The Dynamics of Dissociation
A Journey Through the Ideal Gas Law
Imagine a closed cylinder filled with a diatomic gas. This is our starting point, a perfectly stable system governed by the elegant rules of thermodynamics. Let's assume the initial number of moles of this diatomic gas is μ0. The pressure is p1, the volume is V1, and the temperature is a cool 250K.
By applying the ideal gas equation, pV=nRT, we can perfectly describe this initial state.
This simple equation is our anchor. It ties together all the macroscopic properties of the gas before any dramatic changes occur.
The Catalyst of Change
Now, the system undergoes a massive transformation. The volume is forcibly doubled to 2V1, and the temperature is cranked up to a blistering 2000K. But the most critical change happens at the microscopic level: dissociation.
The intense heat causes 25% of the diatomic molecules to break their bonds. This is where many students make a critical error. When one diatomic molecule (like O2) breaks apart, it doesn't just disappear; it forms two separate monoatomic atoms (like 2O). This fundamental conservation of atoms means the total number of particles—and therefore the total number of moles—will increase.
Let's calculate the new number of moles, μ2. The remaining, intact diatomic molecules make up 75% of the original amount, which is 0.75μ0. The 25% that dissociated (0.25μ0) yields twice as many monoatomic moles, giving us 2×0.25μ0=0.5μ0.
Adding these together gives us the total moles in the final state:
μ2=0.75μ0+0.5μ0=1.25μ0
The Grand Synthesis
Armed with our new mole count, we can write the ideal gas equation for the final state. The new pressure is p2, the volume is 2V1, and the temperature is 2000K.
p2(2V1)=(1.25μ0)R(2000)
To find the ratio of the final pressure to the initial pressure, p1p2, we simply divide our final state equation by our initial state equation. This is a beautiful mathematical maneuver because all the constants and initial variables—like V1, μ0, and the universal gas constant R—will gracefully cancel out.
p1V1p2(2V1)=μ0R(250)1.25μ0R(2000)
Simplifying the right side, we divide 2000 by 250 to get 8.
Multiplying 1.25 by 8 yields exactly 10. Finally, dividing both sides by 2 reveals our answer.
The pressure in the final state is exactly five times the initial pressure. This problem beautifully illustrates how macroscopic changes in volume and temperature, combined with microscopic changes like molecular dissociation, collectively dictate the final state of a gas.