1997
DOI: 10.1002/(sici)1096-9918(199702)25:2<64::aid-sia203>3.0.co;2-9
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Surface Spectroscopic Studies of Factors Influencing Xanthate Adsorption on Coal Pyrite Surfaces†

Abstract: The relative adsorption of fluoroxanthates on several different coal pyrites has been found to depend on the degree to which the pyrite surfaces are oxidized. Maximum xanthate adsorption occurs in the absence of pyrite surface oxidation and is affected by the presence of polysulfides and metal‐deficient sulfides on the pyrite surface. The structure and electronic properties of the xanthate molecule may also affect its adsorption. 3‐(Trifluoromethyl)benzyl xanthate was found to selectively adsorb on pyrite vs. … Show more

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Cited by 7 publications
(5 citation statements)
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“…In addition, parts c and f of Figure S1 in the SI show the sulfur spectra (S 2p) of fresh and deactivated surfaces, respectively. Sulfur was not detectable on the fresh nZVI surface compared to a significant detectable sulfur peak on the deactivated nZVI surface at a BE of 168.6 eV, which implies the presence of sulfur as sulfate (e.g., FeSO 4 , Fe 2 (SO 4 ) 3 ) rather than sulfide (e.g., FeS, FeS 2 ) or other sulfur forms. , In the peer-reviewed literature, ,, the reference peaks of FeSO 4 in the sulfur spectra (S 2p) were detected at 169.0 (±0.2) eV. Therefore, ferrous sulfate (FeSO 4 ) is most likely formed on the deactivated nZVI surface.…”
Section: Resultsmentioning
confidence: 98%
“…In addition, parts c and f of Figure S1 in the SI show the sulfur spectra (S 2p) of fresh and deactivated surfaces, respectively. Sulfur was not detectable on the fresh nZVI surface compared to a significant detectable sulfur peak on the deactivated nZVI surface at a BE of 168.6 eV, which implies the presence of sulfur as sulfate (e.g., FeSO 4 , Fe 2 (SO 4 ) 3 ) rather than sulfide (e.g., FeS, FeS 2 ) or other sulfur forms. , In the peer-reviewed literature, ,, the reference peaks of FeSO 4 in the sulfur spectra (S 2p) were detected at 169.0 (±0.2) eV. Therefore, ferrous sulfate (FeSO 4 ) is most likely formed on the deactivated nZVI surface.…”
Section: Resultsmentioning
confidence: 98%
“…According to the literature and blank experiments using different kinds of iron species, the former set of spectra are possibly assigned to magnetite, although it is dangerous to conclude the kind of species only by the chemical shift in the XPS. Baltrus and Diehl have assigned similar spectra to a mixture of Fe 2+ and Fe 3+ from pyrite oxidation . On the other hand, the latter reduced species is considered to be pyrrhotite or troilite .…”
Section: Resultsmentioning
confidence: 98%
“…On the other hand, the latter reduced species is considered to be pyrrhotite or troilite . The S(2p) spectra showed the peaks of elemental sulfur and sulfide on the outer surface, whereas in the inside of the residue, only the peaks of sulfide were observed. One of possible reasons why the depth profile of the iron species was markedly changed is the oxidation of “surface” iron species into magnetite by water.
9 Effects of catalyst precursor on XPS spectra of the residue from Wandoan coal and vacuum residue using syngas−water.
…”
Section: Resultsmentioning
confidence: 99%
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