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'''Carbon dioxide''' ([[chemical formula]] '''CO<sub>2</sub>''') is a naturally occurring [[chemical compound]] composed of two [[oxygen]] [[atom]]s [[covalent bond|covalently bonded]] to a single [[carbon]] atom. It is a [[gas]] at [[standard temperature and pressure]] and exists in [[Earth's atmosphere]] in this state, as a [[trace gas]] at a concentration of 0.039% by volume.
'''Carbon dioxide''' ([[chemical formula]] '''CO<sub>2</sub>''') is a naturally occurring [[chemical compound]] composed of two [[oxygen]] [[atom]]s [[covalent bond|covalently bonded]] to a single [[carbon]] atom. It is a [[gas]] at [[standard temperature and pressure]] and exists in [[Earth's atmosphere]] in this state, as a [[trace gas]] at a concentration of 0.039% by volume.


As part of the [[carbon cycle]] known as [[photosynthesis]], [[plant]]s, [[algae]], and [[cyanobacteria]] absorb carbon dioxide, [[light]], and [[water]] to produce [[carbohydrate]] [[energy]] for themselves and [[oxygen]] as a waste product.<ref>{{cite book|author1=Donald G. Kaufman|author2=Cecilia M. Franz|title=Biosphere 2000: protecting our global environment|url=http://books.google.com/books?id=nm5FAAAAYAAJ|accessdate=11 October 2011|year=1996|publisher=Kendall/Hunt Pub. Co.|isbn=978-0-7872-0460-0}}</ref> But in darkness photosynthesis cannot occur, and during the resultant [[Cellular respiration|respiration]] small amounts of carbon dioxide are produced.<ref>[http://www.legacyproject.org/activities/foodfactories.html Food Factories]. www.legacyproject.org. Retrieved on 2011-10-10.</ref> Carbon dioxide also is a by-product of [[combustion]]; is emitted from [[volcano]]es, [[hot springs]], and [[geysers]]; and is freed from [[carbonate rock]]s by [[dissolution]].
As part of the [[carbon cycle]] known as [[photosynthesis]], [[plant]]s, [[algae]], and [[cyanobacteria]] absorb carbon dioxide, [[light]], and [[water]] to produce [[carbohydrate]] [[energy]] for themselves and [[oxygen]] as a waste product.<ref>{{cite book|author1=Donald G. Kaufman|author2=Cecilia M. Franz|title=Biosphere 2000: protecting our global environment|url=http://books.google.com/books?id=nm5FAAAAYAAJ|accessdate=11 October 2011|year=1996|publisher=Kendall/Hunt Pub. Co.|isbn=978-0-7872-0460-0}}</ref> But in darkness photosynthesis cannot occur, and during the resultant [[Cellular respiration|respiration]] small amounts of carbon dioxide are produced.<ref>[http://www.legacyproject.org/activities/foodfactories.html Food Factories]. www.legacyproject.org. Retrieved on 2011-10-10.</ref> Carbon dioxide is also produced by [[combustion]] of coal or hydrocarbons, the fermentation of liquids and the breathing of humans and animals. In addition it is emitted from [[volcano]]es, [[hot springs]], [[geysers]] and other places where the earth’s crust is thin; and is freed from [[carbonate rock]]s by [[dissolution]]. CO<sub>2</sub> is also found in lakes at depth under the sea, and commingled with oil and gas deposits.<ref>{{cite web|url=http://www.globalccsinstitute.com/publications/good-plant-design-and-operation-onshore-carbon-capture-installations-and-onshore-pipe-5|title=General Properties and Uses of Carbon Dioxid, Good Plant Design and Operation for Onshore Carbon Capture Installations and Onshore Pipelines|publisher=Energy Institute|accessdate=2012-03-14}}</ref>


{{As of|2011|11}}, [[carbon dioxide in the Earth's atmosphere]] is at a concentration of 390 [[parts per million|ppm]] by [[volume]].<ref>[ftp://ftp.cmdl.noaa.gov/ccg/co2/trends/co2_mm_mlo.txt Mauna Loa CO<sub>2</sub> annual mean data] from NOAA. "Trend" data was used. See also: [http://www.esrl.noaa.gov/gmd/ccgg/trends/ Trends in Carbon Dioxide] from NOAA.</ref> Atmospheric concentrations of carbon dioxide fluctuate slightly with the change of the seasons, driven primarily by seasonal plant growth in the [[Northern Hemisphere]]. Concentrations of carbon dioxide fall during the northern spring and summer as plants consume the gas, and rise during the northern autumn and winter as plants go dormant, die and decay. Taking all this into account, the concentration of CO<sub>2</sub> grew by about 2 ppm in 2009.<ref>{{cite web|url=http://www.esrl.noaa.gov/gmd/ccgg/trends/#mlo_growth|title=Annual Mean Growth Rate for Mauna Loa, Hawaii|work=Trends in Atmospheric Carbon Dioxide|publisher=NOAA Earth System Research Laboratory|accessdate=28 April 2010}}</ref> Carbon dioxide is a [[greenhouse gas]] as it transmits [[visible spectrum|visible light]] but absorbs strongly in the [[infrared]] and [[near-infrared]], before slowly re-emitting the infrared at the same wavelength as what was absorbed.
{{As of|2011|11}}, [[carbon dioxide in the Earth's atmosphere]] is at a concentration of 390 [[parts per million|ppm]] by [[volume]].<ref>[ftp://ftp.cmdl.noaa.gov/ccg/co2/trends/co2_mm_mlo.txt Mauna Loa CO<sub>2</sub> annual mean data] from NOAA. "Trend" data was used. See also: [http://www.esrl.noaa.gov/gmd/ccgg/trends/ Trends in Carbon Dioxide] from NOAA.</ref> Atmospheric concentrations of carbon dioxide fluctuate slightly with the change of the seasons, driven primarily by seasonal plant growth in the [[Northern Hemisphere]]. Concentrations of carbon dioxide fall during the northern spring and summer as plants consume the gas, and rise during the northern autumn and winter as plants go dormant, die and decay. Taking all this into account, the concentration of CO<sub>2</sub> grew by about 2 ppm in 2009.<ref>{{cite web|url=http://www.esrl.noaa.gov/gmd/ccgg/trends/#mlo_growth|title=Annual Mean Growth Rate for Mauna Loa, Hawaii|work=Trends in Atmospheric Carbon Dioxide|publisher=NOAA Earth System Research Laboratory|accessdate=28 April 2010}}</ref> Carbon dioxide is a [[greenhouse gas]] as it transmits [[visible spectrum|visible light]] but absorbs strongly in the [[infrared]] and [[near-infrared]], before slowly re-emitting the infrared at the same wavelength as what was absorbed.

