<?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>1993-8012</journal-id>
<journal-title><![CDATA[Minería y Geología]]></journal-title>
<abbrev-journal-title><![CDATA[Min. Geol.]]></abbrev-journal-title>
<issn>1993-8012</issn>
<publisher>
<publisher-name><![CDATA[EDUM. Universidad de Moa]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1993-80122021000100030</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Evaluación de la vulnerabilidad a la intrusión marina en el sector Güira-Quivicán del acuífero costero Cuenca Sur de Artemisa y Mayabeque]]></article-title>
<article-title xml:lang="en"><![CDATA[Evaluating vulnerability to marine intrusion in Cuenca Sur coastal aquifer at Güira-Quivicán sector in Artemisa and Mayabeque provinces]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Valcarce-Ortega]]></surname>
<given-names><![CDATA[Rosa María]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Forcada-Labrador]]></surname>
<given-names><![CDATA[Carlos Enrique]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Tecnológica de La Habana  ]]></institution>
<addr-line><![CDATA[ La Habana]]></addr-line>
<country>Cuba</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>03</month>
<year>2021</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>03</month>
<year>2021</year>
</pub-date>
<volume>37</volume>
<numero>1</numero>
<fpage>30</fpage>
<lpage>43</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_arttext&amp;pid=S1993-80122021000100030&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_abstract&amp;pid=S1993-80122021000100030&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_pdf&amp;pid=S1993-80122021000100030&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN El sector Güira-Quivicán del acuífero cárstico costero Cuenca Sur aporta el 58 % del agua que abastece a la capital cubana. El agua subterránea en este acuífero drena libremente al mar, por lo que es imprescindible el control sistemático de la intrusión marina. Para evaluar la vulnerabilidad del acuífero a la intrusión salina fue aplicado el método GALDIT, que es un método paramétrico de superposición de rangos ponderados de la información hidrogeológica referida a: tipo de acuífero, conductividad hidráulica, nivel piezométrico, distancia a la costa, áreas con evidencias de intrusión salina y espesor del acuífero. El método fue adaptado a las características del área y a la información disponible y se obtuvo alta vulnerabilidad a la intrusión marina en el 31,5 % de este sector, mientras el 49,5 % tiene vulnerabilidad moderada. La alta correlación estadística entre el mapa de vulnerabilidad a la intrusión marina y el mapa de profundidad de la intrusión salina elaborado a partir de la interpretación de los sondeos eléctricos verticales medidos en el área, demuestra la validez de los resultados que se presentan.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Güira-Quivicán sector of Cuenca Sur coastal karstic aquifer contributes 58 % of the water the Cuban capital supplies. Groundwater in this aquifer drains freely into the sea, making systematic control of marine intrusion essential. To assess the vulnerability of the aquifer to saline intrusion, the GALDIT method was applied which is a parametric method of superposition of weighted ranges of hydrogeological information refering to: type of aquifer, hydraulic conductivity, piezometric level, distance to the coast, areas where saline intrusion and aquifer thickness is evident. The method was adapted to the available information and the characteristics of the area obtaining high vulnerability to marine intrusion in 31,5 % of this sector, while 49,5 % has moderate vulnerability. The high statistical correlation between the map of vulnerability to marine intrusion and the depth map of saline intrusion made from the interpretation of vertical electrical soundings measured in the area shows the validity of the results presented.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[intrusión salina]]></kwd>
<kwd lng="es"><![CDATA[vulnerabilidad a la intrusión marina]]></kwd>
<kwd lng="es"><![CDATA[método GALDIT, acuífero costero]]></kwd>
<kwd lng="en"><![CDATA[saline intrusion]]></kwd>
<kwd lng="en"><![CDATA[vulnerability to marine intrusion]]></kwd>
<kwd lng="en"><![CDATA[GALDIT method, coastal aquifer]]></kwd>
</kwd-group>
</article-meta>
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