“…First, we noticed the diffraction peaks (and their corresponding planes) of CS located at 2θ of 31.2° (18,2,1), 34.1° (20,0,1), 37.9° (10,0,3), 46.8° (0,16,0), and 48.9° (886) matched well the CS monoclinic phase (JCPDS no: 23-0958). [24] Similarly, the diffraction peaks (and their corresponding planes) of CCO located at 2θ of 31.25° (220), 36.96° (311), 38.63° (222), 44.68° (400), 59.66° (511), and 65.25° (440) matched well the characteristic peaks of the spinel lattice (JCPDS No 71-0816) (Figure 1a). [25] For the CS/CCO composites, all the peaks also matched the standard patterns of the CS and CCO, confirming that their formation and the growth of CS did not alter their respective crystal structures.…”