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====Repeating Key Relations==== <table border="0" cellpadding="5" align="center"> <tr> <td align="left"><font color="orange"><b>Density:</b></font></td> <td align="right"> <math>\frac{\rho(\varpi, z)}{\rho_c}</math> </td> <td align="center"> <math>=</math> </td> <td align="left"> <math> \biggl[1 - \chi^2 - \zeta^2(1-e^2)^{-1} \biggr] \, ,</math> </td> </tr> <tr> <td align="left"><font color="orange"><b>Gravitational Potential:</b></font></td> <td align="right"> <math>\frac{ \Phi_\mathrm{grav}(\varpi,z)}{(-\pi G\rho_c a_\ell^2)} </math> </td> <td align="center"> <math>=</math> </td> <td align="left"> <math> \frac{1}{2} I_\mathrm{BT} - A_\ell \chi^2 - A_s \zeta^2 + \frac{1}{2}\biggl[(A_{s s} a_\ell^2) \zeta^4 + 2(A_{\ell s}a_\ell^2 )\chi^2 \zeta^2 + (A_{\ell \ell} a_\ell^2) \chi^4 \biggr] \, . </math> </td> </tr> </tr> <tr> <td align="left"><font color="orange"><b>Vertical Pressure Gradient:</b></font></td> <td align="right"><math>\biggl[\frac{1}{(\pi G\rho_c^2 a_\ell^2)} \biggr] \frac{\partial P}{\partial \zeta}</math></td> <td align="center"><math>=</math></td> <td align="left"> <math> \frac{\rho}{\rho_c} \cdot \biggl[ 2A_{\ell s}a_\ell^2 \chi^2\zeta - 2A_s \zeta + 2A_{ss} a_\ell^2 \zeta^3 \biggr] </math> </td> </tr> </table> From the [[#Starting_Key_Relations|above (9<sup>th</sup> Try) examination]] of the vertical pressure gradient, we determined that a reasonably good approximation for the normalized pressure throughout the configuration is given by the expression, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"><math>\biggl[\frac{1}{(\pi G\rho_c^2 a_\ell^2)} \biggr] \int \biggl[\frac{\partial P}{\partial \zeta}\biggr] d\zeta </math></td> <td align="center"><math>=</math></td> <td align="left"> <math> \biggl[-A_s \zeta^2 + \frac{1}{2}A_{ss}a_\ell^2 \zeta^4 + \frac{1}{2}(1-e^2)^{-1}A_s\zeta^4 - \frac{1}{3}(1-e^2)^{-1}A_{ss} a_\ell^2 \zeta^6 \biggr]\chi^0 + \biggl[ A_{\ell s}a_\ell^2 \zeta^2 + A_s\zeta^2 - \frac{1}{2}A_{ss}a_\ell^2 \zeta^4 - \frac{1}{2}(1-e^2)^{-1}(A_{\ell s}a_\ell^2 \zeta^4 ) \biggr]\chi^2 + \biggl[- A_{\ell s}a_\ell^2 \zeta^2 \biggr]\chi^4 + ~\mathrm{const.} </math> </td> </tr> </table> If we set <math>\chi = 0</math> — that is, if we look along the vertical axis — this approximation should be particularly good, resulting in the expression, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"><math>P_z \equiv \biggl\{ \biggl[\frac{1}{(\pi G\rho_c^2 a_\ell^2)} \biggr] \int \biggl[\frac{\partial P}{\partial \zeta}\biggr] d\zeta \biggr\}_{\chi=0}</math></td> <td align="center"><math>=</math></td> <td align="left"> <math>P_c^* - A_s \zeta^2 + \frac{1}{2}A_{ss}a_\ell^2 \zeta^4 + \frac{1}{2}(1-e^2)^{-1}A_s\zeta^4 - \frac{1}{3}(1-e^2)^{-1}A_{ss} a_\ell^2 \zeta^6 \, . </math> </td> </tr> </table> <table border="1" align="center" cellpadding="8" width="80%"><tr><td