
A new 3D code for electromagnetic induction tomography with intended applications to environmental imaging problems has been developed. The approach consists of calculating the fields within a volume using an implicit finite-difference frequency-domain formulation. The volume is terminated by an anisotropic perfectly matched layer region that simulates an infinite domain by absorbing outgoing waves. Extensive validation of this code has been done using analytical and semianalytical results from other codes, and some of those results are presented in this paper. The new code is written in Fortran 90 and is designed to be easily parallelized. Finally, an adjoint field method of data inversion, developed in parallel for solving the fully nonlinear inverse problem for electrical conductivity imaging (e.g., for mapping underground conducting plumes), uses this code to provide solvers for both forward and adjoint fields. Results obtained from this inversion method for high-contrast media are encouraging and provide a significant improvement over those obtained from linearized inversion methods.
Software, source code, etc. for problems pertaining to optics and electromagnetic theory, implicit finite-difference frequency-domain formulation, 3D code, electromagnetic induction tomography, anisotropic perfectly matched layer region, Fortran 90, Finite difference methods applied to problems in optics and electromagnetic theory
Software, source code, etc. for problems pertaining to optics and electromagnetic theory, implicit finite-difference frequency-domain formulation, 3D code, electromagnetic induction tomography, anisotropic perfectly matched layer region, Fortran 90, Finite difference methods applied to problems in optics and electromagnetic theory
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