Poloidal–toroidal decomposition
In vector analysis, a mathematical discipline, a poloidal–toroidal decomposition of a three-dimensional solenoidal vector field F writes it as a sum of a poloidal vector field and a toroidal vector field:
Thus, the vector field can be considered to be generated by a pair of scalar potentials Ψ and Φ. This decomposition is a restricted form of Helmholtz decomposition, and has been used in dynamo theory.
Poloidal and toroidal vector fields
A vector field is called toroidal if it can be written as
for some scalar field
.[1] Every toroidal field is solenoidal, because the divergence of the curl vanishes. A solenoidal vector field
is toroidal if and only if it is tangential to spheres around the origin (
).[2]
A vector field is called poloidal if it is the curl of a toroidal field; in other words, if there is a scalar field
such that
.[3] Thus, the curl of a toroidal field is poloidal; reversibly, the curl of a poloidal field is toroidal.[2] This leads to another characterization of poloidal vector fields: a solenoidal vector field is poloidal if and only if its curl is tangential to spheres around the origin.[4]
The decomposition
Every solenoidal vector field can be written as the sum of a toroidal and poloidal field. This decomposition is unique if it is required that the average of the scalar fields
and
vanishes on every sphere of radius
.[3]
Poloidal–toroidal decompositions also exist in Cartesian coordinates, but a mean-field flow has to included in this case. For example, every solenoidal vector field can be written as
where denote the unit vectors in the coordinate directions.[5]
See also
Notes
- ↑ Backus 1986, p. 87.
- ↑ 2.0 2.1 Backus, Parker & Constable 1996, p. 178.
- ↑ 3.0 3.1 Backus 1986, p. 88.
- ↑ Backus, Parker & Constable 1996, p. 179.
- ↑ Jones 2008, p. 62.
References
- Numerical simulations of stellar convective dynamos. I — The model and method, Glatzmaier, G. A.; Journal of Computational Physics, vol. 55, Sept. 1984, pp. 461–484.
- Hydrodynamic and hydromagnetic stability, Chandrasekhar, Subrahmanyan; International Series of Monographs on Physics, Oxford: Clarendon, 1961, p. 622.
- Decomposition of solenoidal fields into poloidal fields, toroidal fields and the mean flow. Applications to the boussinesq-equations, Schmitt, B. J. and von Wahl, W; in The Navier-Stokes Equations II — Theory and Numerical Methods, pp. 291–305; Lecture Notes in Mathematics, Springer Berlin/ Heidelberg, Vol. 1530/ 1992.
- Anelastic Magnetohydrodynamic Equations for Modeling Solar and Stellar Convection Zones, Lantz, S. R. and Fan, Y.; The Astrophysical Journal Supplement Series, Volume 121, Issue 1, Mar. 1999, pp. 247–264.
- Plane poloidal-toroidal decomposition of doubly periodic vector fields: Part 1. Fields with divergence and Part 2. Stokes equations. G. D. McBain. ANZIAM J. 47 (2005)
- Backus, George (1986), "Poloidal and toroidal fields in geomagnetic field modeling", Reviews in Geophysics 24: 75–109, doi:10.1029/RG024i001p00075.
- Backus, George; Parker, Robert; Constable, Catherine (1996), Foundations of Geomagnetism, Cambridge University Press, ISBN 0-521-41006-1.
- Jones, Chris (2008), Course 2: Dynamo Theory, Elsevier, doi:10.1016/S0924-8099(08)80006-6, ISBN 9780080548128.