Research on Processes and Responses of Rainfall-Runoff-Sediment Yield on Loess Hillslope
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Research on Processes and Responses of Rainfall-Runoff-Sediment Yield on Loess Hillslope
Vol. 22, Issue 2, Pages: 24-28(2008)
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CLC:S157.1
Published:2008
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WANG Zhan-li, JIN Xue-yan, MA Chun-yan, et al. Research on Processes and Responses of Rainfall-Runoff-Sediment Yield on Loess Hillslope[J]. 2008, 22(2): 24-28.
DOI:
WANG Zhan-li, JIN Xue-yan, MA Chun-yan, et al. Research on Processes and Responses of Rainfall-Runoff-Sediment Yield on Loess Hillslope[J]. 2008, 22(2): 24-28.DOI:
Research on Processes and Responses of Rainfall-Runoff-Sediment Yield on Loess Hillslope
Rainfall and runoff are the main dynamic factors which cause soil erosion on the Loess Plateau.Research on processes of rainfall
runoff and sediment yield can serve as development of process-based mode of soil erosion
soil and water conservation
and ecology construction on loess region.Based on analyzing the data of natural unsteady rainfall
runoff and sediment yield processes observed in Zizhou field experimental station
and applying non-linear modelling technology
the dynamic variational processes and responded relationship of rainfall-runoff-sediment yield on loess hillslope are studied.The research results show that the variation processes of accumulated rainfall amount with rainfall time
the variation processes of accumulated runoff depth with runoff time
the variation processes of accumulated erosion modulus with sediment yield time
the responses of variation processes of accumulated runoff depth to variation processes of accumulated rainfall amount
the responses of variation processes of accumulated erosion modulus to variation processes of accumulated runoff depth are all displayed with non-linear relationships.All of them can be divided into two types and can be described with extanded S curve model and extanded power function model respectively.