Modelling spatial distribution of surface runoff and sediment yield in a Chinese river basin without continuous sediment monitoring

被引:13
|
作者
Schmalz, B. [1 ]
Zhang, Q. [2 ]
Kuemmerlen, M. [3 ,4 ,5 ]
Cai, Q. [6 ]
Jaehnig, S. C. [3 ,4 ,5 ]
Fohrer, N. [1 ]
机构
[1] Univ Kiel, Inst Nat Resource Conservat, Dept Hydrol & Water Resources Management, D-24118 Kiel, Germany
[2] Chinese Acad Sci, Nanjing Inst Geog & Limnol, Key Lab Watershed Geog Sci, Nanjing 210008, Jiangsu, Peoples R China
[3] Biodivers & Climate Res Ctr BiK F, Dept River Ecol & Conservat, Gelnhausen, Germany
[4] Senckenberg Res Inst, Gelnhausen, Germany
[5] Nat Hist Museum, Gelnhausen, Germany
[6] Chinese Acad Sci, Inst Hydrobiol, State Key Lab Freshwater Ecol & Biotechnol, Wuhan 430072, Peoples R China
关键词
surface runoff; streamflow; Poyang area; land use; SWAT; China; sediment; SOURCE POLLUTION MODEL; SOIL-EROSION; YANGTZE-RIVER; SOUTHERN CHINA; AQUATIC ECOSYSTEMS; FOOD SECURITY; LAND-USE; CATCHMENT; MACROINVERTEBRATES; AGGREGATION;
D O I
10.1080/02626667.2014.967245
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
In numerous river basins, continuous data are available for streamflow, but not for sediment transport, soil erosion and sediment yield. Our study shows an approach to assess the spatial distribution of surface runoff and sediment yield in a data-scarce Chinese river basin. Specific objectives of this study were (a) to use the process-based, ecohydrological model SWAT and to parameterize it by fixing as many parameters as possible in advance using field observations, measured data and literature; (b) to calculate streamflow and suspended sediment at the basin outlet as well as surface runoff and sediment yield in each sub-basin using SWAT; and (c) to validate and check the credibility of our simulated results using published literature on land use and associated land management. Our modelling results show a spatial distribution of sediment yield between all 50 sub-basins (0 to 7 t ha(-1) year(-1)) with highest amounts predicted for cabbage cultivation (37.5 t ha(-1) year(-1)) and only low values for forest (0.2 t ha(-1) year(-1)). Previous studies used for validation purposes approve our findings. [GRAPHICS] Editor Z.W. Kundzewicz; Guest editor V. Krysanova
引用
收藏
页码:801 / 824
页数:24
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