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Kinetic Monte Carlo simulations of the water gas shift reaction on Cu(111) from density functional theory based calculations

[Display omitted] •A first principles kinetic Monte Carlo study of the water gas shift reaction on Cu(111).•The associative mechanism (carboxyl intermediate) was the main reaction path.•There is a change in the rate-limiting step from low to high temperature.•Mixtures with higher CO proportion enhan...

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Published in:Journal of catalysis 2016-01, Vol.333, p.217-226
Main Authors: Prats, Hèctor, Álvarez, Leny, Illas, Francesc, Sayós, Ramón
Format: Article
Language:English
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Summary:[Display omitted] •A first principles kinetic Monte Carlo study of the water gas shift reaction on Cu(111).•The associative mechanism (carboxyl intermediate) was the main reaction path.•There is a change in the rate-limiting step from low to high temperature.•Mixtures with higher CO proportion enhance the production of H2. A systematic first-principles kinetic Monte Carlo study of the water gas shift reaction taking place on the Cu(111) surface is presented including adsorption/desorption, diffusion and other elementary chemical reactions, totalling 34 elementary steps with all reaction rates obtained from periodic density functional theory based calculations. The kinetic Monte Carlo simulations were carried out at different partial pressures and temperatures. The results show that the diffusion processes cannot be neglected and that the reaction proceeds predominantly through an associative mechanism via a carboxyl intermediate. The analysis of temperature dependence shows an Arrhenius behaviour with an apparent activation energy of 0.5–0.8eV in agreement with experiments and with previous microkinetic studies. The effect of H2O/CO ratio on this reaction shows that mixtures with higher CO proportion enhance the reactivity, also in accordance with previous studies. The present work allows one to ascertain the relative importance of the different steps in the mechanism of water gas shift reaction over Cu(111) at several conditions as well as to see the coverage evolution of the surface.
ISSN:0021-9517
1090-2694
DOI:10.1016/j.jcat.2015.10.029