Relevance of Co, Ag-ferrierite catalysts acidity and cation siting to CH4-NOx-SCR activity

The influence of acidity on Ag,Co exchanged ferrierite obtained from different parent forms was tested in CH4-DeNO(x) reaction. Ag and Co cation siting distribution and residual zeolite acidity were evaluated by means of a quantitative evaluation of catalyst acidity through NH3-TPD experiments and a detailed structural catalyst characterization by Rietveld refinement. A new nomencluature for the cation sites in hydrated and dehydrated cation exchange ferrierites was introduced for sake of clarity. The sites relative populations obtained by the UV-Vis spectra did not agree with the values given by the Rietveld refinement and the SCR activity scale since the high abundance of Co cations in the retained most active position, Co2a, was shown by the less active catalyst obtained from the Na,K form. It was concluded that SCR, activity does not; only depend on Co and Ag siting within the zeolite framework but also by the presence of residnal acidity evidenced on the most active catalysts. CH4 combustion tests showed that the presence of residnal acidity appears relevant to SCR catalytic performances, likely related to its ability in methane activation. The importance of the coexistence, of Co and zeolitic acid sites for the HC-SCR suggested that SCR reaction could proceed on a dual site.