<?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>S0187-57792011000200211</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[CONTENIDO DE CARBONO EN SUELOS CON DIFERENTES USOS AGROPECUARIOS EN EL TRÓPICO MEXICANO]]></article-title>
<article-title xml:lang="en"><![CDATA[Carbon Content in Soils with Several Farming Uses in the Mexican Tropic]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sánchez-Hernández]]></surname>
<given-names><![CDATA[Rufo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ramos-Reyes]]></surname>
<given-names><![CDATA[Rodimiro]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Geissen]]></surname>
<given-names><![CDATA[Violette]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Mendoza-Palacios]]></surname>
<given-names><![CDATA[Juan de Dios]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cruz-Lázaro]]></surname>
<given-names><![CDATA[Efraín de la]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Salcedo-Pérez]]></surname>
<given-names><![CDATA[Eduardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Palma-López]]></surname>
<given-names><![CDATA[David J.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Juárez Autónoma de Tabasco DACA ]]></institution>
<addr-line><![CDATA[ Tabasco]]></addr-line>
<country>México</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,El Colegio de la Frontera Sur Unidad Villahermosa (ECOSUR) ]]></institution>
<addr-line><![CDATA[Villahermosa Tabasco]]></addr-line>
<country>México</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad de Guadalajara CUCEI ]]></institution>
<addr-line><![CDATA[Guadalajara Jalisco]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Colegio de Postgraduados Campus Tabasco ]]></institution>
<addr-line><![CDATA[Cárdenas Tabasco]]></addr-line>
<country>México</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>06</month>
<year>2011</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>06</month>
<year>2011</year>
</pub-date>
<volume>29</volume>
<numero>2</numero>
<fpage>211</fpage>
<lpage>219</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-57792011000200211&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-57792011000200211&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-57792011000200211&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN El suelo es un almacén de carbono (C) importante en la mitigación de los gases de efecto invernadero, debido a que protege físicamente la materia orgánica (MO). Por ello, se realizó un estudio en un Distrito de Temporal Tecnificado en la parte sur del estado de Tabasco para cuantificar el C asociado a suelos bajo diferentes usos. Se realizó una clasificación supervisada de imágenes satelitales para identificar los usos y tipos de suelos más frecuentes, se obtuvieron muestras de suelo a 0-15 cm y 15-30 cm; los resultados indicaron que los usos de suelo más frecuentes fueron: pastizales, plantaciones de eucalipto, cacao y cítricos y, áreas reducidas de piña y arroz. Los suelos predominantes en el área de estudio fueron los Vertisoles éutricos (VReu), Plintosoles dístricos (PTdy), Acrisoles plínticos (ACpl), Acrisoles húmicos (AChu) y Acrisoles gléyicos (ACgl), estos suelos difieren en el origen genético del material parental, edad y exposición al ambiente, sus características junto con el aporte de residuos orgánicos de cada uso de suelo, regularon la acumulación en el suelo de la materia orgánica (MO) y del C en ambas profundidades. La mayor acumulación de MO y C se registró en la superficie y decreció en un 36% a los 15 cm de profundidad. Los usos de suelo que mayor cantidad de MO y C acumularon fueron piña, cítricos, eucalipto y pasto; las menores cantidades fueron registradas en arroz, caña de azúcar y cacao. La mayor acumulación de MO y C se registró en cultivos establecidos en PTdy y ACpl, estos suelos presentan acidez que afectan estrechamente la descomposición de la MO. Los VReu y ACgl presentan alto porcentaje de arcilla y acidez (pH alrededor de cinco), condiciones que facilitan la degradación de la MO y no permite la acumulación de C en el perfil.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The soil is a store of carbon (C) very important in the mitigation of the greenhouse gases, due to the fact that it protects physically the organic matter (OM). For it, a study was realized in a Rain Technificated District in the South part of the Tabasco State, to quantify the C associated with soils under several uses. A supervised classification of satellite images was realized to identify the more frequent uses and soil classes, soil samples at 0-15 cm y 15-30 cm depth were obtained. The results indicated that the more frequent uses were: grassland, eucalyptus, cocoa and citric plantations and small areas of rice and pineapple. The predominant soils in the study area were the Eutric Vertisols (VReu), Distric Plintosols (PTdy), Plintic Acrisols (ACpl), Humic Acrisols (AChu) and Gleyic Acrisols (ACgl), these soils differ in the genetic origin of the parent material, age and environmental exposition; its characteristics together with the contribution of organic residues of each soil use, regulated the accumulation in the organic matter (OM) and C in both depths. The major OM and C accumulation were registered in the surface and decreased to 36% at 15 cm depth. The soil uses that accumulated OM and C were pineapple, citric, eucalyptus and grassland; the less account were registered in rice, sugarcane and cocoa. The major OM and C accumulation were registered in crops established on PTdy and ACpl, these soils present acidity that closely affect the OM decomposition. The VReu and ACgl present high clay content and, acidity around five; these conditions facilitate the OM decomposition and does not allow OC accumulation in the soil profile.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[materia orgánica del suelo]]></kwd>
<kwd lng="es"><![CDATA[acidez]]></kwd>
<kwd lng="es"><![CDATA[lomeríos]]></kwd>
<kwd lng="es"><![CDATA[aluvial]]></kwd>
<kwd lng="es"><![CDATA[arcilloso]]></kwd>
<kwd lng="en"><![CDATA[soil organic matter]]></kwd>
<kwd lng="en"><![CDATA[acidity]]></kwd>
<kwd lng="en"><![CDATA[highland]]></kwd>
<kwd lng="en"><![CDATA[alluvial]]></kwd>
<kwd lng="en"><![CDATA[clayey]]></kwd>
</kwd-group>
</article-meta>
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