Geodesic
On the pulsed electromagnetic field interaction with flat boundary of absorbing media
Matematičeskoe modelirovanie, Tome 6 (1994) no. 1, pp. 99-109 
V. M. Kondrat'ev; I. G. Chernyshev. On the pulsed electromagnetic field interaction with flat boundary of absorbing media. Matematičeskoe modelirovanie, Tome 6 (1994) no. 1, pp. 99-109. http://geodesic.mathdoc.fr/item/MM_1994_6_1_a4/
@article{MM_1994_6_1_a4,
     author = {V. M. Kondrat'ev and I. G. Chernyshev},
     title = {On the pulsed electromagnetic field interaction with flat boundary of absorbing media},
     journal = {Matemati\v{c}eskoe modelirovanie},
     pages = {99--109},
     year = {1994},
     volume = {6},
     number = {1},
     language = {ru},
     url = {http://geodesic.mathdoc.fr/item/MM_1994_6_1_a4/}
}
TY  - JOUR
AU  - V. M. Kondrat'ev
AU  - I. G. Chernyshev
TI  - On the pulsed electromagnetic field interaction with flat boundary of absorbing media
JO  - Matematičeskoe modelirovanie
PY  - 1994
SP  - 99
EP  - 109
VL  - 6
IS  - 1
UR  - http://geodesic.mathdoc.fr/item/MM_1994_6_1_a4/
LA  - ru
ID  - MM_1994_6_1_a4
ER  - 
%0 Journal Article
%A V. M. Kondrat'ev
%A I. G. Chernyshev
%T On the pulsed electromagnetic field interaction with flat boundary of absorbing media
%J Matematičeskoe modelirovanie
%D 1994
%P 99-109
%V 6
%N 1
%U http://geodesic.mathdoc.fr/item/MM_1994_6_1_a4/
%G ru
%F MM_1994_6_1_a4

Voir la notice de l'article provenant de la source Math-Net.Ru

A calculation technique is presented which describes the reflected and refracted electromagnetic fields (EMF) generated by a pulsed radiation source elevated above the ground surface near the air-ground interface boundary. The technique is based on numerical integration using the finite differences method of the one-dimensional unstationary Maxwell equations system at the lag time. It allows to calculate reflected and refracted EMF at any angles of incidence, incident signal shape and soil electrophysical characteristics inlcuding a multi-layered one. The EMF calculation results in the air and ground are given.