A study of?bond enthalpy?can explain why ozone and oxygen in the atmosphere play very different roles in the flow of energy
These processes have a profound effect on the amount of solar radiation reaching ground level
The structure of oxygen and ozone molecules influences the amount of energy needed to break their bonds:
The structure of oxygen and ozone
The double bond in oxygen is stronger than the?delocalised π bonds?in ozone
We say the?bond order?of oxygen is?2?and the?bond order?of ozone is?1.5
Both bonds are broken by ultraviolet radiation but the bond in oxygen requires radiation of higher energy and shorter wavelength than the bond in ozone
High energy UV radiation in the stratosphere breaks the oxygen-oxygen double bond creating oxygen atoms
These oxygen atoms have unpaired electrons- they are known as?free radicals
The?free radicals?are highly reactive and quickly attack oxygen molecules forming ozone in an?exothermic?reaction, which raises the temperature of the stratosphere
The temperature in the stratosphere is maintained by the balance of ozone formation and ozone depletion in a process known as the Chapman Cycle
It is not a closed system as matter and energy flow in and out, but it is what is called a?steady state
The Chapman cycle
Unfortunately, chemicals we have introduced into the atmosphere have interfered with this steady state resulting in ozone depleting at a faster rate than it is replaced
Amongst these chemicals are?chlorofluorocarbons (CFCs)?found in refrigerants, propellants and solvents
CFCs?are greatly damaging to stratospheric ozone and have been largely replaced by safer alternatives following the 1985 Montreal Protocol
The depletion of ozone has allowed greater amounts of harmful?UV light?to reach the surface of the Earth
UV light?has been linked to greater incidence of skin cancer and cataracts as well as the destruction of phytoplankton and reduced plant growth