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nonleaky confined aquifer
General assumptions. The aquifer is bounded above and below by completely impermeable aquicludes. The water level doesn’t fall lower than the aquifer top. The aquifer has a uniform thickness over the entire area. Pumping and observation wells are fully penetrating.
Conceptual models
Infinite aquifer (Theis’s method)
Aquifer with one lateral boundary
Combination of a recharge and no-flow boundaries
Recharge and no-flow boundaries
Recharge + recharge and no-flow boundaries
No-flow + no-flow and recharge boundaries