“…In Figure a, we illustrate the X-ray diffraction patterns for Zn x Fe 3– x O 4 ( x = 0/0.1/0.2/0.3/0.4) under 2θ values ranging from 20 to 80°. We can observe here that the occurring peaks are contributed from the indexed crystal planes, (220), (311), (400), (422), (511), and (440), respectively, and the diffraction peaks of Zn x Fe 3– x O 4 ( x = 0.1/0.2/0.3/0.4) are similar to those of pure Fe 3 O 4 , indicating that all of these samples have a crystal unit with face-centered cubic inverse spinel structure. ,− To check the peak displacement by changing x , as shown in Figure b, the strongest diffraction peak is selected from the (311) plane in 2θ ranging from 34 to 37° to study the structure change of the crystal unit. Taking the (311) peak of Fe 3 O 4 as the baseline, we can notice that with the increase of x , the (311) peak tends to shift to a lower angle.…”