Cited by 99CO2 Sequestration and Geologic InteractionsGroundwater and Isotope GeochemistryGeological and Geochemical Analysis

In situ sequestration of atmospheric CO2 at low temperature and surface cracking of serpentinized peridotite in mine shafts

Beinlich, Andreas, Austrheim, Håkon·2012·Chemical Geology

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Crossref · 10.1016/j.chemgeo.2012.09.015

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89 of 89 references verified0 citation errors · 0 not checkable

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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.”
  • 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,”
  • 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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