Revision as of 01:25, 14 March 2012

Carbon dioxide
Structural formula of carbon dioxide with bond length
Ball and stick model of carbon dioxide
Ball and stick model of carbon dioxide
Spacefill model of carbon dioxide
Spacefill model of carbon dioxide
Names
Other names
Carbonic acid gas
Carbonic anhydride
Carbonic oxide
Carbon oxide
Carbon(IV) oxide
Dry ice (solid phase)
Identifiers
3D model (JSmol)
3DMet
1900390
ChEBI
ChemSpider
ECHA InfoCard 100.004.271 Edit this at Wikidata
EC Number
  • 204-696-9
E number E290 (preservatives)
989
KEGG
MeSH Carbon+dioxide
RTECS number
  • FF6400000
UNII
UN number 1013
  • InChI=1S/CO2/c2-1-3 checkY
    Key: CURLTUGMZLYLDI-UHFFFAOYSA-N checkY
  • InChI=1/CO2/c2-1-3
    Key: CURLTUGMZLYLDI-UHFFFAOYAO
  • O=C=O
  • C(=O)=O
Properties
CO2
Molar mass 44.009 g·mol−1
Appearance Colorless gas
Odor Odorless
Density 1562 kg/m3 (solid at 1 atm and −78.5 °C)
770 kg/m3 (liquid at 56 atm and 20 °C)
1.977 kg/m3 (gas at 1 atm and 0 °C)
Melting point −78.5 °C; −109.2 °F; 194.7 K
Boiling point −56.6 °C; −69.8 °F; 216.6 K
1.45 g/L at 25 °C, 100 kPa
Acidity (pKa) 6.35, 10.33
1.1120
Viscosity 0.07 cP at −78.5 °C
zero
Structure
linear
Thermochemistry
214 J·mol−1·K−1
−393.5 kJ·mol−1
Hazards
NFPA 704 (fire diamond)
NFPA 704 four-colored diamondHealth 2: Intense or continued but not chronic exposure could cause temporary incapacitation or possible residual injury. E.g. chloroformFlammability 0: Will not burn. E.g. waterInstability 0: Normally stable, even under fire exposure conditions, and is not reactive with water. E.g. liquid nitrogenSpecial hazards (white): no code
2
0
0
Related compounds
Other anions
 Carbon disulfide
Carbon diselenide
Other cations
 Silicon dioxide
Germanium dioxide
Tin dioxide
Lead dioxide
Supplementary data page
Carbon dioxide (data page)
Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa).
checkY verify (what is checkY☒N ?)

Carbon dioxide (chemical formula CO2) is a naturally occurring chemical compound composed of two oxygen atoms covalently bonded to a single carbon atom. It is a gas at standard temperature and pressure and exists in Earth's atmosphere in this state, as a trace gas at a concentration of 0.039% by volume.

As part of the carbon cycle known as photosynthesis, plants, algae, and cyanobacteria absorb carbon dioxide, light, and water to produce carbohydrate energy for themselves and oxygen as a waste product.[1] But in darkness photosynthesis cannot occur, and during the resultant respiration small amounts of carbon dioxide are produced.[2] Carbon dioxide is also produced by combustion of coal or hydrocarbons, the fermentation of liquids and the breathing of humans and animals. In addition it is emitted from volcanoes, hot springs, geysers and other places where the earth’s crust is thin; and is freed from carbonate rocks by dissolution. CO2 is also found in lakes at depth under the sea, and commingled with oil and gas deposits.[3]

As of November 2011, carbon dioxide in the Earth's atmosphere is at a concentration of 390 ppm by volume.[4] Atmospheric concentrations of carbon dioxide fluctuate slightly with the change of the seasons, driven primarily by seasonal plant growth in the Northern Hemisphere. Concentrations of carbon dioxide fall during the northern spring and summer as plants consume the gas, and rise during the northern autumn and winter as plants go dormant, die and decay. Taking all this into account, the concentration of CO2 grew by about 2 ppm in 2009.[5] Carbon dioxide is a greenhouse gas as it transmits visible light but absorbs strongly in the infrared and near-infrared, before slowly re-emitting the infrared at the same wavelength as what was absorbed.

Before the advent of human-caused release of carbon dioxide to the atmosphere, concentrations tended to increase with increasing global temperatures, acting as a positive feedback for changes induced by other processes such as orbital cycles.[6] There is a seasonal cycle in CO2 concentration associated primarily with the Northern Hemisphere growing season.[7]

Carbon dioxide has no liquid state at pressures below 5.1 standard atmospheres (520 kPa). At 1 atmosphere (near mean sea level pressure), the gas deposits directly to a solid at temperatures below −78.5 °C (−109.3 °F; 194.7 K) and the solid sublimes directly to a gas above −78.5 °C. In its solid state, carbon dioxide is commonly called dry ice.

CO2 is an acidic oxide: an aqueous solution turns litmus from blue to pink. It is the anhydride of carbonic acid, an acid which is unstable in aqueous solution, from which it cannot be concentrated. In organisms carbonic acid production is catalysed by the enzyme, carbonic anhydrase.

CO
2 + H
2O ⇌ H
2CO
3

CO2 is toxic in higher concentrations: 1% (10,000 ppm) will make some people feel drowsy.[8] Concentrations of 7% to 10% cause dizziness, headache, visual and hearing dysfunction, and unconsciousness within a few minutes to an hour.[9]

Chemical and physical properties

Structure and bonding

The carbon dioxide molecule is linear and centrosymmetric. The two C-O bonds are equivalent and are short (116.3 pm), consistent with double bonding.[10] Since it is centrosymmetric, the molecule has no electrical dipole. Consistent with this fact, only two vibrational bands are observed in the IR spectrum - an antisymmetic stretching mode at 2349 cm-1 and a bending mode near 666 cm-1. There is also a symmetric stretching mode at 1388 cm-1 which is only observed in the Raman spectrum.

In aqueous solution

Carbon dioxide is soluble in water, in which it reversibly converts to H
2CO
3 (carbonic acid). The relative concentrations of CO
2, H
2CO
3, and the deprotonated forms HCO−
3 (bicarbonate) and CO2−
3(carbonate) depend on the pH. In neutral or slightly alkaline water (pH > 6.5), the bicarbonate form predominates (>50%) becoming the most prevalent (>95%) at the pH of seawater. In very alkaline water (pH > 10.4), the predominant (>50%) form is carbonate. The oceans, being mildly alkaline with typical pH = 8.2 – 8.5, contain about 120 mg of bicarbonate per liter.

Being diprotic, carbonic acid has two acid dissociation constants, the first one for the dissociation into the bicarbonate (also called hydrogen carbonate) ion (HCO3−):

H2CO3 ⇌ HCO3− + H+
Ka1 = 2.5×10−4 ; pKa1 = 3.6 at 25 °C.[10]

At high pH, the bicarbonate ion dissociates significantly into the carbonate ion (CO32−):

HCO3− ⇌ CO32− + H+
Ka2 = 4.69×10−11 ; pKa2 = 10.329

Chemical reactions of CO2

Overall, CO2 is a weak electrophile. Its reaction with basic water illustrates this property, in which case hydroxide is the nucleophile. Other nucleophiles react as well. For example, carbanions as provided by Grignard reagents and organolithium compounds react with CO2 to give carboxylates:

MR + CO2 → RCO2M (where M = Li or MgBr and R = alkyl or aryl).

In metal carbon dioxide complexes, CO2 serves as a ligand, which can facilitate the conversion of CO2 to other chemicals.[11]

The reduction of CO2 to CO is ordinarily a difficult and slow reaction:

CO2 + 2 e- + 2H+ → CO + H2O

The redox potential for this reaction near pH 7 is about -0.53 V vs NHE. The nickel-containing enzyme carbon monoxide dehydrogenase catalyses this process.[12]

Physical properties

Carbon dioxide pressure-temperature phase diagram showing the triple point and critical point of carbon dioxide
Sample of solid carbon dioxide or "dry ice" pellets
Further information: Carbon dioxide (data page)

Carbon dioxide is colorless. At low concentrations, the gas is odorless. At higher concentrations it has a sharp, acidic odor.

At standard temperature and pressure, the density of carbon dioxide is around 1.98 kg/m3, about 1.5 times that of air. At atmospheric pressure and a temperature of −78.51 °C (−109.32 °F), carbon dioxide changes directly from a solid phase to a gaseous phase through sublimation, or from gaseous to solid through deposition.

Liquid carbon dioxide forms only at pressures above 5.1 atm; the triple point of carbon dioxide is about 518 kPa at −56.6 °C (see phase diagram, above). The critical point is 7.38 MPa at 31.1 °C.[13] Another form of solid carbon dioxide observed at high pressure is an amorphous glass-like solid.[14] This form of glass, called carbonia, is produced by supercooling heated CO2 at extreme pressure (40–48 GPa or about 400,000 atmospheres) in a diamond anvil. This discovery confirmed the theory that carbon dioxide could exist in a glass state similar to other members of its elemental family, like silicon (silica glass) and germanium dioxide. Unlike silica and germania glasses, however, carbonia glass is not stable at normal pressures and reverts to gas when pressure is released.

