Appendix/Ramblings/ToroidalCoordinates

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Toroidal Configurations and Related Coordinate Systems

This rather long and rambling chapter reveals how my train of thought progressed as I effectively taught myself how to use a toroidal coordinate system to determine the gravitational potential of an axisymmetric configuration. A summary of the key results from this chapter can be found in a primary chapter of this H_Book titled, Using Toroidal Coordinates to Determine the Gravitational Potential.

Preamble

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, if I recall correctly, the argument of this special function (or its inverse) seemed to resemble the radial coordinate of Morse & Feshbach's orthogonal toroidal coordinate system — see more on this, below.

Off-center Circle

In what follows, it will be useful to recall the algebraic expression that defines a circle whose center is not positioned at the origin of a Cartesian coordinate system. Specifically, consider a circle of radius, rc, whose center is located a distance x0 along the plus-x axis and a distance y0 along the plus-y axis. The equation for this circle is,

(xx0)2+(yy0)2=rc2.

Toroidal Coordinates

Presentation by MF53

The orthogonal toroidal coordinate system (ξ1,ξ2,ξ3=cosφ) discussed by MF53 has the following properties:

xa

=

[(ξ121)1/2ξ1ξ2]cosφ,

ya

=

[(ξ121)1/2ξ1ξ2]sinφ,

za

=

(1ξ22)1/2ξ1ξ2,

ϖa[(xa)2+(ya)2]1/2

=

(ξ121)1/2ξ1ξ2,

ra[(xa)2+(ya)2+(za)2]1/2

=

[ξ1+ξ2ξ1ξ2]1/2.

According to MF53, the associated scale factors of this orthogonal coordinate system are:

h1a

=

1(ξ1ξ2)(ξ121)1/2,

h2a

=

1(ξ1ξ2)(1ξ22)1/2,

h3a

=

[(ξ121)1/2ξ1ξ2]1sinφ.

That means that, in the meridional plane, an area element should be,

dσ=(h1dξ1)(h2dξ2)=a2[dξ1(ξ1ξ2)(ξ121)1/2][dξ2(ξ1ξ2)(1ξ22)1/2].

Tohline's Ramblings

My inversion of these coordinate definitions has led to the following expressions:

ξ1

=

r(r2+1)[χ2(r21)2+ζ2(r2+1)2]1/2,

ξ2

=

r(r21)[χ2(r21)2+ζ2(r2+1)2]1/2,

where,

χϖa;ζzaandr=(χ2+ζ2)1/2.

Apparently the allowed ranges of the two meridional-plane coordinates are:

+1ξ1and1ξ2+1.

Example Toroidal Surfaces

In the accompanying figure labeled "Toroidal Coordinate System," we've outlined three different ξ1=constant meridional contours for the MF53 toroidal coordinate system. The illustrated values are,

ξ1

=

1.1

 

(blue);

ξ1

=

1.2

 

(red);

ξ1

=

1.5

 

(gold).

The inner and outer edges of the toroidal surface in the equatorial plane should be determined by setting ξ2=1 (inner) and ξ2=+1 (outer). Hence,

χinner

=

(ξ121)1/2ξ1+1=[(ξ11)(ξ1+1)]1/2

χouter

=

(ξ121)1/2ξ11=[(ξ1+1)(ξ11)]1/2

The equatorial-plane location of the "center" of each torus is,

χ0=12(χouter+χinner)=ξ1(ξ121)1/2,

and the so-called distortion parameter,

δχouterχinnerχ0=2ξ1.


Properties of ξ1=constant Toroidal Surfaces

Curve in
Figure

ξ1

χinner

χouter

χ0

δ

Blue

1.1

0.218

4.583

2.400

1.818

Red

1.2

0.302

3.317

1.809

1.667

Gold

1.5

0.447

2.236

1.342

1.333


What function ζ(ϖ) coincides with these ξ1=constant surfaces? (To be answered!)


Meridional contours of constant ξ1.
Meridional contours of constant ξ1.

Off-center Circle

The curves drawn in the above figure labeled "Toroidal Coordinate System" resemble circles whose centers are positioned a distance χ0 away from the origin. Let's examine whether this is the case by drawing on the familiar expression for such a configuration, as presented above. If this is the case, then the circle as illustrated in the figure will have z0=0 and a radius,

αcrca

=

χouterχ0

 

=

[(ξ1+1)(ξ11)]1/2ξ1(ξ121)1/2

 

=

1(ξ121)1/2,

and the algebraic expression describing the circle will take the form,

(χχ0)2+ζ2=αc2=(ξ121)1.

Let's evaluate the left-hand-side of this expression to see if it indeed reduces to (ξ121)1.

LHS

=

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

 

=

1(ξ1ξ2)2(ξ121){(ξ121)ξ1(ξ1ξ2)}2+(1ξ22)(ξ1ξ2)2

 

=

(ξ1ξ21)2(ξ1ξ2)2(ξ121)+(1ξ22)(ξ1ξ2)2

 

=

1(ξ1ξ2)2(ξ121)[(ξ1ξ21)2+(ξ121)(1ξ22)]

 

=

1(ξ1ξ2)2(ξ121)[ξ12ξ222ξ1ξ2+1)+(ξ121ξ12ξ22+ξ22)]

 

=

ξ122ξ1ξ2+ξ22(ξ1ξ2)2(ξ121)

 

=

1(ξ121).

