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

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</tr>
</tr>
</table>
</table>
===The n<sub>e</sub> = 1 Envelope===
<table border="1" cellpadding="8" width="80%" align="center"><tr><td align="left">
Let's compare this with the equivalent expression [[SSC/Stability/InstabilityOnsetOverview#Polytropic_Stability|presented separately]], namely,
<div align="center">
<font color="maroon"><b>Polytropic LAWE (linear adiabatic wave equation)</b></font><br />
{{ Math/EQ_RadialPulsation02 }}
</div>
The [[SSC/Structure/Polytropes/Analytic#n_=_5_Polytrope|equilibrium, off-center equilibrium solution]] for n = 1 polytropes states that,
<table border="0" cellpadding="5" align="center">
<tr>
  <td align="right">
<math>\phi_{n=1}</math>
  </td>
  <td align="center">
<math>=</math>
  </td>
  <td align="left">
<math>
- \frac{A}{\eta} \cdot \sin(B-\eta)
\, ;
</math>
  </td>
</tr>
<tr>
  <td align="right">
<math>\frac{d\phi}{d\eta}</math>
  </td>
  <td align="center">
<math>=</math>
  </td>
  <td align="left">
<math>
- A \frac{d}{d\eta}\biggl\{
\eta^{-1} \cdot \sin(B-\eta)
\biggr\}
</math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>=</math>
  </td>
  <td align="left">
<math>
A \biggl\{
\eta^{-2} \cdot \sin(B-\eta)
+
\eta^{-1} \cdot \cos(B-\eta)
\biggr\}
\, ;
</math>
  </td>
</tr>
<tr>
  <td align="right">
<math>\Rightarrow ~~~ Q = - \frac{\eta}{\phi}\frac{d \phi}{d\eta}</math>
  </td>
  <td align="center">
<math>=</math>
  </td>
  <td align="left">
<math>
- \eta\biggl[- \frac{A}{\eta} \cdot \sin(B-\eta) \biggr]^{-1}
A \biggl\{
\eta^{-2} \cdot \sin(B-\eta)
+
\eta^{-1} \cdot \cos(B-\eta)
\biggr\}
</math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>=</math>
  </td>
  <td align="left">
<math>
\eta\biggl[\frac{\eta}{\sin(B-\eta)} \biggr]
\biggl\{
\eta^{-2} \cdot \sin(B-\eta)
+
\eta^{-1} \cdot \cos(B-\eta)
\biggr\}
</math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>=</math>
  </td>
  <td align="left">
<math>
\biggl[\frac{1}{\sin(B-\eta)} \biggr]
\biggl\{1 + \eta \cdot \cot(B-\eta)
\biggr\}
</math>
  </td>
</tr>
</table>
Hence, the LAWE may be written as,
<table border="0" cellpadding="5" align="center">
<tr>
  <td align="right">
<math>0</math>
  </td>
  <td align="center">
<math>=</math>
  </td>
  <td align="left">
<math>
\frac{d^2x}{d\xi^2} + \biggl[4 - 6Q\biggr] \frac{1}{\xi}\cdot \frac{dx}{d\xi}
+6\biggl[\biggl(\frac{\sigma_c^2}{6\gamma_\mathrm{g}}\biggr) \frac{\xi^2}{\theta} - \biggl(3 - \frac{4}{\gamma_\mathrm{g}}\biggr) Q\biggr]\frac{x}{\xi^2}
</math>
  </td>
</tr>
</table>
</td></tr></table>


=Related Discussions=
=Related Discussions=


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Revision as of 18:24, 27 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+(43γg)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, σc23ω2/(2πGρc), we can rewrite this LAWE as,

0

=

d2xdr02+[4(g0r0ρ0r02P0)]1r0dxdr0+(ρ0r02P0)[2πGρcσc23γg(34γg)g0r0]xr02,

where, as a reminder, g0GM(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*[Kc3/2G3/2ρc1/5]r*3[Kc3/2G3/2ρc6/5]=[Gρc]Mr*r*3;

ρ0r02P0

=

ρ*ρc(r*)2[KcG1ρc4/5](P*)1[Kc1ρc6/5]=[G1ρc1]ρ*(r*)2(P*)1;

g0r0ρ0r02P0

=

[Gρc]Mr*r*3[G1ρc1]ρ*(r*)2(P*)1=Mr*ρ*P*r*.

Making these substitutions, the LAWE can be rewritten as,

0

=

d2xdr02+[4Mr*ρ*P*r*]1r0dxdr0+1Gρc[ρ*(r*)2P*][2πGρcσc23γg(34γg)GρcMr*(r*)3]xr02;

then, multiplying through by [KG1ρc4/5] allows us to everywhere switch from (r0)2 to (r*)2, namely,

0

=

d2xd(r*)2+[4Mr*ρ*P*r*]1r*dxd(r*)+[ρ*(r*)2P*][2πσc23γg(34γg)Mr*(r*)3]x(r*)2.

