Abstract
In order to reduce contaminant mass loadings, thermal cover systems may be incorporated in the design of waste rock piles located in regions of continuous permafrost. In this study, reactive transport modeling was used to improve the understanding of coupled thermo-hydrological and chemical processes controlling the evolution of a covered waste rock pile located in Northern Canada. Material properties from previous field and laboratory tests were incorporated into the model to constrain the simulations. Good agreement between simulated and observational temperature data indicates that the model is capable of capturing the coupled thermo-hydrological processes occurring within the pile. Simulations were also useful for forecasting the pile’s long-term evolution with an emphasis on water flow and heat transport mechanisms, but also including geochemical weathering processes and sulfate mass loadings as an indicator for the release of contaminated drainage. An uncertainty analysis was carried out to address different scenarios of the cover’s performance as a function of the applied infiltration rate, accounting for the impacts of evaporation, runoff, and snow ablation. The model results indicate that the cover performance is insensitive to the magnitude of recharge rates, except for limited changes of the flow regime in the shallow active layer. The model was expanded by performing an additional sensitivity analysis to assess the role of cover thicknesses. The simulated results reveal that a cover design with an appropriate thickness can effectively minimize mass loadings in drainage by maintaining the active layer completely within the cover.
Highlights
Large volumes of waste rock are generated and removed from the subsurface during mining operations. This waste rock poses long-term environmental risks related to acid rock drainage (ARD) or contaminated neutral drainage (CND), if sufficient pH-buffering minerals are present in the waste rock, such as carbonate minerals
Simulations show that seasonal temperature fluctuations at greater depth are much lower and lag significantly behind temperature changes near the surface due to the effects of heat conduction, consistent with observed patterns. Both measured and simulated results show that the core of the waste rock pile (WRP) remains frozen and nearly constant in extent, even in the warm seasons for the first 4 years, with only the cover thawing in summer and early fall
In addition to experimental or field tests, reactive transport modeling (RTM) provides a versatile tool for assessing the performance of thermal covers in permafrost environments and their impact on limiting sulfide mineral oxidation and mass loadings
Summary
Large volumes of waste rock (considered non-economically viable materials) are generated and removed from the subsurface during mining operations This waste rock (which is usually stored in large and unsaturated stockpiles at ground surface) poses long-term environmental risks related to acid rock drainage (ARD) or contaminated neutral drainage (CND), if sufficient pH-buffering minerals are present in the waste rock, such as carbonate minerals. Thermal covers ( known as insulation covers) are a unique option in cold regions where permafrost is typically found due to prevailing cold temperatures, implying that soils remain perennially frozen for at least two consecutive years [5,9,10,11,12]
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