Yes! So this means that the ξ1=constant toroidal contours can be described by the off-center circle expression,

(χχ0)2+ζ2=(χouterχ0)2,

or,

[χξ1(ξ121)1/2]2+ζ2=1(ξ121).

It also means that, while ξ1 is the official radial coordinate of MF53's toroidal coordinate system, the actual dimensionless radius of the relevant cross-sectional circle is,

αc

=

1(ξ121)1/2.

Papaloizou-Pringle Tori

Summary of Structure

As derived elsewhere, the accretion tori constructed by Papaloizou & Pringle (1984; hereafter PP84) have the following surface properties. For a given choice of the dimensionless Bernoulli constant, CB',

χinner

=

11+12CB';

χouter

=

1112CB';

χ0

=

12(χouter+χinner)=12CB';

δ

χouterχinnerχ0=212CB'.

So if I want to construct PP84 tori that are approximately the same size/shape as the MF53 tori illustrated above, I should choose values of the dimensionless Bernoulli constant as follows:

χ0|PP84

=

χ0|MF53

12CB'

=

ξ1(ξ121)1/2

CB'

=

(ξ121)1/22ξ1.

In the accompanying figure labeled "Papaloizou-Pringle Tori," we've drawn three different CB'=constant meridional contours for the PP84 tori where the values of the dimensionless Bernoulli constants have been chosen to produce values of χ0 that are identical to the values displayed by the three MF53 tori shown above. The following table details properties of these three PP84 tori that have been constructed in an effort to facilitate comparison with the table shown above for MF53 tori.

Properties of CB'=constant PP84 Toroidal Surfaces

Curve in
Figure

CB'

χinner

χouter

χ0

δ

Red

0.208

0.567

4.234

2.400

1.528

Blue

0.276

0.599

3.019

1.809

1.338

Gold

0.373

0.665

2.019

1.342

1.009

Advantageous Coordinate System

According to Kojima's (1986) review of the PP84 discussion — see his equation (14) — surfaces of constant density can be defined by the coordinate, χPP, where,

tanχPP

zz2ϖ2+z2+ϖ2+z21

Indeed, equation (6.6) of PP84 defines the coordinate, χPP, via the expression,

tanχPP

cosθcos2θ+1ϖ0/r,

where,

z=rcosθ

        and        

ϖ=rsinθ.

Let's see if these match. Starting from the Kojima expression, we have,

tanχPP

=

rcosθr2cos2θr+r1

 

=

cosθcos2θ+11/r.

Hence, they are the same, as long as we appreciate that Kojima assumes all length scales are normalized to ϖ0. Let's express this coordinate in terms of the (ξ1,ξ2) toroidal coordinates as defined by MF53, namely,

za

=

(1ξ22)1/2ξ1ξ2,

ϖa[(xa)2+(ya)2]1/2

=

(ξ121)1/2ξ1ξ2,

ra[(xa)2+(ya)2+(za)2]1/2

=

[ξ1+ξ2ξ1ξ2]1/2.

Kojima's expression becomes:

tanχPP

=

z[z2ϖ2+z2+ϖ2+z21]1

 

=

(1ξ22)1/2ξ1ξ2{[(1ξ22)(ξ1ξ2)2][ξ1ξ2ξ1+ξ2]1/2+[ξ1+ξ2ξ1ξ2]1/21}1

 

=

(1ξ22)1/2{(1ξ22)(ξ1ξ2)[ξ1ξ2ξ1+ξ2]1/2+(ξ1+ξ2)1/2(ξ1ξ2)1/2(ξ1ξ2)}1

 

=

(1ξ22)1/2{(1ξ22)(ξ1ξ2)1/2(ξ1+ξ2)1/2+(ξ1+ξ2)1/2(ξ1ξ2)1/2(ξ1ξ2)}1

 

=

(1ξ22)1/2(ξ1ξ2)1/2(ξ1+ξ2)1/2{(1ξ22)+(ξ1ξ2)(ξ1+ξ2)(ξ1ξ2)(ξ1+ξ2)1/2(ξ1ξ2)1/2}1

 

=

(1ξ22)1/2(ξ12ξ22)1/2{(1ξ22)+(ξ12ξ22)(ξ1ξ2)(ξ12ξ22)1/2}1

 

=

[(1ξ22)(ξ12ξ22)]1/2{[(1ξ22)(ξ12ξ22)]+1[(ξ1ξ2)(ξ1+ξ2)]1/2}1.

This does not appear to be very useful or productive!

CCGF Expansion

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, for example, that when expressed in terms of cylindrical coordinates, the axisymmetric potential is,

Φ(R,z)=2GR1/2q0,

where,

q0=(R)1/2ρ(R,z)Q1/2(X)dRdz,

and the dimensionless argument (the modulus) of the special function, Q1/2, is,

XR2+R2+(zz)22RR.

Note: Here we are using X instead of χ (as used by CT99) to represent this dimensionless parameter in order to avoid confusion with our use of χ, above. 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 elliptical integral of the first kind and, for our particular problem,

μ2

2(1+X)1

 

=

2[1+R2+R2+(zz)22RR]1

 

=

[4RR(R+R)2+(zz)2].

