Chemical analysis of snow and ice samples-High sensitive measurement of 210Pb in snow and ice samples by using alpha spectrometry-

The natural radioactive nuclide, ^Pb, with a half-life of 22.3 years in snow and ice is useful for considering the origin of atmospheric aerosols and also for estimating the sedimentation rate onto a glacier. The α spectrometric method for sensitive analysis of ^Pb in ice samples and the method of i...

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Bibliographic Details
Main Authors: Toshitaka Suzuki, Kazutaka Ohta, Yoshiyuki Fujii, Okitsugu Watanabe
Format: Article in Journal/Newspaper
Language:English
Published: National Institute of Polar Research 1996
Subjects:
geo
Online Access:https://doi.org/10.15094/00008945
https://doaj.org/article/5c4c2f55b107463d970b1102c06ea80a
Description
Summary:The natural radioactive nuclide, ^Pb, with a half-life of 22.3 years in snow and ice is useful for considering the origin of atmospheric aerosols and also for estimating the sedimentation rate onto a glacier. The α spectrometric method for sensitive analysis of ^Pb in ice samples and the method of ice core dating are described in this paper. Measurements of ^Pb in ice cores from the Arctic glacier, Åsgardfonna, in the Svalbard archipelagos have been made. The activity of ^Pb was obtained by counting α rays from its daughter nuclide, ^Po (half-life 138 days). The specific activity of ^Pb at the surface of the glacier, 110mBq/kg, decreased exponentially with depth to 4.72mBq/kg at about 30m depth. Below 30m, the activities were nearly constant and its average value from 30m to 180m was 4.85±1.33mBq/kg. The results indicate that the atmospheric ^Pb deposit onto a glacier decays as a function of time at a rate controlled by its half-life.