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*HRW66ρ¯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(34γg)(n+1)V(x)ξ2]x

 

=

d2xdξ2+[4ξ(n+1)θ(dθdξ)]dxdξ+(n+1)θ[σc26γgαξ(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]xiξi(n+1)[σc26γgαξi(θ')i]xi

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

xi

x+x2Δξ;

and,

xi

x+2xi+xΔξ2,

which will provide an approximate expression for x+xi+1, given the values of xxi1 and xi. Specifically, if the center of the configuration is denoted by the grid index, i=1, then for zones, i=3N,

θi[x+2xi+xΔξ2]

=

[4θi(n+1)ξi(θ')i][x+x2ξiΔξ](n+1)[σc26γgαξi(θ')i]xi

θi[x+Δξ2]+[4θi(n+1)ξi(θ')i][x+2ξiΔξ]

=

θi[2xi+xΔξ2][4θi(n+1)ξi(θ')i][x2ξiΔξ](n+1)[σc26γgαξi(θ')i]xi

x+[2θi+4ΔξθiξiΔξ(n+1)(θ')i]

=

x[4ΔξθiξiΔξ(n+1)(θ')i2θi]+xi{4θi2Δξ2(n+1)[σc26γgαξi(θ')i]}

 

=

x[4ΔξθiξiΔξ(n+1)(θ')i2θi]+xi{4θiΔξ2(n+1)3[σc2γg2α(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

[σc2γg2α].

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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