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

0

=

x+r*x+𝒦x,

where,

x

=

dxdr*

      and      

x

=

d2xd(r*)2;

and,

𝒦(ρ*P*)[(σc2γg)2π3(34γg)Mr*(r*)3];

and,

{4(ρ*P*)Mr*(r*)}.

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

Drawing from our "Table 2" profiles, let's evaluate 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*

=

(23π)1/2[ξ3(1+ξ23)3/2](2π3)1/2ξ1=2ξ2(1+ξ23)3/2

=

42ξ2(1+ξ23)3/2(1+ξ23)1/2=42ξ2(1+ξ23)1.

Also,

𝒦

=

(1+ξ23)1/2{(σc2γg)2π3(34γg)2ξ2(1+ξ23)3/2(2π3)ξ2}=2π3(1+ξ23)1/2{(σc2γg)2(34γg)(1+ξ23)3/2}

Hence, the LAWE becomes,

0

=

[2π3]d2xdξ2+[]2π3ξ1dxdξ+2π3(1+ξ23)1/2{(σc2γg)2(34γg)(1+ξ23)3/2}x.

Multiplying through by 3ξ2/(2π) gives,

0

=

ξ2d2xdξ2+[4ξ2ξ3(1+ξ23)1]dxdξ+ξ2(1+ξ23)1/2{(σc2γg)2(34γg)(1+ξ23)3/2}x.

Let's compare this with the equivalent expression presented separately, namely,

Polytropic LAWE (linear adiabatic wave equation)

0=d2xdξ2+[4(n+1)Q]1ξdxdξ+(n+1)[(σc26γg)ξ2θαQ]xξ2

where:    Q(ξ)dlnθdlnξ,    σc23ω22πGρc,     and,     α(34γg)

The primary E-type solution for n = 5 polytropes states that,

θn=5

=

[1+ξ23]1/2.

Q=ξθdθdξ

=

ξ[1+ξ23]1/2ddξ[1+ξ23]1/2

 

=

+ξ[1+ξ23]1/2{ξ3[1+ξ23]3/2}

 

=

ξ23[1+ξ23]1.

Hence, the LAWE may be written as,

0

=

d2xdξ2+[46Q]1ξdxdξ+6[(σc26γg)ξ2θ(34γg)Q]xξ2

 

=

d2xdξ2+{42ξ2[1+ξ23]1}1ξdxdξ+{(σc2γg)ξ2[1+ξ23]1/22ξ2(34γg)[1+ξ23]1}xξ2

 

=

d2xdξ2+{42ξ2[1+ξ23]1}1ξdxdξ+{(σc2γg)[1+ξ23]1/22(34γg)[1+ξ23]1}x

Versus above,

0

=

ξ2d2xdξ2+[4ξ2ξ3(1+ξ23)1]dxdξ+ξ2(1+ξ23)1/2{(σc2γg)2(34γg)(1+ξ23)3/2}x.

If we set γg=6/5 and we set σc2=0, this becomes,

0

=

ξ2d2xdξ2+[4ξ2ξ3(1+ξ23)1]dxdξ+23ξ2(1+ξ23)1x

Next, try the solution, x=(1ξ2/15)dx/dξ=2ξ/15 and d2x/dx2=2/15:

LAWE

=

215ξ2[4ξ2ξ3(1+ξ23)1]2ξ15+23ξ2(1+ξ23)1[1ξ2/15]

15(1+ξ23)  LAWE

=

2ξ2(1+ξ23)[60ξ(1+ξ23)30ξ3]2ξ15+10ξ2[1ξ2/15]

 

=

2ξ22ξ43[60ξ210ξ4]215+1015[15ξ2ξ4]

 

=

2ξ22ξ43[4ξ223ξ4]2+[10ξ223ξ4]

 

=

2ξ22ξ438ξ2+43ξ4+[10ξ223ξ4]

 

=

0.

The ne = 1 Envelope

Let's compare this with the equivalent expression presented separately, namely,

Polytropic LAWE (linear adiabatic wave equation)

0=d2xdξ2+[4(n+1)Q]1ξdxdξ+(n+1)[(σc26γg)ξ2θαQ]xξ2

where:    Q(ξ)dlnθdlnξ,    σc23ω22πGρc,     and,     α(34γg)

The equilibrium, off-center equilibrium solution for n = 1 polytropes states that,

ϕn=1

=

Aηsin(Bη);

dϕdη

=

Addη{η1sin(Bη)}

 

=

A{η2sin(Bη)+η1cos(Bη)};

Q=ηϕdϕdη

=

η[Aηsin(Bη)]1A{η2sin(Bη)+η1cos(Bη)}

 

=

η[ηsin(Bη)]{η2sin(Bη)+η1cos(Bη)}

 

=

[1sin(Bη)]{1+ηcot(Bη)}

Hence, the LAWE may be written as,

0

=

d2xdξ2+[46Q]1ξdxdξ+6[(σc26γg)ξ2θ(34γg)Q]xξ2

Related Discussions

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