Dynamic models for impact-initiated stress waves through snow columns
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 configu...
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ftdoajarticles:oai:doaj.org/article:d581497e470b49c08aa49427fdb022e5 2024-09-15T18:15:41+00:00 Dynamic models for impact-initiated stress waves through snow columns Samuel Vincent Verplanck Edward Eagan Adams https://doi.org/10.1017/jog.2024.26 https://doaj.org/article/d581497e470b49c08aa49427fdb022e5 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143024000261/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2024.26 0022-1430 1727-5652 https://doaj.org/article/d581497e470b49c08aa49427fdb022e5 Journal of Glaciology, Pp 1-15 avalanches snow mechanics snow Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article ftdoajarticles https://doi.org/10.1017/jog.2024.26 2024-08-05T17:49:33Z 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 Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 1 15 |
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Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
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ftdoajarticles |
language |
English |
topic |
avalanches snow mechanics snow Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
avalanches snow mechanics snow Environmental sciences GE1-350 Meteorology. Climatology QC851-999 Samuel Vincent Verplanck Edward Eagan Adams Dynamic models for impact-initiated stress waves through snow columns |
topic_facet |
avalanches snow mechanics snow Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
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. |
format |
Article in Journal/Newspaper |
author |
Samuel Vincent Verplanck Edward Eagan Adams |
author_facet |
Samuel Vincent Verplanck Edward Eagan Adams |
author_sort |
Samuel Vincent Verplanck |
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 |
url |
https://doi.org/10.1017/jog.2024.26 https://doaj.org/article/d581497e470b49c08aa49427fdb022e5 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology, Pp 1-15 |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143024000261/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2024.26 0022-1430 1727-5652 https://doaj.org/article/d581497e470b49c08aa49427fdb022e5 |
op_doi |
https://doi.org/10.1017/jog.2024.26 |
container_title |
Journal of Glaciology |
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1 |
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15 |
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1810453623104077824 |