Photochemical Smog Flashcards
major constituents in the atmosphere
N2, 78%; O2, 20%
properties of nitrogen
exists as a diatomic molecule (N2) held by covalent triple bonds (super strong), and takes large amounts of energy to break the triple bond and form new compounds.
formation of oxides of nitrogen (NOx)
with sufficient energy from high temps:
N2 + O2 –> 2NO (nitric oxide)
2NO + O2 –> 2NO2 (nitrogen dioxide)
what is the troposphere?
the lowest layer of the atmosphere containing 75% of all gases by mass in the atmosphere.
atmosphere levels
lowest to highest: troposphere, stratosphere, mesosphere, thermosphere, exosphere
pollutants in photochemical smog
NO, NO2, CO3, UHC
nitric oxide, nitric dioxide, ozone, unburned hydrocarbons
formation of ozone
N2 + O2 –> 2NO
2NO + O2 –> 2NO2
NO2 -(UV)-> NO + O
O + O2 –> O3
what is photochemical smog?
a complex mixture of primary chemicals (directly from a source) and secondary chemicals (from reactions involving light and heat) between pollutants in the atmosphere.
conditions of photochemical smog
- high concentration of pollutants (in urban areas the conc can vary throughout the day)
- sunlight (UV to photodissociate NO)
- still air mass (heat can disperse)
- temperature inversion (warmer air becomes trapped in cooler air)
what is temperature inversion?
when warm air is trapped between layers of cooler air, the pollutants are trapped in the first cool layer.