CO2 in Natural Ice
Abstract Natural ice contains approximately 100 p.p.m. (by weight) of enclosed air. This air is mainly located in bubbles. Carbon dioxide is an exception. We estimate the fraction of CO 2 present in bubbles to be only about 20%. The remaining part is dissolved in the ice. Measurements of the CO 2 co...
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Language: | English |
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Cambridge University Press (CUP)
1978
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Online Access: | http://dx.doi.org/10.1017/s0022143000033487 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033487 |
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crcambridgeupr:10.1017/s0022143000033487 2024-03-03T08:46:05+00:00 CO2 in Natural Ice Stauffer, B. Berner, W. 1978 http://dx.doi.org/10.1017/s0022143000033487 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033487 en eng Cambridge University Press (CUP) Journal of Glaciology volume 21, issue 85, page 291-300 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1978 crcambridgeupr https://doi.org/10.1017/s0022143000033487 2024-02-08T08:39:08Z Abstract Natural ice contains approximately 100 p.p.m. (by weight) of enclosed air. This air is mainly located in bubbles. Carbon dioxide is an exception. We estimate the fraction of CO 2 present in bubbles to be only about 20%. The remaining part is dissolved in the ice. Measurements of the CO 2 content of ice samples from temperate and cold glacier ice as well as of freshly fallen snow and of a laboratory-grown single crystal are presented. Glaciological implications are discussed. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 21 85 291 300 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Stauffer, B. Berner, W. CO2 in Natural Ice |
topic_facet |
Earth-Surface Processes |
description |
Abstract Natural ice contains approximately 100 p.p.m. (by weight) of enclosed air. This air is mainly located in bubbles. Carbon dioxide is an exception. We estimate the fraction of CO 2 present in bubbles to be only about 20%. The remaining part is dissolved in the ice. Measurements of the CO 2 content of ice samples from temperate and cold glacier ice as well as of freshly fallen snow and of a laboratory-grown single crystal are presented. Glaciological implications are discussed. |
format |
Article in Journal/Newspaper |
author |
Stauffer, B. Berner, W. |
author_facet |
Stauffer, B. Berner, W. |
author_sort |
Stauffer, B. |
title |
CO2 in Natural Ice |
title_short |
CO2 in Natural Ice |
title_full |
CO2 in Natural Ice |
title_fullStr |
CO2 in Natural Ice |
title_full_unstemmed |
CO2 in Natural Ice |
title_sort |
co2 in natural ice |
publisher |
Cambridge University Press (CUP) |
publishDate |
1978 |
url |
http://dx.doi.org/10.1017/s0022143000033487 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033487 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 21, issue 85, page 291-300 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000033487 |
container_title |
Journal of Glaciology |
container_volume |
21 |
container_issue |
85 |
container_start_page |
291 |
op_container_end_page |
300 |
_version_ |
1792501956835540992 |