2DStructure/ToroidalCoordinates

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Using Toroidal Coordinates to Determine the Gravitational Potential[edit]

Preface[edit]

Abstract
Joel E. Tohline (September, 2017)

"The important question we have tried to clarify concerns the possibility of converting the remaining double integral … into a line integral … this question remains open."

— Drawn from §6 of Trova, Huré & Hersant (2012)

It appears as though we have found an answer to this question posed by Trova, et al. (2012). The detailed derivations and associated scratch-work that support the summary discussion of this chapter can be found under the Appendix/Ramblings category of this H_Book and in our accompanying discussion of Dyson-Wong toroids.

Gravitational Potential surface for infinitesimally thin hoop
Gravitational Potential surface for infinitesimally thin hoop
Infinitesimally Thin Hoop

As has been known for approximately a century, at any meridional-plane coordinate location, (ϖ,z), the gravitational potential due to an axisymmetric, infinitesimally thin ring (TR) of radius, a, and total mass, M, is given by the "key expression,"

ΦTR(ϖ,z)

=

[2GMπ]K(k)(ϖ+a)2+z2

where:k{4ϖa/[(ϖ+a)2+z2]}1/2

and K(k) is the complete elliptic integral of the first kind. Making the coordinate-name substitutions, (ϖ,z)(R*,z*), to match much of this chapter's variable notation, we have alternatively,

ΦTR(R*,Z*)

=

[GMπ][k(R*a)1/2]K(k).

A number of research groups (e.g., Cohl & Tohline (1999), Bannikova et al. (2011), Trova, et al. (2012), Fukushima (2016)) have recognized that the gravitational potential due to any axisymmetric configuration of finite extent can be obtained by integrating over the meridional-plane surface area that is occupied by the configuration, while weighting the volume density, ρ(ϖ,z), according to the prescription,

Φ(R*,Z*)

=

Gπconfig[μ(R*ϖ)1/2]K(μ)ρ(ϖ,z)2πϖdϖdz,

where,

μ2

=

[4R*ϖ(R*+ϖ)2+(Z*z)2].

We, like Trova, et al. (2012), have wondered whether there is a possibility of converting this double integral into a single (line) integral. This is a particularly challenging task when this expression for the gravitational potential is couched in terms of cylindrical coordinates because the modulus of the elliptic integral is explicitly a function of both ϖ and z.

We have recently realized that if a switch is made from cylindrical coordinates to a toroidal coordinate system, (η,θ), that is defined such that,

ϖ=R*sinhη(coshηcosθ),

      and      

(Z*z)=R*sinθ(coshηcosθ),

then the expression for the modulus of the elliptic integral becomes,

μ2

=

2[1+1tanhη]1,

which is a function of only one coordinate — the "radial" coordinate, η — and the integral expression for the gravitational potential becomes,

Φ(R*,Z*)

=

+23/2GR*2ηminηmaxK(μ)sinhηdη(sinhη+coshη)1/2θmin(η)θmax(η)ρ(η,θ)[dθ(coshηcosθ)5/2].

If the configuration's density is constant, then, as is shown below, the integral over the angular coordinate variable, θ, can be completed analytically. Hence, the task of evaluating the gravitational potential (both inside and outside) of a uniform-density, axisymmetric configuration having any surface shape has been reduced a problem of carrying out a single, line integration. We specifically illustrate how this approach can be used to evaluate the gravitational potential of a uniform-density torus with a circular cross-section and aspect ratio, R/d=3.

Note:  As we have reviewed separately, it appears as though over forty years ago C.-Y. Wong (1973) successfully employed toroidal coordinates to derive a closed-form expression for the potential (inside as well as outside) of a uniform-density torus with a circular cross-section; see, for example, his Figure 7. That is to say, he was even able to carry out the final line integral in closed form. We have not (yet) been able to demonstrate that our expression for the potential of a circular-cross-section torus is identical to his.


Exploring the Use of
Toroidal Coordinates
to Determine the
Gravitational
Potential

As I have studied the structure and analyzed the stability of (both self-gravitating and non-self-gravitating) toroidal configurations over the years, I have often wondered whether it might be useful to examine such systems mathematically using a toroidal — or at least a toroidal-like — coordinate system. Is it possible, for example, to build an equilibrium torus for which the density distribution is one-dimensional as viewed from a well-chosen toroidal-like system of coordinates?

I should begin by clarifying my terminology. In volume II (p. 666) of their treatise on Methods of Theoretical Physics, Morse & Feshbach (1953; hereafter MF53) define an orthogonal toroidal coordinate system in which the Laplacian is separable.1 (See details, below.) It is only this system that I will refer to as the toroidal coordinate system; all other functions that trace out toroidal surfaces but that don't conform precisely to Morse & Feshbach's coordinate system will be referred to as toroidal-like.

I became particularly interested in this idea while working with Howard Cohl (when he was an LSU graduate student). Howie's dissertation research uncovered a Compact Cylindrical Greens Function technique for evaluating Newtonian potentials of rotationally flattened (especially axisymmetric) configurations.2,3 The technique involves a multipole expansion in terms of half-integer-degree Legendre functions of the 2nd kind — see NIST digital library discussion — where, we have discovered, the argument of this special function is a function only of the radial coordinate of Morse & Feshbach's orthogonal toroidal coordinate system — see more on this, below.

Statement of the Problem[edit]

Expression for the Axisymmetric Potential[edit]

Cohl & Tohline (1999; hereafter CT99) derive an expression for the Newtonian gravitational potential in terms of a Compact Cylindrical Green's Function expansion. They show — see, for example, their equation (31) — that when expressed in terms of cylindrical coordinates, the potential at any meridional location, ϖ=R* and Z=Z*, due to an axisymmetric mass distribution, ρ(ϖ,Z), is

Φ(R*,Z*)=2Gq0R*1/2,

where,

q0=Σϖ1/2Q1/2(X)ρ(ϖ,Z)dσ,

dσ=dϖdZ is a differential area element in the meridional plane, and the dimensionless argument (the modulus) of the special function, Q1/2, is,

XR*2+ϖ2+(Z*Z)22R*ϖ.

Next, following the lead of CT99, we note that according to the Abramowitz & Stegun (1965),

Q1/2(X)=μK(μ),

where, the function K(μ) is the complete elliptic integral of the first kind and, for our particular problem,

μ2

2(1+X)1

 

=

2[1+R*2+ϖ2+(Z*Z)22R*ϖ]1

 

=

[4R*ϖ(R*+ϖ)2+(Z*Z)2].

Hence, we can write,

q0=ϖ1/2μK(μ)ρ(ϖ,Z)dϖdZ.

