Application Of 137CS fingerprinting technique to interpreting sediment production records from reservoir deposits in a small catchment of the Hilly Loess Plateau, China

被引:36
|
作者
Zhang XinBao [1 ]
Wen ZhongMing
Feng MingYi
Yang QinKe
Zhang JinJun
机构
[1] Chinese Acad Sci, Inst Mt Hazards & Environm, Chengdu 610041, Peoples R China
[2] Minit Water Resources, Chengdu 610041, Peoples R China
[3] Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China
[4] Chinese Acad Sci, Inst Soil & Water Conservat, State Key Lab Soil Eros & Dryland Farming Loess P, Yangling 712100, Peoples R China
[5] MWR, Yangling 712100, Peoples R China
[6] China W Normal Univ, Nanchong 637002, Peoples R China
来源
关键词
Hilly Loess Plateau; small catchment; reservoir deposit; (CS)-C-137 fingerprinting technique; sediment yield;
D O I
10.1007/s11430-007-2013-5
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
According to variations of Cs-137 and clay contents, 44 flood couplets were identified in a profile of reservoir deposit with a vertical length of 28.12 m in the Yuntaishan Gully. Couplet 27 at the middle of the profile had the highest average Cs-137 content of 12.65 Bq(.)kg(-1), which indicated the 1963s' deposits, then Cs-137 content decreased both downward and upward in the profile. The second top and bottom couplets had average Cs-137 contents of 2.15 Bq(.)kg(-1) and 0.92 Bq(.)kg(-1), respectively. By integrated analysis of reservoir construction and management history, variations of Cs-137 contents over the profile, sediment yields of flood couplets and rainfall data during the period of 1958-1970, individual storms related to the flood couplets were identified. 44 floods with a total sediment yield of 2.36 x 10(4) m(3) occurred and flood events in a year varied between 1 and 10 times during the period of 1960-1970. 7-10 flood events occurred during the wet period of 1961-1964 with very wet autumn, while only 1-2 events during the dry period of 1965-1969. Average annual specific sediment yield was 1.29 x 10(4) t(.)km(-2.)a(-1) for the Yuntaishan Gully during the period of 1960-1970, which was slightly higher than 1.11 X 10(4) t(.)km(-2-)a(-1) for the Upper Yanhe River Basin above the Ganguyi Hydrological Station and slightly lower than 1.40 X 10(4) t(.)km(-2.)a(-1) for the nearby Zhifang Gully during the same period. Annual specific sediment yields for the Yuntaishan Gully were correlated to the wet season's rainfalls well.
引用
收藏
页码:254 / 260
页数:7
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