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Uncertainty in Acoustic Mine Uncertainty in Acoustic Mine Detection due to Environmental Detection due to Environmental Variability Variability Peter C. Chu and LCDR Nick A. Vares Vares Peter C. Chu and LCDR Nick A. Naval Postgraduate


  1. Uncertainty in Acoustic Mine Uncertainty in Acoustic Mine Detection due to Environmental Detection due to Environmental Variability Variability Peter C. Chu and LCDR Nick A. Vares Vares Peter C. Chu and LCDR Nick A. Naval Postgraduate School Naval Postgraduate School Ruth E. Keenan Ruth E. Keenan Scientific Application International Scientific Application International Corporation Corporation Email: pcchu@nps.edu pcchu@nps.edu Email: http:// www.oc.nps.navy.mil/~ chu www.oc.nps.navy.mil/~ chu http:// Sponsored by the Naval Oceanographic Office Sponsored by the Naval Oceanographic Office

  2. Purpose Purpose � Determine the impact of bottom type � Determine the impact of bottom type and wind variations on bottom moored and wind variations on bottom moored mine detection mine detection � Determine the significance of � Determine the significance of transducer depth on bottom moored transducer depth on bottom moored mine detection mine detection

  3. Navy Relevance Navy Relevance � Littoral engagement � Littoral engagement � Mine warfare � Mine warfare � Diesel submarines � Diesel submarines � Unmanned Undersea Vehicles (UUVs) � Unmanned Undersea Vehicles (UUVs)

  4. CASS/GRAB CASS/GRAB � Comprehensive Acoustic Simulation � Comprehensive Acoustic Simulation System (CASS) System (CASS) � Gaussian Ray Bundle (GRAB) Eigenray � Gaussian Ray Bundle (GRAB) Eigenray model model � Navy standard model for active and � Navy standard model for active and passive range dependent acoustic passive range dependent acoustic propagation, reverberation and signal propagation, reverberation and signal excess excess � Frequency range 600Hz to 100 kHz Frequency range 600Hz to 100 kHz �

  5. CASS/GRAB Model Description CASS/GRAB Model Description � � The CASS model is the range The CASS model is the range CASS dependent improvement of the dependent improvement of the Comprehensive Acoustic Generic Sonar Model (GSM). Generic Sonar Model (GSM). System Simulation CASS performs signal excess CASS performs signal excess Propagation Model 1: FAME calculations. calculations. Propagation Model 2: GRAB � � The GRAB model is a subset of The GRAB model is a subset of Gaussian Ray Bundle OAML GRAB v1.0 the CASS model and its main the CASS model and its main Environmental Interpolations function is to compute Environmental Model Interpolations function is to compute Surface and Bottom Forward Loss Volume Attenuation eigenrays and propagation loss eigenrays and propagation loss Sound Speed Algorithms Call GRAB as inputs in the CASS signal as inputs in the CASS signal Propagation Model 3: COLOSSUS excess calculations. excess calculations. Propagation Model 4: AMOS equations Backscatter Models Reverberation Noise Models Signal to Noise Signal Excess Graphic Displays System Parameters (Beamforming)

  6. Comprehensive Acoustic Comprehensive Acoustic Simulation System/Guassian Simulation System/Guassian Ray Bundle (CASS/GRAB) Ray Bundle (CASS/GRAB) � In the GRAB model, the travel time, source angle, target � In the GRAB model, the travel time, source angle, target angle, and phase of the ray bundles are equal to those angle, and phase of the ray bundles are equal to those values for the classic ray path. values for the classic ray path. � The main difference between the GRAB model and a classic The main difference between the GRAB model and a classic � ray path is that the amplitude of the Gaussian ray bundles ray path is that the amplitude of the Gaussian ray bundles is global, affecting all depths to some degree whereas is global, affecting all depths to some degree whereas classic ray path amplitudes are local. GRAB calculates classic ray path amplitudes are local. GRAB calculates amplitude globally by distributing the amplitudes according amplitude globally by distributing the amplitudes according to the Gaussian equation to the Gaussian equation { } β Γ 2 [ ] ν ν 2 Ψ = − − σ , 0 exp 05 . ( ) / z z ν ν ν π σ 2 p r ν ν , r

  7. Mine Hunting Sonar Mine Hunting Sonar � Generic VHF forward looking � Generic VHF forward looking � CASS/GRAB input file for MIW with � CASS/GRAB input file for MIW with signal excess output signal excess output � Generic bottom moored mine � Generic bottom moored mine

  8. AN/SQQ- -32 Mine Hunting 32 Mine Hunting AN/SQQ Sonar System Sonar System � The CASS/GRAB � The CASS/GRAB Acoustic model input Acoustic model input file used in this study file used in this study simulates a VHF simulates a VHF forward looking sonar, forward looking sonar, similar to the Acoustic similar to the Acoustic Performance of the Performance of the AN/SQQ- -32. 32. AN/SQQ � The AN/SQQ � The AN/SQQ- -32 is the 32 is the key mine hunting key mine hunting component of the U.S. component of the U.S. Navy’ ’s Mine Hunting s Mine Hunting Navy and Countermeasure and Countermeasure ships. ships.

