SSC/Stability/BiPolytropes/RedGiantToPN/Pt4: Difference between revisions

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<tr>
<tr>
   <th align="center" colspan="7">
   <th align="center" colspan="7">
'''Table 2:'''  Properties of Marginally Unstable Bipolytropes Having<br /><br /><math>~(n_c, n_e) = (5, 1)</math> and <math>~(\gamma_c, \gamma_e) = (\tfrac{6}{5}, 2)</math><br /><br />Determined from Integration of the LAWE
Properties of Marginally Unstable Bipolytropes Having<br /><br /><math>~(n_c, n_e) = (5, 1)</math> and <math>~(\gamma_c, \gamma_e) = (\tfrac{6}{5}, 2)</math><br /><br />Determined from Integration of the Envelope's LAWE
   </th>
   </th>
</tr>
</tr>
Line 1,586: Line 1,586:
   <td align="right">1.66869</td>
   <td align="right">1.66869</td>
   <td align="right">0.53886</td>
   <td align="right">0.53886</td>
   <td align="right">0.0</td>
   <td align="right">0.49776</td>
   <td align="center">&#8212;</td>
   <td align="center">&#8212;</td>
   <td align="center">&#8212;</td>
   <td align="center">&#8212;</td>
   <td align="center">&#8212;</td>
   <td align="center">&#8212;</td>
</tr>
<tr>
  <td align="center">0.50</td>
  <td align="right">2.27928</td>
  <td align="right">0.30602</td>
  <td align="right">0.40178</td>
  <td align="center">&#8212;</td>
  <td align="center">&#8212;</td>
  <td align="center">&#8212;</td>
</tr>
<tr>
  <td align="center"><math>\tfrac{1}{3}</math></td>
  <td align="right">2.58201</td>
  <td align="right">0.17629</td>
  <td align="right">0.218242</td>
  <td align="center">&#8212;</td>
  <td align="center">&#8212;</td>
  <td align="center">&#8212;</td>
</tr>
</table>
==Power-Series Expression for x<sub>P</sub>==
As a [[SSC/Stability/BiPolytropes/RedGiantToPN/Pt2#Reminder|reminder]], the analytic expression for <math>x_P</math> throughout the envelope is,
<div align="center">
<table border="0" cellpadding="5" align="center">
<tr>
  <td align="center" colspan="3"><font color="maroon"><b>Precise Solution to the Polytropic LAWE</b></font></td>
</tr>
<tr>
  <td align="right">
<math>~\frac{x_P}{b}</math>
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>~\frac{(n-1)}{2n}\biggl[1 + \biggl(\frac{n-3}{n-1}\biggr) \biggl( \frac{1}{\eta \phi^{n}}\biggr) \frac{d\phi}{d\eta}\biggr]</math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>~-\biggl[ \biggl( \frac{1}{\eta \phi}\biggr) \frac{d\phi}{d\eta}\biggr]</math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>~\frac{1}{\eta^2}\biggl[ -\frac{d\ln \phi}{d\ln \eta}\biggr] </math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>~\frac{Q_1}{\eta^2} \, ,</math>
  </td>
</tr>
</table>
</div>
where,
<div align="center">
<math>~
Q_1 \equiv - \frac{d \ln \phi}{ d\ln \eta}
= \biggl[1- \eta\cot(\eta-B) \biggr] = \biggl[1 + \eta\cot(B - \eta) \biggr]\, .
</math>
</div>
Let's define <math>\epsilon \equiv (\eta_\mathrm{surf} - \eta) =  (B - \eta +  \pi )</math>, which will go to zero as <math>\eta</math> approaches the surface.  Recognizing as well that <math>\cot(\epsilon - \pi) = \cot(\epsilon)</math>, we can write,
<table border="0" cellpadding="5" align="center">
<tr>
  <td align="right">
<math>~\frac{x_P}{b}</math>
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>~\frac{1}{(B + \pi - \epsilon)^2} \biggl\{1+ (B + \pi - \epsilon)\cot(\epsilon - \pi) \biggr\}</math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>~\frac{1}{(B + \pi - \epsilon)^2} \biggl\{1+ (B + \pi - \epsilon)\cot(\epsilon ) \biggr\}</math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>
\biggl[ B + \pi - \epsilon\biggr]^{-2}
+
\biggl[ B + \pi - \epsilon\biggr]^{-1}\cot(\epsilon )
