Litcius/Paper detail

Numerical Analysis of Enhanced Conductive Deep Borehole Heat Exchangers

Théo Renaud, Lehua Pan, Hannah Rose Doran, Gioia Falcone, Patrick G. Verdin

2021Sustainability19 citationsDOIOpen Access PDF

Abstract

Geothermal energy is a reliable and mature energy source, but it represents less than 1% of the total renewable energy mix. While the enhanced geothermal system (EGS) concept faces technical validation challenges and suffers from public acceptance issues, the development of unconventional deep-well designs can help to improve their efficiency and reliability. Modelling single-EGS-well designs is key to assessing their long-term thermal performances, particularly in unconventional geological settings. Numerical results obtained with the T2WELL/EOS1 code have been validated with available experimental data from a deep borehole heat exchanger (DBHE), where a temperature of 358 ∘C has been measured at a depth of 1962 m. Based on a calibrated model, the thermal performances of two enhanced thermal conductive DBHEs with graphite were compared for high geothermal gradients. The analysis highlights the potential recovery of a variable fraction of vapour. Graphite used along the well appears to be the most suitable solution to enhance the thermal output by 5 to 8% when compared to conventional wells. The theoretical implementation of such well in the Newberry volcano field was investigated with a single and doublet DBHE. The findings provide a robust methodology to assess alternative engineering solutions to current geothermal practices.

Topics & Concepts

Geothermal gradientBoreholeGeothermal energyHeat exchangerPetroleum engineeringRenewable energyThermalGeothermal heatingElectrical conductorEnvironmental scienceReliability (semiconductor)Thermal energyNuclear engineeringProcess engineeringGeologyMechanical engineeringEngineeringGeotechnical engineeringMeteorologyGeophysicsThermodynamicsElectrical engineeringPower (physics)PhysicsGeothermal Energy Systems and ApplicationsCO2 Sequestration and Geologic InteractionsSoil and Unsaturated Flow