“…More detailed results were obtained by deconvolution of the XPS O 1s and N 1s spectra, which provided evidence for several different O and N species being distributed on the carbon-rich surfaces (Figure ). In the N 1s core region, four main components at 398.9 eV (±0.1 eV), 400.2 eV (±0.1 eV), 401.6 eV (±0.2 eV), and 405.8 eV (the latter one exceptionally for SK) were distinguished and attributed to pyridinic, pyrrolic, quaternary nitrogen, and oxidized nitrogen species, respectively. , In turn, in the O 1s spectra, three essential peaks appeared at 531.1 eV (±0.1 eV), 532.2 eV (±0.1 eV), and 533.8 eV (±0.1 eV) and were assigned to CO (oxygen atom in carbonyl), OC–O (oxygen atom in ester, anhydride and carboxylic acid), and C–O (oxygen atom in phenol/ether), respectively. , Furthermore, one more component was found at 533.3 eV for the HNO 3 treated sample (SK) and assigned to nitro groups . Obviously, during the modification of SK with NH 3 (sample SK_N), the nitro species were reduced completely, forming mainly pyridinic and pyrrolic functionalities (cf.…”