Bathymetry in front of St Mark’s Square, Venice.
Natural salt march channel near Scanello, imaged in high resolution bathymetry and co-registered side scan data using Kongsberg GeoAcoustics GeoSwath Plus Compact. The bathymetry shows coverage from the waterline down to maximum of 7 m depth which was achieved with only two passes in the 80 m wide channel.
Salt marshes in the Venetian Lagoon with the island of Burano.
KONGSBERG GeoSwath Plus COMPACT multibeam echosounder chosen to gather data up to the waterline with a coverage of up to 12 times the water depth in shallow water environment.
Kongsberg GeoAcoustics was recently invited by the The Venice Institute of Marine Science (ISMAR-CNR) to demonstrate their GeoSwath Plus technology by gathering high resolution bathymetry data for
monitoring changes in the Venetian Lagoon.
The Venice Institute of Marine Science (ISMAR-CNR) is engaged in research and monitoring projects of the lagoon. This is the world’s best known estuarine lagoon, which does not only have historical
importance for sheltering the City of Venice but is a fascinating ever changing environment with only 8% covered by land, 12% by open water and the remaining 80% by mud flats, tidal shallows and salt
marshes. This geographical setting, hosting complex ecosystems, is influenced by tidal cycles entering through three sea inlets and freshwater and sediment supplied by river influx.
Monitoring of changes to the environment is becoming ever more important with changing sea levels and as the human impact increases. The MOSE flood protection project enables the closing of the sea
inlets and dredging activities.
The GeoSwath Plus COMPACT effectively covers large, very shallow water areas providing highly repeatable data to allow monitoring of even the smallest changes through time. Kongsberg GeoAcoustics
GeoSwath Plus Compact multibeam echosounder was chosen due to its capabilities to gather data up to the waterline with a coverage of up to 12 times the water depth in shallow water environment. Repeat
surveys were carried out and showed to be consistent albeit the difficult hydrological conditions with large tidal currents and fresh water mixing, leading to high temporal and lateral sound speed
variations. In addition the system offers true co-registered and geo-referenced side scan data which can be used for seabed classification and textural mapping.