SSC/Stability/BiPolytropes/Pt3: Difference between revisions

From JETohlineWiki
Jump to navigation Jump to search
Joel2 (talk | contribs)
Joel2 (talk | contribs)
 
(10 intermediate revisions by the same user not shown)
Line 122: Line 122:


Hence, multiplying the LAWE through by <math>~(K_c/G)\rho_c^{-4 / 5}</math> gives,
Hence, multiplying the LAWE through by <math>~(K_c/G)\rho_c^{-4 / 5}</math> gives,
<table border="0" cellpadding="5" align="center">
<tr>
  <td align="right">
<math>~0</math>
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>~
\frac{d^2x}{dr_0^2} + \biggl[\frac{4}{r_0} - \biggl(\frac{g_0 \rho_0}{P_0}\biggr) \biggr] \frac{dx}{dr_0}
+ \biggl(\frac{\rho_0}{\gamma_\mathrm{g} P_0} \biggr)\biggl[\omega^2 + (4 - 3\gamma_\mathrm{g})\frac{g_0}{r_0} \biggr]  x
</math>
  </td>
</tr>
</table>


<table border="0" cellpadding="5" align="center">
<table border="0" cellpadding="5" align="center">
Line 1,712: Line 1,692:
   <td align="left">
   <td align="left">
<math>~- \frac{2\xi^2}{15} \biggl[ \frac{(15 - \xi^2)}{15} \biggr]^{-1} = - \frac{2\xi^2}{(15 - \xi^2)}  \, .</math>
<math>~- \frac{2\xi^2}{15} \biggl[ \frac{(15 - \xi^2)}{15} \biggr]^{-1} = - \frac{2\xi^2}{(15 - \xi^2)}  \, .</math>
  </td>
</tr>
</table>
From a  numerical integration of the model for which <math>\mu_e/\mu_c =1</math>, we have found that,
<math>~[ ~\xi_i = 1.6686460157,~x_i = +0.81437470~]</math>, which is consistent with the parabolic expression if we set, <math>x_0 = 1</math>. Also, from the parabolic expression, we deduce that <math>[d\ln x/d\ln\xi]_\mathrm{core} = - 0.455872</math>, which matches the numerically determined logarithmic slope.
<table border="1" align="center" width="80%" cellpadding="5"><tr><td align="left">
<table border="0" align="left" width="25%" cellpadding="20">
<tr><td align="center">
[[File:Mod0MuRatio100.png|250px|Example eigenvector]]
</td></tr>
</table>
Also note: &nbsp; From [[SSC/Stability/BiPolytropes/Pt3#Equilibrium_Properties_of_Marginally_Unstable_Models|Table 2, above]], we see that <math>R^*_\mathrm{surf} = 2.139737</math>; and from a [[SSC/Structure/BiPolytropes/Analytic51/Pt2#Parameter_Values|separate Table 1]], <math>r^*_\mathrm{core} = (3/2\pi)^{1 / 2} \xi_i = 1.153015</math>.  This means that, <math>q \equiv r^*_\mathrm{core}/R^*_\mathrm{surf} = 0.538858</math>.
</td></tr></table>
Next, following the [[#Interface|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,
<table border="0" cellpadding="5" align="center">
<tr>
  <td align="right">
<math>~
\biggl\{ \frac{d\ln x}{d\ln r}\biggr|_i \biggr\}_\mathrm{env}
=
\biggl\{ \frac{d\ln x}{d\ln \eta}\biggr|_i \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|_i \biggr\}_\mathrm{core} </math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>~3\biggl(\frac{3}{5}  -1\biggr) + \frac{3}{5} \biggl\{  - \frac{2\xi^2}{(15 - \xi^2)} \biggr\}_\mathrm{core} </math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>~- \frac{6}{5} + \frac{6}{5} \biggl[  - \frac{\xi^2}{(15 - \xi^2)} \biggr\}_\mathrm{core} </math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>-\frac{6}{5}\biggl[  1 +  \frac{\xi^2}{(15 - \xi^2)} \biggr]\biggr\} </math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">
<math>~=</math>
  </td>
  <td align="left">
<math>-\biggl[ \frac{18}{(15 - \xi^2)} \biggr]  = - 1.473523</math>&nbsp; &nbsp; <font color="red"><b>Yes!</b></font>
   </td>
   </td>
</tr>
</tr>

Latest revision as of 13:29, 19 January 2026

Radial Oscillations of (nc, ne) = (5, 1) Models[edit]


Part I:   The Search
 

Part II:  Review of MF85b
 

III:  (5,1) Radial Oscillations
 

IV:  Reconciliation
 

    These four chapters, labeled Parts I - IV, are segments of the much longer chapter titled, SSC/Stability/BiPolytropes/PlannedApproach. An accompanying organizational index has helped us write this chapter succinctly.

