Microstructure-based modeling of snow mechanics: a discrete element approach

Rapid and large deformations of snow are mainly controlled by grain rearrangements, which occur through the failure of cohesive bonds and the creation of new contacts. We exploit a granular description of snow to develop a discrete element model based on the full 3-D microstructure captured by micro...

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Main Authors: P. Hagenmuller, G. Chambon, M. Naaim
Format: Article
Language:English
Published: Copernicus Publications 2015-10-01
Series:The Cryosphere
Online Access:http://www.the-cryosphere.net/9/1969/2015/tc-9-1969-2015.pdf
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spelling doaj-d168c7183e0c42c490e735740324db312020-11-24T22:54:17ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242015-10-01951969198210.5194/tc-9-1969-2015Microstructure-based modeling of snow mechanics: a discrete element approachP. Hagenmuller0G. Chambon1M. Naaim2Météo-France – CNRS, CNRM-GAME, UMR 3589, CEN, 38400 Saint Martin d'Hères, FranceIrstea, UR ETGR Erosion torrentielle, neige et avalanches, 38402 Saint Martin d'Hères, FranceIrstea, UR ETGR Erosion torrentielle, neige et avalanches, 38402 Saint Martin d'Hères, FranceRapid and large deformations of snow are mainly controlled by grain rearrangements, which occur through the failure of cohesive bonds and the creation of new contacts. We exploit a granular description of snow to develop a discrete element model based on the full 3-D microstructure captured by microtomography. The model assumes that snow is composed of rigid grains interacting through localized contacts accounting for cohesion and friction. The geometry of the grains and of the intergranular bonding system are explicitly defined from microtomographic data using geometrical criteria based on curvature and contiguity. Single grains are represented as rigid clumps of spheres. The model is applied to different snow samples subjected to confined compression tests. A detailed sensitivity analysis shows that artifacts introduced by the modeling approach and the influence of numerical parameters are limited compared to variations due to the geometry of the microstructure. The model shows that the compression behavior of snow is mainly controlled by the density of the samples, but that deviations from a pure density parameterization are not insignificant during the first phase of deformation. In particular, the model correctly predicts that, for a given density, faceted crystals are less resistant to compression than rounded grains or decomposed snow. For larger compression strains, no clear differences between snow types are observed.http://www.the-cryosphere.net/9/1969/2015/tc-9-1969-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author P. Hagenmuller
G. Chambon
M. Naaim
spellingShingle P. Hagenmuller
G. Chambon
M. Naaim
Microstructure-based modeling of snow mechanics: a discrete element approach
The Cryosphere
author_facet P. Hagenmuller
G. Chambon
M. Naaim
author_sort P. Hagenmuller
title Microstructure-based modeling of snow mechanics: a discrete element approach
title_short Microstructure-based modeling of snow mechanics: a discrete element approach
title_full Microstructure-based modeling of snow mechanics: a discrete element approach
title_fullStr Microstructure-based modeling of snow mechanics: a discrete element approach
title_full_unstemmed Microstructure-based modeling of snow mechanics: a discrete element approach
title_sort microstructure-based modeling of snow mechanics: a discrete element approach
publisher Copernicus Publications
series The Cryosphere
issn 1994-0416
1994-0424
publishDate 2015-10-01
description Rapid and large deformations of snow are mainly controlled by grain rearrangements, which occur through the failure of cohesive bonds and the creation of new contacts. We exploit a granular description of snow to develop a discrete element model based on the full 3-D microstructure captured by microtomography. The model assumes that snow is composed of rigid grains interacting through localized contacts accounting for cohesion and friction. The geometry of the grains and of the intergranular bonding system are explicitly defined from microtomographic data using geometrical criteria based on curvature and contiguity. Single grains are represented as rigid clumps of spheres. The model is applied to different snow samples subjected to confined compression tests. A detailed sensitivity analysis shows that artifacts introduced by the modeling approach and the influence of numerical parameters are limited compared to variations due to the geometry of the microstructure. The model shows that the compression behavior of snow is mainly controlled by the density of the samples, but that deviations from a pure density parameterization are not insignificant during the first phase of deformation. In particular, the model correctly predicts that, for a given density, faceted crystals are less resistant to compression than rounded grains or decomposed snow. For larger compression strains, no clear differences between snow types are observed.
url http://www.the-cryosphere.net/9/1969/2015/tc-9-1969-2015.pdf
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