Reson SeaBat 7125 ROV, Operator'S Manual

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ACTIVE SONAR USAGE
SeaBat 7125 ROV Operator‟s Manual
Page 95 May 30, 2011
Version 3
geometrical spreading exist everywhere in the underwater environment, they are
considered to be the most important loss mechanisms.
In the SeaBat system it is possible to compensate for loss caused by absorption and
geometrical spreading. In addition, the SeaBat system allows for changes in the speed
of sound, a parameter which is important in the beamforming process.
For instructions on how to adjust these settings, see
section 5.7.3 Ocean Settings .
6.5.1 Loss of Sound by Absorption
The amount of loss of sound through absorption in water depends on the water
conditions and the sound frequency. As sound moves through the water, the water
absorbs it by converting some of the acoustic energy to heat. The absorption loss is
proportional with the salinity of the water and the sound frequency: the higher the salinity
or frequency, the greater the loss (see
Figure 40 ). The figure also shows that an
increased temperature will increase the absorption loss.
The absorption loss value is part of the formula that the SeaBat system uses to calculate
the amount of gain to apply to the sonar return signal (see
section 6.2.4 above ).
If the exact absorption loss value is not known, a value of 110dB/km for salt water and
70dB/km for fresh water is recommended for 400kHz operation, and a value of 50dB/km
for salt water and 20dB/km for fresh water is recommended for 200kHz operation. For
instructions on how to adjust this setting, see
section 5.7.3.1 Change the Absorption
Loss Value (Absorption) .
Figure 40 provides a general reference for acoustic absorption at different frequencies
and salinity in three different temperature environments.