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Air Pollution 
Ms Noor Rosyidah Binti Sajuni 
School of Engineering 
rosyidah@ucsi.edu.my
2 
Content 
• Definition, 
• Unit of measurement, 
• Sources of air pollution, 
• Classification of air pollutants, 
• Type of air pollutants, 
• Air quality index (AQI), 
• Effects of pollutant to environment and human, 
• ozone depletion, 
• acid rain, 
• green house effect, 
• climate change, 
• global warming, 
• Meteorology, 
• air pollution monitoring device, 
• control and preventive action.
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Definition 
Air pollution may be defined as the presence in the air (outdoor 
atmosphere) of one or more contaminants or combinations thereof in such 
quantities and of such durations as may be or tend to be injurious to 
human, animal or plant life, or property, or which unreasonably 
interferes with the comfortable enjoyment of life or property or conduct 
of business.
4 
Unit of Measurement 
• Air quality measurement are commonly reported in terms of: 
– micrograms per cubic meter (μg/m3) 
– parts per million (ppm) or parts per billion (ppb) 
• For particulate matter, sizes are expressed in micron or micrometer. 
– ppm is a volume-to-volume ratio, which makes it independent of local 
temperature and pressure. 
ppmx xMWx L m x g g 
MW gram molecularweight of the gas 
V P 
2 2 
2 
V P 
1 1 
1 
6 3 3 6 
3 
: 
10 10 / 10 / 
( / ) 
/ 
T 
T 
V L mol 
g m 
 
 
  
