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Chemical kinetics of water‐rock interactions

Lasaga, Antonio C.·1984·Journal of Geophysical Research: Solid Earth

Abstract

The recent literature on the kinetics of water‐rock interactions is reviewed. The data are then extended to provide a quantitative framework for the description of weathering and alteration. The available experimental data on dissolution of silicates verifies quantitatively the usual mineral stability series in sedimentary petrology. The rate of hydration of carbonic acid is shown to be a possible limiting factor in water‐rock interactions. The framework is developed to enable use of laboratory dissolution experimental results and thermodynamics to arrive at a rate law applicable up to equilibrium and therefore applicable to natural systems. The kinetic justification for the significance of a water‐rock ratio is discussed. With a proper treatment of fluid flow, the equations are applied to the weathering profile leading to the development of bauxites from nepheline syenites.

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Metadata

Authors
Lasaga, A. C.
Venue
Journal of Geophysical Research: Solid Earth
Published
1984-06-10
Volume
89
Issue
B6
Pages
4009-4025
ISSN
0148-0227 (ISSN-L)
OpenAlex
W2078916507
Cited by
1,279
References
0
FWCI
15.41
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Chemical kinetics of water‐rock interactions. https://app.cochat.ai/papers/10.1029/jb089ib06p04009
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Lasaga, A. C. (1984). Chemical kinetics of water‐rock interactions. Journal of Geophysical Research: Solid Earth. https://doi.org/10.1029/jb089ib06p04009

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.