Carbon Capture and Storage

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Carbon Capture and Storage PRESENTATION TO THE PORTFOLIO COMMITTEE OF ENVIRONMENT, TUESDAY 21 AUGUST 2007 CCS: 210807

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Carbon Capture and Storage. PRESENTATION TO THE PORTFOLIO COMMITTEE OF ENVIRONMENT, TUESDAY 21 AUGUST 2007. CCS: 210807. Carbon Sequestration. - PowerPoint PPT Presentation

Transcript of Carbon Capture and Storage

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Carbon Capture and Storage

PRESENTATION TO THE PORTFOLIO COMMITTEE OF

ENVIRONMENT, TUESDAY 21 AUGUST 2007

CCS: 210807

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Carbon Sequestration

• Carbon capture and storage (CCS) is an approach to mitigating global warming by capturing carbon dioxide (CO2) from large point sources such as power plants and subsequently storing it instead of releasing it into the atmosphere. Technology for capturing of CO2 is already commercially available for large CO2 emitters, such as power plants; however, capture is meaningless without storage. Storage of CO2, on the other hand, is a relatively untried concept and as yet (2007) no power plant operates with a full carbon capture and storage system.

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Worldwide large stationarysources of CO2

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CO2 storage

• Various forms have been conceived for permanent storage of CO2. These forms include gaseous storage in various deep geological formations (including saline formations and exhausted gas fields), liquid storage in the ocean, and solid storage by reaction of CO2 with metal oxides to produce stable carbonates

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Geological storage

• Also known as geo-sequestration, this method involves injecting carbon dioxide directly into underground geological formations. Oil fields, gas fields, saline formations, unminable coal seams, and saline-filled basalt formations have been suggested as storage sites. Here, various physical (e.g., highly impermeable caprock) and geochemical trapping mechanisms would prevent the CO2 from escaping to the surface. CO2 is sometimes injected into declining oil fields to increase oil recovery (enhanced oil recovery). This option is attractive because the storage costs are offset by the sale of additional oil that is recovered. Disadvantages of old oil fields are their geographic distribution and their limited capacity.

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……Storage

• Unminable coal seams can be used to store CO2 because CO2 adsorbs to the surface of coal. However, the technical feasibility depends on the permeability of the coal bed. In the process of absorption the coal releases previously absorbed methane, and the methane can be recovered (Enhanced Coal Bed Methane recovery). The sale of the methane can be used to offset the cost of the CO2 storage.

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….. Storage• Saline formations contain highly mineralized brines, and have

so far been considered of no benefit to humans. Saline aquifers have been used for storage of chemical waste in a few cases. The main advantage of saline aquifers is their large potential storage volume and their common occurrence. This will reduce the distances over which CO2 has to be transported. The major disadvantage of saline aquifers is that relatively little is known about them, compared to oil fields. To keep the cost of storage acceptable the geophysical exploration may be limited, resulting in larger uncertainty about the aquifer structure. Unlike storage in oil fields or coal beds no side product will offset the storage cost. Leakage of CO2 back into the atmosphere may be a problem in saline aquifer storage. However, current research shows that several trapping mechanisms immobilize the CO2 underground, reducing the risk of leakage.

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….. Storage

• For well-selected, designed and managed geological storage sites, IPCC estimates that CO2 could be trapped for millions of years, and the sites are likely to retain over 99% of the injected CO2 over 1,000 years.

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….. Storage

• Ocean storage

• Two main concepts exist. The 'dissolution' type injects CO2 by ship or pipeline into the water column at depths of 1000 m or more, and the CO2 subsequently dissolves. The 'lake' type deposits CO2 directly onto the sea floor at depths greater than 3000 m, where CO2 is denser than water and is expected to form a 'lake' that would delay dissolution of CO2 into the environment.

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Dissolution and lake type storages

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CCS v non-CCS

• CCS applied to a modern conventional power plant could reduce CO2 emissions to the atmosphere by approximately 80-90% compared to a plant without CCS. Capturing and compressing CO2 requires much energy and would increase the fuel needs of a plant with CCS by about 10-40%. These and other system costs are estimated to increase the cost of energy from a power plant with CCS by 30-60% depending on the specific circumstances.

