290 3 Grain Boundary Motion
motion at somewhat lower temperatures is most probably related to the in-
teraction of the grain boundary with mobile liquid lead droplets. Above the
wetting transition temperature, the boundary is completely wetted by liquid
lead, and this drastically changes the mechanism of grain boundary motion.
Therefore, the observed temperature dependence of grain boundary migration
in Al doped with minor amounts (20 ppm) of Pb [331] suggests that the lead
solubility in Al is indeed negligible, so that even at concentrations as low as
20 ppm lead exists in aluminum as a second phase.
The size of lead particles can be estimated [331] using the experimentally
determined grain boundary mobilities at T<T
w
(Fig. 3.110). For fine parti-
cles their dominant mechanism of motion is the mechanism of surface diffusion
[207] (Table 3.2). The experimentally determined velocity of grain boundary
motion at T<T
w
can be considered as the critical velocity for the joint mo-
tion of grain boundary and particles. From this the radius of the particles was
estimated as 5 · 10
−8
≤ r ≤ 10
−7
m.
If grain boundary migration at T<T
w
is controlled by the mobility of
liquid lead droplets, then the activation enthalpy of grain boundary motion
should be close to the activation enthalpy of droplet motion [208]. This conclu-
sion is supported by the experimental data. As is well known, the activation
enthalpy for surface diffusion is significantly lower than that for the bulk dif-
fusion. The activation enthalpy for bulk self-diffusion in Al is H
D
∼ 1.5eV,
whereas the activation enthalpy for boundary migration at T<T
w
was found
to be 0.8–1.0 eV for both grain boundaries studied.
Wetting phenomena at grain boundaries require two phases (liquid and
solid) being in equilibrium with each other. The contact angle Θ depends on
the grain boundary surface tension γ and the surface tension of solid-liquid
interface γ
SL
: γ =2γ
SL
cosΘ (Fig. 3.111).
For γ ≥ 2γ
SL
the boundary is completely wetted by the liquid phase, and
Θ = 0. In the latter case the boundary cannot coexist with the liquid and is
replaced by a layer of the liquid phase. The temperature dependencies of the
surface tensions γ and γ
SL
are schematically shown in Fig. 3.112. The wetting
transition at the grain boundary occurs at the temperature T
w
,whereγ(T )
intersects 2γ
SL
(T ). If two grain boundaries have different surface tensions,
we may expect that their wetting transitions occur at different temperatures:
namely the lower the γ, the higher the T
w
. This agrees with experimental
results [331]: the energy of the Σ7 special boundary is lower than the energy
of the 40.5
◦
non-special boundary, and the wetting transition temperature for
the special grain boundary (T
w,s.
= 560
◦
C) is noticeably higher than that for
the non-special one (T
w,ns.
= 535
◦
C) (Fig. 3.110).
Usually the wetting transition at a grain boundary is observed under cir-
cumstances where a bicrystal is in contact (equilibrium) with a large amount
of liquid. Such type of wetting may be called an “external” wetting in contrast
to the “internal” wetting, when the wetting liquid is distributed as fine par-
ticles (droplets) in the bulk of the grains. For an internal wetting transition,
when the grain boundary becomes covered by a liquid layer of thickness λ at
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