Inversion of electrical conductivity data with Tikhonov regularization approach: some considerations

Electromagnetic induction measurements, which are generally used to determine lateral variations of apparent
 electrical conductivity, can provide quantitative estimates of the subsurface conductivity at different depths.
 Quantitative inference about the Earth's interior from e...

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Main Authors: C. Manzi, E. Bonomi, G. P. Deidda
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2003-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/3427
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spelling doaj-a81954ab4d004ff3919c4b2c6cb29ceb2020-11-24T23:35:29ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2003-06-0146310.4401/ag-3427Inversion of electrical conductivity data with Tikhonov regularization approach: some considerationsC. ManziE. BonomiG. P. DeiddaElectromagnetic induction measurements, which are generally used to determine lateral variations of apparent
 electrical conductivity, can provide quantitative estimates of the subsurface conductivity at different depths.
 Quantitative inference about the Earth's interior from experimental data is, however, an ill-posed problem. Using
 the generalised McNeill's theory for the EM38 ground conductivity meter, we generated synthetic apparent
 conductivity curves (input data vector) simulating measurements at different heights above the soil surface. The
 electrical conductivity profile (the Earth model) was then estimated solving a least squares problem with Tikhonov
 regularization optimised with a projected conjugate gradient algorithm. Although the Tikhonov approach improves
 the conditioning of the resulting linear system, profile reconstruction can be surprisingly far from the desired true
 one. On the contrary, the projected conjugate gradient provided the best solution without any explicit regularization
 ( a= 0) of the objective function of the least squares problem. Also, if the initial guess belongs to the image of the
 system matrix, Im(A), we found that it provides a unique solution in the same subspace Im(A).http://www.annalsofgeophysics.eu/index.php/annals/article/view/3427inverse problemsTikhonov regularizationprojected conjugate gradienthigh-frequency electromagnetics
collection DOAJ
language English
format Article
sources DOAJ
author C. Manzi
E. Bonomi
G. P. Deidda
spellingShingle C. Manzi
E. Bonomi
G. P. Deidda
Inversion of electrical conductivity data with Tikhonov regularization approach: some considerations
Annals of Geophysics
inverse problems
Tikhonov regularization
projected conjugate gradient
high-frequency electromagnetics
author_facet C. Manzi
E. Bonomi
G. P. Deidda
author_sort C. Manzi
title Inversion of electrical conductivity data with Tikhonov regularization approach: some considerations
title_short Inversion of electrical conductivity data with Tikhonov regularization approach: some considerations
title_full Inversion of electrical conductivity data with Tikhonov regularization approach: some considerations
title_fullStr Inversion of electrical conductivity data with Tikhonov regularization approach: some considerations
title_full_unstemmed Inversion of electrical conductivity data with Tikhonov regularization approach: some considerations
title_sort inversion of electrical conductivity data with tikhonov regularization approach: some considerations
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2003-06-01
description Electromagnetic induction measurements, which are generally used to determine lateral variations of apparent
 electrical conductivity, can provide quantitative estimates of the subsurface conductivity at different depths.
 Quantitative inference about the Earth's interior from experimental data is, however, an ill-posed problem. Using
 the generalised McNeill's theory for the EM38 ground conductivity meter, we generated synthetic apparent
 conductivity curves (input data vector) simulating measurements at different heights above the soil surface. The
 electrical conductivity profile (the Earth model) was then estimated solving a least squares problem with Tikhonov
 regularization optimised with a projected conjugate gradient algorithm. Although the Tikhonov approach improves
 the conditioning of the resulting linear system, profile reconstruction can be surprisingly far from the desired true
 one. On the contrary, the projected conjugate gradient provided the best solution without any explicit regularization
 ( a= 0) of the objective function of the least squares problem. Also, if the initial guess belongs to the image of the
 system matrix, Im(A), we found that it provides a unique solution in the same subspace Im(A).
topic inverse problems
Tikhonov regularization
projected conjugate gradient
high-frequency electromagnetics
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/3427
work_keys_str_mv AT cmanzi inversionofelectricalconductivitydatawithtikhonovregularizationapproachsomeconsiderations
AT ebonomi inversionofelectricalconductivitydatawithtikhonovregularizationapproachsomeconsiderations
AT gpdeidda inversionofelectricalconductivitydatawithtikhonovregularizationapproachsomeconsiderations
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