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The physical problem dealt with in this article is the unsteady groundwater flow in an aquifer of limited horizontal extent and arbitrary boundary shape.The unsteady ground-water level is described ...
This paper deals with two cases. The first case concerns a solution for the drawdown in a given well which makes it possible to monitor and/or model the drawdown in other wells in the system and deter...
Rapid soil moisture variations were measured with TDR equipment at five depths ranging from 0.1 to 0.9 m during five consecutive infiltration experiments under ponding. Each time, 27 mm of water were ...

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