Mechanisms controlling albite dissolution/precipitation kinetics as a function of chemical affinity: New insights from experiments in 29Si spiked solutions at 150 and 180 °C-Reference-Cited by-同舟云学术

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Mechanisms controlling albite dissolution/precipitation kinetics as a function of chemical affinity: New insights from experiments in 29Si spiked solutions at 150 and 180 °C

Published:2024-06 Issue: Volume:374 Page:284-303
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Schott Jacques,Saldi Giuseppe D.^ORCID,Zhu Chen,Gong Lei,Chen Kaiyun

Funder

Indiana University Bloomington

Centre National de la Recherche Scientifique

National Science Foundation

Publisher

Elsevier BV

Reference81 articles.

1. Thermodynamic and kinetic constraints on reaction rates among minerals and aqueous solutions;Aagard;Am. J. Sci.,1982

2. Assesment of feldspar solubility constants in water in the range 0° to 350°C at vapor saturation pressures;Arnórsson;Am. J. Sci.,1999

3. Mineral dissolution kinetics as a function of distance from equilibrium – new experimental results;Arvidson;Chem. Geol.,2010

4. Compilation of Mineral Dissolution Rates in Kinetics of Water-Rock Interaction;Bandstra,2008

5. Albite dissolution kinetics as a function of distance from equilibrium: implications for natural feldspar weathering;Beig;Geochim. Cosmochim. Acta,2006

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