Crystal alignment in sea ice ...
The c-axes of grains in a sheet of sea ice not only lie in the plane perpendicular to the direction of heat flow but also may align about a particular axis in that plane. It has been suggested that the existence of horizontal temperature gradients or the current at the ice-water interface are likely...
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Online Access: | https://dx.doi.org/10.17863/cam.39796 https://www.repository.cam.ac.uk/handle/1810/292640 |
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ftdatacite:10.17863/cam.39796 2024-02-04T10:04:24+01:00 Crystal alignment in sea ice ... Langhorne, Pat 1982 https://dx.doi.org/10.17863/cam.39796 https://www.repository.cam.ac.uk/handle/1810/292640 en eng Apollo - University of Cambridge Repository open.access All Rights Reserved http://www.rioxx.net/licenses/all-rights-reserved/ http://purl.org/coar/access_right/c_abf2 Dissertation Thesis thesis 1982 ftdatacite https://doi.org/10.17863/cam.39796 2024-01-05T09:46:34Z The c-axes of grains in a sheet of sea ice not only lie in the plane perpendicular to the direction of heat flow but also may align about a particular axis in that plane. It has been suggested that the existence of horizontal temperature gradients or the current at the ice-water interface are likely driving forces for this ordering. In addition to making relevant field observations ,we have carried out experiments to discover which factor exerts the greatest influence on the resulting distribution of c-axes. Apparatus to grow NaCl ice in the presence of a water current has been constructed in the cold room at the Scott Polar Research Institute. Two lengthy experiments have been performed in saline water (34%,), one with a current of 3cms$^-1$ beneath the growing ice and a corresponding "null" experiment in which there was no forced flow. Two similar experiments were carried out with brackish water (20%). The growth rate of the ice and the shape of the ice-water interface at the completion of the experiment ... Thesis Scott Polar Research Institute Sea ice DataCite Metadata Store (German National Library of Science and Technology) |
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DataCite Metadata Store (German National Library of Science and Technology) |
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ftdatacite |
language |
English |
description |
The c-axes of grains in a sheet of sea ice not only lie in the plane perpendicular to the direction of heat flow but also may align about a particular axis in that plane. It has been suggested that the existence of horizontal temperature gradients or the current at the ice-water interface are likely driving forces for this ordering. In addition to making relevant field observations ,we have carried out experiments to discover which factor exerts the greatest influence on the resulting distribution of c-axes. Apparatus to grow NaCl ice in the presence of a water current has been constructed in the cold room at the Scott Polar Research Institute. Two lengthy experiments have been performed in saline water (34%,), one with a current of 3cms$^-1$ beneath the growing ice and a corresponding "null" experiment in which there was no forced flow. Two similar experiments were carried out with brackish water (20%). The growth rate of the ice and the shape of the ice-water interface at the completion of the experiment ... |
format |
Thesis |
author |
Langhorne, Pat |
spellingShingle |
Langhorne, Pat Crystal alignment in sea ice ... |
author_facet |
Langhorne, Pat |
author_sort |
Langhorne, Pat |
title |
Crystal alignment in sea ice ... |
title_short |
Crystal alignment in sea ice ... |
title_full |
Crystal alignment in sea ice ... |
title_fullStr |
Crystal alignment in sea ice ... |
title_full_unstemmed |
Crystal alignment in sea ice ... |
title_sort |
crystal alignment in sea ice ... |
publisher |
Apollo - University of Cambridge Repository |
publishDate |
1982 |
url |
https://dx.doi.org/10.17863/cam.39796 https://www.repository.cam.ac.uk/handle/1810/292640 |
genre |
Scott Polar Research Institute Sea ice |
genre_facet |
Scott Polar Research Institute Sea ice |
op_rights |
open.access All Rights Reserved http://www.rioxx.net/licenses/all-rights-reserved/ http://purl.org/coar/access_right/c_abf2 |
op_doi |
https://doi.org/10.17863/cam.39796 |
_version_ |
1789972834941927424 |