Modeling snow slab avalanches caused by weak-layer failure – Part 2: Coupled mixed-mode criterion forskier-triggered anticracks

Using the analytical model presented in Part 1 ofthis two-part paper, a new conceptual understanding of an-ticrack nucleation in weak layers is proposed. To obtain asufficient condition for onset of failure, two necessary con-ditions must be satisfied simultaneously: (i) the weak layermust be overlo...

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Published in:The Cryosphere
Main Authors: Rosendahl, Philipp L., Weißgraeber, Philipp
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus 2020
Subjects:
Online Access:http://tuprints.ulb.tu-darmstadt.de/11574/
https://tuprints.ulb.tu-darmstadt.de/11574/1/rosendahl2.pdf
https://doi.org/10.5194/tc-14-131-2020
https://doi.org/10.25534/tuprints-00011574
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spelling ftulbdarmstadt:oai:tuprints.ulb.tu-darmstadt.de:11574 2023-09-05T13:23:43+02:00 Modeling snow slab avalanches caused by weak-layer failure – Part 2: Coupled mixed-mode criterion forskier-triggered anticracks Rosendahl, Philipp L. Weißgraeber, Philipp 2020 text http://tuprints.ulb.tu-darmstadt.de/11574/ https://tuprints.ulb.tu-darmstadt.de/11574/1/rosendahl2.pdf https://doi.org/10.5194/tc-14-131-2020 https://doi.org/10.25534/tuprints-00011574 en eng Copernicus https://tuprints.ulb.tu-darmstadt.de/11574/1/rosendahl2.pdf Rosendahl, Philipp L. <http://tuprints.ulb.tu-darmstadt.de/view/person/Rosendahl=3APhilipp_L=2E=3A=3A.html> Weißgraeber, Philipp <http://tuprints.ulb.tu-darmstadt.de/view/person/Wei=DFgraeber=3APhilipp=3A=3A.html> (2020):Modeling snow slab avalanches caused by weak-layer failure – Part 2: Coupled mixed-mode criterion forskier-triggered anticracks.In: The Cryosphere, 14 (1), pp. 131-145. Copernicus, ISSN 1994-0424, DOI:10.25534/tuprints-00011574 <https://doi.org/10.25534/tuprints-00011574>, [Article] CC BY 4.0 International - Creative Commons, Attribution info:eu-repo/semantics/openAccess Article NonPeerReviewed info:eu-repo/semantics/article 2020 ftulbdarmstadt https://doi.org/10.5194/tc-14-131-202010.25534/tuprints-00011574 2023-08-22T19:46:05Z Using the analytical model presented in Part 1 ofthis two-part paper, a new conceptual understanding of an-ticrack nucleation in weak layers is proposed. To obtain asufficient condition for onset of failure, two necessary con-ditions must be satisfied simultaneously: (i) the weak layermust be overloaded in terms of stress and (ii) the initiatingcrack must release enough energy for the formation of newsurfaces. This so-called coupled criterion was proposed byLeguillon (2002). No assumptions on initial defects withinthe weak layer are needed. Instead, the failure criterion pro-vides both critical loading and the size of initiating cracks.It only requires the fundamental material properties strengthand fracture toughness as inputs. Crack initiation and sub-sequent propagation are covered by a single criterion con-taining both a strength-of-materials and a fracture mechanicscondition.Analyses of skier-loaded snowpacks show the impact ofslab thickness and slope angle on critical loading and crackinitiation length. In the limit cases of very thick slabs andvery steep slopes, we obtain natural avalanche release. A dis-cussion of different mixed-mode stress and energy criteriareveals that a wrong choice of mixed-mode hypotheses canyield unphysical results. The effect of material parameterssuch as density and compliance on weak-layer collapse is il-lustrated.The framework presented in this two-part series harnessesthe efficiency of closed-form solutions to provide fast andphysically sound predictions of critical snowpack loads us-ing a new conceptual understanding of mixed-mode weak-layer failure. It emphasized the importance of both stress andenergy in avalanche release. Article in Journal/Newspaper The Cryosphere TU Darmstadt: tuprints The Cryosphere 14 1 131 145
institution Open Polar
collection TU Darmstadt: tuprints
op_collection_id ftulbdarmstadt
language English
