On the detection objects buried at a shallow depth using seismic wave reflections
On the detection objects buried at a shallow depth using seismic wave reflections
This paper concerns the detection of shallow (of the order 1 m) buried objects using seismic excitation. Time-extended signals are used to generate a compressional wave using a shaker attached to the ground. The wave propagates through the ground, reflects off a buried object and is captured by an array of geophones on the surface. The envelopes of the cross-correlation functions between the measured ground velocities and the excitation signal are calculated and summed to generate a cross-sectional image of the ground. The wide cross-correlation peaks caused by high ground attenuation are partially compensated for by using the generalized cross-correlation function called the phase transform. Simple simulations are conducted to demonstrate the method, and some field experiments have been carried out aimed at the detection of a buried concrete pipe. In the experiments the pipe could be detected using the method proposed, with experimental and simulated data producing good agreement.
1366-1374
Papandreou, Ben
df5b58cf-c49c-45f1-a3e7-01ed286d970d
Brennan, Michael J.
87c7bca3-a9e5-46aa-9153-34c712355a13
Rustighi, Emiliano
9544ced4-5057-4491-a45c-643873dfed96
March 2011
Papandreou, Ben
df5b58cf-c49c-45f1-a3e7-01ed286d970d
Brennan, Michael J.
87c7bca3-a9e5-46aa-9153-34c712355a13
Rustighi, Emiliano
9544ced4-5057-4491-a45c-643873dfed96
Papandreou, Ben, Brennan, Michael J. and Rustighi, Emiliano
(2011)
On the detection objects buried at a shallow depth using seismic wave reflections.
Journal of the Acoustical Society of America, 129 (3), .
(doi:10.1121/1.3552878).
(PMID:21428500)
Abstract
This paper concerns the detection of shallow (of the order 1 m) buried objects using seismic excitation. Time-extended signals are used to generate a compressional wave using a shaker attached to the ground. The wave propagates through the ground, reflects off a buried object and is captured by an array of geophones on the surface. The envelopes of the cross-correlation functions between the measured ground velocities and the excitation signal are calculated and summed to generate a cross-sectional image of the ground. The wide cross-correlation peaks caused by high ground attenuation are partially compensated for by using the generalized cross-correlation function called the phase transform. Simple simulations are conducted to demonstrate the method, and some field experiments have been carried out aimed at the detection of a buried concrete pipe. In the experiments the pipe could be detected using the method proposed, with experimental and simulated data producing good agreement.
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e-pub ahead of print date: 9 March 2011
Published date: March 2011
Organisations:
Dynamics Group
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Local EPrints ID: 333352
URI: http://eprints.soton.ac.uk/id/eprint/333352
ISSN: 0001-4966
PURE UUID: 8cdc3e6d-4095-4205-9170-56da0a8d613d
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Date deposited: 06 Mar 2012 12:10
Last modified: 14 Mar 2024 10:31
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Author:
Ben Papandreou
Author:
Michael J. Brennan
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