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An upwind finite volume method on non-orthogonal quadrilateral meshes for the convection diffusion equation in porous media

机译:多孔介质对流扩散方程的非正交四边形网格上的Unumnond有限体积方法

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摘要

The aim of this work is to solve the two-dimensional convection diffusion equation on non-rectangular grids formed only by quadrilaterals honoring the internal structures of a reservoir (preferential flow channels, faults, areas of high permeability contrast, changes in sediment type, etc.), taking into account different physical configurations of the porous medium. To take advantage of the good representation of the domain through these meshes, the finite volume method was used, which is conservative and facilitates the treatment of the boundary conditions. In this method, the convection diffusion equation is integrated on each quadrilateral (control volume) of the mesh, thus obtaining the integral form of the equation. The velocity value in the face of each quadrilateral is determined according to the direction of the flow (upwind scheme). After approximating the integrals involved and taking into account the boundary conditions, a discrete equation in each control volume showed up. Finally, a large sparse linear system is obtained, generally non-symmetric and ill-conditioned, which can be solved by iterative methods such as GMRES with incomplete LU preconditioning. Different scenarios were considered varying boundary conditions (Dirichlet and Neumann type), source term, and diffusion constant fluid velocity. The results are consistent with the physical interpretation of each configuration.
机译:这项工作的目的是解决仅由四边形形成的非矩形网格上的二维对流扩散方程,识别储层的内部结构(优惠流动通道,故障,高渗透率对比,沉积物变化,等等的变化等。),考虑到多孔介质的不同物理配置。为了利用这些网格来利用域的良好表示,使用了有限体积法,这是保守的,并有助于治疗边界条件。在该方法中,对流扩散方程集成在网格的每个四边形(控制体积)上,从而获得了等式的整体形式。根据流动(上冲程方案)的方向确定每个四边形的面部的速度值。在近似涉及的积分并考虑边界条件之后,每个控制卷中的离散式示出。最后,获得了大的稀疏线性系统,通常是非对称的和不良的,其可以通过迭代方法如GMRES具有不完整的LU预处理来解决。不同的情景被认为是不同的边界条件(Dirichlet和Neumann类型),源期限和扩散恒定流体速度。结果与每个配置的物理解释一致。

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