Seismic wave scattering representation for the layered half-space with
lateral inhomogeneities subjected to a seismic dislocation source has
been formulated in the companion paper with the use of first-order pe
rturbation (Born-type approximation) technique. The total wavefield is
obtained as a superposition of the mean and the scattered wave fields
, which are generated, respectively, by a series of double couples of
body forces equivalent to the seismic dislocation source and by fictit
ious body forces equivalent to the existence of the lateral inhomogene
ities in the layered half-space. The responses in both the mean and th
e scattered wave fields are found with the aid of an integral transfor
m technique and wave propagation analysis. The characteristics of the
scattered waves and their effects on the mean waves or corresponding i
nduced ground and/or underground mean responses are investigated in th
is paper. In particular, coupling phenomena between P-SV and SH waves
and wave number shifting effects between the mean and the scattered wa
ve responses are presented in detail. With the lateral inhomogeneities
being assumed as a homogeneous random field a qualitative analysis is
provided for estimating the effects of the lateral inhomogeneities on
the ground motion, which is related to a fundamental issue: whether a
real earth medium can or cannot be approximately considered as a late
rally homogeneous layer. The effects of the lateral inhomogeneities on
the ground motion time history are also presented as a quantitative a
nalysis. Finally, a numerical example is carried out for illustration
purposes.