 
Standard conditions: V=22.4 L/mol @ 273K & 760 mmHg
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Source of Air Pollution 
• Mobile sources -- automobiles, gas-powered lawn tools and mowers, boats, 
planes etc 
• Agriculture sources -- Enclosed farm animals – manure release gases eg 
ammonia; aerial drift of excess fertilizers and 
pesticides; 
• Natural -- forest fires, volcanoes, dust storm 
Volcanoes – ash, acid mist, hydrogen sulfide & other toxic gas. 
 Sea spray & decaying vegetation – major source of reactive sulfur 
compound. 
 Trees & bushes – volatile organic compounds 
Storms in arid regions –dust clouds. 
Fermentation in swamp & break-down of cellulose in guts of 
termites & ruminant animals – ⅔ of world methane (natural gas).
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Geographic Factors 
• Sources and emission rates of pollution 
• Topography: Mountains as barriers for air movement, forming 
temperature inversion layer and promoting pollution over certain areas 
• Atmospheric conditions: 
Temperature, cloud 
cover, and wind affecting 
the transportation or 
dispersion of pollutants
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Classification of Air Pollutants 
Categories of pollutants 
● Primary – emitted directly from a source 
● Secondary – formed in the atmosphere from a reaction of primary pollutants 
It is a substance or effect dwelling temporarily or permanently in the air , which 
adversely alters the environment by interfering with the health, the comfort, or 
the food chain, or by interfering with the property values of people. 
Basic Pollutants 
Pollutant Abbreviation Type 
Carbon Monoxide CO Primary 
SO Primary 2 Sulfur Dioxide 
O Secondary 3 Ozone 
NO Secondary 2 Nitrogen Dioxide 
HC Primary & Secondary 
Hydrocarbon Compounds (also 
called VOCs – volatile organic 
compounds ) 
Particulate Matter PM Primary & Secondary 
Lead Pb Primary & Secondary
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Type of Pollutants 
• Suspended particulate matter – complex mixture of solid particles & aerosols 
(liquid particles) suspended in the air. We see these particles as dust, smoke, spores, 
algal cell & haze. PM smaller than 2.5 micrometers (PM2.5)–most dangerous. 
• Volatile organic compounds (VOCs) – gasoline, paint solvents & organic cleaning 
solutions, which evaporate & enter the air in a vapor state, as well as fragments of 
molecules resulted from the incomplete oxidation of fuels & wastes. VOCs are 
prime agents of ozone formation. Plants = largest sources of VOCs, ~350 million 
tons of isoprene (C5H8) & 450 million tons of terpenes (C10H15) each year. About 
400 million tons of methane are produced from wetlands & bacteria. 
• Carbon Monoxide (CO) – Invisible, odorless gas. From incomplete combustion of 
fuel (coal, oil, charcoal or gas), incineration of biomass or material. ~ 1 billion 
metric tons release each year, half from human activities.~90% of CO is consumed 
in photochemical reaction that produce ozone.
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• Hazardous Air Pollutants (HAPs) -Air toxic include carcinogenic chemicals, 
radioactive materials & other chemicals (asbestos, vinyl chloride & Benzene). EPA 
has identified 166 categories of major sources and 8 area sources for HAPs. 
• Some of the HAPs (EPA)
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• Nitrogen oxides (NOx).- highly reactive gas formed when nitrogen in fuel or 
combustion air is heated above 650ºC in the presence of oxygen. Converted to 
nitric acid=major source of acid deposition. NOx is a lung irritant. 
• Sulfur oxides (SOx), mainly sulfur dioxide (SO2)-poisonous gas to plant & animal. 
Converted to sulfuric acid in air. Major source of acid deposition. 
– Natural sources =evaporation from sea spray, erosion of sulfate-containing 
dust from arid soils, fumes from volcanoes, biogenic emission of hydrogen 
sulfide (H2S) & organic sulfur-containing compounds (i.e. dimethylsulfide, 
methyl mercaptan, carbon disulfide ). 
– Yearly input to air: 114 million metric ton. Anthropogenic sources = ⅔ of 
worldwide sulfur flux. Mainly from combustion of sulfur-containing fuel (coal 
& oil), purification of sour (sulfur-containing) natural gas or oil, smelting of 
sulfide ores. China & US = largest sources of anthropogenic sulfur (from coal 
burning).
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• Lead & heavy metal- World wide lead ~ 2 million metric tons/year, or ⅔ of all 
metallic air pollution. Most from leaded-gasoline. Lead=metabolic poison & 
neurotoxin. ~20% of all inner-city children suffer some degree of mental 
retardation from high Pb level. Mercury (Hg) =neurotoxin. 2 largest sources = 
coal burning power plants & WASTE INCINERATION. Arsenic (from metal 
smelter, coal combustion & pesticides. 
• Ozone & other photochemical oxidant -ozone=ground level pollutant, strong 
oxidizing reagent & damages vegetation, building material (such as paint, 
rubber & plastic) & sensitive tissue (eyes & lungs). Hydrocarbons in the air 
contribute to accumulation of ozone by removing NO in the formation of 
compounds (such as peroxyacetyl nitrate (PAN), which is another damaging 
photochemical oxidant.
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• Haze - Opaque condition of atmosphere caused by tiny suspended solid or 
liquid particles; Normally from open burning 
• Industrial & Photochemical Smog -
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Source: EPA website
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Smog Production
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Temperature Inversion 
• Several weather conditions intensify levels of industrial & 
photochemical smogs. 
• Most significant – temperature inversion. 
• Temperature inversions are defined as the increase of air 
temperature with altitude. Such an increase represents a reversal of 
the normal temperature condition of the troposphere (the region of 
the atmosphere in contact with the Earth's surface), where 
temperature usually decreases with height. (Britannica Online, 1998)
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Temperature Inversion 
• In (a), daytime temperature highest near ground – earth absorbs heat & radiates to the air near 
the ground. The warm air near ground rises, carrying pollutants.
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Temperature Inversion 
• In (b), 2 types of mechanisms create inversion: 
1. Unstable type – cold front slides under an adjacent warmer air mass 
OR cool air subsides down a mountain slope to displace warmer air 
in the valley below. 
2. Stable type – Rapid night-time cooling in a valley/basin where air 
movement is restricted. Best example (Los Angeles)-a city 
surrounded by 3 side mountains & climate is dry & sunny. Lots of 
aerosol & gaseous chemical from motor vehicles. Skies are generally 
clear at night, allowing rapid radiant heat loss, and the ground cools 
quickly. Surface areas are cooled by conduction, while upper layers 
remain relatively warm. During the night, cool & humid onshore 
breezes slide in under the contaminated air. Density differences 
retard vertical mixing.
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Indoor Air Pollution 
• Environmental health hazards 
at homes and workplaces 
• A variety of substances: 
Smoke, chemicals, microbes, 
and radon 
• Different sources: 
Insulation materials, 
wood products, 
poisonous gases 
due to poor ventilation, 
cleaning chemicals, etc. 
http://gsc.nrcan.gc.ca/gamma/radon_e.php
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Adverse Effects of Air Pollution on Humans 
• Air pollution is not a single entity. 
• Synergistic effects = 2 or more factors combine to produce an effect greater 
than their simple sum. 
• I.E. plants & animals may be so stressed by pollution – become > 
vulnerable to other environmental factors (drought/attack by parasites & 
disease). 
• Humans breathe ~ 14 kg of air/day. 
• Some symptoms of air pollution involve moist surfaces of eyes, nose & 
throat, the major site of impact is the lungs. 
• 3 categories of impact: 
– Chronic: Pollutants cause the gradual deterioration of a variety of 
physiological functions over a period of years. 
– Acute: Pollutants bring on life-threatening reactions within a period of 
hours/days 
– Carcinogenic: Pollutants initiate changes within cells that lead to 
uncontrolled growth & division (cancer).
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Air Pollution – Chronic effects on Humans 
• Chronic Effects-Almost everyone living in areas of urban air pollution suffers from 
chronic effects. 
– Sulfur dioxide (SO2) – long term exposure → bronchitis (inflammation of the 
bronchi) 
– Ozone & particulate – inflammation → fibrosis of the lung (scarring that 
permanently impairs lung function). 
– CO – reduce the capacity of blood to carry O2 → heart disease. 
– NO (Nitrogen Oxides) – impair immune system → leaving the lungs open to 
attack by bacteria & viruses.
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fig_12_02
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Air pollution effects on agriculture & forest 
• Plants are more sensitive than humans. 
• The pollutant responsible is usually sulfur dioxide. 
• Forest under stress from pollution = more susceptible to damage by insects 
& pathogens. 
• 2 probable ways : 
– Direct toxic. Within a few days of exposure, molting (discoloration) 
occurs in leaves due to chlorosis (Bleaching of chlorophyll) and then 
necrotic (dead) spots develop. If injury is severe, the whole plant may 
be killed.
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Air pollution effects on agriculture & forest 
– Air pollutants (ethylene=component of automobile exhaust & release 
from petroleum refineries & chemical plant), that act as metabolic 
regulators or plant hormones & disrupt normal patterns of growth & 
development. 
