2020
DOI: 10.1007/s11837-020-04182-9
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Investigation into the Function of Zero-Valent Iron (ZVI) in the Process of Fayalite Formation

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Cited by 6 publications
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“…Figure b shows the spectra of Fe 2p (SFT sample), where the binding energy (BE) of 710.9 eV is attributed to Fe 2+ (fayalite), while the peak at 713.3 eV corresponds to Fe 3+ due to the presence of magnetite and franklinite in the SFT sample. The Fe 2p 3/2 –Fe 2p 1/2 binding energies of Fe 2+ ions in fayalite were reported to be 709–722.6, 710.7–724, 711.1–724.6, and 709.7–723 eV. Satellite peaks are generally used to derive information regarding oxidation states.…”
Section: Resultsmentioning
confidence: 99%
“…Figure b shows the spectra of Fe 2p (SFT sample), where the binding energy (BE) of 710.9 eV is attributed to Fe 2+ (fayalite), while the peak at 713.3 eV corresponds to Fe 3+ due to the presence of magnetite and franklinite in the SFT sample. The Fe 2p 3/2 –Fe 2p 1/2 binding energies of Fe 2+ ions in fayalite were reported to be 709–722.6, 710.7–724, 711.1–724.6, and 709.7–723 eV. Satellite peaks are generally used to derive information regarding oxidation states.…”
Section: Resultsmentioning
confidence: 99%