a) How does flux, F, depend on luminosity, L, and distance, r?
Since the luminosity remains constant, the flux must decrease as the light spreads out from the Sun in a sphere (essentially the photons are spreading out as they move away from the Sun). The relation, then, is just the luminosity divided by the surface area of the expanding sphere: F=L4πr2
b) The Solar flux at the Earth-Sun distance has been measured to high precision, and for the purposes of this exercise is given by F⊕=1.4×106ergscm2s. Given that the Sun's angular diameter is θ=0.57∘, what is the effective temperature of the Sun?
Since the luminosity remains constant, we can set the luminosities at the two distances equal. This means:
4πR2⊙F⊙=4πa2F⊕, where R⊙ is the radius of the Sun and a is 1AU, or the distance from the Earth to the Sun (1.5×1013cm).
R2⊙F⊙=a2F⊕
F⊙=a2F⊕R2⊙
Now that we've figured out what the flux at the surface of the Sun should be, we can use that to find the temperature using F=σT4, where σ=5.7×10−5ergcm2sK4, the Stefan-Boltzmann constant.
T=(F⊙σ)1/4
T=(a2F⊕R2⊙σ)1/4
We have a and F⊕, but we need to find R⊙. We can do this based on the angular diameter of the Sun, using trig:
R⊙=7.46×1010cm
Finally, we can plug all the values in and solve to get a final answer T≈5600K.
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