Nuragheite, Th(MoO4)2·H2O, The Second Natural Thorium Molybdate And Its Relationships To Ichnusaite And Synthetic Th(MoO4)2†
-
Paolo Orlandi
,
Luca Bindi
Abstract
The new mineral species nuragheite, Th(MoO4)2·H2O, has been discovered in the Mo-Bi mineralization of Su Seinargiu, Sarroch, Cagliari, Sardinia, Italy. It occurs as colorless thin {100} tabular crystals, up to 200 μm in length, associated with muscovite, xenotime-(Y), and ichnusaite, Th(MoO4)2·3H2O. Luster is pearly to adamantine; nuragheite is brittle, with a perfect (100) cleavage. Owing to the very small amount of available material and its intimate association with ichnusaite, density and optical properties were not measured. Electron microprobe analysis gave (wt% = mean of six spot analyses): MoO3 49.38, ThO2 45.39, H2Ocalc 3.09, total 97.86. On the basis of eight O atoms per formula unit and assuming one H2O group, in agreement with the crystal structure data, the chemical formula of nuragheite is Th1.00Mo2.00O8·H2O. Main diffraction lines, corresponding to multiple hkl indices, are [d in Å (relative visual intensity)]: 5.28 (m), 5.20 (m), 5.04 (m), 4.756 (m), 3.688 (m), 3.546 (vs), 3.177 (s), 3.024 (m). The crystal structure study gives a monoclinic unit cell, space group P21/c, with a = 7.358(2), b = 10.544(3), c = 9.489(2) Å, β = 91.88(2)°, V = 735.8(2) Å3, Z = 4. The crystal structure has been solved and refined to a final R1 = 0.078 on the basis of 1342 “observed” reflections [Fo > 4σ(Fo)]. It consists of (100) layers formed by ninefold-coordinated Th-centered polyhedra and Mo-centered tetrahedra. Its crystal structure is discussed in relation to that of ichnusaite and that of synthetic orthorhombic Th(MoO4)2. The relationship between the progressive loss of water in the interlayer and the layer topology passing from ichnusaite through nuragheite to synthetic (ThMoO4)2 is examined. Nuragheite, the second thorium molybdate reported so far in nature, adds new data to the understanding of the crystal chemistry of actinide molybdates potentially forming during the alteration of spent nuclear fuel and influencing the release of radionuclides under repository conditions.
© 2015 by Walter de Gruyter Berlin/Boston
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- The system Na2CO3-FeCO3 at 6 GPa and its relation to the system Na2CO3-FeCO3-MgCO3
- Chlorine-hydroxyl diffusion in pargasitic amphibole
- The use of cation-cation and anion-anion bonds to augment the bond-valence model
- AIM analysis and the form of the bond-valence equation
- Atomistic simulation on mixing thermodynamics of calcite-smithsonite solid solutions
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- Tetrataenite in terrestrial rock
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