Cu-oxide
catalysts have a tendency to deactivate dramatically in
reverse water gas shift (RWGS) reaction, because of the aggregation
of supported copper particles at high temperatures. Herein, β-Mo2C, which is a typical type of transition-metal carbide, has
been demonstrated to be capable of dispersing and stabilizing copper
particles. Cu/β-Mo2C catalysts exhibit good catalytic
activity and stability for the RWGS reaction. Under relatively high
weight hourly space velocity (WHSV = 300 000 mL/g/h), the optimized
1 wt % Cu/β-Mo2C exhibits superior activity
over traditional oxide-supported Pt- and Cu-based catalysts. The activity
was well-maintained in a 40 h stability test, and the catalyst shows
stable reactivity in a six-cycle start-up cool-down experiment. Detailed
structure characterizations demonstrate that the strong interaction
between Cu and β-Mo2C effectively promotes the dispersion
of supported copper and prevents the aggregation of Cu particles,
which accounts for the extraordinary activity and stability for the
RWGS reaction.
CO
oxidation at room temperature over the Au/CeO2 catalyst
was investigated, of which the induction period arising from unreduced
cationic Au was disclosed. The effect of humidity in reactant stream
on catalyst activity was investigated during induction and deactivation
periods. The induction period was significantly reduced from 44.8
min in dry stream to 3.3 min in wet stream containing 0.58 vol % of
H2O. The induction period was slightly shortened by further
increasing water concentration in the reactant stream. The maximum
initial activity was achieved with a wet stream containing 0.74 vol
% of H2O vapor. In situ DRIFTS measurements suggested that
humidity contributed to the formation and consumption of reaction
intermediates [COOH]s and hence enhanced the initial activity.
After the induction period, the deactivation phenomena of Au/CeO2 catalyst at varied rates under both wet and dry streams were
observed. In contrast to a slow deactivation under dry stream, a fast
deactivation in wet stream was first observed due to rapid blockage
of active sites by water adsorption, followed by a slow deactivation
rate due to gradual formation of surface carbonate species over catalyst
with time on stream. A mechanism was proposed to illustrate the existence
of induction period under both wet and dry streams.
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