Thermal conduction
Apply Fourier’s law, thermal resistance and sign conventions to conduction, with links to convection and radiation.
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ContinueThis page gives the UY1 working model/result for Conduction. You reuse it when you turn thermal intuition into calculable models (energy balances, process reasoning, and kinetic/statistical links), with careful sign/units checks.
- Module path: Thermodynamics (UY1)
- Full routing: UY1 assessment map
- Math toolkit: Mathematics for undergraduate physics
At a glance
- Prerequisites: temperature gradient, energy conservation, basic calculus.
- Outcomes: apply Fourier’s law in 1D and interpret thermal conductance/resistance.
- Key result: Q dot = -kA dT/dx.
- Common trap: dropping the minus sign without controlling direction conventions.
Setup
Model a homogeneous slab/rod in 1D (x direction):
- Cross-sectional area A constant.
- Thermal conductivity k constant (for first-pass UY1 problems).
- T(x) smooth.
Physical interpretation:
- k (thermal conductivity) tells you how strongly a material conducts heat for a given gradient. Large k (metals) means a small gradient can carry large heat flow.
- Heat flow is driven by a gradient: conduction is the “diffusion of microscopic energy” through matter.
Sign convention:
- Positive x to the right.
- Positive Q dot taken as heat flow in +x direction.
Bridge note (O-Level to UY1):
- O-Level: heat flows hot to cold.
- UY1 upgrade: quantify local flux with a differential law and sign.
Core derivation / explanation
Fourier’s law (1D):
The minus sign enforces hot-to-cold flow:
- If dT/dx < 0 (temperature decreases rightward), then Q dot > 0 (flow rightward).
For steady conduction through uniform slab length L with end temperatures Tₕ > Tc:
Define thermal resistance:
This mirrors Ohm’s-law structure.
Limit checks:
- k → 0 gives Q dot → 0 (perfect insulator in this model).
- L → 0 gives very large Q dot for a fixed Δ T (the “short path” limit).
- Keep a consistent direction convention: the minus sign in Fourier’s law enforces “hot to cold”. - If k depends strongly on T, the steady slab result Q dot = kAΔ T/L must be replaced by an integral form. - Real systems can have contact resistances and multi-dimensional spreading; the 1D slab model is a controlled approximation.
Units check:
Physical sanity check:
- Larger k or A increases heat rate.
- Larger L lowers heat rate.
Heat rate through a copper rod
Worked example 1
Conduction through copper
Problem
Show full solution
Apply the steady slab law
Method
Use Q dot = kAΔ T/L for the hot-to-cold rate.Reason
Constant conductivity and insulated sides give a linear steady temperature gradient along the rod.Working
Answer
Q dot = (kAΔ T)/L = ((400)(2.0 × 10⁻⁴)(40))/0.50 = 6.4 W.Interpret the rate
Working
Answer
The rod transfers 6.4 J each second from hot to cold: Q dot = 6.4 W. This is a power, not a total heat energy.
Practice set
Check your understanding 1
For steady conduction through a uniform slab, what happens to Q dot when thickness doubles with conductivity, area and end temperatures fixed?
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Check your understanding 2
A uniform wall has k = 0.8 W m⁻¹K⁻¹, area 10 m², thickness 0.20 m and a temperature difference of 15 K. Find the steady heat rate, neglecting edge losses.
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Check your understanding 3
Temperature decreases as x increases in a rod. A calculation using positive k,A gives negative Q dot, defined as positive toward increasing x. What sign error should you check?
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Summary + next steps
- Conduction is quantified by local gradient-driven transport.
- Fourier’s law plus geometry gives practical heat-rate formulas.
- Thermal resistance form helps with multilayer systems.
Next steps:
- See transient profile formation in UY1: build up of temperature gradient.
- Then combine layers in UY1: thermal conduction through a compound slab.
- Compare with boundary transport in UY1: convection and radiative exchange in UY1: radiation.
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Syllabus and review details
No official syllabus alignment is listed for this lesson.