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A Computer Program for Predicting Recharge with a Master Recession Curve

By Christopher S. Heppner, John R. Nimmo
eBook
$1.99
By Christopher S. Heppner, John R. Nimmo
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Water-table fluctuations occur in unconfined aquifers owing to ground-water recharge following precipitation and infiltration, and ground-water discharge to streams between storm events. Ground-water recharge can be estimated from well hydrograph data using the water-table fluctuation (WTF) principle, which states that recharge is equal to the product of the water-table rise and the specific yield of the subsurface porous medium. The water-table rise, however, must be expressed relative to ...

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