Difference between revisions of "Laplace-Beltrami equation"
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''Beltrami equation'' | ''Beltrami equation'' | ||
− | A generalization of the [[Laplace equation|Laplace equation]] for functions in a plane to the case of functions | + | A generalization of the [[Laplace equation|Laplace equation]] for functions in a plane to the case of functions $ u $ |
+ | on an arbitrary two-dimensional Riemannian manifold $ R $ | ||
+ | of class $ C ^ {2} $. | ||
+ | For a surface $ R $ | ||
+ | with local coordinates $ \xi , \eta $ | ||
+ | and [[First fundamental form|first fundamental form]] | ||
− | + | $$ | |
+ | d s ^ {2} = E d \xi ^ {2} + 2 F d \xi d \eta + G d \eta ^ {2} , | ||
+ | $$ | ||
the Laplace–Beltrami equation has the form | the Laplace–Beltrami equation has the form | ||
− | + | $$ \tag{* } | |
+ | \Delta u \equiv \ | ||
+ | |||
+ | \frac \partial {\partial \xi } | ||
+ | |||
+ | \left ( | ||
− | + | \frac{F | |
+ | \frac{\partial u }{\partial \eta } | ||
+ | - G | ||
+ | \frac{\partial u }{\partial \xi } | ||
+ | }{\sqrt {E G - F ^ { 2 } } } | ||
− | + | \right ) | |
+ | + | ||
+ | \frac \partial {\partial \eta } | ||
− | + | \left ( | |
− | + | \frac{F | |
+ | \frac{\partial u }{\partial \xi } | ||
+ | - E | ||
+ | \frac{\partial u }{\partial \eta } | ||
+ | }{\sqrt {E G - F ^ { 2 } } } | ||
+ | |||
+ | \right ) = 0 . | ||
+ | $$ | ||
+ | |||
+ | For $ E = G $ | ||
+ | and $ F = 0 $, | ||
+ | that is, when $ ( \xi , \eta ) $ | ||
+ | are [[Isothermal coordinates|isothermal coordinates]] on $ R $, | ||
+ | equation (*) becomes the Laplace equation. The Laplace–Beltrami equation was introduced by E. Beltrami in 1864–1865 (see [[#References|[1]]]). | ||
+ | |||
+ | The left-hand side of equation (*) divided by $ \sqrt {E G - F ^ { 2 } } $ | ||
+ | is called the second Beltrami differential parameter. | ||
+ | |||
+ | Regular solutions $ u $ | ||
+ | of the Laplace–Beltrami equation are generalizations of harmonic functions and are usually called harmonic functions on the surface $ R $( | ||
+ | cf. also [[Harmonic function|Harmonic function]]). These solutions are interpreted physically like the usual harmonic functions, e.g. as the velocity potential of the flow of an incompressible liquid flowing over the surface $ R $, | ||
+ | or as the potential of an electrostatic field on $ R $, | ||
+ | etc. Harmonic functions on a surface retain the properties of ordinary harmonic functions. A generalization of the [[Dirichlet principle|Dirichlet principle]] is valid for them: Among all functions $ v $ | ||
+ | of class $ C ^ {2} ( G) \cap C ( \overline{G}\; ) $ | ||
+ | in a domain $ G \subset R $ | ||
+ | that take the same values on the boundary $ \partial G $ | ||
+ | as a harmonic function $ v \in C ( \overline{G}\; ) $, | ||
+ | the latter gives the minimum of the Dirichlet integral | ||
+ | |||
+ | $$ | ||
+ | D ( v) = {\int\limits \int\limits } _ { G } \nabla v \cdot \sqrt {E G - F ^ { 2 } } \ | ||
+ | d \xi d \eta , | ||
+ | $$ | ||
where | where | ||
− | + | $$ | |
+ | \nabla v = \ | ||
+ | |||
+ | \frac{E \left ( | ||
+ | \frac{\partial v }{\partial \eta } | ||
+ | \right ) ^ {2} | ||
+ | - 2 F | ||
+ | \frac{\partial v }{\partial \xi } | ||
+ | |||
+ | \frac{\partial v }{\partial \eta } | ||
+ | + | ||
+ | G \left ( | ||
+ | \frac{\partial v }{\partial \xi } | ||
+ | \right ) ^ {2} }{E G - F ^ { 2 } } | ||
+ | |||
+ | $$ | ||
