Active measurements near a particle trajectory determine the background flow in the pressure-wave reachable set for polytropic compressible Euler equations assuming nonzero vorticity.
Inverse boundary value problems of determining nonlinear coefficients for the JMGT equation
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abstract
We consider inverse boundary value problems for the Jordan-Moore-Gibson-Thompson (JMGT) equation in nonlinear acoustics with quadratic nonlinearities of Kuznetsov-type and Westervelt-type. We show that the associated boundary Dirichlet-to-Neumann map uniquely determines the nonlinear coefficients $\beta$ in the Westervelt-type model, and the pair $(\beta,\kappa)$ in the Kuznetsov-type model, provided that the observation time is greater than the maximal boundary-to-boundary geodesic travel time. The results are obtained in both the Euclidean setting and on compact Riemannian manifolds with proper geometric assumptions. The proof is based on the idea of second order linearization combined with the construction of geometric optics and Gaussian beam solutions, reducing the inverse problem of uniqueness to the injectivity of associated geodesic ray transforms.
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math.AP 2years
2026 2representative citing papers
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An inverse problem for compressible Euler's equations
Active measurements near a particle trajectory determine the background flow in the pressure-wave reachable set for polytropic compressible Euler equations assuming nonzero vorticity.
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