SSC/Stability/BiPolytropes/RedGiantToPN/Pt4: Difference between revisions
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if, as [[SSC/Stability/BiPolytropes/Pt3#Foundation|in a separate discussion]], <math>n=5</math> and <math>\theta = (1+\xi^2/3)^{-1 / 2}</math> … | if, as [[SSC/Stability/BiPolytropes/Pt3#Foundation|in a separate discussion]], <math>n=5</math> and <math>\theta = (1+\xi^2/3)^{-1 / 2}</math> … | ||
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<math>a_n \xi \, ,</math> | <math>a_n \xi \, ,</math> | ||
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<math>~\rho_c \theta^{n} \, ,</math> | <math>~\rho_c \theta^{n} \, ,</math> | ||
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Revision as of 14:51, 19 January 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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Notice that,
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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,
Related Discussions
- Instability Onset Overview
- Analytic
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Appendices: | VisTrailsEquations | VisTrailsVariables | References | Ramblings | VisTrailsImages | myphys.lsu | ADS | |