Journal ArticleDOI
Vertically integrated flow in stratified aquifers
TLDR
In this article, a set of continuous discharge potentials that can be used to determine the vertically integrated flow in stratified aquifers is presented, which is valid for any values of hydraulic conductivity; there are no limitations of the contrast for the method to be valid.About:
This article is published in Journal of Hydrology.The article was published on 2017-05-01. It has received 9 citations till now. The article focuses on the topics: Aquifer & Hydraulic head.read more
Citations
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Journal ArticleDOI
Defining the Effect of Stratification in Coastal Aquifers Using a New Parameter
Journal ArticleDOI
Water flow across the interface of contrasting materials: Pressure discontinuity and its implications
TL;DR: A pore-scale model is presented to simulate fluid flow in columns filled with two stratified media, which yields a pressure discontinuity at the strata interface.
Journal ArticleDOI
Water table rise in urban shallow aquifer with vertically-heterogeneous soils: Girinskii’s potential revisited
TL;DR: In this paper, the Dupuit-Forchheimer approximation (Girinskii potential) and numerically by FDM-MODFLOW and F... were used to study the hydraulic conductivity of an aquifer.
Journal ArticleDOI
Experimental investigation of solute transport across transition interface of porous media under reversible flow directions.
TL;DR: In this paper , a mobile and immobile (MIM) model was proposed to better capture the directionally dependent transport of solutes through a sharp/transition interface than the advection-dispersion equation (ADE).
References
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Journal ArticleDOI
Handbook of Mathematical Functions
Book
Dynamics of fluids in porous media
TL;DR: In this paper, the Milieux poreux Reference Record was created on 2004-09-07, modified on 2016-08-08 and the reference record was updated in 2016.
Journal ArticleDOI
Three-Dimensional, Transient, Saturated-Unsaturated Flow in a Groundwater Basin
TL;DR: In this article, a three-dimensional finite difference model was developed for the treatment of saturated-unsaturated transient flow in small nonhomogeneous, anisotropic geologic basins.