“…The peaks in the diffraction pattern of Zn 1 − x Mn x O at 31.81°, 34.43°, and 36.30° can be indexed to a hexagonal wurtzite structure, which consists of three prominent peaks corresponding to (100), (002), and (101) planes, respectively. Compared with the peak position of ZnO (inset), that of Zn 1 − x Mn x O was found to shift towards lower angles with Mn incorporation, probably due to the larger ionic radius of Mn 2+ (0.066 nm) relative to that of Zn 2+ (0.060 nm) [ 20 , 21 ]. The XPS survey spectrum confirms that the sample mainly contains Zn, Mn, and O (Fig.…”