Energy made in the core has to get out. In the Sun's inner region it travels as light, but not in a straight line: the gas is so dense that a photon is absorbed or scattered after a tiny distance, the mean free path $\ell$, and sent off again in a random direction. Building on the conditions at the center, we can estimate how long the trip takes.
Why it works
Key idea
Radiation and convection
In the Sun, energy diffuses outward by radiation from the core to about 0.7 of the radius. Farther out the gas is cooler and far more opaque, and radiation would need a very steep temperature drop to carry the energy. Instead the gas churns: hot blobs rise, cool and sink, in the convective zone, whose tops you can see as granules on the surface. Stars more massive than about 1.3 Suns have convective cores (their energy is made in a small, very hot region); stars below about 0.35 solar masses are convective all the way through.
Worked examples
Worked example: Counting steps
- $N = (D/\ell)^2 = (100\text{ cm}/1\text{ cm})^2$.
Answer: $N = 10{,}000$ steps, not 100.
Worked example: Escaping the Sun
- $t = R^2/(\ell c) = (6.96 \times 10^{8})^2/(10^{-3} \times 3.00 \times 10^{8})$.
- $t = 1.6 \times 10^{12}$ s.
Answer: About 51,000 years. With $\ell = 0.5$ mm, about 100,000 years. A straight flight would take 2.3 seconds.
Worked example: Where the mean free path comes from
- $\ell = 1/(n_e\sigma_T)$.
- $= 1/(6.65 \times 10^{1})$ m.
Answer: $\ell \approx 1.5$ cm. Deeper in, densities are higher and absorption by ions adds to the scattering, so the average step in the Sun is much shorter.
Common mistake