SSC/Stability/n1PolytropeLAWE/Pt4

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Radial Oscillations of n = 1 Polytropic Spheres (Pt 4)


Part I:   Search for Analytic Solutions
 

Part II:  New Ideas
 

Part III:  What About Bipolytropes?
 

Part IV:  Most General Structural Solution
 

Preamble Regarding Chatterji

As far as we have been able to ascertain, the first technical examination of radial oscillation modes in n=1 polytropes was performed — using numerical techniques — in 1951 by L. D. Chatterji; at the time, he was in the Mathematics Department of Allahabad University. His two papers on this topic were published in, what is now referred to as, the Proceedings of the Indian National Science Academy (PINSA). The citations that immediately follow this opening paragraph provide inks to both of these papers by Chatterji, but the links may be insecure. Apparently Springer is archiving recent PINSA volumes, but their holdings do not date back as early as 1951.

A detailed review of Chatterji51 is provided in an accompanying discussion.

Equilibrium Structure

When n=1, the relevant Lane-Emden equation is,

1ξ2ddξ(ξ2dΘHdξ)=−ΘH ,

and we find that the solution is, quite generally,

θ

=

A[sin⁡ξξ]−B[cos⁡ξξ]=1ξ{Asin⁡ξ−Bcos⁡ξ}

in which case,

dθdξ

=

ddξ{A[sin⁡ξξ]−B[cos⁡ξξ]}

 

=

A[−sin⁡ξξ2+cos⁡ξξ]+B[cos⁡ξξ2+sin⁡ξξ]

 

=

1ξ2[−Asin⁡ξ+Bcos⁡ξ]+1ξ[Acos⁡ξ+Bsin⁡ξ],

and,

Q(ξ)≡−dln⁡θdln⁡ξ

=

−ξθ⋅{1ξ2[−Asin⁡ξ+Bcos⁡ξ]+1ξ[Acos⁡ξ+Bsin⁡ξ]}

 

=

1ξθ⋅{[Asin⁡ξ−Bcos⁡ξ]+ξ[−Acos⁡ξ−Bsin⁡ξ]}

 

=

{1−ξ[Acos⁡ξ+Bsin⁡ξAsin⁡ξ−Bcos⁡ξ]}.

If we set β≡tan−1(B/A), we can rewrite the expression for θ as,

θ

=

Aξ{sin⁡ξ−BAcos⁡ξ}

 

=

Aξ{sin⁡ξ−tan⁡βcos⁡ξ}

 

=

Aξcos⁡β{sin⁡ξcos⁡β−cos⁡ξsin⁡β}

 

=

Acos⁡β⋅sin⁡(ξ−β)ξ,

Beech88, §3, p. 221, Eq. (6)
EFC98, §2, p. 831, Eq. (2)

and the expression for Q as,

Q(ξ)

=

{1−ξ[cos⁡ξcos⁡β+sin⁡ξsin⁡βsin⁡ξcos⁡β−cos⁡ξsin⁡β]}

 

=

{1−ξ[cos⁡(ξ−β)sin⁡(ξ−β)]}

 

=

[1−ξcot⁡(ξ−β)].

SUMMARY of EQUILIBRIUM STRUCTURE
and switching notation from θ(ξ) to ϕ(η)

When n=1, the relevant Lane-Emden equation is,

1η2ddη(η2dϕdη)=−ϕ .

Its solution, quite generally, is

ϕ

=

A[sin⁡ηη]−B[cos⁡ηη],

where A and B are scalar constants, in which case,

Q(η)≡−dln⁡ϕdln⁡η

=

{1−η[Acos⁡η+Bsin⁡ηAsin⁡η−Bcos⁡η]}.


Alternatively, drawing from Eq. (6) of Beech88, this solution can be written in the form,

ϕ

=

αBeech⋅sin⁡(η−βBeech)η,

in which case,

Q(η)

=

[1−ηcot⁡(η−βBeech)],

where, in terms of the coefficients A and B,

βBeech

≡

tan−1(B/A)

      and      

αBeech

≡

Acos⁡βBeech=A[1+(B/A)2]1/2.

