SSC/Stability/n1PolytropeLAWE/Pt4: Difference between revisions

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</table>
</table>


 
==Preamble Regarding Chatterji==
As far as we have been able to ascertain, the first technical examination of radial oscillation modes in <math>n=1</math> polytropes was performed &#8212; using numerical techniques &#8212; in 1951 by L. D. Chatterji; at the time, he was in the Mathematics Department of Allahabad University.  His two papers on this topic were published in, what  is now referred to as, the ''Proceedings of the Indian National Science Academy'' (PINSA).  The citations that immediately follow this opening paragraph provide inks to both of these papers by Chatterji, but the links may be insecure.  <!-- (Citations/links to articles that provide analyses of models having other polytropic indexes are provided at the [[#See_Also|bottom of this chapter]].) --> Apparently [https://www.springer.com/journal/43538 Springer] is archiving recent PINSA volumes, but their holdings do not date back as early as 1951.
As far as we have been able to ascertain, the first technical examination of radial oscillation modes in <math>n=1</math> polytropes was performed &#8212; using numerical techniques &#8212; in 1951 by L. D. Chatterji; at the time, he was in the Mathematics Department of Allahabad University.  His two papers on this topic were published in, what  is now referred to as, the ''Proceedings of the Indian National Science Academy'' (PINSA).  The citations that immediately follow this opening paragraph provide inks to both of these papers by Chatterji, but the links may be insecure.  <!-- (Citations/links to articles that provide analyses of models having other polytropic indexes are provided at the [[#See_Also|bottom of this chapter]].) --> Apparently [https://www.springer.com/journal/43538 Springer] is archiving recent PINSA volumes, but their holdings do not date back as early as 1951.


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A detailed review of {{ Chatterji51hereafter }} is provided in [[SSC/Structure/BiPolytropes/Analytic51Renormalize/Pt2#Setup|an accompanying discussion]].
A detailed review of {{ Chatterji51hereafter }} is provided in [[SSC/Structure/BiPolytropes/Analytic51Renormalize/Pt2#Setup|an accompanying discussion]].
==Establish Relevant (n=1) LAWE==
From [[SSC/Stability/n1PolytropeLAWE#WorkInProgress|a related discussion]] &#8212; or [[SSC/Stability/InstabilityOnsetOverview#Polytropic_Stability|a broader overview of Instability Onset]] &#8212; we find the
<div align="center">
<font color="maroon"><b>Polytropic LAWE (linear adiabatic wave equation)</b></font><br />
{{ Math/EQ_RadialPulsation02 }}
</div>
For an isolated n = 1 <math>(\gamma_g = 2, \alpha = 1)</math> polytrope, we know that,
<table border="0" align="center" cellpadding="5">
<tr>
  <td align="right">
<math>\theta</math>
  </td>
  <td align="center">=</td>
  <td align="left">
<math>\frac{\sin\xi}{\xi}</math>
  </td>
  <td align="right">
&nbsp; &nbsp; <math>\Rightarrow ~~~ Q(\xi) \equiv - \frac{d \ln \theta}{d\ln \xi}</math>
  </td>
  <td align="center">=</td>
  <td align="left">
<math>\biggl[1 - \xi\cot\xi\biggr] \, .</math>
  </td>
</tr>
</table>
Hence, the relevant LAWE is,
<table border="0" align="center" cellpadding="5">
<tr>
  <td align="right">
<math>0</math>
  </td>
  <td align="center">=</td>
  <td align="left">
<math>
\frac{d^2 x}{d\xi^2}
+
\biggl[4 - 2(1 - \xi\cot\xi)\biggr] \frac{1}{\xi} \cdot \frac{dx}{d\xi}
+
2 \biggl[\biggl( \frac{\sigma_c^2}{12}\biggr)\frac{\xi^3}{\sin\xi} - (1 - \xi\cot\xi)  \biggr]\frac{x}{\xi^2}
</math>
  </td>
</tr>
</table>
<div align="center">
<font color="maroon"><b>LAWE for n = 1 Polytrope</b></font><br />
<table border="0" align="center" cellpadding="5">
<tr>
  <td align="right">
<math>0</math>
  </td>
  <td align="center">=</td>
  <td align="left">
<math>
\frac{d^2 x}{d\xi^2}
+
\frac{2}{\xi} \biggl[1 +  \xi\cot\xi\biggr] \frac{dx}{d\xi}
+
\frac{1}{2} \biggl[\biggl( \frac{\sigma_c^2}{3}\biggr)\frac{\xi}{\sin\xi} - \frac{4}{\xi^2} \biggl(1 - \xi\cot\xi \biggr)  \biggr]x
</math>
  </td>
</tr>
</table>
</div>
This matches precisely the expression derived immediately above.
[[SSC/Stability/Polytropes#Boundary_Conditions|Surface boundary condition]]:
<table border="0" align="center" cellpadding="5">
<tr>
  <td align="right">
<math>- \frac{d\ln x}{d\ln \xi} \biggr|_\mathrm{surf}</math>
  </td>
  <td align="center">=</td>
  <td align="left">
<math>
\biggl( \frac{3-n}{n+1}\biggr) + \frac{n\sigma_c^2}{6(n+1)}
\biggl[ \frac{\xi}{\theta'}\biggr]_\mathrm{surf}
</math>
  </td>
</tr>
<tr>
  <td align="right">
<math>\Rightarrow ~~~ - \frac{d\ln x}{d\ln \xi} \biggr|_\mathrm{surf}</math>
  </td>
  <td align="center">=</td>
  <td align="left">
<math>
1 + \frac{\sigma_c^2}{12}
\biggl[ \frac{\xi^3}{(\xi \cos\xi - \sin\xi)}\biggr]_{\xi=\pi}
=
1 - \frac{\pi^2 \sigma_c^2}{12}
</math>
  </td>
</tr>
</table>
</td></tr></table>


