<?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>1405-3322</journal-id>
<journal-title><![CDATA[Boletín de la Sociedad Geológica Mexicana]]></journal-title>
<abbrev-journal-title><![CDATA[Bol. Soc. Geol. Mex]]></abbrev-journal-title>
<issn>1405-3322</issn>
<publisher>
<publisher-name><![CDATA[Sociedad Geológica Mexicana A.C.]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1405-33222019000100011</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2019v71n1a2</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[A micromorphological analysis for quantifying structure descriptors in a young constructed technosol]]></article-title>
<article-title xml:lang="es"><![CDATA[Análisis micromorfológico para cuantificar descriptores estructurales en un tecnosol construido reciente]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Watteau]]></surname>
<given-names><![CDATA[Françoise]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Jangorzo]]></surname>
<given-names><![CDATA[Nouhou Salifou]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Schwartz]]></surname>
<given-names><![CDATA[Christophe]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Laboratoire Sols et Environnement  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>France</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Université Dan Dicko Dankoulodo de Maradi  ]]></institution>
<addr-line><![CDATA[ Maradi]]></addr-line>
<country>Niger</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2019</year>
</pub-date>
<volume>71</volume>
<numero>1</numero>
<fpage>11</fpage>
<lpage>20</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222019000100011&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222019000100011&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222019000100011&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Evaluating soil structure dynamics is a major challenge when analysing or modelling pedogenesis. Constructed Technosols are considered, by definition, to be good candidates for pedogenetic studies, insofar as their initial characteristics and implementation conditions are controlled. Thus, we developed an approach based on image analysis of soil microstructures in order to specify the structure dynamics of a constructed Technosol. We described and quantified porosity and aggregation descriptors on a microscale (1) from pictures of mesocosms performed during 14 months, using an innovative automatic high-resolution image-acquisition device (Soilinsight®), and (2) from thin sections sampled in situ in a 1 ha field experiment at t0 and t2 (17 months). Plant root system architecture of Lupinus albus and the behavior of introduced earthworms (Lumbricus castaneus) were described using the Soilinsight®device. After 14 months, the pore surface was 10 times greater in the presence of plants and macrofauna than in the control samples. Although the biological activity promoted the genesis of aggregates, their dynamics were irregular. In fact, the proportion of aggregates varied depending on both root age and worm action. In situ, the soil was progressively compacted due to a significant decrease in the number of &gt;2000 µm pores. In the same way, three aggregate descriptors-number, area and shape-were selected as the most significant indicators of soil aggregation evolution during the early stages of pedogenesis. In conclusion, this approach, based on the quantification of microstructure parameters, did indeed allow the description and monitoring of 2D soil structure dynamics in both field and mesocosms conditions. Completed with 3D soil structure data, this micromorphological analysis could advantageously contribute to the impact of climatic and biological agents modelling on a structural evolution of Technosols during initial pedogenesis.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La evaluación de la dinámica estructural del suelo es una de las principales dificultades para analizar o modelar edafogénesis. Los Tecnosuelos construidos son considerados, por definición, como buenos candidatos para el estudio de la edafogénesis, ya que tanto sus características iniciales como las condiciones de implementación están controladas. Así, desarrollamos un enfoque basado en el análisis de imagen de las microestructuras del suelo para especificar la dinámica estructural de un Tecnosuelo construido. Describimos y cuantificamos los descriptores de porosidad y agregación a microescala en (1) imágenes captadas de un experimento en mesocosmos desarrollado durante 14 meses, mediante la utilización de un sistema innovador para la adquisición automática de imágenes de alta resolución (Soilinsight®) y en (2) láminas delgadas muestreadas in situ en una parcela experimental de 1 ha a t0 y t2 (17 meses). La arquitectura del sistema radical de Lupinus albus y el comportamiento de las lombrices (Lumbricus castaneus) introducidas en los mesocosmos fueron descritos gracias al sistema Soilinsight®. Después de 14 meses, la superficie de los poros es 10 veces mayor en presencia de plantas y macrofauna que en los controles. Si bien la actividad biológica promovió la formación de los agregados, su dinámica fue irregular. De hecho, la proporción de agregados varió en función de la edad de las raíces y de la acción de las lombrices. In situ, el suelo ha sufrido una compactación progresiva debido a una disminución significativa del número de poros &gt; 2000 µm. De la misma forma, tres descriptores de los agregados -número, área y forma- han sido seleccionados como los indicadores más significativos de la evolución de la agregación del suelo durante las fases tempranas de la edafogénesis. En conclusión, el enfoque basado en la cuantificación de parámetros microestructurales ha permitido la descripción y monitoreo en 2D de la dinámica estructural del suelo en condiciones de campo y de mesocosmos. Este análisis micromorfológico, combinado con datos de la estructura del suelo en 3D, puede contribuir a la modelación del impacto de agentes climáticos y biológicos sobre la evolución estructural de Tecnosuelos durante las primeras fases de la edafogénesis.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[micropedology]]></kwd>
<kwd lng="en"><![CDATA[biological activity]]></kwd>
<kwd lng="en"><![CDATA[structure dynamics]]></kwd>
<kwd lng="en"><![CDATA[image analysis]]></kwd>
<kwd lng="en"><![CDATA[Soilinsight®]]></kwd>
<kwd lng="es"><![CDATA[microedafología]]></kwd>
<kwd lng="es"><![CDATA[actividad biológica]]></kwd>
<kwd lng="es"><![CDATA[dinámica estructural]]></kwd>
<kwd lng="es"><![CDATA[análisis de imagen]]></kwd>
<kwd lng="es"><![CDATA[Soilinsight®]]></kwd>
</kwd-group>
</article-meta>
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