Kinetic
measurements, microkinetic modeling, and CO and O2 uptake
experiments lead to a proposed mechanism for CO oxidation
on dispersed Ag cluster surfaces. CO turnovers occur via kinetically
relevant reactions between O2* and CO* on Ag cluster surfaces
nearly saturated with O* and CO*. The operating pressure ratio of
O2 to the square of CO, [O2]-to-[CO]2, dictates the relative O* and CO* coverages and in turn the rate
coefficients. Low [O2]-to-[CO]2 ratios lead
to Ag cluster surfaces saturated with CO*, during which the first-order
rate coefficients (r
CO[CO]−1) increase linearly with the pressure ratio. As the [O2]-to-[CO]2 ratio increases, the CO* coverages decrease
and O* coverages concomitantly increase, and the rate coefficients
become independent of the [O2]-to-[CO]2 ratio.
CO* binds to Ag clusters more strongly than O*, and as a result, CO*
coverages decrease and O* coverages increase as the reaction temperature
rises when comparing at a constant [O2]-to-[CO]2 ratio. The rate coefficients for CO oxidation on CO* covered Ag
clusters initially increase with increasing Ag cluster diameter to
∼5 nm, but decrease with a further increase in Ag diameter
beyond 5 nm. The former trend reflects more weakly bound and reactive
O2* and CO*, and the latter likely reflects the depletion
of O2* molecules.