The effect of time on the weathering of silicate minerals: why do weathering rates differ in the laboratory and field?
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Silicate dissolution is well known to slow over time as mineral surfaces age; thus, ideal rates quickly become inapplicable.
“At the most fundamental level, silicate dissolution is well known to slow over time as mineral surfaces age; thus, ideal rates quickly become inapplicable. 16-18”
From A framework for understanding efficiency losses of Ocean Alkalinity Enhancement (2026) · cites this paper as [17]
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A framework for understanding efficiency losses of Ocean Alkalinity Enhancement
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- Authors
- White, A. F., & Brantley, S. L.
- Affiliations
- United States Geological Survey (US)
- Pennsylvania State University (US)
- Corresponding author
- White, Art F
- ORCID
- Brantley, Susan L
- Venue
- Chemical Geology
- Publisher
- Elsevier BV
- Published
- 2003-12
- Volume
- 202
- Issue
- 3-4
- Pages
- 479-506
- ISSN
- 0009-2541 (ISSN-L)
- OpenAlex
- W2124781550
- Cited by
- 1,196
- References
- 1
- Citations by year
- 2026: 71 · 2025: 68 · 2024: 68 · 2023: 69 · 2022: 68 · 2021: 51 · 2020: 51 · 2019: 60 · 2018: 63 · 2017: 65 · 2016: 49 · 2015: 66 · 2014: 56 · 2013: 59 · 2012: 63
- FWCI
- 39.36
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Chemical Geology (publishedVersion)
- Topics
- Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil and Environmental Studies
- 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
- chemical weathering rates, plagioclase, kaolinization, K-feldspar, hornblende, biotite, column experiments, weathering profiles, secondary precipitation, BET surface area
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