Abstract
Results concerning the lattice re-orientation caused bv abrasion on single crvstals of beryllium have been obtained by electron diffraction. The occurrence of twinning found in certain cases in sub-surface regions of abraded singlecrystal beryllium surfaces was dependent upon the initial crystal orientation with relaiion to the direction of the applied compressive stresses. The operative {101-bar2} set of twinning planes was found to be the one which most facilitated development of the characteristic oblique STA001! compression fibre texture produced by the abrasion in the outermost surface layers by rotational slip or flexural rotational slip of the sub-surface twin. (auth)
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