Get 20M+ Full-Text Papers For Less Than $1.50/day. Start a 14-Day Trial for You and Your Team.

Learn More →

Potential for offsetting diamond mine carbon emissions through mineral carbonation of processed kimberlite: an assessment of De Beers mine sites in South Africa and Canada

Potential for offsetting diamond mine carbon emissions through mineral carbonation of processed... De Beers kimberlite mine operations in South Africa (Venetia and Voorspoed) and Canada (Gahcho Kué, Victor, and Snap Lake) have the potential to sequester carbon dioxide (CO2) through weathering of kimberlite mine tailings, which can store carbon in secondary carbonate minerals (mineral carbonation). Carbonation of ca. 4.7 to 24.0 wt% (average = 13.8 wt%) of annual processed kimberlite production could offset 100% of each mine site’s carbon dioxide equivalent (CO2e) emissions. Minerals of particular interest for reactivity with atmospheric or waste CO2 from energy production include serpentine minerals, olivine (forsterite), brucite, and smectite. The most abundant minerals, such as serpentine polymorphs, provide the bulk of the carbonation potential. However, the detection of minor amounts of highly reactive brucite in tailings from Victor, as well as the likely presence of brucite at Venetia, Gahcho Kué, and Snap Lake, is also important for the mineral carbonation potential of the mine sites. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Mineralogy and Petrology Springer Journals

Potential for offsetting diamond mine carbon emissions through mineral carbonation of processed kimberlite: an assessment of De Beers mine sites in South Africa and Canada

Download PDF
11 pages
Read Article

Loading next page...
 
/lp/springer_journal/potential-for-offsetting-diamond-mine-carbon-emissions-through-mineral-PlyTC0i8iM
Publisher
Springer Journals
Copyright
Copyright © 2018 by Springer-Verlag GmbH Austria, part of Springer Nature
Subject
Earth Sciences; Mineralogy; Inorganic Chemistry; Geochemistry
ISSN
0930-0708
eISSN
1438-1168
DOI
10.1007/s00710-018-0589-4
Publisher site
See Article on Publisher Site

Abstract

De Beers kimberlite mine operations in South Africa (Venetia and Voorspoed) and Canada (Gahcho Kué, Victor, and Snap Lake) have the potential to sequester carbon dioxide (CO2) through weathering of kimberlite mine tailings, which can store carbon in secondary carbonate minerals (mineral carbonation). Carbonation of ca. 4.7 to 24.0 wt% (average = 13.8 wt%) of annual processed kimberlite production could offset 100% of each mine site’s carbon dioxide equivalent (CO2e) emissions. Minerals of particular interest for reactivity with atmospheric or waste CO2 from energy production include serpentine minerals, olivine (forsterite), brucite, and smectite. The most abundant minerals, such as serpentine polymorphs, provide the bulk of the carbonation potential. However, the detection of minor amounts of highly reactive brucite in tailings from Victor, as well as the likely presence of brucite at Venetia, Gahcho Kué, and Snap Lake, is also important for the mineral carbonation potential of the mine sites.

