2021
DOI: 10.1590/1678-992x-2018-0368
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Adsorption and desorption of arsenic and its immobilization in soils

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Cited by 9 publications
(6 citation statements)
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References 38 publications
(66 reference statements)
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“…Such discrepant contents as those obtained in the present study (26.59 -0.56 mg kg -1 ) may indicate the need for standardizing more than one quality reference value (QRV), thus reducing the possibility of classifying natural contents as contamination or allowing soils with very low contents to be contaminated. VRQs can be split into groups with different clay and/or iron oxide contents, since this study (Table 6), as well as several others (Campos et al, 2013, De Menezes et al, 2020, Almeida et al, 2020, found positive correlation between arsenic content and those said attributes. Source: Author's own production, 2020.…”
Section: Resultsmentioning
confidence: 57%
“…Such discrepant contents as those obtained in the present study (26.59 -0.56 mg kg -1 ) may indicate the need for standardizing more than one quality reference value (QRV), thus reducing the possibility of classifying natural contents as contamination or allowing soils with very low contents to be contaminated. VRQs can be split into groups with different clay and/or iron oxide contents, since this study (Table 6), as well as several others (Campos et al, 2013, De Menezes et al, 2020, Almeida et al, 2020, found positive correlation between arsenic content and those said attributes. Source: Author's own production, 2020.…”
Section: Resultsmentioning
confidence: 57%
“…The As concentration of AT increased continuously from 1.044 mg/L (natural pH 8.36) with added KOH and reached 4.476 mg/L at pH 13 due to the dissolution of arsenopyrite (Equation (8)) and the deprotonation in alkaline solution because of the amphoteric property of As [ 35 ]. With decreasing pH, the As concentration of AT decreased to the lowest value at pH 5.5 (0.626 mg/L) and then increased to the highest value at pH 2 (25.491 mg/L), which was attributed to the adsorption of iron and aluminum oxides/hydroxides on As in different valence states and the dissolution of the oxides/hydroxides as the pH went down [ 36 ]. The As equilibrium concentration of T-3 and PST was between one and two orders of magnitude lower than that of AT over a pH range of 2–13 due to the reaction of hydration products of SSB and OPC with As in AT; the As concentration of T-3-90d was 0.0276 mg/L at natural pH 12.16, while that of PST-90d was 0.004 mg/L at natural pH 12.56.…”
Section: Resultsmentioning
confidence: 99%
“…The set of physical, chemical and mineralogical characteristics gives the soil a specific capacity to retain anionic species. The Inceptisols, due to their lower Fe and Al content, especially gibbsite, were the soil class with the lowest adsorption of anionic species (Almeida et al, 2021).…”
Section: Soil Chemical Characteristicsmentioning
confidence: 96%
“…Due to the soil diversity in Brazil, soil characterization is essential to better agricultural or environmental usage and subsequent management. Mineralogical studies are very important to understanding the physical and chemical properties of the soil (Camargo et al, 2008;Almeida et al, 2021). Phosphorous adsorption is mainly attributed to gibbsite, goethite and hematite, the predominant minerals in highly weathered soils (Fontes and Weed, 1996;Schaefer et al, 2008;Fontes, 2012).…”
Section: Introductionmentioning
confidence: 99%