Abstract
The reaction between NO and NH 3 over a Pt(100) single-crystal surface was studied at low pressures (1.5 × 10 −6−6 × 10 −5 Torr), at temperatures between 420 and 485 K, and with NO/NH 3 ratios ranging from 0.1 to 4.3. It is shown that this reaction shows oscillatory behaviour. Besides single-peaked rate oscillations also various multiple-peaked and aperiodic oscillations were observed. The influence of temperature, NO/NH 3 ratio, pressure and the addition of oxygen on the oscillations were assessed. In order to elucidate more details concerning the mechanism of the reduction reaction, labelled compounds ( 15NH 3 and 18O 2) were used. Based on the results obtained, a model for the reaction mechanism is proposed which can explain all experimental observations. The model involves the formation of NO islands on the surface. The reaction between NO and ammonia proceeds rapidly at the boundaries between the NO islands, with parts of the crystal where vacancies and NH 3 fragments are present. It was found that oxygen plays a minor role at the temperatures and pressures used, but that it is not just a spectator molecule. Addition of oxygen at up to 83% of the reaction mixture does not stop the oscillations observed. A short comparison between the NOH 2 and the NONH 3 reaction is given. Furthermore, it cannot be ruled out that the reversible (5 × 20) ↔ (1 × 1) surface reconstruction, which is known to take place upon NO adsorption on Pt(100), plays a role in the appearance of oscillations, but, as will be shown, this is not necessarily the case. A model for the oscillations is proposed in which surface vacant sites are the key factors determining the oscillating behaviour of the NO reduction by NH 3 or H 2.
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