Carbon dioxide sink 5980 224468389 2008-07-08T23:43:53Z Paleorthid 125638 Tagging or repairing external links using [[User:Dispenser/Link checker|checklinks tool]] A '''carbon dioxide (CO<sub>2</sub>) sink''' is a [[carbon dioxide]] reservoir that is increasing in size, and is the opposite of a carbon dioxide "source". The main natural sinks are: # the oceans' [[biological pump]] and # plants and other organisms that use [[photosynthesis]] to remove carbon from the atmosphere by incorporating it into [[Biomass (ecology)|biomass]] and releasing oxygen into the atmosphere. The process by which carbon dioxide sinks (natural and artificial) remove CO<sub>2</sub> from the atmosphere is known as carbon [[sequestration]]. Public awareness of the significance of CO<sub>2</sub> sinks has grown since passage of the [[Kyoto Protocol]], which allows their use as a form of [[carbon offset]]. == Kyoto Protocol == Because growing vegetation absorbs [[carbon dioxide]], the [[Kyoto Protocol]] allows countries that have large areas of forest (or other vegetation) to deduct a certain amount from their emissions, thus making it easier for them to achieve the desired net emission levels. Some countries want to be able to trade in emission rights in carbon emission markets, to make it possible for one country to buy the benefit of carbon dioxide sinks in another country. If overall limits on greenhouse gas emission are put into place, such a "cap-and-trade" market mechanism will tend to find cost-effective ways to reduce emissions.<ref>{{cite web | url=http://www.rff.org/Documents/RFF-RPT-Renewables.pdf | archiveurl=http://web.archive.org/web/20070604191032/http://www.rff.org/Documents/RFF-RPT-Renewables.pdf | archivedate=2007-06-04 | title=Electricity, Renewables, and Climate Change: Searching for a Cost-Effective Policy | author=Karen Palmer and Dallas Burtraw | publisher=[[Resources for the Future]]}}</ref> There is as yet no [[carbon audit regime]] for all such markets globally, and none is specified in the Kyoto Protocol. Each nation is on its own to verify actual carbon emission reductions (CER), and to account for carbon sequestration using some less formal method. In the [[Clean Development Mechanism]], only [[afforestation]] and [[reforestation]] are eligible to produce CERs in the first commitment period of the Kyoto Protocol (2008–2012). Forest conservation activities or activities avoiding [[deforestation]], which would result in emission reduction through the conservation of existing carbon stocks, are not eligible at this time.<ref>Manguiat, M. S. Z., Verheyen, R., Mackensen, J. & Scholz, G. (2005), ''Legal aspects in the implementation of CDM forestry projects'', number 59 in ‘IUCN Environmental Policy and Law Papers’, IUCN. Available from: http://www.iucn.org/themes/law/pdfdocuments/EPLP59EN.pdf</ref> Also, agricultural carbon sequestration is not possible yet.<ref>Rosenbaum, K. L., Schoene, D. & Mekouar, A. (2004), ''Climate change and the forest sector. Possible national and subnational legislation'', number 144 in ‘FAO Forestry Papers’, FAO. Available from: http://www.fao.org/docrep/007/y5647e/y5647e00.HTM</ref> ==Storage in vegetation and soils== Carbon stored in soils oxidizes rapidly; this, in addition to high rainfall levels, is the reason why tropical jungles have very thin organic soils. The forest eco-system may eventually become carbon neutral. Forest fires release absorbed carbon back into the atmosphere, as does deforestation due to rapidly increased oxidation of soil organic matter. The dead trees, plants, and moss in [[peat]] bogs undergo slow [[anaerobic decomposition]] below the surface of the bog. This process is slow enough that in many cases the bog grows rapidly and [[Carbon fixation|fixes]] more carbon from the atmosphere than is released. Over time, the peat grows deeper. Peat bogs inter approximately one-quarter of the carbon stored in land plants and soils.<ref>{{cite web | last =Chester | first =Bronwyn | authorlink = | coauthors = | title =The case of the missing sink | work = | publisher=[[McGill University|McGill]] Reporter |date=[[20 April]] [[2000]] | url =http://www.mcgill.ca/reporter/32/15/roulet/ | format = | doi = | accessdate = 2008-07-08}}</ref> Under some conditions, forests and peat bogs may become sources of CO<sub>2</sub>, such as when a forest is flooded by the construction of a hydroelectric dam. Unless the forests and peat are harvested before flooding, the rotting vegetation is a source of CO<sub>2</sub> and [[methane]] comparable in magnitude to the amount of carbon released by a fossil-fuel powered plant of equivalent power.<ref>{{cite web | url=http://www.newscientist.com/article.ns?id=dn7046 | title=Hydroelectric power's dirty secret revealed | publisher=[[New Scientist]] | date=[[24 February]] [[2005]] | accessdate=2008-07-08 | author=Duncan Graham-Rowe}}</ref> === Regenerative Agriculture === [[Regenerative agriculture]], if practiced on the planet’s 3.5 billion tillable acres, could sequester up to 40% of current CO2 emissions.<ref>A [http://www.rodaleinstitute.org/files/Rodale_Research_Paper.pdf report] recently released by [http://www.hero-farmers.org/ Rodale Institute] and based on nearly 30 years of research in its side-by-side studies of organic and conventional agriculture.</ref><ref>[http://www.grist.org/feature/2008/05/09/index.html?source=rss Timothy LaSalle of Rodale on the surprising climate benefits of organic farming | By Anna Lappé | Grist | Grist Feature | 09 May 2008<!