Occurrence and nature of thermolabile compounds in the Boom Clay kerogen (Oligocene, underground Mol Laboratory, Belgium)
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.
VALVE CLOSURE RESPONSE TO URANIUM EXPOSURE FOR A FRESHWATER BIVALVE (CORBICULA FLUMINEA): QUANTIFICATION OF THE INFLUENCE OF pH
URANIUM COMPLEXATION AND UPTAKE BY A GREEN ALGA IN RELATION TO CHEMICAL SPECIATION: THE IMPORTANCE OF THE FREE URANYL ION
Origins and levels of artificial radionuclides within the Rhône river waters (France) for the last forty years: an analysis of the radioecological sensitivity of river systems.
