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Geochemical Journal
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A thermodynamic treatment of chemical reactions in orthopyroxene

Yasutami Oka
Geochemical Journal, Vol. 11, No. 2, P. 101-106, 1977

ABSTRACT

Mixing of Fe and Mg in orthopyroxene crystalline solution can be represented by a multicomponent regular solution model when the molecules (MgM1MgM2Si2O6, FeM1FeM2Si2O6, FeM1MgM2Si2O6 and MgM1FeM2Si2O6) are introduced as its components. In this regular solution model, there are three independent interaction parameters (WM1, WM2 and WM12) which correspond to the cation interactions between M1 and M1 sites, M2 and M2 sites and M1 and M2 sites, respectively. These parameters can not be determined uniquely by site-occupancy measurements only. Some thermodynamic formulations for orthopyroxene are given by using these parameters.

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