(41c) Synthesis Gas Conversion over Rh-Based Catalysts Promoted By Fe and Mn
AIChE Annual Meeting
2017
2017 Annual Meeting
Catalysis and Reaction Engineering Division
Science and Engineering of Catalyst Preparation
Sunday, October 29, 2017 - 4:10pm to 4:30pm
Here, we present our results on synthesis gas conversion to oxygenates and hydrocarbons over Rh-based catalysts promoted by Fe and Mn. We show that selective deposition of Fe and Mn species on Rh nanoparticles can be achieved by controlled surface reactions. By carrying out reactions at 523 K, 580 psi and CO/H2=1/1, the catalytic results show that the interaction between Rh and Fe promotes the selective production of ethanol through hydrogenation of acetaldehyde and enhances the selectivity towards C2 oxygenates, which include ethanol and acetaldehyde. Mn promotes the overall reaction rate and the selectivity towards C2+ hydrocarbons, primarily alkenes. Trimetallic Rh-Fe-Mn catalysts surpass the performance of their bimetallic counterparts. The highest selectivities towards ethanol (36.9%) and C2 oxygenates (39.6%) were achieved over the Rh-Fe-Mn ternary system with a molar ratio of 1:0.15:0.10, as opposed to the selectivities obtained over Rh/SiO2 which were 3.5% and 20.4%, respectively. Moreover, 55% of the total products are industrially valuable oxygenates and C2+ hydrocarbons. To understand the nature of Fe and Mn species, measurements obtained from X-ray photoelectron spectroscopy suggest that Fe and Mn exist as metallic iron and manganese oxides on Rh surface upon reduction. Through density functional theory (DFT) calculations, we reveal that manganese oxide is more stable on the Rh (211) step-edges whereas metallic iron has no preference over Rh (111) and (211). Fourier transform infrared spectroscopy of adsorbed CO and DFT calculations suggest that the adsorption of CO on Fe and/or MnOx modified Rh (211) step-edges is altered compared to the binding of CO to clean Rh (211) surface. Accordingly, MnOx species and Fe alter the bonding of CO on Rh step-edges and shift their selectivity away from CH4, while reduced Fe species also alter the reactivity of Rh terrace sites.
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