Infrared emission and infrared spectroscopy has been used to study a series of selected natural smithsonites from different origins. An intense broad infrared band at 1440 cm −1 is assigned to the ν 3 CO 3 2− antisymmetric stretching vibration. An additional band is resolved at 1335 cm −1. An intense sharp Raman band at 1092 cm −1 is assigned to the CO 3 2− symmetric stretching vibration. Infrared emission spectra show a broad antisymmetric band at 1442 cm −1 shifting to lower wavenumbers with thermal treatment. A band observed at 870 cm −1 with a band of lesser intensity at 842 cm −1 shifts to higher wavenumbers upon thermal treatment and is observed at 865 cm −1 at 400 °C and is assigned to the CO 3 2− ν 2 mode. No ν 2 bending modes are observed in the Raman spectra for smithsonite. The band at 746 cm −1 shifts to 743 cm −1 at 400 °C and is attributed to the CO 3 2− ν 4 in phase bending modes. Two infrared bands at 744 and around 729 cm −1 are assigned to the ν 4 in phase bending mode. Multiple bands may be attributed to the structural distortion ZnO 6 octahedron. This structural distortion is brought about by the substitution of Zn by some other cation. A number of bands at 2499, 2597, 2858, 2954 and 2991 cm −1 in both the IE and infrared spectra are attributed to combination bands.
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