Study on magnetite oxidation using synchrotron X–ray diffraction and X–ray absorption spectroscopy: Vacancy ordering transition in maghemite (γ–Fe2O3)
Author:
Affiliation:
1. Division of Earth Evolution Sciences, Graduate School of Life and Environmental Sciences, University of Tsukuba
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/116/4/116_210304/_pdf
Reference47 articles.
1. Annersten, H. and Hafner, S.S. (1973) Vacancy distribution in synthetic spinels of the series magnetite–γ–iron(III) oxide. Zeitschrift für Kristallographie, 137, 321–340.
2. Babay, S., Mhiri, T. and Toumi, M. (2015) Synthesis, structural and spectroscopic characterizations of maghemite γ–Fe2O3 prepared by one–step coprecipitation route. Journal of Molecular Structure, 1085, 286–293.
3. Bajt, S., Sutton, S.R. and Delaney, J.S. (1994) X–ray microprobe analysis of iron oxidation states in silicates and oxides using X–ray absorption near edge structure (XANES). Geochimica et Cosmochimica Acta, 58, 5209–5214.
4. Bosi, F., Hålenius, U. and Skogby, H. (2009) Crystal chemistry of the magnetite–ulvöspinel series. American Mineralogist, 94, 181–189.
5. Cervellino, A., Frison, R., Cernuto, G., Guagliardi, A. and Masciocchi, N. (2014) Lattice parameters and site occupancy factors of magnetite–maghemite core–shell nanoparticles. A critical study. Journal of Applied Crystallography, 47, 1755–1761.
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