The Physical Dipole Model and Polarizability for Magnetostatic Object Parameter Estimation

Author:

Furey John S.12,Butler Dwain K.12

Affiliation:

1. U.S. Army Engineer Research and Development Center, Environmental Laboratory, 3909 Halls Ferry Road, Vicksburg, Miss. 39180

2. Applied Geophysics Consultancy LLC, 211 Grinders Place, Vicksburg, Miss. 39180

Abstract

The physical dipole is the next simplest model of a magnetic object beyond the point dipole model. The theory and analytical properties of the physical dipole are developed and explored, and compare favorably with alternative models, including limiting cases of prolate spheroids and other shapes. The general applicability of explicitly modeling the demagnetization properties of magnetic materials is critically reviewed, and reasons proffered to use the object polarizability instead, especially for the external field properties of most relevance. Neither the physical dipole model nor polarizability is currently used for magnetostatic parameter estimation of magnetic objects such as unexploded ordnance. It is recommended that their utility be further explored with field data.

Publisher

Environmental and Engineering Geophysical Society

Subject

Geophysics,Geotechnical Engineering and Engineering Geology,Environmental Engineering

Reference54 articles.

1. Altshuler, T., 1996, Shape and orientation effects on magnetic signature prediction for unexploded ordnance: in Proceedings 1996 UXO Forum, Williamsburg, VA, 282–291.

2. Altshuler, T., A. Andrews, and D. Sparrow, 1997, Mine and UXO detection: measures of performance and their implication in real-world scenarios: Proceedings of SPIE, 3079, 281–292.

3. Barrow, B., R. DiMarco, N. Khadr, and H. Nelson, 1997, Processing and analysis of UXO signatures measured with MTADS: in Proceedings 1997 UXO Forum, Nashville, TN, 8–18.

4. U.S. Army Engineer Research and Development Center;Billings S.,2002

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