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Chlorine atoms contribute to the destruction of the earth's ozone layer by the following sequence of reactions: $$\begin{array}{l}\mathrm{Cl}+\mathrm{O}_{3} \rightarrow \mathrm{ClO}+\mathrm{O}_{2} \\ \mathrm{ClO}+\mathrm{O} \rightarrow \mathrm{Cl}+\mathrm{O}_{2}\end{array}$$ where the O atoms in the second step come from the decomposition of ozone by sunlight: $$\mathrm{O}_{3}(\mathrm{g}) \rightarrow \mathrm{O}(\mathrm{g})+\mathrm{O}_{2}(\mathrm{g})$$ What is the net equation on summing these three equations? Why does this lead to ozone loss in the stratosphere? What is the role played by Cl in this sequence of reactions? What name is given to species such as ClO?

Short Answer

Expert verified
Net equation: O₃ → 2O₂. Cl catalyzes ozone breakdown, causing ozone loss. ClO is a free radical.

Step by step solution

01

Analyze the Initial Reactions

Let's first understand the given reactions. The first reaction shows chlorine atom (Cl) reacting with ozone (O₃) to form chlorine monoxide (ClO) and oxygen (O₂). The second reaction indicates chlorine monoxide (ClO) reacting with atomic oxygen (O) to reform Cl and form O₂. The atomic oxygen in this step is produced by the decomposition of ozone (O₃) into O and O₂.
02

Write the Reactions

List the reactions given in the problem: 1. Cl + O₃ → ClO + O₂ 2. ClO + O → Cl + O₂ 3. O₃ → O + O₂ (decomposition of ozone)
03

Derive the Net Reaction

To find the net reaction, we sum up all three individual reactions: - Cl from reaction 1 is regenerated in reaction 2, so it cancels out. - ClO from reaction 1 is consumed in reaction 2, so it cancels out. - O (from reaction 3) is also consumed in reaction 2, leaving only the O₃ decomposition and the formation of 2 O₂. Upon cancellation, the net reaction becomes: O₃ → O₂ + O₂ Simplifying, the net equation is: O₃ → 2O₂
04

Explain Ozone Loss

The net reaction indicates the conversion of ozone (O₃) into oxygen molecules (O₂). This shows that ozone is being decomposed. Therefore, chlorine acts as a catalyst in reactions that lead to the decomposition of ozone into more stable oxygen molecules, reducing the amount of ozone and contributing to ozone layer depletion.
05

Identify the Role of Chlorine

Chlorine (Cl) acts as a catalyst in these reactions. It is not consumed in the net reaction; instead, it facilitates the breakdown of ozone (O₃) into oxygen (O₂), then emerges unchanged at the end of the reaction sequence to repeat the cycle with new ozone molecules.
06

Define the Name of Species Like ClO

Species like ClO that are intermediates in reactions and participate in the chemical transformation are often referred to as 'free radicals'. Free radicals are highly reactive due to the presence of unpaired electrons.

