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Discussion on the Construction of Sediment Retention Works in the Concentrated Coarse Sediment Source Areas of the Yellow River

机译:黄河集中粗沉积源区沉积物施工施工探讨

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The sticking point for the regulation of the Yellow River lies in sediment,where coarse sediment is most critical.Ever since a long time ago,a large quantity of sediment moves to the lower Yellow River due to severe soil loss from the loess plateau,particularly the coarse sediment fraction which silted in the lower course,directly threatening the safety of the people and properties on both banks of the lower Yellow River.Trapping of the sediment to the Yellom River in the loess plateau region of the Yellow River Basin is the most effective solution to the Yellow River sediment problem.There are 454,000 km2areas subject to soil erosion in the loess plateau region of the Yellow River Basin,which mean a very high difficulty in harnessing,and that long-term unremitting efforts are needed.In order to make the limited investments give play to the effect of sedimentation reduction as early as possible,the coarse sediment that make the biggest contribution to the sedimentation of the lower Yellow River must be controlled.Years of research shows that the 18,800 km2 concentrated coarse sediment source areas of the middle Yellow River are the key to stopping the coarse sediment from flowing into the Yellow River.Construction of sediment retention works in these areas can play an enormous role in balancing runoff-sediment relationship,containing the uninterrupted development of course shrinking and "secondary suspended river",reducing the sedimentation of the lower course,and extending the service life of the large reservoirs for sediment retention.This paper analyzes the influence of the coarse sediment on the rise of the lower riverbed,discusses the construction measures,layout and scale of the sediment retention works,predicts the effect of construction of the sediment retention works in the concentrated coarse sediment source areas,and addresses the safety issues to which attention must be given in the engineering construction.
机译:黄河调节的粘附点位于沉积物中,其中粗沉积物是最重要的。然而,由于长时间以前,由于黄土高原的严重土壤损失,因此大量的沉积物移动到下黄河上,特别是在较低的过程中淤积的粗沉积物分数,直接威胁到较低黄河两岸的人民和物业的安全。对黄河流域黄土高原地区的耶利姆地区的沉积物是最多的黄河沉积物问题的有效解决方案。黄河流域黄土高原地区的土壤侵蚀受到454,000公里,这意味着在利用非常高的难度,并且需要长期的不懈努力。在使有限的投资尽可能早就发挥沉积物减少的影响,这是对较低叶片沉降产生最大贡献的粗糙沉积物必须控制低河。研究中的18,800平方公里集中粗沉积物源区是阻止粗泥土流入黄河的关键。这些地区的沉积物保留工程的建设可以发挥作用巨大作用在平衡径流沉积关系中,含有不间断的发展课程萎缩和“二次悬浮河”,减少了下程的沉降,并延长了大型水库的使用寿命,沉积物保留了沉积物。这篇论文分析了影响下河床升高的粗糙沉积物讨论了沉积物保留工程的施工措施,布局和规模,预测了沉积物保留工作的效果在集中的粗沉积源区域,解决了安全问题必须注意工程建设。

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