SSC/Stability/BiPolytropes/RedGiantToPN/Pt2: Difference between revisions

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Drawing from our [[SSC/Structure/BiPolytropes/Analytic51/Pt2#Profile|"Table 2" profiles]],
 
==Specific Case of (n<sub>c</sub>, n<sub>e</sub>) = (5,1)==
Drawing from our [[SSC/Structure/BiPolytropes/Analytic51/Pt2#Profile|"Table 2" profiles]], let's evaluate <math>\mathcal{H}</math> and <math>\mathcal{K}</math> for the two separate regions of bipolytrope model.
 
===The n<sub>c</sub> = 5 Core===
<div align="center">
<math></math>
 
<math>r^*= \biggl( \frac{3}{2\pi}\biggr)^{1 / 2}\xi</math>
</div>
<table border="0" cellpadding="5" align="center">
 
<tr>
  <td align="right">
<math>\frac{\rho^*}{P^*}</math>
  </td>
  <td align="center">
<math>
=
</math>
  </td>
  <td align="left">
<math>
\biggl(1 + \frac{\xi^2}{3}\biggr)^{- 5 / 2}
\biggl(1 + \frac{\xi^2}{3}\biggr)^{6 / 2}
=
\biggl(1 + \frac{\xi^2}{3}\biggr)^{1 / 2}
</math>
  </td>
</tr>
 
<tr>
  <td align="right">
<math>\frac{M^*}{r^*}</math>
  </td>
  <td align="center">
<math>
=
</math>
  </td>
  <td align="left">
<math>
\biggl(\frac{2\cdot 3}{\pi}\biggr)^{1 / 2}
\biggl[\xi^3 \biggl(1 + \frac{\xi^2}{3}\biggr)^{- 3 / 2}\biggr]
\biggl(\frac{2\pi}{3}\biggr)^{1 / 2} \xi^{-1}
=
2\xi^2 \biggl(1 + \frac{\xi^2}{3}\biggr)^{- 3 / 2}
</math>
  </td>
</tr>
 
<tr>
  <td align="right">
<math>\Rightarrow ~~~\mathcal{H}</math>
  </td>
  <td align="center">
<math>=</math>
  </td>
  <td align="left">
<math>
4 - 2\xi^2 \biggl(1 + \frac{\xi^2}{3}\biggr)^{- 3 / 2} \biggl(1 + \frac{\xi^2}{3}\biggr)^{1 / 2}
=
4 - 2\xi^2 \biggl(1 + \frac{\xi^2}{3}\biggr)^{- 1}
\, .
</math>
  </td>
</tr>
</table>
 


=Related Discussions=
=Related Discussions=


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Revision as of 15:14, 26 December 2025

Main Sequence to Red Giant to Planetary Nebula (Part 2)


Part I:  Background & Objective

 


Part II: 

 


Part III: 

 


Part IV: 

 

Foundation

In an accompanying discussion, we derived the so-called,

Adiabatic Wave (or Radial Pulsation) Equation

d2xdr02+[4r0−(g0ρ0P0)]dxdr0+(ρ0γgP0)[ω2+(4−3γg)g0r0]x=0

whose solution gives eigenfunctions that describe various radial modes of oscillation in spherically symmetric, self-gravitating fluid configurations.

Introducing the dimensionless frequency-squared, σc2≡3ω2/(2πGρc), we can rewrite this LAWE as,

0

=

d2xdr02+[4−(g0r0⋅ρ0r02P0)]1r0⋅dxdr0+(ρ0r02P0)[2πGρcσc23γg−(3−4γg)g0r0]xr02,

where, as a reminder, g0≡GM(r0)/r02. Now, for our (nc,ne)=(5,1) bipolytrope, we have found it useful to adopt the following four dimensionless variables:

ρ*

≡

ρ0ρc

;    

r*

≡

r0[Kc1/2/(G1/2ρc2/5)]

P*

≡

P0Kcρc6/5

;    

Mr*

≡

Mr[Kc3/2/(G3/2ρc1/5)]

This means that,

g0r0=GM(r0)r03

=

GMr*[Kc3/2G−3/2ρc−1/5]r*−3[Kc−3/2G3/2ρc6/5]=[Gρc]Mr*r*−3;

ρ0r02P0

=

ρ*ρc(r*)2[KcG−1ρc−4/5](P*)−1[Kc−1ρc−6/5]=[G−1ρc−1]ρ*(r*)2(P*)−1;

g0r0⋅ρ0r02P0

=

[Gρc]Mr*r*−3⋅[G−1ρc−1]ρ*(r*)2(P*)−1=Mr*ρ*P*r*.

Making these substitutions, the LAWE can be rewritten as,

0

=

d2xdr02+[4−Mr*ρ*P*r*]1r0⋅dxdr0+1Gρc[ρ*(r*)2P*][2πGρcσc23γg−(3−4γg)GρcMr*(r*)3]xr02;

then, multiplying through by [KG−1ρc−4/5] allows us to everywhere switch from (r0)2 to (r*)2, namely,

0

=

d2xd(r*)2+[4−Mr*ρ*P*r*]1r*⋅dxd(r*)+[ρ*(r*)2P*][2πσc23γg−(3−4γg)Mr*(r*)3]x(r*)2.

In shorthand, we can rewrite this equation in the form,

0

=

x″+ℋr*x′+𝒦x,

where,

x′

=

dxdr*

      and      

x″

=

d2xd(r*)2;

and,

𝒦≡(ρ*P*)[(σc2γg)2π3−(3−4γg)Mr*(r*)3];

and,

ℋ

≡

{4−(ρ*P*)Mr*(r*)}.

Specific Case of (nc, ne) = (5,1)

Drawing from our "Table 2" profiles, let's evaluate ℋ and 𝒦 for the two separate regions of bipolytrope model.

The nc = 5 Core

r*=(32π)1/2ξ

ρ*P*

=

(1+ξ23)−5/2(1+ξ23)6/2=(1+ξ23)1/2

M*r*

=

(2⋅3π)1/2[ξ3(1+ξ23)−3/2](2π3)1/2ξ−1=2ξ2(1+ξ23)−3/2

⇒ℋ

=

4−2ξ2(1+ξ23)−3/2(1+ξ23)1/2=4−2ξ2(1+ξ23)−1.


Related Discussions

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