Automatic mass of the boundary double-layer density #
For an oriented smooth convex Jordan boundary, the double-layer density
rho_xi(t) = Im (gamma'(t) / (gamma(t) - xi)) / pi
has mass one at every frontier point. The proof chooses a parameter s for
xi, divides the boundary chord by gamma'(s), and rotates it by -I.
Convex support puts this normalized chord in Complex.slitPlane. Its
principal argument therefore lifts continuously from 0 to pi during one
period, and its derivative is exactly pi * rho_xi. Positivity makes the
lift monotone, which supplies derivative integrability; the improper
fundamental theorem then gives the mass identity.
Main declarations #
crouzeixBoundaryDoubleLayerDensity_periodic-- the density is periodic;canonicalNormal_support_all_of_Ioc-- oriented support on one fundamental interval propagates to every parameter;integral_crouzeixBoundaryDoubleLayerDensity_eq_one_of_oriented_carrier_point-- one consistently oriented carrier point forces unit mass at every frontier basepoint;crouzeixBoundaryPhaseContractive_of_oriented_carrier_point-- the same geometry gives sharp boundary-phase contractivity for every polynomial.
The explicit boundary double-layer density has the same period as the boundary trace.
An oriented support inequality verified on the standard half-open fundamental interval holds at every real parameter.
If one point of the open carrier lies consistently on the inward side of the canonical oriented tangent line, then the boundary double-layer density based at every frontier point has interval-integral mass one.
A consistently oriented point of the carrier makes every polynomial boundary phase contractive.