Subcritical crack propagation in glacial quarrying during subglacial water pressure variation

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...

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Published in:Journal of Glaciology
Main Authors: Lin Li, Yipeng Huang, Ningchuan Su
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2023
Subjects:
Online Access:https://doi.org/10.1017/jog.2022.126
https://doaj.org/article/c09f2ed5f7cf4bcb9e8dc6f6abdbf9b1
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spelling ftdoajarticles:oai:doaj.org/article:c09f2ed5f7cf4bcb9e8dc6f6abdbf9b1 2023-08-20T04:07:38+02:00 Subcritical crack propagation in glacial quarrying during subglacial water pressure variation Lin Li Yipeng Huang Ningchuan Su 2023-08-01T00:00:00Z https://doi.org/10.1017/jog.2022.126 https://doaj.org/article/c09f2ed5f7cf4bcb9e8dc6f6abdbf9b1 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143022001265/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.126 0022-1430 1727-5652 https://doaj.org/article/c09f2ed5f7cf4bcb9e8dc6f6abdbf9b1 Journal of Glaciology, Vol 69, Pp 1071-1079 (2023) Crack propagation glacial quarrying water pressure fluctuation Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.1017/jog.2022.126 2023-07-30T00:36:44Z 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 Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 1 9
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Crack propagation
glacial quarrying
water pressure fluctuation
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Crack propagation
glacial quarrying
water pressure fluctuation
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Lin Li
Yipeng Huang
Ningchuan Su
Subcritical crack propagation in glacial quarrying during subglacial water pressure variation
topic_facet Crack propagation
glacial quarrying
water pressure fluctuation
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description 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 Lin Li
Yipeng Huang
Ningchuan Su
author_facet Lin Li
Yipeng Huang
Ningchuan Su
author_sort Lin Li
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
publishDate 2023
url https://doi.org/10.1017/jog.2022.126
https://doaj.org/article/c09f2ed5f7cf4bcb9e8dc6f6abdbf9b1
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology, Vol 69, Pp 1071-1079 (2023)
op_relation https://www.cambridge.org/core/product/identifier/S0022143022001265/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2022.126
0022-1430
1727-5652
https://doaj.org/article/c09f2ed5f7cf4bcb9e8dc6f6abdbf9b1
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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