Establish Relevant (n=1) LAWE

From a related discussion — or a broader overview of Instability Onset — we find the

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)

Furthermore — see, for example, here,

Exact Solution to the Polytropic LAWE

xP≡3(n−1)2n[1+(n−3n−1)(1ξθn)dθdξ],

in which case for n=1,

xP=−3(1ξθ)dθdξ=−3(1ξ2)dln⁡θdln⁡ξ=3ξ2Q.


Isolated Sphere

For an isolated n = 1 (γg=2,α=1) polytrope, we know that,

θ

=

sin⁡ξξ

    ⇒Q(ξ)≡−dln⁡θdln⁡ξ

=

[1−ξcot⁡ξ].

Hence, the relevant LAWE is,

0

=

d2xdξ2+[4−2(1−ξcot⁡ξ)]1ξ⋅dxdξ+2[(σc212)ξ3sin⁡ξ−(1−ξcot⁡ξ)]xξ2

LAWE for n = 1 Polytrope

0

=

d2xdξ2+2ξ[1+ξcot⁡ξ]dxdξ+12[(σc23)ξsin⁡ξ−4ξ2(1−ξcot⁡ξ)]x

Surface boundary condition:

−dln⁡xdln⁡ξ|surf

=

(3−nn+1)+nσc26(n+1)[ξθ′]surf

⇒−dln⁡xdln⁡ξ|surf

=

1+σc212[ξ3(ξcos⁡ξ−sin⁡ξ)]ξ=π=1−π2σc212

Spherical Shell

In the context of a spherically symmetric n = 1 (γg=2,α=1) shell (envelope) outside of a spherically symmetric bipolytropic core, we should adopt the more general Lane-Emden structural solution,

θ

=

A[sin⁡ξξ]−B[cos⁡ξξ]

    ⇒Q(ξ)≡−dln⁡θdln⁡ξ

=

[1−ξcot⁡(ξ−β)]=ξ2xP3.

Reminder: the expression for xP is,

xP=3ξ2[1−ξcot⁡(ξ−β)].

Playing around a bit, we find that,

ξ23⋅xP = 1−ξ⋅cos⁡(ξ−β)sin⁡(ξ−β)
  = 1−ξ[cos⁡(ξ−β)sin⁡(ξ−β)]⋅(ξ−β)(ξ−β)
  = 1−ξ[cos⁡(ξ−β)(ξ−β)][(ξ−β)sin⁡(ξ−β)]

As a result, the governing LAWE becomes,

0 = d2xPdξ2+[4−2Q]1ξ⋅dxPdξ+2[(σc212)0ξ2θ−Q]xPξ2
  = d2xPdξ2+4ξ⋅dxPdξ−[2Q]1ξ⋅dxPdξ−[2Q]xPξ2
  = d2xPdξ2+4ξ⋅dxPdξ−2Q{1ξ⋅dxPdξ+xPξ2}
  = d2xPdξ2+4ξ⋅dxPdξ−2ξ2xP3{1ξ⋅dxPdξ+xPξ2}
  = d2xPdξ2+[4ξ−2ξxP3]⋅dxPdξ−2xP23.

Let's plug in the expression for xP, namely, xP=3[1−ξcot⁡(ξ−β)]/ξ2. We have, first of all,

xp2 = 32ξ4[1−ξcot⁡(ξ−β)]2

 

= 32ξ4[1−2ξcot⁡(ξ−β)+ξ2cot⁡2(ξ−β)];

dxpdξ

= ddξ{3ξ2[1−ξcot⁡(ξ−β)]}

 

= [1−ξcot⁡(ξ−β)]ddξ{3ξ2}−3ξddξ[cot⁡(ξ−β)]−3ξ2[cot⁡(ξ−β)]

 

= −6ξ3[1−ξcot⁡(ξ−β)]+3ξ[1+cot⁡2(ξ−β)]−3ξ2[cot⁡(ξ−β)]

 

= −6ξ3+3ξ2[cot⁡(ξ−β)]+3ξ+3ξ[cot⁡2(ξ−β)].


Note for later use that,

xP2r2(dln⁡xPdln⁡r)2=(dxPdr)2

=

{−6ξ3+3ξ2[cot⁡(ξ−β)]+3ξ+3ξ[cot⁡2(ξ−β)]}2

Recognize that we have used the trigonometric relations,

ddξ[cot⁡(u)]

= −1sin2(u)dudξ=−[1+cot2(u)]dudξ.

