SSC/Stability/BiPolytropes/Pt4

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Reconciliation


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 qν 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+(43γg)g0r0]x=0

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

0

=

ddr0[r04γP0dxdr0]+[ω2ρ0r04+(3γ4)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[4r03P0r04g0ρ0]+[ω2ρ0r04(3γ4)r03g0ρ0]x

 

=

r04γP0{d2xdr02+[4r0g0ρ0P0]dxdr0+ρ0γP0[ω2(3γ4)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)ρc4/5 gives,

0

=

r04γP0{d2xdr*2+[4(ρ*P*)Mr*(r*)]1r*dxdr*+(ρ*P*)[2πσc23γgαgMr*(r*)3]x}

 

=

(r*)4[Kc1/2/(G1/2ρc2/5)]4γP*[Kcρc6/5]{d2xdr*2+[4(ρ*P*)Mr*(r*)]1r*dxdr*+(ρ*P*)[2πσc23γgαgMr*(r*)3]x}

 

=

[Kc3G2ρc2/5](r*)4γP*{d2xdr*2+[4(ρ*P*)Mr*(r*)]1r*dxdr*+(ρ*P*)[2πσc23γgαgMr*(r*)3]x}.

That is, multiplying the second expression through by, (Kc/G)ρc4/5G2ρc2/5/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

=

GKc2ρc2/5{ddr0[r04γP0dxdr0]+[ω2ρ0r04+(3γ4)r03dP0dr0]x}

 

=

GKc2ρc2/5{(Kc2ρc2/5G)ddr*[(r*)4γP*dxdr*]+[ω2(Kc2G2ρc8/5)ρcρ*(r*)4+(3γ4)(KcGρc4/5)Kcρc6/5(r*)3dP*dr*]x}

 

=

ddr*[(r*)4γP*dxdr*]+[(ω2Gρc)ρ*(r*)4+(3γ4)(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*4πxd[(r*)4γcP*dxdr*]+0rcore*[(ω2Gρc)ρ*(r*)4+(3γc4)(r*)3dP*dr*]4πx2dr*

 

 

+rcore*R*4πxd[(r*)4γeP*dxdr*]+rcore*R*[(ω2Gρc)ρ*(r*)4+(3γe4)(r*)3dP*dr*]4πx2dr*

 

=

[4πx(r*)4γcP*dxdr*]0rcore*0rcore*4π[(r*)4γcP*(dxdr*)2]dr*0rcore*[(3γc4)Mr*ρ*]4πx2r*dr*

 

 

+[4πx(r*)4γeP*dxdr*]rcore*R*rcore*R*4π[(r*)4γeP*(dxdr*)2]dr*rcore*R*[(3γe4)Mr*ρ*]4πx2r*dr*+0R*[(ω2Gρc)ρ*(r*)4]4πx2dr*

 

=

0rcore*x2(dlnxdlnr*)2γc4π(r*)2P*dr*+0rcore*(3γc4)x2(Mr*r*)4πρ*(r*)2dr*[4πx2(r*)3γcP*(dlnxdlnr*)]0rcore*

 

 

rcore*R*x2(dlnxdlnr*)2γe4π(r*)2P*dr*+rcore*R*(3γe4)x2(Mr*r*)4πρ*(r*)2dr*[4πx2(r*)3γeP*(dlnxdlnr*)]rcore*R*+0R*4π(ω2Gρc)ρ*(r*)4x2dr*.


Energy Normalization:

(γ1)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(γc1)x2(dlnxdlnr*)2dUint*0rcore*(3γc4)x2dWgrav*+[4πx2(r*)3γcP*(dlnxdlnr*)]0rcore*

 

 

+rcore*R*γe(γe1)x2(dlnxdlnr*)2dUint*rcore*R*(3γe4)x2dWgrav*+[4πx2(r*)3γeP*(dlnxdlnr*)]rcore*R*

 

=

2γc30rcore*x2(dlnxdlnr*)2dStherm*(3γc4)0rcore*x2dWgrav*+4πxi2(rcore*)3γcPi*{dlnxdlnr*|i}core

 

 

