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Updated: Apr 9, 2026

High Pressure Single Crystal Diffraction at PX^2
Published on: January 16, 2017
Crystal structure of the Fe-member of usovite
1Institute for Chemical Technologies and Analytics, Division of Structural Chemistry, Vienna University of Technology, Getreidemarkt 9/164-SC, A-1060 Vienna, Austria.
Abstract:
Crystals of the title compound, with the idealized composition Ba2CaFeAl2F14, dibarium calcium iron(II) dialuminium tetra-deca-fluoride, were obtained serendipitously by reacting a mixture of the binary fluorides BaF2, CaF2 and AlF3 in a leaky steel reactor. The compound crystallizes in the usovite structure type (Ba2CaMgAl2F14), with Fe(2+) cations replacing the Mg(2+) cations. The principal building units are distorted [CaF8] square-anti-prisms (point group symmetry 2), [FeF6] octa-hedra (point group symmetry -1) and [AlF6] octa-hedra that are condensed into undulating (2) ∞[CaFeAl2F14](4-) layers parallel (100). The Ba(2+) cations separate the layers and exhibit a coordination number of 12. Two crystal structure models with a different treatment of the disordered Fe site [mixed Fe/Ca occupation, model (I), versus underoccupation of Fe, model (II)], are discussed, leading to different refined formulae Ba2Ca1.310 (15)Fe0.690 (15)Al2F14 [model (I)] and Ba2CaFe0.90 (1)Al2F14 [model (II)].
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