Thermal Engineering

Radiation Heat Transfer

Heat crossing a vacuum as glowing light

Radiation heat transfer is the exchange of thermal energy by electromagnetic waves — heat that travels as light and so needs no medium at all, crossing empty space at 3×10⁸ m/s. Every surface above absolute zero glows, mostly in the infrared, and the power it radiates follows the Stefan-Boltzmann law: Q = εσAT⁴. The fourth-power dependence on absolute temperature is the whole story — a doubling of T radiates 16 times more heat, which is why radiation rules furnaces, rocket nozzles and reentry shields while barely registering at room temperature. The net heat actually exchanged between two surfaces is set by their temperatures, their emissivities, and the view factor that decides how much of each other they see.

  • Stefan-Boltzmann lawQ = εσAT⁴
  • Stefan-Boltzmann constant σ5.670×10⁻⁸ W/m²K⁴
  • Temperature scaling∝ T⁴ (double T → 16×)
  • Emissivity ε range0.02 (polished) – 0.98 (matte black)
  • Medium requiredNone — works in vacuum
  • Peak wavelength (300 K)~9.7 µm (far infrared)

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The Stefan-Boltzmann law

Radiation is the third mode of heat transfer, alongside conduction and convection. The crucial difference is that it carries energy as electromagnetic waves rather than through a material, so it works perfectly across a vacuum. For an ideal emitter — a blackbody — the total power radiated per unit area over all wavelengths is:

E_b = σ · T⁴       (blackbody emissive power, W/m²)

Q   = ε · σ · A · T⁴   (real surface, total power, W)

where:
  σ = 5.670×10⁻⁸ W/m²K⁴   (Stefan-Boltzmann constant)
  ε = emissivity            (0 ≤ ε ≤ 1, dimensionless)
  A = radiating area        (m²)
  T = absolute temperature  (K, never °C)

The single most important feature is the fourth power. Because Q ∝ T⁴, doubling the absolute temperature multiplies the radiated power by sixteen. A surface at 600 K radiates 16× more than the same surface at 300 K, and a tungsten filament at 3000 K radiates roughly 10,000× more than it would at 300 K. Always work in kelvin — using °C here gives nonsense.

The radiation isn't monochromatic; it spans a spectrum described by Planck's law, and the wavelength of peak emission follows Wien's displacement law, λ_max·T ≈ 2898 µm·K. At human body temperature (310 K) the peak sits near 9.4 µm in the far infrared, invisible to the eye. Heat a steel bar past ~800 K and the spectrum's short-wavelength tail reaches into the visible, and it glows red — the same physics that lets a thermal camera "see" warm objects in the dark.

Emissivity and Kirchhoff's law

Real surfaces are not blackbodies. Emissivity ε scales the blackbody power down to what an actual surface emits. By Kirchhoff's law of thermal radiation, at a given temperature and wavelength a surface's emissivity equals its absorptivity: a good emitter is a good absorber. This single fact governs every radiation design decision — you cannot make a surface shed heat well by radiation without also making it soak up incoming radiation well.

SurfaceEmissivity ε (long-wave IR)BehaviourTypical use
Polished silver / aluminum0.02 – 0.05Reflects, barely emitsVacuum-flask walls, MLI on spacecraft
Bright stainless steel0.10 – 0.20Low emitterCryogenic shields, kitchen surfaces
Oxidized / weathered metal0.6 – 0.85Emits well once dulledEngine exhausts, old radiators
Black anodized aluminum0.80 – 0.88Strong emitter, light weightElectronics heat sinks, optics housings
Matte black paint / soot0.95 – 0.98Near-blackbodyRadiator panels, solar absorbers, sensor baffles
Human skin~0.98Near-blackbody in IRWhy thermal cameras read body temperature accurately

Note that emissivity is wavelength-dependent. A selective surface exploits this: a solar collector coating can have high absorptivity (≈0.95) for the Sun's visible/near-IR spectrum yet low emissivity (≈0.1) in the long-wave IR it would otherwise re-radiate, trapping the energy. Spacecraft white paint does the opposite — low solar absorptivity, high IR emissivity — to stay cool in sunlight.

