<?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>S0035-001X2012000300013</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Application of the alpha spectrometry for the study of core sediment extracted in the San Marcos dam in Chihuahua]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Méndez García]]></surname>
<given-names><![CDATA[C.]]></given-names>
</name>
<xref ref-type="aff" rid="A01"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[García-Tenorio]]></surname>
<given-names><![CDATA[R.]]></given-names>
</name>
<xref ref-type="aff" rid="A02"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rentería Villalobos]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<xref ref-type="aff" rid="A01"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Montero Cabrera]]></surname>
<given-names><![CDATA[María Elena]]></given-names>
</name>
<xref ref-type="aff" rid="A01"/>
</contrib>
</contrib-group>
<aff id="A01">
<institution><![CDATA[,Centro de Investigación en Materiales Avanzados  ]]></institution>
<addr-line><![CDATA[Chihuahua Chih.]]></addr-line>
<country>México</country>
</aff>
<aff id="A02">
<institution><![CDATA[,Universidad de Sevilla ETS Arquitectura Applied Nuclear Physics Group]]></institution>
<addr-line><![CDATA[Seville ]]></addr-line>
<country>Spain</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>06</month>
<year>2012</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>06</month>
<year>2012</year>
</pub-date>
<volume>58</volume>
<numero>3</numero>
<fpage>234</fpage>
<lpage>237</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0035-001X2012000300013&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0035-001X2012000300013&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0035-001X2012000300013&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[The determination of the specific activities of 210Po and isotopic uranium by alpha spectrometry was performed in a sediment core from San Marcos Dam. The objective of this work was to analyze the vertical distribution of isotopic uranium and 210Po and the behavior of these radionuclides along sediment core collected from the San Marcos Dam. Sample was divided into 11 sections, in which 210Po and Isotopic Uranium were determined using liquid-liquid extraction with tributyl phosphate (TBP). Furthermore, it was made a comparison between the TBP technique and the technique of extraction chromatography using UTEVA resins for uranium. The results of specific activities for 210Po show a trend to decrease along the core, whereas the uranium isotopic does not show a pointed trend. The results of isotopic ratios between the 234U and 238U show that they are close to secular equilibrium in each of the core sections. The comparison between the two uranium extraction techniques indicates that chemical yield is better using the UTEVA technique than TBP extraction.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[La determinación de las actividades específicas de 210Po y uranio isotópico mediante espectrometría alfa fue realizada en un núcleo de sedimento de la Presa San Marcos. El objetivo de este trabajo fue analizar la distribución vertical de uranio isotópico y de 210Po así como el comportamiento de estos radionúclidos a lo largo del núcleo de sedimento recolectado en la presa San Marcos. La muestra fue dividida en 11 secciones. Para la determinación de 210Po y de uranio isotópico en cada una de las secciones se utilizó la técnica de extracción líquidol íquido con tributil fosfato (TBP). También se realizó una comparación entre la técnica del TBP y la técnica de cromatografía de extracción con resinas UTEVA para el uranio isotópico. Los resultados de las actividades específicas para 210Po muestran una tendencia decreciente a lo largo del núcleo, mientras que para uranio isotópico muestran una tendencia no monótona. Los resultados de las relaciones isotópicas entre el 234U y el 238U muestran estar cerca del equilibrio secular en cada una de las secciones del núcleo. La comparación entre las dos técnicas de extracción de uranio indica que se tiene un mayor rendimiento químico mediante empleando la técnica de UTEVA.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[alpha spectrometry]]></kwd>
<kwd lng="en"><![CDATA[uranium]]></kwd>
<kwd lng="en"><![CDATA[polonium]]></kwd>
<kwd lng="en"><![CDATA[sediment core]]></kwd>
<kwd lng="es"><![CDATA[Espectrometría alfa]]></kwd>
