For real and on a bounded regular domain, let be the zero-boundary kernel. The problem , on the boundary is solvable exactly when for every . The sign follows from Green second identity. After subtracting a boundary extension of , this is the usual orthogonality of the forcing to the null space of the self-adjoint Dirichlet realization. All solutions then differ by an element of .
Dirichlet Green function in a quadrant 2026-10-06
For the positive Laplacian convention , the method of images in the first quadrant reflects an interior pole across each axis with negative sign and across both with positive sign:The Dirichlet Green function vanishes on both axes. Its outward normal derivative on the horizontal axis isand the vertical-axis kernel follows by exchange of coordinates. Green second identity converts these derivatives into the quadrant Poisson integral for boundary data.
A global relation is an identity connecting transforms or integrals of the boundary traces of a solution. For a formally self-adjoint operator , Green second identity givesfor every homogeneous adjoint solution . Exponential adjoint families turn this into a spectral identity between the Dirichlet boundary condition and unknown normal derivative.
Kirchhoff–Helmholtz representation 2026-10-05
With the normal directed out of an obstacle into the fluid, a field solving outside has the representationHere is the outgoing Green function for the three-dimensional Helmholtz equation and the observation point lies outside the obstacle. The formula follows from Green second identity; the normal to the exterior fluid on its inner boundary is the negative of the stated obstacle normal. The surface term represents the scattered field.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 75 1 c Solution Created 2026-10-03 Updated 2026-10-06
Retain from part (b), and use time translation invariance to write . Define the temporal Fourier transform byMultiplying the transformed Green function equation by givesThis is a symmetric divergence-form spatial operator, although the original unweighted operator need not be symmetric in the ordinary volume measure.
Let . The product rule gives the bilinear Green second identityThe frequency terms cancel. Integrating over the domain, the right side becomesThe boundary integral is zero for common homogeneous Dirichlet boundary condition, Neumann boundary condition or reciprocal Robin boundary condition conditions. In an unbounded domain, use the same outgoing limiting-absorption prescription for both Green functions; it gives the corresponding vanishing boundary pairing. This identity has no complex conjugation: it proves transpose wave reciprocity, not a Hermitian or time-reversal identity. We obtain the weighted acoustic Green-function reciprocityThe factor is frequency independent, so inverse Fourier transform gives the same relation at equal time lag. Both time arguments below have lag , henceReciprocity exchanges source and receiver while preserving elapsed time; it does not turn a causal response into an advanced one.
Past exam of the mathematics course of the University of Cambridge 2015 iii Paper 70 3 Solution Created 2026-10-03 Updated 2026-10-06
Fix the convention , , and let . With , two families of modified Helmholtz adjoint plane waves areBoth satisfy , since the products of their and exponents are . They obey . Green second identity gives the two conjugate global relations for the modified Helmholtz equationFor real boundary traces, . Thus the second identity is the conjugate spectral companion, rather than an unrelated extra boundary condition. In complex differential form the first relation is equivalentlyIts integrand is a closed one-form: differentiating its coefficients gives . This supplies a direct derivation of the global relation as well as its outward-normal sign convention.
Write the known Dirichlet boundary condition on side as and the unknown outward normal derivative as , with . For any linear combination of the adjoint waves, the global relation isExpanding the in a finite basis and enforcing these identities at selected collocation points for a global relation gives a linear system with a known right side. The square permits especially simple paired tests.
Let , , and for . Define four real adjoint solutionsThey satisfy the modified Helmholtz equation because . Each is a linear combination of two adjoint exponentials, hence is obtained from the two spectral global relations. More explicitly, put , so . For the convention above, the required spectral pairs areAppropriate phase-weighted differences produce . For example the top test is . The conjugate relation ensures a real system for real data. This is sine collocation of square modified Helmholtz global relations.
The functions are an orthonormal Fourier sine basis on . Set and compute the known quantity by numerical integration. Since , each adjoint test vanishes on both adjacent sides. On its own side it equals , and on the opposite side it equals , where . Thus the square modified Helmholtz Dirichlet-to-Neumann coefficients obeyEach block is inverted explicitly: for opposite sides ,Compute these coefficients for and reconstruct . This is a semi-analytical scheme: the spectral basis integrals and two-by-two inverses are explicit, while the known boundary integrals are evaluated numerically. Increase and the quadrature resolution until the desired convergence is observed; compatible smooth side data have convergent normal-trace expansions, while corner singularities require the usual weaker trace interpretation and more careful quadrature.
The requested weak interaction between sides is particularly clear: the adjacent-side unknown traces contribute exactly zero, and the opposite-side coefficient is . The own-side coefficient stays equal to one. Thus diagonal dominance of paired square global-relation collocation is genuine after pairing; individual uncombined exponential samples need not have the same conditioning. The eigenvalues of each block are , so its condition number is .
There is also a direct localization check for an individual adjoint wave. On side with outward unit normal and tangent , the normalized test has . Its opposite-side magnitude is , and its magnitude integrates to at most along either adjacent side. This side localization of modified Helmholtz plane waves explains why suitable large spectral parameters suppress remote-side effects even before the exact sine cancellation.
Finally the interior solution can be evaluated from the computed traces using the two-dimensional modified Helmholtz fundamental solutionHere is the Modified Bessel function of the second kind, and . Replace by its computed finite Fourier sine series and use numerical integration; at interior points the boundary kernels are smooth. The sign follows from Green second identity with this fundamental-solution convention. This completes the numerical integration of the boundary value problem with a Dirichlet boundary condition, rather than stopping at an equation for its unknown boundary derivatives.