See also: Supercritical carbon dioxide, dry ice, and MO diagram

History

Crystal structure of dry ice

Carbon dioxide was one of the first gases to be described as a substance distinct from air. In the seventeenth century, the Flemish chemist Jan Baptist van Helmont observed that when he burned charcoal in a closed vessel, the mass of the resulting ash was much less than that of the original charcoal. His interpretation was that the rest of the charcoal had been transmuted into an invisible substance he termed a "gas" or "wild spirit" (spiritus sylvestre).[citation needed]

The properties of carbon dioxide were studied more thoroughly in the 1750s by the Scottish physician Joseph Black. He found that limestone (calcium carbonate) could be heated or treated with acids to yield a gas he called "fixed air." He observed that the fixed air was denser than air and supported neither flame nor animal life. Black also found that when bubbled through an aqueous solution of lime (calcium hydroxide), it would precipitate calcium carbonate. He used this phenomenon to illustrate that carbon dioxide is produced by animal respiration and microbial fermentation. In 1772, English chemist Joseph Priestley published a paper entitled Impregnating Water with Fixed Air in which he described a process of dripping sulfuric acid (or oil of vitriol as Priestley knew it) on chalk in order to produce carbon dioxide, and forcing the gas to dissolve by agitating a bowl of water in contact with the gas.[15] This was the invention of Soda water.

Carbon dioxide was first liquefied (at elevated pressures) in 1823 by Humphry Davy and Michael Faraday.[16] The earliest description of solid carbon dioxide was given by Charles Thilorier, who in 1834 opened a pressurized container of liquid carbon dioxide, only to find that the cooling produced by the rapid evaporation of the liquid yielded a "snow" of solid CO2.[17]

Isolation and production

Carbon dioxide is mainly produced as an unrecovered side product of four technologies: combustion of fossil fuels, production of hydrogen by steam reforming, ammonia synthesis, and fermentation. It can be obtained by or from air distillation, however, this method is inefficient.

The combustion of all carbon-containing fuels, such as methane (natural gas), petroleum distillates (gasoline, diesel, kerosene, propane), but also of coal and wood, will yield carbon dioxide and, in most cases, water. As an example the chemical reaction between methane and oxygen is given below.

CH
4+ 2 O
2→ CO
2+ 2 H
2O

The production of quicklime (CaO), a compound that enjoys widespread use, involves the heating (calcining) of limestone at about 850 °C:

CaCO
3→ CaO + CO
2

Iron is reduced from its oxides with coke in a blast furnace, producing pig iron and carbon dioxide:[18]

Fe
2O
3+ 3 CO → 2 Fe + 3 CO
2

Yeast metabolizes sugar to produce carbon dioxide and ethanol, also known as alcohol, in the production of wines, beers and other spirits, but also in the production of bioethanol:

C
6H
12O
6 → 2 CO
2+ 2 C
2H
5OH

All aerobic organisms produce CO
2 when they oxidize carbohydrates, fatty acids, and proteins in the mitochondria of cells. The large number of reactions involved are exceedingly complex and not described easily. Refer to (cellular respiration, anaerobic respiration and photosynthesis). The equation for the respiration of glucose and other monosachharides is:

C
6H
12O
6 + 6 O
2 → 6 CO
2 + 6 H
2O

Photoautotrophs (i.e. plants, cyanobacteria) use another modus operandi: Plants absorb CO
2 from the air, and, together with water, react it to form carbohydrates:

nCO2 + nH
2O → (CH
2O)n + nO
2

Laboratory methods

A variety of chemical routes to carbon dioxide are known, such as the reaction between most acids and most metal carbonates. For example, the reaction between hydrochloric acid and calcium carbonate (limestone or chalk) is depicted below:

2 HCl+ CaCO
3→ CaCl
2+ H
2CO
3

The carbonic acid (H2CO3) then decomposes to water and CO2. Such reactions are accompanied by foaming or bubbling, or both. In industry such reactions are widespread because they can be used to neutralize waste acid streams.

Industrial production

Industrial carbon dioxide can be produced by several methods, many of which are practiced at various scales.[19] In its dominant route, carbon dioxide is produced as a side product of the industrial production of ammonia and hydrogen. These processes begin with the reaction of water and natural gas (mainly methane).[20]

Although carbon dioxide is not often recovered, carbon dioxide results from combustion of fossil fuels and wood as well fermentation of sugar in the brewing of beer, whisky and other alcoholic beverages. It also results from thermal decomposition of limestone, CaCO
3, in the manufacture of lime (Calcium oxide, CaO). Directly from natural carbon dioxide springs, where it is produced by the action of acidified water on limestone or dolomite.

Uses

Carbon dioxide bubbles in a soft drink.

Carbon dioxide is used by the food industry, the oil industry, and the chemical industry.[19]

Precursor to chemicals

In the chemical industry, carbon dioxide is mainly consumed as an ingredient in the production of urea and methanol. Metal carbonates and bicarbonates, as well as some carboxylic acids derivatives (e.g., sodium salicylate) are prepared from CO2.

Foods

Carbon dioxide is a food additive used as a propellant and acidity regulator in the food industry. It is approved for usage in the EU[21] (listed as E number E290), USA[22] and Australia and New Zealand[23] (listed by its INS number 290).

A candy called Pop Rocks is pressurized with carbon dioxide gas at about 40 bar (580 psi). When placed in the mouth, it dissolves (just like other hard candy) and releases the gas bubbles with an audible pop.

Leavening agents cause dough to rise by producing carbon dioxide. Baker's yeast produces carbon dioxide by fermentation of sugars within the dough, while chemical leaveners such as baking powder and baking soda release carbon dioxide when heated or if exposed to acids.

Beverages

Carbon dioxide is used to produce carbonated soft drinks and soda water. Traditionally, the carbonation in beer and sparkling wine came about through natural fermentation, but many manufacturers carbonate these drinks with carbon dioxide recovered from the fermentation process. In the case of bottled and kegged beer, recycled carbon dioxide carbonation is the most common method used. With the exception of British Real Ale, draught beer is usually transferred from kegs in a cold room or cellar to dispensing taps on the bar using pressurized carbon dioxide, sometimes mixed with nitrogen.

Wine making

Carbon dioxide in the form of dry ice is often used in the wine making process to cool down bunches of grapes quickly after picking to help prevent spontaneous fermentation by wild yeasts. The main advantage of using dry ice over regular water ice is that it cools the grapes without adding any additional water that may decrease the sugar concentration in the grape must, and therefore also decrease the alcohol concentration in the finished wine.

Dry ice is also used during the cold soak phase of the wine making process to keep grapes cool. The carbon dioxide gas that results from the sublimation of the dry ice tends to settle to the bottom of tanks because it is heavier than air. The settled carbon dioxide gas creates a hypoxic environment which helps to prevent bacteria from growing on the grapes until it is time to start the fermentation with the desired strain of yeast.

Carbon dioxide is also used to create a hypoxic environment for carbonic maceration, the process used to produce Beaujolais wine.

Carbon dioxide is sometimes used to top up wine bottles or other storage vessels such as barrels to prevent oxidation, though it has the problem that it can dissolve into the wine, making a previously still wine slightly fizzy. For this reason, other gases such as nitrogen or argon are preferred for this process by professional wine makers.

Inert gas

It is one of the most commonly used compressed gases for pneumatic (pressurized gas) systems in portable pressure tools. Carbon dioxide also finds use as an atmosphere for welding, although in the welding arc, it reacts to oxidize most metals. Use in the automotive industry is common despite significant evidence that welds made in carbon dioxide are more brittle than those made in more inert atmospheres, and that such weld joints deteriorate over time because of the formation of carbonic acid. It is used as a welding gas primarily because it is much less expensive than more inert gases such as argon or helium. When used for MIG welding, CO2 use is sometimes referred to as MAG welding, for Metal Active Gas, as CO2 can react at these high temperatures. It tends to produce a hotter puddle than truly inert atmospheres, improving the flow characteristics. Although, this may be due to atmospheric reactions occurring at the puddle site. This is usually the opposite of the desired effect when welding, as it tends to embrittle the site, but may not be a problem for general mild steel welding, where ultimate ductility is not a major concern.

