Understanding the wetting behaviors of water on quartz surfaces and underlying mechanisms when immersed in varying gas environments is crucial for the efficient implementation of geological engineering projects, such as H2gas geo-storage, natural gas production, and greenhouse gas geo-sequestration.In the present work, classical molecular dynamic (MD) simulations are applied to investigate the deionized (DI) water and brine (with a salinity of ∼1.5 M and ∼3.5 M) wettability of quartz surfaces and interfacial properties in the presence of various gas species (i.e., H2, CH4, and CO2) under a typical geological condition (333K and 20 MPa). The inherent mechanisms regulating surface wettability are revealed by Young’s equation and interaction energy analysis. Thanks to the strong electrostatic interaction, water forms several adsorption layers on quartz surfaces, whereas gas molecules are mainly adsorbed on the region where the water is not accessible through van der Waals interaction. The presence of salt ions has negligible effects on water and gas distributions as they tend to be depleted from the surface area. When immersed in varying gas species, the contact angle (CA) of water on quartz follows an order of CO2 > CH4 > H2due to the faster decay in gas–solid interaction compared with gas–water interaction. Increasing salt ions is generally unfavorable for the spreading of water on quartz surfaces regardless of gas types resulting in a larger CA value, which is primarily attributed to the augmented gas–water interfacial tension. This study provides important insights into the wettability behaviors of water on quartz surfaces under varying gas conditions and deepens the understanding of the molecular origin of wetting characteristics on quartz surfaces, which is beneficial for explaining relevant phenomena and leading engineering practice.
Read full abstract