The interaction behaviors between the hydraulic fracture and natural fracture in hot dry rock

IF 4.6 0 ENERGY & FUELS Geoenergy Science and Engineering Pub Date : 2025-04-01 Epub Date: 2025-01-27 DOI:10.1016/j.geoen.2025.213731
Zixiao Xie , Zhongwei Huang , Zhaowei Sun , Gensheng Li , Xiaoguang Wu , Xu Zhang , Rui Yang , Tengda Long , Wenchao Zou , Yaoyao Sun , Xinyu Qin , Dawei Zhang
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Abstract

Hydraulic fracturing is a prerequisite for efficiently extracting heat from hot dry rock (HDR), which is expected to create complex and inter-connected fracture networks between injection and production wells. Natural fractures are widely distributed within HDR and would prominently affect the propagation of hydraulic fractures. However, little work has been done utilizing granite specimens to investigate the interactive role between natural fractures and artificial fractures under the influence of thermal stress. We hereby performed high-temperature hydraulic fracturing tests on granite outcrops embedded with pre-existing natural fractures to reveal the fracture interaction behaviors. Consequently, the fracture interaction modes for guiding the generation of complex fracture networks were established. The findings indicate that a greater temperature differential between the injection fluid and the rock promotes the stimulation of natural fractures, attributable to the combined effects of thermal stress and fluid pressure exerted on the fracture interface. As the initial rock temperature rose to 180 °C, the activation of the natural fractures was likely to occur even under a relatively large injection rate and horizontal stress difference ratio, which unfavored the opening of the natural fracture. Additionally, with the increment of the rock temperature, the fracture conductivity of the generated fracture network rises accordingly. The average fracture conductivity of granite under 180 °C is around 5 times and 1.3 times higher than that of those under 25 °C and 100 °C, respectively. Furthermore, the reactivation of the natural fracture enlarges both the volume and surface area of the fracture networks in comparison to the crossing-only pattern, and this could be further enhanced as the hydraulic fracture propagated through the natural fractures afterward. The findings are expected to provide a comprehensive insight into the hydraulic fracturing of HDR with natural fractures.
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干热岩中水力裂缝与天然裂缝的相互作用行为
水力压裂是有效地从热干岩(HDR)中提取热量的先决条件,这将在注入井和生产井之间形成复杂且相互连接的裂缝网络。天然裂缝在HDR内分布广泛,对水力裂缝的扩展影响显著。然而,利用花岗岩试样研究热应力作用下天然裂缝与人工裂缝之间的相互作用却很少。为此,我们对嵌有天然裂缝的花岗岩露头进行了高温水力压裂试验,以揭示裂缝的相互作用行为。建立了指导复杂裂缝网络生成的裂缝相互作用模式。研究结果表明,由于热应力和施加在裂缝界面上的流体压力的共同作用,注入流体与岩石之间的温差越大,促进了天然裂缝的增产。当岩石初始温度升至180℃时,即使在较大的注入速率和水平应力差比下,天然裂缝也有可能被激活,不利于天然裂缝的开启。此外,随着岩石温度的升高,生成的裂缝网络的裂缝导流能力也相应升高。花岗岩在180℃下的平均断裂导电性分别是25℃和100℃下的5倍和1.3倍左右。此外,与单纯的交叉模式相比,天然裂缝的重新激活扩大了裂缝网络的体积和表面积,并且随着水力裂缝随后通过天然裂缝扩展,这一点可能会进一步增强。该研究结果有望为HDR天然裂缝的水力压裂提供全面的见解。
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