Abstract
The reaction of Y/Eu, Cu, Fe oxides and Ba carbonate in a ratio of 1:2:1:2 at 980°C in an oxygen current forms double-phase systems; in each system, the major phase is a 123 type orthorhombic three-layered structure, and the secondary phase, amounting to about one-third of the major phase, is a tetragonal, nearly pseudocubic 123 structure. Both phases in the yttrium and europium systems are characterized by formation of weak superstructures with doubled parameters of the ordinary three-layered cell. In each system, the two phases seem to differ in the content and distribution of iron. Based on the gamma resonance data, it is concluded that ∼2/3 of iron atoms occupy Cu(2) positions in the form of Fe3+ and are magnetically ordered at room temperature. The other Fe atoms occupy Cu(1) positions with different coordinations; some of the octahedrally coordinated Fe3+ ions in Cu(1) positions (major part in the case of the Eu system) are magnetically ordered, probably, under the influence of magnetic ordering in Cu(2) sublattices containing Fe3+ ions.
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Additional information
N. N. Semyonov Institute of Chemical Physics, Russian Academy of Sciences. Translated fromZhurnal Strukturnoi Khimii, Vol. 39, No. 2, pp. 267–274, March–April, 1998.
This work was supported by RFFR grant No. 95-03-08227.
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Stukan, R.A., Yudina, N.G., Stukan, M.R. et al. RBa2Cu2FeO7 phases (R=Y, Eu): Synthesis, structure, and mössbauer spectra. J Struct Chem 39, 217–223 (1998). https://doi.org/10.1007/BF02873621
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DOI: https://doi.org/10.1007/BF02873621