International audienceIn addition to isomorphic cation substitutions, smectite layers may present anionic substitutions with fluorine replacing the structural hydroxyl groups and inducing a reduced number of H2O molecules hydrating interlayer cations. The resulting additional versatility of smectite layers could be used to fine-tune the hydrophilicity of pure or intercalated smectite pending a detailed understanding of interlayer water organization. The present article thus reports on the hydration of (fluoro-)hectorite samples exhibiting similar charge density (structural formulae: [Na0.8 nH2O]inter[Mg5.2Li0.8]oct[Si8.0]tetO20(OH,F)4). Water sorption isotherms and PIGE/PIXE analyses allowed constraining the water content over the probed ra...