Analysis on Characteristics of the Rainfall-Runoff in Beizhangdian Watershed


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Beizhangdian watershed is a typical semi-dry and semi-humid region, where human activities have little effect on the hydrological cycle. Based on a 30-year hydrological observation data, the precipitation, runoff, and rainfall-runoff relationship were researched by the hydrology statistics analysis methods. The results indicated that the inter-annual change of rainfall-runoff of the watershed is remarkable, the annual distribution of rainfall-runoff is extremely uneven, and rainfall-runoff mainly occurred in flood season (June ~ September). There is a good uniformity between the variation tendency of annual rainfall and annual runoff in time and amount, the correlation coefficient of rainfall and runoff is 0.74, the value of the F-test is 4.23.



Edited by:

Xuejun Zhou






R. Liang et al., "Analysis on Characteristics of the Rainfall-Runoff in Beizhangdian Watershed", Applied Mechanics and Materials, Vols. 90-93, pp. 2578-2582, 2011

Online since:

September 2011




[1] Department of Water Resources of Shanxi Province, in: Handbook of Hydrologic Calculation in Shanxi Province, Yellow River Conservancy Press (2011). (In Chinese).

[2] Yingming Li and Junfeng Pan, in: Shanxi Rivers, Science Press (2004). (In Chinese).

[3] Jin Hua: The theories and applications study of Double-excess runoff generation model (Doctoral Dissertation, 2006). (In Chinese).

[4] Daojiang Yan and Shouze Ye, in: Engineering Hydrology (The Third Edition), China Waterpower Press (2000). (In Chinese).

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