SSC/Structure/PolytropesEmbedded: Difference between revisions

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===Whitworth's Presentation===
===Whitworth's Presentation===


In §5 of his paper, [http://adsabs.harvard.edu/abs/1981MNRAS.195..967W Whitworth (1981)] also presents the set of parametric  
In §5 of his paper, {{ Whitworth81}} — hereafter, {{ Whitworth81hereafter }} — also presents the set of parametric  
equations that define what the equilibrium radius, <math>~R_\mathrm{eq}</math>, is of an embedded polytrope for a certain imposed external pressure, <math>~P_\mathrm{e}</math>, namely,
equations that define what the equilibrium radius, <math>R_\mathrm{eq}</math>, is of an embedded polytrope for a certain imposed external pressure, <math>P_\mathrm{e}</math>, namely,
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<math>
<math>
~P_\mathrm{rf} \biggl\{  2^{-8/\eta} \biggl(\frac{5|\eta-1|}{\eta} \biggr)^3 \biggl(\frac{3}{\xi} \biggr)^4  
P_\mathrm{rf} \biggl\{  2^{-8/\eta} \biggl(\frac{5|\eta-1|}{\eta} \biggr)^3 \biggl(\frac{3}{\xi} \biggr)^4  
\biggl|\frac{d\theta_n}{d\xi} \biggr|^{-2} \biggr\}_{\xi_e}^{\eta/(3\eta - 4)} \theta_n^{\eta/(\eta-1)}  
\biggl|\frac{d\theta_n}{d\xi} \biggr|^{-2} \biggr\}_{\xi_e}^{\eta/(3\eta - 4)} \theta_n^{\eta/(\eta-1)}  
</math>
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where, in order to obtain the second line of the two relations we have used the substitution, <math>~\eta \rightarrow (1+1/n)</math>, and, as is detailed in an [[SSC/Structure/PolytropesASIDE1|accompanying ASIDE]], Whitworth "referenced" <math>~P_\mathrm{e}</math> and <math>~R_\mathrm{eq}</math> to, respectively,
where, in order to obtain the second line of the two relations we have used the substitution, <math>\eta \rightarrow (1+1/n)</math>, and, as is detailed in an [[SSC/Structure/PolytropesASIDE1|accompanying ASIDE]], {{ Whitworth81hereafter }} "referenced" <math>P_\mathrm{e}</math> and <math>R_\mathrm{eq}</math> to, respectively,


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Via these normalizations, Whitworth &#8212; as did Horedt (1970) &#8212; chose to express <math>~R_\mathrm{eq}</math> and <math>~P_\mathrm{e}</math> in terms of {{Math/MP_PolytropicConstant}} and the system's total mass, <math>~M</math>.
Via these normalizations, {{ Whitworth81hereafter }} &#8212; as did {{ Horedt70hereafter }} &#8212; chose to express <math>R_\mathrm{eq}</math> and <math>P_\mathrm{e}</math> in terms of {{Math/MP_PolytropicConstant}} and the system's total mass, <math>M</math>.


To convert from Whitworth's expressions, which use one set of normalization parameters <math>~(R_\mathrm{rf},P_\mathrm{rf})</math>, to Horedt's expressions, which use a somewhat different set of normalization parameters &#8212; identified here as <math>~(R_\mathrm{Horedt},P_\mathrm{Horedt})</math> &#8212; one simply needs to make use of the relations,
To convert from Whitworth's expressions, which use one set of normalization parameters <math>(R_\mathrm{rf},P_\mathrm{rf})</math>, to Horedt's expressions, which use a somewhat different set of normalization parameters &#8212; identified here as <math>(R_\mathrm{Horedt},P_\mathrm{Horedt})</math> &#8212; one simply needs to make use of the relations,
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===Stahler's Presentation===
===Stahler's Presentation===
Similarly, in Appendix B of his work, [http://adsabs.harvard.edu/abs/1983ApJ...268..165S Steven W. Stahler (1983)] states that the mass, <math>~M</math>, associated with the equilibrium radius, <math>~R_\mathrm{eq}</math>, of embedded polytropic spheres is,
Similarly, in Appendix B of his work, {{ Stahler83 }} &#8212; hereafter, {{ Stahler83hereafter }} &#8212; states that the mass, <math>M</math>, associated with the equilibrium radius, <math>R_\mathrm{eq}</math>, of embedded polytropic spheres is,
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Notice that, via these two normalizations, Stahler chose to express <math>~R_\mathrm{eq}</math> and <math>~M</math> in terms of {{Math/MP_PolytropicConstant}} and the applied external pressure, <math>~P_\mathrm{e}</math>.
Notice that, via these two normalizations, {{ Stahler83hereafter }} chose to express <math>R_\mathrm{eq}</math> and <math>M</math> in terms of {{Math/MP_PolytropicConstant}} and the applied external pressure, <math>P_\mathrm{e}</math>.
 
