air_pollutants_sources and potency.pptx
TRANSCRIPT
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Introduction
The composition and chemistry of the atmosphere is of importancebecause of the interactions between the atmosphere and living organisms.
The composition of the Earth's atmosphere has been changed by humanactivity and some of these changes are harmful to human health, cropsand ecosystems.
Examples of problems: ACID RAINS (ACID PRECIPITATION): Deposition of acidic
components in rain, snow, fog, dew, or dry particles. Occurs when SO2and NOx are emitted into the atmosphere, undergo chemicaltransformations and are absorbed by water droplets in clouds. The dropletsthen fall to earth as rain, sn, snow or sleet.
PHOTOCHEMICAL SMOG: mixture of air pollutants, usually highlyreactive and oxidizing including: NOx, tropospheric ozone, VOCs,PAN, Aldehydes, etc.
GLOBAL WARMING: Observed increase in the average temperatureof the Earths Atmosphere and oceans in recent decades.
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Air PollutantsS.
No.
Pollutants Sources
1. Suspended particulate Matter,
SPM
Automobile, power plants, boilers, Industries requiring crushing
and grinding such as quarry, cement.
2. Sulphur dioxide Power plants, boilers, sulphuric acid manufacture, ore refining,
petroleum refining.
3. Oxides of nitrogen NO, NO2
(NOX)
Automobiles, power plants, nitricacid manufacture, also a
secondary pollutant
4. Lead Ore refining, battery manufacturing, automobiles.
5. Carbon monoxide Automobiles
6. Hydrocarbons Automobiles, petroleum refining
7. Chlorine Chlor-alkali plants.8. Fluoride Fertilizer, aluminum refining
9. Peroxyacetyl nitrate, PAN Secondary pollutant
10. Formaldehyde Secondary pollutant
11. Ozone Secondary pollutant
12. Hydrogen sulphide Pulp and paper, petroleum refining.
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Types of Air Pollution
Air Pollution various substances added to theatmosphere by natural events and human activitiesin high enough concentrations to cause harm tohumans, other organisms, or materials
Primary air pollutant a substance emitted directlyto the atmosphere
Secondary Air Pollutant a substance formed in theatmosphere as a result of reactions involvingprimary pollutants
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NAAQS Standards for Ambient Air Pollution
Pollutant[final rule cite]
Primary/Secondary
Averaging Time
Level Form
Carbon Monoxide[76 FR 54294, Aug 31, 2011]
primary
8-hour 9 ppmNot to be exceeded more thanonce per year1-hour 35 ppm
Lead[73 FR 66964, Nov 12, 2008]
primaryandsecondary
Rolling 3monthaverage
0.15 g/m3(1)
Not to be exceeded
Nitrogen Dioxide[75 FR 6474, Feb 9, 2010][61 FR 52852, Oct 8, 1996]
primary 1-hour 100 ppb98th percentile, averaged over 3years
primaryandsecondary
Annual 53 ppb (2) Annual Mean
Ozone
[73 FR 16436, Mar 27, 2008]
primaryandsecondary
8-hour 0.075 ppm(3)
Annual fourth-highest dailymaximum 8-hr concentration,averaged over 3 years
Particle Pollution
Dec 14, 2012
PM2.5
primary Annual 12 g/m3annual mean, averaged over 3years
secondary Annual 15 g/m3annual mean, averaged over 3years
primaryandsecondary
24-hour 35 g/m3 98th percentile, averaged over 3years
http://www.epa.gov/air/criteria.html
http://www.epa.gov/airquality/carbonmonoxide/http://www.gpo.gov/fdsys/pkg/FR-2011-08-31/html/2011-21359.htmhttp://www.gpo.gov/fdsys/pkg/FR-2011-08-31/html/2011-21359.htmhttp://www.epa.gov/airquality/lead/http://www.gpo.gov/fdsys/pkg/FR-2008-11-12/html/E8-25654.htmhttp://www.gpo.gov/fdsys/pkg/FR-2008-11-12/html/E8-25654.htmhttp://www.epa.gov/airquality/nitrogenoxides/http://www.gpo.gov/fdsys/pkg/FR-2010-02-09/html/2010-1990.htmhttp://www.gpo.gov/fdsys/pkg/FR-1996-10-08/html/96-25786.htmhttp://www.epa.gov/airquality/ozonepollution/http://www.gpo.gov/fdsys/pkg/FR-2008-03-27/html/E8-5645.htmhttp://www.gpo.gov/fdsys/pkg/FR-2008-03-27/html/E8-5645.htmhttp://www.epa.gov/airquality/particlepollution/http://www.epa.gov/airquality/particlepollution/http://www.