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Preferred orientation arises when crystallites have a tendency to align along a certain direction, resulting in a nonrandom distribution of crystallite orientations in the sample, affecting the relative intensities of given peaks. This is often most severe when the morphology is strongly anisotropic (e.g., flat plates or long needles), and the effects are often seen by comparison of the relative intensities of peaks in data collected in both disc and capillary geometries. The preferred orientation effects of platelike crystallites can be minimized by collection in capillary mode.
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