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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Language: | English |
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Cambridge University Press (CUP)
1988
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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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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 |
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Open Polar |
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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 |
_version_ |
1810449918021599232 |