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European Journal of Mineralogy; November, December 2006; v. 18; no. 6; p. 691-704; DOI: 10.1127/0935-1221/2006/0018-0691
© 2006 E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers
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Articles

Order and anti-order in olivine II: Thermodynamic analysis and crystal-chemical modelling

Herbert Kroll1, Armin Kirfel2 and Rolf Heinemann1

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,


Formula

{Delta}G0exch = {Delta}H0exch – T{Delta}S0exch relates to the exchange reaction FeM2 + MgM1 {leftrightarrow} FeM1 + MgM2. Since for the investigated olivine both {Delta}H0exch and {Delta}S0exch are positive ({Delta}H0exch = 1.2 kJ/mol, {Delta}S0exch = 3.7 J/mol K), an ordered Fe2+,Mg configuration is favoured by the enthalpic part of {Delta}G0exch whereas the vibrational entropic part favours anti-ordering. As a result, at low temperatures, where {Delta}H0exch > T{Delta}S0exch, Fe2+ prefers M2. Since, however, the energy T{Delta}S0exch steadily increases with increasing temperature it promotes Fe2+ into M1 and full disorder is attained at a crossover temperature Tco where {Delta}H0exch = Tco {Delta}S0exch. Above Tco, T{Delta}S0exch becomes progressively larger than {Delta}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 {Delta}H0exch being relatively small in FeMg olivine compared to the temperature proportional energy T{Delta}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 {Delta}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 ({chi}) 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


Formula

Accordingly, the small value of {Delta}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 {Delta}H0exch. In MnMg olivine, it is the radius ratio that dominates, contrary to CoMg and NiMg olivine where the electronegativity ratios control {Delta}H0exch. Consequently, Mn prefers M2, and Co and Ni segregate into M1.

{Delta}S0exch can be split into vibrational, {Delta}S0,vibexch, and electronic exchange entropies, {Delta}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, {Delta}S0exch can be satisfactorily modelled by


Formula

The resulting lnKD = –({Delta}H0exch – T {Delta}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.




This article has been cited by other articles:


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Eur J MineralHome page
V. Taroev, J. Gottlicher, H. Kroll, A. Kashaev, L. Suvorova, H. Pentinghaus, H. Bernotat-Wulf, U. Breit, V. Tauson, and V. Lashkevich
Synthesis and structural state of K-feldspars in the system K[AlSi3O8]-K[FeSi3O8]
European Journal of Mineralogy, August 1, 2008; 20(4): 635 - 651.
[Abstract] [Full Text] [PDF]


Home page
Eur J MineralHome page
R. Heinemann, H. Kroll, A. Kirfel, and B. Barbier
Order and anti-order in olivine III: Variation of the cation distribution in the Fe,Mg olivine solid solution series with temperature and composition
European Journal of Mineralogy, February 1, 2007; 19(1): 15 - 27.
[Abstract] [Full Text] [PDF]




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