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Isotopic evidence of passive mineral carbonation in mine wastes from the Dumont Nickel Project (Abitibi, Quebec)

bul.description.provenanceemo spbfr
bul.rights.raisonEmbargoInfiniPour que le document soit diffusé en libre accès, en accord avec le délai prescrit par l’éditeur de International Journal of Greenhouse Gas Control, il faudrait déposer la version acceptée pour publication, incluant toutes les modifications demandées, mais sans la mise en page de la revue. Pour ce faire, effectuez une demande de modification à l’aide de la liste des dépôts diffusés à partir du tableau de
dc.contributor.authorBeaudoin, Georges
dc.contributor.authorDupont, Pierre
dc.contributor.authorGras, Antoine
dc.contributor.authorBussière, Bruno
dc.contributor.authorLemieux, Jean-Michel
dc.contributor.authorPlante, Benoît
dc.contributor.authorMolson, John W. H.
dc.coverage.spatialAbitibi (Québec)fr
dc.description.abstractNatural weathering of ultramafic rocks in mine tailings captures atmospheric CO2 through the formation of magnesium carbonates. The Dumont Nickel Project (DNP) is of particular interest as it will generate 1.7 Gt of ultramafic residues. A field experiment has been conducted at the DNP site in order to understand the process of natural CO2 sequestration. Two experimental cells were built using waste rock and mineral processing tailings and were instrumented with gas sampling ports and probes to monitor water saturation and suction. A decrease of the interstitial gas-phase CO2 concentration in both cells, from atmospheric values (∼390 ppmv) near the surface to ∼100 ppmv near the bottom, reflects active CO2 consumption by the residues. The total carbon content of the weathered DNP mine waste ranges from 0.2 wt% to 6.5 wt% C. Hydrotalcites supergroup minerals (pyroaurite-3R, brugnatellite, pyroaurite 2-H), aragonite, nesquehonite, dypingite and hydromagnesite were absent from the unweathered residues and precipitated in the cells during passive mineral carbonation. In situ measurements using Wavelength-Scanned Cavity Ring Down Spectroscopy reveal an increase of δ13C(air) from −8‰ near the surface of the cells to ∼2‰ near the bottom that is correlated with the decrease in CO2 concentration. This trend is explained by kinetic carbon isotope fractionation during dissolution of atmospheric CO2 in interstitial water (ΔDIC-CO2 = −11.2‰). Secondary carbonates, precipitated from the interstitial water, are characterized by a moderately high δ18O and low δ13C. These isotopic compositions of the carbonates are consistent with precipitation in an evaporative environment where the kinetic carbon fractionation during atmospheric CO2 dissolution produces interstitial water depleted in 13C. Moreover, isotopic compositions of hydrotalcite supergroup minerals and other carbonate minerals are consistent with modern precipitation from the weathering of mining residue. These observations demonstrate the atmospheric source for the sequestered CO2 and help constrain a conceptual model of the carbonation reaction in the
dc.subjectMineral carbonationfr
dc.subjectCarbonation mechanismsfr
dc.subjectCO2 sequestrationfr
dc.subjectMining residuesfr
dc.subjectCarbon and oxygen isotopesfr
dc.subjectExperimental field cellfr
dc.subject.rvmMinéraux carbonatésfr
dc.subject.rvmPiégeage du carbonefr
dc.subject.rvmCarbone -- Isotopesfr
dc.subject.rvmOxygène -- Isotopesfr
dc.titleIsotopic evidence of passive mineral carbonation in mine wastes from the Dumont Nickel Project (Abitibi, Quebec)fr
dc.typearticle de recherche
dc.type.legacyCOAR1_1::Texte::Périodique::Revue::Contribution à un journal::Article::Article de recherchefr
dcterms.bibliographicCitationInternational journal of greenhouse gas control, Vol. 60, 10–23 (2017)fr
dspace.accessstatus.time2023-05-24 18:03:13
rioxxterms.project.funder-nameRNC Mineralsfr
rioxxterms.project.funder-nameNatural Sciences and Engineering Research Council of Canada Collaborative Research and Development (NSERC CRD)fr
rioxxterms.versionVersion of Record (VoR)fr
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