<?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>S0035-001X2003000400008</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Heat transfer in asymmetric convective cooling and optimized entropy generation rate]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ibáñez]]></surname>
<given-names><![CDATA[G.]]></given-names>
</name>
<xref ref-type="aff" rid="A01"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cuevas]]></surname>
<given-names><![CDATA[S.]]></given-names>
</name>
<xref ref-type="aff" rid="A01"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[López de Haro]]></surname>
<given-names><![CDATA[M.]]></given-names>
</name>
<xref ref-type="aff" rid="A01"/>
</contrib>
</contrib-group>
<aff id="A01">
<institution><![CDATA[,Universidad Nacional Autónoma de México Centro de Investigación en Energía ]]></institution>
<addr-line><![CDATA[Temixco Morelos]]></addr-line>
<country>México</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>08</month>
<year>2003</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>08</month>
<year>2003</year>
</pub-date>
<volume>49</volume>
<numero>4</numero>
<fpage>338</fpage>
<lpage>343</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0035-001X2003000400008&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0035-001X2003000400008&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0035-001X2003000400008&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[The steady viscous flow between two infinite parallel planes, is used to illustrate the possibility of minimizing the global entropy generation rate by cooling the external surfaces convectively in an asymmetric way. The flow is generated by both an axial pressure gradient and the uniform motion of the upper surface (generalized Couette flow). The temperature field is determined using boundary conditions of the third kind. The analytic expressions for the velocity and temperature fields of the fluid are used to calculate the global entropy generation rate explicitly. In dimensionless terms, this function depends on the dimensionless ratio of the two possible velocity scales (characterized by the magnitudes of the pressure gradient and the upper surface velocity), the dimensionless ambient temperature and the convective heat transfer coefficients (Biot numbers) of each surface which, in general, are not assumed to be the same. When the Biot numbers for each surface are equal, the entropy generation rate shows a monotonic increase. However, when the Biot numbers are different this function displays a minimum for specific cooling conditions. Besides, we calculate the local Nusselt number at the upper wall for minimum entropy generation conditions.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Se estudia el flujo de un fluido viscoso entre dos planos paralelos infinitos con el objetivo de ilustrar la posibilidad de minimizar la producción global de entropía a través del enfriamiento asimétrico por convección del sistema. El flujo se debe a un gradiente de presión axial y al movimiento uniforme del plano o pared superior del sistema (flujo de Couette generalizado). El campo de temperatura se determina usando condiciones de frontera del tercer tipo. Las expresiones analíticas de los campos de velocidad y temperatura del fluido se utilizan para calcular explícitamente la producción global de entropía del sistema. Esta función, expresada en forma adimensional, depende de la razón de las dos posibles escalas de velocidad (una caracterizada por la magnitud del gradiente de presión y la otra por la velocidad del plano superior), de la temperatura ambiente adimensional y de los coeficientes de transferencia de calor por convección de cada plano (números de Biot), los que, en general, se consideran distintos. Cuando los números de Biot de cada superficie son iguales, la producción global de entropía tiene un comportamiento monótono creciente; sin embargo, cuando los números de Biot son diferentes, esta función muestra un mínimo para condiciones de enfriamiento específicas. Además, se calculó el número local de Nusselt de la pared superior para condiciones de mínima disipación de energía.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Entropy generation minimization]]></kwd>
<kwd lng="en"><![CDATA[optimization]]></kwd>
<kwd lng="en"><![CDATA[heat transfer]]></kwd>
<kwd lng="es"><![CDATA[Minimización de la producción de entropía]]></kwd>
<kwd lng="es"><![CDATA[optimización]]></kwd>
<kwd lng="es"><![CDATA[transferencia de calor]]></kwd>
</kwd-group>
</article-meta>
</front><body><![CDATA[ <p align="justify"><font face="verdana" size="4">Investigaci&oacute;n</font></p>  	    <p align="justify">&nbsp;</p>     <p align="center"><font face="verdana" size="4"><b>Heat transfer in asymmetric convective cooling and optimized entropy generation rate</b></font></p>          <p align="center">&nbsp;</p>     <p align="center"><font face="verdana" size="2"><b>G. Ib&aacute;&ntilde;ez*, S. Cuevas and M. L&oacute;pez de Haro</b></font></p>          <p align="justify">&nbsp;</p>     <p align="justify"><font face="verdana" size="2"><i>Centro de Investigaci&oacute;n en Energ&iacute;a, Universidad Nacional Aut&oacute;noma de M&eacute;xico, Apartado Postal 34, Temixco, Mor. 62580, M&eacute;xico,</i> *e&#45;mail: <a href="mailto:gid@cie.unam.mx">gid@cie.unam.mx</a></font></p>           <p align="justify">&nbsp;</p>     <p align="justify"><font face="verdana" size="2">Recibido el 27 de noviembre de 2002.    <br>     Aceptado el 13 de enero de 2003.</font></p>       ]]></body>
