SSC/Stability/BiPolytropes/RedGiantToPN/Pt4: Difference between revisions

From JETohlineWiki
Jump to navigation Jump to search
Joel2 (talk | contribs)
Joel2 (talk | contribs)
Line 134: Line 134:
and, once the dimensionless polytropic temperature, <math>\theta(\xi)</math>, is known, the radial dependence of key physical variables is given by the expressions,
and, once the dimensionless polytropic temperature, <math>\theta(\xi)</math>, is known, the radial dependence of key physical variables is given by the expressions,
<table border="0" cellpadding="5" align="center">
<table border="0" cellpadding="5" align="center">
<tr>
  <td align="center" colspan="3">&nbsp;</td>
  <td align="center" colspan="3">
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> &hellip;
  </td>
</tr>


<tr>
<tr>
Line 145: Line 151:
<math>a_n \xi \, ,</math>
<math>a_n \xi \, ,</math>
   </td>
   </td>
<td align="center">&nbsp; &nbsp; &nbsp; if, as in a [[SSC/Stability/BiPolytropes/Pt3#Foundation|separate discussion]], 
<math>n=5 ~~~~\Rightarrow</math></td>


   <td align="right">
   <td align="right">
<math>r_0</math>
&nbsp; &nbsp; &nbsp;<math>r_0</math>
   </td>
   </td>
   <td align="center">
   <td align="center">
Line 170: Line 173:
<math>~\rho_c \theta^{n} \, ,</math>
<math>~\rho_c \theta^{n} \, ,</math>
   </td>
   </td>
<td align="center">&nbsp; &nbsp; &nbsp; <math>\Rightarrow</math></td>


   <td align="right">
   <td align="right">
<math>~\rho_0</math>
&nbsp; &nbsp; &nbsp;<math>\rho_0</math>
   </td>
   </td>
   <td align="center">
   <td align="center">
Line 195: Line 196:
<math>~K\rho_0^{(n+1)/n} = K\rho_c^{(n+1)/n} \theta^{n+1} \, ,</math>
<math>~K\rho_0^{(n+1)/n} = K\rho_c^{(n+1)/n} \theta^{n+1} \, ,</math>
   </td>
   </td>
<td align="center">&nbsp; &nbsp; &nbsp; <math>\Rightarrow</math></td>


   <td align="right">
   <td align="right">
<math>~P_0</math>
&nbsp; &nbsp; &nbsp;<math>P_0</math>
   </td>
   </td>
   <td align="center">
   <td align="center">
Line 221: Line 220:
\, ,</math>
\, ,</math>
   </td>
   </td>
<td align="center">&nbsp; &nbsp; &nbsp; <math>\Rightarrow</math></td>


   <td align="right">
   <td align="right">
<math>~g_0</math>
&nbsp; &nbsp; &nbsp;<math>g_0</math>
   </td>
   </td>
   <td align="center">
   <td align="center">
Line 237: Line 234:
</tr>
</tr>
</table>
</table>


<table border="1" align="center" cellpadding="5" width="80%"><tr><td align="left">
<table border="1" align="center" cellpadding="5" width="80%"><tr><td align="left">

Revision as of 14:46, 19 January 2026

Main Sequence to Red Giant to Planetary Nebula


Part I:  Background & Objective

 


Part II: 

 


Part III: 

 


Part IV: 

 

Succinct

Generic

Adiabatic Wave (or Radial Pulsation) Equation

d2xdr02+[4r0(g0ρ0P0)]dxdr0+(ρ0γgP0)[ω2+(43γg)g0r0]x=0

may also be written as …

0

=

d2xdr*2+{4(ρ*P*)Mr*(r*)}1r*dxdr*+(ρ*P*){2πσc23γg(34γg)Mr*(r*)3}x.

In shorthand, we can rewrite this equation in the form,

0

=

x+r*x+𝒦x,

where,

x

=

dxdr*

      and      

x

=

d2xd(r*)2;

and,

𝒦(ρ*P*)[(σc2γg)2π3(34γg)Mr*(r*)3];

and,

{4(ρ*P*)Mr*(r*)}.

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,

an

[(n+1)K4πGρc(1n)/n]1/2;

and, once the dimensionless polytropic temperature, θ(ξ), is known, the radial dependence of key physical variables is given by the expressions,

 

if, as in a separate discussion, n=5 and θ=(1+ξ2/3)1/2

r0

=

anξ,

     r0

=

[KGρc4/5]1/2(32π)1/2ξ,

ρ0

=

ρcθn,

     ρ0

=

ρcθ5,

P0

=

Kρ0(n+1)/n=Kρc(n+1)/nθn+1,

     P0

=

Kρc6/5θ6,

g0

=

GM(r0)r02=Gr02[4πan3ρc(ξ2dθdξ)],

     g0

=

GM(r0)r02=Gr02[4πan3ρc(ξ2dθdξ)],

Notice that,

g0ρ0r0P0

=

Gan2ξ2[4πan3ρc(ξ2dθdξ)]ρcθnanξ[Kρc(n+1)/nθn+1]1

 

=

4πGK[ρc11/n](ξdθdξ)θ1an2

 

=

(n+1)(ξθdθdξ);

ρ0r02P0

=

ρcθn(anξ)2[Kρc(n+1)/nθn+1]1

 

=

K1ρc1/nan2ξ2θ

 

=

[(n+1)4πGρc]ξ2θ.

As a result, for polytropes we can write,

0

=

d2xdr02+[4(g0ρ0r0P0)]1r0dxdr0+(ρ0r02γgP0)[ω2+(43γg)g0r0]xr02

 

=

d2xdr02+[4(g0ρ0r0P0)]1r0dxdr0+[ω2γg(ρ0r02P0)(34γg)(g0ρ0r0P0)]xr02

 

=

d2xdr02+[4(n+1)Q]1r0dxdr0+(n+1)[ω2γg[14πGρc]ξ2θ(34γg)Q]xr02.

Finally, multiplying through by an2 — which everywhere converts r0 to ξ — gives, what we will refer to as the,

Polytropic LAWE (linear adiabatic wave equation)

0=d2xdξ2+[4(n+1)Q]1ξdxdξ+(n+1)[(σc26γg)ξ2θαQ]xξ2

where:    Q(ξ)dlnθdlnξ,    σc23ω22πGρc,     and,     α(34γg)

Related Discussions

Tiled Menu

Appendices: | VisTrailsEquations | VisTrailsVariables | References | Ramblings | VisTrailsImages | myphys.lsu | ADS |