Illite dissolution kinetics from 100 to 280 °C and pH 3 to 9-Reference-Cited by-同舟云学术

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Illite dissolution kinetics from 100 to 280 °C and pH 3 to 9

Published:2017-07 Issue: Volume:209 Page:9-23
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Smith Megan M.,Dai Zurong,Carroll Susan A.

Funder

U.S. Department of Energy (DOE), Office of Energy Efficiency and Renewable Energy (EERE), Geothermal Technologies Office

U.S. Department of Energy by Lawrence Livermore National Laboratory

LLNL-JRNL

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference49 articles.

1. Illite equilibria in solutions: III. A re-interpretation of the data of Sass et al. (1987);Aja;Geochim. Cosmochim. Acta,1991

2. Basal plane reactivity of phyllosilicates studied in situ by hydrothermal atomic force microscopy (HAFM);Aldushin;Geochim. Cosmochim. Acta,2006

3. The combined effect of pH and temperature on smectite dissolution rate under acidic conditions;Amran;Geochim. Cosmochim. Acta,2005

4. Kaolinite and smectite dissolution rate in high molar KOH solutions at 35 and 80°C;Bauer;Appl. Geochem.,1998

5. Evaluation of mineral reactive surface area estimates for prediction of reactivity of a multi-mineral sediment;Beckingham;Geochim. et Cosmochim. Acta,2016

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