ParabolicDensity/Axisymmetric/Structure: Difference between revisions

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\biggr]
\biggr]
\biggr\}  
\biggr\}  
</math>
-
  </td>
H_c h(\xi) \, .
</tr>
 
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">&nbsp;</td>
  <td align="left">
<math>
- H_c h
</math>
</math>
   </td>
   </td>
Line 1,159: Line 1,149:


</td></tr></table>
</td></tr></table>
Adopting this last expression for the enthalpy, we have,
<table border="0" cellpadding="5" align="center">
<tr>
  <td align="right">
<math>\frac{h(\xi_1)}{h_0}</math>
  </td>
  <td align="center">
<math>=</math>
  </td>
  <td align="left">
<math>
1 -
h_2 a_s^2\biggl[ \biggl(\frac{z}{a_s}\biggr)^2 + \biggl(\frac{\varpi}{a_\ell}\biggr)^2\biggr]
-
h_4 a_s^4 \biggl[ \biggl(\frac{z}{a_s}\biggr)^4
+ 2\biggl(\frac{z}{a_s}\biggr)^2\biggl(\frac{\varpi}{a_\ell}\biggr)^2
+ \biggl(\frac{\varpi}{a_\ell}\biggr)^4 \biggr]
\, .
</math>
  </td>
</tr>
</table>
Hence,
<table border="0" cellpadding="5" align="center">
<tr>
  <td align="right">
<math>\Psi(\varpi, z)</math>
  </td>
  <td align="center"><math>=</math></td>
  <td align="left">
<math>
C_B + \pi G \rho_c a_\ell^2\biggl\{
\frac{1}{2} I_\mathrm{BT} 
- \biggl[A_\ell \biggl(\frac{\varpi^2}{a_\ell^2}\biggr) + A_s \biggl( \frac{z^2}{a_\ell^2}\biggr) \biggr]
+ \frac{1}{2} \biggl[
A_{\ell \ell} a_\ell^2  \biggl(\frac{\varpi^4}{a_\ell^4}\biggr)
+ A_{ss} a_\ell^2  \biggl(\frac{z^4}{a_\ell^4}\biggr) 
+ 2A_{\ell s}a_\ell^2 \biggl( \frac{\varpi^2 z^2}{a_\ell^4}\biggr)
\biggr]
\biggr\}
</math>
  </td>
</tr>
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center">&nbsp;</td>
  <td align="left">
<math>
-
H_c h_0 \biggl\{
1 -
h_2 a_s^2\biggl[ \biggl(\frac{z}{a_s}\biggr)^2 + \biggl(\frac{\varpi}{a_\ell}\biggr)^2\biggr]
-
h_4 a_s^4 \biggl[ \biggl(\frac{z}{a_s}\biggr)^4
+ 2\biggl(\frac{z}{a_s}\biggr)^2\biggl(\frac{\varpi}{a_\ell}\biggr)^2
+ \biggl(\frac{\varpi}{a_\ell}\biggr)^4 \biggr]
\biggr\}
</math>
  </td>
</tr>
</table>
----


At the pole configuration &#8212; that is, when <math>(\varpi, z) = (0, a_s)</math> &#8212; we want the enthalpy to go to zero.  That means,
At the pole configuration &#8212; that is, when <math>(\varpi, z) = (0, a_s)</math> &#8212; we want the enthalpy to go to zero.  That means,

Revision as of 13:25, 11 August 2024

Parabolic Density Distribution


Part I:   Gravitational Potential

 


Part II:   Spherical Structures

 


Part III:   Axisymmetric Equilibrium Structures

 


Part IV:   Triaxial Equilibrium Structures (Exploration)

 

Axisymmetric (Oblate) Equilibrium Structures

Setup

Here we specifically discuss the case of configurations that exhibit concentric ellipsoidal iso-density surfaces of the form,

ρ

=

ρc[1(x2+y2a2+z2as2)],

that is, axisymmetric (am=a, i.e., oblate) configurations with parabolic density distributions. Much of our presentation, here, is drawn from our separate, detailed description of what we will refer to as Ferrers potential.

This can be rewritten in terms of T1 Coordinates. In particular, defining, qa/as and,

ξ1

[z2+(ϖq)2]1/2=as[(zas)2+(ϖa)2]1/2

ρρc

=

[1(ξ1as)2].

