中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Modelling the runoff-sediment yield relationship using a proportional function in hilly areas of the loess plateau, north china

文献类型:期刊论文

作者Zheng Mingguo1,2; Cai Qiangguo1; Cheng Qinjuan1,2
刊名Geomorphology
出版日期2008-01-15
卷号93期号:3-4页码:288-301
关键词Flow-sediment relationship Sediment yield Temporal scale Loess plateau of china
ISSN号0169-555X
DOI10.1016/j.geomorph.2007.03.001
通讯作者Cai qiangguo(caiqg@igsnrr.ac.cn)
英文摘要Based on data observed at the 12 small watersheds in hilly areas of the loess plateau, north china, the relationship between event runoff volume and sediment yield is examined. the results reveal that the runoff-sediment yield relationship at the inter-event timescale is mainly determined by the runoff-sediment concentration relationship at the intra-event timescale. in the study area, the sediment concentration tends to be stable when the flow discharge exceeds a certain critical value. many factors that are important for determining the characteristics of low-magnitude events, such as flow discharge, particle size of fluvial sediment, and accumulation of loose material on land surfaces prior to a rainstorm, appear to have little importance for high-magnitude events. consequently, mean sediment concentration tends to be stable for large flood events, suggesting a strong similarity between the two flow-sediment relationships at inter-and intra-event temporal scales. furthermore, a proportional function is proposed to predict event sediment yield, and the correspondence between the predicted and observed sediment yields is examined. the performance of the model is good for high-magnitude events, especially extreme events. the applicability of the proposed model at the annual timescale is also discussed. (c) 2007 published by elsevier b.v.
WOS关键词SOIL-EROSION ; BASIN ; FLOW
WOS研究方向Physical Geography ; Geology
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
语种英语
WOS记录号WOS:000255899700009
出版者ELSEVIER SCIENCE BV
URI标识http://www.irgrid.ac.cn/handle/1471x/2388004
专题中国科学院大学
通讯作者Cai Qiangguo
作者单位1.Chinese Acad Sci, Key Lab Water Cycle & Related Land Surface Proc, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
2.Chinese Acad Sci, Grad Sch, Beijing 100039, Peoples R China
推荐引用方式
GB/T 7714
Zheng Mingguo,Cai Qiangguo,Cheng Qinjuan. Modelling the runoff-sediment yield relationship using a proportional function in hilly areas of the loess plateau, north china[J]. Geomorphology,2008,93(3-4):288-301.
APA Zheng Mingguo,Cai Qiangguo,&Cheng Qinjuan.(2008).Modelling the runoff-sediment yield relationship using a proportional function in hilly areas of the loess plateau, north china.Geomorphology,93(3-4),288-301.
MLA Zheng Mingguo,et al."Modelling the runoff-sediment yield relationship using a proportional function in hilly areas of the loess plateau, north china".Geomorphology 93.3-4(2008):288-301.

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来源:中国科学院大学

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