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dc.contributor.authorSuriya Ounnunkaden_US
dc.contributor.authorSukon Phanichphanten_US
dc.contributor.authorPongtip Winotaien_US
dc.contributor.authorI. Ming Tangen_US
dc.date.accessioned2018-09-10T04:06:24Z-
dc.date.available2018-09-10T04:06:24Z-
dc.date.issued2007-06-01en_US
dc.identifier.issn15213951en_US
dc.identifier.issn03701972en_US
dc.identifier.other2-s2.0-34250310485en_US
dc.identifier.other10.1002/pssb.200642123en_US
dc.identifier.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=34250310485&origin=inwarden_US
dc.identifier.urihttp://cmuir.cmu.ac.th/jspui/handle/6653943832/61195-
dc.description.abstractSite preference of Cr in the M-type barium ferrite ceramics was monitored by powder X-ray diffraction (XRD), magnetization measurements and Mössbauer spectroscopy. The calcined BaFe12-xCrxO19 powders (x = 0.0-0.8) obtained by the sol gel method were die-pressed into pellets and then sintered at 1300°C in a oxygen atmosphere for 12 hrs. All the phases of the ceramics were of the pure magnetoplumbite structure. The saturation magnetization (Ms) is found to be a function of Cr ion content. The Ms of the ceramics decreases due to the dilution of the magnetic interaction with increasing Cr concentration. The coercivity (H c) of the ceramics increases due to finer grain observed by scanning electron microscopy (SEM). Fitted Mössbauer spectra show that Cr ions preferentially occupy into the 2a, 12k and 4f2 Fe crystallographic sites. © 2007 WILEY-VCH Verlag GmbH & Co. KGaA.en_US
dc.subjectMaterials Scienceen_US
dc.subjectPhysics and Astronomyen_US
dc.titleCr-site preference of BaFe<inf>12-x</inf>Cr<inf>x</inf>O<inf>19</inf> hexaferrite ceramics monitored by Mössbauer spectroscopyen_US
dc.typeJournalen_US
article.title.sourcetitlePhysica Status Solidi (B) Basic Researchen_US
article.volume244en_US
article.stream.affiliationsChiang Mai Universityen_US
article.stream.affiliationsMahidol Universityen_US
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