2011
DOI: 10.1021/es2003765
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Organic Matter—Solid Phase Interactions Are Critical for Predicting Arsenic Release and Plant Uptake in Bangladesh Paddy Soils

Abstract: Agroecological zones within Bangladesh with low levels of arsenic in groundwater and soils produce rice that is high in arsenic with respect to other producing regions of the globe. Little is known about arsenic cycling in these soils and the labile fractions relevant for plant uptake when flooded. Soil porewater dynamics of field soils (n = 39) were recreated under standardized laboratory conditions to investigate the mobility and interplay of arsenic, Fe, Si, C, and other elements, in relation to rice grain … Show more

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Cited by 187 publications
(97 citation statements)
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“…Both As(V) and As(III) are mainly sequestered by iron minerals (Macur et al 2004;Islam et al 2005), and the adsorption and desorption of As from the minerals determines the mobility of As in the soil (Smedley and Kinniburgh 2002). Dissolved organic matter could compete with As for adsorption sites at mineral surface, decrease As(V) and As(III) adsorption and enhanced As release to the soil solution in the paddy soil Williams et al 2011). Organic matters (OM) and OM-Fe complexes bind As on the minerals, which also promote desorption of arsenic from solid phases by altering soil/solution equilibrium, while simultaneously impacting on the bioavailability Sharma et al 2011).…”
Section: Discussionmentioning
confidence: 99%
“…Both As(V) and As(III) are mainly sequestered by iron minerals (Macur et al 2004;Islam et al 2005), and the adsorption and desorption of As from the minerals determines the mobility of As in the soil (Smedley and Kinniburgh 2002). Dissolved organic matter could compete with As for adsorption sites at mineral surface, decrease As(V) and As(III) adsorption and enhanced As release to the soil solution in the paddy soil Williams et al 2011). Organic matters (OM) and OM-Fe complexes bind As on the minerals, which also promote desorption of arsenic from solid phases by altering soil/solution equilibrium, while simultaneously impacting on the bioavailability Sharma et al 2011).…”
Section: Discussionmentioning
confidence: 99%
“…R value (ratio of CDGT to Csol) reflects the resupply potential of an element to the soil solution, providing an additional measure of the ability of a soil to maintain the CDGT flux [43]. Comparison of the soil R values (0.06-0.09) from this study with those for other metals (Cd, Zn, Ni and As), encompassing a wide range of soil types [54][55][56][57], shows that typically W resupply is relatively poorly sustained. This is further supported by the high (>90%) non-available residual fraction of W observed in acidic and neutral soils [10,18,58].…”
Section: Measurement Of W In Soils Using Pz Pf and Sf Dgt'smentioning
confidence: 98%
“…Dissolved As generally has been considered an indicator for As availability, although some researchers pointed out that it is not a good predictor for As uptake by rice (Williams et al 2011;Norton et al 2013). The addition of OAs potentially increases (Xie and Huang 1998;Suda et al 2015) and decreases (Das et al 2005) dissolved As through a variety of mechanisms (see ''Introduction'' section).…”
Section: Implication and Further Studiesmentioning
confidence: 99%