Thermomechanical coupling seepage in fractured shale under stimulation of supercritical carbon dioxide

Guojun Liu, Delei Shang, Peng Chu, Yuan Zhao, Jun Lu, Jianhua Li
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Abstract

As a waterless fracturing fluids for gas shale stimulation with low viscosity and strong diffusibility, supercritical CO2 is promising than the water by avoiding the clay hydration expansion and reducing reservoir damage. The permeability evolution influenced by the changes of the temperature and stress is the key to gas extraction in deep buried shale reservoirs. Thus, the study focuses on the coupling influence of effective stress, temperature, and CO2 adsorption expansion effects on the seepage characteristics of Silurian Longmaxi shale fractured by supercritical CO2. The results show that when the gas pressure is 1–3 MPa, the permeability decreases significantly with the increase in gas pressure, and the Klinkenberg effects plays a predominant role at this stage. When the gas pressure is 3–5 MPa, the permeability increases with the increase in gas pressure, and the influence of effective stress on permeability is dominant. The permeability decreases exponentially with the increase in effective stress. The permeability of shale after the adsorption of CO2 gas is significantly lower than that of before adsorption; the permeability decreases with the increase in temperature at 305.15 K–321.15 K, and with the increase in temperature, the permeability sensitivity to the temperature decreases. The permeability is closely related to supercritical CO2 injection pressure and volume stress; when the injection pressure of supercritical CO2 is constant, the permeability decreases with the increase in volume stress. The results can be used for the dynamic prediction of reservoir permeability and gas extraction in CO2-enhanced shale gas development.
超临界二氧化碳刺激下压裂页岩中的热力学耦合渗流
超临界二氧化碳作为一种用于页岩气开采的无水压裂液,具有粘度低、扩散性强等特点,与水相比,具有避免粘土水化膨胀、减少储层损害等优点。受温度和应力变化影响的渗透率演化是深埋页岩储层天然气开采的关键。因此,本研究重点探讨了有效应力、温度和二氧化碳吸附膨胀效应对超临界二氧化碳压裂志留系龙马溪页岩渗流特征的耦合影响。结果表明,当气体压力为 1-3 MPa 时,渗透率随气体压力的增加而显著降低,此时克林肯贝格效应起主导作用。当气体压力为 3-5 MPa 时,渗透率随气体压力的增加而增加,有效应力对渗透率的影响占主导地位。随着有效应力的增加,渗透率呈指数下降。吸附 CO2 气体后的页岩渗透率明显低于吸附前;在 305.15 K-321.15 K 温度范围内,渗透率随温度的升高而降低,且随着温度的升高,渗透率对温度的敏感性降低。渗透率与超临界二氧化碳注入压力和体积应力密切相关;当超临界二氧化碳注入压力恒定时,渗透率随体积应力的增加而降低。研究结果可用于 CO2 增强页岩气开发中储层渗透率和采气量的动态预测。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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