epa.gov/air/criteria.htmlhttp://www.epa.gov/air/criteria.htmlhttp://www.epa.gov/air/criteria.htmlhttp://www.epa.gov/air/criteria.htmlhttp://www.epa.gov/airquality/particlepollution/http://www.gpo.gov/fdsys/pkg/FR-2008-03-27/html/E8-5645.htmhttp://www.epa.gov/airquality/ozonepollution/http://www.gpo.gov/fdsys/pkg/FR-1996-10-08/html/96-25786.htmhttp://www.gpo.gov/fdsys/pkg/FR-2010-02-09/html/2010-1990.htmhttp://www.epa.gov/airquality/nitrogenoxides/http://www.gpo.gov/fdsys/pkg/FR-2008-11-12/html/E8-25654.htmhttp://www.epa.gov/airquality/lead/http://www.gpo.gov/fdsys/pkg/FR-2011-08-31/html/2011-21359.htmhttp://www.epa.gov/airquality/carbonmonoxide/ -
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Air Quality Index (AQI)
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AQI Ratings
Air Quality Index(AQI) Values
Levels of HealthConcern
Colors
0 to 50 Good Green
51 to 100 Moderate Yellow
101 to 150 Unhealthy forSensitive Groups
Orange
151 to 200 Unhealthy Red
201 to 300 Very Unhealthy Purple
301 to 500 Hazardous Maroon
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AQI Calculations
If multiple pollutants are measured at a monitoring site, then thelargest or "dominant"Air Quality Indexvalue is reported for thelocation.
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WHO AIR QUALITY GUIDELINES
Substance Lowest concentration atwhich adverse effects are
observed
Duration ofexposure
Lead 0.5 g/m3 1 year
PM -- Doseresponse
SO2 500 g/m3 10 minutes
CO 30 mg/m3 1 hour
NO2 200 g/m3 1 hour
Ozone 120 g/m3 8 hours
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Primary standards provide public healthprotection, including protecting the health of"sensitive" populations such as asthmatics,children, and the elderly.
Secondary standards provide public welfareprotection, including protection againstdecreased visibility and damage to animals,crops, vegetation, and buildings.
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AIR POLLUTION SOURCES
Outdoor air quality is affected by:
Industrial or agricultural activities
Treatment of industrial effluents and domestic residues Traffic
Solid waste management
Cottage industries
Chemical incidents and spills
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Agriculture
Domestic Sources
Other Industry and waste disposal
Road Transport
Power Generation
http://www.eea.europa.eu/publications/2599XXX/page010.html
http://www.eea.europa.eu/publications/2599XXX/page010.htmlhttp://www.eea.europa.eu/publications/2599XXX/page010.html -
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Basic Pollutants Toxics Air toxics (hazardous air pollutants) are known or suspected to
cause cancer or other serious health effects.
EPAs 188 hazardous air pollutants include
Benzene (motor fuel, oil refineries, chemical processes)
Perchlorethylene (dry cleaning, degreasing) Chloroform (solvent in adhesive and pesticides, by-product of
chlorination processes)
BTEX, Dioxins, PAHs, Metals (Hg, Cr)
Area/
Other
25%
Mobile
(nonroad)
20%
Mobile
(onroad)
31%
Point
24%
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Differences between toxics and criteria pollutants
Health criteria are different No AQI-like standards for toxics
Cancer/non-cancer benchmarks (long-term exposures)
Short-term exposure limits for some
A challenge to monitor Usually not available in real-time
Example: Dioxin requires 28 days of sampling to
acquire measurable amounts in ambient air
Often localized near source
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Particulate Matter Composition
Primary PM (directlyemitted)
Suspended dust
Sea salt
Organic carbon
Elemental carbon
Metals from combustion
Small amounts of sulfateand nitrate
Secondary PM (precursor gases
that form PM in the atmosphere)
Sulfur dioxide (SO2): forms
sulfates
Nitrogen oxides (NOx): forms
nitrates
Ammonia (NH3): forms ammoniumcompounds
Volatile organic compounds
(VOCs): form organic carbon
compounds
PM is composed of a mixture of primary and secondarycompounds.