Hence, we can write,

q0=(R)1/2ρ(R,z)μK(μ)dRdz.


Confirmation Provided by Trova, Huré and Hersant

In their study of the potential of self-gravitating, axisymmetric discs, A. Trova, J.-M. Huré and F. Hersant (2012; MNRAS, 424, 2635) write (see their equation 1),

Φ(R,Z)

=

2GϖRρ(ϖ,z)kK(k)dϖdz,

where, the modulus, k, of the complete elliptical integral of the first kind is (see their equation 2),

k

=

2ϖR(ϖ+R)2+(Zz)2,

and its relevant domain is, 0k1. After associating zZ, z'z, and R'ϖ, we see that the modulus, k, used by Trova et al. (2012), is precisely the same as the argument, μ, defined in CT99. Hence, the two expressions for the axisymmetric potential, Φ(R,Z), are identical.


Recognition as Circle

If we scale all of the lengths in CT99's expression for X, to a and, along the lines of what was done above, define,

χRaandζzza,

we can rewrite the expression in the form,

(Ra)2+χ2+ζ2

=

2X(Ra)χ.

Now, because,

[χX(Ra)]2

=

χ22X(Ra)χ+X2(Ra)2

2X(Ra)χ

=

χ2[χX(Ra)]2+X2(Ra)2,

we can further rewrite the expression as,

(Ra)2+χ2+ζ2

=

χ2[χX(Ra)]2+X2(Ra)2

[χX(Ra)]2+ζ2

=

(Ra)2(X21).

Finally, if we adopt the specific scale factor, a=R, we have,

(χX)2+ζ2=(X21).

So, a curve of constant X produces an off-center circle whose center is located at X and whose radius is X21.

Relating CCGF Expansion to Toroidal Coordinates

We see that curves of constant X (as defined in CT99) are in every respect identical to curves of constant ξ1 (as defined in MF53). The association is straightforward:

EUREKA!

X21=1ξ121.


Do It Again

The question that I've had in the back of my mind for quite some time is, "For what astrophysically interesting problem might we effectively use the toroidal coordinate system in order to derive a much cleaner analytic description of an axisymmetric potential?" Originally, I thought that a suitable configuration might be a uniform-density torus that has a perfectly circular cross-section. After all, the surface of such a torus can be perfectly described as a ξ1=  constant configuration. In a subsection presented below, I began investigating this problem, setting up a toroidal coordinate system to appropriately conform to the surface of such a torus, then calling upon WolframAlpha's online integration tool to complete the integral over the orthogonal coordinate, ξ2, analytically. After giving the problem considerable more thought, however, I realized that, while I could legitimately move the mass-density outside of that first integral, it was not legitimate to move the μK(μ) factor outside of that integral. While it is true that CT99 showed that the μK(μ) factor only depends on the first coordinate in a toroidal coordinate system, it is a different toroidal coordinate system from the one that conveniently aligns with the physical torus! Let's set up the double integral again, but this time let's use the toroidal coordinate system that is defined within the CCGF discussion. We begin by describing geometric relationships between pairs of off-center circles and deriving algebraic expressions that define the conditions under which such circles overlap and/or simply intersect.

Overlap Between Two Off-Center Circles

Figure 2 displays two off-center circles. The solid pink circle represents a meridional cross-section through a uniform-density, axisymmetric torus whose center lies in the equatorial plane of a (ϖ,Z), cylindrical coordinate system; as depicted, ϖt is the size of the major radius of this torus and its cross-sectional radius is rt. The other circle represents a single, ξ1 = constant (toroidal) surface in toroidal coordinates; its major radius is, R0, and its cross-sectional radius is r0. The center of this ξ1 = constant circle lies in the equatorial system of the associated toroidal coordinate system, which is parallel to but, as depicted, lies a distance, Z0, above the equatorial plane of the (ϖ,Z), cylindrical coordinate system.

As drawn, the figure does not identify the precise location of the origin of the toroidal coordinate system. But, in accordance with the properties of such coordinate systems, the origin must lie inside of the referenced circle and to the left of — that is, closer to the Z (symmetry) axis than — the center of the circle, R0.

Figure 2

Diagram of Torus and Toroidal Coordinates

If the size of the ξ1 = constant surface is varied while all the other key parameters (R0,Z0,ϖt,rt) are held fixed, what is the range of values of r0 over which the two depicted circles overlap and/or simply intersect?

Initial Contact

Geometrically we appreciate that, as r0 is increased, the two circles will first touch at a point that lies along the (blue-dashed) line-segment that connects the centers of both circles. More specifically, the initial interception will be at the point identified in Figure 2 by the solid blue dot lying on the surface of the pink torus. The distance between the two centers — which we will denote as h — is also the hypotenuse of a right triangle whose other two sides are of length (opposite the angle, α) ϖtR0 and (adjacent to the angle, α) Z0. We see that the initial interception will occur when r0+rt=h, that is, when

r0=r+

hrt

 

=

[(ϖtR0)2+Z02]1/2rt

 

=

(ϖtR0)[1+Λ2]1/2rt,

where,

Λ

Z0ϖtR0.