Net exchange between two surfaces

A surface doesn't just emit — it also receives radiation from everything around it. What matters for heat flow is the net exchange. For a small grey object at T₁ inside large surroundings at T₂ (the surroundings effectively act as a blackbody), the net radiated power is:

Q_net = ε · σ · A · (T₁⁴ − T₂⁴)

When both surfaces are finite and grey, the geometry enters through the view factor F₁₂ and both emissivities. For two opaque grey surfaces forming an enclosure:

           σ · (T₁⁴ − T₂⁴)
Q_net = ───────────────────────────────────────────
        (1−ε₁)/(ε₁A₁) + 1/(A₁F₁₂) + (1−ε₂)/(ε₂A₂)

The three denominator terms are radiation "resistances":
  surface resistance 1  +  space (geometric) resistance  +  surface resistance 2

This radiation-network view is powerful: you treat each emissivity term and each view-factor term as a resistor and add them in series, exactly like an electrical circuit. For two large parallel plates (A₁ = A₂ = A, F₁₂ = 1) it collapses to the form used for vacuum flasks:

         σ · A · (T₁⁴ − T₂⁴)
Q_net = ───────────────────────
          1/ε₁ + 1/ε₂ − 1

View factors

The view factor F₁₂ is the fraction of radiation leaving surface 1 that strikes surface 2 directly. It is pure geometry — it depends only on the sizes, shapes, separation and orientation of the surfaces, never on temperature or emissivity. Two rules make view-factor bookkeeping tractable:

  • Reciprocity: A₁·F₁₂ = A₂·F₂₁. A small surface facing a large one has a large view factor toward it, but the large surface sees only a small fraction back.
  • Summation: for any surface in an enclosure, the view factors to all surfaces it can see (including itself, if concave) sum to 1: ΣF₁ⱼ = 1.

Concrete cases: two infinite parallel plates have F₁₂ = 1. A small instrument package floating deep in space radiates with F ≈ 1 toward the cold sky (≈ 3 K). A pipe inside a large duct has F = 1 toward the duct, while the duct sees only a sliver of the pipe. Misjudging the view factor is one of the most common errors in radiator sizing — a panel that "sees" a hot neighbouring structure instead of cold space can lose half its rejection capacity.

Worked example: radiative cooling of a satellite panel

A flat radiator panel on a spacecraft is 1.5 m × 1.0 m (A = 1.5 m²), coated matte white with ε = 0.92, held at T₁ = 320 K, and radiates to deep space at T₂ = 4 K with view factor F ≈ 1. How much heat does it reject?

Q_net = ε · σ · A · (T₁⁴ − T₂⁴)

  ε = 0.92
  σ = 5.670×10⁻⁸ W/m²K⁴
  A = 1.5 m²
  T₁⁴ = 320⁴   = 1.049×10¹⁰ K⁴
  T₂⁴ = 4⁴     = 256 K⁴  (negligible)

Q = 0.92 × 5.670×10⁻⁸ × 1.5 × 1.049×10¹⁰
  = 0.92 × 5.670×10⁻⁸ × 1.574×10¹⁰
  = 0.92 × 892
  ≈ 821 W

The panel sheds about 821 W with no fan, no coolant, no air — pure radiation. Drop the panel temperature to 280 K and the T⁴ term falls to 6.15×10⁹, cutting rejection to ≈ 481 W: a 12.5% drop in temperature costs you 41% of your cooling. This steep penalty is exactly why spacecraft thermal engineers fight to keep radiators as hot as the payload will tolerate.

