Bispherical coordinates: Difference between revisions

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'''Paraboloidal coordinates''' are a three-dimensional [[orthogonal coordinates|orthogonal]] [[coordinate system]] <math>(\lambda, \mu, \nu)</math> that generalizes the two-dimensional [[parabolic coordinates|parabolic coordinate system]].  Similar to the related [[ellipsoidal coordinates]], the paraboloidal coordinate system has [[orthogonal coordinates|orthogonal]] [[quadratic]] [[Coordinate system#Coordinate surface|coordinate surfaces]] that are ''not'' produced by rotating or projecting any two-dimensional orthogonal coordinate system.
 
[[File:Parabolic coordinates 3D.png|thumb|right|300px|[[Coordinate system#Coordinate surface|Coordinate surfaces]] of the three-dimensional paraboloidal coordinates.]]
 
==Basic formulae==
 
The Cartesian coordinates <math>(x, y, z)</math> can be produced from the ellipsoidal coordinates
<math>( \lambda, \mu, \nu )</math> by the equations
 
:<math>
x^{2} = \frac{\left( A - \lambda \right) \left( A - \mu \right) \left( A - \nu \right)}{B - A}
</math>
 
:<math>
y^{2} = \frac{\left( B - \lambda \right) \left( B - \mu \right) \left( B - \nu \right)}{A - B}
</math>
 
:<math>
z =
\frac{1}{2} \left( A + B - \lambda - \mu -\nu \right)
</math>
 
where the following limits apply to the coordinates
 
:<math>
\lambda < B < \mu < A < \nu
</math>
 
Consequently, surfaces of constant <math>\lambda</math> are elliptic [[paraboloid]]s
 
:<math>
\frac{x^{2}}{\lambda - A} +  \frac{y^{2}}{\lambda - B}  = 2z + \lambda
</math>
 
and surfaces of constant <math>\nu</math> are likewise
 
:<math>
\frac{x^{2}}{\nu - A} +  \frac{y^{2}}{\nu - B}  = 2z + \nu
</math>
 
whereas surfaces of constant <math>\mu</math> are hyperbolic [[paraboloid]]s
 
:<math>
\frac{x^{2}}{\mu - A} +  \frac{y^{2}}{\mu - B} = 2z + \mu
</math>
 
==Scale factors==
 
The scale factors for the paraboloidal coordinates <math>(\lambda, \mu, \nu )</math> are
:<math>
h_{\lambda} = \frac{1}{2} \sqrt{\frac{\left( \mu - \lambda \right) \left( \nu - \lambda \right)}{ \left( A - \lambda \right) \left( B - \lambda \right)}}
</math>
 
:<math>
h_{\mu} = \frac{1}{2} \sqrt{\frac{\left( \nu - \mu \right) \left( \lambda - \mu \right)}{ \left( A - \mu \right) \left( B - \mu \right)}}
</math>
 
:<math>
h_{\nu} = \frac{1}{2} \sqrt{\frac{\left( \lambda - \nu \right) \left( \mu - \nu \right)}{ \left( A - \nu \right) \left( B - \nu \right)}}
</math>
 
Hence, the infinitesimal volume element equals
 
:<math>
dV = \frac{\left( \mu - \lambda \right) \left( \nu - \lambda \right) \left( \nu - \mu\right)}{8\sqrt{\left( A - \lambda \right) \left( B - \lambda \right) \left( A - \mu \right) \left( \mu - B \right) \left( \nu - A \right) \left( \nu  - B \right) }} \  d\lambda d\mu d\nu
</math>
 
Differential operators such as <math>\nabla \cdot \mathbf{F}</math>
and <math>\nabla \times \mathbf{F}</math> can be expressed in the coordinates <math>(\lambda, \mu, \nu)</math> by substituting the scale factors into the general formulae found in [[orthogonal coordinates]].
 
==References==
{{reflist}}
 
==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|lccn=52011515 | page = 664}}
*{{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 = 184&ndash;185 | 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 = 180 | lccn = 5914456}}
*{{cite book | author = Arfken G | year = 1970 | title = Mathematical Methods for Physicists | edition = 2nd | publisher = Academic Press | location = Orlando, FL | pages = 119&ndash;120}}
*{{cite book | author = Sauer R, Szabó I | year = 1967 | title = Mathematische Hilfsmittel des Ingenieurs | publisher = Springer Verlag | location = New York | page = 98 | 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 = Paraboloidal Coordinates (μ, ν, λ) | 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 = 44&ndash;48 (Table 1.11) | isbn = 978-0-387-18430-2}}
 
==External links==
*[http://mathworld.wolfram.com/ConfocalParaboloidalCoordinates.html MathWorld description of confocal paraboloidal coordinates]
 
{{Orthogonal coordinate systems}}
 
[[Category:Coordinate systems]]

Revision as of 19:32, 14 December 2013

Paraboloidal coordinates are a three-dimensional orthogonal coordinate system that generalizes the two-dimensional parabolic coordinate system. Similar to the related ellipsoidal coordinates, the paraboloidal coordinate system has orthogonal quadratic coordinate surfaces that are not produced by rotating or projecting any two-dimensional orthogonal coordinate system.

Coordinate surfaces of the three-dimensional paraboloidal coordinates.

Basic formulae

The Cartesian coordinates can be produced from the ellipsoidal coordinates by the equations

where the following limits apply to the coordinates

Consequently, surfaces of constant are elliptic paraboloids

and surfaces of constant are likewise

whereas surfaces of constant are hyperbolic paraboloids

Scale factors

The scale factors for the paraboloidal coordinates are

Hence, the infinitesimal volume element equals

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

References

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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.

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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 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.

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External links

Template:Orthogonal coordinate systems