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carbon monoxide +2

Carbon monoxide

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For the songs, see Carbon Monoxide (Regina Spektor song) and Carbon Monoxide (Cake song).

Carbon monoxide

  

  

Preferred IUPAC name[hide]

Carbon monoxide

  

Other names[hide]

Carbon monooxide

Carbonous oxide

Carbon(II) oxide

Carbonyl

  

Identifiers

  

CAS number

630-08-0 

PubChem

281 

ChemSpider

275 

UNII

7U1EE4V452 

EC number

211-128-3

UN number

1016

KEGG

D09706 

MeSH

Carbon+monoxide

ChEBI

CHEBI:17245 

RTECS number

FG3500000

Beilstein Reference

3587264

Gmelin Reference

421

Jmol-3D images

Image 1

SMILES

[show]

  

InChI

[show]

  

Properties

  

Molecular formula

CO

Molar mass

28.010 g/mol

Appearance

colorless gas

Odor

odorless

Density

789 kg/m3, liquid

1.250 kg/m3 at 0 °C, 1 atm

1.145 kg/m3 at 25 °C, 1 atm

Melting point

205.02 °C, 68 K, -337 °F

Boiling point

191.5 °C, 82 K, -313 °F

Solubility in water

27.6 mg/1 L (25 °C)

Solubility

soluble in chloroform, acetic acid, ethyl acetate, ethanol, ammonium hydroxide, benzene

kH

1.04 atm-m3/mol

Refractive index (nD)

1.0003364

Dipole moment

0.122 D

Thermochemistry

  

Std enthalpy of

formation ΔfHo298

110.5 kJ·mol1

Std enthalpy of

combustion ΔcHo298

283.4 kJ/mol

Standard molar

entropy So298

197.7 J·mol1·K1

Specific heat capacity, C

29.1 J/K mol

Hazards

  

MSDS

External MSDS

EU Index

006-001-00-2

EU classification

F

T+

R-phrases

R61 R12 R26 R48/23

S-phrases

S53 S45

NFPA 704

4

2

0

Flash point

191 °C (82 K; 311.8 °F)

Autoignition

temperature

609 °C (882 K; 1,128 °F)

Explosive limits

12.5–74.2%

Related compounds

  

Related carbon oxides

Carbon dioxide

Carbon suboxide

Oxocarbons

Supplementary data page

  

Structure and

properties

n, εr, etc.

Thermodynamic

data

Phase behaviour

Solid, liquid, gas

Spectral data

UV, IR, NMR, MS

   

 (verify) (what is: 

/

?)

Except where noted otherwise, data are given for materials in their standard state (at 25 °C, 100 kPa)

  

Infobox references

  

Carbon monoxide (CO) is a colorless, odorless, and tasteless gas that is slightly less dense than air. It is toxic to humans and animals when encountered in higher concentrations, although it is also produced in normal animal metabolism in low quantities, and is thought to have some normal biological functions. In the atmosphere, it is spatially variable, short lived, having a role in the formation of ground-level ozone.

Carbon monoxide consists of one carbon atom and one oxygen atom, connected by a triple bond that consists of two covalent bonds as well as one dative covalent bond. It is the simplest oxocarbon, and isoelectronic with the cyanide ion and molecular nitrogen. In coordination complexes the carbon monoxide ligand is called carbonyl.

Carbon monoxide is produced from the partial oxidation of carbon-containing compounds; it forms when there is not enough oxygen to produce carbon dioxide (CO2), such as when operating a stove or an internal combustion engine in an enclosed space. In the presence of oxygen, including atmospheric concentrations, carbon monoxide burns with a blue flame, producing carbon dioxide.[1] Coal gas, which was widely used before the 1960s for domestic lighting, cooking, and heating, had carbon monoxide as a significant fuel constituent. Some processes in modern technology, such as iron smelting, still produce carbon monoxide as a byproduct.[2]

Worldwide, the largest source of carbon monoxide is natural in origin, due to photochemical reactions in the troposphere that generate about 5×1012 kilograms per year.[3] Other natural sources of CO include volcanoes, forest fires, and other forms of combustion.

In biology, carbon monoxide is naturally produced by the action of heme oxygenase 1 and 2 on the heme from hemoglobin breakdown. This process produces a certain amount of carboxyhemoglobin in normal persons, even if they do not breathe any carbon monoxide. Following the first report that carbon monoxide is a normal neurotransmitter in 1993,[4][5] as well as one of three gases that naturally modulate inflammatory responses in the body (the other two being nitric oxide and hydrogen sulfide), carbon monoxide has received a great deal of clinical attention as a biological regulator. In many tissues, all three gases are known to act as anti-inflammatories, vasodilators, and promoters of neovascular growth.[6] Clinical trials of small amounts of carbon monoxide as a drug are ongoing.

