Reactive Transport Modeling of Natural Carbon Sequestration in Ultramafic Mine Tailings

• Autores: Bea, Sergio Andrés; Wilson, S. A.; Mayer, Klaus Ulrich; Dipple, G. M.; Power, I. M.; Gamazo, Pablo Andrés
• Año de publicación: 2012
• Idioma: inglés
• Tipo de recurso: artículo
• Materia: reactive transport modeling; carbon sequestration; BET; kinetic dissolution/precipitation
• Institución: Consejo Nacional de Investigaciones Científicas y Técnicas

Atmospheric CO2 is naturally sequestered in ultramafi c mine tailings as a result of the weathering of serpentine minerals [Mg3Si2O5(OH)4] and brucite [Mg(OH)2], and subsequent mineralization of CO2 in hydrated magnesium carbonate minerals, such as hydromagnesite [Mg5(CO3)4(OH)2·4H2O]. Understanding the CO2 trapping mechanisms is key to evaluating the capacity of such tailings for carbon sequestration. Natural CO2 sequestration in subaerially exposed ultramafic tailings at a mine site near Mount Keith, Australia is assessed with a process-based reactive transport model. The model formulation includes unsaturated flow, equations accounting for energy balance and vapor diffusion, fully coupled with solute transport, gas diffusion, and geochemical reactions. Atmospheric boundary conditions accounting for the effect of climate variations are also included. Kinetic dissolution of serpentine, dissolution-precipitation on of brucite and primary carbonates-calcite (CaCO3), dolomite [MgCa(CO3)2], magnesite (MgCO3), as well as the formation of hydromagnesite, halite (NaCl), gypsum (CaSO4·2H2O), blödite [Na2Mg(SO4)2·4H2O], and epsomite [MgSO4·7H2O]-are considered. Simulation on results are consistent with field observations and mineralogical data from tailings that weathered for 10 yr. Precipitation of hydromagnesite is both predicted and observed, and is mainly controlled by the dissolution on of serpentine (the source of Mg) and equilibrium with CO2 ingressing from the atmosphere. The predicted rate for CO2 entrapment in these tailings ranges between 0.6 and 1 kg m-2 yr-1. However, modeling results suggest that this rate is sensitive to CO2 ingress through the mineral waste and may be enhanced by several mechanisms, including atmospheric pumping.
Fil: Bea, Sergio Andrés. Comisión de Investigaciones Científicas de la Provincia de Buenos Aires. Instituto de Hidrología de Llanuras "Dr. Eduardo Jorge Usunoff". - Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tandil. Instituto de Hidrología de Llanuras "Dr. Eduardo Jorge Usunoff". - Universidad Nacional del Centro de la Provincia de Buenos Aires. Instituto de Hidrología de Llanuras "Dr. Eduardo Jorge Usunoff"; Argentina. University of British Columbia; Canadá. Lawrence Berkeley National Laboratory; Estados Unidos
Fil: Wilson, S. A.. University of British Columbia; Canadá. Monash University; Australia
Fil: Mayer, Klaus Ulrich. University of British Columbia; Canadá
Fil: Dipple, G. M.. University of British Columbia; Canadá
Fil: Power, I. M.. University of British Columbia; Canadá
Fil: Gamazo, Pablo Andrés. Universidad de la República. Centro Universitario del Litoral Norte. Centro Universitario de Salto; Uruguay