Abstract
Sequestration of carbon dioxide in deep-sea sediments has been proposed for the long-term storage of anthropogenic CO(2) that can take advantage of the current offshore infrastructure. It benefits from the negative buoyancy effect and hydrate formation under conditions of high pressure and low temperature. However, the multiphysics process of injection and postinjection fate of CO(2) and the feasibility of subseabed disposal of CO(2) under different geological and operational conditions have not been well studied. With a detailed study of the coupled processes, we investigate whether storing CO(2) into deep-sea sediments is viable, efficient, and secure over the long term. We also study the evolution of multiphase and multicomponent flow and the impact of hydrate formation on storage efficiency. The results show that low buoyancy and high viscosity slow down the ascending plume and the forming of the hydrate cap effectively reduces permeability and finally becomes an impermeable seal, thus limiting the movement of CO(2) toward the seafloor. We identify different flow patterns at varied time scales by analyzing the mass distribution of CO(2) in different phases over time. We observe the formation of a fluid inclusion, which mainly consists of liquid CO(2) and is encapsulated by an impermeable hydrate film in the diffusion-dominated stage. The trapped liquid CO(2) and CO(2) hydrate finally dissolve into the pore water through diffusion of the CO(2) component, resulting in permanent storage. We perform sensitivity analyses on storage efficiency under variable geological and operational conditions. We find that under a deep-sea setting, CO(2) sequestration in intact marine sediments is generally safe and permanent.