Abstract
A comprehensive theory of the catalytic formation of water on rhodium tips
in high electric fields is performed. The kinetic parameters are obtained
through experimental data and density functional theory calculations of O and H adsorbed on rhodium clusters and at low indexed rhodium surfaces as a function of coverage and the electric field. A kinetic mean field model is then setup and generalized to all of surface orientations present on
the rhodium tip. The theory is consistent with the coverage and
temperature dependence of the total sticking coefficient and the
temperature-programmed desorption rates of O$_2$ on Rh(111), Rh(110) and Rh(100). It is also consistent with the temperature-programmed desorption rates of H$_2$ on these three surfaces as well. The experimental evidence of subsurface oxygen is found to be necessary in the model. The model reproduces the existence region for kinetic oscillations in good agreement with field ion microscopy experiments and exhibits a good agreement with the observed bistability region.
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