2023
DOI: 10.1016/j.scitotenv.2022.159897
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Mechanisms of changing speciation and bioavailability of selenium in agricultural mollisols of northern cold regions

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Cited by 8 publications
(7 citation statements)
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“…It is already known that Se bioavailability differs significantly between the dryland and paddy soils. , Land use change from conventional drylands to the current paddy wetlands can alter both structure (e.g., loss of stable aggregates) and physical–chemical–biological conditions of the Mollisol vadose zone. , For instance, the cultivated Mollisols suffer from soil acidity and redox shift that are companied by variations in the functional microbial community mediating redox zonation and nutrient release. , These factors affect directly the adsorption and redox transformation of Se species . In the context of global warming which impacts the cold regions disproportionately, these agricultural interventions make the Mollisols and Se in them prone to soil erosion, dehumification, and anthropogenic flooding. , Behind these changes is the increased potential of Se mobilization from the Mollisol layers, which are marginal or only moderately sufficient in Se. , Consequences for the bioavailability and sustainability of Se in the Mollisol agroecosystems, as well as the underlying processes and controlling mechanisms, however, remain to be elucidated.…”
Section: Introductionmentioning
confidence: 99%
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“…It is already known that Se bioavailability differs significantly between the dryland and paddy soils. , Land use change from conventional drylands to the current paddy wetlands can alter both structure (e.g., loss of stable aggregates) and physical–chemical–biological conditions of the Mollisol vadose zone. , For instance, the cultivated Mollisols suffer from soil acidity and redox shift that are companied by variations in the functional microbial community mediating redox zonation and nutrient release. , These factors affect directly the adsorption and redox transformation of Se species . In the context of global warming which impacts the cold regions disproportionately, these agricultural interventions make the Mollisols and Se in them prone to soil erosion, dehumification, and anthropogenic flooding. , Behind these changes is the increased potential of Se mobilization from the Mollisol layers, which are marginal or only moderately sufficient in Se. , Consequences for the bioavailability and sustainability of Se in the Mollisol agroecosystems, as well as the underlying processes and controlling mechanisms, however, remain to be elucidated.…”
Section: Introductionmentioning
confidence: 99%
“…3,10 Behind these changes is the increased potential of Se mobilization from the Mollisol layers, which are marginal or only moderately sufficient in Se. 11,12 Consequences for the bioavailability and sustainability of Se in the Mollisol agroecosystems, as well as the underlying processes and controlling mechanisms, however, remain to be elucidated. Hydro(bio)geochemical dynamics in the vadose zone form the basis of Se mobility and thus bioavailability through the food chain.…”
Section: Introductionmentioning
confidence: 99%
“…SeO − ), elemental selenium (Se) and methionine selenea (MetSe) [8] [9]. The chemical form of selenium influences its bioavailability and toxicity to living organisms (Wang et al, 2012).…”
Section: Introductionmentioning
confidence: 99%
“…Selenium can be adsorbed onto sediment particles or precipitated as insoluble compounds. The concentration of selenium in sediments can vary considerably depending on the sources of inputs, the physicochemical properties of the sediment and environmental conditions [8] [9] [10]. Selenium can be toxic to aquatic organisms at relatively low concentrations [11] [12].…”
Section: Introductionmentioning
confidence: 99%
“…Organic matters and iron minerals are known to influence Se mobility and biogeochemistry. Sediments are critical components of Se geochemistry. Jones et al found that in the contaminated wetland they were studying, the sediment was storing 75% of the entering Se. , Oxic conditions at the sediment–water interface (SWI) can influence the Se sequestration.…”
Section: Introductionmentioning
confidence: 99%