CO2 mineralization of kimberlite residues from the Gahcho Kué Diamond Mine, Northwest Territories, Canada

• CO 2 batch leaches, shot-term assessments, and year-long weathering columns were used to predict and quantify CO 2 sequestration. • Gahcho Kué Diamond Mine resides can remove 12 kg CO 2 /t based on labile Ca and Mg. • Year-term monitoring predicted a sequestration rate of 0.63 kg CO 2 /t/yr without enhancements. • An assessment of CO 2 sequestration for 40-days immediately following deposition reveals the total removal 0.86 kg CO 2 /t, as the residues were allowed to dry. • Incorporating enhanced weathering into mine closure would lead to substantial CO 2 removal. Kimberlite residues generated at diamond mines have the potential to substantially reduce net greenhouse gas emissions and contribute towards carbon-neutral mining. As part of the De Beers CarbonVault™, we conducted experiments using fine kimberlite residues from the Gahcho Kué Diamond Mine, Northwest Territories, Canada, to assess the mine's potential for CO 2 sequestration. Batch CO 2 leach tests indicate a CO 2 sequestration potential of 12 kg CO 2 /t based on easily extractable cations from non-carbonate sources. However, an evaluation of the short-term reactivity of the residues post-deposition revealed the ability to sequester 0.86 kg CO 2 /t when residues were allowed to dry through optimal water saturation (30–40 %). Furthermore, year-long weathering columns determined a CO 2 removal rate of 0.63 kg CO 2 /t/yr, primarily through mineral trapping. Extrapolating these rates to current annual residue production and emissions indicates that 7 % of the mine's estimated CO 2 e emissions could be sequestered over the life of mine. These rates are based on optimal storage conditions that keep residues exposed for long periods, which should be a consideration of residue management practices during the operating life of the mine and post closure. Further on-site investigations are necessary to refine rates and account for climatic conditions. Assessments conducted in this study affirm the suitability of Gahcho Kué residues for CO 2 sequestration and present strategies for optimizing this process.

Authors

Institutions

Publication Details

Journal
International journal of greenhouse gas control
Published
2025-04-17
DOI
https://doi.org/10.1016/j.ijggc.2025.104376
Citations
3
Primary Topic
CO2 Sequestration and Geologic Interactions
Type
article
Field-Weighted Citation Impact
2.40

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

CO2 mineralization of kimberlite residues from the Gahcho Kué Diamond Mine, Northwest Territories, Canada

Ian Malcom Power, D. McDonald, Sasha Wilson, Carlos Paulo
3 citations
International journal of greenhouse gas control
CO2 Sequestration and Geologic Interactions
2.40
article

CO2 mineralization of kimberlite residues from the Gahcho Kué Diamond Mine, Northwest Territories, Canada

Ian Malcom Power, D. McDonald, Sasha Wilson, Carlos Paulo
article en
3 citations

Abstract

• CO 2 batch leaches, shot-term assessments, and year-long weathering columns were used to predict and quantify CO 2 sequestration. • Gahcho Kué Diamond Mine resides can remove 12 kg CO 2 /t based on labile Ca and Mg. • Year-term monitoring predicted a sequestration rate of 0.63 kg CO 2 /t/yr without enhancements. • An assessment of CO 2 sequestration for 40-days immediately following deposition reveals the total removal 0.86 kg CO 2 /t, as the residues were allowed to dry. • Incorporating enhanced weathering into mine closure would lead to substantial CO 2 removal. Kimberlite residues generated at diamond mines have the potential to substantially reduce net greenhouse gas emissions and contribute towards carbon-neutral mining. As part of the De Beers CarbonVault™, we conducted experiments using fine kimberlite residues from the Gahcho Kué Diamond Mine, Northwest Territories, Canada, to assess the mine's potential for CO 2 sequestration. Batch CO 2 leach tests indicate a CO 2 sequestration potential of 12 kg CO 2 /t based on easily extractable cations from non-carbonate sources. However, an evaluation of the short-term reactivity of the residues post-deposition revealed the ability to sequester 0.86 kg CO 2 /t when residues were allowed to dry through optimal water saturation (30–40 %). Furthermore, year-long weathering columns determined a CO 2 removal rate of 0.63 kg CO 2 /t/yr, primarily through mineral trapping. Extrapolating these rates to current annual residue production and emissions indicates that 7 % of the mine's estimated CO 2 e emissions could be sequestered over the life of mine. These rates are based on optimal storage conditions that keep residues exposed for long periods, which should be a consideration of residue management practices during the operating life of the mine and post closure. Further on-site investigations are necessary to refine rates and account for climatic conditions. Assessments conducted in this study affirm the suitability of Gahcho Kué residues for CO 2 sequestration and present strategies for optimizing this process.

International journal of greenhouse gas controlVol. 144
University of Alberta (CA), Trent University (CA)
Canada Research Chairs, Mitacs, De Beers Group, Natural Sciences and Engineering Research Council of Canada
Openalex Percentile: Top 13%
CO2 Sequestration and Geologic Interactions
2.40
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.