A Mössbauer study of the oxidation state of Fe in silicate melts
By K. D. Jayasuriya, Hugh St.C. Oʼneill, A. Berry, S. Campbell. 2004
216 citations recorded by the source corpus.
Subfields: Ceramics and Composites, Geophysics, Mechanical Engineering
View Paper: https://www.semanticscholar.org/paper/2d70f2a0b36a15322e65d03c4a42d584f71d954d
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In Ceramics and Composites
In Geophysics
In Mechanical Engineering
Citations in the corpus
- Amorphous Materials: Properties, structure, and durability: Oxidation state of iron in hydrous phono-tephritic melts (2008, background): “…state in silicate melts and to predict the prevailing oxygen fugacity in a magmatic system from Fe-redox ratios of quenched melts (e.g., Sack et al. 1980; Kilinc et al. 1983; Kress and Carmichael 1988, 1991; Mysen 1988; Borisov and Shapkin 1989; Nikolaev et al. 1996; Jayasuriya et al. 2004).”
- A Simple Thermodynamic Model for Melting of Peridotite in the System NCFMASOCr (2015, methodology): “Because the model allows calculation of the Fe3þ/RFe ratio of melts through the internal allmelt equilibrium 4 hmþq1⁄4 2 faþO2 it was fitted to the calibrations of Kress & Carmichael (1991), Jayasuriya et al. (2004) and O’Neill et al. (2006). A very small enthalpy increment to hm leads to a very goo”