It is used in many consumer products that require pressurized gas because it is inexpensive and nonflammable, and because it undergoes a phase transition from gas to liquid at room temperature at an attainable pressure of approximately 60 bar (870 psi, 59 atm), allowing far more carbon dioxide to fit in a given container than otherwise would. Life jackets often contain canisters of pressured carbon dioxide for quick inflation. Aluminum capsules of CO2 are also sold as supplies of compressed gas for airguns, paintball markers, inflating bicycle tires, and for making carbonated water. Rapid vaporization of liquid carbon dioxide is used for blasting in coal mines. High concentrations of carbon dioxide can also be used to kill pests. Liquid carbon dioxide is used in supercritical drying of some food products and technological materials, in the preparation of specimens for scanning electron microscopy and in the decaffeination of coffee beans.

Fire extinguisher

Carbon dioxide extinguishes flames, and some fire extinguishers, especially those designed for electrical fires, contain liquid carbon dioxide under pressure. Carbon dioxide extinguishers work well on small flammable liquid and electrical fires, but not on ordinary combustible fires, as it is so dry. Carbon dioxide has also been widely used as an extinguishing agent in fixed fire protection systems for local application of specific hazards and total flooding of a protected space.[24]International Maritime Organization standards also recognize carbon dioxide systems for fire protection of ship holds and engine rooms. Carbon dioxide based fire protection systems have been linked to several deaths, because it does not support life in the concentrations used to extinguish fire (40% or so), however, it is not considered to be toxic to humans. A review of CO2 systems identified 51 incidents between 1975 and the date of the report, causing 72 deaths and 145 injuries.[25]

Super critical CO2 as solvent

See also: Supercritical carbon dioxide

Liquid carbon dioxide is a good solvent for many lipophilic organic compounds and is used to remove caffeine from coffee. Carbon dioxide has attracted attention in the pharmaceutical and other chemical processing industries as a less toxic alternative to more traditional solvents such as organochlorides. It is used by some dry cleaners for this reason (see green chemistry).

Agricultural and biological applications

Plants require carbon dioxide to conduct photosynthesis. Greenhouses may (if of large size, must) enrich their atmospheres with additional CO2 to sustain and increase plant growth.[26][27] A photosynthesis-related drop (by a factor less than two) in carbon dioxide concentration in a greenhouse compartment would kill green plants, or, at least, completely stop their growth. At very high concentrations (100 times atmospheric concentration, or greater), carbon dioxide can be toxic to animal life, so raising the concentration to 10,000 ppm (1%) or higher for several hours will eliminate pests such as whiteflies and spider mites in a greenhouse.[28] Carbon dioxide is used in greenhouses as the main carbon source for Spirulina algae.

In medicine, up to 5% carbon dioxide (130 times atmospheric concentration) is added to oxygen for stimulation of breathing after apnea and to stabilize the O
2/CO
2 balance in blood.

It has been proposed that carbon dioxide from power generation be bubbled into ponds to grow algae that could then be converted into biodiesel fuel.[29]

Oil recovery

Carbon dioxide is used in enhanced oil recovery where it is injected into or adjacent to producing oil wells, usually under supercritical conditions. This kind of production may increase original oil recovery by 7 per cent to 23 per cent further from primary extraction [30].It acts as both a pressurizing agent and, when dissolved into the underground crude oil, significantly reduces its viscosity, enabling the oil to flow more rapidly through the earth to the removal well.[31] In mature oil fields, extensive pipe networks are used to carry the carbon dioxide to the injection points.

Refrigerant

Liquid and solid carbon dioxide are important refrigerants, especially in the food industry, where they are employed during the transportation and storage of ice cream and other frozen foods. Solid carbon dioxide is called "dry ice" and is used for small shipments where refrigeration equipment is not practical. Solid carbon dioxide is always below −78.5 °C at regular atmospheric pressure, regardless of the air temperature.

Liquid carbon dioxide (industry nomenclature R744 or R-744) was used as a refrigerant prior to the discovery of R-12 and may enjoy a renaissance due to the fact that r134a contributes to climate change. Its physical properties are highly favorable for cooling, refrigeration, and heating purposes, having a high volumetric cooling capacity. Due to its operation at pressures of up to 130 bar (1880 psi), CO2 systems require highly resistant components that have already been developed for mass production in many sectors. In automobile air conditioning, in more than 90% of all driving conditions for latitudes higher than 50°, R744 operates more efficiently than systems using R-134a. Its environmental advantages (GWP of 1, non-ozone depleting, non-toxic, non-flammable) could make it the future working fluid to replace current HFCs in cars, supermarkets, hot water heat pumps, among others. Coca-Cola has fielded CO2-based beverage coolers and the U.S. Army is interested in CO2 refrigeration and heating technology.[32][33]

The global automobile industry is expected to decide on the next-generation refrigerant in car air conditioning. CO2 is one discussed option.(see Sustainable automotive air conditioning)

Coal bed methane recovery

In enhanced coal bed methane recovery, carbon dioxide is pumped into the coal seam to displace methane.[34]

Niche uses

A carbon dioxide laser.

Carbon dioxide is so inexpensive and so innocuous, that it finds many small uses that represent what might be called niche uses. For example it is used in the carbon dioxide laser, which is one of the earliest type of lasers.

Carbon dioxide can be used as a mean of controlling the pH of swimming pools, by continuously adding gas to the water, thus keeping the pH level from rising. Among the advantages of this is the avoidance of handling (more hazardous) acids. Similarly, it is also used in the maintaining reef aquaria, where it is commonly used in calcium reactors to temporarily lower the pH of water being passed over calcium carbonate in order to allow the calcium carbonate to dissolve into the water more freely where it is used by some corals to build their skeleton.

In the Earth's atmosphere

The Keeling Curve of atmospheric CO2 concentrations measured at Mauna Loa Observatory.
Main article: Carbon dioxide in Earth's atmosphere
Main article: Carbon cycle

Carbon dioxide in earth's atmosphere is considered a trace gas currently occurring at an average concentration of about 390 parts per million by volume or 591 parts per million by mass.[35] The total mass of atmospheric carbon dioxide is 3.16×1015 kg (about 3,000 gigatonnes). Its concentration varies seasonally (see graph at right) and also considerably on a regional basis, especially near the ground. In urban areas concentrations are generally higher and indoors they can reach 10 times background levels. Carbon dioxide is a greenhouse gas.

Yearly increase of atmospheric CO2: In the 1960s, the average annual increase was 37% of the 2000–2007 average.[36]

Five hundred million years ago carbon dioxide was 20 times more prevalent than today, decreasing to 4–5 times during the Jurassic period and then slowly declining with a particularly swift reduction occurring 49 million years ago.[37][38] Human activities such as the combustion of fossil fuels and deforestation have caused the atmospheric concentration of carbon dioxide to increase by about 35% since the beginning of the age of industrialization.[39]

Up to 40% of the gas emitted by some volcanoes during subaerial eruptions is carbon dioxide.[40] It is estimated that volcanoes release about 130–230 million tonnes (145–255 million tons) of CO2 into the atmosphere each year. Carbon dioxide is also produced by hot springs such as those at the Bossoleto site near Rapolano Terme in Tuscany, Italy. Here, in a bowl-shaped depression of about 100 m diameter, local concentrations of CO2 rise to above 75% overnight, sufficient to kill insects and small animals, but it warms rapidly when sunlit and the gas is dispersed by convection during the day.[41] Locally high concentrations of CO2, produced by disturbance of deep lake water saturated with CO2 are thought to have caused 37 fatalities at Lake Monoun, Cameroon in 1984 and 1700 casualties at Lake Nyos, Cameroon in 1986.[42] Emissions of CO2 by human activities are currently more than 130 times greater than the quantity emitted by volcanoes, amounting to about 27 billion tonnes per year.[43]

