2017
DOI: 10.1002/sia.6364
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Intensity modulation of the Shirley background of the Cr 3p spectra with photon energies around the Cr 2p edge

Abstract: The background in X-ray photoelectron spectroscopy data originates, partially, from inelastically scattered photoelectrons. In fact, the current theoretical methods for calculating the background intensity are based on electron energy losses. However, a critical part of the experimental signal, which is known as the Shirley background, cannot be described within the current formalisms. This suggests that the Shirley electrons are not associated with energy losses of photoelectrons and must originate from a dif… Show more

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Cited by 16 publications
(22 citation statements)
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“…The choice of fitting function and background has been the subject of many studies over the past 50 years and the references therein. In this section, three different approaches to combining Gaussian and Lorentzian function for fitting XPS spectra are described.…”
Section: The Choice Of Fitting Functionmentioning
confidence: 99%
“…The choice of fitting function and background has been the subject of many studies over the past 50 years and the references therein. In this section, three different approaches to combining Gaussian and Lorentzian function for fitting XPS spectra are described.…”
Section: The Choice Of Fitting Functionmentioning
confidence: 99%
“…We note that the Cr2p, Cr3p, and Cr3s spectra in Figures 1 and 2 of the paper by Herrera‐Gomez et al are asymmetric to the higher binding energy side, as is the O1s spectrum in their Figure 2, indicating the presence of sub‐peaks; the C1s spectrum is not shown. While the presence of the O1s spectrum clearly indicates the existence of an oxide, this possibility was not considered in their discussion of the Cr peaks.…”
Section: Conditions Of Applicabilitymentioning
confidence: 51%
“…The reason for this is evident: The background is removed before the component peak is separated into its sub‐peaks and, for closely overlapping sub‐peaks, this results in a single step‐shaped baseline, rather than one for each sub‐peak. Perhaps because Herrera‐Gomez et al do not consider sub‐peaks, no mention is made of this problem in their paper.…”
Section: Conditions Of Applicabilitymentioning
confidence: 99%
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