Abstract
Metastable solid solutions (SS) Mn3FeTiSbO9 and Mn4FeTi2SbO12 with the ilmenite structure (space group R \(\bar 3\)) have been prepared by quenching at normal conditions. The compositions of the compounds have been justified using EDX spectroscopy and X-ray diffraction. The magnetic properties of SSs have been analyzed by comparison with ferrimagnetic ilmenite Mn2FeSbO6 (T N = 269 K) as a natural mineral and ceramics obtained at high pressure and high temperature. The solid solutions have been characterized as dilute magnetic systems formed as a result of substitution of nonmagnetic cations Ti4+ for a part of Fe3+ and Sb5+ cations. Mn3FeTiSbO9 is considered as a ferromagnetic with T N = 171 K and Mn4FeTi2SbO12 as a magnetic with the concentration of magnetic clusters below the percolation threshold.
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Original Russian Text © G.V. Bazuev, A.V. Korolev, B.G. Golovkin, 2016, published in Fizika Tverdogo Tela, 2016, Vol. 58, No. 7, pp. 1289–1295.
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Bazuev, G.V., Korolev, A.V. & Golovkin, B.G. Dilute ferrimagnetism of ilmenites Mn3FeTiSbO9 and Mn4FeTi2SbO12 . Phys. Solid State 58, 1332–1338 (2016). https://doi.org/10.1134/S1063783416070064
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DOI: https://doi.org/10.1134/S1063783416070064