RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN >> 2016, Vol. 25 >> Issue (12): 1879-1885.doi: 10.11870/cjlyzyyhj201612011

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OUTPUT CHARACTERISTICS OF SURFACE RUNOFF IN TYPICAL KARST WATERSHED

TU Cheng-long1, LU Xiao-hui2, LIU Rui-lu3, LI Yong3, LI Rui3, SUN Quan-zhong3, LI Long-bo4   

  1. 1. State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China;
    2. Guizhou Normal University, Guiyang 550081, China;
    3. Soil and Water Conservation Station of Guizhou Province, Guiyang 550081, China;
    4. Guiyang Engineering corporation. China Power. Guiyang 550081, China
  • Received:2016-06-03 Revised:2016-09-12 Online:2016-12-20
  • Supported by:
    Ministry of Water Resources of the People's Republic of China(201401050);National Key Scientific Research Program(2013CB956702);National Natural Science Foundation of China(41261058);Qian Ke He J([2013]2298)

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Abstract: Modeling on runoff dynamics in Karst region of Southwest of China is nearly impossible due to high heterogeneity of carbonate structure and composition, and the shortage of observed data in site. It is helpful to know the different water processes through observing and analyzing the variation of flow output in a small watershed exit. Based on the background, this research has analyzed flow output in a whole calendar year. The results indicated that the flow output emerged only from May to October. With the influences of rainfall intensity and conversion process of interflow to surface runoff, the flow output broken out after several hours of rain, then faded out slowly in May. But the flow output gathered strength with rain in June to October and the lag-effect was shorter than in May. With exception of May, the relationship between rainfall and flow output amount was significant from June to October. There were seasonal variationsin conversion of interflow to surface flow, which determined the flow duration in exit of watershed. The amount of flow output accounted for approximately 23.1% of annual rainfall.

Key words: karst, watershed, surface runoff, output

CLC Number: 

  • TV121
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