analytic and experimental results of spatial correlations of vector intensity sensors
DESCRIPTION
Analytic and Experimental Results of Spatial Correlations of Vector Intensity Sensors. Nathan K. Naluai Graduate Program in Acoustics Pennsylvania State University University Park, PA 16802 [email protected]. “Diffuse Field” Model of Isotropic Noise. - PowerPoint PPT PresentationTRANSCRIPT
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
Analytic and Experimental Results of Spatial Correlations of
Vector Intensity Sensors
Nathan K. NaluaiGraduate Program in AcousticsPennsylvania State University
University Park, PA [email protected]
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
“Diffuse Field” Model of Isotropic Noise
• Generally assumes sound coming from all directions
• One model definition (Jacobsen)– Sound field in unbounded medium– Generated by distant, uncorrelated sources– Sources uniformly distributed over all directions– Field would be homogeneous and isotropic– Time-averaged intensity is zero at all positions
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
kij
θi
φj
ux(rb ,t)
uz(ra ,t)
x
y
z
p(0,t)
Coordinate System Orientation
tutprR azpu ,,0E),(||
r
Notation conventions:
tutprR bzpu ,,0E),( r
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
Analytic Solutions for Spatial Correlationsof Separated Sensors in Isotropic Noise
kd
kddpp
sin
2
cossin3
|| kd
kdkdkddpu
3
2 sin2cos2sin3
|| kd
kdkdkdkdkdduu
3
cossin3
kd
kdkdkdduu
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
Instantaneous Intensity:
The correlation between spatially separated intensity sensors is:
Intensity Correlation Derivations
ttpt ,,),( rurrI
2211
2211
21
E
,,,,E
),(),(E),(
upup
ttpttp
ttrRII
rurrur
rIrI
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
For four Gaussian random variables [Bendat & Piersol]:
Can re-write the intensity correlation expression as
Intensity Correlation Derivations
xywzxzwyyzwxwxyz EEEEEEE
122121212211 EEEEEE),( upupuuppupuprRII
0EE
)(
)cos()()sin(
2limE
2211
2
2
011
upup
kr
krkrkr
c
Aup
r
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
Analytic Expressions for Spatial Correlationsof Intensity Sensors in Isotropic Noise
yxII IIdyx
where,0
4
2 cossinsin3
kd
kdkdkdkddII
4
22 sincos2sin23
|| kd
kdkdkdkdkddII
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
Correlations for Separated Sensors in Isotropic Noise
0 0.5 1 1.5-1
-0.5
0
0.5
1
Cor
rela
tion
Coe
ffic
ient
Spacing (in wavelengths, λ)
uu
||pu
pp
||uu
0 0.5 1 1.5-1
-0.5
0
0.5
1
Spacing (in wavelengths, λ)
Cor
rela
tion
Coe
ffic
ient
II
||IIpp
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
N4
N7
N10
Computational Experiment Design/Layout
• Computational Simulation in MATLAB environment
• Source distribution determined by variable M, (no. of sources about “equator”)
• Each source generating noise (0-6.4kHz band)
• Signals oversampled to allow for 1mm separation resolution
• Assumptions– Plane wave superposition– Sensor separation: 7cm– Air-like medium (c, ρ)
r1
r2
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
0 1 2 3 4 5 6 7 80
0.2
0.4
0.6
0.8
1
Pressure-Pressure Spatial Correlations
ρ pp2
kd
SimulationTheory
Input Parameters for Computational Experiment
• Where S can be considered the number of sample “locations” in field.
• Resulting curve is the average over those locations
51M
Hz12800sf
256FFTN
64avgN
10S
m07.0d dd xyxy ,, 22
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
Equal Amplitude Distribution (Ideal Case)
0 1 2 3 4 5 6 7 80
0.2
0.4
0.6
0.8
1
xy2
kd
Simulation
Theory
2||pu
2uu
2||uu
2pp
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
Equal Amplitude Distribution (Ideal Case)
0 0.5 1 1.5 2 2.5 3 3.5 40
0.2
0.4
0.6
0.8
1
kd
Simulation
Theory
xy2 2
II
2||II
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
Random Amplitude Source Weighting
0 1 2 3 4 5 6 7 80
0.5
1
kd
Random Amplit.TheoryCOS Weighting2
||pu
0 1 2 3 4 5 6 7 80
0.5
1
kd
Random Amplit.TheoryCOS Weighting
2
||uu
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
Effect of Inter-channel Phase Offsets on Correlation
0 0.5 1 1.5 2 2.5 3 3.5 400.10.20.30.40.50.6
kd
TheoryMismatched
2
||pu
0 0.5 1 1.5 2 2.5 3 3.5 400.10.20.30.40.50.6
kd
TheoryMismatched
2
||pu
Random Phase held fixed over averaging period
Phase shift applied on every 3rd average
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
Physical Correlation Measurements
• Reverberant Acoustic Test Tank (ASB-PSU)
• Two Lubell LL-9162 sources (uncorrelated noise)– Low freq. rolloff at 1-kHz
• pa-probe (McConnell)– Sensitivity axes aligned
• Outputs recorded at four separate locations in tank.– 64 avgs at each location
5.5m
8.5m
6.1 m
0.197 m
to Amp (R-Ch)
to Amp (L-Ch)
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
0 1 2 3 4 5 6 7 80
0.5
1
kd
TheorySimulationExperimental
0 1 2 3 4 5 6 7 80
0.5
1
kd
TheorySimulationExperimental
Physical Correlation Measurements
2pp
2
||pu
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
0 1 2 3 4 5 6 7 80
0.5
1
kd
TheorySimulationExperimental
0 1 2 3 4 5 6 7 80
0.5
1
kd
TheorySimulationExperimental
Physical Correlation Measurements
2
uu
2
||uu
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
0 1 2 3 4 5 6 7 80
0.5
1
kd
TheorySimulationExperimental
0 1 2 3 4 5 6 7 80
0.5
1
kd
TheorySimulationExperimental
Physical Correlation Measurements
2
||II
2
II
Pacific Rim Underwater Acoustics Conf.
Vancouver, BC, Canada
03-05 Oct 2007
Naluai – NAVAIRAcoustics SystemsPatuxent River, MD 20670
Summary
• Analytical solutions for spatially separated Intensity measurements have been derived and verified experimentally
• Constant phase offsets have no effect on the agreement between the coherence and the theoretical predictions
• Intensity measurements demonstrate shorter correlation lengths than the component measures
• Suggest that intensity processing of vector sensor arrays may be less susceptible to ambient noise contamination than traditional pressure hydrophone array.
• Examine performance of intensity vector sensor arrays– Possible gains in directivity