Estimating the effective elastic modulus and specific fracture energy of snowpack layers from field experiments

ABSTRACT Measurements of the mechanical properties of snow are essential for improving our understanding and the prediction of snow failure and hence avalanche release. We performed fracture mechanical experiments in which a crack was initiated by a saw in a weak snow layer underlying cohesive snow...

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Published in:Journal of Glaciology
Main Authors: VAN HERWIJNEN, ALEC, GAUME, JOHAN, BAIR, EDWARD H., REUTER, BENJAMIN, BIRKELAND, KARL W., SCHWEIZER, JÜRG
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2016
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2016.90
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143016000903
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spelling crcambridgeupr:10.1017/jog.2016.90 2024-09-15T18:15:39+00:00 Estimating the effective elastic modulus and specific fracture energy of snowpack layers from field experiments VAN HERWIJNEN, ALEC GAUME, JOHAN BAIR, EDWARD H. REUTER, BENJAMIN BIRKELAND, KARL W. SCHWEIZER, JÜRG 2016 http://dx.doi.org/10.1017/jog.2016.90 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143016000903 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by-nc-nd/4.0/ Journal of Glaciology volume 62, issue 236, page 997-1007 ISSN 0022-1430 1727-5652 journal-article 2016 crcambridgeupr https://doi.org/10.1017/jog.2016.90 2024-09-04T04:04:50Z ABSTRACT Measurements of the mechanical properties of snow are essential for improving our understanding and the prediction of snow failure and hence avalanche release. We performed fracture mechanical experiments in which a crack was initiated by a saw in a weak snow layer underlying cohesive snow slab layers. Using particle tracking velocimetry (PTV), the displacement field of the slab was determined and used to derive the mechanical energy of the system as a function of crack length. By fitting the estimates of mechanical energy to an analytical expression, we determined the slab effective elastic modulus and weak layer specific fracture energy for 80 different snowpack combinations, including persistent and nonpersistent weak snow layers. The effective elastic modulus of the slab ranged from 0.08 to 34 MPa and increased with mean slab density following a power-law relationship. The weak layer specific fracture energy ranged from 0.08 to 2.7 J m −2 and increased with overburden. While the values obtained for the effective elastic modulus of the slab agree with previously published low-frequency laboratory measurements over the entire density range, the values of the weak layer specific fracture energy are in some cases unrealistically high as they exceeded those of ice. We attribute this discrepancy to the fact that our linear elastic approach does not account for energy dissipation due to non-linear parts of the deformation in the slab and/or weak layer, which would undoubtedly decrease the amount of strain energy available for crack propagation. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 62 236 997 1007
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description ABSTRACT Measurements of the mechanical properties of snow are essential for improving our understanding and the prediction of snow failure and hence avalanche release. We performed fracture mechanical experiments in which a crack was initiated by a saw in a weak snow layer underlying cohesive snow slab layers. Using particle tracking velocimetry (PTV), the displacement field of the slab was determined and used to derive the mechanical energy of the system as a function of crack length. By fitting the estimates of mechanical energy to an analytical expression, we determined the slab effective elastic modulus and weak layer specific fracture energy for 80 different snowpack combinations, including persistent and nonpersistent weak snow layers. The effective elastic modulus of the slab ranged from 0.08 to 34 MPa and increased with mean slab density following a power-law relationship. The weak layer specific fracture energy ranged from 0.08 to 2.7 J m −2 and increased with overburden. While the values obtained for the effective elastic modulus of the slab agree with previously published low-frequency laboratory measurements over the entire density range, the values of the weak layer specific fracture energy are in some cases unrealistically high as they exceeded those of ice. We attribute this discrepancy to the fact that our linear elastic approach does not account for energy dissipation due to non-linear parts of the deformation in the slab and/or weak layer, which would undoubtedly decrease the amount of strain energy available for crack propagation.
format Article in Journal/Newspaper
author VAN HERWIJNEN, ALEC
GAUME, JOHAN
BAIR, EDWARD H.
REUTER, BENJAMIN
BIRKELAND, KARL W.
SCHWEIZER, JÜRG
spellingShingle VAN HERWIJNEN, ALEC
GAUME, JOHAN
BAIR, EDWARD H.
REUTER, BENJAMIN
BIRKELAND, KARL W.
SCHWEIZER, JÜRG
Estimating the effective elastic modulus and specific fracture energy of snowpack layers from field experiments
author_facet VAN HERWIJNEN, ALEC
GAUME, JOHAN
BAIR, EDWARD H.
REUTER, BENJAMIN
BIRKELAND, KARL W.
SCHWEIZER, JÜRG
author_sort VAN HERWIJNEN, ALEC
title Estimating the effective elastic modulus and specific fracture energy of snowpack layers from field experiments
title_short Estimating the effective elastic modulus and specific fracture energy of snowpack layers from field experiments
title_full Estimating the effective elastic modulus and specific fracture energy of snowpack layers from field experiments
title_fullStr Estimating the effective elastic modulus and specific fracture energy of snowpack layers from field experiments
title_full_unstemmed Estimating the effective elastic modulus and specific fracture energy of snowpack layers from field experiments
title_sort estimating the effective elastic modulus and specific fracture energy of snowpack layers from field experiments
publisher Cambridge University Press (CUP)
publishDate 2016
url http://dx.doi.org/10.1017/jog.2016.90
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143016000903
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 62, issue 236, page 997-1007
ISSN 0022-1430 1727-5652
op_rights http://creativecommons.org/licenses/by-nc-nd/4.0/
op_doi https://doi.org/10.1017/jog.2016.90
container_title Journal of Glaciology
container_volume 62
container_issue 236
container_start_page 997
op_container_end_page 1007
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