Abstract:

The transient  response of an electromagnetic plane wave obliquity incident upon the earth has been of interest to scientists in expiration geophysics The Hertizian vector corresponding to the reflected wave is expressed in terms of a single integral over a finite interval., in this paper, we study the validity of the diffusion approximation for a travail  electromagnetic plane wave obliquity incident in the earth which is modeled as a conductive half – space , we rely investigate the component for the transverse electric