</math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>
(B+\pi)^{-2}\biggl[ 1 - \lambda\biggr]^{-2}
+
(B+\pi)^{-1}\biggl[ 1 - \lambda\biggr]^{-1}\cot(\epsilon )
\, ,
</math>
  </td>
</tr>
<tr>
  <td align="right">
<math>~(B+\pi)^{2}\cdot \frac{x_P}{b}</math>
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>
\biggl[ 1 - \lambda\biggr]^{-2}
+
(B+\pi)\biggl[ 1 - \lambda\biggr]^{-1}\cot(\epsilon )
\, ,
</math>
  </td>
</tr>
</table>
where, <math>\lambda \equiv \epsilon/(B+\pi)</math>.  Drawing from the binomial series,
<table border="0" cellpadding="5" align="center">
<tr>
  <td align="right">
<math>~(B+\pi)^{2}\cdot \frac{x_P}{b}</math>
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>
\biggl[ 1 + 2 \lambda + 3\lambda^2 + 4\lambda^3 + 5\lambda^4 + O(\lambda^5)\biggr]
+
(B+\pi)\biggl[ 1 + \lambda + \lambda^2 + \lambda^3 + \lambda^4 + \lambda^5 + \lambda^6 + O(\lambda^7)\biggr]\cdot
\biggl[\frac{1}{\epsilon} - \frac{\epsilon}{3} - \frac{\epsilon^3}{45} + O(\epsilon^5)  \biggr]
</math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>
\biggl[ 1 + 2 \lambda + 3\lambda^2 + 4\lambda^3 + 5\lambda^4 + O(\lambda^5)\biggr]
+
\frac{(B+\pi)}{\epsilon}\biggl[ 1 + \lambda + \lambda^2 + \lambda^3 + \lambda^4 + \lambda^5 + \lambda^6 + O(\lambda^7)\biggr]
</math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
&nbsp;
  </td>
  <td align="left">
<math>
+~
\frac{(B+\pi)}{\epsilon}\biggl[ 1 + \lambda + \lambda^2 + \lambda^3 + \lambda^4 + \lambda^5 + \lambda^6 + O(\lambda^7)\biggr]\cdot
\biggl[- \frac{\epsilon^2}{3} \biggr]
+~
\frac{(B+\pi)}{\epsilon}\biggl[ 1 + \lambda + \lambda^2 + \lambda^3 + \lambda^4 + \lambda^5 + \lambda^6 + O(\lambda^7)\biggr]\cdot
\biggl[- \frac{\epsilon^4}{45} \biggr]
+ O(\epsilon^5)
</math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>
\biggl[ 1 + 2 \lambda + 3\lambda^2 + 4\lambda^3 + 5\lambda^4 + O(\lambda^5)\biggr]
+
\frac{1}{\lambda}\biggl[ 1 + \lambda + \lambda^2 + \lambda^3 + \lambda^4 + \lambda^5 + \lambda^6 + O(\lambda^7)\biggr]
</math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
&nbsp;
  </td>
  <td align="left">
<math>
-~
\frac{(B+\pi)^2\lambda}{3} 
\biggl[ 1 + \lambda + \lambda^2 + \lambda^3 + \lambda^4 + \lambda^5 + \lambda^6 + O(\lambda^7)\biggr]
-~\frac{(B+\pi)^4\lambda^3}{45} 
\biggl[ 1 + \lambda + \lambda^2 + \lambda^3 + \lambda^4 + \lambda^5 + \lambda^6 + O(\lambda^7)\biggr]
+ O(\epsilon^5)
</math>
  </td>
</tr>
</table>
==Guessing Game==
===Methodical Thinking===
<ol type="A"><li>First Try
<ol>
  <li>
Pick a value of <math>r_\mathrm{norm} = r_0/r_\mathrm{surf}</math> and read off the normalized amplitude at that radial location.  For example, <math>x_\mathrm{norm} = 2.333</math> at <math>r_\mathrm{norm} = 0.500</math>.
  </li>
  <li>
The corresponding value of <math>\eta = r_\mathrm{norm}\times \eta_\mathrm{surf} = 0.500 \times 2.6243 = 1.31215</math>.
  </li>
  <li>
Notice as well that the logarithmic slope at this chosen location is (pull this from column "N" in excel "Sheet03333") - 1.52363.
  </li>
  <li>
The corresponding value of <math>\xi = (2\pi/3)^{1 / 2}\times r_\mathrm{0} = </math>
  </li>
</ol>
</li>
<li>Second Try
<ol>
  <li>Pick a value of <math>(\mu_e/\mu_c)</math>, and a value of the interface location, <math>\xi</math>; the corresponding value of <math>\eta</math> is,
<div align="center">
<math>\eta = \biggl[3^{1 / 2}\biggl(\frac{\mu_e}{\mu_c}\biggr)\theta^2  \biggr]\xi \, .</math>
</div>
  </li>
  <li>We can immediately deduce that,
<div align="center">
<math>r_0 = \biggl( \frac{3}{2\pi}\biggr)^{1 / 2} \xi = \biggl[(2\pi)^{1 / 2}\biggl(\frac{\mu_e}{\mu_c}\biggr)\theta^2 \biggr]^{-1} \eta \, ;</math>
