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Spatial distribution of soil erosion and suspended sediment transport rate for Chou-Shui river basin |
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| Authors: | Chin-Ping Lin Ching-Nuo Chen Yu-Min Wang Chih-Heng Tsai Chang-Tai Tsai |
| Institution: | 1. Department of Civil Engineering, National Pingtung University of Science and Technology, Pingtung, Taiwan. 2. International Master’s Program of Soil and Water Engg., National Pingtung University of Science and Technology, Pingtung, Taiwan. 3. Department of Information Communication, University of Kang Ning, No. 188, Sec. 5, Anzhong Road, Tainan, 70970, Taiwan. 4. Department of Hydraulics and Ocean Engineering, National Cheng-Kung University, No. 1, University Road, Tainan City, 70101, Taiwan. |
| Abstract: | In this study, a Physiographic Soil Erosion–Deposition Model (PSED) is applied for better management of a watershed. The PSED model can effectively evaluate the key parameters of watershed management: surface runoff discharge, suspended sediment transport rate, quantity of soil erosion, and spatial distribution of soil erosion and deposition. A basin usually contains multiple watersheds. These watersheds may have complex topography and heterogeneous physiographic properties. The PSED model, containing a physiographic rainfall-runoff model and a basin scale erosion–deposition model, can simulate the physical mechanism of the entire erosion process based on a detailed calculation of bed-load transportation, surface soil entrainment, and the deposition mechanism. With the assistance of Geographic Information Systems (GIS), the PSED model can handle and analyze extremely large hydrologic and physiographic datasets and simulate the physical erosion process without the need for simplification. We verified the PSED model using three typhoon events and 40 rainfall events. The application of PSED to Chou-Shui River basin shows that the PSED model can accurately estimate discharge hydrographs, suspended sediment transport rates, and sediment yield. Additionally, we obtained reasonable quantities of soil erosion as well as the spatial distribution of soil erosion and deposition. The results show that the PSED model is capable of calculating spatially distributed soil erosion and suspended sediment transport rates for a basin with multiple watersheds even if these watersheds have complex topography and heterogeneous physiographic properties. |
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