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Assessing the hydrological effect of the check dams in the Loess Plateau, China, by model simulations

机译:通过模型模拟评估中国黄土高原止水坝的水文效应

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Check dams are commonly used for soil conservation. In the Loess Plateau ofChina, check dams have been widely constructed as the principal means toretain floodwater and intercept soil sediments since the 1970s. Forinstance, there are more than 6572 check dams in the Yanhe watershed withan area of 7725 km2 in the Loess Plateau. However, little research hasbeen done to quantify the hydrological effects of the check dams.In this research, the SWAT model (Soil and Water Assessment Tool) wasapplied to simulate the runoff and sediment in the Yanhe watershed. Wetreated the 1950s to 1960s as the reference period since there were very fewcheck dams during the period. The model was firstly calibrated and validatedin the reference period. The calibrated model was then used in the laterperiods to simulate the hydrological effects of the check dams.The results showed that the check dams had a regulation effect on runoff anda retention effect on sediment. From 1984 to 1987, the runoff in rainyseason (from May to October) decreased by 1.54 m3 s?1 (14.7%) to 3.13m3 s?1 (25.9%) due to the check dams; while in dry season (fromNovember to the following April), runoff increased by 1.46 m3 s?1(60.5%) to 1.95 m3 s?1 (101.2%); the sediment in rainy seasondecreased by 2.49 × 106 ton (34.6%) to 4.35 × 106 ton (48.0%).From 2006 to 2008, the runoff in rainy seasondecreased by 0.79 m3 s?1 (15.5%) to 1.75 m3 s?1 (28.9%), and therunoff in dry season increased by 0.51 m3 s?1 (20.1%) to 0.97 m3 s?1(46.4%); the sediment in rainy season decreased by2.03 × 106 ton (79.4%) to 3.12 × 106 ton(85.5%).Construction of the large number of check dams in the Loess Plateau hasenhanced the region's capacity to control the runoff and sediment. In theYanhe watershed, the annual runoff was reduced by less than 14.3% due tothe check dams; and the sediment in rainy season was blocked by up to85.5%. Thus, check dams are effective measures for soil erosion controlin the Loess Plateau.
机译:止水坝通常用于水土保持。自1970年代以来,在中国的黄土高原,止水坝被广泛地用作挡住洪水和拦截土壤沉积物的主要手段。例如,黄土高原延河流域有超过6572个止水坝,面积达7725 km 2 。但是,关于量化检查坝的水文影响的研究还很少。 在这项研究中,SWAT模型(水土评估工具)用于模拟延河流域的径流和泥沙。我们将1950年代至1960年代作为参考期,因为在此期间止水坝很少。首先在参考期间对模型进行了校准和验证。然后在以后的阶段中使用校准的模型来模拟止水坝的水文影响。 结果表明,止水坝对径流有调节作用,对沉积物有保留作用。从1984年到1987年,雨季(5月至10月)的径流减少了1.54 m 3 s ?1 (14.7%),降至3.13m 3 s ?1 (25.9%)由于止水坝;在干旱季节(从11月到次年4月),径流增加了1.46 m 3 s ?1 (60.5%),达到1.95 m 3 s ?1 (101.2%);雨季泥沙减少2.49×10 6 吨(34.6%)至4.35×10 6 吨(48.0%)。2006年至2008年,雨季径流减少由0.79 m 3 s ?1 (15.5%)增至1.75 m 3 s ?1 (28.9%) ,旱季的径流增加0.51 m 3 s ?1 (20.1%)至0.97 m 3 s ?1 < /sup>(46.4%);雨季泥沙减少了2.03×10 6 吨(79.4%),降至3.12×10 6 吨(85.5%)。 黄土高原上的大量拦河坝增强了该地区控制径流和泥沙的能力。在延河流域,由于拦河坝的作用,年径流量减少了不到14.3%。雨季泥沙淤积达85.5%。因此,检查水坝是控制黄土高原水土流失的有效措施。

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