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Slingram Frequency-domain EMI - 3D Linear Inversion of Magnetic Susceptibility MeasurementsNormal access

Authors: J. Thiesson, F. Simon, M. Dabas and A. Tabbagh
Event name: Near Surface Geoscience 2016 - 22nd European Meeting of Environmental and Engineering Geophysics
Session: Modelling, Inversion and Data-processing II
Publication date: 04 September 2016
DOI: 10.3997/2214-4609.201602018
Organisations: EAGE
Language: English
Info: Extended abstract, PDF ( 1.2Mb )
Price: € 20

The very limited range of magnetic permeability variations (from 1.0001 to 1.01 in relative values) that can be observed in soils allows performing 3D linear inversions. To achieve this goal, we propose to successively define a reference conductivity and susceptibility profile, apply a 2D (x, y) Fourier transform to the apparent susceptibility variations mapped by the different instrument geometries, invert in z in the spectral domain over a series of predefined layers and determine the lateral variations in each layer by inverse Fourier transform. This process is applied to both synthetic and archaeological survey data.

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