It was demonstrated that a system that can exchange energy and volume with a reservoir is in equilibrium with the reservoir when the pressure is the same in the system as in the reservoir. This idea can be extended to a complicated set of many interacting subsystems to arrive at the conclusion that pressure and temperature must be uniform at equilibrium.
Recall the method that was used to demonstrate the uniformity of
and
:
from a conservation principle (i.e., constant internal energy and constant volume)
for an extensive variable, and with a maximal principle for entropy (i.e.,
)
it followed that the intensive variables associated with the conserved quantities must
be equal at equilibrium.
At constant temperature and pressure, the Gibbs free energy
of the system is minimized at equilibrium-this is another extremal
principle
With another conservation principle, another equality
can be derived.
For a closed system, the total number or atoms or molecules of a particular type
is conserved; this is an additional constraint for each species in the
possible
phases:
![]() |
(20-1) |
where the equations are written out for the
-type atoms.
Using a similar expression for each of the
-conserved species and putting
this into the expression for
:
![]() |
(20-2) |
Because
is minimized at equilibrium at constant
and
, it follows
that if any species
can be exchanged between the
-phase and the
-phase
(i.e., one can consider virtual changes with nonzero values of
)
then it follows from Equation 20-2 that
at equilibrium.
To see this consider three different cases:
In other words, a chemical species could be spontaneously transported from a phase of larger chemical potential to one of lower chemical potential.
At equilibrium, the chemical potential of any transportable species,
![]() |
(20-3) |