Abstract
The influence of the subsurface oxygen in monomer–dimer (CO–NO) surface reaction is studied by Monte Carlo simulation. Three different reaction mechanisms are considered. In mechanism A, the presence of subsurface adds two extra steps to the usual four steps of simple Langmuir–Hinshelwood mechanism of the system. In mechanism B, one single step is added to the usual four steps in order to incorporate diffusion of oxygen from surface to subsurface (which has experimental evidence). In mechanism C, the presence of subsurface modifies two steps of the usual four. Mechanism A reveals a phase diagram with two transition points and a steady reactive state. Mechanisms B and C do not generate any steady reactive state. The effect of the diffusion of adsorbed species on the surface is also considered. The diffusion of N atoms has significant effect on the phase diagrams of mechanisms A and B. In mechanism C, the diffusion of CO molecule presents an interesting situation in which usual “second-order” transition has been eliminated. The usual “first-order” transition has been changed into second order.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.