Section: New Results
Inverse problems for elliptic operators
Participants : Laurent Baratchart, Aline Bonami [Univ. Orléans] , Slah Chaabi, Sylvain Chevillard, Maureen Clerc [EPI Athena] , Yannick Fischer, Sandrine Grellier [Univ. Orléans] , Doug Hardin [Vanderbilt Univ.] , Abderrazek Karoui [Univ. Bizerte, Tunisie] , Juliette Leblond, Jean-Paul Marmorat, Ana-Maria Nicu, Théo Papadopoulo [EPI Athena] , Jonathan Partington, Elodie Pozzi, Edward Saff.
Boundary value problems for Laplace equation in 3-D
Solving overdetermined Cauchy problems for the Laplace equation on a spherical layer (in 3-D) in order to process incomplete experimental data is a necessary ingredient of the team's approach to inverse source problems, in particular for applications to EEG since the latter involves propagating the initial conditions from the boundary to the center of the domain where the singularities (i.e., the sources) are sought after. Here, the domain is typically made of several homogeneous layers of different conductivities.
Such problems offer an opportunity to state and solve extremal
problems for harmonic fields for which an analog of the Toeplitz
operator approach to bounded extremal problems [45] has
been obtained in [2] . Still, a best approximation on the subset of a general
vector field generated by a harmonic gradient under a
Issues of robust interpolation on the sphere from incomplete pointwise data are also under study in order to improve numerical accuracy of our reconstruction schemes. Spherical harmonics, Slepian bases and related special functions are of special interest (thesis of A.-M. Nicu), while splines, spherical wavelets, cubature techniques should be considered as well.
It turns out that Slepian functions are eigenfunctions of truncated Toeplitz operators in the complex plane (the framework of 2-D problems). These properties will be used in order to quantify the robustness properties of our resolution schemes for
The analogous problem in
The above issue is also interesting in
Sources recovery in 3-D domains, application to MEEG and geophysics
The problem of sources recovery can be handled in 3-D balls by using best rational approximation on 2-D cross sections (disks) from traces of the boundary data on the corresponding circles (see section 4.1 ).
In 3-D, functional or clinical active regions in the cortex are often represented by pointwise sources that have to be localized from measurements on the scalp of a potential satisfying a Laplace equation (EEG, electroencephalography). In the work [7] it was shown how to proceed via best rational approximation on a sequence of 2-D disks cut along the inner sphere, for the case where there are at most 2 sources. A long-haul research on the behaviour of poles of best rational approximants of fixed degree to functions with branch points was completed this year [19] , which shows that the technique carries over to finitely many sources.
In this connection, a dedicated software “FindSources3D” (see section 5.7 ) has been developed, in collaboration with the team Athena.
Further, it appears that in the rational approximation step of these schemes, multiple poles possess a nice behaviour with respect to the branched singularities (see figure 4 ). This is due to the very basic physical assumptions on the model (for EEG data, one should consider triple poles). Though numerically observed, there is no mathematical justification so far why these multiple poles have such strong accumulation properties, which remains an intriguing observation. This is the topic of [30] .
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Also, magnetic data from MEG (magneto-encephalography) will soon become available, which should enhance the accuracy of source recovery algorithms.
This approach also appears to be interesting for geophysical issues, namely discretizing the gravitational potential by means of pointwise masses. This is one topic of A.-M. Nicu's PhD thesis.
Magnetic sources localization from observations of the field away from the support of the magnetization is an issue under investigation in a joint effort with the Math. department of Vanderbilt University and the Earth Sciences department at MIT. The goal is to recover the magnetic properties of rock samples (meteorites) from fine measurements extremely close to the sample that can nowadays be obtained using SQUIDs (supraconducting coil devices).
The magnetization operator is the Riesz potential of the divergence of the magnetization, When the latter has bounded variation, we already described the kernel of this operator (the so-called silent magnetizations or silent source distributions) in terms of measures whose balayage on the boundary of the sample vanishes. This however, is not so very effective, computationally.
The case of a thin slab (the magnetization is then modelled as a vector field on a portion of the plane) has proved more amenable.
We have shown that that silent sources from above or below can be
characterized via the Hardy-Hodge decomposition mentioned in section
6.2.1 . The smoothness assumptions have been weakened considerably to
accomodate magnetizations that may be any distribution with compact support,
more generally any finite sum of partial derivatives of any order of
Meanwhile, the severe ill-posedness of the reconstruction challenges discrete Fourier methods, one of the main problems being the truncation of the observations outside the range of the SQUID measurements. A next step will be to develop the extrapolation techniques initiated by the project team, using bounded extremal problems, in an attempt to overcome this issue.
Boundary value problems for 2-D conductivity equations, application to plasma control
In collaboration with the CMI-LATP (University Marseille I) and in the framework of the ANR AHPI, the team considers 2-D diffusion processes with variable conductivity. In particular its complexified version, the so-called conjugate or real Beltrami equation, was investigated. In the case of a smooth domain, and for Lipschitz conductivity, we analyzed the Dirichlet problem for solutions in Sobolev and then in Hardy classes [8] .
Their traces merely lie in
This year we generalized the construction to finitely connected Dini-smooth
domains and
In the transversal section of a tokamak (which is a disk if the vessel is idealized into a torus), the so-called poloidal flux is subject to some conductivity equation outside the plasma volume for some simple explicit smooth conductivity function, while the boundary of the plasma (in the Tore Supra tokamak) is a level line of this flux [53] . Related magnetic measurements are available on the chamber, which furnish incomplete boundary data from which one wants to recover the inner (plasma) boundary. This free boundary problem (of Bernoulli type) can be handled through the solutions of a family of bounded extremal problems in generalized Hardy classes of solutions to real Beltrami equations, in the annular framework. Such approximation problems also allow us to approach a somewhat dual extrapolation issue, raised by colleagues from the CEA for the purpose of numerical simulation. It consists in recovering magnetic quantities on the outer boundary (the chamber) from an initial guess of what the inner boundary (plasma) is.
In the particular case at hand, the conductivity is
On the half-plane, the conductivity