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• Storage of the CO2 is envisaged either in deep geological formations, deep oceans, or in the form of mineral carbonates. In the case of deep ocean storage, there is a risk of greatly increasing the problem of ocean acidification, a problem that also stems from the excess of carbon dioxide already in the atmosphere and oceans.

• Geological formations are currently considered the most promising sequestration sites, and these are estimated to have a storage capacity of at least 2000 Gt CO2. IPCC estimates that the economic potential of CCS could be between 10% and 55% of the total carbon mitigation effort until year 2100.

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Geological storage options

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conceptual plan for converting methane gas into hydrogen and CO2, then pumping the separated CO2 offshore to assist with efficient oil production from the Miller oilfield.

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World CO2 emissions

The quantity has steadily increased since the start of the industrial revolution (1800's) and peaked late in the last century. Worldwide, emissions are still rising.

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How does CO2 affect climate ?

The average temperature of the Earth is rising, especially when measured at the poles. Note that the average Earth surface temperature correlates well with the amount of CO2 in the atmosphere (i.e. as the CO2 levels in the atmosphere have increased, the surface temperature has gone up at the same time).

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How does CO2 affect oceans?

• About half of the extra CO2 from the atmosphere will dissolve in the oceans, making the water more acidic. The diagram shows how acidic the oceans will become in the future, upto the year 3000. To work this out, it was necessary to:

• predict how CO2 emissions will change in the future (the top of the diagram)

• calculate how this will change the amount of CO2 in the atmosphere (middle part of the diagram)

• finally work out how acidic the oceans will become (bottom part of the diagram)

• The acidity is shown as a change in pH units. The effects of this change on marine life is unknown, but could be disastrous.

Diagram from Caldeira, K. & Wickett, M.E. (2003) Nature, v. 425. p. 365

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…CO2 and OceansThe ocean already holds 400 Billion tons of fossil fuel CO2. Consequently, the ocean is already 0.1 pH units more acid than before industrial CO2 emissions. This means nutrients for plankton in the North Sea, and all shallow ocean waters, are

changing rapidly. This is the base of the food chain for invertebrates, shells and, eventually, economic fishing. By 2050 the ocean will be five times more acid than at any time since glaciation (change pH 8.4 to pH

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Cost of CCS

• Capturing and compressing CO2 requires much energy, significantly raising the running costs of CCS-equipped power plants. In addition there are added investment or capital costs. The process would increase the energy needs of a plant with CCS by about 10-40%. The costs of storage and other system costs are estimated to increase the costs of energy from a power plant with CCS by 30-60%, depending on the specific circumstances.

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…..Cost

• For the world scale, estimates are commonly about 2% of Global Domestic Product. That is one year of normal growth.

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CO2 transport

• After capture, the CO2 must be transported to suitable storage sites. This is done by pipeline, which is generally the cheapest form of transport, or by ship when no pipelines are available. Both methods are currently used for transporting CO2 for other applications.

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Environmental effects• A third concept is to convert the CO2 to bicarbonates (using

limestone) or hydrates.• The environmental effects of ocean storage are generally

negative, but poorly understood. Large concentrations of CO2 kills ocean organisms, but another problem is that dissolved CO2 would eventually equilibrate with the atmosphere, so the storage would not be permanent. Also, as part of the CO2 reacts with the water to form carbonic acid, H2CO3, the acidity of the ocean water increases. The resulting environmental effects on benthic life forms are poorly understood. Even though life appears to be rather sparse in the deep ocean basins, energy and chemical effects in these deep basins could have far reaching implications. Much more work is needed here to define the extent of the potential problems.

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….Environmental effects

• The time it takes water in the deeper oceans to circulate to the surface has been estimated to be on the order of 1600 years, varying upon currents and other changing conditions. Costs for deep ocean disposal of liquid CO2 are estimated at 40-80USD/ton (2002 USD). This figure covers the cost of sequestration at the powerplant and naval transport to the disposal site.

• The bicarbonate approach would reduce the pH effects and enhance the retention of CO2 in the ocean, but this would also increase the costs and other environmental effects.

