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Title: Optimal Experiments with Acoustic-Seismic Sensors


1
Optimal Experiments with Acoustic-Seismic Sensors
  • James McClellan and Waymond R. Scott, Jr.
  • School of Electrical and Computer Engineering
  • Georgia Institute of Technology
  • Atlanta, GA 30332-0250
  • jim.mcclellan_at_ece.gatech.edu
  • 404-894-8325

2
Outline
  • Introduction
  • Seismic System
  • Spectrum Analysis of Seismic Waves
  • Location with Acoustic/Seismic Arrays
  • Maneuvering Array (3x10)
  • Cumulative Array strategy for imaging
  • Optimal Experiments
  • Examples

3
Prototype Seismic Mine Detection System
4
Data Movies
  • All wave types
  • Only the reflected wave
  • After k-domain processing

5
Typical Surface Sensor Arrays Used in
Experimental Model at Field Test Sites
Data is collected by 3-axis sensor - x,
Horizontal Channel - z, Vertical Channel
Elastic Wave Source
Linear Array of 16 Triaxial Accelerometers
Linear Array of 8 Triaxial Geophones
6
Seismic SensorPseudo Color Graph y 20 cm
Bag of Dry Sand 5 cm Deep
Crushed Can 3 cm Deep
Mine TS-50 1.5 cm Deep
7
Extract Reflected Waves
  • Surface Waves Velocity vs. Frequency
  • Parametric Model for surface waves
  • IQML (Prony, Steiglitz-McBride)
  • Multi-Channel Modeling
  • Need robust method to work with field data
  • Extract various types of waves
  • Individual modes
  • Exploit data collected from tri-axial sensors
  • Polarization can be used to identify different
    wave types

8
Frequency-Domain Model
  • 2-D Fourier transform of sensor data s (x, t)
    represents signal as propagating plane waves
  • Slowness k / ?
  • Velocity ? / k
  • k wave-number
  • ? temporal frequency

Constant velocity is a ray from the origin
9
Parametric Model for One Channel
  • STEPS
  • Take 1-D Fourier transform over time,
    s(x,t)-gtS(x,?)
  • ARMA Modeling is done across x to obtain
  • a space-frequency (k , ? ) model,
  • Estimate a(?) and k(?) by IQML (aka St-McB/Prony)

10
Results from Vector IQML
  • k(?) vs. ? becomes velocity vs. O
  • Extract individual modes from (k , ? ) and
    reconstruct them in time domain from the model
    parameters, i.e., Sum across frequency

11
Spectrum Analysis via Prony
TS-50 at 1cm
VS1.6 at 5cm
12
Home in on a Target
  • Problem Statement
  • Use a small number of source receiver positions
    to locate targets, i.e., landmines
  • Minimize the number of measurements
  • Three phases
  • Probe phase use a small 2-D array (rectangle or
    cross)
  • Find general target area by imaging with
    reflected waves
  • Adaptive placement of additional sensors
  • Maneuver receiver(s) to increase resolution
  • Use Theory of Optimal Experiments
  • On-top of the target
  • End-game Verify the resonance

13
Adaptive Sensor Placement
Target
Source
Probe Array
Probe Array finds general target area
14
Ground Contacting Seismic Sensor Array Deployed
on a Small Robotic Platform
Source Platform
Sensor Platforms
15
Experimental Setup of Seismic Landmine Detection
Measurements
16
Choose Next Sensor Position
  • Want to formulate an optimal maneuvering strategy
  • Instead of adding One Sensor, move the Whole
    Array to the next optimal position
  • Append the array data at the new position with
    previous data
  • Estimate the target location
  • Find the best next sensor position

17
Steps in Optimal Maneuver
  • Wave Separation by Prony
  • Imaging algorithm
  • - Data Model
  • - ML solution for target position
    estimates
  • - Performance bounds for position
    estimates
  • Next optimal Array Position
  • - D-optimal Design
  • - Constrained Optimization

18
Data Model
19
Target Position Estimate
  • The Cramer-Rao lower bound (CRLB) provides a
    lower bound for the variances of the unbiased
    estimators
  • CRLB requires the inverse of the Fisher
    information matrix

20
Fisher Information Matrix for Position Estimate
21
Theory of Optimal Experiments
  • The theory of optimal experiments uses various
    measures of the Fisher information matrix to
    produce decision rules
  • Determinant
  • Trace
  • Maximum value along the diagonal
  • D-optimal Design uses the determinant

X. Liao and L. Carin, Application of the
Theory of Optimal Experiments to Adaptive
Electromagnetic-Induction Sensing of Buried
Targets,'' IEEE Trans. on Pattern Analysis and
Machine Intelligence, vol. 26 , no.8, pp.
961-972, August 2004.
22
Next Optimal Position
23
Unique Problems for Seismic
  • Target position is estimated from reflected
    seismic energy
  • Source is nearby
  • Need separation between forward and reverse waves
  • Array position has to be between source and
    targets always
  • Landmines reflections are not omni-directional
  • Next array position has to be Constrained
  • Between source and estimated target position
  • Two ways to implement constrained optimization
  • Circle constraint, or Penalty Function

24
Constrained optimization for next array position
25
Experimental Data Setup
  • Single TS-50 landmine is buried at 1cm
  • Reflected waves are separated at each position by
    using a line array of 15 sensors (3cm apart)
  • Actual receiver is a single sensor (Synthetic
    Array)
  • Measurements are grouped into line arrays
  • From each line array, three sensors at equal
    distance positions are chosen
  • With three line arrays, an array of nine sensors
    is available for 2-D imaging
  • Inverse of the cost function is plotted for
    imaging algorithm