<font color="red"><b>NOTE:</b></font> &nbsp; An [[SSC/Structure/StahlerMassRadius|accompanying chapter]] presents a much more detailed description of the ''sequences'' of truncated polytropic spheres that are derived and discussed by {{ Stahler83hereafter }}.


===Reconciliation===
===Reconciliation===

Latest revision as of 14:04, 19 July 2024

Embedded Polytropic Spheres[edit]


Part I:   General Properties

 


Part II:  Truncated Configurations with n = 1

 


Part III:  Truncated Configurations with n = 5

 


Part IV:  Other Considerations

 


Embedded
Polytropes

In a separate discussion we have shown how to determine the structure of isolated polytropic spheres. These are rather idealized stellar structures in which the pressure and density both drop to zero at the surface of the configuration (for 0 ≤ n < 5) or in which the equilibrium configuration extends to infinity (for 5 ≤ n ≤ ∞). Here we consider how the equilibrium radius of a polytropic configuration of a given M and Kn is modified when it is embedded in an external medium of pressure Pe. We will begin by reviewing the general properties of embedded (and truncated) polytropes for a wide range of polytropic indexes, principally summarizing the published descriptions provided by 📚 Gp. Horedt (1970, MNRAS, Vol. 151, pp. 81 - 86), by 📚 A. Whitworth (1981, MNRAS, Vol. 195, pp. 967 - 977), by Kimura (1981a), and by 📚 S. W. Stahler (1983, ApJ, Vol. 268, pp. 165 - 184). Then we will focus in more detail on polytropes of index n = 1 and n = 5 because their structures can be described by closed-form analytic expressions.  
 

General Properties[edit]

Horedt's Presentation[edit]

It appears as though 📚 Horedt (1970) — hereafter, Horedt70 — was the first to draw an analogy between the mass limit that is associated with bounded isothermal spheres — the so-called Bonnor-Ebert spheres — and the limiting mass that can be found in association with equilibrium sequences of embedded polytropes that have polytropic indexes n>3. Using a tilde to denote values of parameters at the (truncated) edge of a pressure-bounded polytropic sphere, Horedt70 (see the bottom of his p. 83) derives the following set of parametric equations relating the configuration's dimensionless radius, ra, to a specified dimensionless bounding pressure, pa:

raReqRHoredt

=

ξ~(ξ~2θ~)(1n)/(n3),

paPePHoredt

=

θ~nn+1(ξ~2θ~)2(n+1)/(n3),

where it is understood that, as discussed elsewhere, θn(ξ) is the solution to the Lane-Emden equation for a polytrope of index n,

θ~

dθndξevaluatedatξ~,

RHoredt

αr(αMM)(1n)/(n3)=[4π(n+1)n(GKn)nMn1]1/(n3),

PHoredt

Kn(αMM)2(n+1)/(n3)=Kn4n/(n3)[(n+1)34πG3M2](n+1)/(n3).

Notice that, via these normalizations, Horedt chose to express Req and Pe in terms of Kn and the system's total mass, M.

