Chloride Segregation Along Grain Boundaries in Ice

Abstract A new technique for precisely detecting chlorides in ice has been developed. It is based on a microchemical contact reaction which takes place when a thin surface layer of ice melts through a membrane filter previously soaked in a concentrated solution of silver nitrate and dried. The silve...

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Published in:Journal of Glaciology
Main Authors: Prodi, F., Nagamoto, C.T.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1971
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000013265
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000013265
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spelling crcambridgeupr:10.1017/s0022143000013265 2024-03-03T08:46:09+00:00 Chloride Segregation Along Grain Boundaries in Ice Prodi, F. Nagamoto, C.T. 1971 http://dx.doi.org/10.1017/s0022143000013265 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000013265 en eng Cambridge University Press (CUP) Journal of Glaciology volume 10, issue 59, page 299-308 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1971 crcambridgeupr https://doi.org/10.1017/s0022143000013265 2024-02-08T08:34:04Z Abstract A new technique for precisely detecting chlorides in ice has been developed. It is based on a microchemical contact reaction which takes place when a thin surface layer of ice melts through a membrane filter previously soaked in a concentrated solution of silver nitrate and dried. The silver chloride thus formed is reduced to metallic silver under ultra-violet light. The results on natural hailstones and laboratory doped ice show that foreign molecules are mainly segregated along the grain boundaries rather than being captured in the ice lattice. The technique, which makes quantitative evaluations possible, appears promising in all experimental studies on natural ice (hailstones and sea ice) and on ice artificially grown in the laboratory (by accretion or by freezing of solutions). Article in Journal/Newspaper Journal of Glaciology Sea ice Cambridge University Press Journal of Glaciology 10 59 299 308
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Prodi, F.
Nagamoto, C.T.
Chloride Segregation Along Grain Boundaries in Ice
topic_facet Earth-Surface Processes
description Abstract A new technique for precisely detecting chlorides in ice has been developed. It is based on a microchemical contact reaction which takes place when a thin surface layer of ice melts through a membrane filter previously soaked in a concentrated solution of silver nitrate and dried. The silver chloride thus formed is reduced to metallic silver under ultra-violet light. The results on natural hailstones and laboratory doped ice show that foreign molecules are mainly segregated along the grain boundaries rather than being captured in the ice lattice. The technique, which makes quantitative evaluations possible, appears promising in all experimental studies on natural ice (hailstones and sea ice) and on ice artificially grown in the laboratory (by accretion or by freezing of solutions).
format Article in Journal/Newspaper
author Prodi, F.
Nagamoto, C.T.
author_facet Prodi, F.
Nagamoto, C.T.
author_sort Prodi, F.
title Chloride Segregation Along Grain Boundaries in Ice
title_short Chloride Segregation Along Grain Boundaries in Ice
title_full Chloride Segregation Along Grain Boundaries in Ice
title_fullStr Chloride Segregation Along Grain Boundaries in Ice
title_full_unstemmed Chloride Segregation Along Grain Boundaries in Ice
title_sort chloride segregation along grain boundaries in ice
publisher Cambridge University Press (CUP)
publishDate 1971
url http://dx.doi.org/10.1017/s0022143000013265
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000013265
genre Journal of Glaciology
Sea ice
genre_facet Journal of Glaciology
Sea ice
op_source Journal of Glaciology
volume 10, issue 59, page 299-308
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000013265
container_title Journal of Glaciology
container_volume 10
container_issue 59
container_start_page 299
op_container_end_page 308
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