Abstract

Density functional theory (DFT) calculation was used to study the hydrogen promotion effect for the selective catalytic reduction (HC-SCR) of NO x over Ag–MFI zeolite. The nature of the bond between an Ag atom and MFI is ionic. One of the roles of hydrogen addition is to neutralize the cationic Ag atom by forming an AgH molecule. We propose that the formation of a Ag 4 cluster is achieved by the AgH diffusion as follows: 2AgH + Ag-Z-Ag → HAg 4H-Z → Ag 4-Z + H 2. With the presence of oxygen, the HAg 4H cluster prefers the formation of HOO − adsorbate to the desorption of H 2. O 2 is physisorbed on the Ag 4 cluster. Thus, the HAg 4H cluster is important for the activation of oxygen. Another role of hydrogen addition is to reproduce the HAg 4H cluster from the Ag 4 cluster which is generated by the SCR reaction from HOOAg 4H species. Since time dependent DFT (TD-DFT) calculation shows that the UV absorption bands of the HAg 4H cluster are weak, UV–vis measurements are not adequate for the study of the reaction mechanisms of HC-SCR.

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