Sulfide drives hydroxyl radicals production in oxic ferric oxyhydroxides environments. (November 2019)

• Record Type: Journal Article
• Authors: Niyuhire, Elias; Yuan, Songhu; Liao, Wenjuan; Zhu, Jian; Liu, Xixiang; Xie, Wenjing; Qian, Ao
• Is Part Of: Chemosphere. Volume 234(2019)
• Page Start: 450
• Page End: 460
• Publication Date: 2019-11
• Subjects: Iron oxyhydroxides -- Sulfide -- Hydroxyl radicals -- Contaminant transformation -- Redox-dynamic; Pollution -- Periodicals; Pollution -- Physiological effect -- Periodicals; Environmental sciences -- Periodicals; Atmospheric chemistry -- Periodicals; 551.511
• DOI: 10.1016/j.chemosphere.2019.06.037
• Languages: English
• ISSNs: 0045-6535

Abstract

Abstract: Perturbation of Fe(III)-bearing oxic environments by reduced species such as sulfide occurs widely in natural and engineered systems. However, whether hydroxyl radicals (OH) can be produced in these environments remains unexplored. Here we show that sulfide drives OH production in Fe(III) oxyhydroxides suspensions under neutral and oxic conditions. For lepidocrocite, ferrihydrite and goethite suspensions at 11.2 mM Fe, the addition of 0.5 mM sulfide produced 14.2, 14.3 and 22.4 μM OH within 120 min, respectively. With addition of sulfide to lepidocrocite suspensions at 11.2 mM Fe, the cumulative OH concentration within 120 min increased from 0 to 14.2, 25.2, 52.6 and 63.1 μM when sulfide dosage increased from 0 to 0.5, 2.5, 5 and 7.5 mM, respectively. At a fixed sulfide dosage of 5 mM, the cumulative OH concentration increased with increasing the number of sulfide additions. The mechanisms of OH production were attributed to the generation of surface-bound Fe(II), most likely in the form of >Fe II OH2 +, and Fe(II) in the solid phase or FeS from the reactions between sulfide and Fe(III), followed by O2 activation. OH production could take place until depletion of sulfide. Finally, we found that the generated OH could oxidize the coexisting redox-active substances like phenol under neutral and oxic conditions. Our findings reveal that sulfide perturbation of Fe(III)-bearing oxic environments is a new source of OH, and contaminants oxidation by OH necessitates consideration in these environments. Graphical abstract: A new abiotic pathway of dark OH production. Image 1 Highlights: .OH can be produced in oxic Fe(III)-bearing environments perturbed by sulfide. Surface-bound Fe(II) and Fe(II) in the solid phase or FeS were produced in sulfide/Fe(III)/O2 systems. O2 activation by surface-bound Fe(II) and/or Fe(II) in the solid phase or FeS was responsible for .OH production. The produced .OH could oxidize organic contaminants. A new abiotic pathway was proposed for dark .OH production in the environment.