On the yellow color of gamma‐irradiated brazilianite from Minas Gerais (Brazil).
dc.contributor.author | Pinheiro, Mauricio Veloso Brant | |
dc.contributor.author | Cipriano, Ricardo Augusto Scholz | |
dc.contributor.author | Karfunkel, Joachim | |
dc.contributor.author | Chaves, Mario Luiz de Sá Carneiro | |
dc.contributor.author | Krambrock, Klaus Wilhelm Heinrich | |
dc.date.accessioned | 2022-09-14T20:47:44Z | |
dc.date.available | 2022-09-14T20:47:44Z | |
dc.date.issued | 2021 | pt_BR |
dc.description.abstract | The origin of gamma irradiation-induced strong yellow color in brazilianite from Brazil is investigated. The irradiation- induced optical absorption band responsible for the color shows an onset in the blue spectral region at about 2.5 eV and maximum centered in the UV at ~ 4.24 eV. From the ratio between the squared value of the line width (W2 ) and the peak energy (M), a value of about 0.09 eV is estimated, which is consistent with an absorption band caused by a Schirmer ́s-type O− bound small polaron. By electron paramagnetic resonance (EPR), we are able to confrm its microscopic structure. This O− hole center is in fact the Al3+–O−X2+–P5+ hole center already identifed by EPR earlier in the literature (where X2+ stands for a nearby divalent cation with negligible abundance of magnetic isotopes). The EPR spectrum of the Al3+–O−X2+–P5+ hole center, along with the O− bound small polaron absorption band responsible for the yellow color, appears simultane- ously at high concentrations after gamma irradiation, and vanishes together for thermal annealing above 300 °C, returning after re-irradiation in a reversible way. Their appearance is concomitant with the H0 centers and Ti3+ electron centers, and possible charge-compensating centers. | pt_BR |
dc.identifier.citation | PINHEIRO, M. V. B. et al. On the yellow color of gamma‐irradiated brazilianite from Minas Gerais (Brazil). Physics and Chemistry of Minerals, v. 48, 2021. Disponível em: <https://link.springer.com/article/10.1007/s00269-021-01159-1>. Acesso em: 29 abr. 2022. | pt_BR |
dc.identifier.doi | https://doi.org/10.1007/s00269-021-01159-1 | pt_BR |
dc.identifier.issn | 1432-2021 | |
dc.identifier.uri | http://www.repositorio.ufop.br/jspui/handle/123456789/15279 | |
dc.identifier.uri2 | https://link.springer.com/article/10.1007/s00269-021-01159-1 | pt_BR |
dc.language.iso | en_US | pt_BR |
dc.rights | restrito | pt_BR |
dc.subject | Brazilianite | pt_BR |
dc.subject | Electron paramagnetic resonance | pt_BR |
dc.subject | Irradiation | pt_BR |
dc.subject | Electron–hole center | pt_BR |
dc.subject | O− hole center | pt_BR |
dc.title | On the yellow color of gamma‐irradiated brazilianite from Minas Gerais (Brazil). | pt_BR |
dc.type | Artigo publicado em periodico | pt_BR |
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