demonstrations:ocean_acidification
Ocean Acidification
Materials: ★★☆ Available in most school laboratories or specialist stores
Difficulty: ★☆☆ Can be easily done by most teenagers
Safety: ★☆☆ Minimal safety procedures required
Categories: Acids and Bases, Global Systems, Pollution and Conservation
Alternative titles:
Summary
By blowing air through water containing a pH indicator, students can observe how dissolved carbon dioxide lowers the pH of water, demonstrating the process of ocean acidification.
Procedure
- Fill two beakers with tap water.
- Add several drops of a pH indicator (aquarium indicator, phenolphthalein or bromothymol blue) to each beaker.
- To the first beaker, add a few drops of vinegar to show how an acid lowers pH (solution turns yellow).
- Sprinkle baking soda into the same beaker to show how a base raises pH (solution turns blue).
- Explain the indicator color changes in terms of acid–base reactions.
- Blow gently through a straw into the second beaker for about 30 seconds.
- Observe the color shift, indicating the water has become acidic due to dissolved carbon dioxide.
Links
Ocean Acidification Demo - ElCheJaimito56:
📄 Ocean acidification - ABC Science: https://www.abc.net.au/science/articles/2011/02/24/3147423.htm
Variations
- Use different indicators, including aquarium indicator, phenolphthalein or bromothymol blue.
- Compare the effect of exhaled air with air from a balloon (ambient air) to highlight the role of CO₂ concentration.
- Use seawater samples instead of tap water to make the demonstration more realistic.
Safety Precautions
- Avoid ingesting indicator solution.
- Dispose of solutions safely in a sink with plenty of water.
- Blow gently through straws to prevent splashing.
Questions to Consider
- What gas in exhaled breath is responsible for lowering the water’s pH?
- How does the change in pH relate to what is happening in the oceans today?
- Why are organisms with calcium carbonate shells particularly vulnerable to ocean acidification?
- What is the difference between short-term pH changes in small systems (like a beaker) and long-term changes in the global ocean?
- Why is the rate of pH change in the oceans more concerning than the absolute pH level?