Synthesis and thermal behavior of Fe3O2(BO4) oxoborate


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Abstract

Iron oxoborate Fe3O2(BO4) has been first produced in solid-phase chemical reactions. Its thermal behavior in the temperature range 20–900°C is studied with the use in-situ high-temperature powder X-ray diffraction. It is shown that Fe3O2(BO4) begins decomposing with the formation of Fe2O3 in the temperature range 660–900°C. Thermal expansion is sharply anisotropic at room temperature (αmaxmin = 7) and becomes more isotropic with an increase in the temperature (αmaxmin = 1.2). The degree of oxidation of Fe3+ has been confirmed by Mössbauer spectroscopy (at a room temperature), and two nonequivalent positions in the structure have been detected, which are occupied by iron atoms with the octahedral environment of the oxygen atoms.

About the authors

Ya. P. Biryukov

Grebenshchikov Institute of Silicate Chemistry; Institute of Earth Sciences

Author for correspondence.
Email: rimma_bubnova@mail.ru
Russian Federation, nab. Makarova 2, St. Petersburg, 199034; Universitetskaya nab. 7/9, St. Petersburg, 199034

R. S. Bubnova

Grebenshchikov Institute of Silicate Chemistry; Institute of Earth Sciences

Email: rimma_bubnova@mail.ru
Russian Federation, nab. Makarova 2, St. Petersburg, 199034; Universitetskaya nab. 7/9, St. Petersburg, 199034

S. K. Filatov

Institute of Earth Sciences

Email: rimma_bubnova@mail.ru
Russian Federation, Universitetskaya nab. 7/9, St. Petersburg, 199034

A. G. Goncharov

Institute of Earth Sciences; Institute of Precambrian Geology and Geochronology

Email: rimma_bubnova@mail.ru
Russian Federation, Universitetskaya nab. 7/9, St. Petersburg, 199034; nab. Makarova 2, St. Petersburg, 199034


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