</div>
and from [[SSC/Stability/BiPolytropes/RedGiantToPN/Pt4#Steps|an accompanying series of analytic expressions]]
<div  align="center">
<table border="1" width="80%" cellpadding="8"><tr><td align="left">
&hellip; note, in particular, that
<table border="0" align="center" cellpadding="8">
<tr>
  <td align="right"><math>\Lambda</math></td>
  <td  align="center"><math>=</math></td>
  <td align="left">
<math>\frac{1}{\eta} + \biggl(\frac{d\phi}{d\eta}\biggr)</math>
  </td>
</tr>
<tr>
  <td align="right">&nbsp;</td>
  <td  align="center"><math>=</math></td>
  <td align="left">
<math>\biggl[3^{-1 / 2}\biggl(\frac{\mu_e}{\mu_c}\biggr)^{-1}\theta^{-2}  \biggr]\cdot \frac{1}{\xi}
+ 3^{1 / 2}\theta^{-3} \biggl(\frac{d\theta}{d\xi}\biggr)</math>
  </td>
</tr>
<tr>
  <td align="right">&nbsp;</td>
  <td  align="center"><math>=</math></td>
  <td align="left">
<math>\biggl(\frac{\mu_e}{\mu_c}\biggr)^{-1}\biggl[ 1+\frac{\xi^2}{3} \biggr]  \cdot \frac{1}{3^{1 / 2}\xi}
+ 3^{1 / 2}\biggl[ 1+\frac{\xi^2}{3} \biggr]^{3/2} \biggl[- \frac{\xi}{3} \biggl(1 + \frac{\xi^2}{3}  \biggr)^{-3/2}\biggr]</math>
  </td>
</tr>
<tr>
  <td align="right">&nbsp;</td>
  <td  align="center"><math>=</math></td>
  <td align="left">
<math>\biggl(\frac{\mu_e}{\mu_c}\biggr)^{-1}\biggl[ 1+\frac{\xi^2}{3} \biggr]  \cdot \frac{1}{3^{1 / 2}\xi}  - \frac{\xi}{3^{1 / 2}} \, .</math>
  </td>
</tr>
</table>
</td></tr></table>
</div>
we also deduce that,
</div>
<div align="center">
<math>r_\mathrm{surf} = \biggl[(2\pi)^{1 / 2}\biggl(\frac{\mu_e}{\mu_c}\biggr)\theta^2 \biggr]^{-1}
\biggl[ \eta + \frac{\pi}{2} + \tan^{-1}(\Lambda)\biggr] </math>
&nbsp; &nbsp; &nbsp; <math>\Rightarrow</math> &nbsp; &nbsp; &nbsp;
<math>\frac{r_0}{r_\mathrm{surf}} =  \eta \cdot \biggl[ \eta + \frac{\pi}{2} + \tan^{-1}(\Lambda)\biggr]^{-1} \, . </math>
</div>
  </li>
</ol>
</li></ol>
===Envelope Displacement Function===
<div align="center">
<math>\xi^2 = \biggl(\frac{2\pi}{3}\biggr) r_0^2 \, .</math>
</div>
<font color="maroon">STEP 3:</font>&nbsp;&nbsp; Throughout the core &#8212; that is, at all radial positions, <math>0 \le r_0 \le (r_0)_\mathrm{int}</math> &#8212; the displacement amplitude and its first and second derivatives, respectively, are given by the expressions,
<table border="0" cellpadding="5" align="center" width="80%">
<tr>
  <td align="right">
<math>x</math>
  </td>
  <td align="center">
<math>=</math>
  </td>
  <td align="left">
<math>
\biggl[1 - \frac{r_0^2}{15a_5^2} \biggr] = \biggl[1 - \frac{\xi^2}{15} \biggr]
\, ;
</math>
  </td>
  <td align="right">(0.814374698)</td>
</tr>
<tr>
  <td align="right">
<math>\Rightarrow ~~~r_0\cdot \frac{dx}{dr_0}</math>
  </td>
  <td align="center">
<math>=</math>
  </td>
  <td align="left">
<math>
-~\frac{2r_0^2}{15a_5^2} = -~\frac{2\xi^2}{15}
\, ;
</math>
  </td>
  <td align="right">(- 0.371250604)</td>
</tr>
<tr>
  <td align="right">
<math>\Rightarrow ~~~ r_0^2 \cdot \frac{d^2x}{dr_0^2}</math>
  </td>
  <td align="center">
<math>=</math>
  </td>
  <td align="left">
<math>
-~\frac{2r_0^2}{15a_5^2} = -~\frac{2\xi^2}{15}
\, ;
</math>
  </td>
  <td align="right">(- 0.371250604)</td>
</tr>
<tr>
  <td align="right">
also &hellip; &nbsp; &nbsp;
<math>
\biggl\{ \frac{d\ln x}{d\ln \xi} \biggr\}_\mathrm{core}
=
\biggl\{ \frac{d\ln x}{d\ln r_0} \biggr\}_\mathrm{core}
= \frac{r_0}{x} \cdot \frac{dx}{dr_0}</math>
  </td>
  <td align="center">
<math>=</math>
  </td>
  <td align="left">
<math>
\biggl[\frac{15}{15 - \xi^2} \biggr] \cdot \biggl[-~\frac{2\xi^2}{15 }\biggr]
=
\biggl[\frac{2\xi^2}{\xi^2 - 15} \biggr]
</math>
  </td>
