Groundwater-flow modeling in the Yucatan karstic aquifer, Mexico

The current conceptual model of the unconfined karstic aquifer in the Yucatan Peninsula, Mexico, is that a fresh-water lens floats above denser saline water that penetrates more than 40km inland. The transmissivity of the aquifer is very high so the hydraulic gradient is very low, ranging from 7-10m...

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Veröffentlicht in:	Hydrogeology journal 2002-10, Vol.10 (5), p.539-552
Hauptverfasser:	Gonzalez-Herrera, Roger, Sanchez-y-Pinto, Ismael, Gamboa-Vargas, Jose
Format:	Artikel
Sprache:	eng
Schlagworte:	Aquifers Channeling Dynamical systems Dynamics Floats Flow system Fluid flow Geophysics Groundwater flow Hydraulic gradient Hydraulics Karst Karstic areas Peninsulas Porous media Saline water Simulation Sinkholes Transmissivity
Online-Zugang:	Volltext
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