Contents

 [hide

History[edit]

Aristotle (384–322 BC) first recorded that burning coals emanated toxic fumes. An ancient method of execution was to shut the criminal in a bathing room with smouldering coals. What was not known was the mechanism of death. Greek physician Galen (129–199 AD) speculated that there was a change in the composition of the air that caused harm when inhaled.[7] In 1776, the French chemist de Lassone produced CO by heating zinc oxide with coke, but mistakenly concluded that the gaseous product was hydrogen, as it burned with a blue flame. The gas was identified as a compound containing carbon and oxygen by the Scottish chemist William Cumberland Cruikshank in the year 1800.[8][9] Its toxic properties on dogs were thoroughly investigated by Claude Bernard around 1846.[10]

During World War II, a gas mixture including carbon monoxide was used to keep motor vehicles running in parts of the world where gasoline and diesel fuel were scarce. External (with a few exceptions) charcoal or wood gas generators were fitted, and the mixture of atmospheric nitrogen, carbon monoxide, and small amounts of other gases produced by gasification was piped to a gas mixer. The gas mixture produced by this process is known as wood gas. Carbon monoxide was also used on a small scale during the Holocaust at some Nazi extermination camps, the most notable by gas vans in Chelmno, and in the Action T4 "euthanasia" program.[11]

Molecular properties[edit]

Carbon monoxide has a molar mass of 28.0, which makes it slightly lighter than air, whose average molar mass is 28.8. According to the ideal gas law, CO is therefore less dense than air. Neither gas is "ideal", however, so neither exactly has the densities predicted by the ideal gas law.

The bond length between the carbon atom and the oxygen atom is 112.8 pm.[12][13] This bond length is consistent with a triple bond, as in molecular nitrogen (N2), which has a similar bond length and nearly the same molecular mass. Carbon–oxygen double bonds are significantly longer, 120.8 pm in formaldehyde, for example.[14] The boiling point (82 K) and melting point (68 K) are very similar to those of N2 (77 K and 63 K, respectively). The bond dissociation energy of 1072 kJ/mol is stronger than that of N2 (942 kJ/mol) and represents the strongest chemical bond known.[15]

The ground electronic state of carbon monoxide is a singlet state[16] since there are no unpaired electrons.

Bonding and dipole moment[edit]

Carbon and oxygen together have a total of 10 valence electrons in carbon monoxide. To satisfy the octet rule for the carbon, the two atoms form a triple bond, with six shared electrons in three bonding molecular orbitals, rather than the usual double bond found in organic carbonyl compounds. Since four of the shared electrons come from the oxygen atom and only two from carbon, one bonding orbital is occupied by two electrons from oxygen, forming a dative or dipolar bond. This causes a C O polarization of the molecule, with a small negative charge on carbon and a small positive charge on oxygen. The other two bonding orbitals are each occupied by one electron from carbon and one from oxygen, forming (polar) covalent bonds with a reverse C O polarization, since oxygen is more electronegative than carbon. In the free carbon monoxide, a net negative charge δ- remains at the carbon end and the molecule has a small dipole moment of 0.122 D.[17]

The molecule is therefore asymmetric: oxygen has more electron density than carbon, and is also slightly positively charged compared to carbon being negative. By contrast, the isoelectronic dinitrogen molecule has no dipole moment.

If carbon monoxide acts as a ligand, the polarity of the dipole may reverse with a net negative charge on the oxygen end, depending on the structure of the coordination complex.[18] See also the section "Coordination chemistry" below.

Bond polarity and oxidation state[edit]

Theoretical and experimental studies show that, despite the greater electronegativity of oxygen, the dipole moment points from the more-negative carbon end to the more-positive oxygen end.[19][20] The three bonds are in fact polar covalent bonds that are strongly polarized. The calculated polarization toward the oxygen atom is 71% for the σ-bond and 77% for both π-bonds.[21]

The oxidation state of carbon in carbon monoxide is +2 in each of these structures. It is calculated by counting all the bonding electrons as belonging to the more electronegative oxygen. Only the two non-bonding electrons on carbon are assigned to carbon. In this count, carbon then has only two valence electrons in the molecule compared to four in the free atom.

Biological and physiological properties[edit]

Toxicity[edit]

Main article: Carbon monoxide poisoning

Carbon monoxide poisoning is the most common type of fatal air poisoning in many countries.[22] Carbon monoxide is colorless, odorless, and tasteless, but highly toxic. It combines with hemoglobin to produce carboxyhemoglobin, which usurps the space in hemoglobin that normally carries oxygen, but is ineffective for delivering oxygen to bodily tissues. Concentrations as low as 667 ppm may cause up to 50% of the body's hemoglobin to convert to carboxyhemoglobin.[23] A level of 50% carboxyhemoglobin may result in seizure, coma, and fatality. In the United States, the OSHA limits long-term workplace exposure levels above 50 ppm.[24] Within short time scales, carbon monoxide absorption is cumulative, since the half-life is about 5 h in fresh air (see main article).

