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The article deals with unsteady ground water flow in an aquifer of limited horizontal extent. The changes in storage are taken to be dependent on a storage coefficient S, and flow rates are taken to...
Annual fluctuations of ground water levels of an aquifer are described as a consequence of water recharging periodically over a part of the aquifer. These areas can be depicted by drawing maps showi...
Approximative formulas for the movement of a continuously growing body of oil on the ground-water table are presented and illustrated. The approximations are many, but the formulas are believed to p...
Water temperature can be used as a tracer for the interaction between river water and groundwater, interpreting time shifts in temperature signals as retarded travel times. The water temperature fluc...

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