Toroidal coordinates
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Toroidal coordinates are a three-dimensional orthogonal coordinate system that results from rotating the two-dimensional bipolar coordinate system about the axis that separates its two foci. Thus, the two foci F_1 and F_2 in bipolar coordinates become a ring of radius a in the xy plane of the toroidal coordinate system; the z-axis is the axis of rotation. The focal ring is also known as the reference circle.


Definition

The most common definition of toroidal coordinates (\tau, \sigma, \phi) is : x = a \ \frac \cos \phi : y = a \ \frac \sin \phi : z = a \ \frac together with \mathrm(\sigma)=\mathrm(z). The \sigma coordinate of a point P equals the angle F_ P F_ and the \tau coordinate equals the natural logarithm of the ratio of the distances d_ and d_ to opposite sides of the focal ring : \tau = \ln \frac. The coordinate ranges are -\pi<\sigma\le\pi, \tau\ge 0 and 0\le\phi < 2\pi.


Coordinate surfaces

Surfaces of constant \sigma correspond to spheres of different radii : \left( x^ + y^ \right) + \left( z - a \cot \sigma \right)^ = \frac that all pass through the focal ring but are not concentric. The surfaces of constant \tau are non-intersecting tori of different radii : z^ + \left( \sqrt - a \coth \tau \right)^ = \frac that surround the focal ring. The centers of the constant-\sigma spheres lie along the z-axis, whereas the constant-\tau tori are centered in the xy plane.


Inverse transformation

The (\sigma, \tau, \phi) coordinates may be calculated from the Cartesian coordinates (''x'', ''y'', ''z'') as follows. The azimuthal angle \phi is given by the formula : \tan \phi = \frac The cylindrical radius \rho of the point P is given by : \rho^ = x^ + y^ = \left(a \frac\right)^ and its distances to the foci in the plane defined by \phi is given by : d_^ = (\rho + a)^ + z^ : d_^ = (\rho - a)^ + z^ The coordinate \tau equals the natural logarithm of the focal distances : \tau = \ln \frac whereas , \sigma, equals the angle between the rays to the foci, which may be determined from the law of cosines : \cos \sigma = \frac. Or explicitly, including the sign, : \sigma = \mathrm(z)\arccos \frac where r=\sqrt . The transformations between cylindrical and toroidal coordinates can be expressed in complex notation as : z+i\rho \ = ia\coth\frac , : \tau+i\sigma \ = \ln\frac.


Scale factors

The scale factors for the toroidal coordinates \sigma and \tau are equal : h_\sigma = h_\tau = \frac whereas the azimuthal scale factor equals : h_\phi = \frac Thus, the infinitesimal volume element equals : dV = \frac \, d\sigma \, d\tau \, d\phi


Differential Operators

The Laplacian is given by \begin \nabla^2 \Phi = \frac & \left \sinh \tau \frac \left( \frac \frac \right) \right. \\[8pt& \quad + \left. \frac \left( \frac \frac \right) + \frac \frac \right] \end For a vector field \vec(\tau,\sigma,\phi) = n_(\tau,\sigma,\phi)\hat_ + n_(\tau,\sigma,\phi) \hat_ + n_ (\tau,\sigma,\phi) \hat_, the Vector Laplacian is given by \begin \Delta \vec(\tau,\sigma,\phi) &= \nabla (\nabla \cdot \vec) - \nabla \times (\nabla \times \vec) \\ &= \frac\vec_ \left \\\ &+ \frac\vec_ \left \\\ &+ \frac\vec_ \left \ \end Other differential operators such as \nabla \cdot \mathbf and \nabla \times \mathbf can be expressed in the coordinates (\sigma, \tau, \phi) by substituting the scale factors into the general formulae found in orthogonal coordinates.


