SSC/Stability/BiPolytropes/RedGiantToPN/Pt4

From JETohlineWiki
Revision as of 19:56, 18 February 2026 by Joel2 (talk | contribs) (Guessing Game)
Jump to navigation Jump to search

Main Sequence to Red Giant to Planetary Nebula


Part I:  Background & Objective

 


Part II: 

 


Part III: 

 


Part IV: 

 

Succinct

Generic

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

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

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)

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)

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

Finite-Difference Expressions

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

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

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

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

  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)

        =

      1η+31/2θ3(dθdξ)

        =

      1η+31/2[1+ξ23]3/2[ξ23(1+ξ23)3/2]

        =

      1ηξ231/2

      we also deduce that,

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

Related Discussions

Tiled Menu

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