<body><![CDATA[<p align="justify">&nbsp;</p>     <p align="justify"><font face="verdana" size="2"><b>Abstract</b></font></p>       <p align="justify"><font face="verdana" size="2">The steady viscous flow between two infinite parallel planes, is used to illustrate the possibility of minimizing the global entropy generation rate by cooling the external surfaces convectively in an asymmetric way. The flow is generated by both an axial pressure gradient and the uniform motion of the upper surface (generalized Couette flow). The temperature field is determined using boundary conditions of the third kind. The analytic expressions for the velocity and temperature fields of the fluid are used to calculate the global entropy generation rate explicitly. In dimensionless terms, this function depends on the dimensionless ratio of the two possible velocity scales (characterized by the magnitudes of the pressure gradient and the upper surface velocity), the dimensionless ambient temperature and the convective heat transfer coefficients (Biot numbers) of each surface which, in general, are not assumed to be the same. When the Biot numbers for each surface are equal, the entropy generation rate shows a monotonic increase. However, when the Biot numbers are different this function displays a minimum for specific cooling conditions. Besides, we calculate the local Nusselt number at the upper wall for minimum entropy generation conditions.</font></p>        <p align="justify"><font face="verdana" size="2"><b>Keywords:</b> Entropy generation minimization; optimization; heat transfer.</font></p>        <p align="justify">&nbsp;</p>      <p align="justify"><font face="verdana" size="2"><b>Resumen</b></font></p>        <p align="justify"><font face="verdana" size="2">Se estudia el flujo de un fluido viscoso entre dos planos paralelos infinitos con el objetivo de ilustrar la posibilidad de minimizar la producci&oacute;n global de entrop&iacute;a a trav&eacute;s del enfriamiento asim&eacute;trico por convecci&oacute;n del sistema. El flujo se debe a un gradiente de presi&oacute;n axial y al movimiento uniforme del plano o pared superior del sistema (flujo de Couette generalizado). El campo de temperatura se determina usando condiciones de frontera del tercer tipo. Las expresiones anal&iacute;ticas de los campos de velocidad y temperatura del fluido se utilizan para calcular expl&iacute;citamente la producci&oacute;n global de entrop&iacute;a del sistema. Esta funci&oacute;n, expresada en forma adimensional, depende de la raz&oacute;n de las dos posibles escalas de velocidad (una caracterizada por la magnitud del gradiente de presi&oacute;n y la otra por la velocidad del plano superior), de la temperatura ambiente adimensional y de los coeficientes de transferencia de calor por convecci&oacute;n de cada plano (n&uacute;meros de Biot), los que, en general, se consideran distintos. Cuando los n&uacute;meros de Biot de cada superficie son iguales, la producci&oacute;n global de entrop&iacute;a tiene un comportamiento mon&oacute;tono creciente; sin embargo, cuando los n&uacute;meros de Biot son diferentes, esta funci&oacute;n muestra un m&iacute;nimo para condiciones de enfriamiento espec&iacute;ficas. Adem&aacute;s, se calcul&oacute; el n&uacute;mero local de Nusselt de la pared superior para condiciones de m&iacute;nima disipaci&oacute;n de energ&iacute;a.</font></p>       <p align="justify"><font face="verdana" size="2"><b>Palabras clave:</b> Minimizaci&oacute;n de la producci&oacute;n de entrop&iacute;a; optimizaci&oacute;n; transferencia de calor.</font></p>        <p align="justify"><font face="verdana" size="2">PACS: 05.70.Ln; 44.27.+g; 47.27.Te</font></p>      <p align="justify">&nbsp;</p>     ]]></body>
<body><![CDATA[<p align="justify"><font face="verdana" size="2"><a href="/pdf/rmf/v49n4/v49n4a8.pdf" target="_blank">DESCARGAR ART&Iacute;CULO EN FORMATO PDF</a></font></p>        <p align="justify">&nbsp;</p>      <p align="justify"><font face="verdana" size="2"><b>Acknowledgments</b></font></p>       <p align="justify"><font face="verdana" size="2">This research was supported by DGAPA&#45;UNAM under project IN103100. G. Ib&aacute;&ntilde;ez thankfully acknowledges financial support from DGIA&#45;UNAM.</font></p>        <p align="justify">&nbsp;</p>      <p align="justify"><font face="verdana" size="2"><b>References</b></font></p>       <!-- ref --><p align="justify"><font face="verdana" size="2">1. A. Bejan, <i>Entropy Generation through Heat and Fluid Flow,</i> (Wiley, New York, 1994).    &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=8296316&pid=S0035-001X200300040000800001&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">2. A. C. Baytas, <i>J. Non&#45;Equilib. Thermodyn.</i> 22 (1997) 145.    &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=8296318&pid=S0035-001X200300040000800002&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --></font></p>        ]]></body>
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