Whitworth's Presentation[edit]

In §5 of his paper, 📚 Whitworth (1981) — hereafter, Whitworth81 — also presents the set of parametric equations that define what the equilibrium radius, Req, is of an embedded polytrope for a certain imposed external pressure, Pe, namely,

Req

=

Rrf{4η5|η1|(ξ3)η|dθndξ|(2η)}ξe1/(3η4)

(ReqRrf)(3n)

=

[4(n+1)5]n(ξe3)(n+1)|dθndξ|ξe(n1),

Pe

=

Prf{28/η(5|η1|η)3(3ξ)4|dθndξ|2}ξeη/(3η4)θnη/(η1)

(PePrf)(3n)

=

28n{(5n+1)3(3ξ)4θn(3n)|dθndξ|2}ξe(n+1),

where, in order to obtain the second line of the two relations we have used the substitution, η(1+1/n), and, as is detailed in an accompanying ASIDE, Whitworth81 "referenced" Pe and Req to, respectively,

Prf(43η)

=

22(4+η)(3453π)η[Kn4G3ηM2η]

Prf(n3)

=

22(5n+1)(3453π)(n+1)[Kn4nG3(n+1)M2(n+1)],

Rrfη

=

22Kn(GM35)ηPrf(1η)

Rrf(n+1)

=

(22Kn)n(GM35)(n+1)Prf1

Rrf(3n)

=

(22Kn)n(3n)/(n+1)(GM35)(3n)Prf(n3)/(n+1)

 

=

(22Kn)n(3n)/(n+1)(GM35)(3n){22(5n+1)(3453π)(n+1)[Kn4nG3(n+1)M2(n+1)]}1/(n+1)

 

=

Knn(22)(n+1)(GM35)(3n)(3453π)[1G3M2]

 

=

22(n+1)π13n+15nKnnGnM1n

Via these normalizations, Whitworth81 — as did Horedt70 — chose to express Req and Pe in terms of Kn and the system's total mass, M.

To convert from Whitworth's expressions, which use one set of normalization parameters (Rrf,Prf), to Horedt's expressions, which use a somewhat different set of normalization parameters — identified here as (RHoredt,PHoredt) — one simply needs to make use of the relations,

(RrfRHoredt)(3n)

=

3(n+1)[522(n+1)]n.

(PrfPHoredt)(3n)

=

28n[(n+1)33453](n+1),

Kimura's Presentation[edit]

At the same time Whitworth's work was being published, Kimura (1981a) also published a derivation of the equations that define the equilibrium properties of embedded, pressure-truncated polytropic configurations. (Note that an erratum has been published correcting typographical errors that appear in a few equations of the original paper.) When compared with, for example, Horedt's published work — which Kimura references — Kimura's set of structural equations are a bit more difficult to digest because they include (a) an equation-of-state index that is different from the traditional polytropic index — specifically (see his equation 6),

σ(n+1)1

— which was Kimura's effort to more gracefully accommodate discussions of isothermal (n=) configurations; and (b) an additional integer index, m, so that a single set of equations can be used to specify the structure of planar (m=1) and cylindrical (m=2) as well as spherical (m=3) configurations. In the present context, we will fix the value to m=3. Kimura also chose to express his structural solutions in terms of a dimensionless radius, ζ, instead of the traditional variable, ξ — note that the two are related via the expression,

ζ=(n+1)1/2ξ;

and in terms of a dimensionless gravitational potential, ϕ, instead of the traditional dimensionless enthalpy variable, θn — note that the two are related via the expression (see Kimura's equation 12),

ϕ=σ1(1θn).

Given this relationship, we note as well that,

ϕ'dϕdζ=dθndξ[σ1dξdζ]=dθndξ(n+1)1/2.

The set of equilibrium equations derived by Kimura (1981a) in what he identifies as "Paper I" — see especially his equations number (16) and (23) — are summarized most succinctly in Table 1 of his "Paper II" (Kimura 1981b). The equations he presents for "radial distance," "pressure," and "fractional mass within ζ~" are, respectively,

ReqRKimura

=

ζ~=(n+1)1/2ξ~,

PePKimura

=

θ~nn+1,

MMKimura

=

ζ~2ϕ~'=(n+1)3/2[ξ2dθndξ]ξ~,

where, expressed in terms of the central pressure, p*, and the polytropic constant, Kn,[note that, in Kimura's paper, H=Knn/(n+1)], the relevant normalization parameters are,

RKimura

(4πG)1/2Hp*σ1/2=(4πG)1/2Knn/(n+1)p*(1n)/[2(n+1)],

PKimura

=

p*,

MKimura

=

(4πG)3/2(4π)H2p*2σ1/2=(4πG3)1/2Kn2n/(n+1)p*(3n)/[2(n+1)].

