Micro-mechanical insights into the dynamics of crack propagation in snow fracture experiments

Abstract Dry-snow slab avalanches result from crack propagation in a highly porous weak layer buried within a stratified and metastable snowpack. While our understanding of slab avalanche mechanisms improved with recent experimental and numerical advances, fundamental micro-mechanical processes rema...

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Autores principales: Grégoire Bobillier, Bastian Bergfeld, Jürg Dual, Johan Gaume, Alec van Herwijnen, Jürg Schweizer
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Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/bb057f31a0094da484be0eace389574f
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spelling oai:doaj.org-article:bb057f31a0094da484be0eace389574f2021-12-02T18:24:55ZMicro-mechanical insights into the dynamics of crack propagation in snow fracture experiments10.1038/s41598-021-90910-32045-2322https://doaj.org/article/bb057f31a0094da484be0eace389574f2021-06-01T00:00:00Zhttps://doi.org/10.1038/s41598-021-90910-3https://doaj.org/toc/2045-2322Abstract Dry-snow slab avalanches result from crack propagation in a highly porous weak layer buried within a stratified and metastable snowpack. While our understanding of slab avalanche mechanisms improved with recent experimental and numerical advances, fundamental micro-mechanical processes remain poorly understood due to a lack of non-invasive monitoring techniques. Using a novel discrete micro-mechanical model, we reproduced crack propagation dynamics observed in field experiments, which employ the propagation saw test. The detailed microscopic analysis of weak layer stresses and bond breaking allowed us to define the crack tip location of closing crack faces, analyze its spatio-temporal characteristics and monitor the evolution of stress concentrations and the fracture process zone both in transient and steady-state regimes. Results highlight the occurrence of a steady state in crack speed and stress conditions for sufficiently long crack propagation distances (> 4 m). Crack propagation without external driving force except gravity is possible due to the local mixed-mode shear-compression stress nature at the crack tip induced by slab bending and weak layer volumetric collapse. Our result shed light into the microscopic origin of dynamic crack propagation in snow slab avalanche release that eventually will improve the evaluation of avalanche release sizes and thus hazard management and forecasting in mountainous regions.Grégoire BobillierBastian BergfeldJürg DualJohan GaumeAlec van HerwijnenJürg SchweizerNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 11, Iss 1, Pp 1-15 (2021)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Grégoire Bobillier
Bastian Bergfeld
Jürg Dual
Johan Gaume
Alec van Herwijnen
Jürg Schweizer
Micro-mechanical insights into the dynamics of crack propagation in snow fracture experiments
description Abstract Dry-snow slab avalanches result from crack propagation in a highly porous weak layer buried within a stratified and metastable snowpack. While our understanding of slab avalanche mechanisms improved with recent experimental and numerical advances, fundamental micro-mechanical processes remain poorly understood due to a lack of non-invasive monitoring techniques. Using a novel discrete micro-mechanical model, we reproduced crack propagation dynamics observed in field experiments, which employ the propagation saw test. The detailed microscopic analysis of weak layer stresses and bond breaking allowed us to define the crack tip location of closing crack faces, analyze its spatio-temporal characteristics and monitor the evolution of stress concentrations and the fracture process zone both in transient and steady-state regimes. Results highlight the occurrence of a steady state in crack speed and stress conditions for sufficiently long crack propagation distances (> 4 m). Crack propagation without external driving force except gravity is possible due to the local mixed-mode shear-compression stress nature at the crack tip induced by slab bending and weak layer volumetric collapse. Our result shed light into the microscopic origin of dynamic crack propagation in snow slab avalanche release that eventually will improve the evaluation of avalanche release sizes and thus hazard management and forecasting in mountainous regions.
format article
author Grégoire Bobillier
Bastian Bergfeld
Jürg Dual
Johan Gaume
Alec van Herwijnen
Jürg Schweizer
author_facet Grégoire Bobillier
Bastian Bergfeld
Jürg Dual
Johan Gaume
Alec van Herwijnen
Jürg Schweizer
author_sort Grégoire Bobillier
title Micro-mechanical insights into the dynamics of crack propagation in snow fracture experiments
title_short Micro-mechanical insights into the dynamics of crack propagation in snow fracture experiments
title_full Micro-mechanical insights into the dynamics of crack propagation in snow fracture experiments
title_fullStr Micro-mechanical insights into the dynamics of crack propagation in snow fracture experiments
title_full_unstemmed Micro-mechanical insights into the dynamics of crack propagation in snow fracture experiments
title_sort micro-mechanical insights into the dynamics of crack propagation in snow fracture experiments
publisher Nature Portfolio
publishDate 2021
url https://doaj.org/article/bb057f31a0094da484be0eace389574f
work_keys_str_mv AT gregoirebobillier micromechanicalinsightsintothedynamicsofcrackpropagationinsnowfractureexperiments
AT bastianbergfeld micromechanicalinsightsintothedynamicsofcrackpropagationinsnowfractureexperiments
AT jurgdual micromechanicalinsightsintothedynamicsofcrackpropagationinsnowfractureexperiments
AT johangaume micromechanicalinsightsintothedynamicsofcrackpropagationinsnowfractureexperiments
AT alecvanherwijnen micromechanicalinsightsintothedynamicsofcrackpropagationinsnowfractureexperiments
AT jurgschweizer micromechanicalinsightsintothedynamicsofcrackpropagationinsnowfractureexperiments
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