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

From JETohlineWiki
Jump to navigation Jump to search
Joel2 (talk | contribs)
Joel2 (talk | contribs)
Line 88: Line 88:
+ (n+1) \biggl[  - \alpha Q\biggr]  
+ (n+1) \biggl[  - \alpha Q\biggr]  
~\biggr\} \eta^{-m - 2}
~\biggr\} \eta^{-m - 2}
</math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center"><math>=</math></td>
  <td align="left">
<math>
\biggl\{~
m(m+1) -4m
+\biggl[ m(n+1) \biggr]  Q
- \biggl[  \alpha(n+1)  \biggr]Q
~\biggr\} \eta^{-m - 2}
</math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center"><math>=</math></td>
  <td align="left">
<math>
\biggl\{~
m^2 - 3m
+ (n+1)( m - \alpha )  Q
~\biggr\} \eta^{-m - 2}
\, .
</math>
</math>
   </td>
   </td>

Revision as of 13:07, 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]1ξ⋅dxdξ+(n+1)[(σc26γg)ξ2θ−αQ]xξ2

where:    Q(ξ)≡−dln⁡θdln⁡ξ,    σc2≡3ω22πGρc,     and,     α≡(3−4γg)

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]1η⋅dxdη+(n+1)[(σc26γg)η2θ−αQ]xη2

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

x

=

η−m⇒dxdη=−mη−m−1       and     d2xdη2=−m(−m−1)η−m−2,

in which case we find that,

C0

=

−m(−m−1)η−m−2+[4−(n+1)Q]1η[−mη−m−1]+(n+1)[−αQ]η−m−2

 

=

{m(m+1)−[4−(n+1)Q][m]+(n+1)[−αQ]}η−m−2

 

=

{m(m+1)−4m+[m(n+1)]Q−[α(n+1)]Q}η−m−2

 

=

{m2−3m+(n+1)(m−α)Q}η−m−2.

Related Discussions

Tiled Menu

Appendices: | VisTrailsEquations | VisTrailsVariables | References | Ramblings | VisTrailsImages | myphys.lsu | ADS |