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Chlorine Catalysis
In the process of ozone depletion, chlorine atoms play a pivotal role through a mechanism known as chlorine catalysis. This is a series of reactions where chlorine (Cl) is temporarily transformed but ultimately regenerated. In essence, chlorine acts as a catalyst, meaning it speeds up the chemical reactions without being consumed by them.
When chlorine atoms react with ozone ( O_3 ), they form chlorine monoxide ( ClO ) and oxygen ( O_2 ). This is the first step in the cycle. Following this, the ClO reacts with an atomic oxygen ( O ) to release another O_2 and regenerate the original chlorine atom.
Chlorine's catalytic behavior is key because it allows each atom to destroy many ozone molecules, leading to substantial depletion over time. The fact that chlorine is recycled in this process makes its impact long-lasting and persistent.
Ozone Layer
The ozone layer is a critical part of Earth's atmosphere, located in the stratosphere. It contains high concentrations of ozone ( O_3 ), which forms a protective shield by absorbing most of the Sun's harmful ultraviolet (UV) radiation.
This layer is vital for life on Earth as it prevents the UV radiation from reaching the planet's surface, where it can cause skin cancer and cataracts in humans, and damage plants and ecosystems.
Ozone depletion occurs when substances like chlorine, often originating from man-made compounds such as chlorofluorocarbons (CFCs), break down ozone molecules. This depletion thins the ozone layer, reducing its ability to absorb UV radiation, thus posing a threat to life by allowing more UV radiation to pass through.
Free Radicals
Free radicals, like chlorine monoxide ( ClO ), are highly reactive species that play a significant role in atmospheric chemistry. They are molecules that have unpaired electrons, which makes them extremely reactive.
In the context of ozone depletion, free radicals are crucial intermediates. For example, ClO is formed when chlorine reacts with ozone. This radical then participates in further reactions that continue the cycle of ozone destruction.
The reactivity of free radicals accelerates the breakdown of ozone into oxygen molecules ( O_2 ), contributing to the thinning of the ozone layer over time. Their high reactivity, combined with the catalytic nature of chlorine, leads to significant and efficient ozone destruction.
Atmospheric Chemistry
Atmospheric chemistry involves the study of chemical processes that occur in the Earth's atmosphere. It is a complex field that includes the transformation and movement of chemicals in different layers of the atmosphere.
Ozone depletion is a prime example of atmospheric chemistry at work. The interaction of sunlight, chlorine atoms, and ozone molecules illustrate how chemical reactions in the atmosphere can have wide-reaching effects.
These reactions occur in the stratosphere, where UV radiation from the sun can initiate the breakdown of ozone. This understanding has led to global efforts to reduce ozone-depleting substances, showing how atmospheric chemistry informs environmental policy and protection efforts.
The continuous study of atmospheric chemistry is crucial for predicting changes in climate, protecting human health, and preserving ecological systems. By understanding the chemistry of the atmosphere, scientists can better understand phenomena like ozone depletion and develop strategies to mitigate its impacts.

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Most popular questions from this chapter

The reaction of \(\mathrm{NO}_{2}(\mathrm{g})\) and \(\mathrm{CO}(\mathrm{g})\) is thought to occur in two steps: Step 1: Slow \(\mathrm{NO}_{2}(\mathrm{g})+\mathrm{NO}_{2}(\mathrm{g}) \rightarrow \mathrm{NO}(\mathrm{g})+\mathrm{NO}_{3}(\mathrm{g})\) Step 2: Fast \(\mathrm{NO}_{3}(\mathrm{g})+\mathrm{CO}(\mathrm{g}) \rightarrow \mathrm{NO}_{2}(\mathrm{g})+\mathrm{CO}_{2}(\mathrm{g})\) (a) Show that the elementary steps add up to give the overall, stoichiometric equation. (b) What is the molecularity of each step? (c) For this mechanism to be consistent with kinetic data, what must be the experimental rate equation? (d) Identify any intermediates in this reaction.

If the rate constant for a reaction triples when the temperature rises from \(3.00 \times 10^{2} \mathrm{K}\) to \(3.10 \times 10^{2} \mathrm{K},\) what is the activation energy of the reaction?

Ozone, \(\mathbf{O}_{3},\) in the earth's upper atmosphere decomposes according to the equation $$2 \mathrm{O}_{3}(\mathrm{g}) \rightarrow 3 \mathrm{O}_{2}(\mathrm{g})$$ The mechanism of the reaction is thought to proceed through an initial fast, reversible step followed by a slow, second step. Step 1: \(\quad\) Fast, reversible \(\mathbf{O}_{3}(\mathrm{g}) \rightleftarrows \mathrm{O}_{2}(\mathrm{g})+\mathrm{O}(\mathrm{g})\) Step 2: \(\quad\) Slow \(\quad \mathbf{O}_{3}(\mathrm{g})+\mathbf{O}(\mathrm{g}) \rightarrow 2 \mathrm{O}_{2}(\mathrm{g})\) (a) Which of the steps is rate-determining? (b) Write the rate equation for the rate-determining step.

The radioactive isotope \(^{64} \mathrm{Cu}\) is used in the form of copper(II) acetate to study Wilson's disease. The isotope has a half-life of 12.70 hours. What fraction of radioactive copper(II) acetate remains after 64 hours?

Describe each of the following statements as true or false. If false, rewrite the sentence to make it correct. (a) The rate-determining elementary step in a reaction is the slowest step in a mechanism. (b) It is possible to change the rate constant by changing the temperature. (c) As a reaction proceeds at constant temperature, the rate remains constant. (d) A reaction that is third order overall must involve more than one step.

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