Abstract

The oxidation of clean polycrystalline aluminium foil was performed in a previously described anaerobic cell and studied by core level and valence band X-ray photoelectron spectroscopy. Oxide free sample surfaces were exposed under inert atmosphere at room temperature to increasingly oxidative environments of water vapor and liquid water beginning with an oxide free metal foil each time. Minor oxidative environments were found to produce a film of boehmite with a thinner outer film of gibbsite. Harsher oxidation in liquid water resulted in an oxide film much thicker than that found on the as received sample which contained an inner composition of gamma alumina with an outer film of gibbsite. As expected, the oxide film observed for ultra high purity polycrystalline aluminiurm foil in the as received state was gibbsite. The valence band of the cleaned metal is discussed in terms of residual surface species. The evaluation and determination of these residual surface species is evaluated following an analysis of two different band structure calculations which use different d orbital exponents. It is found that while the density of states is almost unaltered by changes in the d exponent, the predicted spectrum is substantially changed. The work makes extensive use of valence band X-ray photoelectron spectroscopy.

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