Anisotropy of Thermal Expansion of Oxoborate Warwickite
- Authors: Biryukov Y.P.1, Bubnova RS.1, Filatov S.K.2
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Affiliations:
- Grebenshchikov Institute of Silicate Chemistry, Russian Academy of Sciences, 199034, St. Petersburg, Russia
- Saint Petersburg State University
- Issue: Vol 49, No 5 (2023)
- Pages: 538-545
- Section: Articles
- URL: https://journals.rcsi.science/0132-6651/article/view/139347
- DOI: https://doi.org/10.31857/S0132665123600231
- EDN: https://elibrary.ru/OMVJEZ
- ID: 139347
Cite item
Abstract
In this paper, the transition metal oxoborate warwickite (Fe2+,Mg)Fe3+(BO3)O is studied for the first time by low- and high-temperature X-ray diffraction in the temperature range from 93 to 513 K. The sharply anisotropic nature of its thermal expansion is revealed. A structural interpretation of the expansion mechanism is given both in terms of the contribution of cationic and oxocentered polyhedra.
About the authors
Ya. P. Biryukov
Grebenshchikov Institute of Silicate Chemistry, Russian Academy of Sciences, 199034, St. Petersburg, Russia
Email: y.p.biryukov@gmail.com
Россия, 199034, наб. Макарова, 2, Санкт-Петербург
R S. Bubnova
Grebenshchikov Institute of Silicate Chemistry, Russian Academy of Sciences, 199034, St. Petersburg, Russia
Email: rimma_bubnova@mail.ru
Россия, 199034, Санкт-Петербург, наб. Макарова, 2
S. K. Filatov
Saint Petersburg State University
Author for correspondence.
Email: filatov.stanislav@gmail.com
Russia, Saint Petersburg
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