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air pollution
material added to the atmosphere that can affect climate and harm organisms
natural pollution
dust storms
volcanoes
fires
unnatural pollution
anthropogenic
burning fossil fuels
Clean Air Act of 1970
provided research funds
regulates criteria pollutants and hazardous air pollutants
enabled citizens to sue violating parties
imposed emission limits
Clean Air Act of 1990
strengthened previous regulations
introduced emissions tradings for sulfur dioxide
acid deposition (rain)
sources: transportation, coal electricity, volcanic eruptions, fire, lightning
primary pollutants: SOx+NOx
coal and cars and coal
secondary pollutants: acids
sulfuric acid and nitric acid
human effects: infrastructure, impacts, limestone
environmental impacts: leaching metals (Al) in soil, and decreased pH outside range of tolerance
solutions to acid rain
scrubbers
uses a limestone “slurry” (water based) to neutralize acid-producing gases before being released into the atmosphere
typically put into exhaust stark
industries
catalytic converters
uses platinum, rhodium, and/or palladium as a catalyst to convert NOx into non-regulated gases
transportation
where is ozone produced?
stratosphere: does not contribute to climate change
natural ozone formation
O+O2 → 03
O3 ←O+O2
natural ozone destruction
O3+ UV →O +O2
ozone depletion
sources: stratosphere, good O3, fridge, ACs, aerosal
primary pollutants: CFCs → Cl, photochemical (light is required)
secondary pollutants: none, Cl+O3 → ClO +02 and ClO +O →Cl +O2
human effects: sunburn (UV-C), skin cancer
environmental impacts: UV-C light, genetically mutates single-celled organisms (phytoplankton), interference with photosynthesis in plants
effect an animals: death of eggs, death of phytoplankton, disruption of food chain
CFCs
non flammable, relatively inert, nontoxic
used as coolants for refrigeration, in foam for plastics, and industrial solvents
once in atmosphere, one molecule survives 100 years
once in the stratosphere (due to atmospheric mixing), CFCs deconstruct under UV light
destroy ozone molecules
CFC destruction (leading to breakdown of ozone)
CFC+ UV → Cl
Cl + O3 → ClO + O2
ClO + O → Cl + O2
nowhere in this process did we create O3
deconstruction weighs down formation
CFCs and Montreal Protocol (1987)
1st Cl atom can destroy a lot of ozone molecules which is faster than it can even be created
banned CFC use in 1987 (US did)
signed by 150+ countries
other ozone depleting substances like Methyl Bromide were also banned
Smog
smoke and fog
London 1952
the great smog event
thermal inversion
mist (water-rich air)
incomplete combustion of sulfur-rich coal (industry)
SO2 formed sulfuric acid
up to 12,000 deaths
reactions are not photochemical
does not require sunlight to form
brown smog
ideal for thermal inversions
created from transportation
thermal inversions
cold air mass that gets injected into area of warm air
deviation from normal increase in temperature as you increase in elevation
results in cooler layer of air being trapped by a warmer layer
can occur during warm fronts
are accentuated due to geography
causes significant air quality issues by keeping pollution close to the ground
smog and information for it
source: requires sunlight, transportation, rush hour
primary pollutants: NOx + VOC
VOC: volatile organic compounds
secondary pollutants: NO2+ UV → NO + O
NO + VOC → formaldehyde
O+ O2 → O3
human effects: respiratory issues, O2 is replaced with O3 in lungs
environmental impacts: decreased photosynthesis because ozone that is exchanged through stomata damaged cells
solutions for SMOG
catalytic converters
scrubbers
baghouse filters
electrostatic precipitators