钛铁矿型 Na2(Fe2/3Te4/3)O6。

IUCrData Pub Date : 2024-05-01 DOI:10.1107/S2414314624004826
Felix Eder , Matthias Weil , M. Bolte (Editor)
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引用次数: 0

摘要

Na2(Fe2/3Te4/3)O6(Z = 3)或 Na3(FeTe2)O9(Z = 2),三钠铁(III)二碲(VI)壬氧化物,采用钛铁矿(FeTiO3,Z = 6)结构类型,Ti 位点(位点对称性 3.)被 Na 取代,而 Fe 位点(位点对称性 3.虽然[(Fe,Te)O6]八面体只发生了轻微的畸变,但[NaO6]八面体却表现出了更强烈的畸变,这一点从键长和一些畸变参数的较大分布中可以看出。
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Ilmenite-type Na2(Fe2/3Te4/3)O6

Na2(Fe2/3Te4/3)O6 was obtained under hydro­thermal conditions and adopts the ilmenite (FeTiO3) structure type.

Na2(Fe2/3Te4/3)O6 (Z = 3) or Na3(FeTe2)O9 (Z = 2), tris­odium iron(III) ditellurium(VI) nona­oxide, adopts the ilmenite (FeTiO3, Z = 6) structure type with the Ti site (site symmetry 3.) replaced by Na and the Fe site (site symmetry 3.) replaced by a mixed-occupied (FeIII,TeVI) site in a Fe:Te ratio of 1:2. Whereas the [(Fe,Te)O6] octa­hedron is only slightly distorted, the [NaO6] octa­hedron shows much stronger distortions, as revealed by a larger spread of the bond lengths and some distortion parameters.

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