Abstract
DURING the past three years I have collected evidence (now being published, submitted July 1949) that a new kind of slip is common in crystals. It is proposed to call it ‘rotational slip’, and it can be defined as the slipping of one part of a crystal on a neighbouring part, so that the two atomic sheets which slide over one another are densely populated planes, as in translational slip, but rotationally displaced about an axis normal to their plane (with or without simultaneous translational displacement) to one of a series of definable new positions where metastable equilibrium can occur. There is then only a two-dimensionally periodic partial fitting together of the two crystal parts. Neither the occurrence nor the nature of such slip has been clearly demonstrated hitherto.
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References
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WILMAN, H. Rotational Slip—a New Deformation Process in Crystals. Nature 165, 321–322 (1950). https://doi.org/10.1038/165321b0
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DOI: https://doi.org/10.1038/165321b0
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