In materials science, a Lomer–Cottrell junction is a particular configuration of dislocations.

When two perfect dislocations encounter along a slip plane, each perfect dislocation can split into two Shockley partial dislocations: a leading dislocation and a trailing dislocation. When the two leading Shockley partials combine, they form a separate dislocation with a burgers vector that is not in the slip plane. This is the Lomer–Cottrell dislocation. It is sessile and immobile in the slip plane, acting as a barrier against other dislocations in the plane. The trailing dislocations pile up behind the Lomer–Cottrell dislocation, and an ever greater force is required to push additional dislocations into the pile-up.

ex. FCC lattice along {111} slip planes

             |leading| |trailing|

${\displaystyle {\frac {a}{2}}[{\text{0 1 1}}]\rightarrow {\frac {a}{6}}[{\text{1 1 2}}]+{\frac {a}{6}}[{\text{-1 2 1}}]}$

${\displaystyle {\frac {a}{2}}[{\text{1 0 -1}}]\rightarrow {\frac {a}{6}}[{\text{1 1 -2}}]+{\frac {a}{6}}[{\text{2 -1 -1}}]}$

Combination of leading dislocations:

${\displaystyle {\frac {a}{6}}[{\text{1 1 2}}]+{\frac {a}{6}}[{\text{1 1 -2}}]\rightarrow {\frac {a}{3}}[{\text{1 1 0}}]}$

The resulting dislocation is along the crystal face, which is not a slip plane in FCC at room temperature.

Lomer–Cottrell dislocation

References