首页> 外文会议>Proceedings of the Ninth International Symposium on River Sedimentation vol.4 >DISCUSSION ON THE DYNAMIC EQUILIBRIUM OF THE DELTA COASTLINE IN THE YELLOW RIVER ESTUARY
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DISCUSSION ON THE DYNAMIC EQUILIBRIUM OF THE DELTA COASTLINE IN THE YELLOW RIVER ESTUARY

机译:黄河口三角洲海岸线动态平衡问题的探讨

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Deposition in the reach within a certain extent downstream of the Yellow River is directly related to the condition that whether the delta coastline of the Yellow River estuary is in dynamic equilibrium. The concept of the dynamic equilibrium in delta coastline of the Yellow River estuary is discussed in the paper, and the incoming sediment amount when the delta coastline of the Yellow River is in dynamic equilibrium is analyzed by the comparison method of transporting sediment outside sea and the related method of incoming sediment to land formation area according to the related observed data. The conclusion shows that the delta coastline of the Yellow River estuary may be in dynamic equilibrium when the annual-averaged incoming sediment amount at Lijin station is about 3.45 x 10~9 t.
机译:黄河下游一定范围内河段的沉积与黄河河口三角洲海岸线是否处于动态平衡状态直接相关。本文讨论了黄河口三角洲海岸线动态平衡的概念,并通过输沙与输沙的比较方法分析了黄河三角洲海岸线动态平衡时的入沙量。根据相关观测资料将沉积物运入土地形成区的相关方法。结论表明,当利津站年平均输入泥沙量约为3.45 x 10〜9 t时,黄河口三角洲海岸线可能处于动态平衡状态。

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