Local Environment of Fe Ions in a 40ZnO · 60B2O3 Glass Matrix


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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.

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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