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首页> 外文期刊>Proceedings of the International Conference on Coastal Engineering >NUMERICAL MODELING OF SHORELINE EVOLUTION AROUND THE RIVER MOUTH
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NUMERICAL MODELING OF SHORELINE EVOLUTION AROUND THE RIVER MOUTH

机译:河口绕岸线演变的数值模拟

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The river sediments transport into coastal water together with wave induced longshore sediment transport make shoreline evolution much complicated. Fig.l shows typical feature of shoreline shape around a river mouth. Recently there are some investigators treated this problem (Grijm, 1964, Bakker ?§Edelmen,1964; Komar,1973; Tsuchiya ?§ Yasuda,1978),and had developed some mathematical or numerical models. This paper proposes a numerical model for predicting long-term shoreline evolution around a river mouth by incorporation certain river parameters into the Willis beach evolution model (1978). The proposed model is at first applied to four ideal cases to investigate its general characteristics and adaptability, and reasonable results are found. In our results the accretion on updrift side is faster than downdrift side under the oblique incident wave condition and the width of the river mouth increase steadily. These results are different from other approachs that the shoreline shape is always nearly symmetrical with respect to the centerline of the river mouth. Finally, as an field case application of the model, a numerical simulation of shoneline changes around the Cho-shui River mouth is performed and compared with field data.
机译:河流沉积物向沿海水域的输送以及波浪引起的近岸沉积物的输送使海岸线的演化变得非常复杂。图1显示了河口周围海岸线形状的典型特征。最近,有一些研究者对这个问题进行了处理(Grijm,1964; Bakker?Edelmen,1964; Komar,1973; Tsuchiya?§Yasuda,1978),并开发了一些数学或数值模型。本文提出了一个数值模型,通过将某些河流参数纳入Willis海滩演化模型(1978年)来预测河口周围的长期海岸线演化。首先将提出的模型应用于四个理想情况,研究其一般特性和适应性,并找到合理的结果。在我们的结果中,在倾斜入射波条件下,向上漂移侧的沉积物要快于向下漂移侧的沉积物,并且河口的宽度稳定增加。这些结果不同于其他方法,即海岸线形状始终相对于河口中心线几乎对称。最后,作为该模型的现场案例应用,对卓水河口周围的鱼线变化进行了数值模拟,并与现场数据进行了比较。

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