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EurOCEAN 2000 - Vlaams Instituut voor de Zee

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hydrophone array (Multiple Outputs). To compensate for the motion of the tow fish<br />

(acoustic transmitter) a real time electronically stabilised system will be <strong>de</strong>veloped, while<br />

for the compensation of the movement of the towed array a special purpose acoustic<br />

<strong>de</strong>vice will be <strong>de</strong>veloped as well.<br />

4. Theoretical and numerical accurate acoustic wave propagation mo<strong>de</strong>ls as well as inverse<br />

procedures will be investigated. The mo<strong>de</strong>ls and procedures will be generalised to inclu<strong>de</strong><br />

realistic cases like oblique interfaces, hybrid velocity profiles (continuously layered and<br />

stepped variations), inhomogeneities and inclusions. Direct inversion computational<br />

methods and parameter estimators, such as an MLE (Maximum Likelihood Estimator),<br />

will be <strong>de</strong>veloped and analysed taking into account instrumental factors, such as noise and<br />

the transmitter and receiver characteristics, which will be obtained by extensive calibration<br />

measurement procedures.<br />

5. The theoretical mo<strong>de</strong>ls and inverse procedures will be validated based on the <strong>de</strong>sign of<br />

measurement procedures adapted to the wave propagation mo<strong>de</strong>ls. The validation will first<br />

be performed based on tank experiments (laboratory scale), before being applied to data<br />

from sea experiments (real-life). Ground truth will be obtained using conventional<br />

equipment and improved geophysical and geotechnical instruments like high resolution<br />

seismics and a geotechnical module.<br />

6. Data analysis will be performed in or<strong>de</strong>r to investigate, in <strong>de</strong>tail, the functional relations<br />

between the estimated acoustical parameters and sedimentological parameters obtained by<br />

ground truth in the sea experiments or from tank experiments, where the simulated sea bed<br />

can be ma<strong>de</strong> composed of calibrated sediments.<br />

The data obtained, during the sea experiments, will be compiled in a GIS (Geographical<br />

Information System). The surveys, conducted in selected representative test areas, will,<br />

therefore, lead to the constitution of a well controlled data base on bottom characteristics. This<br />

data base will be available on a CD-ROM and the small test areas may be used as benchmark<br />

for future instrument calibration.<br />

PROJECT METHODOLOGY<br />

In this project, the estimation problem is formulated in the framework of system i<strong>de</strong>ntification.<br />

The noise on input as well as output data will be taken into account, since, besi<strong>de</strong> direct<br />

inversion schemes, a Maximum Likelihood approach will be used. This approach allows also<br />

the incorporation of the calibration procedure, which is a necessary step, but which has been<br />

omitted in various previous studies, as well as the mo<strong>de</strong>l validation, since mo<strong>de</strong>l errors can be<br />

<strong>de</strong>tected and corrected easily as well.<br />

A key issue of this project requires the use of a parametric array. Although the principles of<br />

operation of this type of sonar have been known for many years, the implementation of a<br />

system for sea surveys during rough surface conditions, for example sea-state 5-6. In particular,<br />

automatic beam stabilisation remains an important problem that will be addressed in <strong>de</strong>tail in<br />

this project, so that the array can be programmed to transmit vertically downwards, through a<br />

repeated range of angles or at some preferential angle irrespective of the towed fish pitch.<br />

In this project, it is aimed to <strong>de</strong>monstrate that the i<strong>de</strong>ntification of sediment parameters can be<br />

performed using un<strong>de</strong>rwater acoustics, because the i<strong>de</strong>ntification of sediment parameters fits<br />

into a global system i<strong>de</strong>ntification approach. First acoustic parameters are estimated using<br />

robust estimators and then, using tank experiments and extensive ground truthing, functional<br />

relations between sedimentological and acoustic are inferred.<br />

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