A Pressure-sintering Model for the Densification of Polar Firn and Glacier Ice

Abstract A comprehensive multi-mechanism theory of pressure sintering has been applied to the densification of two polar ice sheets. The comparison, which is made using pressure-sintering mechanism maps, indicates that power-law creep is the controlling mechanism between 50% and 98% theoretical dens...

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Published in:Journal of Glaciology
Main Author: Wilkinson, D.S.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1988
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000009047
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000009047
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spelling crcambridgeupr:10.1017/s0022143000009047 2024-09-15T18:12:20+00:00 A Pressure-sintering Model for the Densification of Polar Firn and Glacier Ice Wilkinson, D.S. 1988 http://dx.doi.org/10.1017/s0022143000009047 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000009047 en eng Cambridge University Press (CUP) Journal of Glaciology volume 34, issue 116, page 40-45 ISSN 0022-1430 1727-5652 journal-article 1988 crcambridgeupr https://doi.org/10.1017/s0022143000009047 2024-07-24T04:03:46Z Abstract A comprehensive multi-mechanism theory of pressure sintering has been applied to the densification of two polar ice sheets. The comparison, which is made using pressure-sintering mechanism maps, indicates that power-law creep is the controlling mechanism between 50% and 98% theoretical density. Lattice diffusion becomes dominant at low porosities. The densification rates predicted by the theory are in good agreement with the data, and suggest that a reasonable estimation of the densification behaviour of a polar ice sheet can be made using the theory, based on information obtained from a relatively shallow core. Article in Journal/Newspaper Ice Sheet Journal of Glaciology Cambridge University Press Journal of Glaciology 34 116 40 45
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract A comprehensive multi-mechanism theory of pressure sintering has been applied to the densification of two polar ice sheets. The comparison, which is made using pressure-sintering mechanism maps, indicates that power-law creep is the controlling mechanism between 50% and 98% theoretical density. Lattice diffusion becomes dominant at low porosities. The densification rates predicted by the theory are in good agreement with the data, and suggest that a reasonable estimation of the densification behaviour of a polar ice sheet can be made using the theory, based on information obtained from a relatively shallow core.
format Article in Journal/Newspaper
author Wilkinson, D.S.
spellingShingle Wilkinson, D.S.
A Pressure-sintering Model for the Densification of Polar Firn and Glacier Ice
author_facet Wilkinson, D.S.
author_sort Wilkinson, D.S.
title A Pressure-sintering Model for the Densification of Polar Firn and Glacier Ice
title_short A Pressure-sintering Model for the Densification of Polar Firn and Glacier Ice
title_full A Pressure-sintering Model for the Densification of Polar Firn and Glacier Ice
title_fullStr A Pressure-sintering Model for the Densification of Polar Firn and Glacier Ice
title_full_unstemmed A Pressure-sintering Model for the Densification of Polar Firn and Glacier Ice
title_sort pressure-sintering model for the densification of polar firn and glacier ice
publisher Cambridge University Press (CUP)
publishDate 1988
url http://dx.doi.org/10.1017/s0022143000009047
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000009047
genre Ice Sheet
Journal of Glaciology
genre_facet Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology
volume 34, issue 116, page 40-45
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000009047
container_title Journal of Glaciology
container_volume 34
container_issue 116
container_start_page 40
op_container_end_page 45
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