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=Radial Pulsation Neutral Mode=
=Radial Pulsation Neutral Mode=
[[SSC/Stability/InstabilityOnsetOverview#Analyses_of_Radial_Oscillations|From our separate discussion]], we have found that,
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  <td align="center" colspan="3"><font color="maroon"><b>Exact Solution to the <math>~(3 \le n < \infty)</math> Polytropic LAWE</b></font></td>
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<math>~\sigma_c^2 = 0</math>
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&nbsp; &nbsp; &nbsp; and &nbsp; &nbsp; &nbsp;
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<math>~x_P \equiv \frac{3(n-1)}{2n}\biggl[1 + \biggl(\frac{n-3}{n-1}\biggr) \biggl( \frac{1}{\xi \theta^{n}}\biggr) \frac{d\theta}{d\xi}\biggr] \, .</math>
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=See Also=
=See Also=


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Revision as of 23:02, 28 August 2021

LAWE

Most General Form

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

Adiabatic Wave (or Radial Pulsation) Equation

d2xdr02+[4r0−(g0ρ0P0)]dxdr0+(ρ0γgP0)[ω2+(4−3γg)g0r0]x=0

whose solution gives eigenfunctions that describe various radial modes of oscillation in spherically symmetric, self-gravitating fluid configurations. The boundary condition conventionally used in connection with the adiabatic wave equation is,

r0dln⁡xdr0

=

1γg(4−3γg+ω2R3GMtot)        at         r0=R.

Polytropic Configurations

Part 1

If the initial, unperturbed equilibrium configuration is a polytropic sphere whose internal structure is defined by the function, θ(ξ), that provides a solution to the,

Lane-Emden Equation

1ξ2ddξ(ξ2dΘHdξ)=−ΘHn

then,

r0

=

anξ,

ρ0

=

ρcθn,

P0

=

Kρ0(n+1)/n=Kρc(n+1)/nθn+1,

g0

=

GM(r0)r02=Gr02[4πan3ρc(−ξ2dθdξ)],

where,

an

=

[(n+1)K4πG⋅ρc(1−n)/n]1/2.

Hence, after multiplying through by an2, the above adiabatic wave equation can be rewritten in the form,

d2xdξ2+[4ξ−g0an(an2ρ0P0)]dxdξ+(an2ρ0γgP0)[ω2+(4−3γg)g0anξ]x

=

0.

In addition, given that,

g0an

=

4πGρc(−dθdξ),

and,

an2ρ0P0

=

(n+1)(4πGρc)θ=an2ρcPc⋅θcθ,

we can write,

0

=

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

 

=

d2xdξ2+[4−(n+1)V(ξ)ξ]dxdξ+(n+1)[ω2(an2ρcγgPc)ξ2θc(n+1)θ−(3−4γg)⋅V(x)]xξ2

where we have adopted the function notation,

V(ξ)

≡

−ξθdθdξ.

Part 2

Drawing from an accompanying discussion, we have the following:

Polytropic LAWE (linear adiabatic wave equation)

0=d2xdξ2+[4−(n+1)Q]1ξ⋅dxdξ+(n+1)[(σc26γg)ξ2θ−αQ]xξ2

where:    Q(ξ)≡−dln⁡θdln⁡ξ,    σc2≡3ω22πGρc,     and,     α≡(3−4γg)

In order to reconcile with the "Part 1" expression, we note first that V(ξ)↔Q(ξ). We note as well that since,

(an2ρcPc)θc

=

(n+1)4πGρc,

we have,

ω2(an2ρcγgPc)ξ2θc(n+1)θ

↔

ω2γg[(n+1)4πGρc]ξ2(n+1)θ=16γg[3ω22πGρc]ξ2θ=(σc26γg)ξ2θ.

All physically reasonable solutions are subject to the inner boundary condition,

dxdξ=0         at         ξ=0,

but the relevant outer boundary condition depends on whether the underlying equilibrium configuration is isolated (surface pressure is zero), or whether it is a "pressure-truncated" configuration. As is the case with the pressure-truncated isothermal spheres, discussed above, if the polytropic configuration is truncated by the pressure, Pe, of a hot, tenuous external medium, then the solution to the LAWE is subject to the outer boundary condition,

−dln⁡xdln⁡ξ=3         at         ξ=ξ~.

But, for isolated polytropes, the sought-after solution is subject to the more conventional boundary condition,

−dln⁡xdln⁡ξ=(3−nn+1)+nσc26(n+1)[ξθ']         at         ξ=ξsurf.

Radial Pulsation Neutral Mode

From our separate discussion, we have found that,

Exact Solution to the (3≤n<∞) Polytropic LAWE

σc2=0

      and      

xP≡3(n−1)2n[1+(n−3n−1)(1ξθn)dθdξ].

See Also

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