Because we expect contours of constant enthalpy (H) to coincide with contours of constant density in equilibrium configurations, we should expect to find that,

HHc

=

h(ξ1).

If the "radial" enthalpy profile resembles our derived spherical enthalpy profile, we should expect to find that,

h(ξ1)

h0[1h2ξ12h4ξ14]

1h(ξ1)h0

h2ξ12+h4ξ14

 

=

h2as2[(zas)2+(ϖa)2]+h4{as2[(zas)2+(ϖa)2]}2

 

=

h2as2[(zas)2+(ϖa)2]+h4as4[(zas)4+2(zas)2(ϖa)2+(ϖa)4]

Gravitational Potential

As we have detailed in an accompanying discussion, for an oblate-spheroidal configuration — that is, when as<am=a — the gravitational potential may be obtained from the expression,

Φgrav(𝐱)(πGρc)

=

12IBTa12(A1x2+A2y2+A3z2)+(A12x2y2+A13x2z2+A23y2z2)+16(3A11x4+3A22y4+3A33z4),

where, in the present context, we can rewrite this expression as,

Φgrav(𝐱)(πGρc)

=

12IBTa2[A(x2+y2)+Asz2]+[Ax2y2+Asx2z2+Asy2z2]+16[3Ax4+3Ay4+3Assz4]

 

=

12IBTa2[Aϖ2+Asz2]+[Ax2y2+Asϖ2z2]+12[A(x4+y4)+Assz4]

 

=

12IBTa2[Aϖ2+Asz2]+A2[(x2+y2)2]+12[Assz4]+[Asϖ2z2]

 

=

12IBTa2[Aϖ2+Asz2]+A2[ϖ4]+12[Assz4]+[Asϖ2z2]

Φgrav(𝐱)(πGρca2)

=

12IBT[A(ϖ2a2)+As(z2a2)]+12[Aa2(ϖ4a4)+Assa2(z4a4)+2Asa2(ϖ2z2a4)].

Index Symbol Expressions

The expression for the zeroth-order normalization term (IBT), and the relevant pair of 1st-order index symbol expressions are:

IBT =

2A+As(1e2)=2(1e2)1/2[sin1ee];

A

=

1e2[sin1ee(1e2)1/2](1e2)1/2;

As =

2e2[(1e2)1/2sin1ee](1e2)1/2,

[EFE], Chapter 3, Eq. (36)
[T78], §4.5, Eqs. (48) & (49)

where the eccentricity,

e[1(asa)2]1/2.

The relevant 2nd-order index symbol expressions are:

a2A

=

14e4{(3+2e2)(1e2)+3(1e2)1/2[sin1ee]};

32a2Ass

=

(4e23)e4(1e2)+3(1e2)1/2e4[sin1ee];

a2As

=

1e4{(3e2)3(1e2)1/2[sin1ee]}.

We can crosscheck this last expression by drawing on a shortcut expression,

As

=

AAs(a2as2)

a2As

=

1e2{AsA}

 

=

1e2{2e2[(1e2)1/2sin1ee](1e2)1/21e2[sin1ee(1e2)1/2](1e2)1/2}

 

=

1e4{[22(1e2)1/2sin1ee][(1e2)1/2sin1ee(1e2)]}

 

=

1e4{(3e2)3(1e2)1/2sin1ee}.

Meridional Plane Equi-Potential Contours

Here, we follow closely our separate discussion of equipotential surfaces for Maclaurin Spheroids, assuming no rotation.

Configuration Surface

In the meridional (ϖ,z) plane, the surface of this oblate-spheroidal configuration — identified by the thick, solid-black curve below, in Figure 1 — is defined by the expression,

ρρc

=

1[ϖ2a2+z2as2]=0

ϖ2a2+z2as2

=

1

z2

=

as2[1ϖ2a2]=a2(1e2)[1ϖ2a2]

za

=

±(1e2)1/2[1ϖ2a2]1/2,

        for 0|ϖ|a1.
Expression for Gravitational Potential

Throughout the interior of this configuration, each associated Φeff = constant, equipotential surface is defined by the expression,

ϕchoiceΦgrav(𝐱)(πGρca2)+12IBT

=

[A(ϖ2a2)+As(z2a2)]12[Aa2(ϖ4a4)+Assa2(z4a4)+2Asa2(ϖ2z2a4)].

