6. Two Very Important Factors in
Atmospheric Chemistry:
(i) Radiant solar energy
Photons put high energy into individual molecules
(ii) Hydroxyl radical, HO•
Most important highly reactive intermediate
7. Loss of Excitation Energy from
Electronically Excited Species:
(i) Emission of a photon (light): NO2* NO2 + h
Called luminescence if instantaneous, phosphorescence if
slower and
Chemiluminescence when the excited species that emits a
photon is formed as the result of a chemical reaction
O3 + NO O2 + NO2* (luminescent species)
(ii) Direct reaction of an excited species
O2* + O3 2O2 + O
(iii) Dissociation
NO2* NO + O (very important tropospheric reaction)
O2* O + O (important in stratosphere leading to O3)
(iv) Photoionization (formation of ions in the ionsphere)
N2* N2
+ + e-
16. Introduction of Ozone:
O3
a gas composed of three atoms of
oxygen
bluish gas that is harmful to breathe
Nearly 90% of the Earth's ozone is in
the stratosphere and is referred to as
the ozone layer
Ozone absorbs a band of ultraviolet
radiation called UVB