ParabolicDensity/Axisymmetric/Structure: Difference between revisions

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A_\ell   
A_\ell   
- \frac{1}{2} A_{\ell \ell} a_\ell^2 = 0.3515026 \,  .  
- \frac{1}{2} A_{\ell \ell} a_\ell^2 = 0.3515026 \,  .  
</math>
  </td>
</tr>
</table>
So we will plot various equipotential surfaces having, <math>0 < \phi_\mathrm{choice} < \phi_\mathrm{choice}|_\mathrm{max} </math>, recognizing that they will each cut through the equatorial plane <math>(z = 0)</math> at the radial coordinate given by,
<table border="0" cellpadding="5" align="center">
<tr>
  <td align="right">
<math>\phi_\mathrm{choice} </math>
  </td>
  <td align="center"><math>=</math></td>
  <td align="left">
<math>
- \frac{1}{2}  A_{ss} a_\ell^2  \zeta^2 
+ \biggl[ A_s - A_{\ell s}a_\ell^2 \biggl( \frac{\varpi^2 }{a_\ell^2}\biggr)\biggr]\zeta
+
A_\ell \biggl(\frac{\varpi^2}{a_\ell^2}\biggr) 
- \frac{1}{2} A_{\ell \ell} a_\ell^2  \biggl(\frac{\varpi^4}{a_\ell^4}\biggr)
\, .
</math>
</math>
   </td>
   </td>

Revision as of 17:41, 6 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

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.

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.

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.

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).

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}.

Given that in this physical system, ζ=z2/a2 must be positive, we must choose the superior root. We conclude therefore that,

z2a2

=

12α{[β24αγ]1/2β}.

But check this statement because it appears that β will sometimes be negative.

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 (and on the surface) of the configuration at (ϖ,z)=(1,0). That is, when,

α

12Assa2

β

Asa2As

γ

ϕchoice+12Aa2A



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

=

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

See Also

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