As has been explained in an accompanying set of notes, this is precisely the same expression for the gravitational potential that A. Trova, J.-M. Huré and F. Hersant (2012; MNRAS, 424, 2635) used in their study of the potential of self-gravitating, axisymmetric discs.

Our objective, here, is to examine whether or not it might be advantageous to transform this expression to one in which the double integral is performed on a toroidal, rather than a cylindrical, coordinate system.

Chosen Test Mass Distribution[edit]

For purposes of illustration, we will follow the lead of Trova, Huré & Hersant (2012) — see the left-hand panel of the following figure ensemble — and seek to determine the gravitational potential, both inside and outside, of a uniform-density, equatorial-plane torus whose (pink) meridional cross-section is exactly a circle. More specifically, as illustrated in our Figure 1 — see the right-hand panel of the following figure ensemble — at all azimuthal angles, a cross-section through the (pink) torus is prescribed by the familiar algebraic expression for an off-center circle, namely,

(ϖtϖ)2+Z2

=

rt2.

Everywhere inside this toroidal surface we set ρ(ϖ,Z)=ρ0, that is, the density is uniform with the value, ρ0.

Figure 4 extracted without modification from p. 2640 of Trova, Huré & Hersant (2012)
"The Potential of Discs from a 'Mean Green Function'"
Monthly Notices of the Royal Astronomical Society, vol. 424, pp. 2635-2645 © RAS

Our Figure 1

To be inserted: Fig. 4 from Trova, Huré & Hersant (2012)

Diagram of Torus and Toroidal Coordinates

Notice that another off-center circle — this one with a purple perimeter and otherwise white, rather than pink — appears in our Figure 1 diagram. In the discussion that follows, it will be used to represent the meridional-plane cross-section of one axisymmetric surface in an MF53 toroidal-coordinate system. Here we simply point out that this "surface" is also prescribed by an algebraic expression for an off-center circle, namely,

(R0ϖ)2+(Z0Z)2

=

r02.

Toroidal Coordinates[edit]

Click here to find a supporting, detailed illustration of Toroidal Coordinates and relevant integration limits.

Properties[edit]

Here we highlight certain properties and features of the MF53 toroidal coordinate system; more details can be found in a related set of our online notes. Most importantly in the context of our discussion, if (at all azimuthal angles) the origin of the toroidal coordinate system is placed at the cylindrical-coordinate location, (a,Z0), the pair of orthogonal coordinates, (ξ1,ξ2), is related to the cylindrical coordinate pair, (ϖ,Z), via the expressions,

  [MF53] Wikipedia

ϖa

=

(ξ121)1/2ξ1ξ2

=

sinhτcoshτcosθ,

(Z0Z)a

=

±(1ξ22)1/2ξ1ξ2

=

sinθcoshτcosθ.

An off-center circle — such as the white circle with purple perimeter depicted in our Figure 1 diagram — is generated if a value of the "radial" coordinate, ξ1, is chosen from within the range,

[MF53]         Wikipedia

+1ξ1<

        or, equivalently        

0τ<,

and held fixed while the "angular" coordinate, ξ2, is varied over the range,

[MF53]         Wikipedia

1ξ2+1

        or, more completely        

π<θπ

Hereafter, we will refer to this ξ1 = constant circle as a "ξ1-circle." A ξ1-circle of radius zero and, hence, the origin of the toroidal coordinate system is associated with the upper limiting value of the radial coordinate, namely, ξ1=; as the value of ξ1 is decreased monotonically, the radius of the circle (for example, the circle of radius, r0, in our Figure 1) steadily grows; and the radius of this circle becomes infinite at the radial coordinate's other limiting value, ξ1=1.

In the Z=Z0 plane, the location of the inner and outer edges of the toroidal-coordinate surface are determined by setting ξ2=1 (inner) and ξ2=+1 (outer). Hence,

(ϖa)inner

=

(ξ121)1/2ξ1+1=[(ξ11)(ξ1+1)]1/2,

(ϖa)outer

=

(ξ121)1/2ξ11=[(ξ1+1)(ξ11)]1/2.

Hence, also, the (cylindrical) radial location of the "center" of each toroidal-coordinate surface — labeled R0 in our Figure 1 — is given by the expression,

R0=a2[(ϖa)outer+(ϖa)inner]=aξ1(ξ121)1/2,

and the surface's cross-sectional radius — labeled r0 in our Figure 1 — is given by the expression,

r0=a2[(ϖa)outer(ϖa)inner]=a(ξ121)1/2.

This last expression quantifies, and its simplicity reinforces, our earlier statement; that is, as the value of ξ1 is decreased monotonically, the radius of the circle, r0, steadily grows. The next-to-last expression makes it clear, as well, that R0 grows larger and, therefore, the location of the center of a ξ1-circle shifts farther away from the symmetry axis as the value of ξ1 is decreased. Notice that, for any off-center circle, the ratio of these to lengths gives the value of the toroidal-coordinate system's dimensionless "radial" coordinate, that is,

R0r0

=

[aξ1(ξ121)1/2][(ξ121)1/2a]=ξ1.

Notice, furthermore, that there is a particular combination of these two lengths that is independent of ξ1, namely,

r0[(R0r0)21]1/2

=

a(ξ121)1/2[ξ121]1/2=a.

This is a manner in which one can determine the radial position, a, of the origin of the toroidal coordinate system that could legitimately be associated with any particular off-center circle, such as the white circle with a purple perimeter drawn in our Figure 1.

Connection With the Physical Problem[edit]

Earlier, we stated that the off-center circle with purple perimeter displayed in Figure 1 is prescribed by the algebraic expression,

(R0ϖ)2+(Z0Z)2

=

r02.

Let's plug in the "toroidal-coordinate" expressions for each parameter that appears on the left-hand side of this relation and see whether, after simplification, it reduces to the right-hand side.

LHS

=

(R0ϖ)2+(Z0Z)2

 

=

[aξ1(ξ121)1/2a(ξ121)1/2ξ1ξ2]2+[±a(1ξ22)1/2ξ1ξ2]2

 

=

a2(ξ121){[ξ1(ξ121)ξ1ξ2]2+[(1ξ22)1/2(ξ121)1/2ξ1ξ2]2}

 

=

a2(ξ121)(ξ1ξ2)2{[ξ1(ξ1ξ2)(ξ121)]2+(1ξ22)(ξ121)}

 

=

a2(ξ121)(ξ1ξ2)2[(1ξ1ξ2)2+(ξ121ξ12ξ22+ξ22)]

 

=

a2(ξ121)(ξ1ξ2)2[ξ122ξ1ξ2+ξ22]

 

=

a2(ξ121).

This, indeed, equals the right-hand side of the relation, which is, r02. It all nicely checks out!

