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Research of fracture initiation and propagation in HDR fracturing under thermal stress from meso-damage perspective

机译:从细观损伤的角度研究热应力作用下HDR压裂的裂纹萌生与扩展

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By HDR (hot dry rock) fracturing the deep buried geothermal energy can be efficiently extracted from the established EGS (enhanced geothermal system). While the fracture initiation and propagation is subjected to the interaction of cryogenic induced thermal stress and liquid pressure. Based on the mesodamage mechanics, elastic thermodynamics and Biot seepage mechanics, a mesoscopic thermo-hydromechanical-damage coupling model (THM-damage) is proposed to analyze the fracturing stimulation in HDR Firstly, the mathematical model and numerical implementation method is validated by high temperature granite fracturing experiments. Secondly, the action mechanism of thermal stress in hydraulic fracturing of HDR is discussed. Thirdly, the evolution of multiple physical fields during the initiation and propagation of HDR fracturing is researched. Finally, the effects of various parameters on HDR fracturing process are also studied. The results indicate that when the rock temperature exceeds 200 degrees C the fracture network can be formed by hydraulic fracturing, which extends along the direction perpendicular to the minimum in-situ stress. Increasing rock temperature can reduce fracture initiation pressure and rock failure pressure. The heat transfer coefficient between fracturing fluid and rock and the rock Young's modulus have influence on the fracture morphology during HDR fracturing under thermal stress. (C) 2019 Elsevier Ltd. All rights reserved.
机译:通过HDR(热干岩石)破裂,可以从已建立的EGS(增强的地热系统)中有效地提取深埋地热能。裂缝的产生和扩展受到低温引起的热应力和液体压力的相互作用。基于介观损伤力学,弹性热力学和Biot渗流力学,提出了介观的热-水-机械-损伤耦合模型(THM-damage)来分析HDR中的压裂增产。首先,通过高温验证了数学模型和数值实现方法花岗岩压裂实验。其次,探讨了HDR水力压裂中热应力的作用机理。第三,研究了HDR压裂发生和传播过程中多个物理场的演化。最后,研究了各种参数对HDR压裂过程的影响。结果表明,当岩石温度超过200摄氏度时,可通过水力压裂形成裂缝网络,该裂缝网络沿垂直于最小现场应力的方向延伸。升高岩石温度可以降低裂缝开始压力和岩石破坏压力。压裂液与岩石之间的传热系数以及岩石的杨氏模量对热应力作用下HDR压裂过程中的断裂形态有影响。 (C)2019 Elsevier Ltd.保留所有权利。

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