-- Bot generated title -->]</ref> Agricultural carbon sequestration has the potential to substantially mitigate global warming impacts. When using biologically based [[regenerative practices]], this dramatic benefit can be accomplished with no decrease in yields or farmer profits. Organically managed soils can convert carbon dioxide from a greenhouse gas into a food-producing asset. In 2006, U.S. carbon dioxide emissions from fossil fuel combustion were estimated at nearly 6.5 billion tons. If a 2,000 lb/ac/year sequestration rate was achieved on all {{convert|434000000|acre|km2}} of cropland in the United States, nearly 1.6 billion tons of carbon dioxide would be sequestered per year, mitigating close to one quarter of the country's total fossil fuel emissions. This is the emission-cutting equivalent of taking one car off the road for every two acres under 21st Century regenerative agricultural management (based on a vehicle average of 15,000 miles per year at 23 mpg; U.S. EPA === Oceans === [[Image:CO2 pump hg.png|thumb|350px|Air-sea exchange of CO<sub>2</sub>]] [[Oceans]] are natural CO<sub>2</sub> sinks, and represent the largest active carbon sink on Earth. This role as a sink for CO<sub>2</sub> is driven by two processes, the [[solubility pump]] and the [[biological pump]].<ref>{{cite journal | last = Raven | first = J. A. | authorlink = | coauthors = P. G. Falkowski | title = Oceanic sinks for atmospheric CO<sub>2</sub> | journal = Plant Cell & Environment | volume = 22 | issue = | pages = 741&ndash;755 | publisher = | date = 1999 | url = | doi = | id = | accessdate = }}</ref> The former is primarily a function of differential CO<sub>2</sub> solubility in [[seawater]] and the [[thermohaline circulation]], while the latter is the sum of a series of biological processes that transport carbon (in [[organic chemistry|organic]] and [[inorganic chemistry of carbon|inorganic]] forms) from the surface [[photic zone|euphotic zone]] to the ocean's interior. A small fraction of the organic carbon transported by the biological pump to the [[seabed|seafloor]] is buried in [[anoxic sea water|anoxic]] conditions under sediments and ultimately forms [[fossil fuel]]s such as [[petroleum|oil]] and [[natural gas]]. At the present time, approximately one third<ref>{{cite journal | last = Takahashi | first = T. | authorlink = | coauthors = S. C. Sutherland, C. Sweeney, A. Poisson, N. Metzl, B. Tilbrook, N. Bates, R. Wanninkhof, R. A. Feely, C. Sabine, J. Olafsson and Y. C. Nojiri | title = Global sea-air CO<sub>2</sub> flux based on climatological surface ocean ''p''CO<sub>2</sub>, and seasonal biological and temperature effects | journal = Deep Sea Research II | volume = 49 | issue = | pages = 1601&ndash;1622 | publisher = | date = 2002 | url = | doi = | id = | accessdate = }}</ref> of [[anthropogenic]] emissions are estimated to be entering the ocean. The solubility pump is the primary mechanism driving this, with the biological pump playing a negligible role. This stems from the limitation of the biological pump by ambient light and nutrients required by the [[phytoplankton]] that ultimately drive it. [[Total inorganic carbon]] is not believed to limit [[primary production]] in the oceans, so its increasing availability in the ocean does not directly affect production (the situation on land is different, since enhanced atmospheric levels of CO<sub>2</sub> essentially "fertilize" land plant growth). However, [[ocean acidification]] by invading anthropogenic CO<sub>2</sub> may affect the biological pump by negatively impacting [[calcium carbonate|calcifying]] organisms such as [[coccolithophore]]s, [[foraminiferans]] and [[pteropod]]s. [[Climate change]] may also affect the biological pump in the future by warming and [[stratification (water)|stratifying]] the surface ocean, thus reducing the supply of limiting nutrients to surface waters. === Soils === Carbon as plant [[organic matter]] is sequestered in [[soil]]s: Soils contain more carbon than is contained in vegetation and the atmosphere combined.<ref>{{cite web | last =Swift | first =Roger S. | authorlink = | coauthors = | title =Soil Science - Abstract: Volume 166(11) November 2001 p 858-871 SEQUESTRATION OF CARBON BY SOIL. | work = | publisher = | date =November 2001 | url =http://www.soilsci.com/pt/re/soilsci/abstract.00010694-200111000-00010.htm;jsessionid=Lz5GXHt22sF0RQH0PlT5NRRzkQ344VBrJCr9522nbHdPSJPy7kcn!1151209438!181195628!8091!-1 | format = | doi = | accessdate = 2007-02-23}}</ref> [[soil carbon|Soils' organic carbon]] ([[humus]]) levels in many agricultural areas have been severely depleted. Organic material in the form of humus accumulates below about 25 degrees Celsius.{{Fact|date=May 2007}} Above this temperature, humus is oxidized much more rapidly. This is part of the reason why tropical soils under jungles are so thin, despite the rapid accumulation of organic material on the jungle floor (the other being extensive rainfall leaching soluble components vital to organic [[soil structure]]). Areas where shifting cultivation or [[slash and burn]] agriculture are practiced are generally only fertile for 2&ndash;3 years before they are abandoned. These tropical jungles are similar to coral reefs in that they are highly efficient at conserving and circulating necessary nutrients, which explains their lushness in a nutrient desert.{{Fact|date=May 2007}}{{Or|date=September 2007}} Grasslands contribute to [[soil organic matter]], mostly in the form of their extensive fibrous root mats. Much of this organic matter can remain unoxidized for long periods of time, depending on rainfall conditions, the length of the winter season, and the frequency of naturally occurring lightning-induced grass-fires necessary to recycle inorganic compounds from existing plant material. While these fires release carbon dioxide, they improve the quality of the grass-lands overall, in turn increasing the amount of carbon retained in the retained humic material. They also deposit carbon directly to the soil in the form of char that does not significantly degrade back to carbon dioxide. The overall effect of carbon sequestration is beneficial for soil since it adds more and more organic carbon to it and leads to improved soil properties. == Enhancing natural sequestration== === Forests === Forests are carbon stores, and they are carbon dioxide sinks when they are increasing in density or area. In Canada's boreal forests as much as 80% of the total carbon is stored in the soils as dead organic matter.