Dynamics of the Ice-Crushing Process

Abstract During fast indentation tests on ice sheets at constant rates, crushing is commonly observed at appropriate combinations of speed and aspect ratio. An analysis is made of this mode of failure, using as a basis a recently conducted test on an ice sheet under controlled conditions. The variat...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Jordaan, Ian J., Timco, Garry W.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1988
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000007085
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000007085
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spelling crcambridgeupr:10.1017/s0022143000007085 2024-03-03T08:45:25+00:00 Dynamics of the Ice-Crushing Process Jordaan, Ian J. Timco, Garry W. 1988 http://dx.doi.org/10.1017/s0022143000007085 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000007085 en eng Cambridge University Press (CUP) Journal of Glaciology volume 34, issue 118, page 318-326 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1988 crcambridgeupr https://doi.org/10.1017/s0022143000007085 2024-02-08T08:34:04Z Abstract During fast indentation tests on ice sheets at constant rates, crushing is commonly observed at appropriate combinations of speed and aspect ratio. An analysis is made of this mode of failure, using as a basis a recently conducted test on an ice sheet under controlled conditions. The variation of load with time is given special attention, and cyclic variation of load is associated with periodic crushing (pulverization) events, followed by clearing of the crushed ice particles. An analysis of the clearing process is summarized in the paper, treating the crushed ice as a viscous material. A detailed analysis of the energy exchanges during the indentation process is given. Elastic variations of stored energy in the indenter and in the ice sheet are calculated; these are relatively minor. The dissipation of energy during a typical load cycle (3 mm movement during 0.05 s) is about 8 J. The energy required to create surfaces of the crushed ice particles is small (0.006 J), as is the work of crushing based on mechanical testing (0.09 J). It is concluded that the process of viscous extrusion of crushed ice is the main seat of energy dissipation, basically as a frictional process. A relationship for the mean thickness of the crushed ice layer is developed, based on energy-balance considerations. Article in Journal/Newspaper Ice Sheet Journal of Glaciology Cambridge University Press Journal of Glaciology 34 118 318 326
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Jordaan, Ian J.
Timco, Garry W.
Dynamics of the Ice-Crushing Process
topic_facet Earth-Surface Processes
description Abstract During fast indentation tests on ice sheets at constant rates, crushing is commonly observed at appropriate combinations of speed and aspect ratio. An analysis is made of this mode of failure, using as a basis a recently conducted test on an ice sheet under controlled conditions. The variation of load with time is given special attention, and cyclic variation of load is associated with periodic crushing (pulverization) events, followed by clearing of the crushed ice particles. An analysis of the clearing process is summarized in the paper, treating the crushed ice as a viscous material. A detailed analysis of the energy exchanges during the indentation process is given. Elastic variations of stored energy in the indenter and in the ice sheet are calculated; these are relatively minor. The dissipation of energy during a typical load cycle (3 mm movement during 0.05 s) is about 8 J. The energy required to create surfaces of the crushed ice particles is small (0.006 J), as is the work of crushing based on mechanical testing (0.09 J). It is concluded that the process of viscous extrusion of crushed ice is the main seat of energy dissipation, basically as a frictional process. A relationship for the mean thickness of the crushed ice layer is developed, based on energy-balance considerations.
format Article in Journal/Newspaper
author Jordaan, Ian J.
Timco, Garry W.
author_facet Jordaan, Ian J.
Timco, Garry W.
author_sort Jordaan, Ian J.
title Dynamics of the Ice-Crushing Process
title_short Dynamics of the Ice-Crushing Process
title_full Dynamics of the Ice-Crushing Process
title_fullStr Dynamics of the Ice-Crushing Process
title_full_unstemmed Dynamics of the Ice-Crushing Process
title_sort dynamics of the ice-crushing process
publisher Cambridge University Press (CUP)
publishDate 1988
url http://dx.doi.org/10.1017/s0022143000007085
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000007085
genre Ice Sheet
Journal of Glaciology
genre_facet Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology
volume 34, issue 118, page 318-326
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000007085
container_title Journal of Glaciology
container_volume 34
container_issue 118
container_start_page 318
op_container_end_page 326
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