Experimental study on mafic rock dissolution rates within CO2-seawater-rock systems
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The observed pH swing is faster and more progressive compared to trends reported for reactions of CO2 with basalt and olivine.
“However, the observed pH swing is faster and more progressive compared to the trends reported for the reactions of CO2 with both basalt52,53 and olivine25.”
From Low temperature carbonation and CO2 mineral trapping in altered hydrotalcite-rich ultrmafic rocks (2025) · cites this paper as [52]
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- Authors
- Marieni, C., Matter, J. M., & Teagle, D. A. H.
- Affiliations
- National Oceanography Centre (GB)
- Corresponding author
- Marieni, Chiara
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 2020-03
- Volume
- 272
- Pages
- 259-275
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W3000277832
- Cited by
- 74
- References
- 92
- Citations by year
- 2026: 13 · 2025: 16 · 2024: 16 · 2023: 16 · 2022: 6 · 2021: 6 · 2020: 1
- FWCI
- 2.60
- Type
- journal article
- Language
- en
- Open access
- green
- doi.org
- Locations
- Geochimica et Cosmochimica Acta (publishedVersion)
- ePrints Soton (University of Southampton) (submittedVersion)
- HAL (submittedVersion)
- Funders
- University of Southampton
- Topics
- Physical Sciences › Environmental Science › Environmental Engineering › CO2 Sequestration and Geologic Interactions
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Keywords
- CO2 sequestration, seawater-rock interaction, incongruent dissolution, silicon release, calcium release, plagioclase dissolution, mass transfer limitations, dissolution kinetics, CO2 geological storage, Juan de Fuca plate, Mid-Atlantic Ridge, Troodos ophiolite
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