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- W1997124690 abstract "A system composed of an unconfined aquifer bounded by two streams or drains is considered in which the drains completely cut through the depth of the aquifer. The water levels in the drains are assumed to be at equal elevation. The aquifer receives either time-varying or uniform vertical recharge. The system is characterized also by the constancy of the hydraulic conductivity and specific yield of the aquifer and the validity of the Dupuit-Forchheimer assumptions. Analytical solutions are developed for the rise, decline, and maximum height of the water table. The solutions are expressed in terms of the weighted mean of the depth of saturation. A procedure for estimating the weighted average depth of the flow medium is presented." @default.
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- W1997124690 date "1974-01-01" @default.
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- W1997124690 title "Rise and decline of the water table induced by vertical recharge" @default.
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- W1997124690 doi "https://doi.org/10.1016/0022-1694(74)90009-2" @default.
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