LBL (Long BaseLine) underwater positioning is an acoustic positioning technique that provides high precision underwater positioning and navigation.
It involves the use of acoustic transponders placed on the seabed, typically hundreds or thousands of meters apart (hence “Long Baseline”).
Core principles of LBL
Ranging and positioning: LBL systems determine the relative position of a target, such as a remotely operated vehicle (ROV), by sending and receiving acoustic signals to transponders with known positions (relative to each other) on the seabed. The system calculates the distance to each transponder by measuring how long the signals take to reach them. Using these distances, the system computes the target’s location, much like a GPS system.
Note: The final positioning accuracy is dependent on several factors that begin with the GPS signals received at the vessel’s antennae. Antennae must be located so that there are minimal obstructions from vessel masts and superstructure, which will provide a clear line of sight to the GNSS satellites. Accurate offsets from the antennae to USBL transceiver and on the ROV are then required so that the best possible “real world” coordinates of the ROV’s common reference point (CRP) can be determined.
Is LBL depth independent?
A key benefit of LBL is that its precision (how consistently the system can reproduce the same position measurement) is independent of water depth.
This is because the LBL array is in a fixed position at the seabed. Distance measurements relative to these fixed points are unaffected by water depth variations.
It is used when the highest level of subsea positioning accuracy (how close the measured position is to the targets true position) is required.
How many ranges are required for LBL positioning?
Theoretically, LBL requires a minimum of three ranges plus knowledge of depth to calculate a unique position. However, in real-world applications, at least four, and ideally five or more ranges, are typically necessary to ensure redundancy, which helps to detect and reject erroneous readings (outliers) and compute a high integrity position.
- Acoustic operation: The system interrogates the transponders acoustically, they respond, and the time of travel is measured. This is then used to calculate the distance and then relative position.
- Speed of sound (SV): The most critical part of this calculation is the speed of sound, or sound velocity (SV). Unlike radio signals, where the speed of light is constant, the speed of sound in water is variable.
Sound speed in water varies primarily due to changes in temperature, salinity and pressure (depth). Warmer temperature and higher salinity increase sound speed, while increasing pressure with depth also raises the speed. These factors vary spatially and with depth, causing sound speed to be variable in water.
If the SV used in the calculation is incorrect, all measurements will be wrong. Sound velocity sensors (like those found in Compatt transponders) are used to measure the SV directly from the environment.