Three-dimensional electromagnetic (EM) modeling in the frequency range
from 100 kHz to about 200 MHz using integral equations is examined. T
he modeling algorithm is formulated in the frequency domain. Time-doma
in responses for ground-penetrating radar (GPR) and very early time ti
me-decaying transients are computed via Fourier transforms. Of vital i
mportance to the modeling problem is the computation of the Hankel tra
nsforms in the Green's functions. The kernels of those Hankel transfor
ms vary rapidly at high frequencies where displacement currents become
important and are even singular for sources in the air, with poles ap
proaching the real axis or branch cuts lying on the real axis. We use
high density Hankel filters and a singularity extraction technique to
circumvent these problems. Our modeling for GPR applications shows tha
t dielectric targets are very obvious in radargrams, with waves reflec
ted by target boundaries arriving at distinctive times, depending on t
he path they travel. While GPR signals are absorbed in conductive medi
a, very early time-transient responses can detect conducting targets i
n conductive media. Our modeling shows that 1-D shallow conductors can
have large transient anomalies in the time window from 50 ns to 100 m
s. Thus 1-D near-surface conductors may be detected by conventional sy
stems operating at mu s ranges. However, shallow 3-D conductors of pra
ctical interest can have much earlier anomaly time windows around 100
ns, These targets can only be detected by very early time-transient eq
uipment. Moreover, very early time transients contain little informati
on on dielectric permittivities, being primarily determined by the con
ductivities of the media. Thus GPR and very early time transients are
excellent complements to each other.