– The concentration of ethylene around highways & industrial areas is 
often high enough to cause injury to sensitive plant. 
– Synergistic effect – when white pine seedlings are exposed to sub-threshold 
[Ozone] & [SO2] individually, no visible injury occurs. If the 
same [ ] of ozone & SO2 given together, visible damage occurs. In 
alfalfa, ozone & SO2 together cause less damage than either one alone.
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Aquatic Effects 
• Reproduction is the most sensitive stage in fish life cycles. 
• Eggs & fry of many spp. of fish are killed when pH drops to ~ 5.0. 
• pH lower than 5 disrupt food chain, killing aquatic plants, insects & 
invertebrate & adult fish. 
• Trout, salmon & other game fish are usually the most sensitive. 
• Carpgar, suckers & other less desirable fish are more resistant. 
• Acidity alters body chemistry, destroys gills & prevents oxygen uptake, 
causes bone decalcification, & disrupt muscle contraction. 
• Acid water also leaches toxic metals such as mercury & aluminium out 
of soil & rocks.
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Air pollution effects on materials 
• Mechanism of deterioration 
– Abrasion 
– Deposition 
– Indirect chemical attack 
– Direct chemical attack 
– Electrochemical corrosion 
• Factor influence the rate of deterioration 
– Moisture 
– Sunlight 
– Temperature 
– Position of exposed material
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Acid Rain 
• Pure rainwater is slightly acidic, (dissolved carbon dioxide). 
• Air also contains naturally occurring organic acids and acidic 
particles. 
• The pH of unpolluted rainwater ranges from about 6 to just below 5. 
• Air compounds containing oxides of sulfur and nitrogen : 
– may then dissolve in cloud droplets, making rainwater more 
acidic (wet deposition), or 
– may mix through the atmosphere, eventually coming into direct 
contact with the ground and vegetation (dry deposition). 
• Both forms can harm soil, lakes, plants, buildings and people 
• More industrial activity in the northern hemisphere. 
• Industry also tends to be concentrated in particular regions. This is 
why acid rain problems are worse in the northern hemisphere.
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Ozone Depletion 
• Ozone forms a layer in the stratosphere (20-40km and up) that provides a 
barrier to ultraviolet (UV) radiation. 
• Although oxygen serves as a barrier to UV radiation, it absorb only over a 
narrow band centered at wavelength of 0.2 μm. 
http://ozone.unep.org
38 http://ozone.unep.org
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Montreal Protocol 1988 
• Following the discovery of the Antarctic ozone hole in late 1985, governments 
recognized the need for stronger measures to reduce the production and 
consumption of a number of CFCs (CFC 11, 12, 113, 114, and 115) and several 
Halons (1211, 1301, 2402). 
• The first general ozone agreement was on 1985. This agreement, known as the 
Vienna Convention for the Protection of the Ozone Layer. 
• Later, the Montreal Protocol on Substances that Deplete the Ozone Layer was 
adopted on 16 September 1987 at the Headquarters of the International Civil 
Aviation Organization in Montreal. The Protocol came into force on 1st January 
1989, when it was ratified by 29 countries and the EEC. Since then several other 
countries have ratified it. 
• The Montreal Protocol and its Amendment constitute a mechanism for the phasing 
out of ozone depleting substances. 
• The control measures and phase out schedules cover both the production and the 
consumption of the target substances. However, even after phase out both 
developed and developing countries are permitted to produce limited quantities in 
order to meet the essential uses for which no alternatives have yet been identified 
http://ozone.unep.org
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Helsinki Declaration 1989 
• Encourage all states that have not done so to join the Vienna Convention 
for the Protection of the Ozone Layer and its Montreal Protocol 
• Agree to phase out the production and the consumption of CFCs controlled 
by the Montreal Protocol as soon as possible but not later than the year 
2000 
• Agree to phase out the production and the consumption of CFCs controlled 
by the Montreal Protocol as soon as possible but not later than the year 
2000 
• Agree to commit themselves, in proportion to their means and resources, to 
accelerate the development of environmentally acceptable substituting 
chemicals, products and technologies 
• Agree to facilitate the access of developing countries to relevant scientific 
information, research results and training and to seek to develop 
appropriate funding mechanisms to facilitate the transfer of technology and 
replacement of equipment at minimum cost to developing countries. 
http://ozone.unep.org
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Climate Change/ Global Warming
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Climate Change/ Global Warming 
• Since 1850, the average global temperature is up by 0.76 °C 
• Most of the warming happened in the last 50 years, due to human activities. 
• Causes: burning fossil fuels for energy, agriculture, deforestation 
• We are already seeing climate change impacts like heat waves and more 
extreme weather events 
• Countries began discussing climate change in 1992, with the creation of the 
UN Framework Convention on Climate Change (UNFCC) 
• The first international commitments to cut CO2 came with the Kyoto 
Protocol in 1997 
• The EU played a leading role in past agreements and advocates strong 
future action
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Effects Of Climate Change On Mercury 
And Persistent Organic Pollutants 
Precipitation 
Winds 
Exchange with 
Surface reservoirs 
Chemistry
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Kyoto Protocol 
• Only a first step 
• It only runs until the end of 2012 
• Not all countries are on board – including the US 
• It doesn't contain commitments for developing countries, and their 
emissions are fast catching up with those of developed countries 
• A new agreement is needed 
• It must be more ambitious, with long-term commitments to deeper 
cuts 
• Developed and developing countries need to act 
• We must keep the commitment to limit warming to 2ºC 
• Global CO2 emissions need to peak by 2020 and halve by 2050 
• Kyoto's successor must include support for developing countries 
and adaptation
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EU actions 
In December 2008, European leaders agreed the climate and energy package, 
with ambitious targets for 2020. 
The package means: 
– 20% cut in greenhouse gas emissions by 2020 – 30% if other developed 
countries agree 
– 20% of energy from renewable sources 
– 20% increase in energy efficiency 
Concrete steps in package include: 
• An extension of emissions trading system 
• Support for carbon capture and storage 
• Country-specific targets for renewable energy
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Air Pollution Meteorology 
• An air pollution problem involves three parts: the source, the movement of 
the pollutant and the recipient. 
• All meteorological phenomena are a result of interaction of the elemental 
properties of the atmosphere, heat, pressure, wind and moisture. 
• The rotation of the earth couple with heat conductivities of the ocean and 
land produced weather.
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Mechanical Turbulence 
• Random fluctuation of wind velocity (speed and direction) 
• Wind is zero at ground surface and rise with elevation to near the speed imposed by 
the pressure gradient. 
• The greater the mean wind speed, the greater the turbulence. 
• The more the mechanical turbulence, the easier it is to disperse the spread the 
atmospheric pollutants. 
Thermal Turbulence 
• Different of air circulation during day time and nights. 
• During clear nights when the ground radiates its heat away to the cold night sky and 
the cold air above it causing a sinking density current.
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Cyclonic conditions 
• Areas of Low pressure are generally 
– fast moving, 
– associated with strong winds and bad weather (tornadoes and hurricanes) 
– upward motion, clouds and precipitation 
 all result in low pollutant concentrations 
Anticyclonic conditions 
• High pressure areas have the opposite conditions: 
– Often slow moving and stagnant 
– Associated with weak pressure gradients and light winds 
– Downward motion – clear skies and good weather 
– Formation of a subsidence inversion that stabilizes the atmosphere and limits 
vertical mixing 
 Conditions that lead to stagnation and high pollutant concentrations
52 
Atmospheric Stability 
• Tendency of atmosphere to resist or enhance vertical motion. 
• Affects dispersion of pollutants 
• It is related with wind speed and change of air temperature with height (lapse rate, 
Г) 
• Lapse rate is the indicator for atmospheric stability. 
• 3 stability categories: neutral, unstable and stable. 
• Unstable atmosphere: Mechanical turbulence enhanced by thermal turbulence. The 
temperature of atmosphere greater than Г : Superadiabatic. Eg. Hot air balloon. 
• Neutral stability: Г increased or decreased by the parcel of air that expand or 
contracts adiabatically as it is raised through atmosphere. 
• Stable atmosphere: Temperature of the atmosphere less than Г it is call 
subadiabatic.
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Determine Atmospheric Stability 
• Stability is the tendency of the atmosphere to resist and enhance vertical 
motion. 
• Lapse rate is the change of air temperature with height. 
• There are 3 stability categories: 
– Neutral Atmosphere 
– Unstable Atmosphere 
– Stable Atmosphere 
• Mathematically, atmospheric stability can be determine as: 
T T 
T 
 
