Welcome, future engineers and physicists! Today, we are going to dive into a fascinating problem that beautifully combines the concepts of thermal radiation and steady-state equilibrium. This is a classic scenario that tests your understanding of the Stefan-Boltzmann Law and your ability to set up a heat balance equation.
Imagine you are standing in a room with three massive, parallel plates kept very close to each other. These aren't just any plates; they are ideal black surfaces, meaning they are perfect absorbers and perfect emitters of radiation. The outer plates are maintained at constant temperatures of 2T and 3T. Our mission is to find the temperature of the middle plate once the system settles into a steady state.
Analyzing the Setup
Let's visualize the system. We have Plate 1 on the left at a temperature of 2T, Plate 3 on the right at a hotter temperature of 3T, and Plate 2 sandwiched in the middle. Let's assume the middle plate reaches an unknown steady temperature, which we will call T0.
What exactly does steady state mean in this context? It means that Plate 2 is in thermal equilibrium. It is no longer heating up or cooling down. For this to happen, the rate at which it absorbs heat must perfectly balance the rate at which it emits heat. Since Plate 3 is the hottest (3T), heat will flow from Plate 3 to Plate 2. Let's call this heat flow Q1. Simultaneously, since Plate 2 is hotter than Plate 1 (2T), heat will flow from Plate 2 to Plate 1. Let's call this heat flow Q2.
In steady state, the heat gained equals the heat lost:
Q1=Q2
The Master Equation
To quantify these heat flows, we turn to one of the most elegant equations in thermodynamics: the Stefan-Boltzmann Law. It states that the net heat transfer rate between two parallel black surfaces is proportional to the difference of the fourth powers of their absolute temperatures.
For the heat flowing from Plate 3 to Plate 2, we can write:
Q1=σA((3T)4−T04)
Similarly, for the heat flowing from Plate 2 to Plate 1, we write:
Q2=σA(T04−(2T)4)
Here, σ is the Stefan-Boltzmann constant, and A is the surface area of the plates.
The Algebraic Journey
Now, we substitute our expressions for
Q1 and
Q2 into our steady-state condition:
σA((3T)4−T04)=σA(T04−(2T)4)
Notice how the constants
σ and
A are present on both sides of the equation. Because the plates have the same area and are made of the same ideal material, these constants beautifully cancel out, leaving us with a pure temperature relationship:
(3T)4−T04=T04−(2T)4
Let's carefully expand the powers. Remember that
(3T)4=34⋅T4=81T4, and
(2T)4=24⋅T4=16T4. Substituting these back in, we get:
81T4−T04=T04−16T4
Final Calculation
We are almost there! Let's group the
T0 terms on one side and the
T terms on the other. By adding
T04 to both sides and adding
16T4 to both sides, we obtain:
81T4+16T4=T04+T04
97T4=2T04
Now, we isolate
T04 by dividing by 2:
T04=297T4
To find our final temperature
T0, we simply take the fourth root of both sides:
T0=(297)41T
And there we have it! The steady-state temperature of the middle plate is exactly (297)41T. This perfectly matches option (c).
This problem is a fantastic reminder of how powerful conservation laws are. By simply stating that 'energy in equals energy out', we were able to navigate through the physics of thermal radiation and arrive at a precise mathematical conclusion. Keep practicing, and always look for the underlying balance in physical systems!