Na+ and HTO diffusion in compacted bentonite: Effect of surface chemistry and related texture

Author:

Melkior T.,Gaucher E.C.,Brouard C.,Yahiaoui S.,Thoby D.,Clinard Ch.,Ferrage E.,Guyonnet D.,Tournassat C.,Coelho D.

Publisher

Elsevier BV

Subject

Water Science and Technology

Reference55 articles.

1. Andra, 2005. Dossier 2005, Argile – Evolution phénoménologique du stockage géologique. In Andra (France) (Ed.), Collection «Les rapports», pp. 253.

2. Mechanism of adsorption and desorption of water vapour by homoionic montmorillonites: 2. The Li+, Na+, K+, Rb+ and Cs+ exchanged forms;Bérend;Clays and Clay Minerals,1995

3. Evolution of the microstructure of interstratified Ca-saturated clays during dehydration: SAXS and HRTEM analysis;Ben Rhaiem;Clay Minerals,1998

4. Bourg, I.C., 2004. Tracer diffusion of water and inorganic ions in compacted saturated sodium bentonite. PhD Thesis, University of California, Berkeley.

5. Mechanism of adsorption and desorption of water vapour by homoionic montmorillonite: 3. the Mg2+, Ca2+, Sr2+ and Ba2+ exchanged forms;Cases;Clays and Clay Minerals,1997

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