2020
DOI: 10.1016/j.chemosphere.2020.126355
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Iron fractions responsible for the variation of Cd bioavailability in paddy soil under variable pe+pH conditions

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Cited by 65 publications
(11 citation statements)
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“…To adapt to adverse anaerobic environment, the roots aerenchyma of rice plant released O 2 in the rhizosphere resulting in the deposition of Fe plaque on the root surfaces through the oxidation of Fe 2+ (ferrous iron) to Fe 3+ (ferric iron) [23]. Iron plaques mainly exist in the form of ferrihydrite (5Fe 2 O 3 .9H 2 O), goethite (α-FeOOH), and lepidocrocite (γ-FeOOH) on the root surfaces [24]. Iron plaque deposits possess ample functional groups with many sorption sites that are capable of binding metal ions in the root zone [25].…”
Section: Introductionmentioning
confidence: 99%
“…To adapt to adverse anaerobic environment, the roots aerenchyma of rice plant released O 2 in the rhizosphere resulting in the deposition of Fe plaque on the root surfaces through the oxidation of Fe 2+ (ferrous iron) to Fe 3+ (ferric iron) [23]. Iron plaques mainly exist in the form of ferrihydrite (5Fe 2 O 3 .9H 2 O), goethite (α-FeOOH), and lepidocrocite (γ-FeOOH) on the root surfaces [24]. Iron plaque deposits possess ample functional groups with many sorption sites that are capable of binding metal ions in the root zone [25].…”
Section: Introductionmentioning
confidence: 99%
“…Increases in soil pH under anaerobic conditions were due to the continuous consumption of H + , including the reduction process of iron oxide, manganese oxide and SO 4 2-(e.g. Fe [OH] 3 + 3H + +e -↔ 4 Fe 2+ + 3H 2 O) (Li et al, 2020;Li and Xu, 2017). After incubation, the pH of SBB and MBB treatments were 6.88 ± 0.02 and 6.90 ± 0.01, which were 13.21% and 13.01% respectively higher than the pH of treatment CK (Fig.…”
Section: Changes In Soil Phmentioning
confidence: 95%
“…According to the authors, low pe + pH may promote the activity of Fe reduction bacteria to produce Fe 2+ , which is re-oxidized to amorphous Fe oxides. However, this hypothesis still needs to be verified by further studies [48]. CBR A and CBR B, respectively, followed by Ca bound P that represents the 37.4% and 32.8% of total P extracted from CBR A and CBR B, respectively (Fig.…”
Section: Iron Mobilization In Cbrmentioning
confidence: 95%
“…7A, was already observed in soils in the presence of living microorganisms [26,47,48], and it was primarily attributed to microbial reduction of crystalline Fe 3+ (hydr)oxides probably followed by the precipitation of amorphous Fe 2+ complexes [47]. Li et al [48] observed that a decrease of pe + pH from 11.06 to 8.29 was accompanied by a 110% increase of amorphous Fe content in rhizosphere soils. According to the authors, low pe + pH may promote the activity of Fe reduction bacteria to produce Fe 2+ , which is re-oxidized to amorphous Fe oxides.…”
Section: Iron Mobilization In Cbrmentioning
confidence: 96%
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