首页> 外文会议>International Conference on Hydroinformatics 2004(HIC2004) vol.1; 20040621-24; Singapore(SG) >A NEW TOPOGRAPHY ADAPTED MESH REFINEMENT FOR 2D UNSTEADY SHALLOW WATER FLOW SIMULATIONS OVER DRY BEDS
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A NEW TOPOGRAPHY ADAPTED MESH REFINEMENT FOR 2D UNSTEADY SHALLOW WATER FLOW SIMULATIONS OVER DRY BEDS

机译:干床上二维二维非稳态浅水流动模拟的新地形学自适应网格细化

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摘要

In two dimensional hydraulic free surface problems, when a mesh is required to be representative of some topography, as the number of cells used to create the mesh increases, the discrete representation of the real problem improves, so the accuracy of the results is enhanced, but the computing time grows and this can be a cumbersome difficulty. On the other hand, the experience says that, when the topography is smooth, larger cells can be used to simulate a flooding event but, if the topography is highly irregular, the number of cells must be increased in order to allow for a correct flow representation. One solution is to generate a mesh with local refinement, in order to reduce the calculation effort and, at the same time, be able to achieve the accuracy in the flow simulation results that a globally fine mesh would provide. When cuadrilateral structured meshes are used, the refinement must be done in all cells contained in the rows and columns connected with the area whose cell-density we want to increase. Unstructured triangular meshes with local mesh refinement can lead to directional cell deformation depending on how they are created, and the grid refinement procedure is more complicated. The solution proposed here consists of using a structured triangular mesh of variable density following the variation of the bed slope. This produces a grid where the local refinement is introduced in the irregular topography zones, with a refinement depending on how irregular the topography is. Furthermore, the new cells are generated following a simple algorithm, without distortions and not affecting the size of the cells in the same row or column far from the area of interest. The performance and efficiency of a finite volume upwind method on different grids will be presented and compared for a river flow simulation problem over dry bed.
机译:在二维水力自由表面问题中,当要求网格代表某些地形时,随着用于创建网格的像元数量的增加,真实问题的离散表示会改善,因此结果的准确性得到了提高,但是计算时间会增加,这可能会很麻烦。另一方面,经验表明,当地形平滑时,可以使用较大的单元来模拟洪水事件,但是,如果地形高度不规则,则必须增加单元的数量以允许正确的流动表示。一种解决方案是生成具有局部细化的网格,以减少计算工作量,同时能够获得全局精细网格将提供的流动模拟结果的准确性。当使用立方形结构网格时,必须在与要增加其单元密度的区域连接的行和列中包含的所有单元中进行细化。具有局部网格细化功能的非结构三角网格可能会导致定向单元变形,具体取决于它们的创建方式,并且网格细化过程更加复杂。这里提出的解决方案包括使用随床斜率变化而变化的密度可变的结构化三角形网格。这将产生一个网格,在该网格中将局部细化引入到不规则形貌的区域中,细化取决于形貌的不规则性。此外,按照简单的算法生成新的单元格,而不会产生失真,并且不会影响远离感兴趣区域的同一行或同一列中单元格的大小。将介绍在不同网格上有限体积迎风方法的性能和效率,并将其与干床上的河水模拟问题进行比较。

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