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On 137Cs migration in water systems of Eastern Fennoscandia


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Abstract

The rate of natural removal of 137Cs from water bodies in Eastern Fennoscandia is evaluated. The half-time T of water purification from global 137Cs in lake–river systems was ~6.5 years and that for river systems was 6.5–10 years. For the 15- and 20-year exposure of 137Cs in watershed soils, its annual input in rivers was 0.021–0.120 and 0.017–0.070% of its reserve. The period of May–December 1986 showed maximal export of 137Cs, i.e., 1.1% of its reserve. 137Cs export into rivers decreased in the region from north to south because of changes in landscape and climate conditions that affect 137Cs migration on watersheds.

About the authors

D. Yu. Bol’shiyanov

Arctic and Antarctic Research Institute

Author for correspondence.
Email: bolshiyanov@aari.ru
Russian Federation, ul. Beringa 38, St. Petersburg, 199397

N. A. Bakunov

Arctic and Antarctic Research Institute

Email: bolshiyanov@aari.ru
Russian Federation, ul. Beringa 38, St. Petersburg, 199397

A. S. Makarov

Arctic and Antarctic Research Institute

Email: bolshiyanov@aari.ru
Russian Federation, ul. Beringa 38, St. Petersburg, 199397

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