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NaCl salt is found in PM near seacoasts and after de-icing materials areapplied
Organic Carbon (OC) consists ofhundreds of separate compoundscontaining mainly carbon, hydrogen,and oxygen
Elemental Carbon (EC) composedof carbon without much hydrocarbonor oxygen. EC is black, often called
soot.
Liquid Water soluble nitrates,sulfates, ammonium, sodium, otherinorganic ions, and some organicmaterial absorb water vapor from theatmosphere
Particulate Matter Composition
Chow and Watson (1997)
Geological Material suspended
dust consists mainly of oxides of Al,
Si, Ca, Ti, Fe, and other metal
oxides
Ammonium ammonium bisulfate,
sulfate, and nitrate are most
common
Sulfate results from conversion of
SO2 gas to sulfate-containingparticles
Nitrate results from a reversible
gas/particle equilibrium between
ammonia (NH3), nitric acid (HNO3),
and particulate ammonium nitrate
Most PM mass in urban and nonurban areas is composedof a combination of the following chemical components
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PM Emissions Sources
Point generally a major facility emitting pollutants from identifiablesources (pipe or smoke stack). Facilities are typically permitted.
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PM Emissions SourcesArea any low-level source of air pollution released over
a diffuse area (not a point) such as consumer products, architectural
coatings, waste treatment facilities, animal feeding operations, construction,
open burning, residential wood burning, swimming pools, and charbroilers
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PM Emissions SourcesMobile
On-road is any moving source of air pollution such as cars, trucks,motorcycles, and buses
Non-road sources include pollutants emitted by combustion engines on
farm and construction equipment, locomotives, commercial marine
vessels, recreational watercraft, airplanes, snow mobiles, agricultural
equipment, and lawn and garden equipment
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PM Emissions SourcesNatural biogenic and geogenic emissions from wildfires, wind blown
dust, plants, trees, grasses, volcanoes, geysers, seeps, soil, and
lightning
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ORIGIN OF THE ATMOSPHERIC AEROSOL
Soil dustSea salt
Aerosol: dispersed condensed matter suspended in a gasSize range: 0.001m (molecular cluster) to 100m (small raindrop)
Environmental importance: health (respiration), visibility, radiative balance,cloud formation, heterogeneous reactions, delivery of nutrients
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Particulate Matter Chemistry
Coagulation: Particles collide and stick together.
Condensation: Gases condense onto a small solid particle
to form a liquid droplet.
Chemical Reaction: Gases react to form particles.
Cloud/Fog Processes: Gases dissolve in a water droplet andchemically react. A particle exists when the water evaporates.
Sulfate
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NOx
Ammonia
VOCs
Particulate Matter Composition
Primary Particles(directly emitted) Secondary Particles(from precursor gases)
Other(sea salt)
Crustal(soil,dust)
OrganicCarbon
Carbon(Soot)
SO2
AmmoniumSulfate
AmmoniumNitrate
Metals
Composition of PMtells us aboutthe sources and
formationprocesses
Gas
Particle
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Sulfur Dioxide
Sulfur dioxide (SO2) belongs to the family of sulfur oxide (SOx)
gases.
Gases are formed when fuel containing sulfur (mainly coal and oil) is
burned and during metal smelting and other industrial processes.
Affects the respiratory system
Reacts in the atmosphere to form acids, sulfates, and sulfites
Contributes to acid rain
Low crown densityof spruce trees
German sandstone
statue, 1908, 1969
Impact of low soil
pH on agriculture
in Victoria
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Sulfate Chemistry Virtually all ambient sulfate (99%)is secondary, formed within theatmosphere from SO2 during thesummer.
