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

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===Finite-Difference Representation of Equilibrium State===
===Finite-Difference Representation of Equilibrium State===
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<div align="center"><font color="red"><b>CAUTION!</b></font> &nbsp; Regarding Our Chosen Lagrangian Fluid Marker</div>
If we were to use <math>\tilde{r}</math> as our primary Lagrangian fluid marker, we would be in a position to analytically specify the function, <math>\tilde{M}_r(\tilde{r})</math>.  Here, however, we will call upon <math>\tilde{M}_r</math> rather than <math>\tilde{r}</math> to serve as the primary Lagrangian fluid marker because mass facilitates our efforts to highlight a variety of important physical properties of bipolytropic configurations. We will therefore need to specify the function, <math>\tilde{r}(\tilde{M}_r)</math> instead of <math>\tilde{M}_r(\tilde{r})</math>.
For the core, this choice does not introduce any particularly difficult computational challenges because we can invert the <math>\tilde{M}_r(\tilde{r})</math> relationship analytically.  This is not the case for the envelope, however; we will not be able to analytically specify <math>\tilde{r}(\tilde{M}_r)</math>.  This is unfortunate, as a ''numerical'' (rather than analytic) specification will necessarily introduce additional errors into our solution of the displacement function &#8212; which already is a small and error-prone quantity.
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<font color="red"><b>STEP1:</b></font>&nbsp; &nbsp; Divide the core into <math>(N_c+1)</math> grid lines &#8212; that is, into <math>N_c</math> radial zones &#8212; associating the first "grid line" with the center of the core and the last grid line with the radial location of the core/envelope interface.  Choosing <math>0 \le \tilde{M}_r \le q</math> as the principal Lagrangian coordinate, and using the available analytic expressions, assign values to the following physical quantities at each grid line:
<font color="red"><b>STEP1:</b></font>&nbsp; &nbsp; Divide the core into <math>(N_c+1)</math> grid lines &#8212; that is, into <math>N_c</math> radial zones &#8212; associating the first "grid line" with the center of the core and the last grid line with the radial location of the core/envelope interface.  Choosing <math>0 \le \tilde{M}_r \le q</math> as the principal Lagrangian coordinate, and using the available analytic expressions, assign values to the following physical quantities at each grid line:

Revision as of 18:21, 20 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];
t~ t[Kc15G13Mtot10]1/4.

Note:  For an n = 5 polytrope (like our bipolytrope's core), the units of the polytropic constant, Kc, are [length13masstime10]1/5.

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,
B = ηiπ2+tan1(Λi),
ηs = π+B=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

Core

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

Envelope

Given that, for the envelope,

M~r

=

𝓂surf1θi1(2π)1/2A[sin(ηB)ηcos(ηB)],      and,

r~

=

𝓂surf2(μeμc)3θi2(2π)1/2η,

we deduce that,

dP~dM~r=M~r4πr~4

=

(14π)𝓂surf1θi1(2π)1/2A[ηcos(ηB)sin(ηB)][𝓂surf2(μeμc)3θi2(2π)1/2η]4

 

=

(124π22π24π4)1/2𝓂surf7θi7A[ηcos(ηB)sin(ηB)][(μeμc)12η4]

 

=

(2π)1/2𝓂surf7θi7(μeμc)12Aη4[ηcos(ηB)sin(ηB)]

As a cross-check …

dP~dη

=

𝓂surf6(μeμc)12θi6[2ϕdϕdη]

 

=

2𝓂surf6(μeμc)12θi6A2η3[ηcos(ηB)sin(ηB)]sin(ηB),

and,

dM~rdη

=

A𝓂surf1θi1(2π)1/2ddη[sin(ηB)ηcos(ηB)]

 

=

A𝓂surf1θi1(2π)1/2{ηsin(ηB)}.

That is,

dP~dM~r

=

2𝓂surf6(μeμc)12θi6A2η3[ηcos(ηB)sin(ηB)]sin(ηB){A𝓂surf1θi1(2π)1/2[ηsin(ηB)]}1

 

=

(2π)1/2𝓂surf7(μeμc)12θi7Aη4[ηcos(ηB)sin(ηB)].

Correct!

Time-Dependent Euler Equation

We begin with the form of the,

Euler Equation

dvrdt=1ρdPdrdΦdr

that is broadly relevant to studies of radial oscillations in spherically symmetric configurations. Recognizing from, for example, a related discussion that, vr=dr/dt, and that,

dΦdr = GMrr2

we obtain our

Desired Form of the Euler Equation

d2rdt2 = 1ρdPdrGMrr2.

Given as well that,

dMrdr=4πr2ρ

we see that,

dMr4πr2 = ρdr
d2rdt2 = 4πr2dPdMrGMrr2
14πr2d2rdt2 = dPdMrGMr4πr4.

Next, if as above, we multiply through by [Kc10G9Mtot7], we obtain the relevant,

Normalized Euler Equation

14πr~2d2r~dt~2 = dP~dM~rM~r4πr~4,

where, as a reminder, the dimensionless time is,

t~ t[Kc15G13Mtot10]1/4.

Finite-Difference Representation of Equilibrium State

CAUTION!   Regarding Our Chosen Lagrangian Fluid Marker

If we were to use r~ as our primary Lagrangian fluid marker, we would be in a position to analytically specify the function, M~r(r~). Here, however, we will call upon M~r rather than r~ to serve as the primary Lagrangian fluid marker because mass facilitates our efforts to highlight a variety of important physical properties of bipolytropic configurations. We will therefore need to specify the function, r~(M~r) instead of M~r(r~).

For the core, this choice does not introduce any particularly difficult computational challenges because we can invert the M~r(r~) relationship analytically. This is not the case for the envelope, however; we will not be able to analytically specify r~(M~r). This is unfortunate, as a numerical (rather than analytic) specification will necessarily introduce additional errors into our solution of the displacement function — which already is a small and error-prone quantity.


STEP1:    Divide the core into (Nc+1) grid lines — that is, into Nc radial zones — associating the first "grid line" with the center of the core and the last grid line with the radial location of the core/envelope interface. Choosing 0M~rq as the principal Lagrangian coordinate, and using the available analytic expressions, assign values to the following physical quantities at each grid line:

  • Mass:     Set (Δm)c=ν/(Nc); then, for i=1thru(Nc+1), set mi=(i1)(Δm)c.

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

Tiled Menu

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