side scan theory and operation
DESCRIPTION
Sidescan Survey Overview A sidescan sonar can be used for a wide variety of survey operations. Search and recovery Geological Identification Pre / Post dredge surveys Target verification and location It is also a useful tool for correlating and verifying bathymetric data Shipwreck with shadow (in white) Sidescan data showing sediment changeTRANSCRIPT
SIDE SCAN Theory and Operation Sidescan Survey Overview
A sidescan sonar can be used for a wide variety of survey
operations. Search and recovery Geological Identification Pre /
Post dredge surveys Target verification and location It is also a
useful tool for correlating and verifying bathymetric data
Shipwreck with shadow (in white) Sidescan data showing sediment
change What you find with a Sidescan Record
Shadow Water Column How the sonar sees the object: Water Column
-Provides information about towfish height. Target-features off the
seafloor will produce a shadow. Bottom sediment -Signal will differ
based upon return angle onincident and seabed absorption. 3 What
happens at Nadir region
There is no White Area under the fish. The secondary lobes ensonify
the nadir. However: The incidence angle makes this area not really
useful The importance of the Shadow
As the towfish gets closer to the seafloor, the shadow size will
increase The importance of the Shadow
The shadow could be more helpful that the shape of the object. The
importance of the Shadow
Same object with his shadow. Take a look at this image. What is it?
The Shadow Effect Imaging the seafloor from above will cast a
shadow of the object.Sometimes the shadow can give you more
information that just the data on the seafloor What you find with a
Sidescan Record
Received Signal T0 (Ping) T2 T1 (First return) T2 (range) Signal VS
Time Time T2 Time T1 T0 T1 T2 What you find with a Sidescan Record
Understand the Amplitude VS Time Signal
The waterfall view is the amplitude coded in color level. Detection
of first return for bottom track Sidescan Theory Sonar system
components
The sonar system (towfish) has a transmit and receive component
takingthe signal (digital) and sending to the acquisition computer
for display andstorage. The echo distance is determined by time,
similar to other sonar systems Display Transmitter / receiver
Sidescan Signal Distance = time (round trip) x Sound Velocity 2
Note the use of Sound Velocity. It is needed to compute the
distance.The default of 1500 m/s will give an error Bottom echo
Time of pulse What is a Sidescan Resolution.
Across Track Resolution depending of the frequency pulse. Along
Track Resolution depending of the aperture Horizontal Aperture
(0.25 to 0.8). The Along Track Resolutionis not linear along the
swath. The Across Track Resolution is the same along the swath The
resolution used to qualified a sidescan is the Along Track
Resolution Across track range resolutionWhy sonars work better at
the outer ranges
Distinguishing two independent objects can be referred to asthe
sonar resolution. If two objects are too close, they will appear as
one on the sidescanrecord. Getting these objects further apart will
show them asindependent objects. How close can they be? Half the
pulse length. Example: A 500khz system has a pulse length of 1 cm.
In practice, that wont be seen, and cannot distinguish an object
thatclose.We can approach this value further away from nadir. The
footprint of sonar (arriving energy) is longer near nadir due to
theangle of incident. Conversely, the further away, the more the
bottomfootprint approaches the pulse length. At the very far end of
the signal, the best resolution would be obtained First return
Along track resolutionwhy objects in the far field cannot be
distinguished
The resolution in the along track direction is dependent on the
sonar Horizontal beam width. The image below represents what
happens when targets in the far field are inside the angular
resolution of the sonar. They become indistinguishable and look as
a single object At the near field, these objects can be
distinguished. Horizontal beam width First return Image quality vs.
location
Targets is these areas might be missed or cannotbe measured
accurately Ideal location for targets The nadir return is degrading
causing by the incidence. The sidescan image typically degrades at
the far end of the swath When running survey operations, the best
image will be in the center of the swath Survey Speed The survey
speed has to take in account the limitation of the sidescan. Speed
< Max Speed Coverage 100 % Speed > Max Speed Coverage <
100 % Height of Contact (H) = L * A / R
Measuring a contact: Three points along the image are needed
altitude (A) , shadow length (L), total distance (R) Each target
will have a shadow; use the tools in Sidescan Survey or HYSCANto
measure contact Height of Contact (H) = L * A / R 20 Sidescan
operation Survey planning: 100% and 200% coverage
100% coverage: At 100 meter range scale, line spacing would be set
for 160 meters. This provides a 20 meter off-track error while
surveying. 200% coverage: This survey plan ensures that the bottom
is covered twice by the Sidescan, covering the nadir region with
the second line pass Line spacing 160 meters Line spacing 80 meters
Swath width 200m Note the overall swath width is twice the range
scale 22 Collecting sonar data is different than echosounder
data
Survey operations will change when running a sidescan sonar Vessel
speed (slow is best 4 to 5 kts is typical) Vessel handling (you
cant stop when towing a sidescan) No turns during collection Line
spacing is fixed (unlike multibeam collection) Nadir area is
obscured. Visual display of waterfall gives immediate results
(sometimes that is good enough for folks) Sidescan files are large,
more storage needed But. Even with all that, sidescan by itself or
part of a surveyoperation provides very good results. Sidescan
positioning Getting the position of the towfish is
critical.Seeingan object but not knowing where it is, will not be
veryuseful. Cable out (layback) Acoustic positioning system (USBL)
ROV (inertial systems on board) Ship mounted (uses on board GPS
with offsets) Which one is best?Dependent of survey operationsand
water depth. How to do a self check of object detection
During survey operations, set the range scale of thesonar to your
operating range. Run past a know object. A buoy block or sand waves
willwork Ensure that you can see the entire swath. If you
cant,shorten the range scale until you do. If you dont see a known
object, chances are you wont find the unknown object. Sidescan
Deployment Towfish deployment Sidescan sonar transducers can be
fixed to a vessel for shallowwater deployment or towed when
operating in deeper water Operating a fixed mount (on survey
vessel)
RANGE SCALE Optimum Fish Height 50 meter 4 10 meters 75 meter 6 15
meters 100 meter 8 20 meters Too shallow, high angle A rule of
thumb to get the best results: Use 8% to 20% of range scale for
fish height Why 8 20% or range scale? This altitude will provide
the best angle of incidence (reflection of an object) for a sonar
return. When using a fixed mounted sidescan the image may degrade
in water depths greater then 40 meters. The angle is too steep Too
high, high angle 27 TOWED Sidescan Operations
TowFish It is critical that the towfish is close to the seafloor.
Remember the 8-20% rule TOWED Without USBL tracking, the navigation
of the fish is an estimation.Using a layback driver based on the
cable out, the fish position is not precise, especially on turns
Hull Mounted For a hull mount, you know the exact position of the
side scan. This is typically used for shallow water applications.
Angle of incident becomes too sharp when working in deep water when
hull mounted Hull Mounted For a hull mount, you must be careful
that the side scan is aligned with the vessel keel.Otherwise, you
must make an adjustment to the yaw offset for the sidescan.