Formation, thermal redox reaction and crystal structure of δ-CaCr2O4

초록

The thermal redox reactions of a Ca-Cr-O system under different atmospheric conditions were investigated by cyclic thermodiffractometry and thermogravimetry. In the first heating process under a reductive atmosphere, CaCrO4 decomposed into CaO and delta-CaCr2O4, a metastable form, with the liberation of free oxygen. In the second process under an oxidizing atmosphere, the CaO and delta-CaCr2O4 produced in the first reduction process reacted to regenerate CaCrO4, indicating that this redox reaction could proceed reversibly upon controlling the atmosphere. The crystal structure of delta-CaCr2O4 was determined, for the first time, on the basis of high-resolution synchrotron powder X-ray diffraction data. delta-CaCr2O4 crystallized in a monoclinic structure with the space group P2(1)/m. The structure can be described as a stacking of CrO2 layers composed of edge-sharing CrO6 octahedra, with calcium ions residing on-site between the layers. The calcium ions were coordinated by six oxygen atoms to form a trigonal prism geometry between the CrO2 layers. The structure of delta-CaCr2O4 was different from those of low-temperature beta-CaCr2O4 (distorted CaFe2O4-type) and high-temperature alpha-CaCr2O4 (P2-type layered structure).

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