The DOI matches its Crossref record; 229 of the 229 references it cites were found in a registry or an index.
Kinetics of Mineral Dissolution
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“Sulfuric acid (H 2 SO 4 ) derived from the oxidation of pyrite: FeS 2 + 3.75 O 2 + 3.5 H 2 O ↔ 2 H 2 SO 4 + Fe(OH) 3 (4) also accounts for a portion of the acid that facilitates weathering in the terrestrial environment (~ 5% of silicate dissolution and 10% of carbonate dissolution) (Brantley, 2008;Torres et al., 2014).”
From Evolution of the Global Carbon Cycle and Climate Regulation on Earth (2020) · cites this paper as Brantley, 2008
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Cited by
Sorted by citations
Aiken, G. R., Hsu‐Kim, H., & Ryan, J. N. (2011) · Environmental Science & Technology · doi:10.1021/es103992s · Cited by 947
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Metadata
- Authors
- Brantley, S. L.
- Affiliations
- Pennsylvania State University (US)
- Corresponding author
- Brantley, Susan L.
- ORCID
- Brantley, Susan L.
- Venue
- Kinetics of Water-Rock Interaction
- Publisher
- Springer New York
- Published
- 2008
- Pages
- 151-210
- OpenAlex
- W116578701
- Cited by
- 349
- References
- 229
- Citations by year
- 2026: 6 · 2025: 16 · 2024: 25 · 2023: 34 · 2022: 20 · 2021: 27 · 2020: 19 · 2019: 23 · 2018: 16 · 2017: 17 · 2016: 26 · 2015: 34 · 2014: 16 · 2013: 24 · 2012: 20
- FWCI
- 21.15
- Type
- book chapter
- Language
- en
- Open access
- closed
- Locations
- Springer eBooks (publishedVersion)
- 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 › Geochemistry and Petrology › Groundwater and Isotope Geochemistry
- Keywords
- mineral dissolution kinetics, silicate minerals, carbonate minerals, oxide minerals, weathering, carbon cycle, soil fertility, aquifer porosity, contaminant transport, CO2 sequestration, ore genesis
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