Journal

Mineralogy and Petrology – Springer Journals

Published: May 28, 2018

References

  • Dynamics of carbon dioxide uptake in chrysotile mining residues – effect of mineralogy and liquid saturation
    Assima, GP; Larachi, F; Beaudoin, G; Molson, J
  • Reactive transport modeling of natural carbon sequestration in ultramafic mine tailings
    Bea, SA; Wilson, SA; Mayer, KU; Dipple, GM; Power, IM; Gamazo, P
  • Quantitative phase analysis using the Rietveld method
    Bish, DL; Howard, SA
  • Ex situ mineral carbonation for CO2 mitigation: evaluation of mining waste resources, aqueous carbonation processability, and life cycle assessment (Carmex project)
    Bodénan, F; Bourgeois, F; Petiot, C; Augé, T; Bonfils, B; Julcour-Lebigue, C; Guyot, F; Boukary, A; Tremosa, J; Lassin, A; Gaucher, EC; Chiquet, P
  • Surface and groundwater, weathering, and soils. Treatise on geochemistry
    Brantley, SL
  • The effect of grain or particle size on x-ray reflections from mixed powders and alloys, considered in relation to the quantitative determination of crystalline substances by x-ray methods
    Brindley, GW
  • The nature of kerolite, its relation to talc and stevensite
    Brindley, GW; Bish, DL; Wan, H-M
  • Adsorption of gases in multimolecular layers
    Brunauer, S; Emmett, PH; Teller, E
  • Stevensite in the modern thrombolites of Lake Clifton, Western Australia: a missing link in microbialite mineralization?
    Burne, RV; Moore, LS; Christy, AG; Troitzsch, U; King, PL; Carnerup, AM; Hamilton, PJ
  • A fundamental parameters approach to X-ray line-profile fitting
    Cheary, RW; Coelho, A
  • Kimberlite-hosted diamond deposits of southern Africa: a review
    Field, M; Stiefenhofer, J; Robey, J; Kurszlaukis, S
  • Carbonated serpentinite (listwanite) at Atlin, British Columbia: a geological analogue to carbon dioxide sequestration
    Hansen, LD; Dipple, GM; Gordon, TM; Kellett, DA
  • Accelerated carbonation of brucite in mine tailings for carbon sequestration
    Harrison, AL; Power, IM; Dipple, GM
  • The impact of evolving mineral-water-gas interfacial areas on mineral-fluid reaction rates in unsaturated porous media
    Harrison, AL; Dipple, GM; Power, IM; Mayer, KU
  • Changes in mineral reactivity driven by pore fluid mobility in partially wetted porous media
    Harrison, AL; Dipple, GM; Song, W; Power, IM; Mayer, KU; Beinlich, A; Sinton, D
  • Quantitative phase analysis from neutron powder diffraction data using the Rietveld method
    Hill, RJ; Howard, CJ
  • Application of symmetrized harmonics expansion to correction of the preferred orientation effect
    Järvinen, M
  • In situ molecular spetroscopic evidence for CO2 intercalation into montmorillonite in supercritical carbon dioxide
    Loring, JS; Schaef, HT; Turcu, RVF; Thompson, CJ; Miller, QRS; Martin, PF; Hu, J; Hoyt, DW; Qafoku, O; Ilton, ES; Felmy, AR; Rosso, KM
  • Permanent storage of carbon dioxide in geological reservoirs by mineral carbonation
    Matter, JM; Kelemen, PB
  • A greenhouse-scale photosynthetic microbial bioreactor for carbon sequestration in magnesium carbonate minerals
    McCutcheon, J; Power, I; Harrison, A; Dipple, G; Southam, G
  • Crystal structure of lizardite-1T from Elba, Italy
    Mellini, M; Viti, C
  • Unit-cell refinement from powder diffraction scans
    Pawley, GS
  • Geochemistry of geologic CO2 sequestration. Miner Soc am, Chantilly
    Power, IM; Harrison, AL; Dipple, GM; Wilson, SA; Kelemen, PB; Hitch, M; Southam, G
  • Strategizing carbon-neutral mines: A case for pilot projects
    Power, IM; McCutcheon, J; Harrison, AL; Wilson, SA; Dipple, GM; Kelly, S; Southam, C; Southam, G
  • A depositional model for hydromagnesite–magnesite playas near Atlin, British Columbia, Canada
    Power, IM; Wilson, SA; Harrison, AL; Dipple, GM; McCutcheon, J; Southam, G; Kenward, PA
  • A profile refinement method for nuclear and magnetic structures
    Rietveld, H
  • Interaction of diamond mine waste and surface water in the Canadian Arctic
    Rollo, HA; Jamieson, HE
  • Low-temperature serpentinization processes and kimberlite groundwater signatures in the Kirkland Lake and Lake Timiskiming kimberlite fields, Ontario, Canada: implications for diamond exploration
    Sader, JA; Leybourne, MI; McClenaghan, MB; Hamilton, SM
  • Quantification of phases with partial or no known crystal structures
    Scarlett, NVY; Madsen, IC
  • In situ XRD study of Ca2+ saturated montmorillonite (STX-1) exposed to anhydrous and wet supercritical carbon dioxide
    Schaef, HT; Ilton, ES; Qafoku, O; Martin, PF; Felmy, AR; Rosso, KM
  • Pyroclastic kimberlite deposits from the Victor Northwest pipe (Ontario, Canada): the transition from phreatomagmatic to magmatic explosivity
    Straaten, BI; Kopylova, MG
  • Post-emplacement serpentinization and related hydrothermal metamorphism in a kimberlite from Venetia, South Africa
    Stripp, GR; Field, M; Schumacher, JC; Sparks, RSJ; Cressey, G
  • Chrysotile dissolution rates: implications for carbon sequestration
    Thom, JM; Dipple, GM; Power, IM; Harrison, AL
  • The nature of disorder in montmorillonite by simulation of X-ray powder patterns
    Viani, A; Gualtieri, AF; Artioli, G
  • Verifying and quantifying carbon fixation in minerals from serpentine-rich mine tailings using the Rietveld method with X-ray powder diffraction data
    Wilson, SA; Raudsepp, M; Dipple, GM
  • Carbon dioxide fixation within mine wastes of ultramafic-hosted ore deposits: examples from the Clinton Creek and Cassiar chrysotile deposits, Canada
    Wilson, SA; Dipple, GM; Power, IM; Thom, JM; Anderson, RG; Raudsepp, M; Gabites, JE; Southam, G
  • Quantifying carbon fixation in trace minerals from processed kimberlite: a comparative study of quantitative methods using X-ray powder diffraction data with applications to the Diavik Diamond Mine, Northwest Territories, Canada
    Wilson, S; Raudsepp, M; Dipple, GM
  • Isotopic disequilibrium during uptake of atmospheric CO2 into mine process waters: implications for CO2 sequestration
    Wilson, SA; Barker, SLL; Dipple, GM; Atudorei, V
  • Subarctic weathering of mineral wastes provides a sink for atmospheric CO2
    Wilson, SA; Dipple, GM; Power, IM; Barker, SLL; Fallon, SJ; Southam, G
  • Offsetting of CO2 emissions by air capture in mine tailings at the Mount Keith Nickel mine, Western Australia: rates, controls and propects for carbon neutral mining
    Wilson, SA; Harrison, AL; Dipple, GM; Power, IM; Barker, SLL; Mayer, KU; Fallon, SJ; Raudsepp, M; Southam, G
  • Formation of low-T hydrated silicates in modern microbialites from Mexico and impliations for microbial fossilization
    Zeyen, N; Benzerara, K; Li, J; Groleau, A; Balan, E; Robert, J-L; Estève, I; Tavera, R; Moreira, D; López-Garcia, P