Diffraction by a Right-Angle Penetrable Wedge: Closed-Form Solution for General Refractive Index
Jonas Matuzas
TL;DR
The paper tackles 2D time-harmonic diffraction by a penetrable right-angle wedge with impedance-matched transmission and general refractive-index ratio $\nu>1$. It develops an explicit genus-one Riemann–Hilbert framework via elliptic uniformization of the Snell surface $\Sigma_\nu$, solving a $2\times2$ RH problem for general forcing data, with the Meixner edge condition enforced by a residue-sum constraint. Extending the lemniscatic case ($\nu^2=2$) to general $\nu>1$, it provides a closed-form solution, a practical evaluation recipe, and a degeneration limit to jet-polynomial regimes, plus a complete Sommerfeld representation linking spectral data to the physical field. The approach yields explicit expressions for the exterior and interior fields, including the far-field diffraction coefficient, and delivers a reproducible symbolic example, making it a versatile building block for more complex wedge and polygon diffraction problems using elliptic-function techniques.
Abstract
We consider the two-dimensional time-harmonic transmission problem for an impedance-matched ($ρ=1$) right-angle penetrable wedge at general refractive index ratio $ν>1$. Starting from Sommerfeld spectral representations, the transmission conditions on the two wedge faces yield a closed spectral functional system whose unknowns live on the Snell surface $Σ_ν: Y^2=ν^2 t^4+2(ν^2-2)t^2+ν^2$. We uniformize $Σ_ν$ by Jacobi/Weierstrass elliptic functions on a torus $\mathbb{C}/Λ$ and solve the resulting $2\times 2$ genus-one Riemann--Hilbert problem in closed form for general finite forcing data. The Sommerfeld radiation condition and the Meixner edge condition are enforced by a simple residue-sum constraint. The construction extends the special lemniscatic case $ν^2=2$ treated in arXiv:2601.04183 and yields a practical evaluation recipe expressed in theta/sigma products and explicit triangular factor matrices. We include the complete Sommerfeld representation connecting the spectral solution to the physical field, explicit forcing data for plane wave incidence, and a worked symbolic example at $ν=3/2$.