<ref>CFS Science Policy Note May, 2007 url=http://cfs.nrcan.gc.ca/news/473</ref> Tropical [[reforestation]] can mitigate global warming until all available land has been reforested with mature forests.<ref>{{cite web | url=http://news.bbc.co.uk/1/hi/sci/tech/6184577.stm | title=Care needed with carbon offsets | author=Jonathan Amos | publisher=[[BBC]] | accessdate=2008-07-08}}</ref><ref>{{cite web | url=https://publicaffairs.llnl.gov/news/news_releases/2005/NR-05-12-04.html | title=Models show growing more forests in temperate regions could contribute to global warming | date=[[5 December]] [[2005]] | publisher=Lawrence Livermore National Laboratory | accessdate=2008-07-08}}</ref><ref>{{cite journal | author=S. Gibbard, K. Caldeira, G. Bala, T. J. Phillips, and M. Wickett | title = Climate effects of global land cover change | journal=Geophysical Research Letters | volume=32 | date=December 2005}}</ref><ref>{{cite web | url=http://www.ncbi.nlm.nih.gov/pubmed/12460485?dopt=abstractplus | title=Forests, carbon and global climate | author=Y. Malhi, P. Meir, and S. Brown | publisher=Institute of Ecology and Resource Management | date=[[15 August]] [[2002]] | accessdate=2008-07-08}}</ref> In the United States in 2004 (the most recent year for which EPA statistics<ref>{{cite web | url=http://epa.gov/climatechange/emissions/usinventoryreport.html | title=U.S. Greenhouse Gas Inventory Reports | publisher=[[United States Environmental Protection Agency|EPA]] | accessdate=2008-07-08}}</ref> are available), forests sequestered 10.6% (637 teragrams<ref name=epa1>{{cite web | url=http://epa.gov/climatechange/emissions/downloads06/06LULUCF.pdf | title=Land Use, Land-Use Change, and Forestry | publisher=[[United States Environmental Protection Agency|EPA]] | accessdate=2008-07-08}}</ref>) of the carbon dioxide released in the United States by the combustion of fossil fuels (coal, oil and natural gas; 5657 teragrams<ref name=epa2>{{cite web | url=http://epa.gov/climatechange/emissions/downloads06/06ES.pdf | title=Executive Summary | publisher=[[United States Environmental Protection Agency|EPA]] | accessdate=2008-07-08}}</ref>). Urban trees sequestered another 1.5% (88 teragrams<ref name=epa1 />). To further reduce U.S. carbon dioxide emissions by 7%, as stipulated by the [[Kyoto Protocol]], would require the planting of "an area the size of [[Texas]] [8% of the area of Brazil] every 30 years".<ref>William H. Schlesinger, dean of the Nicholas School of the Environment and Earth Sciences at Duke University, in Durham, North Carolina.</ref> [[Carbon offset]] programs are planting millions of fast-growing trees per year to reforest tropical lands, for as little as $0.10 per tree; over their typical 40-year lifetime, one million of these trees will fix 0.9 teragrams of carbon dioxide<ref>{{cite web | url=http://www.treesftf.org/about/cooling.htm | title=About Us: Global Cooling Center | publisher=Trees for the Future}}</ref>.In Canada, reducing timber harvesting would have very little impact on carbon dioxide emissions because of the combination of harvest and stored carbon in manufactured wood products along with the regrowth of the harvested forests. Additionally, the amount of carbon released from harvesting is small compared to the amount of carbon lost each year to forest fires and other natural disturbances.<ref> CFS Science Policy Note May, 2007 url=http://cfs.nrcan.gc.ca/news/473</ref> Former U.S. Vice President Al Gore shared the Nobel Peace Prize in 2007 with the United Nation's International Panel on Climate Change. The Panel concluded that "a sustainable forest management strategy aimed at maintaining or increasing forest carbon stocks, while producing an annual sustained yield of timbre fibre or energy from the forest, will generate the largest sustained mitigation benefit"<ref>{{cite web | url=http://www.ipcc.ch/ | title=IPCC Fourth Assessment Report (AR4) }}</ref> Life expectancy of forests varies throughout the world, influenced by tree species, site conditions and natural disturbance patterns. In some forests carbon may be stored for centuries, while in other forests carbon is released with frequent stand replacing fires. Forests that are harvested prior to stand replacing events allow for the retention of carbon in manufactured forest products such as lumber. Only a portion of the carbon removed from logged forests ends up as durable goods and buildings - the remainder ends up as sawmill by-products such as pulp, paper and pallets. For instance, of the 1,692 teragrams of carbon harvested from forests in Oregon and Washington (U.S) from 1900 to 1992, only 23% is in long-term storage in forest products. <ref>{{cite web | url=http://www.springerlink.com/content/u51867621j8307m7/ | title=Harmon, Harmon, Ferrell and Brooks. Modeling Carbon Stores in Oregon and Washington Forest Products 1900&ndash;1992. Climate Change 33:521-550 (1996).