LIU Yuan-li, ZHENG Fen-li, WANG Bin, et al. Assessment of WEPP Model Applicability in Black Soil Zone of Northeast China-A Case Study of Slope Gradient and Soil and Water Conservation Measures[J]. Bulletin of Soiland Water Conservation, 2010, 29(1): 139-145.
DOI:
LIU Yuan-li, ZHENG Fen-li, WANG Bin, et al. Assessment of WEPP Model Applicability in Black Soil Zone of Northeast China-A Case Study of Slope Gradient and Soil and Water Conservation Measures[J]. Bulletin of Soiland Water Conservation, 2010, 29(1): 139-145.DOI:
Assessment of WEPP Model Applicability in Black Soil Zone of Northeast China-A Case Study of Slope Gradient and Soil and Water Conservation Measures
Based on data observed from the automatic meteorological station near runoff plots and measured soil loss data from field runoff plots at Binxian Experimental Station in 2008
runoff and soil loss from the plots in black soil zone
Northeast of China were simulated.The simulation results were compared with measured values and the applicability of WEPP model was assessed.Results showed that Nash -Sutcliffe model efficiencies of event runoff simulation on different slopes by WEPP were 0.47
0.03
and-5.9
respectively.Nash - Sutcliffe model efficiencies of event soil loss simulation were 0.58
0.72
and 0.60
respectively.It indicated that event simulation result of soil loss was better than event simulation result of run-off.WEPP model was sensitive to the change of slope.Nash - Sutcliffe model efficiencies of event runoff simulation to soybean
Dallis grass
alfalfa
and elm were 0.81
0.71
0.83
and 0.94
whereas Nash-Sut-cliffe model efficiencies of event soil loss simulation were 0.81
0.71
0.83 and 0.94
respectively.This show that simulation results of alfalfa and soybean were better
compared with simulation results of grass and elm and simulation results of bare land on different slopes.From the above results
WEPP can be used to simulate event runoff and soil loss under different soil and water conservation measures and event soil loss at different slope gradients on bare land
but it is not suitable to simulate event runoff at different slope gradients on bare land.
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Impacts of rainfall and vegetation on soil erosion in Dabie Mountains forest reform area
Simulation of soil erosion resistance and soil erosion process in arid valley region of southeastern Xizang Autonomous Region
Soil erosion in northern foothills of Qinling Mountains (Xi’an section) from 2010 to 2023
Related Author
Wang Jianxun
Zheng Fenli
Jiang Zhongshan
Zhang Xunchang
ZHANG Pengyu
WANG Quanjiu
ZHOU Beibei
Li Gao
Related Institution
College of Resource and Environment, Northwest Agriculture and Forestry University, Yangling
The State Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling
USDA-ARS Grazinglands Research Laboratory, EI Reno, Oklahoma 73036, U. S
Institute of Water Resources and Hydrologic Engineering, Xian University of Technology, Xian
Tianjin Bibo Environmental Resources Development Limited Company