SSC/Virial/Isothermal

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Virial Equilibrium of Isothermal Spheres[edit]

Review[edit]

In an introductory discussion of the virial equilibrium structure of spherically symmetric configurations — see especially the section titled, Energy Extrema — we deduced that a system's equilibrium radius, Req, measured relative to a reference length scale, R0, i.e., the dimensionless equilibrium radius,

χeqReqR0,

is given by the root(s) of the following equation:

2Cχ2+(1δ1γg)3Bχ33γg+δ1γg3BI3Aχ13Dχ3=0,

where the definitions of the various coefficients are,

A

15GMtot2R0𝔣W𝔣M2,

B

KMtot(3Mtot4πR03)γg1𝔣A𝔣Mγg=cs¯2Mtot𝔣A𝔣Mγg,

BI

cs2Mtot,

C

5J24MtotR02𝔣M𝔣T,

D

43πR03Pe.

Once the pressure exerted by the external medium (Pe), and the configuration's mass (Mtot), angular momentum (J), and specific entropy (via K) — or, in the isothermal case, sound speed (cs) — have been specified, the values of all of the coefficients are known and χeq can be determined.

Isolated, Nonrotating Configuration[edit]

For a nonrotating configuration (C=J=0) that is not influenced by the effects of a bounding external medium (D=Pe=0), the statement of virial equilibrium is,

(1δ1γg)3(γg1)Bχ33γg+δ1γgBIAχ1=0.

Isothermal Evolutions[edit]

For isothermal configurations (δ1γg=1), one and only one equilibrium state arises where,

BI=Aχ1,

that is,

Req=R0χeq=ABIR0=GM5cs2.

Nonrotating Configuration Embedded in an External Medium[edit]

For a nonrotating configuration (C=J=0) that is embedded in, and is influenced by the pressure Pe of, an external medium, the statement of virial equilibrium is,

(1δ1γg)3Bχ33γg+δ1γg3BI3Aχ13Dχ3=0.

Bounded Isothermal[edit]

For isothermal configurations (δ1γg=1), we deduce that equilibrium states exist at radii given by the roots of the equation,

3BI3Aχ13Dχ3=0.

Bonnor's (1956) Equivalent Relation[edit]

Inserting the expressions for the coefficients BI, A, and D gives,

3Mcs235GM2R=3Pe(4π3R3),

or, because the volume V=(4πR3/3) for a spherical configuration, we can write,

3PeV=3Mcs235(4π3)1/3GM2V1/3.

It is instructive to compare this expression for a self-gravitating, isothermal equilibrium sphere to the one that appears as Eq. (1.2) in 📚 W. B. Bonnor (1956, MNRAS, Vol. 116, pp. 351 - 359):

Reprint of the opening (introductory) paragraph from …
W. B. Bonnor (1956)
Boyle's Law and gravitational instability
Monthly Notices of the Royal Astronomical Society
Vol. 116, pp. 351 - 359

"It has recently been suggested by Terletsky that for a large mass M of gas, of volume V and temperature T, containing N molecules under boundary pressure p, the equation of state should be not

PV

=

NkT

(1.1)

but

PV

=

NkTαGM2V1/3,

(1.2)

where k is Boltzmann's constant, G is Newton's constant of gravitation, and α is a constant depending on the shape of the mass. The proposed correction of Boyle's Law arises because, for a large mass, one has to take account of the gravitational interactions between the molecules."

Y. P. Terletsky (1952, Zh. Eksper. Teor. Fiz., Vol. 22, p. 506)


Notes from J. E. Tohline regarding this referenced article:


Once we realize that, for an isothermal configuration, twice the thermal energy content, 2S, can be written as (3NkT) just as well as via the product, (3Mcs2), we see that our expression is identical to the one derived by 📚 Bonnor (1956) if we set the prefactor on his last term, α=(4π/3)1/3/5. (Indeed, later on the first page of his paper, 📚 Bonnor (1956) points out that this is the appropriate value for α when considering a uniform-density sphere.)

P-V Diagram[edit]

Returning to the dimensionless form of this expression and multiplying through by [χ/(3D)], we obtain,

χ4BIDχ+AD=0.

Now, taking a cue from the solution presented above for an isolated isothermal configuration, we choose to set the previously unspecified scale factor, R0, to,

R0=GM5cs2,

in which case BI=A, and the quartic equation governing the radii of equilibrium states becomes, simply,

χ4χΠ+1Π=0,

where,

ΠDBI=4πR03Pe3Mcs2=4πPeG3M2353cs8.

For a given choice of Pe and cs, Π1/2 can represent a dimensionless mass, in which case,

M=Π1/2(35322π)1/2(cs8PeG3)1/2.

Alternatively, for a given choice of configuration mass and sound speed, this parameter, Π, can be viewed as a dimensionless external pressure; or, for a given choice of M and Pe, Π1/8 can represent a dimensionless sound speed. In most of what follows we will view Π as a dimensionless external pressure.

