Light is absorbed over very short distances in the water environment.
In working underwater, the lack of long range vision is a major limiting
factor. In the early days of underwater work, performed manually, limited
vision was not as significant because the
diver
could not move from one place to another very quickly. As robotics and
instrumental intervention arrived at the worksite, the need to extend
our vision became more vital. This becomes even more important because
with our remote presence we can move more quickly from one place to another.
To meet the demands of "seeing" further underwater, engineers have turned
away from the visible light spectrum and to another form of transmittable
energy underwater: sound. Sound is also attenuated in the dense water
environment, but not over as short a distance as light. Although the resolution
of acoustic imaging does not approach optics, it does provide a remarkable
extension of our vision, as the images of the aircraft and collapsed bridge
in the figures on this page show.
Those
working underwater, including oceanographers, marine geologists, and ROV
Pilots now depend heavily on sound energy to transform the things we cannot
see underwater into numbers, graphs, and pictures. The ROV pilot in particular
requires that the imaging sonar provide him with accurate and quickly
updated images. The instruments that transmit and receive these sound
pulses have become sophisticated and more accurate in the past few decades.
Underwater, sound transmission is limited. This is most notable in useable
ranges. High-frequency sound energy is greatly reduced by seawater. Low-frequency
sound energy is reduced at a much lesser rate. For instance, a sound pulse
of 50 Hertz can be transmitted many thousands of kilometers in the ocean,
but a pulse of 300 kHz, a common imaging sonar frequency, can be transmitted
less than 3,281 ft (1,000 m).
As
applied to underwater vehicles, sonar systems in use today include mapping
and collision avoidance types. Side scan sonar transducers can be mounted
on the sides of a vehicle, such as the one shown to the right, to provide
a "map" of the seafloor. An advantage of side looking sonar on an ROV
is that a long-range image can be provided out to the side of the vehicle's
track. One disadvantage of side scan on a vehicle is that, while vehicles
can be flown at low altitude along the seafloor, the side scan requires
some amount of altitude in order to gain the necessary range. This problem
is not new to the combination of long range acoustic and short-range optical
imaging underwater. It is not always possible to fully utilize both simultaneously.
Almost
every medium and large vehicle does utilize, however, a forward-looking
sonar for navigation, collision avoidance and target delineation. These
sonars are most often rotary sonars, commonly known as scanning sonar,
such as the MS 900 scanning sonar by Kongsberg Simrad shown to the left.
They consist of a transducer head, which rotates and is mounted on an
electronics bottle. Common frequencies in these units range from about
300 kHz to 600 kHz and above. Again, the tradeoff between the higher resolution
of the high frequency and the longer range of the low frequency comes
into play. A vehicle may have more than one rotary scan sonar mounted
on it. Two frequencies on two sonar heads working simultaneously, for
example, will give a pilot a rapid informational update for targets and
terrain on both high resolution and long range.
The
fact that towed side scan sonars "fly" high above their targets
gives them their ability to observe objects, often through the "shadows"
cast by the sonar beam. This is shown graphically in the figure of the
ship image to the right.
Today, color monitors and digital processing enhance the sonar operators
ability to identify targets.