“…The diffraction pattern of Fe 3 O 4 /GO composite with the main peaks at 2 θ = 30.2, 35.2, 43.2, 53.4, 57.2, and 62.5° are indexed to (220), (311), (400), (422), (511), and (440) planes of the magnetite structure (JPPDS NO.19‐0629) [35]. However, no diffraction peak of GO was observed for Fe 3 O 4 /GO, indicating the destruction of the regular layer stacking of GO due to crystal growth of Fe 3 O 4 between interlayer of GO sheets [36, 37].…”