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Air Pollution
DSE-III
Dr. Banita Pattnaik
Faculty in Chemistry,
Rama Devi Women’s University
1
o Major regions of Atmosphere
o Atmosphere as a Resource
o Types and Sources of Air Pollution
• Major Classes of Air Pollutants
• Sources of Outdoor Air Pollutants
• Urban Air Pollution
o Chemical and photochemical reactions in
atmosphere
o Photochemical smog: its constituents and
photochemistry
o Effects of Air Pollution
2
Major Regions of Atmosphere: On the basis of temperature:
What is atmosphere? Discuss the different zones of atmosphere.
3
Troposphere (Tropo = turning or changing)
• Bottom layer 🡪 from Earth’s surface to about 12
kilometers altitude (0 to 7.5 miles)
• Where we live & weather happens, clouds form, air
moves a lot here 🡪it’s turbulent and well-mixed
• gets colder with increasing altitude…to about -550 C (-
670 F) at the top (tropopause) (Temperature range 150C to
-560C)
Think about how it gets colder on a mountain?
4
Troposphere
o most of atmosphere’s
mass is here 🡪 the
densest layer because
gravitational pull is
stronger here
o Jet stream is in
upper troposphere &
lower stratosphere…
o Airplanes do not fly
higher than about 11
km …~7 miles up
5
Stratosphere: Strato = layer or “spreading
out” ...air does not move a lot here
o above the troposphere
o You can see where it begins
because large cumulonimbus
storm clouds reach into and
stop at the lower stratosphere
o Extends to ~50 km (31 mi)
o Way less air pressure
here…less mass above, less
density and less gravitational
force
6
Stratosphere
o OZONE is formed in this
layer….O3 absorbs most UV
radiation from sun
o temperatures increase with
altitude in the stratosphere
because of ozone.
As ozone molecules absorb UV they
get energized, move faster and
produce heat
Is ozone
good or
bad?
7
Mesosphere
o ~50-90 km (31 – 50 mi)
o meso = middle
o 99.9% of mass lies below the
mesosphere
o Not enough oxygen to
breathe but % is still the
same (What % is that?)
o Most meteoroids burn up
here…. the air is very thin,
but still dense enough to
slow down meteoroids due
because of friction
8
Mesosphere
o There is not an ozone layer to cause heating
so, temperatures decrease with altitude in
the mesophere
o Coldest layer! down to -1480 F (-1000C ) at
the mesopause…
What is a
“pause”?
What is a “pause”?
9
Thermosphere
o Above the mesosphere to ~690 km
(430 miles)….with no real upper limit
🡪 space!
o least dense of all layers …. few
molecules are far apart & moving
fast because of radiation absorption
10
Thermosphere
o temps can reach 2,0000
C (3,6000 F) … but would
feel very cold…too few
hot molecules to transfer
heat
o Temperatures can vary greatly
here because of solar activity
o Thermo = heat
o Sometimes divided into
two layers : ionosphere
and exosphere
11
Ionosphere
o lower part of thermosphere
o solar radiation very strong here & is absorbed by
the few oxygen & nitrogen molecules resulting in
electrically charged gas particles (ions) that cause
heat (O2
+, O+
, NO+)
o AM radio waves bounce off these ions and back
to earth
o Aurora Borealis(Northern Lights) ….glowing ions
12
Exosphere
o ” Outer thermosphere & outermost layer
of the atmosphere
o Exo = “outer(To infinity & beyond! )
o Satellites orbit here
o Atoms & molecules
escape into space here
o TV & cell phone signals
travel to satellites here
and are bounced back
13
Atmosphere as a Resource
o Atmospheric Composition
• Nitrogen 78.08%
• Oxygen 20.95%
• Argon 0.93%
• Carbon dioxide 0.04%
o Ecosystem services
• Blocks UV radiation
• Moderates the climate
• Redistributes water in the
hydrologic cycle
14
Air Pollution
Chemicals added to the atmosphere by natural events or
human activities in high enough concentrations to be
harmful.
or
It is the direct or indirect changes in one/more components
of biosphere that are harmful for living entities.
