Formation and annealing of micropores in hematite.

dc.contributor.authorDauwe, C.
dc.contributor.authorCosta, Geraldo Magela da
dc.contributor.authorVan Hoecke, T.
dc.contributor.authorSegers, D.
dc.date.accessioned2017-05-30T15:23:39Z
dc.date.available2017-05-30T15:23:39Z
dc.date.issued1995
dc.description.abstractIn iron oxide powders positrons are trapped in the surface layers and the value of the S-parameter is an indicator of the total specific surface, including external surface and internal surfaces of micropores. The evolution of micropores is followed when α-FeOOH is thermally decomposed into α-Fe2O3 . It is shown that the micropore formation is not linked to the decomposition process, but that they also form in hematite synthesized from a ferrihydrite precursor in aqueous solution.pt_BR
dc.identifier.citationDAUWE, C. et al. Formation and annealing of micropores in hematite. Acta Physica Polonica A, v. 88, p. 119-123, 1995. Disponível em: <http://przyrbwn.icm.edu.pl/APP/PDF/88/a088z1p16.pdf>. Acesso em: 20 abr. 2017.pt_BR
dc.identifier.doihttp://dx.doi.org/10.12693/APhysPolA.88.119
dc.identifier.issn1898-749X
dc.identifier.urihttp://www.repositorio.ufop.br/handle/123456789/7826
dc.identifier.uri2http://przyrbwn.icm.edu.pl/APP/PDF/88/a088z1p16.pdfpt_BR
dc.language.isoen_USpt_BR
dc.rightsrestritopt_BR
dc.titleFormation and annealing of micropores in hematite.pt_BR
dc.typeArtigo publicado em periodicopt_BR

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