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On a partial data inverse problem for the semi-linear wave equation

Boya Liu, Weinan Wang

TL;DR

We address recovering time-dependent nonlinearities of order at least three in a semi-linear wave equation from partial boundary data on a globally hyperbolic Lorentzian manifold with boundary. The approach combines higher-order linearization with Gaussian beam quasimodes that reflect off the boundary, enabling control of inaccessible boundary terms under arbitrarily small measurement sets. The main contributions are a partial data uniqueness result for the cubic nonlinearity $V_3$ and an inductive procedure to recover all higher coefficients $V_m$ ($m\ge4$) on the reachable set ${\mathbb U}$, assuming no conjugate points along null geodesics in ${\mathbb U}$. This demonstrates that nonlinear interactions can compensate for limited data and provides a framework for partial data inverse problems in nonlinear hyperbolic PDEs with minimal geometric restrictions.

Abstract

We show that a partial Dirichlet-to-Neumann map, where the measurement set is arbitrarily small, uniquely determines the time-dependent nonlinearity of order three or higher in a semi-linear wave equation up to natural obstructions on a Lorentzian manifold with boundary. In particular, we do not impose any geometric or size restrictions on the measurement set. The proof relies on the technique of higher order linearization combined with the construction of Gaussian beams with reflections on the boundary.

On a partial data inverse problem for the semi-linear wave equation

TL;DR

We address recovering time-dependent nonlinearities of order at least three in a semi-linear wave equation from partial boundary data on a globally hyperbolic Lorentzian manifold with boundary. The approach combines higher-order linearization with Gaussian beam quasimodes that reflect off the boundary, enabling control of inaccessible boundary terms under arbitrarily small measurement sets. The main contributions are a partial data uniqueness result for the cubic nonlinearity and an inductive procedure to recover all higher coefficients () on the reachable set , assuming no conjugate points along null geodesics in . This demonstrates that nonlinear interactions can compensate for limited data and provides a framework for partial data inverse problems in nonlinear hyperbolic PDEs with minimal geometric restrictions.

Abstract

We show that a partial Dirichlet-to-Neumann map, where the measurement set is arbitrarily small, uniquely determines the time-dependent nonlinearity of order three or higher in a semi-linear wave equation up to natural obstructions on a Lorentzian manifold with boundary. In particular, we do not impose any geometric or size restrictions on the measurement set. The proof relies on the technique of higher order linearization combined with the construction of Gaussian beams with reflections on the boundary.

Paper Structure

This paper contains 16 sections, 6 theorems, 102 equations.

Key Result

Theorem 1.1

Let $(\mathcal{M},g)$ be a $(1+n)$-dimensional globally hyperbolic Lorentzian manifold with $n\ge 2$, and let $\Sigma = (0,T)\times \partial M$ be its lateral boundary. Let $\Gamma \subset \Sigma$ be an arbitrary non-empty open set. Assume that null-geodesics do not have conjugate points in $\mathbb

Theorems & Definitions (7)

  • Theorem 1.1
  • Theorem 2.1
  • proof
  • Proposition 2.2
  • Lemma 3.1
  • Lemma 3.2
  • Lemma 4.1