10.5 Mechanisms of Dislocation Motion and Plastic Deformation 441
effects of the dynamics of dislocation motion from those of the development
of the microstructure in which the dislocations move. Accordingly, dislocation
properties and macroscopic deformation data will be discussed in parallel.
10.5.1 Glide or Climb Motion of Dislocations
It’s amazing how long it can take to see the obvious. But of course it’s only
obvious now.
- Ian Stewart, Mathematician
While the deformation curves of different quasicrystals measured in the
high-temperature range are quite similar, irrespective of the particular chemi-
cal composition and quasicrystal structure, the ranges of the temperature and
flow stresses scatter widely. However, Takeuchi showed that in a plot of the
upper yield stress versus the temperature, the curves of the different icosa-
hedral quasicrystals approach each other, if the axes are suitably normalized
[736]. The scaling relations are σ
y
= σ
y
/E and T
= T/(E¯a
3
), where E is the
bulk modulus, and ¯a, an average of the Goldschmidt diameters of the atoms
constituting the quasicrystal. The possibility of normalizing the temperature
dependence of the flow stress suggests that similar mechanisms control the
plastic deformation in different quasicrystalline materials.
Since the first direct observation of dislocation motion in an icosahedral
quasicrystal in 1995 in [647], it had been assumed that the main mode of
dislocation motion is glide, although there had been hints that this may be
wrong. As described in Sect. 10.3.1, in situ straining experiments by the group
of Caillard have clearly shown that the motion of dislocations with quasiperi-
odic Burgers vectors is dominated by climb [701,704]. In decagonal Al–Ni–Co
quasicrystals deformed along the tenfold axis, dislocations with a periodic
Burgers vector move also by pure climb (Sect. 10.3.2).
Nevertheless, some combination of climb and glide seems to be possible,
too. In the Videos 10.1 and 10.3, dislocations change the projected width
of their planes of motion without changing the orientation of the traces of
the planes, as also illustrated in Fig. 10.19. For geometrical reasons, this is
only possible by a combination of climb and glide. In the post-mortem TEM
study of samples deformed at 300
◦
C, some dislocations had moved in a mixed
mode [702]. Thus, some contribution of glide to the deformation should also
be possible.
While many dislocations have zero orientation factors for glide and max-
imum ones for climb (set A), there also exist dislocation bands with zero
orientation factors for both glide and climb (set B) like those presented in
Fig. 10.12. As it will be discussed in Sect. 10.5.8, the latter dislocations may
climb under a chemical stress originating from sub- or supersaturations of
point defects, which are generated by the dislocations climbing under the
external stress.
The slip plane of a dislocation is a selected plane of conservative motion
with respect to the volume of the system, i.e., ΔV = 0 in (3.3). The question