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Stefan-Boltzmann Radiation Calculator - Heat Transfer (Free)

A glowing furnace, the warmth of the sun, a red-hot element — all reach you through thermal radiation, no contact or air required. Unlike conduction and convection, radiation needs no medium and grows explosively with temperature: it scales with the fourth power of absolute temperature. The Stefan-Boltzmann law captures this, and this free Stefan-Boltzmann Radiation Calculator computes the radiative heat transfer from a surface to its surroundings (or between two surfaces), plus blackbody emissive power, from temperature, emissivity and area.

Stefan-Boltzmann Eq Calculator
Figure 1 Stefan-Boltzmann Eq Calculator


The Stefan-Boltzmann Radiation Calculator

Choose the case, enter temperatures (°C), emissivity and area, and get the net radiative heat plus blackbody emissive power. Temperatures are converted to kelvin internally.

☀ Stefan-Boltzmann Radiation Calculator

Radiative heat · emissive power · surface-to-surroundings or surface-to-surface
Surface → surroundings
Between two surfaces
Inputs
Two large parallel surfaces
net radiative heat
flux (W/m²)
blackbody Eₛ hot (W/m²)
hot surface (K)
σ = 5.67×10−8 W/m²K⁴. Surface→surroundings: Q = εσA(Tₛ⁴ − Tₛ₰₨⁴). Two gray parallel plates: Q = σA(T₁⁴ − T₂⁴)/(1/ε₁ + 1/ε₂ − 1). Temperatures in kelvin.
Validation note: a 1 m² surface at 500 °C radiating to 25 °C surroundings with ε = 0.9 gives Q ≈ 17,831 W, with the hot surface's blackbody emissive power ≈ 20,260 W/m². Two large parallel gray plates (ε = 0.8 each) at 500 and 25 °C exchange ≈ 13,208 W/m² — all matching standard references.

The Stefan-Boltzmann Law

Every surface above absolute zero radiates. The Stefan-Boltzmann law gives the emitted power per unit area of a real surface:

E = ε σ T⁴

and the net radiative heat exchanged with large surroundings:

Q = ε σ A (Tₛ⁴ − Tₛ₰₨⁴)

where σ = 5.67×10−8 W/m²K⁴ is the Stefan-Boltzmann constant, ε emissivity, A area, and temperatures are absolute (kelvin). Radiation is the third heat-transfer mode alongside conduction and the convection captured by our Nusselt number calculator.

Emissivity Explained

Emissivity (ε) rates how well a real surface radiates versus an ideal blackbody (ε = 1):

SurfaceEmissivity ε
Polished aluminium / silver0.02 – 0.1
Oxidised metal0.6 – 0.85
Painted / anodised surface0.8 – 0.95
Human skin, water, wood0.9 – 0.98
Perfect blackbody (ideal)1.0
Design lever: a shiny low-ε surface radiates (and absorbs) very little — the principle behind reflective insulation and radiant barriers. A dull dark surface radiates strongly — wanted in radiators, unwanted in solar-exposed tanks.

The Fourth-Power Effect

The T⁴ dependence is what makes radiation special:

double T (in K) → 16× the radiated power

This is why radiation is negligible for a warm wall but dominant in a furnace or flame. It also means you must use absolute temperature — a common and serious error is plugging in Celsius.

Surface-to-Surface Exchange

Between two large parallel gray surfaces, emissivities combine:

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

For more complex geometries you also need a view factor (how much of one surface "sees" the other). Real furnace and enclosure radiation is a major use of CFD radiation models (DO, P-1, S2S).

Radiation vs Convection

  • High temperature (furnaces, combustion, glowing metal) → radiation often dominates.
  • Vacuum / space → radiation is the only mode (no fluid for convection).
  • Near room temperature → convection usually larger, but radiation is never zero.

In building energy, radiant exchange works alongside the conduction in the U-value / R-value calculation to set total heat flow.

Worked Example

A 1 m² oxidised surface at 500 °C (773 K) radiating to a room at 25 °C (298 K), ε = 0.9:

  • Q = 0.9 × 5.67e-8 × 1 × (773⁴ − 298⁴)
  • 773⁴ = 3.57×1011; 298⁴ = 7.89×109
  • Q = 0.9 × 5.67e-8 × (3.57e11 − 0.079e11) ≈ 17,831 W

Nearly 18 kW from one square metre — the fourth-power law in action. The cool surroundings contribute little because 298⁴ « 773⁴.

Common Mistakes

  • Using Celsius instead of kelvin. The #1 radiation error — T must be absolute.
  • Forgetting the surroundings term. Net heat uses (Ts⁴ − Tsur⁴), not just Ts⁴.
  • Assuming ε = 1. Real surfaces radiate less; use the actual emissivity.
  • Ignoring view factors for surfaces that don't fully face each other.
  • Neglecting radiation at high T. Above a few hundred °C it often beats convection.

Frequently Asked Questions

What is the Stefan-Boltzmann law?

Radiated power per unit area is proportional to absolute temperature to the fourth power: E = εσT⁴. It makes hot surfaces radiate far more than warm ones.

What is the Stefan-Boltzmann constant?

σ ≈ 5.67×10−8 W/m²K⁴ — the constant linking absolute temperature to radiated power.

What is emissivity?

A 0–1 property of how well a surface radiates vs an ideal blackbody. Polished metals < 0.1; painted/oxidised surfaces > 0.8; blackbody = 1.

Why does radiation depend on temperature to the fourth power?

It comes from integrating Planck's law over all wavelengths. Doubling absolute temperature gives 16× the radiated power.

When is radiation important compared to convection?

At high temperatures (furnaces, combustion) and in vacuum/space it dominates. Near room temperature convection is usually larger, but radiation is never zero.

Conclusion

Thermal radiation is the heat-transfer mode that needs no medium and explodes with temperature: Q = εσA(Tₛ⁴ − Tₛ₰₨⁴). Remember to work in kelvin, use the real emissivity, include the surroundings, and respect the fourth-power law — and you can predict radiant heat from a hot surface or between two surfaces in seconds with the calculator above.


For more heat transfer, thermal-radiation and CFD tutorials plus free engineering calculators, explore Free CFD Tutorial. If this tool helped you, please share it with your fellow engineers and students.

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