A thermodynamic model of Fe–Cr spinels

• Published in: Contributions to mineralogy and petrology 2005-07, Vol.149 (5), p.591-599
• Main Author: Kurepin, Viktor A.
• Format: Article
• Language: English
• Subjects: Chromium; Comparative analysis; Geochemistry; Iron; Iron oxides; Mineralogy; Petrology; Temperature effects; Thermodynamics
• ISSN: 0010-7999; 1432-0967
• DOI: 10.1007/s00410-005-0669-4

A new thermodynamic model for multi-component spinel solid solutions has been developed which takes into account thermodynamic consequences of cation mixing in spinel sublattices. It has been applied to the evaluation of thermodynamic functions of cation mixing and thermodynamic properties of Fe3O4-FeCr2O4 spinels using intracrystalline cation distribution in magnetite, lattice parameters and activity-composition relations of magnetite-chromite solid solutions. According to the model, cation distribution in binary spinels, (Fe1-x2+ Fex3+)[Fex2+Fe2-2y-x3+Cr2y]O4, and their thermodynamic properties depend strongly on Fe2+-Cr3+ cation mixing. Mixing of Fe2+-Fe3+ and Fe3+-Cr3+ can be accepted as ideal. If Fe2+, Fe3+ and Cr are denoted as 1, 3 and 4 respectively, the equation of cation distribution is -RT ln(x2/((1-x)(2-2y-x)))= DeltaG13* + (1-2x)W13+y(W14-W13-W34) where DeltaG13* is the difference between the Gibbs energy of inverse and normal magnetite, Wij is a Margules parameter of cation mixing and DeltaG13*, J/mol =-23,000+13.4 T, W14=36 kJ/mol, W13=W34=0. The positive nonconfigurational Gibbs energy of mixing is the main reason for changing activity-composition relations with temperature. According to the model, the solvus in Fe3O4-FeCr2O4 spinel has a critical temperature close to 500 degrees C, which is consistent with mineralogical data.[PUBLICATION ABSTRACT]