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Tidal current and sediment numerical modeling of flow cutoff in the South Branch of the Oujiang Estuary

机译:瓯江河口南部流动截止潮流和沉积物数值模型

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A numerical model of tidal current and sediment movement under the combined action of wave and current are set up with irregular triangular grid. The model is verified with in situ data, and the results show that the calculated water elevations at 19 stations, currents, suspended sediment at 19 vertical lines and seabed evolution are all in good agreement with measured data. This numerical model is applied in the tidal current and sediment movement simulations in stopping flow transport through the South Branch of the Oujiang Estuary and the feasibility to cut off the flow in the South Branch of the Oujiang Estuary is demonstrated by numerical simulation experiments. The results show that flow cutoff in the South Branch by heightening the present submerged dyke is technically feasible as far as its impact on hydrodynamic sediment environment is concerned.
机译:利用不规则三角网,建立了波和电流组合作用下潮流和泥沙运动的数值模型。该模型以原位数据验证,结果表明,19个站,电流,19个垂直线和海底演进的计算的水升高都与测量数据一致。这种数值模型应用于潮流和沉积物运动模拟,通过瓯江河口的南部分支停止流动运输,并通过数值模拟实验证明了瓯江河口南部南部流动的可行性。结果表明,由于其对流体动力学沉积物环境的影响,南部分支中的流动截止在技术上是可行的。

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