[1]XU Xuexuan,MU Xingmin,JIANG Dingsheng,et al.Study of Rainfall Redistribution on Slope in Loess Hilly Region[J].Research of Soil and Water Conservation,2002,9(03):249-250,253.
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Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume:
9
Number of periods:
2002年03期
Page number:
249-250,253
Column:
Public date:
1900-01-01
- Title:
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Study of Rainfall Redistribution on Slope in Loess Hilly Region
- Author(s):
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XU Xuexuan1, MU Xingmin1, JIANG Dingsheng1, WANG Yu2, WANG Wei1
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1. Institute of Soil and Water Conservation, Northwest Sci tech University of Agriculture and Forestry, Yangling 712100, Shaanxi Province, China;
2. Baota Branch of Yanhe Comprehensive Control Office of the World Bank Loan Program in Yanan, Shaanxi, Ch
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- Keywords:
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rainfall; runoff; redistribution on slope; loess hilly region
- CLC:
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S273.29
- DOI:
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- Abstract:
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Based on field study of rainfall redistribution on slope, authors put forward that the transition of rainfall to soil water is affected by slope length, land use form, etc.in both intensity and orientation.The results showed that soil could get more rainfall with slope length increasing from top to bottom.With a 20 m increase of slope length, the increase of incepted rainfall is 0.77 mm in grassland or 0.92 mm in shrub land.In the trial study, the 60 m slope length of shrub (or grassland) could reduce 4.91 mm (or 4.1 mm) of runoff compared with that of slope farmland, which accounts for 56.52% (47.16% )of runoff cut rate.K a representatives rate of water incepted from rainfall, was also in the same way.Forestry land had higher K a than that of grassland.It is also stated that the subsoil water movement is the main cause of slope soil water difference.