<?xml version="1.0" encoding="ISO-8859-1"?><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
<front>
<journal-meta>
<journal-id>1026-8774</journal-id>
<journal-title><![CDATA[Revista mexicana de ciencias geológicas]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. mex. cienc. geol]]></abbrev-journal-title>
<issn>1026-8774</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geología]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1026-87742025000100001</article-id>
<article-id pub-id-type="doi">10.22201/igc.20072902e.2025.1.1836</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Experimental study of infiltration through subsidence-reactivated surface discontinuities]]></article-title>
<article-title xml:lang="es"><![CDATA[Estudio experimental de infiltración a través de discontinuidades superficiales reactivadas por subsidencia]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Hernández-Marín]]></surname>
<given-names><![CDATA[Martín]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[González-Cervantes]]></surname>
<given-names><![CDATA[Norma]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Guerrero-Martinez]]></surname>
<given-names><![CDATA[Lilia]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rodríguez-Padilla]]></surname>
<given-names><![CDATA[Christian Emmanuel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Pacheco-Martínez]]></surname>
<given-names><![CDATA[Jesús]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Autónoma de Aguascalientes Departamento de Ingeniería Civil ]]></institution>
<addr-line><![CDATA[ Aguascalientes]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Autónoma de Aguascalientes  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Autónoma de Aguascalientes Observatorio de Riesgos Hidrogeológicos ]]></institution>
<addr-line><![CDATA[ Aguascalientes]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2025</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2025</year>
</pub-date>
<volume>42</volume>
<numero>1</numero>
<fpage>1</fpage>
<lpage>16</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742025000100001&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742025000100001&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742025000100001&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The main objective of this work is to investigate the influence of surface geological discontinuities on the hydraulic properties of the subsoil, studying an area affected by a fault (surface scarp) and a fracture (horizontal surface opening), which are separated by about 18 meters each other, forming part of a discontinuity system located within the Aguascalientes Valley (VA), Mexico. Both discontinuities are currently active due to the process of subsidence that the VA has been experiencing for more than 45 years, this emphasizes the relevance of this study since in most cases the studies are focused on regional inactive faults. In addition, studying some of the hydraulic properties of active discontinuities in the VA is significant because this valley currently has a large number of such structures with similar geologic conditions. As part of the methodology, 33-meter profiles of infiltration rates and hydraulic conductivity were obtained by applying permeability tests in the field, as well as 38-meter Electrical Resistance Tomography (ERT) profiles, in order to obtain and analyze the general characteristics of the subsoil and discontinuities. Subsequently, four ERT tests were applied in synchrony with punctual permeability test. The first ones in profiles of 14-17 meters, and the second ones in four points located at distances of under one meter from the discontinuities. These synchronized tests made it possible to visualize, in ERT profiles, the flow path of water injected into the subsurface through the permeameter, as well as the influence of the discontinuities on the hydraulic parameters mentioned above. The results show that the hydraulic parameters obtained in the areas close to the discontinuities, particularly the fault, are higher than those in the areas more distant from both discontinuities, probably due to their constant mechanical activity, being these increases of up to two orders of magnitude, obtaining maximum values of 2.08E-03 m/s for the infiltration velocity and 5.22E-05 m/s of hydraulic conductivity. On the other hand, observations from the simultaneous ERT-permeability tests suggest that discontinuities, particularly the fault, directly influence the path of infiltrated water, allowing the water to tend to move towards the displacement plane.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen El presente trabajo tiene como objetivo primordial el investigar la influencia de las discontinuidades geológicas superficiales sobre las propiedades hidráulicas del subsuelo, estudiando un área afectada por una falla (escarpe superficial) y una fractura (abertura horizontal superficial), las cuales se encuentran separadas por aproximadamente 18 metros entre sí, formando parte de un sistema de discontinuidades localizado dentro del Valle de Aguascalientes (VA), México. Ambas discontinuidades están actualmente activas debido al proceso de subsidencia que ha estado experimentando el VA desde hace más de 45 años, lo que enfatiza la relevancia de este estudio ya que, en la mayoría de los casos, los estudios se enfocan sobre fallas regionales inactivas. Además, el estudiar algunas propiedades hidráulicas de las discontinuidades activas del VA es significante ya que este valle actualmente cuenta con una gran cantidad de estas estructuras con condiciones geológicas similares. Como parte de la metodología, se obtuvieron perfiles de 33 metros de tasas de infiltración y conductividad hidráulica aplicando pruebas de permeabilidad en campo, así como perfiles de Tomografía Eléctrica Resistiva (TER) de 38 metros, con el fin de determinar y analizar las características generales del subsuelo y discontinuidades. Posteriormente, se aplicaron cuatro ensayos TER en sincronía con pruebas puntuales de permeabilidad, los primeros en perfiles de 14-17 metros, y los segundos en cuatro puntos situados a distancias inferiores a un metro de las discontinuidades. Estos ensayos sincronizados permitieron visualizar, en perfiles TER, el recorrido del flujo de agua inyectada en el subsuelo a través del permeámetro, así como la influencia de las discontinuidades sobre los parámetros hidráulicos mencionados. Los resultados muestran que los parámetros hidráulicos obtenidos en las zonas próximas a las discontinuidades, en particular de la falla, son mayores que en las zonas más distantes a ambas discontinuidades, debido probablemente a la su constante actividad mecánica, siendo estos incrementos de hasta dos órdenes de magnitud, obteniéndose valores máximos de 2.08E-03 m/s para la velocidad de infiltración y 5.22E-05 m/s de conductividad hidráulica. Por otro lado, las observaciones realizadas a partir de los ensayos simultáneos TER-permeabilidad sugieren que las discontinuidades, en particular la falla, influyen directamente en la trayectoria del agua infiltrada, permitiendo que el agua tienda a dirigirse hacia el plano de desplazamiento.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[hydrogeology]]></kwd>
<kwd lng="en"><![CDATA[Aguascalientes Valley]]></kwd>
<kwd lng="en"><![CDATA[subsidence-activated discontinuities]]></kwd>
<kwd lng="en"><![CDATA[field permeameter]]></kwd>
<kwd lng="en"><![CDATA[Electrical Resistance Tomography (ERT)]]></kwd>
<kwd lng="en"><![CDATA[infiltration dynamics]]></kwd>
<kwd lng="es"><![CDATA[hidrogeología]]></kwd>
<kwd lng="es"><![CDATA[Valle de Aguascalientes]]></kwd>
<kwd lng="es"><![CDATA[discontinuidades activadas por hundimiento]]></kwd>
<kwd lng="es"><![CDATA[permeámetro de campo]]></kwd>
<kwd lng="es"><![CDATA[Tomografía de Resistencia Eléctrica (ERT)]]></kwd>
<kwd lng="es"><![CDATA[dinámica de infiltración]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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