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1 Institut für Mineralogie, Westfälische Wilhelms-Universität, Corrensstr. 24, 48149 Münster, Germany
2 Mineralogisch-Petrologisches Institut, Poppelsdorfer Schloss, 53115 Bonn, Germany
* Corresponding author, e-mail: kroll{at}nwz.uni-muenster.de
The equilibrium order/anti-order behaviour in olivine Fe0.48Mg0.52[SiO4] is analysed in terms of the Thompson (1969, 1970) model for the Gibbs energy due to ordering, Gord,
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G0exch =
H0exch T
S0exch relates to the exchange reaction FeM2 + MgM1
FeM1 + MgM2. Since for the investigated olivine both
H0exch and
S0exch are positive (
H0exch = 1.2 kJ/mol,
S0exch = 3.7 J/mol K), an ordered Fe2+,Mg configuration is favoured by the enthalpic part of
G0exch whereas the vibrational entropic part favours anti-ordering. As a result, at low temperatures, where
H0exch > T
S0exch, Fe2+ prefers M2. Since, however, the energy T
S0exch steadily increases with increasing temperature it promotes Fe2+ into M1 and full disorder is attained at a crossover temperature Tco where
H0exch = Tco
S0exch. Above Tco, T
S0exch becomes progressively larger than
H0exch and stimulates further fractionating of Fe2+ into M1 corresponding to increasing anti-order. The unusual phenomenon of anti-order increasing at increasing temperatures is due to
H0exch being relatively small in FeMg olivine compared to the temperature proportional energy T
S0exch. In other AB olivines (A, B = Mn, Fe, Co, Ni, Mg) the exchange enthalpies are much larger, between 9 and 20 kJ/mol, so that they dominate
G0exch to a degree that precludes a crossover from ordered to anti-ordered states up to the melting point.
The exchange enthalpies reported for MnMg, FeMg, CoMg, NiMg and MnFe olivines can be rationalized in terms of cation radius (r) and electronegativity (
) ratios of the A and B cations. In a novel approach, both radii and electronegativities have been derived from topological analyses of the procrystal electron density distributions of pure M2[SiO4] olivines (M = Mn, Fe, Co, Ni, Mg) yielding a very satisfactory description by
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Accordingly, the small value of
H0exch found for FeMg olivine is a consequence of opposite radius and electronegativity contributions which almost cancel. In MnFe olivine, although both contributions are small, they cooperate resulting in a moderate value of
H0exch. In MnMg olivine, it is the radius ratio that dominates, contrary to CoMg and NiMg olivine where the electronegativity ratios control
H0exch. Consequently, Mn prefers M2, and Co and Ni segregate into M1.
S0exch can be split into vibrational,
S0,vibexch, and electronic exchange entropies,
S0,elexch. Describing the first in terms of a new octahedral distortion parameter, Df, and estimating the second from the Boltzmann distribution of the 3d-electrons,
S0exch can be satisfactorily modelled by
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The resulting lnKD = (
H0exch T
S0exch)/RT allows, for the first time and to the best of our knowledge, an exclusively electron density based description of the experimentally observed temperature variations of the site occupancies in AB olivines. This modelling of lnKD allows also for predicting the temperature variation of equilibrium cation distributions in AB olivines not investigated so far.
Key-words: olivine, order, anti-order, thermodynamic analysis, exchange enthalpy, nonconfigurational entropy, electronic entropy, topological analysis, ionic radius, electronegativity.
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