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Ozone, \(\mathrm{O}_{\mathfrak{3}}\), decomposes to molecular oxygen in the stratosphere according to the reaction \(2 \mathrm{O}_{3}(g) \longrightarrow 3 \mathrm{O}_{2}(g)\). Would an increase in pressure favor the formation of ozone or of oxygen?

Short Answer

Expert verified
An increase in pressure will favor the formation of ozone \((\mathrm{O}_3)\), as the reaction will shift to the left (towards the reactants) to minimize the effect of the pressure increase, according to Le Chatelier's Principle.

Step by step solution

01

Understand Le Chatelier's Principle

Le Chatelier's Principle states that if a system at equilibrium is subjected to change in concentration, pressure, or temperature, the equilibrium will shift to counteract the change and establish a new equilibrium.
02

Identify the change in the system

In this case, the change in the system is an increase in pressure. According to Le Chatelier's Principle, the reaction will shift to minimize the effect of the pressure increase.
03

Analyze the effect of pressure on the reaction

The given reaction is: \( 2 \mathrm{O}_{3}(g) \longrightarrow 3 \mathrm{O}_{2}(g) \) On the left-hand side of the reaction (reactants), there are 2 moles of gaseous ozone, and on the right-hand side of the reaction (products), there are 3 moles of gaseous oxygen.
04

Apply Le Chatelier's Principle to determine the favored side

Since an increase in pressure will be minimized by a decrease in the total number of gas molecules, the reaction will shift in the direction that has fewer moles of gas. In this case, the reaction will shift to the left (towards the reactants). Hence, an increase in pressure will favor the formation of ozone \( (\mathrm{O}_{3})\).

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Key Concepts

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

Chemical Equilibrium
Imagine a crowded dance floor where dancers move in and out with a certain rhythm. In a similar way, chemical equilibrium is like a dance between reactants and products. It occurs when the rate of the forward reaction, where reactants turn into products, is equal to the rate of the reverse reaction, where products revert back to reactants. It's important to note that when a chemical system is at equilibrium, it's dynamic - reactions don't stop happening; they occur at equal rates, maintaining a consistent concentration of substances involved.

Understanding equilibrium is crucial because it helps us predict how a reaction will respond to changes. This is where Le Chatelier's Principle comes into play, as it helps us understand that if a disturbance is introduced, like a change in pressure, the equilibrium will shift to counteract the change.
Stratospheric Ozone Decomposition
The decomposition of ozone in the stratosphere might seem like a distant concept, but it's surprisingly close to everyday life – it is important for understanding environmental science and protecting our planet. Ozone, or \(\mathrm{O}_{3}\), in the stratosphere absorbs harmful ultraviolet radiation from the sun, playing a critical role in shielding life on Earth.

The reaction given in the exercise, \(2 \mathrm{O}_{3}(g) \longrightarrow 3 \mathrm{O}_{2}(g)\), shows that two molecules of ozone decompose to form three molecules of molecular oxygen. While this reaction is natural and necessary for the formation of ozone, understanding it can also lend insight into environmental phenomena such as the depletion of the ozone layer, in which human activities can inadvertently accelerate this process.
Reaction Shift Due to Pressure Change
When you're in an elevator, and more people get in, you can feel the space getting tighter; similarly, increasing the pressure in a reaction's environment is like filling up that elevator. Le Chatelier's Principle suggests that the reaction will try to 'make more room.' How does it do this? By shifting toward the side with fewer moles of gas. In the stratospheric ozone decomposition reaction, this would mean favoring the side with the fewer gas molecules.

