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Vulnerability to contamination of the Zaachila aquifer, Oaxaca, Mexico

The aquifer of Zaachila was evaluated following conventional methods (DRASTIC, AVI, and GOD). Depth to the watertable was established from a set of wells. Accordingly, the groundwater flows from N to S. Hydraulic conductivity ranges between1.81647E-05 and 1.70411E-04 m/s, while transmissivity varies...

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Publicado en:Geofísica Internacional
Autores principales: Salvador I. Belmonte-Jiménez, J. Oscar Campos-Enríquez, Miguel A. Alatorre Zamora
Formato: Artigo
Lenguaje:Inglês
Publicado: Universidad Nacional Autónoma de México 2005
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Acceso en línea:https://www.redalyc.org/articulo.oa?id=56844307
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