Groundwater flow equation, overview, derivation, and solution

Darcy’s law is the basic of flow, and it produces a partial differential equation similar to heat transfer when coupled with an continuity that explains conservation fluid mass during flow through porous media. This article, titled groundwater equation, covers derivation equations in both steady transient states. We look at some most common approaches methods for developing analytical or numerical solutions. The flaws limits these solutions reproducing behavior water on aquifer are also discussed article.