Dissolution kinetics of platinum mine by-products for nature-based and engineered carbon dioxide removal

In addition to deep reductions in greenhouse gas emissions, active removal of atmospheric CO 2 is essential to limit global warming to <2 °C above pre-industrial levels. Dissolution of crushed silicate rocks by carbonic acid converts CO 2 into stable carbon species (alkalinity, carbonate minerals), but its effectiveness for CO 2 removal (CDR) depends on identifying suitably abundant and reactive feedstocks. Here, we assess dissolution rates of crushed by-products (overburden, processed tailings, smelter slags) from platinum group metal (PGM) mining operations within the Bushveld Complex, South Africa, during reaction with water and CO 2 under far from equilibrium conditions. Mine tailings had fastest bulk dissolution rates (∼10 -10 to 10 -8 mol m -2 s -1 ), with fresh material sourced directly from concentrator conveyor belts reacting faster than tailings collected from settling ponds. Glassy slag material dissolved at rates of 10 -11 to 10 -9 mol m -2 s -1 , whereas plagioclase-rich overburden rocks reacted more slowly, with dissolution rates of 10 -12 to 10 -10 mol m -2 s -1 . Finer-grained overburden material generally dissolved more slowly than coarser fractions, likely due to particle clustering, surface passivation and/or enrichment of slower-reacting clays in finer material. Under CO 2 -saturated conditions, relative bulk dissolution rates of PGM by-products were generally faster (by ∼1-3 orders of magnitude) than for other potential CDR feedstocks, such as basalt and gabbro. At the global scale, weathering of PGM by-products has the potential to sequester up to one gigatonne of CO 2 per year, of which the Bushveld Complex may account for as much as 75%. However, we caution that while our experiments show that PGM by-products have high intrinsic reactivity, they are unlikely to deliver durable and substantial CDR under field conditions where factors such as availability of CO 2 and soil water flow rate may inhibit dissolution. The CDR potential of PGM by-products is only likely to be fully realised with process intensification, such as using reactors or through microbial augmentation.

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Journal
Applied Geochemistry
Published
2026-06-30
DOI
https://doi.org/10.1016/j.apgeochem.2026.106964
Primary Topic
CO2 Sequestration and Geologic Interactions
Type
article
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article

Dissolution kinetics of platinum mine by-products for nature-based and engineered carbon dioxide removal

J. Matter, Rachael H. James, Liam A. Bullock, Manon T. Duret et al.
Applied Geochemistry
CO2 Sequestration and Geologic Interactions
article

Dissolution kinetics of platinum mine by-products for nature-based and engineered carbon dioxide removal

J. Matter, Rachael H. James, Liam A. Bullock, Manon T. Duret, E. M. Mervine, E. Smith, D. Hasson, D.A.H. Teagle, A. Cunningham
article en

Abstract

In addition to deep reductions in greenhouse gas emissions, active removal of atmospheric CO 2 is essential to limit global warming to <2 °C above pre-industrial levels. Dissolution of crushed silicate rocks by carbonic acid converts CO 2 into stable carbon species (alkalinity, carbonate minerals), but its effectiveness for CO 2 removal (CDR) depends on identifying suitably abundant and reactive feedstocks. Here, we assess dissolution rates of crushed by-products (overburden, processed tailings, smelter slags) from platinum group metal (PGM) mining operations within the Bushveld Complex, South Africa, during reaction with water and CO 2 under far from equilibrium conditions. Mine tailings had fastest bulk dissolution rates (∼10 -10 to 10 -8 mol m -2 s -1 ), with fresh material sourced directly from concentrator conveyor belts reacting faster than tailings collected from settling ponds. Glassy slag material dissolved at rates of 10 -11 to 10 -9 mol m -2 s -1 , whereas plagioclase-rich overburden rocks reacted more slowly, with dissolution rates of 10 -12 to 10 -10 mol m -2 s -1 . Finer-grained overburden material generally dissolved more slowly than coarser fractions, likely due to particle clustering, surface passivation and/or enrichment of slower-reacting clays in finer material. Under CO 2 -saturated conditions, relative bulk dissolution rates of PGM by-products were generally faster (by ∼1-3 orders of magnitude) than for other potential CDR feedstocks, such as basalt and gabbro. At the global scale, weathering of PGM by-products has the potential to sequester up to one gigatonne of CO 2 per year, of which the Bushveld Complex may account for as much as 75%. However, we caution that while our experiments show that PGM by-products have high intrinsic reactivity, they are unlikely to deliver durable and substantial CDR under field conditions where factors such as availability of CO 2 and soil water flow rate may inhibit dissolution. The CDR potential of PGM by-products is only likely to be fully realised with process intensification, such as using reactors or through microbial augmentation.

Applied GeochemistryVol. 207
The University of Queensland (AU), National Oceanography Centre (GB), Instituto Geológico y Minero de España (ES), University of Chicago (US), Geophysical Laboratory (US)
Fundación General CSIC, Natural Environment Research Council, H2020 Marie Skłodowska-Curie Actions
Openalex Percentile: Top 11%
CO2 Sequestration and Geologic Interactions
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