}}</ref> In addition to mitigating climate change, conserving forests to store carbon also helps provide valuable "ecosystem services" like clean water, soil conservation, wildlife habitat, and quality of life. The global cooling effect of carbon sequestration by forests is partially counterbalanced in that reforestation can decrease the reflection of sunlight ([[albedo]]). Mid-to-high latitude forests have a much lower albedo during snow seasons than flat ground, thus contributing to warming. ===Oceans=== {{seealso|Iron fertilization}} {{seealso|Ocean nourishment}} One way to increase the carbon sequestration efficiency of the oceans is to add micrometre-sized iron particles in the form of either [[hematite]] (iron oxide) or [[melanterite]] (iron sulfate) to certain regions of the ocean. This has the effect of stimulating growth of [[plankton]]. Iron is an important nutrient for [[phytoplankton]], usually made available via upwelling along the [[continental shelves]], inflows from rivers and streams, as well as deposition of dust suspended in the [[Earth's atmosphere|atmosphere]]. Natural sources of ocean iron have been declining in recent decades, contributing to an overall decline in ocean productivity (NASA, 2003). Yet in the presence of iron nutrients plankton populations quickly grow, or 'bloom', expanding the base of [[biomass]] productivity throughout the region and removing significant quantities of CO<sub>2</sub> from the atmosphere via [[photosynthesis]]. A test in 2002 in the [[Southern Ocean]] around [[Antarctica]] suggests that between 10,000 and 100,000 carbon atoms are sunk for each iron atom added to the water. More recent work in Germany (2005) suggests that any biomass carbon in the oceans, whether exported to depth or recycled in the [[euphotic zone]], represents long-term storage of carbon. This means that application of iron nutrients in select parts of the oceans, at appropriate scales, could have the combined effect of restoring ocean productivity while at the same time mitigating the effects of human caused emissions of carbon dioxide to the atmosphere. Because the effect of periodic small scale phytoplankton blooms on ocean ecosystems is unclear, more studies would be helpful. Phytoplankton have a complex effect on cloud formation via the release of substances such as [[dimethyl sulfide]] (DMS) that are converted to sulfate aerosols in the atmosphere, providing [[cloud condensation nuclei]], or CCN. But the effect of small scale plankton blooms on overall DMS production is unknown. Other nutrients such as nitrates, phosphates, and silica as well as iron may cause ocean fertilization. There has been some speculation that using pulses of fertilization (around 20 days in length) may be more effective at getting carbon to ocean floor than sustained fertilization.<ref>{{cite web | url=http://www.netl.doe.gov/publications/proceedings/01/carbon_seq/p25.pdf | title=Sequestration of CO<sub>2</sub> by ocean fertilization | author=Michael Markels, Jr and Richard T. Barber | publisher=NETL Conference on Carbon Sequestration | date=May 14&ndash;17, 2001 | accessdate=2008-07-08 }}</ref> There is some controversy over seeding the oceans with iron however, due to the potential for increased toxic phytoplankton growth (e.g. "[[red tide]]"), declining water quality due to overgrowth, and increasing anoxia in areas harming other sea-life such as zooplankton, fish, coral, etc.<ref>{{cite web | url=http://www.greenseaventure.com/Questions_Concerns.html | title=Questions and Concerns | publisher=GreenSea Venture | accessdate=2008-07-08}}</ref><ref>{{cite journal | url=http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6T8F-4DH2JCT-1&_user=10&_coverDate=12%2F30%2F2004&_rdoc=1&_fmt=&_orig=search&_sort=d&view=c&_acct=C000050221&_version=1&_urlVersion=0&_userid=10&md5=013c171e38287b45b13181a8fb73aa03 | title=Effects of selenium, iron and cobalt addition to growth and yessotoxin production of the toxic marine dinoflagellate Protoceratium reticulatum in culture | doi = 10.1016/j.jembe.2004.08.014 <!--Retrieved from URL by DOI bot-->| journal=Journal of Experimental Marine Biology and Ecology | author=Simon M. Mitrovica, Monica Fernández Amandia, Lincoln McKenzieb, Ambrose Fureya and Kevin J. James | volume=313 | issue=2 | date=[[30 December]] [[2004]] | pages=337&ndash;351 | accessdate=2008-07-08}}</ref> === Soils === Since the 1850s, a large proportion of the world's grasslands have been tilled and converted to croplands, allowing the rapid oxidation of large quantities of soil organic carbon. However, in the United States in 2004 (the most recent year for which EPA statistics are available), agricultural soils including pasture land sequestered 0.8% (46 teragrams<ref name=epa1 />) as much carbon as was released in the United States by the combustion of fossil fuels (5988 teragrams<ref name=epa2 />). The annual amount of this sequestration has been gradually increasing since 1998<ref name=epa1 />. Methods that significantly enhance carbon sequestration in soil include [[no-till farming]], residue mulching, [[cover crop]]ping, and [[crop rotation]], all of which are more widely used in [[organic farming]] than in conventional farming.<ref>{{cite web | url=http://www.news.cornell.edu/stories/July05/organic.farm.vs.other.ssl.html | title=Organic farming produces same corn and soybean yields as conventional farms, but consumes less energy and no pesticides, study finds | author=Susan S. Lang | date=[[13 July]], [[2005]] | accessdate=2008-07-08}}</ref><ref>Pimentel, David, et al, Bioscience: 55:7, July 2005</ref> Because only 5% of US farmland currently uses no-till and residue mulching, there is a large potential for carbon sequestration.<ref>{{cite journal |quotes= |last=Lal |first=R |authorlink= |coauthors=et al |year=2004 |month=April |title=Managing Soil Carbon |journal=Science |volume=304 |issue= |pages=393 |id= |url=http://www.sciencemag.org/cgi/content/summary/304/5669/393?maxtoshow=&HITS=&hits=&RESULTFORMAT=&author1=Morgan%2C+mg&fulltext=soil&andorexactfulltext=and&searchid=1&FIRSTINDEX=0&resourcetype=HWCIT | doi = 10.1126/science.1093079 <!--Retrieved from url by DOI bot--> |accessdate= |pmid=15087532 }}</ref> Conversion to pastureland, particularly with good management of grazing, can sequester even more carbon in the soil. [[Terra preta]], an [[anthropogenic]], high-carbon soil, is also being investigated as a sequestration mechanism. By [[pyrolysis|pyrolysing]] biomass, about half of its carbon can be reduced to [[charcoal]], which can persist in the soil for centuries, and makes a useful soil amendment, especially in tropical soils (''[[biochar]]'' or ''agrichar'').