Parabolic cylindrical coordinates

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Coordinate surfaces of parabolic cylindrical coordinates. The red parabolic cylinder corresponds to σ=2, whereas the yellow parabolic cylinder corresponds to τ=1. The blue plane corresponds to z=2. These surfaces intersect at the point P (shown as a black sphere), which has Cartesian coordinates roughly (2, -1.5, 2).

In mathematics, parabolic cylindrical coordinates are a three-dimensional orthogonal coordinate system that results from projecting the two-dimensional parabolic coordinate system in the perpendicular z-direction. Hence, the coordinate surfaces are confocal parabolic cylinders. Parabolic cylindrical coordinates have found many applications, e.g., the potential theory of edges.

Basic definition

Parabolic coordinate system showing curves of constant σ and τ the horizontal and vertical axes are the x and y coordinates respectively. These coordinates are projected along the z-axis, and so this diagram will hold for any value of the z coordinate.

The parabolic cylindrical coordinates Template:Math are defined in terms of the Cartesian coordinates Template:Math by:

x=στy=12(τ2σ2)z=z

The surfaces of constant Template:Math form confocal parabolic cylinders

2y=x2σ2σ2

that open towards Template:Math, whereas the surfaces of constant Template:Math form confocal parabolic cylinders

2y=x2τ2+τ2

that open in the opposite direction, i.e., towards Template:Math. The foci of all these parabolic cylinders are located along the line defined by Template:Math. The radius Template:Math has a simple formula as well

r=x2+y2=12(σ2+τ2)

that proves useful in solving the Hamilton–Jacobi equation in parabolic coordinates for the inverse-square central force problem of mechanics; for further details, see the Laplace–Runge–Lenz vector article.

Scale factors

The scale factors for the parabolic cylindrical coordinates Template:Math and Template:Math are:

hσ=hτ=σ2+τ2hz=1

Differential elements

The infinitesimal element of volume is

dV=hσhτhzdσdτdz=(σ2+τ2)dσdτdz

The differential displacement is given by:

d𝐥=σ2+τ2dσσ^+σ2+τ2dττ^+dz𝐳^

The differential normal area is given by:

d𝐒=σ2+τ2dτdzσ^+σ2+τ2dσdzτ^+(σ2+τ2)dσdτ𝐳^

Del

Let Template:Math be a scalar field. The gradient is given by

f=1σ2+τ2fσσ^+1σ2+τ2fττ^+fz𝐳^

The Laplacian is given by

2f=1σ2+τ2(2fσ2+2fτ2)+2fz2

Let Template:Math be a vector field of the form:

𝐀=Aσσ^+Aττ^+Az𝐳^

The divergence is given by

𝐀=1σ2+τ2((σ2+τ2Aσ)σ+(σ2+τ2Aτ)τ)+Azz

The curl is given by

×𝐀=(1σ2+τ2AzτAτz)σ^(1σ2+τ2AzσAσz)τ^+1σ2+τ2((σ2+τ2Aτ)σ(σ2+τ2Aσ)τ)𝐳^

Other differential operators can be expressed in the coordinates Template:Math by substituting the scale factors into the general formulae found in orthogonal coordinates.

Relationship to other coordinate systems

Relationship to cylindrical coordinates Template:Math:

ρcosφ=στρsinφ=12(τ2σ2)z=z

Parabolic unit vectors expressed in terms of Cartesian unit vectors:

σ^=τ𝐱^σ𝐲^τ2+σ2τ^=σ𝐱^+τ𝐲^τ2+σ2𝐳^=𝐳^

Parabolic cylinder harmonics

Since all of the surfaces of constant Template:Math, Template:Math and Template:Math are conicoids, Laplace's equation is separable in parabolic cylindrical coordinates. Using the technique of the separation of variables, a separated solution to Laplace's equation may be written:

V=S(σ)T(τ)Z(z)

and Laplace's equation, divided by Template:Math, is written:

1σ2+τ2[S¨S+T¨T]+Z¨Z=0

Since the Template:Math equation is separate from the rest, we may write

Z¨Z=m2

where Template:Math is constant. Template:Math has the solution:

Zm(z)=A1eimz+A2eimz

Substituting Template:Math for Z¨/Z, Laplace's equation may now be written:

[S¨S+T¨T]=m2(σ2+τ2)

We may now separate the Template:Math and Template:Math functions and introduce another constant Template:Math to obtain:

S¨(m2σ2+n2)S=0
T¨(m2τ2n2)T=0

The solutions to these equations are the parabolic cylinder functions

Smn(σ)=A3y1(n2/2m,σ2m)+A4y2(n2/2m,σ2m)
Tmn(τ)=A5y1(n2/2m,iτ2m)+A6y2(n2/2m,iτ2m)

The parabolic cylinder harmonics for Template:Math are now the product of the solutions. The combination will reduce the number of constants and the general solution to Laplace's equation may be written:

V(σ,τ,z)=m,nAmnSmnTmnZm

Applications

The classic applications of parabolic cylindrical coordinates are in solving partial differential equations, e.g., Laplace's equation or the Helmholtz equation, for which such coordinates allow a separation of variables. A typical example would be the electric field surrounding a flat semi-infinite conducting plate.

See also

Bibliography

Template:Orthogonal coordinate systems