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=LAWE= ==Most General Form== In an [[SSC/Perturbations#2ndOrderODE|accompanying discussion]], we derived the so-called, <div align="center" id="2ndOrderODE"> <font color="#770000">'''Adiabatic Wave''' (or ''Radial Pulsation'') '''Equation'''</font><br /> {{Math/EQ_RadialPulsation01}} </div> <!-- <div align="center" id="2ndOrderODE"> <font color="#770000">'''Adiabatic Wave Equation'''</font><br /> <math> \frac{d^2x}{dr_0^2} + \biggl[\frac{4}{r_0} - \biggl(\frac{g_0 \rho_0}{P_0}\biggr) \biggr] \frac{dx}{dr_0} + \biggl(\frac{\rho_0}{\gamma_\mathrm{g} P_0} \biggr)\biggl[\omega^2 + (4 - 3\gamma_\mathrm{g})\frac{g_0}{r_0} \biggr] x = 0 \, , </math> </div> --> where the [[SSC/Perturbations#g0|gravitational acceleration]], <table border="0" align="center" cellpadding="8"> <tr> <td align="right"><math>g_0</math></td> <td align="center"><math>\equiv</math></td> <td align="left"> <math> \frac{GM_r}{r_0^2} = - \frac{1}{\rho_0} \frac{dP_0}{dr_0} ~~~\Rightarrow ~~~ \frac{g_0\rho_0 r_0}{P_0} = - \frac{d\ln P_0}{d\ln r_0} \, . </math> </td> </tr> </table> The solution to this equation gives eigenfunctions that describe various radial modes of oscillation in spherically symmetric, self-gravitating fluid configurations. The boundary condition conventionally used in connection with the adiabatic wave equation is, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>r_0 \frac{d\ln x}{dr_0}</math> </td> <td align="center"> <math>=</math> </td> <td align="left"> <math>\frac{1}{\gamma_g} \biggl( 4 - 3\gamma_g + \frac{\omega^2 R^3}{GM_\mathrm{tot}}\biggr) </math> at <math>r_0 = R \, .</math> </td> </tr> </table> ==Polytropic Configurations== ===Part 1=== If the initial, unperturbed equilibrium configuration is a [[SSC/Structure/Polytropes#Polytropic_Spheres|polytropic sphere]] whose internal structure is defined by the function, <math>\theta(\xi)</math>, that provides a solution to the, <div align="center"> <span id="LaneEmdenEquation"><font color="#770000">'''Lane-Emden Equation'''</font></span> <br /> {{Math/EQ_SSLaneEmden01}} </div> then, <div align="center"> <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>r_0</math> </td> <td align="center"> <math>=</math> </td> <td align="left"> <math>a_n \xi \, ,</math> </td> </tr> <tr> <td align="right"> <math>\rho_0</math> </td> <td align="center"> <math>=</math> </td> <td align="left"> <math>\rho_c \theta^{n} \, ,</math> </td> </tr> <tr> <td align="right"> <math>P_0</math> </td> <td align="center"> <math>=</math> </td> <td align="left"> <math>K\rho_0^{(n+1)/n} = K\rho_c^{(n+1)/n} \theta^{n+1} \, ,</math> </td> </tr> <tr> <td align="right"> <math>g_0</math> </td> <td align="center"> <math>=</math> </td> <td align="left"> <math>\frac{GM(r_0)}{r_0^2} = \frac{G}{r_0^2} \biggl[ 4\pi a_n^3 \rho_c \biggl(-\xi^2 \frac{d\theta}{d\xi}\biggr) \biggr] \, ,</math> </td> </tr> </table> </div> where, <div align="center"> <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>a_n</math> </td> <td align="center"> <math>=</math> </td> <td align="left"> <math>\biggl[\frac{(n+1)K}{4\pi G} \cdot \rho_c^{(1-n)/n} \biggr]^{1/2} \, .</math> </td> </tr> </table> </div> Hence, after multiplying through by <math>~a_n^2</math>, the above adiabatic wave equation can be rewritten in the form, <div align="center"> <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~\frac{d^2x}{d\xi^2} + \biggl[\frac{4}{\xi} - \frac{g_0}{a_n}\biggl(\frac{a_n^2 \rho_0}{P_0}\biggr) \biggr] \frac{dx}{d\xi} + \biggl(\frac{a_n^2\rho_0}{\gamma_\mathrm{g} P_0} \biggr)\biggl[\omega^2 + (4 - 3\gamma_\mathrm{g})\frac{g_0}{a_n\xi} \biggr] x </math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~0 \, .