Abstract
The interaction of oxygen and nitric oxide with clean aluminium surfaces has been investigated by X-ray photoelectron spectroscopy. Studies have been in the main confined to the temperature range 80–290 K and pressure range 10
-6
–10
-2
Pa. The Al(2p) level is shown to exhibit a shifted component at a binding energy of ~ 74.5 eV after oxygen interaction at 80 K. A curve-fitting and deconvolution analysis of the shifted peak indicates that it is made up of two components, one at a binding energy of 74.0 eV and the other at 75.3 eV. The lower binding energy component (designated
α
) develops preferentially at 80 K while the higher binding energy one (
β
), assigned to Al
2
O
3
, is dominant at 290 K. We suggest that
α
is an incorporated oxygen structure which is a precursor to the formation of Al
2
O
3
. The initial sticking probability of oxygen at 80 K is 0.07 while at 290 K it is 0.02. The plasmon-loss features associated with the Al(2s) peak are shown to be sensitive to oxygen adsorption and therefore useful in confirming the surface monolayer. At 290 K and an oxygen pressure of 10
4
Pa the oxide thickness is estimated to be about 0.9 nm. When NO was adsorbed at 80 K three distinct N(1s) peaks were observed at binding energies of about 397, 403 and 407 eV. We assign the 397 eV peak to N
δ-
ads
arising from dissociation of the molecule and the two higher binding energy peaks to N
δ-
ads
and N
2
O
ads
. The N(1s) peak characteristic of NO
δ-
ads
is close to the lower binding energy peak of the two N(1s) peaks associated with N
2
O
ads
while the O(1s) of NO
δ-
ads
overlaps with the O(1s) peak of the surface oxide at a binding energy of about 532 eV. Mass spectroscopic analysis of the gas phase indicated that on warming to 85 K, the adlayer formed at 80 K, N
2
O was desorbed, confirming our assignment of the core-level spectra. The NO
δ-
and N
2
O species are not observed at 290 K while at 80 K exposure of the adlayer to water vapour results in the complete removal of weakly adsorbed N
2
O. By monitoring the intensities of the Al(2p), N(1s) and O(1s) peaks, estimates were made of the absolute and relative concentrations of the various species and various molecular processes delineated.
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