  <td align="right">(-0.455871977)<sup>&dagger;</sup></td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>=</math>
  </td>
  <td align="left">
<math>
\biggl[\frac{4\pi r_0^2/3}{2\pi r_0^2/3 - 15} \biggr]
</math>
  </td>
  <td align="right">&nbsp;</td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>=</math>
  </td>
  <td align="left">
<math>
\biggl[\frac{2r_0^2}{r_0^2 - 45/(2\pi)} \biggr]
\, .
</math>
  </td>
  <td align="right">&nbsp;</td>
</tr>
</table>
<font color="maroon">STEP #4:</font>&nbsp; &nbsp; From the determination of the logarithmic slope of the displacement function at the edge of the core &#8212; <i>i.e.,</i> at the core-envelope interface &#8212; determine the slope as viewed from the perspective of the envelope.
<table border="0" cellpadding="5" align="center" width="80%">
<tr>
  <td align="right">
<math>~
\biggl\{ \frac{d\ln x}{d\ln r_0}\biggr|_\mathrm{int} \biggr\}_\mathrm{env}
=
\biggl\{ \frac{d\ln x}{d\ln \eta}\biggr|_\mathrm{int} \biggr\}_\mathrm{env}
</math>
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>~3\biggl(\frac{\gamma_c}{\gamma_e}  -1\biggr) + \frac{\gamma_c}{\gamma_e}
\biggl\{ \frac{d\ln x}{d\ln \xi}\biggr|_\mathrm{int} \biggr\}_\mathrm{core}</math>
  </td>
  <td align="right">(-1.473523186)<sup>&dagger;</sup></td>
</tr>
<tr>
  <td align="right">
<math>\Rightarrow ~~~
\biggl\{ \frac{d\ln x}{d\ln r_0}\biggr\}_\mathrm{env}
</math>
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>~3\biggl(\frac{\gamma_c}{\gamma_e}  -1\biggr) + \frac{\gamma_c}{\gamma_e}
\biggl[\frac{2r_0^2}{r_0^2 - 45/(2\pi)} \biggr] </math>
  </td>
  <td align="right">&nbsp;</td>
</tr>
<tr>
  <td align="right">
<math>\Rightarrow ~~~
\biggl\{ \frac{dx}{x}\biggr\}_\mathrm{env}
</math>
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>~3\biggl(\frac{\gamma_c}{\gamma_e}  -1\biggr)\frac{dr_0}{r_0} + \frac{\gamma_c}{\gamma_e}
\biggl[\frac{2r_0^2}{r_0^2 - 45/(2\pi)} \biggr]\frac{dr_0}{r_0} </math>
  </td>
  <td align="right">&nbsp;</td>
</tr>
<tr>
  <td align="right">
<math>\Rightarrow ~~~
d\ln x \biggr|_\mathrm{env}
</math>
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>~3\biggl(\frac{\gamma_c}{\gamma_e}  -1\biggr)d\ln r_0 + \frac{\gamma_c}{\gamma_e}
\biggl[\frac{2r_0}{r_0^2 - 45/(2\pi)} \biggr]dr_0 </math>
  </td>
  <td align="right">&nbsp;</td>
</tr>
<tr>
  <td align="right">
<math>\Rightarrow ~~~
\ln x \biggr|_\mathrm{env}
</math>
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>
\ln r_0^{3(\gamma_c/\gamma_e - 1) }
- \frac{2\gamma_c}{\gamma_e}
\int\frac{r_0\cdot dr_0}{45/(2\pi)-r_0^2} 
</math>
  </td>
  <td align="right">&nbsp;</td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>\ln \biggl[r_0\biggr]^{3(\gamma_c/\gamma_e - 1) }
+ \frac{\gamma_c}{\gamma_e}\cdot \ln\biggl[45/(2\pi)-r_0^2 \biggr]
+ \ln \Gamma
</math>
  </td>
  <td align="right">&nbsp;</td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>\ln \biggl[r_0\biggr]^{3(\gamma_c/\gamma_e - 1) }
+ \ln\biggl[45/(2\pi)-r_0^2 \biggr]^{\gamma_c/\gamma_e}
+ \ln \Gamma
</math>
  </td>
  <td align="right">&nbsp;</td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>\ln \biggl\{~\biggl[r_0\biggr]^{3(\gamma_c/\gamma_e - 1) }
\cdot \biggl[45/(2\pi)-r_0^2 \biggr]^{\gamma_c/\gamma_e}
\cdot \Gamma~\biggr\}
</math>
  </td>
  <td align="right">&nbsp;</td>
</tr>
<tr>
  <td align="right">
<math>\Rightarrow ~~~
x \biggr|_\mathrm{env}
</math>
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>\biggl[r_0\biggr]^{3(\gamma_c/\gamma_e - 1) }
\cdot \biggl[45/(2\pi)-r_0^2 \biggr]^{\gamma_c/\gamma_e}
\cdot \Gamma
\, .
</math>
  </td>
  <td align="right">&nbsp;</td>
</tr>
</tr>
</table>
</table>

