<?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>2007-9028</journal-id>
<journal-title><![CDATA[Ecosistemas y recursos agropecuarios]]></journal-title>
<abbrev-journal-title><![CDATA[Ecosistemas y recur. agropecuarios]]></abbrev-journal-title>
<issn>2007-9028</issn>
<publisher>
<publisher-name><![CDATA[Universidad Juárez Autónoma de Tabasco, Dirección de Investigación y Posgrado]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S2007-90282018000200283</article-id>
<article-id pub-id-type="doi">10.19136/era.a5nl4.1418</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Tasa de sedimentos en suspensión por efectos de un vertedor lateral en un río de planicie]]></article-title>
<article-title xml:lang="en"><![CDATA[Suspended sediment rate due to effects of a lateral spillway in a plain river]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rodríguez-Bastarmérito]]></surname>
<given-names><![CDATA[Roberto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Saiz-Hernández]]></surname>
<given-names><![CDATA[Juan Arcadio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Burgos-Flores]]></surname>
<given-names><![CDATA[Dagoberto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Guerra-Cobian]]></surname>
<given-names><![CDATA[Víctor Hugo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Lizarraga-Mendiola]]></surname>
<given-names><![CDATA[Liliana]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ortíz-Gómez]]></surname>
<given-names><![CDATA[Ruperto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Juárez Autónoma de Tabasco División Académica de Ingeniería y Arquitectura ]]></institution>
<addr-line><![CDATA[Cunduacán Tabasco]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad de Sonora  ]]></institution>
<addr-line><![CDATA[Hermosillo Sonora]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Autónoma de Nuevo León  ]]></institution>
<addr-line><![CDATA[San Nicolás de Los Garza Nuevo León]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Universidad Autónoma del Estado de Hidalgo  ]]></institution>
<addr-line><![CDATA[Pachuca de Soto Hidalgo]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af5">
<institution><![CDATA[,Universidad de Zacatecas  ]]></institution>
<addr-line><![CDATA[Zacatecas ]]></addr-line>
<country>Mexico</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>5</volume>
<numero>14</numero>
<fpage>283</fpage>
<lpage>291</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S2007-90282018000200283&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S2007-90282018000200283&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S2007-90282018000200283&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN: Los canales de desvío y vertedores laterales en un río de planicie, derivan los flujos líquidos excedentes, reduciendo los niveles y evitando el desbordamiento de los cauces, lo que mitiga las inundaciones. El estudio tuvo el objetivo de determinar la tasa de sedimentos en suspensión por efectos de un vertedor lateral en un río de planicie. El funcionamiento de estas estructuras cambia el comportamiento del flujo líquido y de los sedimentos que transporta en suspensión, provocando cambios en la morfología e hidrodinámica del cauce. Se utilizó un perfilador de flujo Doppler (ADCP) River Ray y un muestreador integral de sedimentos en suspensión US-DH59, para medir los flujos líquidos y sólidos en el río de la Sierra en el Estado de Tabasco, México y en el vertedor lateral El Censo. Los datos obtenidos en campo se utilizaron para evaluar los efectos del vertedor lateral sobre la hidrodinámica y morfología del cauce. Los resultados muestran que hay un incremento de 109.4% en la tasa de sedimentos en el flujo aguas abajo del vertedor y desequilibrio geomorfológico, lo que denotan una alteración al comportamiento natural del flujo bifásico compuesto por una fase de flujo líquido y otra de flujo de sedimentos.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT: Diversion canals and lateral spillways in a plain river divert surplus liquid flows, reducing the levels and avoiding the overflow of the channels, which mitigates flooding. The objective of the study was to determine the suspended sediment rate due to the effects of a lateral spillway in a plain river. The operation of these structures changes the behavior of the liquid flow and the sediments that it transports in suspension, causing changes in the morphology and hydrodynamics of the channel. A RiverRay Acoustic Doppler Current Profiler (ADCP) and a US-DH59 depth-integrating suspended sediment sampler were used to measure the liquid and solid flows in the Sierra River in the State of Tabasco, Mexico and in the El Censo lateral spillway. The data obtained in the field were used to evaluate the effects of the lateral spillway on the hydrodynamics and morphology of the channel. The results show a 109.4% increase in the sediment rate in the flow downstream of the spillway and geomorphological imbalance, which denote an alteration to the natural behavior of the biphasic flow composed of a liquid flow phase and a sediment flow one.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Flujo bifásico]]></kwd>
<kwd lng="es"><![CDATA[inundaciones]]></kwd>
<kwd lng="es"><![CDATA[hidrodinámica]]></kwd>
<kwd lng="es"><![CDATA[morfología]]></kwd>
<kwd lng="es"><![CDATA[transporte de sedimentos]]></kwd>
<kwd lng="en"><![CDATA[Biphasic flow]]></kwd>
<kwd lng="en"><![CDATA[floods]]></kwd>
<kwd lng="en"><![CDATA[hydrodynamics]]></kwd>
<kwd lng="en"><![CDATA[morphology]]></kwd>
<kwd lng="en"><![CDATA[sediment transport]]></kwd>
</kwd-group>
</article-meta>
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