A new uranyl silicate sheet derived from phosphuranylite topology in the structure of Cs4[(UO2)5(SiO3OH)2O2F4]

Evgeny V. Nazarchuk, Oleg I. Siidra, Dmitri O. Charkin, Yana G. Tagirova
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Abstract

A new uranyl silicate Cs4[(UO2)5(SiO3OH)2O2F4] (1), was obtained via a hydrothermal route. The new compound is monoclinic, P21/n, a = 8.3870(2), b = 13.4612(2), c = 10.9503(2) Å, β = 91.223(2)°, V = 1236.00(4) Å3; the structure has been solved and refined down to R 1 = 0.022. Therein, the phosphouranylite units (PUs) associate into a new type of uranyl-silicate layers, [(UO2)5(SiO3OH)2O2F4]4−, which interleave with the Cs+ cations. Topological analysis of PU based structures indicates that these layers in 1 provide a unique example of complexes constructed only via association of the PU and not involving other building units.
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在 Cs4[(UO2)5(SiO3OH)2O2F4]结构中,从磷铀矿拓扑结构衍生出一种新的铀硅酸盐薄片
通过水热法获得了一种新的铀硅酸盐 Cs4[(UO2)5(SiO3OH)2O2F4] (1)。新化合物呈单斜型,P21/n,a = 8.3870(2),b = 13.4612(2),c = 10.9503(2)埃,β = 91.223(2)°,V = 1236.00(4) Å3;该结构已被求解并细化至 R 1 = 0.022。其中,磷酰单位(PUs)结合成一种新型的铀硅酸盐层,即[(UO2)5(SiO3OH)2O2F4]4-,与 Cs+ 阳离子交错。对基于 PU 的结构进行的拓扑分析表明,1 中的这些层是仅通过 PU 关联而不涉及其他构建单元构建复合物的独特实例。
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