Heavy Metals in the Environment 2002
DOI: 10.1201/9780203909300.ch6
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Arsenic in the Environment

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Cited by 119 publications
(95 citation statements)
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References 114 publications
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“…The background As concentration in soils is controlled by the lithology of the parent rocks (Yan Chu, 1994) and it is important to assess this in a given area prior to remediation. In view of the potential risk of bioaccumulation and toxicity of As (Bhumbla and Keefer, 1994;Bhattacharya et al, 1997Bhattacharya et al, , 2001), the geochemical behaviour of As in nature has generated much concern in environmental research in recent years. Under the range of Eh and pH in soil compartments, As normally occurs in qIII and qV oxidation states (Cullen and Reimer, 1989 under oxidising conditions (peqpH)8) (Sadiq et al, 1983;Masscheleyn et al, 1991).…”
Section: Chemistry Of Cca Metals In Soilsmentioning
confidence: 99%
“…The background As concentration in soils is controlled by the lithology of the parent rocks (Yan Chu, 1994) and it is important to assess this in a given area prior to remediation. In view of the potential risk of bioaccumulation and toxicity of As (Bhumbla and Keefer, 1994;Bhattacharya et al, 1997Bhattacharya et al, , 2001), the geochemical behaviour of As in nature has generated much concern in environmental research in recent years. Under the range of Eh and pH in soil compartments, As normally occurs in qIII and qV oxidation states (Cullen and Reimer, 1989 under oxidising conditions (peqpH)8) (Sadiq et al, 1983;Masscheleyn et al, 1991).…”
Section: Chemistry Of Cca Metals In Soilsmentioning
confidence: 99%
“…For preparing ICS, a FeCl 3 solution (100 mL, 0.1 M), adjusted to pH 4, 7, or 10 with 0.1 M HNO 3 or NaOH, was mixed with raw sand (100 g) in a rotary evaporator for 2 h. For MCS, a Mn(NO 3 ) 2 solution (100 mL, 0.1 M), previously adjusted to pH 4, 7 or 10, was mixed with raw sand (100 g) in the rotary evaporator. For IMCS, FeCl 3 (50 mL, 0.1 M) and Mn(NO 3 ) 2 (50 mL, 0.1 M) solutions, previously adjusted to pH 4, were mixed at different ratios with raw sand (100 g) in the rotary evaporator.…”
Section: ■ Materials and Methodsmentioning
confidence: 99%
“…In each experiment, the desired mass of precipitator was mixed with 500 mL of 2 mg/L phosphate. The solution pH was adjusted over the reaction time using 0.01 M HNO 3 and NaOH. The solution was mixed at 30 rpm for 24 h.…”
Section: ■ Materials and Methodsmentioning
confidence: 99%
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“…Bacterial As(III) oxidase genes are phylogenetically diverse and ecologically widespread [85]. Microbial oxidation of As(III) to As(V) occur under both aerobic and anaerobic soil conditions, which significantly enhance the immobilization of As in the soils, due to the fact that As(V) can more easily co-precipitate with ferric iron or be adsorbed by ferrihydrite [86]. In the rhizosphere soil, it remains unclear whether the activity of As(III) oxidizing bacteria (expression of aroA-like gene [85]) is elevated by the root exudates or the oxygen released from the rice roots to result in more As(V) binding on iron minerals in soil and iron plaque on rice roots, thus to reduce the bioavailability of As to rice roots.…”
Section: Interactions Of Microorganisms With Iron Oxidesmentioning
confidence: 99%