Next, taking a hint from the EUREKA! moment recorded in our accompanying notes, let's rewrite the function X in terms of toroidal rather than cylindrical coordinates, where X is the argument of the special function, Q1/2, that appears in the above definition of q0. More specifically, let's assume that the coordinate location at which the gravitational potential is to be evaluated, (R*,Z*), is taken to be the cylindrical-coordinate location of the origin of the toroidal coordinate system, (a,Z0). Given this association, we can write,

X

R*2+ϖ2+(Z*Z)22R*ϖ

 

=

a2+ϖ2+(Z0Z)22aϖ

 

=

1+(ϖ/a)2+[(Z0Z)/a]22(ϖ/a)

X2

=

[2(ϖa)]2{1+(ϖa)2+[(Z0Z)a]2}2

 

=

[2(ξ121)1/2ξ1ξ2]2{1+[(ξ121)1/2ξ1ξ2]2+[±(1ξ22)1/2ξ1ξ2]2}2

 

=

(ξ1ξ2)24(ξ121)[1+(ξ121)(ξ1ξ2)2+(1ξ22)(ξ1ξ2)2]2

 

=

14(ξ121)(ξ1ξ2)2[(ξ1ξ2)2+(ξ121)+(1ξ22)]2

 

=

[2ξ1(ξ1ξ2)]24(ξ121)(ξ1ξ2)2

 

=

ξ12ξ121.

Hence, when the function, q0, is rewritten in terms of the elliptic integral of the first kind, K(μ), the modulus of K can be written as,

μ2

=

2[1+X]1

 

=

2[1+ξ1(ξ121)1/2]1

 

=

2(ξ121)1/2(ξ121)1/2+ξ1.

This is the key result motivating the use of a toroidal coordinate system to evaluate the gravitational potential: When expressed in an appropriately defined toroidal coordinate system, the modulus of the special function is a function of one, rather than two, spatial coordinates. This gives some hope that the integral over the second (angular) coordinate, ξ2, can be completed analytically, giving rise to an expression for the gravitational potential whose evaluation only requires numerical integration over a single (radial) coordinate, ξ1.

Finally, drawing on discussion in our accompanying set of notes, we recognize that, expressed in terms of toroidal coordinates, the differential area element in the meridional plane is,

dσ

=

a2[dξ1(ξ1ξ2)(ξ121)1/2][dξ2(ξ1ξ2)(1ξ22)1/2].

Putting everything together, then, the (indefinite) integral expression for q0, expressed in terms of toroidal-coordinates, is,

q0

=

[a(ξ121)1/2ξ1ξ2]1/2μK(μ)ρ(ξ1,ξ2)[a(ξ1ξ2)(ξ121)1/2][a(ξ1ξ2)(1ξ22)1/2]dξ1dξ2

 

=

a5/2(ξ121)1/4μK(μ)dξ1ρ(ξ1,ξ2)[dξ2(ξ1ξ2)5/2(1ξ22)1/2]

 

=

21/2a5/2[(ξ121)1/2+ξ1]1/2K(μ)dξ1ρ(ξ1,ξ2)[dξ2(ξ1ξ2)5/2(1ξ22)1/2].


Making the substitution,

ξ2cosθ                 dξ2sinθdθ ,

gives,

q0

=

21/2a5/2ξ1|minξ1|maxK(μ)dξ1[(ξ121)1/2+ξ1]1/2θminθmaxρ(ξ1,θ)[dθ(ξ1cosθ)5/2],

where we have now explicitly introduced four parameters to set definite limits on the nested pair of integrations. Making the additional substitution,

ξ1coshx                 dξ1sinhxdx ,

gives,

q0

=

21/2a5/2xminxmaxK(μ)sinhxdx(sinhx+coshx)1/2θminθmaxρ(ξ1,θ)[dθ(ξ1cosθ)5/2],

where, written in terms of x,

μ

=

[2sinhxsinhx+coshx]1/2.

Perform Angular Integration Over Test Mass Distribution[edit]

While, in principle, the pair of nested integrals must be carried out over all of space using the limits,

ξ1|min=1,ξ1|max=,θmin=π,     and     θmax=+π,

in practice, the limits should be set to reflect the volume boundaries of the mass distribution that is responsible for generating the gravitational potential. Here we present analytic expressions for these limits in the case of the (pink) toroidal test mass distribution specified above; details regarding the derivation of these expressions can be found in our accompanying set of notes.

Identifying Limits of Integration[edit]

Figure 2

Diagram of Torus and Toroidal Coordinates

The animation shown here in Figure 2 builds upon the configuration displayed in our Figure 1, above. It shows a meridional cross-section through the selected (pink) uniform-density, toroidal mass distribution, whose geometric properties are fully determined by specifying values for ϖt and rt. (For the example illustrated in Figure 2, we have specified the same values used by Trova, Huré & Hersant (2012) to construct their Figure 4, as reprinted above; namely, ϖt=3/4 and rt=1/4.) Throughout the Figure 2 animation sequence, these two parameters have been fixed — thereby fixing the properties of the (pink) torus — and, in addition, we have fixed the location of the origin of a toroidal coordinate system — identified by the red-filled circular dot. We explicitly associate this coordinate-system origin with the (cylindrical) coordinates of the point in space at which we choose to evaluate the gravitational potential, namely, (R*,Z*)=(a,Z0). [For illustration purposes, in Figure 2 we have set (a,Z0)=(1/3,3/4).]

While the values of the four primary model parameters (a,Z0,ϖt,rt) are held fixed, Figure 2 depicts in a quantitatively precise manner how the size of a ξ1= constant toroidal surface (the off-center circle traced by the sequence of black dots) varies as the value of the radial coordinate, ξ1, is varied. In each frame of the animation sequence, the value of ξ1 that was used to define the (black) ξ1-circle is printed in the lower-right corner of the image; additional quantitative details associated with each animation frame can be obtained from the table titled, "Example 2" in our accompanying notes.


As the value of ξ1 is varied from large values (small black circles) to smaller values (larger black circles), there is a maximum value, ξ1|max, at which the ξ1-circle first makes contact with the (pink) equatorial-plane torus, and there is a minimum value, ξ1|min, at which it makes its final contact. These are the limiting values of the toroidal radial coordinate to be used in the integration that produces q0. At all values within the parameter range,

ξ1|max>ξ1>ξ1|min,

the ξ1-circle intersects the surface of the torus in two locations, defined by two different values of the associated angular coordinate, ξ2. In each frame of the animation, points of intersection are marked with small yellow diamonds; the coordinates of these points of intersection are listed in the table associated with example 2, in our accompanying notes. For each relevant value of ξ1, these are the limiting values of the toroidal angular coordinate to be used in the integration that produces q0. It should be realized that, at the first and final points of contact, the two values of ξ2 are degenerate.