Air Pollution
15
Types and Sources of Air Pollution
Two categories:
oNatural
• Forest fire by lightening
• Soil erosion
• Volcanic eruption
• Decomposition of organic matter and natural
radioactivity
o From human activity
• U V radiation due to Ozone layer depletion
• Nuclear fall out radioactive materials
• From industries
• From burning of fossil fuel
16
Two categories
o Primary Air Pollutant (Contributes ~ 90%)
• Harmful substance that is emitted
directly into the atmosphere
o Secondary Air Pollutant
• Harmful substance formed in the
atmosphere when a primary air pollutant
reacts with substances normally found in
the atmosphere or with other air
pollutants
Types and Sources of Air Pollution
17
Major Air Pollutants
18
19
Chemical and Photochemical
Reactions
20
Major Classes of Air Pollutants
o Carbon Oxides
o Hydrocarbons
o Nitrogen Oxides
o Sulfur Oxides
o Particulate Material
o Ozone
21
Carbon Oxides and Hydrocarbons
o Carbon Oxides
• Gases carbon monoxide (CO) and carbon
dioxide (CO2)
• Greenhouse gases
o Hydrocarbons
• Diverse group of organic compounds that
contain only hydrogen and carbon (ex: CH4-
methane)
• Some are related to photochemical smog and
greenhouse gases
22
Nitrogen and Sulfur Oxides
o Nitrogen Oxides
• Gases produced by the chemical interactions
between atmospheric nitrogen and oxygen at
high temperature
• Problems
• Greenhouse gases
• Cause difficulty breathing
o Sulfur Oxides
• Gases produced by the chemical interactions
between sulfur and oxygen
• Causes acid precipitation
23
Particulate Material
o Thousands of different solid or liquid
particles suspended in air
• Includes: soil particles, soot, lead, zinc,
asbestos, sea salt, and sulfuric acid droplets
o Dangerous for two reasons
• May contain materials with toxic or
carcinogenic effects
• Extremely small particles can become lodged in
lungs
24
Ozone
o Tropospheric Ozone
• Man- made pollutant in the lower atmosphere
• Secondary air pollutant
• Component of photochemical smog
o Stratospheric Ozone
• Essential component that screens out UV
radiation in the upper atmosphere
• Man- made pollutants (ex: CFCs) can destroy it
O2 plays an important role in Troposphere and O3 in Stratosphere
25
Sources of Outdoor Air Pollution
o Two main sources
• Transportation
• Industry
o Intentional forest
fires is also high
26
Urban Air Pollution
o Photochemical Smog (ex: Los Angeles below)
• Brownish-orange haze formed by chemical reactions
involving sunlight, nitrogen oxide, and hydrocarbons
27
Two very important Factors on
Atmospheric chemistry
Important Gaseous Atmospheric Chemical Species
28
Gaseous atmospheric Chemical Species
o Sunlight of U V region and Hydroxyl radicals (OH.)
are important as it provides a way to pump high level
of energy into a single gas molecule to start a series
of Chemical reactions.
o Hydroxyl free radicals are the most reactive
intermediate and currency of day time atmospheric
phenomena where as NO3 radicals are important
intermediate in night time atmospheric chemistry.
o Both solid and liquid particles in atmospheric aerosols
and clouds serve as sources and sinks for gas-phase
species, as sites for surface reactions.
29

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Air_Pollution_1.pptx

  • 1. Air Pollution DSE-III Dr. Banita Pattnaik Faculty in Chemistry, Rama Devi Women’s University 1
  • 2. o Major regions of Atmosphere o Atmosphere as a Resource o Types and Sources of Air Pollution • Major Classes of Air Pollutants • Sources of Outdoor Air Pollutants • Urban Air Pollution o Chemical and photochemical reactions in atmosphere o Photochemical smog: its constituents and photochemistry o Effects of Air Pollution 2
  • 3. Major Regions of Atmosphere: On the basis of temperature: What is atmosphere? Discuss the different zones of atmosphere. 3
  • 4. Troposphere (Tropo = turning or changing) • Bottom layer 🡪 from Earth’s surface to about 12 kilometers altitude (0 to 7.5 miles) • Where we live & weather happens, clouds form, air moves a lot here 🡪it’s turbulent and well-mixed • gets colder with increasing altitude…to about -550 C (- 670 F) at the top (tropopause) (Temperature range 150C to -560C) Think about how it gets colder on a mountain? 4
  • 5. Troposphere o most of atmosphere’s mass is here 🡪 the densest layer because gravitational pull is stronger here o Jet stream is in upper troposphere & lower stratosphere… o Airplanes do not fly higher than about 11 km …~7 miles up 5
  • 6. Stratosphere: Strato = layer or “spreading out” ...air does not move a lot here o above the troposphere o You can see where it begins because large cumulonimbus storm clouds reach into and stop at the lower stratosphere o Extends to ~50 km (31 mi) o Way less air pressure here…less mass above, less density and less gravitational force 6
  • 7. Stratosphere o OZONE is formed in this layer….O3 absorbs most UV radiation from sun o temperatures increase with altitude in the stratosphere because of ozone. As ozone molecules absorb UV they get energized, move faster and produce heat Is ozone good or bad? 7