And,

d2xpdξ2

= ddξ{−6ξ3+3ξ+3ξ2[cot⁡(ξ−β)]+3ξ[cot⁡2(ξ−β)]}

 

= 18ξ4−3ξ2−6ξ3[cot⁡(ξ−β)]−3ξ2[1+cot⁡2(ξ−β)]−3ξ2[cot⁡2(ξ−β)]−6ξ[cot⁡(ξ−β)][1+cot⁡2(ξ−β)]

 

= 18ξ4−6ξ2−6ξ3[cot⁡(ξ−β)]−6ξ2⋅cot⁡2(ξ−β)−6ξ[cot⁡(ξ−β)]−6ξ⋅cot⁡3(ξ−β).

Hence,

d2xPdξ2+[4ξ−2ξxP3]⋅dxPdξ−2xP23

= {18ξ4−6ξ2−6ξ3[cot⁡(ξ−β)]−6ξ2⋅cot⁡2(ξ−β)−6ξ[cot⁡(ξ−β)]−6ξ⋅cot⁡3(ξ−β)}

 

  +[4ξ−2ξxP3]⋅{−6ξ3+3ξ2[cot⁡(ξ−β)]+3ξ+3ξ[cot⁡2(ξ−β)]}

 

  −{6ξ4[1−2ξcot⁡(ξ−β)+ξ2cot⁡2(ξ−β)]}

 

= 18ξ4−6ξ2−6ξ3[cot⁡(ξ−β)]−6ξ[cot⁡(ξ−β)]−6ξ2⋅cot⁡2(ξ−β)−6ξ⋅cot⁡3(ξ−β)

 

  +4ξ{−6ξ3+3ξ2[cot⁡(ξ−β)]+3ξ+3ξ[cot⁡2(ξ−β)]}

 

  +[2ξxP3]⋅{6ξ3−3ξ2[cot⁡(ξ−β)]−3ξ−3ξ[cot⁡2(ξ−β)]}

 

  +6ξ4[−1+2ξcot⁡(ξ−β)−ξ2cot⁡2(ξ−β)]

 

= 18ξ4−6ξ2−6ξ3[cot⁡(ξ−β)]−6ξ[cot⁡(ξ−β)]−6ξ2⋅cot⁡2(ξ−β)−6ξ⋅cot⁡3(ξ−β)

 

  −24ξ4+12ξ3[cot⁡(ξ−β)]+12ξ2+12ξ2[cot⁡2(ξ−β)]

 

  +2ξ[1−ξcot⁡(ξ−β)]⋅{6ξ3−3ξ2[cot⁡(ξ−β)]−3ξ−3ξ[cot⁡2(ξ−β)]}

 

  +6ξ4[−1+2ξcot⁡(ξ−β)−ξ2cot⁡2(ξ−β)]

 

= −6ξ4+6ξ2+6ξ3[cot⁡(ξ−β)]−6ξ[cot⁡(ξ−β)]+6ξ2⋅cot⁡2(ξ−β)−6ξ⋅cot⁡3(ξ−β)

 

  −12ξ3⋅cot⁡(ξ−β)+6ξ⋅cot⁡(ξ−β)+6ξ2[cot⁡2(ξ−β)]+6ξ[cot⁡3(ξ−β)]

 

  +12ξ4−6ξ3[cot⁡(ξ−β)]−6ξ2−6ξ2[cot⁡2(ξ−β)]

 

  −6ξ4+12ξ3⋅cot⁡(ξ−β)−6ξ2⋅cot⁡2(ξ−β)

 

= −6ξ[cot⁡(ξ−β)]+6ξ2⋅cot⁡2(ξ−β)−6ξ⋅cot⁡3(ξ−β)

 

  +6ξ⋅cot⁡(ξ−β)+6ξ2[cot⁡2(ξ−β)]+6ξ[cot⁡3(ξ−β)]

 

  −12ξ2[cot2(ξ−β)]

 

= 0.