About half of SO2 oxidation to sulfate
occurs in the gas phase throughphotochemical oxidation in the daytime.NOx and hydrocarbon emissions tend toenhance the photochemical oxidation rate.
At least half of SO2 oxidation takes placein cloud droplets as air molecules react in clouds.
Within clouds, soluble pollutant gases, such as SO2, are scavenged by waterdroplets and rapidly oxidize to sulfate.
Only a small fraction of cloud droplets deposit out as rain; most dropletsevaporate and leave a sulfate residue or convective debris.
Typical conversion rate 1-10% per hour
Husar (1999)
Heterogeneous Oxidation
Chemistry(2 of 4)
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Mechanisms of Converting S(IV) toS(VI)
Why is converting to S(VI) important?
It allows sulfuric acid to enter or form within cloud drops
and aerosol particles, increasing their acidity
Mechanisms
1. Gas-phase oxidation of SO2(g) to H2SO4(g) followed by
condensation of H2SO4(g)
2. Dissolution of SO2(g) into liquid water to form
H2SO3(aq) followed by aqueous chemical conversion of
H2SO3(aq) and its dissociation products to H2SO4(aq) and
its dissociation products.
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Particulate Matter Chemistry
Nitrate Chemistry NO2 can be converted to nitric acid (HNO3) by reaction with hydroxyl
radicals (OH) during the day.
The reaction of OH with NO2 is about 10 times faster than the OH reaction
with SO2.
The peak daytime conversion rate of NO2 to HNO3 in the gas phase isabout 10% to 50% per hour.
During the nighttime, NO2 is converted into HNO3 by a series of
reactions involving ozone and the nitrate radical.
HNO3 reacts with ammonia to form particulate ammonium nitrate
(NH4NO3).
Thus, PM nitrate can be formed at night and during the day; daytime
photochemistry also forms ozone.
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Winds Clouds, fog Winds Temperature
Temperature Temperature Precipitation Relative humidity
Solar radiation Relative humidity Winds
Vertical mixing Solar radiation
condensation and
coagulation
photochemical production
cloud/fog processes
gases condense onto particles
cloud/fog processes Measurement
Issues Inlet cut points Vaporization of nitra
H2O, VOCs Adsorption of VOCs Absorption of H2O
transport
sedimentation(dry deposition)
wet deposition
Mechanical Sea salt Dust
Combustion Motor vehicles Industrial Fires
Other gaseous
Biogenic Anthropogenic
Particles NaCl Crustal
Particles Soot Metals OC
Gases NOx SO2 VOCs NH3
Gases
VOCs NH3 NOx
SourcesSample
CollectionPM Transport/LossPM
FormationEmissions
Chemical Processes
eteorological Processes
Particulate Matter Chemistry
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Phenomena Emissions PM Formation PM Transport/Loss
Aloft PressurePattern No direct impact. No direct impact. Ridges tend to produce conditions conducive for accumulat ion of PM2.5.Troughs tend to produce conditions conducive for dispersion and removal of PM andozone.In mountain-valley regions, strong wintertime inversions and high PM2.5 levels may not bealtered by weak troughs.High PM2.5 concentrations often occur during the approach of a trough from the west.
Winds andTransport
No direct impact. In general, stronger winds dispersepollutants, resulting in a less idealmixture of pollutants for chemicalreactions that produce PM2.5.
Strong surface winds tend to disperse PM2.5 regardless of season.Strong winds can create dust which can increase PM2.5 concentrations.
TemperatureInversions
No direct impact. Inversions reduce vertical mixing andtherefore increase chemical
concentrations of precursors. Higherconcentrations of precursors canproduce faster, more efficientchemical reactions that producePM2.5.
A strong inversion acts to limit vertical mixing allowing for the accumulation of PM2.5.
Rain Reduces soil and fire emissions Rain can remove precursors ofPM2.5.
Rain can remove PM2.5.
Moisture No direct impact. Moisture acts to increase theproduction of secondary PM2.5including sulfates and nitrates.
No direct impact.
Temperature Warm temperatures are associatedwith increased evaporative,biogenic, and power plantemissions, which act to increasePM2.5. Cold temperatures can alsoindirectly influence PM2.5concentrations (i.e., home heatingon winter nights).
