2011
DOI: 10.1007/978-3-642-22122-4_38
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Solubility Controls of Arsenic, Nickel, and Iron in Uranium Mine Tailings

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Cited by 5 publications
(5 citation statements)
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“…Since 1996, mill tailings from this mill have been deposited in the Deilmann TMF. In this TMF, knowledge of the long-term geochemical controls on arsenic (of which there is an estimated 17 000 tonnes) is important because its dominant sink is adsorption onto 2-line ferrihydrite generated in the mill 41 and regulators require an understanding of the geochemical controls over a 10 000 year time period. 42 The Deilmann tailings are alkaline and oxic (mean pH 9.8; mean Eh þ200 mV), 38 with an ambient temperature of 1À2 °C.…”
Section: Characterization Of the Iron Oxide Phases In Time-seriesmentioning
confidence: 99%
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“…Since 1996, mill tailings from this mill have been deposited in the Deilmann TMF. In this TMF, knowledge of the long-term geochemical controls on arsenic (of which there is an estimated 17 000 tonnes) is important because its dominant sink is adsorption onto 2-line ferrihydrite generated in the mill 41 and regulators require an understanding of the geochemical controls over a 10 000 year time period. 42 The Deilmann tailings are alkaline and oxic (mean pH 9.8; mean Eh þ200 mV), 38 with an ambient temperature of 1À2 °C.…”
Section: Characterization Of the Iron Oxide Phases In Time-seriesmentioning
confidence: 99%
“…The results of the estimates of transformation rates are supported by spectroscopic observations of in situ tailings samples, which show no measurable conversion of ferrihydrite over the past ∼20 years. 41 In addition, field studies from the Sain-Yrieix gold mining district of France indicate As-associated ferrihydrite remains stable over centuries, with no Fe(III) oxides, such as hematite or goethite, being reported. 46 Finally, the potential for the development of dissimilatory iron reduction in the tailings is a valid concern with regard to the long-term stability of the ferrihydrite and adsorbed arsenate, and we are currently investigating its impact in this system.…”
Section: Characterization Of the Iron Oxide Phases In Time-seriesmentioning
confidence: 99%
“…Briefly, dissolved As occurs in two principal oxidation states, As(III) or As(V), depending on the predominant geochemical conditions. The occurrence of As in mining environments has been well documented (Foster et al, 1998;Morin & Calas, 2006;Walker et al, 2009;Essilfie-Dughan et al, 2013). Dissolved As can be attenuated by iron oxide minerals, which have a net positive surface charge under acidic to circumneutral conditions (Goldberg & Johnston, 2001;Dixit & Hering, 2003;Kanel et al, 2005).…”
Section: Introductionmentioning
confidence: 99%
“…This causes additional hazards associated with the release of As into water aquifers. [18][19][20][21][22][23][24] In cases when reduction conditions prevail, such as at the Ruprechtov site in the Czech Republic, As occurs in the form of arsenopyrite (FeAsS) in tertiary sediments forming layered aggregates with secondary uraninite and arsenopyrite. 19 Mixed copper uranyl arsenate-phosphate species have been identied in the soils from an abandoned U mine in the UK as a result of many years of the mining activities at the site.…”
Section: Introductionmentioning
confidence: 99%