Posted by Mark on Wednesday, March 4, 2009 at 4:19am.
We don't give "detailed solutions" to long-winded problems here. Here is how to go about solving them yourself. If you want further help, show your work.
a) The ratio of the orbital distance to the distance of the star (in the same units) is the angle in radians. Convert that to degrees and then arc seconds.
b) Use Kepler's third law in the form
M = R^3/T^2
where M is the mass of Fomalhgaut in "suns", R is the orbit radius in AU and T is the period in years. In two years, the planet moves 2/T of the orbit circumference. Compute that distance (X)
c) X/(star distance) in radians
Convert that to arc seconds
d) Set the received energy from the star (one side only, using the projected area pi r^2) equal to the energy that the planet radiates away (using 4 pi r^2 for the surface area). The planet's radius, r, cancels out. So does sigma. Use the Stefan Boltzmann law for both star and planet and solve for the planet temperature. The planet's received radiated power is
4 pi*R^2(sigma)*Tstar^4 * pi r^2/(4 pi d^2) and that equals
4 pi r^2 (sigma)*Tplanet^4
(the energy raidated away by the planet).
d is the distance of the planet from the star. Solve for Tplanet
pi*(R/d)^2 *Tstar^4 = Tplanet^4
You can compare Tplanet with the freezing point of water, which is not very sensitive to the pressure. Whether it exists as a liqud or not will depend upon atmospheric pressure, which you don't know.
(e) Use the formula I just derived to compute Tstar to make Tplanet = 280 K (about the equilibrium T of earth)
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