137Cs budget during the period of 1960s in a small drainage basin on the Loess Plateau of China

被引:38
|
作者
Zhang, X
Walling, DE
Yang, Q
He, X
Wen, Z
Qi, Y
Feng, M
机构
[1] Chinese Acad Sci, Inst Mt Hazards & Environm, Chengdu 610041, Peoples R China
[2] MWR, Inst Mt Hazards & Environm, Chengdu 610041, Peoples R China
[3] Chinese Acad Sci, Inst Soil & Water Conservat, State Key Lab Soil Eros & Dryland Farming Loess P, Yangling 712100, Peoples R China
[4] MWR, Inst Soil & Water Conservat, State Key Lab Soil Eros & Dryland Farming Loess P, Yangling 712100, Peoples R China
[5] Univ Exeter, Dept Geog & Archaeol, Exeter EX4 4RJ, Devon, England
[6] Chinese Acad Sci, Grad Sch, Beijing 100039, Peoples R China
[7] China W Normal Univ, Nanchong 637002, Peoples R China
基金
中国国家自然科学基金;
关键词
Cs-137; budget; 1960s; enrichment coefficient; the Loess Plateau;
D O I
10.1016/j.jenvrad.2005.07.007
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A sediment profile with a thickness of 28.12 m in a failed reservoir in a small catchment of the Yuntaishan Gully in the Loess Plateau of China consisted of 44 flood couplets deposited during the period from 1960 to 1970 with total volume of 2.36 X 10(6) m(3). Specific sediment yields for a flood event varied from 300 t km(-2) to 14,400 t km(-2) and annual sediment yields varied from 2500 t km(-2) in 1966 to 40,000 t km(-2) in 1964 with a mean value of 12,700 t km(-2) a(-1) for the period. Average annual Cs-137 concentrations of the sediments increased from 0.92 Bq kg(-1) in 1960 to 4.82 Bq kg(-1) in 1963, then decreased to 1.53 Bq kg(-1) in 1970. The total Cs-137 activity in the reservoir sediments was 9.22 X 10(9) Bq, which accounted for 31.9% of the total Cs-137 fallout precipitation of 2.89 X 10(10) Bq within the catchment during the period. The proportion of the Cs-137 loss from the catchment to the Cs-137 fallout precipitation within the catchment in a year varied between 8.01% and 66.8%, and it was 20.9% for the peak Cs-137 deposition year of 1963 and 52.0% in 1964. By analysis of the Cs-137 budget in the catchment for the Cs-137 peak precipitation period from 1962 to 1964, the Cs-137 surface enrichment coefficient Gamma should be Much less than 0.23. And for calculation of soil losses on the cultivated land in the inter-gully area by using the Mass Balance Model 11, the value of Gamma should be 0.05-0.1. (C) 2005 Elsevier Ltd. All rights reserved.
引用
收藏
页码:78 / 91
页数:14
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