<?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>1659-4266</journal-id>
<journal-title><![CDATA[Cuadernos de Investigación UNED]]></journal-title>
<abbrev-journal-title><![CDATA[Cuadernos de Investigación UNED]]></abbrev-journal-title>
<issn>1659-4266</issn>
<publisher>
<publisher-name><![CDATA[Universidad Estatal a Distancia de Costa Rica]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1659-42662017000100023</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Comparación de tres métodos de infiltración para calcular el balance hídrico del suelo, en la Cuenca del río Suquiapa, El Salvador]]></article-title>
<article-title xml:lang="en"><![CDATA[Comparison of three infiltration methods to calculate soil water balance in the Suquiapa River Basin, El Salvador]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Alvarado Batres]]></surname>
<given-names><![CDATA[César]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Barahona-Palomo]]></surname>
<given-names><![CDATA[Marco]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de El Salvador Escuela de Física Facultad de Ciencias Naturales y Matemática]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>El Salvador</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad de Costa Rica Escuela Centroamericana de Geología ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Costa Rica</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>06</month>
<year>2017</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>06</month>
<year>2017</year>
</pub-date>
<volume>9</volume>
<numero>1</numero>
<fpage>23</fpage>
<lpage>33</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_arttext&amp;pid=S1659-42662017000100023&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_abstract&amp;pid=S1659-42662017000100023&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_pdf&amp;pid=S1659-42662017000100023&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La infiltración del agua en el suelo juega un papel fundamental en el ciclo hidrológico. Dependiendo de las condiciones geológicas, puede permanecer en el suelo en forma de humedad; escurrir como flujo subsuperficial y aflorar como una naciente efímera; o recargar el acuífero, entre otros. Aquí presentamos una comparación de los valores de la recarga potencial para una misma cuenca, con tres métodos de infiltración comúnmente utilizados in situ: doble anillo, Porchet y permeámetro de Guelph. Observamos una correlación buena (r2=0,74) entre los valores obtenidos por medio del método del doble anillo y el permeámetro de Guelph; la correlación entre el método de Porchet y estos otros dos métodos es mala (r2 inferior a 0,02).Los valores de recarga obtenidos muestran que no hay una variación significativa entre estos métodos de infiltración, obteniendo resultados dentro del intervalo de confianza]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Water infiltration in the soil has a fundamental role in the hydrological cycle. Depending on geological conditions, it can remain in the soil as moisture, drain as subsurface flow and emerge as an ephemeral; or recharge the aquifer, among others. We compared three commonly used field methods: Double ring, Porchet and Guelph permeameter.Double ring and Guelph correlate well (r2 = 0.74), but their correlation with Porchet is poor (r2 less than 0.02).The values obtained by these methods were used for the determination of the potential recharge to the aquifer by means of the soil water balance, using common method in Central America. The recharge values were all similar and within the confidence interval.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[agua]]></kwd>
<kwd lng="es"><![CDATA[infiltración]]></kwd>
<kwd lng="es"><![CDATA[doble anillo]]></kwd>
<kwd lng="es"><![CDATA[permeámetro de Guelph]]></kwd>
<kwd lng="es"><![CDATA[balance hídrico del suelo]]></kwd>
<kwd lng="es"><![CDATA[cuenca]]></kwd>
<kwd lng="en"><![CDATA[water]]></kwd>
<kwd lng="en"><![CDATA[infiltration,double ring]]></kwd>
<kwd lng="en"><![CDATA[Guelph permeameter]]></kwd>
<kwd lng="en"><![CDATA[soil water balance]]></kwd>
<kwd lng="en"><![CDATA[basin]]></kwd>
</kwd-group>
</article-meta>
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