<kwd lng="es"><![CDATA[uranio]]></kwd>
<kwd lng="es"><![CDATA[polonio]]></kwd>
<kwd lng="es"><![CDATA[núcleo de sedimento]]></kwd>
</kwd-group>
</article-meta>
</front><body><![CDATA[ <p align="justify"><font face="verdana" size="4">F&iacute;sica de la radiaci&oacute;n</font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="center"><font face="verdana" size="4"><b>Application of the alpha spectrometry for the study of core sediment extracted in the San Marcos dam in Chihuahua</b></font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="center"><font face="verdana" size="2"><b>C. M&eacute;ndez Garc&iacute;a<sup>1</sup>, R. Garc&iacute;a&#45;Tenorio<sup>2</sup>, M. Renter&iacute;a Villalobos<sup>1</sup> and  Mar&iacute;a Elena Montero Cabrera<sup>1;*</sup></b></font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2"><i><sup>1</sup> Centro de Investigaci&oacute;n en Materiales Avanzados, CIMAV, Miguel de Cervantes 120, 31109, Chihuahua, Chih., M&eacute;xico. </i>Corresponding author: <a href="mailto:elena.montero@cimav.edu.mx">elena.montero@cimav.edu.mx</a></font></p>     <p align="justify"><font face="verdana" size="2"><i><sup>2</sup> Applied Nuclear Physics Group, Universidad de Sevilla, ETS Arquitectura,   Avda. Reina Mercedes s/n, 41012 Seville, Spain.</i> e&#45;mail: <a href="mailto:284700727@alumnos.fcfm.buap.mx">284700727@alumnos.fcfm.buap.mx</a></font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2">Recibido el 3 de junio de 2011;    ]]></body>
<body><![CDATA[<br> aceptado el 1 de febrero de 2012</font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2"><b>Abstract</b></font></p>     <p align="justify"><font face="verdana" size="2">The determination of the specific activities of <sup>210</sup>Po and isotopic uranium by alpha spectrometry was performed in a sediment core from San Marcos Dam. The objective of this work was to analyze the vertical distribution of isotopic uranium and <sup>210</sup>Po and the behavior of these radionuclides along sediment core collected from the San Marcos Dam. Sample was divided into 11 sections, in which <sup>210</sup>Po and Isotopic Uranium were determined using liquid&#45;liquid extraction with tributyl phosphate (TBP). Furthermore, it was made a comparison between the TBP technique and the technique of extraction chromatography using UTEVA resins for uranium. The results of specific activities for <sup>210</sup>Po show a trend to decrease along the core, whereas the uranium isotopic does not show a pointed trend. The results of isotopic ratios between the <sup>234</sup>U and <sup>238</sup>U show that they are close to secular equilibrium in each of the core sections. The comparison between the two uranium extraction techniques indicates that chemical yield is better using the UTEVA technique than TBP extraction.</font></p>     <p align="justify"><font face="verdana" size="2"><b>Keywords:</b> alpha spectrometry; uranium; polonium; sediment core.</font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2"><b>Resumen</b></font></p>     <p align="justify"><font face="verdana" size="2">La determinaci&oacute;n de las actividades espec&iacute;ficas de <sup>210</sup>Po y uranio isot&oacute;pico mediante espectrometr&iacute;a alfa fue realizada en un n&uacute;cleo de sedimento de la Presa San Marcos. El objetivo de este trabajo fue analizar la distribuci&oacute;n vertical de uranio isot&oacute;pico y de <sup>210</sup>Po as&iacute; como el comportamiento de estos radion&uacute;clidos a lo largo del n&uacute;cleo de sedimento recolectado en la presa San Marcos. La muestra fue dividida en 11 secciones. Para la determinaci&oacute;n de <sup>210</sup>Po y de uranio isot&oacute;pico en cada una de las secciones se utiliz&oacute; la t&eacute;cnica de extracci&oacute;n l&iacute;quidol &iacute;quido con tributil fosfato (TBP). Tambi&eacute;n se realiz&oacute; una comparaci&oacute;n entre la t&eacute;cnica del TBP y la t&eacute;cnica de cromatograf&iacute;a de extracci&oacute;n con resinas UTEVA para el uranio isot&oacute;pico. Los resultados de las actividades espec&iacute;ficas para <sup>210</sup>Po muestran una tendencia decreciente a lo largo del n&uacute;cleo, mientras que para uranio isot&oacute;pico muestran una tendencia no mon&oacute;tona. Los resultados de las relaciones isot&oacute;picas entre el <sup>234</sup>U y el <sup>238</sup>U muestran estar cerca del equilibrio secular en cada una de las secciones del n&uacute;cleo. La comparaci&oacute;n entre las dos t&eacute;cnicas de extracci&oacute;n de uranio indica que se tiene un mayor rendimiento qu&iacute;mico mediante empleando la t&eacute;cnica de UTEVA.</font></p>     <p align="justify"><font face="verdana" size="2"><b>Descriptores:</b> Espectrometr&iacute;a alfa; uranio; polonio; n&uacute;cleo de sedimento.</font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     ]]></body>
