Ozone Depletion Chemistry
Ozone layer depletion in IGCSE Chemistry: what ozone is, how CFCs destroy it, the consequences of a thinner ozone layer, and alternatives to CFCs for Cambridge 0620.
Published by IGCSEChemistry.com.my
Chemistry teaching team: K. S. Tan (15+ years teaching IGCSE Chemistry) and Ms Yash (10+ years teaching IGCSE Chemistry) and Ms Kartini (15+ years teaching IGCSE Chemistry).
Mapped to Cambridge IGCSE Chemistry 0620 (2026–2028). Last updated 2026-08-19.
Ozone depletion is tested in the Cambridge 0620 environmental chemistry section. Candidates need to know what ozone is, how CFCs destroy it, the consequences of ozone depletion, and the alternatives that have replaced CFCs.
What is ozone?
Ozone (O₃) is a molecule made of three oxygen atoms. It is found naturally in the stratosphere (15-30 km above the Earth’s surface), where it forms the ozone layer.
How the ozone layer forms
Ozone is continuously created and destroyed by UV radiation:
Formation: 3O₂ → 2O₃ (UV radiation splits O₂; the free O atoms combine with other O₂ molecules)
Breakdown: 2O₃ → 3O₂ (UV radiation also breaks ozone apart)
Under natural conditions, these two processes are in balance, maintaining a steady ozone concentration.
The role of the ozone layer
The ozone layer absorbs most of the Sun’s harmful ultraviolet (UV-B and UV-C) radiation, preventing it from reaching the Earth’s surface. Without this protection, life on land would be exposed to damaging levels of UV radiation.
CFCs and ozone depletion
What are CFCs?
CFCs (chlorofluorocarbons) are synthetic compounds containing carbon, chlorine, and fluorine. They were widely used as:
- Refrigerants (in fridges and air conditioners)
- Propellants (in aerosol spray cans)
- Solvents (for cleaning electronics)
- Blowing agents (for making expanded polystyrene foam)
CFCs were popular because they are non-toxic, non-flammable, and chemically unreactive at ground level.
How CFCs destroy ozone
- CFCs are very stable and do not break down in the lower atmosphere
- They slowly drift up to the stratosphere over several years
- In the stratosphere, intense UV radiation breaks the C-Cl bond, releasing a free chlorine atom (Cl radical)
CF₂Cl₂ → CF₂Cl + Cl (UV breaks the C-Cl bond)
- The chlorine atom reacts with ozone:
Cl + O₃ → ClO + O₂
- The ClO then reacts with another oxygen atom:
ClO + O → Cl + O₂
- The chlorine atom is regenerated — it is not used up. It acts as a catalyst for ozone destruction. A single chlorine atom can destroy thousands of ozone molecules before it is eventually removed from the stratosphere.
Overall equation: 2O₃ → 3O₂ (catalysed by Cl atoms from CFCs)
Consequences of ozone depletion
| Effect | Explanation |
|---|---|
| Increased skin cancer rates | More UV-B radiation reaches the surface, damaging DNA in skin cells |
| Increased eye cataracts | UV radiation damages the lens of the eye |
| Damage to crops | UV inhibits photosynthesis and damages plant tissues |
| Harm to marine plankton | Plankton near the ocean surface are killed by UV; this disrupts the marine food chain |
| Damage to materials | UV degrades plastics, paints, and building materials faster |
The ozone hole
The most severe ozone depletion occurs over Antarctica each spring (September-October), creating the “ozone hole.” Extreme cold in the polar stratosphere accelerates the chemical reactions that destroy ozone.
Solutions — the Montreal Protocol
In 1987, the Montreal Protocol was signed — an international agreement to phase out the production and use of CFCs. It is one of the most successful environmental treaties:
- CFC production has been reduced by over 99%
- The ozone layer is slowly recovering
- Full recovery is expected by around 2060-2070
Alternatives to CFCs
| Alternative | Use | Advantage | Limitation |
|---|---|---|---|
| HFCs (hydrofluorocarbons) | Refrigerants | Do not contain chlorine; do not damage ozone | Some are potent greenhouse gases |
| HCFCs (hydrochlorofluorocarbons) | Transitional refrigerants | Break down faster in the atmosphere | Still contain chlorine (being phased out) |
| Hydrocarbons (propane, butane) | Refrigerants, aerosols | No ozone damage, low greenhouse effect | Flammable |
| CO₂ | Some refrigeration | No ozone damage | Greenhouse gas |
Ozone depletion vs the greenhouse effect
Students often confuse these two issues:
| Feature | Ozone depletion | Greenhouse effect |
|---|---|---|
| Where | Stratosphere | Troposphere |
| Problem | UV radiation reaching Earth | Heat trapped in the atmosphere |
| Caused by | CFCs (and related compounds) | CO₂, CH₄, and other greenhouse gases |
| Solution | Montreal Protocol (phase out CFCs) | Reduce fossil fuel use |
| Effect | Skin cancer, crop damage | Global warming, sea level rise |
Worked exam question
Explain how chlorofluorocarbons (CFCs) cause the depletion of the ozone layer. [3]
CFCs are released into the atmosphere and drift up to the stratosphere [1]. UV radiation breaks the C-Cl bond, releasing chlorine atoms/radicals [1]. The chlorine atoms react with ozone molecules (Cl + O₃ → ClO + O₂), destroying them, and the chlorine is regenerated to destroy more ozone — acting as a catalyst [1].
Common exam mistakes
- Saying CFCs “burn a hole in the ozone layer” — the ozone is destroyed by catalytic chemical reactions, not burning.
- Confusing ozone depletion with the greenhouse effect — they are separate environmental problems caused by different chemicals.
- Forgetting that chlorine acts as a catalyst — the key point is that one Cl atom destroys many O₃ molecules because it is regenerated.
- Saying “ozone causes global warming” — ozone depletion allows UV through; global warming is caused by greenhouse gases trapping heat.
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