Appendix/Ramblings/51BiPolytropeStability/NoAnalytic: Difference between revisions

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Line 25: Line 25:
   <td align="center">1</td>
   <td align="center">1</td>
   <td align="right">1.6686460157</td>
   <td align="right">1.6686460157</td>
</tr>
<tr>
  <td align="center"><math>\tfrac{1}{2}</math></td>
  <td align="right">2.27925811317</td>
</tr>
<tr>
  <td align="center">0.345</td>
  <td align="right">2.560146865247</td>
</tr>
<tr>
  <td align="center"><math>\tfrac{1}{3}</math></td>
  <td align="right">2.582007485476</td>
</tr>
<tr>
  <td align="center">0.309</td>
  <td align="right">2.6274239687695</td>
</tr>
<tr>
  <td align="center"><math>\tfrac{1}{4}</math></td>
  <td align="right">2.7357711469398</td>
</tr>
</tr>
</table>  
</table>  

Revision as of 19:33, 19 July 2022

Do Not Confine Search to Analytic Eigenvector

Overview

STEP01:
Develop an algorithm (for Excel) that numerically integrates the LAWEs from the center to the surface of a (nc,ne)=(5,1) bipolytrope, for an arbitrary specification of the three parameters:   μe/μc,ξi, and σc2.

  • Enforce the proper interface matching condition(s) at the interface location, ξi.
  • Note that in general, for an arbitrarily chosen set of the three parameter values, the resulting surface displacement function will not match the desired boundary condition.

STEP02:
Fix your chosen value of the parameter pair, (μe/μc,ξi), and vary σc2 until the proper surface boundary condition is realized.

  • In an accompanying discussion, we claim to have identified at what point along various μe/μc sequences the fundamental mode of radial oscillation becomes unstable — that is, when σc2=0. For a given choice of μe/μc, it would be wise to begin our eigenvector search at a value of ξi that is smaller than specified in the following table:
    μeμc ξi
    1 1.6686460157
    12 2.27925811317
    0.345 2.560146865247
    13 2.582007485476
    0.309 2.6274239687695
    14 2.7357711469398

See Also

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