Frazil Formation in Water of Different Salinities and Supercoolings

Abstract The formation of frazil in water of different salinities and initial supercoolings was studied in the laboratory. Experiments were conducted both on genuine and artificial sea-waters. From analysing the experimental results, it was found that the production rate of frazil is highly sensitiv...

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Published in:Journal of Glaciology
Main Authors: Tsang, Gee, Hanley, Thomas O’D.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1985
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000006298
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000006298
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spelling crcambridgeupr:10.1017/s0022143000006298 2024-09-09T19:49:01+00:00 Frazil Formation in Water of Different Salinities and Supercoolings Tsang, Gee Hanley, Thomas O’D. 1985 http://dx.doi.org/10.1017/s0022143000006298 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000006298 en eng Cambridge University Press (CUP) Journal of Glaciology volume 31, issue 108, page 74-85 ISSN 0022-1430 1727-5652 journal-article 1985 crcambridgeupr https://doi.org/10.1017/s0022143000006298 2024-08-28T04:02:57Z Abstract The formation of frazil in water of different salinities and initial supercoolings was studied in the laboratory. Experiments were conducted both on genuine and artificial sea-waters. From analysing the experimental results, it was found that the production rate of frazil is highly sensitive to the initial supercooling of the water and will increase over three orders of magnitude as the initial supercooling increases from zero to 2° C. By properly non-dimensionalizing the parameters, it was found that the normalized concentration of frazil in water is principally a function of the normalized time. For the rate of production of frazil, however, it was found that the normalized rate of frazil production, besides being a function of the normalized time, is also affected by the salinity and the initial supercooling of the water. Different frazil crystals formed in water of different salinities and initial supercoolings are thought to be the reason for the different curves of frazil production rate. The normalization of parameters requires the determination of some characteristic parameters which were found to be well-defined functions of initial supercooling and salinity. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 31 108 74 85
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract The formation of frazil in water of different salinities and initial supercoolings was studied in the laboratory. Experiments were conducted both on genuine and artificial sea-waters. From analysing the experimental results, it was found that the production rate of frazil is highly sensitive to the initial supercooling of the water and will increase over three orders of magnitude as the initial supercooling increases from zero to 2° C. By properly non-dimensionalizing the parameters, it was found that the normalized concentration of frazil in water is principally a function of the normalized time. For the rate of production of frazil, however, it was found that the normalized rate of frazil production, besides being a function of the normalized time, is also affected by the salinity and the initial supercooling of the water. Different frazil crystals formed in water of different salinities and initial supercoolings are thought to be the reason for the different curves of frazil production rate. The normalization of parameters requires the determination of some characteristic parameters which were found to be well-defined functions of initial supercooling and salinity.
format Article in Journal/Newspaper
author Tsang, Gee
Hanley, Thomas O’D.
spellingShingle Tsang, Gee
Hanley, Thomas O’D.
Frazil Formation in Water of Different Salinities and Supercoolings
author_facet Tsang, Gee
Hanley, Thomas O’D.
author_sort Tsang, Gee
title Frazil Formation in Water of Different Salinities and Supercoolings
title_short Frazil Formation in Water of Different Salinities and Supercoolings
title_full Frazil Formation in Water of Different Salinities and Supercoolings
title_fullStr Frazil Formation in Water of Different Salinities and Supercoolings
title_full_unstemmed Frazil Formation in Water of Different Salinities and Supercoolings
title_sort frazil formation in water of different salinities and supercoolings
publisher Cambridge University Press (CUP)
publishDate 1985
url http://dx.doi.org/10.1017/s0022143000006298
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000006298
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 31, issue 108, page 74-85
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000006298
container_title Journal of Glaciology
container_volume 31
container_issue 108
container_start_page 74
op_container_end_page 85
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