“…For the Co containing samples, the diffraction peaks at 2Â ca. 31 • , 37 • , 45 • , 60 • and 65 • , corresponding to (2 2 0), (3 1 1), (4 0 0), (5 1 1) and (4 4 0) reflections were discerned, which was a typical feature of Co 3 O 4 in agreement with the previous reports [44][45][46] and the UV-vis data presented above. The diameter of Co 3 O 4 crystallites calculated from the width of the (3 1 1) diffraction peak are shown in Table 1 This may be due to that high Mn amount and more calcination times favor agglomeration of supported cobalt oxide particles.…”