1997
DOI: 10.2134/jeq1997.00472425002600020014x
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Arsenic Transport in Contaminated Mine Tailings following Liming

Abstract: The practice of liming to remediate contaminated soils and mine tailings has the potential to mobilize arsenic (As), due to the pH dependence of As sorption reactions on oxide minerals and layer silicates. The objectives of this study were to determine the effects of liming on As mobility in mine tailings and identify possible mechanisms controlling As mobilization with increased pH. Six mine tailing samples obtained from an abandoned copper smelter near Anaconda, Montana were analyzed for total As and soluble… Show more

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Cited by 73 publications
(40 citation statements)
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“…The practice of liming to remediate contaminated soils and mine tailings has the potential to mobilize arsenic due to the pH dependence of As sorption reactions on oxide minerals and layer silicates (Jones et al 1997). It may also be of concern for other trace elements such as Cu, Mo, U, V, and Se.…”
Section: Field Applicationsmentioning
confidence: 99%
“…The practice of liming to remediate contaminated soils and mine tailings has the potential to mobilize arsenic due to the pH dependence of As sorption reactions on oxide minerals and layer silicates (Jones et al 1997). It may also be of concern for other trace elements such as Cu, Mo, U, V, and Se.…”
Section: Field Applicationsmentioning
confidence: 99%
“…Until now, mine tailings are frequently treated with lime amendment and/or are simply placed in landfills at designated disposal sites. Lime treatment, however, may result in enhanced As mobilization due to the pH dependence of As sorption by mineral solid phases (Jones et al 1997). When the conditions turn anaerobic, the reductive dissolution of As-bearing iron hydroxides occurs, causing desoprtion of arsenate and arsenite species (McGeehan & Naylor 1994).…”
Section: Introductionmentioning
confidence: 99%
“…Furthermore, in soil with CaCO 3 , Ca 2þ ions reduce adsorption and increase solubility of Cd 2þ (Lagerwerff and Brower, 1972). In the case of As, because it is co-precipitated fundamentally with Fe oxyhydroxides, and the quantity precipitated decreases as pH increases (Jones et al, 1997;Tyler and Olson, 2001;Simón et al, 2005), high solubility and low precipitation and/ or adsorption of As would be expected in Area B, characterized by a basic pH and a relatively low Fe concentration (similar concentration as in Area C). The low Fe concentration in Area B would be attributable to the low concentration on sulphur-mining wastes (mean ¼ 62 g kg À1 ), far lower than in other types of mining wastes, such as sulphide (mean ¼ 359 mg kg À1 ; Alastuey et al, 1999).…”
Section: Spread Of the Pollutants In Soilmentioning
confidence: 89%