Debugging LaTeX layout:

 

  −12ξ2[cot2(ξ−β)]

 

  −12ξ2[cot3(ξ−β)]

 

 

+[cot1(ξ−β)]+6ξ2[cot2(ξ−β)m]+6ξ[cot3(ξ−β)]

Hydrostatic Balance and Virial Equilibrium

General Expression for Virial

Here we draw heavily from our accompanying "style sheet" synopsis of spherically symmetric configurations.

First, we pull the equation for

Hydrostatic Balance

dPdr=−GMrρr2

from subsection ① of the synopsis; then, guided by subsection ②, we multiply both sides through by rdV=4πr3dr and integrate over the volume. This gives,

0

=

−∫0Rr(dPdr)dV−∫0Rr(GMrρr2)dV

 

=

−∫0R4πr3(dPdr)dr−∫0R(GMrr)dMr,

where we have used the relations,

dV=4πr2dr

and,

   dMr=ρdV⇒Mr=4π∫0rρr2dr.

Now, given that,

ddr(4πr3P)

=

4πr3(dPdr)+12πPr2

⇒−4πr3(dPdr)

=

12πr2P−ddr(4πr3P),

we can rewrite the integral expression in the form,

0

=

∫0R[12πr2P−ddr(4πr3P)]dr−∫0R(GMrr)dMr

 

=

∫0R3[4πr2P]dr−∫0R(GMrr)dMr−∫0R[d(3PV)]

 

=

3(γ−1)Uint+Wgrav−[3PV]0R,

where,

Wgrav

=

−∫0R(GMrr)dMr

     and,      

Uint

=

1(γ−1)∫0R4πr2Pdr.

Note as well that Uint=2Stherm/[3(γ−1)].

Calculate Relevant Energy Expressions

Adopting the energy normalization shown here01 along with the other variable normalizations defined here02, we have …

Thermal Energy

S*≡S[Kc5/G3]1/2=32(γ−1)⋅Uint[Kc5/G3]1/2 =

32[Kc5/G3]1/2∫rinnerrouter4πr2Pdr

  =

32{Kc−5/2G3/2}∫rinnerrouter{Kc3/2G−3/2ρ0−6/5⋅Kcρ06/5}4π(r*)2P*dr*

  =

32∫rinnerrouter4π(r*)2P*dr*.

Plugging in the derived radial profiles for r* and P*, we have,

S* =

6π(32π)3/2∫ξinnerξouterξ2(1+ξ23)−3dξ

  =

6π(32π)3/233/223∫ξinnerξouter8⋅ξ23(1+ξ23)−3dξ31/2

  =

[(22⋅32π2)(3323π3)(3326)]1/2∫ξinnerξouter8⋅ξ23(1+ξ23)−3dξ31/2

  =

(3827π)1/2∫ξinnerξouter8⋅ξ23(1+ξ23)−3dξ31/2.

After making the substitution, x≡ξ/3, this expression matches the expression for S* obtained separately.

For later use, we note that,

dS* =

32[4πr2Pdr[Kc5/G3]1/2]=6π(32π)3/2ξ2(1+ξ23)−3dξ.

Gravitational Potential Energy

W*=Wgrav[Kc5/G3]

=

[Kc−5/2G3/2]∫rinnerrouter(−GMrr)dMr

 

=

−[Kc−5/2G3/2]∫rinnerrouter4πGMrρrdr

 

=

−[Kc−5/2G3/2]∫rinnerrouter4πG[Kc3/2G−3/2ρ0−1/5]Mr*[ρ*ρ0][KcG−1ρ0−4/5]r*dr*

 

=

−∫rinnerrouter4πMr*ρ*r*dr*.

Plugging in the derived radial profiles for r*, ρ* and Mr*, we have,

W*

=

−4π∫ξinnerξouter(2⋅3π)1/2[ξ3(1+ξ23)−3/2](1+ξ23)−5/2(32π)ξdξ

 

=

−4π(2⋅3π)1/2(32π)∫ξinnerξouter[ξ3(1+ξ23)−3/2](1+ξ23)−5/2ξdξ

 

=

−(24π2)1/2(2⋅3π)1/2(3222π2)1/2∫ξinnerξouter[ξ4(1+ξ23)−4]dξ

 

=

−[23⋅33π]1/2∫ξinnerξouter35/2⋅[χ4(1+χ2)−4]dχ.

