Subcritical crack propagation in glacial quarrying during subglacial water pressure variation

Abstract Glacial quarrying stems from the fracturing of subglacial bedrock. Much evidence shows that subcritical crack propagation of bedrock is closely related to subglacial water pressure fluctuations. Here we employ a model that assesses the impact of subglacial water pressure fluctuation on cavi...

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Published in:Journal of Glaciology
Main Authors: Li, Lin, Huang, Yipeng, Su, Ningchuan
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2023
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2022.126
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143022001265
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spelling crcambridgeupr:10.1017/jog.2022.126 2024-09-15T18:15:37+00:00 Subcritical crack propagation in glacial quarrying during subglacial water pressure variation Li, Lin Huang, Yipeng Su, Ningchuan 2023 http://dx.doi.org/10.1017/jog.2022.126 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143022001265 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Journal of Glaciology volume 69, issue 276, page 1071-1079 ISSN 0022-1430 1727-5652 journal-article 2023 crcambridgeupr https://doi.org/10.1017/jog.2022.126 2024-08-07T04:04:45Z Abstract Glacial quarrying stems from the fracturing of subglacial bedrock. Much evidence shows that subcritical crack propagation of bedrock is closely related to subglacial water pressure fluctuations. Here we employ a model that assesses the impact of subglacial water pressure fluctuation on cavity length and subcritical crack propagation, while analyzing the effect of a pre-existing crack location using a phase-field model (PFM). Our results indicate that the cavity length is reduced during diurnal fluctuations in water pressure. There are two patterns of subcritical crack propagation on the corner of the step. The first stems from a rapid drop in water pressure. The second occurs after the water pressure recovers from the fluctuation to the initial steady state. This pattern is a consequence of enhanced stress concentration on the step since the modeled cavity length exceeds its steady value and has higher efficiency in promoting subcritical crack propagation. Additionally, based on the PFM results, we speculate that the subcritical crack initiation and propagation happen on a broader scale, including the ice-bed contact region and its adjacent region. Our findings imply that the duration of subcritical crack propagation is short and typically ceases once the cavity length adjusts to reduced water pressure levels. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 1 9
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Glacial quarrying stems from the fracturing of subglacial bedrock. Much evidence shows that subcritical crack propagation of bedrock is closely related to subglacial water pressure fluctuations. Here we employ a model that assesses the impact of subglacial water pressure fluctuation on cavity length and subcritical crack propagation, while analyzing the effect of a pre-existing crack location using a phase-field model (PFM). Our results indicate that the cavity length is reduced during diurnal fluctuations in water pressure. There are two patterns of subcritical crack propagation on the corner of the step. The first stems from a rapid drop in water pressure. The second occurs after the water pressure recovers from the fluctuation to the initial steady state. This pattern is a consequence of enhanced stress concentration on the step since the modeled cavity length exceeds its steady value and has higher efficiency in promoting subcritical crack propagation. Additionally, based on the PFM results, we speculate that the subcritical crack initiation and propagation happen on a broader scale, including the ice-bed contact region and its adjacent region. Our findings imply that the duration of subcritical crack propagation is short and typically ceases once the cavity length adjusts to reduced water pressure levels.
format Article in Journal/Newspaper
author Li, Lin
Huang, Yipeng
Su, Ningchuan
spellingShingle Li, Lin
Huang, Yipeng
Su, Ningchuan
Subcritical crack propagation in glacial quarrying during subglacial water pressure variation
author_facet Li, Lin
Huang, Yipeng
Su, Ningchuan
author_sort Li, Lin
title Subcritical crack propagation in glacial quarrying during subglacial water pressure variation
title_short Subcritical crack propagation in glacial quarrying during subglacial water pressure variation
title_full Subcritical crack propagation in glacial quarrying during subglacial water pressure variation
title_fullStr Subcritical crack propagation in glacial quarrying during subglacial water pressure variation
title_full_unstemmed Subcritical crack propagation in glacial quarrying during subglacial water pressure variation
title_sort subcritical crack propagation in glacial quarrying during subglacial water pressure variation
publisher Cambridge University Press (CUP)
publishDate 2023
url http://dx.doi.org/10.1017/jog.2022.126
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143022001265
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 69, issue 276, page 1071-1079
ISSN 0022-1430 1727-5652
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2022.126
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 9
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