“…The slight difference of peak intensity in the Ag 3 PO 4 /Ag/AgI series may be due to the decomposition of small part of silver halide . As for the AgX, the characteristic diffraction peaks ascribed to (110), (200), (220), (311), and (222) facets, consistent with AgCl (Figure b). The five apparent peaks at 26.7, 31.0, 44.4, 55.0, and 64.5° contributed to the facets (111), (200), (220), (222), and (400), respectively, which originate from the AgBr (JCPDS card no.…”