Geological
storage options suitable for the injection of supercritical CO2 include
depleted oil and gas reservoirs, enhanced oil recovery methods, deep unused
saline water-saturated reservoir rocks, deep unmineable coal seams and enhance
coal-bed methane recovery methods (IPCC 2005). For well selected, designed, operated
and monitored sites, it is likely that 99% or more of the CO2 injected into
these stores would be retained for 1000 years (IPCC 2005).
The
IPCC (2005) have estimated that 460–3,030 Pg of carbon can be stored in geological
reservoirs (oil and gas fields, unmineable coal seams and deep saline
formations).
Oceanic
injection of CO2 as been proposed as an alternative to geological
storage, however there is assumed to be significant detrimental impact on
ecosystems, so this method is generally considered to be unviable (Lenton,
2011).
The IPCC
(2005) have ruled out other geologic storage options such as basalts, oil or
gas rich shales, salt caverns or abandoned mines as having no significant
contribution to make.
One
more recent storage idea is to inject CO2 into deep-sea sediments at a depth where
it is gravitationally stable (<3,000 m water depth and a few hundred metres
sediment depth) (House et al. 2006). CO2 would stay in its liquid phase at such high pressures and low
temperatures and would be denser than overlying pore fluid with CO2 hydrates forming a cap over the stored liquid CO2.
Concerns
highlighted include the unknown implications of the pore water displaced into
the ocean and the importance of site selection as landslide events could
release the CO2. In continental USA alone storage
capacity for this method is measured at. >104 Gt CO2 (>2700 Pg C) (House et al. 2006). It is proposed that no verification
or monitoring would be required due to the chemistry and physics of the over
and underlying hydrates and fluids —an idea that may not be well received (Harvey
and Huang 1995).
If this
suggested form of carbon storage stands up to subsequent investigation, then
when combined with storage options investigated within the IPCC’s SRCCS there
may be sufficient capacity to store in excess of all the known fossil fuel resources
of ∼3700 Pg C (IPCC 2007).
Next up, stratospheric aerosol injection.
Next up, stratospheric aerosol injection.
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