Key Laboratory of Groundwater Resources and Environment, Ministry of Education, Jilin University, Changchun 130021, China.
Key Laboratory of Groundwater Resources and Environment, Ministry of Education, Jilin University, Changchun 130021, China.
Sci Total Environ. 2021 Nov 20;796:149066. doi: 10.1016/j.scitotenv.2021.149066. Epub 2021 Jul 15.
Carbon dioxide (CO) geological storage (CGS) is an effective way for reducing greenhouse emissions. The injection of CO into the deep formation changes the pore pressure and effective stresses in the reservoir, thus leading to changes in stress-dependent porosity and permeability. These changes give feedback to the injection rate, migration, storage amount of CO in the target reservoir. In this study, we focus on the Liujiagou reservoir, one of the first demonstration CGS project in saline aquifers in the Ordos Basin, China. The mathematical model that defines the relationship between the permeability and the injection pressure (or effective stress) was obtained by laboratory experiments. On this basis, the permeability-stress law was successfully integrated into the thermo-hydro-mechanical (THM) coupled simulator TOUGH2Biot to simulate the feedback between the flow and mechanical response. The improved simulator was used to analyze the effects of reservoir mechanical response on CO geological storage efficiency. The modeling results indicated that the mechanical response of the reservoir had little effect on reservoir pore pressure and porosity, but it had a significant effect on reservoir permeability and the migration distance, injection rate, and total storage amount of CO. The maximum increases in the lateral migration distance of CO caused by the reservoir mechanical response reached 13.1% using 5 MPa injection pressure. In addition, the total CO storage amount increased by 11.6% after 5 years of continuous CO injection. Furthermore, when the injection pressure was greater, the reservoir mechanical response had stronger enhancement effects on CGS. Overall, the results suggested that the reservoir mechanical response during CO injection was beneficial for increasing CGS efficiency and emphasized the importance of considering the mechanical response in CGS.
二氧化碳(CO)地质封存(CGS)是减少温室气体排放的有效方法。将 CO 注入深部地层会改变储层中的孔隙压力和有效应力,从而导致与应力相关的孔隙度和渗透率发生变化。这些变化会对注入速率、CO 在目标储层中的迁移和储存量产生反馈。在这项研究中,我们关注的是中国鄂尔多斯盆地咸水含水层中首个 CO 地质封存示范项目之一的刘家沟储层。通过实验室实验获得了定义渗透率与注入压力(或有效应力)之间关系的数学模型。在此基础上,成功地将渗透率-应力规律集成到热-水-力学(THM)耦合模拟器 TOUGH2Biot 中,以模拟流动和机械响应之间的反馈。改进后的模拟器用于分析储层机械响应对 CO 地质封存效率的影响。建模结果表明,储层的机械响应对储层孔隙压力和孔隙度影响不大,但对储层渗透率以及 CO 的迁移距离、注入速率和总储存量有显著影响。储层机械响应引起的 CO 横向迁移距离最大增加了 13.1%,使用 5 MPa 的注入压力。此外,在连续 5 年注入 CO 后,CO 的总储存量增加了 11.6%。此外,当注入压力较大时,储层机械响应对 CGS 的增强效果更强。总体而言,结果表明 CO 注入期间的储层机械响应有利于提高 CGS 效率,并强调了在 CGS 中考虑机械响应的重要性。