338 9 Intermetallic Alloys
dislocations in TiAl at room temperature were also used to explain the flow
stress anomaly. Both models assume that cross slip leading to the forma-
tion of pinning centers is thermally activated so that the number of pinning
points increases with increasing temperature. However, above about 430
◦
C,
the dominating ordinary dislocations no longer bow out between localized
obstacles. In the in situ experiments, the ordinary dislocations are created
instantaneously in an avalanche, which had already been observed in earlier
in situ experiments, as reviewed in [552]. If they move again, they are smoothly
bent, moving in a viscous way as shown in Fig. 9.13 and Video 9.6, similarly
to NiAl described in Sect. 9.4. This had not been observed before in TiAl. It
clearly contradicts the cross slip models of the flow stress anomaly. First, the
dislocation segments no longer show the curly shape, and second, the disloca-
tions move continuously, but not in the proposed pinning–unzipping mode. As
discussed earlier, the dislocations are not confined to their slip planes, indi-
cating that climb is involved. Smoothly curved dislocations not lying on a slip
plane were recently observed also in a post-mortem study [553]. This view is
supported by the formation of helical dislocation structures in two-phase Ti–
Al during in situ heating experiments [554]. Climb requires lattice diffusion
of both atomic species. The formation and migration energies of vacancies in
TiAl are between 1 and 1.6 eV [555,556]. Thus, these vacancies are present and
mobile in the temperature range around the flow stress maximum. However,
climb usually facilitates dislocation motion and results in recovery so that it
does not induce additional friction.
Since the low-temperature mechanism of precipitation hardening ceases to
operate above 575
◦
C, an additional process must cause the increase or at least
the constancy of the flow stress in the range of the anomaly, associated with
the viscous type of dislocation motion. Viscous motion at high temperatures is
not consistent with simple models of a superposition of long- and short-range
obstacles to dislocation motion, as outlined in Sect. 5.2.2 and Fig. 5.20. In
the high-temperature (athermal) case, the dislocation motion becomes very
jerky. It is a major aim of the intermetallics chapter of this book to stress
that diffusion-controlled processes may give rise to additional friction imped-
ing the motion of dislocations in intermetallic alloys. Locking mechanisms
and diffusion-controlled processes are compared in [557]. These diffusion pro-
cesses may have quite different origins as will be discussed in the present and
following sections. γ-TiAl probably is a relatively simple case where point
defect atmospheres form around the dislocations as described in Sect. 4.11.
The atmosphere formation may be superimposed with climb, which follows
from the dislocations not being restricted to their glide planes at high temper-
atures. The atmospheres around dislocations may form from solute impurities
as proposed in [552] to cause strain ageing effects. Such effects have been
observed between 150 and 350
◦
C [558], i.e., at temperatures where the pre-
cipitation hardening ceases to contribute to the flow stress. The amplitude of
strain ageing increases when the Al content decreases below 50%. It is there-
fore concluded that the responsible point defects are antisite defects which