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dc.contributor.authorSoares, Robson de Mirandapt_BR
dc.contributor.authorSabioni, Antônio Claret Soarespt_BR
dc.contributor.authorResck, Inês Sabionipt_BR
dc.contributor.authorFalcomer, Viviane Aparecida Silvapt_BR
dc.contributor.authorDias, José Alvespt_BR
dc.contributor.authorSilva, Naira Machado dapt_BR
dc.contributor.authorMenezes, Sônia Maria Cabral dept_BR
dc.contributor.authorCosta, Geraldo Magela dapt_BR
dc.date.accessioned2017-12-07T04:48:30Z-
dc.date.available2017-12-07T04:48:30Z-
dc.date.issued2007-03pt_BR
dc.identifier.citationSOARES, Robson de Miranda et al. Structural characterization of mullites synthesized by thermal decomposition of topaz. Materials Research, São Carlos, v. 10, n. 1, p. 75-78, jan./mar. 2007. DOI: https://doi.org/10.1590/S1516-14392007000100016. Disponível em: http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1516-14392007000100016&lng=en&nrm=iso. Acesso em: 12 jan. 2021.pt_BR
dc.identifier.urihttp://repositorio.unb.br/handle/10482/27082-
dc.language.isoenpt_BR
dc.publisherABM, ABC, ABPolpt_BR
dc.rightsAcesso Abertopt_BR
dc.titleStructural characterization of mullites synthesized by thermal decomposition of topazpt_BR
dc.typeArtigopt_BR
dc.subject.keywordMulitapt_BR
dc.subject.keywordTopáziopt_BR
dc.subject.keywordRaio X - difraçãopt_BR
dc.rights.licenseMaterials Research - All the contents of this journal, except where otherwise noted, is licensed under a Creative Commons Attribution License (CC BY NC 4.0). Fonte: https://www.scielo.br/scielo.php?script=sci_arttext&pid=S1516-14392007000100016&lng=en&tlng=en. Acesso em: 12 jan. 2021.-
dc.identifier.doihttps://dx.doi.org/10.1590/S1516-14392007000100016pt_BR
dc.description.abstract1The structure of mullite obtained by thermal decomposition of topaz at 1340 °C and after additional thermal treatment at 1600 °C was characterized by 29Si and 27Al MAS NMR spectroscopy and x ray diffraction. No amorphous phase was detected by these techniques. The 29Si MAS NMR spectra of the mullite samples showed four resonance peaks at -81, -86, -90 and -94 ppm. The peak at -81 ppm corresponded to silicon near oxygen vacancies in the mullite structure. The peak at 86 ppm was related to a sillimanite-type site and was the major contribution, ranging from 42 to 50%. The two other peaks, at -90.0 ppm and -94 ppm, were interpreted as resulting from rearrangements of the sillimanite-type site by the replacement of AlO4 by SiO4 tetrahedra16. The 27Al MAS NMR data of the two samples exhibited three different peaks, two of which were attributed to tetrahedral sites at 40 -45 and 63 -67 ppm, while the third was assigned to an octahedral site at about -6 ppm. The ratio of tetrahedral to octahedral aluminum sites was found to depend on the temperature applied during the preparation of the mullite and was higher at 1600 °C.-
dc.description.unidadeInstituto de Química (IQ)pt_BR
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