SSC/BipolytropeGeneralizationVersion2

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Bipolytrope Generalization[edit]

Setup[edit]

In a more general context, we have discussed a Gibbs-like free-energy function of the generic form,

𝔊=Wgrav+𝔖therm+Tkin+PeV+

Here we are interested in examining the free energy of isolated, nonrotating, spherically symmetric bipolytropes, so we can drop the term that accounts for the influence of an external pressure and we can drop the kinetic energy term. But we need to consider separately the contributions to the reservoir of thermodynamic energy by the core and envelope. In particular, we will assume that compressions/expansions occur adiabatically, but that the core and the envelope evolve along separate adiabats — γc and γe, respectively.

Review of Isolated Polytrope[edit]

If we were configuring isolated polytropes — instead of bipolytropes — the free-energy expression would be, simply,

𝔊=Wgrav+𝔖A,

and, following the detailed steps presented in our introductory discussion of the free energy of spherically symmetric, configurations, properly normalized expressions for the two contributing energy terms would be,

WgravEnorm

=

0χ=Redge*3[Mr(r*)Mtot]r*ρ*dr*

 

=

{(ρcρ¯)013x[Mr(x)Mtot][ρ(x)ρc]dx}eqχ1,

𝔖AEnorm

=

1(γg1)0χ=Redge*4π(r*)2P*dr*

 

=

1(γg1)(4π3)1γ{(ρcρ¯)γ013x2[P(x)Pc]dx}eqχ33γ,

where,

Mr(x)Mtot

=

(ρcρ¯)eq0x3x2[ρ(x)ρc]dx.

We note that, because Mr(x)/Mtot=1 in the limit, x1, we can write,

(ρcρ¯)eq

=

[013x2(ρ(x)ρc)dx]1,

or, if desired, the central-to-mean density ratio in one or both energy terms could be replaced by a term involving the normalized central pressure and the dimensionless equilibrium radius, χeq, via the relation,

[(34π)ρcρ¯]eqγ

=

[(PcPnorm)χ3γ]eq.

Bipolytrope[edit]

When considering an isolated, spherically symmetric bipolytropic configuration, each energy term will be made up of separate contributions coming from the core and envelope, that is,

𝔊=(Wgrav+𝔖A)core+(Wgrav+𝔖A)env.

Partitioning the Mass[edit]

The core will be principally defined in terms of two dimensionless parameters — q and ν — which are, respectively, the core's radius relative to the bipolytrope's total radius, and the core's mass relative to the total mass of the bipolytropic configuration, specifically,

q

xi=riRedge,

ν

McoreMtot.

Given the separate (equilibrium) density profiles of the core and the envelope while sticking to the notation used in our introductory discussion, we can write,

(For0r*ri*)       Mr

=

(4π3)Rnorm3ρnorm0r*3(r*)2ρcore*dr*

 

=

Mtotχ30x3[ρcore(x)ρ¯core][Mcore/(xiRedge)3Mtot/Rnorm3]x2dx

 

=

Mtot(νq3)0x3[ρ(x)ρ¯]corex2dx;

(Forri*r*Redge*)       Mr

=

Mcore+(4π3)Rnorm3ρnormri*r*3(r*)2ρenv*dr*

 

=

Mcore+Mtotχ3xix3[ρenv(x)ρ¯env]{Menv/[(1xi3)Redge3]Mtot/Rnorm3}x2dx

 

=

Mtot{ν+(1ν1q3)xix3[ρ(x)ρ¯]envx2dx}.

EXAMPLES

Separate Contributions to Gravitational Potential Energy[edit]

Given the separate (equilibrium) density and Mr profiles of the core and the envelope while sticking to the notation used in our introductory discussion, we can write,

Wgrav|core

=

Enorm0ri*3[Mr(r*)Mtot]r*ρ*dr*

 

=

Enormχ1(νq3)0xi3x[Mr(x)Mtot]core[ρ(x)ρ¯]coredx

Wgrav|env

=

Enormri*χ=Redge*3[Mr(r*)Mtot]r*ρ*dr*

 

=

Enormχ1(1ν1q3)xi13x[Mr(x)Mtot]env[ρ(x)ρ¯]envdx


EXAMPLES

Separate Thermodynamic Energy Reservoirs[edit]

