SSC/Stability/BiPolytropes/RedGiantToPN/Pt4: Difference between revisions
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<font color="orange"><b>B:</b></font> Divide the radial coordinate grid into 99 spherical shells <math>\Rightarrow~ \Delta_r = [(r_0)_\mathrm{surf} - (r_0)_\mathrm{int}]/99.</math> Then tabulate 100 values of <math>(r_0)_i, \eta_i, (Q_1)_i = [1 - \eta\cot(\eta-B) ]_i</math>. | <font color="orange"><b>B:</b></font> Divide the radial coordinate grid into 99 spherical shells <math>\Rightarrow~ \Delta_r = [(r_0)_\mathrm{surf} - (r_0)_\mathrm{int}]/99.</math> Then tabulate 100 values of <math>(r_0)_i, \eta_i, (Q_1)_i = [1 - \eta\cot(\eta-B) ]_i</math>. | ||
Generally speaking, after multiplying through by <math>r_0^2</math>, the finite-difference representation of the envelope's LAWE takes the form, | |||
<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> | |||
r_0^2\biggl[\frac{x_+ - 2x_i + x_-}{\Delta_r^2}\biggr] | |||
+ \biggl[4 - 2 Q_1 \biggr] r_0 \biggl[\frac{x_+ - x_-}{2 \Delta_r}\biggr] | |||
- \biggl[2 Q_1 \biggr] x_i | |||
</math> | |||
</td> | |||
</tr> | |||
<tr> | |||
<td align="right"> | |||
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</td> | |||
<td align="center"> | |||
<math>=</math> | |||
</td> | |||
<td align="left"> | |||
<math> | |||
x_+ \biggl\{ \frac{r_0^2}{\Delta_r^2} + (4-2Q_1)\frac{r_0}{2 \Delta_r} \biggr\} | |||
+ | |||
x_i \biggl\{- \frac{2r_0^2}{\Delta_r^2} - 2Q_1 \biggr\} | |||
+ | |||
x_- \biggl\{ \frac{r_0^2}{\Delta_r^2} - (4-2Q_1) \frac{r_0}{2 \Delta_r} \biggr\} | |||
</math> | |||
</td> | |||
</tr> | |||
</table> | |||
Solving for <math>x_+</math> … | |||
===Steps=== | ===Steps=== | ||
Revision as of 18:24, 5 February 2026
Main Sequence to Red Giant to Planetary Nebula
Part I: Background & Objective
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Part II:
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Part III:
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Part IV:
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Succinct
Generic
may also be written as …
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In shorthand, we can rewrite this equation in the form,
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where,
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and |
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and,
and,
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Specific Polytropes
In a separate discussion, we have shown that configurations with a polytropic equation of state exhibit a characteristic length scale that is given by the expression,
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and, once the dimensionless polytropic temperature, , is known, the radial dependence of key physical variables is given by the expressions,
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if, as in a separate discussion, and … |
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Combining variable expressions from the above right-hand column, we find that for polytropes,
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More generally, combining variable expressions from the above left-hand column, we find,
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As a result, for polytropes we can write,
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Finally, multiplying through by — which everywhere converts to — gives, what we will refer to as the,
BiPolytrope
Let's stick with the dimensional version and set , in which case the Polytropic LAWE is,
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Core (n = 5)
For the core, we know that . Hence,
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Now, given that,
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we can everywhere make the substitution,
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Note, also, that throughout the core, the relevant LAWE is,
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Next, try the solution,
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in which case,
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Setting gives the desired result, namely,
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Envelope (n = 1)
From the variable expressions in the right-hand column of Step 8 of the construction chapter,
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For the envelope, we know from separate work that,
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Numerical Integration Through Envelope
Finite-Difference Expressions
The discussion in this subsection is guided by our previous attempt at numerical integration.
Here, we focus on the LAWE that is relevant to the envelope, namely,
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where we have plugged in the values, . Using the general finite-difference approach described separately, we make the substitutions,
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and, |
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which will provide an approximate expression for , given the values of and .
A: Pick ; this will give analytic expressions for , , and for , as well as analytic expressions for and .
B: Divide the radial coordinate grid into 99 spherical shells Then tabulate 100 values of .
Generally speaking, after multiplying through by , the finite-difference representation of the envelope's LAWE takes the form,
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Solving for …
Steps
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STEP 1: Specify the interface location from the perspective of the core; that is, specify , in which case,
STEP 2: Adopting the normalization , determine numerous additional equilibrium properties at the interface, such as …
STEP 3: Throughout the core — that is, at all radial positions, — the displacement amplitude and its first and second derivatives, respectively, are given by the expressions,
STEP #4: From the determination of the logarithmic slope of the displacement function at the edge of the core — i.e., at the core-envelope interface — determine the slope as viewed from the perspective of the envelope.
†This analytically determined value matches the previous determination that was obtained via numerical integration of the LAWE. | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Throughout the envelope — that is, over the range, — the radial coordinate, , is a linear function of and takes on values given by the expression,
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(0.769211186 × η) |
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Here we examine some of the properties of the fundamental-mode eigenfunctions that we have found are associated with marginally unstable, bipolytropes.
| Figure 5 |
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Consider the model on the sequence for which ; key properties of this specific equilibrium model are enumerated in the first row of numbers provided in Table 2, above. Figure 5 shows how our numerically derived, fundamental-mode eigenfunction, , varies with the fractional radius over the entire range, . By prescription, the eigenfunction has a value of unity and a slope of zero at the center . Integrating the LAWE outward from the center, through the model's core (blue curve segment), drops smoothly to the value at the interface . Our numerical integration of the LAWE showed that, at the interface, the logarithmic slope of the core (blue) segment of the eigenfunction is,
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Next, following the above discussion of matching conditions at the interface, we determined that, from the perspective of the envelope, the slope of the eigenfunction at the interface must therefore be,
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Adopting this "env" slope along with the amplitude, , as the appropriate interface boundary conditions, we integrated the LAWE from the interface to the surface, obtaining the green-colored segment of the eigenfunction that is shown in Figure 5. The amplitude continued to steadily decrease, reaching a value of , at the model's surface . At the surface, this envelope (green) segment of the eigenfunction exhibits a logarithmic slope that matches to eight significant digits the value that is expected from astrophysical arguments for this marginally unstable model, namely,
Related Discussions
- Instability Onset Overview
- Analytic
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Appendices: | VisTrailsEquations | VisTrailsVariables | References | Ramblings | VisTrailsImages | myphys.lsu | ADS | |