In this communication we propose an interpretation of friction-induced
sub-surface texture results obtained by Krause et al. [1]. The variat
ion of X-ray texture measurements with depth in single phase metals wa
s found to increase sharply, peaking at a small depth from the surface
then decaying slowly into the sample. However, TEM studies showed a c
ontinuous and exponential decrease in grain rotation with depth [2]. W
e argue that the X-ray texture results reflect an experimental artifac
t originating from the superposition of the sub-surface residual stres
ses with grain rotation to give the observed peak in the X-ray texture
measurements.