<?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>2007-1132</journal-id>
<journal-title><![CDATA[Revista mexicana de ciencias forestales]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. mex. de cienc. forestales]]></abbrev-journal-title>
<issn>2007-1132</issn>
<publisher>
<publisher-name><![CDATA[Instituto Nacional de Investigaciones Forestales, Agrícolas y Pecuarias]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S2007-11322017000500143</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Comportamiento hidrológico de una pequeña cuenca de uso silvopastoril en el sureste de Coahuila]]></article-title>
<article-title xml:lang="en"><![CDATA[Hydrological behavior of a small rangeland and forest watershed in southeastern Coahuila]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Velásquez Valle]]></surname>
<given-names><![CDATA[Miguel A.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Esquivel Arriaga]]></surname>
<given-names><![CDATA[Gerardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sánchez Cohen]]></surname>
<given-names><![CDATA[Ignacio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Castillo Quiroz]]></surname>
<given-names><![CDATA[David]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cano Pineda]]></surname>
<given-names><![CDATA[Antonio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Gutiérrez Luna]]></surname>
<given-names><![CDATA[Ramón]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,INIFAP  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Centro Nacional de Investigación Disciplinaria en Relación Agua-Suelo-Planta-Atmósfera  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,INIFAP  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>10</month>
<year>2017</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>10</month>
<year>2017</year>
</pub-date>
<volume>8</volume>
<numero>43</numero>
<fpage>143</fpage>
<lpage>164</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S2007-11322017000500143&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S2007-11322017000500143&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S2007-11322017000500143&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen: El deterioro de los ecosistemas forestales pone en riesgo el almacenamiento y flujo del agua de lluvia. En el estado de Coahuila, existen 450 mil hectáreas de superficie forestal, las cuales son un área de captación de agua de lluvia. Para lograr un mayor aprovechamiento de este recurso es indispensable el monitoreo continuo de variables hidrológicas en las cuencas, principalmente, donde existe incertidumbre climática. El objetivo del presente estudio fue documentar el comportamiento hidrológico de una pequeña cuenca de uso ganadero-forestal, a partir del monitoreo de variables y el empleo de un modelo hidrológico de parámetros semidistribuidos espacialmente de la Cuenca Experimental del INIFAP, ubicada en el municipio Saltillo, Coah. Con registros históricos, cuantificados durante 2016 de precipitación pluvial se realizó el análisis de la respuesta hidrológica. Se utilizó el modelo WIN TR-55 para explicar la ausencia de escurrimiento, en función de parámetros semidistribuidos. Con los datos pluviométricos de 2016, se observó que las áreas de aportación de flujo superficial son las laderas y que la parte baja de la misma (el valle) actúa como un área buffer que restringe el escurrimiento superficial hacia la estación de aforo. En función a las simulaciones con el Modelo WIN TR - 55, se requiere una lámina precipitada diaria (máxima en 24 horas) mayor a 65 mm para registrar flujo superficial en la estación de aforo.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract: The deterioration of the ecosystem forest puts rain water storage and flow at risk. The State of Coahuila comprises 450 000 hectares of forests that serve as a rainwater catchment area. Continuous monitoring of the hydrological variables of the watershed is essential for make a better use of this resource, particularly where there is climatic uncertainty. The objective of this study was to document the hydrological behavior of a small experimental forest and rangeland watershed by monitoring the variables and through the use of a hydrological model with spatially semi-distributed parameters of the Experimental Watershed of INIFAP in Saltillo, Coahuila. The hydrological response of the watershed was analyzed based on the historical precipitation records quantified for 2016. The WIN TR-55 model was used to explain the absence of runoff in terms of the semi-distributed parameters of the watershed. The precipitation data for 2016 showed that source areas of surface runoff are the mountainsides, and that the bottom (the valley) acts as a buffer area that restricts its flow towards the runoff gauging station. According to the model simulations, a daily precipitation of over 65 mm is required in order to record surface flow at the runoff gauging station.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Área fuente]]></kwd>
<kwd lng="es"><![CDATA[curva numérica]]></kwd>
<kwd lng="es"><![CDATA[escurrimiento superficial]]></kwd>
<kwd lng="es"><![CDATA[modelo WIN TR - 55]]></kwd>
<kwd lng="es"><![CDATA[monitoreo de precipitación]]></kwd>
<kwd lng="es"><![CDATA[procesos hidrológicos]]></kwd>
<kwd lng="en"><![CDATA[Source area]]></kwd>
<kwd lng="en"><![CDATA[curve number]]></kwd>
<kwd lng="en"><![CDATA[surface runoff]]></kwd>
<kwd lng="en"><![CDATA[WIN TR - 55 model]]></kwd>
<kwd lng="en"><![CDATA[rainfall monitoring]]></kwd>
<kwd lng="en"><![CDATA[hydrological process]]></kwd>
</kwd-group>
</article-meta>
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