Planck's Law

Category: Thermal – Radiation | Revised 2026-10-01
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Planck's Law

Theory: the blackbody spectrum

Overview

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Radiation calculations often just use σT⁴. When do we need Planck's law itself?

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When material properties vary with wavelength. Glass passes visible light but blocks long infrared; paint and metal emissivities vary with wavelength; sensors and cameras see only certain bands. In these cases you need the energy split by wavelength. Let's integrate Planck's law numerically, confirm the total is σT⁴, and see where emission concentrates at familiar temperatures.

Planck's formula

$$ E_{b\lambda}(\lambda,T) = \frac{C_1}{\lambda^5\left[\exp\!\left(\dfrac{C_2}{\lambda T}\right) - 1\right]},\quad C_1 = 3.742\times10^8\ \mathrm{W\,\mu m^4/m^2},\ C_2 = 14{,}388\ \mathrm{\mu m\,K} $$

Total, peak and band fraction

$$ \int_0^\infty E_{b\lambda}\,d\lambda = \sigma T^4,\qquad \lambda_{max}T = 2{,}898\ \mathrm{\mu m\,K},\qquad F_{\lambda_1\to\lambda_2} = \frac{1}{\sigma T^4}\int_{\lambda_1}^{\lambda_2}E_{b\lambda}\,d\lambda $$

Integrated over all wavelengths it gives σT⁴; peak wavelength is inversely proportional to temperature. The band fraction F gives the share of emission within a band.

Coffee Break Trivia

The birth of the quantum

In 1900 Germany's Max Planck found a formula matching measured blackbody spectra. Deriving it required assuming energy came only in discrete multiples of hν. Planck regarded this as a mathematical device, but it became the starting point of quantum theory. Radiation thermometers that measure hot objects without contact are also based on Planck's formula.

Worked examples

Example 1: numerical integral and σT⁴

TemperatureNumerical integralσT⁴
300 K459.3 W/m²459.3 W/m²
1,000 K56.7 kW/m²56.7 kW/m²
5,800 K64.2 MW/m²64.2 MW/m²

Example 2: peak wavelength

TemperatureExamplePeak wavelength
300 KRoom-temperature object9.66 µm
1,000 KRed-hot iron2.90 µm
1,500 KNear molten steel1.93 µm
2,800 KIncandescent filament1.03 µm
5,800 KSun's surface0.50 µm

Example 3: band fractions

BandTemperatureFraction
Visible 0.38–0.78 µm2,800 K9.7%
Visible 0.38–0.78 µm5,800 K46.6%
Thermal camera 8–14 µm300 K37.6%
Glass-transmitted, below 2.7 µm5,800 K97.2%
Glass-transmitted, below 2.7 µm300 K0.002%
Above 4 µm1,000 K51.9%
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An incandescent lamp turns less than a tenth of its emission into light. And glass passing sunlight but trapping indoor heat is also about wavelength.

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At a 2,800 K filament the emission peaks at 1 µm in the near infrared, and visible wavelengths are just the tail. The sun at 5,800 K peaks mid-visible, so nearly half becomes light. Glass is the same story: 97% of sunlight lies below 2.7 µm and passes through, but room-temperature emission is almost all longer infrared, absorbed by glass and hardly escaping. That trapped heat is how a greenhouse works. Low-e window coatings exploit this by reflecting long infrared to cut heat transfer.

Use in analysis

  1. If emissivity or transmissivity varies with wavelength, compute by bands (band model).
  2. Get each band's blackbody fraction from integrals of Planck's formula (F functions).
  3. When temperatures differ greatly, as with sunlight and room-temperature emission, use at least short- and long-wave bands.
  4. For radiation thermometers and thermal cameras, use emissivity in the measured band.
  5. Gas radiation (CO₂, water vapour) occurs only at specific wavelengths, requiring spectral treatment.
Coffee Break Trivia

“A thermal camera read the metal too cold”

At a plant, a thermal camera read heated metal parts over 100 K below thermocouple values. The metal's emissivity in the long-wave 8–14 µm band was only about 0.1, while the camera remained set to 0.95. Painting a reference spot with black high-temperature paint and matching emissivity there gave correct temperatures. Without attention to spectral emissivity, radiation thermometry can be badly off.

Common mistakes

Mistakes and fixes

MistakeEffectFix
Treating glass as graySolar gain and loss wrongTwo or more bands
Ignoring spectral emissivityLarge thermometry errorsUse in-band values
Unit mix-up (µm vs m)Orders-of-magnitude errorsCheck constant units
Using °C in T⁴Large radiation errorUse kelvin
Gray gas assumptionFurnace errorsSpectral models
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