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….Environmental effects• Leakage• A major concern with CCS is whether leakage of stored

CO2 will compromise CCS as a climate change mitigation option. For well-selected, designed and managed geological storage sites, IPCC estimates that CO2 could be trapped for millions of years, and are likely to retain over 99% of the injected CO2 over 1000 years. For ocean storage, the retention of CO2 would depend on the depth; IPCC estimates 30-85% would be retained after 500 years for depths 1000-3000 m. Mineral storage is not regarded as having any risks of leakage. The IPCC recommends that limits be set to the amount of leakage that can take place.

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Norway’s Sleipner gas field• To further investigate the safeness of CO2 sequestration,

we can look into Norway's Sleipner gas field, as it is the oldest plant that sequesters CO2 in an industrial scale. According to an environmental assessment of the gas field which was conducted after ten years of operation, the author affirmed that geographic sequestration of CO2 was the most definite way to store CO2 permanently.

• "Available geological information shows absence of major tectonic events after the deposition of the Utsira formation [saline reservoir]. This implies that the geological environment is tectonically stable and a site suitable for carbon dioxide storage. The solubility trapping [is] the most permanent and secure form of geological storage."

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…Example CCS projects

• As of 2005, three industrial-scale storage projects are in operation. Sleipner is the oldest project (1996) and is located in the North Sea where Norway's Statoil strips carbon dioxide from natural gas with amine solvents and disposes of this carbon dioxide in a saline formation. The carbon dioxide is a waste product of the field's natural gas production and the gas contains more (9% CO2) than is allowed into the natural gas distribution network. Storing it underground avoids this problem and saves Statoil hundreds of millions of euro in avoided carbon taxes. Sleipner stores about one million tonnes CO2 a year.

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Statoil

•The Sleipner A project injects carbon dioxide into saltwater aquifers deep beneath the sea floor off the Norwegian coast. The project turns a profit due to the presence of Norway’s high carbon taxes.

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…Example CCS projects

• The Weyburn project Weyburn started in 2000 and is located in an oil reservoir discovered in 1954 in Weyburn, Southeastern Saskatchewan, Canada. The CO2 for this project is captured at the Great Plains Coal Gasification plant in Beulah, North Dakota which has produced methane from coal for more than 30 years. At Weyburn, the CO2 will also be used for enhanced oil recovery with an injection rate of about 1.5 million tonnes per year.

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…Example CCS projects

• The third site is In Salah, which like Sleipner is a natural gas reservoir located in In Salah, Algeria. The CO2 will be separated from the natural gas and re-injected into the subsurface at a rate of about 1.2 million tonnes per year.

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…Example CCS projects

• A major Canadian initiative called the Integrated CO2 Network (ICO2N) is a proposed system for the capture, transport and storage of carbon dioxide (CO2). ICO2N members represent a group of industry participants providing a framework for carbon capture and storage development in Canada.

• Currently, the United States government has approved the construction of what they claim to be the world's first CCS power plant, FutureGen.

• In the Netherlands, an 68 MW oxyfuel plant ("Zero Emission Power Plant") is being planned and is expected to be operational in 2009.

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Global C storage in vegetation

In terms of quantity of carbon stored, tropical and boreal forests are visibly outstanding. The values for carbon storage in vegetation in the tropics reach a maximum of 250 metric tons per hectare.

Temperate forests and tropical savannas store less than the tropical and boreal forests. Non-woody grasslands and drylands store less than the forested areas, and sparsely vegetated and bare desert areas have the least carbon storage potential.

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Capturing carbon dioxide from small, mobile sources, such as cars, would be more difficult. But with power plants comprising 40 percent of the world's fossil fuel-derived carbon emissions, the potential for reductions is significant.Estimates of worldwide storage capacity range from 2 trillion to 10 trillion tons of carbon dioxide, according to the Intergovernmental Panel on Climate Change (IPCC) in its report on carbon capture and storage. Global emissions in 2004 totaled 27 billion tons, according to the U.S. Department of Energy's Energy Information Administration.If all human-induced emissions were sequestered, enough capacity would exist to accommodate more than 100 years' worth of emissions, - IPCC.

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Safety smarts

• The goal of carbon sequestration is to store the carbon dioxide permanently, i.e. very, very long-term, geological time periods.

