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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Published in:Journal of Glaciology
Main Authors: Gow, Anthony J., Ramseier, René O.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1963
Subjects:
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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spelling 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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