A 3D Coupled Thermal-Hydraulic-Mechanical THM Model Using EDFM and XFEM for Hydraulic-Fracture-Dominated Geothermal Reservoirs

Xiangyu Yu, Cong Wang, Xia Yan, Shihao Wang, Lei Wang, P. Winterfeld, Yushu Wu
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引用次数: 1

Abstract

Enhanced Geothermal Systems (EGS) are those geothermal reservoirs artificially fractured to create paths for injected low-temperature fluid which is then heated up along the flow path until production for electricity generation. This heat recovery involves three tightly coupled processes: thermal, hydraulic and mechanical which interacts with each other and in turn affects the energy production. The local temperature field would be disturbed by injected fuild, resulting in thermal/poroelastic responses near the hydraulic fractured area which are the dominant factors of fluid flow. In this paper, the three-dimensional (3D) Embedded Discrete Fracture Model (EDFM) was adopted to describe the geometry of the fracture and simulate fluid flow and heat transfer between fractures and the matrix, while mechanics, including displacement of the strong discontinuity (fractures), was solved by the 3D eXtended Finite Element Method (XFEM). With the capability of modeling fractures of arbitrary shapes within a 3D reservoir domain using 3D EDFM-XFEM, a coupled THM model was developed based on the unconditionally stable fixed-stress split sequential-implicit method, where the fluid flow/heat transfer module and mechanics module are solved iteratively until convergence within a time step. Fluid flow/heat transfer and XFEM with internal/external tractions are both validated by comparison with existing simulators. We conducted simulations for two synthetic geothermal reservoir heat recovery cases to investigate the effects of the injection temperature and boundary traction condition on the production temperature and fracture deformation. The results indicate that the fracture aperture and permeability is sensitive to temperature variation and hence impacts the production rate/temperature. Thermal strain might be the dominant factor of rock deformation, especially in the shallow depth where geostress is at a low level.
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基于EDFM和XFEM的水力裂缝型地热储层热-水力-力学三维耦合THM模型
增强型地热系统(EGS)是指对地热储层进行人工压裂,为注入的低温流体创造通道,然后沿着流动路径加热,直到生产用于发电。这种热回收涉及三个紧密耦合的过程:热、水力和机械,它们相互作用,进而影响能源生产。注入的流体会干扰局部温度场,在水力压裂区附近产生热/孔弹性响应,这是流体流动的主导因素。本文采用三维(3D)嵌入式离散裂缝模型(EDFM)描述裂缝的几何形状,模拟裂缝与基体之间的流体流动和传热,采用三维扩展有限元法(XFEM)求解强不连续(裂缝)的位移等力学问题。利用三维eddm - xfem对三维储层区域内任意形状裂缝的建模能力,建立了基于无条件稳定定应力分裂顺序隐式方法的耦合THM模型,其中流体流动/传热模块和力学模块迭代求解,直到在一个时间步长内收敛。通过与现有仿真器的比较,验证了流体流动/传热和具有内/外牵引力的XFEM。通过对两个合成地热储层热采实例的模拟,研究了注入温度和边界牵引条件对生产温度和裂缝变形的影响。结果表明,裂缝孔径和渗透率对温度变化非常敏感,从而影响产量/温度。热应变可能是岩石变形的主导因素,特别是在地应力较低的浅层深度。
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