Letting,

ζz2a2,

we can rewrite this expression for ϕchoice as,

ϕchoice

=

A(ϖ2a2)+Asζ12Aa2(ϖ4a4)12Assa2ζ2Asa2(ϖ2a2)ζ

 

=

12Assa2ζ2+[AsAsa2(ϖ2a2)]ζ+A(ϖ2a2)12Aa2(ϖ4a4).

Potential at the Pole

At the pole, (ϖ,z)=(0,as). Hence,

ϕchoice|mid

=

12Assa2(as2a2)2+[AsAsa2(ϖ2a2)0](as2a2)+A(ϖ2a2)012Aa2(ϖ4a4)0

 

=

As(as2a2)12Assa2(as2a2)2.

General Determination of Vertical Coordinate (ζ)

Given values of the three parameters, e, ϖ, and ϕchoice, this last expression can be viewed as a quadratic equation for ζ. Specifically,

0

=

αζ2+βζ+γ,

where,

α

12Assa2

 

=

13{(4e23)e4(1e2)+3(1e2)1/2e4[sin1ee]},

β

Asa2(ϖ2a2)As

 

=

1e4{(3e2)3(1e2)1/2sin1ee}(ϖ2a2)2e2[(1e2)1/2sin1ee](1e2)1/2,

γ

ϕchoice+12Aa2(ϖ4a4)A(ϖ2a2)

 

=

ϕchoice+18e4{(3+2e2)(1e2)+3(1e2)1/2[sin1ee]}(ϖ4a4)1e2[sin1ee(1e2)1/2](1e2)1/2(ϖ2a2).

The solution of this quadratic equation gives,

ζ

=

12α{β±[β24αγ]1/2}.

Should we adopt the superior (positive) sign, or is it more physically reasonable to adopt the inferior (negative) sign? As it turns out, β is intrinsically negative, so the quantity, β, is positive. Furthermore, when γ goes to zero, we need ζ to go to zero as well. This will only happen if we adopt the inferior (negative) sign. Hence, the physically sensible root of this quadratic relation is given by the expression,

ζ

=

12α{β[β24αγ]1/2}.


Here we present a quantitatively accurate depiction of the shape of the (Ferrers) gravitational potential that arises from oblate-spheroidal configurations having a parabolic density distribution. We closely follow the discussion of equi-gravitational potential contours that arise in (uniform-density) Maclaurin spheroids. In order to facilitate comparison with Maclaurin spheroids, we will focus on a model with …

asa=0.582724, e=0.81267,  
A=Am=0.51589042, As=0.96821916, IBT=1.360556,
a2A=0.3287756, a2Ass=1.5066848, a2As=0.6848975.

[NOTE:   Along the Maclaurin spheroid sequence, this is the eccentricity that marks bifurcation to the Jacobi ellipsoid sequence — see the first model listed in Table IV (p. 103) of [EFE] and/or see Tables 1 and 2 of our discussion of the Jacobi ellipsoid sequence. It is unlikely that this same eccentricity has a comparably special physical relevance along the sequence of spheroids having parabolic density distributions.]

The largest value of the gravitational potential that will arise inside (actually, on the surface) of the configuration is at (ϖ,z)=(1,0). That is, when,

ϕchoice|max

=

A12Aa2=0.3515026.

So we will plot various equipotential surfaces having, 0<ϕchoice<ϕchoice|max, recognizing that they will each cut through the equatorial plane (z=0) at the radial coordinate given by,

ϕchoice

=

12Assa2ζ20+[AsAsa2(ϖ2a2)]ζ0+A(ϖ2a2)12Aa2(ϖ4a4)

0

=

12Aa2χ2Aχ+ϕchoice,

where,

χϖ2a2.

The solution to this quadratic equation gives,

χeqplane

=

1Aa2{A±[A22Aa2ϕchoice]1/2}

 

=

AAa2{1[12Aa2ϕchoiceA2]1/2}.

Note that, again, the physically relevant root is obtained by adopting the inferior (negative) sign, as has been done in this last expression.

