Velocity Reconstruction from Flow-Induced Magnetic Fields
Abstract
We study the inverse problem of reconstructing an incompressible velocity field v from observations of the induced magnetic field b. In the presence of a strong, constant background field F, the evolution of the magnetic perturbation b is governed by the linearized induction equation. We analyze the system on both the entire space Ω= Rd and a periodic domain Ω= Πi=1d [0, Li), which models a homogeneous medium with side lengths Li > 0. We analyze this problem by decomposing it into the injectivity of a parabolic forward map and the solvability of a divergence-free transport sub-problem. On the whole space Rd, we show that the transport sub-problem is well-posed when data is prescribed on a non-characteristic hypersurface transverse to F. On the torus, we establish a sharp uniqueness criterion based on the rational dependence of the ratios \Fi/Li\i=1d between the background-field components and the corresponding domain periods. Furthermore, we show that for the reconstructed velocity to belong to L2, a sufficient condition is that the background field must satisfy a Diophantine condition. The proof combines injectivity of the parabolic forward map with uniqueness for a steady transport equation along F.
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