2007
DOI: 10.1065/jss2007.04.220
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Anaerobic sediment potential acidification and metal release risk assessment by chemical characterization and batch resuspension experiments

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Cited by 25 publications
(26 citation statements)
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“…In polluted anaerobic sediments, microbiologically catalyzed sulfate reduction originates in sulfides (acid-volatile sulfide, AVS) and redox potential changes can promote sediment acidification by oxidation of sulfide to sulfate where about 0.3 to 3.0 pH in sediment decreased (Di Nanno et al 2007). Ionizable organic contaminants (IOCs) like ibuprofen exist in aqueous phase as ionic forms and/or neutral forms.…”
Section: Introductionmentioning
confidence: 99%
“…In polluted anaerobic sediments, microbiologically catalyzed sulfate reduction originates in sulfides (acid-volatile sulfide, AVS) and redox potential changes can promote sediment acidification by oxidation of sulfide to sulfate where about 0.3 to 3.0 pH in sediment decreased (Di Nanno et al 2007). Ionizable organic contaminants (IOCs) like ibuprofen exist in aqueous phase as ionic forms and/or neutral forms.…”
Section: Introductionmentioning
confidence: 99%
“…During sediment oxidation, metals bound to sulfides and organic phase are released rapidly to the water column, accompanied by the pH decrease (Figure ). Previous studies have noted that sediment oxidation can potentially cause acidification, and can lead to significant amounts of toxic metal release . The pH decrease during the first week of sediment oxidation shows fast acidification in all sediment samples.…”
Section: Discussionmentioning
confidence: 66%
“…Following the oxidation of sediment samples, the sulfate release in the water column accompanied microbial oxidation of reduced sulfidic minerals, primarily pyrrhotite (FeS; Equation 2) and pyrite (FeS 2 ; Equation ), commonly found in mining waste materials as sedimentary iron sulfides . The resulting solution of sulfate characterized by a slightly yellowish brown color, colloidal suspensions, is an indication that iron (III) oxyhydroxysulfate mineral jarosite precipitation (Equation 4) is formed as a secondary sulfate mineral .…”
Section: Discussionmentioning
confidence: 99%
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