Tutorials
2D Solvers for Groundwater Modeling
The 2D solvers provided in this toolbox are designed for efficient modeling of groundwater flows in porous media. These solvers leverage the Dupuit-Forchheimer approximation, which simplifies the problem by reducing it to two dimensions, assuming the vertical velocity component is negligible.
This approximation significantly reduces the computational cost, making the 2D solvers ideal for large-scale simulations of aquifers and watersheds, especially when detailed 3D simulations are not necessary or feasible. By solving for water height and flow, without capillary effects, the solvers can accurately simulate the dynamics of water and solute transport in both saturated and unsaturated zones.
The following solvers are available in the 2D groundwater modeling suite:
steadyGroundwater2DFoam for steady-state simulations
groundwater2DFoam for transient groundwater flow
porousScalarTransport2DFoam for passive tracer transport
groundwaterTransport2DFoam for coupled water and solute transport simulations
Here a quick view of the watershed for every 2D validation cases:
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With: (a) Mesh - (b) Permeability field - (c) DEM for upper limit - (d) DEM for lower limit



