The Tale of Two Chambers
Imagine two rooms side by side, separated by a wall that allows heat to pass through but cannot move. Room 1 (S1) is completely rigid—its walls are fixed, meaning its volume can never change. Room 2 (S2), however, has a flexible wall—a freely movable piston exposed to the outside atmosphere. This means the pressure inside Room 2 will always adjust to match the constant atmospheric pressure outside.
Both rooms contain exactly one mole of a monoatomic gas. Because they are at different temperatures, heat will naturally flow from the hotter room to the colder one through the conducting partition. Our goal is to find out exactly how long it takes for the initial temperature difference, ΔT0, to drop to half its value.
The Thermodynamics of Heat Exchange
Let's assume S1 is hotter than S2. Heat will flow from S1 to S2. According to Fourier's law of heat conduction, the rate of this heat transfer is directly proportional to the temperature difference ΔT=TS1−TS2:
As S1 loses heat, its temperature drops. Because its volume is fixed, this is an isochoric process. All the heat lost goes directly into decreasing its internal energy. Using the molar heat capacity at constant volume (Cv=23R for a monoatomic gas), we can write:
−dQ=nCvdT1⟹dT1=−3R2dQ
Meanwhile, S2 absorbs this exact same heat. But S2 is at constant pressure! As it heats up, it expands, doing work against the atmosphere. This is an isobaric process. We must use the molar heat capacity at constant pressure (Cp=25R):
Forging the Master Equation
We are interested in the temperature difference, ΔT. Let's see how fast this difference is shrinking by taking its derivative with respect to time:
Substituting our expressions for the temperature changes of each individual gas:
dtd(ΔT)=−3R2dtdQ−5R2dtdQ=−dtdQ(3R2+5R2)
Adding the fractions gives us 15R16. Now, we substitute our very first equation for the rate of heat conduction, dtdQ:
dtd(ΔT)=−15R16(xKAΔT)=−15xR16KAΔT
Notice the beautiful negative sign! It mathematically guarantees that the temperature difference is decaying over time, exactly as physics dictates.
The Final Countdown
We now have a classic first-order separable differential equation. We separate the variables and integrate from time t=0 (where the difference is ΔT0) to time t (where the difference is 2ΔT0):
∫ΔT0ΔT0/2ΔTd(ΔT)=−15xR16KA∫0tdt
Evaluating the integral yields the natural logarithm:
ln(ΔT0ΔT0/2)=−15xR16KAt
ln(21)=−15xR16KAt⟹−ln2=−15xR16KAt
Solving for t, we get:
We are given that ln2≈0.7. Plugging this in:
t=1615×0.7KAxR=1610.5KAxR=0.65625KAxR
Rounding to two decimal places, we find that t≈0.66KAxR. Comparing this to the given form t=nKAxR, we conclude that n=0.66.