In the oceans

Main article: Carbon cycle

Carbon dioxide dissolves in the ocean to form carbonic acid (H2CO3), bicarbonate (HCO3-) and carbonate (CO32-), and there is about fifty times as much carbon dissolved in the sea water of the oceans as exists in the atmosphere. The oceans act as an enormous carbon sink, and have taken up about a third of CO2 emitted by human activity.[44]

As the concentration of carbon dioxide increases in the atmosphere, the increased uptake of carbon dioxide into the oceans is causing a measurable decrease in the pH of the oceans which is referred to as ocean acidification. Although the natural absorption of CO
2 by the world's oceans helps mitigate the climatic effects of anthropogenic emissions of CO
2, results in a decrease in the pH of the oceans. This reduciton in pH impacts the biological systems in the oceans, primarily oceanic calcifying organisms. These impacts span the food chain from autotrophs to heterotrophs and include organisms such as coccolithophores, corals, foraminifera, echinoderms, crustaceans and molluscs. Under normal conditions, calcite and aragonite are stable in surface waters since the carbonate ion is at supersaturating concentrations. However, as ocean pH falls, so does the concentration of this ion, and when carbonate becomes undersaturated, structures made of calcium carbonate are vulnerable to dissolution. Even if there is no change in the rate of calcification, therefore, the rate of dissolution of calcareous material increases.[45]

Research has already found that corals,[46][47][48] coccolithophore algae,[49][50][51][52] coralline algae,[53] foraminifera,[54] shellfish[55] and pteropods[56][57] experience reduced calcification or enhanced dissolution when exposed to elevated CO
2.

Gas solubility decreases as the temperature of water increases (except when both pressure exceeds 300 bar and temperature exceeds 393 K, only found near deep geothermal vents)[58] and therefore the rate of uptake from the atmosphere decreases as ocean temperatures rise.

Most of the CO2 taken up by the ocean, which is about 30% of the total released into the atmosphere,[59] forms carbonic acid in equilibrium with bicarbonate. Some of these chemical species are consumed by photosynthestic organisms, that remove carbon from the cycle. Increased CO2 in the atmosphere has led to decreasing alkalinity of seawater, and there is concern that this may adversely affect organisms living in the water. In particular, with decreasing alkalinity, the availability of carbonates for forming shells decreases,[60] although there's evidence of increased shell production by certain species under increased CO2 content.[61]

NOAA states in their May 2008 "State of the science fact sheet for ocean acidification" that:
"The oceans have absorbed about 50% of the carbon dioxide (CO2) released from the burning of fossil fuels, resulting in chemical reactions that lower ocean pH. This has caused an increase in hydrogen ion (acidity) of about 30% since the start of the industrial age through a process known as “ocean acidification.” A growing number of studies have demonstrated adverse impacts on marine organisms, including:

  • The rate at which reef-building corals produce their skeletons decreases, while production of numerous varieties of jellyfish increases.
  • The ability of marine algae and free-swimming zooplankton to maintain protective shells is reduced.
  • The survival of larval marine species, including commercial fish and shellfish, is reduced."

Also, the Intergovernmental Panel on Climate Change (IPCC) writes in their Climate Change 2007: Synthesis Report:[62]
"The uptake of anthropogenic carbon since 1750 has led to the ocean becoming more acidic with an average decrease in pH of 0.1 units. Increasing atmospheric CO2 concentrations lead [sic] to further acidification [...] While the effects of observed ocean acidification on the marine biosphere are as yet undocumented, the progressive acidification of oceans is expected to have negative impacts on marine shell-forming organisms (e.g. corals) and their dependent species."

Some marine calcifying organisms (including coral reefs) have been singled out by major research agencies, including NOAA, OSPAR commission, NANOOS and the IPCC, because their most current research shows that ocean acidification should be expected to impact them negatively.[63]

Carbon dioxide is also introduced into the oceans through hydrothermal vents. The Champagne hydrothermal vent, found at the Northwest Eifuku volcano at Marianas Trench Marine National Monument, produces almost pure liquid carbon dioxide, one of only two known sites in the world.[64]

Biological role

Carbon dioxide is an end product in organisms that obtain energy from breaking down sugars, fats and amino acids with oxygen as part of their metabolism, in a process known as cellular respiration. This includes all plants, animals, many fungi and some bacteria. In higher animals, the carbon dioxide travels in the blood from the body's tissues to the lungs where it is exhaled. In plants using photosynthesis, carbon dioxide is absorbed from the atmosphere.


Photosynthesis and carbon fixation

Overview of photosynthesis and respiration. Carbon dioxide (at right), together with water, form oxygen and organic compounds (at left) by photosynthesis, which can be respired to water and (CO2).
Figure 2. Overview of the Calvin cycle and carbon fixation

Carbon fixation is the removal of carbon dioxide from the air and its incorporation into solid compounds. Plants, algae, and many species of bacteria (cyanobacteria) fix carbon and create their own food by photosynthesis. Photosynthesis uses carbon dioxide and water to produce sugars and occasionally other organic compounds, releasing oxygen as a waste product.

Ribulose-1,5-bisphosphate carboxylase oxygenase, commonly known by the shorter name RuBisCO, is an enzyme involved in the first major step of carbon fixation, a process by which atmospheric carbon dioxide is converted by plants to energy-rich molecules such as glucose. It is also thought to be the single most abundant protein on Earth.[65]

These phototrophs use the products of their photosynthesis as internal food sources and as raw material for the construction of more complex organic molecules, such as polysaccharides, nucleic acids and proteins. These are used for their own growth, and also as the basis for the food chains and webs whereby other organisms, including animals such as ourselves, are fed. Some important phototrophs, the coccolithophores synthesise hard calcium carbonate scales. A globally significant species of coccolithophore is Emiliania huxleyi whose calcite scales have formed the basis of many sedimentary rocks such as limestone, where what was previously atmospheric carbon can remain fixed for geological timescales.

Plants can grow up to 50 percent faster in concentrations of 1,000 ppm CO2 when compared with ambient conditions, though this assumes no change in climate and no limitation on other nutrients.[66] Research has shown that elevated CO2 levels cause increased growth reflected in the harvestable yield of crops, with wheat, rice and soybean all showing increases in yield of 12–14% under elevated CO2 in FACE experiments.[67][68]

Studies have shown that increased CO2 leads to fewer stomata developing on plants[69] which leads to reduced water usage.[70] Studies using FACE have shown that increases in CO2 lead to decreased concentration of micronutrients in crop plants.[71] This may have knock-on effects on other parts of ecosystems as herbivores will need to eat more food to gain the same amount of protein.[72]

Plants also emit CO2 during respiration, and so the majority of plants and algae, which use C3 photosynthesis, are only net absorbers during the day. Though a growing forest will absorb many tons of CO2 each year, the World Bank writes that a mature forest will produce as much CO2 from respiration and decomposition of dead specimens (e.g., fallen branches) as is used in biosynthesis in growing plants.[73] However six experts in biochemistry, biogeology, forestry and related areas writing in the science journal Nature that "Our results demonstrate that old-growth forests can continue to accumulate carbon, contrary to the long-standing view that they are carbon neutral." [74] Mature forests are valuable carbon sinks, helping maintain balance in the Earth's atmosphere. Additionally, and crucially to life on earth, photosynthesis by phytoplankton consumes dissolved CO2 in the upper ocean and thereby promotes the absorption of CO2 from the atmosphere.[75]

Toxicity

See also: Carbon dioxide poisoning
Main symptoms of carbon dioxide toxicity, by increasing volume percent in air.[8]

Carbon dioxide content in fresh air (averaged between sea-level and 10 kPa level, i.e., about 30 km altitude) varies between 0.036% (360 ppm) and 0.039% (390 ppm), depending on the location.[76]

Adaptation to increased levels of CO2 occurs in humans. Continuous inhalation of CO2 can be tolerated at three percent inspired concentrations for at least one month and four percent inspired concentrations for over a week. It was suggested that 2.0 percent inspired concentrations could be used for closed air spaces (e.g. a submarine) since the adaptation is physiological and reversible. Decrement in performance or in normal physical activity does not happen at this level.[77][78] However, it should be noted that submarines have carbon dioxide scrubbers which reduce a significant amount of the CO2 present.[79]

Acute carbon dioxide toxicity is sometimes known by the names given to it by miners: blackdamp (also called choke damp or stythe). Blackdamp is primarily nitrogen and carbon dioxide and kills via suffocation (having displaced oxygen). Miners would try to alert themselves to dangerous levels of blackdamp and other gasses in a mine shaft by bringing a caged canary with them as they worked. The canary is more sensitive to environmental gasses than humans and as it became unconscious would stop singing and fall off its perch. The Davy lamp could also detect high levels of blackdamp (which collect near the floor) by burning less brightly, while methane, another suffocating gas and explosion risk would make the lamp burn more brightly).