For later reference, we note that the cylindrical coordinates associated with this initial point of contact — i.e., the point identified in Figure 2 by the solid blue dot lying on the surface of the pink torus — are,

ϖ+

=

ϖtrtsinα

 

=

ϖtrt(ϖtR0)[(ϖtR0)2+Z02]1/2

 

=

ϖtrt[1+Λ2]1/2,

and,

Z+

=

rtcosα

 

=

rtZ0[(ϖtR0)2+Z02]1/2

 

=

rtΛ[1+Λ2]1/2.

Final Contact

It is easy to see, geometrically, that if the (blue-dashed) line-of-centers and, in particular, if r0 is increased beyond the "initial contact" length of r+, by exactly a length that equals the diameter of the pink torus, 2rt, then the ξ1 = constant circle will make its last contact with the circle that defines the surface of the equatorial-plane torus. Associating the subscript "-" with this point of last contact, we have,

r

r++2rt

 

=

(ϖtR0)[1+Λ2]1/2+rt,

and the associated coordinate-location of this last point of contact,

ϖ

=

ϖt+rt[1+Λ2]1/2,

and,

Z

=

rtΛ[1+Λ2]1/2.

Region of Overlap

From the above discussion and derivations, we conclude that the ξ1 = constant circle will overlap the pink torus and will, accordingly, intersect the surface of that torus in two places for all values of r+<r0<r, that is, for,

(ϖtR0)[1+Λ2]1/2rt

<r0<

(ϖtR0)[1+Λ2]1/2+rt.

Reality Check One

Let's see if these derived results make sense. As a first example, let's assign values of various Figure 2 parameters as follows:

Example 1A
ϖt rt Z0 α
34 14 1 π6

(Notice that the first pair of these parameter values aligns with the properties of the pink torus that was sketched in Figure 4 of Trova, Huré & Hersant (2012) — as reprinted immediately below — and that the chosen value of Z0 aligns with the z-coordinate of their "Point B.")

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

Figure 4 from Trova, Huré & Hersant (2012)

ϖt=34;rt=14

Point A: (ϖ,Z)=(34,0)

Point B: (ϖ,Z)=(1,1)

Point C: (ϖ,Z)=(10,10)


Taken together, this choice for the values of α and Z0 implies: (1) That the hypotenuse of the blue right-triangle in our Figure 2 and, hence, the distance between the centers of the two circles, is

h=Z0cosα=233;

and, (2) that the side of the triangle that is opposite the angle, α, is,

ϖtR0

=

hsinα=33,

which, taken together with the choice of ϖt, gives,

R0

=

3433=943120.17265.

With this set of parameters held fixed, it is clear that, in order for the ξ1 = constant circle to make first/final contact with the pink torus, it will need to have a radius,

r±=hrt=23314.

Let's see if this expectation matches the result obtained via the expressions derived above. Specifically, we find,

Λ

Z0ϖtR0=3;

hence,

r±

=

(ϖtR0)[1+Λ2]1/2rt

 

=

33[1+(3)2]1/214

 

=

23314.

This precisely matches our expectation.

Relate to Toroidal Coordinate System

Determine Overall Scale Length

In order to fully tie our "region of overlap" discussion back to MF53's system of toroidal coordinates, we must identify the specific location of the origin of that coordinate system in, for example, the Figure 2 diagram. As above, we will place the origin of the coordinate system an, as yet unspecified, distance, a, from the symmetry axis while, as illustrated in Figure 2, displacing it a distance, Z0, above the (cylindrical coordinate system's) equatorial plane. Referring back to the properties of toroidal coordinate systems, as discussed above, we know that in the Z=Z0 plane, the inner and outer edges of a ξ1 = constant torus/circle have radial locations,

ϖinnera=χinner

=

[(ξ11)(ξ1+1)]1/2,

ϖoutera=χouter

=

[(ξ1+1)(ξ11)]1/2.

Hence, the major radius of the ξ1 = constant toroidal surface is,

R0

=

12(ϖouter+ϖinner)

 

=

a2{[(ξ1+1)(ξ11)]1/2+[(ξ11)(ξ1+1)]1/2}

 

=

a2[(ξ1+1)+(ξ11)(ξ121)1/2]

 

=

aξ1(ξ121)1/2,

and its cross-sectional radius is,

r0

=

12(ϖouterϖinner)

 

=

a2{[(ξ1+1)(ξ11)]1/2[(ξ11)(ξ1+1)]1/2}

 

=

a2[(ξ1+1)(ξ11)(ξ121)1/2]

 

=

a(ξ121)1/2.

This also means that, if r0 and R0 are specified, the associated values of ξ1 and the scale length, a, are,

ξ1

=

R0r0,

and,

a

=

r0[(R0r0)21]1/2.


Revise Overlap Discussion

Let's reassess the conclusions drawn in our overlap discussion, above. Rather than varying r0 while holding R0 fixed, let's consider varying ξ1 while fixing the coordinate location of the origin of the toroidal coordinate system, (a,Z0). This is the approach that is appropriately aligned with integration over the (pink) toroidal mass distribution.

