In situ sequestration of atmospheric CO2 at low temperature and surface cracking of serpentinized peridotite in mine shafts
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Brucite carbonation has been documented in TSF1 tailings at Mount Keith and in a sub-arctic mine shaft.
“Bea et al. (2012) and Beinlich and Austrheim (2012) have also documented brucite carbonation in mine tailings from TSF1 at Mount Keith and in a sub-arctic mine shaft, respectively.”
From Offsetting of CO2 emissions by air capture in mine tailings at the Mount Keith Nickel Mine, Western Australia: Rates, controls and prospects for carbon neutral mining (2014) · cites this paper as Beinlich and Austrheim, 2012
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 [28]
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 [26]
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 [26]
Stable carbon and oxygen isotopic compositions of hydrated Mg-carbonate minerals formed from weathering of ultramafic mine tailings at Diavik, Mount Keith, and other ultramafic-hosted mines in Norway are consistent with carbon mineralization under CO2 limited conditions.
“Stable carbon and oxygen isotopic compositions of hydrated Mg-carbonate minerals formed from weathering of ultramafic mine tailings at Diavik [17], Mount Keith [16], and other ultramafic-hosted mines in Norway [26] are consistent with carbon mineralization under CO 2 limited conditions.”
From Strategizing carbon-neutral mines: A case for pilot projects (2014) · cites this paper as [26]
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- Authors
- Beinlich, A., & Austrheim, H.
- Affiliations
- University of Oslo (NO)
- Corresponding author
- Beinlich, Andreas
- Venue
- Chemical Geology
- Publisher
- Elsevier BV
- Published
- 2012-11
- Volume
- 332-333
- Pages
- 32-44
- ISSN
- 0009-2541 (ISSN-L)
- OpenAlex
- W2050339905
- Cited by
- 99
- References
- 90
- Citations by year
- 2026: 4 · 2025: 8 · 2024: 5 · 2023: 6 · 2022: 7 · 2021: 9 · 2020: 6 · 2019: 6 · 2018: 8 · 2017: 14 · 2016: 4 · 2015: 5 · 2014: 8 · 2013: 7 · 2012: 2
- FWCI
- 5.48
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Chemical Geology (publishedVersion)
- eSpace (Curtin University) (submittedVersion)
- Funders
- Norges Forskningsråd
- Topics
- Physical Sciences › Environmental Science › Environmental Engineering › CO2 Sequestration and Geologic Interactions
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Groundwater and Isotope Geochemistry
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Keywords
- serpentinized peridotite, nesquehonite, Rayleigh distillation, heavy isotope enrichment, subcritical crack growth, mine shafts, chromite, CO2 sequestration
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