2016
DOI: 10.1016/j.chemosphere.2015.12.043
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Redox effects on release kinetics of arsenic, cadmium, cobalt, and vanadium in Wax Lake Deltaic freshwater marsh soils

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Cited by 178 publications
(54 citation statements)
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“…for the detoxification process), resulting in the production of organic As(V) species that can be scavenged by plants and organisms or bound to Fe(III) oxyhydroxides. This decrease in As mobility, subsequent to the establishment of oxidizing conditions, was previously discussed by Frohne et al (2014) and Shaheen et al (2016). The proposed mechanism was the precipitation of Fe(III)-oxyhydroxides and subsequent As binding.…”
Section: Implications For As Dynamics In Wetlandsmentioning
confidence: 58%
“…for the detoxification process), resulting in the production of organic As(V) species that can be scavenged by plants and organisms or bound to Fe(III) oxyhydroxides. This decrease in As mobility, subsequent to the establishment of oxidizing conditions, was previously discussed by Frohne et al (2014) and Shaheen et al (2016). The proposed mechanism was the precipitation of Fe(III)-oxyhydroxides and subsequent As binding.…”
Section: Implications For As Dynamics In Wetlandsmentioning
confidence: 58%
“…In addition, the proportion of 4 in S IN was significantly higher than that in S IA during the whole incubation period. This may be attributed to the more As(V) reduction to As(III) and less decomposition of dissolved organic matters in soils under anoxic condition than that under aerobic condition [8,11].…”
Section: Effect Of Redox Conditions On As Fractions Inmentioning
confidence: 99%
“…Thus, it is essential to understand the stabilization/aging processes of As related to the change of As fractions in soils. And the stabilization/aging processes of As in soils not only depended on the properties of amendments but also were affected by some environmental conditions, such as temperature and redox conditions [5,[8][9][10]. For instance, the crystallization of Fe (hydr)oxides and the diffusion of As in micropores from the outer layers into the inner complex are accelerated after the temperature elevated, resulting in the transformation of labile fractions of As into unlabile fractions [5,9].…”
Section: Introductionmentioning
confidence: 99%
“…The distribution of PTMs including Cr and Pb between the liquid and solid phase of floodplain soils and their release dynamics is mainly affected by soil properties and by changes of redox potential (E H ), soil pH, and metal carriers such as iron (Fe), manganese (Mn), dissolved organic carbon (DOC), and sulfate (SO 4 2À ) (Rinklebe et al, 2016a,b;Rupp et al, 2010;Schulz-Zunkel et al, 2015;Shaheen et al, 2013;Shaheen et al, 2014aShaheen et al, , 2016. A proper understanding of the geochemistry of Cr and Pb in floodplain soils is limited particularly under dynamic reducing-oxidizing conditions.…”
Section: Introductionmentioning
confidence: 99%