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Автор Finkel, R. C.
Автор Nishiizumi, K.
Автор Elmore, D.
Автор Ferraro, R. D.
Автор Gove, H. E.
Дата выпуска 1980
dc.description Concentrations of the cosmogenic radioisotope <sup>36</sup>Cl (t<sub>1/2</sub>=3.0×10<sup>5</sup> yr) in Antarctic ice and in rain and an upper limit to the seawater value have been determined using van de Graaff accelerator high energy mass spectrometry. Chlorine‐36 concentrations in Antarctic ice lie in the range (2.5‐8.7)×10<sup>6</sup> atoms <sup>36</sup>Cl/kg. Recent firn from Siple Station and ice samples collected from the Allan Hills ice field at locations where meteorites have been brought to the surface by glacial flow and ablation have <sup>36</sup>Cl contents which vary by more than a factor of three. This variation can be attributed either to the effects of atmospheric mixing and scavenging or to radioactive decay in very old ice. The <sup>36</sup>Cl concentration found in a sample of recent rainwater is much lower than has been reported in samples collected in the early 1960’s, suggesting that there has been a large decrease in the concentration of atmospheric <sup>36</sup>Cl derived from nuclear weapons tests over this time period. If measurement sensitivities can be increased somewhat, calculations indicate that the bomb spike of <sup>36</sup>Cl may potentially be a useful oceanographic mixing tracer.
Формат application.pdf
Копирайт Copyright 1980 by the American Geophysical Union.
Тема CRYOSPHERE
Тема Snow
Тема Glaciology
Тема GEOCHEMISTRY
Тема Geochemistry: Geochronology (age determinations by radioactive processes)
Тема HYDROLOGY
Тема Glaciology
Тема Snow and ice
Тема OCEANOGRAPHY: GENERAL
Тема Oceanography: Circulation
Название <sup>36</sup>Cl in polar ice, rainwater and seawater
Тип article
DOI 10.1029/GL007i011p00983
Electronic ISSN 1944-8007
Print ISSN 0094-8276
Журнал Geophysical Research Letters
Том 7
Первая страница 983
Последняя страница 986
Выпуск 11
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