Paulo, Carlos
Predicting and monitoring drainage chemistry during mineral weathering for CO2 sequestration
Mineral feedstocks, including alkaline mine wastes, can sequester CO2 as a dissolved phase (e.g., HCO3-) or a solid carbonate via enhanced rock weathering (ERW). For this thesis, the release of easily accessible Ca and Mg from non-carbonate sources was determined for kimberlite residues from several diamond mines and commonly proposed ERW rock types, including wollastonite and olivine. Batch leaches determined the CO2 sequestration potentials of kimberlites to be in the range of 3–12 kg CO2/t, which was exceeded by most ERW feedstocks. Leaches also assessed the release of Ni and Cr, elements of concern in ERW settings, and P and K, which benefit agricultural soils. Year-long leaching columns were deployed using kimberlite from the Gahcho Kué and Venetia diamond mines, wollastonite skarn, and olivine sand from the initial assessment. The kimberlite residues sequestered 0.03 kg CO2/t as dissolved inorganic carbon and 0.6 kg CO2/t as solid total inorganic carbon. Weathering of wollastonite skarn resulted in CO2 removal rates via mineral trapping of CO2 of 6.31 kg CO2/t, while the olivine sand yielded rates of 0.5 kg CO2/t via solubility trapping. Both methodologies used in this study demonstrated value in the prediction and monitoring of drainage chemistry as it relates to ERW and CO2 mineralization. Implementation of these strategies can progress ERW efforts by providing confidence in feedstock selection and the verification of carbon offsets.
Author Keywords: CO2 mineralization, Drainage chemistry, Enhanced weathering, Mine wastes, Mineral trapping, Solubility trapping