NANASep 11, 2007

Residual Velocities in Steady Free Boundary Value Problems of Vector Laplacian Type

arXiv:0709.1734131 citationsh-index: 45
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Provides a theoretical framework and numerical method for solving steady free boundary problems, relevant to researchers in PDEs and computational fluid dynamics.

The paper develops a technique for analyzing linear well-posedness of a class of vector elliptic free boundary problems with a steady interface, focusing on '2+2' models with vector Laplacian. It then proposes an iterative method using non-physical residual velocities for superior numerical properties, demonstrated on a two-phase flow model.

This paper describes a technique to determine the linear well-posedness of a general class of vector elliptic problems that include a steady interface, to be determined as part of the problem, that separates two subdomains. The interface satisfies mixed Dirichlet and Neumann conditions. We consider ``2+2'' models, meaning two independent variables respectively on each subdomain. The governing equations are taken to be vector Laplacian, to be able to make analytic progress. The interface conditions can be classified into four large categories, and we concentrate on the one with most physical interest. The well-posedness criteria in this case are particularly clear. In many physical cases, the movement of the interface in time-dependent situations can be reduced to a normal motion proportional to the residual in one of the steady state interface conditions (the elliptic interior problems and the other interface conditions are satisfied at each time). If only the steady state is of interest, one can consider using other residuals for the normal velocity. Our analysis can be extended to give insight into choosing residual velocities that have superior numerical properties. Hence, in the second part, we discuss an iterative method to solve free boundary problems. The advantages of the correctly chosen, non-physical residual velocities are demonstrated in a numerical example, based on a simplified model of two-phase flow with phase change in porous media.

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