Abstract
This chapter deals with the finite element solutions for saturated porous media (groundwater). Groundwater modeling is concerned with the motion of subsurface water in aquifers and aquifer systems, which can be unconfined or confined. Solutions are required for fully 3D, vertical or essentially horizontal 2D and axisymmetric isothermal flow of homogeneous flow in saturated porous media with and without free surface(s), including fully anisotropic flow situations and the incorporation of multi-layer well condition.
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