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Modeling sediment concentration and transport induced by storm surge in Hengmen Eastern Access Channel

机译:横门东部通道内风暴潮引起的泥沙浓度和输沙模拟

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Sediment is an important factor for excavation, dredging and maintenance of Hengmen Eastern Access Channel in Pearl River Estuary. As storm surge is considered as an important role in determining sediment re-suspension and transport, as well as creating landforms in the areas of estuary and coast, along with the storm surge disaster damage in Pearl River Estuary is one of the most serious events in China, reasonable simulation of storm-induced sediment concentration, transport and channel siltation in Hengmen Eastern Access Channel is of much significance. Based on the feasibility condition of less research on numerical simulation of storm-induced sediment concentration and transport, especially channel siltation in the Pearl River Estuary, using a curvilinear grid, a nested and coupled model which combines typhoon model, hydrodynamic model (Delft3D-FLOW), wave model (Delft3D-WAVE) and sediment transport model (Delft3D-SED) was set up for the region of Pearl River Estuary. After a series of model verifications, which showed that this coupled model performed well to reflect the characteristics of the typhoon field, tidal currents, wave height, storm surge, distribution of suspended sediment in the studied region, the model was applied to study the storm-induced sediment concentration and transport in Hengmen Eastern Access Channel. Through simulation of one extra tropical storm surge process with this coupled numerical model, the storm-induced sediment concentration and transport in Hengmen Eastern Access Channel were studied, and the storm-induced erosion and deposition were further discussed. Results showed that the effect of storm surge on sediment concentration, transport and siltation was significant. Under the influence of storm surge, the velocity and bed stress around Hengmen Eastern Access Channel increased significantly, which led the re-suspension and transport of sediment, and thus, the higher sediment concentration and more channel siltation occurred. By running this coupled model, the simulated results can be employed in the optimum decision making of Hengmen Eastern Access Channel Regulation Project.
机译:泥沙是珠江口横门东通道的开挖,疏and和维护的重要因素。由于风暴潮被认为是决定泥沙重新悬浮和运输以及在河口和海岸地区形成地貌的重要作用,而风暴潮在珠江口造成的破坏是该州最严重的事件之一。在中国,合理模拟横门东部通道内风暴引起的泥沙浓度,输沙和河道淤积具有重要意义。基于较少的可行性条件,利用曲线网格,结合台风模型,水动力模型(Delft3D-FLOW)的嵌套耦合模型,对风暴诱发的沉积物浓度和输运,尤其是珠江口河道淤积的数值模拟进行了研究。 ),建立了珠江口区域的波浪模型(Delft3D-WAVE)和泥沙迁移模型(Delft3D-SED)。经过一系列的模型验证,结果表明该耦合模型能够很好地反映台风场的特征,潮汐流,波高,风暴潮,研究区域内悬浮泥沙的分布,该模型被用于研究风暴引起的横门东通道的沉积物浓度和运移。通过这种耦合数值模型模拟了一个额外的热带风暴潮过程,研究了横门东部通道内风暴引起的沉积物浓度和运移,并进一步讨论了风暴引起的侵蚀和沉积。结果表明,风暴潮对沉积物浓度,运移和淤积的影响是显着的。在风暴潮的影响下,横门东部通道周围的速度和床应力显着增加,导致了沉积物的重新悬浮和运移,从而导致了较高的沉积物浓度和更多的通道淤积。通过运行该耦合模型,可以将模拟结果用于横门市东部通道调整项目的最佳决策。

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