SSC/Stability/BiPolytropes/Pt4

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Reconciliation[edit]


Part I:   The Search
 

Part II:  Review of MF85b
 

III:  (5,1) Radial Oscillations
 

IV:  Reconciliation
 

    These four chapters, labeled Parts I - IV, are segments of the much longer chapter titled, SSC/Stability/BiPolytropes/PlannedApproach. An accompanying organizational index has helped us write this chapter succinctly.

Figure 7: Conflicting Instability Regions
Marginally unstable models

Figure 7, shown here on the right, is identical to the right-hand panel of Figure 4, as displayed above. From a standard global, free-energy analysis — such as the one summarized above — we have determined that the red-dashed curve shown in the right panel of Figure 6 divides the q−ν plane into dynamically stable (below and to the right) and unstable (above and to the left) regions.


Variational Principle[edit]

Setup[edit]

Let's follow the guidelines of the variational principle. Instead of starting with the form of the LAWE given above, namely,

Adiabatic Wave (or Radial Pulsation) Equation

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

we will start with a form that is more amenable to the variational principle, namely,

0

=

ddr0[r04γP0dxdr0]+[ω2ρ0r04+(3γ−4)r03dP0dr0]x.

ASIDE: Let's show that these two expressions are equivalent. Remembering that,

dP0dr0

=

−g0ρ0=−(GMrr02)ρ0,

the second expression becomes,

0

=

r04γP0d2xdr02+γdxdr0[4r03P0−r04g0ρ0]+[ω2ρ0r04−(3γ−4)r03g0ρ0]x

 

=

r04γP0{d2xdr02+[4r0−g0ρ0P0]dxdr0+ρ0γP0[ω2−(3γ−4)g0r0]x}.

Hence, we must multiply the first expression through by r04γP0 in order to obtain the second expression.


From above, we realize that multiplying the second expression through by (Kc/G)ρc−4/5 gives,

0

=

r04γP0{d2xdr*2+[4−(ρ*P*)Mr*(r*)]1r*dxdr*+(ρ*P*)[2πσc23γg−αgMr*(r*)3]x}

 

=

(r*)4[Kc1/2/(G1/2ρc2/5)]4γP*[Kcρc6/5]{d2xdr*2+[4−(ρ*P*)Mr*(r*)]1r*dxdr*+(ρ*P*)[2πσc23γg−αgMr*(r*)3]x}

 

=

[Kc3G2ρc2/5](r*)4γP*{d2xdr*2+[4−(ρ*P*)Mr*(r*)]1r*dxdr*+(ρ*P*)[2πσc23γg−αgMr*(r*)3]x}.

That is, multiplying the second expression through by, (Kc/G)ρc−4/5⋅G2ρc2/5/Kc3=G/(Kc2ρc2/5) , should give a desirable, totally dimensionless version of the LAWE. Remembering that,

ρ*

≡

ρ0ρc

;    

r*

≡

r0[Kc1/2/(G1/2ρc2/5)]

P*

≡

P0Kcρc6/5

;    

Mr*

≡

Mr[Kc3/2/(G3/2ρc1/5)]

dP*dr*

=

−Mr*ρ*(r*)2

;    

Enorm

=

[Kc5G3]1/2

let's try it.

0

=

GKc−2ρc−2/5{ddr0[r04γP0dxdr0]+[ω2ρ0r04+(3γ−4)r03dP0dr0]x}

 

=

GKc−2ρc−2/5{(Kc2ρc2/5G)ddr*[(r*)4γP*dxdr*]+[ω2(Kc2G2ρc8/5)ρcρ*(r*)4+(3γ−4)(KcGρc4/5)Kcρc6/5(r*)3dP*dr*]x}

 

=

ddr*[(r*)4γP*dxdr*]+[(ω2Gρc)ρ*(r*)4+(3γ−4)(r*)3dP*dr*]x.

