2020
DOI: 10.1016/j.watres.2020.115631
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The formation of •OH with Fe-bearing smectite clays and low-molecular-weight thiols: Implication of As(III) removal

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Cited by 29 publications
(5 citation statements)
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“…Previous studies regarding the influence of ligands on · OH production and contaminant degradation in Fe­(II)–O 2 model systems partly support our hypothesis. Ligands such as ethylene diamine tetraacetic acid (EDTA), nitrilotriacetic acid (NTA), and sodium tripolyphosphate (TPP) have been proven to increase the yield of · OH production upon oxygenation of dissolved Fe­(II), pyrite, magnetite, , and Fe­(II)-bearing clay minerals. Particularly, for the oxygenation of reduced nontronite (a model Fe-rich clay mineral), Zeng et al found that ligands could dissolve a fraction of solid Fe­(II) and then enhance the yield and rate of oxidant production through electron transfer from solid Fe­(II) to dissolved Fe­(III) . Because of the much more complicated composition of real sediments, it is still uncertain to what extent and how ligands influence · OH production and contaminant degradation during sediment oxygenation.…”
Section: Introductionsupporting
confidence: 65%
“…Previous studies regarding the influence of ligands on · OH production and contaminant degradation in Fe­(II)–O 2 model systems partly support our hypothesis. Ligands such as ethylene diamine tetraacetic acid (EDTA), nitrilotriacetic acid (NTA), and sodium tripolyphosphate (TPP) have been proven to increase the yield of · OH production upon oxygenation of dissolved Fe­(II), pyrite, magnetite, , and Fe­(II)-bearing clay minerals. Particularly, for the oxygenation of reduced nontronite (a model Fe-rich clay mineral), Zeng et al found that ligands could dissolve a fraction of solid Fe­(II) and then enhance the yield and rate of oxidant production through electron transfer from solid Fe­(II) to dissolved Fe­(III) . Because of the much more complicated composition of real sediments, it is still uncertain to what extent and how ligands influence · OH production and contaminant degradation during sediment oxygenation.…”
Section: Introductionsupporting
confidence: 65%
“…Low molecular weight organic acids, with oxalic acid (OA) being the most representative and active one, are frequently found in subsurface environments. It is generally recognized that the presence of organic acids could impact the photolysis generation of ROS in iron-bearing mineral systems under light irradiation . Recently, several studies have demonstrated that organic acids can also alter the interfacial physicochemical properties of iron-bearing minerals, which ultimately affects the generation of ROS and the subsequent transformation of pollutants in darkness. The dark environment is crucial for gaining insights into the role of organic acids and iron minerals in ROS production as well as the transformation of pollutants in light-deprived subsurface areas. There are two principal explanations associated with the ROS production in this scenario.…”
Section: Introductionmentioning
confidence: 99%
“…The observed Fe(II)-EPS complexes are likely important forms of bioavailable Fe(II) for micro-organisms, thereby in uencing Fe cycling and production of ROS (eg. •OH), and then affecting transfer and transformation of heavy metals, such as As or Sb(Sun et al, 2020).ConclusionsOur ndings clarify the mechanism of EPS-mediated •OH production by Fe(II) chemical oxidation in acidic conditions. Oxic experiments results substantiate that Fe( ) complexation by EPS increases the •OH yield from the in uence of carboxyl and hydroxyl groups in EPS.…”
mentioning
confidence: 62%