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Identification of Metallic Spheroids by Classification of Their Electromagnetic Induction Responses

Authors:
  • McFysics Consulting

Abstract

An investigation into the feasibility of applying pattern recognition concepts to the classification of metallic objects by their electromagnetic induction responses was performed. The effect on the response of a limited set of steel spheroids due to various factors such as object shape, size, and orientation was examined and a pattern recognition scheme based on these results was proposed. Implementation of the scheme involved the development of a novel extension to the nearest mean vector type of classifier in which the concept of the class mean as a point in feature space was generalized to be a curve. The resultant pattern recognition scheme was tested on a representative test set which included 815 responses, corresponding to 104 variations in object and orientation. A success rate of greater than 96 percent was achieved. It is noted that the classifier extension developed provides a viable approach to classification of responses that very continuously with respect to a single parameter.
... Depending on the number of variables involved, such a locus could be a curve, a surface or a higher order manifold. A novel approach t o solving such pattern classi cation problems was developed Chesney et al., 1984, McFee and . This technique has been already discussed under magnetostatics. ...
... This technique has been already discussed under magnetostatics. The earlier Chesney et al., 1984 v ariant o f t h e technique was applied to measured EMI responses of four steel spheroids, similar in dimensions to artillery shells. The measurements were taken in a nonmetallic laboratory, and data were collected at di erent orientations and depths of the objects. ...
... The CSEM method also can detect and, to some extent, classify man-made targets such as pipes, underground structures and unexploded ordnance (UXO) (Chesney et al., 1984; Qian and Boerner, 1995; Huang and Won, 2003). The method is sensitive to subsurface spatial variations in electrical conductivity. ...
... In near-surface geophysical applications, controlled-source electromagnetic (CSEM) methods are widely used because they are capable of detecting and mapping the distribution of fluids, large voids, faults or lithological contacts (Nobes, 1996; Tezkan, 1999; Pellerin, 2002; Everett and Meju, 2003). The CSEM method also can detect and, to some extent, classify man-made targets such as pipes, underground structures and unexploded ordnance (UXO) (Chesney et al., 1984; Qian and Boerner, 1995; Huang and Won, 2003). The method is sensitive to subsurface spatial variations in electrical conductivity. ...
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The response of geological materials at the scale of meters and the response of buried targets of different shapes and sizes using controlled-source electromagnetic induction (CSEM) is investigated. This dissertation focuses on three topics; i) frac- tal properties on electric conductivity data from near-surface geology and processing techniques for enhancing man-made target responses, ii) non-linear inversion of spa- tiotemporal data using continuation method, and iii) classification of CSEM transient and spatiotemporal data. In the first topic, apparent conductivity profiles and maps were studied to de- termine self-affine properties of the geological noise and the effects of man-made con- ductive metal targets. 2-D Fourier transform and omnidirectional variograms showed that variations in apparent conductivity exhibit self-affinity, corresponding to frac- tional Brownian motion. Self-affinity no longer holds when targets are buried in the near-surface, making feasible the use of spectral methods to determine their pres- ence. The difference between the geology and target responses can be exploited using wavelet decomposition. A series of experiments showed that wavelet filtering is able to separate target responses from the geological background. In the second topic, a continuation-based inversion method approach is adopted, based on path-tracking in model space, to solve the non-linear least squares prob- lem for unexploded ordnance (UXO) data. The model corresponds to a stretched- exponential decay of eddy currents induced in a magnetic spheroid. The fast inversion of actual field multi-receiver CSEM responses of inert, buried ordnance is also shown. Software based on the continuation method could be installed within a multi-receiver CSEM sensor and used for near-real-time UXO decision. In the third topic, unsupervised self-organizing maps (SOM) were adapted for data clustering and classification. The use of self-organizing maps (SOM) for central- loop CSEM transients shows potential capability to perform classification, discrimi- nating background and non-dangerous items (clutter) data from, for instance, unex- ploded ordnance. Implementation of a merge SOM algorithm showed that clustering and classification of spatiotemporal CSEM data is possible. The ability to extract tar- get signals from a background-contaminated pattern is desired to avoid dealing with forward models containing subsurface response or to implement processing algorithm to remove, to some degree, the effects of background response and the target-host interactions.
... The role of pattern recognition methods such as machine learning and target feature extraction, as an alternative to inversion, is gaining rapid acceptance in areas such as unexploded ordnance (UXO) and landmine detection. An important early paper in classification of buried spheroids by their CSEM response is by Chesney et al. (1984). It would be interesting to explore whether such concepts can be applied to hydrogeophysical settings in which the subsurface target is not necessarily an isolated, well-defined man-made object but instead could be a subtle, finely-distributed and irregular variation in the subsurface electrical conductivity distribution. ...
