Liouville's equation
- 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.
In differential geometry, Liouville's equation, named after Joseph Liouville,[1][2] 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:
- [math]\displaystyle{ \Delta_0\log f = -K f^2, }[/math]
where ∆0 is the flat Laplace operator
- [math]\displaystyle{ \Delta_0 = \frac{\partial^2}{\partial x^2} +\frac{\partial^2}{\partial y^2} = 4 \frac{\partial}{\partial z} \frac{\partial}{\partial \bar z}. }[/math]
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.[3]
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:
- [math]\displaystyle{ \Delta_0 u = - K e^{2u}. }[/math]
Other two forms of the equation, commonly found in the literature,[4] are obtained by using the slight variant 2 log f ↦ u of the previous change of variables and Wirtinger calculus:[5] [math]\displaystyle{ \Delta_0 u = - 2K e^{u}\quad\Longleftrightarrow\quad \frac{\partial^2 u}{{\partial z}{\partial \bar z}} = - \frac{K}{2} e^{u}. }[/math]
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.[3][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
- [math]\displaystyle{ \Delta_{\mathrm{LB}} = \frac{1}{f^2} \Delta_0 }[/math]
as follows:
- [math]\displaystyle{ \Delta_{\mathrm{LB}}\log\; f = -K. }[/math]
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 [math]\displaystyle{ z }[/math] such that the Hopf differential is [math]\displaystyle{ \mathrm{d}z^2 }[/math].
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.[6] Its form is given by
- [math]\displaystyle{ u(z,\bar z) = \ln \left( 4 \frac{ \left|{\mathrm{d} f(z)}/{\mathrm{d} z}\right|^2 }{ ( 1+K \left|f(z)\right|^2)^2 } \right) }[/math]
where f (z) is any meromorphic function such that
Application
Liouville's equation can be used to prove the following classification results for surfaces:
[7] A surface in the Euclidean 3-space with metric dl2 = g(z,)dzd, and with constant scalar curvature K is locally isometric to:
.- the sphere if K > 0;
- the Euclidean plane if K = 0;
- 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
- ↑ Hilbert assumes K = -1/2, therefore the equation appears as the following semilinear elliptic equation
- [math]\displaystyle{ \frac{\partial^2 f}{\partial x^2} + \frac{\partial^2 f}{\partial y^2} = e^f }[/math]
Citations
- ↑ Liouville, Joseph (1838). "Sur la Theorie de la Variation des constantes arbitraires". Journal de mathématiques pures et appliquées 3: 342–349. http://sites.mathdoc.fr/JMPA/PDF/JMPA_1838_1_3_A26_0.pdf.
- ↑ Ehrendorfer, Martin. "The Liouville Equation: Background - Historical Background". The Liouville Equation in Atmospheric Predictability. pp. 48–49. https://www.ecmwf.net/sites/default/files/elibrary/2003/9271-liouville-equation-atmospheric-predictability.pdf.
- ↑ 3.0 3.1 See (Hilbert 1900): Hilbert does not cite explicitly Joseph Liouville.
- ↑ See (Dubrovin Novikov) and (Henrici 1993).
- ↑ See (Henrici 1993).
- ↑ 6.0 6.1 6.2 See (Henrici 1993).
- ↑ See (Dubrovin Novikov).
Works cited
- Dubrovin, B. A.; Novikov, S. P.; Fomenko, A. T. (1992), Modern Geometry–Methods and Applications. Part I. The Geometry of Surfaces, Transformation Groups, and Fields, Graduate Studies in Mathematics, 93 (2nd ed.), Berlin–Heidelberg–New York: Springer Verlag, pp. xv+468, ISBN 3-540-97663-9.
- Henrici, Peter (1993), Applied and Computational Complex Analysis, Wiley Classics Library, 3 (Reprint ed.), New York - Chichester - Brisbane - Toronto - Singapore: John Wiley & Sons, pp. X+637, ISBN 0-471-58986-1, https://books.google.com/books?id=vKZPsjaXuF4C.
- Hilbert, David (1900), "Mathematische Probleme" (in German), Nachrichten von der Königlichen Gesellschaft der Wissenschaften zu Göttingen, Mathematisch-Physikalische Klasse (3): 253–297, http://gdz.sub.uni-goettingen.de/dms/load/img/?PPN=PPN252457811_1900&DMDID=DMDLOG_0037, translated into English by Mary Frances Winston Newson as Hilbert, David (1902), "Mathematical Problems", Bulletin of the American Mathematical Society 8 (10): 437–479, doi:10.1090/S0002-9904-1902-00923-3, https://www.ams.org/journals/bull/1902-08-10/S0002-9904-1902-00923-3/.
Original source: https://en.wikipedia.org/wiki/Liouville's equation.
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