Foundation[edit]

In an accompanying discussion, we derived the so-called,

Adiabatic Wave (or Radial Pulsation) Equation

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

whose solution gives eigenfunctions that describe various radial modes of oscillation in spherically symmetric, self-gravitating fluid configurations. Assuming that the underlying equilibrium structure is that of a bipolytrope having (nc,ne)=(5,1), it makes sense to adopt the normalizations used when defining the equilibrium structure, namely,

ρ*

ρ0ρc

;    

r*

r0[Kc1/2/(G1/2ρc2/5)]

P*

P0Kcρc6/5

;    

Mr*

Mr[Kc3/2/(G3/2ρc1/5)]

We note as well that,

g0

=

GM(r0)r02

 

=

G[Mr*ρc1/5(KcG)3/2][r*ρc2/5(KcG)1/2]2

 

=

GMr*(r*)2[ρc3/5(KcG)1/2].

Hence, multiplying the LAWE through by (Kc/G)ρc4/5 gives,

0

=

d2xdr*2+[4r*ρc2/5(KcG)1/2(g0ρ0P0)]dxdr*+ρc4/5(KcG)(ρ0γgP0)[ω2+(43γg)g0r0]x

 

=

d2xdr*2+{4r*ρc2/5(KcG)1/2GMr*(r*)2[ρc3/5(KcG)1/2][ρcρ*P*Kcρc6/5]}dxdr*+ρc4/5(KcG)[ρcρ*γgP*Kcρc6/5]{ω2+(43γg)GMr*(r*)2[ρc3/5(KcG)1/2]ρc2/5r*(GKc)1/2}x

 

=

d2xdr*2+{4r*Mr*(r*)2[ρ*P*]}dxdr*+(1Gρc)[ρ*γgP*]{ω2+(43γg)GρcMr*(r*)3}x

 

=

d2xdr*2+{4r*(ρ*P*)Mr*(r*)2}dxdr*+(ρ*P*){ω2γgGρc+(4γg3)Mr*(r*)3}x

 

=

d2xdr*2+{4(ρ*P*)Mr*(r*)}1r*dxdr*+(ρ*P*){2πσc23γgαgMr*(r*)3}x.

Profile[edit]

Now, referencing the derived bipolytropic model profile, we should incorporate the following relations:


Table 1: Radial Profile of Various Physical Variables

Variable

Throughout the Core
0ξξi

Throughout the Envelope
ηiηηs

Plotted Profiles

ξi=0.5

ξi=1.0

ξi=3.0

r*

(32π)1/2ξ

(μeμc)1θi2(2π)1/2η

 

ρ*

(1+13ξ2)5/2

(μeμc)θi5ϕ(η)

P*

(1+13ξ2)3

θi6[ϕ(η)]2

Mr*

(23π)1/2[ξ3(1+13ξ2)3/2]

(μeμc)2θi1(2π)1/2(η2dϕdη)

In order to obtain the various envelope profiles, it is necessary to evaluate ϕ(η) and its first derivative using the information presented in Step 6, above.


Therefore, throughout the core we have,

ρ*P*

=

(1+13ξ2)1/2;

Mr*r*

=

(23π)1/2[ξ3(1+13ξ2)3/2](2π3)1/21ξ=2ξ2(1+13ξ2)3/2;

and, throughout the envelope we have,

ρ*P*

=

(μeμc)θi1ϕ(η)1;

Mr*r*

=

(μeμc)2θi1(2π)1/2(η2dϕdη)[(μeμc)1θi2(2π)1/2η]1=2(μeμc)1θiη(η2dϕdη).

NOTE on 15 May 2019:  Prior to this date the last RHS expression had an incorrect exponent on η. It previously (incorrectly) read,

Mr*r*

=

2(μeμc)1θiη(η2dϕdη).