Re-expressed, the pair of boundaries of the "region of overlap," r±, give:

(r0±rt)2

=

(ϖtR0)2+Z02

[a(ξ121)1/2±rt]2

=

[ϖtaξ1(ξ121)1/2]2+Z02

[a±rt(ξ121)1/2]2

=

[ϖt(ξ121)1/2aξ1]2+Z02(ξ121)

a2±2art(ξ121)1/2+rt2(ξ121)

=

ϖt2(ξ121)2aϖtξ1(ξ121)1/2+a2ξ12+Z02(ξ121)

(ξ121)1/2[2aϖtξ1±2art]

=

[ϖt2+a2+Z02](ξ121)

(ξ121)1/2

=

2a(ϖtξ1±rt)(ϖt2+a2+Z02)

 

=

1[ξ1±rtϖt],

where,

12[a2+ϖt2+Z02aϖt].

After squaring both sides of this equation, we find that the values of ξ1 corresponding to the limits of overlap can be obtained from the roots of the following quadratic equation:

2(ξ121)

=

[ξ1±rtϖt]2

 

=

ξ12±ξ1(2rtϖt)+(rtϖt)2,

that is,

0

=

(12)ξ12±ξ1(2rtϖt)+[(rtϖt)2+2].


After setting up this expression, it dawned on me that the "plus or minus" generalization is not appropriate in this situation. While either result — say, the "plus" result — can be shifted from a r0R0 specification to a aξ1 specification, the pair of results generally will not share the same value of the scale length, a. Hence the pair of solutions will be unrelated when viewed from the perspective of the toroidal coordinate system. Instead, let's determine the value of a from the "first contact" solution — the superior sign in the expression — then figure out what the "final contact" solution will be if this scale length is held fixed. The solution to the quadratic equation is:

ξ1

=

12(12){(2rtϖt)±(2rtϖt)24(12)[(rtϖt)2+2]}

 

=

rtϖt(12){1±1(12)[1+(ϖtrt)2]}.

Given that the allowed range of values for the "radial" toroidal coordinate is, 1ξ1, the relevant root is,

ξ1|first

=

rtϖt(12){1(12)[1+(ϖtrt)2]1}.

Reality Check Two

Let's examine the behavior of these expressions, given the structural parameters provided in Example 1A, as defined above. Earlier, we deduced that "first contact" occurs when,

R0

=

3433=94312,

and,

r0=r+

=

23314=83312.

Hence, we should find that,

ξ1|first

=

R0r0=9438330.19084,

and,

a

=

r0[(R0r0)21]1/2.


Other

Now, the surface of an equatorial-plane torus having major radius, ϖt, and cross-sectional radius, rt, is described by the expression,

So, as the vertical coordinate varies over the range, rtz+rt, the horizontal coordinate varies over the range, (ϖtrt)ϖ(ϖt+rt). But, more importantly, for a given value of ϖ, the corresponding value of the vertical coordinate is,

z=±[rt2(ϖϖt)2]1/2.

Yet Again

Walk Through Step-By-Step

Keep the scale length of the toroidal coordinate system, a, fixed while varying the value of ξ1 and, hence, the radius,

r0=a(ξ121)1/2,

of the ξ1 = constant circle (hereafter, ξ1-circle). The (cylindrical) coordinate location of the center of this circle will be, (R0,Z0), where,

R0=aξ1(ξ121)1/2.

For the time being, we will assume that Z0>0, as illustrated in our Figure 2. Our initial aim is to determine the range of values of ξ1 for which the ξ1-circle touches or overlaps the equatorial-plane torus, whose position and size are as defined in our Figure 2.

Lowest Point on Circle

We will identify the (cylindrical) coordinates of the lowest point on the ξ1-circle as (R0,Zmin), where,

Zmin=Z0r0=Z0a(ξ121)1/2.

The ξ1-circle cannot possibly touch the equatorial-plane torus until ξ1 drops to a value such that Zmin is less than or equal to the radius of the torus, rt. This means that touching/overlap cannot occur unless,

ξ1ξmax[1+(aZ0rt)2]1/2.

A Critical Value of the Scale Length

Now, the two circles will come into contact at this limiting value, ξmax, only if the corresponding "radial" coordinate location of the center of the ξ1 circle exactly equals ϖt, that is, only if

aξmax(ξmax21)1/2

=

ϖt

a2ξmax2

=

ϖt2(ξmax21)

ξmax2

=

ϖt2(ϖt2a2)

1+(aZ0rt)2

=

ϖt2(ϖt2a2)

(ϖt2a2)(Z0rt)2+a2(ϖt2a2)

=

ϖt2(Z0rt)2

0

=

a2(Z0rt)2a2(ϖt2a2)

 

=

a2[(Z0rt)2ϖt2]+a4

a=acrit

[ϖt2(Z0rt)2]1/2.

Points of Intersection

In all meridional planes, the surface of the equatorial-plane torus is defined by the off-center circle expression,

(ϖϖt)2+z2

=

rt2

z2

=

rt2(ϖϖt)2.

Independently, we know that the surface of the off-center, ξ1-circle is defined by the expression,

(ϖR0)2+(zZ0)2

=

r02

[zZ0]2

=

a2(ξ121)[ϖaξ1(ξ121)1/2]2

z22zZ0+Z02

=

a2(ξ121)[ϖ22aϖξ1(ξ121)1/2+a2ξ12(ξ121)]

 

=

a2ϖ2+2aϖξ1(ξ121)1/2.

