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Mathematical development and verification of a non-orthogonal finite volume model for groundwater flow applications

机译:用于地下水流动的非正交有限体积模型的数学开发和验证

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摘要

The mathematical development of a two-dimensional finite volume model for groundwater flow is described. Based on the hydraulic equations for saturated flow, the model deploys an improved least squares gradient reconstruction technique to evaluate the gradient at the control volume face, derived from the application of the finite volume formulation and using a cell-centred structured quadrilateral grid. The model has been compared to a finite difference model with orthogonal grids. The effects of grid non-orthogonality and skewness are investigated. The model was verified by comparison with analytical solutions and the results for a finite difference model. The finite volume model was then applied successfully to an aquifer discharging in a section of the River Tawe, UK, and the results were compared with results from MODFLOW and observed hydraulic heads. Results of the numerical model tests and field exercise showed that the use of finite volume method provides modellers with a consistent substitute for the finite difference methods with the same ease of use and an improved flexibility and accuracy in simulating irregular boundary geometries.
机译:描述了地下水流动的二维有限体积模型的数学发展。基于饱和流的水力方程,该模型采用了一种改进的最小二乘梯度重建技术来评估控制体积面上的梯度,该技术源自有限体积公式的应用并使用以单元为中心的结构四边形网格。该模型已与具有正交网格的有限差分模型进行了比较。研究了网格非正交和偏斜的影响。通过与解析解以及有限差分模型的结果进行比较来验证该模型。然后将有限体积模型成功地应用于英国Tawe河段的含水层流量,并将结果与​​MODFLOW和观察到的水头的结果进行了比较。数值模型测试和现场练习的结果表明,有限体积方法的使用为建模人员提供了一致的替代方法,同时具有易用性,并且在模拟不规则边界几何时具有更高的灵活性和准确性。

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