Activity-composition relations in FeTiO3-MnTiO3 ilmenite solid solutions from EMF measurements at 1050–1300 K |
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Authors: | Hugh St. C. O'Neill Mark I. Pownceby Victor J. Wall |
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Affiliation: | (1) Bayerisches Geoinstitut, Universität Bayreuth, Postfach 101251, D-8580 Bayreuth, Federal Republic of Germany;(2) Earth Sciences Department, Monash University, 3168 Clayton, VIC, Australia |
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Abstract: | The activity of FeTiO3 in the binary ilmenitepyrophanite (FeTiO3-MnTiO3) solid solution has been determined for the temperature range 1050–1300 K by displacement of the reaction: 2 FeTiO3=2 Fe+2 TiO2+O2 in T-O2 space, using an electrochemical technique with calcia- and yttria-stabilized zirconia solid electrolytes. The activities show small positive deviations from ideality, which, although the data are unusually precise, may be perfectly described by the simple regular solution model, with an interaction parameter, WFe-Mnilm, of 2.2±0.3 kJ g-atom–1, which is independent of temperature. This value, together with the experimental data on the partitioning of Fe and Mn between ilmenite and garnet (Pownceby et al. 1987), gives WFe-Mngt=1.2±0.5 kJ g-atom–1 for the almandine-spessartine (Fe3Al2Si3O12-Mn3Al2Si3O12) solid solution. |
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