Extension of the Dupuit–Forchheimer Model for Non-Hydrostatic Flows in Unconfined Aquifers

The classical Dupuit–Forchheimer approach, commonly used in analysing unconfined groundwater-flow systems, relies on the assumption of a negligible vertical component of the flow. This approximation is valid only when the convergence of streamlines is very limited and the drawdown of the phrea...

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Autor principal:	Yebegaeshet T. Zerihun
Formato:	Artigo
Idioma:	Inglês
Publicado em:	MDPI AG 2018-06-01
coleção:	Fluids
Assuntos:	groundwater hydrodynamics unconfined flow problems porous media seepage surface hillslope hydrology free-boundary problems
Acesso em linha:	http://www.mdpi.com/2311-5521/3/2/42
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