view article

Figure 5
Specimen coordinate system P, orientation-dependent crystallographic coordinate system Mathematical equation and laboratory coordinate symtem L for (a) Cu and (b) Mo. (c) Plane view of an experimental sample with coordinates of specimen P for Cu and Mo when β = 0° (the Mathematical equation and P axes are aligned). Sharing a common Mathematical equation axis (sample normal), the Mo crystallographic coordinate system is oriented 30° clockwise relative to the Cu system about this axis. For the Mo layer, the coordinate system PMo is defined following convention and to remain consistent with the reference, such that stresses are evaluated in a frame rotated with respect to PCu according to the crystallographic OR between Cu and Mo. In this framework, the stress tensor of each layer is determined with respect to its corresponding coordinate system. Although referred to as a specimen coordinate system by convention, PMo should be understood as a layer-specific reference frame used for stress evaluation.

Journal logoJOURNAL OF
APPLIED
CRYSTALLOGRAPHY
ISSN: 1600-5767
Follow J. Appl. Cryst.
Sign up for e-alerts
Follow J. Appl. Cryst. on Twitter
Follow us on facebook
Sign up for RSS feeds