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GEOPHYSICS, VOL. 75, NO. 3 �MAY-JUNE 2010�; P. B103–B114, 9 FIGS. 10.1190/1.3377009
nexploded ordnance discrimination using magnetic and electromagnetic ensors: Case study from a former military site
tephen D. Billings1, Leonard R. Pasion2, Laurens Beran3, Nicolas Lhomme1, Lin-Ping Song3, ouglas W. Oldenburg3, Kevin Kingdon1, David Sinex3, and Jon Jacobson1
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In a study at a military range with the objective to discriminate potentially hazardous 4.2-inch mortars from nonhazardous shrapnel, range, and cultural debris, six different discrimination techniques were tested using data from an array of magnetome- ters, a time-domain electromagnetic induction �EMI� cart, an ar- ray of time-domain sensors, and a time-domain EMI cart with a wider measurement bandwidth. Discrimination was achieved us- ing rule-based or statistical classification of feature vectors ex- tracted from dipole or polarization tensor models fit to detected anomalies. For magnetics, the ranking by moment yielded better discrimination results than that of apparent remanence from rela- tively large remanent magnetizations of several of the seeded items. The magnetometer results produced very accurate depths and fewer failed fits attributable to noisy data or model insuffi-
d l e t b t f s c v a m
ed 16 S .billing
iency. The EMI-based methods were more effective than the agnetometer for intrinsic discrimination ability. The higher sig-
al-to-noise ratio, denser coverage, and more precise positioning f the EM-array data resulted in fewer false positives than the MI cart. When depth constraints from the magnetometer data ere used to constrain the EMI fits through cooperative inver-
ion, discrimination performance improved considerably. The ide-band EMI sensor was deployed in a cued-interrogation ode over a subset of anomalies. This produced the highest-
uality data because of collecting the densest data around each arget and the additional late time-decay information available ith the wide-band sensor. When the depth from the magnetome-
er was used as a constraint in the cooperative inversion process, ll 4.2-inch mortars were recovered before any false positives ere encountered.
Unexploded ordnance �UXO� poses a major safety hazard in any parts of the world, including Canada, the United States, and ustralia, where UXO is present at former and active military rang-
s. During the past 10 years, significant research effort has been fo- used on developing methods to discriminate between hazardous XO and nonhazardous scrap metal, shrapnel, and geology �e.g., ell et al., 2001; Collins et al., 2001; Hart et al., 2001; Pasion and ldenburg, 2001; Zhang et al., 2003a; Zhang et al., 2003b; Billings, 004�. The most promising discrimination methods typically pro- eed by first recovering a set of parameters that specify a physics- ased model of the object being interrogated. For example, in time-
Manuscript received by the Editor 25 June 2009; revised manuscript receiv 1Sky Research Inc., Vancouver, British Columbia, Canada. E-mail: stephen skyresearch.com; email@example.com. 2Sky Research Inc., Vancouver, British Columbia, Canada, and The Univ
umbia, Canada. E-mail: firstname.lastname@example.org. 3The University of British Columbia — Geophysical Inversion Facility, V
ca; email@example.com; firstname.lastname@example.org. 2010 Society of Exploration Geophysicists.All rights reserved.
omain electromagnetic �TEM� data, the parameters are the object ocation and the polarization tensor �typically two or three collocat- d orthogonal dipoles along with their orientation and some parame- erization of the time-decay curve�. For magnetics, the physics- ased model is generally a static magnetic dipole. Once the parame- ers are recovered by inversion, a subset of the parameters is used as eature vectors to guide a statistical or rule-based classifier. There are ignificant advantages in collecting both types of data, including in- reased detection, stabilization of EM inversions by cooperative in- ersion of the magnetics �Pasion et al., 2008�, and extra dimension- lity in the feature space that may improve classification perfor- ance �e.g., Zhang et al., 2003a�.
eptember 2009; published online 20 May 2010. email@example.com; firstname.lastname@example.org; kevin.kingdon
f British Columbia, Geophysical Inversion Facility, Vancouver, British Co-
er, British Columbia, Canada. E-mail: email@example.com; firstname.lastname@example.org
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B104 Billings et al.
