Elliptic coordinate system: Difference between revisions

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[[File:Elliptic cylindrical coordinates.png|thumb|right|350px|[[Coordinate system#Coordinate surface|Coordinate surfaces]] of elliptic cylindrical coordinates.  The yellow sheet is the prism of a half-hyperbola corresponding to ν=-45°, whereas the red tube is an elliptical prism corresponding to μ=1.  The blue sheet corresponds to ''z''=1.  The three surfaces intersect at the point '''P''' (shown as a black sphere) with [[Cartesian coordinate system|Cartesian coordinates]] roughly (2.182, -1.661, 1.0).  The foci of the ellipse and hyperbola lie at ''x'' = ±2.0.]]
 
'''Elliptic cylindrical coordinates''' are a three-dimensional [[orthogonal coordinates|orthogonal]] [[coordinate system]] that results from projecting the two-dimensional [[elliptic coordinates|elliptic coordinate system]] in the
perpendicular <math>z</math>-direction.  Hence, the [[Coordinate system#Coordinate surface|coordinate surfaces]] are [[prism (geometry)|prisms]] of confocal [[ellipse]]s and [[hyperbola]]e. The two [[Focus (geometry)|foci]]
<math>F_{1}</math> and <math>F_{2}</math> are generally taken to be fixed at <math>-a</math> and
<math>+a</math>, respectively, on the <math>x</math>-axis of the [[Cartesian coordinate system]].
 
==Basic definition==
 
The most common definition of elliptic cylindrical coordinates <math>(\mu, \nu, z)</math> is
 
:<math>
x = a \ \cosh \mu \ \cos \nu
</math>
 
:<math>
y = a \ \sinh \mu \ \sin \nu
</math>
 
:<math>
z = z
\!</math>
 
where <math>\mu</math> is a nonnegative real number and <math>\nu \in [0, 2\pi)</math>.
 
These definitions correspond to ellipses and hyperbolae.  The trigonometric identity
 
:<math>
\frac{x^{2}}{a^{2} \cosh^{2} \mu} + \frac{y^{2}}{a^{2} \sinh^{2} \mu} = \cos^{2} \nu + \sin^{2} \nu = 1
</math>
 
shows that curves of constant <math>\mu</math> form [[ellipse]]s, whereas the hyperbolic trigonometric identity
 
:<math>
\frac{x^{2}}{a^{2} \cos^{2} \nu} - \frac{y^{2}}{a^{2} \sin^{2} \nu} = \cosh^{2} \mu - \sinh^{2} \mu = 1
</math>
 
shows that curves of constant <math>\nu</math> form [[hyperbola]]e.
 
==Scale factors==
 
The scale factors for the elliptic cylindrical coordinates <math>\mu</math> and <math>\nu</math> are equal
 
:<math>
h_{\mu} = h_{\nu} = a\sqrt{\sinh^{2}\mu + \sin^{2}\nu}
</math>
 
whereas the remaining scale factor <math>h_{z}=1</math>.
Consequently, an infinitesimal volume element equals
 
:<math>
dV = a^{2} \left( \sinh^{2}\mu + \sin^{2}\nu \right) d\mu d\nu dz
</math>
 
and the Laplacian equals
 
:<math>
\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}} \right) + \frac{\partial^{2} \Phi}{\partial z^{2}}
</math>
 
Other differential operators such as <math>\nabla \cdot \mathbf{F}</math> and <math>\nabla \times \mathbf{F}</math> can be expressed in the coordinates <math>(\mu, \nu, z)</math> by substituting
the scale factors into the general formulae found in [[orthogonal coordinates]].
 
==Alternative definition==
 
An alternative and geometrically intuitive set of elliptic coordinates <math>(\sigma, \tau, z)</math> are sometimes used, where <math>\sigma = \cosh \mu</math> and <math>\tau = \cos \nu</math>.  Hence, the curves of constant <math>\sigma</math> are ellipses, whereas the curves of constant <math>\tau</math> are hyperbolae.  The coordinate <math>\tau</math> must belong to the interval [-1, 1], whereas the <math>\sigma</math>
coordinate must be greater than or equal to one.
The coordinates <math>(\sigma, \tau, z)</math> have a simple relation to the distances to the foci <math>F_{1}</math> and <math>F_{2}</math>.  For any point in the (x,y) plane, the ''sum'' <math>d_{1}+d_{2}</math> of its distances to the foci equals <math>2a\sigma</math>, whereas their ''difference'' <math>d_{1}-d_{2}</math> equals <math>2a\tau</math>.
Thus, the distance to <math>F_{1}</math> is <math>a(\sigma+\tau)</math>, whereas the distance to <math>F_{2}</math> is <math>a(\sigma-\tau)</math>.  (Recall that <math>F_{1}</math> and <math>F_{2}</math> are located at <math>x=-a</math> and <math>x=+a</math>, respectively.)
 
