Abstract
The theory of associated solutions provides a simple but rigorous framework for the use of speciation reactions to model nonideal mixing behavior of silicate melt components. Application of the theory of the system Ab-Qz-H2O requires only P-T solidus data in the anhydrous and H2O-saturated systems Ab-H2O and Ab-Qz-H2O to calibrate equilibrium constants of proposed modeling reactions. Investigation of the systems Ab-H2O and Ab-Qz-H2O indicates that if a modeling reaction producing a sodium silicate species is considered, neither interaction between albite and silica melt to produce new complexes nor nonideal mixing of species is required and agreement between predicted and experimental eutectic compositions can be obtained by considering only disproportionation in albite melts. The thermodynamic consequence of these assumptions is that the Ab and Qz melt components mix ideally. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 316-331 |
| Number of pages | 16 |
| Journal | American Mineralogist |
| Volume | 79 |
| Issue number | 3-4 |
| State | Published - 1994 |
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