Numerical Integration[edit]

General Approach[edit]

Here, we begin by recognizing that the 2nd-order ODE that must be integrated to obtain the desired eigenvectors has the generic form,

0

=

x+r*x+𝒦x,

where,

x

=

dxdr*

      and      

x

=

d2xd(r*)2.

Adopting the same approach as before when we integrated the LAWE for pressure-truncated polytropes, we will enlist the finite-difference approximations,

x

x+x2δr*

      and      

x

x+2xj+x(δr*)2.

The finite-difference representation of the LAWE is, therefore,

x+2xj+x(δr*)2

=

r*[x+x2δr*]𝒦xj

x+2xj+x

=

δr*2r*[x+x](δr*)2𝒦xj

xj+1[1+(δr*2r*)]

=

[2(δr*)2𝒦]xj[1(δr*2r*)]xj1.

In what follows we will also find it useful to rewrite 𝒦 in the form,

𝒦(σc2γg)𝒦1αg𝒦2.

The relevant coefficient expressions for all regions of the configuration are,

{4(ρ*P*)Mr*(r*)}

      ,      

𝒦1

2π3(ρ*P*)

      and      

𝒦2

(ρ*P*)Mr*(r*)3.

Special Handling at the Center[edit]

In order to kick-start the integration, we set the displacement function value to x1=1 at the center of the configuration (ξ1=0), then draw on the derived power-series expression to determine the value of the displacement function at the first radial grid line, ξ2=δξ, away from the center. Specifically, we set,

x2

=

x1[1(n+1)𝔉(δξ)260]n=5=x1[1𝔉(δξ)210].

Special Handling at the Interface[edit]

Integrating outward from the center, the general approach will work up through the determination of xj+1 when "j+1" refers to the interface location. In order to properly transition from the core to the envelope, we need to determine the value of the slope at this interface location. Let's do this by setting j = i, then projecting forward to what x+ would be — that is, to what the amplitude just beyond the interface would be — if the core were to be extended one more zone. Then, the slope at the interface (as viewed from the perspective of the core) will be,

x'i|core

12δr*{x+xi1}

 

=

xi12δr*+12δr*{[2(δr*)2𝒦]xi[1(δr*2r*)]xi1}[1+(δr*2r*)]1

 

=

12δr*{[2(δr*)2𝒦]xi[1(δr*2r*)]xi1[1+(δr*2r*)]xi1}[1+(δr*2r*)]1

 

=

12δr*{[2(δr*)2𝒦]xi2xi1}[1+(δr*2r*)]1

Conversely, as viewed from the envelope, if we assume that we know xi and x'i, we can determine the amplitude, xi+1, at the first zone beyond the interface as follows:

x

xi+12δr*x'i|env

xi+1[1+(δr*2r*)]

=

[2(δr*)2𝒦]xi[1(δr*2r*)][xi+12δr*x'i|env]

xi+1[1+(δr*2r*)]+[1(δr*2r*)]xi+1

=

[2(δr*)2𝒦]xi+[1(δr*2r*)]2δr*x'i|env

xi+1

=

[112(δr*)2𝒦]xi+[1(δr*2r*)]δr*x'i|env

Splitting Analysis Into Separate Core and Envelope Components[edit]

Core:[edit]

Given that, 2π/3r*=ξ, lets multiply the LAWE through by 3/(2π). This gives,

0

=

d2xdξ2+{4(ρ*P*)Mr*(r*)}1ξdxdξ+32π(ρ*P*){2πσc23γgαgMr*(r*)3}x.

Specifically for the core, therefore, the finite-difference representation of the LAWE is,

x+2xj+x(δξ)2

=

ξ[x+x2δξ][3𝒦2π]xj

x+2xj+x

=

δξ2ξ[x+x](δξ)2[3𝒦2π]xj

xj+1[1+(δξ2ξ)]

=

[2(δξ)2(3𝒦2π)]xj[1(δξ2ξ)]xj1.

This also means that, as viewed from the perspective of the core, the slope at the interface is

[dxdξ]interface

=

12δξ{[2(δξ)2(3𝒦2π)]xi2xi1}[1+(δξ2ξ)]1.

