Thermotransport effects in grain boundaries in lead were studied by means of a temperature gradient (≤60 K cm −1) lying parallel to the planes of the boundaries. The temperature gradient was observed to result in grain boundary sliding, migration and enhanced boundary diffusion. These effects are interpreted in terms of climb and/or glide motion of grain boundary dislocations induced by the gradient. The behaviour of boundaries in temperature gradients seems to differ from the behaviour reported in concentration gradients (diffusion induced boundary migration) suggesting different mechanisms to operate in both cases.
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