中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Slope runoff study in situ using rainfall simulator in mountainous area of North China

文献类型:SCI/SSCI论文

作者Yu J. J. ; Yang C. ; Liu C. M. ; Song X. F. ; Hu S. S. ; Li F. D. ; Tang C. Y.
发表日期2009
关键词simulated rainfall slope plot runoff generation process mountainous area of North China soil infiltration
英文摘要Simulated rainfall is a valid tool to examine the runoff generation on the slope. 13 simulated rainfall experiments with different rainfall intensities and durations are completed in a 5 m x 10 m experimental plot in mountainous area of North China. Simultaneously, rainfall, surface runoff, soil-layer flow, mantel-layer flow and soil moisture are monitored respectively. From the results, it is found that the hydrographs in all layers have the characteristics of rapid rise and fall. The recessions of surface flow and soil-layer flow are much faster than that of mantel-layer flow. Surface flow, the main contributor, makes up more than 60% of the total runoff in the study area. It even exceeds 90% in the cases of high intensity rainfall events. Runoff coefficient (ratio of total runoff to rainfall amount) is mainly influenced by rainfall amount, rainfall intensity and antecedent soil moisture, and the relationship can be well expressed by a multiple linear regression function alpha = 0.002P + 0.182i + 4.88W(a) - 0.821. The relation between the rainfall intensity and the lag time of three flows (surface runoff, soil-layer flow and mantel-layer flow) is shown to be exponential. Then, the result also shows that the recession constant is 0.75 for surface runoff, is 0.94 for soil-layer and mantel-layer flow in this area. In this study area, the dominant infiltration excess runoff is simulated by Horton model. About 0.10 mm/min percolation is observed under the condition of different rainfall intensities, therefore the value is regarded as the steady infiltration rate of the study area.
出处Journal of Geographical Sciences
19
4
461-470
收录类别SCI
语种英语
ISSN号1009-637X
源URL[http://ir.igsnrr.ac.cn/handle/311030/22507]  
专题地理科学与资源研究所_历年回溯文献
推荐引用方式
GB/T 7714
Yu J. J.,Yang C.,Liu C. M.,et al. Slope runoff study in situ using rainfall simulator in mountainous area of North China. 2009.

入库方式: OAI收割

来源:地理科学与资源研究所

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