SSC/Structure/BiPolytropes/51RenormaizePart2: Difference between revisions

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<math>\phi = A \biggl[ \frac{\sin(\eta - B)}{\eta} \biggr]</math><br />
<math>\phi = A \biggl[ \frac{\sin(\eta - B)}{\eta} \biggr]</math><br />
<math>\frac{d\phi}{d\eta} = \frac{A}{\eta^2} \biggl[ \eta\cos(\eta-B) - \sin(\eta-B) \biggr] </math>
<math>\frac{d\phi}{d\eta} = -\frac{A}{\eta^2} \biggl[ \sin(\eta-B) - \eta\cos(\eta-B)\biggr] </math>
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Revision as of 12:34, 19 August 2022

Radial Oscillations in (nc,ne) = (5,1) Bipolytropes

Logically, this chapter extends the discussion — specifically the subsection titled, Try Again — found in the "Ramblings" chapter in which we introduced a total-mass-based renormalization of models along sequences of (nc,ne)=(5,1) bipolytropes.

Building Each Model

Basic Equilibrium Structure

Most of the details underpinning the following summary relations can be found here.

New Normalization
ρ~ ρ[(KcG)3/21Mtot]5;
P~ P[Kc10G9Mtot6];
r~ r[(KcG)5/2Mtot2],
M~r MrMtot;
H~ H[Kc5/2G3/2Mtot].

Quantity

Core
0ξξi


θ=[1+13ξ2]1/2
dθdξ=ξ3[1+13ξ2]3/2

Envelope
ηiηηs


ϕ=A[sin(ηB)η]
dϕdη=Aη2[sin(ηB)ηcos(ηB)]

r~

𝓂surf2(μeμc)4(32π)1/2ξ

𝓂surf2(μeμc)3θi2(2π)1/2η

ρ~

𝓂surf5(μeμc)10(1+13ξ2)5/2

𝓂surf5(μeμc)9θi5ϕ

P~

𝓂surf6(μeμc)12(1+13ξ2)3

𝓂surf6(μeμc)12θi6ϕ2

M~r

𝓂surf1(μeμc)2(23π)1/2[ξ3(1+13ξ2)3/2]

𝓂surf1θi1(2π)1/2(η2dϕdη)

Note that, for a given specification of the molecular-weight ratio, μe/μc, and the interface location, ξi,

θi = (1+13ξi2)1/2,
ηi = (μeμc)3θi2ξi,
Λi = ξi3[(μeμc)11θi2ξi21],
A = ηi(1+Λi2)1/2,
ηs = π2+ηi+tan1(Λi),

in which case,

𝓂surf = (2π)1/2Aηsθi,
ρ~c =

𝓂surf5(μeμc)10,

νMcoreMtot = (μeμc)23[ξi3θi4Aηs],
qrcoreR = (μeμc)3[ξiθi2ηs].

Additional Relations

The analytically prescribed radial pressure gradient in the core can be obtained as follows.

dM~rdξ =

𝓂surf1(μeμc)2(23π)1/2{3ξ2(1+13ξ2)3/2ξ4(1+13ξ2)5/2}

  =

𝓂surf1(μeμc)2(23π)1/2{3ξ2(1+13ξ2)ξ4}(1+13ξ2)5/2

  =

𝓂surf1(μeμc)2(23π)1/2{3ξ2(1+13ξ2)5/2}

dξdM~r =

𝓂surf(μeμc)2(π23)1/2{13ξ2(1+13ξ2)5/2}.

Also,

dP~dξ =

𝓂surf6(μeμc)12{2ξ(1+13ξ2)4}

Hence,

dP~dM~r =

𝓂surf6(μeμc)12{2ξ(1+13ξ2)4}𝓂surf(μeμc)2(π23)1/2{13ξ2(1+13ξ2)5/2}

  =

𝓂surf7(μeμc)14(2π33)1/21ξ(1+13ξ2)3/2.

For comparison, in hydrostatic balance we expect …

dPdMr=dPdrdrdMr

=

GMrρr214πr2ρ=GMr4πr4

dP~dM~r=[dPdMr][Kc10G9Mtot6]Mtot

=

GMr4πr4[Kc10G9Mtot7]

 

=

M~r4πr4[Kc10G10Mtot8]

 

=

M~r4πr~4

 

=

14π𝓂surf1(μeμc)2(23π)1/2[ξ3(1+13ξ2)3/2]{𝓂surf2(μeμc)4(32π)1/2ξ}4

 

=

{𝓂surf7(μeμc)14(22π232)}14π(23π)1/2[1ξ(1+13ξ2)3/2]

 

=

{𝓂surf7(μeμc)14}(2π33)1/2[1ξ(1+13ξ2)3/2].

This matches our earlier expression, as it should.

Takeaway Expression

dP~dM~r

=

M~r4πr~4

Now, for the envelope we find that,

Example Models Along BiPolytrope Sequence 0.3100

For the case of (nc,ne)=(5,1) and μe/μc=0.3100, we consider here the examination of models with three relatively significant values of the core/envelope interface:

  • Model D (ξi,ρ¯/ρc,q,ν)(2.06061,1.1931E+02,0.16296,0.13754): Approximate location along the sequence of the model with the maximum fractional core radius.
  • Model C (ξi,ρ¯/ρc,q,ν)(2.69697,3.0676E+02,0.15819,0.19161): Approximate location along the sequence of the onset of fundamental-mode instability.
  • Model A (ξi,ρ¯/ρc,q,ν)(9.0149598,1.1664E+06,0.075502255,0.337217006): Exact location along the sequence of the model with the maximum fractional core mass.

Model C

Here we examine a discrete representation of a model along the μe/μc=0.31 sequence whose core/envelope interface is located a ξi=2.69697.

See Also

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