SSC/Stability/BiPolytropes/RedGiantToPN/Pt4
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
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 .
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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 #4: | ||||||||||||||||||||||||||||||||||||||||||||
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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