Abstract
If a wustite sample prepared above 1000 °C is annealed at 225 °C stoichiometric FeO occurs as a metastable decomposition intermediate, as has been demonstrated röntgenographically and by means of the Mössbauer-effect. © 1970, Walter de Gruyter. All rights reserved.
Cite
CITATION STYLE
APA
Hentschel, B. (1970). Stoichiometric FeO as Metastable Intermediate of the Decomposition of Wustite at 225 °C. Zeitschrift Fur Naturforschung - Section A Journal of Physical Sciences, 25(12), 1996–1997. https://doi.org/10.1515/zna-1970-1241
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