Temperature dependence of the hyperfine parameters of maghemite and Al-substituted maghemites.

dc.contributor.authorCosta, Geraldo Magela da
dc.contributor.authorGrave, Eddy De
dc.contributor.authorBowen, L. H.
dc.contributor.authorBakker, P. M. A. de
dc.contributor.authorVandenberghe, Robert Emile
dc.date.accessioned2017-05-30T15:01:40Z
dc.date.available2017-05-30T15:01:40Z
dc.date.issued1995
dc.description.abstractSynthetic aluminum-substituted maghemite samples, 7-(AlyFel_y)203, with y = 0, 0.032, 0.058, 0.084, 0.106 and 0.151 have been studied by M6ssbauer spectroscopy at 8 K and in the range 80 K to 475 K at steps of 25 K. The spectra have been analysed as a superposition of two sextets composed of asymmetrical Lorentzians. The A- and B-site isomer shifts were constrained as: 6A---- 6B-- 0.12 mm/s. From the temperature dependence of 6B it was possible to determine the characteristic M6ssbauer temperature and the intrinsic shift. Both quantities clearly increase with increasing A1 content, at least up to 10 mole%. The temperature dependence of the Aand B-sites hyperfine fields could be satisfactorily reproduced using the molecular-field theory assuming an antiparallel spin configuration. The exchange integrals were found as: JAB = --25 K; JAA = --18 K and JBB= --3 K. The hyperfine fields show a crossing in the vicinity of 300 K as a result of the relatively strong A-A interaction. The Curie temperature for the non-substituted sample was calculated to be 930 K and decreases to 765 K for the sample with 15 mol% A1. The gradual decrease of the saturation value of the A-site hyperfine field with increasing A1 substitution and the constancy of this quantity for the B sites, suggest that the A1 cations occupy the B sites.pt_BR
dc.identifier.citationCOSTA, G. M. da et al. Temperature dependence of the hyperfine parameters of maghemite and Al-substituted maghemites. Physics and Chemistry of Minerals, v. 22, p. 178-185, 1995. Disponível em: <https://link.springer.com/article/10.1007/BF00202298>. Acesso em: 20 abr. 2017.pt_BR
dc.identifier.doihttps://doi.org/10.1007/BF00202298
dc.identifier.issn1432-2021
dc.identifier.urihttp://www.repositorio.ufop.br/handle/123456789/7823
dc.identifier.uri2https://link.springer.com/article/10.1007/BF00202298pt_BR
dc.language.isoen_USpt_BR
dc.rightsrestritopt_BR
dc.titleTemperature dependence of the hyperfine parameters of maghemite and Al-substituted maghemites.pt_BR
dc.typeArtigo publicado em periodicopt_BR

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