Phase Relationships in Sea Ice as a Function of Temperature

Quantitative measurements of the liquid water phase in a sample of sea ice were made with a nuclear magnetic resonance spectrometer. The measurements are used to compute the phase relationships in sea ice as a function of temperature. A model for sea-water based upon a mixture of seven binary salts...

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Published in:Journal of Glaciology
Main Author: Richardson, C.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1976
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000013770
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000013770
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spelling crcambridgeupr:10.1017/s0022143000013770 2024-03-03T08:46:04+00:00 Phase Relationships in Sea Ice as a Function of Temperature Richardson, C. 1976 http://dx.doi.org/10.1017/s0022143000013770 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000013770 en eng Cambridge University Press (CUP) Journal of Glaciology volume 17, issue 77, page 507-519 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1976 crcambridgeupr https://doi.org/10.1017/s0022143000013770 2024-02-08T08:34:04Z Quantitative measurements of the liquid water phase in a sample of sea ice were made with a nuclear magnetic resonance spectrometer. The measurements are used to compute the phase relationships in sea ice as a function of temperature. A model for sea-water based upon a mixture of seven binary salts is used for these computations. The n.m.r. measurements are related to the solvation water which is associated with each binary salt. This solvation water is bound to the salt in a pseudo-crystalline structure, with the amount of water determined by the eutectic concentration of the salt. The results are given in tabular form and differ somewhat from previously published tables. Two controversial hydrated salts were added to the table, based on the n.m.r. data. Article in Journal/Newspaper Journal of Glaciology Sea ice Cambridge University Press Journal of Glaciology 17 77 507 519
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Richardson, C.
Phase Relationships in Sea Ice as a Function of Temperature
topic_facet Earth-Surface Processes
description Quantitative measurements of the liquid water phase in a sample of sea ice were made with a nuclear magnetic resonance spectrometer. The measurements are used to compute the phase relationships in sea ice as a function of temperature. A model for sea-water based upon a mixture of seven binary salts is used for these computations. The n.m.r. measurements are related to the solvation water which is associated with each binary salt. This solvation water is bound to the salt in a pseudo-crystalline structure, with the amount of water determined by the eutectic concentration of the salt. The results are given in tabular form and differ somewhat from previously published tables. Two controversial hydrated salts were added to the table, based on the n.m.r. data.
format Article in Journal/Newspaper
author Richardson, C.
author_facet Richardson, C.
author_sort Richardson, C.
title Phase Relationships in Sea Ice as a Function of Temperature
title_short Phase Relationships in Sea Ice as a Function of Temperature
title_full Phase Relationships in Sea Ice as a Function of Temperature
title_fullStr Phase Relationships in Sea Ice as a Function of Temperature
title_full_unstemmed Phase Relationships in Sea Ice as a Function of Temperature
title_sort phase relationships in sea ice as a function of temperature
publisher Cambridge University Press (CUP)
publishDate 1976
url http://dx.doi.org/10.1017/s0022143000013770
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000013770
genre Journal of Glaciology
Sea ice
genre_facet Journal of Glaciology
Sea ice
op_source Journal of Glaciology
volume 17, issue 77, page 507-519
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000013770
container_title Journal of Glaciology
container_volume 17
container_issue 77
container_start_page 507
op_container_end_page 519
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