“…It was found that several peaks at 2θ values of 22.41°, 31.75°, 32.22°, 37.64°, 38.95°, 39.48°, 45.75°, 51.73°, 56.36°, and 56.96° correspond to (012), (104), (110), (113), (006), (202), (024), (122), (018), and (214) miller planes, respectively. These crystal planes are attributed to the rhombohedral perovskite phase ( R 3 c ) of BiFeO 3 (JCPDS no.. 86-1518). ,, The crystal structure of BiFeO 3 -NC (single phase R 3 c ) would change into another phase once doped with magnesium ions . This could be due to the partial transformation of the Bi–O bond into the Mg–O bond once the partial replacement of Bi 3+ ions by Mg 2+ ions occurred.…”