<?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>0121-4470</journal-id>
<journal-title><![CDATA[Momento]]></journal-title>
<abbrev-journal-title><![CDATA[Momento]]></abbrev-journal-title>
<issn>0121-4470</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional de Colombia]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0121-44702018000100063</article-id>
<article-id pub-id-type="doi">10.15446/mo.n56.69826</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[CARACTERIZACIÓN MAGNÉTICA E HIPERFINA DE LA TRANSFORMACIÓN TÉRMICA CuO - Fe 2 O 3 A Fe 3 O 4]]></article-title>
<article-title xml:lang="en"><![CDATA[MAGNETIC AND HYPERFINE CHARACTERIZATION OF THE THERMAL TRANSFORMATION CuO - Fe 2 O 3 TO Fe 3 O 4]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Betancur]]></surname>
<given-names><![CDATA[Juan D.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Restrepo]]></surname>
<given-names><![CDATA[Johans]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Fernández]]></surname>
<given-names><![CDATA[Jhon J.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Perez]]></surname>
<given-names><![CDATA[Oswaldo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Escuela Colombiana de Ingeniería Julio Garavito Departamento de Ciencias Naturales ]]></institution>
<addr-line><![CDATA[Bogotá ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad de Antioquia Instituto de Física Grupo de Magnetismo y Simulación]]></institution>
<addr-line><![CDATA[Medellín ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad de Antioquia  ]]></institution>
<addr-line><![CDATA[Medellín ]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>06</month>
<year>2018</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>06</month>
<year>2018</year>
</pub-date>
<numero>56</numero>
<fpage>63</fpage>
<lpage>75</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S0121-44702018000100063&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S0121-44702018000100063&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S0121-44702018000100063&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Se presenta un estudio magnético acerca de la transformación térmica de hematita dopada con CuO (Fe2O3 + CuO). El tratamiento térmico se realizó a una temperatura de 375±1 oC, en una atmosfera controlada compuesta por 20% de hidrógeno y 80% de nitrógeno. Las muestras fueron caracterizadas por espectroscopia Mössbauer a temperatura ambiente, magnetización en función de la temperatura y ciclos de histeresis a 10K. Los resultados sugieren que los campos hiperfinos y los anchos de línea A y B permanecen esencialmente constantes con el aumento de la concentración de CuO, mientras que a la vez surge una componente paramagnética, lo cual es indicativo de la aparición de un precipitado o nueva fase de Fe - Cu, i.e. no hay una incorporación efectiva del cobre en la estructura de la magnetita. La magnetización de saturación cae aproximadamente de 87 emu/g a 78 emu/g, consistente con la presencia de dicha fase paramagnética. Se presenta también un aumento de la coerctividad desde ~576 Oe hasta ~621 Oe con el aumento del %CuO desde 2% hasta 20%. Tal aumento se atribuye también a dicha fase paramagnética actuando como centro de anclaje de las paredes de dominio, sumado al efecto de anclaje de las posibles vacancias inducidas por el tratamiento térmico. Finalmente, se observa una inversión de la magnetización en la temperatura de Verwey. Los datos sugieren que mediante el método de síntesis empleado se obtienen partículas de magnetita Fe3O4 coexistiendo con precipitados de Fe - Cu, lo cual modifica las propiedades magnéticas y genera un efecto interesante en la magnetización a la temperatura de Verwey.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract A magnetic study about the thermal transformation of hematite doped with CuO (Fe2O3 + CuO) is presented. The heat treatment was carried out at a temperature of 375±1 oC, in a controlled atmosphere composed by 20 % hydrogen and 80 % nitrogen. Samples were characterized by Mössbauer spectroscopy at room temperature, magnetization as a function of temperature and hysteresis loops at 10K. Our results suggest that both the hyperfine fields and linewidths of the A and B sites remain essentially constant with increasing the CuO concentration, while at the same time a paramagnetic component arises, which is indicative of the appearance of a precipitate or a new phase of Fe - Cu, i.e. there is not an effective incorporation of the copper into the structure of the magnetite. The saturation magnetization falls from approximately 87 emu/g to 78 emu/g, consistent with such a paramagnetic phase. Also, an increase in the coercivity from ~576 Oe up to ~621 Oe by increasing the percentage of CuO from 2 % up to 20 % is observed. Such increase is also attributed to the paramagnetic phase acting as pinning center for domain walls, besides also de pinning effect due to vacancies induced by the thermal treatment. Finally, an inversion of the magnetization in the Verwey temperature is observed. The data suggest that by means of the synthesis method employed, it is possible to obtain Fe3O4 magnetite particles coexisting with precipitates of Fe - Cu, giving rise to a modification in the magnetic properties and generating an interesting effect in the magnetization at the Verwey temperature.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Magnetita]]></kwd>
<kwd lng="es"><![CDATA[Hematita]]></kwd>
<kwd lng="es"><![CDATA[Espectroscopia Mössbauer]]></kwd>
<kwd lng="es"><![CDATA[Temperatura de Verwey]]></kwd>
<kwd lng="en"><![CDATA[Magnetite]]></kwd>
<kwd lng="en"><![CDATA[Hematite]]></kwd>
<kwd lng="en"><![CDATA[Mössbauer Spectroscopy]]></kwd>
<kwd lng="en"><![CDATA[Verwey Temperature]]></kwd>
</kwd-group>
</article-meta>
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