Analysis of the finite element method for transmission/mixed boundary value problems on general polygonal domains
Electronic transactions on numerical analysis, Tome 37 (2010), pp. 41-69.

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Summary: We study theoretical and practical issues arising in the implementation of the Finite Element Method for a strongly elliptic second order equation with jump discontinuities in its coefficients on a polygonal domain $\Omega $that may have cracks or vertices that touch the boundary. We consider in particular the equation - $div(A\nabla u) = f \in $Hm - $1(\Omega )$ with mixed boundary conditions, where the matrix A has variable, piecewise smooth coefficients. We establish regularity and Fredholm results and, under some additional conditions, we also establish well-posedness in weighted Sobolev spaces. When Neumann boundary conditions are imposed on adjacent sides of the polygonal domain, we obtain the decomposition $u = ureg + \sigma $, into a function ureg with better decay at the vertices and a function $\sigma $that is locally constant near the vertices, thus proving well-posedness in an augmented space. The theoretical analysis yields interpolation estimates that are then used to construct improved graded meshes recovering the (quasi-)optimal rate of convergence for piecewise polynomials of degree m $\geq 1$. Several numerical tests are included.
Classification : 65N30, 35J25, 46E35, 65N12
Keywords: Neumann-Neumann vertex, transmission problem, augmented weighted Sobolev space, finite element method, graded mesh, optimal rate of convergence
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     title = {Analysis of the finite element method for transmission/mixed boundary value problems on general polygonal domains},
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     volume = {37},
     year = {2010},
     language = {en},
     url = {http://geodesic.mathdoc.fr/item/ETNA_2010__37__a23/}
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Li, Hengguang; Mazzucato, Anna; Nistor, Victor. Analysis of the finite element method for transmission/mixed boundary value problems on general polygonal domains. Electronic transactions on numerical analysis, Tome 37 (2010), pp. 41-69. http://geodesic.mathdoc.fr/item/ETNA_2010__37__a23/