When the two circles intersect, the (cylindrical) coordinates of the point(s) at which the intersection occurs, (ϖ,z)=(ϖi,zi) must be shared by both circles. Eliminating z between these two off-center circle expressions allows us to solve for the "radial" coordinate, ϖi, of the intersection point(s). Specifically we find,

[rt2(ϖϖt)2]2[rt2(ϖϖt)2]1/2Z0+Z02

=

a2ϖ2+2aϖξ1(ξ121)1/2

2[rt2(ϖϖt)2]1/2Z0

=

Z02+a2+ϖ2+[rt2(ϖϖt)2]2aϖξ1(ξ121)1/2

 

=

Z02+a2+ϖ2+rt2(ϖ22ϖϖt+ϖt2)ϖ[2aξ1(ξ121)1/2]

 

=

K+2ϖ[ϖtaξ1(ξ121)1/2],

where,

KZ02+a2(ϖt2rt2).

Squaring both sides of this expression gives,

4Z02[rt2(ϖ22ϖϖt+ϖt2)]

=

K2+4ϖK[ϖtaξ1(ξ121)1/2]+4ϖ2[ϖtaξ1(ξ121)1/2]2

0

=

[K2+4Z02(ϖt2rt2)]+ϖ[4Kβ8Z02ϖt]+4ϖ2[Z02+β2],

where,

βϖtaξ1(ξ121)1/2.

The roots of this quadratic equation provide the sought-after coordinate(s), ϖi, of the point(s) of intersection. Specifically,

ϖi

=

18[Z02+β2]{[8Z02ϖt4Kβ]±[8Z02ϖt4Kβ]216[Z02+β2][K2+4Z02(ϖt2rt2)]}

 

=

[8Z02ϖt4Kβ]8[Z02+β2]{1±116[Z02+β2][K2+4Z02(ϖt2rt2)][8Z02ϖt4Kβ]2}

 

=

2Z02ϖtKβ2(Z02+β2){1±1},

where,

(Z02+β2)[K2+4Z02(ϖt2rt2)](2Z02ϖtKβ)2.

Now, from the definition of Toroidal Coordinates, as provided above, we know that the cylindrical coordinate, ϖ, is related to the pair of meridional-plane toroidal coordinates via the expression,

ϖa

=

(ξ121)1/2ξ1ξ2.

Therefore, once ϖi has been determined for a given choice of ξ1, the corresponding value of ξ2 at the intersection point is,

ξ2

=

ξ1(ξ121)1/2(ϖi/a).

Finally, given the pair of coordinate values, (ξ1,ξ2)i, the value of the (cylindrical) z-coordinate at the intersection point can be obtained via the relation,

Z0aza

=

(1ξ22)1/2ξ1ξ2

z

=

Z0a(1ξ22)1/2ξ1ξ2.

Limiting Values

All other parameters (a,Z0,ϖt,rt) being held fixed, as the coordinate, ξ1, is varied, there will be a maximum value, ξ1|max, at which the ξ1-circle will first make contact with the (pink) equatorial-plane torus, and there will be a minimum value, ξ1|min, at which it will have its final contact. At all values within the parameter range,

ξ1|max>ξ1>ξ1|min,

the ξ1-circle will intersect the surface of the torus in two locations, defined by two different values of the associated angular coordinate, ξ2 — see, for example, the coordinates listed in the table associated with example 2, below — but at the first and final points of contact, the two values of ξ2 will be degenerate. Let's derive the mathematical relations that give the values of ξ1|max and ξ1|min.

The expression derived above for the "radial" coordinate of the points of intersection, ϖi, gives two physically viable, real numbers as long as the composite parameter, 1>0. But only one real value is obtained when =1, and that occurs when,

(2Z02ϖtKβ)2

=

(Z02+β2)[K2+4Z02(ϖt2rt2)].

In this expression, β is the only parameter that depends on ξ1. So, temporarily using the shorthand notation,

Λ[K2+4Z02(ϖt2rt2)]

let's solve for the "critical" value(s), βcrit. We have,

4Z04ϖt24Z02ϖtKβ+K2β2

=

Z02Λ+Λβ2

(K2Λ)β2(4Z02ϖtK)β+(4Z04ϖt2Z02Λ)

=

0.

The roots of this quadratic equation give,

βcrit

=

2Z02ϖtK(K2Λ)[11(K2Λ)(4Z04ϖt2Z02Λ)4Z04ϖt2K2]

 

=

2Z02ϖtK4Z02(ϖt2rt2)[11+4Z02(ϖt2rt2)(4Z04ϖt2Z02Λ)4Z04ϖt2K2]

 

=

ϖtK2(ϖt2rt2)[11+(ϖt2rt2)(4Z02rt2K2)ϖt2K2].

Notice that a single critical value of — specifically, =1 — translates nicely into a pair of values of βcrit; these presumably relate directly to the pair of limiting coordinate values, ξ1|max and ξ1|min, that we are seeking. Via the definition of β, we find,

ξ1(ξ121)1/2

=

(ϖtβa)

ξ12

=

(ϖtβa)2(ξ121)

ξ12[(ϖtβa)21]

=

(ϖtβa)2

ξ1

=

[(ϖtβ)2(ϖtβ)2a2]1/2.

Upon evaluation of this expression in conjunction with the pair of βcrit values, the table, below, provides numerical values for the limiting values of ξ1|max and ξ1|min, along with the respective values of their accompanying (degenerate) coordinate, ξ2.