 
2 1 : 
Z Z 
2 1 
Z 
Lapse Rate 
 
 

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Vertical Temperature 
Profiles 
Environmental lapse rate (ELR) 
Dry adiabatic lapse rate (DALR) 
If, 
ELR > DALR =sub adiabatic 
condition, atmosphere is stable. 
ELR >> DALR= Inversion 
conditions. Very stable atmosphere. 
ELR= DALR= atmosphere is 
neutral. 
ELR< DALR = super adiabatic 
condition, atmosphere is unstable. 
Shapes of plumes depends upon 
atmospheric stability conditions.
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Subsidence inversion due to adiabatic warming of downward moving air 
(usually in an area of High Pressure)
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Stability Classes 
• Developed for use in dispersion models 
• Stability classified into 6 classes (A – F) 
• A: strongly unstable 
• B: moderately unstable 
• C: slightly unstable 
• D: neutral 
• E: slightly stable 
• F: moderately stable 
Surface wind 
speed at 10 m 
(m/s) 
Day Night 
Incoming Solar radiation Cloud Cover 
Strong Moderate Slight Thinly Overcast Mostly Cloudy 
< 2 A (s = 1) A-B B (s = 2) 
2-3 A-B B C (s = 3) E (s = 5) F (s = 6) 
3-5 B B-C C D E 
5-6 C C-D D (s = 4) D D 
>6 C D D D D
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Atmospheric Dispersion 
• Emission point characteristic 
• Nature of pollutant 
• Meteorology 
• Terrain 
• Anthropogenic structures
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Effect of wind 
• Wind diffuses pollutants by stretching them along the wind direction. 
• Wind speed also enhances turbulence, and thus vertical and horizontal 
diffusion. 
• Variations in wind direction are also important as they lead to sinuous 
plumes 
• The greatest potential for pollution is in low wind situations because 
horizontal transport and turbulent diffusion are both curtailed. 
• Local circulations (land/sea breezes etc.) are not good pollution ventilators 
because they are associated with low wind speeds, they are closed systems, 
and there usually is a diurnal reversal → pollution comes back.
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C: Inversions 
• Temperature inversions represent a situation in which the atmosphere is 
very stable and the mixing depth is significantly restricted. 
• When an inversion exists and winds are light, diffusion is inhibited and 
high pollution concentrations are to be expected in areas where pollution 
sources exist. 
• Surface temperature inversions form because the ground is a more 
effective radiator than the air above. Inversions aloft are associated with 
sinking air that characterizes centers of high air pressure (anticyclones).
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Inversion
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This is an example 
of a generalized 
temperature profile 
for a surface 
inversion. 
Temperature-profile 
changes in bottom 
diagram after the 
sun has heated the 
surface.
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An Inversion Aloft
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D: Air Mixing Depth 
• The direct effect of wind speed is to influence the concentration of 
pollutants. 
• Atmospheric stability determines the extent to which vertical motions will 
mix the pollution with cleaner air above the surface layers. 
• The vertical distance between Earth's surface and the height to which 
convectional movements extend is called the mixing depth. 
• Generally, the greater the mixing depth, the better the air quality.
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Mixing Height of atmosphere 
The height of the base of the inversion layer from ground surface.
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Stacks in Industry 
 Emissions from industrial stacks are regulated to protect human and 
environmental health 
 Industrial facilities are required to obtain permits to emit into the 
atmosphere and to demonstrate their compliance with regulations 
 In the process of applying for permits, dispersion models are generally 
used to assess the impact of point source emission 
• A dispersion model is essentially a computational procedure for predicting 
concentrations downwind of a pollutant source 
• Routinely used in: 
 Environmental impact assessments 
 Risk analysis 
 Emergency planning
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Classes of Air Quality Models 
 The air quality modeling procedures can be categorized into four generic 
classes: Gaussian, numerical, statistical or empirical and physical 
 The emphasis is on Gaussian-plume type models for continuous releases, 
which are at the core of most U.S. Environmental Protection Agency 
(EPA) regulatory models 
 Gaussian models are the most widely used techniques for estimating the 
impact of nonreactive pollutants. 
Model Parameters 
 The model is based on our knowledge of the following parameters: 
 The emissions characteristics (stack exit velocity, plume rise, temperature, 
stack diameter) 
 Terrain (surface roughness, local topography, nearby buildings) 
 State of the atmosphere (wind speed, stability, mixing height, wind 
direction)
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Dispersion = Advection (Transport) + Dilution (Diffusion) 
Transport 
Source Receptor 
Re-entrainment 
Fick’s law of diffusion J= - D * D C/Dx 
Where, J= Mass Flux; D = Diffusivity coefficient,; D C/Dx = Concentration gradient 
Diffusion of pollutants occur due to turbulence, which further depends upon many factors: 
a. Ambient temperature 
b. Temperature of emissions 
c. Roughness factors 
d. Wind velocity 
e. Wind direction 
f. Humidity 
g. Stability
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Air Pollutants Cycle
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General Characteristics of Stack Plumes 
• Dispersion of pollutants 
• Wind – carries pollution downstream from source 
• Atmospheric turbulence -- causes pollutants to 
fluctuate from mainstream in vertical and crosswind directions 
• Mechanical & atmospheric heating both present at same time but in 
varying ratios 
• Affect plume dispersion differently
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Plume Types 
• Plume types are important because they help us understand under what 
conditions there will be higher concentrations of contaminants at ground 
level.
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Looping Plume 
• High degree of convective turbulence 
• Superadiabatic lapse rate -- strong 
instabilities 
• Associated with clear daytime conditions 
accompanied by strong solar heating & light 
winds 
• High probability of high concentrations 
sporadically at ground level close to stack. 
• Occurs in unstable atmospheric conditions.
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Coning Plume 
• Stable with small-scale turbulence 
• Associated with overcast moderate to 
strong winds 
• Roughly 10° cone 
• Pollutants travel fairly long distances 
before reaching ground level in 
significant amounts 
• Occurs in neutral atmospheric 
conditions
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Fanning Plume 
• Occurs under large negative lapse rate 
• Strong inversion at a considerable 
distance above the stack 
• Extremely stable atmosphere 
• Little turbulence 
• If plume density is similar to air, travels 
downwind at approximately same 
elevation
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Lofting Plume 
• Favorable in the sense that fewer 
impacts at ground level. 
• Pollutants go up into environment. 
• They are created when atmospheric 
conditions are unstable above the 
plume and stable below.
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Fumigation 
• Most dangerous plume: 
contaminants are all coming 
down to ground level. 
• They are created when 
atmospheric conditions are stable 
above the plume and unstable 
below. 
• This happens most often after the 
daylight sun has warmed the 
atmosphere, which turns a night 
time fanning plume into 
fumigation for about a half an 
hour.
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Legislation & Standards 
• Topographic, meteorological, and land-use characteristics of areas within 
an air region will vary. 
• The social and economic development of an area will result in different 
degrees of air pollution and demands for air quality.
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Air Quality Monitoring : Air Pollutant Index (API) or 
Air Quality Index (AQI) 
• A general index used to assess air quality; 
• Values calculated based on the average concentration of each of the 
monitored pollutants: CO, SO2, NO2, O3, Fine SP Matter (PM10) 
• The dominant pollutant with the highest concentration will determine the 
API value; 
• Normally PM10 will be dominant; 
• During late afternoon and early evening O3 can be high too
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Air Quality Index (AQI) Values Levels of Health Concern 
151 to 200 
201 to 300 
301 to 500 
Unhealthy 
Very Unhealthy 
Hazardous 
0 to 50 
51 to 100 
101 to 150 
Good 
Moderate 
Unhealthy 
for Sensitive Groups 
The Air Quality Index
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Threshold level 
• Threshold level = the pollutant level below which no ill effects are 
observed. 
• Above threshold level, the effect of pollutant depends on dose (dose = 
concentration X time of exposure). 
• 3 factors determine level of pollution: 
– Amount of pollutants entering the air 
– Amount of space into which the pollutants are dispersed. 
– Mechanisms that remove pollutants from air
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Environmental Quality (Clean Air) Regulations 1978
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Air Quality Management 
• Air quality management is fundamentally concerned with the achievement 
of economic, awareness and regulatory objectives. 
– Identifying threats to natural ecosystems or population health 
– Informing the public about air quality and raising awareness 
– Determining compliance with national or international standards 
– Providing objective inputs to AQM 
– Policy development and prioritization of management actions 
– Development/validation of management tools 
– Assessing point or area source impacts 
– Trend qualification, to identify future problems or progress against 
management/control targets
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Instrumentation Selection 
• Consider monitoring objectives and data quality objectives 
• Required time resolution of measurement 
• Resource availability 
• Talk to other users 
• Independent type approval/designation 
• Cost/Budget
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Air Pollution Measurement
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Air Pollution Control 
• Two different approaches: 
- Pollution Prevention at the source – the better alternative 
- Treatment of fumes as they are formed – the classical approach 
• Emission control equipment is designed to remove or reduce particulates, 
aerosols (solids and liquid forms), and gaseous byproducts from various sources and, 
in some instances, emissions resulting from inefficient design and operation. 
• The operating principles of aerosol collection equipment include: 
– 1. inertial entrapment by altering the direction and velocity of the effluent; 
– 2. increasing the size of the particles through conglomeration or liquid 
mist entrainment to subject the particles to inertial and gravitational 
forces within the operational range of the control device; 
– 3. impingement of particles on impact surfaces, baffles, or filters; and 
– 4. precipitation of contaminants in electrical fields or by thermal convection. 
• The collection of gases and vapors is based on the particular physical and chemical 
properties of the gases to be controlled.
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Particulate Collectors and Separators 
• Settling chambers 
– the settling of particles larger than 40 m in diameter in trays that can be 
removed for cleaning. Special designs can intercept particles as small 
as 10 m. 
• Cyclones 
– impose a downward spiraling movement on the tangentially directed 
incoming dust-laden gas, causing separation of particles by centrifugal 
force and collection at the bottom of the cone. Particle sizes collected 
range from 5 to 200 m at gas flows of 30 to 25,000 ft3 /min. Removal 
efficiency below 10 m particle size is low. Cyclones can be placed in 
series or combined with other devices to increase removal efficiency.
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cyclone
96 
Collection Efficiency 
In order to calculate the efficiency, first the particle size with 50% collection 
efficiency (dp50%) as the baseline needs to be determined 
μ is dynamic viscosity of air (based on gas temperature) 
b is inlet width, 
Ne is the number of effective turns (number of turns the flow makes from the 
entrance to the midpoint of the core section), 
Vi is inlet velocity and 
ρp is particle density. 
 