In order to compare Kimura's equilibrium expressions for Req and Pe with the corresponding expressions presented by Horedt and by Whitworth, we need to replace p* by M in both expressions. Inverting Kimura's expression for M, we have,

p*(3n)/[2(n+1)]

=

M(n+1)3/2(ξ~2θ~')1(4πG3)1/2Kn2n/(n+1).

Hence,

PKimura

=

[M(n+1)3/2(ξ~2θ~')1(4πG3)1/2Kn2n/(n+1)]2(n+1)/(3n),

 

=

[M2(n+1)3(ξ~2θ~')2(4πG3)1Kn4n/(n+1)](n+1)/(n3),

 

=

PHoredt[(ξ~2θ~')2](n+1)/(n3)

Pe

=

PHoredtθ~n+1(ξ~2θ~')2(n+1)/(n3),

which matches Horedt's expression for Pe. Also after replacement we obtain,

RKimura

=

(4πG)1/2Kn/(n+1)[M(n+1)3/2(ξ~2θ~')1(4πG3)1/2Kn2n/(n+1)](1n)/(3n)

 

=

M(n1)/(n3)(ξ~2θ~')(1n)/(n3)(n+1)3(1n)/2(n3)(4π)[(1n)(3n)]/[2(3n)]G[3(1n)(3n)]/[2(3n)][Knn(3n)2n(1n)]1/[(n+1)(3n)]

 

=

M(n1)/(n3)(ξ~2θ~')(1n)/(n3)(n+1)3(1n)/2(n3)(4π)1/(n3)Gn/(n3)Knn/(n3)

Req

=

ξ~(ξ~2θ~')(1n)/(n3)(n+1)[3(1n)+(n3)]/2(n3)[4π(GKn)nM(n1)]1/(n3)

 

=

RHoredtξ~(ξ~2θ~')(1n)/(n3),

which exactly matches Horedt's expression for Req.

Stahler's Presentation[edit]

Similarly, in Appendix B of his work, 📚 Stahler (1983) — hereafter, SWS — states that the mass, M, associated with the equilibrium radius, Req, of embedded polytropic spheres is,

M

=

MSWS(n34π)1/2{θn(n3)/2ξ2|dθndξ|}ξe

Req

=

RSWS(n4π)1/2{ξθn(n1)/2}ξe

where, from his equations (7) and (B3) we deduce,

MSWS=(n+1nG)3/2Kn2n/(n+1)Pe(3n)/[2(n+1)],

RSWS=(n+1nG)1/2Knn/(n+1)Pe(1n)/[2(n+1)].

Notice that, via these two normalizations, SWS chose to express Req and M in terms of Kn and the applied external pressure, Pe.

NOTE:   An accompanying chapter presents a much more detailed description of the sequences of truncated polytropic spheres that are derived and discussed by SWS.

Reconciliation[edit]

Here we demonstrate that Whitworth's and Stahler's presentations are equivalent to one another. We begin by plugging Stahler's definition of MSWS into his expression for M, then inverting it to obtain an expression for Pe in terms of M and Kn.

M

=

[(n+1)34πG3]1/2Kn2n/(n+1)Pe(3n)/[2(n+1)]{θn(n3)/2ξ2|dθndξ|}ξe

Pe(3n)

=

[4πG3(n+1)3](n+1)Kn4nM2(n+1){θn(n3)/2ξ2|dθndξ|}ξe2(n+1)

 

=

[4πG3M2(n+1)3](n+1)Kn4n{θn(3n)ξ4|dθndξ|2}ξe(n+1)

Alternatively, plugging Whitworth's definition of Prf into his expression for Pe gives,

Pe(3n)

=

22(5n+1)(π3453)(n+1)28n34(n+1)(5n+1)3(n+1)[G3M2](n+1)Kn4n{θn(3n)ξ4|dθndξ|2}ξe(n+1)

 

=

22(n+1)[π(n+1)3](n+1)[G3M2](n+1)Kn4n{θn(3n)ξ4|dθndξ|2}ξe(n+1).

