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Effect of Comprehensive Management on Runoff and Sediment Reduction in Yanwachuan Watershed, Loess Tableland, China

机译:黄土高原烟洼川流域综合治理对减少径流和泥沙的影响

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To evaluate the effect of comprehensive management on runoff and sediment reduction in meso-scalewatersheds, the Yanwachuan watershed of Loess tableland gully region in China was investigated. Variationtrends of the runoff and sediment from 1981 to 2009 were analysed, and the year of abrupt changewas identified using the double mass curve method, accumulative departure method, moving t-testmethod and Yamamoto method. Next, the effects of comprehensive management on runoff andsediment reductions were quantitatively evaluated based on the runoff/sediment coefficient methodand double mass curve method, both capable of separating the effect of climate change from that ofcomprehensive management. Finally, the driving forces of runoff and sediment variations werediscussed from both climatic and comprehensive management aspects. The results showed that therunoff and sediment in the watershed had significantly decreased since an abrupt change in 1997.During the change period (1998-2009), the erosive precipitation and precipitation erosivity had beenreduced by 32.4% and 17.4%, respectively, compared with the base period (1981-1997); the areas offorest and grass had increased; and the normalized difference vegetation index (NDVI) had increasedby 20.6% with significantly enlarged vegetation coverage. The benefit value of runoff reduction andsediment reduction were 27.3% and 76.2%, respectively. The resultant runoff and sediment reductionsin the watershed were the synergy of climate change and comprehensive management, with greaterthan 90% reduction contributed by comprehensive management. All these results supported thatcomprehensive management played the dominant role in runoff and sediment reductions..
机译:为了评价中尺度流域综合管理对径流减少和泥沙减少的影响,研究了黄土高原沟壑区盐洼川流域。分析了1981〜2009年径流和泥沙变化趋势,并采用双质量曲线法,累积偏离法,移动t检验法和山本法确定了突变年。接下来,基于径流/泥沙系数法和双重质量曲线法,定量评估了综合管理对径流和泥沙减少的影响,这两种方法都能够将气候变化的影响与综合管理的影响区分开。最后,从气候和综合管理两个方面探讨了径流和泥沙变化的驱动力。结果表明,自1997年突变以来,流域的径流和沉积物显着减少。在变化时期(1998-2009年),侵蚀性降水和降水侵蚀力分别比侵蚀性降低32.4%和17.4%。基期(1981-1997);森林和草地面积增加;归一化植被指数(NDVI)增加了20.6%,植被覆盖率显着增加。径流减少和泥沙减少的收益分别为27.3%和76.2%。流域的径流和沉积物减少是气候变化和综合管理的协同作用,综合管理贡献了90%以上的减少。所有这些结果都表明,综合管理在径流和泥沙减少中起着主导作用。

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