Toroidal coordinates

Illustration of toroidal coordinates, which are obtained by rotating a two-dimensional bipolar coordinate system about the axis separating its two foci. The foci are located at a distance 1 from the vertical z-axis. The red sphere is the σ = 30° isosurface, the blue torus is the τ = 0.5 isosurface, and the yellow half-plane is the φ = 60° isosurface. The green half-plane marks the x-z plane, from which φ is measured. The black point is located at the intersection of the red, blue and yellow isosurfaces, at Cartesian coordinates roughly (0.996, −1.725, 1.911).

Toroidal coordinates are a three-dimensional orthogonal coordinate system that results from rotating the two-dimensional bipolar coordinate system about the axis that separates its two foci. Thus, the two foci $F_{1}$ and $F_{2}$ in bipolar coordinates become a ring of radius $a$ in the $xy$ plane of the toroidal coordinate system; the $z$ -axis is the axis of rotation. The focal ring is also known as the reference circle.

Definition

The most common definition of toroidal coordinates $(\sigma ,\tau ,\phi )$ is

x=a\ {\frac {\sinh \tau }{\cosh \tau -\cos \sigma }}\cos \phi

y=a\ {\frac {\sinh \tau }{\cosh \tau -\cos \sigma }}\sin \phi

z=a\ {\frac {\sin \sigma }{\cosh \tau -\cos \sigma }}

where the $\sigma$ coordinate of a point $P$ equals the angle $F_{{1}}PF_{{2}}$ and the $\tau$ coordinate equals the natural logarithm of the ratio of the distances $d_{1}$ and $d_{{2}}$ to opposite sides of the focal ring

\tau =\ln {\frac {d_{{1}}}{d_{{2}}}}.

The coordinate ranges are $-\pi <\sigma \leq \pi$ and $\tau \geq 0$ and $0\leq \phi <2\pi .$

Coordinate surfaces

Rotating this two-dimensional bipolar coordinate system about the vertical axis produces the three-dimensional toroidal coordinate system above. A circle on the vertical axis becomes the red sphere, whereas a circle on the horizontal axis becomes the blue torus.

Surfaces of constant $\sigma$ correspond to spheres of different radii

\left(x^{{2}}+y^{{2}}\right)+\left(z-a\cot \sigma \right)^{{2}}={\frac {a^{{2}}}{\sin ^{{2}}\sigma }}

that all pass through the focal ring but are not concentric. The surfaces of constant $\tau$ are non-intersecting tori of different radii

z^{{2}}+\left({\sqrt {x^{{2}}+y^{{2}}}}-a\coth \tau \right)^{{2}}={\frac {a^{{2}}}{\sinh ^{{2}}\tau }}

that surround the focal ring. The centers of the constant- $\sigma$ spheres lie along the $z$ -axis, whereas the constant- $\tau$ tori are centered in the $xy$ plane.

Inverse transformation

The (σ, τ, φ) coordinates may be calculated from the Cartesian coordinates (x, y, z) as follows. The azimuthal angle φ is given by the formula

\tan \phi ={\frac {y}{x}}

The cylindrical radius ρ of the point P is given by

\rho ^{{2}}=x^{{2}}+y^{{2}}

and its distances to the foci in the plane defined by φ is given by

d_{{1}}^{{2}}=(\rho +a)^{{2}}+z^{{2}}

d_{{2}}^{{2}}=(\rho -a)^{{2}}+z^{{2}}

Geometric interpretation of the coordinates σ and τ of a point P. Observed in the plane of constant azimuthal angle φ, toroidal coordinates are equivalent to bipolar coordinates. The angle σ is formed by the two foci in this plane and P, whereas τ is the logarithm of the ratio of distances to the foci. The corresponding circles of constant σ and τ are shown in red and blue, respectively, and meet at right angles (magenta box); they are orthogonal.

The coordinate τ equals the natural logarithm of the focal distances

\tau =\ln {\frac {d_{{1}}}{d_{{2}}}}

whereas the coordinate σ equals the angle between the rays to the foci, which may be determined from the law of cosines

\cos \sigma =-{\frac {4a^{{2}}-d_{{1}}^{{2}}-d_{{2}}^{{2}}}{2d_{{1}}d_{{2}}}}

where the sign of σ is determined by whether the coordinate surface sphere is above or below the x-y plane.