<body><![CDATA[<p align="justify"><font face="verdana" size="2">PACS: 91.67.Pq; 91.67.Qr; 91.67.Ty.</font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2"><a href="/pdf/rmf/v58n3/v58n3a13.pdf" target="_blank">DESCARGAR ART&Iacute;CULO EN FORMATO PDF</a></font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2"><b>Acknowledgments</b></font></p>     <p align="justify"><font face="verdana" size="2">The authors wish to thank the Autonomous University of Puebla for the financial support under project OSA&#45;EXC11&#45;G.</font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2"><b>References</b></font></p>     <!-- ref --><p align="justify"><font face="verdana" size="2">1. P.C. Goodell, in Technical Committee Meeting, Uranium deposits in volcanic rocks Vol. TC&#45;490/3. (STI/PUB/690), IAEA El Paso, Texas. , 1985, p. 97.    &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=8377951&pid=S0035-001X201200030001300001&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --></font></p>     ]]></body>
<body><![CDATA[<!-- ref --><p align="justify"><font face="verdana" size="2"> 2. H. Ferr&iacute;z, in <i>Technical Committee Meeting, Uranium deposits in volcanic rocks,</i> Vol. TC&#45;490/3. (STI/PUB/690), IAEA El   Paso, Texas, 1985, p. 197.    &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=8377953&pid=S0035-001X201200030001300002&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --></font></p>     <!-- ref --><p align="justify"><font face="verdana" size="2">3. M. Reyes&#45;Cortes, M.E. Montero&#45;Cabrera, M. Renteria&#45;   Villalobos, L. Fuentes&#45;Montero, L. Fuentes&#45;Cobas, E.F.   Herrera&#45;Peraza, H. Esparza&#45;Ponce, et al., Rev. Mex. Fis S. 53   (2007) 23.    &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=8377955&pid=S0035-001X201200030001300003&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --></font></p>     <!-- ref --><p align="justify"><font face="verdana" size="2">4. Manuel Reyes Cort&eacute;s, Caracterizaci&oacute;n de los minerales de   uranio del &aacute;rea de San Marcos, Chihuahua. Influencia hidrogeol&oacute;gica., Thesis in Doctor en Ciencia de Materiales, F&iacute;sica   de Materiales, Centro de Investigaci&oacute;n en Materiales Avanzados,   (2009)</font>&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=8377957&pid=S0035-001X201200030001300004&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --><!-- ref --><p align="justify"><font face="verdana" size="2">5. Manuel Reyes&#45;Cort&eacute;s, Luis Fuentes&#45;Cobas, Enrique Torres&#45;   Moye, Hilda Esparza&#45;Ponce, and Mar&iacute;a Montero&#45;Cabrera,   MinPe 99 (2010) 121.    &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=8377958&pid=S0035-001X201200030001300005&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --></font></p>     <!-- ref --><p align="justify"><font face="verdana" size="2">6. Marusia Renter&iacute;a Villalobos, Modelo conceptual de las concentraciones   de uranio en agua superficial y subterr&aacute;nea en la zona   de San Marcos&#45;Sacramento Thesis in Doctorado en Ciencia y   Tecnolog&iacute;a Ambiental, Medio Ambiente y Energ&iacute;a, Centro de   Investigaci&oacute;n en Materiales Avanzados, (2007)</font>&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=8377960&pid=S0035-001X201200030001300006&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --><!-- ref --><p align="justify"><font face="verdana" size="2">7. M. Renter&iacute;a Villalobos, M. Silva, M. Reyes, C. G. M&eacute;ndez,   D. Burciaga, E. F. Herrera, and M. E. Montero, in 10 International Conference on the Biogeochemistry of Trace Elements (ICOBTE), Centro de Investigaci&oacute;n en Materiales Avanzados, Chihuahua, M&eacute;xico, 2009.    &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=8377961&pid=S0035-001X201200030001300007&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --></font></p>     ]]></body>
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