N   
e L Z 
(2 ) c c 
c 
H
97 
Empirical Cyclone Collection Efficiency
98
99 
Properties of Dry Air at 1 atm
100 
Air Filters: Baghouse & cloth screen 
• The filter medium governs the temperature of the gas to be filtered, particle 
size removed, capacity and loading, and durability of the filter. 
• Filter operating temperatures vary from about 200F (93C) for wool or 
cotton to 450 to 500F (232–260C) for glass fiber. 
• Baghouse filter: The tubular bags are 5 to 18 in. in diameter and from 2 to 
30 ft in length. The dust-laden gas stream to be filtered passes through the 
bags where the particles build up on the inside and, in so doing, increase 
the filtering efficiency. Periodic shaking of the bags (tubes) causes the 
collected dust to fall off and restore the filtering capacity. The baghouse 
filter has particular application in cement plants, heavy metallurgical 
operations, and other dusty operations. Efficiencies exceeding 99% and 
particle removal below 10 m in size are reported, depending on the major 
form and buildup. Baghouses are usually supplemented by scrubber 
systems.
101 
Cloth-screen filters used in the smaller grinding, tumbling, and abrasive 
cleaning operations. Dust-laden air passes through one or more cloth 
screens in series. The screens are replaced as needed. Other types of filters 
use packed fibers, filter beds, granules, and oil baths. 
Electrostatic Precipitation (ESP) charge the particles by using electrostatic 
force to attract them to wall
102 
Baghouse Cleaning Method 
1. Pulse Jet System: 
Air to Cloth Ratio: 0.033 to 0.083 m/s. 
2. Shaker Style System: 
Air to Cloth Ratio : 0.01 to 0.017 m/s 
3. Reverse Air System: 
Air to Cloth Ratio : 0.01 to 0.02 m/s
103
104 
Calculation for Baghouse 
• Estimate Fan Size 
– air flow rate in cubic feet per minute (cfm), using the surface area of 
the bags and assume a typical air to cloth ratio. The air to cloth ratio is 
the air volume per square foot of bag (cfm). 
Bag Circumference = п x Bag Diameter 
Bag Area = Bag length x bag circumference 
Area of baghouse = Gas flow rate/air to cloth ratio (m/s) 
Number of bag = Area of baghouse / Bag Area
105 
wA 
Q 
 
i e for gravity settling we wrote 
. . : 
Lh with A 
Q 
H h 
v L 
t 
HV 
avg 
replace V with 
avg 
block 
, 
. 
 
 
 
wA 
 1  exp(  ) 
 
D A k 
wA 
 
 
   
1 exp modified , ~ 0.5 
Q 
Deutsch Andersen equation 
Q 
k 
 
mixed 
mixed 
   
 
  
 
 
•Block flow: 
•Mixed flow:
106
107 
Scrubbers are of different types, selected for specific applications. They 
include spray towers, ejector venturis, venturi scrubbers, and packed-bed, 
plate, moving-bed, centrifugal, impingement, and entrainment types. 
• Wet collectors are generally used to remove gases such as hydrogen 
chloride, nitrous oxides, and sulfur dioxide and particles that form as a 
dust, fog, or mist. A high-pressure liquid spray is applied to the gas passing 
through the washer, filter, venturi, or other device. 
• The three important operations of air washers or wet gas scrubbers: 
– Humidification (of air): This process increases size of fine dust 
particles and makes collection easier 
– Contact of liquid and dust filled air: This is the key operation that 
governs collection efficiency of the scrubber. Water droplets in the path 
of the air stream collect dust particles while the air stream flows around 
it 
– Separation of dirty liquid and clean air: During this operation, the dust-water 
mixture accumulates, and as they grow larger, they collect into 
the hopper.
108
109 
table_12_14
110
111 
table_12_13
112 
Removing Sulfur Dioxide – “scrubbers”
113
114 
Example: 
• An aggregate plant at Lime Ridge has been found to be in violation of 
particulate discharge standards. A mechanical shaker baghouse has been 
selected for particulate control. Estimate the number of bags required for a 
gas flow rate of 20m3/s if each back is 15cm in diameter and 12 m in 
length. The manufacturer’s recommended air to cloth ratio for aggregate 
plants is 0.01 m/s. 
• Determine the efficiency of a cyclone having the following characteristic 
for 10μm in diameter with density of 800kg/m3. 
– Cyclone barrel diameter=0.5m 
– Gas flow rate=4m3/s 
– Gas temperature=25°C 
– Dynamic viscosity, μ=18.5 μPa.s
123 
Particulate Matter Chemistry (1 of 4) 
Coagulation: Particles collide and stick together. 
Condensation: Gases condense onto a small solid particle 
to form a liquid droplet. 
Cloud/Fog Processes: Gases dissolve in a water droplet and chemically 
react. A particle exists when the water evaporates. 
Sulfate 
Chemical Reaction: Gases react to form particles.
124 
Particulate Matter Composition (2 of 3) 
NOx 
Ammoni 
a 
VOCs 
PM contains many compounds 
Primary Particles 
(directly emitted) 
Secondary Particles 
(from precursor gases) 
Other 
(sea salt) 
Crustal 
(soil,dust) 
Organic 
Carbon 
Carbon 
(Soot) 
SO2 
Ammonium 
Sulfate 
Ammonium 
Nitrate 
Metals 
Composition of PM 
tells us about 
the sources and 
formation processes 
Gas 
Particle