In our introductory discussion of the free energy function for spherically symmetric configurations, we developed expressions that define the separate contributions to the thermodynamic energy reservoir that pertain to the core and envelope of bipolytropic configurations. In that discussion we pointed out that, in general for the core, the pressure drops monotonically from a value of P0 at the center of the configuration according to an expression of the form,

Pcore(x)=P0[1pc(x)]      for      0xq,

and that, for the envelope, the pressure drops monotonically from a value of Pie at the interface according to an expression of the form,

Penv(x)=Pie[1pe(x)]      for      qx1,

where pc(x) and pe(x) are both dimensionless functions that will depend on the equations of state that are chosen for the core and envelope, respectively. By prescription, the pressure in the envelope must drop to zero at the surface of the bipolytropic configuration, hence, we should expect that pe(1)=1. Furthermore, by prescription, the pressure in the core will drop to a value, Pic, at the interface, so we can write,

Pic=P0[1pc(q)].

In equilibrium — that is, when Redge=Req — we will demand that the pressure at the interface be the same, whether it is referenced in the core or in the envelope, that is, we will demand that Pic=Pie. It is therefore strategically advantageous to rewrite the expression for the run of pressure through the core in terms of the pressure at the interface rather than in terms of the central pressure; specifically,

Pcore(x)=Pic[1pc(x)1pc(q)].

KEY QUESTION: How should piecewise pressure be normalized?

Here we will operate under two constraints when relating the central pressure, P0, to the core pressure at the interface, Pic. First, the pressure in the core will drop monotonically from its central value according to the following very general prescription,

Pcore(x)=P0[1pc(x)].

Second, it is the pressure at the interface, Pic=Pcore(q), that will be determined by the virial equilibrium condition. There are two possible ways to determine the central pressure from knowledge of Pic, but which is the physically correct method to embrace?

Case A: Addition …

P0=Pic+ΔP,     where     ΔPP0pc(q),

in which case, we should write that,

Pcore(x)=(Pic+ΔP)P0pc(x).


Case B: Multiplication …

Pic=P0[1pc(q)]P0=Pic[1pc(q)],

in which case, we should write that,

Pcore(x)=Pic[1pc(x)1pc(q)].

Prior to August 2014, we have been naively implementing "Case A," effectively assuming that the quantity, ΔP (as well as Pic), is held fixed as we search for the equilibrium value of P0. See, for example, the comment dated 12 February 2014 in connection with my discussions with Kundan Kadam, or even the "new derivation" summarized in the table below, where we have set,

ΔP=Πq2.

But we now suspect that "Case B" is the proper approach to embrace because, once the parameter q has been specified, it allows for the function, Pcore(x), to scale with the system size in exactly the same way as the interface pressure scales with size.


With these generic expressions for the pressure profile in hand, the separate components of the thermodynamic energy reservoir derived in our introductory discussion are,

(𝔖AEnorm)core

=

4π(γc1)[Picχ3γcPnorm]eqχ33γc0q[1pc(x)1pc(q)]x2dx

(𝔖AEnorm)env

 

4π(γe1)[Pieχ3γePnorm]eqχ33γeq1[1pe(x)]x2dx.


EXAMPLES

Generalized Free-Energy Expression[edit]

Bringing all of these expressions together, the normalized free-energy function for bipolytropes is,

𝔊*𝔊Enorm

=

(WgravEnorm)core+(𝔖AEnorm)core+(WgravEnorm)env+(𝔖AEnorm)env

 

=

3𝒜χ1core(1γc)χ33γcenv(1γe)χ33γe,

where,

𝒜

(νq3)0q[Mr(x)Mtot]core[ρ(x)ρ¯]corexdx+(1ν1q3)q1[Mr(x)Mtot]env[ρ(x)ρ¯]envxdx,

core

4π3[Picχ3γcPnorm]eq0q3[1pc(x)1pc(q)]x2dx,

env

4π3[Pieχ3γePnorm]eqq13[1pe(x)]x2dx.


ASIDE: In some of our older derivations, the function names score and senv were introduced as a shorthand notation. When referenced to our present, broad treatment of the free-energy function for bipolytropes, we note that,

q3score

=

0q3[1pc(x)1pc(q)]x2dx,

(1q3)senv

=

q13[1pe(x)]x2dx.

We also previously adopted the coefficient notation (with no subscript) for what is now called core, and we used 𝒞 for what is now labeled env.

