Thermo-hydro-mechanical ===================== Formulations: -------------- HH and HH2 modeling: * Pure hydraulics, without thermal, without mechanics * HH: 2 phases, 1 component per phase * HH2: 2 phases, 2 components per phase Two-phase flows in porous media * SUSHI (Scheme Using Stabilization and Hybrid Interfaces), formulation in finite volumes Flows in a crack/propagation under fluid pressure * Joint with hydro-mechanical coupling *Selective integration*_ JHMS Regularization adapted to porous media * Volume deformation gradient modeling to avoid location problems Damage model dedicated to heterogeneous materials * Random distribution of micro-defects (Weibull) D_ PLAN_GRAD_SIGM + ENDO_HETEROGENE * Rock fracturing due to gas injection Laws of behavior -------------------- Mechanics * Cyclic Hujeux law: Multi-mechanism law for sands and clays, earth dikes * Laws of Lagle and Kleine, of viscous Drücker-Prager: viscoplastic laws for rocks (especially argillites); rocks from storage sites Hydraulics * Mualem-Van Genuchten's law: hydrodynamic law of unsaturated soils. Taking into account the disexisting/appearance of phases. Storage site rocks