Stability Analysis

Here, as well, we draw heavily from our accompanying "style sheet" synopsis of spherically symmetric configurations.

This time, we pull the

LAWE:   Linear Adiabatic Wave (or Radial Pulsation) Equation

0

=

ddr[r4γPdxdr]+[ω2ρr4+(3γ−4)r3dPdr]x,

from subsection ④ of the synopsis; then, guided by subsection ⑤, we multiply both sides through by 4πxdr to obtain,

−[4πx2(ω2ρr4)]dr

=

4πx{ddr[r4γP(dxdr)]}dr+{[(3γ−4)4πx2r3(dPdr)]}dr.

Now, given that,

ddr[4πxγr4P(dxdr)]

=

4πxddr[γr4P(dxdr)]+[γr4P(dxdr)]ddr[4πx]

⇒4πxddr[γr4P(dxdr)]

=

ddr[4πxγr4P(dxdr)]−[4πγr4P(dxdr)2],

we can rewrite this last expression in the form,

−[4πx2(ω2ρr4)]dr

=

ddr[4πxγr4P(dxdr)]dr−[4πγr4P(dxdr)2]dr+{[(3γ−4)4πx2r3(dPdr)]}dr

⇒[4πx2(ω2ρr4)]dr

=

−d[4πxγr4P(dxdr)]+[4πγr4P(dxdr)2]dr−[(3γ−4)4πx2r3(−GMrρr2)]dr

Note that, in order to obtain the last term on the RHS of this expression, we used the hydrostatic balance relation to replace the pressure gradient in terms of the gravitational potential. Finally, integrating over the volume of the configuration gives,

∫0R[4πx2(ω2ρr4)]dr

=

∫0R[4πγr4P(dxdr)2]dr−∫0R[(3γ−4)x2(−GMrr)4πρr2]dr−[4πxγr4P(dxdr)]0R,

or,

∫0R[4πx2(ω2ρr4)]dr

=

∫0R[x2(dln⁡xdln⁡r)24πγr2P]dr⏞TERM1−∫0R[(3γ−4)x2(−GMrr)4πρr2]dr⏟TERM2+[γ4πx2r2P(−dln⁡xdln⁡r)]0R⏞TERM3.

Given that (from above),

dS* =

32[4πr2Pdr[Kc5/G3]1/2]=6π(32π)3/2ξ2(1+ξ23)−3dξ,

we can write,

TERM1[Kc5/G3]1/2 =

γxP2(dln⁡xPdln⁡r)2[4πr2Pdr[Kc5/G3]1/2]

  =

γxP2(dln⁡xPdln⁡r)2{(23)6π(32π)3/2ξ2(1+ξ23)−3dξ},

Furthermore, given that for a truncated n=5 configuration,

xp =

1−ξ215

⇒dxpdξ =

−215ξ

⇒dln⁡xpdln⁡ξ =

−ξxP[215ξ]=−[215ξ2][1515−ξ2]=−[2ξ215−ξ2]

⇒xP2(dln⁡xpdln⁡ξ)2 =

[15−ξ215]2[2ξ215−ξ2]2=[2ξ215]2,

we have,

TERM1[Kc5/G3]1/2 =

γ[2ξ215]2{(23)6π(32π)3/2ξ2(1+ξ23)−3dξ}

  =

γ[223252](23)6π(32π)3/2{ξ6(1+ξ23)−3dξ}

  =

γ[24π3252][3323π3]1/2{ξ6(1+ξ23)−3dξ}

  =

γ[253⋅54π]1/2{ξ6(1+ξ23)−3dξ}.

Hence, after making the replacement χ≡ξ/3⇒ξ=31/2χ, we find that,

∫0χsurfTERM1[Kc5/G3]1/2 =

γ[253⋅54π]1/2⋅37/2∫0χsurf{χ6(1+χ2)−3dχ}

  =

γ[253⋅54π]1/2⋅37/2⋅18{χsurf(8χsurf4+25χsurf2+15)(1+χsurf2)2−15tan−1(χsurf)}

where, we have completed the integral with the assistance of the WolframAlpha online integrator:

Mathematica Integral
Mathematica Integral

See Also

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