Abstract
Classical Powder Diffraction usually assumes samples with
completely random orientation distribution of the crystallites. It
can be generalized to non-random orientation distribution
(texture) by introducing a texture factor which enters the
expression of the integral intensity directly and serves as a
weight function in expressions of peak shift or peak broadening.
Hence, all methods of powder diffraction, for instance, phase
analysis, crystal structure analysis, stress analysis, particles
size analysis, can also be carried out with textured samples.Textured polycrystalline samples may be considered as being
intermediate between single crystals and random powder samples.
Hence, they contain information about the directions of reciprocal
lattice vectors