=See Also=
=See Also=


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{{ SGFfooter }}

Revision as of 14:29, 15 July 2025

Radial Oscillations of n = 1 Polytropic Spheres (Pt 4)


Part I:   Search for Analytic Solutions
 

Part II:  New Ideas
 

Part III:  What About Bipolytropes?
 

Part IV:  Most General Structural Solution
 

Preamble Regarding Chatterji

As far as we have been able to ascertain, the first technical examination of radial oscillation modes in n=1 polytropes was performed — using numerical techniques — in 1951 by L. D. Chatterji; at the time, he was in the Mathematics Department of Allahabad University. His two papers on this topic were published in, what is now referred to as, the Proceedings of the Indian National Science Academy (PINSA). The citations that immediately follow this opening paragraph provide inks to both of these papers by Chatterji, but the links may be insecure. Apparently Springer is archiving recent PINSA volumes, but their holdings do not date back as early as 1951.

A detailed review of Chatterji51 is provided in an accompanying discussion.

Establish Relevant (n=1) LAWE

From a related discussion — or a broader overview of Instability Onset — we find the

Polytropic LAWE (linear adiabatic wave equation)

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)

For an isolated n = 1 (γg=2,α=1) polytrope, we know that,

θ

=

sin⁡ξξ

    ⇒Q(ξ)≡−dln⁡θdln⁡ξ

=

[1−ξcot⁡ξ].

Hence, the relevant LAWE is,

0

=

d2xdξ2+[4−2(1−ξcot⁡ξ)]1ξ⋅dxdξ+2[(σc212)ξ3sin⁡ξ−(1−ξcot⁡ξ)]xξ2

LAWE for n = 1 Polytrope

0

=

d2xdξ2+2ξ[1+ξcot⁡ξ]dxdξ+12[(σc23)ξsin⁡ξ−4ξ2(1−ξcot⁡ξ)]x

This matches precisely the expression derived immediately above.

Surface boundary condition:

−dln⁡xdln⁡ξ|surf

=

(3−nn+1)+nσc26(n+1)[ξθ′]surf

⇒−dln⁡xdln⁡ξ|surf

=

1+σc212[ξ3(ξcos⁡ξ−sin⁡ξ)]ξ=π=1−π2σc212


See Also

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