A 3D physical model was built to study the possibilities of detection
of shallow underground diffracting objects by means of high resolution
seismic methods. The model structure is inspired from a real field si
tuation. It is composed of two superposed layers, several centimeters
thick, the lower one presenting a cylindrical hole of 3 cm diameter to
simulate a diffracting tunnel. This situation typically corresponds t
o the problem of the detection of meter size cavities situated at dept
hs of 10 to 12 m. The success of the model mostly results from the spe
cificity of the source developed (Mini-sparker). This source generates
a very short, omnidirectional and high power acoustic pulse, which is
difficult to obtain with conventional piezoelectric sources, but must
be as close as possible to real shallow seismic sources. The model is
used in this paper to discuss the efficiency of typical large depth s
eismic measurement and processing techniques for the detection of shal
low diffracting objects. Results are first presented for a ''Rubber-Pl
exiglass'' structure which corresponds to rather good conditions of de
tection. It is shown, in this condition, that an appropriate choice of
the geometry of the measurement system (Common-Offset with minimal of
fset) allows detection of the cavity without post-processing. A more c
omplex structure situation is then considered by means of a ''Plexigla
ss-Plexiglass'' structure. In this second model, the tunnel reflection
amplitude is always hidden by the coherent noise, whatever the geomet
ry of the measurement system. It is shown, in the situation considered
, that post-processing like bidimensional filtering can be applied aft
er Common-Offset measurements (with minimal offset) with enough effici
ency to enhance signal to noise ratio up to the detection of the diffr
acting object presence.