Influence of saline groundwater discharge on river water chemistry in the Athabasca oil sands region - A chloride stable isotope and mass balance approach

摘要

A chloride mass and stable isotope (delta Cl-37) balance approach was employed to calculate the effect of saline groundwater discharge into the Athabasca and Clearwater rivers in the Athabasca Oil Sands Region (AOSR) in north-eastern Alberta, Canada. Saline groundwater affected by halite, carbonate, and anhydrite dissolution discharges Na-Cl type water with total dissolved solids (TDS) up to 51,700 mg/L from exposed Devonian and Cretaceous units in the river valleys in this area. In this study, nine springs discharging groundwater with a median Cl concentration of 9800 mg/L were sampled and chloride stable isotope ratios were determined, with delta Cl-37 values ranging from 0.2 to 1.0%. In contrast, river waters had historical monthly median Cl concentrations between 5.9 and 49.5 mg/L and delta Cl-37 values between -2.2 and -1.4%. The discharge rate of saline groundwater was calculated to be 100 +/- 20 L/s into the Clearwater River and 134 +/- 68 L/s into the Athabasca River. The chemical composition and discharge rates of saline groundwater were used to estimate its contribution to the mass fluxes of major ions, metals, and PAHs in the Athabasca and Clearwater rivers. Overall, saline groundwater contributed less than 0.2% of river discharge, but 0.04-39% of major ion concentrations in the rivers, with highest contributions under winter low-flow conditions. In the Clearwater River, saline groundwater contributed 23-39% of average monthly Cl flux and 18-32% of average monthly Na flux. For the same major ion fluxes in the Athabasca River, saline groundwater contributed 12-18% and 6-12%, respectively. The influence of saline groundwater discharge on the mass flux of trace elements in the rivers was found to be negligible, contributing less than 1% of river fluxes of Cu, Ni, Pb, and Zn. Similarly, the influence on mass flux of PAHs in the rivers was found to be negligible ( 0.03%) but quantifiable. These results provide important insights on the natural contribution