| Energy transition and low-carbon emission reduction are issues that my country has to solve in recent years.Injecting CO2 that causes the greenhouse effect into shale reservoirs can not only increase the production of shale gas,solve the problem of energy transition,but also sequester CO2.Realize environmental benefits in the stratum.In this paper,the Longmaxi Formation shale is used as the research object,and the adsorption kinetics of CH4 and CO2 on shale is carried out under different experimental conditions by volume method.The results show that increasing the pressure will significantly increase the CO2 and CH4 on shale.Adsorption capacity,increasing the temperature will reduce the adsorption capacity of CO2 and CH4 on shale.Based on the experimentally obtained adsorption capacity-time curve,the diffusion coefficient of CO2and CH4 on shale was calculated using a single-hole diffusion model.The diffusion coefficient of CO2 on shale is positively correlated with pressure and temperature,while the diffusion coefficient of CH4 on shale is negatively correlated with pressure and temperature.Compared with the quasi-first-order kinetic model and Bangham model,the quasi-second-order kinetic model can better fit the experimental data.In the rapid adsorption stage,the adsorption rate of CO2 continues to decrease,and the adsorption rate of CH4 first increases and then decreases.In the adsorption equilibrium stage,the adsorption rate of the two gases on shale is zero.Increasing pressure and temperature will reduce the adsorption rate constants of CO2 and CH4 on shale.In order to explore the effect of CO2 huff and puff gas injection on increasing shale gas production and CO2 storage,three CO2 injection pressures of 5MPa,7.5MPa,and10.5MPa were carried out for Yanchang Formation shale,at three temperatures of 305K,307K,and 318K,0min,30min Experimental study of CO2 huff and puff gas injection to displace shale gas under three well-simmering times of,60min.The Coats-Smith two-zone model was used to model the CO2 penetration curve.The results show that the Coats-Smith two-zone model is very sufficient.A good description of the migration mechanism of CO2 and CH4 on shale during competitive adsorption.The increase in CO2 injection pressure mainly increases the mass transfer driving force for CO2 diffusion and adsorption to the shale matrix,increases the CO2 diffusion coefficient,reduces the CH4 diffusion coefficient,and leads to a decrease in the recovery rate of CH4.The retention rate has increased.Therefore,reducing the pressure is beneficial to increase the recovery rate of CH4,and can also increase the recovery rate of pure CH4.As the temperature increases,the recovery rate of CH4 and the storage rate of CO2 increase,but the increase is very small.Therefore,the appropriate experimental temperature should be selected according to the characteristics of the shale reservoir to maximize the benefits.The increase in simmering time accelerates the adsorption and analysis of CO2 and CH4 on shale and shortens the time for CO2 and CH4 to reach adsorption equilibrium on shale.CO2 has different effects on the recovery rate of CH4and the storage rate of CO2 under different conditions.When the injected CO2 is in the gaseous state,as the simmering time increases,the recovery rate of CH4 increases,and the storage rate of CO2 decreases;when CO2 is in the supercritical state In the state,the recovery rate of CH4 and the storage rate of CO2 decrease with the increase of the simmering time. |