Selective Catalytic Reduction of NO by NH3 on Cu-Faujasite Catalysts: An Experimental and Quantum Chemical Approach

The selective catalytic reduction (SCR) of NO by NH3 in the presence of O2 on Cu‐faujasite (Cu‐FAU) has been studied. Substitution of some Cu2+ with H+ and Na+ cations, compensating for the negative charge of the zeolite framework, forms the various CuHNa‐FAU studied. The amount of Cu was held constant and the proportion of H+ and Na+ varied in the sample. The substitution of Na+ for H+ increases sharply the SCR rate by lowering the temperature of reaction by about 150 K. It is proposed that the rate increase mainly comes from an unhindered migration of Cu from hidden to active sites and a modification of the redox properties of Cu species. The former was demonstrated by diffuse reflectance IR spectroscopy of adsorbed CO. The change in redox properties was demonstrated by a faster oxidation of Cu+ to Cu2+ (rate‐determining step). Quantum chemical calculations on model clusters of CuHNa‐FAU indicate that the faster rate of oxidation can be explained by a higher lability of protons in the absence of Na, which can be then removed from the catalyst more easily to yield H2O during the oxidation process. More sodium, more active. Cu‐faujasite is a catalyst for the selective catalytic reduction of NO by NH3. Substitution of some of the Cu2+ with H+ and Na+ ions increases sharply the SCR rate with an increase in Na; the rate increase appears mainly to comes from an unhindered migration of Cu from hidden to active sites and a modification of the Cu redox properties. This experimental result was verified with quantum chemical calculations on model clusters of CuHNa‐FAU (as shown).