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Effect of Human Activities on Overall Trend of Sedimentation in the Lower Yellow River, China

机译:人类活动对黄河下游沉积物总体趋势的影响

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摘要

The Yellow River has been intensively affected by human activities, particularly in the past 50 years, including soil-water conservation in the upper and middle drainage basin, flood protection in the lower reaches, and flow regulation and water diversion in the whole drainage basin. All these changes may impact sedimentation process of the lower Yellow River in different ways. Assessing these impacts comprehensively is important for more effective environmental management of the drainage basin. Based on the data of annual river flow, sediment load, and channel sedimentation in the lower Yellow River between 1950 and 1997, the purpose of this paper is to analyze the overall trend of channel sedimentation rate at a time scale of 50 years, and its formative cause. It was found in this study that erosion control measures and water diversion have counteractive impacts on sedimentation rate in the lower Yellow River. Although both annual river flow and sediment decreased, there was no change in channel sedimentation rate. A regression analysis indicated that the sedimentation in the lower Yellow River decreased with the sediment input to the lower Yellow River but increased with the river flow input, In the past 30-40 years, the basin-wide practice of erosion and sediment control measures resulted in a decline in sediment supply to the Yellow River; at the same time, the human development of water resources that required river flow regulation and water diversion caused great reduction in river flow. The former may reduce the sedimentation in the lower Yellow River, but the reduction of river flow increased the sedimentation. When their effects counterbalanced each other, the overall trend of channel sedimentation in the lower Yellow River remained unchanged. This fact may help us to better understand the positive and negative effects of human activities in the Yellow River basin and to pay more attention to the negative effect of the development of water resources. The results of this study demonstrate that, if the overuse of river water cannot be controlled, the reduction of channel sedimentation in the lower Yellow River cannot be realized through the practice of erosion and sediment control measures.
机译:黄河受到人类活动的严重影响,特别是在过去的50年中,包括上,中流域的水土保持,下游的防洪以及整个流域的流量调节和引水。所有这些变化可能以不同的方式影响黄河下游的沉积过程。全面评估这些影响对于更有效地管理流域至关重要。本文基于1950年至1997年黄河下游的年河流量,泥沙负荷和河道淤积数据,分析了50年时间尺度上河道淤积率的总体趋势及其变化趋势。形成原因。在这项研究中发现,侵蚀控制措施和引水对黄河下游的沉积速率有反作用。尽管年度河流流量和沉积物均减少,但河道沉积率没有变化。回归分析表明,黄河下游的泥沙量随黄河下游的泥沙输入量而减少,但随河水输入量的增加而增加。在过去的30-40年中,全流域的侵蚀和泥沙控制措施​​得到了实践。黄河的泥沙供应减少;同时,需要调水调水的人类水资源开发大大减少了河流量。前者可以减少黄河下游的沉积,但是河流流量的减少增加了沉积。当它们的影响相互抵消时,黄河下游河道沉积的总体趋势保持不变。这一事实可能有助于我们更好地了解黄河流域人类活动的积极和消极影响,并更多地关注水资源开发的消极影响。研究结果表明,如果不能控制河水的过度使用,则黄河下游河道沉积物的减少不能通过侵蚀和泥沙控制措施​​来实现。

著录项

  • 来源
    《Environmental Management》 |2004年第5期|p.637-653|共17页
  • 作者

    XU JIONGXIN;

  • 作者单位

    Institute of Geographical Sciences and Natural Resources Research;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 环境保护管理;
  • 关键词

  • 入库时间 2022-08-17 13:34:05

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