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The global inverse fractional conductivity problem

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arxiv 2204.04325 v1 pith:SEWU4HLN submitted 2022-04-08 math.AP

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keywords conductivityexteriorfractionalinverseproblemequationglobalmaps
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We prove \emph{global} uniqueness for an inverse problem for the fractional conductivity equation on domains that are bounded in one direction. The conductivities are assumed to be isotropic and nontrivial in the exterior of the domain, while the data is given in the form of partial Dirichlet-to-Neumann (DN) maps measured in nondisjoint open subsets of the exterior. This can be seen as the fractional counterpart of the classical inverse conductivity problem. The proof is based on a unique continuation property (UCP) for the DN maps and an exterior determination method from the partial exterior DN maps. This is analogous to the classical boundary determination method by Kohn and Vogelius. The most important technical novelty is the construction of sequences of special solutions to the fractional conductivity equation whose Dirichlet energies in the limit can be concentrated at any given point in the exterior. This is achieved independently of the UCP and despite the nonlocality of the equation. Due to the recent counterexamples by the last two authors, our results almost completely characterize uniqueness for the inverse fractional conductivity problem with partial data for isotropic global conductivities.

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Cited by 2 Pith papers

Reviewed papers in the Pith corpus that reference this work. Sorted by Pith novelty score. Full citation record

  1. An Inverse Obstacle Problem for the Fractional Schr\"odinger Equation

    math.AP 2026-07 accept novelty 6.0 of 10

    A countable family of scaled exterior measurements of the fractional Schrödinger obstacle problem determines the nonnegative potential throughout the domain.

  2. Partial data stability for the inverse fractional conductivity problem

    math.AP 2025-05 conditional novelty 6.0 of 10

    Partial exterior measurements stably determine the fractional conductivity, with logarithmic (resp. log-log) stability when conductivities agree in the exterior (resp. when their difference has compact support).

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