Toroidal coordinates

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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 F1 and F2 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.


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[edit] Basic definition

The most common definition of toroidal coordinates (σ,τ,φ) 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 σ coordinate of a point P equals the angle F1PF2 and the τ coordinate equals the natural logarithm of the ratio of the distances d1 and d2 to opposite sides of the focal ring

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


Surfaces of constant σ 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 τ 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-σ spheres lie along the z-axis, whereas the constant-τ tori are centered in the xy plane.


[edit] Scale factors

The scale factors for the toroidal coordinates σ and τ 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

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

and the Laplacian is given by

\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) +  \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]

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


[edit] Applications

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 does not allow a separation of variables. A typical example would be the electric field surrounding a conducting ring.

[edit] References

  • Korn GA and Korn TM. (1961) Mathematical Handbook for Scientists and Engineers, McGraw-Hill.