Agricultural catchment;
Chernobyl accident;
East European plain;
The Lokna river basin;
Radioactive contamination;
Radiocesium;
FOREST-STEPPE ZONE;
SEDIMENT REDISTRIBUTION;
VERTICAL-DISTRIBUTION;
SPATIAL VARIABILITY;
EROSION RATES;
LOKNA RIVER;
SMALL BASIN;
TO-PLANT;
RADIOCESIUM;
CESIUM-137;
D O I:
10.1016/j.jenvrad.2020.106386
中图分类号:
X [环境科学、安全科学];
学科分类号:
08 ;
0830 ;
摘要:
A detailed study of Cs-137 redistribution was conducted within a small agricultural catchment in the highly contaminated Plavsk radioactive hotspot in the Tula region of Central Russia, 32 years after the Chernobyl nuclear power plant (NPP) accident, which occurred on April 26,1986. Although more than three decades have passed since the Chernobyl NPP incident, Cs-137 contamination is high. The Cs-137 inventory varies from 67 to 306 kBq.m(-2), which is 2-6 times higher than the radiation safety standard; however, the soils remain suitable for crop cultivation. The initial Cs-137 fallout within the Plavsk radioactive hotspot was extremely heterogeneous, with a trend of decreasing Cs-137 inventories from the NW to the SE directions within the studied territory. Contemporary Cs-137 inventories are also very heterogeneous in the studied catchment. However, the trend of the initial Cs-137 fallout does not appear in the contemporary Cs-137 inventories on the slopes. Two methods of interpolation (expert-visual and automatic) were used to calculate the Cs-137 budget, revealing high similarity in their Cs-137 loss estimates; however, a large discrepancy was observed in their (137)Css gain estimates. A detailed analysis of Cs-137 redistribution revealed the importance of hollows and "plow ramparts" (positive topographic forms on the boundaries of cultivated fields) in the transport and deposition of sediments. A quarter of the total Cs-137 gain was deposited within the arable land, whereas a quarter was deposited within the non-plowing sides of the dry valley; the other half was deposited in the valley bottom. About 7-8 x 10(6) kBq of the Cs-137 inventory flowed out of the catchment area, which was only about 2% of the Cs-137 fallout after the Chernobyl NPP accident. About 89% of the total Cs-137 reserve is concentrated in the top (0-25 cm) layer of soils, regardless of land use or location within the catchment.
机构:
Chinese Acad Sci, Key Lab Water Cycle & Related Land Surface Proc, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R ChinaChinese Acad Sci, Key Lab Water Cycle & Related Land Surface Proc, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
Fang, Haiyan
Li, Qiuyan
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Chinese Acad Sci, Key Lab Water Cycle & Related Land Surface Proc, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R ChinaChinese Acad Sci, Key Lab Water Cycle & Related Land Surface Proc, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
Li, Qiuyan
Sun, Liying
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机构:
Chinese Acad Sci, Key Lab Water Cycle & Related Land Surface Proc, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R ChinaChinese Acad Sci, Key Lab Water Cycle & Related Land Surface Proc, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
Sun, Liying
Cai, Qiangguo
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机构:
Chinese Acad Sci, Key Lab Water Cycle & Related Land Surface Proc, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R ChinaChinese Acad Sci, Key Lab Water Cycle & Related Land Surface Proc, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China