Some Crystal Growth Features of Sea Ice

Abstract Laboratory studies of the supercooling and freezing of baths of sea-water are described and compared with features of natural sea ice. By using dyes the convection cells in the sea-water test baths could be studied. and the growth of crystals relative to this cell structure could be observe...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Author: Bennington, Kenneth O.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1963
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000028306
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000028306
id crcambridgeupr:10.1017/s0022143000028306
record_format openpolar
spelling crcambridgeupr:10.1017/s0022143000028306 2024-03-03T08:46:07+00:00 Some Crystal Growth Features of Sea Ice Bennington, Kenneth O. 1963 http://dx.doi.org/10.1017/s0022143000028306 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000028306 en eng Cambridge University Press (CUP) Journal of Glaciology volume 4, issue 36, page 669-688 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1963 crcambridgeupr https://doi.org/10.1017/s0022143000028306 2024-02-08T08:36:15Z Abstract Laboratory studies of the supercooling and freezing of baths of sea-water are described and compared with features of natural sea ice. By using dyes the convection cells in the sea-water test baths could be studied. and the growth of crystals relative to this cell structure could be observed. Brine expelled by the separation of ice from the system commonly followed the pre-existing convection channels. Sections of sea ice are interpreted in the light of these observations, and sea ice is shown to inherit drainage channels and banding features from the characteristics of the parent liquid system. Article in Journal/Newspaper Journal of Glaciology Sea ice Cambridge University Press Journal of Glaciology 4 36 669 688
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Bennington, Kenneth O.
Some Crystal Growth Features of Sea Ice
topic_facet Earth-Surface Processes
description Abstract Laboratory studies of the supercooling and freezing of baths of sea-water are described and compared with features of natural sea ice. By using dyes the convection cells in the sea-water test baths could be studied. and the growth of crystals relative to this cell structure could be observed. Brine expelled by the separation of ice from the system commonly followed the pre-existing convection channels. Sections of sea ice are interpreted in the light of these observations, and sea ice is shown to inherit drainage channels and banding features from the characteristics of the parent liquid system.
format Article in Journal/Newspaper
author Bennington, Kenneth O.
author_facet Bennington, Kenneth O.
author_sort Bennington, Kenneth O.
title Some Crystal Growth Features of Sea Ice
title_short Some Crystal Growth Features of Sea Ice
title_full Some Crystal Growth Features of Sea Ice
title_fullStr Some Crystal Growth Features of Sea Ice
title_full_unstemmed Some Crystal Growth Features of Sea Ice
title_sort some crystal growth features of sea ice
publisher Cambridge University Press (CUP)
publishDate 1963
url http://dx.doi.org/10.1017/s0022143000028306
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000028306
genre Journal of Glaciology
Sea ice
genre_facet Journal of Glaciology
Sea ice
op_source Journal of Glaciology
volume 4, issue 36, page 669-688
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000028306
container_title Journal of Glaciology
container_volume 4
container_issue 36
container_start_page 669
op_container_end_page 688
_version_ 1792502036012466176