• Comment: I think this topic belongs on Wikipedia. However, the article was declined before (and now) because you have too many statements that do not have sources to verify them. There are also large sections where the article is inadequately sources. For instance there is "see Newton 2001" without specifics, plus the reference is incomplete (ISBN, URL etc). We are more picky than journals, everything has to be able to be verified by a non-expert. Ldm1954 (talk) 12:34, 3 September 2024 (UTC)

In Mathematics, and in particular Fluid Mechanics, the point vortex system is a well-studied dynamical system consisting of a number of points on the plane (or other surface) moving according to a law of interaction that derives from fluid motion. It was first introduced by Hermann von Helmholtz[1] in 1858, as part of his investigation into the motion of vortex filaments in 3 dimensions. It was first written in Hamiltonian form by Gustav Kirchhoff[2] a few years later.

A single point vortex in a fluid is like a whirlpool, with the fluid rotating about a central point (the point vortex itself). The speed of the surrounding fluid is inversely proportional to the distance of a fluid element to the point vortex. The constant of proportionality (or it divided by 2π) is called the vorticity or vortex strength of the point vortex. This is positive if the fluid rotates anticlockwise (like a cyclone in the Northern hemisphere) or negative if it rotates clockwise (anticyclone in the N. hemisphere), and has a constant value for each point vortex.

It was realized by Helmholtz that if there are several point vortices in an ideal fluid, then the motion of each depends only on the positions and strengths of the others, thereby giving rise to a system of ordinary differential equations whose variables are the coordinates of the point vortices (as functions of time).

The study of point vortices has been called a Classical Mathematics Playground by the fluid dynamicist Hassan Aref (2007), due to the many areas of classical mathematics that can be brought to bear for the analysis of this dynamical system.

Mathematical formulation

edit

For  , consider   points in the plane, with coordinates   (for  ) and vortex strengths  . Then Helmholtz’s equations of motion of the points are[3]

 

where   (the square of the distance between vortex   and vortex  ).

Hamiltonian version

edit

Consider the function (called the Kirchhoff-Routh Hamiltonian) given by

 

where   is given above.

The equations of motion are then given by

 

Note: if we put, for example,   and   then these become Hamilton’s usual canonical equations.

Complex notation

edit

Authors often use complex numbers to denote the positions of the vortices, with  . Then   and Helmholtz’s equations become

 

And the Hamiltonian version is, for the same Hamiltonian as above,

 

Conserved quantities

edit

In addition to the Hamiltonian, there are three (real) conserved quantities[4]. Two of these form the moment of vorticity and the third is the angular impulse:

 

In complex notation, this becomes

 

The third (the angular impulse) is

 

In the case that the total vorticity (or total circulation)   is non-zero, then by analogy with the centre of mass, the vector

 

is called the centre of vorticity.

These conserved quantities are related to the Euclidean symmetries of the system via Noether’s theorem. The angular impulse corresponds to the rotational symmetry of the system while the moment of vorticity corresponds to translational symmetries.

Two point vortices

edit

This simplest case can be solved exactly, and was already described by Helmholtz. Since the Hamiltonian is conserved it follows that the distance between the two vortices is constant.

If   then the centre of vorticity   is fixed and it follows from a short calculation that each of the two vortices moves in circles with centre  . The rate of rotation is constant, with period equal to  , where d is the separation of the vortices: this is easily derived from the equations of motion[5].

If   then the two vortices move at constant velocity in a direction perpendicular to the line joining the vortices, with speed equal to   where d is the separation of the vortices.

Three point vortices

edit

The case of 3 point vortices is completely integrable so is not chaotic. The first study of this case was made by Gröbli in his 1877 thesis[6]. Further work was done by J.L. Synge (1949). A summary and further investigation can be found in the paper of Aref (1979).

One property[7] is there are two types of relative equilibrium, which are motions where the 3 vortices move while maintaining their separations. The two types are firstly where the 3 vortices are collinear, and secondly where they form the vertices of an equilateral triangle. This is similar to the analogous property of 3 attracting bodies in celestial mechanics, especially their central configurations.

Rings of point vortices

edit

If N identical point vortices are placed at the vertices of a regular polygon, the configuration is known as a ring. It was known to Kelvin[8] that given such a configuration the vortices rotate at a constant rate (depending on the common vorticity and the radius) about the centre of vorticity, which lies at the centre of the polygon; he also knew that for three identical vortices this motion was (linearly) stable.

In his Adams Prize essay of 1843[9], J.J. Thomson (later famous for discovering the electron) analyzed the equations of motion near such a ring and showed that for   the ring is linearly stable, while for   it is unstable. The   case is known as Thomson’s heptagon and is degenerate (more eigenvalues of the linear approximation are zero than would be expected from the conservation laws). The nonlinear stability of Thomson’s heptagon was finally settled by Dieter Schmidt (2004) who showed, using normal form theory, that it is indeed stable.

