Concept:
Under steady-state heat conduction through a composite wall arrangement where layers or plates are connected in a series orientation, the rate of heat transfer through each individual layer must remain completely identical. This is governed by Fourier's Law of Heat Conduction, which states:
\[
Q = -k \cdot A \cdot \frac{\Delta T}{\Delta x}
\]
Where:
• \( Q \) is the total steady-state rate of heat flow across the cross-sectional area.
• \( k \) represents the unique physical parameter known as the thermal conductivity of the material.
• \( A \) represents the surface area perpendicular to the direction of heat flow.
• \( \Delta T \) represents the temperature drop across the corresponding thickness.
• \( \Delta x \) or \( L \) represents the spatial thickness of the physical plate.
Step 1: Setting up variables and identifying constraints from the problem description.
Let us establish and explicitly define the parameter metrics for both Plate A and Plate B:
• Thickness of Plate A: \( L_A \)
• Thickness of Plate B: \( L_B \)
• Thermal conductivity of Plate A: \( k_A \)
• Thermal conductivity of Plate B: \( k_B \)
• Temperature difference across Plate A: \( \Delta T_A \)
• Temperature difference across Plate B: \( \Delta T_B \)
The text directly provides a structural constraint regarding the thickness relation: "Plate B has twice the thickness of plate A." Mathematically, this gives:
\[
L_B = 2 \cdot L_A
\]
Step 2: Equating the steady-state heat flow rates for a series network.
Since the configuration is in series and normal to the flow of heat, the heat flux (\( q = Q/A \)) through Plate A matches the heat flux through Plate B perfectly:
\[
q_A = q_B
\]
Applying Fourier's equation to each individual layer independently, we can write:
\[
\frac{k_A \cdot \Delta T_A}{L_A} = \frac{k_B \cdot \Delta T_B}{L_B}
\]
Now, let us substitute the expression for thickness, \( L_B = 2 \cdot L_A \), into the right-hand side of our steady-state balance equation:
\[
\frac{k_A \cdot \Delta T_A}{L_A} = \frac{k_B \cdot \Delta T_B}{2 \cdot L_A}
\]
We can eliminate the common denominator term \( L_A \) from both sides by multiplying the entire mathematical equation by \( L_A \):
\[
k_A \cdot \Delta T_A = \frac{k_B \cdot \Delta T_B}{2}
\]
Rearranging this algebraic formulation to express the ratio of the temperature differences across both individual components gives:
\[
\frac{\Delta T_A}{\Delta T_B} = \frac{k_B}{2 \cdot k_A}
\]
Step 3: Evaluating the conditional limit for temperature variations.
The core objective is to determine the specific criteria required so that "the temperature difference across plate A is greater than that across plate B." Mathematically, this condition is written as:
\[
\Delta T_A > \Delta T_B
\]
Dividing both sides by the positive quantity \( \Delta T_B \), this statement transforms into:
\[
\frac{\Delta T_A}{\Delta T_B} > 1
\]
Now, substitute our previously derived ratio involving thermal conductivities into this inequality:
\[
\frac{k_B}{2 \cdot k_A} > 1
\]
Since the thermal conductivity coefficients are strictly positive engineering constants, we can perform standard algebraic cross-multiplication without flipping the direction of our inequality sign:
\[
k_B > 2 \cdot k_A
\]
To isolate the parameter \( k_A \), divide both sides of this final inequality constraint by the integer constant 2:
\[
\frac{k_B}{2} > k_A \quad \Rightarrow \quad k_A < \frac{1}{2} \, k_B
\]
Rewriting this fraction in standard decimal notation yields:
\[
k_A < 0.5 \, k_B
\]
Note that under steady-state operation, the specific heat capacity parameters (\( C_{pA} \) and \( C_{pB} \)) play absolutely no operational role because temperature distribution profiles across the system are time-invariant (\( \partial T / \partial t = 0 \)). Hence, variations in heat capacity parameters do not impact steady temperature differentials.