Uniqueness of Sobolev weak solutions of a wave equation Created 2026-10-05 Updated 2026-10-06
For the weak energy solution of a variable-coefficient wave equation, uniqueness can be proved without using as a spatial test function. For a difference with zero data, fix and test by for , extended by zero afterwards. Put , so . Integration by parts in time for the symmetric principal form, and in space for the first-order terms, giveFor short enough intervals the last term is absorbed. The Gronwall inequality forces , and repetition proves uniqueness on the full interval. This antiderivative test is valid at the stated space-time regularity, unlike an unqualified direct energy test by .
Van der Corput sum-integral lemma 2026-10-06
For a real phase with continuous monotone derivative and , the sum-integral discrepancy has the displayed uniform bound. Periodization and the Dirichlet-Jordan convergence theorem express it as symmetric nonzero Fourier modes. Integration by parts gives endpoint terms and reciprocal-derivative variations. Monotonicity bounds their total variation by . Pairing the leading endpoint terms reduces them to the uniformly bounded sine series. The exclusion of integer nonzero frequencies is essential.
Vanishing boundary condition Created 2026-09-28 Updated 2026-10-14
A vanishing boundary condition requires the relevant field, variation, or flux to tend to zero on the boundary. It removes boundary terms produced by integration by parts.
For the real-coefficient differential operator , integration by parts givesIf tends to zero at both endpoints and remain bounded there, the boundary term vanishes without prescribing endpoint values. Thus regular endpoint behaviour can supply the domain condition that makes the expression symmetric. Endpoint degeneracy alone is insufficient for arbitrary singular functions: for and , one has at zero. A self-adjoint differential operator requires a specified admissible domain, rather than only a formal differential expression.
For a smooth harmonic function on a manifold without boundary, assume its nonzero superlevel sets are compact. On a regular positive superlevel set , integration by parts gives . Applying the same argument to proves . This avoids assuming an unstated decay rate for the boundary flux at infinity.
Velocity-alignment energy dissipation 2026-10-25
For the mean-field alignment equation, multiply by and use integration by parts. Exchanging with and averaging the two results gives the displayed nonpositive kinetic energy derivative. The factor accounts for counting ordered pairs twice. Total momentum is conserved, so the dissipated part is motion relative to the global mean velocity.
Velocity-alignment entropy production 2026-10-25
For the mean-field alignment equation in position and velocity coordinates, put . Its force has velocity-space divergence . Consequently integration by parts gives the nonnegative derivative in the title, assuming suitable positivity, decay and integrability. The fine-grained Gibbs entropy decreases because these dynamics contract phase space; the interaction is dissipative.
Viscous magnetic-relaxation energy identity 2026-10-14
For constant mass density , kinematic viscosity , ideal induction, zero boundary velocity and tangent magnetic field, put . Multiplying the momentum equation by and integrating cancels pressure work and advective flux. The magnetic-energy derivative is minus the integral of Lorentz force density dotted with velocity, canceling the same work in the kinetic-energy equation. Integration by parts then gives the displayed identity. For incompressible flow with zero boundary velocity, .
Wallis integrals 2026-10-14
The Wallis integrals are for integers . Integration by parts gives for , with , . HenceBecause in the integration interval, for . Combining this with the recurrence gives , proving that the ratio tends to one and yielding the Wallis product.
Wave energy estimate 2026-10-06
If with d'Alembert operator , then , where . Test the wave equation against , use integration by parts, and apply the Cauchy-Schwarz inequality. The same energy estimate applies to a finite system of wave equations.
Wave map energy 2026-10-06
Weak convergence of bounded-variation integrators Created 2026-10-07 Updated 2026-10-14
If continuously differentiable converge uniformly on a compact interval and have uniformly bounded total variation of a function, then for every continuous . For continuously differentiable test functions this is integration by parts. Uniform approximation by polynomials extends the conclusion to continuous tests using the variation bound.
Weak formulation Created 2026-09-24 Updated 2026-10-14
A weak formulation multiplies a differential equation by a test function, integrates, and uses integration by parts to move derivatives away from the unknown function. Natural boundary conditions appear in the resulting boundary terms.
Weak-star convergence in BV 2026-10-07
Convergence in the displayed sense combines strong function convergence with weak-star convergence of derivative vector measures against tests. Strong convergence and a uniform variation bound imply the derivative convergence by integration by parts and uniform test-function approximation. Conversely the Uniform boundedness principle bounds the derivative measures of a convergent sequence.
For a nonreal regular Rayleigh equation for inviscid shear flow mode vanishing at the walls, put . The equation becomes . Multiplication by and integration by parts gives the displayed identity. With , its imaginary and real parts give and . Since , these imply Howard's semicircle theorem.
Yosida approximation 2026-10-25
For a contraction semigroup with semigroup generator , the bounded operators approximate on its generator domain. The Laplace-transform formula for a semigroup resolvent and strong continuity give for every vector : split into a short interval and an exponentially small tail. For , integration by parts gives , so . No operator norm convergence of is implied.
Zeldovich planar flux balance 2026-10-14
For a stationary planar advected magnetic flux potential, average its advection-diffusion equation horizontally and split it into mean and fluctuation. The mean transport is , with . Multiplying the fluctuation equation by and applying integration by parts gives . A vanishing mean derivative removes the constant term in the first correlation, yielding the displayed dissipative identity. The boundary assumptions must eliminate surface terms; a periodic layer replaces, rather than accompanies, decay at vertical infinity.