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dc.contributor.author Liferovich R.P.
dc.contributor.author Mitchell R.H.
dc.date.accessioned 2025-04-19T06:19:50Z
dc.date.available 2025-04-19T06:19:50Z
dc.date.issued 2006
dc.identifier https://elibrary.ru/item.asp?id=14803852
dc.identifier.citation The Canadian Mineralogist, 2006, 44, 5, 1089-1097
dc.identifier.issn 0008-4476
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/49010
dc.description.abstract Synthetic (Ca1-xNax)(Ti1-x Nbx)OSiO4 and Ca(Ti1-2x NbxAlx)OSiO4 solid solutions have been prepared for x = 0.1 and 0.2 by ceramic methods and their crystal structure determined by Rietveld analysis. At ambient conditions, the isomorphic capacity of (F,OH)-free titanite is ~0.25 apfu Nb in a single-site scheme of substitution (2VITi4+ ⇌ VIAl3+ + VINb5+) and ~0.22 apfu Nb in a two-site scheme (VIICa2++VITi4+ ⇌ VIINa++VINb5+). All cations located at the VIIX and VIY sites are disordered. Analysis of tetrahedron bond-lengths indicates the absence of Al3+ replacing Si4+ in coordination tetrahedra. All Nb-doped varieties of titanite adopt space group A2/a. Thus, both single-site and complex multivalent schemes of substitution destroy the coherence of the off-centering of chains of octahedra typical of the CaTiOSiO4 end member, resulting in a P21/a → A2/a phase transition. The (Ca1-xNax) (Ti1-xNbx)OSiO4 scheme of substitution incorporates the larger cations at both the VIIX and VIY sites, whereas the Ca(Ti1-2x NbxAlx)OSiO4 scheme involves only VIY-site (Al3+, Nb5+) cations, with a slightly smaller "average" radius. Unit-cell dimensions change insignificantly and vary sympathetically with the change of average radii of the cations in the (Ca1-xNax) (Ti1-xNbx)OSiO4 series and vary insignificantly in the Ca(Ti1-2x NbxAlx)OSiO4 series. Both Nb-doped titanite and pure CaTiOSiO4 consist of distorted polyhedra. The seven-fold coordination polyhedra and octahedra in Nb-doped titanite are slightly less stretched as compared to those in pure CaTiOSiO4. The SiO4 tetrahedron is compressed in Nb-doped titanite as compared to that in the pure CaTiOSiO4. The experimental data obtained suggest that the existence of a titanite analogue with more than 50 mol.% of NaNbOSiO4 end member is unlikely. The solid solution involving the smaller VI(Al,Nb) cations theoretically could be stabilized at high pressure, suggesting the existence of a potentially new species dominated by the Ca(AlNb)OSiO4 end member. The synthetic titanite compositions may be suitable for the sequestration of radioactive waste containing 94Nb.
dc.subject ALUMINUM
dc.subject CRYSTAL STRUCTURE
dc.subject DISTORTION
dc.subject NIOBIUM
dc.subject RADWASTE DISPOSAL
dc.subject RIETVELD ANALYSIS
dc.subject SODIUM
dc.subject TITANITE
dc.title SOLID SOLUTIONS OF NIOBIUM IN SYNTHETIC TITANITE
dc.type Статья
dc.identifier.doi 10.2113/gscanmin.44.5.1089


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