SSC/Stability/BiPolytropes/Pt4

From JETohlineWiki
Revision as of 15:21, 8 January 2024 by Joel2 (talk | contribs)
Jump to navigation Jump to search

Reconciliation


Part I:   The Search
 

Part II:  Review of MF85b
 

III:  (5,1) Radial Oscillations
 

IV:  Reconciliation
 
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

Setup

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

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

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


Tiled Menu

Appendices: | VisTrailsEquations | VisTrailsVariables | References | Ramblings | VisTrailsImages | myphys.lsu | ADS |