2019
DOI: 10.1016/j.carbon.2019.04.016
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Three-dimensional structure made with nitrogen-doped reduced graphene oxide with spherical porous morphology

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Cited by 18 publications
(16 citation statements)
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“…In the FTIR spectra (Supporting Information, Figure S6), the broad peak at 3356 cm −1 associated with −OH stretching vibration directly evidenced the existence of GAG cladding in 4 . Furthermore, the characteristic carbonate ν 4 peak at 712 cm −1 in 3 and 4 further supported the formation of calcite species . Owing to the spin‐orbit splitting, the X‐ray photoelectron spectroscopy (XPS) spectrum showed that the Ca 2p spectrum exhibited two contributions, 2p 3/2 and 2p 1/2 , in 4 (Supporting Information, Figure S7).…”
Section: Resultsmentioning
confidence: 86%
“…In the FTIR spectra (Supporting Information, Figure S6), the broad peak at 3356 cm −1 associated with −OH stretching vibration directly evidenced the existence of GAG cladding in 4 . Furthermore, the characteristic carbonate ν 4 peak at 712 cm −1 in 3 and 4 further supported the formation of calcite species . Owing to the spin‐orbit splitting, the X‐ray photoelectron spectroscopy (XPS) spectrum showed that the Ca 2p spectrum exhibited two contributions, 2p 3/2 and 2p 1/2 , in 4 (Supporting Information, Figure S7).…”
Section: Resultsmentioning
confidence: 86%
“…In addition, Figure C and 4E represent the C 1s high‐resolution spectra of Pd−Mn/rGO and pure GO, respectively. The peaks at 284.6 eV, 285 ev, 286.45 eV and 288.5 eV are correspondingly attributed to un‐oxidized C−C, C=C, C−OH and C=O . Interestingly, the measured CC/CO ratio (2.6) for the Pd−Mn/rGO is greater than that for the GO (2.21), recommending the presence of rGO in the Pd−Mn/rGO nano‐composite.…”
Section: Resultsmentioning
confidence: 99%
“…In the FTIR spectra (Supporting Information, Figure S6), the broad peak at 3356 cm À1 associated with À OH stretching vibration directly evidenced the existence of GAGc ladding in 4.F urthermore,t he characteristic carbonate n 4 peak at 712 cm À1 in 3 and 4 further supported the formation of calcite species. [21] Owing to the spin-orbit splitting,t he X-ray photoelectron spectroscopy (XPS) spectrum showed that the Ca 2p spectrum exhibited two contributions,2p 3/2 and 2p 1/2 ,in4 (Supporting Information, Figure S7). Thet wo peaks located at 347.2 and 350.7 eV (referenced to adventitious C 1s peak [22] at 284.8 eV) were assigned to CaCO 3 (D 2p = 3.5 eV).…”
Section: Resultsmentioning
confidence: 99%