28 1 Thermodynamics of Grain Boundaries
surface solution can indicate their activity, which, naturally, should be related
to their surface concentration, i.e. to the fraction of the atoms of a particu-
lar kind in the surface. However, the values of the chemical potentials are
assigned to surface atoms, which are the surface excesses but not the real
atoms of the surface (boundary) solution. The surface activities and the sur-
face concentrations are activities and concentrations not of the atoms making
up the interface, but of the excess atoms in the Gibbs method. Compatibility
between the thermodynamic approach, given above, and the model theories
is possible only when the number of “excess thermodynamic” atoms coincides
with the number of the real or model atoms.
For interphases this can be achieved if the dividing surface is placed at a cer-
tain position. So, for the system gas-condensed phase the imaginary dividing
surface will be placed between the monolayer and the bulk of the condensed
phase. Then, due to the fact that the gas density is negligible compared to
the density of the condensed phase, the adsorption quantities are simply the
numbers of atoms of a certain kind per unit area of the surface layer, and the
surface concentration is (Fig. 1.8)
c
s
i
=Γ
i
/
i
Γ
i
(1.108)
Therefore, if the surface activity is known as a function of the surface concen-
tration, we get a comprehensive description of the thermodynamic properties
of the surface.
There is an essentially different situation for grain boundaries. As men-
tioned, the surface excesses are independent of the position of the dividing
surface, and the values of the grain boundary adsorptions will always differ
significantly from the number of atoms in the grain boundary. Consequently,
the Gibbs method, where the surface excess of volume is zero, is not applica-
ble. The alternative approach is known as the method of the surface layer of
finite thickness. We still consider the phases as homogeneous, but now they do
not come into contact along the two-dimensional dividing surface to which, in
the Gibbs method, surface excess quantities belong, but instead are divided
by a surface layer of a finite thickness. As a result the net volume of the
phase V
s
(the volume of the transition layer) is less than the total volume of
the system. Accordingly the expressions for the other surface excesses will be
changed as well; for example, the number of the particles is
N
s
=
˜
N − n
v
V
α
+ V
β
=
˜
N − n
v
V + n
v
V
s
(1.109)
where
˜
N is the number of all particles in the system.
Inasmuch as the surface excess of the volume differs from zero, the right-
hand side of the Gibbs equation will contain an additional term that includes
the pressure differential
dγ = −s
s
dT −
k
i
Γ
i
dμ
i
+ V
s
dp (1.110)
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