align="left"> Note that in the limit that <math>z \rightarrow a_s</math> — that is, at the pole along the vertical (symmetry) axis where the <math>P_z</math> should drop to zero — we should set <math>\zeta \rightarrow (1 - e^2)^{1 / 2}</math>. This allows us to determine the central pressure. <table border="0" cellpadding="5" align="center"> <tr> <td align="right"><math>P_c^* </math></td> <td align="center"><math>=</math></td> <td align="left"> <math>A_s (1-e^2) - \frac{1}{2}A_{ss}a_\ell^2 (1-e^2)^2 - \frac{1}{2}(1-e^2)^{-1}A_s(1-e^2)^2 + \frac{1}{3}(1-e^2)^{-1}A_{ss} a_\ell^2 (1-e^2)^3 </math> </td> </tr> <tr> <td align="right"> </td> <td align="center"><math>=</math></td> <td align="left"> <math>A_s (1-e^2) - \frac{1}{2}A_s(1-e^2) + \frac{1}{3}A_{ss} a_\ell^2 (1-e^2)^2 - \frac{1}{2}A_{ss}a_\ell^2 (1-e^2)^2 </math> </td> </tr> <tr> <td align="right"> </td> <td align="center"><math>=</math></td> <td align="left"> <math>\frac{1}{2}A_s(1-e^2) - \frac{1}{6}A_{ss} a_\ell^2 (1-e^2)^2 \, . </math> </td> </tr> </table> </td></tr></table> This means that, along the vertical axis, the pressure gradient is, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"><math>P_z \equiv \biggl\{ \biggl[\frac{1}{(\pi G\rho_c^2 a_\ell^2)} \biggr] \int \biggl[\frac{\partial P}{\partial \zeta}\biggr] d\zeta \biggr\}_{\chi=0}</math></td> <td align="center"><math>=</math></td> <td align="left"> <math>P_c^* - A_s \zeta^2 + \frac{1}{2}A_{ss}a_\ell^2 \zeta^4 + \frac{1}{2}(1-e^2)^{-1}A_s\zeta^4 - \frac{1}{3}(1-e^2)^{-1}A_{ss} a_\ell^2 \zeta^6 \, . </math> </td> </tr> </table> <table border="0" cellpadding="5" align="center"> <tr> <td align="right"><math>\frac{\partial P_z}{\partial\zeta}</math></td> <td align="center"><math>=</math></td> <td align="left"> <math>- 2A_s \zeta + 2A_{ss}a_\ell^2 \zeta^3 + 2(1-e^2)^{-1}A_s\zeta^3 - 2(1-e^2)^{-1}A_{ss} a_\ell^2 \zeta^5 \, . </math> </td> </tr> </table> This should match the more general "<font color="orange">vertical pressure gradient</font>" expression when we set, <math>\chi=0</math>, that is, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"><math>\biggl\{ \biggl[\frac{1}{(\pi G\rho_c^2 a_\ell^2)} \biggr] \frac{\partial P}{\partial \zeta} \biggr\}_{\chi=0}</math></td> <td align="center"><math>=</math></td> <td align="left"> <math> \biggl[ 1 - \cancelto{0}{\chi^2} - \zeta^2(1-e^2)^{-1}\biggr]\cdot \biggl[ 2A_{\ell s}a_\ell^2 \zeta \cancelto{0}{\chi^2} - 2A_s \zeta + 2A_{ss} a_\ell^2 \zeta^3 \biggr] </math> </td> </tr> <tr> <td align="right"> </td> <td align="center"><math>=</math></td> <td align="left"> <math> \biggl[- 2A_s \zeta + 2A_{ss} a_\ell^2 \zeta^3 \biggr] + \zeta^2(1-e^2)^{-1} \biggl[2A_s \zeta - 2A_{ss} a_\ell^2 \zeta^3 \biggr] </math> </td> </tr> </table> <b><font color="red">Yes! The expressions match!</font></b>
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