Article ID Journal Published Year Pages File Type
4526438 Advances in Water Resources 2009 4 Pages PDF
Abstract

The solution of second order elliptic partial differential equations typically arising for flow problems, e.g., in porous media, is frequently expressed as face fluxes of a flow field at hexahedral cells. In this letter, we show by example that the following properties are incompatible: (1) A local velocity reconstruction, (2) reproduction of uniform flow for general hexahedral cells, and (3) a flow field in H(div). This is in particular relevant to mixed finite element methods approximating H(div), and to other methods trying to reconstruct a flow field in a hexahedron using only local face fluxes, e.g., streamline tracing methods for reservoir simulation.

Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
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