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Enhanced Geothermal Systems (EGS) in hot dry rock (HDR) often require hydraulic stimulation to create permeable flow paths. In naturally fractured reservoirs, hydraulic fractures are strongly guided by pre-existing fractures, shaping connectivity and controlling post-stimulation fluid flow and heat transfer. This study investigates the influence of hydraulic-fracturing parameters on thermal recovery in Single-Well Enhanced Geothermal Systems (SEGS) with natural fractures. A two-dimensional hydraulic-fracturing model is developed using the finite element method (FEM) with zero-thickness cohesive elements to simulate fracture initiation and propagation under the influence of natural fractures. The resulting fracture geometries are embedded into a coupled thermo-hydro-mechanical (THM) model to simulate long-term heat extraction. Parametric analyses include fracturing cluster spacing, number of clusters, injection rate, and natural fracture orientation. Results show that cluster spacing affects both fracture geometry and thermal-front evolution: larger spacing promotes longer fractures but may reduce cold-front coverage near the production zone. Natural fracture orientation dominates stimulation effectiveness: larger intersection angles enhance cross-connected networks, increase fluid-rock contact, and improve both heat extraction rate and cumulative production. Increasing the number of clusters shortens individual fractures and intensifies preferential flow along pre-existing fractures, reducing long-term recovery. Higher injection rates enhance fracture propagation and network complexity, enlarging the effective heat-exchange area and strengthening convective heat transfer. By explicitly linking stimulation-induced fracture geometry to subsequent THM heat extraction, this study provides quantitative guidance for optimizing hydraulic-fracturing design in SEGS development.
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Su et al. (2026) studied this question.
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