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Transcript of Course and Learning Outcome(s) Course and Learning Outcome(s
Course and Learning Outcome(s)Course and Learning Outcome(s)
[CO1] Student is able to explain the concept of sound [ ] p punderwater, SONAR system, depth sounding, and bathymetric mapping.
[LO01] Explain generation of sound underwater, Sound Level, intensity unit acoustic wave properties pulse (length repetition)intensity, unit, acoustic wave properties, pulse (length, repetition), particle celerity, impedance.
[LO02] Explain propagation of sound underwater propagation [LO02] Explain propagation of sound underwater, propagation mechanism, Transmission Loss, role of water properties, active SONAR equation (NL/RL dominated).
Generation of soundGeneration of sound
S d h i ll d d di b i h Sounds are mechanically generated due to disturbance in the medium
Pressure differences
Disturbance in a medium is considered as pressureDisturbance in a medium is considered as pressure differences/gradient working at a unit area
It compresses medium particles to a side that will be followed byIt compresses medium particles to a side that will be followed by decompression in the other side
Sound or acoustic pressure (p)
E d N/ 2 P
Sound or acoustic pressure (p)
Expressed as N/m2 = Pap0
+p
p0
pp0+pp0–p p0
p = p – p0
compressiondilation
p p p0withp = pressure difference = disturbancep = instantaneous pressurep = instantaneous pressurep0 = hydrostatic pressure (pressure without disturbance)
Natural soundNatural sound
1 = no sound2 = ‘audible’ sound3 = hydrostatic pressure3 = hydrostatic pressure4 = sound pressure
Particle displacementParticle displacement
D d ( ) di l f di i l ( ) i Due to sound pressure (p), displacement of medium particle () is expressed as*:
= /2f
with = particle velocitywith = particle velocity
*medium produces specific vibration due to a given sound pressure and frequency
Sound speed and particle velocitySound speed and particle velocity
S d d ( ) i h l i f i f i Sound speed (c) is the celerity of propagation of acoustic wave through medium
Particle velocity () is motion of molecules in the medium due to Particle velocity () is motion of molecules in the medium due to sound generation and depends on the applied pressure (p) and medium density ():
p = c
with = 2f, then:
p = c2fp = c2f
Acoustic impedance (Z )Acoustic impedance (Za)
A di d ifi ib i (i i l di l A medium produces specific vibration (i.e. particle displacement, particle velocity) due to applied pressure at a given frequency.
Za relates p and
Sound or acoustics intensity (I)Sound or acoustics intensity (I)
S d i ( ) ki i ( ) Sound or acoustic power (P) working on a unit area (A)
PI
P is directly proportional to p2
AI
P is directly proportional to p
Note:
Sound Pressure Level (SPL)Sound Pressure Level (SPL)
SPL i l d S d L l ( ) SPL is also termed as Sound Level (L)
pref = 1Pa
2
2
10log10Lfp
p
refp
commonly written as just 20log(p) dB
Use of dBUse of dB
A i f i l l h Acoustic power ranges from a very tiny level to a very huge one Use of large numbers are impractical Instead of using power level, dB (deciBel) unit is usedg p , ( )
dB is a relative power of a given intensity with respect to a reference (in water p = 1Pa)reference (in water pref = 1Pa)
PropagationPropagation
P i Propagation Since the medium is elastic, the side experiencing compression balances it and transfers the compressing force to the other side p gand so on and sofort. Consecutive compression and dilation propagates energy to all directions.
Speed of propagation (c)The speed of acoustic wave propagation is mainly governed byThe speed of acoustic wave propagation is mainly governed by medium density.
P i d ( ) i h di i d b Propagation speed (c) in the medium is governed by
Medium density ()Medium density ()In practical sense, higher density of medium facilitate a more efficient transfer of energy
Elasticity modulus (E)This relates to the so-called medium compressibility
c = (E/)0.5c (E/)p = EV/V
Sound experiences lossSound experiences loss
S d i i l i h i i di f Sound intensity losses with increasing distance from sources Geometrical spreading and attenuation are the primary
mechanism of loss acoustic energy
ensonified
gy
e so edsurface20logR
source
increasing distance from source
20logR
SLincreasing distance from sourceR
Loss mechanismLoss mechanism
G i l di Geometrical spreadingAcoustic energy experiences loss since the energy is spread to all directions
AttenuationThrough out the medium, the propagated acoustic energy also g p p g gyexperiences loss. This is due to inter-particle collision and relaxation of molecules in the water that converts acoustic energy into other forms (e g heat)energy into other forms (e.g. heat)
Hydro-acoustic systemHydro-acoustic system
H d i li i i f d h h Hydro-acoustic system relies on transmission of sound through water
i.e. SONAR = SOund Navigation And Ranging active SONAR
Notes: Passive system = listening for soundPassive system listening for sound Active system = making sound and listening to the echo
SONAR equation SLSONAR equation
S
SL
Sensor Source Level (SL) Detection Threshold (DT)
Medium
DT DI
Medium Noise Level (NL) Transmission Loss (TL) Reverberation Level (RL) NLReverberation Level (RL)
Source Target Strength (TS)
TL NL
RL
TS
Reverberation and noiseReverberation and noise
Si l b d d if i i h h b k d d Signal can be detected if it is stronger than the background due to reverberation and noise
noise is due to wind, wave, biological activity, and shipping
reverberation is backcattered sound from source decayingreverberation is backcattered sound from source, decaying source’s replicate
SIGNAL > BACKGROUND
EL drops with increasing distance due to TL
Rr is range (R) when RL ELRL domination above NL
Rn is range (R) when NL ELNL domination above RL