Chemistry - SCH3U - Unit 6 - Gases and Atmospheric Chemistry
KMT, atmosphere, air quality
States matter
Solid
Defined shape and volume
Virtually incompressible
Does not flow easily
Strong force attraction between entities
Liquid
Take shape of container but has definite volume
Slightly compressible
Flows readily
Medium force of attraction between entities
Gas
Take shape and volume of container
Highly compressible
Flows readily
Low force of attraction between entities
Kinetic molecular theory
Robert Brown 1773 - 1858
Examine pollen speck suspend water and found pollen move at random
Brownian motion
Random movement of microscopic particle suspended in liquid/gas
Kinetic molecular theory
Develop from scientific interpretation of Brown observation
Entities in solid, liquid, gas are in constant motion
As move they collide other object in path
Kinetic = come from greek work kinema (mean constant motion)
Kinetic energy = energy of moving object
How entities move
Transitional motion
Movement of entity along linear path
Liquid and gas
Rotational motion
Spinning of entity in place
Liquid and gas
Very limited in solid
Vibrational motion
Back and forth vibration of entity
Solid and liquid and gas
Kinetic energy and temperature
When substances warmed entities move more rapidly
Fast entity move = more kinetic energy
Temperature = measure of average kinetic energy of entity in substance
Thermometer work from entity of substance collide with thermometer so energy transfer liquid in thermometer cause expand
As more energy transfer in solid it vibrate faster
Eventually attractive force broken which allow entity flow past
Change state solid to liquid
Warming liquid increase kinetic energy of entity
Eventually attractive force completely overcome
Liquid boil and change state to gas
Atmosphere
Atmosphere = thin blanket moisture and gas that protect Earth from outer space environment
Mostly concentrated first 100km of Earth surface
Stabalize surface temperature which make Earth habitable
Most dense surface Earth
Molecule in air pushed together by atmosphere above
Atmosphere less dense with higher altitude
Atmosphere layer
Troposphere
Closest Earth surface
Warmest near Earth surface
Temperature decrease with altitude
Solar energy absorb by Earth transfered to air molecule as thermal energy
Air movement determine weather
Stratosphere
Dry region with higher then normal concentration ozone
Ozone has ability trap ultraviolet radiation of sun
Trapped energy release gas molecule with increase kinetic energy
Temperature increase with altitude
Due to increase of kinetic energy
Mesosphere
Extend 50km - 85km
Low gas concentration
Contain little ozon
Temperature decrease with altitude
Thermosphere/ionosphere
Extend beyond 85km
Gas molecule absorb solar radiation to become ionized
Will emit visible radiation (auroras)
Warms thermosphere
Auroras particularily over polar region
Also called aurora borealis, northern lights, aurora austrialis, southern lights
Composition of atmosphere
Troposphere and stratosphere have biggest influence
Nitrogen (N_2 )
Most abundant gas in atmosphere
Important all biological system
Cycle Earth through nitrogen cycle
Nitrogen fixing bacteria convert nitrogen gas into soluble nitrate
Soluble nitrate = form plant can easily absorb through roots
Nitrogen release back atmosphere from body decay plant and animal and waster
Oxygen (O_2 ) and ozone (O_3 )
Make up 21% of atmosphere
Required for cellular respiration
Most ozone in atmosphere concentrate in statosphere
Ozone absorb UV light effectively making it radiation shielf
Prevent excessive UV read Earth surface
Ozone also found troposphere where it is air pollutant and key ingredient in smog
Other gases
Argon, water vapour, carbon dioxide make majority remain gas in atmosphere
Argon = colourless, odourless, chemically inert
Water vapour = 1% - 3% in atmosphere
Over 99% of all water vapour in troposphere in water cycle
Carbon dioxide only 0.036% of lower atmosphere
But essential for life on Earth
Returned to atmosphere by living organism
From waster product of cellular respiration
Greenhouse effect and climate change
Atmosphere help keep Earth surface warm by trap thermal energy from ground
Without atmosphere Earth average temperature = -18°C
With atmosphere Earth average temperature = 15°C and rising
How atmosphere keep Earth warm
Atmosphere is transpart to higher energy radiation of sun