description Using the analytical model presented in Part 1 ofthis two-part paper, a new conceptual understanding of an-ticrack nucleation in weak layers is proposed. To obtain asufficient condition for onset of failure, two necessary con-ditions must be satisfied simultaneously: (i) the weak layermust be overloaded in terms of stress and (ii) the initiatingcrack must release enough energy for the formation of newsurfaces. This so-called coupled criterion was proposed byLeguillon (2002). No assumptions on initial defects withinthe weak layer are needed. Instead, the failure criterion pro-vides both critical loading and the size of initiating cracks.It only requires the fundamental material properties strengthand fracture toughness as inputs. Crack initiation and sub-sequent propagation are covered by a single criterion con-taining both a strength-of-materials and a fracture mechanicscondition.Analyses of skier-loaded snowpacks show the impact ofslab thickness and slope angle on critical loading and crackinitiation length. In the limit cases of very thick slabs andvery steep slopes, we obtain natural avalanche release. A dis-cussion of different mixed-mode stress and energy criteriareveals that a wrong choice of mixed-mode hypotheses canyield unphysical results. The effect of material parameterssuch as density and compliance on weak-layer collapse is il-lustrated.The framework presented in this two-part series harnessesthe efficiency of closed-form solutions to provide fast andphysically sound predictions of critical snowpack loads us-ing a new conceptual understanding of mixed-mode weak-layer failure. It emphasized the importance of both stress andenergy in avalanche release.
format Article in Journal/Newspaper
author Rosendahl, Philipp L.
Weißgraeber, Philipp
spellingShingle Rosendahl, Philipp L.
Weißgraeber, Philipp
Modeling snow slab avalanches caused by weak-layer failure – Part 2: Coupled mixed-mode criterion forskier-triggered anticracks
author_facet Rosendahl, Philipp L.
Weißgraeber, Philipp
author_sort Rosendahl, Philipp L.
title Modeling snow slab avalanches caused by weak-layer failure – Part 2: Coupled mixed-mode criterion forskier-triggered anticracks
title_short Modeling snow slab avalanches caused by weak-layer failure – Part 2: Coupled mixed-mode criterion forskier-triggered anticracks
title_full Modeling snow slab avalanches caused by weak-layer failure – Part 2: Coupled mixed-mode criterion forskier-triggered anticracks
title_fullStr Modeling snow slab avalanches caused by weak-layer failure – Part 2: Coupled mixed-mode criterion forskier-triggered anticracks
title_full_unstemmed Modeling snow slab avalanches caused by weak-layer failure – Part 2: Coupled mixed-mode criterion forskier-triggered anticracks
title_sort modeling snow slab avalanches caused by weak-layer failure – part 2: coupled mixed-mode criterion forskier-triggered anticracks
publisher Copernicus
publishDate 2020
url http://tuprints.ulb.tu-darmstadt.de/11574/
https://tuprints.ulb.tu-darmstadt.de/11574/1/rosendahl2.pdf
https://doi.org/10.5194/tc-14-131-2020
https://doi.org/10.25534/tuprints-00011574
genre The Cryosphere
genre_facet The Cryosphere
op_relation https://tuprints.ulb.tu-darmstadt.de/11574/1/rosendahl2.pdf
Rosendahl, Philipp L. <http://tuprints.ulb.tu-darmstadt.de/view/person/Rosendahl=3APhilipp_L=2E=3A=3A.html>
Weißgraeber, Philipp <http://tuprints.ulb.tu-darmstadt.de/view/person/Wei=DFgraeber=3APhilipp=3A=3A.html> (2020):Modeling snow slab avalanches caused by weak-layer failure – Part 2: Coupled mixed-mode criterion forskier-triggered anticracks.In: The Cryosphere, 14 (1), pp. 131-145. Copernicus, ISSN 1994-0424, DOI:10.25534/tuprints-00011574 <https://doi.org/10.25534/tuprints-00011574>, [Article]
op_rights CC BY 4.0 International - Creative Commons, Attribution
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5194/tc-14-131-202010.25534/tuprints-00011574
container_title The Cryosphere
container_volume 14
container_issue 1
container_start_page 131
op_container_end_page 145
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