Abstract

Four catalysts, 1.5% Fe/SiO2, 3.0% Fe/SiO2, 5.7% Fe/carbon, and Fe2O3, exhibited different phase transformations when subjected to reduction and reaction conditions. After reduction at 673 K in H2 for 16 h, 31% of the iron in 1.5% Fe/SiO2 was in superparamagnetic Fe0 particles with the remainder in Fe2+ species, while 3.0% Fe/SiO2 contained 91% of its iron as α-Fe0 with the remainder as superparamagnetic Fe2+ species. The iron in 5.7% Fe/C existed mostly as α-Fe0 (63%) with the balance present as Fe2+ species, which were mostly superparamagnetic, and the Fe2O3 was completely reduced to α-Fe0. After 8 h on stream, only Fe2+ and Fe3+ species were detected in 1.5% Fe/SiO2, which gave only decomposition products; the 5.7% Fe/C catalyst contained α-Fe, Fe2+, Fe3+, and θ-Fe3C phases and had completely deactivated, and the two active, stable catalysts—3.0% Fe/SiO2 and Fe2O3—showed the presence of both α-Fe and FeO phases under steady-state reaction conditions. It is proposed that the former phase provides sites to activate H2, and the latter provides different sites to adsorb and activate acetic acid by producing a reactive acetate intermediate. DRIFTS, coupled with TPD and TPR experiments, revealed that surface acetate species are formed during acetic acid adsorption at 300 K on iron surfaces and they appear to be an active intermediate at the reaction temperatures used here. Reaction of this surface acetate with H atoms via a Langmuir–Hinshelwood-type mechanism is proposed to be the principal reaction pathway for acetic acid reduction to acetaldehyde.

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