“…These diffractions were assigned to (001), (200), (220), (3 1), (2 2), (3 1), (4 1), and (420) crystal planes of Form I considering their two‐theta value. For the sample without any treatment, the intensity distribution of the diffraction indicates an anisotropic structure in the sample 40 . As T h was higher than 236°C, the intensity distribution of the diffraction was changed obviously from a combination of arc and circle to full circle with increasing T h , indicating a transition of orientation from oriented to randomly distributed one.…”