Computing Jupiter's Thermal Time Scale

jkrivda
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1. Jupiter radiates more energy than it receives from the Sun by 8.7x10-10L0. Jupiter's radius is 7.0x109cm and its mass is 1.9x1030g. Compute its thermal time scale. Could gravitational collapse power this luminosity for Jupiter's entire lifetime of 4.5 Gyr?



2. Kelvin-Helmholtz (aka thermal) timescale equation is given by: t=ΔEg/L . ΔEg=GM2/R ... so, t=GM2/RL



3. Not sure what to sub in for "L" in the timescale equation. I'm guessing I have to use the 8.7x10-10 to figure that out. Any tips in the right direction would be greatly appreciated!
 
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L for the timescale equation is just the luminosity of Jupiter. 8.7x10-10Lo is referring to the intrinsic luminosity of Jupiter as a fraction of the solar luminosity. Astronomical units that have that subscript that looks like a dot with a circle around it are solar units.
 
so i just convert the solar luminosity fraction to erg/s and then plug and chug?
 
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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