“…The principal 2θ peaks for orthorhombic strontianite occurred at 20.47°, 25.29°, 29.59°, 31.47°, 36.28°, 41.42°, 44.29°, 47.45°, and 50.06°, corresponding to (110), (111), (002), (121), (112), (220), (221), (132), and (113) planes, respectively. For the monoclinic nesquehonite, the 2θ peaks occurred at 18.01, 23.12, 24.86, 27.57, 29.44, 32.21, 35.78, and 47.20° corresponding to (101), (200), (103), (013), (400), (212), (301), and (400) planes, , respectively. The crystallite sizes were 24.85 ± 3, 18 ± 2, and 88.32 ± 3 nm for witherite, strontianite, and nesquehonite, respectively.…”