Abstract
The phase composition of magnetic microspheres isolated from Ekibastuz coal fly ash in six narrow size ranges is determined by Mössbauer spectroscopy. The major phase in the microspheres is nonstoichiometric, cation-substituted (Al, Mg, and Ti) magnetite. Their magnetic properties are shown to depend on the Fe content and cation distribution over the spinel sites.
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Translated from Neorganicheskie Materialy, Vol. 41, No. 1, 2005, pp. 54–63.
Original Russian Text Copyright © 2005 by Bayukov, N. Anshits, Balaev, Sharonova, Rabchevskii, Petrov, A. Anshits.
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Bayukov, O.A., Anshits, N.N., Balaev, A.D. et al. Mössbauer study of magnetic microspheres isolated from power plant fly ash. Inorg Mater 41, 50–59 (2005). https://doi.org/10.1007/s10789-005-0079-z
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DOI: https://doi.org/10.1007/s10789-005-0079-z