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A Novel PiezoelectricCable Infrasound Sensor Initial Results

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Title: A Novel PiezoelectricCable Infrasound Sensor Initial Results


1
A Novel Piezoelectric-Cable Infrasound Sensor -
Initial Results
  • F. Kern, S. Africk, R. Chaves and P. Cataldi
  • Physical Sciences Inc.
  • 20 New England Business Center
  • Andover, MA 01810
  • M. Hedlin and C. Coon,
  • Laboratory for Atmospheric Acoustics, Scripps
    Institution of Oceanography, University of
    California, San Diego, CA
  • October 2003

SBIR Data Rights Contract No. DTRA01-01-C-0050 Co
ntractor Name Physical Sciences Inc. Address 20
New England Business Center, Andover, MA
01810-1077 Expiration of SBIR Data Rights Period
15 September 2008 The Governments rights to
use, modify, reproduce, release, perform,
display, or disclose technical data or computer
software marked with this legend are restricted
during the period shown as provided in paragraph
(b)(4) of the Rights in Noncommercial Technical
Data and Computer Software C Small Business
Innovative Research (SBIR) Program clause
contained in the above identified contract. No
restrictions apply after the expiration data
shown above. Any reproduction of technical data,
computer software, or portions thereof marked
with this legend must also reproduce the
markings. Distribution Statement B Distribution
authorized to Federal agencies only. Other
requests for this document shall be referred to
the Defense Threat Reduction Agency/AM COTR --
Captain Dirk Barker
2
What is Piezocable?
  • Pressure produces strain between shield and
    center core
  • PVDF is radially poled to produce electrical
    response to strain
  • Coax with PVDF copolymer piezoelectric
    dielectric
  • Coax with PVDF spiral wrap piezoelectric
    "dielectric"

3
Advantages of Piezocable
  • Direct electronic transduction "speed of light"
    averaging over array length
  • Eliminates mechanical systems(manifold and
    microbarograph)
  • Enables novel enhanced performance options
  • signal processing options
  • noise reduction strategies
  • infrasound station geometries
  • Environmentally robust

4
All-Electronic Reception and Local Processing
5
Comparison with Standard Systems
6
Background Piezocable Noiseand Calibration
Measurements
  • Background noise in steel tube to minimize
    thermal, pressure, and EMI excitations
  • Calibrations in short and long plastic chambers
    with modified compressor
  • Calibrations in foam tube with compressor also
    made

7
Piezocable Amplifiers
  • Signal Amplification (up to 60 dB)
  • Impedance transition
  • Very low noise
  • Calibration signals added

Piezocable amplifiers, calibration signal
generator and batteries
8
Amplifier Noise with 20 nF Capacitor Cable
Simulator
  • Amplifier noise -110.7 dB re 1 V2 at 1 Hz w/ 58
    dB amp gain
  • This meets the required spec

9
Outdoor Testing at PSI
10
Outside PSI Data Sample
Uncoiled cables in thermally insulating foam
under snow cover Wind speed 14 mph
Power Spectrum
Coherence
  • Conclusions
  • Good coherence on two sensor/amplifier pairs
  • Sensitivity consistent to less than 2 dB

11
Outdoor Testing (In Massachusetts)
  • Conclusions Cables will have to be buried for
    operation in windy environments. Tests in quiet
    environment needed to compare to current arrays
    (e.g. Piñon Flat).

12
Piñon Flat
New 100m Dirt Trench
New section, including old 30m trench, looking
West
New section looking East
13
Piezocable Infrasound Sensor Test StationPiñon
Flat Observatory
14
Piñon Flat Testing
15
Typical Acoustic Signal Observed by Piezocable
SensorsPiñon Flat Observatory
  • Signal arrives from South East
  • Signal velocity 370 m/s (not seismic)
  • Data filtered w/ 0.7-2.0 Hz bandpass to remove
    wind noise
  • Signal is observed on three piezocable sensors,
    microbarograph, and permanent pipe array.

16
Acoustic Event Observed on Three Piezocable
Sensors and USCD MicrobarographPiñon Flat
Observatory, DOY 268
17
Quiet Periods Piñon Flat Observatory
18
Directivity Implied from Acoustic Event Detected
by Perpendicular Piezocable Sensors
  • Signal observed on all three sensors
  • Sensitivity of PVDF/Amplifiers 10 dB less than
    microbarograph as expected
  • 100 m sensor has very little energy above 3 Hz,
    the cutoff for 100 m
  • 30 m sensor does not filter 4-6 Hz, cutoff at 11
    Hz
  • Spatial filter of 100 m sensor implies
    North/South signal incidence

19
Possible Wind Noise Event
20
Wind Noise Geometry
From Sensors
21
Microbarom Event - DOY 268 Observed on Three
Piezocables and Reference Microbarograph
22
Continuing Efforts
  • Characterize signal reception and environmental
    noise sensitivities and statistics to generate
    receiver characteristics.
  • Absolute signal sensitivity when in T.I. tube and
    when buried
  • Noise statistics - variability with
  • Time
  • Wind speed and direction
  • Frequency
  • Sensor length
  • Optimize packaging and deployment
  • Thermal insulating hose
  • Electronic shielding
  • Depth of burial and medium (gravel, dirt)
  • Evaluate potential effectiveness of multiple line
    arrays for noise control and novel signal
    processing
  • Evaluate magnitude of environmental
    electromagnetic noise with coax cable and
    possible use as a signal-free reference for
    electromagnetic noise cancellation

23
Summary and Conclusions
  • Piezocable sensors are an inexpensive means to
    measure infrasound
  • Over large apertures
  • With flexible geometries
  • At "speed-of-light"
  • Electronically-formed arrays of lines can provide
    directivity, signal enhancement and noise
    rejection. On-site or remote reconfiguration is
    possible to adjust to changing site conditions
  • Piezocable sensor/amplifier systems meet the CTBT
    noise specification
  • Signal events identified on permanent arrays have
    been detected on piezocable sensors with
    anticipated sensitivity

24
Summary and Conclusions (continued)
  • Microbaroms clearly identifiable in piezocable
    output.
  • Length averaging (spatial filtering) has been
    observed.
  • A means to infer signal incidence direction using
    perpendicular lines has been demonstrated.
  • Six piezocable sensors and two RG174A coax
    reference cables operating 24/7 at Piñon Flat and
    data analysis is ongoing.
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