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IGCSE Chemistry: Cambridge 0620 tutoring, Malaysia

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

  1. CFCs are very stable and do not break down in the lower atmosphere
  2. They slowly drift up to the stratosphere over several years
  3. 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)

  1. The chlorine atom reacts with ozone:

Cl + O₃ → ClO + O₂

  1. The ClO then reacts with another oxygen atom:

ClO + O → Cl + O₂

  1. 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

EffectExplanation
Increased skin cancer ratesMore UV-B radiation reaches the surface, damaging DNA in skin cells
Increased eye cataractsUV radiation damages the lens of the eye
Damage to cropsUV inhibits photosynthesis and damages plant tissues
Harm to marine planktonPlankton near the ocean surface are killed by UV; this disrupts the marine food chain
Damage to materialsUV 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

AlternativeUseAdvantageLimitation
HFCs (hydrofluorocarbons)RefrigerantsDo not contain chlorine; do not damage ozoneSome are potent greenhouse gases
HCFCs (hydrochlorofluorocarbons)Transitional refrigerantsBreak down faster in the atmosphereStill contain chlorine (being phased out)
Hydrocarbons (propane, butane)Refrigerants, aerosolsNo ozone damage, low greenhouse effectFlammable
CO₂Some refrigerationNo ozone damageGreenhouse gas

Ozone depletion vs the greenhouse effect

Students often confuse these two issues:

FeatureOzone depletionGreenhouse effect
WhereStratosphereTroposphere
ProblemUV radiation reaching EarthHeat trapped in the atmosphere
Caused byCFCs (and related compounds)CO₂, CH₄, and other greenhouse gases
SolutionMontreal Protocol (phase out CFCs)Reduce fossil fuel use
EffectSkin cancer, crop damageGlobal 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

  1. Saying CFCs “burn a hole in the ozone layer” — the ozone is destroyed by catalytic chemical reactions, not burning.
  2. Confusing ozone depletion with the greenhouse effect — they are separate environmental problems caused by different chemicals.
  3. Forgetting that chlorine acts as a catalyst — the key point is that one Cl atom destroys many O₃ molecules because it is regenerated.
  4. Saying “ozone causes global warming” — ozone depletion allows UV through; global warming is caused by greenhouse gases trapping heat.

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Frequently asked questions

How do CFCs destroy the ozone layer?

CFCs rise into the stratosphere where UV radiation breaks them apart, releasing chlorine atoms. Each chlorine atom acts as a catalyst — it reacts with ozone (O3) to form ClO and O2, then the ClO reacts with another oxygen atom to regenerate the Cl atom. A single chlorine atom can destroy thousands of ozone molecules.

Why is the ozone layer important?

The ozone layer in the stratosphere absorbs most of the Sun's harmful ultraviolet (UV) radiation, protecting living organisms from skin cancer, eye cataracts, and damage to crops and marine plankton.

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