Experiment Description: Two air types, atmospheric and exhaled, are bubbled through separate lime water (Ca(OH)₂) solutions. Diagram (I) represents atmospheric air, and Diagram (II) represents exhaled air.
Air Sample Composition: Atmospheric air contains approximately 0.03–0.04% CO₂. Exhaled air has a significantly higher CO₂ concentration, around 4%.
Reaction Mechanism: Carbon dioxide from the air reacts with calcium hydroxide in lime water. This reaction produces insoluble calcium carbonate, causing the lime water to turn milky:
\[\text{Ca(OH)}_2 + \text{CO}_2 \rightarrow \text{CaCO}_3 + \text{H}_2\text{O}\]
The formation of calcium carbonate (CaCO₃) is responsible for the observed milkiness.
Experimental Observations: Test tube (I) shows slow milkiness development due to the low CO₂ content in atmospheric air. Test tube (II) exhibits rapid milkiness formation because exhaled air, rich in CO₂, reacts more quickly with lime water.
Experimental Conclusion: The accelerated milkiness in test tube (II) demonstrates that exhaled air contains a greater amount of carbon dioxide compared to atmospheric air, leading to a faster reaction rate with lime water.