A better understanding of the mobility of the CO2 phase and the sweep within the CH4 hydrate-bearing sediments is required for the success of CO2 storage and concurrent CH4 production. In this work, we investigate the injectivity of CO2 in CH4-hydrate-saturated porous media and the subsequent dissociation of CH4 / CO2 mixed hydrate at the pore level. A total of six pore-scale visualization experiments were performed using a high-pressure water-wetted silicon wafer-based micromodel whose pore network resembles a cross section of sandstone. Liquid CO2 was injected at a constant volumetric rate of 0.2-0.5 ml / hour at a high saturation of CH4 hydrate (SH = 0.81-0.99) at P = 59-69 bar and T = 3.3-4.5°C. The results confirmed the presence of two different hydrate arrangements at the end of the CO2 injection, such that the hydrate phase change and liquid distribution were influenced by the invasion behaviour of the liquid phase and the initial distribution of CH4 hydrate. Invasion of the CO2-rich liquid phase resulted in the formation of massive hydrates without residual liquid saturation. While the CH4 rich liquid phase invaded the hydrates and produced an excess of the liquid phase in the field of view. Later, massive hydrates were dissociated by stepwise depressurization, with multiple dissociation and reformation recorded between the thermodynamic stability pressure of pure CH4 hydrates and pure CO2 hydrates, supported by the presence of the liquid phase. Continuous mobilization of liquid phase and mixing of liquid and gas phases led to localized hydrate reforming below the CH4 hydrate stability pressure. This is the first pore-scale visualization of CO2 injection into CH4-hydrate saturated porous media and
ManuscriptClick here to view linked References demonstrates the feasibility of combining CO2 Injection into CH4 hydrate with stepwise depressurization to produce CH4 gas.