Density inversion of selected microgravity anomalies using L2-smoothing and minimum support focusing stabilizers

Interpretation and inversion of microgravity anomalies belong to important tasks of near-surface geophysics, mostly in cavities detection in engineering, environmental and archaeological applications. One of the mostly used concepts of inversion in applied gravimetry is based on the approximation of...

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Main Authors: Ivan ZVARA, Roman PAŠTEKA, Roland KARCOL
Format: Article
Language:English
Published: Earth Science Institute, Slovak Academy of Sciences, Slovakia 2021-03-01
Series:Contributions to Geophysics and Geodesy
Subjects:
Online Access:https://journal.geo.sav.sk/cgg/article/view/259
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spelling doaj-903fdb48cb014f3990dc8d45bc2c180d2021-03-19T08:08:27ZengEarth Science Institute, Slovak Academy of Sciences, SlovakiaContributions to Geophysics and Geodesy1338-05402021-03-01511638110.31577/congeo.2020.51.1.4259Density inversion of selected microgravity anomalies using L2-smoothing and minimum support focusing stabilizersIvan ZVARA0Roman PAŠTEKA1Roland KARCOL2Faculty of Natural Sciences, Comenius University, Bratislava, Slovak Republic Faculty of Natural Sciences, Comenius University, Bratislava, Slovak RepublicFaculty of Natural Sciences, Comenius University, Bratislava, Slovak RepublicInterpretation and inversion of microgravity anomalies belong to important tasks of near-surface geophysics, mostly in cavities detection in engineering, environmental and archaeological applications. One of the mostly used concepts of inversion in applied gravimetry is based on the approximation of the model space by means of 2D or 3D elementary sources with the aim to estimate their densities by means of the solution of a corresponding linear equation system. There were published several approaches trying to obtain correct and realistic results, which describe real parameters of the sources. In the proposed contribution we analyse the properties of two additional functionals, which describe additional properties of the searched solution – namely so-called L2-smoothing and minimum support focusing stabilizers. For the inversion itself, we have used the regularized conjugate gradient method. We have studied properties of these two stabilizers in the case of one synthetic model and one real-world dataset (microgravity data from St. Nicholas church in Trnava). Results have shown that proposed algorithm with the minimum support stabilizer can generate satisfactory model results, from which we can describe real geometry, dimensions and physical properties of interpreted cavities.https://journal.geo.sav.sk/cgg/article/view/259gravimetry, interpretation, inversion, regularisation, cavities
collection DOAJ
language English
format Article
sources DOAJ
author Ivan ZVARA
Roman PAŠTEKA
Roland KARCOL
spellingShingle Ivan ZVARA
Roman PAŠTEKA
Roland KARCOL
Density inversion of selected microgravity anomalies using L2-smoothing and minimum support focusing stabilizers
Contributions to Geophysics and Geodesy
gravimetry, interpretation, inversion, regularisation, cavities
author_facet Ivan ZVARA
Roman PAŠTEKA
Roland KARCOL
author_sort Ivan ZVARA
title Density inversion of selected microgravity anomalies using L2-smoothing and minimum support focusing stabilizers
title_short Density inversion of selected microgravity anomalies using L2-smoothing and minimum support focusing stabilizers
title_full Density inversion of selected microgravity anomalies using L2-smoothing and minimum support focusing stabilizers
title_fullStr Density inversion of selected microgravity anomalies using L2-smoothing and minimum support focusing stabilizers
title_full_unstemmed Density inversion of selected microgravity anomalies using L2-smoothing and minimum support focusing stabilizers
title_sort density inversion of selected microgravity anomalies using l2-smoothing and minimum support focusing stabilizers
publisher Earth Science Institute, Slovak Academy of Sciences, Slovakia
series Contributions to Geophysics and Geodesy
issn 1338-0540
publishDate 2021-03-01
description Interpretation and inversion of microgravity anomalies belong to important tasks of near-surface geophysics, mostly in cavities detection in engineering, environmental and archaeological applications. One of the mostly used concepts of inversion in applied gravimetry is based on the approximation of the model space by means of 2D or 3D elementary sources with the aim to estimate their densities by means of the solution of a corresponding linear equation system. There were published several approaches trying to obtain correct and realistic results, which describe real parameters of the sources. In the proposed contribution we analyse the properties of two additional functionals, which describe additional properties of the searched solution – namely so-called L2-smoothing and minimum support focusing stabilizers. For the inversion itself, we have used the regularized conjugate gradient method. We have studied properties of these two stabilizers in the case of one synthetic model and one real-world dataset (microgravity data from St. Nicholas church in Trnava). Results have shown that proposed algorithm with the minimum support stabilizer can generate satisfactory model results, from which we can describe real geometry, dimensions and physical properties of interpreted cavities.
topic gravimetry, interpretation, inversion, regularisation, cavities
url https://journal.geo.sav.sk/cgg/article/view/259
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