Equipotential Contours that Lie Entirely Within Configuration

For all 0<ϕchoiceϕchoice|mid, the equipotential contour will reside entirely within the configuration. In this case, for a given ϕchoice, we can plot points along the contour by picking (equally spaced?) values of χeqplaneχ0, then solve the above quadratic equation for the corresponding value of ζ.

In our example configuration, this means … (to be finished)

Hydrostatic Balance (Algebraic Condition)

Following our separate discussion of the equilibrium structure of Maclaurin spheroids, and given that our solution of the Poisson equation fixes the expression for Φgrav, the algebraic expression ensuring hydrostatic balance is,

H(ϖ,z)

=

CB[Φgrav(ϖ,z)+Ψ(ϖ,z)],

where, Ψ is the centrifugal potential. NOTE:   Generally when modeling axisymmetric astrophysical systems (see our accompanying discussion of simple rotation profiles) it is assumed that Ψ does not functionally depend on z. Here, our other constraints — for example, demanding that the configuration have a parabolic density distribution — may force us to adopt a z-dependent rotation profile.

Here, we know that the adopted parabolic density distribution gives rise to a gravitational potential of the form,

Φgrav(𝐱)(πGρca2)

=

12IBT[A(ϖ2a2)+As(z2a2)]+12[Aa2(ϖ4a4)+Assa2(z4a4)+2Asa2(ϖ2z2a4)].

Hence,

Ψ(ϖ,z)

=

CBΦgrav(ϖ,z)H(ϖ,z)

 

=

CB+πGρca2{12IBT[A(ϖ2a2)+As(z2a2)]+12[Aa2(ϖ4a4)+Assa2(z4a4)+2Asa2(ϖ2z2a4)]}Hch(ξ).


This can be rewritten in terms of T1 Coordinates. In particular, defining, qa/as and,

ξ1

[z2+(ϖq)2]1/2=as[(zas)2+(ϖa)2]1/2

ρρc

=

[1(ξ1as)2].

Because we expect contours of constant enthalpy (H) to coincide with contours of constant density in equilibrium configurations, we should expect to find that,

HHc

=

h(ξ1).

If the "radial" enthalpy profile resembles our derived spherical enthalpy profile, we should expect to find that,

h(ξ1)

h0[1h2ξ12h4ξ14]

1h(ξ1)h0

h2ξ12+h4ξ14

 

=

h2as2[(zas)2+(ϖa)2]+h4{as2[(zas)2+(ϖa)2]}2

 

=

h2as2[(zas)2+(ϖa)2]+h4as4[(zas)4+2(zas)2(ϖa)2+(ϖa)4]

Adopting this last expression for the enthalpy, we have,

h(ξ1)h0

=

1h2as2[(zas)2+(ϖa)2]h4as4[(zas)4+2(zas)2(ϖa)2+(ϖa)4].

Hence,

Ψ(ϖ,z)

=

CB+πGρca2{12IBT[A(ϖ2a2)+As(z2a2)]+12[Aa2(ϖ4a4)+Assa2(z4a4)+2Asa2(ϖ2z2a4)]}

 

 

Hch0{1h2as2[(zas)2+(ϖa)2]h4as4[(zas)4+2(zas)2(ϖa)2+(ϖa)4]}




At the pole configuration — that is, when (ϖ,z)=(0,as) — we want the enthalpy to go to zero. That means,

CB(πGρca2)

=

[Φgrav(ϖ,z)(πGρca2)+Ψ(ϖ,z)(πGρca2)]pole

 

=

[Ψ(ϖ,z)(πGρca2)]pole+12IBT[A(ϖ2a2)0+As(1e2)]+12[Aa2(ϖ4a4)0+Assa2(1e2)2+2Asa2(ϖ2z2a4)0]

 

=

[Ψ(ϖ,z)(πGρca2)]pole+12IBT[As(1e2)]+12[Assa2(1e2)2].

For centrally condensed configurations, it is astrophysically reasonable to assume that Φ(ϖ,z) is of the form such that the centrifugal potential goes to zero when ϖ0. Adopting that assumption here means,

CB(πGρca2)

=

12IBT[As(1e2)]+12[Assa2(1e2)2].

See Also

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