Distribution, characterization, and geochemical controls of elements of concern in uranium mine tailings, Key Lake, Saskatchewan, Canada

Author:

Shaw Sean A.,Hendry M. Jim,Essilfie-Dughan Joseph,Kotzer Tom,Wallschläger Dirk

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Pollution,Environmental Chemistry

Reference50 articles.

1. The stabilities of calcium arsenates;Bothe;J. Hazard. Mater.,1999

2. Mineralogy and U/Pb, Pb/Pb, and Sm/Nd geochronology of the Key Lake uranium deposit, Athabasca Basin, Saskatchewan, Canada;Carl;Can. J. Earth Sci.,1992

3. Structural characterization of poorly-crystalline scorodite, iron(III)-arsenate co-precipitates and uranium mill neutralized raffinate solids using X-ray absorption fine structure spectroscopy;Chen;Geochim. Cosmochim. Acta,2009

4. Effects of sorbed arsenate on the crystallization of ferrihydrite in Uranium Mill Tailings;Das;Environ. Sci. Technol.,2011

5. Delaney, T.A., Hockley, D.E., Chapman, J.T., Holl, N.C., 1998. Geochemical characterization of tailings at the McArthur River Mine, Saskatchewan. In: Tailings and Mine Waste ’98, Proc. 5th Int. Conf., Fort Collins, Colorado, January 1998.

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