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

  1. Fill two beakers with tap water.
  2. Add several drops of a pH indicator (aquarium indicator, phenolphthalein or bromothymol blue) to each beaker.
  3. To the first beaker, add a few drops of vinegar to show how an acid lowers pH (solution turns yellow).
  4. Sprinkle baking soda into the same beaker to show how a base raises pH (solution turns blue).
  5. Explain the indicator color changes in terms of acid–base reactions.
  6. Blow gently through a straw into the second beaker for about 30 seconds.
  7. Observe the color shift, indicating the water has become acidic due to dissolved carbon dioxide.

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?