A semianalytical solution for the Boussinesq equation with nonhomogeneous constant boundary conditions

The Boussinesq groundwater equation is widely used in hydrology to predict streamflow from an unconfined aquifer and derive the aquifer's saturated hydraulic conductivity and drainable porosity, and to predict water table height in drainage engineering. In this work, we solve this equation in a...

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Veröffentlicht in:	Water resources research 2014-08, Vol.50 (8), p.6549-6556
Hauptverfasser:	Dias, Nelson L., Chor, Tomás L., de Zárate, Ailín Ruiz
Format:	Artikel
Sprache:	eng
Schlagworte:	Approximation aquifer discharge Aquifers Boundary conditions Boussinesq equation Drainage engineering groundwater hydrology Hydrology Porosity Stream discharge Stream flow Unconfined aquifers Water table
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