Abstract
An integrated study of samples of Bi1−x A x FeO3±y (A = Sr, Ca) systems for 0 ≤ x ≤ 1 (step 0.1) is performed using X-ray diffraction (XRD), Mössbauer spectroscopy (MS), and X-ray photoelectron spectroscopy (XPS). Considerable deviations of actual elemental compositions from nominal ones in the samples of both systems are discovered. Both Fe3+ and Fe4+ ions are found to be present in the samples of the Bi1−x Sr x FeO3±y system with x > 0. No Fe4+ ions are discovered upon substitution of Bi3+ by Ca2+ in Bi1−x Ca x FeO3±y , neither by Mössbauer spectroscopy, nor by XPS. Charge compensation in Bi1−x Ca x FeO3±y takes place mostly via creation of oxygen vacancies.
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Acknowledgements
This study was supported by the Ministry of Education and Science of Russian Federation (grants Nos. 3.6105.2017/BCh, 3.5346.2017/BCh, and RFMEFI60714X0110).
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Kozakov, A.T. et al. (2017). Crystal Structure, Phase and Elemental Composition and Chemical Bonding in Bi1−X A X FeO3±Y Systems (A = Sr, Ca; 0 ≤X ≤ 1) from X-ray Diffraction, Mössbauer, and X-ray Photoelectron Spectra. In: Parinov, I., Chang, SH., Jani, M. (eds) Advanced Materials. Springer Proceedings in Physics, vol 193. Springer, Cham. https://doi.org/10.1007/978-3-319-56062-5_13
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DOI: https://doi.org/10.1007/978-3-319-56062-5_13
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