SSC/Stability/Polytropes/Pt3

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Radial Oscillations of Polytropic Spheres[edit]


Part I:   Wave Equation
 

Part II:  Boundary Conditions
 

III:  Tables
 


Tables[edit]

Quantitative Information Regarding Eigenvectors of Oscillating Polytropes

(Γ1=5/3)

n

ρcρ¯

Excerpts from Table 1 of

📚 Hurley, Roberts, & Wright (1966)

s2(n+1)/(4πGρc)

Excerpts from Table 3 of

J. P. Cox (1974)

σ02R3/(GM)

(n+1)*Cox743*HRW66⋅ρ¯ρc

0

1

1/3

1

1

1

3.30

0.38331

1.892

0.997

1.5

5.99

0.37640

2.712

1.002

2

11.4

0.35087

4.00

1.000

3

54.2

0.22774

9.261

1.000

3.5

153

0.12404

12.69

1.003

4.0

632

0.04056

15.38

1.000

Numerical Integration from the Center, Outward[edit]

Here we show how a relatively simple, finite-difference algorithm can be developed to numerically integrate the governing LAWE from the center of a polytropic configuration, outward to its surface.

Drawing from our above discussion, the LAWE for any polytrope of index, n, may be written as,

0

=

d2xdξ2+[4−(n+1)V(ξ)ξ]dxdξ+[ω2(an2ρcγgPc)θcθ−(3−4γg)⋅(n+1)V(x)ξ2]x

 

=

d2xdξ2+[4ξ−(n+1)θ(−dθdξ)]dxdξ+(n+1)θ[σc26γg−αξ(−dθdξ)]x

where,

σc2

≡

3ω22πGρc.

Following a parallel discussion, we begin by multiplying the LAWE through by θ, obtaining a 2nd-order ODE that is relevant at every individual coordinate location, ξi, namely,

θixi″

=

−[4θi−(n+1)ξi(−θ')i]xi′ξi−(n+1)[σc26γg−αξi(−θ')i]xi

Now, using the general finite-difference approach described separately, we make the substitutions,

xi′

≈

x+−x−2Δξ;

and,

xi″

≈

x+−2xi+x−Δξ2,

which will provide an approximate expression for x+≡xi+1, given the values of x−≡xi−1 and xi. Specifically, if the center of the configuration is denoted by the grid index, i=1, then for zones, i=3→N,

θi[x+−2xi+x−Δξ2]

=

−[4θi−(n+1)ξi(−θ')i][x+−x−2ξiΔξ]−(n+1)[σc26γg−αξi(−θ')i]xi

⇒θi[x+Δξ2]+[4θi−(n+1)ξi(−θ')i][x+2ξiΔξ]

=

−θi[−2xi+x−Δξ2]−[4θi−(n+1)ξi(−θ')i][−x−2ξiΔξ]−(n+1)[σc26γg−αξi(−θ')i]xi

⇒x+[2θi+4Δξθiξi−Δξ(n+1)(−θ')i]

=

x−[4Δξθiξi−Δξ(n+1)(−θ')i−2θi]+xi{4θi−2Δξ2(n+1)[σc26γg−αξi(−θ')i]}

 

=

x−[4Δξθiξi−Δξ(n+1)(−θ')i−2θi]+xi{4θi−Δξ2(n+1)3[σc2γg−2α(−3θ'ξ)i]}.

In order to kick-start the integration, we will set the displacement function value to x1=1 at the center of the configuration (ξ1=0), then we will 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 will set,

x2

=

x1[1−(n+1)𝔉Δξ260],

where,

𝔉

≡

[σc2γg−2α].

See Also[edit]

  • In an accompanying Chapter within our "Ramblings" Appendix, we have played with the adiabatic wave equation for polytropes, examining its form when the primary perturbation variable is an enthalpy-like quantity, rather than the radial displacement of a spherical mass shell. This was done in an effort to mimic the approach that has been taken in studies of the stability of Papaloizou-Pringle tori.
  • n=32 … D. Lucas (1953, Bul. Soc. Roy. Sci. Liege, 25, 585) … Citation obtained from the Prasad & Gurm (1961) article.
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