Carbon dioxide differential above outdoor levels at steady state conditions (when the occupancy and ventilation system operation are sufficiently long that CO2 concentration has stabilized) are sometimes used to estimate ventilation rates per person. CO2 is considered to be a surrogate for human bio-effluents and may correlate with other indoor pollutants. Higher CO2 concentrations are associated with occupant health, comfort and performance degradation. ASHRAE Standard 62.1–2007 ventilation rates may result in indoor levels up to 2,100 ppm above ambient outdoor conditions. Thus if the outdoor ambient is 400 ppm, indoor levels may reach 2,500 ppm with ventilation rates that meet this industry consensus standard. Levels in poorly ventilated spaces can be found even higher than this (range of 3,000 or 4,000).

Human physiology

Content

The body produces approximately 2.3 pounds (1 kg) of carbon dioxide per day per person.[80]

In humans, this carbon dioxide is carried through the venous system and is breathed out through the lungs. Therefore, the carbon dioxide content in the body is high in the venous system, and decreases in the respiratory system, resulting in lower levels along any arterial system. Carbon dioxide content in this sense is often given as the partial pressure, which is the pressure which carbon dioxide would have had if it alone occupied the volume.[81]

In humans, the carbon dioxide contents are as follows:

Reference ranges or averages for partial pressures of carbon dioxide (abbreviated PCO2)
Unit Venous blood gas Alveolar pulmonary
gas pressures		 Arterial blood carbon dioxide
kPa 5.5[82]-6.8[82] 4.8 4.7[82]-6.0[82]
mmHg 41[83]-51[83] 36 35[84]-45[84]

Transport in the blood

CO2 is carried in blood in three different ways. (The exact percentages vary depending whether it is arterial or venous blood).

Hemoglobin, the main oxygen-carrying molecule in red blood cells, carries both oxygen and carbon dioxide. However, the CO2 bound to hemoglobin does not bind to the same site as oxygen. Instead, it combines with the N-terminal groups on the four globin chains. However, because of allosteric effects on the hemoglobin molecule, the binding of CO2 decreases the amount of oxygen that is bound for a given partial pressure of oxygen. The decreased binding to carbon dioxide in the blood due to increased oxygen levels is known as the Haldane Effect, and is important in the transport of carbon dioxide from the tissues to the lungs. Conversely, a rise in the partial pressure of CO2 or a lower pH will cause offloading of oxygen from hemoglobin, which is known as the Bohr Effect.

Regulation of respiration

Carbon dioxide is one of the mediators of local autoregulation of blood supply. If its levels are high, the capillaries expand to allow a greater blood flow to that tissue.

Bicarbonate ions are crucial for regulating blood pH. A person's breathing rate influences the level of CO2 in their blood. Breathing that is too slow or shallow causes respiratory acidosis, while breathing that is too rapid leads to hyperventilation, which can cause respiratory alkalosis.

Although the body requires oxygen for metabolism, low oxygen levels normally do not stimulate breathing. Rather, breathing is stimulated by higher carbon dioxide levels. As a result, breathing low-pressure air or a gas mixture with no oxygen at all (such as pure nitrogen) can lead to loss of consciousness without ever experiencing air hunger. This is especially perilous for high-altitude fighter pilots. It is also why flight attendants instruct passengers, in case of loss of cabin pressure, to apply the oxygen mask to themselves first before helping others; otherwise, one risks losing consciousness.[85]

The respiratory centers try to maintain an arterial CO2 pressure of 40 mm Hg. With intentional hyperventilation, the CO2 content of arterial blood may be lowered to 10–20 mm Hg (the oxygen content of the blood is little affected), and the respiratory drive is diminished. This is why one can hold one's breath longer after hyperventilating than without hyperventilating. This carries the risk that unconsciousness may result before the need to breathe becomes overwhelming, which is why hyperventilation is particularly dangerous before free diving.

