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===Nonrotating, Oblate-Spheroidal Collapse=== The analogous collapse from rest of a nonrotating, uniform-density, oblate spheroid with equatorial radius, <math>~\varpi_\mathrm{eq}(t)</math>, and polar radius, <math>~Z_p(t)</math>, is governed by the equations, <div align="center"> <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~\frac{d^2 \varpi_\mathrm{eq}}{dt^2}</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ -~\frac{\partial\Phi}{\partial \varpi} \biggr|_{\varpi_{eq}} \, , </math> </td> </tr> <tr> <td align="right"> <math>~\frac{d^2 Z_\mathrm{p}}{dt^2}</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ -~\frac{\partial\Phi}{\partial Z} \biggr|_{Z_{p}} \, , </math> </td> </tr> </table> </div> where, to within an additive constant, <div align="center"> <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~\Phi(\varpi,Z)</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ \pi G \rho [ A_1(e) \varpi^2 + A_3(e) Z^2] \, . </math> </td> </tr> </table> </div> We should clarify and emphasize that this expression for the time-dependent gravitational potential has been written in terms of the (time-varying) eccentricity of the spheroid, <math>~e</math>, as measured in the meridional plane. Specifically, <div align="center"> <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~e </math> </td> <td align="center"> <math>~\equiv</math> </td> <td align="left"> <math>~ \biggl( 1 - \frac{Z_p^2}{\varpi_\mathrm{eq}^2} \biggr)^{1/2} </math> </td> </tr> <tr> <td align="right"> <math>~\Rightarrow~~~~~ Z_p</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ \varpi_\mathrm{eq} \biggl( 1 - e^2 \biggr)^{1/2} \, , </math> </td> </tr> </table> </div> and, as is derived in our accompanying discussion of the [[ThreeDimensionalConfigurations/HomogeneousEllipsoids#Oblate_Spheroids_.28a1_.3D_a2_.3E_a3.29|properties of homogeneous ellipsoids]], <table align="center" border=0 cellpadding="3"> <tr> <td align="right"> <math> ~A_1(e) </math> </td> <td align="center"> <math> ~= </math> </td> <td align="left"> <math> ~\frac{1}{e^2} \biggl[ \frac{\sin^{-1}e}{e} - (1-e^2)^{1/2} \biggr] (1-e^2)^{1/2} \, , </math> </td> </tr> <tr> <td align="right"> <math> ~A_3(e) </math> </td> <td align="center"> <math> ~= </math> </td> <td align="left"> <math> ~\frac{2}{e^2} \biggl[ (1-e^2)^{-1/2} - \frac{\sin^{-1}e}{e} \biggr] (1-e^2)^{1/2} \, . </math> </td> </tr> </table> Hence, <table align="center" border=0 cellpadding="3"> <tr> <td align="right"> <math> ~\nabla\Phi </math> </td> <td align="center"> <math> ~= </math> </td> <td align="left"> <math> ~2\pi G \rho \biggl[ \hat{e}_\varpi A_1(e) + \hat{e}_Z A_3(e) Z \biggr] \, , </math> </td> </tr> </table> and the pair of governing dynamical equations become, <div align="center"> <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~\frac{d^2 \varpi_\mathrm{eq}}{dt^2}</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ - 2\pi G \rho A_1(e) \varpi_\mathrm{eq} = - \frac{3}{2} \biggl[ \frac{GM}{\varpi_\mathrm{eq} Z_\mathrm{p}} \biggr] A_1(e) \, , </math> </td> </tr> <tr> <td align="right"> <math>~\frac{d^2 Z_\mathrm{p}}{dt^2}</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ - 2\pi G \rho A_3(e) Z_\mathrm{p} = - \frac{3}{2} \biggl[ \frac{GM}{\varpi_\mathrm{eq}^2} \biggr] A_3(e) \, , </math> </td> </tr> </table> </div> where we have used the relation that is valid for uniform-density, oblate spheoids, <div align="center"> <math> ~\rho = \frac{3M}{4\pi \varpi_\mathrm{eq}^2 Z_\mathrm{p}} \, . </math> </div>
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