Photochemical reaction ratesincrease with temperature.
Although warm surface temperatures are generally associated with poor air qualityconditions, very warm temperatures can increase vertical mixing and dispersion ofpollutants.Warm temperatures may volatize Nitrates from a solid to a gas.Very cold surface temperatures during the winter may produce strong surface-basedinversions that confine pollutants to a shallow layer.
Clouds/Fog No direct impact. Water droplets can enhance theformation of secondary PM2.5.Clouds can limit photochemistry,which limits photochemicalproduction.
Convective clouds are an indication of strong vertical mixing, which disperses pollutants.
Season Forest fires, wood burning,
agriculture burning, field tilling,windblown dust, road dust, andconstruction vary by season.
The sun angle changes with season,
which changes the amount of solarradiation available forphotochemistry.
No direct impact.
Meteorology
How weather affects PM emissions, formation, and transport
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ANNUAL MEAN PARTICULATEMATTER (PM) CONCENTRATIONS AT U.S. SITES,1995-2000
NARSTO PM Assessment, 2003
PM10 (particles > 10m) PM2.5 (particles > 2.5m)
Red circles indicate violations of national air quality standard:50g m-3 for PM10 15g m-3 for PM2.5
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AEROSOL OPTICAL DEPTH (GLOBAL MODEL)
Annual mean
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AEROSOL OBSERVATIONS FROM SPACE
Biomass fire haze in central America yesterday (4/30/03)
Fire locationsin red
Modis.gsfc.nasa.gov
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BLACK CARBON EMISSIONS
Chin et al. [2000]
DIESEL
DOMESTICCOAL BURNING
BIOMASSBURNING
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RADIATIVE FORCING OF CLIMATE, 1750-PRESENT
Kyoto also failed to address two major pollutants that have an impact on warming:black soot andtropospheric ozone.Both are proven health hazards.Reducing both would not only address
climate change, but also dramatically improve people's health. (George W. Bush, June 11 2001 RoseGarden speech)
IPCC [2001]
P i l I H H l h d MORE
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Particles Impact Human Health and MORE
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Nitrogen Oxides
Nitrogen oxides, or NOx, is the generic term for a group of highlyreactive gases, all of which contain nitrogen and oxygen in varyingamounts.
Nitrogen dioxide is most visually prominent (it is the yellow-browncolor in smog)
The primary man-made sources of NOx are motor vehicles;electric utilities; and other industrial, commercial, and residentialsources that burn fuels
Affects the respiratory system
Involved in other pollutant chemistry
One of the main ingredients in the formation of ground-level ozone
Reacts to form nitrate particles, acid aerosols, and NO2, which also causerespiratory problems
Contributes to the formation of acid rain (deposition)
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NOx EMISSIONS (Tg N yr-1) TO TROPOSPHERE
Fossil Fuel
23.1
Aircraft0.5
Biofuel
2.2
BiomassBurning
5.2
Soils5.1
Lightning5.8
Stratosphere0.2
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NOx
Oxides of nitrogen formed in combustion processes are usuallydue to either thermal fixation of atmospheric nitrogen incombustion air or to the conversion of chemically boundnitrogen in the fuel. Thermal fixation occurs when combustiontemperature is above 1600C. For natural gas and distillate oilnearly all NO results from thermal fixation. For residue oil and
coal, the contribution to NO emission from fuel bound nitrogenmay be significant.
The concentration of NOx formed increases with increase in
excess oxygen maintained in the combustion process and withthe increase in temperature of the furnace. For coal basedthermal power plants in India, it ranges between 100 and 200mg/Nm3 in the flue gas. In the case of natural gas and liquidfuels, the emission limits for flue gases prescribed in Europeancountries is in the range of 200 - 400 mg/Nm3.