The most common symptoms of carbon monoxide poisoning may resemble other types of poisonings and infections, including symptoms such as headache, nausea, vomiting, dizziness, fatigue, and a feeling of weakness. Affected families often believe they are victims of food poisoning. Infants may be irritable and feed poorly. Neurological signs include confusion, disorientation, visual disturbance, syncope and seizures.[25]

Some descriptions of carbon monoxide poisoning include retinal hemorrhages, and an abnormal cherry-red blood hue.[26] In most clinical diagnoses these signs are seldom noticed.[25] One difficulty with the usefulness of this cherry-red effect is that it corrects, or masks, what would otherwise be an unhealthy appearance, since the chief effect of removing deoxygenated hemoglobin is to make an asphyxiated person appear more normal, or a dead person appear more lifelike, similar to the effect of red colorants in embalming fluid. The "false" or unphysiologic red-coloring effect in anoxic CO-poisoned tissue is related to the meat-coloring commercial use of carbon monoxide, discussed below.

Carbon monoxide also binds to other molecules such as myoglobin and mitochondrial cytochrome oxidase. Exposures to carbon monoxide may cause significant damage to the heart and central nervous system, especially to the globus pallidus,[27] often with long-term sequelae. Carbon monoxide may have severe adverse effects on the fetus of a pregnant woman.[28]

Normal human physiology[edit]

Carbon monoxide is produced naturally by the human body as a signaling molecule. Thus, carbon monoxide may have a physiological role in the body, such as a neurotransmitter or a blood vessel relaxant.[29] Because of carbon monoxide's role in the body, abnormalities in its metabolism have been linked to a variety of diseases, including neurodegenerations, hypertension, heart failure, and inflammation.[29]

Microbiology[edit]

Carbon monoxide is a nutrient for methanogenic bacteria,[30] a building-block for acetylcoenzyme A. This is the theme for the emerging field of bioorganometallic chemistry. Extremophile micro-organisms can, thus, metabolise carbon monoxide in such locations as the thermal vents of volcanoes.[31]

In bacteria, carbon monoxide is produced via the reduction of carbon dioxide by the enzyme carbon monoxide dehydrogenase, an Fe-Ni-S-containing protein.[32]

CooA is a carbon monoxide sensor protein.[33] The scope of its biological role is still unknown; it may be part of a signaling pathway in bacteria and archaea. Its occurrence in mammals is not established.

Occurrence[edit]

Carbon monoxide occurs in various natural and artificial environments. Typical concentrations in parts per million are as follows:

   

ppmv: parts per million by volume (note: volume fraction is equal to mole fraction for ideal gas only, see volume (thermodynamics))

  

Concentration

Source

0.1 ppmv

Natural atmosphere level (MOPITT)[35]

0.5–5 ppmv

Average level in homes[36]

5–15 ppmv

Near-properly adjusted gas stoves in homes, modern vehicle exhaust emissions[37]

17 ppmv

Atmosphere of Venus

100–200 ppmv

Exhaust from automobiles in the Mexico City central area[38]

700 ppmv

Atmosphere of Mars

5,000 ppmv

Exhaust from a home wood fire[39]

7,000 ppmv

Undiluted warm car exhaust without a catalytic converter[37]

Composition of dry atmosphere, by volume[34]

Atmospheric presence[edit]

   

The streak of red, orange, and yellow across South America, Africa, and the Atlantic Ocean in this animation points to high levels of carbon monoxide on September 30, 2005.

   

Carbon Monoxide concentrations in Northern Hemisphere spring as measured with the MOPITT instrument.

Carbon monoxide is present in small amounts in the atmosphere, chiefly as a product of volcanic activity but also from natural and man-made fires (such as forest and bushfires, burning of crop residues, and sugarcane fire-cleaning). The burning of fossil fuels also contributes to carbon monoxide production. Carbon monoxide occurs dissolved in molten volcanic rock at high pressures in the Earth's mantle.[40] Because natural sources of carbon monoxide are so variable from year to year, it is extremely difficult to accurately measure natural emissions of the gas.

Carbon monoxide has an indirect radiative forcing effect by elevating concentrations of methane and tropospheric ozone through chemical reactions with other atmospheric constituents (e.g., the hydroxyl radical, OH.) that would otherwise destroy them.[41] Through natural processes in the atmosphere, it is eventually oxidized to carbon dioxide. Carbon monoxide concentrations are both short-lived in the atmosphere and spatially variable.

In the atmosphere of Venus carbon monoxide occurs as a result of the photodissociation of carbon dioxide by electromagnetic radiation of wavelengths shorter than 169 nm.

Due to its long lifetime in the mid-troposphere, carbon monoxide is also used as tracer of transport for pollutant plumes.[42]

Urban pollution[edit]

Carbon monoxide is a temporary atmospheric pollutant in some urban areas, chiefly from the exhaust of internal combustion engines (including vehicles, portable and back-up generators, lawn mowers, power washers, etc.), but also from incomplete combustion of various other fuels (including wood, coal, charcoal, oil, paraffin, propane, natural gas, and trash).

Large CO pollution events can be observed from space over cities.[43]

Role in ground-level ozone formation[edit]

Main article: Tropospheric Ozone

Carbon monoxide is, along with aldehydes, part of the series of cycles of chemical reactions that form photochemical smog. It reacts with hydroxyl radical (OH) to produce a radical intermediate HOCO, which transfers rapidly its radical hydrogen to O2 to form peroxy radical (HO2) and carbon dioxide (CO2).[44] Peroxy radical subsequently reacts with nitrogen oxide (NO) to form nitrogen dioxide (NO2) and hydroxyl radical. NO2 gives O(3P) via photolysis, thereby forming O3 following reaction with O2. Since hydroxyl radical is formed during the formation of NO2, the balance of the sequence of chemical reactions starting with carbon monoxide and leading to the formation of ozone is:

CO + 2O2 + hν CO2 + O3

(where hν refers to the photon of light absorbed by the NO2 molecule in the sequence)

Although the creation of NO2 is the critical step leading to low level ozone formation, it also increases this ozone in another, somewhat mutually exclusive way, by reducing the quantity of NO that is available to react with ozone.[45]

Indoor pollution[edit]

In closed environments, the concentration of carbon monoxide can easily rise to lethal levels. On average, 170 people in the United States die every year from carbon monoxide produced by non-automotive consumer products.[46] However, according to the Florida Department of Health, "every year more than 500 Americans die from accidental exposure to carbon monoxide and thousands more across the U.S. require emergency medical care for non-fatal carbon monoxide poisoning"[47] These products include malfunctioning fuel-burning appliances such as furnaces, ranges, water heaters, and gas and kerosene room heaters; engine-powered equipment such as portable generators; fireplaces; and charcoal that is burned in homes and other enclosed areas. The American Association of Poison Control Centers (AAPCC) reported 15,769 cases of carbon monoxide poisoning resulting in 39 deaths in 2007.[48] In 2005, the CPSC reported 94 generator-related carbon monoxide poisoning deaths.[46] Forty-seven of these deaths were known to have occurred during power outages due to severe weather, including Hurricane Katrina.[46] Still others die from carbon monoxide produced by non-consumer products, such as cars left running in attached garages. The Centers for Disease Control and Prevention estimates that several thousand people go to hospital emergency rooms every year to be treated for carbon monoxide poisoning.[49]

Blood presence[edit]

Carbon monoxide is absorbed through breathing and enters the blood stream through gas exchange in the lungs. Normal circulating levels in the blood are 0% to 3%, and are higher in smokers. Carbon monoxide levels cannot be assessed through a physical exam. Laboratory testing requires a blood sample (arterial or venous) and laboratory analysis on a CO-Oximeter. Additionally, a noninvasive carboxyhemoglobin (SpCO) test method from Pulse CO-Oximetry exists and has been validated compared to invasive methods.[50]

Astrophysics[edit]

Outside of Earth, carbon monoxide is the second-most common molecule in the interstellar medium, after molecular hydrogen. Because of its asymmetry, the carbon monoxide molecule produces far brighter spectral lines than the hydrogen molecule, making CO much easier to detect. Interstellar CO was first detected with radio telescopes in 1970. It is now the most commonly used tracer of molecular gas in general in the interstellar medium of galaxies, as molecular hydrogen can only be detected using ultraviolet light, which requires space telescopes. Carbon monoxide observations provide much of the information about the molecular clouds in which most stars form.[51]

Production[edit]

Many methods have been developed for carbon monoxide's production.[52]

Industrial production[edit]

A major industrial source of CO is producer gas, a mixture containing mostly carbon monoxide and nitrogen, formed by combustion of carbon in air at high temperature when there is an excess of carbon. In an oven, air is passed through a bed of coke. The initially produced CO2 equilibrates with the remaining hot carbon to give CO. The reaction of CO2 with carbon to give CO is described as the Boudouard reaction.[53] Above 800 °C, CO is the predominant product:

CO2 + C 2 CO (ΔH = 221 kJ/mol)

Another source is "water gas", a mixture of hydrogen and carbon monoxide produced via the endothermic reaction of steam and carbon:

H2O + C H2 + CO (ΔH = +131 kJ/mol)

Other similar "synthesis gases" can be obtained from natural gas and other fuels.

Carbon monoxide is also a byproduct of the reduction of metal oxide ores with carbon, shown in a simplified form as follows:

MO + C M + CO

Since CO is a gas, the reduction process can be driven by heating, exploiting the positive (favorable) entropy of reaction. The Ellingham diagram shows that CO formation is favored over CO2 in high temperatures.

Laboratory preparation[edit]

Carbon monoxide is conveniently produced in the laboratory by the dehydration of formic acid, for example with sulfuric acid.[54][55] Another method is heating an intimate mixture of powdered zinc metal and calcium carbonate, which releases CO and leaves behind zinc oxide and calcium oxide:

Zn + CaCO3 ZnO + CaO + CO

Coordination chemistry[edit]

Main article: metal carbonyl

   

The HOMO of CO is a σ MO.

   

The LUMO of CO is a π*antibonding MO.

Most metals form coordination complexes containing covalently attached carbon monoxide. Only metals in lower oxidation states will complex with carbon monoxide ligands. This is because there must be sufficient electron density to facilitate back-donation from the metal dxz-orbital, to the π*molecular orbital from CO. The lone pair on the carbon atom in CO, also donates electron density to the d on the metal to form a sigma bond. This electron donation is also exhibited with the cis effect, or the labilization of CO ligands in the cis position. In nickel carbonyl, Ni(CO)4 forms by the direct combination of carbon monoxide and nickel metal at room temperature. For this reason, nickel in any tubing or part must not come into prolonged contact with carbon monoxide (corrosion). Nickel carbonyl decomposes readily back to Ni and CO upon contact with hot surfaces, and this method is used for the industrial purification of nickel in the Mond process.[56]

In nickel carbonyl and other carbonyls, the electron pair on the carbon interacts with the metal; the carbon monoxide donates the electron pair to the metal. In these situations, carbon monoxide is called the carbonyl ligand. One of the most important metal carbonyls is iron pentacarbonyl, Fe(CO)5:

   

Many metal-CO complexes are prepared by decarbonylation of organic solvents, not from CO. For instance, iridium trichloride and triphenylphosphine react in boiling 2-methoxyethanol or DMF to afford IrCl(CO)(PPh3)2.

Metal carbonyls in coordination chemistry are usually studied using infrared spectroscopy.

Organic and main group chemistry[edit]

In the presence of strong acids and water, carbon monoxide reacts with alkenes to form carboxylic acids in a process known as the Koch–Haaf reaction.[54] In the Gattermann–Koch reaction, arenes are converted to benzaldehyde derivatives in the presence of AlCl3 and HCl.[55] Organolithium compounds (e.g. butyl lithium) react with carbon monoxide, but these reactions have little scientific use.

Although CO reacts with carbocations and carbanions, it is relatively nonreactive toward organic compounds without the intervention of metal catalysts.[57]

With main group reagents, CO undergoes several noteworthy reactions. Chlorination of CO is the industrial route to the important compound phosgene. With borane CO forms an adduct, H3BCO, which is isoelectronic with the acylium cation [H3CCO]+. CO reacts with sodium to give products resulting from C-C coupling such as sodium acetylenediolate 2Na+

·C

2O2

2. It reacts with molten potassium to give a mixture of an organometallic compound, potassium acetylenediolate 2K+

·C

2O2

2, potassium benzenehexolate 6K+

C

6O6

6,[58] and potassium rhodizonate 2K+

·C

6O2

6.[59]

The compounds cyclohexanehexone or triquinoyl (C6O6) and cyclopentanepentone or leuconic acid (C5O5), which so far have been obtained only in trace amounts, can be regarded as polymers of carbon monoxide.

At pressures of over 5 gigapascals, carbon monoxide converts into a solid polymer of carbon and oxygen. This is metastable at atmospheric pressure but is a powerful explosive.[60][61]

Uses[edit]

Chemical industry[edit]

Carbon monoxide is an industrial gas that has many applications in bulk chemicals manufacturing.[62] Large quantities of aldehydes are produced by the hydroformylation reaction of alkenes, carbon monoxide, and H2. Hydroformylation is coupled to the Shell Higher Olefin Process to give precursors to detergents.

Phosgene, useful for preparing isocyanates, polycarbonates, and polyurethanes, is produced by passing purified carbon monoxide and chlorine gas through a bed of porous activated carbon, which serves as a catalyst. World production of this compound was estimated to be 2.74 million tonnes in 1989.[63]

CO + Cl2 COCl2

Methanol is produced by the hydrogenation of carbon monoxide. In a related reaction, the hydrogenation of carbon monoxide is coupled to C-C bond formation, as in the Fischer-Tropsch process where carbon monoxide is hydrogenated to liquid hydrocarbon fuels. This technology allows coal or biomass to be converted to diesel.

In the Monsanto process, carbon monoxide and methanol react in the presence of a homogeneous rhodium catalyst and hydroiodic acid to give acetic acid. This process is responsible for most of the industrial production of acetic acid.

An industrial scale use for pure carbon monoxide is purifying nickel in the Mond process.

Meat coloring[edit]

Carbon monoxide is used in modified atmosphere packaging systems in the US, mainly with fresh meat products such as beef, pork, and fish to keep them looking fresh. The carbon monoxide combines with myoglobin to form carboxymyoglobin, a bright-cherry-red pigment. Carboxymyoglobin is more stable than the oxygenated form of myoglobin, oxymyoglobin, which can become oxidized to the brown pigment metmyoglobin. This stable red color can persist much longer than in normally packaged meat.[64] Typical levels of carbon monoxide used in the facilities that use this process are between 0.4% to 0.5%.

The technology was first given "generally recognized as safe" (GRAS) status by the U.S. Food and Drug Administration (FDA) in 2002 for use as a secondary packaging system, and does not require labeling. In 2004 the FDA approved CO as primary packaging method, declaring that CO does not mask spoilage odor.[65] Despite this ruling, the process remains controversial for fears that it masks spoilage.[66] In 2007 a bill[67] was introduced to the United States House of Representatives to label modified atmosphere carbon monoxide packaging as a color additive, but the bill died in subcommittee. The process is banned in many other countries, including Japan, Singapore, and the European Union.[68][69][70]

Medicine[edit]

In biology, carbon monoxide is naturally produced by the action of heme oxygenase 1 and 2 on the heme from hemoglobin breakdown. This process produces a certain amount of carboxyhemoglobin in normal persons, even if they do not breathe any carbon monoxide.

Following the first report that carbon monoxide is a normal neurotransmitter in 1993,[4][5] as well as one of three gases that naturally modulate inflammatory responses in the body (the other two being nitric oxide and hydrogen sulfide), carbon monoxide has received a great deal of clinical attention as a biological regulator. In many tissues, all three gases are known to act as anti-inflammatories, vasodilators, and encouragers of neovascular growth.[6] However, the issues are complex, as neovascular growth is not always beneficial, since it plays a role in tumor growth, and also the damage from wet macular degeneration, a disease for which smoking (a major source of carbon monoxide in the blood, several times more than natural production) increases the risk from 4 to 6 times.

There is a theory that, in some nerve cell synapses, when long-term memories are being laid down, the receiving cell makes carbon monoxide, which back-transmits to the transmitting cell, telling it to transmit more readily in future. Some such nerve cells have been shown to contain guanylate cyclase, an enzyme that is activated by carbon monoxide.[5]

Studies involving carbon monoxide have been conducted in many laboratories throughout the world for its anti-inflammatory and cytoprotective properties. These properties have potential to be used to prevent the development of a series of pathological conditions including ischemia reperfusion injury, transplant rejection, atherosclerosis, severe sepsis, severe malaria, or autoimmunity. Clinical tests involving humans have been performed, however the results have not yet been released.[71]

Lasers[edit]

Carbon monoxide has also been used as a lasing medium in high-powered infrared lasers.[72]

   

원본 위치 <http://en.wikipedia.org/wiki/Carbon_monoxide>

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4. 일산화탄소

   

가. 성상

(1) 분자량 28.01, 비중 1.25㎏/㎥, 녹는점 -205.1℃, 끓는점 -191.5℃, 자동점화온도 608.9℃

(2) 최소,최대 폭발한계 농도 12.5∼74%

(3) 무색, 무미, 무취의 기체로 연소시 파란불꽃이 생성되며, 일명 "연탄가스"라고 한다.

나. 자연계분포

(1) 자연발생원 : 산불, 광화학반응 등

(2) 환경농도 : 0.1∼0.2ppm(북반구), 0.04∼0.06ppm(남반구)

(3) 자연체류시간 : 1∼3개월

다. 발생 및 오염원

(1) 발생

(가) 석탄, 목재, 종이, 기름, 유류, 가스 등과 같은 유기성 물질이 폭발하거나 연소시에 주로 발생한다.

(나) 불완전연소

연소시 산소가 부족하거나 연소온도가 낮으면 완전연소가 일어나지 못하여 불완전 연소생성물인 일산화탄소(CO)가 생성된다. 그러므로 일산화탄소는 연탄의 연소가스나 자동차의 배기가스중에 많이 포함되어 있으며, 큰 산불이 일어날 때도 주위에 산소가 부족하여 많은 양의 일산화탄소가 발생되기도 하고 담배를 피울 때 담배연기 속에 함유되어 배출되기도 한다.

