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A Dislocation Reaction in the Face-Centred Cubic Lattice Export

Philosophical Magazine, Vol. 42 (1951), pp. 1327-1331.

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The marked difference in the initial rates of strain-hardening of hexagonal and cubic crystals has often been ascribed to some form of interference between slip on non-parallel planes in the cubic material. It is shown in this paper that dislocations on two intersecting slip planes can attract one another and combine to form a "sessile" dislocation (Frank 1949), which may act as a considerable immobile nucleus of internal stress, and so cause the crystal to harden.


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