On 137Cs migration in water systems of Eastern Fennoscandia
- Authors: Bol’shiyanov D.Y.1, Bakunov N.A.1, Makarov A.S.1
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Affiliations:
- Arctic and Antarctic Research Institute
- Issue: Vol 43, No 3 (2016)
- Pages: 533-538
- Section: Water Quality and Protection: Environmental Aspects
- URL: https://journals.rcsi.science/0097-8078/article/view/173987
- DOI: https://doi.org/10.1134/S0097807816030039
- ID: 173987
Cite item
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.
Keywords
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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