Please use this identifier to cite or link to this item: http://www.repositorio.ufop.br/jspui/handle/123456789/13601
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dc.contributor.authorToledo, José Roberto de-
dc.contributor.authorGonçalves, Raphaela de Oliveira-
dc.contributor.authorDias, Lorena N.-
dc.contributor.authorChaves, Mario Luiz de Sá Carneiro-
dc.contributor.authorKarfunkel, Joachim-
dc.contributor.authorCipriano, Ricardo Augusto Scholz-
dc.contributor.authorPinheiro, Mauricio Veloso Brant-
dc.contributor.authorKrambrock, Klaus Wilhelm Heinrich-
dc.date.accessioned2021-08-27T18:01:23Z-
dc.date.available2021-08-27T18:01:23Z-
dc.date.issued2020pt_BR
dc.identifier.citationTOLEDO, J. R. de. et al. Radiation-induced defects in montebrasite: An electron paramagnetic resonance study of O – hole and Ti3+ electron centers. American Mineralogist, v. 105, p. 1051-1059, jul. 2020. Disponível em: <https://www.degruyter.com/document/doi/10.2138/am-2020-7168/html>. Acesso em: 24 mar. 2021.pt_BR
dc.identifier.issn1945-3027-
dc.identifier.urihttp://www.repositorio.ufop.br/jspui/handle/123456789/13601-
dc.description.abstractMontebrasite is a lithium aluminum phosphate mineral with the chemical formula LiAlPO4(Fx,OH1–x) and considered a rare gemstone material when exhibiting good crystallinity. In general, montebrasite is colorless, sometimes pale yellow or pale blue. Many minerals that do not have colors contain hydroxyl ions in their crystal structures and can develop color centers after ionization or particle irradiation, examples of which are topaz, quartz, and tourmaline. The color centers in these minerals are often related to O– hole centers, where the color is produced by bound small polarons inducing absorption bands in the near UV to the visible spectral range. In this work, colorless montebrasite specimens from Minas Gerais state, Brazil, were investigated by electron paramagnetic resonance (EPR) for radiation-induced defects and color centers. Although γ irradiation (up to a total dose of 1 MGy) did not visibly modify color, a 10 MeV electron irradiation (80 MGy) induced a pale greenish-blue color. Using EPR, O– hole centers were identified in both γ- or electron-irradiated montebrasite samples showing superhyperfine interactions with two nearly equivalent 27Al nuclei. In addition, two different Ti3+ electron centers were also observed. From the γ irradiation dose dependency and thermal stability experiments, it is concluded that production of O– hole centers is limited by simultaneous creation of Ti3+ electron centers located between two equivalent hydroxyl groups. In contrast, the concentration of O– hole centers can be strongly increased by high-dose electron irradiation independent of the type of Ti3+ electron centers. From detailed analysis of the EPR angular rotation patterns, microscopic models for the O– hole and Ti3+ electron centers are presented, as well as their role in the formation of color centers discussed and compared to other minerals.pt_BR
dc.language.isoen_USpt_BR
dc.rightsrestritopt_BR
dc.subjectElectron paramagnetic resonancept_BR
dc.subjectIrradiationpt_BR
dc.subjectElectron-hole centerpt_BR
dc.subjectColor enhancementpt_BR
dc.titleRadiation-induced defects in montebrasite : an electron paramagnetic resonance study of O – hole and Ti3+ electron centers.pt_BR
dc.typeArtigo publicado em periodicopt_BR
dc.identifier.uri2https://www.degruyter.com/document/doi/10.2138/am-2020-7168/htmlpt_BR
dc.identifier.doihttps://doi.org/10.2138/am-2020-7168pt_BR
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