<ref>{{cite web | url=http://www.css.cornell.edu/faculty/lehmann/biochar/Biochar_home.htm | title=Biochar: the new frontier | author=Johannes Lehmann | accessdate=2008-07-08}}</ref> <ref name='abc.net.au/catalyst/s2012892'>{{cite news | first=Mark | last=Horstman | title=Agrichar – A solution to global warming? | date=2007-09-23 | publisher=Australian Broadcasting Corporation | url =http://www.abc.net.au/catalyst/stories/s2012892.htm | work =ABC TV Science: Catalyst | accessdate = 2008-07-08 }}</ref> === Savanna === [[Controlled burn]]s on far north Australian [[savanna]]s can result in an overall carbon sink. One working example is the West Arnhem Fire Management Agreement, started to bring "strategic fire management across 28,000 km² of Western Arnhem Land". Deliberately starting controlled burns early in the dry season results in a mosaic of burnt and unburnt country which reduces the area of burning compared with stronger, late dry season fires. In the early dry season there are higher moisture levels, cooler temperatures, and lighter wind than later in the dry season; fires tend to go out overnight. Early controlled burns also results in a smaller proportion of the grass and tree biomass being burnt. <ref name='savanna.ntu.edu.au/arnhem_fire_proj'> {{cite web|url=http://savanna.ntu.edu.au/information/arnhem_fire_project.html |title=West Arnhem Land Fire Abatement Project |accessdate=2008-07-08 |work=Savanna Information |publisher=Tropical Savannas Cooperative Research Centre }}</ref> Emission reductions of 256,000 tonnes of CO<sub>2</sub> have been made as at 2007.<ref name='savanna.ntu.edu.au/Eureka_arnhem_fire_proj'> {{cite web|url=http://savanna.ntu.edu.au/news/topical_savannas109.html |title=Eureka Win for West Arnhem Land Fire Project |accessdate=2008-07-08 |work=Savanna Information |publisher=Tropical Savannas Cooperative Research Centre }}</ref> ==Artificial sequestration== For carbon to be sequestered artificially (i.e. not using the natural processes of the carbon cycle) it must first be captured, ''or'' it must be significantly delayed or prevented from being re-released into the atmosphere (by combustion, decay, etc.) from an existing carbon-rich material, by being incorporated into an enduring usage (such as in construction). Thereafter it can be passively stored ''or'' remain productively utilized over time in a variety of ways. For example, upon harvesting, wood (as a carbon-rich material) can be immediately burned or otherwise serve as a fuel, returning its carbon to the atmosphere, ''or'' it can be incorporated into construction or a range of other durable products, thus sequestering its carbon over years or even centuries. One ton of dry wood is equivalent to 1.8 tons of Carbon dioxide. Indeed, a very carefully-designed and durable, energy-efficient and energy-capturing building has the potential to sequester (in its carbon-rich construction materials), as much as or more carbon than was released by the acquisition and incorporation of all its materials and than will be released by building-function "energy-imports" during the structure's (potentially multi-century) existence. Such a structure might be termed "carbon neutral" or even "carbon negative". Building construction and operation (electricity usage, heating, etc) are estimated to contribute nearly ''half'' of the annual human-caused carbon additions to the atmosphere.<ref>{{cite web | last =| first =| authorlink = | coauthors = | title=Climate Change, Global Warming, and the Built Environment - Architecture 2030| work = | publisher = | date =| url =http://www.architecture2030.org | format = | doi = | accessdate = 2007-02-23}}</ref> [[Natural-gas]] purification plants often already have to remove carbon dioxide, either to avoid [[dry ice]] clogging gas tankers or to prevent carbon-dioxide concentrations exceeding the 3% maximum permitted on the natural-gas distribution grid. Beyond this, one of the most likely early applications of carbon capture is the capture of carbon dioxide from [[flue gas]]es at [[power station]]s (in the case of coal, this is known as "[[clean coal]]"). A typical new 1000-MW [[coal-fired power station]] produces around 6 million tons of carbon dioxide annually. Adding carbon capture to existing plants can add significantly to the costs of energy production; scrubbing costs aside, a 1000-MW coal plant will require the storage of about 50 million [[barrel]]s of carbon dioxide a year. However, scrubbing is relatively affordable when added to new plants based on [[coal gasification]] technology, where it is estimated to raise energy costs for households in the United States using only coal-fired electricity sources from 10 cents per kWh to 12 cents.<ref>{{cite journal | title=Can We Bury Global Warming? | author=Robert H. Socolow | journal=[[Scientific American]] | date=July 2005 | pages=42}}</ref> ===Carbon capture=== {{main|Carbon capture and storage}} Currently, capture of carbon dioxide is performed on a large scale by absorption of carbon dioxide onto various [[Amine gas treating|amine-based solvents]]. Other techniques are currently being investigated, such as [[pressure swing adsorption]], [[temperature swing adsorption]], [[Gas separation|gas separation membranes]], and [[Distillation#Industrial_distillation|cryogenics]]. Recent pilot studies include [[Flue gas|flue capture]] and conversion to [[baking soda]] and use of [[algae]] for conversion to [[Algae#Energy_source|fuel]] or [[Algae#Fertilizer|feed]]. In coal-fired power stations, the main alternatives to retrofitting amine-based absorbers to existing power stations are two new technologies: [[Integrated Gasification Combined Cycle|coal gasification