Energetics of crystalline solutions
B. Mishra
PART – 2
ENERGETICS OF CRYSTALLINE SOLUTIONS
In the previous section, dealing with pure crystalline phases, we derived an expression for G = G (P, T). However, most of the rock forming minerals (silicates) and those constitute ore deposits (sulfides) occur as solid solutions of two or more end member components. Hence, it is appropriate to bring in the compositional variable for deducing the free energy of formation of a phase, i.e., G = G (P, T, X). Accordingly, in this section, we deal with energetics (total change in Gibbs free energy), pertaining to formation binary crystalline solution phases.
The activity of a pure phase component (i) is related to free energy through the relation
Gi
P ,T
= Gi
where Gi
Gi
0 , P ,T
φ , P ,T
(1)
is the free energy of component ‘i’ in phase φ at P, T.
P ,T
0 , P ,T
+ RT ln ai
is the free energy of component ‘i’ if it were a pure phase at P, T
(as derived in eqn. (24) in Part –1) ai
φ , P ,T
is the activity of the component ‘i’ in phase ‘ φ ’ at P, T.
Also,
ai
φ , P ,T
φ
= X i .γ i
φ , P ,T
(2)
φ
where X i = mole fraction of component ‘i’ on phase φ and, γ i
φ , P ,T
= activity coefficient of ‘i’ in phase φ
1