2003
DOI: 10.1002/sia.1546
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Quantitative chemical composition of thin films with infrared spectroscopic ellipsometry: application to hydrated oxide films on aluminium

Abstract: A method to quantify the composition of thin films using infrared spectroscopic ellipsometry (IRSE), supplemented by visible spectroscopic ellipsometry (VISSE), is proposed. Because ellipsometry measures the thickness and optical constants of a surface layer simultaneously, the absorption coefficient of the film as a function of wavelength can be obtained. Using values of the absorption coefficients for the pure components of the film, the percentages (mol.% or wt.%) of each component in the film can be calcul… Show more

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Cited by 36 publications
(28 citation statements)
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“…When the aluminum substrate is taken out from the boiling deionized water, the aluminum surface has high surface‐free energy and, hence, the adventitious hydrocarbon is adsorbed on the surface. By hydration, the aluminum surface becomes porous as a result of a formation of pseudoboehmite,6, 14–15 and,, hence, more surface area leads to the reduction of the adventitious carbon concentration compared with the degreased substrate. Since OC (BE = 532.0–532.1 eV) and OC (BE = 533.2–533.6 eV) components can also be observed in the O1s peaks, the cross reference of C1s and O1s peak fits allow to quantify aluminum oxide (O 2− ) and hydroxide (OH − ) components of O1s.…”
Section: Resultsmentioning
confidence: 99%
“…When the aluminum substrate is taken out from the boiling deionized water, the aluminum surface has high surface‐free energy and, hence, the adventitious hydrocarbon is adsorbed on the surface. By hydration, the aluminum surface becomes porous as a result of a formation of pseudoboehmite,6, 14–15 and,, hence, more surface area leads to the reduction of the adventitious carbon concentration compared with the degreased substrate. Since OC (BE = 532.0–532.1 eV) and OC (BE = 533.2–533.6 eV) components can also be observed in the O1s peaks, the cross reference of C1s and O1s peak fits allow to quantify aluminum oxide (O 2− ) and hydroxide (OH − ) components of O1s.…”
Section: Resultsmentioning
confidence: 99%
“…The second peak, showing the most important changes as a function of the storage and pretreatment conditions, is due to pseudoboehmite (AlOOH). 12 As expected, an alkaline pretreatment enhances the dissolution of the oxide layer and allows the precipitation of hydroxyl groups at the remaining oxide according to the model described by Vedder and Vermilyea. 13 Another support for the presence of pseudoboehmite is the asymmetric peak at around 3500 cm 1 .…”
Section: Methodsmentioning
confidence: 87%
“…13 Another support for the presence of pseudoboehmite is the asymmetric peak at around 3500 cm 1 . Indeed, this peak can be deconvoluted into two components: one for the OH stretching of water (near 3500 cm 1 ) and one for the OH stretching of AlOOH (near 3300 cm 1 according to Van Gils et al 12 ). However, the peak at about 1100 cm 1 is relatively broad meaning that other absorptions may be present.…”
Section: Methodsmentioning
confidence: 99%
“…2. The refractive indices were based on literature values [1,5]. ψ mod and ∆ mod were computed by the equations of Azzam and Bashara [6] for polarised light reflected from a layered structure of different materials of uniform thickness positioned on each other.…”
Section: Resultsmentioning
confidence: 99%
“…Most of the available work in this subject is based on ex-situ spectroscopic techniques [1][2][3]. The surfaces characterised ex situ may be quite different from the actual surface during reactions between the organic molecules and the oxide covered aluminium surface in a solution.…”
Section: Introductionmentioning
confidence: 99%