Mechanical and flow behaviours and their interactions in coalbed geosequestration of CO2

Studying gas transport mechanisms in coal seams is crucial in determining the suitability of coal formations for geosequestration and/or CO2-enhanced coal bed methane recovery (ECBM), estimating CO2 storage capacity and recoverable volume of methane, and predicting the long-term integrity of CO2 storage and possible leakages. Due to the dual porosity nature of coal, CO2 transport is a combination of viscous flow and Fickian diffusion. Moreover, CO2 is adsorbed by the coal which leads to coal swelling which can change the porous structure of coal and consequently affects the gas flow properties of coal, i.e. its permeability. In addition, during CO2 permeation, the coal seam undergoes a change in effective stress due to the pore pressure alteration and this can also change the permeability of the coal seam. In addition, depending on the in situ conditions of the coal seam and the plan of the injection scheme, carbon dioxide can be in a supercritical condition which increases the complexity of the problem. We provide an overview of the recent studies on porous structure of coal, CO2 adsorption onto coal, mechanisms of CO2 transport in coalbeds and their measurement, and hydro-mechanical response of coal to CO2 injection and identify opportunities for future research.