Envelope:[edit]

Given that,

(μeμc)θi2(2π)1/2r*=η,

let's multiply the LAWE through by (2π)1θi4(μe/μc)2. This gives,

0

=

d2xdη2+{4(ρ*P*)Mr*(r*)}1ηdxdη+12πθi4(μeμc)2(ρ*P*){2πσc23γgαgMr*(r*)3}x.

Specifically for the envelope, therefore, the finite-difference representation of the LAWE is,

x+2xj+x(δη)2

=

η[x+x2δη](μeμc)2[𝒦2πθi4]xj

x+2xj+x

=

δη2η[x+x](δη)2(μeμc)2[𝒦2πθi4]xj

xj+1[1+(δη2η)]

=

[2(δη)2(μeμc)2(𝒦2πθi4)]xj[1(δη2η)]xj1.

This also means that, once we know the slope at the interface (see immediately below), the amplitude at the first zone outside of the interface will be given by the expression,

xi+1

=

[112(δη)2(μeμc)2(𝒦2πθi4)]xi+[1(δη2η)]δη[dxdη]interface.

Interface[edit]

If we consider only cases where γe=γc, then at the interface we expect,

dlnxdlnr*

=

dlnxdlnξ=dlnxdlnη

r*dxdr*

=

ξdxdξ=ηdxdη

dxdr*

=

(2π3)1/2dxdξ=(μeμc)θi2(2π)1/2dxdη.

Switching at the interface from ξ to η therefore means that,

[dxdη]interface

=

13(μeμc)1θi2[dxdξ]interface.

If, however, we want to consider values for the adiabatic index that are different in the two regions, we have to follow the above-outlined guidelines, that is,

dlnxdlnη|i

=

3(γcγe1)+γcγe(dlnxdlnξ)i

[dxdη]i

=

xiηi{3(γcγe1)+γcγeξixi[dxdξ]i}

 

=

3xiηi(γcγe1)+γcγe13(μeμc)1θi2[dxdξ]i.

Eigenvectors for Marginally Unstable Models with (γc, γe) = (6/5, 2)[edit]

We now have the tools in hand to identify the eigenvectors — that is, various radial eigenfunctions and the corresponding eigenfrequency for each — associated with various modes of oscillation in (nc,ne)=(5,1) bipolytropes. Which models should we examine?


In our accompanying review of the bipolytrope stability analysis presented by Murphy & Fiedler (1983b), our primary objective was to show that we were able to match their results quantitatively. We therefore set μe/μc = 1 — the only μ-ratio that they considered — and picked values of the core-envelope interface radius, ξi, that were listed among their set of chosen models. For a fixed value of ξi, we integrated the relevant LAWE from the center toward the surface for many different eigenfrequency (σc2) guesses until an eigenfunction was found whose behavior at the surface matched with high precision the physically justified surface boundary condition.


With the above virial stability analysis in mind (see especially Figure 3), here we have chosen to focus on models that reside along six of the equilibrium sequences that have already been analytically identified, above — specifically, the sequences for which μe/μc = 1, ½, 0.345, ⅓, 0.309, and ¼ — and to examine oscillation modes under the assumption that,

γc=(nc+1)nc=65,       and       γe=(ne+1)ne=2.

Fundamental Modes[edit]

We decided to examine, first, whether any model along each sequence marks a transition from dynamically stable to dynamically unstable configurations. We accomplished this by setting σc2 = 0, then integrating the relevant LAWE from the center toward the surface for many different guesses of the core-envelope interface radius until an eigenfunction with no radial nodes — i.e., an eigenfunction associated with the fundamental mode of radial oscillation — was found whose behavior at the surface matched with high precision the physically desired surface boundary condition. We were successful in this endeavor. A marginally unstable model was identified on each of the six separate equilibrium sequences.

Equilibrium Properties of Marginally Unstable Models[edit]

Table 2 summarizes some of the equilibrium properties of these six models. For example, the second column of the table gives the value of the core-envelope interface radius, ξi, associated with each marginally unstable model. The table also lists: the value of the model's dimensionless radius, Rsurf*, the key structural parameters, q & ν, and the central-to-mean density associated with each model; and in each case the dimensionless thermal energy (𝔰) and dimensionless gravitational potential energy (𝔴) associated, separately, with the core and the envelope. Note that, once the pair of parameters, (μe/μc,ξi), has been specified, we can legitimately assign high-precision values to all of the other model parameters because they are analytically prescribed.

