Geothermal & Supercritical
Doublets, direct-use, flash power, EGS, and supercritical.
How long until the cold front reaches the producer? How should the doublet be spaced to protect the resource? Will a high-enthalpy well flash to steam — or go supercritical — and how much power can it deliver?
What Permeon models
- Low-enthalpy brine doublets for district heating / direct-use — thermal-breakthrough timing and the retarded cold front (thermal "protection").
- High-enthalpy water–steam flash through to supercritical (IAPWS-IF97 Region 3, valid beyond the critical point) with implicit steam wells — on CPU and GPU, with MPI scaling.
- Saline supercritical (H₂O–NaCl) for IDDP-class targets: salinity-shifted critical point, halite precipitation and injectivity decline (experimental).
- Enhanced-geothermal (EGS) fractured wells and doublets.
- Cold-reinjection thermal stressing coupled to the geomechanics (THM).
Validation: Validated against common commercial and research codes and analytic thermal-front solutions; the supercritical GPU flash matches the CPU result.