SSC/Stability/BiPolytropes/RedGiantToPN/Pt3: Difference between revisions

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</tr>  
</tr>  
<td align="center">
<td align="center">
<math>C_0 = \frac{d^2x}{d\xi^2} + \biggl[ 4 - (n+1) Q \biggr] \frac{1}{\xi} \cdot \frac{dx}{d\xi}   
<math>C_0 = \frac{d^2x}{d\eta^2} + \biggl[ 4 - (n+1) Q \biggr] \frac{1}{\eta} \cdot \frac{dx}{d\eta}   
+ (n+1) \biggl[ \biggl( \frac{\sigma_c^2}{6\gamma_g } \biggr)  \frac{\xi^2}{\theta}  
+ (n+1) \biggl[ \biggl( \frac{\sigma_c^2}{6\gamma_g } \biggr)  \frac{\eta^2}{\theta}  
- \alpha Q\biggr]  \frac{x}{\xi^2} </math>
- \alpha Q\biggr]  \frac{x}{\eta^2} </math>
</td>
</td>
</tr>
</table>
After setting <math>\sigma_c^2 = 0</math>, let's guess an eigenfunction of the form,
<table border="0" cellpadding="5" align="center">
<tr>
  <td align="right">
<math>x</math>
  </td>
  <td align="center">
<math>=</math>
  </td>
  <td align="left">
<math>
\eta^{-m}~~~\Rightarrow ~~~ \frac{dx}{d\eta} = -m\eta^{-m-1}
</math>
&nbsp; &nbsp; &nbsp; and &nbsp; &nbsp;
<math> \frac{d^2x}{d\eta^2} = -m(-m-1)\eta^{-m-2} \, ,</math>
  </td>
</tr>
</table>
in which case we find that,
<table border="0" cellpadding="5" align="center">
<tr>
  <td align="right">
<math>C_0</math>
  </td>
  <td align="center"><math>=</math></td>
  <td align="left">
<math>
-m(-m-1)\eta^{-m-2}
+ \biggl[ 4 - (n+1) Q \biggr] \frac{1}{\eta} \biggl[ -m\eta^{-m-1} \biggr]
+ (n+1) \biggl[  - \alpha Q\biggr]  \eta^{-m - 2}
</math>
  </td>
</tr>
</table>
</tr>
</tr>
</table>
</table>

Revision as of 13:48, 6 January 2026

Main Sequence to Red Giant to Planetary Nebula (Part 3)


Part I:  Background & Objective

 


Part II: 

 


Yabushita68-Motivated Analysis

 


Part IV: 

 

Yabushita68-Motivated Analysis

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


Polytropic LAWE

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

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

Motivated by the derivation presented by 📚 S. Yabushita (1968, MNRAS, Vol. 140, pp. 109 - 120), let's now insert an integration constant, C0, into this 2nd-order ODE to obtain what we henceforth will refer to as the,

Yabushita68-Motivated Polytropic LAWE

C0=d2xdη2+[4(n+1)Q]1ηdxdη+(n+1)[(σc26γg)η2θαQ]xη2

After setting σc2=0, let's guess an eigenfunction of the form,

x

=

ηmdxdη=mηm1       and     d2xdη2=m(m1)ηm2,

in which case we find that,

C0

=

m(m1)ηm2+[4(n+1)Q]1η[mηm1]+(n+1)[αQ]ηm2

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