26
First Iteration
ACTUAL TARGET (135,135) 5 ESTIMATE (102,120)
27
Next array position values calculated on half
circle of radius30cm
Values calculated on half circle
28
Second Iteration
ACTUAL TARGET (135,135) 5 ESTIMATE ALONE
(100,127), CUM(112,127)
ALONE
CUMULATIVE
29
Next Array Position
Values calculated on half circle
30
Third Iteration
ACTUAL TARGET (135,135) 5 ESTIMATE ALONE
(143,138), CUM(127,133)
ALONE
CUMULATIVE
31
Fourth Iteration
ACTUAL TARGET (135,135) 5 ESTIMATE ALONE
(124,144), CUM(146,139)
CUMULATIVE
ALONE
32
Four Iterations Cumulative Imaging
33
Implementation
  • 2D array (3 X 10)
  • Three lines having 10 sensors each
  • Sensors are ground contacting accelerometers
  • LabView is used to control the movement of array
    and seismic source firing and interface with
    MATLAB
  • Processing algorithms are implemented in MATLAB
  • Target is a VS1.6 mine buried at 5cm

34
Experimental Setup of Seismic Landmine Detection
Measurements
35
Seismic Detection of VS-1.6 AT Landmine Buried
5cm Deep in Experimental Model
Landmine (22.2 cm diameter) buried 110 cm from
first measurement location in 171 cm linear
scan. 5 measurements with center line of sensor
array along a line over the burial
location. Compressional, Rayleigh Surface, and
Reflected Waves. Resonance of Landmine-Soil
System. Interactions of incident waves with
buried landmine evident in measured data.
36
Wave Separation at each iteration along top-most
line array
2
1
3
4
37
Demo in Sandbox
EXPERIMENTAL SETUP
  • Target is localized in four iterations
  • Each iteration takes 10 secs. for processing and
    30 secs. for data acquisition
  • Total time for four iterations is 2 minutes
  • Typical raster scan takes a few hours to locate
    the target with a large number of measurements

38
Demo in Sandbox
EXPERIMENTAL SETUP
  • Target is localized in four iterations
  • Bracket start
  • Each iteration takes 10 secs. for processing and
    30 secs. for data acquisition
  • Total time for four iterations is 2 minutes
  • Typical raster scan takes a few hours to locate
    the target with a large number of measurements

MOVIE of Experiment
39
Four Iterations
40
Four Iterations bracket start
41
End-game Detection
  • We can further scan in line with the last
    estimated target position
  • Extract the reverse wave and try to locate the
    exact location of resonance
  • Movies shown the extracted wave with the line
    array of 30 sensors, which is moved toward the
    target with 1cm increment
  • Target center is (50,50) and the starting
    location and position of target is shown

42
Movie VS-1.6 (5cm)
Extracted reverse wave as array moves near and
above the target
43
Movie TS-50 (1cm)
Extracted reverse wave as array moves near and
above the target
44
Constrained optimization for next array position
(2)
45
Target Position Estimate
46
Cramer-Rao Lower Bound
  • The Cramer-Rao lower bound (CRLB) is an
    information theoretic inequality, which provides
    a lower bound for the variances of the unbiased
    estimators
  • The Cramer-Rao lower bound is the inverse of
    Fisher information matrix

47
Next Optimal Position
48
Wideband RELAX algorithm
49
Surface Plot for Displays
50
Examples using Sandbox Data
  • Single source is used
  • Only the Reverse wave is used in processing
  • Or, passive listening for Buried structures
  • Remove the Forward wave
  • Prony analysis, or spatial filter
  • Frequency range
  • obtained from Spectrum Analysis of measured data
  • Future work
  • use RELAX to separate Forward and Reverse waves
  • Cylindrical wave model

51
Steps in Optimal Maneuver
  • Acquire data at the dense array
  • Separate the forward and reflected waves
  • Form a 2-D Imaging array at the new position
  • Append new data to data from old positions
  • Use 2-D Image to estimate the target position
  • Find the next optimal array position
  • Then move the array to the new position
  • Repeat these steps until target is localized

52
Wave Extraction via Prony
Position of upper line array 10 sensors, 3cm apart
53
Extracted Reverse Wave (synthesized at one sensor)
54
Wave Extraction via Prony
Position of middle line array 10 sensors, 3cm
apart
55
Extracted Reverse Wave (synthesized at one sensor)
56
Wave Extraction via Prony
Position of lower line array 10 sensors, 3cm apart
57
Extracted Reverse Wave (synthesized at one sensor)
58
Seismic Sensor
59
Review from January
  • Probe Phase
  • Pick five sensors in a cross pattern
  • Apply Imaging algorithm and plot the surface over
    a search grid
  • Maneuver Phase
  • Add one more sensor depending upon which
    direction to move
  • Increase aperture of triangulation
  • Spatial resolution increases which narrows down
    the area in which to search for target

60
TS-50 (1cm)
Source at (-20,50)
61
Next Measurement
1
2
3
62
Steps in Optimal Maneuver
63
Next Array Position
Circle constraint R30cm
Movement Penalty
64
Four Iterations another run
65
All Four Iterations Imaging with one array at a
time
66
Data Model
  • P-element array with position of every sensor is
    given in terms of array center
  • Seismic wave penetration depth depends on
    frequency, hence a band of frequencies is used in
    processing
  • K near-field wideband targets
  • In the DFT, select L Frequency components
  • Goal estimate location (z) of the targets from
    measured array data

67
Movie of Experiment
  • Demonstrate in real-time
  • Extraction of reflected waves is crucial
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