Liu Jianjun, Li Guang, Zhang Yue
School of Geoscience and Technology, Southwest Petroleum University, Chengdu, China.
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu, China.
PLoS One. 2016 Mar 31;11(3):e0152066. doi: 10.1371/journal.pone.0152066. eCollection 2016.
CO2 flooding of coalbed methane (CO2-ECBM) not only stores CO2 underground and reduces greenhouse gas emissions but also enhances the gas production ratio. This coupled process involves multi-phase fluid flow and coal-rock deformation, as well as processes such as competitive gas adsorption and diffusion from the coal matrix into fractures. A dual-porosity medium that consists of a matrix and fractures was built to simulate the flooding process, and a mathematical model was used to consider the competitive adsorption, diffusion and seepage processes and the interaction between flow and deformation. Due to the effects of the initial pressure and the differences in pressure variation during the production process, permeability changes caused by matrix shrinkage were spatially variable in the reservoir. The maximum value of permeability appeared near the production well, and the degree of rebound decreased with increasing distance from the production well.
二氧化碳驱替煤层气(CO2-ECBM)不仅能将二氧化碳封存于地下并减少温室气体排放,还能提高产气率。这一耦合过程涉及多相流体流动和煤岩变形,以及诸如竞争性气体吸附和从煤基质向裂缝扩散等过程。构建了一个由基质和裂缝组成的双孔隙介质来模拟驱替过程,并使用数学模型来考虑竞争性吸附、扩散和渗流过程以及流动与变形之间的相互作用。由于初始压力的影响以及生产过程中压力变化的差异,基质收缩引起的渗透率变化在储层中呈空间变化。渗透率最大值出现在生产井附近,且回弹程度随与生产井距离的增加而降低。