ParabolicDensity/Axisymmetric/Structure: Difference between revisions

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=====Potential at the Pole=====
=====Potential at the Pole=====
At the pole, <math>(\varpi, z) = (0, a_s)</math>.  Hence,
At the pole, <math>(\varpi, z) = (0, a_s)</math>.  Hence,


<table border="0" cellpadding="5" align="center">
<table border="0" cellpadding="5" align="center">
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<tr>
<tr>
   <td align="right">
   <td align="right">
<math>\phi_\mathrm{choice} </math>
<math>\phi_\mathrm{choice}\biggr|_\mathrm{mid} </math>
   </td>
   </td>
   <td align="center"><math>=</math></td>
   <td align="center"><math>=</math></td>
   <td align="left">
   <td align="left">
<math>
<math>
- \frac{1}{2}  A_{ss} a_\ell^2  \zeta^2   
- \frac{1}{2}  A_{ss} a_\ell^2  \biggl(\frac{a_s^2}{a_\ell^2}\biggr)^2   
+ \biggl[ A_s - A_{\ell s}a_\ell^2 \biggl( \frac{\varpi^2 }{a_\ell^2}\biggr)\biggr]\zeta
+ \biggl[ A_s - A_{\ell s}a_\ell^2 \cancelto{0}{\biggl( \frac{\varpi^2 }{a_\ell^2}\biggr)}\biggr]\biggl(\frac{a_s^2}{a_\ell^2}\biggr)
+
+
A_\ell \biggl(\frac{\varpi^2}{a_\ell^2}\biggr)   
A_\ell \cancelto{0}{\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)
- \frac{1}{2} A_{\ell \ell} a_\ell^2  \cancelto{0}{\biggl(\frac{\varpi^4}{a_\ell^4}\biggr)}
\, .  
</math>
  </td>
</tr>
 
<tr>
  <td align="right">
&nbsp;
  </td>
  <td align="center"><math>=</math></td>
  <td align="left">
<math>
A_s \biggl(\frac{a_s^2}{a_\ell^2}\biggr)
- \frac{1}{2}  A_{ss} a_\ell^2  \biggl(\frac{a_s^2}{a_\ell^2}\biggr)^2 \, .
</math>
</math>
   </td>
   </td>
</tr>
</tr>
</table>
</table>


=====General Determination of Vertical Coordinate (&zeta;)=====
=====General Determination of Vertical Coordinate (&zeta;)=====

Revision as of 19:26, 7 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+y2aℓ2+z2as2)],

that is, axisymmetric (am=aℓ, 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=aℓ — 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)

=

12IBTaℓ2−[Aℓ(x2+y2)+Asz2]+[Aℓℓx2y2+Aℓsx2z2+Aℓsy2z2]+16[3Aℓℓx4+3Aℓℓy4+3Assz4]

 

=

12IBTaℓ2−[Aℓϖ2+Asz2]+[Aℓℓx2y2+Aℓsϖ2z2]+12[Aℓℓ(x4+y4)+Assz4]

 

=

12IBTaℓ2−[Aℓϖ2+Asz2]+Aℓℓ2[(x2+y2)2]+12[Assz4]+[Aℓsϖ2z2]

 

=

12IBTaℓ2−[Aℓϖ2+Asz2]+Aℓℓ2[ϖ4]+12[Assz4]+[Aℓsϖ2z2]

⇒Φgrav(𝐱)(−πGρcaℓ2)

=

12IBT−[Aℓ(ϖ2aℓ2)+As(z2aℓ2)]+12[Aℓℓaℓ2(ϖ4aℓ4)+Assaℓ2(z4aℓ4)+2Aℓsaℓ2(ϖ2z2aℓ4)].

Index Symbol Expressions

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

IBT =

2Aℓ+As(1−e2)=2(1−e2)1/2[sin−1ee];

Aℓ

=

1e2[sin−1ee−(1−e2)1/2](1−e2)1/2;

As =

2e2[(1−e2)−1/2−sin−1ee](1−e2)1/2,

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

where the eccentricity,

e≡[1−(asaℓ)2]1/2.

The relevant 2nd-order index symbol expressions are:

aℓ2Aℓℓ

=

14e4{−(3+2e2)(1−e2)+3(1−e2)1/2[sin−1ee]};

32aℓ2Ass

=

(4e2−3)e4(1−e2)+3(1−e2)1/2e4[sin−1ee];

aℓ2Aℓs

=

1e4{(3−e2)−3(1−e2)1/2[sin−1ee]}.