Table 2: Properties of Marginally Unstable Bipolytropes Having

(nc,ne)=(5,1) and (γc,γe)=(65,2)

Determined from Integration of the LAWE

μeμc ξi Rsurf* qrcoreRsurf νMcoreMtot ρcρ¯ 𝔰core 𝔴core 𝔰env 𝔴env
1 1.6686460157 2.139737 0.53885819 0.497747626 8.51704656 3.021916335 -3.356583022 1.47780476 -5.642859167
12 2.27925811317 5.146499 0.306021732 0.401776274 63.29514949 4.241287117 -6.074241035 4.284931508 -10.97819621
0.345 2.560146865247 9.554041 0.185160563 0.234302525 209.7739052 4.639705843 -7.125754184 11.72861751 -25.61089252
13 2.582007485476 10.120558 0.176288391 0.218241608 230.4125398 4.667042505 -7.200966267 13.15887139 -28.45086152
0.309 2.6274239687695 11.464303 0.158362807 0.184796947 279.0788798 4.722277318 -7.354156963 17.1374434 -36.36528446
14 2.7357711469398 15.895632 0.118924863 0.11071211 430.0444648 4.84592201 -7.70305421 37.84289623 -77.67458196


As was expected from our above discussion of virial equilibrium conditions, we found that to high precision for each of these equilibrium models,

(𝔴core+𝔴env)+2(𝔰core+𝔰env)

=

0.

However, contrary to expectations, in no case did we find that 𝔰core/𝔰env=5. That is to say, we found that none of the models lies on the (red-dashed) curve in the qν parameter space that separates stable from unstable models as defined by our above free-energy-based stability analysis. The left-hand panel of Figure 4 shows this (red-dashed) demarcation curve; for all intents and purposes, it is a reproduction of the right-hand panel of Figure 3, above — turning-point markers have been removed to minimize clutter, the equilibrium sequences have been labeled, and the horizontal axis has been extended to unity in order to include a longer portion of the μe/μc=1 sequence. The orange triangular markers that appear in the right-hand panel of Figure 4 pinpoint where each of the Table 2 "marginally unstable" models resides in this qν plane. Clearly, all six of the orange triangles lie well off of — and to the stable side of — the red-dashed demarcation curve. This discrepancy, which has resulted from our use of two separate approaches to stability analysis, will be discussed further and gratifyingly resolved, below.

Figure 4
Marginally unstable models

Eigenfunction Details[edit]

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.


Key Reminder: We were able to find an eigenfunction whose surface boundary condition matched the desired value — in this particular case, a logarithmic slope of negative one — to this high level of precision only by iterating many times and, at each step, fine-tuning our choice of the equilibrium model's radial interface location, ξi before performing a numerical integration of the LAWE.


The discontinuous jump that occurs in the slope of the eigenfunction at the interface results from our assumption that the effective adiabatic index of material in the core (γc=6/5) is different from the effective adiabatic index of the envelope material (γe=2). In an effort to emphasize and more clearly illustrate the behavior of this fundamental-mode eigenfunction as it crosses the core/envelope interface, we have added a pair of dashed line segments to the Figure 5 plot. The red-dashed line segment touches, and is tangent to, the blue segment of the eigenfunction at the location of the core/envelope interface; it has a slope,

dxd(r/R)|i=xi(ri/R){dlnxdlnr|i}core

=

0.455872(0.814370.53885819)=0.68895.

On the other hand, the purple-dashed line segment touches, and is tangent to, the green segment of the eigenfunction at the location of the core/envelope interface; it has a slope,

dxd(r/R)|i=xi(ri/R){dlnxdlnr|i}env

=

1.47352(0.814370.53885819)=2.22691.

For comparison purposes, the eigenfunction shown in Figure 5 has been presented again in Figure 6, along with several other of our numerically derived eigenfunctions, but in Figure 6 the plotted amplitude has been renormalized to give a surface value — rather than a central value — of unity.


