IlkerFer andPeterM.Haugan DissolutionfromaliquidCO lakedisposedinthedeepocean

The rate of dissolution of CO 2 from a liquid CO 2 source to the overlying deep-ocean water is retarded when a thin hydrate film is present over the interface.. This mechanism is

The dissolution kinetics and near field dynamics of the ascending particles and the subsequent peeling of the dense, CO 2 -enriched plume water have been simulated by extending

The interface between the liquid CO 2 lake and the hydrate film, as well as the one between the dense, CO 2 -enriched seawater plume and the ambient water may undergo various

The model can be used to study the dynamics of the interface between liquid CO 2 and seawater in the deep ocean, including the evolution of the hydrate layer.. If restricted

By measuring the relative concentrations of CO, CO 2 , and particulate matter in the smoke plume, a partitioning of the mass of carbon between those can be established, and

It was found that the injection of CO 2 in hydrate bearing sandstone could result in CO 2 sequestration either by the formation of additional hydrate with the excess water or

In this paper we describe the controlled formation of a plume of CO 2 rich water at great depth by forcing seawater flow over the liquid CO 2 surfaceb. We present the results

The interface between the liquid CO 2 lake and the hydrate film, as well as that between the dense, CO 2 -enriched seawater plume and ambient water, could undergo various types