radar tunnel detection · underground tunnels present both military and homeland security threats:...
TRANSCRIPT
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s
Carey Rappaport and Jose Martinez-Lorenzo
ALERT Center of Excellence Northeastern University, Boston, MA
ADSA-CBP 01, Boston, MA - June, 2018
Radar Tunnel Detection
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Challenges and Conclusions
Finding tunnels along border is hard: • Lots of terrain to cover • Variable depth • Randomly varying rough ground surface • Unknown soil dielectric constant • Lossy (moist) soils obscure signals • Attended sensors are expensive, unattended sensors are targets
There is hope: • Tunnels have distinctive feature of long aspect ratio • Tunnels are filled with known target material (air) • Airborne SL-SAR can scan region quickly • Underground focusing (UF) is essential for detection
UF-SL-SAR imaging is compelling for Mexican and Middle Eastern borders
Here’s Why…
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Underground tunnels present both military and homeland security threats: • Transit routes for trafficking drugs, people and weapons • Detonation access under high security facilities • Avoid security checkpoints (especially on the borders)
Near Otay Messa, CA (Sandy H, Getty Images 2006)
Tijuana, Mexico (David Maung, AP, 2004)
Height: 1.5 – 2 m
Width: 0.5 – 1 m
Length: 0.1 – 10 km
Problem formulation
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Current methods
Most of the currently proposed solutions rely on land-based Ground Penetrating Radar (GPR)
Time consuming
Expensive
Trade-off between image quality & scanning time
Radio Frequency Tomography for Tunnel Detection [Lo Monte 2010]
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Why Spotlight-SAR?
Synthetically focus for narrow illumination spots
Generate high resolution images
Scans large regions in short amount of time
Spotlight SAR [Natural Resources Canada 2005]
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System configuration and challenges
Penetration
Depth d10
= Distance for
the power to
drop by a factor
of 10 (-10 dB)
(19%wet)
(26%wet)
Penetration Depth v. Frequency for various dielectric materials
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Multiple angles and frequencies for higher resolution: 128 frequencies from 50 MHz to 550 MHz
19 angles from -45 degrees to 45 degrees
Parametrize permittivity
Tunnel: 1 m x 1.5 m
Simulation configuration
Parameter: roughness height
Several angles and
several frequencies
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Underground Focusing Considerations
Enhances Spotlight – SAR capabilities
Takes into account wave refraction assuming a flat surface
Needs estimation of soil characteristics
Image quality and tunnel detectability depend on soil properties
Underground media variation presents challenges
Transmitter Refraction point
Target
ε1
ε2
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Non-dispersive sandy soil resolution: focal spot size
Refraction focusing at
underground point
y= 0.5 m y= 0 m
y= -4 m
y= -4 m
y= 0.5 m y= 0 m
Focusing at point on surface
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Field Scattered by Rough Surface Imperfections / Tunnel: 550 MHz , -45 deg.
Magnitude Scattered No Tunnel
Transverse distance (m)
Depth
(m
)
Magnitude Scattered Tunnel
Transverse distance (m)
Depth
(m
)
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Focused at 0.5m Focused at 0.5 m
Magnitude Total field No Tunnel
Magnitude Total field Tunnel
From 0.5 m to -9 m
Focused at 0 m Focused at 0 m Focused at -1 m Focused at -1 m Focused at -2 m Focused at -2 m Focused at -3 m Focused at -3 m Focused at -4 m Focused at -4 m Focused at -5 m Focused at -5 m Focused at -6 m Focused at -6 m Focused at -7 m Focused at -7 m Focused at -8 m Focused at -8 m Focused at -8 m Focused at -8 m
Range focusing dry sand: total field
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Nominal Image Reconstruction
Magnitude of scattered field [dB scale]
Original geometry Tunnel
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Wavenumber Estimation
Case I: Non-dispersive dry clay soil Simulation: ε = 8 ε0 (1+0.01 i )
Imaging: parameter sweep
εr = [1,3,4, 6, 8, 10, 12, 14]
Roughness height sweep:
R = [0.1 0.2 0.3 0.4 0.5 0.6]
Case II: Lossy clay loam soil Simulation: ε = A.P. Hill firing point
Imaging: parameter sweep
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Case I: Non-dispersive dry clay soil
Imaging with permittivity sweep
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Image reconstruction with εr = 1
Magnitude of scattered field [dB scale]
Original geometry Tunnel
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Image reconstruction with εr = 3
Magnitude of scattered field [dB scale]
Original geometry Tunnel
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Image reconstruction with εr = 4
Magnitude of scattered field [dB scale]
Original geometry Tunnel
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Image reconstruction with εr = 6