The above quartic equation can be rearranged immediately to give the external pressure that is required to obtain a particular configuration radius, namely,

Π=(χ1)χ4.

The resulting behavior is shown by the black curve in Figure 2.

Figure 2: Equilibrium Isothermal P-V Diagram

The black curve traces out the function,

Π=(χ1)/χ4,

and shows the dimensionless external pressure, Π, that is required to construct a nonrotating, self-gravitating, isothermal sphere with an equilibrium radius χ. The pressure becomes negative at radii χ<1, hence the solution in this regime is unphysical.

Figure 1 displays the free energy surface that "lies above" the two-dimensional parameter space (1.2<χ<1.51; 0.103<Π<0.104) that is identified here by the thin, red rectangle.

Equilibrium P-R Diagram
Equilibrium P-R Diagram

In the absence of self-gravity (i.e., A=0), the product of the external pressure and the volume should be constant. The corresponding relation, Π=χ3, is shown by the blue dashed curve in the figure. As the figure illustrates, when gravity is included the P-V relationship pulls away from the PV = constant curve at sufficiently small volumes. Indeed, the curve turns over at a finite pressure, Πmax, and for every value of Π<Πmax a second, more compact equilibrium configuration appears. The location of Πmax along the curve is identified by setting Π/χ=0, that is, it occurs where,

Πχ=4χ5(χ1)+χ4=0,

χ=2231.333333.

Hence,

Πmax=(223)4(2231)=33280.105469;

therefore, from above,

Mmax=(3453210π)1/2(cs8PeG3)1/21.77408(cs8PeG3)1/2.

Quartic Solution[edit]

In the above PV diagram discussion, we rearranged the quartic equation governing equilibrium configurations to give Π for any chosen value of χ. Alternatively, the four roots of the quartic equation — χ1, χ2, χ3 and χ4 in the presentation that follows — will identify the radii at which a spherical configuration will be in equilibrium for any choice of the external pressure, Π, assuming the roots are real.

Roots of the quartic equation: χ4χΠ1+Π1=0

χ1

=

+12yr1/2+12Dq;

χ2

=

+12yr1/212Dq;

χ3

=

12yr1/2+12Eq;

χ4

=

12yr1/212Eq,

where,

Dq

yr1/2[2Πyr3/21]1/2,

Eq

yr1/2[2Πyr3/21]1/2,

and,

yr(12Π2)1/3{[1+12833Π]1/3+[112833Π]1/3},

is the real root of the cubic equation,

y34yΠ1Π2=0.

Because Π must be positive in physically realistic solutions, we conclude that the two roots involving Eq — that is, χ3 and χ4 — are imaginary and, hence, unphysical. The other two roots — χ1 and χ2 — will be real only if the arguments inside the radicals in the expression for yr are positive. That is, χ1 and χ2 will be real only for values of the dimensionless external pressure,

ΠΠmax3328.

This is the same upper limit on the external pressure that was derived above, via a different approach, and translates into a maximum mass for a pressure-bounded isothermal configuration of,

Mmax=Πmax1/2(35322π)1/2(cs8G3Pe)1/2=(3453210π)1/2(cs8G3Pe)1/2.


When combined, a plot of χ1 versus Π and χ2 versus Π will reproduce the solid black curve shown in Figure 2, but with the axes flipped. The top-right quadrant of Figure 3 presents such a plot, but in logarithmic units along both axes; also Π is normalized to Πmax and χ is normalized to the equilibrium radius (4/3) at that pressure. This is the manner in which Whitworth (1981, MNRAS, 195, 967) chose to present this result for uniform-density, spherical isothermal (γg=1) configurations. Our solid and dashed curve segments — identifying, respectively, the χ1(Π) and χ2(Π) solutions to the above quadratic equation — precisely match the solid and dashed curve segments labeled "1" in Whitworth's Figure 1a (replicated here in the bottom-right quadrant of Figure 3).

Figure 3: Equilibrium R-P Diagram

Top: The solid curve traces the function χ1(Π) and the dashed curve traces the function χ2(Π), where χ1 and χ2 are the two real roots of the quartic equation,

χ4χΠ+1Π=0.

Logarithmic units are used along both axes; Π is normalized to Πmax; and χ is normalized to the equilibrium radius (4/3) at Πmax.

Bottom: A reproduction of Figure 1a from Whitworth (1981, MNRAS, 195, 967). The solid and dashed segments of the curve labeled "1" identify the equilibrium radii, Req, that result from embedding a uniform-density, isothermal (γg=1) gas cloud in an external medium of pressure Pex.

Comparison: The curve shown above that traces out χ1(Π) and χ2(Π) should be identical to the "Whitworth" curve labeled "1".

To be compared with Whitworth (1981)
To be compared with Whitworth (1981)
Whitworth (1981) Figure 1a
Whitworth (1981) Figure 1a

See Also[edit]


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