Fundamental study on hydraulic fracturing simulation with DEM under high pressure and high temperature condition

H. Ohtani, H. Mikada, J. Takekawa
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Abstract

One of the most attractive topics in geothermal development is the realization of enhanced geothermal systems in ductile zones. Thermal energy extraction from hot dry rock may require hydraulic fracturing through rocks in ductile zones, where rocks are supposed to deform in a ductile way due to the high pressure and high temperature (HPHT) conditions. One of the key factors in its realization is, therefore, to understand mechanical behavior of ductile rocks and hydraulically created fractures under the HPHT conditions, which have not been well investigated in the past. Numerical simulations are widely accepted as the effective approach to understand the mechanism of hydraulic fracturing. Numerical studies taking cooling effects from injected fluid on hydraulic fracturing into consideration have been conducted. Though distinct element methods (DEM) are frequently used to understand brittle failure or ductile deformation mechanism of rock, hydraulic fracturing simulations including both ductile behaviors and cooling effects due to injected fluid in the HPHT environment has not been fully investigated yet. Since the mechanical response to the fluid injection shows drastic changes at the brittle-ductile transitional condition, incorporation of the transitional behavior of granite into DEM is an essential step. In this study, we demonstrated hydraulic fracturing simulations with degradation approaches for the bond properties in DEM, i.e. degradation model and bi-linear approximation model, to replicate semi-brittle or ductile behavior at the HPHT condition. The numerical simulation results showed that results from bi-linear approximation model, which is suitable for replicating ductile behavior of granite, were consistent with laboratory experiment results under the HPHT condition. We can observe the cooling of rock mass due to injected fluid, while a considerable interaction between solid and fluid cannot be observed due to the shortness of injection time.
高压高温条件下基于DEM的水力压裂模拟基础研究
地热开发中最具吸引力的课题之一是在韧性带中实现增强型地热系统。从干热岩石中提取热能可能需要通过延性带的岩石进行水力压裂,因为在高温高压条件下,岩石应该以延性的方式变形。因此,实现这一目标的关键因素之一是了解高温高压条件下韧性岩石和水力裂缝的力学行为,这在过去还没有得到很好的研究。数值模拟作为理解水力压裂机理的有效手段已被广泛接受。考虑注入流体对水力压裂的冷却作用,进行了数值研究。尽管离散元方法(DEM)经常用于理解岩石的脆性破坏或延性变形机制,但包括高温高压环境下注入流体的延性行为和冷却效果在内的水力压裂模拟尚未得到充分研究。由于流体注入的力学响应在脆性-韧性过渡条件下表现出剧烈的变化,因此将花岗岩的过渡行为纳入DEM是必不可少的一步。在这项研究中,我们演示了水力压裂模拟中使用DEM中粘结性能的退化方法,即退化模型和双线性近似模型,以复制高温高压条件下的半脆性或延性行为。数值模拟结果表明,在高温高压条件下,双线性近似模型的结果与室内实验结果一致,该模型适用于模拟花岗岩的延性行为。我们可以观察到注入流体对岩体的冷却作用,但由于注入时间较短,无法观察到固液之间有较大的相互作用。
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