Dynamic models for impact-initiated stress waves through snow columns

Abstract The objective of this research is to model snow's response to dynamic, impact loading. Two constitutive relationships are considered: elastic and Maxwell-viscoelastic. These material models are applied to laboratory experiments consisting of 1000 individual impacts across 22 snow colum...

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Published in:Journal of Glaciology
Main Authors: Verplanck, Samuel Vincent, Adams, Edward Eagan
Other Authors: Montana State University
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2024
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2024.26
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143024000261
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spelling crcambridgeupr:10.1017/jog.2024.26 2024-09-15T18:15:37+00:00 Dynamic models for impact-initiated stress waves through snow columns Verplanck, Samuel Vincent Adams, Edward Eagan Montana State University 2024 http://dx.doi.org/10.1017/jog.2024.26 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143024000261 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Journal of Glaciology page 1-15 ISSN 0022-1430 1727-5652 journal-article 2024 crcambridgeupr https://doi.org/10.1017/jog.2024.26 2024-08-21T04:03:56Z Abstract The objective of this research is to model snow's response to dynamic, impact loading. Two constitutive relationships are considered: elastic and Maxwell-viscoelastic. These material models are applied to laboratory experiments consisting of 1000 individual impacts across 22 snow column configurations. The columns are 60 cm tall with a 30 cm by 30 cm cross-section. The snow ranges in density from 135 to 428 kg m −3 and is loaded with both short-duration (~1 ms) and long-duration (~10 ms) impacts. The Maxwell-viscoelastic model more accurately describes snow's response because it contains a mechanism for energy dissipation, which the elastic model does not. Furthermore, the ascertained model parameters show a clear dependence on impact duration; shorter duration impacts resulted in higher wave speeds and greater damping coefficients. The stress wave's magnitude is amplified when it hits a stiffer material because of the positive interference between incident and reflected waves. This phenomenon is observed in the laboratory and modeled with the governing equations. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 1 35
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract The objective of this research is to model snow's response to dynamic, impact loading. Two constitutive relationships are considered: elastic and Maxwell-viscoelastic. These material models are applied to laboratory experiments consisting of 1000 individual impacts across 22 snow column configurations. The columns are 60 cm tall with a 30 cm by 30 cm cross-section. The snow ranges in density from 135 to 428 kg m −3 and is loaded with both short-duration (~1 ms) and long-duration (~10 ms) impacts. The Maxwell-viscoelastic model more accurately describes snow's response because it contains a mechanism for energy dissipation, which the elastic model does not. Furthermore, the ascertained model parameters show a clear dependence on impact duration; shorter duration impacts resulted in higher wave speeds and greater damping coefficients. The stress wave's magnitude is amplified when it hits a stiffer material because of the positive interference between incident and reflected waves. This phenomenon is observed in the laboratory and modeled with the governing equations.
author2 Montana State University
format Article in Journal/Newspaper
author Verplanck, Samuel Vincent
Adams, Edward Eagan
spellingShingle Verplanck, Samuel Vincent
Adams, Edward Eagan
Dynamic models for impact-initiated stress waves through snow columns
author_facet Verplanck, Samuel Vincent
Adams, Edward Eagan
author_sort Verplanck, Samuel Vincent
title Dynamic models for impact-initiated stress waves through snow columns
title_short Dynamic models for impact-initiated stress waves through snow columns
title_full Dynamic models for impact-initiated stress waves through snow columns
title_fullStr Dynamic models for impact-initiated stress waves through snow columns
title_full_unstemmed Dynamic models for impact-initiated stress waves through snow columns
title_sort dynamic models for impact-initiated stress waves through snow columns
publisher Cambridge University Press (CUP)
publishDate 2024
url http://dx.doi.org/10.1017/jog.2024.26
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143024000261
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
page 1-15
ISSN 0022-1430 1727-5652
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2024.26
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 35
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