Enhanced weathering of kimberlite residues in a field experiment: implications for carbon removal quantification and mine waste valorization

Scaling up enhanced rock weathering (ERW) will require gigatonnes of suitable rock, which could include mine wastes such as the estimated 3.9 Gt of kimberlite residues from historic diamond mining. Here, we conducted meter-scale field experiments (2021–2023) in Ontario, Canada, to assess fine proces...

Full description

Saved in:
Bibliographic Details
Main Authors: Zivi R. Schaffer, Kwon Rausis, Ian M. Power, Carlos Paulo
Format: Article
Language:English
Published: Frontiers Media S.A. 2025-07-01
Series:Frontiers in Climate
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fclim.2025.1592626/full
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1850109174419030016
author Zivi R. Schaffer
Kwon Rausis
Ian M. Power
Carlos Paulo
author_facet Zivi R. Schaffer
Kwon Rausis
Ian M. Power
Carlos Paulo
author_sort Zivi R. Schaffer
collection DOAJ
description Scaling up enhanced rock weathering (ERW) will require gigatonnes of suitable rock, which could include mine wastes such as the estimated 3.9 Gt of kimberlite residues from historic diamond mining. Here, we conducted meter-scale field experiments (2021–2023) in Ontario, Canada, to assess fine processed kimberlite residues for ERW and test carbon-based methods for CO2 removal (CDR) quantification, including CO2 fluxes, and measurements of soil and porewater inorganic carbon. A control plot consisted of local calcareous (16.1 wt.% calcite) Brunisolic soil to assess background weathering rates. Two soil plots were amended with 20 and 40 kg of kimberlite residues from the Gahcho Kué Diamond Mine (Northwest Territories, Canada) that contained 30.2 wt.% lizardite [Mg3Si2O5(OH)4], 9.4 wt.% forsterite (Mg2SiO4), and 1.9 wt.% calcite (CaCO3). Coinciding with increases in Mg and Si, dissolved inorganic carbon increased in porewaters with kimberlite dosage (amended: 64–118 mg C/L, control: 56 ± 14 mg C/L), demonstrating CO2 solubility trapping. Water chemistry data, coupled with a water budget derived from weather and soil moisture data, were used to determine CDR rates. The removal rates by the kimberlite residues were up to 1.4 t CO2/ha over 3 years calculated using porewater inorganic carbon loadings, with Ca and Si loadings allowing for partitioning of rates into removal contributions by kimberlite-derived carbonate weathering (~75%) and silicate weathering (~25%), respectively. CO2 fluxes and soil inorganic carbon proved ineffective for CDR quantification, given the high effluxes due to soil respiration and high and variable carbonate content of the soils, respectively. Stable carbon isotope data demonstrated that the removed CO2 was derived from organic carbon, suppressing soil CO2 effluxes to the atmosphere. This study has implications for repurposing environmentally safe mine wastes for ERW with the potential to reduce net CO2 emissions and storage and remediation costs in the mining industry. We highlight similarities between kimberlite residues and basalt fines, a common quarry by-product used in ERW, advocating for the use of processed rock from current and legacy mining operations for CDR. Further, our CDR monitoring approaches that effectively distinguish between silicate and carbonate weathering may be utilized in other ERW applications.
format Article
id doaj-art-b6bd2545596d454e8734fc935836216a
institution OA Journals
issn 2624-9553
language English
publishDate 2025-07-01
publisher Frontiers Media S.A.
record_format Article
series Frontiers in Climate
