Analysis of the structural parameters controlling the temperature window of the process of SCR-NOx by low paraffins over metal-exchanged zeolites

Catalytic activity of H- and FeH-ferrierite (FER) zeolites with iron content from 50 to 4000 ppm in NO–NO₂ equilibration and SCR of NO_x by propane was measured, both in NO₂-poor and NO₂-rich streams. The activity of FeH-FER in SCR in NO₂-poor streams depends strongly on the Fe content; this relationship is valid down to traces of iron, while no such correlation was indicated in NO₂-rich streams. This was rationalized by realizing the negligible activity of zeolite protons for NO–NO₂ equilibration. Accordingly the SCR activity of H-FER in NO₂-poor streams necessitates presence of iron traces. In the NO₂–O₂–propane mixtures a process in absence of zeolite catalyst initiating propane oxidation and NO₂→NO conversion, but without N₂ formation, was evidenced at temperatures over 350 °C. It is suggested that such a radical process participate in characteristic narrow temperature window for NO_x reduction by propane.