combined-cycle]] and [[Oxy-fuel combustion]]. Gasification first produces a "[[syngas]]" primarily of [[hydrogen]] and [[carbon monoxide]], which is burned, with carbon dioxide filtered from the flue gas. Oxy-fuel combustion burns the coal in [[oxygen]] instead of [[Air#Composition|air]], producing only carbon dioxide and [[water vapour]], which are relatively easily separated. Some of the combustion products must be returned to the combustion chamber, either before or after separation, otherwise the temperatures would be too high for the turbine. Another long-term option is carbon capture directly from the air using [[hydroxides]]. The air would literally be scrubbed of its CO<sub>2</sub> content. This idea offers an alternative to non-[[Fossil fuel|carbon-based fuels]] for the transportation sector. Examples of carbon sequestration at coal plants include converting carbon from smokestacks into baking soda,<ref>utility company [http://www.luminant.com/ Luminant]'s pilot version at its [http://www.luminant.com/plants/big_brown.aspx Big Brown Steam Electric Station] in [[Fairfield, Texas]]</ref><ref>[http://www.skyonic.com/theCompany.php Skyonic] plans to circumvent storage problems of [[Supercritical carbon dioxide|liquid CO2]] by storing baking soda in mines, landfills, or simply to be sold as industrial or food-grade [[baking soda]].</ref> and algae-based carbon capture, circumventing storage by converting algae into fuel or feed.<ref>[http://www.greenfuelonline.com/index.html GreenFuel Technologies Corp.]</ref> ===Oceans=== Another proposed form of carbon sequestration in the ocean is direct injection. In this method, carbon dioxide is pumped directly into the water at depth, and expected to form "lakes" of liquid CO<sub>2</sub> at the bottom. Experiments carried out in moderate to deep waters (350 - 3600 m) indicate that the liquid CO<sub>2</sub> reacts to form solid CO<sub>2</sub> [[clathrate hydrate]]s, which gradually dissolve in the surrounding waters. This method, too, has potentially dangerous environmental consequences. The carbon dioxide does react with the water to form [[carbonic acid]], H<sub>2</sub>CO<sub>3</sub>; however, most (as much as 99%) remains as dissolved molecular CO<sub>2</sub>. The equilibrium would no doubt be quite different under the high pressure conditions in the deep ocean. In addition, if deep-sea bacterial [[methanogens]] that reduce carbon dioxide were to encounter the carbon dioxide sinks, levels of [[methane]] gas may increase, leading to the generation of an even worse greenhouse gas<ref>[http://www.csmonitor.com/2008/0428/p01s04-wogi.html Potent greenhouse-gas methane has been rising | csmonitor.com<!-- Bot generated title -->]</ref>. The resulting environmental effects on [[benthic]] life forms of the [[bathypelagic]], [[abyssopelagic]] and [[hadopelagic]] zones are unknown. 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. Carbon storage in or under oceans may not be compatible with the [[Convention on the Prevention of Marine Pollution by Dumping of Wastes and Other Matter]]<ref>{{cite web | url=http://www.theyworkforyou.com/wrans/?id=2005-07-04a.7044.h | title=Carbon Sequestration | author=Norman Baker and Ben Bradshaw | accessdate=2008-07-08 | date=[[4 July]] [[2005]]}}</ref>. An additional method of long-term ocean-based sequestration is to gather [[crop residue]] such as corn stalks or excess hay into large weighted bales of biomass and deposit it in the [[alluvial fan]] areas of the deep [[ocean basin]]. Dropping these residues in alluvial fans would cause the residues to be quickly buried in silt on the sea floor, sequestering the biomass for very long time spans. Alluvial fans exist in all of the world's oceans and seas where river deltas fall off the edge of the [[continental shelf]] such as the [[Mississippi Delta|Mississippi alluvial fan]] in the [[gulf of Mexico]] and the [[Nile Delta|Nile alluvial fan]] in the [[Mediterranean Sea]]. A downside, however, would be an increase in aerobic bacteria growth due to the introduction of biomass, leading to more competition for oxygen resources in the deep sea, similar to the [[Oxygen Minimum Zone]]. <!-- --[[Special:Contributions/140.247.40.183|140.247.40.183]] ([[User talk:140.247.40.183|talk]]) 07:45, 29 April 2008 (UTC)--> === Geological sequestration === The method of ''geo-sequestration'' or ''geological storage'' involves injecting carbon dioxide directly into underground geological formations. Declining [[oil field]]s, saline [[aquifer]]s, and unminable [[coal seam]]s have been suggested as storage sites. Caverns and old mines that are commonly used to store natural gas are not considered, because of a lack of storage safety. CO<sub>2</sub> has been injected into declining oil fields for more than 30 years, to increase oil recovery. This option is attractive because the storage costs are offset by the sale of additional oil that is recovered. Further benefits are the existing infrastructure and the geophysical and geological information about the oil field that is available from the oil exploration. All oil fields have a geological barrier preventing upward migration of oil. It is supposed that these geological barriers will also be sufficient as long-term barrier to contain the injected CO<sub>2</sub>. Identified possible problems are the many 'leak' opportunities provided by old oil wells, the need for very high pressures (about 80 times air pressure) and low temperatures (below about 20 degrees Celsius) to keep the CO<sub>2</sub> liquified (only practical very deep underneath the sea) and the conversion of CO<sub>2</sub> into acids which can damage the geological barrier. Other disadvantages of old oil fields are their geographic distribution and their limited capacity. Unminable coal seams can be used to store CO<sub>2</sub>, because CO<sub>2</sub> absorbs to the