Liouville's equation

In differential geometry, Liouville's equation, named after Joseph Liouville,[2][3] is the nonlinear partial differential equation satisfied by the conformal factor f of a metric f2(dx2 + dy2) on a surface of constant Gaussian curvature K:

[1]For Liouville's equation in dynamical systems, see Liouville's theorem (Hamiltonian).
For Liouville's equation in quantum mechanics, see Von Neumann equation.
For Liouville's equation in Euclidean space, see Liouville–Bratu–Gelfand equation.

where 0 is the flat Laplace operator

Liouville's equation appears in the study of isothermal coordinates in differential geometry: the independent variables x,y are the coordinates, while f can be described as the conformal factor with respect to the flat metric. Occasionally it is the square f2 that is referred to as the conformal factor, instead of f itself.

Liouville's equation was also taken as an example by David Hilbert in the formulation of his nineteenth problem.[4]

Other common forms of Liouville's equation

By using the change of variables log f  u, another commonly found form of Liouville's equation is obtained:

Other two forms of the equation, commonly found in the literature,[5] are obtained by using the slight variant 2 log f  u of the previous change of variables and Wirtinger calculus:[6]

Note that it is exactly in the first one of the preceding two forms that Liouville's equation was cited by David Hilbert in the formulation of his nineteenth problem.[4][lower-alpha 1]

A formulation using the Laplace–Beltrami operator

In a more invariant fashion, the equation can be written in terms of the intrinsic Laplace–Beltrami operator

as follows:

Properties

Relation to Gauss–Codazzi equations

Liouville's equation is equivalent to the Gauss–Codazzi equations for minimal immersions into the 3-space, when the metric is written in isothermal coordinates such that the Hopf differential is .

General solution of the equation

In a simply connected domain Ω, the general solution of Liouville's equation can be found by using Wirtinger calculus.[7] Its form is given by

where f (z) is any meromorphic function such that

  • df/dz(z)  0 for every z  Ω.[7]
  • f (z) has at most simple poles in Ω.[7]

Application

Liouville's equation can be used to prove the following classification results for surfaces:

Theorem.[8] A surface in the Euclidean 3-space with metric dl2 = g(z,_z)dzd_z, and with constant scalar curvature K is locally isometric to:

  1. the sphere if K > 0;
  2. the Euclidean plane if K = 0;
  3. the Lobachevskian plane if K < 0.

See also

  • Liouville field theory, a two-dimensional conformal field theory whose classical equation of motion is a generalization of Liouville's equation

Notes

  1. Hilbert assumes K = -1/2, therefore the equation appears as the following semilinear elliptic equation

Citations

  1. Liouville, Joseph (1838). "Sur la Theorie de la Variation des constantes arbitraires". Journal de Mathématiques Pures et Appliquées. 3: 342–349.
  2. Liouville, Joseph. "Sur la Theorie de la Variation des constantes arbitraires" (PDF). Journal de mathématiques pures et appliquées. 3: 342–349.
  3. Ehrendorfer, Martin. "The Liouville Equation: Background - Historical Background". The Liouville Equation in Atmospheric Predictability (PDF). pp. 48–49.
  4. See (Hilbert 1900, p. 288): Hilbert does not cite explicitly Joseph Liouville.
  5. See (Dubrovin, Novikov & Fomenko 1992, p. 118) and (Henrici 1993, p. 294).
  6. See (Henrici 1993, pp. 287–294).
  7. See (Henrici 1993, p. 294).
  8. See (Dubrovin, Novikov & Fomenko 1992, pp. 118–120).

Works cited

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