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UNDER WATER
COMMUNICATION
INTRODUCTION
Technique of sending and receiving message below water.
Most commonly employed using hydrophones.
Difficult due to factors like multi-path propagation, time
variations of the channel, small available bandwidth and
strong signal attenuation.
Underwater communication uses acoustic waves instead
of electromagnetic waves.
DEFICIENCY IN CURRENT COMMUNICATION
Future ocean environment will be increasingly
complicated.
Radio waves propagate under water at extremely low
frequencies (30Hz-300Hz) & require large antennae and
high transmission power.
Optical waves do not suffer much attenuation but are
affected by scattering.
Acoustic waves are the single best solution for
communicating Under water.
ABOUT Underwater Acoustics is the study of propagation of sound
in water & interaction of mechanical waves that constitute
with water & its boundaries.
Typical frequencies associated with Underwater Acoustics
are 10Hz to 1MHz
The propagation of sound in the ocean at frequencies lower
than 10 Hz is not possible.
Frequencies above 1 MHz are rarely used because they are
absorbed very quickly.
Underwater Acoustics is also known as
HYDROACOUSTICS.
PEOPLE WHO THOUGHT IT IS POSSIBLE
"If you cause your ship to stop and place the
head of a long tube in the water and place the
outer extremity to your ear, you will hear ships
at a great distance from you.“
In 1687 Isaac Newton wrote
his Mathematical Principles of Natural
Philosophy which included the first
mathematical treatment of sound.
THE MAIN INITIATIVE TO DEVELOP THE
TECHNOLOGY
BASIC ACOUSTIC COMMUNICATION MODEL
ACOUSTIC MODEM
Converts digital data into
special underwater sound
signals.
These signals are then
received by a second
acoustic modem and
converted back into
digital data.
Oceanographers use acoustics to
control underwater instruments
and acquire the data that they
collect remotely.
This technology can also be used
to control small, unmanned
submarines, called Autonomous
Undersea Vehicles (AUV's), and
get data back from them in real-
time.
HYDROPHONE
• Hydrophones are designed to be used underwater for
recording or listening to underwater sound.
• Hydrophones are based on a piezoelectric transducer that
generates electricity when subjected to a pressure change
• Transducers can convert a sound signal into an electrical
signal since sound is a pressure wave.
• From late in World War I until the introduction of
active sonar, hydrophones were the sole method for
submarines to detect targets while submerged
PIEZOELECTRIC TRANSDUCER• Piezoelectricity means electricity resulting from pressure.
• It is a device that transforms one type of energy to another by taking advantage
of the piezoelectric properties of certain crystals or other materials.
• Piezoelectric material is subjected to stress or force, it
generates an electrical potential or voltage proportional
to the magnitude of the force.
• This type of transducer ideal as a converter of
mechanical energy or force into electric potential.
A piezoelectric disk generates
a voltage when deformed
DIRECTIONAL HYDROPHONESFocused Transducers
• Uses a single transducer element with a dish or conical-shaped
sound reflector to focus the signals
• Can be produced from a low-cost omnidirectional type
• Must be used while stationary, as the reflector impedes its
movement through water
Array of Hydrophones
• Multiple hydrophones can be arranged in an array
• It will add the signals from the desired direction while subtracting
signals from other directions.
• Hydrophones are arranged in a "line array“, but may be in two- or
three-dimensional arrangements
Array of Hydrophones
Sound is transmitted by the ship and reflected off the submerged submarine.
The reflected sound reaches hydrophone A first, then hydrophone B, and
finally hydrophone C. The time-of-arrival-difference between the
hydrophones in the array is used to determine the direction to the submarine.
SOSUS HYDROPHONES
• The United States Navy's initial intent for the
system was for tracking Soviet submarines,
which had to pass through the gap to attack
targets further west.
• Sound Surveillance System, is a chain of underwater
listening posts located around the world in places such as
the Atlantic Ocean near Greenland, Iceland and the United
Kingdom — the GIUK gap, and at various locations in
the Pacific Ocean.
• Using the sounds made by the seismic event, scientists can tell if the event
is an earthquake or a volcanic eruption.
• NOAA uses the Navy's Sound Surveillance System (SOSUS) and
additional hydrophones to monitor the North Pacific Ocean and the North
Atlantic Ocean for seismic events.
• Hydrophones located around the Pacific Ocean monitor the ocean for
sounds of seismic events. The sounds made by a seismic event are also
used to accurately locate the event.
• Sonar (sound navigation and ranging) is a technology that
uses acoustical waves to sense the location of objects in the
ocean.
• The simplest sonar devices send out a sound pulse from
a transducer, and then precisely measure the time it takes for
the sound pulses to be reflected back to the transducer.
• The distance to an object can be calculated using this time
difference and the speed of sound in the water (approximately
1,500 meters per second).
SONAR
More sophisticated sonar systems can provide additional
direction and range information. Sonar was developed
during World War I as an aid in finding both submarines
and icebergs.
SONAR
Autonomous vehicles
working under the ice
can be controlled and
their data can be
transmitted to a
topside station using
underwater acoustic
links
Autonomous Underwater
Vehicle
ACOUSTIC LINKS ARE USED TO CONTROL UNDERWATER INSTRUMENTS AND
ACQUIRE THE DATA REMOTELY
APPLICATIONS OF AUV’S & OTHER DEVICES USING
ACOUSTIC SIGNALS
U.S. National Oceanic and
Atmospheric
Administration (NOAA)
Deep-ocean Assessment
and Reporting of
Tsunamis (DART)
program has installed
bottom pressure sensors
near regions with a
history of tsunami
generation, to measure
waves as they spread.
CLOSE-UP OF A DART II SURFACE BUOY
• An acoustic link transmits data from
the bottom pressure sensor to the
surface buoy.
• Then satellite links relay the data to
NOAA tsunami warning centres.
• Real-time data about tsunamis is given
to NOAA forecaster that could
potentially impact coastal areas.
Underwater data links can be
combined with satellite data links to
provide data in real-time from
instruments on the seafloor to
scientists ashore.
The AUV Designed By PIBHMC
This AUV has Been
Constructed by The U.S
Navy to Detect
underwater proximity
mines and approaching
torpedo's.
BlueFin -21 Also known as “Mine-
Hunter”
DETECTING UNDER WATER OBJECTS
• A robot crawler carries a modem, a
camera, and a digital signal-
processing unit.
• Traversing the seafloor, searches for
an object.
• When object found, sends an acoustic
signal to a ship or shore based station
• Can then be commanded to take a
still frame photo, compress it and
transfer the image to an acoustic
signal that is sent back to the
investigator
There is an increasing
interest in USWN
technologies and their
potential
applications. However,
there are several open
issues to solve in order to
provide an
efficient and reliable data
transport to the
applications.