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Non‐destructive depth analysis of the surface oxide layer on Mg 2 Si with XPS and XAS
Author(s) -
Esaka Fumitaka,
Nojima Takehiro,
Udono Haruhiko,
Magara Masaaki,
Yamamoto Hiroyuki
Publication year - 2016
Publication title -
surface and interface analysis
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.52
H-Index - 90
eISSN - 1096-9918
pISSN - 0142-2421
DOI - 10.1002/sia.5939
Subject(s) - x ray photoelectron spectroscopy , x ray absorption spectroscopy , analytical chemistry (journal) , surface layer , absorption spectroscopy , synchrotron radiation , electron spectroscopy , chemistry , oxide , yield (engineering) , electron , chemical state , materials science , layer (electronics) , nuclear magnetic resonance , optics , nanotechnology , physics , organic chemistry , chromatography , metallurgy , quantum mechanics
Depth analysis of the surface oxide layer on a Mg 2 Si crystal was performed with X‐ray photoelectron spectroscopy (XPS) and X‐ray absorption spectroscopy (XAS). In XPS, X‐rays from synchrotron radiation with the energies between 2100 and 3300 eV were used as the excitation sources for depth analysis. The Si 1s and Mg 1s XPS spectra show the formation of a thinner SiO 2‐X layer at outermost surface and a thicker MgO layer at lower surface on the Mg 2 Si. In XAS, total electron yield and partial electron yield (PEY) acquisition modes were used for the measurement of Si K‐edge. The PEY spectrum was obtained by detecting electrons with a fixed kinetic energy of 5, 10, 20, 30, 40, or 50 eV. Although the PEY spectrum with electrons of 5 eV shows similar features with the total electron yield spectrum, detection of electrons with 50 eV gives an increase in the ratio of a peak at 1843.7 eV to the peak assigned to Mg 2 Si. The peak at 1843.7 eV can be assigned to the formation of SiO 2‐X on the Mg 2 Si. From XPS and XAS results, it is indicated that a thinner SiO 2‐X layer at outermost surface and a thicker MgO layer at lower surface are formed at initial oxidation of the Mg 2 Si. Copyright © 2016 John Wiley & Sons, Ltd.