coal surface, ensuring safe long-term storage. In the process it releases methane that was previously adsorbed to the coal surface and that may be recovered. Again the sale of the methane can be used to offset the cost of the CO<sub>2</sub> storage, although release or burning of methane would of course at least partially offset the obtained sequestration result. Saline aquifers contain highly mineralized brines and have so far been considered of no benefit to humans except in a few cases where they have been used for the storage of chemical waste. Their advantages include a large potential storage volume and relatively common occurrence reducing the distance over which CO<sub>2</sub> 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 structure of a given aquifer. Unlike storage in oil fields or coal beds, no side product will offset the storage cost. Leakage of CO<sub>2</sub> back into the atmosphere may be a problem in saline-aquifer storage. However, current research shows that several ''trapping mechanisms'' immobilize the CO<sub>2</sub> underground, reducing the risk of leakage. A major research project examining the geological sequestration of carbon dioxide is currently being performed at an oil field at [[Weyburn, Saskatchewan|Weyburn]] in south-eastern [[Saskatchewan]]. In the [[North Sea]], Norway's [[Statoil]] natural-gas platform [[Sleipner]] strips carbon dioxide out of the natural gas with amine solvents and disposes of this carbon dioxide by geological sequestration. Sleipner reduces emissions of carbon dioxide by approximately one million tonnes a year. The cost of geological sequestration is minor relative to the overall running costs. As of April 2005, [[BP]] is considering a trial of large-scale sequestration of carbon dioxide stripped from power plant emissions in the [[Miller oilfield]] as its reserves are depleted. In October 2007, the [[Bureau of Economic Geology]] at [[The University of Texas at Austin]] received a 10-year, $38 million subcontract to conduct the first intensively monitored, long-term project in the United States studying the feasibility of injecting a large volume of CO<sub>2</sub> for underground storage<ref>"Bureau of Economic Geology Receives $38 Million for First Large-Scale U.S. Test Storing Carbon Dioxide Underground" [http://www.jsg.utexas.edu/news/rels/102407.html]</ref>. The project is a research program of the [http://www.sseb.org/currentprograms/cpa_cmi.htm Southeast Regional Carbon Sequestration Partnership (SECARB)], funded by the [[National Energy Technology Laboratory]] of the [[United States Department of Energy|U.S. Department of Energy (DOE)]]. The SECARB partnership will demonstrate CO<sub>2</sub> injection rate and storage capacity in the [[Tuscaloosa-Woodbine]] geologic system that stretches from Texas to Florida. Beginning in fall 2007, the project will inject CO2 at the rate of one million tons per year, for up to 1.5 years, into brine up to {{convert|10000|ft|m}} below the land surface near the [[Cranfield oil field]] about {{convert|15|mi|km}} east of [[Natchez, Mississippi]]. Experimental equipment will measure the ability of the subsurface to accept and retain CO2. === Mineral sequestration === Mineral sequestration aims to trap carbon in the form of solid [[carbonate]] salts. This process occurs slowly in nature and is responsible for the deposition and accumulation of [[limestone]] (calcium carbonate) over geologic time. [[Carbonic acid]] in groundwater slowly reacts with complex [[silicates]] to dissolve [[calcium]], [[magnesium]], [[alkalis]] and [[silica]] and leave a residue of [[clay minerals]]. The dissolved calcium and magnesium react with [[bicarbonate]] to precipitate calcium and magnesium carbonates, a process that organisms use to make shells. When the organisms die, their shells are deposited as sediment and eventually turn into limestone. Limestones have accumulated over billions of years of geologic time and contain much of Earth's carbon. Ongoing research aims to speed up similar reactions involving alkali carbonates<ref>"Carbon-capture Technology To Help UK Tackle Global Warming", ''ScienceDaily'' July 27, 2007, http://www.sciencedaily.com/releases/2007/07/070727091001.htm</ref>. One proposed reaction is that of the rock [[dunite]], or its hydrated equivalent [[serpentinite]] with carbon dioxide to form the carbonate mineral [[magnesite]], plus silica and iron oxide ([[magnetite]]). Serpentinite sequestration is favored because of the non-toxic and predictable nature of magnesium carbonate. However, the ideal reaction (reaction 1) takes place only with extremely [[magnesium]]-rich [[olivine]] or [[serpentine]] minerals. The presence of [[iron]] in the olivine or serpentine will reduce the efficiency of the circuit and reactions 2 and 3 must take place, producing a [[slag]] of [[silica]] and [[magnetite]]. ==== Serpentinite reactions ==== '''Reaction 1'''<br> ''Mg-Olivine + Water + Carbon dioxide → Serpentine + Magnesite + Silica ''<br> :(Mg)<sub>2</sub>SiO<sub>4</sub> + nH<sub>2</sub>O + CO<sub>2</sub> &rarr; Mg<sub>3</sub>[Si<sub>2</sub>O<sub>5</sub>(OH)<sub>4</sub>] + MgCO<sub>3</sub> + SiO<sub>2</sub> + H<sub>2</sub>O (This is a non stoichiometric reaction just to show the principle). '''Reaction 2'''<br> ''Fe-Olivine + Water + Carbonic acid → Serpentine + Magnetite + Magnesite + Silica '' :4(Fe,Mg)<sub>2</sub>SiO<sub>4</sub> + nH<sub>2</sub>O + H<sub>2</sub>CO<sub>3</sub> &rarr; 2Mg<sub>3</sub>[Si<sub>2</sub>O<sub>5</sub>(OH)<sub>4</sub>] + 2Fe<sub>3</sub>O<sub>4</sub> + 2MgCO<sub>3</sub> + SiO<sub>2</sub> + H<sub>2</sub>O '''Reaction 3'''<br> ''Serpentine + carbon dioxide → Magnesite + silica + water''<br> :Mg<sub>3</sub>[Si<sub>2</sub>O<sub>5</sub>(OH)<sub>4</sub>] + 3CO<sub>2</sub> &rarr; 3MgCO<sub>3</sub> + 2SiO<sub>2</sub> + 2H<sub>2</sub>O ==== Zeolitic imidazolate frameworks ==== {{main|Zeolitic imidazolate frameworks}} Zeolitic imidazolate frameworks is a [[metal-organic framework]] carbon dioxide sink which could be used to keep industrial emissions of [[carbon dioxide]] out of the [[atmosphere]].