Scale factors

The scale factors for the toroidal coordinates $\sigma$ and $\tau$ are equal

h_{\sigma }=h_{\tau }={\frac {a}{\cosh \tau -\cos \sigma }}

whereas the azimuthal scale factor equals

h_{\phi }={\frac {a\sinh \tau }{\cosh \tau -\cos \sigma }}

Thus, the infinitesimal volume element equals

dV={\frac {a^{3}\sinh \tau }{\left(\cosh \tau -\cos \sigma \right)^{3}}}\,d\sigma \,d\tau \,d\phi

and the Laplacian is given by

{\begin{aligned}\nabla ^{2}\Phi ={\frac {\left(\cosh \tau -\cos \sigma \right)^{{3}}}{a^{{2}}\sinh \tau }}&\left[\sinh \tau {\frac {\partial }{\partial \sigma }}\left({\frac {1}{\cosh \tau -\cos \sigma }}{\frac {\partial \Phi }{\partial \sigma }}\right)\right.\\[8pt]&{}\quad +\left.{\frac {\partial }{\partial \tau }}\left({\frac {\sinh \tau }{\cosh \tau -\cos \sigma }}{\frac {\partial \Phi }{\partial \tau }}\right)+{\frac {1}{\sinh \tau \left(\cosh \tau -\cos \sigma \right)}}{\frac {\partial ^{2}\Phi }{\partial \phi ^{2}}}\right]\end{aligned}}

Other differential operators such as $\nabla \cdot \mathbf{F}$ and $\nabla \times \mathbf{F}$ can be expressed in the coordinates $(\sigma ,\tau ,\phi )$ by substituting the scale factors into the general formulae found in orthogonal coordinates.

Toroidal harmonics

Standard separation

The 3-variable Laplace equation

\nabla ^{2}\Phi =0

admits solution via separation of variables in toroidal coordinates. Making the substitution

\Phi =U{\sqrt {\cosh \tau -\cos \sigma }}

A separable equation is then obtained. A particular solution obtained by separation of variables is:

\Phi ={\sqrt {\cosh \tau -\cos \sigma }}\,\,S_{\nu }(\sigma )T_{{\mu \nu }}(\tau )V_{\mu }(\phi )\,

where each function is a linear combination of:

S_{\nu }(\sigma )=e^{{i\nu \sigma }}\,\,\,\,{\mathrm {and}}\,\,\,\,e^{{-i\nu \sigma }}

T_{{\mu \nu }}(\tau )=P_{{\nu -1/2}}^{\mu }(\cosh \tau )\,\,\,\,{\mathrm {and}}\,\,\,\,Q_{{\nu -1/2}}^{\mu }(\cosh \tau )

V_{\mu }(\phi )=e^{{i\mu \phi }}\,\,\,\,{\mathrm {and}}\,\,\,\,e^{{-i\mu \phi }}

Where P and Q are associated Legendre functions of the first and second kind. These Legendre functions are often referred to as toroidal harmonics.

Toroidal harmonics have many interesting properties. If you make a variable substitution $\,\!1<z=\cosh \eta \,$ then, for instance, with vanishing order (the convention is to not write the order when it vanishes) and $\,\!n=0$

Q_{{-{\frac 12}}}(z)={\sqrt {{\frac {2}{1+z}}}}K\left({\sqrt {{\frac {2}{1+z}}}}\right)

and

P_{{-{\frac 12}}}(z)={\frac {2}{\pi }}{\sqrt {{\frac {2}{1+z}}}}K\left({\sqrt {{\frac {z-1}{z+1}}}}\right)

where $\,\!K$ and $\,\!E$ are the complete elliptic integrals of the first and second kind respectively. The rest of the toroidal harmonics can be obtained, for instance, in terms of the complete elliptic integrals, by using recurrence relations for associated Legendre functions.

The classic applications of toroidal coordinates are in solving partial differential equations, e.g., Laplace's equation for which toroidal coordinates allow a separation of variables or the Helmholtz equation, for which toroidal coordinates do not allow a separation of variables. Typical examples would be the electric potential and electric field of a conducting torus, or in the degenerate case, an electric current-ring (Hulme 1982).

