<?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>S0187-57792019000100035</article-id>
<article-id pub-id-type="doi">10.28940/tl.v37i1.367</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Efecto del uso del suelo en las formas y disponibilidad de fósforo de un Andisol de la Meseta P&#8217;urhépecha, Michoacán]]></article-title>
<article-title xml:lang="en"><![CDATA[Effects of land use on phosphorus fractions and availability in an Andisol from the P&#8217;urhépecha Plateau, Michoacán]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Bayuelo Jiménez]]></surname>
<given-names><![CDATA[Jeannette S.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ochoa]]></surname>
<given-names><![CDATA[Iván]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cruz Torres]]></surname>
<given-names><![CDATA[Eulogio de la]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Muraoka]]></surname>
<given-names><![CDATA[Takashi]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Michoacana de San Nicolás de Hidalgo Instituto de Investigaciones Agropecuarias y Forestales ]]></institution>
<addr-line><![CDATA[Tarímbaro Michoacán]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Unipalma de los Llanos S.A. Subdirección de Investigación y Desarrollo ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Instituto Nacional de Investigaciones Nucleares  ]]></institution>
<addr-line><![CDATA[Ocoyoacac Estado de México]]></addr-line>
<country>México</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Universidad de São Paulo Centro de Energía Nuclear para la Agricultura ]]></institution>
<addr-line><![CDATA[Piracicaba SP]]></addr-line>
<country>Brazil</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>35</fpage>
<lpage>44</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-57792019000100035&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-57792019000100035&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-57792019000100035&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Los Andisoles se distinguen por su habilidad para retener fósforo (P), lo cual restringe la productividad agrícola. Se planteó la hipótesis que la disponibilidad de P en las diferentes formas extraídas secuencialmente, variaría de acuerdo al uso del suelo y su intercambio dependería de las características químicas del mismo. En este estudio, se usaron los métodos de extracción secuencial y dilución isotópica para evaluar el efecto del uso del suelo y la adición de fertilizante en las fracciones inorgánicas y orgánicas de P y su disponibilidad. Se incluyeron muestras de suelo de un sitio con una larga historia de fertilización y otro de una área adyacente de bosque nativo, al cual se les aplicó KH2 32PO4. El suelo se fraccionó secuencialmente después de un periodo de 49 días de incubación y se determinó la proporción (%) de 32P recuperado en cada fracción. En todas las fracciones se recuperó 32P, lo que demuestra la existencia de intercambio entre el 32P y P natural del suelo. Las reacciones de intercambio ocurrieron mayormente en las fracciones inorgánicas. Las fracciones de resina-Pi, NaHCO3-Pi e NaOH0.1-Pi aumentaron con la fertilización de P, siendo la fracción de NaOH0.1-Pi, la mayor fuente del nutriente. El mayor incremento de 32P recuperado en la fracción de NaOH0.1-Pi, indica que el P añadido y transformado en esta fracción es altamente intercambiable y contribuye con la fertilidad de este suelo. Las fracciones recalcitrantes presentaron poco P intercambiable. En contraste, en el suelo de bosque sin fertilizar, más del 20% del 32P se recuperó en las fracciones de Bic-Po y NaOH-Po, 49 días después de que se añadió el radiotrazador. La transformación de las fracciones de P fue dependiente del tipo de suelo y la adición de P. El P aplicado permaneció, preferiblemente, en la forma que puede ser intercambiable con la solución del suelo y, por consiguiente, puede estar disponible para la planta.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Summary Andisols are distinguished by a high phosphorus (P) adsorption capacity, which is a restrictive factor for plant growth. This study, it was hypothesized that the availability of P in the different forms extracted sequentially, would vary according to the land use, and its exchange would depend on its chemical characteristics. For this purpose, sequential extraction and isotopic dilution techniques were utilized to measure the effect of land use systems and corresponding P fertilizer inputs on size of inorganic and organic P forms and their lability. An Andisol sample from a field site with a long history of P amendments and another sample from a contiguous forested area under natural vegetation were treated with applied KH2 32PO4. The soil samples were sequentially extracted for P fractions after 49 days (d) of incubation. Recovery of 32P in each P form was evaluated. The recovery of 32P in all soil P fractions exhibited that 32P had undergone exchange with the native P. The exchange reaction occurred mainly in the Pi fractions. Resin-Pi, Bic-Pi and NaOH-Pi were increased by P fertilization, with the greater level occurring for NaOH-Pi. The highest increase of the 32P recovered in the NaOH0.1-Pi fraction of the P-fertilized Andisol shows that the added P changed into this form stays highly exchangeable and contributes P fertility to this soil type. The recalcitrant inorganic fractions contained almost no exchangeable P. In contrast, in native soil with no P input, more than 20% of the 32P was recovered in Bic-Po and NaOH-Po forms 49 d after the labeled P was added. The change in soil P fraction was associated with soil type and P addition. Nonetheless, the applied P persisting in the fraction can be exchangeable with solution P and, hence, can be plant-available.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[fraccionamiento de Hedley]]></kwd>
<kwd lng="es"><![CDATA[radiotrazador]]></kwd>
<kwd lng="es"><![CDATA[intercambio isotópico]]></kwd>
<kwd lng="es"><![CDATA[fertilidad del suelo]]></kwd>
<kwd lng="en"><![CDATA[Hedley fractionation]]></kwd>
<kwd lng="en"><![CDATA[radioisotopic tracer]]></kwd>
<kwd lng="en"><![CDATA[isotopic exchange]]></kwd>
<kwd lng="en"><![CDATA[soil fertility]]></kwd>
</kwd-group>
</article-meta>
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