<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-04-14T07:17:54Z</responseDate><request verb="GetRecord" identifier="oai:www.recercat.cat:2445/32225" metadataPrefix="oai_dc">https://recercat.cat/oai/request</request><GetRecord><record><header><identifier>oai:recercat.cat:2445/32225</identifier><datestamp>2025-11-19T20:27:17Z</datestamp><setSpec>com_2072_1057</setSpec><setSpec>col_2072_478822</setSpec><setSpec>col_2072_478917</setSpec><setSpec>col_2072_478923</setSpec></header><metadata><oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
   <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:identifier>0021-8979</dc:identifier>
   <dc:identifier>https://hdl.handle.net/2445/32225</dc:identifier>
   <dc:identifier>080535</dc:identifier>
   <dc:language>eng</dc:language>
   <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:format>7 p.</dc:format>
   <dc:format>application/pdf</dc:format>
   <dc:format>application/pdf</dc:format>
   <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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