464 Solution phases with sublattices
Exercise 21.2
In the plot of a
M
versus y
C
for an interstitial solution of C in M it may seem surprising
in view of Raoult’s law that the curve for a
M
does not approach the diagonal close to
y
C
= 0. Find the reason and calculate the initial slope according to Raoult’s law.
Hint
Raoult’s law says that a
M
should approach x
M
, i.e.1 − x
C
, not 1 − y
C
.Evaluate x
M
from
y
C
using the formula M
b
(Va, C)
1
with b = 1/3 (the value for bcc).
Solution
Forabinary interstitial solution we have x
M
= b/(b + y
C
) = 1/(1 + y
C
/b)
∼
=
1 −
y
C
/b = 1 − 3y
C
. The initial slope should be –3 and not –1.
21.3 Reciprocal solution phases
With a stoichiometric phase one usually means a phase with a constant composition. This
may, for instance, be caused by a crystalline structure which is composed of different
sublattices, one for each component. An example is cementite, Fe
3
C. Such a phase is
also described as a compound. When a further component is added, it may go into one
of the existing sublattices, an example being manganese-alloyed cementite, (Fe,Mn)
3
C.
The composition of such a phase may thus vary along a line in the ternary phase diagram
and it is sometimes described as a quasi-binary phase. Such phases were described
in Section 21.1.Ifstill another component is added, two alternatives result, examples
being (Fe,Mn,Cr)
3
C and (Fe,Mn)
3
(C,N)
1
. The latter type of phase is sometimes called a
reciprocal solution phase because the central alloy can be regarded as a solution between
either Fe
3
C and Mn
3
NorFe
3
N and Mn
3
C. Both kinds of phases have the restriction
to the variation in composition which we have called stoichiometric constraint. The
composition of a reciprocal solution phase is represented by two sets of site fractions,
one set for each sublattice, y
A
+ y
B
= 1 and y
C
+ y
D
= 1.
Accepting the stoichiometric constraint it is logical to consider the binary compounds
as the components of the system. They were introduced in Section 4.8 and are called
component compounds. Let us discuss the reciprocal case represented by (A,B)
b
(C,D)
c
.
This is a quaternary phase but its composition can only be varied with two degrees of
freedom instead of three due to the stoichiometric constraint. All possible compositions
can thus be represented on a plane just like a ternary system. As shown in Fig. 13.12,a
square diagram is now the natural shape and each corner is an end-member and represents
a component compound. Perpendicular to that plane we may plot the Gibbs energy (see
Fig. 21.2).
The diagram demonstrates that it is, in general, impossible to place a plane through
the four points representing the Gibbs energy values of the four component compounds.
The question is then what surface of reference one should use when giving the Gibbs