<?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>0016-7169</journal-id>
<journal-title><![CDATA[Geofísica internacional]]></journal-title>
<abbrev-journal-title><![CDATA[Geofís. Intl]]></abbrev-journal-title>
<issn>0016-7169</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geofísica]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0016-71692016000100005</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Geological Differentiation of Groundwater Threshold Concentrations of Arsenic, Vanadium and Fluorine in El Bajio Guanajuatense, Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rodríguez]]></surname>
<given-names><![CDATA[Ramiro]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Morales-Arredondo]]></surname>
<given-names><![CDATA[Iván]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rodríguez]]></surname>
<given-names><![CDATA[Isaías]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica ]]></institution>
<addr-line><![CDATA[México D.F.]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Programa de Posgrado en Ciencias de la Tierra ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>03</month>
<year>2016</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>03</month>
<year>2016</year>
</pub-date>
<volume>55</volume>
<numero>1</numero>
<fpage>5</fpage>
<lpage>15</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0016-71692016000100005&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0016-71692016000100005&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0016-71692016000100005&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract: Groundwater background values, (GBV), of risky elements can be integrated as a component in groundwater management policies. Variations of GBV in rural areas with agricultural activity and in urban areas with industrial development can be related to contamination processes. Methods to calculate GBV were applied in Salamanca and Juventino Rosas, an industrial city and a farming community located in Central Mexico. A statistical treatment for rejection of deviant values was used for outliers (Dixon's Q test). GBV were calculated using the Grubb test. Variations in arsenic and vanadium GBV are explained in terms of potential contamination sources and migration mechanisms. Arsenic and vanadium are contained in particulate emitted by a thermoelectric plant. Particulate was deposited over vulnerable areas that facilitate its migration to local aquifers. Differences in fluoride GBV are explained in terms of the geological framework.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen: Los valores de fondo del agua subterránea, BGV (por sus siglas en ingles), de elementos riesgosos, pueden ser integrados como componentes en las políticas de manejo del agua subterránea. Variaciones de los BGV en áreas rurales con actividad agrícola y en áreas urbanas con desarrollo industrial pueden ser referidas a procesos de contaminación del agua. Métodos para calcular los BGV fueron aplicados en una comunidad agrícola en el centro de México. Un tratamiento estadístico para rechazar valores anómalos fue usado (Prueba de Dixon). Los valores de fondo fueron calculados usando el método de Grubb. Variaciones en los valores de fondo de arsénico y vanadio son explicados en términos de fuentes potenciales de contaminación y mecanismos de migración. El arsénico y el vanadio estaban contenidos en particulado emitido por una planta termoeléctrica. El particulado fue depositado sobre áreas vulnerables lo que facilitó su migración hacia acuíferos someros locales. Diferencia en los valores de fondo de fluoruros son explicados en términos del marco geológico.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[arsenic]]></kwd>
<kwd lng="en"><![CDATA[background values]]></kwd>
<kwd lng="en"><![CDATA[El Bajio Mexico]]></kwd>
<kwd lng="en"><![CDATA[fluorine]]></kwd>
<kwd lng="en"><![CDATA[groundwater]]></kwd>
<kwd lng="es"><![CDATA[arsénico]]></kwd>
<kwd lng="es"><![CDATA[valores de fondo]]></kwd>
<kwd lng="es"><![CDATA[El Bajío México]]></kwd>
<kwd lng="es"><![CDATA[fluoruros]]></kwd>
<kwd lng="es"><![CDATA[agua subterránea]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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