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ALEXANDRU – VLAD LAZAR 1, GHEORGHE – VIOREL UNGUREANU 1,2, ALEXANDRU – DAN IONESCU 1, ANDREI – DANIEL BALAHURA 1*, ROBERT LAZAR 1, ALEXANDRU MAGHER 1 1 SC Marine Research SRL 2 University of Bucharest *vlad.lazar@marine-research.ro
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Content 1. Introduction 2. Methods 3. Results 4. Conclusions
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1. Introduction Seabed mapping – great importance for marine management Acoustic Seabed Classification (ASC) - applications in marine geology and biology, environmental sciences, coastal engineering and fisheries Goal – discussing the use of interferometric sonars for ASC Geophysical methods – coverage, non- invazive Case study – 42 ha site offshore Mangalia
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2. Methods Interferometic sonar – Kongsberg GeoSwath Plus 250 Positioning and motion compesation – Applanix POS MV 320 Ground-truthing – grab samples and ROV Sediment type – laser grain size analysis
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Why interferometric sonar? Co-register bathymetry and side scan sonar data Millimeter depth resolution 240 ⁰ field of view Up to 12 times water depth coverage high productivity Integrated IMU and real time motion corrections
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Processing Bathymetry Side scan Amplitude Remove water column Range (Along-Across)Gain corrections Swath Swamp
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3. Results 250 m Bathymetry mapSide-scan mosaic
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Type 1 Rocks High rugosity Large bathymetry variations Strong backscatter Type 2 Limestone platform High rugosity Smaller bathymetry variations Strong backscatter
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Type 3 Soft sediments Low rugosity Small bathymetry variations Low backscatter Moderate rugosity Small bathymetry variations Medium backscatter Type 4 Covered limestone platform
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ROV inspection - Rocks Laser Grain-size analysis – fine sand
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Acoustic Seafloor Classification
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4. Conclusions Fast evolution of geophysical methods compact, more and better results Interferometers are a valuable tool for ASC Combined methods Easy to detect seafloor types Ground truthing and ROV images are very important for quality results
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Thank you! www.marine-research.com
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