We mentioned in class on Tuesday that ozone has both beneficial and detrimental roles in the atmosphere

Ozone found in the stratosphere absorbs dangerous high-energy ultraviolet light and has a benefical role.  Ozone in the troposphere (at ground level) is a pollutant.  It is a toxic gas and is also a key ingredient in Los Angeles type smog (aka photochemical smog). 

The purpose of the demonstration was to make some photochemical smog.  We first needed some ozone.  The reactions that produce ozone in the stratosphere are very simple.

Molecular oxygen (O2) absorbs ultraviolet (UV) light and is split into two oxygen atoms.  The oxygen atoms then react with oxygen molecules to make ozone (O3).  This is the process that we will use to make some ozone for the smog demonstration.  We'll use oxygen in the air and a small lamp that emits UV light (the bulb was placed inside a glass flask that was covered with a black cloth to insure that people in the classroom weren't exposed to dangerous UV light.

The next step in the demonstration was to introduce some hydrocarbons into the flash so that it could react with the ozone.  Hydrocarbons are compounds that contain hydrogen and carbon (I mentioned they also contained oxygen in class, apparently that isn't correct).  In the demonstration some lemon peel was put into the flask.  The lemony smell from the lemon peels is a hydrocarbon.


The reaction between the ozone and the lemon peel produces some product gas (invisible).  The product gas condenses however and forms small drops or particles that scatter light.  At this point a smog cloud becomes visible.

Here's a pictorial summary of the photochemical smog demonstration.