An alternative separation

Alternatively, a different substitution may be made (Andrews 2006)

\Phi ={\frac {U}{{\sqrt {\rho }}}}

where

\rho ={\sqrt {x^{2}+y^{2}}}={\frac {a\sinh \tau }{\cosh \tau -\cos \sigma }}.

Again, a separable equation is obtained. A particular solution obtained by separation of variables is then:

\Phi ={\frac {a}{\rho }}\,\,S_{\nu }(\sigma )T_{{\mu \nu }}(\tau )V_{\mu }(\phi )\,

where each function is a linear combination of:

S_{\nu }(\sigma )=e^{{i\nu \sigma }}\,\,\,\,{\mathrm {and}}\,\,\,\,e^{{-i\nu \sigma }}

T_{{\mu \nu }}(\tau )=P_{{\mu -1/2}}^{\nu }(\coth \tau )\,\,\,\,{\mathrm {and}}\,\,\,\,Q_{{\mu -1/2}}^{\nu }(\coth \tau )

V_{\mu }(\phi )=e^{{i\mu \phi }}\,\,\,\,{\mathrm {and}}\,\,\,\,e^{{-i\mu \phi }}.

Note that although the toroidal harmonics are used again for the T function, the argument is $\coth \tau$ rather than $\cosh \tau$ and the $\mu$ and $\nu$ indices are exchanged. This method is useful for situations in which the boundary conditions are independent of the spherical angle $\theta$ , such as the charged ring, an infinite half plane, or two parallel planes. For identities relating the toroidal harmonics with argument hyperbolic cosine with those of argument hyperbolic cotangent, see the Whipple formulae.

References

Byerly, W E. (1893) An elementary treatise on Fourier's series and spherical, cylindrical, and ellipsoidal harmonics, with applications to problems in mathematical physics Ginn & co. pp. 264–266
Arfken G (1970). Mathematical Methods for Physicists (2nd ed.). Orlando, FL: Academic Press. pp. 112–115.
Andrews, Mark (2006). "Alternative separation of Laplace's equation in toroidal coordinates and its application to electrostatics". Journal of Electrostatics. 64 (10): 664–672. doi:10.1016/j.elstat.2005.11.005.
Hulme, A. (1982). "A note on the magnetic scalar potential of an electric current-ring". Mathematical Proceedings of the Cambridge Philosophical Society. 92 (01): 183–191. doi:10.1017/S0305004100059831.

Bibliography

Morse P M, Feshbach H (1953). Methods of Theoretical Physics, Part I. New York: McGraw–Hill. p. 666.
Korn G A, Korn T M (1961). Mathematical Handbook for Scientists and Engineers. New York: McGraw-Hill. p. 182. LCCN 59014456.
Margenau H, Murphy G M (1956). The Mathematics of Physics and Chemistry. New York: D. van Nostrand. pp. 190–192. LCCN 55010911.
Moon P H, Spencer D E (1988). "Toroidal Coordinates (η, θ, ψ)". Field Theory Handbook, Including Coordinate Systems, Differential Equations, and Their Solutions (2nd ed., 3rd revised printing ed.). New York: Springer Verlag. pp. 112–115 (Section IV, E4Ry). ISBN 0-387-02732-7.

External links

MathWorld description of toroidal coordinates

Orthogonal coordinate systems

Two dimensional	Cartesian coordinate system Polar coordinate system Parabolic coordinate system Bipolar coordinates Elliptic coordinates

Three dimensional	Cartesian coordinate system Cylindrical coordinate system Spherical coordinate system Parabolic cylindrical coordinates Paraboloidal coordinates Oblate spheroidal coordinates Prolate spheroidal coordinates Ellipsoidal coordinates Elliptic cylindrical coordinates Toroidal coordinates Bispherical coordinates Bipolar cylindrical coordinates Conical coordinates 6-sphere coordinates Flat-ring cyclide coordinates Flat-disk cyclide coordinates Bi-cyclide coordinates Cap-cyclide coordinates Concave bi-sinusoidal single-centered coordinates Concave bi-sinusoidal double-centered coordinates Convex inverted-sinusoidal spherically aligned coordinates Quasi-random-intersection cartesian coordinates

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