Examples

Diagram of Torus and Toroidal Coordinates

Diagram of Torus and Toroidal Coordinates

For reference purposes, Figure 2 has been displayed here, again, in the lefthand panel of Figure 4; the animation sequence presented in the righthand panel illustrates how the ξ1-circle (depicted by the locus of small black dots) intersects the surface of the (pink) equatorial-plane torus as the value of ξ1 is varied over the parameter range,

ξ1|maxξ1ξ1|min,

for a toroidal coordinate system whose origin (filled, red dot) remains fixed at the (cylindrical) coordinate location, (ϖ,z)=(a,Z0)=(13,34). For a toroidal coordinate system with this specified origin and an equatorial-plane torus having ϖt=34 and rt=14 — as recorded in the top row of numbers in the Table, below — the ξ1-circle makes first contact with the torus when ξ1=ξ1|max=1.1927843 and it makes final contact when ξ1=ξ1|min=1.0449467. The animation sequence contains ten unique frames: The value of ξ1 that is associated with the ξ1-circle in each case appears near the bottom-right corner of the animation frame. These parameter values have also been recorded in the first column of ten separate rows in the following table, along with other relevant parameter values. For example, in each frame of the animation, the points of intersection between the surface of the torus and the ξ1-circle are identified by filled, green diamonds; the (cylindrical) coordinates associated with these points of intersection, (ϖi,zi), are listed in each table row, along with the corresponding value of the toroidal coordinate system's angular, ξ2 coordinate.

Example 2
ϖt rt Z0 a K
34 14 34 13 (512)2
Torus Intersection Points
ξ1 β Intersection #1 (superior sign) Intersection #2 (inferior sign)
ξ2 ϖi zi ξ2 ϖi zi
1.1927843 +0.138485 1.000000 0.885198 0.704606 0.245844 Degenerate Coordinate Values
1.176 +0.116568 0.981258 0.922142 0.812595 0.242037 0.841611 0.616896 0.211621
1.160 +0.092267 0.962725 0.933386 0.864726 0.222121 0.824945 0.584858 0.187691
1.144 +0.063705 0.943871 0.940238 0.908969 0.192948 0.813713 0.560766 0.163372
1.127 +0.027202 0.924221 0.944608 0.949856 0.150191 0.806047 0.539788 0.135318
1.111 0.015045 0.907444 0.946487 0.980806 0.096065 0.802617 0.523232 0.105244
1.094 0.071947 0.894425 0.945995 0.999208 0.019887 0.803522 0.509118 0.066901
1.078 0.142539 0.892548 0.942353 0.989322 0.072283 0.810056 0.500846 0.020554
1.061 0.247448 0.916366 0.932024 0.916375 0.186599 0.827074 0.505248 0.050956
1.0449467 0.398902 1.000000 0.885198 0.632605 0.220722 Degenerate Coordinate Values

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 2 sketch, a vertical, light-blue line connects this center to the equatorial plane.



Material that appears after this point in our presentation is under development and therefore
may contain incorrect mathematical equations and/or physical misinterpretations.
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Confusing and Misleading Steps

But Not Every Circle Will Do

It is very important to appreciate that, although surfaces of constant X (or, equivalently, surfaces of constant ξ1) are always off-center circles, it is not the case that every off-center circle will prove to be a X=constant surface in the most relevant toroidal coordinate system. To be more specific, suppose we want to evaluate the potential at some location (R,0) inside or outside of a uniform-density torus whose meridional cross-section is a circle of radius rc and whose center is located on the x-axis at position x0. The equation describing the cross-sectional surface of this torus is,

(Rx0)2z2=rc2.

Dividing through by the square of a (as yet unspecified) scale length, a, gives,

[χ2x0a]2ζ2=rc2a2.

This dimensionless expression will only describe a X=constant surface in an MF53 toroidal coordinate system if, simultaneously,

X=x0aandX21=rc2a2.

That is, only if,

a=(x02rc2)1/2.

But in the above discussion we were only able to associate the dimensionless argument of the special function in CT99's CCGF expansion with the "radial" coordinate of the MF53 toroidal coordinate system by setting a=R, that is, only by setting the scale length equal to the cylindrical coordinate value R at which the potential is to be evaluated. So the surface of our torus will only align with a ξ1=constant surface in a toroidal coordinate system if,

R=(x02rc2)1/2.

This is a very tight constraint that usually will not be satisfied.


Multipole Moment in Toroidal Coordinates

While it might not be interesting or useful to impose this constraint in general, it will likely be instructive to evaluate the potential at the location where this constraint is satisfied. That is, we want to evaluate the potential inside a uniform density, circular-cross-section torus at the location,

Φ[(x02rc2)1/2,0]=2G(x02rc2)1/4q0.

Since in this case the argument of Q1/2 can be expressed in terms of the "radial" toroidal coordinate, it is reasonable to write the relevant moment of the mass distribution, q0, entirely in terms of toroidal coordinates. Specifically,

q0=a5/2[(ξ121)1/2ξ1ξ2]1/2ρ(ξ1,ξ2)Q1/2(ξ1)[dξ1(ξ1ξ2)(ξ121)1/2][dξ2(ξ1ξ2)(1ξ22)1/2].

