ParabolicDensity/GravPot

Parabolic Density Distribution

Part I:   Gravitational Potential

Part II:   Spherical Structures

Part III:   Axisymmetric Equilibrium Structures

Part IV:   Triaxial Equilibrium Structures (Exploration)

Gravitational Potential

Setup

In an accompanying chapter titled, Properties of Homogeneous Ellipsoids (1), we have shown how analytic expressions may be derived for the gravitational potential inside of uniform-density ellipsoids. In that discussion, we largely followed the derivations of [EFE]. In the latter part of the nineteenth-century, 📚 N. M. Ferrers (1877, Quart. J. Pure Appl. Math., Vol. 14, pp. 1 - 22) showed that very similar analytic expressions can be derived for ellipsoids that have certain, specific inhomogeneous mass distributions. Here we specifically discuss the case of configurations that exhibit concentric ellipsoidal iso-density surfaces of the form,

$\rho$

=

${\rho }_c[1-(\frac{x^2}{a_1^2}+\frac{y^2}{a_2^2}+\frac{z^2}{a_3^2}\left)\right],$

that is, 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.

We begin by reminding the reader that, for a uniform-density configuration, the "interior" potential will be given by the expression,

${\mathrm{\Phi }}_{\mathrm{g}\mathrm{r}\mathrm{a}\mathrm{v}}(\mathbf{𝐱})$

=

$-\pi G{\rho }_c[I_{\mathrm{B}\mathrm{T}}{a}_1^2-(A_1{x}^2+A_2{y}^2+A_3{z}^2\left)\right].$

As we have shown in a separate presentation, if the three principal axes of the configuration are unequal in length and related to one another such that $a_1>a_2>a_3$, the appropriate expressions for the four leading coefficients are,

$A_1$	$=$	$\frac{2a_2{a}_3}{a_1^2}\left[\frac{F(\theta ,k)-E(\theta ,k)}{k^2{\sin }^3\theta }\right];$
$A_2$	$=$	$\frac{2a_2{a}_3}{a_1^2}\left[\frac{E(\theta ,k)-(1-k^2)F(\theta ,k)-(a_3/a_2)k^2\sin \theta }{k^2(1-k^2){\sin }^3\theta }\right];$
$A_3$	$=$	$\frac{2a_2{a}_3}{a_1^2}\left[\frac{(a_2/a_3)\sin \theta -E(\theta ,k)}{(1-k^2){\sin }^3\theta }\right];$
$I_{\mathrm{B}\mathrm{T}}$	$=$	$\frac{2a_2{a}_3}{a_1^2}\left[\frac{F(\theta ,k)}{\sin \theta }\right].$

[EFE], Chapter 3, Eqs. (33), (34) & (35)

As can readily be demonstrated, this scalar potential satisfies the differential form of the

Poisson Equation

${\mathrm{\nabla }}^2\mathrm{\Phi }=4\pi G\rho$

As we have also demonstrated, if the longest axis, $a_1$, and the intermediate axis, $a_2$, of the ellipsoid are equal to one another, then an equatorial cross-section of the object presents a circle of radius $a_1$ and the object is referred to as an oblate spheroid. For homogeneous oblate spheroids, evaluation of the integrals defining $A_i$ and $I_{\mathrm{B}\mathrm{T}}$ gives,

$A_1$	$=$	$\frac{1}{e^2}[\frac{{\sin }^{-1}e}{e}-(1-e^2{)}^{1/2}](1-e^2{)}^{1/2};$
$A_2$	$=$	$A_1;$
$A_3$	$=$	$\frac{2}{e^2}[(1-e^2{)}^{-1/2}-\frac{{\sin }^{-1}e}{e}](1-e^2{)}^{1/2};$
$I_{\mathrm{B}\mathrm{T}}$	$=$	$2A_1+A_3(1-e^2)=2(1-e^2{)}^{1/2}[\frac{{\sin }^{-1}e}{e}],$

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

where the eccentricity,

$e\equiv [1-(\frac{a_3}{a_1}{)}^2{]}^{1/2}.$

 

See Also