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Dynamic changes of sediment load in the middle reaches of the Yellow River basin, China and implications for eco-restoration

机译:黄河中游地区泥沙负荷动态变化及其对生态修复的意义

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摘要

Abrupt reduction of the sediment load in the middle reaches of the Yellow River has extracted much attention during the past several decades due to global climate changes and intensive human activities. This paper investigates the spatial and temporal variations of annual sediment load in the section between Hekouzhen and Longmen in the middle reaches of the Yellow River basin from 1962 to 2009 by using annual observations at 21 hydrological gauging stations (4 mainstream and 17 tributaries stations), by making use of Mann-Kendall test and simple linear regression for trend detection, and the sequential cluster analysis method and Student's t test for changing point detection. The results suggest that sediment load from both mainstream and tributaries show significant decreasing trends at confidence level of 0.01. Evident abrupt changing points are detected around 1970s for most stations, but for Toudaoguai station and Fugu station are found in the mid-1980s, which are mainly attributed to the operation of Longyangxia Dam. In addition, abrupt changes in the sediment series at some stations from the tributaries were found around the late 1990s, this situation may be resulted from the "Green for Grain" project launched in 1999. Sediment budget analysis indicates that the 17 tributaries contributes 70.60% sediment load to the whole research area, which suggests that the majority sediment load contribution to He-Long region is from these tributaries. The comparison among three mainstream sections implies that the sediment is mainly from Wubao-Longmen section. And contribution of tributaries in each mainstream section is mainly from Huangfuchuan River, Kuye River, Wuding River and Yan River. The reduction of the sediment load is mainly caused by human activities especially soil and water conservation projects (such as afforestation, terraces, reservoirs and dams). In summary, the results in this study provide a further evidence for a more exact sediment source region and implementing soil and water conservation measures more effectively in the middle reaches of the Yellow River basin, China. (C) 2014 Elsevier B.V. All rights reserved.
机译:在过去的几十年中,由于全球气候变化和人类密集活动,黄河中游泥沙负荷的突然减少引起了很多关注。本文利用21个水文监测站(4个主干站和17个支流站)的年度观测资料,调查了1962年至2009年黄河中游河口镇与龙门之间段年沉积物的时空变化,通过使用Mann-Kendall检验和简单线性回归进行趋势检测,并使用顺序聚类分析方法和Student t检验进行变化点检测。结果表明,当置信度为0.01时,来自主流和支流的泥沙负荷都显示出明显的下降趋势。大多数站都在1970年代左右发现了明显的突变点,但在1980年代中期发现了头岛拐站和府谷站,这主要归因于龙羊峡大坝的运行。此外,在1990年代末期发现了支流某些站点的沉积物系列的突然变化,这种情况可能是由于1999年启动的“绿色换粮”项目所致。沉积物预算分析表明,这17个支流贡献了70.60%整个研究区的泥沙负荷,这表明河隆地区的泥沙负荷主要来自这些支流。通过对三大主流断面的比较,表明沉积物主要来自五宝—龙门断面。支流在每个主干段的贡献主要来自皇甫川河,古野河,武定河和Yan河。泥沙量减少主要是由于人类活动,特别是水土保持项目(如绿化,梯田,水库和水坝)。综上所述,本研究结果为黄河中游地区更精确的泥沙源区和更有效地实施水土保持措施提供了进一步的证据。 (C)2014 Elsevier B.V.保留所有权利。

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