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

From JETohlineWiki
Jump to navigation Jump to search
Joel2 (talk | contribs)
No edit summary
Joel2 (talk | contribs)
Line 26: Line 26:
{{ Math/EQ_RadialPulsation02 }}
{{ Math/EQ_RadialPulsation02 }}
</div>
</div>
 
Motivated by [[SSC/Stability/Isothermal#Yabushita_(1968)|the derivation presented by]]  {{ Yabushita68full }}, let's now insert an integration constant, <math>C_0</math>, into this 2<sup>nd</sup>-order ODE to obtain what we henceforth will refer to as the,
Let's now insert an additive constant, <math>C_0</math>, to this 2<sup>nd</sup>-order ODE as follows:
<table border=0 cellpadding=2 align="center">
<table border=0 cellpadding=2 align="center">
<tr>
<tr>
<td align="right">
<td align="center" colspan="1">
[[Image:LSUkey.png|25px|link=Appendix/EquationTemplates#Stability:_Radial_Pulsation]]
<font color="maroon"><b>Yabushita68-Motivated Polytropic LAWE</b></font><br />
</td>  
</td>
</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\xi^2} + \biggl[ 4 - (n+1) Q \biggr] \frac{1}{\xi} \cdot \frac{dx}{d\xi}   
Line 38: Line 38:
- \alpha Q\biggr]  \frac{x}{\xi^2} </math>
- \alpha Q\biggr]  \frac{x}{\xi^2} </math>
</td>
</td>
</tr>
<tr>
  <td align="center" colspan="2">
where:&nbsp; &nbsp; <math>Q(\xi) \equiv - \frac{d\ln\theta}{d\ln\xi} \, ,</math> &nbsp;&nbsp; <math>\sigma_c^2 \equiv \frac{3\omega^2}{2\pi G\rho_c} \, ,</math> &nbsp; &nbsp; and, &nbsp; &nbsp; <math>\alpha \equiv \biggl(3 - \frac{4}{\gamma_\mathrm{g}}\biggr)</math>
  </td>
</tr>
</tr>
</table>
</table>

Revision as of 13:26, 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=d2xdξ2+[4(n+1)Q]1ξdxdξ+(n+1)[(σc26γg)ξ2θαQ]xξ2

Related Discussions

Tiled Menu

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