Notice in the animation that, while the origin of the selected toroidal coordinate system (the filled red dot) remains fixed, the center of the ξ1-circle does not remain fixed. In order to highlight this behavior, the location of the center of the ξ1-circle has been marked by a filled, light-blue square and, in keeping with the earlier Figure 1 diagram, a vertical, light-blue line connects this center to the equatorial plane of the cylindrical coordinate system.

Associated Analytic Expressions[edit]

We define the following terms that are functions only of the four principal model parameters, (a,Z0,ϖt,rt), and therefore can be treated as constants while carrying out the pair of nested integrals that determine q0:

  Parameters evaluated for Figure 2

κ

Z02+a2(ϖt2rt2)

   

5224320.17361111

C

1+(2Z0κ)2(ϖt2rt2)

   

1714095438.3248

β±

κ2[ϖtrtC(ϖt+rt)(ϖtrt)]

   

52263[11714093254]

Then,

ξ1|max=[1(aϖtβ+)2]1/21.1927843         and         ξ1|min=[1(aϖtβ)2]1/21.0449467,

which implies,

xmax=tanh1(aϖtβ+)0.61137548         and         xmin=tanh1(aϖtβ)0.29871048.



Also let,

ξ1coshx,         in which case,         (ξ121)1/2sinhx     and,     (1ξ12)1/2=ξ1(ξ121)1/2cothx,

and define,

 Evaluated for
  xmax(i.e.ξ1|max)


          xmin(i.e.ξ1|min)


A(ξ1)

(Z0a)2+[cothxϖta]2

   

5.23510376

         

6.49460545

B(ξ1)

cothxϖta+(2ϖtZ02aκ)

   

14.1645439

         

15.77670608

Figure 3

Diagram of Torus and xi_2-constant Toroidal Coordinate curve

Then, for each value of the radial coordinate, ξ1=coshx, within the range,

xmaxxxmin,

the limiting values (±) of the angular coordinate are,

ξ2|±

=

coshxsinhx(2a2κAB)[1±1ACB2]1.

This provides the desired analytic expression for the two limits of integration over the angular coordinate that must be carried out in order to evaluate the key function, q0, in our determination of the gravitational potential at the cylindrical-coordinate location, (R*,Z*)=(a,Z0).

We should note that at both limits — that is, at the two values of x for which the functions A and B have been evaluated, immediately above — the ratio under the square-root,

ACB2=1.

Hence, at both radial-coordinate limits, the two angular-coordinate limits, ξ2|±, are degenerate. Furthermore, we have discovered that the value of this degeneracy angle is exactly the same at both radial-coordinate limits; specifically, we find that, for our chosen test-mass distribution,

ξ2|deg0.885198.

This means that exactly the same ξ2-constant, toroidal-coordinate "line" intersects the surface of the (pink) test-mass torus at both the point of first contact (ξ1|max) and the point of final contact (ξ1|min). In order to illustrate this, this particular ξ2-constant "line" has been traced by a sequence of red dots in Figure 3. As just described, it passes smoothly through the points on the surface of the (pink) torus where the ξ1-circles make first (small black-dotted circle) and final (large black-dotted circle) contact.

Integrate[edit]

Because the density is uniform throughout our test model torus, it can be pulled out of both integrals. In combination with the limits of integration just derived, we can therefore write,

q0

=

21/2a5/2ρ0tanh1[a/(ϖtβ)]tanh1[a/(ϖtβ+)]K(μ)sinhxdx(sinhx+coshx)1/2cos1(ξ2|)cos1(ξ2|+)[dθ(ξ1cosθ)5/2].

Now, using WolframAlpha's online integrator, we find …

WolframAlpha Integration

Hence, the inner integral over our toroidal system's angular coordinate gives,

cos1(ξ2|)cos1(ξ2|+)[dθ(ξ1cosθ)5/2]

=

{23(ξ121)2(ξ1cosθ)3/2[sinθ(5ξ12+4ξ1cosθ+1)

 

 

+(ξ1+1)(ξ11)2(ξ1cosθξ11)3/2F(θ2|2ξ11)

 

 

+4ξ1(ξ11)(ξ1cosθξ11)1/2(cosθξ1)E(θ2|2ξ11)]}cos1(ξ2|)cos1(ξ2|+)

 

=

23(ξ121)2[sinθ(5ξ124ξ1cosθ1)(ξ1cosθ)3/2]cos1(ξ2|)cos1(ξ2|+)

 

 

+2(ξ11)1/23(ξ121)2[4ξ1E(θ2|2ξ11)(ξ1+1)F(θ2|2ξ11)]cos1(ξ2|)cos1(ξ2|+)

This last expression exactly matches the expression found in the integral tables published by Gradshteyn & Ryzhik (1965) — specifically, relation 2.575(5) — after it is realized that the second argument of both elliptic integral functions, as published in GR65, is the square-root of the parameter, m=k2, provided by WolframAlpha.

We now have to deal with the realization that, for our particular problem, ξ11, which means that the second argument, m=2/(1ξ1), of both elliptical integral functions is negative (if not zero). Following the discussion provided at mymathlib.com, we define,

k12ξ11       and       k1'1(ik1)2=1+2ξ11=ξ1+1ξ11,

in which case,

k1k1'=2ξ1+1,

and we can write,

F(θ2|2ξ11)F(θ2,ik1)

=

1k1'[K(k1k1')F(πθ2,k1k1')],

E(θ2|2ξ11)E(θ2,ik1)

=

k1'[E(k1k1')E(πθ2,k1k1')].


Hence,

cos1(ξ2|)cos1(ξ2|+)[dθ(ξ1cosθ)5/2]

=

23(ξ121)2{[sinθ(5ξ124ξ1cosθ1)(ξ1cosθ)3/2]

 

 

+4ξ1(ξ11)1/2ξ1+1ξ11[E(2ξ1+1)E(πθ2,2ξ1+1)]

 

 

(ξ11)1/2(ξ1+1)ξ11ξ1+1[K(2ξ1+1)F(πθ2,2ξ1+1)]}cos1(ξ2|)cos1(ξ2|+)

 

=

2(ξ1+1)1/23(ξ121)2[sinθ(5ξ124ξ1cosθ1)(ξ1+1)1/2(ξ1cosθ)3/2

 

 

4ξ1E(πθ2,2ξ1+1)+(ξ11)F(πθ2,2ξ1+1)]cos1(ξ2|)cos1(ξ2|+).

