1992
DOI: 10.1016/0016-2361(92)90026-k
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ESCA investigations on Schleenhain lignite lithotypes and the hydrogenation residues

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Cited by 43 publications
(8 citation statements)
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“…Figure shows typical XPS spectra of S 2p for the studied coal samples: dem L and Cz, as well as L and Cz oxidized by O 2 /Na 2 CO 3 or PAA which represent highly and moderately oxidized samples. The fitting of S2p peaks (without fixing either positions or half-widths) gave the following binding energies: 163.6 ± 0.1, 165.1 ± 0.2, and 168.0 ± 0.3 eV which correspond respectively to sulfides + thiophenes + thioethers + mercaptans, , sulfoxide C−SO−C, , or sulfones C−SO 2 - C . The first and the third peak are in a very good agreement with literature and the second in a reasonable one; however, it must be added that no constriction on the binding energy was used in the fitting program.…”
Section: Resultssupporting
confidence: 70%
“…Figure shows typical XPS spectra of S 2p for the studied coal samples: dem L and Cz, as well as L and Cz oxidized by O 2 /Na 2 CO 3 or PAA which represent highly and moderately oxidized samples. The fitting of S2p peaks (without fixing either positions or half-widths) gave the following binding energies: 163.6 ± 0.1, 165.1 ± 0.2, and 168.0 ± 0.3 eV which correspond respectively to sulfides + thiophenes + thioethers + mercaptans, , sulfoxide C−SO−C, , or sulfones C−SO 2 - C . The first and the third peak are in a very good agreement with literature and the second in a reasonable one; however, it must be added that no constriction on the binding energy was used in the fitting program.…”
Section: Resultssupporting
confidence: 70%
“…The corresponding S2p peak was curve resolved using a mixed Lorentzian± Gaussian line shape. Sulfur functionality in coals is assigned from the observed shifting of the binding energy (BE) of the level S2p for different organic sulfur compounds taken as models listed in the literature: 158.7±159.6 eV pyritic, 161.2±162.5 eV sul®dic, 163.7±164.0 eV thiophenes, thioeters and mercaptanes, 166.0 eV sulfoxide, 168.0 eV sulfone, 169.2 eV sulfonate, and 174.8±175.8 eV sulfate [22]. Table 2 shows the quantitative results for sulfur forms obtained by the ASTM method.…”
Section: Methodsmentioning
confidence: 99%
“…It could be observed that the great contribution mainly resulted from various organic oxygen sources of C−O groups at the BE value ∼532.9 eV, CO groups at the BE value ∼531.4 eV, and OC−O groups at the BE value ∼535.4 eV in LZ coal. 68,69 Meanwhile, inorganic oxygen sources from different minerals in LZ coal should be noted, mainly including some oxides, quartz (SiO 2 ), and kaolinite (Al 2 Si 2 O 5 (OH) 4 ) as shown in Figure 5a. Especially for the latter two silicon-based minerals, they owned the propensity to enrich on the upper surface of coal particles 22 and overlapped with some organic oxygen functional groups (e.g., CO groups, C−O groups) in a certain XPS regions, 70 which complicated identification and quantification of the related organic oxygen functional groups.…”
Section: Energy and Fuelsmentioning
confidence: 99%