Latest revision as of 13:33, 19 February 2026

Main Sequence to Red Giant to Planetary Nebula[edit]


Part I:  Background & Objective

 


Part II: 

 


Part III: 

 


Part IV: 

 

Succinct[edit]

Generic[edit]

Adiabatic Wave (or Radial Pulsation) Equation

d2xdr02+[4r0(g0ρ0P0)]dxdr0+(ρ0γgP0)[ω2+(43γg)g0r0]x=0

may also be written as …

0

=

d2xdr*2+{4(ρ*P*)Mr*(r*)}1r*dxdr*+(ρ*P*){2πσc23γg(34γg)Mr*(r*)3}x.

In shorthand, we can rewrite this equation in the form,

0

=

x+r*x+𝒦x,

where,

x

=

dxdr*

      and      

x

=

d2xd(r*)2;

and,

𝒦(ρ*P*)[(σc2γg)2π3(34γg)Mr*(r*)3];

and,

{4(ρ*P*)Mr*(r*)}.

Specific Polytropes[edit]

In a separate discussion, we have shown that configurations with a polytropic equation of state exhibit a characteristic length scale that is given by the expression,

an

[(n+1)K4πGρc(1n)/n]1/2;

and, once the dimensionless polytropic temperature, θ(ξ), is known, the radial dependence of key physical variables is given by the expressions,

    

if, as in a separate discussion, n=5 and θ=(1+ξ2/3)1/2

r0

=

anξ,

     r0

=

[K5Gρc4/5]1/2(32π)1/2ξ,

ρ0

=

ρcθn,

     ρ0

=

ρcθ5,

P0

=

Kρ0(n+1)/n=Kρc(n+1)/nθn+1,

     P0

=

K5ρc6/5θ6,

M(r0)

=

4πρcan3(ξ2dθdξ)=ρc(3n)/(2n)[(n+1)3K34πG3]1/2(ξ2dθdξ),

     M(r0)

=

[K53G3ρc2/5]1/2(233π)1/2(ξ2dθdξ),

g0

=

GM(r0)r02=Gr02[4πan3ρc(ξ2dθdξ)],

     g0

=

{[K5Gρc4/5]1/2(32π)1/2ξ}2[6K54πGρc4/5]3/2[4πGρc](ξ2dθdξ)]

 

 

=

(23π23)[64π]3/2[GK5ρc4/5][K5Gρc4/5]3/2[Gρc](dθdξ)]

 

 

=

(233π)1/2[K5Gρc6/5]1/2(dθdξ)].

Combining variable expressions from the above right-hand column, we find that for n=5 polytropes,

g0ρ0r0P0

=

(233π)1/2[K5Gρc6/5]1/2(dθdξ)]ρcθ5[K5Gρc4/5]1/2(32π)1/2ξ[K5ρc6/5θ6]1

 

=

6(ξθdθdξ).

More generally, combining variable expressions from the above left-hand column, we find,

g0ρ0r0P0

=

Gan2ξ2[4πan3ρc(ξ2dθdξ)]ρcθnanξ[Kρc(n+1)/nθn+1]1

 

=

4πGK[ρc11/n](ξdθdξ)θ1an2

 

=

(n+1)(ξθdθdξ);

ρ0r02P0

=

ρcθn(anξ)2[Kρc(n+1)/nθn+1]1

 

=

K1ρc1/nan2ξ2θ

 

=

[(n+1)4πGρc]ξ2θ.

As a result, for polytropes we can write,

0

=

d2xdr02+[4(g0ρ0r0P0)]1r0dxdr0+(ρ0r02γgP0)[ω2+(43γg)g0r0]xr02

 

=

d2xdr02+[4(g0ρ0r0P0)]1r0dxdr0+[ω2γg(ρ0r02P0)(34γg)(g0ρ0r0P0)]xr02

 

=

d2xdr02+[4(n+1)Q]1r0dxdr0+(n+1)[ω2γg[14πGρc]ξ2θ(34γg)Q]xr02.

Finally, multiplying through by an2 — which everywhere converts r0 to ξ — gives, what we will refer to as the,

Polytropic LAWE (linear adiabatic wave equation)

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

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

BiPolytrope[edit]

Let's stick with the dimensional (r0) version and set ω2=0, in which case the Polytropic LAWE is,

0

=

d2xdr02+[4(n+1)Q]1r0dxdr0[(n+1)αQ]xr02.

Core (n = 5)[edit]

For the n=5 core, we know that θ=(1+ξ2/3)1/2. Hence,

dθdξ

=

ξ3(1+ξ23)3/2

Q5dlnθdlnξ=ξθdθdξ

=

[ξ3(1+ξ23)3/2]ξ(1+ξ23)1/2

 

=

[ξ23(1+ξ23)1]

 

=

(ξ23+ξ2).

Now, given that,

a52

=

32π[K5G1ρc4/5],

we can everywhere make the substitution,

ξ2

(r0a5)2=2π3[K51Gρc4/5]r02.

Note, also, that throughout the core, the relevant LAWE is,

0

=

d2xdr02+[46Q5]1r0dxdr0[6αQ5]xr02.

Next, try the solution,

x

=

[1r0215a52],

dxdr0

=

2r015a52,

d2xdr02

=

215a52,

in which case,

LAWE

=

d2xdr02+[46Q5]1r0dxdr0[6αQ5]xr02

 

=

215a52+[46Q5][215a52][6αQ5]1r02[1r0215a52]

 

=

215a52+[46Q5][215a52][6αQ5]1r02[15a52r0215a52]

 

=

215a52+[46Q5][215a52][6αQ5]115a52[15ξ2ξ2]

15a52×LAWE

=

10+12Q5[6αQ5][15ξ2ξ2]

 

=

10+12(ξ23+ξ2)[6α(ξ23+ξ2)][15ξ2ξ2]

 

=

10(3+ξ2)+12ξ2[6α(ξ23+ξ2)][15ξ2ξ2]

15a52(3+ξ2)×LAWE

=

30+2ξ26α(15ξ2).

