CO2
sequestration FAQ
New international
rules to allow storage of carbon dioxide (CO2) in sub-seabed geological formations
have come into force on 10 February 2007.
What is sequestration
of CO2 in geological formations?
CO2
sequestration is the capture and permanent storage in geological formations
of carbon dioxide that would otherwise be emitted to the atmosphere.
Why is CO2
sequestration being developed?
Elevated
levels of CO2 in the atmosphere caused by CO2
emissions from the combustion of fossil fuels (coal, oil or gas) contribute
to climate change and ocean acidification. The use of CO2
sequestration is only one option of a range of measures to tackle these challenges,
including, first and foremost, the need to further develop and use low carbon
forms of energy and conservation measures to reduce emissions.
What happens
if the oceans become more acidic?
The oceans
are a massive reservoir of CO2. Oceanic carbon includes a
portion of that resulting from human activity. Recent studies reveal that the
oceans have absorbed nearly half of the approximately 1,300 Gigatonnes of CO2
emitted to the atmosphere from anthropogenic fossil fuel combustion sources
during the last 200 years. Ocean chemistry has helped buffer some of the effects
of climate change. However, increased CO2 absorption by the
surface ocean has already resulted in a pH reduction (i.e., acidification of
the surface ocean) of 0.1 unit - from pH 8.2 to 8.1 over the last 200 years.
Studies indicate that with a "business as usual" scenario, by the
year 2100 the pH of the surface mixed layer could decrease by more than 0.3
units and by 2250 by 0.7 units. This would create a lower pH than that known
to have been experienced in at least the last 20 million years. The best scientific
information currently available suggests that these changes in ocean chemistry
could have a profound effect on corals, shellfish, specific groups of phytoplankton
such as coccolithophores, and other calcareous organisms thereby affecting biodiversity
and disrupting the marine food web and ocean biogeochemistry. Increased CO2
in seawater may also directly affect the physiology of some marine organisms,
such as squid.
Ocean acidification
caused by elevated emissions of CO2 is therefore a cause for
serious concern.
How does CO2
sequestration work?
CO2
is separated (captured) from flue gases, pressurized, and transported by pipeline
or vessel to the selected geological storage site using established technology.
The capture, transport and storage process itself also requires energy, so one
has to think in terms of how to achieve the greatest overall benefit. Some of
the existing infrastructure of depleted offshore oil and gas fields, where available,
might be used for CO2 sequestration after adaptation. Otherwise,
this infrastructure will have to be built. The proper selection and assessment
of the storage site will be important to ensure that the CO2
remains in the geological formation over the long term.
What is the
potential for capturing CO2?
The main
potential for CO2 capture is in the electricity generating
sector where fossil fuels are used, but interesting opportunities exist in fuels
processing and other energy-intensive industrial sectors. Coal-fired power plants
have the highest CO2 emissions and offer, therefore, the best
potential for CO2 sequestration.
What is the
potential for CO2 sequestration?
The main
underground CO2 storage potential is in depleted oil and gas
fields and in deep subterranean and sub-sea saline aquifers. Suitable geological
formations exist in many places around the world and can provide storage of
significant amounts of CO2, equivalent to decades or even
centuries of global emissions.
What are the
risks of CO2 sequestration?
CO2
could leak while being transported, or after storage. There are two different
kinds of leakage scenarios: (1) abrupt leakage, through injection well failure,
or leakage up an abandoned well; and (2) gradual leakage, through undetected
faults, fractures, or wells. The potential consequences of leakage are currently
poorly characterized but will depend on the location, scale, geographical extent
and prevailing conditions in the overlying environment.
How can the
risks associated with CO2 sequestration be minimized?
The risks
associated with leakage and transport of CO2 can be minimized
through the use of standard engineering practices such as monitoring and metering.
Pipeline transport of CO2 requires attention to route selection,
overpressure protection, leak detection and other design factors. With appropriate
site selection based on available geological information, a monitoring programme
to detect problems, a regulatory system and the use of remediation methods to
stop or control CO2 releases if they arise, the local health,
safety and environment risks of CO2 sequestration would be
comparable to the risks of current activities such as natural gas storage and
enhanced oil recovery.
The 'Risk
Assessment and Management Framework for CO2 Sequestration'
developed in 2006 and the Guidelines being developed under the London Protocol
are designed to address these issues (see also below).
Features
of storage sites with a low probability of CO2 leakage include:
(1) highly impermeable cap rocks; (2) geological stability; (3) absence of leakage
paths; and (4) effective trapping mechanisms of the sequestered CO2.
What are the
new rules for CO2 sequestration in sub-seabed geological formations?
