Loading…

A thermodynamic model of Fe–Cr spinels

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-...

Full description

Saved in:
Bibliographic Details
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:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary: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]
ISSN:0010-7999
1432-0967
DOI:10.1007/s00410-005-0669-4