Pregled bibliografske jedinice broj: 171093
The role of uranium(V) ion in the chemical composition of meta-autunite from pegmatites of Quintos de Baixo, Brazil
The role of uranium(V) ion in the chemical composition of meta-autunite from pegmatites of Quintos de Baixo, Brazil // Neues Jahrbuch für Mineralogie, Abhandlungen, 181 (2005), 1; 27-38 (međunarodna recenzija, članak, znanstveni)
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Naslov
The role of uranium(V) ion in the chemical composition of meta-autunite from pegmatites of Quintos de Baixo, Brazil
Autori
Bermanec, Vladimir ; Wegner, Reinhard ; Kniewald, Goran ; Rakvin, Boris ; Palinkaš, Ladislav ; Rajić, Maša ; Tomašić, Nenad ; Furić, Krešimir
Izvornik
Neues Jahrbuch für Mineralogie, Abhandlungen (0077-7757) 181
(2005), 1;
27-38
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
meta-autunite; pentavalent uranium; non-stoichiometric uranium oxides; X-ray diffraction; IR spectroscopy; thermal analysis; differential pulse polarography; electron paramagnetic resonance; Borborema; Quintos de Baixo pegmatites
Sažetak
Meta-autunite from the pegmatite mineralization of Quintos de Baixo, Brazil was investigated. The total uranium content and elemental analysis yield the formula Ca(UVIO2)2-x(UVO2)x(H3O+)x(PO4)2.(6-x)H2O for the meta-autunite. The natural sample crystallizes tetragonally in the space group P4/nmm having unit cell parameters a=6.990(1) Å ; ; ; ; , c=8.445 (1) Å ; ; ; ; and V=412.6(1) Å ; ; ; ; 3 calculated from X-ray diffraction data. Thermal analysis showed a weight loss of 16.03 wt% in four distinct processes up to 1500º ; ; ; ; C. Electron paramagnetic resonance (EPR) spectroscopy provides evidence that part of the uranium present in meta-autunite is in the pentavalent state. High temperature diffraction data show lowering of the symmetry, decreasing the unit cell parameters and finally, the breaking of the structure of the phosphate phase and formation of monoclinic uranium oxide and an amorphous phase. At 80°C meta-autunite I transforms into the meta-autunite II with orthorhombic symmetry, while further heating produces changes in the diffraction pattern due to dehydration, although all the heating products could be by analogy identified as meta-autunite II. The calculated unit cell parameters for this phase decrease from a=7.253(4) Å ; ; ; ; , b=6.537(3) Å ; ; ; ; , c=7.008(4) Å ; ; ; ; at 82°C to a=6.38(2) Å ; ; ; ; , b=5.82(1) Å ; ; ; ; , c=6.68(1) Å ; ; ; ; at 204°C. Uranium oxide phases originating from the breakdown of the phosphate structure show temperature dependant stability. At 1050°C hexagonal U2O3 analogous with  -Al2O3 is present with symmetry (R c) and unit cell parameters (a=4.806(1) Å ; ; ; ; , c=13.138(4) Å ; ; ; ; , V=262.9(1) Å ; ; ; ; 3).
Izvorni jezik
Engleski
Znanstvena područja
Fizika, Geologija, Kemija
POVEZANOST RADA
Ustanove:
Institut "Ruđer Bošković", Zagreb,
Prirodoslovno-matematički fakultet, Zagreb,
Brodarski institut d.o.o.
Profili:
Ladislav Palinkaš
(autor)
Krešimir Furić
(autor)
Maša Rajić Linarić
(autor)
Vladimir Bermanec
(autor)
Nenad Tomašić
(autor)
Boris Rakvin
(autor)
Goran Kniewald
(autor)
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus