Abstract

Deep geothermal energy sources harvested by circulating fluids in engineered geothermal energy systems can be a solution for diesel-based northern Canadian communities. However, poor knowledge of relevant geology and thermo-hydro-mechanical data introduces significant uncertainty in numerical simulations. Here, a first-order assessment was undertaken following a “what-if” approach to help design an engineered geothermal energy system for each of the uncertain scenarios. Each possibility meets the thermal energy needs of the community, keeping the water losses, the reservoir flow impedance and the thermal drawdown within predefined targets. Additionally, the levelized cost of energy was evaluated using the Monte Carlo method to deal with the uncertainty of the inputs and assess their influence on the output response. Hydraulically stimulated geothermal reservoirs of potential commercial interest were simulated in this work. In fact, the probability of providing heating energy at a lower cost than the business-as-usual scenario with oil furnaces ranges between 8 and 92%. Although the results of this work are speculative and subject to uncertainty, geothermal energy seems a potentially viable alternative solution to help in the energy transition of remote northern communities.

Highlights

  • The results reveal that the hydromechanical properties significantly influence the estimated initial aperture of the fractures (Figure 7)

  • The simulations reveal that the development of hydraulically stimulated geothermal reservoirs is favored in a high temperature, hydraulically conductive and mechanically weak subsurface, i.e., the best-case scenario assumed in this study

  • Geothermal energy off-grid technologies are a potential solution for improving the energetic framework of the 239 Canadian remote northern communities that rely solely on diesel for electricity and space heating

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Summary

Introduction

The first hydraulic stimulation experiments in crystalline rocks were done at Fenton Hill (e.g., [34]) The success of these field experiments opened new opportunities to explore geothermal energy sources in areas that were previously considered unviable (e.g., crystalline rocks with very low permeability). This new concept of recovering the Earth’s heat via a pressurized closed-loop circulation of fluid from the surface through a hydraulically stimulated and confined reservoir several kilometers deep made in crystalline basement rocks marked an important conceptual turning point in the geothermal energy industry

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