Ozone Depletion

Lajoy Tucker

Teacher

Lajoy Tucker

Introduction & Definitions

  • Ozone in the upper atmosphere absorbs harmful ultraviolet (UV) radiation, protecting life on Earth.

  • Ozone is formed and broken down naturally in a reversible cycle:

  • The presence of chlorofluorocarbons (CFCs) in the stratosphere disrupts this balance, leading to ozone depletion.

  • Chlorofluorocarbons are organic compounds containing carbon, chlorine, and fluorine historically used as refrigerants and in aerosols.

Role of CFCs in Ozone Depletion

  • CFCs are unreactive in the lower atmosphere but break down in the upper atmosphere under UV light:

Example:

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  • A bond undergoes homolytic fission resulting in the formation of two radicals (the covalent bond breaks evenly giving one electron to each to the bonded atoms)

  • bonds are not broken as they are stronger than bonds

  • The chlorine radical produced initiates a chain reaction that destroys ozone molecules.

Catalytic Cycle of Ozone Depletion

Chlorine radicals catalyse the breakdown of ozone via a chain reaction:

Step 1:

Step 2:

Overall Reaction:

  • The chlorine radical is regenerated, allowing one to destroy many ozone molecules.

Environmental Impact and Legislation

The discovery that CFCs deplete ozone led to global concern and international agreements, such as the Montreal Protocol (1987), to phase out CFCs.

Chemists contributed by:

  • Providing evidence from atmospheric studies.

  • Developing alternatives to CFCs, such as hydrofluorocarbons , which do not release radicals.

Summary of Key Reactions and Equations

Stage

Reaction

Description

Initiation

UV light breaks bond producing two radicals

Propagation 1

Chlorine radical attacks ozone

Propagation 2

Chlorine oxide radical reacts again

Overall

Net loss of ozone molecules

Practice Questions

Question 1

Write two equations to show how chlorine radicals catalyse the decomposition of ozone

Answer

Question 2

Explain why a single CFC molecule can destroy many ozone molecules

Answer

The chlorine radical () is regenerated during the catalytic cycle, so it can participate in many cycles of ozone destruction.

Give an equation to show the photodissociation of

Answer

A bond is broken by homolytic fission. The bond is stronger and therefore not broken.

Tips

  • Always show radicals clearly using a dot .

  • Use UV above the arrow when showing photodissociation.

  • Don't confuse CFCs with greenhouse gases — this topic focuses on ozone depletion, not climate change.

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