</math> </td> </tr> </table> </div> In addition, given that, <div align="center"> <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~\frac{g_0}{a_n}</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~4\pi G \rho_c \biggl(-\frac{d \theta}{d\xi} \biggr) \, ,</math> </td> </tr> </table> </div> and, <div align="center"> <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~\frac{a_n^2 \rho_0}{P_0}</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~\frac{(n+1)}{(4\pi G\rho_c)\theta} = \frac{a_n^2 \rho_c}{P_c} \cdot \frac{\theta_c}{\theta}\, ,</math> </td> </tr> </table> </div> we can write, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>0 </math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>\frac{d^2x}{d\xi^2} + \biggl[\frac{4 - (n+1)V(\xi)}{\xi} \biggr] \frac{dx}{d\xi} + \biggl[\omega^2 \biggl(\frac{a_n^2 \rho_c }{\gamma_g P_c} \biggr) \frac{\theta_c}{\theta} - \biggl(3-\frac{4}{\gamma_g}\biggr) \cdot \frac{(n+1)V(x)}{\xi^2} \biggr] x </math> </td> </tr> <tr> <td align="right"> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>\frac{d^2x}{d\xi^2} + \biggl[\frac{4 - (n+1)V(\xi)}{\xi} \biggr] \frac{dx}{d\xi} + (n+1)\biggl[\omega^2 \biggl(\frac{a_n^2 \rho_c }{\gamma_g P_c} \biggr) \frac{\xi^2 \theta_c}{(n+1)\theta} - \biggl(3-\frac{4}{\gamma_g}\biggr) \cdot V(x) \biggr] \frac{x}{\xi^2} </math> </td> </tr> </table> where we have adopted the function notation, <div align="center"> <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>V(\xi)</math> </td> <td align="center"> <math>\equiv</math> </td> <td align="left"> <math>- \frac{\xi}{\theta} \frac{d \theta}{d\xi} \, .</math> </td> </tr> </table> </div> ===Part 2=== Drawing from an [[SSC/Stability/InstabilityOnsetOverview#Polytropic_Stability|accompanying discussion]], we have the following: <div align="center"> <font color="maroon"><b>Polytropic LAWE (linear adiabatic wave equation)</b></font><br /> {{ Math/EQ_RadialPulsation02 }} </div> <table border="1" align="center" width="80%" cellpadding="8"><tr><td align="left"> In order to reconcile with the "Part 1" expression, we note first that <math>V(\xi) \leftrightarrow Q(\xi)</math>. We note as well that since, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>\biggl(\frac{a_n^2 \rho_c }{P_c} \biggr)\theta_c</math> </td> <td align="center"> <math>=</math> </td> <td align="left"> <math>\frac{(n+1)}{4\pi G\rho_c}\, , </math> </td> </tr> </table> we have, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>\omega^2 \biggl(\frac{a_n^2 \rho_c }{\gamma_g P_c} \biggr) \frac{\xi^2 \theta_c}{(n+1)\theta}</math> </td> <td align="center"> <math>\leftrightarrow</math> </td> <td align="left"> <math> \frac{\omega^2}{\gamma_g} \biggl[\frac{(n+1)}{4\pi G\rho_c} \biggr] \frac{\xi^2 }{(n+1)\theta} = \frac{1}{6\gamma_g} \biggl[\frac{3\omega^2}{2\pi G\rho_c} \biggr] \frac{\xi^2 }{\theta} = \biggl( \frac{\sigma_c^2}{6\gamma_g}\biggr) \frac{\xi^2 }{\theta} \, . </math> </td> </tr> </table> </td></tr></table> All physically reasonable solutions are subject to the inner boundary condition, <div align="center"> <math>\frac{dx}{d\xi} = 0</math> at <math>\xi = 0 \, ,</math> </div> but the relevant outer boundary condition depends on whether the underlying equilibrium configuration is isolated (surface pressure is zero), or whether it is a "pressure-truncated" configuration. As is the case with the pressure-truncated isothermal spheres, discussed above, if the polytropic configuration is truncated by the pressure, <math>P_e</math>, of a hot, tenuous external medium, then the solution to the LAWE is subject to the outer boundary condition, <div align="center"> <math>-\frac{d\ln x}{d\ln\xi} = 3</math> at <math>\xi = \tilde\xi \, .</math> </div> But, for ''isolated'' polytropes, the sought-after solution is subject to the more conventional boundary condition, <div align="center"> <math>- \frac{d\ln x}{d\ln \xi} = \biggl(\frac{3-n}{n+1}\biggr) + \frac{n\sigma_c^2}{6(n+1)} \biggl[\frac{\xi}{\theta^'}\biggr] </math> at <math>\xi = \xi_\mathrm{surf} \, .</math><br /> </div>
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