Modeling of crack propagation in weak snowpack layers using the discrete element method

Dry-snow slab avalanches are generally caused by a sequence of fracture processes including (1) failure initiation in a weak snow layer underlying a cohesive slab, (2) crack propagation within the weak layer and (3) tensile fracture through the slab which leads to its detachment. During the past dec...

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Published in:The Cryosphere
Main Authors: J. Gaume, A. van Herwijnen, G. Chambon, K. W. Birkeland, J. Schweizer
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2015
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-9-1915-2015
http://www.the-cryosphere.net/9/1915/2015/tc-9-1915-2015.pdf
https://doaj.org/article/cacf17119781478180f91e74b3d9a7a9
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:cacf17119781478180f91e74b3d9a7a9 2023-05-15T18:32:22+02:00 Modeling of crack propagation in weak snowpack layers using the discrete element method J. Gaume A. van Herwijnen G. Chambon K. W. Birkeland J. Schweizer 2015-10-01 https://doi.org/10.5194/tc-9-1915-2015 http://www.the-cryosphere.net/9/1915/2015/tc-9-1915-2015.pdf https://doaj.org/article/cacf17119781478180f91e74b3d9a7a9 en eng Copernicus Publications 1994-0416 1994-0424 doi:10.5194/tc-9-1915-2015 http://www.the-cryosphere.net/9/1915/2015/tc-9-1915-2015.pdf https://doaj.org/article/cacf17119781478180f91e74b3d9a7a9 undefined The Cryosphere, Vol 9, Iss 5, Pp 1915-1932 (2015) geo info Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2015 fttriple https://doi.org/10.5194/tc-9-1915-2015 2023-01-22T18:11:43Z Dry-snow slab avalanches are generally caused by a sequence of fracture processes including (1) failure initiation in a weak snow layer underlying a cohesive slab, (2) crack propagation within the weak layer and (3) tensile fracture through the slab which leads to its detachment. During the past decades, theoretical and experimental work has gradually led to a better understanding of the fracture process in snow involving the collapse of the structure in the weak layer during fracture. This now allows us to better model failure initiation and the onset of crack propagation, i.e., to estimate the critical length required for crack propagation. On the other hand, our understanding of dynamic crack propagation and fracture arrest propensity is still very limited. To shed more light on this issue, we performed numerical propagation saw test (PST) experiments applying the discrete element (DE) method and compared the numerical results with field measurements based on particle tracking. The goal is to investigate the influence of weak layer failure and the mechanical properties of the slab on crack propagation and fracture arrest propensity. Crack propagation speeds and distances before fracture arrest were derived from the DE simulations for different snowpack configurations and mechanical properties. Then, in order to compare the numerical and experimental results, the slab mechanical properties (Young's modulus and strength) which are not measured in the field were derived from density. The simulations nicely reproduced the process of crack propagation observed in field PSTs. Finally, the mechanical processes at play were analyzed in depth which led to suggestions for minimum column length in field PSTs. Article in Journal/Newspaper The Cryosphere Unknown The Cryosphere 9 5 1915 1932
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
info
spellingShingle geo
info
J. Gaume
A. van Herwijnen
G. Chambon
K. W. Birkeland
J. Schweizer
Modeling of crack propagation in weak snowpack layers using the discrete element method
topic_facet geo
info
description Dry-snow slab avalanches are generally caused by a sequence of fracture processes including (1) failure initiation in a weak snow layer underlying a cohesive slab, (2) crack propagation within the weak layer and (3) tensile fracture through the slab which leads to its detachment. During the past decades, theoretical and experimental work has gradually led to a better understanding of the fracture process in snow involving the collapse of the structure in the weak layer during fracture. This now allows us to better model failure initiation and the onset of crack propagation, i.e., to estimate the critical length required for crack propagation. On the other hand, our understanding of dynamic crack propagation and fracture arrest propensity is still very limited. To shed more light on this issue, we performed numerical propagation saw test (PST) experiments applying the discrete element (DE) method and compared the numerical results with field measurements based on particle tracking. The goal is to investigate the influence of weak layer failure and the mechanical properties of the slab on crack propagation and fracture arrest propensity. Crack propagation speeds and distances before fracture arrest were derived from the DE simulations for different snowpack configurations and mechanical properties. Then, in order to compare the numerical and experimental results, the slab mechanical properties (Young's modulus and strength) which are not measured in the field were derived from density. The simulations nicely reproduced the process of crack propagation observed in field PSTs. Finally, the mechanical processes at play were analyzed in depth which led to suggestions for minimum column length in field PSTs.
format Article in Journal/Newspaper
author J. Gaume
A. van Herwijnen
G. Chambon
K. W. Birkeland
J. Schweizer
author_facet J. Gaume
A. van Herwijnen
G. Chambon
K. W. Birkeland
J. Schweizer
author_sort J. Gaume
title Modeling of crack propagation in weak snowpack layers using the discrete element method
title_short Modeling of crack propagation in weak snowpack layers using the discrete element method
title_full Modeling of crack propagation in weak snowpack layers using the discrete element method
title_fullStr Modeling of crack propagation in weak snowpack layers using the discrete element method
title_full_unstemmed Modeling of crack propagation in weak snowpack layers using the discrete element method
title_sort modeling of crack propagation in weak snowpack layers using the discrete element method
publisher Copernicus Publications
publishDate 2015
url https://doi.org/10.5194/tc-9-1915-2015
http://www.the-cryosphere.net/9/1915/2015/tc-9-1915-2015.pdf
https://doaj.org/article/cacf17119781478180f91e74b3d9a7a9
genre The Cryosphere
genre_facet The Cryosphere
op_source The Cryosphere, Vol 9, Iss 5, Pp 1915-1932 (2015)
op_relation 1994-0416
1994-0424
doi:10.5194/tc-9-1915-2015
http://www.the-cryosphere.net/9/1915/2015/tc-9-1915-2015.pdf
https://doaj.org/article/cacf17119781478180f91e74b3d9a7a9
op_rights undefined
op_doi https://doi.org/10.5194/tc-9-1915-2015
container_title The Cryosphere
container_volume 9
container_issue 5
container_start_page 1915
op_container_end_page 1932
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