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首页> 外文期刊>Advances in Water Resources >Two-dimensional numerical modeling of dam-break flows over natural terrain using a central explicit scheme
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Two-dimensional numerical modeling of dam-break flows over natural terrain using a central explicit scheme

机译:使用中心显式方案对自然地形上的溃坝水流进行二维数值模拟

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摘要

A two-dimensional (2D) numerical model has been developed to solve shallow water equations for simulation of dam-break flows. The spatial derivatives are discretized using a well-balanced explicit central upwind conservative scheme. The scheme is Riemann solver free and guarantees the positivity of the flow depth over complex topography if the Courant number is kept less than 0.25. The time integration is performed by Euler's scheme. The model is verified against analytical results for water surface elevation and discharge for three benchmark test cases. A good agreement between analytical solutions and computed results is observed. The property of well-balancing in still water over an uneven bottom is also confirmed. The model is then validated by simulating a laboratory experiment in which a dam break flow propagates over a triangular obstacle. The model performance was found to be satisfactory. A dam break laboratory experimental test case on a frictionless horizontal bottom is also simulated for 2D validation of the model, and good agreement between simulation and the experimental data is observed. The suitability of the proposed model for real life applications is demonstrated by simulating the Malpasset dam-break event, which occurred in 1959 in France. The computed arrival time of the flood wave front and the maximum flow depths at various observation points matched well with the measurements on a 1/400 scale physical model. The overall performance indicates that this model can be applied for simulation of dam-break waves in real life cases.
机译:已经开发了二维(2D)数值模型来求解浅水方程,以模拟溃坝流。使用良好平衡的显式中央迎风保守方案离散化空间导数。该方案无Riemann求解器,并且如果Courant数保持小于0.25,则可以确保流深度在复杂地形上为正。时间积分由欧拉方案执行。针对三个基准测试案例,针对水面高程和流量的分析结果验证了该模型。观察到分析解决方案和计算结果之间的良好一致性。还证实了在不平坦的底部上的静止水中的良好平衡特性。然后通过模拟一个实验室实验来验证模型,在该实验中,溃坝流在三角形障碍物上传播。发现模型性能令人满意。还对无摩擦水平底部的溃坝实验室实验测试案例进行了仿真,以进行模型的2D验证,并且观察到仿真与实验数据之间的良好一致性。通过模拟1959年在法国发生的Malpasset溃坝事件,证明了所提出模型在现实生活中的适用性。计算出的洪水波阵面到达时间和各个观测点的最大流量深度与1/400比例物理模型上的测量值非常吻合。总体性能表明,该模型可用于模拟现实生活中的溃坝浪。

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