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http://hdl.handle.net/1843/83720
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DC Field | Value | Language |
---|---|---|
dc.creator | Eder Luiz Tolentino Junior | pt_BR |
dc.creator | Coralie Heinis Dias | pt_BR |
dc.creator | Mario Luiz de Sá Carneiro Chaves | pt_BR |
dc.creator | Klaus Wilhelm Heinrich Krambrock | pt_BR |
dc.creator | Mauricio Veloso Brant Pinheiro | pt_BR |
dc.date.accessioned | 2025-07-22T12:10:07Z | - |
dc.date.available | 2025-07-22T12:10:07Z | - |
dc.date.issued | 2019 | - |
dc.citation.volume | 46 | pt_BR |
dc.citation.spage | 203 | pt_BR |
dc.citation.epage | 213 | pt_BR |
dc.identifier.doi | https://doi.org/10.1007/s00269-018-0998-2 | pt_BR |
dc.identifier.issn | 1432-2021 | pt_BR |
dc.identifier.uri | http://hdl.handle.net/1843/83720 | - |
dc.description.resumo | Natural greenish-yellow titanites from two localities in Brazil (Bananal/Capelinha, MG and Xambioá, TO) were characterized by electron paramagnetic resonance (EPR) and optical absorption. Along with vanadyl ions (VO2+) substituting Ti4+, two other paramagnetic centers were identified: the Fe3+ and the Mn2+. For the VO2+, the principal values and orientations of the g and A tensors were derived from a careful analysis of the angular dependence of the EPR spectra. The obtained results, although different to previously reported data, still support the model for the VO2+ bonds to the nearest oxygen (O1) in the TiO6-distorted octahedra. In addition, the titanite optical absorption spectra were analyzed, and the yellow color was ascribed to Fe3+ ↔ O2− ligand–metal charge transfer transitions (LMCT) in the near-ultraviolet, extending to the violet and blue spectral ranges. The VO2+ center seen by EPR was in low concentration and had no visible effect on the color. Finally, γ-irradiation up to 200 kGy and thermal treatments in oxidizing/reducing atmospheres up to 600–700 °C also had no big influence on the dominant yellow color. | pt_BR |
dc.description.sponsorship | CNPq - Conselho Nacional de Desenvolvimento Científico e Tecnológico | pt_BR |
dc.description.sponsorship | FAPEMIG - Fundação de Amparo à Pesquisa do Estado de Minas Gerais | pt_BR |
dc.description.sponsorship | CAPES - Coordenação de Aperfeiçoamento de Pessoal de Nível Superior | pt_BR |
dc.language | eng | pt_BR |
dc.publisher | Universidade Federal de Minas Gerais | pt_BR |
dc.publisher.country | Brasil | pt_BR |
dc.publisher.department | ICX - DEPARTAMENTO DE FÍSICA | pt_BR |
dc.publisher.initials | UFMG | pt_BR |
dc.relation.ispartof | Physics and Chemistry of Minerals | pt_BR |
dc.rights | Acesso Restrito | pt_BR |
dc.subject | Titanite | pt_BR |
dc.subject | Electron paramagnetic resonance | pt_BR |
dc.subject | Vanadyl | pt_BR |
dc.subject | Iron | pt_BR |
dc.subject.other | Ressonância paramagnética eletrônica | pt_BR |
dc.subject.other | Ferro | pt_BR |
dc.title | On the greenish-yellow color of natural Brazilian titanite | pt_BR |
dc.type | Artigo de Periódico | pt_BR |
dc.url.externa | https://link.springer.com/article/10.1007/s00269-018-0998-2 | pt_BR |
dc.identifier.orcid | https://orcid.org/0000-0001-6294-5059 | pt_BR |
dc.identifier.orcid | https://orcid.org/0000-0002-7562-0285 | pt_BR |
dc.identifier.orcid | https://orcid.org/0000-0001-5722-6260 | pt_BR |
Appears in Collections: | Artigo de Periódico |
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