WebTools. Used in hydrogeology, the groundwater flow equation is the mathematical relationship which is used to describe the flow of groundwater through an aquifer. The transient flow of groundwater is described by a form of the diffusion equation, similar to that used in heat transfer to describe the flow of heat in a solid ( heat conduction ). Websteady-state Thiem equation [Thiem 1906], which can be applied to quasi-steady-state conditions when the rate of removal of water from storage near the pumping well is zero. The head in the well is calculated from the following equation [Anderson and Woessner 1992]: re, ln 2 WT e wij w Qr hh πTr ⎛⎞ =−⎜ ⎝⎠ ⎟ (1)
Assumptions of Dupuits Theory
WebFurthermore, the future version of the software will include the option to calculate the ROI of the wells under unconfined conditions, and most probably, we will use the Dupuit formula … http://www.aqtesolv.com/theis-unconfined.htm fisher dlc3010
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