We have therefore succeeded in deriving an expression for the gravitational potential of a uniform-density torus that requires numerical integration over only one dimension, that is, the "radial" dimension, ξ1. The final, combined expression is,

Φ(a,Z0)

=

25/2Gρ0a23ξ1|minξ1|max(ξ1+1)1/2K(μ)dξ1(ξ121)2[(ξ121)1/2+ξ1]1/2[sinθ(5ξ124ξ1cosθ1)(ξ1+1)1/2(ξ1cosθ)3/2

 

 

4ξ1E(πθ2,2ξ1+1)+(ξ11)F(πθ2,2ξ1+1)]cos1(ξ2|)cos1(ξ2|+).


Code Layout[edit]

Here are some suggestions related to the development of a computer program that can perform the one-dimensional integral over ξ1.

STEP 1:  Specify numerical values for torus parameters … varpi_t & r_t

STEP 2:  Associate the parameters "a" and "Z0" with the cylindrical coordinate 
         location (R*,Z*) at which gravitational potential is to be evaluated.

STEP 3:  Given the numerical values for these four parameters, calculate "kappa", 
         "C", "beta_plus", and "beta_minus" as prescribed by the following algebraic 
         relations …

κ

Z02+a2(ϖt2rt2)

C

1+(2Z0κ)2(ϖt2rt2)

β±

κ2[ϖtrtC(ϖt+rt)(ϖtrt)]

STEP 4:  The (numerical values of the) limits of integration are set by the following 
         two expressions …

ξ1|max=[1(aϖtβ+)2]1/2

and

ξ1|min=[1(aϖtβ)2]1/2.

STEP 4 (cont.):  Establish a 1D grid with, say, 100 zones, assigning values of xi_1 
         that are equally spaced between these two limiting values; let "delta" be the 
         grid spacing.  (Perhaps use logarithmic spacing.)  The mid-point value of 
         the coordinate location of the accompanying 99 grid cells should also be 
         determined.

STEP 5:  For each of the 99 grid-cell coordinate values, "xi1", calculate the following 
         parameter, or aggregate-term, values:

Φ0

25/2Gρ0a23;

μ

[2(ξ121)1/2(ξ121)1/2+ξ1]1/2;

coef

(ξ1+1)1/2K(μ)(ξ121)2[(ξ121)1/2+ξ1]1/2;

tempbeta

ϖtaξ1(ξ121)1/2;

A

(Z0a)2+(tempbeta)2;

B

(2ϖtZ02aκ)(tempbeta);

(ϖia)±

κ2a2BA[1±1ACB2];

ξ2|±

=

ξ1(ξ121)1/2(ϖi/a)±;

θmax

=

cos1(ξ2|+);

θmin

=

cos1(ξ2|);

T(θ)

sinθ(5ξ124ξ1cosθ1)(ξ1+1)1/2(ξ1cosθ)3/24ξ1E(πθ2,2ξ1+1)+(ξ11)F(πθ2,2ξ1+1),

Φ(a,Z0)

=

Φ0n=199deltacoef[T(θmax)T(θmin)].

Special Case[edit]

In the context of the (pink torus) test-mass distribution being discussed here, a review of the properties of a toroidal coordinate system highlights one particularly interesting (cylindrical) coordinate location at which the gravitational potential should be evaluated:

{R*,Z*}={rt[(ϖtrt)21]1/2,0}.

By placing the origin of the toroidal coordinate system at this and only this location — that is, by setting,

a

=

rt[(ϖtrt)21]1/2=(ϖt2rt2)1/2,

— the limits of integration can be specified very simply: There is only one ξ1-circle that intersects the surface of the torus and it does so by, not simply intersecting, but by perfectly aligning with the surface. This perfect overlap with the surface of the torus happens for the coordinate circle associated with,

ξ1=ξsϖtrt.

All ξ1-circles larger than this one — that is, all circles corresponding to values of

ξ1<ξs

— lie entirely outside of the (pink) torus and therefore need not be included in the integration to determine the gravitational potential; while all ξ1-circles smaller than this one — that is, all circles corresponding to values of

ξ1>ξs

— lie entirely inside of the (pink) torus. Hence, in this special case the radial-coordinate integration limits are,

ξ1|min=ϖtrt         and         ξ1|max=.

Furthermore, because the corresponding ξ1-circles fall entirely inside (or on the surface of) the torus for all values of ξ1 in this latter range, the integral over the "angular" toroidal coordinate, θcos1ξ2, will have the simple limits,

θmin=π         and         θmax=+π.

(More practically, we will integrate from zero to π, and double the result.) Hence, the inner integral over our toroidal system's angular coordinate gives,

ππ[dθ(ξ1cosθ)5/2]

=

20π[dθ(ξ1cosθ)5/2]

 

=

4(ξ1+1)1/23(ξ121)2[sinθ(5ξ124ξ1cosθ1)(ξ1+1)1/2(ξ1cosθ)3/24ξ1E(πθ2,2ξ1+1)+(ξ11)F(πθ2,2ξ1+1)]0π

 

=

4(ξ1+1)1/23(ξ121)2[4ξ1E(π2,2ξ1+1)(ξ11)F(π2,2ξ1+1)]

 

=

4(ξ1+1)1/23(ξ121)2[4ξ1E(2ξ1+1)(ξ11)K(2ξ1+1)].

So, we have,

q0

=

21/2a5/2ρ0ϖt/rt[(ξ121)1/2+ξ1]1/2K(μ){4(ξ1+1)1/23(ξ121)2[4ξ1E(2ξ1+1)(ξ11)K(2ξ1+1)]}dξ1,

 

=

25/2a5/2ρ03ϖt/rt(ξ1+1)1/2K(μ)(ξ121)2[(ξ121)1/2+ξ1]1/2[4ξ1E(2ξ1+1)(ξ11)K(2ξ1+1)]dξ1

Φ(ϖt2rt2,0)

=

27/2(ϖt2rt2)Gρ03ϖt/rt(ξ1+1)1/2K(μ)(ξ121)2[(ξ121)1/2+ξ1]1/2[4ξ1E(2ξ1+1)(ξ11)K(2ξ1+1)]dξ1,

where,

μ

=

[2(ξ121)1/2(ξ121)1/2+ξ1]1/2.

TO BE DONE:


As we have detailed in an accompanying discussion, using toroidal coordinates Wong (1973) derived an expression for the potential at any point inside or outside of a uniform-density torus that has a circular cross-section — as illustrated by the pink torus, above. At some point, we should compare the expression that Wong derived to our independent derivation, as presented in this chapter; in particular, our "special case" should be compared with Wong's equation (2.57), which gives an expression for the potential after integration over both of the angular toroidal coordinates, (θ,ψ), but before the radial integration has been completed. His expression is,

ΦWong(η',θ')

=

GU(η',θ')

 

=

29/2Gρ0a23(coshη'cosθ')1/2nϵncos(nθ')η0dη[Qn1/22(coshη)sinhη]

 

 

×Pn1/2(coshη)Qn1/2(coshη').

