2000
DOI: 10.1016/s0169-4332(00)00443-8
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Use of XPS in the determination of chemical environment and oxidation state of iron and sulfur samples: constitution of a data basis in binding energies for Fe and S reference compounds and applications to the evidence of surface species of an oxidized pyrite in a carbonate medium

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Cited by 683 publications
(393 citation statements)
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“…[49][50][51]. The peak at 533.1 eV, present in all cases, has been attributed as reported elsewhere [52,53] to ZSM5 lattice oxygen.…”
Section: +supporting
confidence: 68%
“…[49][50][51]. The peak at 533.1 eV, present in all cases, has been attributed as reported elsewhere [52,53] to ZSM5 lattice oxygen.…”
Section: +supporting
confidence: 68%
“…This result also supported by iron(III) sulfate peak at 713.25 eV 38) that can be seen only on untreated pyrite. Natural oxidation of untreated pyrite might cause the following oxidation reaction to produce iron sulfate.…”
Section: Effect Of Treatment Time Of Silicate Coating On Pyrite Oxidasupporting
confidence: 64%
“…The most interesting feature for the GO-H-E sample is the shift in the S2p peak from 168.1 eV to 168.4 eV which we link to the oxidation of all SO 3 (from sulfonic groups) into SO 4 (from sulfates) after exposure to ammonia. 46 Formation of sulfates is further supported by analyzing the filtrate of a GO-H-was stirred overnight, and then filtrated. .…”
Section: Resultsmentioning
confidence: 99%