<?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>0035-001X</journal-id>
<journal-title><![CDATA[Revista mexicana de física]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. mex. fis.]]></abbrev-journal-title>
<issn>0035-001X</issn>
<publisher>
<publisher-name><![CDATA[Sociedad Mexicana de Física]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0035-001X2018000200197</article-id>
<article-id pub-id-type="doi">10.31349/revmexfis.64.197</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Sobre la relación entre las distribuciones de los tamaños de poros y partículas del suelo]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[López-Lambraño]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Fuentes]]></surname>
<given-names><![CDATA[C.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[López-Ramos]]></surname>
<given-names><![CDATA[A.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Autónoma de Baja California Facultad de Ingeniería, Arquitectura y Diseño ]]></institution>
<addr-line><![CDATA[Ensenada Baja California]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Instituto Mexicano de Tecnología del Agua  ]]></institution>
<addr-line><![CDATA[Jiutepec Morelos]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Pontificia Bolivariana Facultad de Ingeniería Civil Escuela de Ingenierías y Arquitectura]]></institution>
<addr-line><![CDATA[ Córdoba]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>04</month>
<year>2018</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>04</month>
<year>2018</year>
</pub-date>
<volume>64</volume>
<numero>2</numero>
<fpage>197</fpage>
<lpage>205</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0035-001X2018000200197&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0035-001X2018000200197&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0035-001X2018000200197&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Las curvas porosimétrica y granulométrica del suelo son relacionadas bajo el supuesto de una relación de vacíos constante en las diferentes escalas y una relación entre los tamaños de poro y partícula en un empaquetamiento dado. En la relación entre los tamaños de poro y partícula se hace intervenir un factor de alargamiento de las partículas basado en el modelo de Arya y Paris o un factor de tortuosidad de las trayectorias de flujo basado en el modelo de Fuentes. Puesto que la curva porosimétrica está asociada a una curva de retención de humedad del suelo, la relación propuesta puede ser utilizada para estimar esta última a partir de la curva granulométrica. La relación entre las curvas es validada en algunos suelos reportados en la literatura, con buenos resultados.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The particle and void sizes distributions of the soil are related with the assumption that a void constant relationship at all different scales and a relationship between pore and particle size of a given packing. In the relationship between pore and particle sizes, a particle elongation factor is applied based on the Arya and Paris model. A flow trajectory tortuosity factor based on the Fuentes model can also be applied. Since the void size distribution is associated to the soil water retention curve, the proposed relationship can be used to estimate this curve from particle size distribution.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Porosidad areal]]></kwd>
<kwd lng="es"><![CDATA[porosidad volumétrica]]></kwd>
<kwd lng="es"><![CDATA[relación fractal área-volumen]]></kwd>
<kwd lng="es"><![CDATA[factor de tortuosidad]]></kwd>
<kwd lng="es"><![CDATA[probabilidad conjunta]]></kwd>
<kwd lng="en"><![CDATA[Areal porosity]]></kwd>
<kwd lng="en"><![CDATA[volumetric porosity]]></kwd>
<kwd lng="en"><![CDATA[fractal area-volume relationship]]></kwd>
<kwd lng="en"><![CDATA[tortuosity factor]]></kwd>
<kwd lng="en"><![CDATA[joint probability]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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