<?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>1405-3195</journal-id>
<journal-title><![CDATA[Agrociencia]]></journal-title>
<abbrev-journal-title><![CDATA[Agrociencia]]></abbrev-journal-title>
<issn>1405-3195</issn>
<publisher>
<publisher-name><![CDATA[Colegio de Postgraduados]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1405-31952017000300245</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Condiciones para modelar el riego por gravedad con propiedades hidrodinámicas equivalentes del suelo]]></article-title>
<article-title xml:lang="en"><![CDATA[Conditions for modeling surface irrigation with effective soil hydraulic properties]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Zataráin]]></surname>
<given-names><![CDATA[Felipe]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Fuentes]]></surname>
<given-names><![CDATA[Carlos]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rendón]]></surname>
<given-names><![CDATA[Luis]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México  ]]></institution>
<addr-line><![CDATA[Jiutepec Morelos]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Instituto Mexicano de Tecnología del Agua  ]]></institution>
<addr-line><![CDATA[Jiutepec Morelos]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,aff3  ]]></institution>
<addr-line><![CDATA[ Morelos]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>05</month>
<year>2017</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>05</month>
<year>2017</year>
</pub-date>
<volume>51</volume>
<numero>3</numero>
<fpage>245</fpage>
<lpage>264</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-31952017000300245&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-31952017000300245&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-31952017000300245&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Para diseñar el riego por gravedad es común hacer mediciones durante un evento de riego y deducir valores promedio o efectivos de la infiltración. Pero, la variabilidad espacial de los suelos puede ser de tal magnitud que la representatividad de estos valores puede cuestionarse. La hipótesis de este estudio fue que utilizar los valores efectivos de las propiedades hidrodinámicas del suelo es válido en ciertas condiciones de riego por gravedad. El objetivo fue analizar esas propiedades, con base en información experimental de infiltración y avance del riego en melgas, a través de la generación de campos correlacionados de la conductividad hidráulica con un método fundamentado en el análisis espectral. El análisis se complementó con la modelación de la fase de avance con valores de las propiedades hidrodinámicas del suelo generados aleatoriamente a partir de su distribución de probabilidad. A pesar de que los campos correlacionados presentaron variabilidad espacial amplia, según el perfil de las láminas infiltradas, el avance en las simulaciones mostró comportamiento similar. Los métodos inversos son válidos para determinar valores medios de las propiedades hidrodinámicas en el riego por gravedad cuando la distribución de la probabilidad es única en el espacio.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract To design a system of surface irrigation, it is common to take measurements during an irrigation event and deduce average or effective values of infiltration. However, spatial variability of the soils can be so great that the representativity of these values may be questionable. The hypothesis of this study was that it is valid to use the effective values of hydrodynamic properties of the soil in certain conditions of surface irrigation. The objective was to analyze these properties based on experimental information on infiltration and advance of water in border irrigation by generating correlated fields of hydraulic conductivity with a method grounded in spectral analysis. The analysis was complemented with modeling of the advance phase with values of hydrodynamic properties of the soil generated randomly from its probability distribution. Although the correlated fields had broad spatial variability, according to infiltrated profiles, advance in the simulations showed similar behavior. Inverse methods are valid to determine mean values of the hydrodynamic properties in surface irrigation when the probability distribution is unique in space.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Infiltración]]></kwd>
<kwd lng="es"><![CDATA[variabilidad espacial]]></kwd>
<kwd lng="es"><![CDATA[campos correlacionados]]></kwd>
<kwd lng="en"><![CDATA[Infiltration]]></kwd>
<kwd lng="en"><![CDATA[spatial variability]]></kwd>
<kwd lng="en"><![CDATA[correlated fields]]></kwd>
</kwd-group>
</article-meta>
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