Setting α=1/3 gives the desired result, namely,

LAWE

=

0.

Envelope (n = 1)[edit]

From the variable expressions in the right-hand column of Step 8 of the construction chapter,

g0ρ0r0P0=GMrr02ρ0r0P0

=

G{[K53G3ρc2/5]1/2(μeμc)2θi1(2π)1/2(η2dϕdη)}{[K5Gρc4/5]1/2(μeμc)1θi2(2π)1/2η}1{ρc(μeμc)θi5ϕ}{K5ρc6/5θi6ϕ2}1

 

=

{(μeμc)2θi1(2π)1/2(η2dϕdη)}{(μeμc)θi2(2π)1/2η1}{(μeμc)θi5ϕ}{θi6ϕ2}

 

=

2(ηϕdϕdη).

For the n=1 envelope, we know from separate work that,

ϕ

=

A[sin(ηB)η]

dϕdη

=

Aη2[ηcos(ηB)sin(ηB)]

Q1dlnϕdlnη=ηϕdϕdη

=

ηA[ηsin(ηB)]Aη2[ηcos(ηB)sin(ηB)]

 

=

[1ηcot(ηB)].

0

=

d2xdr02+[4(n+1)Q1]1r0dxdr0[(n+1)αQ1]xr02.

Numerical Integration Through Envelope[edit]

Finite-Difference Expressions[edit]

The discussion in this subsection is guided by our previous attempt at numerical integration.

Here, we focus on the LAWE that is relevant to the envelope, namely,

0

=

d2xdr02+[4(n+1)Q1]1r0dxdr0[(n+1)αQ1]xr02,

 

=

d2xdr02+[42Q1]1r0dxdr0[2Q1]xr02,

where we have plugged in the values, (n,α)=(1,1). Using the general finite-difference approach described separately, we make the substitutions,

[dxdr0]i

x+x2Δr;

      and,     

[d2xdr02]i

x+2xi+xΔr2;

which will provide an approximate expression for x+xi+1, given the values of xxi1 and xi.

A:     Pick ξint; this will give analytic expressions for ηint, B, and for ηsurf, as well as analytic expressions for (r0)int and (r0)surf.

B:     Divide the radial coordinate grid into 99 spherical shells Δr=[(r0)surf(r0)int]/99. Then tabulate 100 values of (r0)i,ηi,(Q1)i=[1ηcot(ηB)]i.

Generally speaking, after multiplying through by r02, the finite-difference representation of the envelope's LAWE takes the form,

0

=

r02[x+2xi+xΔr2]+[42Q1]r0[x+x2Δr][2Q1]xi

 

=

x+{r02Δr2+(42Q1)r02Δr}+xi{2r02Δr22Q1}+x{r02Δr2(42Q1)r02Δr}

Multiplying through by (Δr2/r02) and solving for x+ gives,

0

=

x+{1+(42Q1)Δr2r0}2xi{1+Q1(Δr2r02)}+x{1(42Q1)Δr2r0}

x+{1+(42Q1)Δr2r0}

=

2xi{1+Q1(Δr2r02)}x{1(42Q1)Δr2r0}

x+

=

{2xi[1+Q1(Δr2r02)]x[1(42Q1)Δr2r0]}[1+(42Q1)Δr2r0]1.

Now, at the interface — as viewed from the perspective of both the core and the envelope — we know the value of xi=xint, but we don't know the value of x as viewed from the envelope. However — see STEP #4 below — we know analytically the value of the first derivative at the interface as viewed from the perspective of the envelope, namely,

[dxdr0]int

=

xintr0{dlnxdlnr0|int}env

Therefore, from the above-specified finite-difference representation of the first derivative, we deduce that,

x

=

x+2Δr[dxdr0]int

Hence, at the interface — and only at the interface — the finite-difference representation of the envelope's LAWE can be written as,

0

=

x+[1+(42Q1)Δr2r0]2xi[1+Q1(Δr2r02)]+{x+2Δr[dxdr0]int}[1(42Q1)Δr2r0]

 

=

x+[1+(42Q1)Δr2r0]2xi[1+Q1(Δr2r02)]+x+[1(42Q1)Δr2r0]2Δr[dxdr0]int[1(42Q1)Δr2r0]

x+[1+(42Q1)Δr2r0]+x+[1(42Q1)Δr2r0]

=

2xi[1+Q1(Δr2r02)]+2Δr[dxdr0]int[1(42Q1)Δr2r0]

x+

=

xi[1+Q1(Δr2r02)]+Δr[dxdr0]int[1(42Q1)Δr2r0].

Steps[edit]

STEP 1:  Specify the interface location from the perspective of the core; that is, specify ξint, in which case,

(r0)int=a5ξint

=

[K5G1ρc4/5]1/2(32π)1/2ξint.

STEP 2:   Adopting the normalization ϕint=1, determine numerous additional equilibrium properties at the interface, such as …

Example numerical values inside parentheses assume (μe/μc)=1 and ξint=1.668646016
(r0)int[K51Gρc4/5]1/2=1.153014872.