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Landfill sites commonly use the space available in disused quarries or special purpose-built structures but not all past landfill operations were adequately controlled or documented such that the site boundaries, and the type and volume of fill are unknown in some old covered landfill sites. Even in controlled sites, the final form and depth extent of the landfill may not conform to those indicated in the original plan submitted to the regulatory authorities during the application for a site license. Thus, a significant amount of work is required in order to accurately define the relevant parameters of a covered landfill site. Our hydrogeophysical interest in landfill sites lies in assessing the pollution threat they pose since they may contain hazardous substances. In conventional geophysical investigation of landfill sites, the usual goals are to determine the geometrical characteristics (size and shape) of the repository and the physiochemical properties of the infill. Of the several non-invasive geophysical methods used in landfill studies, the electrical and electromagnetic (EM) methods are the most popular owing to their inherent ability to detect changes related to variations in fluid content, chemical composition and temperature in the subsurface, and the minimum capital and labor outlay required to use them in small-scale surveys (Whiteley and Jewell, 1992; Meju 2000). Since the presence of saline fluids in the ground enhances its ability to conduct electrical current, it is possible to locate a leachate plume by measuring the resistivity distribution in the subsurface. The main ground resistivity measurement techniques employed in landfill studies are the direct current (dc) resistivity and/or induced polarization (IP) methods (e.g.
... The role of pattern recognition methods such as machine learning and target feature extraction, as an alternative to inversion, is gaining rapid acceptance in areas such as unexploded ordnance (UXO) and landmine detection. An important early paper in classification of buried spheroids by their CSEM response is by Chesney et al. (1984). It would be interesting to explore whether such concepts can be applied to hydrogeophysical settings in which the subsurface target is not necessarily an isolated, well-defined man-made object but instead could be a subtle, finely-distributed and irregular variation in the subsurface electrical conductivity distribution. ...
... The design set for an object consisted of the feature vectors for all orientations (15' increments) at a given depth. A continuous parameter pattern classifier [19] , similar to the one used in magnetostatics , was able to classify the objects with a probability of misclassification of about 1% if the design and test sets were obtained for the same object depth. If the two sets were taken from depths differing by 0.1 m, the probability increased to about 11%. ...
... In near-surface geophysical applications, controlled-source electromagnetic (CSEM) methods are widely used because they are capable of detecting and mapping the distribution of fluids, large voids, faults, or lithological contacts (Nobes, 1996; Tezkan, 1999; Pellerin, 2002; Everett and Meju, 2003). The CSEM method also can detect and, to some extent, classify man-made targets such as pipes, underground structures, and unexploded ordnance (UXO) (Chesney et al., 1984; Qian and Boerner, 1995; Huang and Won, 2003). The method is sensitive to subsurface spatial variations in electrical conductivity . ...
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Controlled-source electromagnetic-conductivity pro-files and maps were obtained on the Brazos Valley, Texas, floodplain to study the fractal statistics of ge-ologic noise and the effects of man-made conduc-tive metal targets. Fourier transform, discrete wavelet transforms, and variogram analyses were used. Targets tend to flatten the power-law power spectrum at small wavenumbers and shift power to higher wavenumbers. Detection and localization of targets can be achieved us-ing wavelet spectrogram techniques. Additionally, vari-ograms from pure background conductivity maps show a power-law trend for all lags, whereas, in the presence of targets, a short power-law trend is followed by a sill corresponding to a loss in spatial correlation. A sim-ple preprocessing step that combines responses from two perpendicular transmitter-receiver orientations en-hances the localization of targets and rejects back-ground signals in profiles and 2D apparent-conductivity maps. Finally, a field example shows how the use of wavelet filtering is able to separate target responses from the geologic background.
... The role of pattern recognition methods such as machine learning and target feature extraction, as an alternative to inversion, is gaining rapid acceptance in areas such as unexploded ordnance (UXO) and landmine detection. An important early paper in classification of buried spheroids by their CSEM response is by Chesney et al. (1984). It would be interesting to explore whether such concepts can be applied to hydrogeophysical settings in which the subsurface target is not necessarily an isolated, well-defined man-made object but instead could be a subtle, finely-distributed and irregular variation in the subsurface electrical conductivity distribution. ...
Chapter
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The controlled-source electromagnetic (CSEM) induction method is emerging as a leading geophysical technique in hydrogeological studies. However, the technique is quite often misunderstood compared to other common techniques of applied geophysics: namely, seismic reflection and refraction, magnetics, gravity, and ground-penetrating radar (GPR). In this chapter we review the fundamental physical principles behind the CSEM prospecting technique, with emphasis on near-surface applications, and present some recent advances in this field that have been made by the authors. CSEM methods are defined here to be those in which the experimenter has knowledge of and control over the electromagnetic field transmitted into the ground and hence excludes magnetotellurics, related natural-source methods, and the various uncontrolled-source methods involving, for example, radio transmissions.
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