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Nodal point ocean well - PowerPoint PPT Presentation

General governing equation for steady-state , heterogeneous , anisotropic conditions

2D Laplace Eqn. --Homogeneous and isotropic aquifer without a sink/source term. --2D flow in a profile; (Unconfined aquifer with a water table boundary condition; recharge occurs as a result of the boundary condition.). General governing equation

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Nodal point ocean well - PowerPoint PPT Presentation

General governing equation for steady-state , heterogeneous , anisotropic conditions