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Ellipsoidal coordinates

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Ellipsoidal coordinates are a three-dimensional orthogonal coordinate system (λ,μ,ν) that generalizes the two-dimensional elliptic coordinate system. Unlike most three-dimensional orthogonal coordinates that feature quadratic coordinate surfaces, the ellipsoidal coordinate system is based on confocal quadrics.

Basic formulae

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The Cartesian coordinates (x,y,z) can be produced from the ellipsoidal coordinates (λ,μ,ν) by the equations

x2=(a2+λ)(a2+μ)(a2+ν)(a2−b2)(a2−c2)
y2=(b2+λ)(b2+μ)(b2+ν)(b2−a2)(b2−c2)
z2=(c2+λ)(c2+μ)(c2+ν)(c2−b2)(c2−a2)

where the following limits apply to the coordinates

−λ<c2<−μ<b2<−ν<a2.

Consequently, surfaces of constant λ are ellipsoids

x2a2+λ+y2b2+λ+z2c2+λ=1,

whereas surfaces of constant μ are hyperboloids of one sheet

x2a2+μ+y2b2+μ+z2c2+μ=1,

because the last term in the lhs is negative, and surfaces of constant ν are hyperboloids of two sheets

x2a2+ν+y2b2+ν+z2c2+ν=1

because the last two terms in the lhs are negative.

The orthogonal system of quadrics used for the ellipsoidal coordinates are confocal quadrics.

Scale factors and differential operators

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For brevity in the equations below, we introduce a function

S(σ) =def (a2+σ)(b2+σ)(c2+σ)

where σ can represent any of the three variables (λ,μ,ν). Using this function, the scale factors can be written

hλ=12(λ−μ)(λ−ν)S(λ)
hμ=12(μ−λ)(μ−ν)S(μ)
hν=12(ν−λ)(ν−μ)S(ν)

Hence, the infinitesimal volume element equals

dV=(λ−μ)(λ−ν)(μ−ν)8−S(λ)S(μ)S(ν)dλdμdν

and the Laplacian is defined by

∇2Φ=4S(λ)(λ−μ)(λ−ν)∂∂λ[S(λ)∂Φ∂λ]+4S(μ)(μ−λ)(μ−ν)∂∂μ[S(μ)∂Φ∂μ]+4S(ν)(ν−λ)(ν−μ)∂∂ν[S(ν)∂Φ∂ν]

Other differential operators such as ∇⋅𝐅 and ∇×𝐅 can be expressed in the coordinates (λ,μ,ν) by substituting the scale factors into the general formulae found in orthogonal coordinates.

Angular parametrization

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An alternative (but non-orthogonal) parametrization exists that closely follows the angular parametrization of spherical coordinates:[1]

x=assin⁡θcos⁡ϕ,
y=bssin⁡θsin⁡ϕ,
z=cscos⁡θ.

Here, s>0 parametrizes the concentric ellipsoids around the origin and θ∈[0,π] and ϕ∈[0,2π] are the usual polar and azimuthal angles of spherical coordinates, respectively. The corresponding volume element is

dxdydz=abcs2sin⁡θdsdθdϕ.

See also

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References

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  1. ↑ "Ellipsoid Quadrupole Moment". 9 October 2013.

Bibliography

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Unusual convention

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  • Landau LD, Lifshitz EM, Pitaevskii LP (1984). Electrodynamics of Continuous Media (Volume 8 of the Course of Theoretical Physics) (2nd ed.). New York: Pergamon Press. pp. 19–29. ISBN 978-0-7506-2634-7. Uses (ξ, η, ζ) coordinates that have the units of distance squared.
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