Worked example: a silvered vacuum flask

Compare the radiant heat leak through a vacuum gap between two walls, both at A = 0.05 m², inner wall T₁ = 363 K (hot coffee, 90 °C), outer wall T₂ = 293 K (20 °C). First with matte-black walls (ε = 0.95), then with silvered walls (ε = 0.04):

Q = σ·A·(T₁⁴ − T₂⁴) / (1/ε₁ + 1/ε₂ − 1)

  σ·A·(T₁⁴ − T₂⁴) = 5.670×10⁻⁸ × 0.05 × (363⁴ − 293⁴)
                   = 5.670×10⁻⁸ × 0.05 × (1.736×10¹⁰ − 7.37×10⁹)
                   = 5.670×10⁻⁸ × 0.05 × 9.99×10⁹
                   ≈ 28.3 W   (numerator)

Black walls:   1/0.95 + 1/0.95 − 1 = 1.105   →  Q ≈ 25.6 W
Silvered:      1/0.04 + 1/0.04 − 1 = 49.0    →  Q ≈ 0.58 W

Silvering the walls cuts the radiant leak from ≈25.6 W to ≈0.58 W — a 44× reduction — which is why a real thermos keeps liquid hot for hours. The vacuum already kills conduction and convection; lowering emissivity is the only lever left for the radiation path.

Radiation versus conduction and convection

ConductionConvectionRadiation
CarrierLattice / electronsMoving fluidElectromagnetic waves
Needs a medium?Yes (solid/fluid)Yes (fluid)No — works in vacuum
Governing lawFourier: q = −k∇TNewton: q = h·ΔTStefan-Boltzmann: q = εσT⁴
Temperature scaling∝ ΔT∝ ΔT (h may vary)∝ (T₁⁴ − T₂⁴)
Dominant whenSolids, small gapsFluids in motionHigh T, vacuum, large ΔT
Key material propertyThermal conductivity kHeat-transfer coeff. hEmissivity ε
Speed of actionDiffusive (slow)Bulk flowSpeed of light

At everyday temperatures around 300 K, natural-convection and radiative heat-transfer coefficients are comparable — both roughly 5–10 W/m²K — so neither dominates. The decisive crossover is temperature: because radiation scales as T⁴ while convection scales roughly as ΔT, radiation overtakes everything once surfaces glow. By 1000 K a furnace wall sheds most of its heat radiantly; in a vacuum, radiation isn't merely dominant, it's the only path.

Where radiation rules the design

  • Reentry heat shields. A capsule at Mach 25 sits in a shock layer near 10,000 K; the ablative or ceramic surface re-radiates a huge fraction of the incoming flux back out — radiation is part of the survival strategy, not just a loss.
  • Rocket nozzles and afterburners. Walls run at 1000–1800 K, where radiation is the leading loss; nozzle extensions are often "radiatively cooled" — designed to glow and dump heat to space rather than carry coolant.
  • Spacecraft thermal control. With no atmosphere, every watt must leave by radiation. Engineers tune emissivity with coatings and stack reflective multi-layer insulation (MLI) to throttle it.
  • Furnaces and kilns. Above ~700 °C the load is heated mostly by radiation from the walls and flame, and view factors decide which parts of the charge heat fastest.
  • Electronics and LEDs. Black-anodized heat sinks add a radiative path on top of convection; in still air, radiation can carry 20–40% of the total from a finned sink.
  • Building energy. Low-emissivity (low-e) window coatings reflect long-wave IR back into a room in winter and out in summer, cutting radiative loss through glass.