Now, guided by the accompanying summary, if we multiply through by 4πxdr* and integrate over the entire volume, we obtain the governing variational relation, namely,

0

=

∫0rcore*4πx⋅d[(r*)4γcP*dxdr*]+∫0rcore*[(ω2Gρc)ρ*(r*)4+(3γc−4)(r*)3dP*dr*]4πx2dr*

 

 

+∫rcore*R*4πx⋅d[(r*)4γeP*dxdr*]+∫rcore*R*[(ω2Gρc)ρ*(r*)4+(3γe−4)(r*)3dP*dr*]4πx2dr*

 

=

[4πx(r*)4γcP*dxdr*]0rcore*−∫0rcore*4π[(r*)4γcP*(dxdr*)2]dr*−∫0rcore*[(3γc−4)Mr*ρ*]4πx2r*dr*

 

 

+[4πx(r*)4γeP*dxdr*]rcore*R*−∫rcore*R*4π[(r*)4γeP*(dxdr*)2]dr*−∫rcore*R*[(3γe−4)Mr*ρ*]4πx2r*dr*+∫0R*[(ω2Gρc)ρ*(r*)4]4πx2dr*

 

=

−∫0rcore*x2(dln⁡xdln⁡r*)2γc4π(r*)2P*dr*+∫0rcore*(3γc−4)x2(−Mr*r*)4πρ*(r*)2dr*−[4πx2(r*)3γcP*(−dln⁡xdln⁡r*)]0rcore*

 

 

−∫rcore*R*x2(dln⁡xdln⁡r*)2γe4π(r*)2P*dr*+∫rcore*R*(3γe−4)x2(−Mr*r*)4πρ*(r*)2dr*−[4πx2(r*)3γeP*(−dln⁡xdln⁡r*)]rcore*R*+∫0R*4π(ω2Gρc)ρ*(r*)4x2dr*.


Energy Normalization:

(γ−1)dUint

=

4πr2Pdr

 

=

4π[Kc1/2G1/2ρc2/5]3Kcρc6/5(r*)2P*dr*

 

=

4π[Kc5G3]1/2(r*)2P*dr*

⇒Enorm

≡

[Kc5G3]1/2

dWgrav

=

−(GMrr)4πr2ρdr

 

=

−(GMr*r*)4π(r*)2ρ*dr*[KcGρc4/5]ρc[Kc3/2G3/2ρc1/5]

 

=

−(Mr*r*)4π(r*)2ρ*dr*Enorm

Hence, the dimensionless governing variational relation becomes,

∫0R*(2π3)σc2(r*)2x2dMr*

=

∫0rcore*γc(γc−1)x2(dln⁡xdln⁡r*)2dUint*−∫0rcore*(3γc−4)x2dWgrav*+[4πx2(r*)3γcP*(−dln⁡xdln⁡r*)]0rcore*

 

 

+∫rcore*R*γe(γe−1)x2(dln⁡xdln⁡r*)2dUint*−∫rcore*R*(3γe−4)x2dWgrav*+[4πx2(r*)3γeP*(−dln⁡xdln⁡r*)]rcore*R*

 

=

2γc3∫0rcore*x2(dln⁡xdln⁡r*)2dStherm*−(3γc−4)∫0rcore*x2dWgrav*+4πxi2(rcore*)3γcPi*{−dln⁡xdln⁡r*|i}core

 

 

+2γe3∫rcore*R*x2(dln⁡xdln⁡r*)2dStherm*−(3γe−4)∫rcore*R*x2dWgrav*−4πxi2(rcore*)3γePi*{−dln⁡xdln⁡r*|i}env

 

=

2γc3∫0rcore*x2(dln⁡xdln⁡r*)2dStherm*−(3γc−4)∫0rcore*x2dWgrav*

 

 

+2γe3∫rcore*R*x2(dln⁡xdln⁡r*)2dStherm*−(3γe−4)∫rcore*R*x2dWgrav*−4πxi2(rcore*)3Pi*[γc{dln⁡xdln⁡r*|i}core−γe{dln⁡xdln⁡r*|i}env]

