“…[34] The spectral features at regions 740, 650, and 460-600 cm −1 are attributed to Sb-O-Sb, Fe-O-Sb, and O-Fe-O bonding, [35] respectively. As Sb-O-Sb bonding mode falls around 740 cm −1 , for the entire range of samples calcinated at different temperature a single prominent peak in the range 740 cm −1 can be ascribed to Sb-O bond or Sb-O stretching, [33,35,36] and as temperature increases this bond disappears and leaves Fe-Sb-O bond. Moreover, there are no prominent bonds observed in the range 1500-4000 cm −1 , hence confirming the absence of broad peaks corresponding to the hydroxyl bands of adsorbed water.…”