| Representation of the second aquifer with 10 extraction wells.

| Representation of the second aquifer with 10 extraction wells.

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The complicated behavior of groundwater system in an arid aquifer is generally studied by solving the governing equations using either analytical or numerical methods. In this regard, analytical methods are just for some aquifers with regular boundaries. Numerical methods used for this aim are finite difference (FDM) and finite element methods (FEM...

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... standard unconfined aquifer with the area of 4,500 Â 10,000 m 2 is derived from Mckinney & Lin (1994) research (Figure 4). Boundary conditions for this aquifer in south and north edges are constant head boundary with 20 m value. ...

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