 

=

2γc3∫0rcore*x2(dln⁡xdln⁡r*)2dStherm*−(3γc−4)∫0rcore*x2dWgrav*

 

 

+2γe3∫rcore*R*x2(dln⁡xdln⁡r*)2dStherm*−(3γe−4)∫rcore*R*x2dWgrav*−4πxi2(rcore*)3Pi*[3(γe−γc)],

where,

dMr*

=

4π(r*)2ρ*dr*,

dUint*

=

1(γ−1)[4π(r*)2P*dr*]=[23(γ−1)]dStherm*,

dWgrav*

=

−(Mr*r*)4π(r*)2ρ*dr*.

Or, for inclusion in our accompanying Tabular Overview,

(2π3)σc2∫0R*(xr*)2dMr*

=

γc(γc−1)∫0rcore*x2(dln⁡xdln⁡r*)2dUint*−(3γc−4)∫0rcore*x2dWgrav*

 

 

+γe(γe−1)∫rcore*R*x2(dln⁡xdln⁡r*)2dUint*−(3γe−4)∫rcore*R*x2dWgrav*

 

 

+32(γc−γe)xi2Pi*Vcore*.

Implementation[edit]

Table 3

μeμc ξi Core Envelope Virial
Integrals over

dStherm*
Integrals over

dWgrav*
Integrals over

dStherm*
Integrals over

dWgrav*
Numerical

[2𝔰tot|𝔴tot|−1]
Analytic
𝔰core
Numerical
𝔰core
TERM1 Analytic
𝔴core
Numerical
𝔴core
TERM2 Analytic
𝔰env
Numerical
𝔰env
TERM3 Analytic
𝔴env
Numerical
𝔴env
TERM4
1 1.6686460157 3.021916335 3.021921 0.116389175 -3.356583022 -3.35666 -2.649752079 1.47780476 1.47791 1.0720821 -5.642859167 -5.642820 -1.91142893 0.000020
12 2.27925811317 4.241287117 4.241410819 0.440878529 -6.074241035 -6.074317546 -4.150731169 4.284931508 4.28547195 1.44651932 -10.97819621 -10.97847622 -0.92598634 0.000057
0.345 2.560146865247 4.639705843 4.6399114 0.6794857 -7.125754184 -7.125854025 -4.5487829 11.72861751 11.730381 1.51410084 -25.61089252 -25.6115597 -0.4496513 0.000097
13 2.582007485476 4.667042505 4.667254935 0.700414598 -7.200966267 -7.201068684 -4.57274936 13.15887139 13.1608467 1.51408246 -28.45086152 -28.45153761 -0.4170461 0.000101
0.309 2.6274239687695 4.722277318 4.722504339 0.744964507 -7.354156963 -7.3542507 -4.61961058 17.1374434 17.1399773 1.51055838 -36.36528446 -36.36591543 -0.3524855 0.000110
14 2.7357711469398 4.84592201 4.846185027 0.857001395 -7.70305421 -7.703178009 -4.7163542 37.84289623 37.8479208 1.47966673 -77.67458196 -77.67408155 -0.2194152 0.000128

𝔰core

≡

∫0rcore*dStherm*

          ;          

TERM1

≡

∫0rcore*x2(dln⁡xdln⁡r*)2dStherm*

𝔴core

≡

∫0rcore*dWgrav*

          ;          

TERM2

≡

∫0rcore*x2dWgrav*

𝔰env

≡

∫rcore*R*dStherm*

          ;          

TERM3

≡

∫rcore*R*x2(dln⁡xdln⁡r*)2dStherm*

𝔴env

≡

∫rcore*R*dWgrav*

          ;          

TERM4

≡

∫rcore*R*x2dWgrav*

NOTE: In all integrals, the fractional radial-displacement function, x, has been normalized
to unity at the center of the spherical model.

