Study on the relationship between rainfall characters and runoff-sediment yield of slopes of different land use types in northern mountain area of Hebei
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DOI:10.7606/j.issn.1000-7601.2011.06.37
Key Words: land use type  rainfall characters  runoff and sediment yield  northern mountain area of Hebei
Author NameAffiliation
JIANG Qinglong College of Resources and Environment Northwest A & F University YanglingShaanxi 712100China 
XIE Yongsheng College of Resources and Environment Northwest A & F University YanglingShaanxi 712100China
Institue of Soil and W ater Consenoation, Chinese Academy of Sciences and Ministry of W ater Resources, Yangling, Shaanxi 712100China 
ZHAO Ting Institue of Soil and W ater Consenoation, Chinese Academy of Sciences and Ministry of W ater Resources, Yangling, Shaanxi 712100China 
ZHANG Yinglong College of Resources and Environment Northwest A & F University YanglingShaanxi 712100China 
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Abstract:
      A study was made in the highly fragile ecological env ironment with serious soil and water loss in northern mountain area of Hebei Province, which was the water source area of the cities of Beijing and Tianjin. Three runoff plots with land use types of forest,open forest and natural grassland were constructed in Caojiagou of Weichang County,and the rainfall characters and runoff and sediment yield of the three plots were analyzed. The results showed that the rainfalls which caused runoff on the plots were mainly moderate rain and heavy rain, and the average rainfall intensity was 5.83 mm/h; correlative analysis showed that there was a positive correlation between runoff and the product of rainfall and rainfall duration; the correlation coefficients between sediment yield modules and the product of rainfall and rainfall in-tensity of forest,open forest and natural grass land were 0.587, 0.501 and 0.613 respectively; the sediment yield mod-ules of open forest and natural grass land showed a highly sigmificant correlation with the runoff depth, while the forest was not. The capacity of soil and water conservation of the three slopes was in the order of forest> natural grass land>open forest.