Case study of electrical resistivity tomography measurements used in landslides investigation, Southern Poland

• Autorzy: Mita M. , Glazer M. , Kaczmarzyk R. , Dąbrowski M. , Mita K.

Identyfikatory

DOI

10.2478/ctg-2018-0007

• Języki publikacji: EN

Abstrakty

EN

Mass movements are an ever present threat to building construction, water management, vegetation formation and biodiversity. This paper presents an approach to landslides research based on non-invasive geoelectrical method - Electrical Resistivity Tomography (ERT). Mapping and displacement monitoring of unstable slopes is crucial for the hazards prevention and assessment. The ERT technique is an effective tool to obtain structural differentiation of geological medium through interpretation of 2D electrical resistivity models. The main advantage of the method is a wide range of applicability what makes its useful during field works on a landslide. It is commonly used for measurements of slope instability, determination of shear surface, landslide susceptibility, depth of bedrock, slip plane geometry. The aim of the work is to identify the geological structures underneath three selected landslides in south Poland: in Racibórz, Milówka and Porąbka. Attempts have been focused on determination of the usefulness of the proposed ERT methodology for evaluation of possible further development of mass movements. On two investigation sites two different arrays have been used: Wenner-Schlumberger and dipole-dipole which allowed to prepare combined data set and resistivity models based on them. Forward modelling of synthetic models based on a priori information allowed to understand anomalies present on resistivity models. Applied approach ensured quality increase of final interpretation of resistivity models.

Słowa kluczowe

EN

electrical resistivity tomography; ERT; numerical modelling; landslide; mass movements

PL

elektryczna tomografia rezystywnościowa; ERT; modelowanie numeryczne; osuwisko; ruchy masowe

• Wydawca: De Gruyter
• Czasopismo: Contemporary Trends in Geoscience
• Rocznik: 2018
• Tom: Vol. 7, iss. 1
• Strony: 110--126
• Opis fizyczny: Bibliogr. 30 poz., rys.

Twórcy

autor

Mita M.

• Science Student Society of Geophysics PREM, Faculty of Earth Sciences, University of Silesia, Będzińska Str. 60, 41-200 Sosnowiec

autor

Glazer M.

• Department of Geomorphology, Faculty of Earth Sciences, University of Silesia, Będzińska Str. 60, 41-200 Sosnowiec

autor

Kaczmarzyk R.

• Science Student Society of Geophysics PREM, Faculty of Earth Sciences, University of Silesia, Będzińska Str. 60, 41-200 Sosnowiec

autor

Dąbrowski M.

• Department of Geology and Hydrogeology, Faculty of Earth Sciences, Nicolaus Copernicus University, Lwowska Str. 1, 87-100 Toruń

autor

Mita K.

• Science Student Society of Geophysics PREM, Faculty of Earth Sciences, University of Silesia, Będzińska Str. 60, 41-200 Sosnowiec

