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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Bibliographic Details
Main Author: Langhorne, Pat
Format: Thesis
Language:English
Published: Apollo - University of Cambridge Repository 1982
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.39796
https://www.repository.cam.ac.uk/handle/1810/292640
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spelling 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)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id 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
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