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 in | Water resources Vol. 42; no. 7; pp. 889 - 896 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Moscow
Pleiades Publishing
01.12.2015
Springer Nature B.V |
Subjects | |
Online Access | Get full text |
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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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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0097-8078 1608-344X |
DOI: | 10.1134/S0097807815070118 |