Dislocation climb is therefore dependent from the velocity of vacancy diffusion.
2.
The driving force for dislocation climb is the movement of vacancies through a crystal lattice.
3.
Since dislocation climb results from individual atoms " jumping " into vacancies, climb occurs in single atom diameter increments.
4.
At low stresses, materials with a low initial dislocation density may creep by dislocation climb alone, known as Harper-Dorn creep.
5.
The most likely mechanism, given the experimental data, is that of dislocation climb, rate limited by the diffusion of solute in the bulk.
6.
Viscous flow near grain boundaries, for example, can give rise to internal slip in the direction of any lattice plane containing the dislocation, while the principal driving force for " dislocation climb " is the movement or diffusion of vacancies through a crystal lattice.
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