Spatial and temporal variation of natural recharge in the semi-arid valley of Aguascalientes, Mexico


Por: Hernández-Marín M., Guerrero-Martínez L., Zermeño-Villalobos A., Rodríguez-González L., Burbey T.J., Pacheco-Martínez J., Martínez-Martínez S.I., González-Cervantes N.

Publicada: 1 dic 2018 Ahead of Print: 1 ene 2018
Resumen:
The investigation involves a temporal and spatial analysis to characterize recharge in the Aguascalientes valley in central Mexico. The results are based on a two-part methodological strategy using a geospatial and numerical analysis. Results from the geospatial analysis are based on the analytical hierarchical process (AHP) method, which involves developing a zoning map that qualifies the conditions for groundwater recharge in the valley. In addition, one-dimensional numerical modeling based on the van Genuchten equation was applied for various soil column configurations to estimate the transit time of recharge through the vadose zone. The analysis was performed over a 20-year period from 1995 to 2015. The results of the geospatial analysis indicate that the optimal area for groundwater recharge is the lower zone of the valley, particularly the portion influenced by surface discontinuities. The shortest estimated period of recharge for water to pass through the vadose zone is approximately 4.25years.

Filiaciones:
Hernández-Marín M.:
 Departamento de Geotecnia e Hidráulica, Universidad Autónoma de Aguascalientes (UAA), Aguascalientes, Mexico

Guerrero-Martínez L.:
 Doctorado en Ciencias de los Ámbitos Antrópicos, Aguascalientes, Mexico

Zermeño-Villalobos A.:
 Maestría en Ingeniería Civil, Aguascalientes, Mexico

Rodríguez-González L.:
 Maestría en Ingeniería Civil, Aguascalientes, Mexico

Burbey T.J.:
 Department of Geosciences, Virginia Tech, Blacksburg, VA, United States

Pacheco-Martínez J.:
 Departamento de Construcción y Estructuras, Aguascalientes, Mexico

Martínez-Martínez S.I.:
 Departamento de Construcción y Estructuras, Aguascalientes, Mexico

González-Cervantes N.:
 Posgrado en Ciencias de la Tierra, Universidad Nacional Autónoma de México (UNAM), Departamento de Geotecnia e Hidráulica, Aguascalientes, Mexico
ISSN: 14312174
Editorial
SPRINGER, 233 SPRING ST, NEW YORK, NY 10013 USA, Estados Unidos America
Tipo de documento: Article
Volumen: 26 Número: 8
Páginas: 2811-2826
WOS Id: 000452085400018

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