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Variations in Basin Sediment Yield and Channel Sediment Transport in the Upper Yangtze River and Influencing Factors

机译:长江上游流域产沙量和河道输沙量变化及其影响因素

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To study the impact of human activity on river basin sediment erosion and sediment transport in the upper Yangtze River, variations in the sediment delivery modulus and the incoming sediment coefficient during the period from 1956 to 2015 were investigated with a cumulative curve method and the Mann-Kendall test. Then, the contribution of human activity on sediment load reductions was calculated quantitatively with a hydrologic method. The results showed that the values of the sediment delivery modulus and the incoming sediment coefficient decreased with time, which indicated a decrease in basin sediment yield and an increase in sediment deficit in recent decades. Moreover, human activities such as reservoir construction, soil conservation, and sand excavation were the main reasons for sediment load reductions, whereas there were no significant trend changes in rainfall, which had a minimal effect on the sediment yield changes in the upper Yangtze River. Of the total reductions in sediment load, sediment trapped by reservoirs contributed close to 88%, whereas soil conservation and other factors only contributed 12%.
机译:为了研究人类活动对长江上游流域泥沙侵蚀和泥沙输送的影响,采用累积曲线法和Mann-方法研究了1956年至2015年期间的泥沙输送模量和输入泥沙系数的变化。肯德尔测试。然后,利用水文方法定量计算了人类活动对减少泥沙负荷的贡献。结果表明,近几十年来,输沙模量和输沙系数随时间减小,表明流域产沙量减少,赤字增加。此外,人类活动如水库建设,水土保持和开挖沙土是减少泥沙量的主要原因,而降雨没有明显的趋势变化,对长江上游的泥沙产量变化影响最小。在减少的沉积物总量中,水库捕获的沉积物占近88%,而土壤保持和其他因素仅占12%。

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