作者: A. YAIR , D. SHARON , H. LAVEE
DOI: 10.1080/02626668009491932
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摘要: Abstract The study describes an experimental site installed in arid region for the of spatial variations rainfall, runoff and erosion processes along slopes. Data obtained indicate that despite frequent development universal overland flow, due to excess generated at upper part slopes, 60–70m length, has little or no chance reaching slope base during most rainstorms thus does not contribute channel flow. distribution areas contributing storm flow was found be similar observed humid regions. In both cases area is limited a belt extending area. An analysis factors affecting pattern zone presented. Suspended sediment data collected correlation exists between concentrations rates.