  9. Detection Sonar and Detection Sonar and Classification Sonar Assembly Classification Sonar Assembly

  10. Input Parameters Input Parameters � Bottom depth Bottom depth � Source level Source level � � � Target depth � Target depth � Pulse length � Pulse length � Transducer depth Transducer depth � Target strength/depth Target strength/depth � � � Wind speed � Transmitter tilt angle � Wind speed � Transmitter tilt angle � Bottom type grain size Bottom type grain size � Surface scattering Surface scattering � � index /reflection model index /reflection model � Frequency min/max Frequency min/max � Bottom scattering Bottom scattering � � /reflection model /reflection model � Self noise Self noise �

  11. Bottom Type Geoacoustic Geoacoustic Properties Properties Bottom Type

  12. Yellow Sea Yellow Sea Bottom Sediment Bottom Sediment Chart Chart � Bottom Sediment � Bottom Sediment types can vary types can vary greatly over a small greatly over a small area area Mud Mud 1. 1. Sand Sand 2. 2. Gravel Gravel 3. 3. Rock Rock 4. 4.

  13. AN/SQQ- -32 Employment 32 Employment AN/SQQ � Variable depth Variable depth � high frequency high frequency sonar system sonar system � Sonar can be place Sonar can be place � at various at various positions in the positions in the water column to water column to optimize the optimize the detection of either detection of either moored or bottom moored or bottom mines. mines.

  14. Two Depths of Transducer Two Depths of Transducer � Shallow Transducer: 17 ft (5.18 m) � Shallow Transducer: 17 ft (5.18 m) � Deep Transducer (25 m) � Deep Transducer (25 m) � Water depth: 30 m � Water depth: 30 m

  15. Uncertainty Uncertainty 0 to 0 Tilt angles + 4 0 12 0 � Tilt angles + 4 � to – – 12 � Wind 5 � Wind 5 – – 25 knots 25 knots � Coarse sand to silt bottoms � Coarse sand to silt bottoms

  16. Shallow Transducer

  17. Deep Transducer

  18. Acoustic Uncertainty Due to Wind and Bottom Type Uncertainty for Shallow Transducer (Range = 300 m)

  19. Acoustic Uncertainty Due to Wind and Bottom Type Uncertainty for Deep Transducer (Range = 300 m)

  20. Difference Between Deep and Shallow Transducers (Range = 300 m)

  21. Acoustic Uncertainty Due to Wind and Bottom Uncertainty for Shallow Transducer (Range = 600 m)

  22. Acoustic Uncertainty Due to Wind and Bottom Uncertaint for Deep Transducer (Range = 600 m)

  23. Difference Between Deep and Shallow Transducers (Range = 600 m)

  24. Acoustic Uncertainty Due to Wind and Bottom Uncertainty for Shallow Transducer (Range = 900 m)

  25. Acoustic Uncertainty Due to Wind and Bottom Uncertainty for Shallow Transducer (Range = 900 m)

  26. Difference Between Deep and Shallow Transducers (Range = 900 m)

  27. Acoustic Uncertainty Due to Wind and Bottom Uncertainty for Shallow Transducer (Range = 1200 m)

  28. Acoustic Uncertainty Due to Wind and Bottom Uncertainty for Deep Transducer (Range = 1200 m)

  29. Difference Between Deep and Shallow Transducers (Range = 1200 m)

  30. Conclusions Conclusions � Bottom type and wind variability are � Bottom type and wind variability are important for sandy silt detections important for sandy silt detections � Acoustic uncertainty due to bottom type and Acoustic uncertainty due to bottom type and � wind data variability is on the order of a few wind data variability is on the order of a few decibels decibels � Deep transducers provide higher signal Deep transducers provide higher signal � excess for most detectable cases excess for most detectable cases

  31. Recommendations Recommendations � Sensor improvements of a few decibels � Sensor improvements of a few decibels are significant for detection are significant for detection � Employment of sensors deeper aids � Employment of sensors deeper aids bottom moored mine detection bottom moored mine detection

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