Results are presented here for a discrimination study pilot pro- ram conducted at the former Camp Sibert, Alabama, U.S.A., spon- ored by the Environmental Security Technology Certification Pro- ram �ESTCP�. The ability to separate munitions from nonhazard- us metallic items or geology is critical to reduce the cost of remedi- ting munitions-contaminated sites. Camp Sibert is particularly well uited for such classification efforts, which require collecting high- uality geophysical data. The site is relatively flat and clear of ob- tructions from vegetation or topography that would hinder survey- ng with cart-based geophysical sensors. In addition, the history of he site indicates there was primarily one type of ordnance deployed here: 4.2-in mortars. The objective at Camp Sibert was to discrimi- ate potentially hazardous 4.2-inch mortars from nonhazardous hrapnel, range, and cultural debris.
Our case study focuses on the results achieved using methodolo- ies developed by ourselves and others �e.g., Pasion and Oldenburg, 001; Billings, 2004; Beran and Oldenburg, 2008; Pasion et al., 008�. We provide an overview of the methodology and point the eader to relevant papers that describe the techniques in greater de- ail. We concentrate primarily on the results achieved — in particu- ar, the comparative performance of the different sensor modalities nd deployment modes. All results reported here were obtained us- ng commercial off-the-shelf �COTS� sensors. These include Geon- cs EM61 and EM63 time-domain metal detectors and an array of eometrics cesium vapor magnetometers. See Gasperikova et al.
2009� for the results of applying a multistatic EMI sensor at the ame site.
Because each COTS instrument measures only one component of vector field, a measurement at a single location provides limited in-
ormation. Consequently, relatively dense 2D measurements are re- uired for accurate recovery of relevant target parameters. These easurements must be very precisely positioned and oriented for
iscrimination to be successful. Data were acquired in full-coverage urvey mode �magnetometer array, EM61 cart, and EM61 array� and n cued-interrogation mode �EM63 cart�, whereby selected prelo- ated anomalies were surveyed densely in the immediate vicinity of he flagged anomaly location picked from a full coverage survey. In ddition to inverting each of the individual sets of data discussed, co- perative inversions also were undertaken for the towed EM61 array nd the EM63 cued-mode data using the magnetometer data to con- train the EM inversions.
Here, we contrast the discrimination and localization abilities of ix sensor combinations:
� Magnetometer array deployed in full-coverage mode with di- pole moment size used for discrimination
� EM61 cart deployed in full-coverage mode �no orientation in- formation recorded�
� EM61 array deployed in full-coverage mode with position and orientation information recorded
� Cooperative inversion of EM61 array and magnetometer array data
� EM63 cart deployed in cued-interrogation mode with position and orientation recorded
� Cooperative inversion of EM63 cart and magnetometer array data
STRUCTURE OF DISCRIMINATION STUDY
Our results are from a blind test of the discrimination performance f the different techniques; the ESTCP managed the discrimination tudy and withheld ground-truth information until after discrimina- ion declarations had been made. All results reported here, unless therwise indicated, were for the original submissions to the ESTCP.
An initial magnetometer survey of the Camp Sibert site was used o select three different areas for the discrimination study: southeast
�SE1�, southeast 2 �SE2�, and southwest �SW�. Combined, the hree areas cover approximately 15 acres. A geophysical prove-out GPO� was established immediately adjacent to the SW area; it in- luded 30 4.2-inch mortars emplaced at different depths and orienta- ions and eight partial mortars, considered as nonhazardous scrap. he ESTCP emplaced 152 4.2-inch mortars in the three areas. The
ocations and depths of 29 of these mortars, along with the locations nd identities of 179 clutter items, were provided to each demonstra- or and used as training data.
In full-coverage survey mode, data were collected using the stan- ard cart platform of the EM61-MK2 system. The Geonics EM61- K2 is a pulse-based time-domain electromagnetic instrument that
ecords data in four time windows centered at 0.216, 0.366, 0.660, nd 1.266 ms after pulse turn-off �e.g., Bosnar, 2001�. EM61-MK2 art data were acquired by an on