<ref> [http://www.cbc.ca/technology/story/2008/02/15/tech-carbon-capture.html CBC News] article ''New materials can selectively capture CO2, scientists say'' published February 15, 2008</ref> ==References== {{reflist|2}} == See also == {{EnergyPortal}} * [[Carbon capture and storage]] * [[Carbon cycle]] * [[Carbon flux]] * [[Carbon offset]] * [[CO2 sequestration]] * [[Center for the Study of Carbon Dioxide and Global Change]] * [[Iron fertilization]] * [[North American Carbon Program]] ==External links== ===General=== *[http://www.jsg.utexas.edu/carboncapture/carbonsequestration.html Carbon Sequestration News] Recent news articles on CO<sub>2</sub> capture and storage. *[http://www.beg.utexas.edu/environqlty/co201.htm Gulf Coast Carbon Center] University of Texas at Austin research center that investigates geologic storage of anthropogenic carbon dioxide in the Gulf Coast region. *[http://www.sinkswatch.org/ SinksWatch] - An initiative to track and scrutinize carbon sink projects *[http://www.netl.doe.gov/technologies/carbon_seq/index.html National Energy Technology Laboratory (NETL) Carbon Sequestration Home Page] *[http://cdiac2.esd.ornl.gov/ U.S. Department of Energy's Office of Science Carbon Sequestration Research Programs] *{{cite web |url=http://www.netl.doe.gov/publications/carbon_seq/2005_roadmap_for_web.pdf |title= U.S. Department of Energy's National Energy Technology Laboratory - Carbon Sequestration Technology Roadmap |archiveurl=http://web.archive.org/web/20070604191032/http://www.netl.doe.gov/publications/carbon_seq/2005_roadmap_for_web.pdf |archivedate=2007-06-04}} *[http://www.offsetopportunity.com/ The Carbon Offset Opportunity Program: A Tool for Collaborative Carbon Sequestration Project Development] *[http://sequestration.mit.edu/ Carbon Capture and Sequestration Technologies Program at MIT] *[http://www.co2captureandstorage.info/ International industry R&D group focussed on CO<sub>2</sub> sequestration] *[http://www.co2captureproject.org/reports/reports.htm CO<sub>2</sub> Capture Project] *[http://www.princeton.edu/~cmi/ Carbon Mitigation Initiative] *[http://www.sseb.org/currentprograms/cpa_cmi.htm Southeast Regional Carbon Sequestration Partnership (SECARB)] *[http://www.abc.net.au/catalyst/stories/s1195633.htm 'Catalyst' on Australian science TV on geosequestration] *[http://www.nacarbon.org/ The U.S. North American Carbon Program] *[http://pangea.stanford.edu/~mhesse/NewsLinks.html Collection of recent news articles on CO<sub>2</sub> capture and storage] *[http://news.bbc.co.uk/2/hi/science/nature/2784227.stm Synthetic Trees Could Purify Air] *[http://www.casmgs.colostate.edu/ The Consortium for Agricultural Soil Mitigation of Greenhouse Gases] *[http://www.geos.ed.ac.uk/sccs/ Scottish Centre for Carbon Storage Research] *[http://www.ceem.unsw.edu.au/content/documents/Diesendorf_Coal-Geoseq.pdf Can geosequestration save the coal industry?] ===Research=== * [http://www.abc.net.au/catalyst/stories/s1901661.htm Short documentary on Australian research into limits on carbon uptake by trees] * [[Food and Agriculture Organization|FAO]] (2004) [http://www.fao.org/docrep/007/y5738e/y5738e00.htm Carbon sequestration in dryland soils] *IEA Reports: [http://www.ieagreen.org.uk/putcback.pdf Putting carbon back into the ground (pdf)] and [http://www.ieagreen.org.uk/oceanrep.pdf Ocean storage of CO<sub>2</sub> (pdf)] *Haszeldine (2005) [http://www.geos.ed.ac.uk/research/subsurface/diagenesis/CO2_sites_biofuel.pdf Deep geological CO<sub>2</sub> storage: principles, and prospecting for bio-energy disposal sites (pdf)] *The Role of Carbon in Agricultural Soils ''in'' Carbon Sequestration - A Better Alternative for Climate Change? Chapter 1: Agricultural Sinks (1999) University of Maryland [http://www.puaf.umd.edu/faculty/nelson/carbseq/pdf/1.pdf pdf format] [http://www.puaf.umd.edu/faculty/nelson/carbseq/CHAPTER%201.doc doc format] * Schlesinger, W.H. 1991. ''Biogeochemistry: An Analysis of Global Change''. Academic Press, San Diego. *[http://www.mcgill.ca/reporter/32/15/roulet/ Peat bogs may be soaking up 10 to 20% of the excess CO<sub>2</sub> generated by human activity] *[http://saga.pmel.noaa.gov/review/dms_climate.html DMS and Climate] *[http://www.ilea.org/birdsey/index.html Carbon Store in U.S. Forests] ===Action=== *[http://pangea.stanford.edu/~mhesse/NewsLinks.html Collection of recent news articles on CO<sub>2</sub> capture and storage] *[http://news.bbc.co.uk/2/hi/science/nature/3930245.stm Britain entertains the idea] *''[[Seattle Times]]'', [[20 February]] [[2004]], [http://seattletimes.nwsource.com/html/nationworld/2001861641_carbon19.html Canada pumps CO<sub>2</sub> underground]{{Dead link|url=http://seattletimes.nwsource.com/html/nationworld/2001861641_carbon19.html|date=July 2008}}(Weyburn oil field) *[http://www.csmonitor.com/2003/0624/p02s02-usgn.html United States pumps CO<sub>2</sub> underground] *Observer [[24 April]] [[2005]] [http://www.guardian.co.uk/science/2005/apr/24/environment.environment Seabed supplies a cure for global warming crisis] *[http://www.tyndall.ac.uk/publications/fact_sheets/t2_21.shtml Tyndall Centre - Assessing the potential for geological carbon sequestration in the UK] *[http://www.cnn.com/2007/TECH/science/11/29/climate.change.soda/index.html "Baking soda could help save planet" - Luminant pilot in Texas] {{Global warming}} [[Category:Carbon dioxide]] [[Category:Climate change]] [[Category:Climate forcing agents]] [[Category:Photosynthesis]] [[ar:بالوعة ثاني اكسيد الكربون]] [[de:Kohlenstoffsenke]] [[fr:Puits de carbone]] [[ja:二酸化炭素貯留]] [[no:Karbonsluk]] [[pt:Sequestro de carbono]] [[sv:Kolsänka]]