Past exam of the mathematics course of the University of Cambridge 2016 ia Paper 3 11C a Solution Created 2026-09-24 Updated 2026-10-06
The product rule for the divergence givesSubtracting cancels the two gradient products. ThereforeTo obtain the requested order of terms, apply this identity with interchanged and use the divergence theorem on the spherical shell. On the outer sphere the shell's outward unit normal is ; on the inner sphere it is . Write on both spheres. Then the resulting Green second identity isThe minus sign records the inward radial direction of the shell's normal on its inner boundary. Thus the normal derivatives in the displayed difference are outward from each individual ball; using shell-outward normals instead would put a plus sign between the two boundary integrals.
Past exam of the mathematics course of the University of Cambridge 2016 ib Paper 4 17B a Solution Created 2026-09-24 Updated 2026-10-06
With the positive logarithmic fundamental solution used here, a Dirichlet Green function for an interior pole satisfiesEquivalently, is harmonic near the pole, is harmonic away from it, and it has the specified logarithmic singularity. Regularity up to the remaining boundary is understood; on an unbounded domain impose the appropriate condition at infinity as well.
Apply Green second identity with and . Since is a harmonic function, the volume integral is . The term vanishes on the boundary by the Dirichlet boundary condition. ThereforeOne may equivalently excise a small disc around the pole and take its radius to zero. The sign is positive because this question uses , not the alternative negative-Laplacian convention.
Past exam of the mathematics course of the University of Cambridge 2016 iii Paper 328 3 i Solution Created 2026-10-03 Updated 2026-10-06
The formal adjoint of is itself. With the bilinear convention used in Green second identity, take any complex-valued satisfying . The product rule for divergence gives the familyEquivalently, the differential one-formis a closed differential form. Arbitrary linear combinations of adjoint solutions give further members of this family. One can also write it as wherever , but the first formula has no division and remains valid at zeros of . For a sesquilinear convention replace by ; no such conjugation is built into the bilinear identity used below.
Past exam of the mathematics course of the University of Cambridge 2017 iii Paper 107 3 b Solution Created 2026-10-03 Updated 2026-10-05
Let with real , and letThe Fredholm alternative for an elliptic Dirichlet problem says that is finite-dimensional. If , all the prescribed data admit a unique solution. In general the exact boundary compatibility in the self-adjoint Fredholm alternative isThese conditions are necessary and sufficient; when they hold, all solutions form . Thus in the second branch some data are incompatible, while compatible data have nonunique solutions. The outward normal derivative fixes the displayed sign.
To prove the alternative, put and . The standard zero-boundary Poisson equation theorem makes an isomorphism. Multiplication by , followed by , is a compact operator : the embedding is compact, and multiplication is bounded. Writing givesThe Fredholm alternative for a compact operator implies finite kernel and cokernel of equal dimension, and invertibility exactly when the kernel vanishes.
For the explicit compatibility conditions, use the self-adjoint Dirichlet realization of on . It has compact resolvent: a sufficiently large positive shift of is coercive, its inverse gains two derivatives, and the Rellich-Kondrachov compactness theorem makes that inverse compact. The Fredholm solvability condition for a self-adjoint operator is . Standard boundary elliptic regularity upgrades the resulting weak solution to for these data and boundary. Thus it gives the same kernel and solvability as the preceding Hölder-space formulation.
Finally Green second identity, with on the boundary and , givesConsequently , proving both necessity and sufficiency with the stated sign. If using complex data and real , replace by in the pairings.
Past exam of the mathematics course of the University of Cambridge 2018 ib Paper 4 17C Solution Created 2026-09-24 Updated 2026-10-03
Remove a small disc about and apply Green second identity to and . Since and , the shrinking inner boundary contributes and gives
For the unit disc, the method of images gives the Dirichlet Green functionwhich vanishes on the boundary by the hinted identity. The boundary representation with evaluates the normal derivative of at , giving the Poisson kernel
Past exam of the mathematics course of the University of Cambridge 2019 iii Paper 335 1 i Solution Created 2026-10-03 Updated 2026-10-05
Use the outgoing Green function for the three-dimensional Helmholtz equationLet point out of the obstacle into the exterior. Apply Green second identity to the field and in a large exterior region. Their Sommerfeld radiation conditions make the outer-sphere contribution vanish. The normal on the exterior region's inner boundary is , so the Kirchhoff–Helmholtz representation isThe first integral is the incident source field . Therefore the scattered field is the surface term. Since solves the homogeneous Helmholtz equation within the obstacle, its surface term is zero at exterior observation points; the same representation can be written using only scattered-field traces:The unknown boundary condition determines these traces, but the representation itself does not require choosing that condition.
Past exam of the mathematics course of the University of Cambridge 2022 ib Paper 3 14A a Solution Created 2026-09-24 Updated 2026-09-25
Apply Green second identity to and the free-space Green function on with a small ball about removed. Both functions are harmonic there, so only boundary terms remain. The contribution from the small sphere tends to becausehas unit delta source, while the remaining small-sphere term vanishes. Taking the radius to zero gives Green's third identity
For , the decaying fundamental solution of in two dimensions is , with the Modified Bessel function of the second kind. Green second identity reconstructs an interior solution from its Dirichlet boundary condition and outward normal derivative as .
Weighted acoustic Green-function reciprocity 2026-10-06
For an operator with positive stationary coefficients and reciprocal boundary conditions, its delta-normalized Green function satisfiesMultiplying its frequency-domain equation by and using the bilinear Green second identity proves the relation. Both Green functions must use the same outgoing or causal prescription. Exchanging source and receiver preserves time lag, and involves no complex conjugation.