
106
Chapter 5. Beyond Crystals
line describes free energy of phase separation between those two points. The points
c
a
and
Cb
in Figure 5.5 have been chosen so that this construction resulted in the
lowest possible free energy.
A typical phase diagram is largely occupied with regions of phase separation.
Consider the diagram in Figure
5.3(B)
for copper and silver. Regions Ag and Cu
are primary phases of fee metal with substitutional impurities. The region marked
"Liquid" is also a homogeneous mixture. Everywhere else, the two metals phase
separate. The solid lines then indicate the concentrations c
a
and
Q,
as a function of
temperature. For example, at 700
°C,
separation occurs between the two concen-
trations that have been marked. In the region denoted "Ag+liquid" a primary alloy
of silver coexists with a liquid containing a greater percentage of copper. The line
describing the composition of the liquid is called the liquidus, while the line de-
termining the composition of the solid is the solidus. The point marked "Eutectic"
has technological significance, since it provides the lowest possible temperature at
which the two metals mix in the molten state. As soon as the two metals are cooled
below the eutectic temperature, however, they begin to phase separate, so if the
goal is a homogeneous material there is a race against time.
Binary phase diagrams have a number of characteristic shapes that appear
bizarre at first glance, but which have a rather natural explanation in terms of sim-
ple assumptions concerning the free energies of solid and liquid phases. The idea
is best illustrated geometrically and is shown in Figure 5.6.
5.3.5 Nonequilibrium Structures in Alloys
A material composed of large numbers of small crystalline regions of different
orientations is said to be built out of
grains,
and the interfaces between them are
grain boundanes. These boundaries may appear on scales ranging from tens of
nanometers to meters. When the crystallites are at the small end of the scale, one
calls the material microcrystalline. Frequently in metals, the crystalline regions are
on the micron scale, and the materials are called polycrystalline. In sea ice, grains
may grow to scales of
meters.
The orientations of adjoining crystalline regions are
fairly random, and if one takes a two-dimensional slice through such a solid, the
grain boundaries form a characteristic network, with the grain boundaries meeting
in vertices, as shown in Figure 5.7. The manner in which grains grow is the subject
of Problem 6.
A type of grain boundary that occurs in substitutional alloys is the antiphase
boundary, which is a grain boundary where the orientations of the crystals on the
two sides are the same, but there is a shift of phase in the lattice as one crosses
the boundary. Antiphase boundaries can form snaking labyrinthine structures of
great complexity [Figure 5.8(A)]. As the concentration of one element in another
increases, one tends to get crystals dominated by one element embedded in crystals
dominated by the other element. For example, one can have small crystals of N13AI
sitting in a background of nearly pure Al. The forms that these intermixed crystals
can take depend upon the dynamical processes by which they form. In the simplest