So Whitworth's and Stahler's relations for Pe(M,Kn) are, indeed, identical. Similarly examining Stahler's expression for the equilibrium radius, we find,

Req

=

(n+14πG)1/2Knn/(n+1)[ξθn(n1)/2]ξe{Pe1/(n+1)}(1n)/2

 

=

(n+14πG)1/2Knn/(n+1)[ξθn(n1)/2]ξe{[4πG3M2(n+1)3]Kn4n/(n+1)[θn(3n)ξ4|dθndξ|2]ξe}(1n)/[2(3n)]

Req(3n)

=

(n+14πG)(3n)/2Knn(3n)/(n+1)ξe3n{[4πG3M2(n+1)3]1/2Kn2n/(n+1)[ξ2|dθndξ|1]ξe}(1n)

 

=

(n+1)[(3n)3(1n)]/2(4π)[(n3)+(1n)]/2G[(n3)+3(1n)]/2[Kn(3n)+2(n1)]n/(n+1)ξe(3n)+2(n1)M(1n)|dθdξ|ξe(n1)

 

=

(n+1)n(4π)1GnKnnM(1n)[ξ(n+1)|dθndξ|(n1)]ξe.

And Whitworth's expression becomes,

Req(3n)

=

22(n+1)π13n+15nKnnGnM1n[4(n+1)5]n(ξe3)(n+1)|dθndξ|ξe(n1)

 

=

(n+1)n(4π)1KnnGnM1nξe(n+1)|dθndξ|ξe(n1).

Hence, Stahler's equilibrium radius, Req, exactly matches Whitworth's Req.

Summary[edit]

Once the function, θn(ξ), and its first derivative with respect to the dimensionless radial coordinate, dθn/dξ, are obtained via a solution of the Lane-Emden equation, the equilibrium radius, Req, and total mass, M, of a pressure-bounded polytrope can be expressed in terms of Stahler's normalizations as follows:

ReqRSWS

=

(n4π)1/2[ξθn(n1)/2]ξe,

MMSWS

=

(n34π)1/2pa(n3)/[2(n+1)],

where,

pa

[θn(n3)/2ξ2|dθndξ|]ξe2(n+1)/(n3)=θn(n+1)(ξ2|dθndξ|)ξe2(n+1)/(n3).

Then, the external pressure, expressed in terms of Whitworth's normalization, is,

PePrf

=

28n/(n3)[(n+1)33453](n+1)/(n3)pa;

and the conversion from Stahler's normalization to Whitworth's normalization of the radius is achieved via the expression,

RSWSRrf

=

[3(n+1)2(n+3)(5n+1)n]1/(n3)(πn)1/2pa(1n)/[2(n+1)].

Chieze's Presentation[edit]

From equations (8), (10), and (68) in Chapter IV of [C67], we can immediately formulate the following expressions for, respectively, Pe(ξ~),Req(ξ~), and Mtot(ξ~):

PePCh

=

θ~n+1,

ReqRCh

=

[n+14π]1/2ξ~

MtotMCh

=

[(n+1)34π]1/2(ξ~2θ~'),

where,

PCh

Kρc(n+1)/n,

RCh

[(KG)ρc1/n1]1/2,

MCh

[(KG)3ρc(3n)/n]1/2.

In this case, the expressions for the physical variable normalizations have been defined in terms of — in addition to G and/or K — the equilibrium configuration's central density, ρc, instead of in terms of Mtot or Pe. These are precisely the expressions for, respectively, Ps(ξs), Rs(ξs), and Ms(ξs) that appear in the appendix of J. P. Chieze (1987, A&A, 171, 225-232) — see, respectively, his equations (A7), (A5), and (A6). [Note that, for the polytropic systems of interest to us, here — that is, systems having 0n< — Chieze's parameter ϵsgn(n+1)=1.]

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