No discernible effect of Mg2+ ions on the equilibrium oxygen isotope fractionation in the CO2-H2O system
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At the small concentration of Mg2+ (2.5 mM) used in the Uchikawa and Zeebe (2013) experiments, we predict the presence of Mg2+ has a negligible effect on α18O, consistent with experimental data.
“At the small concentration of Mg 2+ (2.5mM) used in the Uchikawa and Zeebe (2013) experiments, we predict the presence of Mg 2+ has a negligible effect on α 18 O, consistent with experimental data.”
From Theoretical constraints on the effects of added cations on clumped, oxygen, and carbon isotope signatures of dissolved inorganic carbon species and minerals (2020) · cites this paper as Uchikawa and Zeebe (2013)
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References 64 · Cited by 16
- Authors
- Uchikawa, J., & Zeebe, R. E.
- Affiliations
- University of Hawaiʻi at Mānoa (US)
- Corresponding author
- Uchikawa, Joji
- Venue
- Chemical Geology
- Publisher
- Elsevier BV
- Published
- 2013-04
- Volume
- 343
- Pages
- 1-11
- ISSN
- 0009-2541 (ISSN-L)
- OpenAlex
- W2151456842
- Cited by
- 16
- References
- 64
- Citations by year
- 2023: 1 · 2022: 3 · 2021: 3 · 2020: 3 · 2019: 1 · 2018: 2 · 2015: 1 · 2014: 2
- FWCI
- 1.25
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Chemical Geology (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Groundwater and Isotope Geochemistry
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- oxygen isotope fractionation, CO2-H2O system, magnesium ions, barium carbonate precipitation, magnesium carbonate, dissolved inorganic carbon, seawater, ionic interactions
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