Extrema and Virial Equilibrium[edit]

Extrema arise in the free-energy function wherever,

𝔊*χ

=

0,

that is, when,

3𝒜χ23coreχ23γc3envχ23γe

=

0.

Values of the dimensionless variable, χ, that provide solutions to this algebraic equation identify the size of equilibrium configurations and will henceforth be labeled with the "eq" subscript, that is,

χχeq

=

ReqRnorm.

Virial Theorem[edit]

We can rewrite the equilibrium condition as,

0

=

χeq1[3𝒜χeq13coreχeq33γc3envχeq33γe]eq

 

=

χeq1Enorm[(Wgrav)core+(Wgrav)env+3(γc1)(𝔖A)core+3(γe1)(𝔖A)env]eq.

Drawing from our introductory discussion of the reservoir of thermodynamic energy, we note that, for adiabatic systems, 𝔊A is equivalent to the internal energy of the system and therefore its relationship to the thermal energy, Stherm, is,

𝔊A=23(γ1)Stherm.

(This applies separately for the core and the envelope.) We therefore recognize that our derived expression for equilibrium systems is none other than the virial theorem applied to bipolytropic configurations, specifically, in equilibrium,

(Wgrav)core+(Wgrav)env+2[(Stherm)core+(Stherm)env]

=

0.

Example Bipolytrope Virial Theorem

Virial theorem for (nc,ne)=(0,0) bipolytrope:


In equilibrium, we will demand that Pie=Pic and we will set χχeq. Hence,

SthermEnorm

=

(SthermEnorm)core+(SthermEnorm)env

 

=

3(γc1)2(𝔖AEnorm)core+3(γe1)2(𝔖AEnorm)env

 

=

2π[Picχ3γcPnorm]eqχeq33γc{(P0Pic)[q3(3bξ5)q5]}

 

 

+2π[Picχ3γePnorm]eqχeq33γe{(1q3)+bξ(P0Pic)[25q5𝔉]}

 

=

2π[P0Pnorm]eqχeq3{[q3(3bξ5)q5]+PicP0(1q3)+25bξq5𝔉}

 

=

2π[P0Pnorm]eqχeq3[q3(3bξ5)q5+(1bξq2)(1q3)+25bξq5𝔉]

 

=

2π[P0Redge4PnormRnorm4]eqχeq1[1(3bξ5)q5bξ(q2q5)+25bξq5𝔉]

 

=

2π[P0Redge4GMtot2]eqχeq1[1+bξ(25q5𝔉35q5+q5q2)]

 

=

2π[1bξ(323π)ν2q6]χeq1{1+bξ[25q5(𝔉+1)q2]}

The virial theorem states that, in equilibrium,

2SthermEnorm

=

WgravEnorm,

which, in turn, implies,

[1bξ(32)ν2q6]χeq1{1+bξ[25q5(𝔉+1)q2]}

=

35(ν2q)f(ν,q)χeq1

1bξ+[25q5(𝔉+1)q2]

=

25q5f

1bξ

=

q2+25q5(f1𝔉).

Now, a bit of algebra shows that,

25q5(f1𝔉)

=

(ρeρc)[2q2(1q)+(ρeρc)(13q2+2q3)].

Hence, we have,

1bξ=(23π3)P0Redge4GMtot2(q3ν)2

=

q2+(ρeρc)[2q2(1q)+(ρeρc)(13q2+2q3)]

P0Redge4GMtot2

=

(323π)(νq3)2{q2+(ρeρc)[2q2(1q)+(ρeρc)(13q2+2q3)]}.

This exactly matches the equilibrium relation that was derived from our detailed force-balance analysis of (nc,ne)=(0,0) bipolytropes.

More Utilitarian Form[edit]

Multiplying the equilibrium condition through by (χ2/3) — and appending the "eq" suffix to χ, throughout — gives,

𝒜

=

coreχeq43γc+envχeq43γe.

Inserting the generic definitions of the coefficients core and env — expressed in shorthand notation as referenced above — and demanding that the interface pressures be identical, gives,

𝒜

=

{4π3[Picχ3γcPnorm]eqq3score}χeq43γc+{4π3[Pieχ3γePnorm]eq(1q3)senv}χeq43γe

 

=

4π3[Piχ4Pnorm]eq[q3score+(1q3)senv]

 

=

4π3[PiRedge4GMtot2]eq[q3score+(1q3)senv].


EXAMPLES

Related Discussions[edit]


See Also[edit]

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