2022
DOI: 10.1021/acs.est.2c04624
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Redox Behavior of Secondary Solid Iron Species and the Corresponding Effects on Hydroxyl Radical Generation during the Pyrite Oxidation Process

Abstract: During the pyrite oxidation process, aqueous ferrous/ferric ions (Fe 2+ /Fe 3+ ), as well as surface-adsorbed Fe 2+ /Fe 3+ , have been widely recognized to dominate hydroxyl radical ( • OH) generation, while this study reveals that the secondary solid iron species also play nonnegligible roles. Based on the different forms and the presence of sites, the secondary solid iron species were classified as Fe coat (iron-containing coating on the pyrite surface) and Fe dep (ex situ-deposited iron (oxyhydr)oxide that … Show more

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Cited by 30 publications
(13 citation statements)
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“…Redox oscillations could activate thermodynamically stable pyrite to produce RAMPs. Given that the crystallinity of iron mineral controls the redox activity following the order of adsorbed Fe > amorphous Fe > crystalline Fe, the above results suggest that redox fluctuations likely promote the production of reactive Fe­(II) and amorphous Fe on the surface of pyrite . Specifically, the abiotic oxidation of pyrite by air and hydrogen peroxide could produce metastable secondary ferric oxyhydroxides coated on the surface of native pyrite at low tide .…”
Section: Resultsmentioning
confidence: 92%
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“…Redox oscillations could activate thermodynamically stable pyrite to produce RAMPs. Given that the crystallinity of iron mineral controls the redox activity following the order of adsorbed Fe > amorphous Fe > crystalline Fe, the above results suggest that redox fluctuations likely promote the production of reactive Fe­(II) and amorphous Fe on the surface of pyrite . Specifically, the abiotic oxidation of pyrite by air and hydrogen peroxide could produce metastable secondary ferric oxyhydroxides coated on the surface of native pyrite at low tide .…”
Section: Resultsmentioning
confidence: 92%
“…Given that the crystallinity of iron mineral controls the redox activity following the order of adsorbed Fe > amorphous Fe > crystalline Fe, 39 the above results suggest that redox fluctuations likely promote the production of reactive Fe(II) and amorphous Fe on the surface of pyrite. 40 Specifically, the abiotic oxidation of pyrite by air and hydrogen peroxide could produce metastable secondary ferric oxyhydroxides coated on the surface of native pyrite at low tide. 40 Afterward, the amorphous ferric precipitates were readily reduced into dissolved ferrous ions by microbial anaerobic respiration at high tide.…”
Section: ■ Results and Discussionmentioning
confidence: 99%
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“…Huminicki and Rimstidt 21 proposed that the formation of iron oxide surface layers during pyrite oxidation is originated from the growth of deposited Fe oxyhydroxide colloids and it occurs only if the growth rate of these colloids exceeds approximately ∼10 −8 mol•s −1 , which is consistent with our recent study. 22 Accordingly, the modification of iron oxide shell layers on pyrite surfaces is inseparable from necessary artificial intervention.…”
Section: Introductionmentioning
confidence: 99%
“…Note: Unless otherwise specified, all experiments were repeated three times and error bars in all figures represented the standard error between the results of parallel experiments. The determination of the characteristic peak in XPS S2p and Fe 2p 3/2 spectra and the corresponding reference is presented in our previous study 22.…”
mentioning
confidence: 99%