The reasons for the too high CO2 selectivity
(near 50
C %) in Co2C-based Fischer–Tropsch to olefins (FTO)
are not clear. Water–gas-shift (WGS) side reaction is thought
to be responsible for this, but in-depth research is lacking. Here,
we revealed the mechanism of the too high CO2 selectivity
in Co2C-based FTO. Kinetic studies showed that WGS reaction
was more likely to occur than the hydrocarbon production reaction.
In addition, a too severe WGS reaction would result in the formation
of an H2-enriched and CO-deficient environment on the catalyst
surface, which was not favorable for the generation of light olefins.
Catalyst characterization results proved that the severe WGS reaction
could also lead to the transformation of prismatic Co2C
to spherical Co2C. Theoretical calculations demonstrated
that prismatic Co2C (020) and Co2C (101) facets
were dominant crystal facets for both FTO and WGS reactions. Furthermore,
in situ diffuse reflectance infrared Fourier transform spectroscopy
experiments found that the H2O produced in FTO completely
participated in the WGS reaction. This clearly revealed why the CO2 selectivity was close to 50 C % in FTO. Therefore, we believed
that accelerating the desorption of H2O on the catalyst
surface and preventing its readsorption are the key elements for inhibiting
CO2 formation in FTO.