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...
Published in: | Journal of Glaciology |
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Language: | English |
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Cambridge University Press (CUP)
1971
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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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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 |
_version_ |
1792502099843481600 |