Point vortices on non-planar surfaces

edit

There has been much interest in recent years on adapting the point vortex system to surfaces other than the plane. The first example was the system on the sphere, where the equations of motion were written down by Bogomolov (1977), with important early work by Kimura (1999) on general surfaces of constant curvature.

More recent work by Dritschel and Boatto (2015) and others shows the importance of the Green's function for the Laplacian and the Robin function for surfaces of non-constant curvature.

Diffeomorphism group

edit

Based on foundational ideas of V.I. Arnold (1966), Jerrold Marsden and Alan Weinstein (1983) showed that the point vortex system could be modelled as a Hamiltonian system on a natural finite dimensional coadjoint orbit of the diffeomorphism group of any orientable surface.

See also

edit

Notes

edit
  1. ^ see H. von Helmholtz (1858)
  2. ^ see G. Kirchhoff (1876)
  3. ^ see Newton (2001), Section 2.1
  4. ^ see Newton (2001), Sec 2.1
  5. ^ see Newton (2001) for details
  6. ^ see W. Gröbli (1877)
  7. ^ see Aref (2009)
  8. ^ Sir W. Thomson (1869)
  9. ^ see J.J. Thomson (1883)

References

edit
  • Aref, H. (1979). "Motion of three vortices". Physics of Fluids. 22 (3): 393–400. Bibcode:1979PhFl...22..393A. doi:10.1063/1.862605.
  • Aref, H. (2009). "Stability of relative equilibria of three vortices". Physics of Fluids. 21 (9): 094101–094101–22. Bibcode:2009PhFl...21i4101A. doi:10.1063/1.3216063. hdl:10919/24389.
  • Aref, H (2007). "Point vortex dynamics: A classical mathematics playground". J. Math. Phys. 48 (6): 065401. Bibcode:2007JMP....48f5401A. doi:10.1063/1.2425103. hdl:10919/25115.
  • Aref, H.; Newton, P.; Stremler, M.; Tokieda, T.; Vainchtein, D.L. (2003). "Vortex Crystals". Adv. Appl. Mechanics. Advances in Applied Mechanics. 39: 1–79. doi:10.1016/S0065-2156(02)39001-X. ISBN 978-0-12-002039-3.
  • Arnold, V. I. (1966). "Sur la géométrie différentielle des groupes de Lie de dimension infinie et ses applications à l'hydrodynamique des fluids parfaits". Ann. Inst. Fourier Grenoble. 16: 319–361. doi:10.5802/aif.233.
  • Bogomolov, V.A. (1977). "Dynamics of vorticity at a sphere". Fluid Dynamics. 12 (6): 863–870. Bibcode:1977FlDy...12..863B. doi:10.1007/BF01090320.
  • Dritschel, D.G.; Boatto, S. (2015). "The motion of point vortices on closed surfaces". Proc. R. Soc. A. 471 (2176): 20140890. Bibcode:2015RSPSA.47140890D. doi:10.1098/rspa.2014.0890.
  • Gröbli, Wolfgang (1877). Spezielle Probleme über die Bewegung geradliniger paralleler Wirbelfäden (Thesis). Zurich: Zürcher and Furrer.
  • Helmoltz, von, Hermann (1858). "Uber Integrale der hydrodynamischen Gleichungen, Welche den Wirbelbewegungen entsprechen". Crelle's Journal für Mathematik. 55: 25–55.
  • Kimura, Y (1999). "Vortex motion on surfaces with constant curvature". Proc. R. Soc. Lond. A. 455 (1981): 245–259. Bibcode:1999RSPSA.455..245K. doi:10.1098/rspa.1999.0311.
  • Kirchhoff, Gustav (1876). "Vorlesungen über mathematische Physik". Mechanik.
  • Marsden, J.E.; Weinstein, A. (1983). "Coadjoint orbits, vortices, and Clebsch variables for incompressible fluids". Physica D. 7 (1–3): 305–323. Bibcode:1983PhyD....7..305M. doi:10.1016/0167-2789(83)90134-3.
  • Moffatt, K. (2008). Vortex Dynamics: the legacy of Helmholtz and Kelvin. IUTAM Symposium on Hamiltonian Dynamics, Vortex Structures, Turbulence. pp. 1–10.
  • Newton, Paul (2001). The N-vortex Problem: Analytical Techniques. Applied Mathematical Science. Vol. 145 (2nd ed.). Springer. ISBN 978-0387952260.
  • Schmidt, Dieter (2004). "The stability of the Thomson heptagon". Regular and Chaotic Dynamics. 9 (4): 519–528. doi:10.1070/RD2004v009n04ABEH000294.
  • Synge, J.L. (1949). "On the motion of three vortices". Can. J. Math. 1 (3): 257–270. doi:10.4153/CJM-1949-022-2.
  • Thomson, J.J. (1883), A Treatise on the Motion of Vortex Rings. An Essay to Which the Adams Prize Was Adjudged in 1882, in the University of Cambridge., Macmillan
  • Thomson, Sir W. (Lord Kelvin) (1869). "On Vortex Motion". Trans. Roy. Soc. Edinburgh. 25: 217–260. doi:10.1017/S0080456800028179.