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The effects of recalculation on estimates of temperature and oxygen fugacity from analyses of multicomponent iron-titanium oxides
American Mineralogist · 1983 · Vol. 68 · pp. 586–594
John C. Stormer✉(University of Georgia)
Abstract
New recalculation scheme based on models of ionic substitution, consistent with a new thermodynamic model for the pure Fe-Ti system. The new scheme tends to give temperature and log fO 2 values falling in the middle of the range of variation.--Modified journal abstract.
Metallurgical Processes and ThermodynamicsIron and Steelmaking ProcessesFugacityTitaniumMineral redox bufferThermodynamicsIonic bondingOxygenAtmospheric temperature rangeRange (aeronautics)Materials scienceMineralogy
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References
A solution model for coexisting iron–titanium oxides
American Mineralogist · 1981 · 487 citations
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