黄土丘陵区小流域尺度生态建设的水文响应研究

Study on hydrological response of eco-construction in a small watershed of Loess Hilly region

  • 摘要: 对黄土丘陵区小流域尺度生态建设的水文响应研究结果表明,土壤水分在坡面上由坡顶向坡脚逐渐富集,泉水流量随土壤水分增加而稳定增加,产流降雨过后泉水流量有较大增加,这种响应约滞后3~10d。高标准生态建设治理后其小流域降雨-土壤水-径流转化并无较大变化,流域产流水平正常,表明水资源对流域治理后生态环境具有持续支持能力。

     

    Abstract: The hydrological response of eco-construction in a small watershed of Loess Hilly region was studied.The results show that the soil moisture increases along the down slope direction,and the spring flow increases with the soil water content increase.When runoff happens, the spring flow may increase 3~10 days afterwards.Eco-construction is caused the decrease in runoff modules in density rainfall fairs,but fully absorbs the rainfall in a long duration with low intensity rainfall fair,showing the eco-construction can be water bearing sustainability in the test region.

     

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