1992
DOI: 10.1016/0368-2048(92)85002-o
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X-ray photoelectron studies of Ca, Sr and Ba and their oxides and carbonates

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Cited by 186 publications
(76 citation statements)
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“…To identify the origin of the Sr surf we compare the BE of Sr 3d, O 1s, and C 1s features. The values of the Sr 3d, O 1s, and C 1s binding energies (in eV) reported in the literature for different Sr, O, and C containing compounds are summarised in Table 6 [36,57,58,68,69]. The feature at 288.5 eV was clearly observed in the C 1s spectra of the LSC perovskite and LSCC57 composite, thereby implying the possibility of carbonate formation.…”
Section: Surface States Of Co and Sr Cations Carbon And Oxygen Ionsmentioning
confidence: 94%
“…To identify the origin of the Sr surf we compare the BE of Sr 3d, O 1s, and C 1s features. The values of the Sr 3d, O 1s, and C 1s binding energies (in eV) reported in the literature for different Sr, O, and C containing compounds are summarised in Table 6 [36,57,58,68,69]. The feature at 288.5 eV was clearly observed in the C 1s spectra of the LSC perovskite and LSCC57 composite, thereby implying the possibility of carbonate formation.…”
Section: Surface States Of Co and Sr Cations Carbon And Oxygen Ionsmentioning
confidence: 94%
“…In the C 1s region, both COS and Na-COS exhibited two signals at 285.0 eV and 289.6 eV, due to C-H and carbonate groups, respectively [29]. The Ca 2p of COS and Na-COS exhibited a doublet with a separation of 3.5 eV, 2p1/2, and 2p3/2 components, whose binding energy (BE) values were 347.00 eV, 350.5 eV, and 346.3 eV, 349.8 eV, respectively, suggesting that the Ca was associated with CaO [30,31]. In the O 1s spectra, both COS and Na-COS displayed doublet peaks; however, the intensity Figure 3 presented C 1s, Ca 2p, O 1s, and Na 1s regions for COS (bottom) and Na-COS (top).…”
Section: Catalyst Characterizationmentioning
confidence: 99%
“…Deconvolution of the O 1s spectra yields three peaks, namely O 1s a (529.0 eV), O 1s b (531.2 eV) and O 1s c (532.9 eV). From the literature, the peak at the 532.9 eV is probably due to the water and hydroxide absorbed on the surface [38][39][40][41], while the peaks at 531.2 eV correspond to carbonate compounds and chemical Adsorption [42][43][44][45][46][47][48][49][50][51]. The main peaks at 529.0 eV (O 1s a) correspond to the oxygen lattice [19,20,50].…”
Section: Xps Studiesmentioning
confidence: 99%