@proceedings {51582,
	title = {Arsenic source and distribution in groundwater from the Cold Lake oil sands region, Alberta},
	year = {2014},
	note = {IN: 2014 GSA Annual Meeting Vancouver, British Columbia October 19-22, 2014.  Geological Society of America Boulder, Colorado.  Paper No. 283-1.},
	month = {10/2014},
	publisher = {Geological Society of America },
	address = {Boulder, CO },
	abstract = {Elevated arsenic concentrations have been observed in shallow groundwater in the Cold Lake Oil Sand Region of Alberta. The geology of this area includes up to 200 m of unconsolidated glacial deposits, with six regional interglacial sand and gravel aquifers, underlain by marine shale. Arsenic concentrations in unconsolidated sediment samples ranged between 1 to 17 ppm. Mineralogical characterization of the sediment samples revealed the presence of fresh framboidal pyrite in the deeper unweathered sediments with variable As contents of up to 1800 ppm. In contrast, the weathered sediments did not contain framboidal pyrite, but exhibited spheroidal Fe-oxyhydroxide grains with elevated As concentrations, interpreted as pseudomorphs after pyrite. X-ray absorption near edge spectroscopy (XANES) indicated that the weathered sediments are dominated by As5+ species having spectral features similar to those of goethite or ferrihydrite with adsorbed As, suggesting that Fe-oxyhydroxides are the dominant As carriers. XANES spectra collected from the unweathered sediment samples indicated the presence of a reduced As species characteristic of arsenopyrite and arsenian pyrite. A survey of over 800 water wells, isolated from industrial activity, were sampled for As and found that 50\% of the wells contained As concentrations exceeding drinking water guidelines of 10 μg/L. Measurements of As speciation from 175 groundwater samples indicate that As(III) was the dominant species in 76\% of the wells. Higher As concentrations in groundwater were associated with increasing depth and reducing conditions, circumneutral pH and lower concentrations of SO4. Speciation modelling showed that the majority of groundwater samples were undersaturated with respect to ferrihydrite, suggesting that reductive dissolution of Fe-oxyhydroxides, likely formed during glaciation, may be the source of some As in deeper groundwater whereas sulfide oxidation of pyrite during weathering is the source of As released to shallow aquifers. Understanding the distribution and form of As present naturally in the region{\textquoteright}s aquifers is important for managing water resources to minimize the potential health risks of As exposure.},
	keywords = {Alberta Innovates, AOSTRA, ARC, chemistry, ERCB, field, groundwater, hydrogeology, in-situ, monitoring},
	author = {Moncur, Michael and Paktunc, Dogan and Birks, S. Jean and Ptacek, Carol J. and Welsh, Brent and Thibault, Yves}
}
