<?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>S0187-57792011000300249</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Movimiento vertical de fósforo en suelos arenosos con fertirriego y uso de mejoradores]]></article-title>
<article-title xml:lang="en"><![CDATA[Vertical Movement of Phosphorous in Sandy Soils with Fertirrigation and Use of Amendments]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Zamudio-González]]></surname>
<given-names><![CDATA[B.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Vázquez A.]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Alcántar González]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Etchevers Barra]]></surname>
<given-names><![CDATA[J. D.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Tadeo Robledo]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,INIFAP- Instituto Nacional de Investigaciones Forestales, Agrícolas y Pecuarias  ]]></institution>
<addr-line><![CDATA[ estado de México]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Autónoma Chapingo Departamento de Suelos ]]></institution>
<addr-line><![CDATA[ estado de México]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Colegio de Postgraduados  ]]></institution>
<addr-line><![CDATA[ estado de México]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,UNAM-FESC  ]]></institution>
<addr-line><![CDATA[ estado de México]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>09</month>
<year>2011</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>09</month>
<year>2011</year>
</pub-date>
<volume>29</volume>
<numero>3</numero>
<fpage>249</fpage>
<lpage>258</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-57792011000300249&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-57792011000300249&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-57792011000300249&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Se evaluó el desplazamiento de fósforo (P) en suelos arenosos al aplicar cinco fuentes de fertilizantes fosfóricos en fertirriego por goteo con agua alcalina de pozo y tratada con ácido sulfúrico y yeso agrícola conocida como aguayeso. La lixiviación y desplazamiento vertical de P se midió por triplicado en columnas verticales empacadas con suelos y subsuelos aluviales calcáreos colectados de terrenos cultivados con vid del noroeste de México. Los fertilizantes probados con la dosis de 50 mg L-1 en solución fueron: ácido fosfórico (H3PO4), fosfato monoamónico (NH4H2PO4, 11-52-0), polifosfato de amonio líquido (10-34-0), Poly-Feed® (15-31-15) y Fertigro® (fertilizante fosfórico líquido mezclado con sustancias húmicas). Se consideraron dos procesos de riego simulado a la profundidad de 0.7 m: el primero para saturar con y sin aguayeso y sin fertilizantes para obtener cinco fracciones de lavado para medir cambios de pH y sales; y un segundo proceso propio del fertirriego con las cinco fuentes fosfóricas para medir lixiviados y el P extractable con H2SO4 0.25 M en siete secciones de 0.1 m de las columnas. Al final del proceso de riego de lavado, las fracciones de drenaje acusaron valores de pH mayores a 8.5, incluso al regar con agua tratada con Am, condición propicia para la precipitación de P. No hubo diferencia estadística de lixiviados solubles de P al aplicar las cinco fuentes fertilizantes. Por balance de masas se encontró que el riego con aguayeso (Am) redujo 40% la disponibilidad de P en las columnas de suelo y 57% en los subsuelos. La mayor disponibilidad promedio de P en la columna y su mayor desplazamiento al regarse con agua alcalina en ambos medios porosos se obtuvo con H3PO4, seguido por NH4H2PO4 y polifosfato de amonio líquido.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract In triplicate vertical columns in the laboratory, packed with calcareous alluvial soil and subsoil collected from fields cultivated with vineyards in the northwestern of Mexico, the displacement of five sources of phosphorus (P) fertilizer were evaluated by drip fertigation associated with well water untreated and treated with sulfuric acid and agricultural gypsum. The tested fertilizer dose of 50 mg L-1 P in solution were: phosphoric acid (H3PO4), monoamonic phosphate NH4H2PO4 (11-52-0), liquid poly ammonium phosphate (10-34-0), Poly- Feed® (15-31-15) and Fertigro® (liquid phosphoric fertilizer mixed with humic substances). It was considered two simulated irrigation processes in columns of 0.7 m depth: first, porous media were saturated with and without treated water and no fertilizers to obtain five wash fractions to measure pH and salts changes; and a second process, fertigation with five sources for measuring P leached and retained into seven sections of 0.1 m of the columns. The results obtained were: first, at the end of washing process, drainage fractions accused pH values higher than 8.5, even with amended water (Am), a favorable condition to the P precipitation; second, there were no leachates soluble of P when supplying the five fertilizer sources; third, the treated water with agricultural gypsum and sulfuric acid, reduced the availability of P in soil columns by 40% and in the subsoil by 57%; fourth, the availability of P increased when the columns were watered with alkaline water in both porous media was obtained with H3PO4, followed by NH4H2PO4 and by liquid poly-ammonium phosphate.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[lixiviación]]></kwd>
<kwd lng="es"><![CDATA[riego por goteo]]></kwd>
<kwd lng="es"><![CDATA[calidad de agua]]></kwd>
<kwd lng="es"><![CDATA[medios porosos]]></kwd>
<kwd lng="en"><![CDATA[leaching]]></kwd>
<kwd lng="en"><![CDATA[drip irrigation]]></kwd>
<kwd lng="en"><![CDATA[water quality]]></kwd>
<kwd lng="en"><![CDATA[and porous media]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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