ISSN 1003-8035 CN 11-2852/P

    CO2流体注入热效应对断层活化影响分析

    Study on fault activation affected by thermal effects of CO2 fluid injection

    • 摘要: 为探究CO2注入高温储层所引发的热效应(由温度场扰动产生的热应力)对断层活化的影响,以内蒙古某矿地下800 m处地层为研究对象,采用数值模拟方法,构建了考虑注入温度影响的二维热-流-固耦合损伤模型。通过设定CO2流体注入温度分别为35 °C、45 °C、55 °C三种工况,系统分析得到了储层渗透率、断层垂向位移以及孔隙压力变化规律并综合采用断层剪切滑移趋势、安全系数及库伦应力参数评估了断层稳定性。研究结果表明:注入温度从35 °C提升至55 °C,注入50 d时CO2羽流最大水平径向距离增加约14%,封存过程中断层区孔隙压力峰值降低约16%,当注入温度达到55 °C时,热效应产生的稳定作用占主导,能有效抑制断层活化。在CO2地质封存工程中充分考虑注入流体热效应,对弱化流体注入诱发的断层响应、保障封存安全具有重要指导意义。

       

      Abstract: To investigate the impact of thermal effects (thermal stress caused by temperature field disturbances) induced by CO2 injection into high-temperature reservoirs on fault activation, a geological formation located 800 meters underground in a mine in Inner Mongolia was taken as the research object. A two-dimensional thermo-hydro-mechanical (THM) coupled damage model considering injection temperature is established by numerical simulation. Three cases with CO2 injection temperatures of 35 °C, 45 °C, and 55 °C were set to systematically analyze the variation laws of reservoir permeability, fault vertical displacement and pore pressure. Fault stability was comprehensively evaluated using fault shear slip tendency, safety factor and Coulomb stress parameters. The results show that when the injection temperature increases from 35 °C to 55 °C, the maximum horizontal radial distance of the CO2 plume increases by about 14% after 50 days of injection, and the peak pore pressure in the fault zone decreases by about 16% during sequestration. When the injection temperature reaches 55 °C, the stabilizing effect generated by thermal effects is dominant, which can effectively inhibit fault activation. Fully considering the thermal effects of injected fluid in CO2 geological sequestration projects is of great guiding significance for weakening the fault response induced by fluid injection and ensuring sequestration safety.

       

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