In this work, the nature, location and evolution of Cu+ ions in Cu-SAPO-34 are investigated by diffuse reflectance infrared Fourier transform spectrum(DRIFTS) of CO adsorption and density functional theory(DFT) calcul...In this work, the nature, location and evolution of Cu+ ions in Cu-SAPO-34 are investigated by diffuse reflectance infrared Fourier transform spectrum(DRIFTS) of CO adsorption and density functional theory(DFT) calculation. By combination with DFT results, characteristic Cu+–CO bands located at 2154 and 2136 cm.1 are attributed to CO adsorbed on Cu+ ions located at sites I(in the plane of six-membered ring connected to the large cages) and site II(in the eight-membered ring cages near the tilted four membered ring) in the framework of H-SAPO-34 zeolite. Subsequently, both the influences of Cu loading and preparation method are considered and discussed. By varying the Cu loading, the site-occupation preference of Cu+ ions on site I is confirmed,especially at low Cu loadings. Through elevating the desorption temperature, migration of Cu+ ions is revealed because of the adsorption-induced effect. Furthermore, a facile and more efficient approach to introduce Cu+ ions into CHA zeolite, compared with solid-state ion exchange with CuCl and conventional ion exchange in aqueous solution, and the different preparation methods also result in different occupations of Cu+ ions.展开更多
基金supported by the National Natural Science Foundation of China(21325626,21406120)
文摘In this work, the nature, location and evolution of Cu+ ions in Cu-SAPO-34 are investigated by diffuse reflectance infrared Fourier transform spectrum(DRIFTS) of CO adsorption and density functional theory(DFT) calculation. By combination with DFT results, characteristic Cu+–CO bands located at 2154 and 2136 cm.1 are attributed to CO adsorbed on Cu+ ions located at sites I(in the plane of six-membered ring connected to the large cages) and site II(in the eight-membered ring cages near the tilted four membered ring) in the framework of H-SAPO-34 zeolite. Subsequently, both the influences of Cu loading and preparation method are considered and discussed. By varying the Cu loading, the site-occupation preference of Cu+ ions on site I is confirmed,especially at low Cu loadings. Through elevating the desorption temperature, migration of Cu+ ions is revealed because of the adsorption-induced effect. Furthermore, a facile and more efficient approach to introduce Cu+ ions into CHA zeolite, compared with solid-state ion exchange with CuCl and conventional ion exchange in aqueous solution, and the different preparation methods also result in different occupations of Cu+ ions.