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In steady state condition, non - linear laminar flow of fluid into an open<br />bottom well just penetrating the semi-infinite porous aquifer is considered. The<br />influence of non-linear laminar flow on discharge and its dependance on related<br />physical quantities is examined. It is found that an open bottom well actually<br />behaves like a hemispherical well, which is an obvious practical phenomenon

Non - linear laminar flow of fluid into an open bottom well