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《Scientia Geographica Sinica》 2001-03
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Research on Transforming Relation from Point to Area of Infiltration Rate on Small Watershed for Hilly and Gully the Loess Region

YUAN Jian ping 1,2 , JIANG Ding sheng 3 (1 Department of Resources and Environment, Beijing Normal University, Beijing 10087; 2. Monitoring Center of Soil and Water Conservation, Miusitry of Water Resources; Beijing 100053; 3 Institute o  
Based on effect factors of transforming from point to area of infiltration rate and crust etc , put forward the formula of changing soil point's infiltration rate to area's rate on small watershed, which is fm=fn×Sn/S×an×bn Here, fm is the average soil area's infiltration rate(mm/min) on behalf of different land using models and topography and landforms, fn is the average soil point's infiltration rate(mm/min) under different land using models and topography and landforms through many field tests, Sn represents areas of different land using models(hm 2), S is Watershed's area(hm 2), an means correct coefficient thinking the effect of crust and system mistake etc , bn is the parameter thinking the effect of soil's water content Comparing the area's infiltration rate between transforming value and observing value, the result showed that relative error was only 2 42 percent , Preliminary gain the equations, which have high precision including single and fixed factors equations between soil area's infiltration rate and different soil control degree, rain quantity The method is advantageous for seeking rain, runoff, infiltration's changing trend after comprehensive control on small watershed
【Fund】: 国家杰出青年科学基金 ( 4 972 5 10 3);; 博士后科研基金共同资助
【CateGory Index】: S152.72
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