In Planck and Blackbody Radiation you saw why quantized energies give the blackbody spectrum. Astrophysicists use the result as a working tool. It tells a star's temperature from its color, its power from its size, and it describes the oldest light in the universe.
Key idea
Where the peak comes from
Why it works
Where σT⁴ comes from
Why it works
Worked examples
Worked example: The Sun's peak
- $\lambda_{\max} = (2.898 \times 10^{-3}\text{ m·K})/(5772\text{ K})$.
- $= 5.02 \times 10^{-7}$ m.
Answer: About 502 nm, blue-green light. (Plotted per unit frequency instead, the peak lands elsewhere, so "the Sun's peak color" depends on how you plot it.)
Worked example: Hotter is brighter at every wavelength
- The factor $2hc^2/\lambda^5$ cancels in the ratio; only $1/(e^x - 1)$ changes.
- $$x_{4000} = \frac{1.4388 \times 10^{-2}}{(5.00 \times 10^{-7})(4000)} = 7.194,$$ and half that at 8,000 K: $x_{8000} = 3.597$.
- Ratio $= (e^{7.194} - 1)/(e^{3.597} - 1) = 1330/35.5 \approx 37.5$.
Answer: Doubling the temperature raises the 500 nm output about 37 times, far more than 2 times.
Worked example: The long-wavelength limit
- Now $$x_{4000} = \frac{1.4388 \times 10^{-2}}{(0.01)(4000)} = 3.6 \times 10^{-4},$$ which is tiny.
- For small $x$, $e^x - 1 \approx x$, so $B_\lambda \approx 2ckT/\lambda^4$ (the Rayleigh–Jeans law), proportional to $T$.
Answer: The ratio is $2.00$: at long wavelengths the hotter body is brighter only in proportion to its temperature.
Common mistake