Prolate spheroidal coordinates

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The three coordinate surfaces of prolate spheroidal coordinates. The red prolate spheroid (stretched sphere) corresponds to μ=1, and the blue two-sheet hyperboloid corresponds to ν=45°. The yellow half-plane corresponds to φ=-60°, which is measured relative to the x-axis (highlighted in green). The black sphere represents the intersection point of the three surfaces, which has Cartesian coordinates of roughly (0.831, -1.439, 2.182).
The three coordinate surfaces of prolate spheroidal coordinates. The red prolate spheroid (stretched sphere) corresponds to μ=1, and the blue two-sheet hyperboloid corresponds to ν=45°. The yellow half-plane corresponds to φ=-60°, which is measured relative to the x-axis (highlighted in green). The black sphere represents the intersection point of the three surfaces, which has Cartesian coordinates of roughly (0.831, -1.439, 2.182).

Prolate spheroidal coordinates are a three-dimensional orthogonal coordinate system that results from rotating the two-dimensional elliptic coordinate system about the focal axis of the ellipse, i.e., the axis on which the foci are located. Rotation about the other axis produces the oblate spheroidal coordinates.

This coordinate system can be used to solve various partial differential equations in which the boundary conditions match its symmetry and shape, such as solving for a field produced by two centers, which are taken as the foci on the z-axis. One example is solving for the wavefunction of an electron moving in the electromagnetic field of two positively charged nuclei, as in the hydrogen ion, H2+. Another example is solving for the electric field generated by two small electrode tips. Other limiting cases include fields generated by a line segment (μ=0) or a line with a missing segment (ν=0).

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[edit] Definition

Prolate spheroidal coordinates μ and ν for a=1. The lines of equal values of μ and ν are shown on the x-z plane, i.e. for φ=0. The surfaces of constant μ and ν are obtained by rotation about the z axis, so that the diagram is valid for any plane containing the z axis: i.e. for any φ.
Prolate spheroidal coordinates μ and ν for a=1. The lines of equal values of μ and ν are shown on the x-z plane, i.e. for φ=0. The surfaces of constant μ and ν are obtained by rotation about the z axis, so that the diagram is valid for any plane containing the z axis: i.e. for any φ.

The most common definition of prolate spheroidal coordinates (μ,ν,φ) is

x = a \ \sinh \mu \ \sin \nu \ \cos \phi
y = a \ \sinh \mu \ \sin \nu \ \sin \phi
z = a \ \cosh \mu \ \cos \nu

where μ is a nonnegative real number and \nu \in [0, \pi]. The azimuthal angle φ belongs to the interval [0,2π).

The trigonometric identity

\frac{z^{2}}{a^{2} \cosh^{2} \mu} + \frac{x^{2} + y^{2}}{a^{2} \sinh^{2} \mu} = \cos^{2} \nu + \sin^{2} \nu = 1

shows that surfaces of constant μ form prolate spheroids, since they are ellipses rotated about the axis joining their foci. Similarly, the hyperbolic trigonometric identity

\frac{z^{2}}{a^{2} \cos^{2} \nu} - \frac{x^{2} + y^{2}}{a^{2} \sin^{2} \nu} = \cosh^{2} \mu - \sinh^{2} \mu = 1

shows that surfaces of constant ν form hyperboloids of revolution.

[edit] Scale factors

The scale factors for the elliptic coordinates (μ,ν) are equal

h_{\mu} = h_{\nu} = a\sqrt{\sinh^{2}\mu + \sin^{2}\nu}

whereas the azimuthal scale factor equals

h_{\phi} = a \sinh\mu \ \sin\nu

Consequently, an infinitesimal volume element equals

dV = a^{3} \sinh\mu \ \sin\nu \ \left( \sinh^{2}\mu + \sin^{2}\nu \right) d\mu d\nu d\phi

and the Laplacian can be written

\nabla^{2} \Phi = \frac{1}{a^{2} \left( \sinh^{2}\mu + \sin^{2}\nu \right)} \left[ \frac{\partial^{2} \Phi}{\partial \mu^{2}} + \frac{\partial^{2} \Phi}{\partial \nu^{2}} + \coth \mu \frac{\partial \Phi}{\partial \mu} + \cot \nu \frac{\partial \Phi}{\partial \nu} \right] + \frac{1}{a^{2} \sinh^{2}\mu \sin^{2}\nu} \frac{\partial^{2} \Phi}{\partial \phi^{2}}

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

[edit] Alternative definition

In principle, a definition of prolate spheroidal coordinates could be degenerate. In other words, a single set of coordinates might correspond to two points in Cartesian coordinates; this is illustrated here with two black spheres, one on each sheet of the hyperboloid and located at (x, y, ±z). However, neither of the definitions presented here are degenerate.
In principle, a definition of prolate spheroidal coordinates could be degenerate. In other words, a single set of coordinates might correspond to two points in Cartesian coordinates; this is illustrated here with two black spheres, one on each sheet of the hyperboloid and located at (x, y, ±z). However, neither of the definitions presented here are degenerate.

