“…The appearance of strong peaks in two structure samples indicates that the produced ZIF‐8 has high crystallinity, which is consistent with previous studies,
[47,52] where the peaks at 2
as 7.30, 10.35, 12.70, 14.80, 16.40, and 18.00° correspond to planes (110), (200), (211), (220), (310), and (222), respectively (Figure 2c–d). The presence of identical peaks in the Ag/ZIF‐8 samples indicates that the Ag NPs were successfully produced, with the peaks at 2
as 38.15° and 44.36° corresponding to planes (111) and (200)
[53] . The area under the Ag peak of the Ag/ZIF‐8 structure is significantly reduced compared to the reverse structure due to the presence of secondary species (ZIF‐8) on the covered surface, but no significant changes deviated in the peaks.…”