126 4 Dislocation Motion
As long as the activation energy to overcome the obstacles and the num-
ber of involved atoms are small, the particles are passed by the aid of thermal
activation, and the flow stress depends on the temperature and the deforma-
tion rate. The dislocation motion is then jerky on the scale of the particle
distance. This is a small scale for solution hardening with Mott statistics, and
a larger one for precipitation hardening with Friedel statistics. The force–
distance curve of even relatively large particles may have a narrow tip so that
thermal activation may still play some role. The Orowan mechanism for large
impenetrable particles is of fully athermal character as the energies to form
even small dislocation loops are too high for thermal activation, as mentioned
in Sect. 3.2.2. In this case, the stress has to be high enough to overcome the
strongest configurations. The dislocation motion is then very jerky on a large
scale.
4.8 Dislocation Intersections
In most cases of plastic deformation, dislocation motion is not restricted to
a single slip system, instead several slip systems are activated simultaneously
(multiple slip). Then, the moving dislocations have to intersect dislocations
of other slip systems, usually having different Burgers vectors. These dis-
locations are called forest dislocations. The process of dislocation cutting is
very complex. The crossing dislocations experience a mutual long-range elastic
interaction, as outlined in Sect. 3.2.5. In general, the interaction includes com-
ponents of the interaction force out of the glide plane, which may induce cross
glide or climb. Within the glide plane, the interaction leads to pinning either
by attractive or repulsive forces with the dislocations bowing out between
the forest dislocations. Figure 4.31 presents an example of an edge disloca-
tion pinned by a screw dislocation with perpendicular Burgers vector (arrow).
The bow-outs may be strong so that the moving dislocations have to form the
critical half-circle (Frank–Read) configuration (3.47) to overcome the forest
dislocations. Then, the segment length L equals the average distance between
the forest dislocations
−1/2
f
,if
f
is the forest dislocation density. Thus, the
contribution of the dislocation forest to the flow stress can be written as
τ
forest
= α
f
μb
2π
√
f
. (4.73)
The factor α
f
describes the strength of the actual interaction force and
should be less than 2π. An alternative process is the formation of dislocation
junctions if the interaction is attractive and reduces the dislocation energies
(see Sect. 3.2.2 and Fig. 3.10). For b.c.c. crystals, values of α
f
≈ 0.4 π were
computed by virtual displacement of the triple nodes bounding the junctions
[227]. In addition to these long-range interactions, there is a short-range con-
tribution due to the formation of jogs or kinks in both dislocations as already
shown in Fig. 3.16. As described in Sect. 3.2.5, the formation energy of the jogs