In our example, \(2 \mathrm{O}_{3}(g) \longrightarrow 3 \mathrm{O}_{2}(g)\), when pressure increases, the system will move towards the side with 2 moles of O3, the side that takes up less space. So, in response to a pressure increase, the system favors the production of ozone (\

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Most popular questions from this chapter

Consider the following equilibrium for which \(\Delta H<0\) $$ 2 \mathrm{SO}_{2}(g)+\mathrm{O}_{2}(g) \rightleftharpoons 2 \mathrm{SO}_{3}(g) $$ How will each of the following changes affect an equilibrium mixture of the three gases: (a) \(\mathrm{O}_{2}(g)\) is added to the system; (b) the reaction mixture is heated; (c) the volume of the reaction vessel is doubled; (d) a catalyst is added to the mixture; (e) the total pressure of the system is increased by adding a noble gas; (f) \(\mathrm{SO}_{3}(g)\) is removed from the system?

At \(800 \mathrm{~K}\), the equilibrium constant for \(\mathrm{I}_{2}(g) \rightleftharpoons 2 \mathrm{I}(\mathrm{g})\) is \(K_{c}=3.1 \times 10^{-5}\). If an equilibrium mixture in a 10.0-L vessel contains \(2.67 \times 10^{-2} \mathrm{~g}\) of \(\mathrm{I}(\mathrm{g})\), how many grams of \(\mathrm{I}_{2}\) are in the mixture?

(a) If \(Q_{c}>K_{c}\), how must the reaction proceed to reach equilibrium? (b) At the start of a certain reaction, only reactants are present; no products have been formed. What is the value of \(Q_{c}\) at this point in the reaction?

Consider the following equilibrium: $$ 2 \mathrm{H}_{2}(g)+\mathrm{S}_{2}(g) \rightleftharpoons 2 \mathrm{H}_{2} \mathrm{~S}(g) \quad K_{c}=1.08 \times 10^{7} \text { at } 700{ }^{\circ} \mathrm{C} $$ (a) Calculate \(K_{p-}\) (b) Does the equilibrium mixture contain mostly \(\mathrm{H}_{2}\) and \(\mathrm{S}_{2}\) or mostly \(\mathrm{H}_{2} \mathrm{~S}\) ? (c) Calculate the value of \(K_{c}\) if you rewrote the equation \(\mathrm{H}_{2}(g)+\frac{1}{2} \mathrm{~S}_{2}(g) \rightleftharpoons \mathrm{H}_{2} \mathrm{~S}(g)\).

Write the expressions for \(K_{c}\) for the following reactions. In each case indicate whether the reaction is homogeneous or heterogeneous. (a) \(2 \mathrm{O}_{3}(g) \rightleftharpoons 3 \mathrm{O}_{2}(g)\) (b) \(\mathrm{Ti}(s)+2 \mathrm{Cl}_{2}(g) \rightleftharpoons \mathrm{TiCl}_{4}(l)\) (c) \(2 \mathrm{C}_{2} \mathrm{H}_{4}(g)+2 \mathrm{H}_{2} \mathrm{O}(g) \rightleftharpoons 2 \mathrm{C}_{2} \mathrm{H}_{6}(g)+\mathrm{O}_{2}(g)\) (d) \(\mathrm{C}(\mathrm{s})+2 \mathrm{H}_{2}(\mathrm{~g}) \rightleftharpoons \mathrm{CH}_{4}(g)\) (e) \(4 \mathrm{HCl}(a q)+\mathrm{O}_{2}(g) \rightleftharpoons 2 \mathrm{H}_{2} \mathrm{O}(l)+2 \mathrm{Cl}_{2}(g)\) (f) \(2 \mathrm{C}_{8} \mathrm{H}_{\mathrm{t}}(l)+25 \mathrm{O}_{2}(g) \rightleftharpoons 16 \mathrm{CO}_{2}(g)+18 \mathrm{H}_{2} \mathrm{O}(g)\) (g) \(2 \mathrm{C}_{8} \mathrm{H}_{18}(l)+25 \mathrm{O}_{2}(g) \rightleftharpoons 16 \mathrm{CO}_{2}(g)+18 \mathrm{H}_{2} \mathrm{O}(l)\)

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