3. Thermo-hydro-mechanical#
3.1. 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
3.2. 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