371 7.5 Analogies with other phase transitions
shows data for a solid, NaMgF
3
with perovskite structure, that behaves in this way. It
is orthorhombic at low temperature, but as temperature increases the lengths of its three
crystallographic axes approach each other and the solid undergoes a lambda-type phase
transition at T
λ
≈ 1050 K, where it takes on cubic symmetry. The figure shows the dif-
ference (in Å) between the lengths of the a and b crystallographic axes (data from Zhao
et al., 1993). This difference serves as the order parameter, and could be converted, if one
wishes, to a non-dimensional variable that takes the value 1 at T = 0 by dividing by a −b
at 0 K. Even without doing this, however, the figure shows clearly that a −b goes to 0 at an
accelerating rate as T
λ
is approached, just as in the case of an order–disorder transition. In
fact, the change in crystal symmetry can be understood as an order–disorder transition by
considering rotations and distortions in the crystalline framework that affect the entropy of
the crystal (see, for example, Putnis, 1992).
The bottom panel in Fig. 7.8 shows the difference between the molar volumes of water
vapor and liquid water coexisting at equilibrium (obviously, pressure cannot be constant
along this curve – why?), normalized to the volume of the vapor. The molar volumes
become equal at the critical temperature (∼647.3 K) and a single supercritical phase exists
at T>T
c
. Two phases exist below T
c
, and their volumes diverge rapidly immediately below
this temperature. We shall return to critical phenomena in fluids in Chapter 9. There are
other important critical phenomena that we will not discuss in this book. Examples include:
the para-ferromagnetic transition at the Curie temperature, responsible, for example, for
the preservation of thermal remanent magnetization in igneous rocks; the appearance of
superconductivity in some materials at low temperature; and the existence of a superfluid
liquid-helium phase near absolute zero. What is common to all of these processes is that in
all of them it is possible to define an order parameter that goes to zero continuously and at
an accelerating rate as the critical temperature is approached from below, and that stays at
zero above the critical temperature.
It has been known for a long time that systems that behave in this way display anomalies
in the second derivatives of the Gibbs free energy in the neighborhood of the critical
temperature. This is true of heat capacity, compressibility and thermal expansion (equations
(4.135)to(4.137)), but for now we will focus on c
P
only. At a first-order phase transition
these three quantities become infinite, because as long as a univariant assemblage is present
energy transfer (either thermal or mechanical) causes changes in entropy and volume at
constant temperature and pressure, by forming some phases at the expense of others. The
“infinite heat capacity” occurs only at the first order phase transition, at which S and V are
discontinuous, but c
P
(and the other second derivatives) behave normally everywhere else.
At a lambda phase transition the second derivatives are anomalous in the neighborhood of
the transition temperature, and diverge strongly (but may or may not become infinite) at the
transition temperature itself. Three examples of this behavior are shown in Fig. 7.9. The top
two correspond to crystal symmetry phase transitions, including the example of NaMgF
3
perovskite. The bottom panel in Fig. 7.9 corresponds to an order–disorder transition caused
by alignment of magnetic moments in ferrosilite. In every case the dashed curve shows what
the “normal” heat capacity would be expected to be. The measured values define a strong
and steep positive anomaly relative to these expected values, which is characteristically
lambda-shaped, hence the name for this type of phase transition. An important point is that,
whether or not c
P
becomes infinite at the transition temperature, the function is integrable
across the transition, i.e., the area under the lambda-shaped anomaly is finite. This area needs
to be known in order to be able to calculate the entropy of the solid at T > T
c
(Section 4.7.1).