Soln. We have, for the three core parameters -
T = Tc q , q = ( r / r c )1/n And q = (P/ Pc ) (1+ 1/n)
At the interface (core-radiative boundary) one finds: q = 0. 7839768
Then, for the (dimensionless) core temperature: t c = t / q
And, since 0.6969 = t c q = t c (0.7839768) then: t c = 0.8876
The dimensional form is: T = Tc q
antilog (7.1643) = T = 1.46 x 107 K
And: Tc = T / q
For which we set up the ratio:
(0.6969)/ / (0.8876) = (1.46 x 107 )/ Tc
Whence: Tc = (1.46 x 107 ) (0.8876)/ (0.6969) = 1.86 x 107 K
Take log T = log (1.86 x 107 ) = 7.2695
Which is the core temperature log value we find at r /R = 0.0, i.e., See Table in Part 1
For core density:
q = ( r / r c )1/n
Where: The polytropic index n can be defined: n = 1/ (g - 1)
where g is the ratio of specific heats. (g = C p / C v )
In a non-relativistic limit one will have g = 5/3 and
n = 1 / (5/3 - 1) = 1/ (2/3) = 3/2
where g is the ratio of specific heats. (g = C p / C v )
In a non-relativistic limit one will have g = 5/3 and
n = 1 / (5/3 - 1) = 1/ (2/3) = 3/2
Then write the core density as: r c = r / q 3/2
Now, take q = 0.7839 SO: q 3/2 = 0.6941
Since we have, at r/R = 0.172, log r = 1.4033 then
antilog (1.4033) = r = 25.31 g/ cm3
Therefore: r c = r / q 3/2 = 25.31 g/ cm3 / 0.6941
And: r c = 36.46 g/ cm3
Now, take log (r c ) = 1.5618
Which is the density log value we find at r /R = 0.0, i.e. the core (See Table in Part 1)
For core pressure, we have: q = (P/ Pc ) (1+ 1/n)
Since: q = (p/ p c ) (1+ 1/n) and n = 1.5 (assigned polytropic index - see top of Lane-Emden function table)
Then: p c = p / q 5/2 and q 5/2 = 0.5441
Then: p c = p / q 5/2 and q 5/2 = 0.5441
And, since we have, from the model table, at r/R = 0.172, log P = 16.6770 then
antilog (16.6770 ) = P = 4.754 x 1016 dyne/ cm 2
Therefore: P c = P / q 5/2 = (4.754 x 1016 dyne/ cm2 )/ 0.5441
P c = 8.737 x 1016 dyne/ cm2
and the log is: 16.9414 or the value shown at r/R = 0.0 (the core)
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