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The mineralogy of arsenic in uranium mine tailings at the Rabbit Lake In-pit Facility, northern Saskatchewan, Canada
Authors:T Pichler  M J Hendry  G E M Hall
Institution:(1) Department of Geology, SCA528, University of South Florida, Tampa, FL 33620, USA e-mail: pichler@chuma.cas.usf.edu Tel: +1-813-9740321 Fax: +1-813-9742654, US;(2) Department of Geological Sciences, University of Saskatchewan, Saskatoon, Canada, S7N 5E2, CA;(3) Geological Survey of Canada, 601 Booth Street, Ottawa, Canada, K1A 0E8, CA
Abstract: A detailed investigation of the mineralogy of As in the tailings of the Rabbit Lake uranium ore processing facility was conducted. The milling/ore extraction process was sampled at three different locations to obtain information about when, where and under what condition secondary As phases form. These samples were compared with four samples of varying As content from the Rabbit Lake in-pit tailings management facility (TMF). Up to 20% As in the tailings are present in primary minerals that reach the tailings directly because they are not dissolved during the uranium extraction. The remaining 80% constitute As that was dissolved during ore extraction and then re-precipitated before being discharged into the tailings pond. It was not possible to conclusively identify any individual re-precipitated (secondary) As minerals in the Rabbit Lake TMF. Indirect evidence from sequential extraction analyses suggests the presence of an amorphous Ca-As phase and a possible, but unlikely, minor amount of an amorphous Fe-As phase. However, the close association between hydrous ferric oxide (HFO) and As could be clearly demonstrated. HFO was identified to be 2-line ferrihydrite and its XRD pattern geometry indicates a substantial amount of adsorbed As. This is in good agreement with SEM, TEM and sequential extraction analyses that all showed the close association of HFO and As. Received: 14 February 2000 · Accepted: 9 May 2000
Keywords:  Arsenic  Hydrous ferric oxide  Mine tailings
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