Abstract
Approaches to solution of the inverse problem of electromagnetic sounding of subsurface layers of the Earth (determination of their permittivity) were considered with allowance for the time boundedness of a signal, presence of signal edges, and validity of the causality principle. Such consideration makes it possible to use the Laplace transform of a signal observed to develop effective methods for solving inverse problems. Peculiarities of solving the direct problem for different permittivity models were analyzed. An attempt of interpreting the effect of an increase in the characteristic frequency of a signal upon its propagation in the surface layers of the Earth was made.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