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Air Pollution Effects and Causes

  • 1. Air Pollution Ms Noor Rosyidah Binti Sajuni School of Engineering rosyidah@ucsi.edu.my
  • 2. 2 Content • Definition, • Unit of measurement, • Sources of air pollution, • Classification of air pollutants, • Type of air pollutants, • Air quality index (AQI), • Effects of pollutant to environment and human, • ozone depletion, • acid rain, • green house effect, • climate change, • global warming, • Meteorology, • air pollution monitoring device, • control and preventive action.
  • 3. 3 Definition Air pollution may be defined as the presence in the air (outdoor atmosphere) of one or more contaminants or combinations thereof in such quantities and of such durations as may be or tend to be injurious to human, animal or plant life, or property, or which unreasonably interferes with the comfortable enjoyment of life or property or conduct of business.
  • 4. 4 Unit of Measurement • Air quality measurement are commonly reported in terms of: – micrograms per cubic meter (μg/m3) – parts per million (ppm) or parts per billion (ppb) • For particulate matter, sizes are expressed in micron or micrometer. – ppm is a volume-to-volume ratio, which makes it independent of local temperature and pressure. ppmx xMWx L m x g g MW gram molecularweight of the gas V P 2 2 2 V P 1 1 1 6 3 3 6 3 : 10 10 / 10 / ( / ) / T T V L mol g m      Standard conditions: V=22.4 L/mol @ 273K & 760 mmHg
  • 5. 5 Source of Air Pollution • Mobile sources -- automobiles, gas-powered lawn tools and mowers, boats, planes etc • Agriculture sources -- Enclosed farm animals – manure release gases eg ammonia; aerial drift of excess fertilizers and pesticides; • Natural -- forest fires, volcanoes, dust storm Volcanoes – ash, acid mist, hydrogen sulfide & other toxic gas.  Sea spray & decaying vegetation – major source of reactive sulfur compound.  Trees & bushes – volatile organic compounds Storms in arid regions –dust clouds. Fermentation in swamp & break-down of cellulose in guts of termites & ruminant animals – ⅔ of world methane (natural gas).
  • 6. 6
  • 7. 7 Geographic Factors • Sources and emission rates of pollution • Topography: Mountains as barriers for air movement, forming temperature inversion layer and promoting pollution over certain areas • Atmospheric conditions: Temperature, cloud cover, and wind affecting the transportation or dispersion of pollutants
  • 8. 8 Classification of Air Pollutants Categories of pollutants ● Primary – emitted directly from a source ● Secondary – formed in the atmosphere from a reaction of primary pollutants It is a substance or effect dwelling temporarily or permanently in the air , which adversely alters the environment by interfering with the health, the comfort, or the food chain, or by interfering with the property values of people. Basic Pollutants Pollutant Abbreviation Type Carbon Monoxide CO Primary SO Primary 2 Sulfur Dioxide O Secondary 3 Ozone NO Secondary 2 Nitrogen Dioxide HC Primary & Secondary Hydrocarbon Compounds (also called VOCs – volatile organic compounds ) Particulate Matter PM Primary & Secondary Lead Pb Primary & Secondary
  • 9. 9 Type of Pollutants • Suspended particulate matter – complex mixture of solid particles & aerosols (liquid particles) suspended in the air. We see these particles as dust, smoke, spores, algal cell & haze. PM smaller than 2.5 micrometers (PM2.5)–most dangerous. • Volatile organic compounds (VOCs) – gasoline, paint solvents & organic cleaning solutions, which evaporate & enter the air in a vapor state, as well as fragments of molecules resulted from the incomplete oxidation of fuels & wastes. VOCs are prime agents of ozone formation. Plants = largest sources of VOCs, ~350 million tons of isoprene (C5H8) & 450 million tons of terpenes (C10H15) each year. About 400 million tons of methane are produced from wetlands & bacteria. • Carbon Monoxide (CO) – Invisible, odorless gas. From incomplete combustion of fuel (coal, oil, charcoal or gas), incineration of biomass or material. ~ 1 billion metric tons release each year, half from human activities.~90% of CO is consumed in photochemical reaction that produce ozone.
  • 10. 10 • Hazardous Air Pollutants (HAPs) -Air toxic include carcinogenic chemicals, radioactive materials & other chemicals (asbestos, vinyl chloride & Benzene). EPA has identified 166 categories of major sources and 8 area sources for HAPs. • Some of the HAPs (EPA)
  • 11. 11 • Nitrogen oxides (NOx).- highly reactive gas formed when nitrogen in fuel or combustion air is heated above 650ºC in the presence of oxygen. Converted to nitric acid=major source of acid deposition. NOx is a lung irritant. • Sulfur oxides (SOx), mainly sulfur dioxide (SO2)-poisonous gas to plant & animal. Converted to sulfuric acid in air. Major source of acid deposition. – Natural sources =evaporation from sea spray, erosion of sulfate-containing dust from arid soils, fumes from volcanoes, biogenic emission of hydrogen sulfide (H2S) & organic sulfur-containing compounds (i.e. dimethylsulfide, methyl mercaptan, carbon disulfide ). – Yearly input to air: 114 million metric ton. Anthropogenic sources = ⅔ of worldwide sulfur flux. Mainly from combustion of sulfur-containing fuel (coal & oil), purification of sour (sulfur-containing) natural gas or oil, smelting of sulfide ores. China & US = largest sources of anthropogenic sulfur (from coal burning).
  • 12. 12 • Lead & heavy metal- World wide lead ~ 2 million metric tons/year, or ⅔ of all metallic air pollution. Most from leaded-gasoline. Lead=metabolic poison & neurotoxin. ~20% of all inner-city children suffer some degree of mental retardation from high Pb level. Mercury (Hg) =neurotoxin. 2 largest sources = coal burning power plants & WASTE INCINERATION. Arsenic (from metal smelter, coal combustion & pesticides. • Ozone & other photochemical oxidant -ozone=ground level pollutant, strong oxidizing reagent & damages vegetation, building material (such as paint, rubber & plastic) & sensitive tissue (eyes & lungs). Hydrocarbons in the air contribute to accumulation of ozone by removing NO in the formation of compounds (such as peroxyacetyl nitrate (PAN), which is another damaging photochemical oxidant.
  • 13. 13 • Haze - Opaque condition of atmosphere caused by tiny suspended solid or liquid particles; Normally from open burning • Industrial & Photochemical Smog -
  • 14. 14 Source: EPA website
  • 16. 16 Temperature Inversion • Several weather conditions intensify levels of industrial & photochemical smogs. • Most significant – temperature inversion. • Temperature inversions are defined as the increase of air temperature with altitude. Such an increase represents a reversal of the normal temperature condition of the troposphere (the region of the atmosphere in contact with the Earth's surface), where temperature usually decreases with height. (Britannica Online, 1998)
  • 17. 17 Temperature Inversion • In (a), daytime temperature highest near ground – earth absorbs heat & radiates to the air near the ground. The warm air near ground rises, carrying pollutants.
  • 18. 18 Temperature Inversion • In (b), 2 types of mechanisms create inversion: 1. Unstable type – cold front slides under an adjacent warmer air mass OR cool air subsides down a mountain slope to displace warmer air in the valley below. 2. Stable type – Rapid night-time cooling in a valley/basin where air movement is restricted. Best example (Los Angeles)-a city surrounded by 3 side mountains & climate is dry & sunny. Lots of aerosol & gaseous chemical from motor vehicles. Skies are generally clear at night, allowing rapid radiant heat loss, and the ground cools quickly. Surface areas are cooled by conduction, while upper layers remain relatively warm. During the night, cool & humid onshore breezes slide in under the contaminated air. Density differences retard vertical mixing.
  • 19. 19
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  • 23. 23 Indoor Air Pollution • Environmental health hazards at homes and workplaces • A variety of substances: Smoke, chemicals, microbes, and radon • Different sources: Insulation materials, wood products, poisonous gases due to poor ventilation, cleaning chemicals, etc. http://gsc.nrcan.gc.ca/gamma/radon_e.php
  • 24. 24 Adverse Effects of Air Pollution on Humans • Air pollution is not a single entity. • Synergistic effects = 2 or more factors combine to produce an effect greater than their simple sum. • I.E. plants & animals may be so stressed by pollution – become > vulnerable to other environmental factors (drought/attack by parasites & disease). • Humans breathe ~ 14 kg of air/day. • Some symptoms of air pollution involve moist surfaces of eyes, nose & throat, the major site of impact is the lungs. • 3 categories of impact: – Chronic: Pollutants cause the gradual deterioration of a variety of physiological functions over a period of years. – Acute: Pollutants bring on life-threatening reactions within a period of hours/days – Carcinogenic: Pollutants initiate changes within cells that lead to uncontrolled growth & division (cancer).
  • 25. 25 Air Pollution – Chronic effects on Humans • Chronic Effects-Almost everyone living in areas of urban air pollution suffers from chronic effects. – Sulfur dioxide (SO2) – long term exposure → bronchitis (inflammation of the bronchi) – Ozone & particulate – inflammation → fibrosis of the lung (scarring that permanently impairs lung function). – CO – reduce the capacity of blood to carry O2 → heart disease. – NO (Nitrogen Oxides) – impair immune system → leaving the lungs open to attack by bacteria & viruses.
  • 27. 27
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  • 30. 30 Air pollution effects on agriculture & forest • Plants are more sensitive than humans. • The pollutant responsible is usually sulfur dioxide. • Forest under stress from pollution = more susceptible to damage by insects & pathogens. • 2 probable ways : – Direct toxic. Within a few days of exposure, molting (discoloration) occurs in leaves due to chlorosis (Bleaching of chlorophyll) and then necrotic (dead) spots develop. If injury is severe, the whole plant may be killed.
  • 31. 31
  • 32. 32 Air pollution effects on agriculture & forest – Air pollutants (ethylene=component of automobile exhaust & release from petroleum refineries & chemical plant), that act as metabolic regulators or plant hormones & disrupt normal patterns of growth & development. – The concentration of ethylene around highways & industrial areas is often high enough to cause injury to sensitive plant. – Synergistic effect – when white pine seedlings are exposed to sub-threshold [Ozone] & [SO2] individually, no visible injury occurs. If the same [ ] of ozone & SO2 given together, visible damage occurs. In alfalfa, ozone & SO2 together cause less damage than either one alone.
  • 33. 33 Aquatic Effects • Reproduction is the most sensitive stage in fish life cycles. • Eggs & fry of many spp. of fish are killed when pH drops to ~ 5.0. • pH lower than 5 disrupt food chain, killing aquatic plants, insects & invertebrate & adult fish. • Trout, salmon & other game fish are usually the most sensitive. • Carpgar, suckers & other less desirable fish are more resistant. • Acidity alters body chemistry, destroys gills & prevents oxygen uptake, causes bone decalcification, & disrupt muscle contraction. • Acid water also leaches toxic metals such as mercury & aluminium out of soil & rocks.
  • 34. 34 Air pollution effects on materials • Mechanism of deterioration – Abrasion – Deposition – Indirect chemical attack – Direct chemical attack – Electrochemical corrosion • Factor influence the rate of deterioration – Moisture – Sunlight – Temperature – Position of exposed material
