Thermal radiation
Apply emissivity and the Stefan–Boltzmann law to net thermal-radiation exchange, using clear signs and limiting cases.
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ContinueThis page gives the UY1 working model/result for Radiation. 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: absolute temperature, surface area, power.
- Outcomes: compute emitted and net radiative heat transfer.
- Key result: Q dot ₙₑₜ = εσ A(Tₛ⁴-Tₛᵤᵣ⁴).
- Common trap: using Celsius instead of kelvin in T⁴ expressions.
Setup
Surface at absolute temperature Tₛ exchanges radiation with surroundings at Tₛᵤᵣ.
- Emissivity 0 ≤ ε ≤ 1.
- Stefan-Boltzmann constant σ = 5.67 × 10⁻⁸ W m⁻²K⁻⁴.
Physical interpretation:
- ε measures how “black” a surface is: ε = 1 is an ideal blackbody; small ε means weak emission/absorption.
- The T⁴ scaling means radiation becomes important at high absolute temperature even when convection is present.
Bridge note:
- Conduction/convection require matter; radiation works across vacuum.
- UY1 upgrade is quantitative net-exchange modeling with emissivity and fourth-power temperature dependence.
Core derivation / explanation
Emission from a gray surface:
Absorption from large isothermal surroundings:
Net from surface to surroundings:
For small temperature difference around mean Tₘ, linearized form:
This allows combined convection+radiation resistance modeling.
- Always use kelvin in any T⁴ expression. - Distinguish emitted power Q dot ₑₘᵢₜ = εσ ATₛ⁴ from net exchange Q dot ₙₑₜ = εσ A(Tₛ⁴-Tₛᵤᵣ⁴). - The simple absorption form used here assumes “large isothermal surroundings” (effectively a view factor of 1). More complex geometries need view factors. - The linearized hᵣ form is only accurate for sufficiently small temperature differences about Tₘ.
Units check:
Physical sign/limit checks:
- If Tₛ > Tₛᵤᵣ, net heat loss is positive outward.
- If Tₛ = Tₛᵤᵣ, net exchange is zero.
- Radiation grows rapidly with temperature because of T⁴ dependence.
Net radiative cooling of a surface
Worked example 1
Emission minus absorption
Problem
Show full solution
Subtract absorbed radiation
Method
Use εσ A(Tₛ⁴-Tₛᵤᵣ⁴).Reason
The enclosure also emits radiation toward the surface, so emission alone overestimates the net loss.Working
Answer
Q dot ₙₑₜ = 0.90(5.67 × 10⁻⁸)(0.50)(400⁴-300⁴) ≈ 4.47 × 10² W.State the outward heat rate
Working
Answer
Q dot ₙₑₜ ≈ 4.47 × 10² W, about 4.5 × 10² W to two significant figures. It is positive outward because 400⁴ > 300⁴; the units are W, not J.
Practice set
Check your understanding 1
A black surface has area 1.2 m² and temperature 350 K inside a large isothermal enclosure at 300 K. Find its net radiative heat-loss rate using σ = 5.67 × 10⁻⁸ W m⁻²K⁻⁴.
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Check your understanding 2
For a gray surface in the same large enclosure, emissivity halves while area and both temperatures stay fixed. What happens to net radiative heat transfer?
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Check your understanding 3
Why can polishing a hot metal surface reduce its radiative heat loss to cooler surroundings?
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Summary + next steps
- Radiation transfer depends strongly on absolute temperature and emissivity.
- Net exchange is a temperature-difference-in-fourth-powers law.
- At high temperature, radiation can dominate over convection.
Next steps:
- For spectral detail and peak wavelength shift, continue to UY1: Planck radiation law and Wien displacement law.
- Compare the other heat-transfer mechanisms: UY1: conduction and UY1: convection.
- Combine convection + conduction (and optionally radiation) using resistances in UY1: convective heat transfer.
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Syllabus and review details
No official syllabus alignment is listed for this lesson.