2017
DOI: 10.1016/j.jhazmat.2016.10.073
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Acid transformation of bauxite residue: Conversion of its alkaline characteristics

Abstract: Graphical abstractHighlights  Speciation and transformation of solid and soluble alkalinities were investigated. SEM, NEXAFS, and STXM were used to observe particle morphology and alkaline Na speciation and distribution. Gypsum combination promoted leaching of Na-bearing solids and the replacement of exchangeable Na. The use of organic citric acid to transform bauxite residue alkalinity.ABSTRACT: Bauxite residue (BR) is a highly alkaline solid hazardous waste produced from bauxite processing for alumina pr… Show more

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Cited by 131 publications
(47 citation statements)
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“…The volume of red mud generated per ton of alumina product is approximately 0.5-2 tons. 1,2 The large demand for alumina has increased the rate of red mud production. Globally, the cumulative stock of red mud exceeds 4 billion tons and is still growing rapidly.…”
Section: Introductionmentioning
confidence: 99%
“…The volume of red mud generated per ton of alumina product is approximately 0.5-2 tons. 1,2 The large demand for alumina has increased the rate of red mud production. Globally, the cumulative stock of red mud exceeds 4 billion tons and is still growing rapidly.…”
Section: Introductionmentioning
confidence: 99%
“…Large areas of metalliferous ore from mining and smelting contain highly toxic metal concentrations, e.g. lead, zinc and manganese, which are phytotoxic to many plant species, and therefore restrict vegetation establishment (Wu et al 2016;Kong et al 2017). Plants that have evolved to colonize heavy metal contaminated soils may be classified into two basic strategies, exclusion mechanisms and accumulation (Baker et al 1989).…”
Section: Introductionmentioning
confidence: 99%
“…Elevated levels of As frequently occur in arsenic mineral deposits, especially in emerged realgar (As 4 S 4 ) mines (Y. Wu, Zhou, et al, ). Because the mineralogical characteristic of As is closely linked to those of iron (Fe) through adsorbing or coprecipitating onto iron (hydr)oxides surface to form the arsenic–iron–minerals (e.g., scorodite) in soils and sediments (Kong, Li, et al, ; Paktunc & Bruggeman, ; C. Wu et al, ; Zhu, Hou, et al, ), As(V) solubilization mainly results from the reductive dissolution of arsenic–iron–minerals under most natural conditions (Gorny et al, ; Kong, Tian, et al, ; Zhu, Cheng, et al, ). However, microbial extracellular electron transfer (EET) process has been identified as a trigger for mediating the reductive dissolution of iron phases, accompanied by the release of As(III) and Fe(II) in flooding anaerobic condition (Z. Chen, Wang, et al, ).…”
Section: Introductionmentioning
confidence: 99%