Spilled petroleum products spread laterally in the capillary transitio
n zone above the water table. Ground penetrating radar (GPR) is a tech
nique that can potentially delineate the air/water capillary transitio
n zone (CTZ), because a varying water content strongly influences the
reflected signal through its effect on the electrical properties. The
vertical water distribution is determined on the pore scale by the gra
in size distribution and on the reservoir scale, mainly, by the permea
bility distribution. We present the integral equations for the reflect
ed signal from a inhomogeneous slab with a depth-dependent dielectric
constant and electrical conductivity. The numerical solution of the eq
uations allows us to compute the signal reflected from different sand
profiles. The results show that the reflected signal is strongly influ
enced by both the grain size distribution and the variation in permeab
ility. A strong frequency dependence is also observed. We present a tw
o-dimensional GPR profile measured in the field that shows a clear eff
ect of the CTZ on the reflection of the radar signal. All these result
s are considered of importance for the interpretation of GPR data invo
lving the capillary transition zone.