This expression should be evaluated at η'=+, in which case it appears as though it should match our "special case" result for all values of the polar angle, θ'.

Let's see if the expression simplifies somewhat by adopting a variable,

ϵ1ξ1                 dξ1d(ϵ1)=ϵ2dϵ.

Making this substitution, and defining,

Φnorm23(ϖt2rt2)Gρ03,

we have,

Φnorm1Φ(ϖt2rt2,0)

=

rt/ϖt021/2ϵ(1+ϵ)1/2K(μ)(1ϵ2)2[(1ϵ2)1/2+1]1/2[4E(2ϵ1+ϵ)(1ϵ)K(2ϵ1+ϵ)]dϵ,

 

=

rt/ϖt0ϵμK(μ)(1ϵ2)2[1+ϵ1ϵ]1/4[4E(2ϵ1+ϵ)(1ϵ)K(2ϵ1+ϵ)]dϵ,

where,

μ

=

21/2[1+(1ϵ2)1/2]1/2.

Total Mass[edit]

How do I know whether or not I have made mistakes in these derivations? Aside from the published work of Trova, Huré & Hersant (2012), how do I know what the correct answer for the gravitational potential of a uniform-density torus is?

A degree of assurance can be drawn by carrying out a similar pair of nested integrations to determine the total mass (or volume) of the torus that is defined by our chosen test-mass distribution. As can be found in many mathematics handbooks, or online, the volume of our defined torus should be,

Vtorus=2π2ϖtrt2.

Using Cylindrical Coordinates[edit]

Total Volume[edit]

Let's start by integrating the three-dimensional volume element, dV3D, over the azimuthal angle to obtain an expression for the two-dimensional differential volume element that is written in terms of the meridional-plane differential area, dσ, as used in our definition of q0, above. Using the notation of MF53 (but employing the opposite sign convention from them), in cylindrical coordinates we have,

dV3D

=

[h1dξ1][h2dξ2][h3dξ3]

 

=

dξ1[ξ11ξ22dξ2]dξ3

 

=

dϖ[ϖd(cosφ)1cos2φ]dz

 

=

+[ϖdφ]dσ,

where, as before in cylindrical coordinates, dσ=dϖdz. From this we obtain,

dV2D

=

ϖdσ02πdφ

 

=

2πϖdσ.

Now in order to finish the volume integration, we need the limits of integration in the meridional plane. These can be obtained from the above algebraic description of the (pink) test-mass torus as an off-center circle. Specifically, we have,

V

=

2π(ϖtrt)(ϖt+rt)ϖdϖrt2(ϖtϖ)2rt2(ϖtϖ)2dz

 

=

4π(ϖtrt)(ϖt+rt)rt2(ϖtϖ)2ϖdϖ

 

=

2π3{3rt2ϖttan1[ϖϖtrt2(ϖtϖ)2][rt2(ϖtϖ)2]1/2(2rt2+ϖt2+ϖtϖ2ϖ2)}(ϖtrt)(ϖt+rt)

 

=

2π3{3rt2ϖttan1[rt0]0}2π3{3rt2ϖttan1[rt0]0}

 

=

2π3[3rt2ϖt(π2)]+2π3[3rt2ϖt(π2)]

 

=

2π2rt2ϖt,

where we have carried out the second integration using the WolframAlpha online integral calculator:

WolframAlpha integration result
WolframAlpha integration result

This is the answer for the volume of a torus that we expected. Good!

Volume with Cropped Top[edit]

Diagram of "Cropped Top" Torus
Diagram of "Cropped Top" Torus

During my development of a computer program to integrate over the volume of a circular torus while using toroidal coordinates, I decided that it would be useful to determine the volume of a torus that has a "cropped top" as illustrated in the accompanying diagram, shown here on the right. Let's evaluate this "cropped-top" volume using cylindrical coordinates so that we will know what the correct answer is when developing an integration scheme using toroidal coordinates. Specifically, let's determine the volume of the "green" portion for a specified value of h<rt.

The radial integration will be evaluated between the limits: (lower) (ϖtb) and (upper) (ϖt+b), where,

b=rt2h2.

And the limits on the vertical integration will be: (lower) h and, as before when integrating over the entire volume, (upper) rt2(ϖtϖ)2. With these limits, the volume integration gives,

Vgreen

=

2π(ϖtb)(ϖt+b)ϖdϖhrt2(ϖtϖ)2dz

 

=

2π(ϖtb)(ϖt+b)ϖdϖ[rt2(ϖtϖ)2h]

 

=

2πh(ϖtb)(ϖt+b)ϖdϖ+2π(ϖtb)(ϖt+b)ϖXdϖ,

where,

X

a0+a1ϖ+a2ϖ2,

a0

(ϖt2rt2),

a1

2ϖt,

a2

1.

Carrying out this pair of integrations gives,

Vgreen

=

πh[(ϖt+b)2(ϖtb)2]+2π[XX3a2a1(2a2ϖ+a1)8a22X](ϖtb)(ϖt+b)

 

 

2πa1(4a0a2a12)(4a2)2(ϖtb)(ϖt+b)dϖX

 

=

πh[ϖt2+2bϖt+b2(ϖt22bϖt+b2)]+π12{8[rt2(ϖtϖ)2]3/2+6ϖt(2ϖ2ϖt)[rt2(ϖtϖ)2]1/2}(ϖtb)(ϖt+b)

 

 

2πa1(4a0a2a12)(4a2)2{1a2sin1[2a2ϖ+a1a124a0a2]}(ϖtb)(ϖt+b)

 

=

4πhbϖt+π3[3ϖtb(rt2b2)1/22(rt2b2)3/2]+π3[3ϖtb(rt2b2)1/2+2(rt2b2)3/2]

 

 

πϖt(a0+ϖt2){sin1[ϖtϖϖt2+a0]}(ϖtb)(ϖt+b)

 

=

4πhbϖt+2πϖtb(rt2b2)1/2πϖtrt2{sin1[brt]sin1[brt]}

 

=

4πhϖt(rt2h2)1/2+2πϖth(rt2h2)1/2+2πϖtrt2sin1[1(hrt)2]1/2

 

=

2πϖtrt2{sin1[1(hrt)2]1/2(hrt)[1(hrt)2]1/2}.

Hence, the fractional volume is,

Analytic Expression for Green Volume

VgreenVtorus

=

1π{sin1[1(hrt)2]1/2(hrt)[1(hrt)2]1/2}.

Diagram of "Cropped Top" Torus
Diagram of "Cropped Top" Torus


REALITY CHECK: This should give a zero (green) volume if h=rt; and the fractional volume should be one-half if h=0. In the former case, our expression gives,

VgreenVtorus

=

1πsin1(0)=0,

as expected. And in the latter case we have,

VgreenVtorus

=

1πsin1(1)=12,

which means that Vgreen is indeed half of the total torus volume, as derived earlier.

