Optical Properties of Salt Ice

Abstract The dependence of the extinction coefficient on salinity was investigated for both NaCl-ice and salt-ice made from natural sea-water. Specimens were prepared under a variety of conditions and examined over the wavelength range 4 000 to 8 000 Â. The effects of scattering from air bubbles tra...

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Published in:Journal of Glaciology
Main Author: Lane, J. W.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1975
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000034481
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000034481
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spelling crcambridgeupr:10.1017/s0022143000034481 2024-03-03T08:46:04+00:00 Optical Properties of Salt Ice Lane, J. W. 1975 http://dx.doi.org/10.1017/s0022143000034481 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000034481 en eng Cambridge University Press (CUP) Journal of Glaciology volume 15, issue 73, page 363-372 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1975 crcambridgeupr https://doi.org/10.1017/s0022143000034481 2024-02-08T08:36:15Z Abstract The dependence of the extinction coefficient on salinity was investigated for both NaCl-ice and salt-ice made from natural sea-water. Specimens were prepared under a variety of conditions and examined over the wavelength range 4 000 to 8 000 Â. The effects of scattering from air bubbles trapped in the ice were examined for ice made from distilled water. It was found that the method of preparing samples markedly affected their structure, but that, when prepared in the same manner, salt-ice made from natural sea-water and NaCl-ice did not show significantly different transmission properties. It was found that, for a wavelength of 6 328 Â, the data could be fit to the relation within an uncertainty of 26%, where k e is the extinction coefficient, x is the salinity of the ice in g/kg. Within an uncertainty of 10%, there was no variation in transmission for ice at the same temperature and salinity over the wavelength range 4 000 to 8 000 Â. All measurements were made at a temperature of -20° C. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 15 73 363 372
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Lane, J. W.
Optical Properties of Salt Ice
topic_facet Earth-Surface Processes
description Abstract The dependence of the extinction coefficient on salinity was investigated for both NaCl-ice and salt-ice made from natural sea-water. Specimens were prepared under a variety of conditions and examined over the wavelength range 4 000 to 8 000 Â. The effects of scattering from air bubbles trapped in the ice were examined for ice made from distilled water. It was found that the method of preparing samples markedly affected their structure, but that, when prepared in the same manner, salt-ice made from natural sea-water and NaCl-ice did not show significantly different transmission properties. It was found that, for a wavelength of 6 328 Â, the data could be fit to the relation within an uncertainty of 26%, where k e is the extinction coefficient, x is the salinity of the ice in g/kg. Within an uncertainty of 10%, there was no variation in transmission for ice at the same temperature and salinity over the wavelength range 4 000 to 8 000 Â. All measurements were made at a temperature of -20° C.
format Article in Journal/Newspaper
author Lane, J. W.
author_facet Lane, J. W.
author_sort Lane, J. W.
title Optical Properties of Salt Ice
title_short Optical Properties of Salt Ice
title_full Optical Properties of Salt Ice
title_fullStr Optical Properties of Salt Ice
title_full_unstemmed Optical Properties of Salt Ice
title_sort optical properties of salt ice
publisher Cambridge University Press (CUP)
publishDate 1975
url http://dx.doi.org/10.1017/s0022143000034481
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000034481
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 15, issue 73, page 363-372
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000034481
container_title Journal of Glaciology
container_volume 15
container_issue 73
container_start_page 363
op_container_end_page 372
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