Hydrogeological investigations in a low permeability claystone formation: The Mont Terri Rock Laboratory
Diffusion as the main process for mass transport in very low water content argillites: 2. Fluid flow and mass transport modeling.
Diffusion as the main process for mass transport in very low water content argillites: 1. Chloride as a natural tracer for mass transport—Diffusion coefficient and concentration measurements in interstitial water.
Rapport final COLOSS (Partie 1) : Principaux résultats sur les activités expérimentales et analytiques.