Using Toroidal Coordinates with Special Alignment[edit]

If, instead, we use a toroidal coordinate system, we have (see p. 666 of MF53),

dV3D

=

[h1dξ1][h2dξ2][h3dξ3]

 

=

[adξ1(ξ1ξ2)ξ121][adξ2(ξ1ξ2)1ξ22][(ξ1211ξ32)1/2adξ3(ξ1ξ2)]

 

=

dσ[a(ξ121)1/2(ξ1ξ2)d(cosφ)1cos2φ]

 

=

+[ϖdφ]dσ,

where, as employed above, a differential area element in the meridional plane of a toroidal-coordinate system is,

dσ

=

a2[dξ1(ξ1ξ2)ξ121][dξ2(ξ1ξ2)1ξ22].

As in the case of the cylindrical coordinate system, because the torus is axisymmetric, integration over the azimuthal angular coordinate in a toroidal coordinate system gives,

dV2D

=

ϖdσ02πdφ

 

=

2πϖdσ.

Cross-check: Wikipedia's Differential Volume Element

dV3D

=

[h1dτ][h2dθ][h3dφ]

 

=

a3[dτcoshτcosθ][dθcoshτcosθ][sinhτdφcoshτcosθ]

 

=

dσϖdφ,

where,

dσ

=

[acoshτcosθ]2dτdθ,

and, as above,

ϖa

=

sinhτcoshτcosθ.

Hence, in agreement with the expression derived using the notation of MF53,

dV2D

=

ϖdσ02πdφ

 

=

2πϖdσ.

Now, if we choose a toroidal coordinate system whose origin is located exactly as defined in our special case, above, the radial-coordinate integration limits should be,

ξ1|min=ϖtrt         and         ξ1|max=;

and the integral over the "angular" toroidal coordinate will have the simple limits,

ξ2|=1         and         ξ2|+=+1.

[COMMENT: Actually, these limits will only capture integration over either the upper hemisphere (Z positive) or the lower hemisphere (Z negative). So I will probably need to double the volume expression that results from these limits.]


So, integration over the remaining two (meridional-plane) coordinates gives,

V

=

2πΣϖdσ

 

=

2πa3ϖt/rtdξ111(ξ121)1/2(ξ1ξ2)[1(ξ1ξ2)ξ121][1(ξ1ξ2)1ξ22]dξ2

 

=

2πa3ϖt/rtdξ111[dξ2(ξ1ξ2)31ξ22].

If, following MF53, we make the substitution,

ξ2cosζ             dξ2sinζdζ,

we can write,

V

=

2πa3ϖt/rtdξ10π[dζ(ξ1cosζ)3]

 

=

πa3ϖt/rtdξ1{sinζ[4ξ123ξ1cosζ1](ξ121)2(ξ1cosζ)22(2ξ12+1)tanh1[(ξ1+1)tan(ζ/2)1ξ12](1ξ12)5/2}0π,

where the expression obtained after integrating over ζ was obtained from WolframAlpha's online integrator.

[COMMENT: This result is problematic because it was derived without enforcing the condition, ξ12>1. Notice, in particular, that the last term includes a couple of square-roots of expressions that will naturally be negative.]

Carrying out this same integration (specifying wider integration limits based on the toroidal-coordinate specification described in Wikipedia) via multiple steps using the integral tables published by Gradshteyn & Ryzhik, I have obtained,

V

=

2πa3ϖt/rtdξ1ππ[dζ(ξ1cosζ)3]

 

=

πa3ϖt/rtdξ1{sinζ[4ξ123ξ1cosζ1](ξ121)2(ξ1cosζ)2+[2(2ξ12+1)(ξ121)5/2]tan1[tan(ζ2)(ξ1+1)1/2(ξ11)1/2]}ππ.

This expression makes more sense; at least the arguments of the square-roots are all positive. Now, evaluating the limits: (1) The first term inside the curly braces goes to zero at both limits; and (2) the argument of the arctangent is ±. Hence, the result of taking the arctangent is +π2, at the upper limit, and is π2 at the lower limit. Hence, we have,

V

=

πa3ϖt/rtdξ1{[2(2ξ12+1)(ξ121)5/2](π2+π2)}

 

=

2π2a3ϖt/rt[(2ξ12+1)(ξ121)5/2]dξ1

 

=

2π2a3[ξ1(ξ121)3/2]ϖt/rt

 

=

2π2a3[ϖtrt2(ϖt2rt)3/2].

Now, in the special case we are considering here,

a

=

rt[(ϖtrt)21]1/2=[ϖt2rt2]1/2.

Hence,

V

=

2π2ϖtrt2,

which is the answer we were expecting for the volume of the (pink) torus.


Move General Case[edit]

NOTE: A complete prescription of the toroidal-coordinate integration limits that are appropriate for a determination of the volume or the gravitational potential of a circular torus can be found in an accompanying discussion.

In the more general case, the expression for the volume integral should be the same; all we should have to do is incorporate the more general integration limits as specified in our above evaluation of the gravitational potential. Hence, in the more general case we should have,

V

=

πa3ξ1|minξ1|maxdξ1{sinζ[4ξ123ξ1cosζ1](ξ121)2(ξ1cosζ)2+[2(2ξ12+1)(ξ121)5/2]tan1[tan(ζ2)(ξ1+1)1/2(ξ11)1/2]}cos1(ξ2|)cos1(ξ2|+).

Next, referencing various trigonometric relations, we note that,

tan(ζ2)

=

±[1cosζ1+cosζ]1/2

 

=

±[1ξ21+ξ2]1/2.

Hence, in our expression for the torus volume, the argument of the arctangent may be written as,

tan(ζ2)(ξ1+1)1/2(ξ11)1/2

=

±[1ξ21+ξ2]1/2(ξ1+1)1/2(ξ11)1/2

 

=

±[(1ξ2)(1+ξ2)(ξ1+1)(ξ11)]1/2

 

=

±[ξ1+1ξ1ξ2ξ2ξ11+ξ1ξ2ξ2]1/2

 

=

±[(ξ1ξ2)(ξ1ξ21)(ξ1ξ2)+(ξ1ξ21)]1/2

 

=

±[1cosα1+cosα]1/2

 

=

tan(α2),

where,

cosα(ξ1ξ21)(ξ1ξ2)             αcos1[(ξ1ξ21)(ξ1ξ2)]=cos1[(ξ1cosζ1)(ξ1cosζ)].

