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Global silicate weathering and CO2 consumption rates deduced from the chemistry of large rivers
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“This is several orders of magnitude slower than dissolution rates for hydrated cement minerals determined through laboratory experiments (10 -8.0 mol of Ca cm -2 s -1 ) 17 but is 2 orders of magnitude faster than the greatest weathering rates for natural catchments (e.g., a global average of 24 t km -2 year -1 , 33 or 100s t km -2 year -1 for tropical volcanic arcs).39,40”
From Rapid Removal of Atmospheric CO2 by Urban Soils (2015) · cites this paper as [39]
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Metadata
- Authors
- Gaillardet, J., Dupré, B., Louvat, P., & Allègre, C. J.
- Affiliations
- Centre National de la Recherche Scientifique (FR)
- Corresponding author
- Gaillardet, J.
- Venue
- Chemical Geology
- Publisher
- Elsevier BV
- Published
- 1999-07
- Volume
- 159
- Issue
- 1-4
- Pages
- 3-30
- ISSN
- 0009-2541 (ISSN-L)
- OpenAlex
- W2008587428
- Cited by
- 3,334
- References
- 62
- Citations by year
- 2026: 293 · 2025: 331 · 2024: 277 · 2023: 273 · 2022: 249 · 2021: 215 · 2020: 202 · 2019: 173 · 2018: 146 · 2017: 129 · 2016: 107 · 2015: 112 · 2014: 124 · 2013: 112 · 2012: 91
- FWCI
- 20.94
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Chemical Geology (publishedVersion)
- Topics
- 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
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Keywords
- silicate weathering, chemical weathering rates, CO2 consumption, river water chemistry, inverse modeling, basalt weathering, oceanic islands, volcanic arc, lithology, carbonate weathering, evaporite weathering, atmospheric inputs
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