The influence of edge effects on crack propagation in snow stability tests

The Extended Column Test (ECT) and the Propagation Saw Test (PST) are two commonly used tests to assess the likelihood of crack propagation in a snowpack. Guidelines suggest beams with lengths of around 1 m, yet little is known about how test length affects propagation. Thus, we performed 163 ECTs a...

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Published in:The Cryosphere
Main Authors: E. H. Bair, R. Simenhois, A. van Herwijnen, K. Birkeland
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2014
Subjects:
Online Access:https://doi.org/10.5194/tc-8-1407-2014
http://www.the-cryosphere.net/8/1407/2014/tc-8-1407-2014.pdf
https://doaj.org/article/7e87e7e6fdee4d939a73548312552305
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:7e87e7e6fdee4d939a73548312552305 2023-05-15T18:32:23+02:00 The influence of edge effects on crack propagation in snow stability tests E. H. Bair R. Simenhois A. van Herwijnen K. Birkeland 2014-08-01 https://doi.org/10.5194/tc-8-1407-2014 http://www.the-cryosphere.net/8/1407/2014/tc-8-1407-2014.pdf https://doaj.org/article/7e87e7e6fdee4d939a73548312552305 en eng Copernicus Publications 1994-0416 1994-0424 doi:10.5194/tc-8-1407-2014 http://www.the-cryosphere.net/8/1407/2014/tc-8-1407-2014.pdf https://doaj.org/article/7e87e7e6fdee4d939a73548312552305 undefined The Cryosphere, Vol 8, Iss 4, Pp 1407-1418 (2014) info envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2014 fttriple https://doi.org/10.5194/tc-8-1407-2014 2023-01-22T19:30:49Z The Extended Column Test (ECT) and the Propagation Saw Test (PST) are two commonly used tests to assess the likelihood of crack propagation in a snowpack. Guidelines suggest beams with lengths of around 1 m, yet little is known about how test length affects propagation. Thus, we performed 163 ECTs and PSTs 1.0–10.0 m long. On days with full crack propagation in 1.0–1.5 m tests, we then made videos of tests 2.0–10.0 m long. We inserted markers for particle tracking to measure collapse amplitude, propagation speed, and wavelength. We also used a finite element (FE) model to simulate the strain energy release rate at fixed crack lengths. We find that (1) the proportion of tests with full propagation decreased with test length; (2) collapse was greater at the ends of the beams than in the centers; (3) collapse amplitude was independent of beam length and did not reach a constant value; (4) collapse wavelengths in the longer tests were around 3 m, two times greater than what is predicted by the anticrack model. We also confirmed the prediction that centered PSTs had double the critical length of edge PSTs. Based on our results, we conclude that cracks propagated more frequently in the shorter tests because of increased stress concentration from the far edge. The FE model suggests this edge effect occurs for PSTs of up to 2 m long or a crack to beam length ratio ≥ 0.20. Our results suggest that ECT and PST length guidelines may need to be revisited. Article in Journal/Newspaper The Cryosphere Unknown The Cryosphere 8 4 1407 1418
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic info
envir
spellingShingle info
envir
E. H. Bair
R. Simenhois
A. van Herwijnen
K. Birkeland
The influence of edge effects on crack propagation in snow stability tests
topic_facet info
envir
description The Extended Column Test (ECT) and the Propagation Saw Test (PST) are two commonly used tests to assess the likelihood of crack propagation in a snowpack. Guidelines suggest beams with lengths of around 1 m, yet little is known about how test length affects propagation. Thus, we performed 163 ECTs and PSTs 1.0–10.0 m long. On days with full crack propagation in 1.0–1.5 m tests, we then made videos of tests 2.0–10.0 m long. We inserted markers for particle tracking to measure collapse amplitude, propagation speed, and wavelength. We also used a finite element (FE) model to simulate the strain energy release rate at fixed crack lengths. We find that (1) the proportion of tests with full propagation decreased with test length; (2) collapse was greater at the ends of the beams than in the centers; (3) collapse amplitude was independent of beam length and did not reach a constant value; (4) collapse wavelengths in the longer tests were around 3 m, two times greater than what is predicted by the anticrack model. We also confirmed the prediction that centered PSTs had double the critical length of edge PSTs. Based on our results, we conclude that cracks propagated more frequently in the shorter tests because of increased stress concentration from the far edge. The FE model suggests this edge effect occurs for PSTs of up to 2 m long or a crack to beam length ratio ≥ 0.20. Our results suggest that ECT and PST length guidelines may need to be revisited.
format Article in Journal/Newspaper
author E. H. Bair
R. Simenhois
A. van Herwijnen
K. Birkeland
author_facet E. H. Bair
R. Simenhois
A. van Herwijnen
K. Birkeland
author_sort E. H. Bair
title The influence of edge effects on crack propagation in snow stability tests
title_short The influence of edge effects on crack propagation in snow stability tests
title_full The influence of edge effects on crack propagation in snow stability tests
title_fullStr The influence of edge effects on crack propagation in snow stability tests
title_full_unstemmed The influence of edge effects on crack propagation in snow stability tests
title_sort influence of edge effects on crack propagation in snow stability tests
publisher Copernicus Publications
publishDate 2014
url https://doi.org/10.5194/tc-8-1407-2014
http://www.the-cryosphere.net/8/1407/2014/tc-8-1407-2014.pdf
https://doaj.org/article/7e87e7e6fdee4d939a73548312552305
genre The Cryosphere
genre_facet The Cryosphere
op_source The Cryosphere, Vol 8, Iss 4, Pp 1407-1418 (2014)
op_relation 1994-0416
1994-0424
doi:10.5194/tc-8-1407-2014
http://www.the-cryosphere.net/8/1407/2014/tc-8-1407-2014.pdf
https://doaj.org/article/7e87e7e6fdee4d939a73548312552305
op_rights undefined
op_doi https://doi.org/10.5194/tc-8-1407-2014
container_title The Cryosphere
container_volume 8
container_issue 4
container_start_page 1407
op_container_end_page 1418
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