (CUP) Journal of Glaciology volume 8, issue 54, page 451-462 ISSN 0022-1430 1727-5652 journal-article 1969 crcambridgeupr https://doi.org/10.1017/s0022143000027039 2024-07-31T04:04:10Z Abstract Slab avalanches are shown to be released by brittle fracture. An analogy is drawn in which the snow-pack is considered to be a macroscopic, molecular model of glass. The analogy is examined qualitatively from two viewpoints: the Griffith fracture criterion, and stress concentration theory. The details of fracture propagation in a layered snow-pack are explained by means of stress concentration theory, and many details of slab avalanches are shown to be consistent with the proposed mechanism. The significance of various fracture surface markings is pointed out. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 8 54 451 462 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
Abstract Slab avalanches are shown to be released by brittle fracture. An analogy is drawn in which the snow-pack is considered to be a macroscopic, molecular model of glass. The analogy is examined qualitatively from two viewpoints: the Griffith fracture criterion, and stress concentration theory. The details of fracture propagation in a layered snow-pack are explained by means of stress concentration theory, and many details of slab avalanches are shown to be consistent with the proposed mechanism. The significance of various fracture surface markings is pointed out. |
format |
Article in Journal/Newspaper |
author |
Sommerfeld, R. A. |
spellingShingle |
Sommerfeld, R. A. The Role of Stress Concentration in Slab Avalanche Release |
author_facet |
Sommerfeld, R. A. |
author_sort |
Sommerfeld, R. A. |
title |
The Role of Stress Concentration in Slab Avalanche Release |
title_short |
The Role of Stress Concentration in Slab Avalanche Release |
title_full |
The Role of Stress Concentration in Slab Avalanche Release |
title_fullStr |
The Role of Stress Concentration in Slab Avalanche Release |
title_full_unstemmed |
The Role of Stress Concentration in Slab Avalanche Release |
title_sort |
role of stress concentration in slab avalanche release |
publisher |
Cambridge University Press (CUP) |
publishDate |
1969 |
url |
http://dx.doi.org/10.1017/s0022143000027039 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000027039 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 8, issue 54, page 451-462 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000027039 |
container_title |
Journal of Glaciology |
container_volume |
8 |
container_issue |
54 |
container_start_page |
451 |
op_container_end_page |
462 |
_version_ |
1810453584137945088 |