CO2 hydrogenation over
Fe-based catalysts
is a promising
pathway to mitigate emissions of this greenhouse gas and provides
a possibility for crude-oil-free production of chemicals and fuels.
Understanding of (i) the role of crystalline phases or/and surface
species in the working catalysts, (ii) the factors affecting their
formation under reaction conditions, and (iii) the kind and reactivity
of surface precursors of gas-phase products is vital for controlling
the efficiency of CO2 hydrogenation. In this study, we
applied time-resolved in situ characterization techniques
for monitoring phase transformations during Fe2O3 reduction, starting of CO2 hydrogenation, steady-state
operation, and finally catalyst deactivation. The obtained structural
information after different times on stream was related to kinetic
data obtained from temporal analysis of H2 and CO2 activation as well as from steady-state isotopic transient kinetic
analysis (SSITKA). Fe2O3 is easily reduced to
Fe3O4 and Fe in H2 above 300 °C.
Fe5C2 and Fe3C, which are quickly
formed from metallic Fe/Fe3O4 under CO2 hydrogenation conditions, do not undergo oxidation with rising time
on the reaction stream under ambient-pressure conditions. Nevertheless,
the catalyst loses its initial activity and, particularly, the selectivity
to hydrocarbons in favor of CO. Thus, we do not confirm the well-recognized
deactivation mechanism of CO/CO2 hydrogenation through
oxidation of iron carbides. Instead, surface carbonaceous species
identified by in situ Raman and pseudo in
situ XPS measurements were concluded to cause catalyst deactivation
and deselectivation due to hindering the catalyst ability to generate
surface species from H2 and CO2. Specifically,
the strength of CO2 adsorption and the catalyst activity
to dissociate adsorbed CO2 to adsorbed CO decrease in the
presence of carbon deposits. Kinetic evaluation of SSITKA tests revealed
the presence of (i) only one kind of surface intermediate yielding
gas-phase CO after 1.5 h on reaction stream but (ii) at least two
kinds (short-lived and long-lived) of surface intermediates participating
in CH4 formation in parallel. Carbon deposits seem to block
the sites responsible for the formation of short-lived intermediates.