See also

References

  1. ^ Donald G. Kaufman; Cecilia M. Franz (1996). Biosphere 2000: protecting our global environment. Kendall/Hunt Pub. Co. ISBN 978-0-7872-0460-0. Retrieved 11 October 2011.
  2. ^ Food Factories. www.legacyproject.org. Retrieved on 2011-10-10.
  3. ^ "General Properties and Uses of Carbon Dioxid, Good Plant Design and Operation for Onshore Carbon Capture Installations and Onshore Pipelines". Energy Institute. Retrieved 2012-03-14.
  4. ^ Mauna Loa CO2 annual mean data from NOAA. "Trend" data was used. See also: Trends in Carbon Dioxide from NOAA.
  5. ^ "Annual Mean Growth Rate for Mauna Loa, Hawaii". Trends in Atmospheric Carbon Dioxide. NOAA Earth System Research Laboratory. Retrieved 28 April 2010.
  6. ^ Attention: This template ({{cite doi}}) is deprecated. To cite the publication identified by doi: 10.1038/329414a0 , please use {{cite journal}} (if it was published in a bona fide academic journal, otherwise {{cite report}} with |doi= 10.1038/329414a0 instead.
  7. ^ Enting, I.G., 1987: Interannual variation in the seasonal cycle of carbon dioxide concentration at Mauna Loa. Journal of Geophysical Research 92:D5, 5497–5504.
  8. ^ a b Cite error: The named reference friedman was invoked but never defined (see the help page).
  9. ^ "Carbon Dioxide as a Fire Suppressant: Examining the Risks". U.S. Environmental Protection Agency:.{{cite news}}: CS1 maint: extra punctuation (link)
  10. ^ a b Greenwood, Norman N.; Earnshaw, Alan (1997). Chemistry of the Elements (2nd ed.). Butterworth-Heinemann. ISBN 978-0-08-037941-8.
  11. ^ M. Aresta (Ed.) "Carbon Dioxide as a Chemical Feedstock" 2010, Wiley-VCH: Weinheim. ISBN 978-3-527-32475-0
  12. ^ Colin Finn, Sorcha Schnittger, Lesley J. Yellowlees, Jason B. Love "Molecular approaches to the electrochemical reduction of carbon dioxide" Chemical Communications 2011, 0000. doi:10.1039/c1cc15393e
  13. ^ "Phase change data for Carbon dioxide". National Institute of Standards and Technology. Retrieved 2008-01-21.
  14. ^ Santoro, M.; Gorelli, FA; Bini, R; Ruocco, G; Scandolo, S; Crichton, WA (2006). "Amorphous silica-like carbon dioxide". Nature. 441 (7095): 857–860. Bibcode:2006Natur.441..857S. doi:10.1038/nature04879. PMID 16778885.
  15. ^ Priestley, Joseph; Hey, Wm (1772). "Observations on Different Kinds of Air". Philosophical Transactions. 62 (0): 147–264. doi:10.1098/rstl.1772.0021.
  16. ^ Davy, Humphry (1823). "On the Application of Liquids Formed by the Condensation of Gases as Mechanical Agents". Philosophical Transactions. 113 (0): 199–205. doi:10.1098/rstl.1823.0020. {{cite journal}}: |format= requires |url= (help)
  17. ^ Duane, H.D. Roller; Thilorier, M. (1952). "Thilorier and the First Solidification of a "Permanent" Gas (1835)". Isis. 43 (2): 109–113. doi:10.1086/349402.
  18. ^ Strassburger, Julius (1969). Blast Furnace Theory and Practice. New York: American Institute of Mining, Metallurgical, and Petroleum Engineers. ISBN 0677104200.
  19. ^ a b Pierantozzi, Ronald (2001). "Carbon Dioxide". Kirk-Othmer Encyclopedia of Chemical Technology. Wiley. doi:10.1002/0471238961.0301180216090518.a01.pub2.
  20. ^ Susan Topham "Carbon Dioxide" in Ullmann's Encyclopedia of Industrial Chemistry, 2005, Wiley-VCH, Weinheim. doi:10.1002/14356007.a05_165
  21. ^ UK Food Standards Agency: "Current EU approved additives and their E Numbers". Retrieved 2011-10-27.
  22. ^ US Food and Drug Administration: "Listing of Food Additives Status Part I". Retrieved 2011-10-27.
  23. ^ Australia New Zealand Food Standards Code"Standard 1.2.4 - Labelling of ingredients". Retrieved 2011-10-27.
  24. ^ National Fire Protection Association Code 12
  25. ^ Carbon Dioxide as a Fire Suppressant: Examining the Risks, US EPA
  26. ^ Plant Growth Factors: Photosynthesis, Respiration, and Transpiration. Ext.colostate.edu. Retrieved on 2011-10-10.
  27. ^ Carbon dioxide. Formal.stanford.edu. Retrieved on 2011-10-10.
  28. ^ Stafford, Ned (2007). "Future crops: The other greenhouse effect". Nature. 448 (7153): 7153. Bibcode:2007Natur.448..526S. doi:10.1038/448526a. PMID 17671477.
  29. ^ Clayton, Mark (2006-01-11). "Algae – like a breath mint for smokestacks". Christian Science Monitor. Retrieved 2007-10-11.
  30. ^ "CO2 for use in enhanced oil recovery (EOR)". Global CCS Institute. Retrieved 2012-02-25.
  31. ^ Austell, J Michael (2005). "CO2 for Enhanced Oil Recovery Needs – Enhanced Fiscal Incentives". Exploration & Production: the Oil & Gas Review. Retrieved 2007-09-28.
  32. ^ "The Coca-Cola Company Announces Adoption of HFC-Free Insulation in Refrigeration Units to Combat Global Warming". The Coca-Cola Company. 2006-06-05. Retrieved 2007-10-11.
  33. ^ "Modine reinforces its CO2 research efforts". R744.com. 2007-06-28.
  34. ^ "Enhanced coal bed methane recovery". ETH Zurich. 2006-08-31.
  35. ^ NOAA ESRL, Trends in Carbon Dioxide, accessed 2010.06
  36. ^ Dr. Pieter Tans (3 May 2008) "Annual CO2 mole fraction increase (ppm)" for 1959–2007 National Oceanic and Atmospheric Administration Earth System Research Laboratory, Global Monitoring Division (additional details.)
  37. ^ "Climate and CO2 in the Atmosphere". Retrieved 2007-10-10.
  38. ^ Berner, Robert A.; Kothavala, Zavareth (2001). "GEOCARB III: A revised model of atmospheric CO2 over Phanerozoic Time" (PDF). American Journal of Science. 301 (2): 182–204. doi:10.2475/ajs.301.2.182. Retrieved 2008-02-15.
  39. ^ "After two large annual gains, rate of atmospheric CO2 increase returns to average". NOAA News Online, Story 2412. 2005-03-31.
  40. ^ Sigurdsson, Haraldur (2000). Encyclopedia of volcanoes. San Diego: Academic Press. ISBN 012643140X. {{cite book}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  41. ^ van Gardingen, P.R. (1997). "Long-term effects of enhanced CO2 concentrations on leaf gas exchange: research opportunities using CO2 springs". In Raschi, A.; Miglietta, F.; Tognetti, R.; van Gardingen, P.R. (Eds.) (ed.). Plant responses to elevated CO2: Evidence from natural springs. Cambridge: Cambridge University Press. pp. 69–86. ISBN 0521582032. {{cite book}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)CS1 maint: multiple names: editors list (link)
  42. ^ Martini, M. (1997). "CO2 emissions in volcanic areas: case histories and hazaards". In Raschi, A.; Miglietta, F.; Tognetti, R.; van Gardingen, P.R. (Eds.) (ed.). Plant responses to elevated CO2: Evidence from natural springs. Cambridge: Cambridge University Press. pp. 69–86. ISBN 0521582032.{{cite book}}: CS1 maint: multiple names: editors list (link)
  43. ^ "Volcanic Gases and Their Effects". Retrieved 2007-09-07.
  44. ^ Doney, Scott C. (2006-11-29). "How Long Can the Ocean Slow Global Warming?". Oceanus. Retrieved 2007-11-21. {{cite web}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  45. ^ Nienhuis, S.; Palmer, A.; Harley, C. (2010). "Elevated CO2 affects shell dissolution rate but not calcification rate in a marine snail". Proceedings of the Royal Society B: Biological Sciences. 277 (1693): 2553–2558. doi:10.1098/rspb.2010.0206. PMC 2894921. PMID 20392726.
  46. ^ Gattuso, J.-P. (1998). "Effect of calcium carbonate saturation of seawater on coral calcification". Global and Planetary Change. 18 (1–2): 37–46. doi:10.1016/S0921-8181(98)00035-6. {{cite journal}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  47. ^ Gattuso, J.-P. (1999). "Photosynthesis and calcification at cellular, organismal and community levels in coral reefs: a review on interactions and control by carbonate chemistry". American Zoologist. 39: 160–183. {{cite journal}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  48. ^ Langdon, C (2005). "Effect of elevated pCO2 on photosynthesis and calcification of corals and interactions with seasonal change in temperature/irradiance and nutrient enrichment". Journal of Geophysical Research. 110 (C09S07): C09S07. Bibcode:2005JGRC..11009S07L. doi:10.1029/2004JC002576. {{cite journal}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  49. ^ Riebesell, Ulf (2000). "Reduced calcification of marine plankton in response to increased atmospheric CO
