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An orthogonal coordinate system is a system of curvilinear coordinates in which each family of surfaces intersects the others at right angles.
Orthogonal coordinates therefore satisfy the additional constraint that
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(1)
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where is the Kronecker delta. Therefore, the line element becomes
and the volume element becomes
where the latter is the Jacobian.
The gradient of a function is given in orthogonal
curvilinear coordinates by
the divergence is
![div(F)=del ·F=1/(h_1h_2h_3)[partial/(partialu_1)(h_2h_3F_1)+partial/(partialu_2)(h_3h_1F_2)+partial/(partialu_3)(h_1h_2F_3)],](/images/equations/OrthogonalCoordinateSystem/NumberedEquation2.gif) |
(11)
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and the curl is
For surfaces of first degree, the only three-dimensional coordinate system of surfaces having orthogonal intersections is Cartesian
coordinates (Moon and Spencer 1988, p. 1). Including degenerate cases, there
are 11 sets of quadratic surfaces having orthogonal coordinates. Furthermore, Laplace's equation and the Helmholtz differential
equation are separable in all of these coordinate systems (Moon and Spencer 1988,
p. 1).
Planar orthogonal curvilinear coordinate systems of degree two or less include two-dimensional Cartesian coordinates
and polar coordinates.
Three-dimensional orthogonal curvilinear coordinate systems of degree two or less include bipolar cylindrical
coordinates, bispherical
coordinates, three-dimensional Cartesian
coordinates, confocal
ellipsoidal coordinates, confocal
paraboloidal coordinates, conical
coordinates, cyclidic coordinates,
cylindrical coordinates,
ellipsoidal coordinates,
elliptic cylindrical
coordinates, oblate
spheroidal coordinates, parabolic
coordinates, parabolic
cylindrical coordinates, paraboloidal
coordinates, prolate
spheroidal coordinates, spherical
coordinates, and toroidal
coordinates. These are degenerate cases of the confocal ellipsoidal coordinates.
Orthogonal coordinate systems can also be built from fourth-order (in particular, cyclidic coordinates) and
higher surfaces (Bôcher 1894), but are generally less important in solving
physical problems than are quadratic surfaces (Moon and Spencer 1988, p. 1).
Arfken, G. "Curvilinear Coordinates" and "Differential Vector Operators." §2.1 and 2.2 in Mathematical Methods for Physicists, 3rd ed. Orlando, FL:
Academic Press, pp. 86-90 and 90-94, 1985.
Bôcher, M. Über die Reihenentwicklungen der Potentialtheorie. Leipzig,
Germany: Teubner, 1894.
Darboux, G. Sur une classe remarquable de courbes et de surfaces algébriques
et sur la théorie des imaginaires. Paris: Hermann, 1896.
Darboux, G. Leçons sur les systemes orthogonaux et les coordonnées
curvilignes. Paris: Gauthier-Villars, 1910.
Gradshteyn, I. S. and Ryzhik, I. M. Tables of Integrals, Series, and Products, 6th ed. San
Diego, CA: Academic Press, pp. 1084-1088, 2000.
Lamé, G. Leçons sur les coordonnées curvilignes et leurs diverses
applications. Paris: Mallet-Bachelier, 1859.
Moon, P. and Spencer, D. E. "Eleven Coordinate Systems." §1 in Field Theory Handbook, Including Coordinate Systems, Differential
Equations, and Their Solutions, 2nd ed. New York: Springer-Verlag, pp. 1-48,
1988.
Morse, P. M. and Feshbach, H. "Curvilinear Coordinates" and "Table of Properties of Curvilinear Coordinates." §1.3 in Methods of Theoretical Physics, Part I. New York: McGraw-Hill,
pp. 21-31 and 115-117, 1953.
Müller, E. "Die verschiedenen Koordinatensysteme." S. 596 in Encyk.
Math. Wissensch., Bd. III.1.1. Leipzig, Germany: Teubner, 1907-1910.
SeeAlso
Curvilinear Coordinates
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