International audienceWe consider the inverse problem in magnetostatics for recovering the moment of a planar magnetization from measurements of the normal component of the magnetic field at a distance from the support. Such issues arise in studies of magnetic material in general and in paleomagnetism in particular. Assuming the magnetization is a measure with L^2-density, we construct linear forms to be applied on the data in order to estimate the moment. These forms are obtained as solutions to certain extremal problems in Sobolev classes of functions, and their computation reduces to solving an elliptic differential-integral equation, for which synthetic numerical experiments are presented
The use of the integral moments for interpreting magnetic data is based on a very elegant property o...
The estimation of the depth to the top and bottom of a magnetic source from magnetic data defines a ...
AbstractThe precession β and the dissipation parameter α of a ferromagnetic material can be consider...
International audienceWe study an inverse problem that consists in estimating the first (zero-order)...
We consider the problem of reconstruction of the overall magnetisation vector (net moment) of a samp...
Scanning magnetic microscopes typically measure the vertical component B_3 of the magnetic field on ...
We consider the problem of reconstruction of the overall magnetisation vector (net moment) of a samp...
International audienceWe consider the inverse problem of recovering the position and moment of a mag...
International audienceRecently developed scanning magnetic microscopes measure the magnetic field in...
This paper deals with the solution of inverse problems in magnetostatics. The cases the authors hav...
We study inverse potential problems with source term the divergence of some unknown (ℝ3-valued) meas...
International audienceInverse problems arising in (geo)magnetism are typically ill-posed, in particu...
The final aim of a magnetic survey is to obtain quantitative information about the geological source...
Journal ArticleParameter estimation in geoelectromagnetics aims to obtain the most important paramet...
International audienceIn the present work, we consider a magnetization moment recovery problem, that...
The use of the integral moments for interpreting magnetic data is based on a very elegant property o...
The estimation of the depth to the top and bottom of a magnetic source from magnetic data defines a ...
AbstractThe precession β and the dissipation parameter α of a ferromagnetic material can be consider...
International audienceWe study an inverse problem that consists in estimating the first (zero-order)...
We consider the problem of reconstruction of the overall magnetisation vector (net moment) of a samp...
Scanning magnetic microscopes typically measure the vertical component B_3 of the magnetic field on ...
We consider the problem of reconstruction of the overall magnetisation vector (net moment) of a samp...
International audienceWe consider the inverse problem of recovering the position and moment of a mag...
International audienceRecently developed scanning magnetic microscopes measure the magnetic field in...
This paper deals with the solution of inverse problems in magnetostatics. The cases the authors hav...
We study inverse potential problems with source term the divergence of some unknown (ℝ3-valued) meas...
International audienceInverse problems arising in (geo)magnetism are typically ill-posed, in particu...
The final aim of a magnetic survey is to obtain quantitative information about the geological source...
Journal ArticleParameter estimation in geoelectromagnetics aims to obtain the most important paramet...
International audienceIn the present work, we consider a magnetization moment recovery problem, that...
The use of the integral moments for interpreting magnetic data is based on a very elegant property o...
The estimation of the depth to the top and bottom of a magnetic source from magnetic data defines a ...
AbstractThe precession β and the dissipation parameter α of a ferromagnetic material can be consider...