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
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Passive carbonate mineral formation from ultramafic tailings produced by nickel, diamond, and asbestos mining operations has been studied at active and historic mine sites.
“Passive carbonate mineral formation from ultramafic tailings produced by nickel, diamond,”
From Carbon Sequestration in Biogenic Magnesite and Other Magnesium Carbonate Minerals (2019) · cites this paper as [26]
Passive carbonation of ultramafic tailings has been documented at several sites under normal mining conditions.
“As an indication of their reactivity, passive carbonation of ultramafic tailings has been documented at several sites under normal mining conditions [11,17,18,20,21,24,26,30].”
From Strategizing carbon-neutral mines: A case for pilot projects (2014) · cites this paper as [21]
Passive carbonation has been documented at Clinton Creek, Diavik, Mount Keith, and other abandoned and active mine sites in Canada, United States, Australia, and Norway.
“Passive carbonation has been documented at Clinton Creek [18,20], Diavik [17,21], and Mount Keith [11,19] as well as other abandoned and active mine sites in Canada, United States, Australia, and Norway [24,26,30,42].”
From Strategizing carbon-neutral mines: A case for pilot projects (2014) · cites this paper as [21]
Clinton Creek produced approximately 11 Mt of chrysotile dominated tailings during its operational lifetime from 1967 to 1978.
“The mine produced approximately 11 Mt of chrysotile dominated tailings (Table 1) during its operational lifetime from 1967 to 1978 [21].”
From Strategizing carbon-neutral mines: A case for pilot projects (2014) · cites this paper as [21]
Metastable phases including lansfordite, nesquehonite, dypingite, and hydromagnesite typically form from weathering of ultramafic mine tailings.
“Thus, metastable phases including lansfordite [MgCO 3 •5H 2 O], nesquehonite [MgCO 3 •3H 2 O], dypingite [Mg 5 (CO 3 ) 4 (OH) 2 •5H 2 O], and hydromagnesite typically form from weathering of ultramafic mine tailings [11,18,20,21,26].”
From Strategizing carbon-neutral mines: A case for pilot projects (2014) · cites this paper as [21]
Passive carbonation at Diavik sequesters an estimated 374-418 g CO2/m2/year.
“Although the climatic conditions are similar at Diavik, passive carbonation at this site only sequesters an estimated 374-418 g CO 2 /m 2 /year [21].”
From Strategizing carbon-neutral mines: A case for pilot projects (2014) · cites this paper as [21]
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References 84 · Cited by 78
- Authors
- Wilson, S., Raudsepp, M., & Dipple, G. M.
- Affiliations
- University of British Columbia (CA)
- Corresponding author
- Wilson, Sasha
- Venue
- Applied Geochemistry
- Publisher
- Elsevier BV
- Published
- 2009-12
- Volume
- 24
- Issue
- 12
- Pages
- 2312-2331
- ISSN
- 0883-2927 (ISSN-L)
- OpenAlex
- W2141630701
- Cited by
- 78
- References
- 84
- Citations by year
- 2026: 3 · 2025: 3 · 2024: 5 · 2023: 5 · 2022: 6 · 2021: 6 · 2020: 4 · 2019: 7 · 2018: 6 · 2017: 5 · 2016: 1 · 2015: 5 · 2014: 5 · 2013: 8 · 2012: 2
- FWCI
- 1.45
- Type
- journal article
- Language
- en
- Update notices
- erratum (2010-02-01)
- Open access
- closed
- Licence
- Locations
- Applied Geochemistry (publishedVersion)
- Topics
- Physical Sciences › Materials Science › Materials Chemistry › X-ray Diffraction in Crystallography
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Mineralogy and Gemology Studies
- Physical Sciences › Environmental Science › Environmental Engineering › CO2 Sequestration and Geologic Interactions
- Keywords
- carbon sequestration, nesquehonite, lizardite, quantitative phase analysis, internal standard method, Rietveld refinement, crystallographic texture, Diavik Diamond Mine, carbon mineralization
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