A. Nylund et I. Olefjord, SURFACE-ANALYSIS OF OXIDIZED ALUMINUM .1. HYDRATION OF AL2O3 AND DECOMPOSITION OF AL(OH)3 IN A VACUUM AS STUDIED BY ESCA, Surface and interface analysis, 21(5), 1994, pp. 283-289
Pure polycrystalline Al (99.998%) was oxidized in dry oxygen and water
. The surface products formed were analysed by ESCA. The thicknesses o
f the amorphous Al2O3 formed during oxidation for 1 h in dry oxygen at
25-degrees-C and 250-degrees-C are 14 and 20 angstrom, respectively.
During exposure of the oxidized sample to water a surface layer of amo
rphous Al2O3 is hydrated and Al(OH)3 is formed by the reaction: Al2O3
+ 3H2O reversible 2Al(OH)3. The hydroxide is not stable in a vacuum. D
uring analysis in the ESCA instrument. Al(OH)3 is decomposed to Al2O3
and H2O because the equilibrium pressure of H2O is higher than the par
tial pressure of water in the vacuum system. It is found that a 7 angs
trom thick layer of Al2O3 is formed on the surface of Al(OH)3. The bin
ding energies of the Al3+(2p) and O2-(1s) signals recorded from Al2O3
formed on Al at 22-degrees-C and at 250-degrees-C are 75.8 and 532.7 e
V, respectively. The binding energies of these peaks are 0.6 eV lower
for a sample preoxidized at 250-degrees-C and then exposed to a humid
atmosphere and immediately analysed. It is suggested that the change o
f the binding energy is due to set up of a space charge during exposur
e to a humid atmosphere. After exposure for a long time to a humid atm
osphere the charging decays and the binding energies approach their no
rmal values.