Hydraulic fracturing in hot dry rock (HDR) geothermal reservoirs is strongly influenced by thermal stresses arising from the temperature difference between the injected fluid and the surrounding rock. This study develops a three-dimensional extended finite element (XFEM) model to analyze the dominant early-stage mechanism of wellbore wall cooling and its effect on fracture initiation and propagation. The model captures the coupled thermo-mechanical behavior of the rock and evaluates how thermal contraction at the wellbore alters breakdown and propagation pressures. Sensitivity analyses show that increasing the temperature difference between the injected fluid and the rock significantly reduces the required fracturing pressure, while the magnitude of this effect depends on the in-situ stress field, thermal expansion coefficient, and Young’s modulus. In contrast, variations in thermal conductivity and permeability have negligible impact on the pressure response. The results confirm that wellbore cooling governs the thermal stress contribution during the early stages of fracturing, while fluid-flow-induced thermal gradients become more relevant at later stages. Overall, the findings improve understanding of thermo-mechanical interactions in HDR fracturing and can assist engineers in predicting fracturing pressures and optimizing stimulation strategies in geothermal energy development.
扫码关注我们
求助内容:
应助结果提醒方式:
