One of
carbonaceous gas in the earth atmosphere which takes part in global carbon
cycle is Carbon Monoxide. Carbon Monoxide (CO) is a colourless, tasteless and
odourless gas which is 96.5% as heavy as air and insoluble in water. Its molecular
weight is 28.1 with a boiling point of -191.5ºC and melting point of -205ºC.
However, it is not uniformly distributed on earth but can be transported long
distances and remains in the atmosphere for a longer duration with an average
residence time of 36-110 days. Some basic chemical reactions that yields CO
are-
I. Incomplete combustion of fuel:
2C + O2 à 2CO
II. Reactions between carbon dioxide and carbon containing materials at very high temperature such as in blast furnaces:
CO2 + C à 2CO
III.
Dissociation
of carbon dioxide at elevated temperature
CO2 ó CO
Sources and Sink of Carbon Monoxide in the Atmosphere
There
are two types of sources of CO in the atmosphere which are natural sources and
man-made sources or anthropogenic sources. Volcanic action, natural gas
emission, electrical discharge during storms, seed germination, marsh gas
production are the natural sources of CO in the atmosphere, however
contribution of these sources is very less as compare to man-made sources.
Man-made sources includes transportation (64%), forest fires (7.2%), agricultural
burning (8.3%) and industrial processes such as iron, steel, paper and
petroleum industries (9.6%). Diesel and petroleum engines in automobiles is the
primary source of carbon monoxide emission in the atmosphere. It is estimated
that each year around 350 million tonnes of CO are emitted in the atmosphere.
Out of which 275 million tonnes are from human sources and 75 million tonnes
from natural sources.
Some
soil micro-organisms such as Aspergillus and Penicillium are major sink of CO.
Route of Exposure to CO
• By
breathing in contaminated air
• Using
malfunctioning equipment
• Smoking
and breathing in other people’s cigarette smoke
• Living
near industries that emit carbon monoxide
• Using
nonelectric heaters
Biochemical Effects of CO
When we are exposed to CO through any route and it enters in our body, it attacks haemoglobin and forms a complex named as carboxyhaemoglobin by displacing oxygen.
O2Hb + CO à COHb + O2
Carboxy haemoglobin is a stronger complex
that reduces the blood’s capacity to carry oxygen.
Effects of various levels of CO on humans
CO level(ppm) |
effects on humans |
10 |
impairment of judgement and visual perception |
100 |
headache, dizziness, weariness |
250 |
loss of consciousness |
750 |
death after several years |
1000 |
rapid death |
Effects on Environment
• Although
CO is a weak greenhouse gas but it influence the presence of other greenhouse
gases such as methane, tropospheric ozone and carbon dioxide.
• CO
reacts with the hydroxyl radical forming a stronger greenhouse gas named as
carbon dioxide.
• It
also increases the concentration of methane which is also a potent greenhouse
gas, because the most common way methane is removed from the atmosphere is when
it reacts with hydroxyl radical.
Control
Measures
• Modification of internal combustion engines to
reduce the amounts of pollutants formed during fuel combustion
• Development
of exhaust system reactors which will complete the combustion process
• Development
of substitute fuel for gasoline
• Alternate
power sources e.g. steam, electric and gas turbine engines
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