Parties
to the 1996 Protocol to the Convention on the Prevention of Marine Pollution
by Dumping of Wastes and Other Matter, 1972 (London Protocol) adopted amendments
on 2 November 2006 to Annex 1 to this Protocol to regulate CO2
sequestration in sub-seabed geological formations. To date, 8 February 2007,
there are 30 Parties to this Protocol.
The rules
state that carbon dioxide streams may only be considered for dumping, if: (1)
disposal is into a sub-seabed geological formation; (2) they consist overwhelmingly
of carbon dioxide (they may contain incidental associated substances derived
from the source material and the capture and sequestration processes used);
and (3) no waste is added for the purpose of its disposal. In other words, these
rules do not permit CO2 sequestration in the deep oceans themselves.
As sub-seabed
geological sequestration of CO2 will now be subject to licensing,
Parties also agreed that guidelines should be developed for adoption when Parties
meet again in November 2007 on how to capture and sequester CO2
in a manner that meets all the requirements of the Protocol and is safe for
the marine environment, over both the short and long terms.
Protection
of the oceans, being part of the 'global commons', requires internationally
agreed standards. The use of geological formations on land for CO2
sequestration, on the other hand, is generally subject to national law.
What is the
effect of the new rules?
The new
rules provide a basis in international environmental law to regulate CO2 sequestration
in sub-seabed geological formations. They also create a climate in which more
research can be done to further develop and improve existing technologies enabling,
in the end, safe sequestration of CO2. Such research requires
time and is costly.
How will the
new rules be enforced?
CO2
sequestration in the sub-seabed will be subject to licences issued by governments.
Every applicant will have to demonstrate the integrity of a proposed sequestration
site with monitoring and mitigation safeguards in place to ensure that the CO2
will be permanently stored as intended. The monitoring provisions will be crucial
components of the license approval process.
The 'Risk
Assessment and Management Framework for CO2 Sequestration'
developed under the London Protocol in 2006 provides provisional information
to regulators and others regarding: (1) the selection of those underground reservoirs
with the best potential for permanent isolation; (2) site-specific risks to
the marine environment of CO2 sequestration; (3) the development
of management strategies to address uncertainties; and (4) the reduction of
residual risks to acceptable levels. If storage sites are selected and managed
appropriately, the probability of leakage from reservoirs should be minimal.
Using the
abovementioned Framework, Guidelines are being prepared for adoption under the
London Protocol in 2007 to cover all the points which need to be taken into
account by applicants for these licences and also by licensing authorities when
assessing these applications and enforcing the permit conditions.
Guidelines
generally provide a good basis for harmonized interpretation and implementation
of the London Protocol. Furthermore, the regular meetings of Parties give the
opportunity to discuss individual CO2 sequestration licences,
both informally and formally.
What research
is currently being done?
Currently,
there are three projects on a larger scale to test deep geological storage of
CO2: (1) the "Sleipner Project" beneath the North
Sea off the Norwegian coast (storage in a deep underground saline water reservoir);
(2) the "Weyburn Project" in Canada (storage in an underground oil
field); and (3) the "In Salah Project" in Algeria (injection of CO2
into a depleted gas reservoir). Further large offshore storage projects are
being developed in several countries, including Norway and the United Kingdom,
while several smaller scale pilot projects have been undertaken and are being
planned. In addition, much research is devoted to develop and test monitoring
techniques and other technical issues, using for instance natural CO2
reservoirs and leakages. These research and pilot projects are carried out in
many countries, including Australia, China, France, Germany, India, Italy, Japan,
Netherlands, United Kingdom and the United States.
Underground
oil and gas reservoirs have already retained materials for geologically significant
periods and offer, in the short term, the most attractive sites for CO2
sequestration.
External links:
Further
information on this issue can be found at:
http://co2captureandstorage.info/:
This website provides a collection of resources related to the capture and storage
of CO2. Deep reductions in greenhouse gas emissions are required
in order to meet the UNFCC goal of stabilising anthropogenic greenhouse gas
emissions.
http://www.iea.org:
the International Energy Agency,
especially its Greenhouse Gas Research and Development Programme at http://www.ieagreen.org.uk/ccs.html
on Capture and Storage of CO2.
http://www.ipcc.ch:
The Intergovernmental Panel on Climate Change. The reader is referred in particular
to the IPCC "Special Report on Carbon Dioxide Capture and Storage",
published in 2005 by Cambridge University Press.
If you need more
information on the CO2 sequestration discussions under the London Convention
and Protocol go to: http://www.londonconvention.org
or contact rcoenen@imo.org.
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