The effect of CaCl2H2O brines on the dehydration of Ca-exchanged montmorillonite (SWy-1) at elevated temperatures and pressures

Author:

Wang Shijie,Koster van Groos A.F.,Guggenheim Stephen

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference33 articles.

1. Transmission and analytical electron microscopy of the smectite-to illite transition;Ahn;Clays and Clay Minerals,1986

2. Fugacity, activity and the equilibrium constant;Anderson,1977

3. Hydration-phase diagram and friction of montmorillonite under laboratory and geologic conditions, with implications for shale compaction, slope stability, and strength of fault gouge;Bird;Tectonophysics,1984

4. Diagenesis of Gulf Coast clay sediments and its possible relation to petroleum migration;Burst;AAPG Bull.,1969

5. Hydration states of smectite in NaCI brine at elevated pressures and temperatures;Colten;Clays and Clay Minerals,1986

Cited by 3 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献

1. Stability of Ca-montmorillonite hydrates: A computer simulation study;The Journal of Chemical Physics;2005-11

2. Calcium Chloride;Handbook of Lithium and Natural Calcium Chloride;2004

3. Le concept d'eau ice-like: hydratation-déshydratation des sels, hydroxydes, zeolites, argiles et matières organiques vivantes ou inertes;Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science;1999-09

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