SciELO - Scientific Electronic Library Online

 
vol.47 número1Hydraulic fracturing as a possible mechanism of dyke-sill transitions and horizontal discordant intrusions in trachytic tabular bodies of Arraial do Cabo, State of Rio de Janeiro, BrazilPaleomagnetic study of Jurassic and Cretaceous rocks north of San Marcos fault, central Coahuila, México índice de autoresíndice de materiabúsqueda de artículos
Home Pagelista alfabética de revistas  

Servicios Personalizados

Revista

Articulo

Indicadores

Links relacionados

  • No hay artículos similaresSimilares en SciELO

Compartir


Geofísica internacional

versión On-line ISSN 2954-436Xversión impresa ISSN 0016-7169

Resumen

FLORES-MARQUEZ, E. L. et al. Numerical modeling of Etla Valley aquifer, Oax., Mexico: Evolution and remediation scenarios. Geofís. Intl [online]. 2008, vol.47, n.1, pp.27-40. ISSN 2954-436X.

Short-term evolution (for 2001, 2005 and 2015) for the shallow aquifer of Etla Valley, Oaxaca, southern Mexico, was simulated based in a 3D hydrological model elaborated from the available geological, geophysical, geochemical, and hydrologic parameters. The numerical simulations were based on Visual MODFLOW code. These simulations indicate that, if the actual extraction regime is maintained, the drawdown of the potentiometric surface will get worse to the SE of the study area (i. e. beneath Oaxaca city). The prevailing aquifer flow direction favors the ground water pollution by fertilizers and leakage from the sewage network (dumped to the Atoyac river). According to the numerical simulation, remediation of this situation is possible if the wells located in the neigborhood of Oaxaca City are relocated at the recharge zones (i. e. at the feet from Sierra de Juárez). This remediation scenario will allow a recovery of the drawdown of the potentiometric surface.

Palabras llave : 3D model; ground water flow; geohydrology; Mexico.

        · resumen en Español     · texto en Inglés     · Inglés ( pdf )

 

Creative Commons License Todo el contenido de esta revista, excepto dónde está identificado, está bajo una Licencia Creative Commons