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    黄河中游龙潼区间水沙变化特征及其对降水和人类活动的响应

    Variation Character of Water and Sediment and Its Response to Rainfall and Human Activities in Longtong Region of the Middle Yellow River

    • 摘要: 为实现黄河中游水土保持效益评价和生态环境政策调整,以1957~2019年龙潼区间降水、径流、输沙和遥感数据为基础,运用累积距平法和双累积曲线等方法,分析了降水和植被指数变化与水沙之间的关系.结果表明:龙潼区间降水量随时间变化呈不明显减小趋势,而径流量和输沙量随时间变化却呈显著减小趋势.径流在1985年发生了由丰到枯的突变,输沙在1985年和2002年发生了由丰到枯的突变.归一化植被指数(NDVI)呈现恢复态势,年均NDVI指数上升1.7%,空间上NDVI指数呈波动增加趋势,区间流域的南部地区植被覆盖度最佳.与基准期A(1957~1985年)相比,B时期(1986~2019年)降水对径流的贡献率为26.21%,而人类活动对径流的贡献率为73.79%.与基准期A(1957~1985年)相比,B时期(1986~2019年)和C时期(2003~2019年)降水对输沙的贡献分别为22.80%和11.73%,而人类活动对输沙的贡献率为分别为77.20%和88.27%.

       

      Abstract: To evaluate the benefits of soil and water conservation and adjust ecological and environmental policies in the middle reaches of the Yellow River,the relationships between precipitation and changes in vegetation index,and water and sediment flows were analyzed using precipitation,runoff,sediment transport and remote sensing data in the Longtong region from 1957 to 2019.The cumulative anomaly method and double cumulative curve were used to analyze the relationship between precipitation and changes in vegetation index,and water and sediment flows.The results showed that precipitation in the Longtong region did not exhibit an apparent decline with time,but runoff and sediment transport exhibited a significant decline with time.The abrupt change to runoff,from abundant to dry,occurred in 1985,and the abrupt change to sediment transport,from abundant to dry,occurred in 1985 and 2002.The normalized vegetation index (NDVI) exhibited a recovery,with an annual increase of 1.7%,and the spatial NDVI exhibited fluctuations in a generally increasing value.Vegetation cover in the southern part of the basin was the best.Compared with the reference period A(1957~1985),the contribution of precipitation to runoff in period B(1986-2019) was 26.21%,while the contribution of anthropogenic to runoff was 73.79%.Compared with the reference period A(1957~1985),the contribution of precipitation in periods B(1986~2019) and C(2003~2019) to sediment transport was 22.80% and 11.73%,respectively,while the contribution of anthropogenic sediment transport were 77.20% and 88.27%,respectively.

       

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