Decoupling feldspar dissolution and precipitation rates at near-equilibrium with Si isotope tracers: Implications for modeling silicate weathering-Reference-Cited by-同舟云学术

Decoupling feldspar dissolution and precipitation rates at near-equilibrium with Si isotope tracers: Implications for modeling silicate weathering

Published:2020-02 Issue: Volume:271 Page:132-153
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Zhu Chen^ORCID,Donald Rimstidt J.,Zhang Yilun,Kang Jinting,Schott Jacques,Yuan Honglin

Funder

U.S. NSF

State Key Laboratory of Continental Dynamics

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference84 articles.

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

4. Mineral dissolution kinetics as a function of distance from equilibrium - New experimental results;Arvidson;Chem. Geol.,2010

5. Application of isotopic doping techniques to evaluation of reaction kinetics and fluid/mineral distribution coefficients: An experimental study of calcite at elevated temperatures and pressures;Beck;Chem. Geol.,1992

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