Origin and hydrogeological setting of saline groundwater discharges to the Athabasca River: Geochemical and isotopic characterization of the hyporheic zone

• Published in: Applied geochemistry 2018-11, Vol.98, p.172-190
• Main Authors: Birks, S.J., Moncur, M.C., Gibson, J.J., Yi, Y., Fennell, J.W., Taylor, E.B.
• Format: Article
• Language: English
• Subjects: Athabasca oil sands; Athabasca river; Glaciogenic; Groundwater-surface; Hyporheic zone; Saline groundwater; Stable isotopes; Water interactions
• ISSN: 0883-2927; 1872-9134
• DOI: 10.1016/j.apgeochem.2018.09.005

Identifying impacts of oil sands development on aquatic ecosystems requires understanding of the natural background water quality. In the Athabasca Oil Sands Region of Alberta this is challenging because the Athabasca River is incised directly into bitumen saturated sands of the McMurray Formation, and other saline Cretaceous and Devonian formations. This study compares the geochemical and isotopic composition of porewater sampled from the alluvial sediment beneath the Athabasca River with regional groundwater data to identify the geological origin of these saline groundwaters, and improve characterization of natural background sources of solutes entering the Athabasca River. Terrain conductivity surveys conducted along the Athabasca River were used to identify areas with evidence of saline groundwater discharge. Porewater samples were obtained from the alluvial sediment using drive point piezometers installed between 1 and 3 m below the water-sediment interface and were analyzed for δ18O, δ2H, δ34SSO4, δ18OSO4, 87Sr/86Sr, δ13C-DIC, δ13C-DOC, 3H, and 14C. The porewater in the alluvial sediment showed variable degrees of mixing with the overlying Athabasca River water, but the geochemical and isotopic composition in zones 1, 3 and 5 are consistent with discharge of saline groundwater from Cretaceous or Devonian units. The low percentages of modern carbon, and δ18O, δ2H, δ34SSO4, δ18OSO4, and 87Sr/86Sr signatures in the deepest porewater samples from Zones 1, 3 and 5 indicate glaciogenic water with high total dissolved solids originating from Devonian sourced solutes. Theses saline groundwater discharge zones occur where higher horizontal hydraulic gradients coincide with areas of higher salinity in the adjacent Cretaceous and Devonian aquifers, and areas with vertical connectivity with underlying Devonian aquifers. The results of this study demonstrate the influence of groundwater-surface water interactions and saline bedrock formation water discharge to water quality along some reaches of the Athabasca River which need to be considered in monitoring and water management strategies. [Display omitted] •Porewater sampled from sediment beneath the Athabasca River shows evidence of discharging saline groundwater.•The geochemical and isotopic signatures of this water are consistent with Cretaceous and Devonian formation waters.•Saline groundwater discharge zones occur where structural features are co-located with high TDS aquifers.•These natural sources of salin