θint

=

[1+ξint23]1/2;

(0.720165375)

(dθdξ)int

=

ξint3[1+ξint23]3/2;

(- 0.207749350)

ηint

=

31/2(μeμc)θint2ξint;

(1.498957494)

(dϕdη)int

=

31/2θint3(dθdξ)int;

(- 0.963393227)

Λint

=

1ηint+(dϕdη)int;

(- 0.296262902)

A

=

ηint(1+Λint2)1/2;

(1.563357124)

B

=

ηintπ2+tan1(Λint).

(- 0.359863580)

ηsurf

=

B+π.

(2.781729074)

STEP 3:   Throughout the core — that is, at all radial positions, 0r0(r0)int — the displacement amplitude and its first and second derivatives, respectively, are given by the expressions,

x

=

[1r0215a52]=[1ξ215];

(0.814374698)

r0dxdr0

=

2r0215a52=2ξ215;

(- 0.371250604)

r02d2xdr02

=

2r0215a52=2ξ215;

(- 0.371250604)

also …     {dlnxdlnξ}core={dlnxdlnr0}core=r0xdxdr0

=

[1515ξ2][2ξ215]=[2ξ2ξ215].

(-0.455871977)

STEP #4:    From the determination of the logarithmic slope of the displacement function at the edge of the core — i.e., at the core-envelope interface — determine the slope as viewed from the perspective of the envelope.

{dlnxdlnr0|int}env={dlnxdlnη|int}env

=

3(γcγe1)+γcγe{dlnxdlnξ|int}core.

(-1.473523186)

This analytically determined value matches the previous determination that was obtained via numerical integration of the LAWE.

Throughout the envelope — that is, over the range, (ηintηηsurf) — the radial coordinate, r0, is a linear function of η and takes on values given by the expression,

r0[K51Gρc4/5]1/2

=

[(μeμc)1θint2(2π)1/2]η

(0.769211186 × η)

1.153014872

r0

2.139737121.

 


From our earlier discussions,


Here we examine some of the properties of the fundamental-mode eigenfunctions that we have found are associated with marginally unstable, (nc,ne)=(5,1) bipolytropes.

Figure 5

Example eigenvector

Consider the model on the μe/μc=1 sequence for which σc2=0; key properties of this specific equilibrium model are enumerated in the first row of numbers provided in Table 2, above. Figure 5 shows how our numerically derived, fundamental-mode eigenfunction, x=δr/r0, varies with the fractional radius over the entire range, 0r/R1. By prescription, the eigenfunction has a value of unity and a slope of zero at the center (r/R=0). Integrating the LAWE outward from the center, through the model's core (blue curve segment), x drops smoothly to the value xi=0.81437 at the interface (ξi=1.6686460157q=rcore/Rsurf=0.53885819). Our numerical integration of the LAWE showed that, at the interface, the logarithmic slope of the core (blue) segment of the eigenfunction is,

{dlnxdlnr|i}core={dlnxdlnξ|i}core

=

0.455872.

Next, following the above discussion of matching conditions at the interface, we determined that, from the perspective of the envelope, the slope of the eigenfunction at the interface must therefore be,

{dlnxdlnr|i}env={dlnxdlnη|i}env

=

3(γcγe1)+γcγe{dlnxdlnξ|i}core=1.47352.

Adopting this "env" slope along with the amplitude, xi=0.81437, as the appropriate interface boundary conditions, we integrated the LAWE from the interface to the surface, obtaining the green-colored segment of the eigenfunction that is shown in Figure 5. The amplitude continued to steadily decrease, reaching a value of xs=0.38203, at the model's surface (r/R=1). At the surface, this envelope (green) segment of the eigenfunction exhibits a logarithmic slope that matches to eight significant digits the value that is expected from astrophysical arguments for this marginally unstable (σc2=0) model, namely,

dlnxdlnη|s=[(ρcρ¯)σc202γe(34γe)]=1.

Numerically Determined Marginally Unstable Models[edit]

The following table should be compared with Table 2 of an earlier attempt at identifying marginally unstable models.

Properties of Marginally Unstable Bipolytropes Having

(nc,ne)=(5,1) and (γc,γe)=(65,2)

Determined from Integration of the Envelope's LAWE

μeμc ξi qrcoreRsurf νMcoreMtot temporary 1 temporary 2 temporary 3
1.00 1.66869 0.53886 0.49776
0.50 2.27928 0.30602 0.40178
13 2.58201 0.17629 0.218242

Power-Series Expression for xP[edit]

As a reminder, the analytic expression for xP throughout the envelope is,

Precise Solution to the Polytropic LAWE

xPb

=

(n1)2n[1+(n3n1)(1ηϕn)dϕdη]

 

=

[(1ηϕ)dϕdη]

 

=

1η2[dlnϕdlnη]

 

=

Q1η2,

where,

Q1dlnϕdlnη=[1ηcot(ηB)]=[1+ηcot(Bη)].

