Chapter 17: Problem 20
Explain how CFCs deplete the ozone layer.
Short Answer
Expert verified
CFCs release chlorine atoms in the stratosphere, which repeatedly destroy ozone molecules, leading to ozone depletion.
Step by step solution
01
Understanding CFCs
Chlorofluorocarbons (CFCs) are man-made compounds consisting of chlorine, fluorine, and carbon. They are stable, nonflammable, and mostly used in air conditioning, refrigeration, and aerosol propellants.
02
Release into the Atmosphere
CFCs are released into the atmosphere through various human activities. Due to their stability, they remain in the lower atmosphere for long periods before gradually rising to the stratosphere.
03
CFCs Reach the Stratosphere
Once in the stratosphere, CFCs are broken down by ultraviolet (UV) radiation. The energy from UV rays is enough to break the bonds between atoms in CFC molecules, releasing chlorine atoms.
04
Role of Free Chlorine Atoms
The free chlorine atoms react with ozone (O₃) molecules in the stratosphere. The reaction can be represented as: \[ \text{Cl} + \text{O}_3 \rightarrow \text{ClO} + \text{O}_2 \] Here, the chlorine atom reacts with an ozone molecule, converting it into oxygen (O₂) and creating a chlorine monoxide (ClO).
05
Ozone Depletion Cycle
The chlorine monoxide (ClO) can further react with another oxygen atom: \[ \text{ClO} + \text{O} \rightarrow \text{Cl} + \text{O}_2 \] In this reaction, the free chlorine atom is regenerated and can repeat the process of breaking down another ozone molecule. This cycle can continue, depleting significant amounts of ozone over time.
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Key Concepts
These are the key concepts you need to understand to accurately answer the question.
Chlorofluorocarbons (CFCs)
Chlorofluorocarbons, commonly known as CFCs, consist of chlorine, fluorine, and carbon. These compounds were popular for being highly efficient in various applications due to their stability, nonflammability, and low toxicity.
- Used extensively in products like refrigerants, air conditioners, foam blowing agents, and aerosol propellants.
- Their molecular stability makes them persist in the atmosphere for long durations without breaking down.
Chlorine Atoms
Chlorine atoms are a significant factor in the depletion of the ozone layer. When CFCs are exposed to ultraviolet radiation in the stratosphere, they break down, releasing free chlorine atoms.
- These chlorine atoms are highly reactive and have the potential to disrupt many chemical processes.
- By reacting with ozone molecules, they catalyze ozone depletion, contributing to a harmful cycle.
Stratosphere
The stratosphere is the second layer of Earth's atmosphere, positioned above the troposphere and below the mesosphere.
- It plays a crucial role by housing the ozone layer, which absorbs the majority of the sun's harmful ultraviolet radiation.
- The ozone layer is situated between approximately 10 km and 50 km above Earth’s surface, mainly concentrated in the lower portion of the stratosphere.
Ultraviolet Radiation
Ultraviolet (UV) radiation is a type of energy emitted by the sun and plays a critical role in both protecting and affecting life on Earth. When UV radiation comes into contact with CFCs in the stratosphere, it initiates a breakdown process.
- UV rays provide the energy necessary to sever the strong molecular bonds in CFCs.
- This process releases chlorine atoms, which then partake in ozone depletion reactions.
Ozone Layer
The ozone layer is a protective shield in the Earth's stratosphere, crucial for life as it absorbs the majority of the sun’s harmful ultraviolet (UV) radiation.
- Consists of high concentrations of ozone (O₃) molecules.
- Protects living organisms by reducing the risk of skin cancer, cataracts, and showing harmful effects on ecosystems.