The discussion focuses on the molecular mass of ozone (48) compared to the average molecular mass of air (29) and questions whether this difference would cause the ozone layer to "fall." It is clarified that gases do not separate by mass until reaching altitudes above the stratosphere, where turbulence and thermal convection mix the atmosphere up to about 60 miles. Ozone exists in a dynamic chemical equilibrium in the stratosphere, continually formed and destroyed through reactions with oxygen and sunlight, which maintains its concentration despite its instability and short half-life of about half an hour. This instability prevents ozone from being well-mixed like other gases, leading to its presence near the surface due to pollution and at high altitudes in the ozone layer. The conversation also touches on gas behavior, noting that while gases expand to fill a volume, certain conditions can lead to pooling, as seen with propane. Overall, the mixing dynamics of gases and the unique properties of ozone are central to understanding its distribution in the atmosphere.