The Application of Fracture Mechanics to the Problem of Crevasse Penetration

Abstract The elastic stress intensity factor is a parameter used in fracture mechanics to describe stress conditions in the vicinity of the tip of a sharp crack. By superimposing solutions of stress intensity factors for different loading conditions, equations are derived which model crevasses in ic...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Smith, R. A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1976
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000013563
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000013563
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spelling crcambridgeupr:10.1017/s0022143000013563 2024-04-07T07:53:42+00:00 The Application of Fracture Mechanics to the Problem of Crevasse Penetration Smith, R. A. 1976 http://dx.doi.org/10.1017/s0022143000013563 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000013563 en eng Cambridge University Press (CUP) Journal of Glaciology volume 17, issue 76, page 223-228 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1976 crcambridgeupr https://doi.org/10.1017/s0022143000013563 2024-03-08T00:35:14Z Abstract The elastic stress intensity factor is a parameter used in fracture mechanics to describe stress conditions in the vicinity of the tip of a sharp crack. By superimposing solutions of stress intensity factors for different loading conditions, equations are derived which model crevasses in ice. Solutions are presented for the theoretical depth of isolated crevasses, free from or partially filled with water. Close agreement exists with a previous calculation by Weertman using a different technique. The effect of crevasse spacing is investigated and it is demonstrated that closer spacing always reduces crevasse depth, but over a wide range of spacing the predicted variation in depth is slight. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Weertman ENVELOPE(-67.753,-67.753,-66.972,-66.972) Journal of Glaciology 17 76 223 228
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Smith, R. A.
The Application of Fracture Mechanics to the Problem of Crevasse Penetration
topic_facet Earth-Surface Processes
description Abstract The elastic stress intensity factor is a parameter used in fracture mechanics to describe stress conditions in the vicinity of the tip of a sharp crack. By superimposing solutions of stress intensity factors for different loading conditions, equations are derived which model crevasses in ice. Solutions are presented for the theoretical depth of isolated crevasses, free from or partially filled with water. Close agreement exists with a previous calculation by Weertman using a different technique. The effect of crevasse spacing is investigated and it is demonstrated that closer spacing always reduces crevasse depth, but over a wide range of spacing the predicted variation in depth is slight.
format Article in Journal/Newspaper
author Smith, R. A.
author_facet Smith, R. A.
author_sort Smith, R. A.
title The Application of Fracture Mechanics to the Problem of Crevasse Penetration
title_short The Application of Fracture Mechanics to the Problem of Crevasse Penetration
title_full The Application of Fracture Mechanics to the Problem of Crevasse Penetration
title_fullStr The Application of Fracture Mechanics to the Problem of Crevasse Penetration
title_full_unstemmed The Application of Fracture Mechanics to the Problem of Crevasse Penetration
title_sort application of fracture mechanics to the problem of crevasse penetration
publisher Cambridge University Press (CUP)
publishDate 1976
url http://dx.doi.org/10.1017/s0022143000013563
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000013563
long_lat ENVELOPE(-67.753,-67.753,-66.972,-66.972)
geographic Weertman
geographic_facet Weertman
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 17, issue 76, page 223-228
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000013563
container_title Journal of Glaciology
container_volume 17
container_issue 76
container_start_page 223
op_container_end_page 228
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