Hence, the volume integral may be written as,

V

=

πa3ξ1|minξ1|maxdξ1{sinζ[4ξ123ξ1cosζ1](ξ121)2(ξ1cosζ)2+[(2ξ12+1)(ξ121)5/2]cos1[(ξ1cosζ1)(ξ1cosζ)]}cos1(ξ2|)cos1(ξ2|+)

 

=

πa3ξ1|minξ1|maxdξ1{(1ξ22)1/2[4ξ123ξ1ξ21](ξ121)2(ξ1ξ2)2+[(2ξ12+1)(ξ121)5/2]cos1[(ξ1ξ21)(ξ1ξ2)]}ξ2|ξ2|+.

Green Cropped-Top Volume[edit]

Now, if we set Z0=h with 0<h<rt, then the horizontal plane defined by z=Z0 will cut through the circular torus, splitting it into two hemispheres — a lower, pink sub-volume and an upper, green sub-volume as depicted in the above diagram. While using toroidal coordinates to perform the volume integral, we recognize that this horizontal plane is also identified by setting the angular coordinate to ξ2=+1 [if a(ϖtb)] or to ξ2=1 [if a(ϖt+b)]. Then, using the former case as an example, for each value of ξ1 (corresponding to a specific ξ1- circle) the integral over the angular, ξ2 coordinate should naturally break into two segments: The segment falling within the green sub-volume should have integration limits, ξ2|+1; and the segment falling within the pink sub-volume should have integration limits, 1ξ2|. Let's see if specification of these limits allows us to derive an analytic expression for the green sub-volume that matches the expression for Vgreen as derived above using cylindrical coordinates.


Notice that, for the green sub-volume, the limits on ξ1 should correspond to ξ2=+1 and ϖ=(ϖt±b). Because, in general,

ϖ

=

a(ξ121)1/2ξ1ξ2,

this means that the limits on ξ1 are (valid only for 0<Z0<rt),

ϖt±b

=

a(ξ121)1/2ξ11

ϖt±rt2Z02

=

a(ξ1+1)1/2(ξ11)1/2ξ11

 

=

a[ξ1+1ξ11]1/2

(ξ11)[ϖt±rt2Z02]2

=

a2(ξ1+1)

ξ1{[ϖt±rt2Z02]2a2}

=

[ϖt±rt2Z02]2+a2

ξ1|±

=

[ϖt±rt2Z02]2+a2[ϖt±rt2Z02]2a2.

Hence, according to our just-derived volume integral, we have,

Toroidal-Coordinate Integral Expression for Green Volume

Vgreen

=

πa3ξ1|ξ1|+dξ1{(1ξ22)1/2[4ξ123ξ1ξ21](ξ121)2(ξ1ξ2)2+[(2ξ12+1)(ξ121)5/2]cos1[(ξ1ξ21)(ξ1ξ2)]}1ξ2|+.

Diagram of "Cropped Top" Torus
Diagram of "Cropped Top" Torus

Note from J. E. Tohline: On 4 November 2015, a fortran subroutine was used to numerically perform this 1D integration and thereby determine the volume of the green segment of a "cropped top" torus. The name of this fortran code was …

philip.hpc.lsu.edu:/home/tohline/fortran/Toroidal/testI3.for

The following table presents results of tests run with different sets of physical parameters and different numbers of 1D integration steps (nzones); note that the analytic expression for the angular integration limit, ξ2|+, is given in the above table of parameter expressions. In the following table, values of Vgreen obtained by numerical integration are compared with values obtained from the analytic expression derived above via a cylindrical-coordinate formulation.

Comparison of "Cropped-Top" Volume Determinations

ϖt rt a Z0 Vgreen/Vtorus
Analytic nzones = 5000 nzones = 500
1D Integration Error 1D Integration Error
34 14 13 0.24 4.7727731D-03 4.7727731D-03 -1.66D-08 4.7727865D-03 -2.8D-06
      0.23 1.3417064D-02 1.3417065D-02 -2.6D-08 1.3417115D-02 -3.8D-06
      0.20 5.2044018D-02 5.2044021D-02 -6.3D-08 5.2044404D-02 -7.4D-06
      0.15 1.4237849D-01 1.4237851D-01 -1.6D-07 1.4238095D-01 -1.7D-05
      0.125 1.9550110D-01 1.9550115D-01 -2.4D-07 1.9550595D-01 -2.5D-05
      0.10 2.5231578D-01 2.5231587D-01 -3.4D-07 2.5232459D-01 -3.5D-05
      0.05 3.7353003D-01 3.7353031D-01 -7.4D-07 3.7355809D-01 -7.5D-05
      0.01 4.7454199D-01 4.7454347D-01 -3.3D-06 4.7465374D-01 -2.4D-04

Total Volume by Summing Four Zones[edit]

Let's stick with a discussion of the situation where we set Z0=h with 0<h<rt, and now determine the total volume by adding together four sub-volumes. The green "cropped-top" region is the first of these sub-volume zones. The remaining (pink) portion of the torus can be broken into three adjoining segments — left-to-right — whose two edge boundaries plus two internal interfaces are identified by the following four special values of the "radial" coordinate:

ξ1|max

=

[1(aϖtβ+)2]1/2,

ξ1|+

=

[ϖt+rt2Z02]2+a2[ϖt+rt2Z02]2a2,

ξ1|

=

[ϖtrt2Z02]2+a2[ϖtrt2Z02]2a2,

ξ1|min

=

[1(aϖtβ)2]1/2.

As presented in the following table, we have determined the values of these four boundary/interface radial coordinates for the same set of parameter values as in the previous table. Notice that, as listed, they represent monotonically increasing values of the radial coordinate. Between the first two boundaries and between the last two boundaries, the limits on the "angular" coordinate should be the normal,  ξ2|ξ2|+. But between the second and third boundaries, the integration limits on the angular coordinate should be,  ξ2|+1.

Various Boundary Values for ξ1

ϖt rt a Z0 ξ1|max ξ1|+ ξ1| ξ1|min
34 14 13 0.24 1.1859 1.3959 1.6326 2.0312
      0.23 1.1900 1.3655 1.7077 2.0630
      0.20 1.2021 1.3180 1.8929 2.1603
      0.15 1.2209 1.2808 2.1611 2.3213
      0.125 1.2291 1.2700 2.2808 2.3963
      0.10 1.2363 1.2622 2.3872 2.4637
      0.05 1.2464 1.2529 2.5436 2.5638
      0.01 1.2499 1.2501 2.5977 2.5985

See Also[edit]

References[edit]

  1. Morse, P.M. & Feshmach, H. 1953, Methods of Theoretical Physics — Volumes I and II
  2. Cohl, H.S. & Tohline, J.E. 1999, ApJ, 527, 86-101
  3. Cohl, H.S., Rau, A.R.P., Tohline, J.E., Browne, D.A., Cazes, J.E. & Barnes, E.I. 2001, Phys. Rev. A, 64, 052509
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