In Figure 6 we show the behavior of the fundamental-mode eigenfunction for each of the marginally unstable models identified in Table 2. In the top figure panel, each curve shows — on a linear-linear plot — how the amplitude varies with radius; in the bottom figure panel, the amplitude is plotted on a logarithmic scale. On each curve, the black plus sign marks the radial location of the core-envelope interface; in the bottom panel, these markers are accompanied by the values of ξi that are associated with each corresponding model (see also the second column of Table 2). Each eigenfunction has been normalized such that the surface amplitude is unity. In the top panel, the value of the central amplitude of the eigenfunction that results from this normalization is recorded near the point where each eigenfunction touches the vertical axis. (In each case, the value provided on the plot is simply the inverse of the value of xs given in Table 3, below.)

file = Dropbox/WorkFolder/Wiki edits/BiPolytrope/LinearPerturbation/FaulknerBipolytrope1.xlsx --- worksheet = Mode0Ensemble
file = Dropbox/WorkFolder/Wiki edits/BiPolytrope/LinearPerturbation/FaulknerBipolytrope1.xlsx --- worksheet = Mode0Ensemble
Figure 6: Eigenfunctions Associated with the Fundamental-Mode of Radial Oscillation

in Marginally Unstable Models having Various μe/μc

Eigenfunctions for Marginally Unstable Models

Notice that, especially as they approach the surface, the "envelope" segments of these six marginally unstable eigenfunction appear to merge into the same curve, irrespective of their value of the ratio of mean molecular weights. Note as well that the discontinuous jump that occurs in the slope of each eigenfunction at the radial location of the core/envelope interface — resulting from our choice to adopt a different adiabatic index, γg, in the core from the one in the envelope — becomes less and less noticeable for smaller and smaller values of the ratio of mean molecular weights.

Is There an Analytic Expression for the Eigenfunction?[edit]

After noticing that, in Figure 6, the envelope segments of all of the marginally unstable eigenfunctions merge into the same curve, we began to wonder whether a single expression — and, even better, an analytically defined expression — would perfectly describe the eigenfunction. We had reason to believe that this might actually be possible because, in pressure-truncated polytropic configurations, we have derived analytic expressions for the marginally unstable, fundamental-mode eigenfunctions of both n=5 and n=1 systems.

Very quickly, we convinced ourselves that a parabolic function does indeed perfectly match the "core" segment of each displayed eigenfunction. Specifically, throughout the core (0ξξi),

xP|core

1ξ215

dxPdξ|core

2ξ15

dlnxPdlnξ|core

2ξ215[(15ξ2)15]1=2ξ2(15ξ2).


The envelope segment posed a much greater challenge. In the context of our discussion of Radial Oscillations of n = 1 Polytropic Spheres, and in an accompanying Ramblings Appendix chapter we have detailed some trial derivations that are mostly blind alleyways. Twice — once in January, 2019 and again (independently) in April 2019 — we have analytically demonstrated that the following appears to work for the envelope:

Given that the Structural Properties of the envelope are described by the Lane-Emden function,

ϕ

=

a0[sin(ηb0)η]

Qdlnϕdlnη

=

[1ηcot(ηb0)],

the relevant LAWE is satisfied by the fractional displacement function,

xP

=

3c0Qη2,

where, c0 is an arbitrary scale factor.

Note that,

dxPdη

=

3c0η2[ηcot(ηb0)+ηcot2(ηb0)]6c0Qη3

dlnxPdlnη=ηxPdxPdη

=

η33c0Q{3c0η2[ηcot(ηb0)+ηcot2(ηb0)]6c0Qη3}

 

=

1Q{[η2ηcot(ηb0)+η2cot2(ηb0)]2Q}

 

=

1Q[η2(1Q)+(1Q)2]2

 

=

1Q[η2Q+Q2]2

 

=

η2Q+Q3.

But, as far as we have been able to determine (as of 16 April 2019), this analytic displacement function does not match the displacement function that has been generated through numerical integration of the LAWE (see the light-green segment of the eigenfunction displayed above in Figure 5). It remains unclear whether (a) the numerical integration is at fault, (b) we are imposing an incorrect slope at the core-envelope interface, or ( c) we are misinterpreting how to compare the two separately derived (one, numerical, and the other, analytic) envelope eigenfunctions.

Try Again (December 2025)[edit]

Don't assume the form of the displacement function throughout the envelope except: (a) Force a logarithmic slope of "minus one" at the surface; and (b) adopt a logarithmic slope at the interface that is consistent with the slope given by the core's analytic function.

