Distribution function of an ideal gas

gdumont
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Hi,

I have the following problem to solve:

Consider a planet of radius R and mass M. The plante's atmosphere is an ideal gas of N particles of mass m at temperature T. Find the equilibrium distribution function of the gas accounting for the gas itself and the gravitationnal potential of the planet.

Here are my thoughts

The equilibrium function of the gas alone is simply the Maxwell-Boltzmann distribution function f_0(\mathbf{v}), so the full distribution is just
<br /> f(\vec{v})=f_0(\vec{v})e^{-U/kT}<br />
where
<br /> U=-\frac{GMm}{r}<br />
is the gravitational potential and r is the distance from the center of the planet to the molecule of velocity \vec{v}. I'm not sure if I should replace r by r-R in U.

Can anyone confirm if I'm right or not?

Thanks
 
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The gas molecules can't penetrate into the surface of the planet, so it makes sense for your model to be described by a potential which is
<br /> U(r) = - \frac{GMm}{r} \,\,\, r &gt; R<br />
and U = \infty for r &lt; R.
 
OK, but is the distribution function OK?
 
Yes, the Maxwell-Boltzmann distribution is the correct one.
 
To solve this, I first used the units to work out that a= m* a/m, i.e. t=z/λ. This would allow you to determine the time duration within an interval section by section and then add this to the previous ones to obtain the age of the respective layer. However, this would require a constant thickness per year for each interval. However, since this is most likely not the case, my next consideration was that the age must be the integral of a 1/λ(z) function, which I cannot model.
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