Now suppose that the density distribution is only a function of the radial coordinate, that is, suppose that ρ=ρ(ξ1). Then the integral can be written as,

q0=a5/2ρ(ξ1)Q1/2(ξ1)[dξ1(ξ121)1/4][dξ2(ξ1ξ2)5/2(1ξ22)1/2].

Presumably the integral over dξ2 can be completed in closed form if the density distribution fills out the entire circular cross-section, that is, if the limits on integration are 1 to +1. Alternatively, write ξ2 in terms of sinθ and integrate from π2 to π2. Let's do this.

q0a5/2

=

0ξ1'ρ(ξ1)Q1/2(ξ1)[dξ1(ξ121)1/4]11[dξ2(ξ1ξ2)5/2(1ξ22)1/2]

 

=

0ξ1'ρ(ξ1)Q1/2(ξ1)[dξ1(ξ121)1/4]π/2π/2[dθ(ξ1sinθ)5/2].

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

WolframAlpha Integration

Hence — continuing to substitute a for ξ1' — the definite integral gives,

π/2π/2[dθ(asinθ)5/2]

=

{23(a21)2(asinθ)3/2[cosθ(5a2+4asinθ+1)

 

 

+(a+1)(a1)2(asinθa1)3/2F(π2θ4|2a1)

 

 

+4a(a1)(sinθa)(asinθa1)1/2E(π2θ4|2a1)]}π2π2

 

=

{23(a21)2(a1)3/2[(a+1)(a1)2(a1a1)3/2F(0|2a1)

 

 

+4a(a1)(1a)(a1a1)1/2E(0|2a1)]}

 

 

{23(a21)2(a+1)3/2[(a+1)(a1)2(a+1a1)3/2F(π2|2a1)

 

 

4a(a1)(1+a)(a+1a1)1/2E(π2|2a1)]}

 

=

{23(a1)2(a+1)2(a1)3/2[(a+1)(a1)2F(0|21a)+4a(a1)(1a)E(0|21a)]}

 

 

{23(a1)2(a+1)2(a+1)3/2[(a+1)(a1)2(a+1a1)3/2F(π2|21a)

 

 

4a(a1)(1+a)(a+1a1)1/2E(π2|21a)]}

 

=

23(a+1)(a1)3/2F(0|21a)8a3(a+1)2(a1)3/2E(0|21a)

 

 

23(a+1)(a1)3/2F(π2|21a)+8a3(a+1)2(a1)3/2E(π2|21a)

 

=

23(a+1)(a1)3/2{[F(0|21a)F(π2|21a)]4a(a+1)[E(0|21a)E(π2|21a)]}.

Now, according to (for example) NIST's Digital Library of Mathematical Functions,

F(0,k)=0   and   F(π2,k)=K(k),

where, K(k) is the complete elliptic integral of the first kind. Also, according to NIST's Digital Library of Mathematical Functions,

E(0,k)=0   and   E(π2,k)=E(k),

where, E(k) is the complete elliptic integral of the second kind. Hence we deduce that,

π/2π/2[dθ(ξ1sinθ)5/2]

=

23(ξ221)(ξ11)1/2[4ξ1(ξ1+1)E(21ξ1)K(21ξ1)],

which implies,

3q02a5/2

=

0ξ1'ρ(ξ1)Q1/2(ξ1)[dξ1(ξ121)5/4(ξ11)1/2][4ξ1(ξ1+1)E(21ξ1)K(21ξ1)].

Next, we might as well also insert the NIST relation,

Q1/2(cosθ)=K[cos(12θ)].


Older, Apparently Irrelevant Material

If we subtract "1" from both sides of this expression, the right-hand-side (RHS) takes on a familiar form:

χCT991

=

12RR[R2+R2+(zz)22RR]

 

=

12RR[(RR)2+(zz)2].

It appears as though the quantity, [2RR(χCT991)]1/2, is the radius rc of a circle whose center is located at either (R,z) or (R,z), that is, whose center is shifted off the origin of a cylindrical coordinate system. I'm not yet sure how/if we can benefit from recognizing this association.

Case A: Suppose we associate R with the center of a toroidal cross-section and, at the same time, associate R with the inner edge of a particular toroidal cross-section that is associated with the toroidal coordinate ξ1. We know that the scale-length a that is associated with the chosen toroidal coordinate system must be given by the ratio,

a=Rχ0.

[NOTE: As I'm doing this, I'm realizing that it may be wiser to associate a directly with the coordinate location R. But let's play this out first and see.]

Then it also will be true that,

a=Rχinner=R[ξ1+1ξ11]1/2.

Hence, we conclude that,

CaseA:RR=χinnerχ0=[ξ11ξ1+1]1/2(ξ121)1/2ξ1=(ξ11)ξ1

ξ1=[1RR]1.

What, then, is the expression for the scale-length a in terms of just R and R? Well ...

ξ1+1=11(R/R)+1=2R/R1(R/R),

and

ξ11=11(R/R)1=R/R1(R/R).

Hence,

a=R[2R/RR/R]1/2=(2RRR2)1/2.


Case B: On the other hand, if we associate R directly with a, then we conclude,

CaseB:RR=χinner=[ξ11ξ1+1]1/2.

(ξ1+1)(RR)2=ξ11.

ξ1[1(RR)2]=[1+(RR)2].

ξ1=[1+(RR)2][1(RR)2]1.


References

  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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