Cited by 349CO2 Sequestration and Geologic InteractionsGeochemistry and Elemental AnalysisGroundwater and Isotope Geochemistry

Kinetics of Mineral Dissolution

Brantley, Susan L.·2008·Kinetics of Water-Rock Interaction

Integrity signals

Registry

Crossref · 10.1007/978-0-387-73563-4_5

Cites

229 of 229 references verified0 citation errors · 0 not checkable

Statistics

Recomputing p-values needs the paper’s full text.

Claims the paper makes

We couldn’t retrieve this paper’s full text, so its claims and self-check weren’t run. The registry and citation checks still apply.

Claims other papers make about this one

Each is checked against this paper’s own text: does it say what the citing paper says it does?

  • Sulfuric acid from pyrite oxidation accounts for about 5% of silicate dissolution and 10% of carbonate dissolution in terrestrial weathering.

    “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

Cites

Flagged first, then by citations

Cited by

Sorted by citations

Authors
Brantley, S. L.
Affiliations
Pennsylvania State University (US)
Corresponding author
Brantley, Susan L.
Venue
Kinetics of Water-Rock Interaction
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

About these checks

Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.

Statistics and arithmetic are recomputed, not judged.

Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.

What counts as a claim ›How we measure confidence ›How we check this ›

Are you an author, or do you see a problem with this page? Request a review