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• W2059565512 abstract "Abstract We synthesized Fe3−xCoxO4 (x=0–0.6) using the hydrothermal method (T=200°C and 400°C) in order to demonstrate the substitutional effects on the populations of the tetrahedral (A) and octahedral (B) sites of magnetite. Our Mossbauer spectroscopy results provided direct evidence for the presence of the Co substitution in the B sublattice. In the case of magnetite synthesized at 400°C, the two sublattices reached equal Fe populations at a cobalt concentration of x=0.1. However, when the substituted magnetite was obtained at 200°C, the cobalt concentration corresponding to equal Fe populations shifted to a higher value (x=0.15)." @default.
• W2059565512 created "2016-06-24" @default.
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• W2059565512 date "2000-06-01" @default.
• W2059565512 modified "2023-09-26" @default.
• W2059565512 title "Population effects in cobalt-substituted magnetite" @default.
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• W2059565512 doi "https://doi.org/10.1016/s0167-577x(00)00012-4" @default.
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