− | is the first Beltrami differential parameter, which is a generalization of the square of the gradient | + | is the first Beltrami differential parameter, which is a generalization of the square of the gradient $ \mathop{\rm grad} ^ {2} u $ |
+ | to the case of functions on a surface. | ||
For generalizations of the Laplace–Beltrami equation to Riemannian manifolds of higher dimensions see [[Laplace operator|Laplace operator]]. | For generalizations of the Laplace–Beltrami equation to Riemannian manifolds of higher dimensions see [[Laplace operator|Laplace operator]]. |
Latest revision as of 22:15, 5 June 2020
Beltrami equation
A generalization of the Laplace equation for functions in a plane to the case of functions $ u $ on an arbitrary two-dimensional Riemannian manifold $ R $ of class $ C ^ {2} $. For a surface $ R $ with local coordinates $ \xi , \eta $ and first fundamental form
$$ d s ^ {2} = E d \xi ^ {2} + 2 F d \xi d \eta + G d \eta ^ {2} , $$
the Laplace–Beltrami equation has the form
$$ \tag{* } \Delta u \equiv \ \frac \partial {\partial \xi } \left ( \frac{F \frac{\partial u }{\partial \eta } - G \frac{\partial u }{\partial \xi } }{\sqrt {E G - F ^ { 2 } } } \right ) + \frac \partial {\partial \eta } \left ( \frac{F \frac{\partial u }{\partial \xi } - E \frac{\partial u }{\partial \eta } }{\sqrt {E G - F ^ { 2 } } } \right ) = 0 . $$
For $ E = G $ and $ F = 0 $, that is, when $ ( \xi , \eta ) $ are isothermal coordinates on $ R $, equation (*) becomes the Laplace equation. The Laplace–Beltrami equation was introduced by E. Beltrami in 1864–1865 (see [1]).
The left-hand side of equation (*) divided by $ \sqrt {E G - F ^ { 2 } } $ is called the second Beltrami differential parameter.
Regular solutions $ u $ of the Laplace–Beltrami equation are generalizations of harmonic functions and are usually called harmonic functions on the surface $ R $( cf. also Harmonic function). These solutions are interpreted physically like the usual harmonic functions, e.g. as the velocity potential of the flow of an incompressible liquid flowing over the surface $ R $, or as the potential of an electrostatic field on $ R $, etc. Harmonic functions on a surface retain the properties of ordinary harmonic functions. A generalization of the Dirichlet principle is valid for them: Among all functions $ v $ of class $ C ^ {2} ( G) \cap C ( \overline{G}\; ) $ in a domain $ G \subset R $ that take the same values on the boundary $ \partial G $ as a harmonic function $ v \in C ( \overline{G}\; ) $, the latter gives the minimum of the Dirichlet integral
$$ D ( v) = {\int\limits \int\limits } _ { G } \nabla v \cdot \sqrt {E G - F ^ { 2 } } \ d \xi d \eta , $$
where
$$ \nabla v = \ \frac{E \left ( \frac{\partial v }{\partial \eta } \right ) ^ {2} - 2 F \frac{\partial v }{\partial \xi } \frac{\partial v }{\partial \eta } + G \left ( \frac{\partial v }{\partial \xi } \right ) ^ {2} }{E G - F ^ { 2 } } $$
is the first Beltrami differential parameter, which is a generalization of the square of the gradient $ \mathop{\rm grad} ^ {2} u $ to the case of functions on a surface.
For generalizations of the Laplace–Beltrami equation to Riemannian manifolds of higher dimensions see Laplace operator.
References
[1] | E. Beltrami, "Richerche di analisi applicata alla geometria" , Opere Mat. , 1 , Milano (1902) pp. 107–198 |
[2] | M. Schiffer, D.C. Spencer, "Functionals of finite Riemann surfaces" , Princeton Univ. Press (1954) |
Laplace-Beltrami equation. Encyclopedia of Mathematics. URL: http://encyclopediaofmath.org/index.php?title=Laplace-Beltrami_equation&oldid=47576