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首页> 外文期刊>Geology of Ore Deposits: A Journal of Theoretical and Applied Papers on All Aspects of Ore Genesis >Crystal Chemistry of Selenates with Mineral-Like Structures:VII. The Structure of (H3O)[(UO2)(SeO4)(SeO2OH)] and Some Structural Features of Selenite-Selenates
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Crystal Chemistry of Selenates with Mineral-Like Structures:VII. The Structure of (H3O)[(UO2)(SeO4)(SeO2OH)] and Some Structural Features of Selenite-Selenates

机译:具有矿物样结构的硒酸盐的晶体化学:VII。 (H3O)[(UO2)(SeO4)(SeO2OH)]的结构和亚硒酸盐-硒酸盐的一些结构特征

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摘要

The crystal structure of a new compound, (H3O)[(UO2)(SeO4)(SeO2OH)] (monoclinic, P2_1, a = 8.6682(19), b = 10.6545(16), c = 9.846(2) A, β = 97.881(17)°, V= 900.7(3) A~3), was solved by direct methods and refined to R1 = 0.050. The structure contains two symmetrically different Se atoms. The Sel site is coordinated by three O atoms as is characteristic of Se~(4+) cations. The Se2 site is coordinated by four O atoms and forms selenate anion SeO4~(2-). 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.
机译:新化合物(H3O)[(UO2)(SeO4)(SeO2OH)]的晶体结构(单斜晶系,P2_1 / n,a = 8.6682(19),b = 10.6545(16),c = 9.846(2)A β= 97.881(17)°,V = 900.7(3)A〜3),通过直接方法求解并精制为R1 = 0.050。该结构包含两个对称不同的Se原子。 Sel位点由三个O原子配位,这是Se〜(4+)阳离子的特征。 Se2位点由四个O原子配位,形成硒酸根阴离子SeO4〜(2-)。该结构基于通过层间H3O-离子连接的亚硒酸盐-硒酸盐片材[(UO2)(SeO4)(SeO2OH)]-。纸张平行于(101)。将其结构与白闪石Pb2Cu2(SeO3)(SeO4)(OH)4进行比较。

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