  • 35. 35 Acid Rain • Pure rainwater is slightly acidic, (dissolved carbon dioxide). • Air also contains naturally occurring organic acids and acidic particles. • The pH of unpolluted rainwater ranges from about 6 to just below 5. • Air compounds containing oxides of sulfur and nitrogen : – may then dissolve in cloud droplets, making rainwater more acidic (wet deposition), or – may mix through the atmosphere, eventually coming into direct contact with the ground and vegetation (dry deposition). • Both forms can harm soil, lakes, plants, buildings and people • More industrial activity in the northern hemisphere. • Industry also tends to be concentrated in particular regions. This is why acid rain problems are worse in the northern hemisphere.
  • 36. 36
  • 37. 37 Ozone Depletion • Ozone forms a layer in the stratosphere (20-40km and up) that provides a barrier to ultraviolet (UV) radiation. • Although oxygen serves as a barrier to UV radiation, it absorb only over a narrow band centered at wavelength of 0.2 μm. http://ozone.unep.org
  • 39. 39 Montreal Protocol 1988 • Following the discovery of the Antarctic ozone hole in late 1985, governments recognized the need for stronger measures to reduce the production and consumption of a number of CFCs (CFC 11, 12, 113, 114, and 115) and several Halons (1211, 1301, 2402). • The first general ozone agreement was on 1985. This agreement, known as the Vienna Convention for the Protection of the Ozone Layer. • Later, the Montreal Protocol on Substances that Deplete the Ozone Layer was adopted on 16 September 1987 at the Headquarters of the International Civil Aviation Organization in Montreal. The Protocol came into force on 1st January 1989, when it was ratified by 29 countries and the EEC. Since then several other countries have ratified it. • The Montreal Protocol and its Amendment constitute a mechanism for the phasing out of ozone depleting substances. • The control measures and phase out schedules cover both the production and the consumption of the target substances. However, even after phase out both developed and developing countries are permitted to produce limited quantities in order to meet the essential uses for which no alternatives have yet been identified http://ozone.unep.org
  • 40. 40 Helsinki Declaration 1989 • Encourage all states that have not done so to join the Vienna Convention for the Protection of the Ozone Layer and its Montreal Protocol • Agree to phase out the production and the consumption of CFCs controlled by the Montreal Protocol as soon as possible but not later than the year 2000 • Agree to phase out the production and the consumption of CFCs controlled by the Montreal Protocol as soon as possible but not later than the year 2000 • Agree to commit themselves, in proportion to their means and resources, to accelerate the development of environmentally acceptable substituting chemicals, products and technologies • Agree to facilitate the access of developing countries to relevant scientific information, research results and training and to seek to develop appropriate funding mechanisms to facilitate the transfer of technology and replacement of equipment at minimum cost to developing countries. http://ozone.unep.org
  • 41. 41 Climate Change/ Global Warming
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  • 43. 43
  • 44. 44 Climate Change/ Global Warming • Since 1850, the average global temperature is up by 0.76 °C • Most of the warming happened in the last 50 years, due to human activities. • Causes: burning fossil fuels for energy, agriculture, deforestation • We are already seeing climate change impacts like heat waves and more extreme weather events • Countries began discussing climate change in 1992, with the creation of the UN Framework Convention on Climate Change (UNFCC) • The first international commitments to cut CO2 came with the Kyoto Protocol in 1997 • The EU played a leading role in past agreements and advocates strong future action
  • 45. 45 Effects Of Climate Change On Mercury And Persistent Organic Pollutants Precipitation Winds Exchange with Surface reservoirs Chemistry
  • 46. 46
  • 47. 47 Kyoto Protocol • Only a first step • It only runs until the end of 2012 • Not all countries are on board – including the US • It doesn't contain commitments for developing countries, and their emissions are fast catching up with those of developed countries • A new agreement is needed • It must be more ambitious, with long-term commitments to deeper cuts • Developed and developing countries need to act • We must keep the commitment to limit warming to 2ºC • Global CO2 emissions need to peak by 2020 and halve by 2050 • Kyoto's successor must include support for developing countries and adaptation
  • 48. 48 EU actions In December 2008, European leaders agreed the climate and energy package, with ambitious targets for 2020. The package means: – 20% cut in greenhouse gas emissions by 2020 – 30% if other developed countries agree – 20% of energy from renewable sources – 20% increase in energy efficiency Concrete steps in package include: • An extension of emissions trading system • Support for carbon capture and storage • Country-specific targets for renewable energy
  • 49. 49 Air Pollution Meteorology • An air pollution problem involves three parts: the source, the movement of the pollutant and the recipient. • All meteorological phenomena are a result of interaction of the elemental properties of the atmosphere, heat, pressure, wind and moisture. • The rotation of the earth couple with heat conductivities of the ocean and land produced weather.
  • 50. 50 Mechanical Turbulence • Random fluctuation of wind velocity (speed and direction) • Wind is zero at ground surface and rise with elevation to near the speed imposed by the pressure gradient. • The greater the mean wind speed, the greater the turbulence. • The more the mechanical turbulence, the easier it is to disperse the spread the atmospheric pollutants. Thermal Turbulence • Different of air circulation during day time and nights. • During clear nights when the ground radiates its heat away to the cold night sky and the cold air above it causing a sinking density current.
  • 51. 51 Cyclonic conditions • Areas of Low pressure are generally – fast moving, – associated with strong winds and bad weather (tornadoes and hurricanes) – upward motion, clouds and precipitation  all result in low pollutant concentrations Anticyclonic conditions • High pressure areas have the opposite conditions: – Often slow moving and stagnant – Associated with weak pressure gradients and light winds – Downward motion – clear skies and good weather – Formation of a subsidence inversion that stabilizes the atmosphere and limits vertical mixing  Conditions that lead to stagnation and high pollutant concentrations
  • 52. 52 Atmospheric Stability • Tendency of atmosphere to resist or enhance vertical motion. • Affects dispersion of pollutants • It is related with wind speed and change of air temperature with height (lapse rate, Г) • Lapse rate is the indicator for atmospheric stability. • 3 stability categories: neutral, unstable and stable. • Unstable atmosphere: Mechanical turbulence enhanced by thermal turbulence. The temperature of atmosphere greater than Г : Superadiabatic. Eg. Hot air balloon. • Neutral stability: Г increased or decreased by the parcel of air that expand or contracts adiabatically as it is raised through atmosphere. • Stable atmosphere: Temperature of the atmosphere less than Г it is call subadiabatic.
  • 53. 53 Determine Atmospheric Stability • Stability is the tendency of the atmosphere to resist and enhance vertical motion. • Lapse rate is the change of air temperature with height. • There are 3 stability categories: – Neutral Atmosphere – Unstable Atmosphere – Stable Atmosphere • Mathematically, atmospheric stability can be determine as: T T T   2 1 : Z Z 2 1 Z Lapse Rate   
  • 54. 54 Vertical Temperature Profiles Environmental lapse rate (ELR) Dry adiabatic lapse rate (DALR) If, ELR > DALR =sub adiabatic condition, atmosphere is stable. ELR >> DALR= Inversion conditions. Very stable atmosphere. ELR= DALR= atmosphere is neutral. ELR< DALR = super adiabatic condition, atmosphere is unstable. Shapes of plumes depends upon atmospheric stability conditions.
  • 55. 55
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  • 58. Subsidence inversion due to adiabatic warming of downward moving air (usually in an area of High Pressure)
  • 59. 59 Stability Classes • Developed for use in dispersion models • Stability classified into 6 classes (A – F) • A: strongly unstable • B: moderately unstable • C: slightly unstable • D: neutral • E: slightly stable • F: moderately stable Surface wind speed at 10 m (m/s) Day Night Incoming Solar radiation Cloud Cover Strong Moderate Slight Thinly Overcast Mostly Cloudy < 2 A (s = 1) A-B B (s = 2) 2-3 A-B B C (s = 3) E (s = 5) F (s = 6) 3-5 B B-C C D E 5-6 C C-D D (s = 4) D D >6 C D D D D
  • 60. 60 Atmospheric Dispersion • Emission point characteristic • Nature of pollutant • Meteorology • Terrain • Anthropogenic structures
  • 61. 61 Effect of wind • Wind diffuses pollutants by stretching them along the wind direction. • Wind speed also enhances turbulence, and thus vertical and horizontal diffusion. • Variations in wind direction are also important as they lead to sinuous plumes • The greatest potential for pollution is in low wind situations because horizontal transport and turbulent diffusion are both curtailed. • Local circulations (land/sea breezes etc.) are not good pollution ventilators because they are associated with low wind speeds, they are closed systems, and there usually is a diurnal reversal → pollution comes back.
  • 62. 64 C: Inversions • Temperature inversions represent a situation in which the atmosphere is very stable and the mixing depth is significantly restricted. • When an inversion exists and winds are light, diffusion is inhibited and high pollution concentrations are to be expected in areas where pollution sources exist. • Surface temperature inversions form because the ground is a more effective radiator than the air above. Inversions aloft are associated with sinking air that characterizes centers of high air pressure (anticyclones).
  • 64. 66 This is an example of a generalized temperature profile for a surface inversion. Temperature-profile changes in bottom diagram after the sun has heated the surface.
  • 66. 68 D: Air Mixing Depth • The direct effect of wind speed is to influence the concentration of pollutants. • Atmospheric stability determines the extent to which vertical motions will mix the pollution with cleaner air above the surface layers. • The vertical distance between Earth's surface and the height to which convectional movements extend is called the mixing depth. • Generally, the greater the mixing depth, the better the air quality.
  • 67. 69 Mixing Height of atmosphere The height of the base of the inversion layer from ground surface.
  • 68. 70 Stacks in Industry  Emissions from industrial stacks are regulated to protect human and environmental health  Industrial facilities are required to obtain permits to emit into the atmosphere and to demonstrate their compliance with regulations  In the process of applying for permits, dispersion models are generally used to assess the impact of point source emission • A dispersion model is essentially a computational procedure for predicting concentrations downwind of a pollutant source • Routinely used in:  Environmental impact assessments  Risk analysis  Emergency planning
  • 69. 71 Classes of Air Quality Models  The air quality modeling procedures can be categorized into four generic classes: Gaussian, numerical, statistical or empirical and physical  The emphasis is on Gaussian-plume type models for continuous releases, which are at the core of most U.S. Environmental Protection Agency (EPA) regulatory models  Gaussian models are the most widely used techniques for estimating the impact of nonreactive pollutants. Model Parameters  The model is based on our knowledge of the following parameters:  The emissions characteristics (stack exit velocity, plume rise, temperature, stack diameter)  Terrain (surface roughness, local topography, nearby buildings)  State of the atmosphere (wind speed, stability, mixing height, wind direction)
