The Durham Geothermal Cogeneration Project targets the radiogenic Weardale Granite and overlying sediments along the Sharnberry–Deerness fault in northeast England. A geothermal gradient of ~32–38 °C/km yields production temperatures of ~210–250°C at ~6.5 km (and ~180–210°C at 5.5 km), well above the 85°C required for current third-generation district heating and technically suitable for fourth-generation operation as customer-side return temperatures are reduced.A four-gate phased development strategy mitigates resource and delivery risk while maximising flexibility. Gate 1 drills a ~2.5 km slim-hole to evaluate fault transmissivity and temperature for comparison with the extremely high artesian flowrates observed in the offset Eastgate #1 well. If artesian behaviour, high fault transmissivity and/or sufficient geothermal gradient are confirmed, Gate 2 advances to a ~6.5 km deep full-scale well with a ~500 m lateral. A successful outcome (≥210°C, ~75 kg/s) enables a seven-lateral fault-flow development (four producers, three injectors) yielding ~39 MWₜ and up to ~40 MWₑ via an Organic Rankine Cycle (ORC). If transmissivity is lower than this, trial stimulation for an Enhanced Geothermal System (EGS) is undertaken. If that is unsuccessful, Gate 3 investigates natural transmissivity and EGS fallbacks at 5.5 km vertical depth, and if not successful, Gate 4 investigates natural transmissivity and EGS in 4.5 km sedimentary rock, which still yields sufficient power generation to meet for parasitic losses but requires higher heat tariffs. Gates 2-4 reuse the existing wellbore, mitigating risk while preserving delivery of the ~39 MWₜ base case.Surface infrastructure comprises a 16.9 km city-wide heat network delivering 101 GWt·h/year to anchor loads including Durham University, the hospital, and civic buildings (achieving ~5.95 MWt·h /m linear heat density). A central energy centre incorporates twin heat exchangers, 900 m³ of thermal storage, SCADA controls, and variable-speed pumps. The high-enthalpy resource enables flexible operation between cogeneration and heat-only modes, with electricity revenues cross-subsidising near-zero heat input prices (£0.01/kWₜ·h), supporting affordable network expansion into lower-density zones. Built-in geothermal redundancy—single-well direct-heat fallback and sustained production under temporary injector outages via siphon effects—avoids reliance on fossil backup or high-cost alternatives, ensuring a resilient, low-carbon supply. A dedicated high-temperature branch (≈100°C) can also meet specialist institutional loads such as hospital sterilisation.
Lines et al. (Wed,) studied this question.