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Authors
Advisor(s)
Abstract(s)
Acoustic propagation in shallow water is greatly
dependent on the geoacoustic properties of the seabottom. This
paper exploits this dependence for estimating geoacoustic sediment
properties from the bottom acoustic returns of known
signals received on a hydrophone line array. There are two major
issues in this approach: one is the feasibility of acoustic inversion
with a limited aperture line array, the other is related to the
knowledge of the geometry of the experimental configuration. To
test the feasibility of this approach, a 40-hydrophone4-m spaced
towed array together with a low-frequency acoustic source, was
operated at a shallow water site in the Strait of Sicily. In order to
estimate the array deformation in real time, it has been equipped
with a set of nonacoustic positioning sensors (compasses, tiltmeters,
pressure gauges). The acoustic data were inverted using
two complementary approaches: a genetic algorithm (GA) like
approach and a radial basis functions (RBF) inversion scheme.
More traditional methods, based on core sampling, seismic survey
and geophone data, together with Hamilton’s regression
curves, have also been employed on the same tracks, in order
to provide a ground truth reference environment. The results
of the experiment, can be summarized as follows: 1) the towed
array movement is not negligible for the application considered
and the use of positioning sensors are essential for a proper
acoustic inversion, 2) the inversion with GA and RBF are in
good qualitative agreement with the ground truth model, and 3)
the GA scheme tends to have better stability properties. On the
other hand, repeated inversion of successive field measurements
requires much less computational effort with RBF.
Description
Keywords
Geoacoustic seafloor Shallow water
Citation
A. Caiti, S. M. Jesus, A. Kristensen, "Geoacoustic seafloor exploration with a towed array in a shallow water area of the Strait of Sicily," IEEE J Ocean. Eng., Vol. 21, Oct 1996, pp. 355-366.
Publisher
IEEE Xplore