1997
DOI: 10.1002/(sici)1096-9918(199711)25:12<924::aid-sia317>3.0.co;2-2
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Correction for the effects of adventitious carbon overlayers in quantitative XPS analysis

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Cited by 69 publications
(52 citation statements)
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“…Accordingly, the trace C 1s signal observed on the SiO x -deposited surface was not possibly from unreacted TEOS molecules, and furthermore, it was impossibly from BOPP itself either because XPS sampling depth had only several nanometers that should be short enough to confine the sampling range within the 150 nm silica film. As a result, the trace C 1s is from adventitious carbonaceous contamination, which was often encountered when the samples were prepared in air and examined in less than optimal vacuum conditions [93].…”
Section: Resultsmentioning
confidence: 99%
“…Accordingly, the trace C 1s signal observed on the SiO x -deposited surface was not possibly from unreacted TEOS molecules, and furthermore, it was impossibly from BOPP itself either because XPS sampling depth had only several nanometers that should be short enough to confine the sampling range within the 150 nm silica film. As a result, the trace C 1s is from adventitious carbonaceous contamination, which was often encountered when the samples were prepared in air and examined in less than optimal vacuum conditions [93].…”
Section: Resultsmentioning
confidence: 99%
“…The C 1s region of the pristine sample shows distinct peaks corresponding to CF 2 (292 eV) residues as it expected in PTFE‐containing samples. Furthermore, the presence of C−C bonds was indicated by a peak at 285 eV, which originated from adventitious carbon that forms a thin layer on air exposed samples . Comparison of the C 1s regions of the deactivated and reactivated samples leads to the conclusion that carbonate species were formed upon electrode storage under industrial conditions, as indicated by the peak at 288 eV (Figure a) .…”
Section: Resultsmentioning
confidence: 99%
“…Furthermore, the presence of CÀC bonds was indicated by ap eak at 285 eV,w hich originated from adventitious carbon that forms at hin layer on air exposed samples. [22] Comparison of the C1sr egions of the deactivated and reactivated samples leads to the conclusion that carbonate speciesw ere formed upon electrode storageu nder industrialc onditions, as indicatedb yt he peak at 288 eV (Figure 5a). [23] Ap ossible origin for that is the formation of Ag 2 CO 3 induced by the adsorption of CO 2 during air exposure.…”
Section: Characterization Of the Surface Ag Speciesmentioning
confidence: 96%
“…This carbon is termed adventitious carbon, 50 and is present as a result of exposure of the clean (high surface energy) gold substrates to air between cleaning and placement in the XPS instrument. The major peaks are due to gold, and there are additional small peaks due to carbon and oxygen.…”
Section: Characterization Of Gold Filmsmentioning
confidence: 99%