Dating of Polar Ice By 32Si

32 Si dating of glacier ice has hitherto been complicated by the poor knowledge of the half life. Furthermore, fall-out of bomb-produced 32 Si impedes the determination of the specific activity of cosmic-ray produced 32 Si in recent precipitation. Measurements on well-dated pre-bomb samples from the...

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Published in:Journal of Glaciology
Main Author: Clausen, Henrik B.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1973
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000031828
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000031828
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spelling crcambridgeupr:10.1017/s0022143000031828 2024-03-03T08:44:37+00:00 Dating of Polar Ice By 32Si Clausen, Henrik B. 1973 http://dx.doi.org/10.1017/s0022143000031828 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000031828 en eng Cambridge University Press (CUP) Journal of Glaciology volume 12, issue 66, page 411-416 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1973 crcambridgeupr https://doi.org/10.1017/s0022143000031828 2024-02-08T08:41:37Z 32 Si dating of glacier ice has hitherto been complicated by the poor knowledge of the half life. Furthermore, fall-out of bomb-produced 32 Si impedes the determination of the specific activity of cosmic-ray produced 32 Si in recent precipitation. Measurements on well-dated pre-bomb samples from the Greenland ice sheet establish a calibration for 32 Si dating of up to 1 000 year old polar ice samples of the magnitude of 1 metric ton. If the technique is used on temperate glaciers, samples of pre-bomb deposits (or from after 1970) must be collected for comparison with samples of old ice, using an apparent half life of 295±25 years. Due to secular cosmic-ray flux variations, the true half life of 32 Si is estimated at the slightly higher value of 330±40 years. Article in Journal/Newspaper glacier Greenland Ice Sheet Journal of Glaciology Cambridge University Press Greenland Journal of Glaciology 12 66 411 416
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Clausen, Henrik B.
Dating of Polar Ice By 32Si
topic_facet Earth-Surface Processes
description 32 Si dating of glacier ice has hitherto been complicated by the poor knowledge of the half life. Furthermore, fall-out of bomb-produced 32 Si impedes the determination of the specific activity of cosmic-ray produced 32 Si in recent precipitation. Measurements on well-dated pre-bomb samples from the Greenland ice sheet establish a calibration for 32 Si dating of up to 1 000 year old polar ice samples of the magnitude of 1 metric ton. If the technique is used on temperate glaciers, samples of pre-bomb deposits (or from after 1970) must be collected for comparison with samples of old ice, using an apparent half life of 295±25 years. Due to secular cosmic-ray flux variations, the true half life of 32 Si is estimated at the slightly higher value of 330±40 years.
format Article in Journal/Newspaper
author Clausen, Henrik B.
author_facet Clausen, Henrik B.
author_sort Clausen, Henrik B.
title Dating of Polar Ice By 32Si
title_short Dating of Polar Ice By 32Si
title_full Dating of Polar Ice By 32Si
title_fullStr Dating of Polar Ice By 32Si
title_full_unstemmed Dating of Polar Ice By 32Si
title_sort dating of polar ice by 32si
publisher Cambridge University Press (CUP)
publishDate 1973
url http://dx.doi.org/10.1017/s0022143000031828
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000031828
geographic Greenland
geographic_facet Greenland
genre glacier
Greenland
Ice Sheet
Journal of Glaciology
genre_facet glacier
Greenland
Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology
volume 12, issue 66, page 411-416
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000031828
container_title Journal of Glaciology
container_volume 12
container_issue 66
container_start_page 411
op_container_end_page 416
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