The
oceanic sequestration has immense potential to sequestrate
giga tonnes of CO2 in a subsea environment primarily in
the hydrate form. The seafloor and upper zone of subsea sediments
are primarily clay-dominated loosely bound sediments. Under these
subsea conditions, CO2 will be in the liquid state during
sequestration. Rheology of CO2 hydrate formation and dissociation
in loosely bound clay sediments is important to infer hydrate stability
and impact on possible subsidence during hydrate dissociation, especially
in slopy and muddy subsea terrain. In this work, experimental investigations
on CO2 hydrate formation in seawater using liquid CO2 in the presence of bentonite clay (1–5 wt % in seawater)
have been performed at 277.15 K and 5 MPa. Experimental pressure and
temperature conditions are considered such that they closely indicate
the subsea conditions. A sample hydrate promoter, tetrahydrofuran,
in varying concentrations has also been used to enhance the CO2 hydrate formation and to investigate its impact on the rheology.
Hydrate slurry shows a shear thinning (pseudoplastic) rheological
behavior. A peculiar trend in terms of increase in viscosity profiles
during hydrate formation has been observed when THF is used, whereas
minimal changes in the viscosity of the CO2 hydrate slurry
are observed in the absence of THF. The magnitude of shear stress
and viscosity increases with THF concentration in the solution. However,
the synergism between bentonite and THF at different concentrations
also plays a crucial role in hydrate growth and stability. This work
is crucial for understanding CO2 hydrate formation from
liquid CO2, typically at higher CO2 injection
depths in clay-bound oceanic sequestration conditions, and will be
useful to examine hydrate formation, flow tendency, and rheology in
slopy and muddy subsea terrains.