Abstract
We demonstrate that the exchange of zeolitic Brønsted acid sites (BAS) with cations from metal-oxides plays a pivotal role in the propagation of hydrocarbon pools (HCP) during CO2 hydrogenation. We estimated the likelihood of cationic species migration from different oxides-In2O3, ZnZrOx, Cr2O3 and their exchange with BAS by computing metal vacancy formation energies. Accordingly, we integrated metal-oxides and SAPO-34 at nanoscale proximity (~1400 nm), to probe the propensity of the cations to exchange with BAS. To assess the influence of ion-exchange on HCP, we measured propylene-to-ethylene (indicates relative propagation of olefin-to-aromatic cycles) and paraffin-to-olefins ratios, which revealed that Inδ+ species inhibited HCP propagation, Znδ+ species enhanced hydrogen transfer, and Crδ+ species did not influence HCP. Combining reactivity data with ammonia temperature programmed desorption, occluded hydrocarbon analysis, 13C solid-state nuclear magnetic resonance (ssNMR) and X-ray photoelectron spectroscopy analysis (XPS), we provide insights into the influence of ion-exchanged species on HCP for rational integration of bifunctional catalysts.
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