Failure modes and design traps

  • Designing in °C instead of K. The T⁴ law only works in absolute temperature. Plugging in Celsius is the classic beginner error and can be wrong by orders of magnitude.
  • Ignoring the surroundings' temperature. A surface emits Q = εσAT₁⁴ but also absorbs from its surroundings; only the net (T₁⁴ − T₂⁴) matters. Forgetting the second term overestimates cooling when surroundings are warm.
  • Emissivity drift in service. A bright surface that oxidizes, gets contaminated, or accumulates micrometeoroid pitting can see its emissivity climb from 0.1 to 0.6 over a mission, wrecking the original thermal balance — radiator and shield coatings are chosen for end-of-life ε, not pristine ε.
  • View-factor blunders. Pointing a radiator where it "sees" a hot adjacent structure, the Sun, or a planet instead of cold space slashes net rejection; this is a frequent cause of spacecraft overheating.
  • Forgetting the selective-surface trade. Solar absorptivity and IR emissivity are different numbers. A coating chosen to absorb sunlight will also be a strong IR emitter unless engineered to be spectrally selective.
  • Assuming radiation is negligible at "low" temperature. In a vacuum or a still, evacuated gap, radiation may be small in absolute terms but it is the only leak — and over weeks it dominates a cryostat's heat budget.

Frequently asked questions

What is radiation heat transfer?

Radiation heat transfer is the movement of thermal energy by electromagnetic waves — mostly infrared light for everyday temperatures. Unlike conduction and convection, it needs no medium: it crosses a vacuum at the speed of light, which is why sunlight heats the Earth across 150 million km of empty space. Every object above absolute zero radiates, and a surface's emitted power follows the Stefan-Boltzmann law, Q = εσAT⁴, scaling with the fourth power of absolute temperature.

What is the Stefan-Boltzmann law?

The Stefan-Boltzmann law states that the total power radiated per unit area by a blackbody is E = σT⁴, where σ = 5.670×10⁻⁸ W/m²K⁴ and T is absolute temperature in kelvin. For a real surface you multiply by emissivity ε (0 to 1), giving E = εσT⁴. The defining feature is the fourth-power dependence: double the absolute temperature and you radiate 2⁴ = 16 times more power. This is why glowing-hot surfaces dump heat so aggressively while cool surfaces barely radiate.

What is emissivity and why does it matter?

Emissivity ε is the ratio of a real surface's radiated power to that of an ideal blackbody at the same temperature, ranging from 0 (perfect reflector) to 1 (perfect emitter). Polished aluminum has ε ≈ 0.04, black anodized aluminum ε ≈ 0.8, oxidized steel ε ≈ 0.8, and matte black paint ε ≈ 0.95. By Kirchhoff's law a good emitter is also a good absorber at the same wavelength, so emissivity is the single dial engineers turn to make a surface shed heat (high ε) or hide from it (low ε, like the multi-layer insulation on spacecraft).

What is a view factor?

A view factor F₁₂ is the fraction of radiation leaving surface 1 that lands directly on surface 2 — a purely geometric number between 0 and 1 set by the sizes, shapes, orientation and separation of the surfaces. Two parallel plates close together have F ≈ 1; a small object in a huge room has F ≈ 1 toward the room but the room sees almost none of it. View factors obey reciprocity (A₁F₁₂ = A₂F₂₁) and summation (the view factors from any surface to all surfaces it sees sum to 1). They turn the surface temperatures and emissivities into an actual net heat rate.

Why does radiation dominate at high temperatures?

Conduction and convection scale roughly linearly with temperature difference (Q ∝ ΔT), but radiation scales with the difference of fourth powers, Q ∝ (T₁⁴ − T₂⁴). At room temperature radiation and natural convection are comparable, but by 1000 K the T⁴ term has exploded — a furnace wall, a rocket nozzle, or a reentry heat shield loses most of its heat by radiation. Below a few hundred kelvin radiation becomes weak, which is why cryogenic systems fight it with reflective shields rather than insulation alone.

How does a thermos flask use radiation physics?

A vacuum flask blocks all three heat paths at once. The double wall with vacuum between kills conduction and convection because there is no medium to carry heat. The remaining path is radiation across the gap, so the walls are silvered to drive emissivity down to ε ≈ 0.02–0.05. With both walls reflective, the net radiant flux Q = σ(T₁⁴ − T₂⁴) / (1/ε₁ + 1/ε₂ − 1) is cut by a factor of roughly 20–40 compared with black walls, which is why coffee stays hot for hours.