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               <dc:title>Cation distribution and magnetization of BaFe12-2xCoxSnxO19 (x=0.9,1.28) single crystals</dc:title>
               <dc:creator>Sandiumenge Ortiz, Felip</dc:creator>
               <dc:creator>Martínez Perea, Benjamin</dc:creator>
               <dc:creator>Batlle Gelabert, Xavier</dc:creator>
               <dc:creator>Galí Medina, Salvador, 1949-</dc:creator>
               <dc:creator>Obradors, Xavier</dc:creator>
               <dc:subject>Materials</dc:subject>
               <dc:subject>Propietats magnètiques</dc:subject>
               <dc:subject>Estructura cristal·lina (Sòlids)</dc:subject>
               <dc:subject>Materials</dc:subject>
               <dc:subject>Magnetic properties</dc:subject>
               <dc:subject>Layer structure (Solids)</dc:subject>
               <dc:description>The distribution of Sn4+ cations within the five crystallographic sites of the magnetoplumbite (M) ‐like compound BaFe12−2xCoxSnxO19 has been analyzed using single‐crystal x‐ray‐diffraction data. The species Fe3+ and Co2+ cannot be distinguished using x rays because of their very similar atomic numbers; however, the calculation of the apparent valencies for the different sites allows an insight into the Co2+ cation segregation. The use of previous data from neutron powder diffraction allows a precise picture of the cation distribution, which indicates a pronounced site selectivity for both Sn4+ and Co2+ cations. The Sn4+ cations prefer the 4f2 sites and to a much lower extent the 12k sites, while they do not enter the octahedral 2a sites at all. Co2+ cations are distributed among tetrahedral and octahedral sites displaying a clear preference for the tetrahedral 4f1 sites. Magnetic measurements indicate that the compound still exhibits uniaxial anisotropy with the easy direction parallel to the c axis. Nevertheless, the magnetic structure shows a considerable degree of noncolinearity. A strong reduction of the magnetic anisotropy regarding that of the undoped compound is also detected.</dc:description>
               <dc:date>2012-10-09T07:54:06Z</dc:date>
               <dc:date>2012-10-09T07:54:06Z</dc:date>
               <dc:date>1992</dc:date>
               <dc:date>2012-10-09T07:54:06Z</dc:date>
               <dc:type>info:eu-repo/semantics/article</dc:type>
               <dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
               <dc:relation>Reproducció del document publicat a: http://dx.doi.org/10.1063/1.352359</dc:relation>
               <dc:relation>Journal of Applied Physics, 1992, vol. 72, num. 10, p. 4608-4614</dc:relation>
               <dc:relation>http://dx.doi.org/10.1063/1.352359</dc:relation>
               <dc:rights>(c) American Institute of Physics , 1992</dc:rights>
               <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
               <dc:publisher>American Institute of Physics</dc:publisher>
               <dc:source>Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)</dc:source>
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