Paper
27 November 2001 Underground structure detection by surface magnetic gradient measurements
Robert E. Kelly
Author Affiliations +
Abstract
This problem involves magnetic induction methods to locate and determine the depth of a subsurface line source of magnetic field. The origin of the field may be self- generated or induced by a surface transmitter. The experimental method requires measuring the horizontal gradient of either the vertical or horizontal component of the field rather than the field itself so as to increase signal to noise ratio. A mathematical outline is presented and experimental results are discussed.
© (2001) COPYRIGHT Society of Photo-Optical Instrumentation Engineers (SPIE). Downloading of the abstract is permitted for personal use only.
Robert E. Kelly "Underground structure detection by surface magnetic gradient measurements", Proc. SPIE 4491, Subsurface and Surface Sensing Technologies and Applications III, (27 November 2001); https://doi.org/10.1117/12.450182
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CITATIONS
Cited by 7 scholarly publications.
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KEYWORDS
Magnetism

Magnetic sensors

Refraction

Wavefronts

Free space

Reflection

Signal to noise ratio

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