424 RADIATIVE HEAT TRANSFER
16.14 Estimate the radial temperature distribution in the sun. You may make the following assumptions:
(i) The sun is a sphere of radius R;
(ii) As a result of high temperatures in the sun the absorption and scattering coefficients may be approxi-
mated to be constant, i.e., κν, βν=const ,f(ν, T,r) (free-free transitions!);
(iii) Due to high temperatures, radiation is the only mode of heat transfer;
(iv) The fusion process may be approximated by assuming that a small sphere at the center of the sun releases
heat uniformly corresponding to the total heat loss of the sun (i.e., assume the sun to be concentric spheres
with a certain heat flux at the inner boundary r=ri).
(a) Relate the heat production to the effective sun temperature TSHMeff=5777 K.
(b) Would you expect the sun to be optically thin, intermediate, or thick? Why? What are the prevailing
boundary conditions?
(c) Find an expression for the temperature distribution (for r>ri).
(d) What is the surface temperature of the sun?
Solution
(a) The total heat leaving the sun, assuming steady state, must equal the internal heat production. Since the
(b) The sun is optically very thick: Shooting a light beam of any wavelength into the sun we would hardly
expect to find a fraction exiting from the other side! Thus, the P1-approximation should do well to model the
sun. Boundary conditions: At r=rithe total amount of heat generation goes into the outer sun over an area
of 4πr2
i, or
τ=τR:−2q=−G.
where we have also scattering assumed to be isotropic. Thus, 4σT4=Gand
τ2q=const =τ2
RqR.