minerals Review Geochemical Stability of Oil Sands Tailings in Mine Closure Landforms Heidi L. Cossey 1, Anya E. Batycky 1 , Heather Kaminsky 2 and Ania C. Ulrich 1,* 1 Department of Civil & Environmental Engineering, University of Alberta, Edmonton, AB T6G 1H9, Canada;
[email protected] (H.L.C.);
[email protected] (A.E.B.) 2 Centre for Oil Sands Sustainability, Northern Alberta Institute of Technology (NAIT), Edmonton, AB T5G 0Y2, Canada;
[email protected] * Correspondence:
[email protected]; Tel.: +1-780-492-8293 Abstract: Oil sands surface mining in Alberta has generated over a billion cubic metres of waste, known as tailings, consisting of sands, silts, clays, and process-affected water that contains toxic organic compounds and chemical constituents. All of these tailings will eventually be reclaimed and integrated into one of two types of mine closure landforms: end pit lakes (EPLs) or terrestrial landforms with a wetland feature. In EPLs, tailings deposits are capped with several metres of water while in terrestrial landforms, tailings are capped with solid materials, such as sand or overburden. Because tailings landforms are relatively new, past research has heavily focused on the geotechnical and biogeochemical characteristics of tailings in temporary storage ponds, referred to as tailings ponds. As such, the geochemical stability of tailings landforms remains largely unknown. This review discusses five mechanisms of geochemical change expected in tailings landforms: consolidation, chemical mass loading via pore water fluxes, biogeochemical cycling, polymer degradation, and surface water and groundwater interactions. Key considerations and knowledge gaps with regard Citation: Cossey, H.L.; Batycky, A.E.; Kaminsky, H.; Ulrich, A.C.