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2016
DOI: 10.1016/j.chemosphere.2016.03.027
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Formation of macroscopic surface layers on Fe(0) electrocoagulation electrodes during an extended field trial of arsenic treatment

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Cited by 53 publications
(28 citation statements)
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“…S1 and S2), our results support the hypothesis that field treatment performance decreases over time because EC generated Fe(II) is trapped at the anode by macroscopic Fe (oxyhydr)oxide surface layers (e.g. magnetite, goethite) formed on the electrode after extended operation [45].…”
Section: Insights Into Field Treatment Performance Over Timesupporting
confidence: 77%
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“…S1 and S2), our results support the hypothesis that field treatment performance decreases over time because EC generated Fe(II) is trapped at the anode by macroscopic Fe (oxyhydr)oxide surface layers (e.g. magnetite, goethite) formed on the electrode after extended operation [45].…”
Section: Insights Into Field Treatment Performance Over Timesupporting
confidence: 77%
“…periods of operation (wet) and storage (dry) [45,59]. One previously proposed explanation for this decreased field performance is a drop in Faradaic efficiency resulting from O 2 evolution after many cycles of operation.…”
Section: Insights Into Field Treatment Performance Over Timementioning
confidence: 99%
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“…According to the difference of reaction rate for various ferric hydrolysates with Ferron reagent, Fea represents ferric ions, monomeric hydroxy complex and ferric oligomer (e.g., Fe 3+ , [Fe(OH)] 2+ , [Fe(OH)2] + ), and Feb is a transition state between Fea and Fec, which is composed of polymeric hydroxy complex with low polymerization degree (e.g., [Fe2(OH)2] 4+ , [Fe13(OH)34] 5+ ). Fec corresponds to the ferric species with high polymerization degree and even ferric precipitation (e.g., Fe(OH)3 (am)) [12]. During the EC process of WFGD wastewater on Fe anode, the species of ferric hydrolysates dominate in form of low or medium polymerization state.…”
Section: Floc Speciation Change On Al Anodementioning
confidence: 99%
“…The ancient use of Fe 0 for safe drinking water provision both at household (Bischof 1877(Bischof , 1878Baker 1934) and large scale (Devonshire 1890;Baker 1934; Van Craenenbroeck 1998) levels has been widely overseen . The redox complex geochemistry of iron (Table 1) (Liu and Millero 1999;Nesic 2007;Antia 2010;Noubactep 2010a, b, c;Luo et al 2013;Noubactep 2016b, c, d, e;van Genuchten et al 2016). The difference in the crystal structure of Fe 0 and generated corrosion products (Table 2) implies that the oxide scale is not primarily a protective one (Lazzari 2008;Noubactep 2010c).…”
Section: Introductionmentioning
confidence: 99%