Use of reservoir deposits to reconstruct the recent changes in sediment yields from a small granite catchment in the Yimeng Mountain region, China
Zhang, Yunqi1,2; Long, Yi3; Li, Bao2; Xu, Shujian2; Wang, Xiaoli2; Liao, Jia1
刊名GEOMORPHOLOGY
2017-09-15
卷号293页码:167-177
关键词Yimeng Mountain Region Small Granite Catchment Sediment Yield Human Disturbance
ISSN号0169-555X
DOI10.1016/j.geomorph.2017.05.017
通讯作者Yunqi Zhang
英文摘要

Information on recent changes in sediment yields from small catchments provides a better understanding of temporal trends in soil loss from certain physical and human-influenced landscapes that have been subjected to recent environmental changes, and will help bridge the current knowledge gap that exists between hillslope erosion and sediment transport in rivers. The Yimeng Mountain region, characterized by alternating granite and limestone, is one of the most susceptible regions to soil erosion in northern China, and has been subjected to intensive anthropogenic activity in recent years. Soil loss from areas underlain by granite is particularly obvious, and is the main sediment source for the Yihe River. In this study, we used reservoir deposits to estimate the changes in sediment yields over the past similar to 50 years from a small catchment underlain by granite, namely the Jiangzhuang catchment in the Yimeng Mountain region. Three cores were collected from the Jiangzhuang Reservoir in the catchment. The activities of Cs-137 and Pb-210(ex) at different depths, clay (grain size < 5 mu m) contents, and sedimentary organic carbon (SOC) contents in the cores were analysed with reference to human activity and environmental change in the catchment. The chronologies of the cores were established by 137Cs and 210Pbex dating. The area-specific sediment yield (SSY) for different time periods since dam construction was estimated from each core by referring to the original capacity curve of the reservoir. The results indicate that the depth profiles of (CS)-C-137, Pb-210(ex), clay, and SOC contents in cores from the Jiangzhuang Reservoir reflect the general history of human disturbances on the catchment over the past similar to 50 years. The estimated SSY value from each core for each period ranged from 7.2 +/- 2.7 to 23.7 +/- 8.3 t ha(-1) y(-1), with a mean of 12.5 +/- 4.6 t ha(-1) y(-1). SSY decreased during 1954-1972, and then showed a general tendency to increase. The temporal pattern of the sediment yield largely reflects the history of environmental change influenced by human activity in the catchment.

语种英语
WOS记录号WOS:000412257100013
内容类型期刊论文
源URL[http://ir.imde.ac.cn/handle/131551/19151]  
专题成都山地灾害与环境研究所_山地表生过程与生态调控重点实验室
作者单位1.Sichuan Agr Univ, Coll Forest, 211 Huimin Rd, Chengdu 611130, Sichuan, Peoples R China
2.Linyi Univ, Shandong Prov Key Lab Water & Soil Conservat & En, Linyi 276005, Shandong, Peoples R China
3.Chinese Acad Sci, Inst Mt Hazards & Environm, Chengdu 610041, Sichuan, Peoples R China
推荐引用方式
GB/T 7714
Zhang, Yunqi,Long, Yi,Li, Bao,et al. Use of reservoir deposits to reconstruct the recent changes in sediment yields from a small granite catchment in the Yimeng Mountain region, China[J]. GEOMORPHOLOGY,2017,293:167-177.
APA Zhang, Yunqi,Long, Yi,Li, Bao,Xu, Shujian,Wang, Xiaoli,&Liao, Jia.(2017).Use of reservoir deposits to reconstruct the recent changes in sediment yields from a small granite catchment in the Yimeng Mountain region, China.GEOMORPHOLOGY,293,167-177.
MLA Zhang, Yunqi,et al."Use of reservoir deposits to reconstruct the recent changes in sediment yields from a small granite catchment in the Yimeng Mountain region, China".GEOMORPHOLOGY 293(2017):167-177.
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