Age Hardening of Snow at the South Pole
The age hardening of artificially and naturally compacted snow has been investigated at the South Pole. Results show that the age-hardening process is greatly retarded at low temperatures. Artificially compacted samples of density 0.55 g./cm. 3 attained a compressive strength of less than 3.0 kg./cm...
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Language: | English |
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Cambridge University Press (CUP)
1963
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Online Access: | http://dx.doi.org/10.1017/s0022143000028069 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000028069 |
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crcambridgeupr:10.1017/s0022143000028069 2024-03-03T08:46:07+00:00 Age Hardening of Snow at the South Pole Gow, Anthony J. Ramseier, René O. 1963 http://dx.doi.org/10.1017/s0022143000028069 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000028069 en eng Cambridge University Press (CUP) Journal of Glaciology volume 4, issue 35, page 521-536 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1963 crcambridgeupr https://doi.org/10.1017/s0022143000028069 2024-02-08T08:36:10Z The age hardening of artificially and naturally compacted snow has been investigated at the South Pole. Results show that the age-hardening process is greatly retarded at low temperatures. Artificially compacted samples of density 0.55 g./cm. 3 attained a compressive strength of less than 3.0 kg./cm. 2 after one year’s ageing at −49° C. Exposure to solar radiation accelerated the age hardening. Irradiated samples attained a strength of 6.0 kg./cm. 2 after 100 hr., increasing to a virtual maximum of 8.0 kg./cm. 2 at the end of 600 hr. Compressive strengths increased with decrease in snow-particle size and with increasing angularity of the particles. Below 3 m. the strength of naturally compacted snow was found to increase rapidly with increase in density. Naturally compacted snow of density 0.55 g./cm. 3 possessed considerably greater strength than any of the age-hardened samples of artificially compacted snow of the same density. Thin-section studies show that age hardening can be correlated with the formation and growth of intergranular bonds, and that bond growth falls off rapidly with decreasing temperature. In view of the low strengths found in both naturally compacted snows near the surface and in artificially compacted snow at the South Pole, “cut-and-cover” under-snow camp construction may not prove too practical at the South Pole. Article in Journal/Newspaper Journal of Glaciology South pole Cambridge University Press South Pole Journal of Glaciology 4 35 521 536 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Gow, Anthony J. Ramseier, René O. Age Hardening of Snow at the South Pole |
topic_facet |
Earth-Surface Processes |
description |
The age hardening of artificially and naturally compacted snow has been investigated at the South Pole. Results show that the age-hardening process is greatly retarded at low temperatures. Artificially compacted samples of density 0.55 g./cm. 3 attained a compressive strength of less than 3.0 kg./cm. 2 after one year’s ageing at −49° C. Exposure to solar radiation accelerated the age hardening. Irradiated samples attained a strength of 6.0 kg./cm. 2 after 100 hr., increasing to a virtual maximum of 8.0 kg./cm. 2 at the end of 600 hr. Compressive strengths increased with decrease in snow-particle size and with increasing angularity of the particles. Below 3 m. the strength of naturally compacted snow was found to increase rapidly with increase in density. Naturally compacted snow of density 0.55 g./cm. 3 possessed considerably greater strength than any of the age-hardened samples of artificially compacted snow of the same density. Thin-section studies show that age hardening can be correlated with the formation and growth of intergranular bonds, and that bond growth falls off rapidly with decreasing temperature. In view of the low strengths found in both naturally compacted snows near the surface and in artificially compacted snow at the South Pole, “cut-and-cover” under-snow camp construction may not prove too practical at the South Pole. |
format |
Article in Journal/Newspaper |
author |
Gow, Anthony J. Ramseier, René O. |
author_facet |
Gow, Anthony J. Ramseier, René O. |
author_sort |
Gow, Anthony J. |
title |
Age Hardening of Snow at the South Pole |
title_short |
Age Hardening of Snow at the South Pole |
title_full |
Age Hardening of Snow at the South Pole |
title_fullStr |
Age Hardening of Snow at the South Pole |
title_full_unstemmed |
Age Hardening of Snow at the South Pole |
title_sort |
age hardening of snow at the south pole |
publisher |
Cambridge University Press (CUP) |
publishDate |
1963 |
url |
http://dx.doi.org/10.1017/s0022143000028069 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000028069 |
geographic |
South Pole |
geographic_facet |
South Pole |
genre |
Journal of Glaciology South pole |
genre_facet |
Journal of Glaciology South pole |
op_source |
Journal of Glaciology volume 4, issue 35, page 521-536 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000028069 |
container_title |
Journal of Glaciology |
container_volume |
4 |
container_issue |
35 |
container_start_page |
521 |
op_container_end_page |
536 |
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1792502034286510080 |