A drawback of these coordinates is that they do not have a 1-to-1 transformation to the [[Cartesian coordinates]]
:<math>
x = a\sigma\tau \!
</math>
 
:<math>
y^{2} = a^{2} \left( \sigma^{2} - 1 \right) \left(1 - \tau^{2} \right)
</math>
 
==Alternative scale factors==
 
The scale factors for the alternative elliptic coordinates <math>(\sigma, \tau, z)</math> are
 
:<math>
h_{\sigma} = a\sqrt{\frac{\sigma^{2} - \tau^{2}}{\sigma^{2} - 1}}
</math>
 
:<math>
h_{\tau} = a\sqrt{\frac{\sigma^{2} - \tau^{2}}{1 - \tau^{2}}}
</math>
 
and, of course, <math>h_{z}=1</math>.  Hence, the infinitesimal volume element becomes
 
:<math>
dV = a^{2} \frac{\sigma^{2} - \tau^{2}}{\sqrt{\left( \sigma^{2} - 1 \right) \left( 1 - \tau^{2} \right)}} d\sigma d\tau dz
</math>
 
and the Laplacian equals
 
:<math>
\nabla^{2} \Phi =
\frac{1}{a^{2} \left( \sigma^{2} - \tau^{2} \right) }
\left[
\sqrt{\sigma^{2} - 1} \frac{\partial}{\partial \sigma}
\left( \sqrt{\sigma^{2} - 1} \frac{\partial \Phi}{\partial \sigma} \right) +
\sqrt{1 - \tau^{2}} \frac{\partial}{\partial \tau}
\left( \sqrt{1 - \tau^{2}} \frac{\partial \Phi}{\partial \tau} \right)
\right] +
\frac{\partial^{2} \Phi}{\partial z^{2}}
</math>
 
Other differential operators such as <math>\nabla \cdot \mathbf{F}</math>
and <math>\nabla \times \mathbf{F}</math> can be expressed in the coordinates <math>(\sigma, \tau)</math> by substituting
the scale factors into the general formulae
found in [[orthogonal coordinates]].
 
==Applications==
The classic applications of elliptic cylindrical coordinates are in solving [[partial differential equations]],
e.g., [[Laplace's equation]] or the [[Helmholtz equation]], for which elliptic cylindrical coordinates allow a
[[separation of variables]].  A typical example would be the [[electric field]] surrounding a
flat conducting plate of width <math>2a</math>.
 
The three-dimensional [[wave equation]], when expressed in elliptic cylindrical coordinates, may be solved by separation of variables, leading to the [[Mathieu differential equation]]s.
 
The geometric properties of elliptic coordinates can also be useful. A typical example might involve
an integration over all pairs of vectors <math>\mathbf{p}</math> and <math>\mathbf{q}</math>
that sum to a fixed vector <math>\mathbf{r} = \mathbf{p} + \mathbf{q}</math>, where the integrand
was a function of the vector lengths <math>\left| \mathbf{p} \right|</math> and <math>\left| \mathbf{q} \right|</math>. (In such a case, one would position <math>\mathbf{r}</math> between the two foci and aligned with the <math>x</math>-axis, i.e., <math>\mathbf{r} = 2a \mathbf{\hat{x}}</math>.)  For concreteness,  <math>\mathbf{r}</math>, <math>\mathbf{p}</math> and <math>\mathbf{q}</math> could represent the [[momentum|momenta]] of a particle and its decomposition products, respectively, and the integrand might involve the kinetic energies of the products (which are proportional to the squared lengths of the momenta).
 
==Bibliography==
*{{cite book | author = [[Philip M. Morse|Morse PM]], [[Herman Feshbach|Feshbach H]] | year = 1953 | title = Methods of Theoretical Physics, Part I | publisher = McGraw-Hill | location = New York | isbn = 0-07-043316-X | page = 657 | lccn = 5211515}}
*{{cite book | author = [[Henry Margenau|Margenau H]], Murphy GM | year = 1956 | title = The Mathematics of Physics and Chemistry | publisher = D. van Nostrand | location = New York | pages = 182&ndash;183 | lccn = 5510911 }}
*{{cite book | author = Korn GA, Korn TM |year = 1961 | title = Mathematical Handbook for Scientists and Engineers | publisher = McGraw-Hill | location = New York | id = ASIN B0000CKZX7 | page = 179 | lccn = 5914456}}
*{{cite book | author = Sauer R, Szabó I | year = 1967 | title = Mathematische Hilfsmittel des Ingenieurs | publisher = Springer Verlag | location = New York | page = 97 | lccn = 6725285}} 
*{{cite book | author = Zwillinger D | year = 1992 | title = Handbook of Integration | publisher = Jones and Bartlett | location = Boston, MA | isbn = 0-86720-293-9 | page = 114}}  Same as Morse & Feshbach (1953), substituting ''u''<sub>''k''</sub> for ξ<sub>''k''</sub>.
*{{cite book | author = Moon P, Spencer DE | year = 1988 | chapter = Elliptic-Cylinder Coordinates (η, ψ, z) | title = Field Theory Handbook, Including Coordinate Systems, Differential Equations, and Their Solutions | edition = corrected 2nd ed., 3rd print | publisher = Springer-Verlag | location = New York | pages = 17&ndash;20 (Table 1.03) | isbn = 978-0-387-18430-2}}
 
