Set and , treating the supplied concentration notation as an ideal-dilute activity approximation. For pure solids and unit water activity, the first chemical equilibrium relation gives and the second gives . Thus plot
Their slopes are and respectively. They intersect at . Both the relevant silica activities and the intersection lie at negative , as expected for a dilute aqueous silica species.
Figure 1.
Original activity diagram: solid stable boundaries, dashed metastable continuations, and three mineral stability fields
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