The carbon monoxide (CO) oxidation reaction, taking place over oxygen-rich
Ru(0001) surfaces, has been used here as a simple probe of the reactivity o
f oxygen species formed by high temperature oxidation procedures. For surfa
ces oxidized at temperatures lower than 950 K a high reaction probability,
within a range of 10(-2), has been found. The kinetics of CO, emission exhi
bit a fast and a long term component which reflects the contributions of th
e topmost and the subsurface oxygen phases, respectively. Both kinetic comp
onents are drastically reduced when working with surfaces resulting from th
e application of the same oxidation procedure but at temperatures above 950
K. For preparation temperatures above 1100 K the reaction probability is b
elow the detection limit. In this temperature range, the oxygen phases show
valence region ultraviolet photoelectron spectroscopy features characteris
tic of a regular RuO2 solid phase. Moreover, these non-reactive surfaces ar
e marked by intense emission of RuO3, RuO4 and Ru2O molecular fragments as
appearing in thermal desorption spectra in a temperature range 1000-1300 K.
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