“…However, actual polycrystalline specimens can be nonideal in different ways (Krivoglaz, 2012): the crystallites in a specimen may have preferred orientations (texture) (Bunge & Morris, 1982;Wenk, 2016); they may be under nonhydrostatic strain (Birch, 1947); and there may be only a very limited number of grains sampled by X-rays (Pakala et al, 2000). Texture induces nonuniform or segmented intensity distribution on a Debye-Scherrer ring (Bunge, 1970), a small number of grains also renders incomplete diffraction rings (Sørensen et al, 2012;Wejdemann & Poulsen, 2016), and nonhydrostatic strain distorts the shape of diffraction rings (Singh, 1993;Higginbotham & McGonegle, 2014).…”