[σc2]μe/μc=1VP

=

32π⋅𝐓𝐄𝐑𝐌𝟓{2γc3[𝐓𝐄𝐑𝐌𝟏]−(3γc−4)[𝐓𝐄𝐑𝐌𝟐]+2γe3[𝐓𝐄𝐑𝐌𝟑]−(3γe−4)[𝐓𝐄𝐑𝐌𝟒]−4πxi2(rcore*)3Pi*[3(γe−γc)]}

 

=

0.036312577×[0.093111340−1.059900832+1.4294428−(−3.82285786)−1.782200484×(2.4)]=0.036312577×[0.00819]

 

=

0.0002973.

[σc2]μe/μc=1/2VP

=

0.020704186×[0.352702823−1.660292468+1.928692426−(−1.85197268)−1.029029184×(2.4)]=0.020704186×[0.003405]

 

=

0.0000705.

[σc2]μe/μc=0.345VP

=

0.019377703×[0.54358856−1.81951316+2.01880112−(−0.8993026)−0.68747441×(2.4)]=0.019377703×[0.003585]

 

=

0.0000695.

[σc2]μe/μc=1/3VP

=

0.019467503×[0.560331678−1.81099744+2.018776613−(−0.8340922)−0.658354814×(2.4)]=0.019467503×[1.602203052−1.580051555]

 

=

0.00043123.

[σc2]μe/μc=0.309VP

=

0.019781992×[0.595971606−1.847844232+2.01407784−(−0.704971)−0.60905486×(2.4)]=0.019781992×[1.467176214−1.461731665]

 

=

0.0001077.

[σc2]μe/μc=1/4VP

=

0.021344909×[0.685601116−1.88654168+1.972888973−(−0.4388304)−0.499262049×(2.4)]=0.021344909×[1.210778809−1.198228918]

 

=

0.000267876.


Table 4

μeμc ξi Analytic
𝔪tot
Numerical
𝔪tot
TERM5 xi rcore* Pi* {−dln⁡xdln⁡r*|i}core {−dln⁡xdln⁡r*|i}env [σc2]VP
1 1.6686460157 4.818155928 4.818145 13.14874521 0.814374698 1.153014872 0.139506172 +0.455871977 +1.47352 0.0002973
12 2.27925811317 9.020985415 9.021084268 23.0612702 0.653665497 1.574940686 0.049058481 +1.059668912 +1.835801347 0.0000705
0.345 2.560146865247 17.41399388 17.4141672 24.63990825 0.563043202 1.769031527 0.030957085 +1.552125296 +2.131275177 0.0000695
13 2.582007485476 18.8449906 18.8451614 24.52624951 0.555549156 1.78413696 0.029889634 +1.600041467 +2.16002488 0.0004312
0.309 2.6274239687695 22.61541791 22.6155686 24.13633675 0.539776219 1.815519219 0.027798189 +1.705239188 +2.223143513 0.0001077
14 2.7357711469398 39.12088278 39.1208075 22.36902623 0.501037082 1.890385851 0.023427588 +1.991720516 +2.39503231 0.0002679

𝔪tot

≡

∫0R*dMr*

          ;          

Isphere*

≡

∫0R*(r*)2dMr*

          ;          

TERM5

≡

∫0R*(r*)2x2dMr*

NOTE: In the TERM5 integral (as elsewhere), the fractional radial-displacement function, x,
has been normalized to unity at the center of the spherical model.

Revised Free-Energy Analysis[edit]

If we set x = constant in the variational principle relation, we have,

(2π3)σc2∫0R*(r*)2dMr*

=

−(3γc−4)∫0rcore*dWgrav*−(3γe−4)∫rcore*R*dWgrav*−4π(rcore*)3Pi*[3(γe−γc)]

⇒(2π3)σc2Isphere*

=

(4−3γc)𝔴core+(4−3γe)𝔴env+Pi*Vcore*[32(γc−γe)],

Notice the similarity between this last expression and the pair of expressions — numbered ⑥ and ⑦ — that arise in the context of pressure-truncated polytropes.

See Also[edit]


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