Experimental and molecular investigation of water adsorption controls in marine and lacustrine shale reservoirs

The restriction of hydrocarbon migration within shale reservoirs by pre-adsorbed water necessitates an inves-tigation into water adsorption control mechanisms within shales. In this study, water vapor adsorption isotherms obtained from marine and lacustrine shale samples along with isotherms from their organic matter and exper-imentally verified kerogen molecular models were used to evaluate water adsorption mechanisms, with simu-lated wet kerogen-quartz nanocomposites. Furthermore, these were also used to investigate organic matter -inorganic interaction controls on water adsorption. Pore size distribution (PSD) controls on water distribution in organic matter were obtained via water vapor adsorption and low-pressure nitrogen adsorption analysis, along with small angle neutron scattering (SANS) analysis. The results reveal water adsorption is linked to changes in mesopore volume within organic matter and porosity in kerogen models. PSD obtained from the shales only reveal mesopore controls at high RH, with water adsorption mainly controlled by oxygen functional groups in organic matter pores and swelling clays. Inorganic controls on water adsorption are also observed in adsorbed water not tightly bound to the shale surface due to a high montmorillonite content in clay interlayers, and organic matter interaction with quartz with a negative relationship between the adsorbed water and the quartz content. Collectively, these findings indicate that CO2 migration in shale reservoirs could be inhibited by water that is distributed in potential CO2 adsorption sites within organic matter pores and montmorillonite.

Automated summary

The study investigates the mechanisms of water adsorption within shales and its impact on CO2 migration in shale reservoirs by analyzing water vapor adsorption isotherms from shale samples and organic matter models. The results suggest that water adsorption is controlled by changes in mesopore volume within organic matter and by the presence of montmorillonite, and it could inhibit CO2 migration in shale reservoirs.