Abstract
The time-domain fields originating from a vertical magnetic dipole placed on the surface of two-layered ground have been derived in an analytical form. The displacement currents in both the two ground layers have been taken into consideration. A previously obtained approximate solution [8] thus represents the late time part of the present solution. It is noteworthy to mention that the term “late time” used in the present work is not considered independently. It depends on both the separation and depth parameters X and D. The condition defining the late time term in [eq.(44), 8] thus seems to be overrestrictive in the case of the layered ground.
Sign-in/Register to access full text options 
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.
