This is an investigation of the effect of different types of forest dislocation on the rate of twin layer broadening, V n, in zinc and beryllium crystals, and on the velocity of the twinning dislocation movement, V t, in zinc crystals under the action of a constant external shear stress. Increasing the forest basal dislocation density, ϱ b, was found to result in increasing V n and reducing V t, while increasing the forest pyramidal dislocation density, ϱ p, causes V n to decrease. An analysis in terms of crystal geometry shows that the dualism of the influence of the basal dislocations stems from the fact that they behave as twinning dislocation sources whose density, increasing with ϱ b, leads to higher V n. The decrease in the effective stress, τ ∗, with increasing ϱ b is estimated. An analysis of the experimental data yielded the relation V t (τ ∗) and an estimate of the activation volume, which amounted to 6 × 10 −21 cm 3. The close coincidence of the activation volumes as obtained from V t (τ ∗) and V n (τ) suggests that the rate-controlling mechanism of the twin layer development in zinc crystals with large forest basal dislocation density is the twinning dislocation inhibition. In Be crystals, the increasing V n effect is observed during untwinning. In Be twinned crystals, electron microscopy revealed twinning dislocations with a density of about 10 5 cm −1 at the twin boundaries and a large forest basal dislocation density inside the twin ( ca. 10 8 cm −2).
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