<?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>S0187-57792019000400391</article-id>
<article-id pub-id-type="doi">10.28940/terra.v37i4.531</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Erodabilidad y riesgo de erosión de suelos negros del centro de México: estudio de un Phaozem]]></article-title>
<article-title xml:lang="en"><![CDATA[Erodibility and erosion risk of black soils of central Mexico: study of a Phaeozem]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Pérez-Salinas]]></surname>
<given-names><![CDATA[Jesús Emmanuel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rodríguez]]></surname>
<given-names><![CDATA[Fernando Rufino]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[López-Santos]]></surname>
<given-names><![CDATA[Armando]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Torres-González]]></surname>
<given-names><![CDATA[Jorge Alejandro]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Meraz-Jiménez]]></surname>
<given-names><![CDATA[Antonio de Jesús]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Díaz-Romo]]></surname>
<given-names><![CDATA[Abraham]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Valdivia-Martínez]]></surname>
<given-names><![CDATA[Oscar]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Autónoma Chapingo  ]]></institution>
<addr-line><![CDATA[ Edo. de México]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Autónoma de Aguascalientes Centro de Ciencias Agropecuarias ]]></institution>
<addr-line><![CDATA[Aguascalientes Ags.]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,United Nations Convention to Combat Desertification ]]></institution>
<addr-line><![CDATA[Bonn ]]></addr-line>
<country>Germany</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2019</year>
</pub-date>
<volume>37</volume>
<numero>4</numero>
<fpage>391</fpage>
<lpage>400</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-57792019000400391&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-57792019000400391&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-57792019000400391&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN: Estimaciones de erosión para los suelos negros de México basados en la Ecuación Universal de Pérdida de Suelo (EUPS), presentan discrepancias debido a generalizaciones que conducen a errores en los límites permisibles, siendo el factor erodabilidad o K (FK) el más sensible. El objetivo de la presente investigación fue obtener el rango razonable FK para un Phaoezem (PH) del centro de México mediante el contraste de dos ecuaciones basadas en la EUPS. Se obtuvieron muestras en forma aleatoria en tres sitios (P1, P2, P3) de una superficie de 3 hectáreas. Se determinó porcentaje de materia orgánica, clase textural, tipos de estructura y permeabilidad. Los resultados revelan diferencias entre FK estimada (FKe) y FK de referencia (FKr), ambas derivadas del método tradicional; sus valores fueron: +0.014, +0.0149 y +0.0152, para P3, P2 y P1, respectivamente. Diferencias que representan subestimaciones 1.25 veces en magnitud para FKr con respecto a FKe. Además de ello, del análisis estadístico se descarta la hipótesis nula (H0) de similitud para los promedios de cada sitio evaluado (P1 = P2 = P3). Aunque las diferencias entre los factores de erodabilidad obtenidos con la ecuación específica para los Molisoles en la Provincia de Yunan, China y la nomografía de referencia desarrollada primordialmente en Estados Unidos de América, son estadísticamente diferentes (&#945; &#8805; 0.001), una combinación de ambas podría dar un rango de máximo y mínimo en las estimaciones de FK, y tendría mejores resultados que con valores por defecto que subestiman los resultados sobre tasas de erosión.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[SUMMARY: Erosion estimates for black soils in Mexico based on the Universal Soil Loss Equation (USLE) present discrepancies due to generalizations that lead to errors in permissible limits, with the erodibility factor or K factor (FK) being the most sensitive. The objective of the present investigation was to obtain a reasonable FK range for a Phaeozem (PH) from central Mexico by contrasting two equations based on the USLE. Samples were randomly obtained at three sites (P1, P2, P3) of a four-hectare area. The percentage of organic matter, textural class, soil structure, and profile permeability were determined. The results reveal differences between the estimated FK (FKe) and reference FK (FKr), whose values were +0.015, +0.028, and +0.029 for P1, P2, and P3, respectively. The differences represent underestimations that are up to 1.7 times greater in magnitude for FKr with respect to FKe. The statistical analysis rejects the null hypothesis (H0) that the means of each site evaluated are the same (P1 = P2 = P3). Although the variances between the factors of erodibility obtained using the equation specific to the Mollisols in Yunnan Province, China, and the reference nomography developed primarily in United States are significantly different (&#945; &#8805; 0.01), a combination of both could provide a range of maximums and minimums in the FK estimates and would yield better results than with the use of default values that tend to underestimate erosion rates.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[erosión hídrica]]></kwd>
<kwd lng="es"><![CDATA[factor K/USLE]]></kwd>
<kwd lng="es"><![CDATA[molisoles]]></kwd>
<kwd lng="en"><![CDATA[water erosion]]></kwd>
<kwd lng="en"><![CDATA[K/USLE factor]]></kwd>
<kwd lng="en"><![CDATA[mollisols]]></kwd>
</kwd-group>
</article-meta>
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