Toroidal harmonics


Standard separation

The 3-variable
Laplace equation In mathematics and physics, Laplace's equation is a second-order partial differential equation named after Pierre-Simon Laplace, who first studied its properties. This is often written as \nabla^2\! f = 0 or \Delta f = 0, where \Delta = \n ...
:\nabla^2\Phi=0 admits solution via
separation of variables In mathematics, separation of variables (also known as the Fourier method) is any of several methods for solving ordinary and partial differential equations, in which algebra allows one to rewrite an equation so that each of two variables occurs ...
in toroidal coordinates. Making the substitution : \Phi=U\sqrt A separable equation is then obtained. A particular solution obtained by
separation of variables In mathematics, separation of variables (also known as the Fourier method) is any of several methods for solving ordinary and partial differential equations, in which algebra allows one to rewrite an equation so that each of two variables occurs ...
is: :\Phi= \sqrt\,\,S_\nu(\sigma)T_(\tau)V_\mu(\phi) where each function is a linear combination of: : S_\nu(\sigma)=e^\,\,\,\,\mathrm\,\,\,\,e^ : T_(\tau)=P_^\mu(\cosh\tau)\,\,\,\,\mathrm\,\,\,\,Q_^\mu(\cosh\tau) : V_\mu(\phi)=e^\,\,\,\,\mathrm\,\,\,\,e^ Where P and Q are associated Legendre functions of the first and second kind. These Legendre functions are often referred to as toroidal harmonics. Toroidal harmonics have many interesting properties. If you make a variable substitution z=\cosh\tau>1 then, for instance, with vanishing order \mu=0 (the convention is to not write the order when it vanishes) and \nu=0 :Q_(z)=\sqrtK\left(\sqrt\right) and :P_(z)=\frac\sqrtK \left( \sqrt \right) where \,\!K and \,\!E are the complete elliptic integrals of the first and second kind respectively. The rest of the toroidal harmonics can be obtained, for instance, in terms of the complete elliptic integrals, by using recurrence relations for associated Legendre functions. The classic applications of toroidal coordinates are in solving
partial differential equations In mathematics, a partial differential equation (PDE) is an equation which imposes relations between the various partial derivatives of a multivariable function. The function is often thought of as an "unknown" to be solved for, similarly to ...
, e.g., Laplace's equation for which toroidal coordinates allow a
separation of variables In mathematics, separation of variables (also known as the Fourier method) is any of several methods for solving ordinary and partial differential equations, in which algebra allows one to rewrite an equation so that each of two variables occurs ...
or the Helmholtz equation, for which toroidal coordinates do not allow a separation of variables. Typical examples would be the
electric potential The electric potential (also called the ''electric field potential'', potential drop, the electrostatic potential) is defined as the amount of work energy needed to move a unit of electric charge from a reference point to the specific point in ...
and electric field of a conducting torus, or in the degenerate case, an electric current-ring (Hulme 1982).


An alternative separation

Alternatively, a different substitution may be made (Andrews 2006) : \Phi=\frac where : \rho=\sqrt=\frac. Again, a separable equation is obtained. A particular solution obtained by
separation of variables In mathematics, separation of variables (also known as the Fourier method) is any of several methods for solving ordinary and partial differential equations, in which algebra allows one to rewrite an equation so that each of two variables occurs ...
is then: :\Phi= \frac\,\,S_\nu(\sigma)T_(\tau)V_\mu(\phi) where each function is a linear combination of: : S_\nu(\sigma)=e^\,\,\,\,\mathrm\,\,\,\,e^ : T_(\tau)=P_^\nu(\coth\tau)\,\,\,\,\mathrm\,\,\,\,Q_^\nu(\coth\tau) : V_\mu(\phi)=e^\,\,\,\,\mathrm\,\,\,\,e^. Note that although the toroidal harmonics are used again for the ''T''  function, the argument is \coth\tau rather than \cosh\tau and the \mu and \nu indices are exchanged. This method is useful for situations in which the boundary conditions are independent of the spherical angle \theta, such as the charged ring, an infinite half plane, or two parallel planes. For identities relating the toroidal harmonics with argument hyperbolic cosine with those of argument hyperbolic cotangent, see the Whipple formulae.


References

*Byerly, W E. (1893)
An elementary treatise on Fourier's series and spherical, cylindrical, and ellipsoidal harmonics, with applications to problems in mathematical physics
' Ginn & co. pp. 264–266 * * *


Bibliography

* * * *


External links



{{Orthogonal coordinate systems Three-dimensional coordinate systems Orthogonal coordinate systems