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Numerical analysis of the influence of sea level rise on sediment deposition in the Yangtze Estuary channels

机译:海平面上升对长江河口沉积物沉积沉积物影响的数值分析

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To explore the influence of sea level rise on sediment deposition in the Yangtze Estuary Deep-water Navigation Channel, this article has simulated the change of flow velocity in North Passage in different situations of sea level rise with MIKE21 FM and calculated the threshold motion velocity of sediment in North Passage. The results show that as sea level rise, flooding and precipitating velocities in upside North Passage increase and in middle North Passage decrease. Precipitating velocities in middle North Passage are greater than threshold motion velocities of sediment and sediment is scoured easily. When precipitating the middle of North Passage is in the washed state and it is beneficial to the construction and maintenance of the Deep-water Navigation Channel in North Passage.
机译:为了探讨海平面上升对长江河口深水导航渠道沉积物沉积的影响,本文已经模拟了北方通道中的流速变化与Mike21 FM的不同情况下,并计算了阈值运动速度北段沉积物。结果表明,随着海平面上升,洪水和膨胀速度越来越多的北极速度,中北通道减少。中北通道中的沉淀速度大于沉积物的阈值运动速度和沉积物很容易擦洗。在促使北段的中间处于水中的状态下,它有利于北段深水导航渠道的构建和维护。

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