For , solve in three dimensions with , finite potential at the origin and decay at infinity. The Green function is in this sign convention. The angular integral supplied by the spherical shell theorem gives
The value at the origin is the limit . A second derivation sets : the radial Poisson equation becomes . Decay excludes the constant-potential term and boundedness at the origin cancels the remaining singularity. Although the source is locally integrable, it is singular at the origin; the resulting potential solves the equation there in the sense of distributions, without an extra Dirac delta.
For the Poisson equation on the unit disk with zero Dirichlet boundary condition, separation of variables in polar coordinates gives . For , boundedness at and select . The resonant mode is . For discontinuous angular data, the Poisson equation is interpreted in its weak formulation; its Dirichlet energy gives uniqueness. Orthogonality of the angular Fourier modes gives , with the resonant case obtained directly or by the limit .
On a smooth bounded connected domain, the homogeneous Neumann problem seeks such that for every . For it is solvable exactly when , and the weak solution is unique up to constants. The Poincare-Wirtinger inequality and the Riesz representation theorem give existence on the mean-zero Sobolev space. The test function one gives necessity of the compatibility condition.
For a radial Dirichlet solution on a fixed three-dimensional shell , . Thus , and bounds by the supremum of that integral. Cauchy-Schwarz inequality in the radial volume measure bounds the integral by . Since , the displayed gradient bound follows. The estimate exploits radiality and does not extend to arbitrary forcing in three dimensions.
Inside any three-dimensional domain containing a ball, let for a fixed smooth compactly supported nonconstant function. The right-hand side has constant norm, whereas diverges. The functions have zero boundary trace, giving a scaling counterexample to a uniform -forcing gradient estimate.
A Poisson kernel represents the harmonic extension of Dirichlet boundary data by an integral over the boundary. When the Dirichlet Green function is normalized by , its negative outward normal derivative gives the displayed kernel. The Poisson kernel for the upper half-space and the Poisson kernel for the upper half-plane give explicit examples with different boundary dimensions. Boundedness or other stated growth conditions are needed when selecting a solution in an unbounded domain.
In three dimensions the Poisson kernel for the upper half-space is
It gives the harmonic function for compatible boundary data. The method of images constructs the zero-boundary Dirichlet Green function by subtracting the reflected-source Green function of the Laplacian from the source kernel. On the boundary plane the outward unit normal is , and , giving the integral formula through Green's second identity.
The kernel is positive and has integral one: in polar coordinates this is . Its mass outside any fixed disk tends to zero as . It is therefore an approximate identity, recovering bounded boundary data at continuity points. At a jump across a smooth curve, the vertical limit gives the average of the two adjacent values; assigning a different value only on that curve does not change the harmonic extension.
Take boundary data one on a disk of radius and zero outside. The Poisson kernel for the upper half-space gives on the axis
The axis value tends to one at the boundary and behaves as far away. The boundary data at the circular rim are understood almost everywhere: changing a value on the rim, a set of planar measure zero, leaves the integral unchanged. This does not assert a continuous boundary extension across the jump.
For the complex upper half-plane, the Poisson kernel is
It is the density of harmonic measure on the real boundary as viewed from .
The Poisson integral convolves boundary data with the Poisson kernel to produce a harmonic function in a half-space. In the upper half-plane,
For boundary value on and zero outside, integrating the Poisson kernel for the upper half-plane gives the displayed bounded harmonic function for . It approaches the assigned values at boundary continuity points and the midpoint value at either jump. Changing the value at an isolated endpoint does not alter the integral. This is the unique bounded harmonic extension; pointwise decay in the vertical direction alone, without a spatial growth restriction, does not give uniqueness.
The conformal map sends to the complex upper half-plane. For bounded continuous boundary values on the horizontal axis and on the vertical axis with equal corner values, set for and for . The bounded harmonic function with those Dirichlet boundary conditions is
Equivalently, if with , this is . The Poisson kernel is a positive approximate identity, so the prescribed edge values are attained. Boundedness is essential for uniqueness on this unbounded domain.
Two bounded harmonic functions continuous to the quadrant edges with the same Dirichlet boundary conditions are equal. Their difference is bounded and zero on both axes. Odd reflection across each axis gives a bounded harmonic extension away from the corner; the removable singularity for a bounded harmonic function fills in that corner. The harmonic Liouville theorem makes that extension constant, and oddness makes the constant zero. This does not exclude unbounded examples such as the zero-boundary harmonic growth in a quadrant.
The harmonic function vanishes on both axes but is nonzero in the quadrant, and . More generally , for a positive integer , vanishes on both axes and is harmonic. Adding these unbounded functions leaves all edge Dirichlet boundary conditions unchanged. Thus decay of the boundary data does not imply decay of every solution, and an edge-data-only formula cannot determine an arbitrary solution's Wirtinger derivative. A boundedness or suitable growth condition must select the solution.
For the bounded Dirichlet Poisson integral in a quadrant, the Wirtinger derivative is
This follows by differentiating the Schwarz integral formula composed with , remembering that for real boundary data is half the derivative of a holomorphic function whose real part is . For complex boundary data, apply the construction to the real and imaginary parts separately and use linearity. If the data and their derivatives decay sufficiently, integration by parts gives
The endpoint terms cancel exactly when . Interior denominators do not vanish because .
The Schwarz integral formula reconstructs a holomorphic function from boundary values of its real part. For a real boundary function on the complex upper half-plane satisfying , the regularized form is
Its real part is the Poisson integral of . The subtraction makes the integral converge and changes only the imaginary normalization. Integration by parts, when the boundary terms vanish, gives ; jumps of are included as Dirac delta function terms in its distributional derivative.
For real boundary data , the displayed holomorphic integral has real part equal to the disk Poisson integral of and imaginary part its normalized harmonic conjugate. If is not identically zero, the real part is strictly positive inside the disk. A holomorphic logarithm then has imaginary part between and , while its real part records the logarithm of the magnitude. This separates uniform imaginary-part control from large real parts on small boundary sets.
For a harmonic function in the quadrant with boundary derivatives and , integrating the data to equal corner values and applying the Schwarz integral formula after the conformal map gives
These are tangential boundary derivatives, so uniqueness requires an additional normalization or growth restriction. A homogeneous contribution has the form with holomorphic in the complex upper half-plane and real on its boundary away from zero. For example, has zero prescribed derivatives on both edges.

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Poisson's equation is a fundamental partial differential equation in mathematical physics that relates the distribution of a scalar potential field to its sources. It is commonly used in electrostatics, gravitational theory, and fluid dynamics.
Poisson's equation by Ciro Santilli 40 Updated 2025-07-16
Generalization of Laplace's equation where the value is not necessarily 0.