  • 70. 72
  • 71. 73 Dispersion = Advection (Transport) + Dilution (Diffusion) Transport Source Receptor Re-entrainment Fick’s law of diffusion J= - D * D C/Dx Where, J= Mass Flux; D = Diffusivity coefficient,; D C/Dx = Concentration gradient Diffusion of pollutants occur due to turbulence, which further depends upon many factors: a. Ambient temperature b. Temperature of emissions c. Roughness factors d. Wind velocity e. Wind direction f. Humidity g. Stability
  • 73. 75 General Characteristics of Stack Plumes • Dispersion of pollutants • Wind – carries pollution downstream from source • Atmospheric turbulence -- causes pollutants to fluctuate from mainstream in vertical and crosswind directions • Mechanical & atmospheric heating both present at same time but in varying ratios • Affect plume dispersion differently
  • 74. 76 Plume Types • Plume types are important because they help us understand under what conditions there will be higher concentrations of contaminants at ground level.
  • 75. 77 Looping Plume • High degree of convective turbulence • Superadiabatic lapse rate -- strong instabilities • Associated with clear daytime conditions accompanied by strong solar heating & light winds • High probability of high concentrations sporadically at ground level close to stack. • Occurs in unstable atmospheric conditions.
  • 76. 78 Coning Plume • Stable with small-scale turbulence • Associated with overcast moderate to strong winds • Roughly 10° cone • Pollutants travel fairly long distances before reaching ground level in significant amounts • Occurs in neutral atmospheric conditions
  • 77. 79 Fanning Plume • Occurs under large negative lapse rate • Strong inversion at a considerable distance above the stack • Extremely stable atmosphere • Little turbulence • If plume density is similar to air, travels downwind at approximately same elevation
  • 78. 80 Lofting Plume • Favorable in the sense that fewer impacts at ground level. • Pollutants go up into environment. • They are created when atmospheric conditions are unstable above the plume and stable below.
  • 79. 81 Fumigation • Most dangerous plume: contaminants are all coming down to ground level. • They are created when atmospheric conditions are stable above the plume and unstable below. • This happens most often after the daylight sun has warmed the atmosphere, which turns a night time fanning plume into fumigation for about a half an hour.
  • 80. 82 Legislation & Standards • Topographic, meteorological, and land-use characteristics of areas within an air region will vary. • The social and economic development of an area will result in different degrees of air pollution and demands for air quality.
  • 81. 83 Air Quality Monitoring : Air Pollutant Index (API) or Air Quality Index (AQI) • A general index used to assess air quality; • Values calculated based on the average concentration of each of the monitored pollutants: CO, SO2, NO2, O3, Fine SP Matter (PM10) • The dominant pollutant with the highest concentration will determine the API value; • Normally PM10 will be dominant; • During late afternoon and early evening O3 can be high too
  • 82. 84 Air Quality Index (AQI) Values Levels of Health Concern 151 to 200 201 to 300 301 to 500 Unhealthy Very Unhealthy Hazardous 0 to 50 51 to 100 101 to 150 Good Moderate Unhealthy for Sensitive Groups The Air Quality Index
  • 83. 85
  • 84. 86 Threshold level • Threshold level = the pollutant level below which no ill effects are observed. • Above threshold level, the effect of pollutant depends on dose (dose = concentration X time of exposure). • 3 factors determine level of pollution: – Amount of pollutants entering the air – Amount of space into which the pollutants are dispersed. – Mechanisms that remove pollutants from air
  • 85. 87 Environmental Quality (Clean Air) Regulations 1978
  • 86. 88 Air Quality Management • Air quality management is fundamentally concerned with the achievement of economic, awareness and regulatory objectives. – Identifying threats to natural ecosystems or population health – Informing the public about air quality and raising awareness – Determining compliance with national or international standards – Providing objective inputs to AQM – Policy development and prioritization of management actions – Development/validation of management tools – Assessing point or area source impacts – Trend qualification, to identify future problems or progress against management/control targets
  • 87. 89 Instrumentation Selection • Consider monitoring objectives and data quality objectives • Required time resolution of measurement • Resource availability • Talk to other users • Independent type approval/designation • Cost/Budget
  • 88. 90
  • 89. 91 Air Pollution Measurement
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  • 91. 93 Air Pollution Control • Two different approaches: - Pollution Prevention at the source – the better alternative - Treatment of fumes as they are formed – the classical approach • Emission control equipment is designed to remove or reduce particulates, aerosols (solids and liquid forms), and gaseous byproducts from various sources and, in some instances, emissions resulting from inefficient design and operation. • The operating principles of aerosol collection equipment include: – 1. inertial entrapment by altering the direction and velocity of the effluent; – 2. increasing the size of the particles through conglomeration or liquid mist entrainment to subject the particles to inertial and gravitational forces within the operational range of the control device; – 3. impingement of particles on impact surfaces, baffles, or filters; and – 4. precipitation of contaminants in electrical fields or by thermal convection. • The collection of gases and vapors is based on the particular physical and chemical properties of the gases to be controlled.
  • 92. 94 Particulate Collectors and Separators • Settling chambers – the settling of particles larger than 40 m in diameter in trays that can be removed for cleaning. Special designs can intercept particles as small as 10 m. • Cyclones – impose a downward spiraling movement on the tangentially directed incoming dust-laden gas, causing separation of particles by centrifugal force and collection at the bottom of the cone. Particle sizes collected range from 5 to 200 m at gas flows of 30 to 25,000 ft3 /min. Removal efficiency below 10 m particle size is low. Cyclones can be placed in series or combined with other devices to increase removal efficiency.
  • 94. 96 Collection Efficiency In order to calculate the efficiency, first the particle size with 50% collection efficiency (dp50%) as the baseline needs to be determined μ is dynamic viscosity of air (based on gas temperature) b is inlet width, Ne is the number of effective turns (number of turns the flow makes from the entrance to the midpoint of the core section), Vi is inlet velocity and ρp is particle density.  N   e L Z (2 ) c c c H
  • 95. 97 Empirical Cyclone Collection Efficiency
  • 96. 98
  • 97. 99 Properties of Dry Air at 1 atm
  • 98. 100 Air Filters: Baghouse & cloth screen • The filter medium governs the temperature of the gas to be filtered, particle size removed, capacity and loading, and durability of the filter. • Filter operating temperatures vary from about 200F (93C) for wool or cotton to 450 to 500F (232–260C) for glass fiber. • Baghouse filter: The tubular bags are 5 to 18 in. in diameter and from 2 to 30 ft in length. The dust-laden gas stream to be filtered passes through the bags where the particles build up on the inside and, in so doing, increase the filtering efficiency. Periodic shaking of the bags (tubes) causes the collected dust to fall off and restore the filtering capacity. The baghouse filter has particular application in cement plants, heavy metallurgical operations, and other dusty operations. Efficiencies exceeding 99% and particle removal below 10 m in size are reported, depending on the major form and buildup. Baghouses are usually supplemented by scrubber systems.
  • 99. 101 Cloth-screen filters used in the smaller grinding, tumbling, and abrasive cleaning operations. Dust-laden air passes through one or more cloth screens in series. The screens are replaced as needed. Other types of filters use packed fibers, filter beds, granules, and oil baths. Electrostatic Precipitation (ESP) charge the particles by using electrostatic force to attract them to wall
  • 100. 102 Baghouse Cleaning Method 1. Pulse Jet System: Air to Cloth Ratio: 0.033 to 0.083 m/s. 2. Shaker Style System: Air to Cloth Ratio : 0.01 to 0.017 m/s 3. Reverse Air System: Air to Cloth Ratio : 0.01 to 0.02 m/s
  • 101. 103
  • 102. 104 Calculation for Baghouse • Estimate Fan Size – air flow rate in cubic feet per minute (cfm), using the surface area of the bags and assume a typical air to cloth ratio. The air to cloth ratio is the air volume per square foot of bag (cfm). Bag Circumference = п x Bag Diameter Bag Area = Bag length x bag circumference Area of baghouse = Gas flow rate/air to cloth ratio (m/s) Number of bag = Area of baghouse / Bag Area
  • 103. 105 wA Q  i e for gravity settling we wrote . . : Lh with A Q H h v L t HV avg replace V with avg block , .    wA  1  exp(  )  D A k wA      1 exp modified , ~ 0.5 Q Deutsch Andersen equation Q k  mixed mixed         •Block flow: •Mixed flow:
  • 104. 106
  • 105. 107 Scrubbers are of different types, selected for specific applications. They include spray towers, ejector venturis, venturi scrubbers, and packed-bed, plate, moving-bed, centrifugal, impingement, and entrainment types. • Wet collectors are generally used to remove gases such as hydrogen chloride, nitrous oxides, and sulfur dioxide and particles that form as a dust, fog, or mist. A high-pressure liquid spray is applied to the gas passing through the washer, filter, venturi, or other device. • The three important operations of air washers or wet gas scrubbers: – Humidification (of air): This process increases size of fine dust particles and makes collection easier – Contact of liquid and dust filled air: This is the key operation that governs collection efficiency of the scrubber. Water droplets in the path of the air stream collect dust particles while the air stream flows around it – Separation of dirty liquid and clean air: During this operation, the dust-water mixture accumulates, and as they grow larger, they collect into the hopper.
  • 106. 108
  • 108. 110
  • 110. 112 Removing Sulfur Dioxide – “scrubbers”
  • 111. 113
  • 112. 114 Example: • An aggregate plant at Lime Ridge has been found to be in violation of particulate discharge standards. A mechanical shaker baghouse has been selected for particulate control. Estimate the number of bags required for a gas flow rate of 20m3/s if each back is 15cm in diameter and 12 m in length. The manufacturer’s recommended air to cloth ratio for aggregate plants is 0.01 m/s. • Determine the efficiency of a cyclone having the following characteristic for 10μm in diameter with density of 800kg/m3. – Cyclone barrel diameter=0.5m – Gas flow rate=4m3/s – Gas temperature=25°C – Dynamic viscosity, μ=18.5 μPa.s
  • 113. 123 Particulate Matter Chemistry (1 of 4) Coagulation: Particles collide and stick together. Condensation: Gases condense onto a small solid particle to form a liquid droplet. Cloud/Fog Processes: Gases dissolve in a water droplet and chemically react. A particle exists when the water evaporates. Sulfate Chemical Reaction: Gases react to form particles.
  • 114. 124 Particulate Matter Composition (2 of 3) NOx Ammoni a VOCs PM contains many compounds Primary Particles (directly emitted) Secondary Particles (from precursor gases) Other (sea salt) Crustal (soil,dust) Organic Carbon Carbon (Soot) SO2 Ammonium Sulfate Ammonium Nitrate Metals Composition of PM tells us about the sources and formation processes Gas Particle