Author:
Palin E. J.,Harrison R. J.
Abstract
Abstract
The systematics of cation ordering in binary spinel solid solutions have been
investigated using an interatomic potential model combined with Monte Carlo
simulations. The formalism to describe a system containing three cation species
ordering over two non-equivalent sub-lattices is developed and the method applied
to the
MgAl2O4-FeAl2O4
binary solid solution. Our results compare favourably with experimental
measurements of site-occupancy data, although the experiments display a slightly
larger degree of non-ideality than the simulations. A possible kinetic origin of
the non-ideal behaviour was examined by performing simulations in which only
exchange of Mg and Fe2+ between tetrahedral and octahedral
sites was permitted below the Al-blocking temperature of 1160 K. This approach
improves the agreement with the experimental site occupancies, and suggests that
the blocking temperature for moving Mg and Fe2+ between
tetrahedral and octahedral sites is significantly lower than for moving
Al
Subject
Geochemistry and Petrology
Cited by
7 articles.
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