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Must make NO2
To make significant amounts of ozone musthave a way to make NO2 without consumingozone
Presence of peroxy radicals, from theoxidation of hydrocarbons, disturbs O3-NO-NO2 cycle
NO + HO2 NO2 + OH
NO + RO2
NO2 + RO
leads to net
production of ozone
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The Hydroxyl Radical
produced from ozone photolysis
for radiation with wavelengths less than 320 nm:
O3 + hv O(1D) + O2
followed by
O(1D) + M O(3P) + M (+O2O3) (~90%)
O(1D) + H2O 2 OH (~10%)
OH initiates the atmospheric oxidation of a wide range of compounds in theatmosphere
referred to as detergent of the atmosphere
typical concentrations near the surface ~106 - 107cm-3
very reactive, effectively recycled
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THE OH RADICAL: MAINTROPOSPHERIC OXIDANT
Primary source: O3 + hn O2 + O(1D) (1)
O(1D) + M O + M (2)
O(1D) + H2O 2OH (3)
Sink: oxidation of reduced species leads to
HO2(RO2) production
CO + OH CO2 + H
CH4 + OH CH3 + H2O
HCFC + OH
Global Mean [OH] = 1.0x106 molecules cm-3
MajorOH sinks
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An example of gridded NOx emissions
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Mapping of Tropospheric NO2
From the GOME satellite instrument (July 1996)
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Ozone
Colorless gas Composed of three oxygen atoms
Oxygen molecule (O2)needed to sustain life
Ozone (O3) the extra oxygen atom makes ozonevery reactive
Secondary pollutant that forms from precursor gases
Nitric oxide combustion product
Volatile organic compounds (VOCs) evaporativeand combustion products
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Ozone Precursor Emissions
Man-made sources
Oxides of nitrogen (NOx) through combustion
VOCs through combustion and numerous other
sources
Natural sources (biogenic)
VOCs from trees/vegetation
NOx from soils (Midwest fertilizer)
Concentration depends on Source location, density, and strength
Meteorology
Emissions Chemistry
Meteorology
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Solar radiation and chemistry
The reaction that produces ozone in theatmosphere:
O + O2 + M O3 + M
Difference between stratospheric andtropospheric ozone generation is in thesource of atomic O
For solar radiation with a wavelength of lessthan 242 nm:
O2 + hv O + O
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Solar radiation and chemistry
Photochemical production of O3 in troposphere tied to NOx (NO +
NO2)
For wavelengths less than 424 nm:
NO2 + hv NO + O
But NO will react with O3
NO + O3 NO2
Cycling has no net effect on ozone
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Tropospheric Ozone Photolysis
Troposphere ozone photolysis takes place in a narrow UV window
(300-320 nm), NO2 broadly below 428
30o equinoxmiddaySolar spectrum
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Ozone ChemistrySummary of ozone chemistry
NO2 + Sunlight NO + O Production
O+ O2 O3 Production
NO + O3 NO2 + O2 Destruction
VOC + OH RO2 + H2O Production of NO2 without the
RO2 + NO NO2 + RO Destruction of O3
Emissions Chemistry
Meteorology
Key processes
Ample sunlight (ultraviolet) High concentrations of precursors (VOC, NO, NO2)
Weak horizontal dispersion Weak vertical mixing
Warm air
RO=Reactive Organic compound such as VOC
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Day and Night Chemistry
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Carbon Monoxide
Odorless, colorless gas
Caused by incomplete combustion of fuel
Most of it comes from motor vehicles
Reduces the transport of oxygen through the
bloodstream
Affects mental functions and visual acuity, evenat low levels
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What breaks the cycle?
Cycle terminated byOH + NO2 HNO3
HO2 + HO2 H2O2
Both HNO3 and H2O2 will photolyze or react with OH to, in
effect, reverse these pathways but reactions are slow (lifetime of several days)
both are very soluble - though H2O2 less-so
washout by precipitation
dry deposition
in PBL they are effectively a loss
situation is more complicated in the upper troposphere
no dry deposition, limited wet removal
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LEAD (Pb) IN AIR
SOURCES
Tetraethyl lead in petrol
Mining and smelting of lead ores
Industry
Waste incineration
Dust (e.g. homes with old lead-based paint, battery recycling,smelters)
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CARCINOGENS IN AIR
Pollutant System affected
Arsenic Lung
Benzene Leukaemia
Chromium VI Lung
Nickel Lung
PAHs Lung
Vinyl chloride liver
Radon Lung, Gastrointestinal