<?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>S1026-87742017000100025</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Evidencias hidrogeoquímicas e isotópicas sobre el origen del agua subterránea en la cuenca hidrográfica Río Actopan, Estado de Veracruz]]></article-title>
<article-title xml:lang="en"><![CDATA[Hidrogeochemical and isotropical evidences on the origin of groundwater in the río Actopan basin, state of Veracruz]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Pérez-Quezadas]]></surname>
<given-names><![CDATA[Juan]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cortés-Silva]]></surname>
<given-names><![CDATA[Alejandra]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Salas-Ortega]]></surname>
<given-names><![CDATA[María del Rocío]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Araguás-Araguás]]></surname>
<given-names><![CDATA[Luis]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Morales-Puente]]></surname>
<given-names><![CDATA[Pedro]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Carrillo-Chávez]]></surname>
<given-names><![CDATA[Alejandro]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Centro de Geociencias ]]></institution>
<addr-line><![CDATA[ Querétaro]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica ]]></institution>
<addr-line><![CDATA[ Ciudad de México]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Veracruzana Centro de Ciencias de la Tierra ]]></institution>
<addr-line><![CDATA[Xalapa Veracruz]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,International Atomic Energy Agency Vienna International Centre ]]></institution>
<addr-line><![CDATA[ Vienna]]></addr-line>
<country>Austria</country>
</aff>
<aff id="Af5">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología ]]></institution>
<addr-line><![CDATA[ Ciudad de México]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af6">
<institution><![CDATA[,Universidad Nacional Autónoma de México Centro de Geociencias ]]></institution>
<addr-line><![CDATA[ Querétaro]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>04</month>
<year>2017</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>04</month>
<year>2017</year>
</pub-date>
<volume>34</volume>
<numero>1</numero>
<fpage>25</fpage>
<lpage>37</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742017000100025&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742017000100025&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742017000100025&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen: Se interpretan datos fisicoquímicos, químicos e isotópicos de aguas de manantiales, pozos y ríos de la cuenca del río Actopan, centro de Veracruz, con el propósito de determinar el origen y circulación del agua subterránea. Algunos manantiales presentan temperaturas entre 9.6 °C y 18.3 °C con conductividad eléctrica menor a 150 µS/cm, sugiriendo un origen de recarga local. Una temperatura de agua subterránea de 38.2 °C y una conductividad eléctrica de 1542 µS/cm, 48 mg/L de Cl- y 721 mg/L de SO4 2- se asocian con flujo profundo e interacción con calcita, dolomita y yeso o anhidrita. Concentraciones de NO3 -&gt;10 mg/L permiten identificar fuentes antrópicas. Los resultados isotópicos de hidrógeno y de oxígeno caen en la tendencia de la Línea Mundial de las Aguas Meteóricas (&#948;2H = 8 &#948;18O + 10), indicando agua originada por las precipitaciones locales. De acuerdo con el gradiente isotópico con respecto a la altitud (Z), (&#948;18O = -2.1 (Z km) - 5.56), se identifican tres tipos de agua: 1) agua evaporada relacionada con la precipitación en temporada seca; 2) agua alineada al gradiente isotópico, recargada durante la temporada de lluvia; 3) agua recargada a cotas ligeramente mayores a su cota teórica de recarga, evidenciando flujo profundo y recarga de agua de río en la planicie costera.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract: Physical-chemical, chemical and isotopic data of spring water, groundwater and river water from the Actopan basin, central Veracruz were analyzed with the purpose of determining the origin and flow of groundwater. Spring water temperature between 9.6 °C and 18.3 °C, and low electrical conductivity (&lt;150 µS/cm) suggest local recharge. Groundwater temperature of 38.2 °C and electrical conductivity of 1542 µS/cm, 48 mg/L of Cl-, y 721 mg/L of SO4 2- are associated to deep flow and rock-water interaction (limestone, dolomite, gypsum/anhydrite). Concentrations of NO3 - &gt; 10 mg/L allow the identification of anthropogenic sources. Hydrogen and oxygen isotope results fit reasonable well with the Global Meteoric Water Line (GMWL, &#948;2H = 8 &#948;18O + 10) indicating that their recharge derives from local precipitation. On the basis of the observed isotope gradient with altitude (Z), (&#948;18O = -2.1 (Z km) - 5.56), three main groups of groundwater have been identified: 1) Evaporated water related to the precipitation in the dry season; 2) water, located on the line defined for the regional isotopic gradient, recharged during the rainy season; and 3) water recharged at levels slightly higher than its theoretical value of recharge, showing a component of deep flow and recharge from river water in the coastal plain.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[origen del agua subterránea]]></kwd>
<kwd lng="es"><![CDATA[&#948;2H]]></kwd>
<kwd lng="es"><![CDATA[&#948;18O]]></kwd>
<kwd lng="es"><![CDATA[cuenca del río Actopan]]></kwd>
<kwd lng="es"><![CDATA[Veracruz]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
<kwd lng="en"><![CDATA[origin of groundwater]]></kwd>
<kwd lng="en"><![CDATA[&#948;2H]]></kwd>
<kwd lng="en"><![CDATA[&#948;18O]]></kwd>
<kwd lng="en"><![CDATA[Actopan basin]]></kwd>
<kwd lng="en"><![CDATA[Veracruz]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
</kwd-group>
</article-meta>
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