<?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>S0187-57792024000100120</article-id>
<article-id pub-id-type="doi">10.28940/terra.v42i0.1877</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Speciation of Zn in Arid Soils with Saline Accumulations. Case Study of the Biskra Region, Algeria]]></article-title>
<article-title xml:lang="es"><![CDATA[Especiación del Zn en Suelos Áridos con Acumulaciones Salinas. Estudio de Caso de la Región de Biskra, Argelia]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Degui]]></surname>
<given-names><![CDATA[Nouara]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Djili]]></surname>
<given-names><![CDATA[Kaddour]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Daoud]]></surname>
<given-names><![CDATA[Youcef]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Belghemmaz]]></surname>
<given-names><![CDATA[Salah]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Higher National Agronomic School Soil Science Department ]]></institution>
<addr-line><![CDATA[ El Harrach]]></addr-line>
<country>Algeria</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,University Saad Dahleb Department of Biotechnology and Agro-ecology ]]></institution>
<addr-line><![CDATA[Blida Blida]]></addr-line>
<country>Algeria</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,University Ferhat Abbas Faculty of Natural Science and Life ]]></institution>
<addr-line><![CDATA[ Sétif]]></addr-line>
<country>Algeria</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2024</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2024</year>
</pub-date>
<volume>42</volume>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0187-57792024000100120&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0187-57792024000100120&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0187-57792024000100120&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Summary Zinc (Zn) deficiency in plants is closely related to its bioavailability in soil. However, the behaviour of Zn in soils, especially in saline areas, remains complex. This research aims to clarify the distribution and dominant forms of Zn in arid soils with salt accumulations from the Biskra region by studying soil samples from ten representative profiles. Soil samples were collected from different horizons of each profile to a depth of 120 cm and subjected to speciation analysis using sequential extraction. The results indicate a deficiency of Zn in all soil samples, resulting in reduced concentrations of different forms of Zn. The dominant forms were residual Zn (R-Zn) and oxide-bound Zn (O-Zn), which accounted for over 90% of total Zn. The study revealed a negative correlation between soil salinity and all Zn forms, except for R-Zn, which showed a positive correlation. Additionally, Zn concentrations showed a negative correlation with gypsum, except for exchangeable Zn (E-Zn). It is important to note that the presence of gypsum in soils was significantly and negatively correlated with O-Zn. Although the sequential extraction method used may have limitations in accurately quantifying all forms of Zn, this study fills a gap in the literature on Zn assessment and speciation in arid soils. The study emphasizes the significance of soil characteristics, particularly salinity and gypsum content, in shaping Zn distribution. Overall, these results contribute to a better understanding of Zn availability and mobility in arid and saline environments, providing valuable insights for improved soil management practices in such regions.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La deficiencia de Zinc (Zn) en las plantas está estrechamente relacionada con su biodisponibilidad en el suelo. Sin embargo, el comportamiento del Zn en los suelos, especialmente en zonas salinas, sigue siendo complejo. Esta investigación tiene como objetivo esclarecer la distribución y las formas predominantes de Zn en suelos áridos con acumulación de sal de la región de Biskra, mediante el estudio de muestras de suelo de diez perfiles representativos. Se recopilaron muestras de suelo de diferentes horizontes de cada perfil hasta una profundidad de 120 cm y se sometieron a análisis de especiación mediante extracción secuencial. Los resultados indican una deficiencia de Zn en todas las muestras de suelo, resultando en concentraciones reducidas de diferentes formas de Zn. Las formas dominantes fueron el Zn residual (R-Zn) y el Zn unido a óxidos (O-Zn), que representaron más del 90% del Zn total. Se encontró una correlación negativa entre la salinidad del suelo y las diferentes formas de Zn, excepto para el R-Zn, que mostró una correlación positiva. Además, las concentraciones de Zn mostraron una correlación negativa con el yeso, excepto para el Zn intercambiable (E-Zn). Cabe destacar que la presencia de yeso en los suelos se correlacionó significativa y negativamente con el O-Zn. Aunque el método de extracción secuencial utilizado puede tener limitaciones para cuantificar con precisión todas las formas de Zn, este estudio llena un vacío en la literatura sobre la evaluación y especiación del Zn en suelos áridos. Destaca la importancia de las características del suelo, en particular la salinidad y el contenido de yeso, en la conformación de la distribución del Zn. En resumen, estos resultados contribuyen a una mejor comprensión de la disponibilidad y movilidad del Zn en ambientes áridos y salinos, proporcionando información valiosa para mejorar las prácticas de gestión del suelo en estas regiones.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[dry lands]]></kwd>
<kwd lng="en"><![CDATA[gypsum-rich land]]></kwd>
<kwd lng="en"><![CDATA[micronutrient deficiency]]></kwd>
<kwd lng="en"><![CDATA[micronutrient distribution]]></kwd>
<kwd lng="en"><![CDATA[saline environment]]></kwd>
<kwd lng="es"><![CDATA[tierras secas]]></kwd>
<kwd lng="es"><![CDATA[tierras ricas en yeso]]></kwd>
<kwd lng="es"><![CDATA[carencia de micronutrientes]]></kwd>
<kwd lng="es"><![CDATA[distribución de micronutrientes]]></kwd>
<kwd lng="es"><![CDATA[entorno salino]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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