Condensed (reduced) phase rule: the phase rule is F = C − P + 2. For solid–liquid equilibria such as alloys, the vapour phase is practically absent and the experiments are done at constant atmospheric pressure, so pressure is not a variable. The degrees of freedom fall by one:
\( F' = C - P + 1 \) (for a two-component system, F' = 3 − P)
Merits of the phase rule
- It applies to both physical and chemical equilibria, and to both homogeneous and heterogeneous systems.
- It classifies systems simply by the number of degrees of freedom, whatever substances are involved.
- It needs no knowledge of molecular structure, because it deals only with macroscopic variables (T, P, composition).
- It predicts how a system behaves when T, P or composition change, and whether a system is in equilibrium.
- It shows that different systems with the same F behave alike.
- It is useful in metallurgy (alloys, eutectics), in extraction (e.g. Pattinson's process) and in preparing freezing mixtures.
Limitations
- It applies only to systems in true equilibrium, so it is of little use for slow-reaching or metastable systems.
- It considers only T, P and composition, and ignores electrical, magnetic and gravitational effects and surface forces.
- All phases must be under the same T and P.
- Solid and liquid phases must not be finely divided, otherwise vapour pressure and solubility change.
- It gives no information on the rate of attainment of equilibrium or on the amounts of the phases.
- It is hard to apply to systems that need a long time to reach equilibrium.