Immediate measures are required to
tackle global warming
and climate
change that may require the storage of enormous quantities of anthropogenic
CO2 in geological and oceanic reservoirs. In terrestrial
storage sites, CO2 is buoyant due to the subsurface temperature
profile. Therefore, if the reservoir is not adequately sealed, stored
CO2 can escape from geological formations. Alternatively,
oceanic sequestration has immense potential to facilitate long-term
sequestration of CO2 beneath the seafloor, thereby assisting
the wider scientific and industrial community to make the world carbon
neutral. There is a far-reaching scope for discussion in this aspect
that will open up new avenues for future developments in this area.
This article discusses the long-term viability, environmental sustainability
and economic potential of CO2 sequestration in the form
of hydrates into oceanic and subsea sediments. Analysis shows that
at above 2800 m depth, CO2 is denser than seawater, which
offers an additional gravitation barrier for CO2 to escape.
This article offers an in-depth analysis of CO2 sequestration
conditions, along with challenges and outlook with relevance to hydrate-based
CO2 sequestration in oceanic conditions. Moreover, the
crucial role of negative buoyancy and hydrate-forming zones (NBZ/HFZs)
and analysis of depth criterion in oceanic conditions have been highlighted.
The review also envisages that sequestration in NBZ region offers
stable storage for years even in geological perturbation and earthquakes;
however the depth of HFZ and NBZ regions depends on sedimentary type,
storage conditions, temperature and pressure.