spelling doaj-art-b6bd2545596d454e8734fc935836216a2025-08-20T02:38:10ZengFrontiers Media S.A.Frontiers in Climate2624-95532025-07-01710.3389/fclim.2025.15926261592626Enhanced weathering of kimberlite residues in a field experiment: implications for carbon removal quantification and mine waste valorizationZivi R. SchafferKwon RausisIan M. PowerCarlos PauloScaling up enhanced rock weathering (ERW) will require gigatonnes of suitable rock, which could include mine wastes such as the estimated 3.9 Gt of kimberlite residues from historic diamond mining. Here, we conducted meter-scale field experiments (2021–2023) in Ontario, Canada, to assess fine processed kimberlite residues for ERW and test carbon-based methods for CO2 removal (CDR) quantification, including CO2 fluxes, and measurements of soil and porewater inorganic carbon. A control plot consisted of local calcareous (16.1 wt.% calcite) Brunisolic soil to assess background weathering rates. Two soil plots were amended with 20 and 40 kg of kimberlite residues from the Gahcho Kué Diamond Mine (Northwest Territories, Canada) that contained 30.2 wt.% lizardite [Mg3Si2O5(OH)4], 9.4 wt.% forsterite (Mg2SiO4), and 1.9 wt.% calcite (CaCO3). Coinciding with increases in Mg and Si, dissolved inorganic carbon increased in porewaters with kimberlite dosage (amended: 64–118 mg C/L, control: 56 ± 14 mg C/L), demonstrating CO2 solubility trapping. Water chemistry data, coupled with a water budget derived from weather and soil moisture data, were used to determine CDR rates. The removal rates by the kimberlite residues were up to 1.4 t CO2/ha over 3 years calculated using porewater inorganic carbon loadings, with Ca and Si loadings allowing for partitioning of rates into removal contributions by kimberlite-derived carbonate weathering (~75%) and silicate weathering (~25%), respectively. CO2 fluxes and soil inorganic carbon proved ineffective for CDR quantification, given the high effluxes due to soil respiration and high and variable carbonate content of the soils, respectively. Stable carbon isotope data demonstrated that the removed CO2 was derived from organic carbon, suppressing soil CO2 effluxes to the atmosphere. This study has implications for repurposing environmentally safe mine wastes for ERW with the potential to reduce net CO2 emissions and storage and remediation costs in the mining industry. We highlight similarities between kimberlite residues and basalt fines, a common quarry by-product used in ERW, advocating for the use of processed rock from current and legacy mining operations for CDR. Further, our CDR monitoring approaches that effectively distinguish between silicate and carbonate weathering may be utilized in other ERW applications.https://www.frontiersin.org/articles/10.3389/fclim.2025.1592626/fullkimberlitemine wasteenhanced weatheringCO2 removalcarbon accountingfield experiment
spellingShingle Zivi R. Schaffer
Kwon Rausis
Ian M. Power
Carlos Paulo
Enhanced weathering of kimberlite residues in a field experiment: implications for carbon removal quantification and mine waste valorization
Frontiers in Climate
kimberlite
mine waste
enhanced weathering
CO2 removal
carbon accounting
field experiment
title Enhanced weathering of kimberlite residues in a field experiment: implications for carbon removal quantification and mine waste valorization
title_full Enhanced weathering of kimberlite residues in a field experiment: implications for carbon removal quantification and mine waste valorization
title_fullStr Enhanced weathering of kimberlite residues in a field experiment: implications for carbon removal quantification and mine waste valorization
title_full_unstemmed Enhanced weathering of kimberlite residues in a field experiment: implications for carbon removal quantification and mine waste valorization
title_short Enhanced weathering of kimberlite residues in a field experiment: implications for carbon removal quantification and mine waste valorization
title_sort enhanced weathering of kimberlite residues in a field experiment implications for carbon removal quantification and mine waste valorization
topic kimberlite
mine waste
enhanced weathering
CO2 removal
carbon accounting
field experiment
url https://www.frontiersin.org/articles/10.3389/fclim.2025.1592626/full
work_keys_str_mv AT zivirschaffer enhancedweatheringofkimberliteresiduesinafieldexperimentimplicationsforcarbonremovalquantificationandminewastevalorization
AT kwonrausis enhancedweatheringofkimberliteresiduesinafieldexperimentimplicationsforcarbonremovalquantificationandminewastevalorization
AT ianmpower enhancedweatheringofkimberliteresiduesinafieldexperimentimplicationsforcarbonremovalquantificationandminewastevalorization
AT carlospaulo enhancedweatheringofkimberliteresiduesinafieldexperimentimplicationsforcarbonremovalquantificationandminewastevalorization