Much of radiation absorb by Earth suface and transform thermal energy
Warm object on Earth surface give off energy as lower energy infrared (IR) radiation
Greenhouse gas (GHG) = gas in atmosphere that trap infrared radiation
Trapped IR contribute greenhouse effect
Most important GHG
Carbon dioxide, methane, water vapour
Less significant GHG
Nitrous oxide, fluorinated gas
Specific frequencies of IR cause greenhouse gas to vibrate
As vibrates reradiates energy
Some sent back Earth surfact which warms ground
Greenhouse effect = process of trap infrared radiation within atmosphere
Concnetrations of greenhouse gass fluctuation over time
Higher concentration correspond period high global temperature
Volcanic emmision, continental drift, change in solar energy, change in ocean circulation, large meteor strike
Human activity over last 200 year cause significant increase GHG in atmosphere
Climate change cause
Change water level
Dsitrupt ecosystem
Less sea ice and degration of permafrost
Reducing GHG emissions
Enforce emission standard fir vehicle
Provide fund to farmer and business to invest environmentally friendly practices
Recycling and reusing
Driving less, public transportation, car pooling
Insulating, cauking, weather stripping
Carbon sequestration = remove carbon dioxide from atmosphere and store it
Biological sequestration
Plants used to naturally sequece/remove carbon dioxide
Geological sequestration
Capture and store carbon dioxide in grand deposit
Has cost
May leak
Negatively affect environment
Expensive
F.K. Hore
Born Englad 1919
Wrote and spoke extensively to raise awarness to issue relate climate change
Won many award for effort
Air quality
Smog = complex mixture air pollutant mostly from human activity
Photochemical smog
Experienced in many city
Contain ground levelo ozone, gases, fine particles
Produce by reaction of vehicle and factory emission with sunlight
Prefix “photo“ = light
Appear as brown haze
Exposure smog cause eye and heart iritation, aggravate pre-exist repiratory issue
Particulate matter, gases, volatile organic compound contribute poor air quality
Particulate matter
Particulate matter = mixture solid and liquid particle in atmsosphere
Size can range few molecule to visible dust particle
Almost all combustion reaction produce some aprticulate matter
Can damage respiratory system
Reduce visibility and threaten air travel
Pollutant gases
Sulfur dioxide (SO_2 )
Clear, colourless gas with strong choking odor
Most of this gas produce by combustion of fossil fuel with sulfur impurity
Contribute to acid precipitation
Can cause respritory irritation, stimulate mucus production, loud wheeze, short of breath
People with preexisting respiratory issues are especially susceptible
Nitrogen oxides (NO, No_2 , N_2O_4 )
Brownish smog result nitrogen dioxide
Other nitrogen oxide
Nitrogen monoxide
Dinitrogen tetroxide
Most nitrogen oxide emission result of vehicle use fossil fuel
Contribute toa cide precipitation
Carbon monoxide (CO)
Colourless, odourless, gas that toxic high concentration
Incomplete combustion produce carbon monoxide and pure carbon
Concentration carbon monoxide higher 25ppm can affect long term health
Volatile organic compound (VOC)
Solid or liquid carbon-contain compound that vaporize readily
Many naturally occur
Eg
Gasoline vapour, pine tree odour, aerosol spray, paint, air freshener, dry clean clothes, wood perservative, clean solvent
Symptom VOC exposer
eye iritation, head ache, rash
Depress central nervous system, cause cancer
Ozone
Powerful bleach
Very corrosive
Produce from reaction of nitrogen oxide and VOC in sunlight
Equations
Fuel burn in air at high temperature
N_2 (g) + O_2 (g) → 2NO (g)
Colourless nitrogen monoxide form reddish brown pollutant nitrogen dioxide
2NO (g)(colourless) + O_2 → 2NO_2 (g)(reddish brown)
Nitrogen dioxide react UV radiation
NO_2 (g) → (UV) NO (g) + O (g)
Oxygen by self to reactive so react with oxygen compound to form ozone
O (g) + O_2 (g) → O_3
VOC not directy involve form ozone
But help form nitrogen dioxide which form ozone
Concentration ozone peak when sunlight most intense
Air quality health index
Environemtn Canada develop Air Quality Helath Index (AQHI)
Based on health risk for level of common air pollutant
Ozone, particulate matter, nitrogen dioxide
Caterogy
1-3
Low risk
4-6
Moderate risk
7-10
High risk
10+
Very high risk