Evaluating the runoff of global-fallout cesium-137 from landscapes of the Ob river basin

The activity of cesium-137 from global atmospheric fallouts was studied in the soils of three 1 st order catchment basins in the taiga, subtaiga, and forest-steppe zones in the Ob basin. Cesium-137 runoff from those catchment basins was evaluated to give 0.48–5.0 in the taiga, 14.9–15.3 in the subta...

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Published inWater resources Vol. 42; no. 7; pp. 889 - 896
Main Authors Semenkov, I. N., Miroshnikov, A. Yu
Format Journal Article
LanguageEnglish
Published Moscow Pleiades Publishing 01.12.2015
Springer Nature B.V
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Summary:The activity of cesium-137 from global atmospheric fallouts was studied in the soils of three 1 st order catchment basins in the taiga, subtaiga, and forest-steppe zones in the Ob basin. Cesium-137 runoff from those catchment basins was evaluated to give 0.48–5.0 in the taiga, 14.9–15.3 in the subtaiga, and 14.1–15.7 mCi km –2 . in the forest-steppe zones. The published data on sediment delivery coefficients and the leveloped typification of river basins were used to extrapolate the obtained data on 137 Cs runoff to the area of developed semihumid and humid river basins under natural vegetation. The runoff of global-fallout 137 Cs from the Ob Basin never exceeds 4% of its total reserves.
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ISSN:0097-8078
1608-344X
DOI:10.1134/S0097807815070118