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Case Study

Using Multibeam Technology to Detect Seabed Changes In Dynamic Environments on the West Coast of Scotland

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Published

Introduction

In late 2020, NORBIT partnered with the Scottish Association for Marine Science (SAMS) to study the evolution of the seabed off the west coast of Scotland.

A survey was performed using the NORBIT iWBMSh integrated multibeam survey system, mounted on a vessel of opportunity. The survey was performed over the course of 2 days.

Two areas were mapped:

  • Falls of Lora (a tidal rapid)
  • Wreck of the SS Breda, sunk in 1942 in Ardmucknish Bay.

Data was acquired with NORBIT DCT and processed using Teledyne CARIS. The data was fed into signal analysis models and compared with previous data to quantify sediment movements.

Map of Scotland, along with logos for NORBIT and Scottish Association for Marine Science (SAMS)
NORBIT partnered with the Scottish Association for Marine Science (SAMS) to study the evolution of the seabed off the west coast of Scotland.

Local History

Situated on the west coast of Scotland, the Falls of Lora is a tidal rapid at the mouth of Loch Etive, approximately 6 miles from Oban. It is popular with divers, kayakers and tourists.

The surrounding area contains a number of well-known ship wrecks which have become popular diving sites. Most of these wrecks sunk during the early 20th century.

NORBIT surveyed the wreck of the SS Breda, a Dutch cargo-passenger ship that was bombed and sunk during World War II. The wreck remains largely intact on the seabed.

Ardmucknish Bay, Argyll and Bute, The town of Oban and SS Breda Cargo Ship.
The SS Breda Cargo Ship, Ardmucknish Bay, Argyll and Bute, and The town of Oban.

Supplied NORBIT iWBMSh Multibeam Echosounder

NORBIT iWBMSh benefits:

  • Frequency agile 200-700kHz.
  • 0.5° x 0.5°beam width resolution at 700kHz.
  • Up to 210°swath width (single head) as standard.
  • HD beamformer providing 512 beams per ping.
  • High performance integrated GNSS/INS system.
  • Integrated sound velocity probe.
  • Small form factor and low power consumption.
  • Designed for rapid mobilization on any platform.
  • Bathymetry and various backscatter and water column data as standard deliverables.
  • Optional integrated LiDAR.
iWBMSh entire system shown to fi in 1 pelicase.
The entire system fits in 1 pelicase.

Installation and Data Collection

The NORBIT iWBMSh was installed on an over-the-side pole mount and configured for operation in less than 1 hour.

  • Line planning and data acquisition was performed on a tablet device using NORBIT’s Data Collection Tool (DCT), a simple to use web-based interface that requires minimal setup (no complex project setups, offsets or geodetic configurations required.)
  • DCT outputs the complete sonar and navigation solution to the well-known s7k data format, which is fully supported by all hydrographic processing software packages.
Survey set up

Results

Bathymetry data

Bathymetry data (gridded to 0.25m) overlaid on aerial imagery.
Bathymetry data (gridded to 0.25m) overlaid on aerial imagery.
Bathymetry data gridded to 0.25m.
Bathymetry Data
The high resolution bathymetry data was processed using Teledyne CARIS and used by scientists to generate the slope rasters pictured (Credit: SAMS).

Falls of Lora Tide Flow

This image shows the direction of ebb flow and flood flow overlayed on bathymetry data.
This image shows the direction of ebb flow and flood flow overlayed on bathymetry data (Credit: SAMS)

Backscatter Data

Bathymetry and backscatter data were collected simultaneously. NORBIT’s automated signal gain settings ensure optimal quality for both data types without compromise.

Bathymetry data gridded to 0.25m resolution. The depth range is 5-30 meters.
Bathymetry data gridded to 0.25m resolution. The depth range is 5-30 meters.
Corresponding backscatter mosaic generated from Snippets data, which provides information about seabed composition.
Corresponding backscatter mosaic generated from Snippets data, which provides information about seabed composition.

Modelling Change in Seabed Topography

Modelling Change in Seabed Topography
Comparing collected data with previous surveys from 2014 allowed scientists to model sediment movements (Credit: SAMS)

Sediment Displacement

This image shows the magnitude and direction of sediment displacement in the Falls of Lora. The length of the arrows represent the magnitude of displacement (Credit: SAMS)

Survey of the SS Breda Ship Wreck

The SS Breda was a cargo ship, 123m in length, which sank during World War II. It rests on the seabed at approximately 26m depth. The above image shows raw point cloud data collected from multiple passes over the wreck.

Point Claud data of the Breda ship wreck
Point Claud data of the Breda ship wreck

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