An alternative and geometrically intuitive set of prolate spheroidal coordinates (σ,τ,φ) are sometimes used, where σ = coshμ and τ = cosν. Hence, the curves of constant σ are prolate spheroids, whereas the curves of constant τ are hyperboloids of revolution. The coordinate τ belongs to the interval [-1, 1], whereas the σ coordinate must be greater than or equal to one.

The coordinates σ and τ have a simple relation to the distances to the foci F1 and F2. For any point in the plane, the sum d1 + d2 of its distances to the foci equals 2aσ, whereas their difference d1 − d2 equals 2aτ. Thus, the distance to F1 is a(σ + τ), whereas the distance to F2 is a(σ − τ). (Recall that F1 and F2 are located at z = − a and z = + a, respectively.)

Unlike the analogous oblate spheroidal coordinates, the prolate spheroid coordinates (σ, τ, φ) are not degenerate; in other words, there is a unique, reversible correspondence (in technical language, a 1-to-1 mapping) between them and the Cartesian coordinates

x = a \sqrt{\left( \sigma^{2} - 1 \right) \left(1 - \tau^{2} \right)} \cos \phi
y = a \sqrt{\left( \sigma^{2} - 1 \right) \left(1 - \tau^{2} \right)} \sin \phi
z = a\ \sigma\ \tau

[edit] Alternative scale factors

The scale factors for the alternative elliptic coordinates (σ,τ,φ) are

h_{\sigma} = a\sqrt{\frac{\sigma^{2} - \tau^{2}}{\sigma^{2} - 1}}
h_{\tau} = a\sqrt{\frac{\sigma^{2} - \tau^{2}}{1 - \tau^{2}}}

while the azimuthal scale factor is now

h_{\phi} = a \sqrt{\left( \sigma^{2} - 1 \right) \left( 1 - \tau^{2} \right)}

Hence, the infinitesimal volume element becomes

dV = a^{3} \left( \sigma^{2} - \tau^{2} \right) d\sigma d\tau d\phi

and the Laplacian equals

\nabla^{2} \Phi = \frac{1}{a^{2} \left( \sigma^{2} - \tau^{2} \right)} \left\{ \frac{\partial}{\partial \sigma} \left[ \left( \sigma^{2} - 1 \right) \frac{\partial \Phi}{\partial \sigma} \right] + \frac{\partial}{\partial \tau} \left[ \left( 1 - \tau^{2} \right) \frac{\partial \Phi}{\partial \tau} \right] \right\} + \frac{1}{a^{2} \left( \sigma^{2} - 1 \right) \left( 1 - \tau^{2} \right)} \frac{\partial^{2} \Phi}{\partial \phi^{2}}

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

As is the case with spherical coordinates, Laplaces equation may be solved by the method of separation of variables to yield solutions in the form of prolate spheroidal harmonics, which are convenient to use when boundary conditions are defined on a surface with a constant prolate spheroidal coordinate (See Smythe, 1968).

[edit] See also

  • Three dimensional orthogonal coordinate systems


[edit] References

[edit] Bibliography

[edit] No angles convention

  • Morse PM, Feshbach H (1953). Methods of Theoretical Physics, Part I. New York: McGraw-Hill, p. 661.  Uses ξ1 = a cosh μ, ξ2 = sin ν, and ξ3 = cos φ.
  • Zwillinger D (1992). Handbook of Integration. Boston, MA: Jones and Bartlett, p. 114. ISBN 0-86720-293-9.  Same as Morse & Feshbach (1953), substituting uk for ξk.
  • Smythe, WR (1968). Static and Dynamic Electricity, 3rd ed., New York: McGraw-Hill. 
  • Sauer R, Szabó I (1967). Mathematische Hilfsmittel des Ingenieurs. New York: Springer Verlag, p. 97. LCCN 67-25285.  Uses coordinates ξ = cosh μ, η = sin ν, and φ.

[edit] Angle convention

  • Korn GA, Korn TM (1961). Mathematical Handbook for Scientists and Engineers. New York: McGraw-Hill, p. 177. LCCN 59-14456.  Korn and Korn use the (μ, ν, φ) coordinates, but also introduce the degenerate (σ, τ, φ) coordinates.
  • Margenau H, Murphy GM (1956). The Mathematics of Physics and Chemistry. New York: D. van Nostrand, pp. 180–182. LCCN 55-10911.  Similar to Korn and Korn (1961), but uses colatitude θ = 90° - ν instead of latitude ν.
  • Moon PH, Spencer DE (1988). "Prolate Spheroidal Coordinates (η, θ, ψ)", Field Theory Handbook, Including Coordinate Systems, Differential Equations, and Their Solutions, corrected 2nd ed., 3rd print ed., New York: Springer Verlag, pp. 28–30 (Table 1.06). ISBN 0-387-02732-7.  Moon and Spencer use the colatitude convention θ = 90° - ν, and re-name φ as ψ.

[edit] Unusual convention

  • Landau LD, Lifshitz EM, Pitaevskii LP (1984). Electrodynamics of Continuous Media (Volume 8 of the Course of Theoretical Physics), 2nd edition, New York: Pergamon Press, pp. 19–29. ISBN 978-0750626347.  Treats the prolate spheroidal coordinates as a limiting case of the general ellipsoidal coordinates. Uses (ξ, η, ζ) coordinates that have the units of distance squared.

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