<?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>0187-5779</journal-id>
<journal-title><![CDATA[Terra Latinoamericana]]></journal-title>
<abbrev-journal-title><![CDATA[Terra Latinoam]]></abbrev-journal-title>
<issn>0187-5779</issn>
<publisher>
<publisher-name><![CDATA[Sociedad Mexicana de la Ciencia del Suelo A.C.]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0187-57792019000100057</article-id>
<article-id pub-id-type="doi">10.28940/tl.v37i1.345</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Parámetros que controlan la percolación profunda en un cultivo de trigo]]></article-title>
<article-title xml:lang="en"><![CDATA[Parameters controlling deep percolation in a wheat crop]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Teófilo Salvador]]></surname>
<given-names><![CDATA[Eduardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Morales Reyes]]></surname>
<given-names><![CDATA[Guillermo Pedro]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Esteller Alberich]]></surname>
<given-names><![CDATA[María Vicenta]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Muciño Castañeda]]></surname>
<given-names><![CDATA[René]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Autónoma del Estado de México Instituto Interamericano de Tecnología y Ciencias del Agua ]]></institution>
<addr-line><![CDATA[Toluca de Lerdo Estado de México]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Autónoma del Estado de México Facultad de Ingeniería ]]></institution>
<addr-line><![CDATA[Toluca Estado de México]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>03</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>03</month>
<year>2019</year>
</pub-date>
<volume>37</volume>
<numero>1</numero>
<fpage>57</fpage>
<lpage>68</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-57792019000100057&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-57792019000100057&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-57792019000100057&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Para estimar la percolación del agua en el suelo es común utilizar el método del balance hídrico, el cual requiere de diversos datos diarios, los cuales muchas veces son incompletos o no son verificados en campo, además de que existe cierta incertidumbre en la estimación de la evapotranspiración del cultivo. En este trabajo el objetivo fue identificar los parámetros que controlan la percolación profunda a partir de la estimación de balances hídricos locales diarios con diferentes coeficientes de cultivo, utilizando para ello datos de estaciones climatológicas y parámetros edafológicos. En el sitio de estudio se llevó a cabo un monitoreo constante de las etapas fenológicas de un cultivo de trigo (temporal) y mensualmente se realizó un muestreo de suelo durante un año en diferentes puntos dentro del sitio. Paralelamente, se realizó el acopio de datos procedentes de estaciones climatológicas, la evaporación se midió con el tanque evaporímetro, se estimó para la evapotranspiración del cultivo un coeficiente único, dual y ajustado por estrés con base en el manual de la FAO, y, a partir de estos datos, se determinó la percolación profunda. Cuando la superficie del suelo estaba saturada o sobresaturada, la evapotranspiración del cultivo fue despreciable, además el crecimiento vertical máximo de la planta fue de 1.02 m y la profundidad de la raíz de 0.35 m. Precipitaciones diarias superiores a 10 mm o acumulado de tres días consecutivos mayor de 18 mm de lluvia; propiciaron la percolación profunda, pero ésta decreció a casi por goteo conforme aumentó el espesor de la franja radicular de 0.30 m a 0.52 m. El crecimiento del cultivo, el espesor de la zona radicular y la incidencia de la precipitación en la superficie del suelo controlaron la percolación profunda. Los valores obtenidos permiten aproximar aún más el valor real de recarga del agua subterránea.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Summary To evaluate the water percolation in the soil, the water balance method is common. This method requires different daily data, which are often incomplete or not verified in field, in addition to some uncertainty regarding crop evapotranspiration. In this research, the parameters that control deep percolation were identified, based on estimation of daily local water balances with different crop coefficients, using data from weather stations and edaphic parameters. At the study site, constant monitoring of the phenological stages of a wheat crop (temporal) was carried out, and monthly soil sampling was performed for one year at different points within the site. At the same time, data were collected from weather stations, evaporation was measured with the evaporimeter tank, evapotranspiration of the crop was estimated for a single coefficient, dual and adjusted for stress based on the FAO manual, and deep percolation was determined from these data. When the soil surface was saturated or supersaturated, evapotranspiration of the crop was negligible. In addition, maximum vertical plant growth was 1.02 m, and root depth was 0.35 m. Daily rainfall greater than 10 mm or cumulative of three consecutive days greater than 18 mm of rainfall led to deep percolation, but this decreased to almost drip as thickness of the root zone increased from 0.30 m to 0.52 m. Crop growth, root zone thickness and incidence of precipitation on the soil surface controlled deep percolation. The values obtained allow us to more closely approximate the actual value groundwater recharge.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[evapotranspiración]]></kwd>
<kwd lng="es"><![CDATA[profundidad radicular]]></kwd>
<kwd lng="es"><![CDATA[recarga]]></kwd>
<kwd lng="en"><![CDATA[evapotranspiration]]></kwd>
<kwd lng="en"><![CDATA[root depth]]></kwd>
<kwd lng="en"><![CDATA[recharge]]></kwd>
</kwd-group>
</article-meta>
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