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K6[Fe8.27(HPO3)12]: a new mixed‐valence iron phosphite
Authors:Farida Hamchaoui  Vronique Alonzo  Houria Rebbah  Eric Le Fur
Abstract:The title compound, hexapotassium octairon(II,III) dodecaphosphonate, exhibiting a two‐dimensional structure, is a new mixed alkali/3d metal phosphite. It crystallizes in the space group Rm, with two crystallographically independent Fe atoms occupying sites of m (Fe1) and 3m (Fe2) symmetry. The Fe2 site is fully occupied, whereas the Fe1 site presents an occupancy factor of 0.757 (3). The three independent O atoms, one of which is disordered, are situated on a mirror and all other atoms are located on special positions with 3m symmetry. Layers of formula Fe3(HPO3)4]2? are observed in the structure, formed by linear Fe3O12 trimer units, which contain face‐sharing FeO6 octahedra interconnected by (HPO3)2? phosphite oxoanions. The partial occupancy of the Fe1 site might be described by the formation of two Fe(HPO3)2]? layers derived from the Fe3(HPO3)4]2? layer when the Fe1 atom is absent. Fe2+ is localized at the Fe1 and Fe2 sites of the Fe3(HPO3)4]2? sheets, whereas Fe3+ is found at the Fe2 sites of the Fe(HPO3)2]? sheets, according to bond‐valence calculations. The K+ cations are located in the interlayer spaces, between the Fe3(HPO3)4]2? layers, and between the Fe3(HPO3)4]2? and Fe(HPO3)2]? layers.
Keywords:crystal structure  hydrothermal synthesis  mixed‐valence iron phosphite  trigonal space group  open‐framework structure
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