(2) 주 배출원

(가) 자동차

1) 가솔린 자동차는 1∼10%, 디젤엔진에서는 약 0.1%의 농도로 배출되나 운전상태, 유 지관리에 따라 배출농도는 차이가 난다.

2) 국내에서는 과거 연탄 사용에 따라 난방연료가 주 배출원이었으나, '90년에 들어서 연 료전환 정책과 자동차 대수의 급격한 증가에 따라 자동차에서 배출되는 일산화탄소 의 배출량이 전체의 90%이상('97년 기준)을 차지하고 있다.

(나) 기 타

주물제조 공정의 용선로, 석유정제시설의 접촉분해 공정, 소성로, 화합물질 제조 등 어떤 공정에서든지 불완전연소가 일어나면 발생 가능하므로 CO의 배출원은 매우 다양하다.

라. 독성 및 영향

(1) 독성

(가) 일산화탄소(CO)는 체내에 산소를 운반하는 역할을 하는 혈액중의 헤모그로빈(Hb)과 결합하여 일산화탄소-헤모그로빈(COHb)을 만들어 혈액의 산소운반능력을 저하시켜 그 농도에 따라 사망에 이를 수 있다.

(나) 혈액중 또는 근육중의 일산화탄소의 대부분이 도시의 대기오염에 기인하는 것만은 아니며 일정량의 일산화탄소는 본래 생체의 신진대사 산물로서 존재하고, 헤모그로빈의 생리적 신진대사결과로서 혈액중에 약간 존재(0.3∼0.8%)한다. 그러나 체내혈액중의 일산화탄소-헤모그로빈량의 증가는 흡입공기중의 일산화탄소농도에 비례한다.

(2) 영향

(가) 일산화탄소 20ppm을 함유한 공기를 4시간 동안 흡입하면 체내혈액중의 일산화탄소-헤모그로빈은 1.64%증가한다. 실제 도시대기중의 일산화탄소 농도는 자동차통행량, 도로조건, 도로로부터 떨어진 거리, 기후조건 등에 의해서 다르지만 자동차의 정체가 심한 도로변에서는 일산화탄소농도는 높게 되며, 이때 일산화탄소-헤모그로빈의 혈중농도는 13∼18%까지 상승하는 것으로 알려져있다. 도심에서 자동차 운전시 30ppm의 일산화탄소를 함유한 공기를 2시간 흡입할 때 혈중 일산화탄소-헤모그로빈은 5% 상승하며 60ppm에서는 10% 상승한다고 한다.

(나) 비교적 고농도의 일산화탄소를 계속해서 흡입하는 직업인으로는 고속도로와 터널의 통행료 징수원, 차량검사원, 교통경찰관, 지하주차장 종사원 등을 들 수 있다.

(다) 혈중 일산화탄소-헤모그로빈의 농도 및 인체 영향은 표 3.4.1과 같으며 증상이 나타나는 호흡시간은 그 사람의 활동상태 즉, 휴식, 보행 및 노동상태에 따라 다를 수 있다.

표 3.4.1 혈중 일산화탄소-헤모그로빈의 농도 및 인체영향

   

COHb(%)

증 상

CO농도(ppm)

호흡시간

4

건강한, 사람은 문제되지 않지만 호흡기계통 질환등의 환자에게는 영향을 줄 수 있다.

9∼30

10∼30 분

5

중추신경에 영향

30

4∼6 시간

  

  

120

1 시간

10

과격한 근육활동시 숨이 참.

40

8 시간

20

보통 활동에도 숨이차고 간혈적 두통

400∼500

1 시간

30

두통, 신경과민, 피로감, 주의력 산만

1,000

1 시간

40∼50

두통, 정신혼란

1,000

1∼2 시간

60∼70

의식혼탁, 호흡증추마비

1,000

4∼5 시간

80

사망

1,500∼2,000

4∼5 시간

   

(3) 오염경로

(가) 일반적으로 높은 농도의 일산화탄소를 함유한 공기를 흡입하는 사람은 짧은 시간에도 혈중 일산화탄소-헤모그로빈의 농도가 높게 된다. 1970년의 미국 시카고의 비흡연 헌혈자의 혈중 일산화탄소-헤모글로빈 농도는 1∼5%이상인 자가 74%였고, 1974년에는 대기중의 일산화탄소농도가 개선되어 혈중 일산화탄소-헤모그로빈 농도가 1.5%를 초과하는 사람이 42%로서 감소되었던 것으로 보아 흡입공기중의 일산화탄소 농도가 혈중 일산화탄소-헤모그로빈 농도에 직접적인 영향을 미친다는 것을 알 수 있다.