Let's define ϵ(ηsurfη)=(Bη+π), which will go to zero as η approaches the surface. Recognizing as well that cot(ϵπ)=cot(ϵ), we can write,

xPb

=

1(B+πϵ)2{1+(B+πϵ)cot(ϵπ)}

 

=

1(B+πϵ)2{1+(B+πϵ)cot(ϵ)}

 

=

[B+πϵ]2+[B+πϵ]1cot(ϵ)

 

=

(B+π)2[1λ]2+(B+π)1[1λ]1cot(ϵ),

(B+π)2xPb

=

[1λ]2+(B+π)[1λ]1cot(ϵ),

where, λϵ/(B+π). Drawing from the binomial series,

(B+π)2xPb

=

[1+2λ+3λ2+4λ3+5λ4+O(λ5)]+(B+π)[1+λ+λ2+λ3+λ4+λ5+λ6+O(λ7)][1ϵϵ3ϵ345+O(ϵ5)]

 

=

[1+2λ+3λ2+4λ3+5λ4+O(λ5)]+(B+π)ϵ[1+λ+λ2+λ3+λ4+λ5+λ6+O(λ7)]

 

 

+(B+π)ϵ[1+λ+λ2+λ3+λ4+λ5+λ6+O(λ7)][ϵ23]+(B+π)ϵ[1+λ+λ2+λ3+λ4+λ5+λ6+O(λ7)][ϵ445]+O(ϵ5)

 

=

[1+2λ+3λ2+4λ3+5λ4+O(λ5)]+1λ[1+λ+λ2+λ3+λ4+λ5+λ6+O(λ7)]

 

 

(B+π)2λ3[1+λ+λ2+λ3+λ4+λ5+λ6+O(λ7)](B+π)4λ345[1+λ+λ2+λ3+λ4+λ5+λ6+O(λ7)]+O(ϵ5)

Guessing Game[edit]

Methodical Thinking[edit]

  1. First Try
    1. Pick a value of rnorm=r0/rsurf and read off the normalized amplitude at that radial location. For example, xnorm=2.333 at rnorm=0.500.
    2. The corresponding value of η=rnorm×ηsurf=0.500×2.6243=1.31215.
    3. Notice as well that the logarithmic slope at this chosen location is (pull this from column "N" in excel "Sheet03333") - 1.52363.
    4. The corresponding value of ξ=(2π/3)1/2×r0=
  2. Second Try
    1. Pick a value of (μe/μc), and a value of the interface location, ξ; the corresponding value of η is,

      η=[31/2(μeμc)θ2]ξ.

    2. We can immediately deduce that,

      r0=(32π)1/2ξ=[(2π)1/2(μeμc)θ2]1η;

      and from an accompanying series of analytic expressions

      … note, in particular, that

      Λ =

      1η+(dϕdη)

        =

      [31/2(μeμc)1θ2]1ξ+31/2θ3(dθdξ)

        =

      (μeμc)1[1+ξ23]131/2ξ+31/2[1+ξ23]3/2[ξ3(1+ξ23)3/2]

        =

      (μeμc)1[1+ξ23]131/2ξξ31/2.

      we also deduce that,

      rsurf=[(2π)1/2(μeμc)θ2]1[η+π2+tan1(Λ)]             r0rsurf=η[η+π2+tan1(Λ)]1.

Envelope Displacement Function[edit]

ξ2=(2π3)r02.

STEP 3:   Throughout the core — that is, at all radial positions, 0r0(r0)int — the displacement amplitude and its first and second derivatives, respectively, are given by the expressions,

x

=

[1r0215a52]=[1ξ215];

(0.814374698)

r0dxdr0

=

2r0215a52=2ξ215;

(- 0.371250604)

r02d2xdr02

=

2r0215a52=2ξ215;

(- 0.371250604)

also …     {dlnxdlnξ}core={dlnxdlnr0}core=r0xdxdr0

=

[1515ξ2][2ξ215]=[2ξ2ξ215]

(-0.455871977)

 

=

[4πr02/32πr02/315]

 

 

=

[2r02r0245/(2π)].

 

STEP #4:    From the determination of the logarithmic slope of the displacement function at the edge of the core — i.e., at the core-envelope interface — determine the slope as viewed from the perspective of the envelope.

{dlnxdlnr0|int}env={dlnxdlnη|int}env

=

3(γcγe1)+γcγe{dlnxdlnξ|int}core

(-1.473523186)

{dlnxdlnr0}env

=

3(γcγe1)+γcγe[2r02r0245/(2π)]

 

{dxx}env

=

3(γcγe1)dr0r0+γcγe[2r02r0245/(2π)]dr0r0

 

dlnx|env

=

3(γcγe1)dlnr0+γcγe[2r0r0245/(2π)]dr0

 

lnx|env

=

lnr03(γc/γe1)2γcγer0dr045/(2π)r02

 

 

=

ln[r0]3(γc/γe1)+γcγeln[45/(2π)r02]+lnΓ

 

 

=

ln[r0]3(γc/γe1)+ln[45/(2π)r02]γc/γe+lnΓ

 

 

=

ln{[r0]3(γc/γe1)[45/(2π)r02]γc/γeΓ}

 

x|env

=

[r0]3(γc/γe1)[45/(2π)r02]γc/γeΓ.

 

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