Until the late 70's bathymetry data of the oceans were commonly acquired by means of single beam echo sounders, along discontinue track lines with an uneven spatial distribution. More recently, the MultiBeam Echo Sounder (MBES) technology was made available to the academic research. These systems provide a full sea floor search and a high resolution imaging of the seafloor. The MBES systems provide depth values along a swath instead of a single point value by means of acoustic pulses arrays. There are several MBES models characterizing by different technical equipments in terms of frequencies, beam number and spacing. MBES systems are used in archaeological and engineering fields, where high resolution data in small areas are required, as well as in deep seafloor mapping aimed at large scale structures detection. MBES may provide also grain size information besides bathymetric data, recording the backscatter values that result from the interaction of acoustic pulses with the seafloor. This tool is particularly important to characterize the distribution of some features on the seafloor such as submarine landslides and other elements that may play an important role in the assessment of the geological hazard along the coasts. Actually some research groups are improving the backscatter analysis to generate a semi-automatic seabed classification method. This contribution will provide an overview of some recent examples studied within the framework of the CNR research projects.

Seafloor Exploration Using the Multibeam Echo Sounder Technology: Some Examples.

Tonielli R;Barra M;Di Martino G;Foglini Federica;Innangi S;Mercorella Alessandra;Rovere Marzia
2011

Abstract

Until the late 70's bathymetry data of the oceans were commonly acquired by means of single beam echo sounders, along discontinue track lines with an uneven spatial distribution. More recently, the MultiBeam Echo Sounder (MBES) technology was made available to the academic research. These systems provide a full sea floor search and a high resolution imaging of the seafloor. The MBES systems provide depth values along a swath instead of a single point value by means of acoustic pulses arrays. There are several MBES models characterizing by different technical equipments in terms of frequencies, beam number and spacing. MBES systems are used in archaeological and engineering fields, where high resolution data in small areas are required, as well as in deep seafloor mapping aimed at large scale structures detection. MBES may provide also grain size information besides bathymetric data, recording the backscatter values that result from the interaction of acoustic pulses with the seafloor. This tool is particularly important to characterize the distribution of some features on the seafloor such as submarine landslides and other elements that may play an important role in the assessment of the geological hazard along the coasts. Actually some research groups are improving the backscatter analysis to generate a semi-automatic seabed classification method. This contribution will provide an overview of some recent examples studied within the framework of the CNR research projects.
2011
Istituto per l'Ambiente Marino Costiero - IAMC - Sede Napoli
Istituto di Scienze Marine - ISMAR
Dipartimento Terra Ambiente
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/173894
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