Seamless Integration of Deep Geothermal Heat into 3rd and 4th Generation District Heating Networks – The Durham (UK) Cogeneration Demonstrator

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.

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Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2025-11-19
DOI
https://doi.org/10.5281/zenodo.18312741
Primary Topic
Geothermal Energy Systems and Applications
Type
article
Field-Weighted Citation Impact
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article

Seamless Integration of Deep Geothermal Heat into 3rd and 4th Generation District Heating Networks – The Durham (UK) Cogeneration Demonstrator

T. Lines, S. McDonald, Z. Moss
Zenodo (CERN European Organization for Nuclear Research)
Geothermal Energy Systems and Applications
article

Seamless Integration of Deep Geothermal Heat into 3rd and 4th Generation District Heating Networks – The Durham (UK) Cogeneration Demonstrator

T. Lines, S. McDonald, Z. Moss
article en

Abstract

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.

Zenodo (CERN European Organization for Nuclear Research)
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Geothermal Energy Systems and Applications
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