Cr-site preference of BaFe12-xCrxO19 hexaferrite ceramics monitored by Mössbauer spectroscopy
Site 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...
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th-cmuir.6653943832-52532014-08-30T02:56:19Z Cr-site preference of BaFe12-xCrxO19 hexaferrite ceramics monitored by Mössbauer spectroscopy Ounnunkad S. Phanichphant S. Winotai P. Tang I.-M. Site 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. 2014-08-30T02:56:19Z 2014-08-30T02:56:19Z 2007 Article 03701972 10.1002/pssb.200642123 http://www.scopus.com/inward/record.url?eid=2-s2.0-34250310485&partnerID=40&md5=71e8301ba50446eca66771b2cb879dd1 http://cmuir.cmu.ac.th/handle/6653943832/5253 English |
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Site 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. |
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Article |
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Ounnunkad S. Phanichphant S. Winotai P. Tang I.-M. |
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Ounnunkad S. Phanichphant S. Winotai P. Tang I.-M. Cr-site preference of BaFe12-xCrxO19 hexaferrite ceramics monitored by Mössbauer spectroscopy |
author_facet |
Ounnunkad S. Phanichphant S. Winotai P. Tang I.-M. |
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Ounnunkad S. |
title |
Cr-site preference of BaFe12-xCrxO19 hexaferrite ceramics monitored by Mössbauer spectroscopy |
title_short |
Cr-site preference of BaFe12-xCrxO19 hexaferrite ceramics monitored by Mössbauer spectroscopy |
title_full |
Cr-site preference of BaFe12-xCrxO19 hexaferrite ceramics monitored by Mössbauer spectroscopy |
title_fullStr |
Cr-site preference of BaFe12-xCrxO19 hexaferrite ceramics monitored by Mössbauer spectroscopy |
title_full_unstemmed |
Cr-site preference of BaFe12-xCrxO19 hexaferrite ceramics monitored by Mössbauer spectroscopy |
title_sort |
cr-site preference of bafe12-xcrxo19 hexaferrite ceramics monitored by mössbauer spectroscopy |
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2014 |
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http://www.scopus.com/inward/record.url?eid=2-s2.0-34250310485&partnerID=40&md5=71e8301ba50446eca66771b2cb879dd1 http://cmuir.cmu.ac.th/handle/6653943832/5253 |
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