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A numerical method for solving anisotropic elliptic boundary value problems on irregular domains in two and three dimensions

Posted on:2002-09-25Degree:Ph.DType:Dissertation
University:The University of UtahCandidate:Dumett, Miguel AngelFull Text:PDF
GTID:1460390011992945Subject:Mathematics
Abstract/Summary:
We present a new second-order stable Cartesian grid algorithm for solving anisotropic elliptic boundary value problems on bounded irregular domains in two dimensions (2D) and three dimensions (3D). The irregular domain is embedded in a uniform Cartesian mesh, but grid points outside of the domain are not used. Second-order local truncation error and the sufficient Gerschgorin criterion for stability impose some conditions to be satisfied by the weights of the discretization scheme at a particular interior grid point. We show that for interior grid points far away from the irregular boundary, these conditions need not always hold. A necessary and sufficient condition, in terms of the anisotropy matrix, for the existence of a Gerschgorin second-order scheme at a given interior grid point is found. This theorem is proved in 2D and 3D. The governing partial differential equations are discretized through a new technique which uses a linear programming approach to find the scheme at points far away from the irregular boundary. Near the irregular boundary, with the addition of boundary information, special discretizations are found by using an optimization approach. As an example, we solve isotropic and anisotropic Laplace equation with Neumann boundary conditions on an annulus in 2D. In addition, we solve isotropic and anisotropic Laplace equation with Neumann boundary conditions on a sphere with a centered hole in 3D. Anisotropy is introduced through a parameter. Several plots and tables show second-order accuracy and stability of the discretization matrix in isotropic Laplacian cases. The influence of anisotropy parameter values in accuracy and stability is also shown.
Keywords/Search Tags:Boundary, Irregular, Isotropic, Grid, Second-order
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