  • 8. Mesosphere o ~50-90 km (31 – 50 mi) o meso = middle o 99.9% of mass lies below the mesosphere o Not enough oxygen to breathe but % is still the same (What % is that?) o Most meteoroids burn up here…. the air is very thin, but still dense enough to slow down meteoroids due because of friction 8
  • 9. Mesosphere o There is not an ozone layer to cause heating so, temperatures decrease with altitude in the mesophere o Coldest layer! down to -1480 F (-1000C ) at the mesopause… What is a “pause”? What is a “pause”? 9
  • 10. Thermosphere o Above the mesosphere to ~690 km (430 miles)….with no real upper limit 🡪 space! o least dense of all layers …. few molecules are far apart & moving fast because of radiation absorption 10
  • 11. Thermosphere o temps can reach 2,0000 C (3,6000 F) … but would feel very cold…too few hot molecules to transfer heat o Temperatures can vary greatly here because of solar activity o Thermo = heat o Sometimes divided into two layers : ionosphere and exosphere 11
  • 12. Ionosphere o lower part of thermosphere o solar radiation very strong here & is absorbed by the few oxygen & nitrogen molecules resulting in electrically charged gas particles (ions) that cause heat (O2 +, O+ , NO+) o AM radio waves bounce off these ions and back to earth o Aurora Borealis(Northern Lights) ….glowing ions 12
  • 13. Exosphere o ” Outer thermosphere & outermost layer of the atmosphere o Exo = “outer(To infinity & beyond! ) o Satellites orbit here o Atoms & molecules escape into space here o TV & cell phone signals travel to satellites here and are bounced back 13
  • 14. Atmosphere as a Resource o Atmospheric Composition • Nitrogen 78.08% • Oxygen 20.95% • Argon 0.93% • Carbon dioxide 0.04% o Ecosystem services • Blocks UV radiation • Moderates the climate • Redistributes water in the hydrologic cycle 14
  • 15. Air Pollution Chemicals added to the atmosphere by natural events or human activities in high enough concentrations to be harmful. or It is the direct or indirect changes in one/more components of biosphere that are harmful for living entities. Air Pollution 15
  • 16. Types and Sources of Air Pollution Two categories: oNatural • Forest fire by lightening • Soil erosion • Volcanic eruption • Decomposition of organic matter and natural radioactivity o From human activity • U V radiation due to Ozone layer depletion • Nuclear fall out radioactive materials • From industries • From burning of fossil fuel 16
  • 17. Two categories o Primary Air Pollutant (Contributes ~ 90%) • Harmful substance that is emitted directly into the atmosphere o Secondary Air Pollutant • Harmful substance formed in the atmosphere when a primary air pollutant reacts with substances normally found in the atmosphere or with other air pollutants Types and Sources of Air Pollution 17
  • 19. 19
  • 21. Major Classes of Air Pollutants o Carbon Oxides o Hydrocarbons o Nitrogen Oxides o Sulfur Oxides o Particulate Material o Ozone 21
  • 22. Carbon Oxides and Hydrocarbons o Carbon Oxides • Gases carbon monoxide (CO) and carbon dioxide (CO2) • Greenhouse gases o Hydrocarbons • Diverse group of organic compounds that contain only hydrogen and carbon (ex: CH4- methane) • Some are related to photochemical smog and greenhouse gases 22
  • 23. Nitrogen and Sulfur Oxides o Nitrogen Oxides • Gases produced by the chemical interactions between atmospheric nitrogen and oxygen at high temperature • Problems • Greenhouse gases • Cause difficulty breathing o Sulfur Oxides • Gases produced by the chemical interactions between sulfur and oxygen • Causes acid precipitation 23
  • 24. Particulate Material o Thousands of different solid or liquid particles suspended in air • Includes: soil particles, soot, lead, zinc, asbestos, sea salt, and sulfuric acid droplets o Dangerous for two reasons • May contain materials with toxic or carcinogenic effects • Extremely small particles can become lodged in lungs 24
  • 25. Ozone o Tropospheric Ozone • Man- made pollutant in the lower atmosphere • Secondary air pollutant • Component of photochemical smog o Stratospheric Ozone • Essential component that screens out UV radiation in the upper atmosphere • Man- made pollutants (ex: CFCs) can destroy it O2 plays an important role in Troposphere and O3 in Stratosphere 25
  • 26. Sources of Outdoor Air Pollution o Two main sources • Transportation • Industry o Intentional forest fires is also high 26
  • 27. Urban Air Pollution o Photochemical Smog (ex: Los Angeles below) • Brownish-orange haze formed by chemical reactions involving sunlight, nitrogen oxide, and hydrocarbons 27
  • 28. Two very important Factors on Atmospheric chemistry Important Gaseous Atmospheric Chemical Species 28
  • 29. Gaseous atmospheric Chemical Species o Sunlight of U V region and Hydroxyl radicals (OH.) are important as it provides a way to pump high level of energy into a single gas molecule to start a series of Chemical reactions. o Hydroxyl free radicals are the most reactive intermediate and currency of day time atmospheric phenomena where as NO3 radicals are important intermediate in night time atmospheric chemistry. o Both solid and liquid particles in atmospheric aerosols and clouds serve as sources and sinks for gas-phase species, as sites for surface reactions. 29