TY - JOUR
T1 - 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
AU - Mervine, Evelyn M.
AU - Wilson, Siobhan A.
AU - Power, Ian M.
AU - Dipple, Gregory M.
AU - Turvey, Connor C.
AU - Hamilton, Jessica L.
AU - Vanderzee, Sterling
AU - Raudsepp, Mati
AU - Southam, Colette
AU - Matter, Juerg M.
AU - Kelemen, Peter B.
AU - Stiefenhofer, Johann
AU - Miya, Zandile
AU - Southam, Gordon
PY - 2018/12
Y1 - 2018/12
N2 - 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.
AB - 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.
UR - http://www.scopus.com/inward/record.url?scp=85047658576&partnerID=8YFLogxK
U2 - 10.1007/s00710-018-0589-4
DO - 10.1007/s00710-018-0589-4
M3 - Article
AN - SCOPUS:85047658576
SN - 0930-0708
VL - 112
SP - 755
EP - 765
JO - Mineralogy and Petrology
JF - Mineralogy and Petrology
T2 - 11th International Kimberlite Conference (IKC)
Y2 - 18 September 2017 through 22 September 2017
ER -