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

Aℓs

=

−Aℓ−As(aℓ2−as2)

⇒aℓ2Aℓs

=

1e2{As−Aℓ}

 

=

1e2{2e2[(1−e2)−1/2−sin−1ee](1−e2)1/2−1e2[sin−1ee−(1−e2)1/2](1−e2)1/2}

 

=

1e4{[2−2(1−e2)1/2sin−1ee]−[(1−e2)1/2sin−1ee−(1−e2)]}

 

=

1e4{(3−e2)−3(1−e2)1/2sin−1ee}.

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−[ϖ2aℓ2+z2as2]=0

⇒ϖ2aℓ2+z2as2

=

1

⇒z2

=

as2[1−ϖ2aℓ2]=aℓ2(1−e2)[1−ϖ2aℓ2]

⇒zaℓ

=

±(1−e2)1/2[1−ϖ2aℓ2]1/2,

        for 0≤|ϖ|aℓ≤1.
Expression for Gravitational Potential

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

ϕchoice≡Φgrav(𝐱)(πGρcaℓ2)+12IBT

=

[Aℓ(ϖ2aℓ2)+As(z2aℓ2)]−12[Aℓℓaℓ2(ϖ4aℓ4)+Assaℓ2(z4aℓ4)+2Aℓsaℓ2(ϖ2z2aℓ4)].

Letting,

ζ≡z2aℓ2,

we can rewrite this expression for ϕchoice as,

ϕchoice

=

Aℓ(ϖ2aℓ2)+Asζ−12Aℓℓaℓ2(ϖ4aℓ4)−12Assaℓ2ζ2−Aℓsaℓ2(ϖ2aℓ2)ζ

 

=

−12Assaℓ2ζ2+[As−Aℓsaℓ2(ϖ2aℓ2)]ζ+Aℓ(ϖ2aℓ2)−12Aℓℓaℓ2(ϖ4aℓ4).

Potential at the Pole

At the pole, (ϖ,z)=(0,as). Hence,

ϕchoice|mid

=

−12Assaℓ2(as2aℓ2)2+[As−Aℓsaℓ2(ϖ2aℓ2)0](as2aℓ2)+Aℓ(ϖ2aℓ2)0−12Aℓℓaℓ2(ϖ4aℓ4)0

 

=

As(as2aℓ2)−12Assaℓ2(as2aℓ2)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

≡

12Assaℓ2

 

=

13{(4e2−3)e4(1−e2)+3(1−e2)1/2e4[sin−1ee]},

β

≡

Aℓsaℓ2(ϖ2aℓ2)−As

 

=

1e4{(3−e2)−3(1−e2)1/2sin−1ee}(ϖ2aℓ2)−2e2[(1−e2)−1/2−sin−1ee](1−e2)1/2,

γ

≡

ϕchoice+12Aℓℓaℓ2(ϖ4aℓ4)−Aℓ(ϖ2aℓ2)

 

=

ϕchoice+18e4{−(3+2e2)(1−e2)+3(1−e2)1/2[sin−1ee]}(ϖ4aℓ4)−1e2[sin−1ee−(1−e2)1/2](1−e2)1/2(ϖ2aℓ2).

The solution of this quadratic equation gives,

ζ

=

12α{−β±[β2−4αγ]1/2}.

Given that in this physical system, ζ=z2/aℓ2 must be positive, we must choose the superior root. We conclude therefore that,

z2aℓ2

=

12α{[β2−4αγ]1/2−β}.

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 …

asaℓ=0.582724, e=0.81267,  
Aℓ=Am=0.51589042, As=0.96821916, IBT=1.360556,
aℓ2Aℓℓ=0.3287756, aℓ2Ass=1.5066848, aℓ2Aℓs=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

=

Aℓ−12Aℓℓaℓ2=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

=

−12Assaℓ2ζ20+[As−Aℓsaℓ2(ϖ2aℓ2)]ζ0+Aℓ(ϖ2aℓ2)−12Aℓℓaℓ2(ϖ4aℓ4)

⇒0

=

12Aℓℓaℓ2χ2−Aℓχ+ϕchoice,

where,

χ≡ϖ2aℓ2.

The solution to this quadratic equation gives,

χ

=

1Aℓℓaℓ2{Aℓ±[Aℓ2−2Aℓℓaℓ2ϕchoice]1/2}

 

=

AℓAℓℓaℓ2{1±[1−2Aℓℓaℓ2ϕchoiceAℓ2]1/2}

See Also

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