    2    ". Nature. 407 (6802): 364–367. doi:10.1038/35030078. PMID 11014189.     {{cite journal}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  50. ^ Zondervan, I. (2001). "Decreasing marine biogenic calcification: a negative feedback on rising atmospheric CO2". Global Biogeochemical Cycles. 15 (2): 507–516. Bibcode:2001GBioC..15..507Z. doi:10.1029/2000GB001321. {{cite journal}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  51. ^ Zondervan, I. (2002). "Effect of CO2 concentration on the PIC/POC ratio in the coccolithophore Emiliania huxleyi grown under light limiting conditions and different day lengths". Journal of Experimental Marine Biology and Ecology. 272 (1): 55–70. doi:10.1016/S0022-0981(02)00037-0. {{cite journal}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  52. ^ Delille, B. (2005). "Response of primary production and calcification to changes of pCO2 during experimental blooms of the coccolithophorid Emiliania huxleyi". Global Biogeochemical Cycles. 19 (2): GB2023. Bibcode:2005GBioC..19.2023D. doi:10.1029/2004GB002318. {{cite journal}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  53. ^ Kuffner, I.B. (2007). "Decreased abundance of crustose coralline algae due to ocean acidification". Nature Geoscience. 1 (2): 114–117. Bibcode:2008NatGe...1..114K. doi:10.1038/ngeo100. {{cite journal}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  54. ^ Phillips, Graham (2007-09-13). "Ocean Acidification – The BIG global warming story". ABC TV Science: Catalyst. Australian Broadcasting Corporation. Retrieved 2007-09-18. {{cite news}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  55. ^ Gazeau, F. (2007). "Impact of elevated CO
    2     on shellfish calcification"    . Geophysical Research Letters. 34 (7): L07603. Bibcode:2007GeoRL..3407603G. doi:10.1029/2006GL028554.     {{cite journal}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  56. ^ Cite error: The named reference orr05 was invoked but never defined (see the help page).
  57. ^ Comeau, C. (2009). "Impact of ocean acidification on a key Arctic pelagic mollusc ("Limacina helicina")". Biogeosciences. 6 (9): 1877–1882. doi:10.5194/bg-6-1877-2009. {{cite journal}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)CS1 maint: unflagged free DOI (link)
  58. ^ Duana, Zhenhao (2003). "An improved model calculating CO2 solubility in pure water and aqueous NaCl solutions from 273 to 533 K and from 0 to 2000 bar". Chemical Geology. 193: 260–271. {{cite journal}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  59. ^ Attention: This template ({{cite doi}}) is deprecated. To cite the publication identified by doi:10.1126/science.1189338, please use {{cite journal}} (if it was published in a bona fide academic journal, otherwise {{cite report}} with |doi=10.1126/science.1189338 instead.
  60. ^ Garrison, Tom (2004). Oceanography: An Invitation to Marine Science. Thomson Brooks. p. 125. ISBN 0534408877.
  61. ^ Ries, Justin B. (2009-12-01). "Marine calcifiers exhibit mixed responses to CO2-induced ocean acidification". Geology. {{cite web}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  62. ^ Climate Change 2007: Synthesis Report, IPCC
  63. ^ PMEL Ocean Acidification Home Page
  64. ^ Lupton, J.; Lilley, M.; Butterfield, D.; Evans, L.; Embley, R.; Olson, E.; Proskurowski, G.; Resing, J.; Roe, K.; Greene, R.; Lebon, G. (2004). "Liquid Carbon Dioxide Venting at the Champagne Hydrothermal Site, NW Eifuku Volcano, Mariana Arc". American Geophysical Union. Fall. Meeting (abstract #V43F-08). Bibcode:2004AGUFM.V43F..08L.{{cite journal}}: CS1 maint: multiple names: authors list (link)
  65. ^ Dhingra A, Portis AR, Daniell H (2004). "Enhanced translation of a chloroplast-expressed RbcS gene restores small subunit levels and photosynthesis in nuclear RbcS antisense plants". Proc. Natl. Acad. Sci. U.S.A. 101 (16): 6315–20. doi:10.1073/pnas.0400981101. PMC 395966. PMID 15067115. (Rubisco) is the most prevalent enzyme on this planet, accounting for 30–50% of total soluble protein in the chloroplast; {{cite journal}}: Unknown parameter |month= ignored (help)CS1 maint: multiple names: authors list (link)
  66. ^ Blom, T.J. (2002-12). "Carbon Dioxide In Greenhouses". Retrieved 2007-06-12. {{cite web}}: Check date values in: |date= (help); Unknown parameter |coauthors= ignored (|author= suggested) (help)
  67. ^ Ainsworth, Elizabeth A. (2008). "Rice production in a changing climate: a meta-analysis of responses to elevated carbon dioxide and elevated ozone concentration" (PDF). Global Change Biology. 14 (7): 1642. doi:10.1111/j.1365-2486.2008.01594.x.
  68. ^ Long, SP; Ainsworth, EA; Leakey, AD; N�sberger, J; Ort, DR (2006). "Food for thought: lower-than-expected crop yield stimulation with rising CO2 concentrations". Science. 312 (5782): 1918–21. Bibcode:2006Sci...312.1918L. doi:10.1126/science.1114722. PMID 16809532. {{cite journal}}: replacement character in |last4= at position 2 (help)
  69. ^ F. Woodward and C. Kelly (1995). "The influence of CO2 concentration on stomatal density". New Phytologist. 131 (3): 311–327. doi:10.1111/j.1469-8137.1995.tb03067.x.
  70. ^ Bert G. Drake; Gonzalez-Meler, Miquel A.; Long, Steve P. (1997). "More efficient plants: A consequence of rising atmospheric CO2?". Annual Review of Plant Physiology and Plant Molecular Biology. 48 (1): 609. doi:10.1146/annurev.arplant.48.1.609. PMID 15012276.
  71. ^ Loladze, I (2002). "Rising atmospheric CO2 and human nutrition: toward globally imbalanced plant stoichiometry?". Trends in Ecology & Evolution. 17 (10): 457. doi:10.1016/S0169-5347(02)02587-9.
  72. ^ Carlos E. Coviella and John T. Trumble (1999). "Effects of Elevated Atmospheric Carbon Dioxide on Insect-Plant Interactions". Conservation Biology. 13 (4): 700. JSTOR 2641685.
  73. ^ "Global Environment Division Greenhouse Gas Assessment Handbook – A Practical Guidance Document for the Assessment of Project-level Greenhouse Gas Emissions". World Bank. Retrieved 2007-11-10.
  74. ^ Luyssaert, Sebastiaan; Schulze, E. -Detlef; Börner, Annett; Knohl, Alexander; Hessenmöller, Dominik; Law, Beverly E.; Ciais, Philippe; Grace, John (2008). "Old-growth forests as global carbon sinks". Nature. 455 (7210): 213. Bibcode:2008Natur.455..213L. doi:10.1038/nature07276. PMID 18784722.
  75. ^ Falkowski, P.; Scholes, RJ; Boyle, E; Canadell, J; Canfield, D; Elser, J; Gruber, N; Hibbard, K; Högberg, P (2000). "The global carbon cycle: a test of our knowledge of earth as a system". Science. 290 (5490): 291–296. Bibcode:2000Sci...290..291F. doi:10.1126/science.290.5490.291. PMID 11030643.
  76. ^ "Graphical map of CO2".
  77. ^ Cite error: The named reference Glatte Jr H. A., Motsay G. J., Welch B. E. 1967 was invoked but never defined (see the help page).
  78. ^ Lambertsen, C. J. (1971). "Carbon Dioxide Tolerance and Toxicity". Environmental Biomedical Stress Data Center, Institute for Environmental Medicine, University of Pennsylvania Medical Center. IFEM. Report No. 2-71. Philadelphia, PA. Retrieved 2008-05-02.
  79. ^ How are people able to breathe inside a submarine?. Howstuffworks.com (2000-04-01). Retrieved on 2011-10-10.
  80. ^ "How much carbon dioxide do humans contribute through breathing?". Retrieved 2009-04-30.
  81. ^ Charles Henrickson (2005). Chemistry. Cliffs Notes. ISBN 0-764-57419-1.
  82. ^ a b c d Derived from mmHg values using 0.133322 kPa/mmHg
  83. ^ a b The Medical Education Division of the Brookside Associates--> ABG (Arterial Blood Gas) Retrieved on Dec 6, 2009
  84. ^ a b Normal Reference Range Table from The University of Texas Southwestern Medical Center at Dallas. Used in Interactive Case Study Companion to Pathologic basis of disease.
  85. ^ a b c d "Carbon dioxide". solarnavigator.net. Retrieved 2007-10-12.

Further reading

  • Tyler Volk (2008), CO2 Rising: The World's Greatest Environmental Challenge, The MIT Press, 223 pages, ISBN 978-0-262-22083-5. A short, balanced primer on CO2's role as a greenhouse gas. Review at Environmental Health Perspectives
  • Shendell, Prill, Fisk, Apte1, Blake & Faulkner, Associations between classroom CO2 concentrations and student attendance in Washington and Idaho, Indoor Air 2004.
  • Seppanen, Fisk and Mendell, Association of Ventilation Rates and CO2 Concentrations with Health and Other Responses in Commercial and Institutional Buildings, Indoor Air 1999.
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