1 / 40

Environmental Variability on Acoustic Prediction Using CASS/GRAB

Environmental Variability on Acoustic Prediction Using CASS/GRAB. Nick A. Vares June 2002. Purpose. Determine the impact of bottom type and wind variations due to limited data on bottom moored mine detection Determine the significance of transducer depth on bottom moored mine detection.

ostinmannual
Télécharger la présentation

Environmental Variability on Acoustic Prediction Using CASS/GRAB

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. Environmental Variability on Acoustic Prediction Using CASS/GRAB Nick A. Vares June 2002

  2. Purpose • Determine the impact of bottom type and wind variations due to limited data on bottom moored mine detection • Determine the significance of transducer depth on bottom moored mine detection

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

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

  5. CASS/GRAB Model Description • The CASS model is the range dependent improvement of the Generic Sonar Model (GSM). CASS performs signal excess calculations. • The GRAB model is a subset of the CASS model and its main function is to compute eigenrays and propagation loss as inputs in the CASS signal excess calculations.

  6. Comprehensive Acoustic Simulation System/Guassian Ray Bundle (CASS/GRAB) • In the GRAB model, the travel time, source angle, target angle, and phase of the ray bundles are equal to those values for the classic ray path. • The main difference between the GRAB model and a classic ray path is that the amplitude of the Gaussian ray bundles is global, affecting all depths to some degree whereas classic ray path amplitudes are local. GRAB calculates amplitude globally by distributing the amplitudes according to the Gaussian equation

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

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

  9. Detection Sonar and Classification Sonar Assembly

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

  11. Bottom Type Geoacoustic Properties

  12. Bottom Type Variability • Muddy sand (3.0) and sandy silt (5.0) • Grain size index variation + 1.0 in 0.5 increments • 5.14 m/s, - 40, bottom 30 m, transducer 5.18 m

  13. Yellow Sea Bottom Sediment Chart • Bottom Sediment types can vary greatly over a small area • Mud • Sand • Gravel • Rock

  14. Wind Variability • Muddy sand (3.0) and sandy silt (5.0) • Tilt angle - 40, bottom 30 m, transducer 5.18 m • 5.14 + 2.57 m/s wind

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

  16. Transducer 5.18 m vs 25 m • Tilt angles + 40 to – 120 • Wind 2.57 to 12.86 m/s • Coarse sand to silt bottoms • 30 m water depth

  17. Conclusions • Bottom type and wind variability are important for sandy silt detections • Bottom type and wind data variability are on the order of a few decibels • Deep transducers provide higher signal excess for most detectable cases

  18. Recommendations • Sensor improvements of a few decibels are significant for detection • Money would be better spent on sensor development • Employment of sensors deeper aids bottom moored mine detection

More Related