SSC/Stability/NeutralMode: Difference between revisions
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-\biggl(\frac{r_0^2}{b}\biggr)\frac{d^2 x_t}{dr_0^2} | -\biggl(\frac{r_0^2}{b}\biggr)\frac{d^2 x_t}{dr_0^2} | ||
-\biggl(\frac{r_0}{b}\biggr)\biggl[ 4 | -\biggl(\frac{r_0}{b}\biggr)\biggl[ 4 + \frac{d\ln P_0}{d\ln r_0}\biggr]\frac{dx_t}{dr_0} | ||
- \biggl(\frac{r_0^2}{b}\biggr) \biggl( \frac{\rho_0}{\gamma_g P_0}\biggr) | - \biggl(\frac{r_0^2}{b}\biggr) \biggl( \frac{\rho_0}{\gamma_g P_0}\biggr) | ||
\biggl[ (4-3\gamma_g)\frac{g_0}{r_0} + \sigma_c^2\biggl(\frac{2\pi G\rho_c}{3}\biggr)\biggr]x_t | \biggl[ (4-3\gamma_g)\frac{g_0}{r_0} + \sigma_c^2\biggl(\frac{2\pi G\rho_c}{3}\biggr)\biggr]x_t | ||
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<math>=</math> | |||
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<math> | |||
-\biggl(\frac{r_0^2}{b}\biggr)\frac{d^2 x_t}{dr_0^2} | |||
-\biggl(\frac{r_0}{b}\biggr)\biggl[ 4 + \frac{d\ln P_0}{d\ln r_0}\biggr]\frac{dx_t}{dr_0} | |||
+ \biggl(\frac{1}{b}\biggr) \frac{1}{\gamma_g} \biggl( \frac{d\ln P_0}{d \ln r_0}\biggr) | |||
(4-3\gamma_g)x_t | |||
- \biggl(\frac{r_0^2}{b}\biggr) \biggl( \frac{\rho_0}{\gamma_g P_0}\biggr) | |||
\biggl[ \sigma_c^2\biggl(\frac{2\pi G\rho_c}{3}\biggr)\biggr]x_t | |||
</math> | </math> | ||
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Revision as of 17:45, 3 September 2021
LAWE
Most General Form
In an accompanying discussion, we derived the so-called,
where the gravitational acceleration,
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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,
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Polytropic Configurations
Part 1
If the initial, unperturbed equilibrium configuration is a polytropic sphere whose internal structure is defined by the function, , that provides a solution to the,
then,
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where,
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Hence, after multiplying through by , the above adiabatic wave equation can be rewritten in the form,
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In addition, given that,
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and,
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we can write,
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where we have adopted the function notation,
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Part 2
Drawing from an accompanying discussion, we have the following:
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In order to reconcile with the "Part 1" expression, we note first that . We note as well that since,
we have,
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All physically reasonable solutions are subject to the inner boundary condition,
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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, , of a hot, tenuous external medium, then the solution to the LAWE is subject to the outer boundary condition,
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But, for isolated polytropes, the sought-after solution is subject to the more conventional boundary condition,
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Radial Pulsation Neutral Mode
The integro-differential version of the statement of hydrostatic balance is
From our separate discussion, we have found that,
| Exact Solution to the Polytropic LAWE | ||
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Let's rewrite the significant functional term in this expressions in terms of basic variables. That is,
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Let's adopt the following trial solution:
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Then we have,
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Given that,
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these expression can be rewritten as,
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and,
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Finally, plugging our trial radial displacement function, , into the LAWE gives,
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LAWE |
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See Also
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Appendices: | VisTrailsEquations | VisTrailsVariables | References | Ramblings | VisTrailsImages | myphys.lsu | ADS | |