Zhai WenBo, Wu Di, Liu XueYing, Xiao XiaoChun, Ding Xin, Miao Feng, Chen XinTong
School of Mechanics and Engineering, Liaoning Technical University, Fuxin, 123000, Liaoning, China.
Liaoning Key Laboratory of Mining Environment and Disaster Mechanics, Liaoning Technical University, Fuxin, Liaoning, China.
Sci Rep. 2024 Dec 28;14(1):30697. doi: 10.1038/s41598-024-78533-w.
This paper first conducted a shale injection CO seepage experiment based on an improved single-vessel pressure pulse attenuation method. The experimental results reveal that the evolution pattern of shale permeability with respect to pore pressure can be divided into before and after phase change. The overall trend is that it first decreases and then increases, which is not a simple exponential form. The exponential fit of the permeability before and after the phase change alone is one-sided. A CO adsorption deformation test was subsequently conducted on shale under the same temperature and gas pressure conditions. The results revealed that with increasing CO pressure, the expansion and deformation of shale first increased but then decreased. The entire deformation process involves three deformation stages: a short compression stage, a slow expansion stage, and a stable deformation stage. The slip effect was corrected by combining adsorption expansion, effective stress, the real gas effect and the dynamic slip factor. The modified permeability model is more consistent with the relationship between permeability and pore pressure.
本文首先基于改进的单容器压力脉冲衰减法进行了页岩注入CO渗流实验。实验结果表明,页岩渗透率随孔隙压力的演化模式可分为相变前后两个阶段。总体趋势是先减小后增大,并非简单的指数形式。单独对相变前后的渗透率进行指数拟合是片面的。随后在相同温度和气体压力条件下对页岩进行了CO吸附变形试验。结果表明,随着CO压力的增加,页岩的膨胀变形先增大后减小。整个变形过程包括三个变形阶段:短暂压缩阶段、缓慢膨胀阶段和稳定变形阶段。通过结合吸附膨胀、有效应力、真实气体效应和动态滑移因子对滑移效应进行了修正。修正后的渗透率模型与渗透率和孔隙压力之间的关系更加吻合。