2003
DOI: 10.1016/s0368-2048(02)00284-0
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Core-level XPS spectra of fullerene, highly oriented pyrolitic graphite, and glassy carbon

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Cited by 190 publications
(157 citation statements)
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“…Figure 3 shows our measured carbon 1s spectrum together with previous experimental results [25,27]. Both the signature of the π plasmon and the presence of at least one additional structure on the π + σ plasmon satellite are clearly visible.…”
Section: Graphite-gw + C *mentioning
confidence: 52%
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“…Figure 3 shows our measured carbon 1s spectrum together with previous experimental results [25,27]. Both the signature of the π plasmon and the presence of at least one additional structure on the π + σ plasmon satellite are clearly visible.…”
Section: Graphite-gw + C *mentioning
confidence: 52%
“…Both the signature of the π plasmon and the presence of at least one additional structure on the π + σ plasmon satellite are clearly visible. The additional structure has been termed P 3 , and measured in various carbon based materials [25] (see also, e.g., [27]), but could never be explained to our knowledge. However, for all measured materials it appears to be situated approximatively at the sum of the materials-dependent energies of the first two main plasmon peaks [25].…”
Section: Graphite-gw + C *mentioning
confidence: 99%
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“…The carbon pi-pi shake-up satellite peak at 290.7 eV (Muller et al 2007) further confirms the presence of aromatic carbon. The fullerenes were first discovered by Kroto, Smalley, andCurl in 1985 (Kroto et al 1985;Dementjev et al 2000;Leiro et al 2003). The fullerenic carbon has a remarkable cage-like polyhedral geometry that is the consequence of arranging sp 2 -bonded carbon atoms in pentagonal and hexagonal rings to form a closed shell (Grieco et al 2000).…”
Section: Carbon Chemical Statesmentioning
confidence: 99%