“…[ 39,40 ] The reduction curve of Co‐SSZ‐13 can be fitted to six peaks centered at 284, 359, 515, 690, 850, and 963 °C, which can be assigned to the reduction of Co oxo‐ions (284 °C), Co 3 O 4 (359 °C), Co‐O‐Co (515 °C), isolated Co 2+ located at the CHA cage (690 °C) and D6Rs (850 °C) and cobalt phyllosilicate (963 °C), respectively. [ 19,20,41,42 ] It illustrates that more varieties of Co species are formed via a conventional incipient wetness impregnation method. More importantly, a large amount of cobalt phyllosilicate is generated due to the reaction between Co and Si in SSZ‐13 zeolite, which is also detected by Wang et al.…”