ρ*

ρ0ρc

;    

r*

r0[Kc1/2/(G1/2ρc2/5)]

P*

P0Kcρc6/5

;    

Mr*

Mr[Kc3/2/(G3/2ρc1/5)]

xP|core

x0[1ξ215]

dxPdξ|core

x0[2ξ15]

dlnxPdlnξ|core

2ξ215[(15ξ2)15]1=2ξ2(15ξ2).

From a numerical integration of the model for which μe/μc=1, we have found that, [ξi=1.6686460157,xi=+0.81437470], which is consistent with the parabolic expression if we set, x0=1. Also, from the parabolic expression, we deduce that [dlnx/dlnξ]core=0.455872, which matches the numerically determined logarithmic slope.

Example eigenvector

Also note:   From Table 2, above, we see that Rsurf*=2.139737; and from a separate Table 1, rcore*=(3/2π)1/2ξi=1.153015. This means that, qrcore*/Rsurf*=0.538858.


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

 

=

3(351)+35{2ξ2(15ξ2)}core

 

=

65+65[ξ2(15ξ2)}core

 

=

65[1+ξ2(15ξ2)]}

 

=

[18(15ξ2)]=1.473523    Yes!

Other Modes[edit]

MuRatio 1.0[edit]

file = Dropbox/WorkFolder/Wiki edits/BiPolytrope/LinearPerturbation/FaulknerBipolytrope1.xlsx --- worksheet = mu100plot
file = Dropbox/WorkFolder/Wiki edits/BiPolytrope/LinearPerturbation/FaulknerBipolytrope1.xlsx --- worksheet = mu100plot
Our Determinations for Marginally Unstable Model Having μe/μc=1
 

[ξi=1.6686460157]

Mode σc2 Ω2σc22(ρcρ¯) xi dlnxdlnr*|i xsurf dlnxdlnr*|surf rR|1 1MrMtot|1 rR|2 1MrMtot|2 rR|3 1MrMtot|3
core env expected measured
1
(Fundamental)
0.00 0.00 +0.81437470 -0.455872 -1.473523 +0.3820 -1 -0.999999992 n/a n/a n/a n/a n/a n/a
2 2.51513333 10.7107538 0.20482050 -7.09124 -5.4547441 - 0.9962 4.355376917 4.35537692 0.64133 0.3502 n/a n/a n/a n/a
3 5.72371888 24.3745901 -0.14269277 +8.046019 +3.627611 +0.9308 11.18729505 11.18729506 0.4837 0.5864 0.842 0.0854 n/a n/a
4 10.3458476 44.0622916 -0.20845197 -0.6949966 -1.61699793 -1.1443 21.03114578 21.03114577 0.3939 0.7154 0.6902 0.2777 0.9115 0.0284

Our determination of eigenvector for mu_ratio = 1  Our determination of multiple eigenvectors for mu_ratio = 1


MuRatio 0.310[edit]

file = Dropbox/WorkFolder/Wiki edits/BiPolytrope/TwoFirstOrderODEs/Bipolytrope51New.xlsx --- worksheet = Fun031FirstOvertone
file = Dropbox/WorkFolder/Wiki edits/BiPolytrope/TwoFirstOrderODEs/Bipolytrope51New.xlsx --- worksheet = Fun031FirstOvertone

Variation of Oscillation Frequency with ξi for μe/μc=0.310

Variation of 2 Modes

ξi Fundamental
(red)
1st Overtone
(blue)
Ω2 σc2 ρcρ¯ Ω2σc22(ρcρ¯)
1.60 3.8944 0.498473 58.398587 14.555059
2.00 3.81053 0.236047 108.69129 12.828126
2.40 2.79491 0.0870005 199.16363 8.6636677
2.609509754 0.00000 0.048214 270.5922 6.5231608
3.00 - 13.287 0.0232907 468.15 5.4517612
3.50 - 44.63801 0.0117478 902.64028 5.3020065
4.00 - 98.215 0.0064276 1656.926 5.3250395
5.00 --- 0.0022154 4900.105 5.4278831
6.00 --- 0.0008785 12544.67 5.5100707
9.014959766 --- 9.61 × 10-5 116641.6 5.6036778
12.0 --- 1.86 × 10-5 6.01 × 10+5 5.5796084

See Also[edit]

Tiled Menu

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