Local Environment of Fe Ions in a 40ZnO · 60B2O3 Glass Matrix
- Authors: Osipov A.A.1, Zainullina R.T.1, Osipova L.M.1, Nikandrova N.K.1, Mironov A.B.1
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Affiliations:
- Institute of Mineralogy, Ural Branch
- Issue: Vol 54, No 3 (2018)
- Pages: 283-287
- Section: Article
- URL: https://journals.rcsi.science/0020-1685/article/view/158425
- DOI: https://doi.org/10.1134/S0020168518030111
- ID: 158425
Cite item
Abstract
The valence state and coordination environment of the Fe ions in a number of Fe-containing zinc borate glasses with the general formula xFe2O3–(100–x)[40ZnO · 60B2O3] (x = 2.5–10 mol %) have been studied by Mössbauer spectroscopy. The results indicate that all of the glasses contain both Fe2+ and Fe3+ ions. The percentage of trivalent ions considerably exceeds that of Fe2+ ions and the relationship between the Fe2+ and Fe3+ concentrations is essentially independent of the Fe2O3 content in the zinc borate matrix. Most of the Fe3+ ions are in tetrahedral coordination, but raising the Fe2O3 content to above 5 mol % leads to a gradual increase in the percentage of Fe ions in octahedral coordination.
Keywords
About the authors
A. A. Osipov
Institute of Mineralogy, Ural Branch
Author for correspondence.
Email: armik@mineralogy.ru
Russian Federation, Miass, Chelyabinsk oblast, 456317
R. T. Zainullina
Institute of Mineralogy, Ural Branch
Email: armik@mineralogy.ru
Russian Federation, Miass, Chelyabinsk oblast, 456317
L. M. Osipova
Institute of Mineralogy, Ural Branch
Email: armik@mineralogy.ru
Russian Federation, Miass, Chelyabinsk oblast, 456317
N. K. Nikandrova
Institute of Mineralogy, Ural Branch
Email: armik@mineralogy.ru
Russian Federation, Miass, Chelyabinsk oblast, 456317
A. B. Mironov
Institute of Mineralogy, Ural Branch
Email: armik@mineralogy.ru
Russian Federation, Miass, Chelyabinsk oblast, 456317
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