Geochemical behavior of amended and non-amended mine tailings as cover materials for acid mine drainage control: Column tests and reactive transport modeling
{"title":"Geochemical behavior of amended and non-amended mine tailings as cover materials for acid mine drainage control: Column tests and reactive transport modeling","authors":"Laila El-Affani , Bruno Bussière , Asif Qureshi , Benoît Plante","doi":"10.1016/j.jconhyd.2025.104564","DOIUrl":null,"url":null,"abstract":"<div><div>Mining companies generate large volumes of waste rock and tailings every year. To reduce these volumes, mining companies can valorize them as construction materials for cover systems such as cover with capillary barrier effects (CCBE). However, questions remain related to the geochemistry of the leachate that percolates through CCBEs made from mining materials. Limestone amendment can be used for increasing the neutralizing potential (NP) of mining materials in the case where the materials have a risk to generate contaminants. This study aims at assessing the performance of low-sulfide tailings, amended or not, and non-acid generating waste rock as components of CCBEs. To do so, five column tests were conducted in the laboratory to assess the long-term geochemical evolution of waste-rock, low-reactive tailings (2 % pyrite), tailings amended with 8 wt% of limestone, CCBE with the moisture-retaining layer (MRL) made of low-reactive tailings (CCBE-T), and CCBE with the MRL made of amended tailings (CCBE-TA). The geochemical evolution of leachates from the different column tests was simulated with MIN3P, a multicomponent reactive transport model. The numerical model was calibrated using results from the column tests. Long-term simulations using the short-term calibrated models suggested that low-reactive tailings could produce AMD when exposed to laboratory conditions, while limestone amendments effectively neutralized the generated acidity and stabilized the pH. Furthermore, incorporating tailings as a MRL in a CCBE reduced sulfide oxidation in the long-term due to the high degree of saturation that limited oxygen diffusion and sulfide reactivity.</div></div>","PeriodicalId":15530,"journal":{"name":"Journal of contaminant hydrology","volume":"272 ","pages":"Article 104564"},"PeriodicalIF":3.5000,"publicationDate":"2025-04-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of contaminant hydrology","FirstCategoryId":"93","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0169772225000695","RegionNum":3,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
引用次数: 0
Abstract
Mining companies generate large volumes of waste rock and tailings every year. To reduce these volumes, mining companies can valorize them as construction materials for cover systems such as cover with capillary barrier effects (CCBE). However, questions remain related to the geochemistry of the leachate that percolates through CCBEs made from mining materials. Limestone amendment can be used for increasing the neutralizing potential (NP) of mining materials in the case where the materials have a risk to generate contaminants. This study aims at assessing the performance of low-sulfide tailings, amended or not, and non-acid generating waste rock as components of CCBEs. To do so, five column tests were conducted in the laboratory to assess the long-term geochemical evolution of waste-rock, low-reactive tailings (2 % pyrite), tailings amended with 8 wt% of limestone, CCBE with the moisture-retaining layer (MRL) made of low-reactive tailings (CCBE-T), and CCBE with the MRL made of amended tailings (CCBE-TA). The geochemical evolution of leachates from the different column tests was simulated with MIN3P, a multicomponent reactive transport model. The numerical model was calibrated using results from the column tests. Long-term simulations using the short-term calibrated models suggested that low-reactive tailings could produce AMD when exposed to laboratory conditions, while limestone amendments effectively neutralized the generated acidity and stabilized the pH. Furthermore, incorporating tailings as a MRL in a CCBE reduced sulfide oxidation in the long-term due to the high degree of saturation that limited oxygen diffusion and sulfide reactivity.
期刊介绍:
The Journal of Contaminant Hydrology is an international journal publishing scientific articles pertaining to the contamination of subsurface water resources. Emphasis is placed on investigations of the physical, chemical, and biological processes influencing the behavior and fate of organic and inorganic contaminants in the unsaturated (vadose) and saturated (groundwater) zones, as well as at groundwater-surface water interfaces. The ecological impacts of contaminants transported both from and to aquifers are of interest. Articles on contamination of surface water only, without a link to groundwater, are out of the scope. Broad latitude is allowed in identifying contaminants of interest, and include legacy and emerging pollutants, nutrients, nanoparticles, pathogenic microorganisms (e.g., bacteria, viruses, protozoa), microplastics, and various constituents associated with energy production (e.g., methane, carbon dioxide, hydrogen sulfide).
The journal''s scope embraces a wide range of topics including: experimental investigations of contaminant sorption, diffusion, transformation, volatilization and transport in the surface and subsurface; characterization of soil and aquifer properties only as they influence contaminant behavior; development and testing of mathematical models of contaminant behaviour; innovative techniques for restoration of contaminated sites; development of new tools or techniques for monitoring the extent of soil and groundwater contamination; transformation of contaminants in the hyporheic zone; effects of contaminants traversing the hyporheic zone on surface water and groundwater ecosystems; subsurface carbon sequestration and/or turnover; and migration of fluids associated with energy production into groundwater.