Resumen
A quantitative study of the surface composition of ferric oxide employing photoemission spectra is presented. It was possible to accurately reproduce the expected composition (Fe2.00±0.05O3) by modeling the background as a combination of Shirley-type (Shirley–Vegh–Salvi–Castle) and slope backgrounds through the active approach. The line-shape employed to fit apparent peak asymmetries was the double-Lorentzian. It was possible to resolve a previously unreported satellite located at ~729 eV.
Idioma original | Inglés |
---|---|
Páginas (desde-hasta) | 253-260 |
Número de páginas | 8 |
Publicación | Surface and Interface Analysis |
Volumen | 49 |
N.º | 4 |
DOI | |
Estado | Publicada - 1 abr. 2017 |
Publicado de forma externa | Sí |