Publication
Numerical analysis of the Navier-Stokes/Darcy coupling
Résumé
We consider a differential system based on the coupling of the Navier-Stokes and Darcy equations for modeling the interaction between surface and porous media flows. We formulate the problem as an interface equation, we analyze the associated (nonlinear) Steklov-Poincare' operators, and we prove its wellposedness. We propose and analyze iterative methods to solve a conforming finite element approximation of the coupled problem.
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Proximité ontologique
Concepts associés (26)
Loi de Darcy
La loi de Darcy est une loi physique qui exprime le débit d'un fluide incompressible filtrant au travers d'un milieu poreux. La circulation de ce fluide entre deux points est déterminée par la conductivité hydraulique ou le coefficient de perméabilité du substrat et par le gradient de pression du fluide. Dans le cas d'un cours d'eau ou d'un réservoir alimentant une nappe, ce gradient est lié à la hauteur de l'eau. Cette loi a été établie en 1856 par Henry Darcy, après qu'il eut réalisé diverses expérimentations visant à déterminer les lois régissant .
Numerical methods for partial differential equations
Numerical methods for partial differential equations is the branch of numerical analysis that studies the numerical solution of partial differential equations (PDEs). In principle, specialized methods for hyperbolic, parabolic or elliptic partial differential equations exist. Finite difference method In this method, functions are represented by their values at certain grid points and derivatives are approximated through differences in these values.
Porous medium
In materials science, a porous medium or a porous material is a material containing pores (voids). The skeletal portion of the material is often called the "matrix" or "frame". The pores are typically filled with a fluid (liquid or gas). The skeletal material is usually a solid, but structures like foams are often also usefully analyzed using concept of porous media. A porous medium is most often characterised by its porosity. Other properties of the medium (e.g.
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