(나) 일산화탄소가 혈중으로 이동되는 속도는 폐포나 폐의 모세혈관중의 일산화탄소 농도, 환기량, 폐의 확산기능, 폐의 모세혈관중의 혈액유량, 일산화탄소 또는 산소의 헤모그로빈과의 결합속도에 의하여 결정된다. 일산화탄소는 헤모그로빈에 대하여 산소보다 200배 이상의 친화력을 가지고 있다.

(다) 인체에 흡입된 일산화탄소의 배출은 오직 호흡기를 통하여 이루어지는데 그 배출속도는 아주 느리다. 이는 일산화탄소가 헤모그로빈에 대하여 강한 친화력이 있기 때문이다. 일산화탄소의 배출반감기 즉 혈중 일산화탄소-헤모그로빈의 농도가 처음농도의 50%에 도달할 때까지 필요한 시간은 1시간 30분에서 4시간 정도이다.

마. 규제법규 및 각종 기준

(1) 환경기준

주요 국가별 환경기준을 표 3.4.2에 나타내었다.

표 3.4.2 주요 국가별 일산화탄소 환경기준 (단위 : ppm이하)

   

국가별

구분

한국

일본

미국

캐나다

네델란드

이탈리아

싱가포르

대만

WHO

1시간 평균

25

-

35

31

32

35

35

35

26

8시간 평균

9

20

9

13

5

9

9

9

9

24시간 평균

-

10

-

-

-

-

-

-

-

   

(2) 배출허용기준

주요 국가별 국내 운행차의 배출허용기준은 표 3.4.3과 같고, 고정배출원의 배출허용기준은 표3.4.4와 같다.

표 3.4.3 국내 운행차 배출허용기준

   

사 용 연 료

차 종

적 용 기 준

  

  

  

'87.12.31 이전

'88.1.1이후 제작

휘발유·가스·알콜

승용차

4.5% 이하

1.2% 이하

  

경·소형화물, 중량자동차

4.5% 이하

  

   

(3) 작업장 환경기준

- 시간가중평균(TWA) : 50ppm

- 한계치(TLV) : 35ppm/10h, 200ppm ceil(순간적으로도 넘어서는 않됨)

- 단기간노출한계(STEL) : 400ppm

- 생명체나 건강에 급성으로 위험한 농도(IDLH) : 1,500ppm

- 최대허용농도(MAC) : 20㎎/㎥(≒16ppm)

   

표 3.4.4 배출시설별 일산화탄소 배출허용기준 (단위 : ppm이하)

   

배 출 시 설

국가별 기준

  

  

  

  

한 국

프랑스

독 일

기 타

가. 발전시설 또는

일반보일러

(1)액체연료사용

(2)고체연료사용

나. 소각시설 또는 소각보일러

   

다. 시멘트 제조시설 중 소성로

라. 기타시설

   

   

350(4)

400(6)

600(12)

   

600(12)

700

500

   

   

   

1,000

   

   

   

   

   

140(3)

200(6)

800(11), 800(17)

*0.75t/h 기준

   

-모든시설 :

호주:800

싱가포르:800

스페인:500

-석유정제시설

500∼1,500

(미국,스페인)

   

바. 오염현황

국내 산업부문별 일산화탄소 배출량을 표 3.4.5에 나타내었다.

표 3.4.5 국내 CO배출량 현황 ('97.기준) (천톤)

   

구분

난 방

산 업

수 송

  

  

  

발 전

  

  

  

소 계

승용차

버스, 트럭

선박, 기타

  

1,129

62

18

1,032

481

528

23

17

   

사. 문제점 및 대책

(1) 문제점

일산화탄소(CO)는 그 배출원이 다양하고, 조업상태에 따른 연소조건에 매우 민감하게 변화하며 불완전연소시에 많은 양이 배출되기 때문에 배출원에서 방지시설로 처리하기가 어렵다.

(2) 대책

(가) 효율적인 공정관리와 연소시 완전연소를 유도한다.

(나) 자동차에는 삼원촉매 장치 등과 같은 저감장치를 부착한다.

참고문헌

1. Encyclopaedia of Occupational Health and Safety, Vol. I,II, (1983).

2. Arthur C. S., (1984), Fundamentals of Air Pollution, 2nd ed.

3. Henry C. P., (1974), Air Pollution

4. 대기오염물질 배출량('97)

5. 대기환경관리(1999)

작성자 : 대기공학과 환경연구사 김대곤(공학석사)

   

   

원본 위치 <http://home.sunchon.ac.kr/~bioenvlab/data2/ham3/3-4.htm>

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