+2γe3rcore*R*x2(dlnxdlnr*)2dStherm*(3γe4)rcore*R*x2dWgrav*4πxi2(rcore*)3γePi*{dlnxdlnr*|i}env

 

=

2γc30rcore*x2(dlnxdlnr*)2dStherm*(3γc4)0rcore*x2dWgrav*

 

 

+2γe3rcore*R*x2(dlnxdlnr*)2dStherm*(3γe4)rcore*R*x2dWgrav*4πxi2(rcore*)3Pi*[γc{dlnxdlnr*|i}coreγe{dlnxdlnr*|i}env]

 

=

2γc30rcore*x2(dlnxdlnr*)2dStherm*(3γc4)0rcore*x2dWgrav*

 

 

+2γe3rcore*R*x2(dlnxdlnr*)2dStherm*(3γe4)rcore*R*x2dWgrav*4πxi2(rcore*)3Pi*[3(γeγc)],

where,

dMr*

=

4π(r*)2ρ*dr*,

dUint*

=

1(γ1)[4π(r*)2P*dr*]=[23(γ1)]dStherm*,

dWgrav*

=

(Mr*r*)4π(r*)2ρ*dr*.

Or, for inclusion in our accompanying Tabular Overview,

(2π3)σc20R*(xr*)2dMr*

=

γc(γc1)0rcore*x2(dlnxdlnr*)2dUint*(3γc4)0rcore*x2dWgrav*

 

 

+γe(γe1)rcore*R*x2(dlnxdlnr*)2dUint*(3γe4)rcore*R*x2dWgrav*

 

 

+32(γcγe)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(dlnxdlnr*)2dStherm*

𝔴core

0rcore*dWgrav*

          ;          

TERM2

0rcore*x2dWgrav*

𝔰env

rcore*R*dStherm*

          ;          

TERM3

rcore*R*x2(dlnxdlnr*)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

=

32π𝐓𝐄𝐑𝐌𝟓{2γc3[𝐓𝐄𝐑𝐌𝟏](3γc4)[𝐓𝐄𝐑𝐌𝟐]+2γe3[𝐓𝐄𝐑𝐌𝟑](3γe4)[𝐓𝐄𝐑𝐌𝟒]4πxi2(rcore*)3Pi*[3(γeγc)]}

 

=

0.036312577×[0.0931113401.059900832+1.4294428(3.82285786)1.782200484×(2.4)]=0.036312577×[0.00819]

 

=

0.0002973.

[σc2]μe/μc=1/2VP

=

0.020704186×[0.3527028231.660292468+1.928692426(1.85197268)1.029029184×(2.4)]=0.020704186×[0.003405]

 

=

0.0000705.

[σc2]μe/μc=0.345VP

=

0.019377703×[0.543588561.81951316+2.01880112(0.8993026)0.68747441×(2.4)]=0.019377703×[0.003585]

 

=

0.0000695.

[σc2]μe/μc=1/3VP

=

0.019467503×[0.5603316781.81099744+2.018776613(0.8340922)0.658354814×(2.4)]=0.019467503×[1.6022030521.580051555]

 

=

0.00043123.

[σc2]μe/μc=0.309VP

=

0.019781992×[0.5959716061.847844232+2.01407784(0.704971)0.60905486×(2.4)]=0.019781992×[1.4671762141.461731665]

 

=

0.0001077.

[σc2]μe/μc=1/4VP

=

0.021344909×[0.6856011161.88654168+1.972888973(0.4388304)0.499262049×(2.4)]=0.021344909×[1.2107788091.198228918]

 

=

0.000267876.


Table 4

μeμc ξi Analytic
𝔪tot
Numerical
𝔪tot
TERM5 xi rcore* Pi* {dlnxdlnr*|i}core {dlnxdlnr*|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)σc20R*(r*)2dMr*

=

(3γc4)0rcore*dWgrav*(3γe4)rcore*R*dWgrav*4π(rcore*)3Pi*[3(γeγc)]

(2π3)σc2Isphere*

=

(43γc)𝔴core+(43γe)𝔴env+Pi*Vcore*[32(γcγe)],

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

See Also


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