==External links==
*[http://mathworld.wolfram.com/EllipticCylindricalCoordinates.html MathWorld description of elliptic cylindrical coordinates]
 
{{Orthogonal coordinate systems}}
 
[[Category:Coordinate systems]]

Latest revision as of 13:50, 28 November 2013

Coordinate surfaces of elliptic cylindrical coordinates. The yellow sheet is the prism of a half-hyperbola corresponding to ν=-45°, whereas the red tube is an elliptical prism corresponding to μ=1. The blue sheet corresponds to z=1. The three surfaces intersect at the point P (shown as a black sphere) with Cartesian coordinates roughly (2.182, -1.661, 1.0). The foci of the ellipse and hyperbola lie at x = ±2.0.

Elliptic cylindrical coordinates are a three-dimensional orthogonal coordinate system that results from projecting the two-dimensional elliptic coordinate system in the perpendicular -direction. Hence, the coordinate surfaces are prisms of confocal ellipses and hyperbolae. The two foci and are generally taken to be fixed at and , respectively, on the -axis of the Cartesian coordinate system.

Basic definition

The most common definition of elliptic cylindrical coordinates is

where is a nonnegative real number and .

These definitions correspond to ellipses and hyperbolae. The trigonometric identity

shows that curves of constant form ellipses, whereas the hyperbolic trigonometric identity

shows that curves of constant form hyperbolae.

Scale factors

The scale factors for the elliptic cylindrical coordinates and are equal

whereas the remaining scale factor . Consequently, an infinitesimal volume element equals

and the Laplacian equals

Other differential operators such as and can be expressed in the coordinates by substituting the scale factors into the general formulae found in orthogonal coordinates.

Alternative definition

An alternative and geometrically intuitive set of elliptic coordinates are sometimes used, where and . Hence, the curves of constant are ellipses, whereas the curves of constant are hyperbolae. The coordinate must belong to the interval [-1, 1], whereas the coordinate must be greater than or equal to one.

The coordinates have a simple relation to the distances to the foci and . For any point in the (x,y) plane, the sum of its distances to the foci equals , whereas their difference equals . Thus, the distance to is , whereas the distance to is . (Recall that and are located at and , respectively.)

A drawback of these coordinates is that they do not have a 1-to-1 transformation to the Cartesian coordinates

Alternative scale factors

The scale factors for the alternative elliptic coordinates are

and, of course, . Hence, the infinitesimal volume element becomes

and the Laplacian equals

Other differential operators such as and can be expressed in the coordinates by substituting the scale factors into the general formulae found in orthogonal coordinates.

Applications

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

The three-dimensional wave equation, when expressed in elliptic cylindrical coordinates, may be solved by separation of variables, leading to the Mathieu differential equations.

The geometric properties of elliptic coordinates can also be useful. A typical example might involve an integration over all pairs of vectors and that sum to a fixed vector , where the integrand was a function of the vector lengths and . (In such a case, one would position between the two foci and aligned with the -axis, i.e., .) For concreteness, , and could represent the momenta of a particle and its decomposition products, respectively, and the integrand might involve the kinetic energies of the products (which are proportional to the squared lengths of the momenta).

Bibliography

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  • 20 year-old Real Estate Agent Rusty from Saint-Paul, has hobbies and interests which includes monopoly, property developers in singapore and poker. Will soon undertake a contiki trip that may include going to the Lower Valley of the Omo.

    My blog: http://www.primaboinca.com/view_profile.php?userid=5889534
  • 20 year-old Real Estate Agent Rusty from Saint-Paul, has hobbies and interests which includes monopoly, property developers in singapore and poker. Will soon undertake a contiki trip that may include going to the Lower Valley of the Omo.

    My blog: http://www.primaboinca.com/view_profile.php?userid=5889534
  • 20 year-old Real Estate Agent Rusty from Saint-Paul, has hobbies and interests which includes monopoly, property developers in singapore and poker. Will soon undertake a contiki trip that may include going to the Lower Valley of the Omo.

    My blog: http://www.primaboinca.com/view_profile.php?userid=5889534
  • 20 year-old Real Estate Agent Rusty from Saint-Paul, has hobbies and interests which includes monopoly, property developers in singapore and poker. Will soon undertake a contiki trip that may include going to the Lower Valley of the Omo.

    My blog: http://www.primaboinca.com/view_profile.php?userid=5889534 Same as Morse & Feshbach (1953), substituting uk for ξk.
  • 20 year-old Real Estate Agent Rusty from Saint-Paul, has hobbies and interests which includes monopoly, property developers in singapore and poker. Will soon undertake a contiki trip that may include going to the Lower Valley of the Omo.

    My blog: http://www.primaboinca.com/view_profile.php?userid=5889534

External links

Template:Orthogonal coordinate systems