Magnitude of scattered field [dB scale]
Original geometry Tunnel
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Image reconstruction with εr = 8
Magnitude of scattered field [dB scale]
Original geometry Tunnel
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Image reconstruction with εr = 10
Magnitude of scattered field [dB scale]
Original geometry Tunnel
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Image reconstruction with εr = 12
Magnitude of scattered field [dB scale]
Original geometry Tunnel
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Image reconstruction with εr = 14
Magnitude of scattered field [dB scale]
Original geometry Tunnel
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Case II: Lossy clay loam soil Imaging with permittivity sweep
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Lossy, dispersive clay loam soil
Average
0.5 1 1.5 2 2.5 3 3.5 4 4.5 5
x 108
0.01
0.012
0.014
0.016
0.018
0.02
0.022
0.024
0.026
0.028
0.03
Frequency (Hz)
Co
nd
ucti
vit
y (
S/m
)
0.5 1 1.5 2 2.5 3 3.5 4 4.5 5
x 108
8.8
9
9.2
9.4
9.6
9.8
10
10.2
10.4
Rela
tive R
eal D
iele
ctr
ic C
on
sta
nt
Frequency (Hz)
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Dispersive clay loam soil
y= 0.5 m y= 0 m y= -4 m
Focusing at point on surface
Refraction focusing at underground point
-25dB
-25dB
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Image reconstruction: ε = 0.1 εhill
Magnitude of scattered field [dB scale]
Original geometry Reconstruction Tunnel response
Width (m)
Heig
ht (m
)
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Width (m)
Heig
ht (m
) Image reconstruction: ε = 0.3 εhill
Magnitude of scattered field [dB scale]
Original geometry Reconstruction Tunnel response
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Magnitude of scattered field [dB scale]
Original geometry Reconstruction Tunnel response
Width (m)
Heig
ht (m
) Image reconstruction: ε = 0.8 εhill
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Magnitude of scattered field [dB scale]
Original geometry Reconstruction Tunnel response
Width (m)
Heig
ht (m
) Image reconstruction: ε = 1 εhill
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Magnitude of scattered field [dB scale]
Original geometry Reconstruction Tunnel response
Width (m)
Heig
ht (m
) Image reconstruction: ε = 2 εhill
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Magnitude of scattered field [dB scale]
Original geometry Reconstruction Tunnel response
Width (m)
Heig
ht (m
) Image reconstruction: ε = 4 εhill
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Magnitude of scattered field [dB scale]
Original geometry Reconstruction Tunnel response
Width (m)
Heig
ht (m
) Image reconstruction: ε = 8 εhill
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Magnitude of scattered field [dB scale]
Original geometry Reconstruction Tunnel response
Width (m)
Heig
ht (m
) Image reconstruction: ε = 12 εhill
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Roughness sweep: dry sandy soil
ε = 2.55 ε0 (1+0.01 i )
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Image reconstruction: Rheight = 0.1 m
Magnitude of scattered field [dB scale]
Original geometry Tunnel Background
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Image reconstruction: Rheight = 0.2 m
Magnitude of scattered field [dB scale]
Original geometry Tunnel Background
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Image reconstruction: Rheight = 0.3 m
Magnitude of scattered field [dB scale]
Original geometry Tunnel Background
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Image reconstruction: Rheight = 0.4 m
Magnitude of scattered field [dB scale]
Original geometry Tunnel Background
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Image reconstruction: Rheight = 0.5 m
Magnitude of scattered field [dB scale]
Original geometry Tunnel Background
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Image reconstruction: Rheight = 0.6 m
Magnitude of scattered field [dB scale]
Original geometry Tunnel Background
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Underground Focusing Spotlight Synthetic Aperture Radar for low-loss soils (deserts):
Successful detection on non-dispersive sandy soil until surface roughness exceeds 0.5 m (for correlation length of 1 m)
Sufficiently high wave number estimate provides accurate tunnel detection
Wrong prediction of tunnel depth
Partial reconstruction of surface
Conclusions -- 1
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Underground Focusing Spotlight Synthetic Aperture Radar for lossy soils:
Unsuccessful tunnel detection even with minimal surface roughness
Soil loss reduces target signal below surface clutter levels
Not suitable for tunnel detection with UF-SL-SAR
Conclusions -- 2
Acknowledgments: Gordon-CenSSIS NSF ERC Program (Award number EEC 9986821) and U.S. Dept. of Homeland Security (Award number 2008-ST-061-ED0001) The views and conclusions contained in this document are those of the authors and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the U.S. Dept. of Homeland Security.