Bibliografia

• Bardel T. (2012) O antropogenicznych przyczynach powstania osuwiska na zboczu byłej kopalni iłów „Kantoria” w Tarnowie. Górnictwo i Geologia 7, 2, 35-47.
• Burtan J., Sokołowski S., Sikora W., Żytko K. (1956) Szczegółowa mapa geologiczna Polski 1:50 000. Milówka Bielsko Biała (M-34-87A). Państwowy Instytut Geologiczny, Państwowy Instytut Badawczy, Oddział Karpacki, Kraków.
• Calamita G, Perrone A., Bellanova J., Giocoli A., Lapenna V., Luongo R., Piscitelli S. (2013) Application of electrical resistivity tomographies for the geoelectrical characterization of Montaguto landslide (southern Italy), Poster Presentation. 32° Convegno nazionale del Gruppo Nazionaledi Geofisica della Terra Solida, Trieste.
• Chambers J.E., Wilkinson P.B., Kuras O., Ford J.R., Gunn D.A., Meldrum P., Pennington C.V.L., Weller A.L., Hobbs P.R.N., Ogilvy, R.D. (2011) Three-dimensional geophysical anatomy of an active landslide in Lias Group mudrocks, Cleveland Basin, UK. Geomorphology 125: 472-484, DOI: 10.1016/j.geomorph.2010.09.017.
• Chen W., Li X., Wang Y., Chen G., Liu S. (2014) Forested landslide detection using LiDAR data and the random forest algorithm: A case study of the Three Gorges, China. Remote Sensing of Environment 152: 291-301, DOI: 10.1016/j.rse.2014.07.004.
• Dostál I. Putiška R. Kušnirák D. (2014) Determination of shear surface of landslides using electrical resistivity tomography 44, 2: 133-147, DOI: 10.2478/congeo-2014-0008.
• Everett M.E. (2013) Electrical resistivity method. [In:] Near-surface applied Geophysics. Cambridge University Press, New York, second edition, 70-104.
• Friedel S., Thielen A., Springman S.M. (2006) Investigation of a slope endangered by rainfall-induced landslides using 3D resistivity tomography and geotechnical testing. Journal of Applied Geophysics 60: 100–114, DOI: 10.1016/j.jappgeo.2006.01. 001.
• Grandjean G., Gourry J.C., Sanchez O., Bitri A., Garambois S. (2011) Structural study of the Ballandaz landslide (French Alps) using geophysical imagery. Journal of Applied Geophysics 75: 531–542, DOI: 10.1016/ j.jappgeo.2011.07.008.
• Jebur M.N., Pradhan B., Tehrany M.S. (2014) Optimization of landslide conditioning factors using very high-resolution airborne laser scanning (LiDAR) data at catchment scale. Remote Sensing of Environment 152: 150–165, DOI: 10.1016/j.rse.2014.05.013.
• Jomard H., Lebourg T., Tric E. (2007) Identification of the gravitational boundary in weathered gneiss by geophysical survey: La Clapière landslide (France). Journal of Applied Geophysics 62: 47–57, DOI: 10.1016/j.jappgeo.2006.07.003.
• Loke M. H. (2015) Rapid 2-D Resistivity & IP inversion using the least-squares method: Wenner (α, β, γ), dipole–dipole, inline pole-pole, pole-dipole, equatorial dipole-dipole, offset pole-dipole, Wenner-Schlumberger, gradient and non-conventional arrays. On land, aquatic and cross-borehole surveys. (Website: accessed 26th January, 2018 http://web.gps.caltech.edu/classes/ge111/Docs/Res2dinv_Guide.pdf).
• Loke M. H. (2016) Tutorial: 2-D and 3-D electrical imaging surveys. (Website: accessed 19th June, 2017 http://www.geotomosoft.com/downloads.php).
• Loke M.H., Barker R.D. (1996) Practical techniques for 3D resistivity surveys and data inversion. Geophysical Prospecting 44: 499-523, DOI: 10.1111/j.1365-2478. 1996.tb00162.x.
• Lowrie W. (2007) Fundamentals of Geophysics. Cambridge University Press, New York, second edition, 207-276.
• Malehmir A., Saleem M.U., Bastani M. (2013) High-resolution reflection seismic investigations of quick-clay and associated formations at a landslide scar in southwest Sweden. Journal of Applied Geophysics 92: 84-102, DOI: 10.1016/j.jappgeo.2013.02. 013.
• Marescot L., Monnet R., Chapellier D. (2008): Resistivity and induced polarization surveys for slope instability studies in the Swiss Alps. Engineering Geology 98: 18–28, DOI: 10.1016/j.enggeo.2008.01.010.
• Marinescu M., Cristea P., Maruntenau C., Mezincescu M. (2017) MASW Seismic Method in Brebu Landslide Area, Romania. IOP Conference Series: Earth and Environmental Science 95 032035, DOI:10.1088/1755-1315/95/3/032035.
• Mizerski W. (2006) Osuwiska. [In:] Geologia dynamiczna. PWN, Warszawa (in Polish), 149-155.
• Nescieruk P. Wójcik A. (1997) Szczegółowa mapa geologiczna Polski 1:50 000. 1012 – Bielsko Biała (M-34-75-C). Państwowy Instytut Geologiczny, Państwowy Instytut Badawczy, Oddział Karpacki, Kraków.
• Pánek T., Hradecký J., Šilhán K. (2008) Application of electrical resistivity tomography (ERT) in the study of various types of slope deformations in anisotropic bedrock: case studies from the flysch Carpathians. Studia Geomorphologica Carpatho-Balcanica 42, 57-73.
• Parasnis D.S. (1979) Electrical methods. [In:] Principles of applied Geophysics. Chapman and Hall Ltd., London, third edition, 98-130, DOI: 10.1007/978-94-009-5814-2.
• Pasierb B. (2012) Techniki pomiarowe metody elektrooporowej. Czasopismo Techniczne 2-Ś 23, 109: 191-199.
• Pilecki Z., Harba P. (2015): Wstępne wyniki badania budowy i właściwości osuwiska metodą interferometrii sejsmicznej z wykorzystaniem wysokoczęstotliwo-ściowego szumu sejsmicznego. Zeszyty Naukowe Instytutu Gospodarki Surowcami Mineralnymi i Energią Polskiej Akademii Nauk 89: 63-75.
• Pilecki Z., Pilecka E. (2016): Podstawowe zasady stosowania metod geofizycznych w badaniu osuwisk i terenów zagrożonych osuwiskami. