Determination of cavities using electrical resistivity tomography

Geophysical surveys for cavity detection are one of the most common nearsurface applications. The usage of resistivity methods is also very straightforward for the air-filled underground voids, which should have theoretically infinite resistivity in the ERT image. In the first part of the paper, we...

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Main Authors: René PUTIŠKA, Maroš NIKOLAJ, Ivan DOSTÁL, David KUŠNIRÁK
Format: Article
Language:English
Published: Earth Science Institute, Slovak Academy of Sciences, Slovakia 2012-06-01
Series:Contributions to Geophysics and Geodesy
Subjects:
Online Access:https://journal.geo.sav.sk/cgg/article/view/72
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spelling doaj-344f207397e54941b699b32283e296782020-11-25T04:10:37ZengEarth Science Institute, Slovak Academy of Sciences, SlovakiaContributions to Geophysics and Geodesy1338-05402012-06-0142220121110.2478/v10126-012-0018-372Determination of cavities using electrical resistivity tomographyRené PUTIŠKA0Maroš NIKOLAJ1Ivan DOSTÁL2David KUŠNIRÁK3Department of Applied and Environmental Geophysics, Faculty of Natural Sciences Comenius UniversityWater Constructions Building Company (state enterprise)Department of Applied and Environmental Geophysics, Faculty of Natural Sciences Comenius UniversityDepartment of Applied and Environmental Geophysics, Faculty of Natural Sciences Comenius UniversityGeophysical surveys for cavity detection are one of the most common nearsurface applications. The usage of resistivity methods is also very straightforward for the air-filled underground voids, which should have theoretically infinite resistivity in the ERT image. In the first part of the paper, we deal with the comparison of detectability of the cavity by several types of the electrode arrays, the second part discusses the effect of a thin layer around the cavity itself, by means of 2D modelling. The presence of this layer deforms the resistivity image significantly as the resistive anomaly could be turned into a conductive one, in the case when the thin layer is more conductive than the background environment. From the electrical array analysis for the model situation a dipole-dipole and combined pole-dipole shows the best results among the other involved electrical arrays.https://journal.geo.sav.sk/cgg/article/view/72electrical resistivity tomography, cavity, resistivity modelling, resistivity inversion
collection DOAJ
language English
format Article
sources DOAJ
author René PUTIŠKA
Maroš NIKOLAJ
Ivan DOSTÁL
David KUŠNIRÁK
spellingShingle René PUTIŠKA
Maroš NIKOLAJ
Ivan DOSTÁL
David KUŠNIRÁK
Determination of cavities using electrical resistivity tomography
Contributions to Geophysics and Geodesy
electrical resistivity tomography, cavity, resistivity modelling, resistivity inversion
author_facet René PUTIŠKA
Maroš NIKOLAJ
Ivan DOSTÁL
David KUŠNIRÁK
author_sort René PUTIŠKA
title Determination of cavities using electrical resistivity tomography
title_short Determination of cavities using electrical resistivity tomography
title_full Determination of cavities using electrical resistivity tomography
title_fullStr Determination of cavities using electrical resistivity tomography
title_full_unstemmed Determination of cavities using electrical resistivity tomography
title_sort determination of cavities using electrical resistivity tomography
publisher Earth Science Institute, Slovak Academy of Sciences, Slovakia
series Contributions to Geophysics and Geodesy
issn 1338-0540
publishDate 2012-06-01
description Geophysical surveys for cavity detection are one of the most common nearsurface applications. The usage of resistivity methods is also very straightforward for the air-filled underground voids, which should have theoretically infinite resistivity in the ERT image. In the first part of the paper, we deal with the comparison of detectability of the cavity by several types of the electrode arrays, the second part discusses the effect of a thin layer around the cavity itself, by means of 2D modelling. The presence of this layer deforms the resistivity image significantly as the resistive anomaly could be turned into a conductive one, in the case when the thin layer is more conductive than the background environment. From the electrical array analysis for the model situation a dipole-dipole and combined pole-dipole shows the best results among the other involved electrical arrays.
topic electrical resistivity tomography, cavity, resistivity modelling, resistivity inversion
url https://journal.geo.sav.sk/cgg/article/view/72
work_keys_str_mv AT reneputiska determinationofcavitiesusingelectricalresistivitytomography
AT marosnikolaj determinationofcavitiesusingelectricalresistivitytomography
AT ivandostal determinationofcavitiesusingelectricalresistivitytomography
AT davidkusnirak determinationofcavitiesusingelectricalresistivitytomography
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