10 Be in Arctic Ocean sediments
The 10 Be deposition rate in two Arctic Ocean cores, ~80°N, was measured to be ≤0.6 atoms cm -2 sec -1 , much less than the 10 Be deposition rate reported for other oceanic regions. Possible causes for the low10Be deposition in the Arctic are: (1) latitudinal variation in the10Be delivery rate from...
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Elsevier Science
1977
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| Online Access: | http://repository.ias.ac.in/16894/ http://linkinghub.elsevier.com/retrieve/pii/0012821X77901224 |
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ftindianacasci:oai:repository.ias.ac.in:16894 |
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ftindianacasci:oai:repository.ias.ac.in:16894 2023-05-15T14:22:58+02:00 10 Be in Arctic Ocean sediments Finkel, R. Krishnaswami, S. Clark, D. L. 1977-06 http://repository.ias.ac.in/16894/ http://linkinghub.elsevier.com/retrieve/pii/0012821X77901224 unknown Elsevier Science Finkel, R. Krishnaswami, S. Clark, D. L. (1977) 10Be in Arctic Ocean sediments Earth and Planetary Science Letters, 35 (2). pp. 199-204. ISSN 0012-821X Article PeerReviewed 1977 ftindianacasci 2013-01-20T10:11:55Z The 10 Be deposition rate in two Arctic Ocean cores, ~80°N, was measured to be ≤0.6 atoms cm -2 sec -1 , much less than the 10 Be deposition rate reported for other oceanic regions. Possible causes for the low10Be deposition in the Arctic are: (1) latitudinal variation in the10Be delivery rate from the stratosphere; (2) the presence of an ice cover on the Arctic, which may inhibit the transfer of atmospherically supplied10Be from sea surface to sediments; and (3) locally low scavenging efficiency of sedimentary particles for 10 Be in the Arctic. Article in Journal/Newspaper Arctic Arctic Arctic Ocean Indian Academy of Sciences: Publication of Fellows Arctic Arctic Ocean |
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Open Polar |
| collection |
Indian Academy of Sciences: Publication of Fellows |
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ftindianacasci |
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unknown |
| description |
The 10 Be deposition rate in two Arctic Ocean cores, ~80°N, was measured to be ≤0.6 atoms cm -2 sec -1 , much less than the 10 Be deposition rate reported for other oceanic regions. Possible causes for the low10Be deposition in the Arctic are: (1) latitudinal variation in the10Be delivery rate from the stratosphere; (2) the presence of an ice cover on the Arctic, which may inhibit the transfer of atmospherically supplied10Be from sea surface to sediments; and (3) locally low scavenging efficiency of sedimentary particles for 10 Be in the Arctic. |
| format |
Article in Journal/Newspaper |
| author |
Finkel, R. Krishnaswami, S. Clark, D. L. |
| spellingShingle |
Finkel, R. Krishnaswami, S. Clark, D. L. 10 Be in Arctic Ocean sediments |
| author_facet |
Finkel, R. Krishnaswami, S. Clark, D. L. |
| author_sort |
Finkel, R. |
| title |
10 Be in Arctic Ocean sediments |
| title_short |
10 Be in Arctic Ocean sediments |
| title_full |
10 Be in Arctic Ocean sediments |
| title_fullStr |
10 Be in Arctic Ocean sediments |
| title_full_unstemmed |
10 Be in Arctic Ocean sediments |
| title_sort |
10 be in arctic ocean sediments |
| publisher |
Elsevier Science |
| publishDate |
1977 |
| url |
http://repository.ias.ac.in/16894/ http://linkinghub.elsevier.com/retrieve/pii/0012821X77901224 |
| geographic |
Arctic Arctic Ocean |
| geographic_facet |
Arctic Arctic Ocean |
| genre |
Arctic Arctic Arctic Ocean |
| genre_facet |
Arctic Arctic Arctic Ocean |
| op_relation |
Finkel, R. Krishnaswami, S. Clark, D. L. (1977) 10Be in Arctic Ocean sediments Earth and Planetary Science Letters, 35 (2). pp. 199-204. ISSN 0012-821X |
| _version_ |
1766295464711290880 |