Articles | Volume 382
Proc. IAHS, 382, 5–9, 2020
Proc. IAHS, 382, 5–9, 2020

Pre-conference publication 22 Apr 2020

Pre-conference publication | 22 Apr 2020

Infiltration of surface water through subsidence failure assessment applying electric prospecting, case Aguascalientes Valley, Mexico

Fernando Acuña-Lara et al.

Related authors

Application of seismic prospecting to determine the width of influence of surface faults associated to land subsidence – a case of study in the Aguascalientes Valley, México
Hugo Luna-Villavicencio, Jesús Pacheco-Martínez, Fernando Acuña-Lara, Martín Hernández-Marín, and Norma González-Cervantes
Proc. IAHS, 382, 781–785,,, 2020
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Cited articles

Aizebeokhai, A. P.: 2D and 3D geoelectrical resistivity imaging: Theory and field design, Sci. Res. Essays, 5, 3597–3599, 2010. 
Aranda-Gómez, J. J.: Geología preliminar del Graben de Aguascalientes, Revista mexicana de ciencias geológicas, 8, 22–31, 1989. 
Dahlin, T., Wisén, R., and Zhang, D.: 3D Effects on 2D Resistivity Imaging – Modelling and Field Surveying Results, Near Surface 2007 – 13th EAGE European Meeting of Environmental and Engineering Geophysics, Istanbul, Turkey,, 2007. 
Harrison-Griffiths, D. and David-Baker, R.: Two-dimensional resistivity mapping with a complex controlled array, 29, 211–226, 1993. 
Hernández Marín, M., Pacheco Martínez, J., Burbey, T. J., Carreón-Freyre, D., Ochoa-González, G. H., and de Lira-Gómez, P.: Evaluation of subsurface infiltration and displacement in a subsidence-reactivated normal fault in the Aguascalientes Valley, Mexico, Environ. Earth Sci., 76, 812,, 2017. 
Short summary
Land subsidence is an anthropogenic hazard triggered by different causes, one of them is groundwater overexploitation over aquifer systems, becoming risk points for aquifer pollution The obtained results showed that the Schlumberger configuration appears to be more helpful to detect changes in the stratigraphy toward depth, while dipole-dipole and Wenner are more suitable to detect lateral variations such as the vertical wastewater leakage in the first 6 to 8 m depth.