Abstract
The crystal structure of a new compound, (H3O)[(UO2)(SeO4)(SeO2OH)] (monoclinic, P21/n, a = 8.6682(19), b = 10.6545(16), c = 9.846(2) Å, β = 97.881(17)°, V = 900.7(3) Å3), was solved by direct methods and refined to R 1 = 0.050. The structure contains two symmetrically different Se atoms. The Se1 site is coordinated by three O atoms as is characteristic of Se4+ cations. The Se2 site is coordinated by four O atoms and forms selenate anion SeO 2−4 . The structure is based on selenite-selenate sheets [(UO2)(SeO4)(SeO2OH)]− linked by the interlayer H3O− ions. The sheets are parallel to (101). The structure is compared to that of schmiederite, Pb2Cu2(SeO3)(SeO4)(OH)4.
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Original Russian Text © S.V. Krivovichev, 2009, published in Zapiski RMO (Proceedings of the Russian Mineralogical Society), 2009, Pt. CXXXVII, No. 3, pp. 130–136.
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Krivovichev, S.V. Crystal chemistry of selenates with mineral-like structures: VII. The structure of (H3O)[(UO2)(SeO4)(SeO2OH)] and some structural features of selenite-selenates. Geol. Ore Deposits 51, 663–667 (2009). https://doi.org/10.1134/S1075701509070150
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DOI: https://doi.org/10.1134/S1075701509070150