• The greatest concern surrounding carbon dioxide storage is the potential for it to leak. The obvious worry is that leakage would lead to more global warming, defeating the purpose of storage in the first place. But studies have shown that leakage, if it happened at all, would be insignificant. The IPCC reported that 99% retention of the carbon dioxide that is stored would be ''very likely'' over 100 years and ''likely'' over 1,000 years. If done right, selecting the site correctly and monitor, it can be near permanent.

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…..Safety smarts

• Of greater concern to the researchers are the potential risks of carbon sequestration to human health, mainly through asphyxiation and groundwater contamination. The threat of asphyxiation-or suffocation due to carbon dioxide displacing oxygen-is very low, because of the unlikelihood of a rapid leakage, which would have to occur to cause a problem.

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…..Safety smarts

• Drinking water contamination is the more probable danger. For example, if carbon dioxide enters the groundwater somehow, it can increase the water's acidity, potentially leaching toxic chemicals, such as lead, from rocks into the water. To address these risks, scientists are studying reservoir geology to better understand what happens after injecting carbon dioxide underground.

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…..Safety smarts

• Carefully selecting places that will not leak, and doing a good job of engineering the injection systems and paying attention to where the carbon dioxide is actually going required.

• While a thorough technical understanding of the risks will reveal best practices, the scientists also stressed the need for good management to see that proper procedures are followed.

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'A family of solutions'• 'A family of solutions'• Critics of carbon sequestration argue that the technology will divert

attention from research on long-term clean energy options, such as renewable power. Worse, they fear it will prolong fossil fuel use, if fossil fuels from some stationary sources can be used more cleanly.

• Continual emphasis on the need to adopt other technologies in addition to carbon sequestration needed

• Geological sequestration be one of a family of solutions for addressing the greenhouse gas issue.

• Energy efficiency and renewable energy are already feasible today and also can define the long-term energy picture.

• Carbon dioxide sequestration is only a bridge technology.

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What if we do nothing?• The longer we wait, the worse it gets. Most scientists believe that the

evidence of high CO2 levels and hot climates in the past is compelling. • Like all preventive medicine, it's easier to put off the fateful day. But when

that day arrives, it causes you more pain, and costs more, compared to early actions. Its important to realise that, even if we act now, the climate will carry on warming for another 3 or 5 degrees Centigrade. Potential for areas to dry and heat up to become uninhabitable desert.

• By acting now, we have a chance to limit that rise to less than 5 Centigrade, by keeping atmospheric CO2 less than 550 parts per million.

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Overview

• Carbon capture and storage (CCS) in geological structures is technically feasible, although further development is needed to optimise it.

• CCS potentially offers carbon emissions reduction at costs similar to offshore wind and nuclear power.

• CCS offers a low-carbon way to use fossil fuels to ensure security of electricity supply.

• Enhanced oil recovery in the North Sea could reduce the cost of CCS and could also act as a lesson.

• Under present economic conditions CCS may not be financially viable. Creating incentives for CCS forms part of the wider debate on economic strategies to reduce CO2 emissions.

• CCS could play a key role in reducing future emissions from the developing world like South Africa

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Acknowledgements• IPCC Special Report, 2005: CO2 Capture and Storage• IPCC Special Report, 2000: Methodological and Technological Issues in Technology• Transfer• IPCC Special Report, 2000: Emissions Scenarios• IPCC Special Report, 2000: Land Use, Land Use Change and Forestry• IPCC National Greenhouse Gas Inventories Programme, 2000• Good Practice Guidance and Uncertainty Management in• National Greenhouse Gas Inventories• Cooperative Research Centre for Greenhouse Gas Technologies

www.co2crc.com.au • Cooperative Research Centre for Coal in Sustainable Development

www.ccsd.biz • International Energy Agency (Carbon Dioxide Capture and Storage)

www.co2captureandstorage.info • IPCC, 2003: Good Practice Guidance for Land Use, Land-use Change, and Forestry.

Institute for Global Environmental Strategies, Havana.• Oremland, R., Marsh, L. M. and Polein, S. (1982). Methane production and simultaneous sulfate

reduction in anoxic marsh sediments. Nature, 296, 143-145.

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END

Thank you for your kind attention