In fracture-dominated reservoirs, studies allude to the spatial variation of fracture surfaces across different scales, and have demonstrated that variation in fracture aperture can lead to flow channeling. For geothermal energy production, the flow-wetted surface area is of particular interest, because it strongly influences the thermal performance of the reservoir. In an enhanced geothermal type system, cold water is circulated through one or more fractures in a hot rock reservoir and fluid collection at one or more producers returns the heated working fluid to ground surface. Therefore, heat is recovered only across the flow-wetted surface area available between injectors and producers. Under channeled flow conditions, reduced flow-wetted surface area can lead to inadequate heat transfer efficiency. In an investigation by Hawkins, et al. (2017), an attempt was made to characterize the spatial distribution of groundwater flow paths and determine the flow-wetted area, the latter then used to predict the thermal performance of the system. Hot water was injected into a cold bedrock 7.6 m below ground surface. As the experiment progressed in time, the temperatures measured were increasingly greater than the predicted temperatures. According to Hawkins, et al. (2018), a possible cause for the deviation could be thermal-mechanical influences. This study sought to determine if accounting for thermal-mechanical influences could explain the differences between the measured and predicted temperatures of the experiment. The system was modeled as a coupled thermo-hydro-mechanical system. The results showed that by using a thermo-hydro-mechanical model, the thermal performance by 6 days (144 hours) was close to the observed data though the profile in the early time was not matched.

Presenter: Rita Okoroafor