Inmathematics, aDirichlet problem asks for afunction which solves a specifiedpartial differential equation (PDE) in the interior of a given region that takes prescribed values on the boundary of the region.[1]
The Dirichlet problem can be solved for many PDEs, although originally it was posed forLaplace's equation. In that case the problem can be stated as follows:
This requirement is called theDirichlet boundary condition. The main issue is to prove the existence of a solution; uniqueness can be proven using themaximum principle.
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The Dirichlet problem goes back toGeorge Green, who studied the problem on general domains with general boundary conditions in hisEssay on the Application of Mathematical Analysis to the Theories of Electricity and Magnetism, published in 1828.[2] He reduced the problem into a problem of constructing what we now callGreen's functions, and argued that Green's function exists for any domain. His methods were not rigorous by today's standards, but the ideas were highly influential in the subsequent developments. The next steps in the study of the Dirichlet's problem were taken byKarl Friedrich Gauss, William Thomson (Lord Kelvin) andPeter Gustav Lejeune Dirichlet, after whom the problem was named, and the solution to the problem (at least for the ball) using thePoisson kernel was known to Dirichlet (judging by his 1850 paper submitted to the Prussian academy). Lord Kelvin and Dirichlet suggested a solution to the problem by avariational method based on the minimization of "Dirichlet's energy". According toHans Freudenthal (in theDictionary of Scientific Biography, vol. 11),Bernhard Riemann was the first mathematician who solved this variational problem based on a method which he calledDirichlet's principle. The existence of a unique solution is very plausible by the "physical argument": any charge distribution on the boundary should, by the laws ofelectrostatics, determine anelectrical potential as solution. However,Karl Weierstrass found a flaw in Riemann's argument, and a rigorous proof of existence was found only in 1900 byDavid Hilbert, using hisdirect method in the calculus of variations. It turns out that the existence of a solution depends delicately on the smoothness of the boundary and the prescribed data.
For a domain having a sufficiently smooth boundary, the general solution to the Dirichlet problem is given by
where is theGreen's function for the partial differential equation, and
is the derivative of the Green's function along the inward-pointing unit normal vector. The integration is performed on the boundary, withmeasure. The function is given by the unique solution to theFredholm integral equation of the second kind,
The Green's function to be used in the above integral is one which vanishes on the boundary:
for and. Such a Green's function is usually a sum of the free-field Green's function and a harmonic solution to the differential equation.
The Dirichlet problem for harmonic functions always has a solution, and that solution is unique, when the boundary is sufficiently smooth and is continuous. More precisely, it has a solution when
for some, where denotes theHölder condition.
In some simple cases the Dirichlet problem can be solved explicitly. For example, the solution to the Dirichlet problem for theunit disk inR2 is given by thePoisson integral formula.[3]
If is a continuous function on the boundary of the open unit disk, then the solution to the Dirichlet problem is given by
The solution is continuous on the closed unit disk and harmonic on
The integrand is known as thePoisson kernel; this solution follows from the Green's function in two dimensions:
where isharmonic () and chosen such that for.
For bounded domains, the Dirichlet problem can be solved using thePerron method, which relies on themaximum principle forsubharmonic functions. This approach is described in many text books.[4] It is not well-suited to describing smoothness of solutions when the boundary is smooth. Another classicalHilbert space approach throughSobolev spaces does yield such information.[5] The solution of the Dirichlet problem usingSobolev spaces for planar domains can be used to prove the smooth version of theRiemann mapping theorem.Bell (1992) has outlined a different approach for establishing the smooth Riemann mapping theorem, based on thereproducing kernels of Szegő and Bergman, and in turn used it to solve the Dirichlet problem. The classical methods ofpotential theory allow the Dirichlet problem to be solved directly in terms ofintegral operators, for which the standard theory ofcompact andFredholm operators is applicable. The same methods work equally for theNeumann problem.[6]
Dirichlet problems are typical ofelliptic partial differential equations, andpotential theory, and theLaplace equation in particular. Other examples include thebiharmonic equation and related equations inelasticity theory.
They are one of several types of classes of PDE problems defined by the information given at the boundary, includingNeumann problems andCauchy problems.
Consider the Dirichlet problem for thewave equation describing a string attached between walls with one end attached permanently and the other moving with the constant velocity i.e. thed'Alembert equation on the triangular region of theCartesian product of the space and the time:
As one can easily check by substitution, the solution fulfilling the first condition is
Additionally we want
Substituting
we get the condition ofself-similarity
where
It is fulfilled, for example, by thecomposite function
with
thus in general
where is aperiodic function with a period:
and we get the general solution
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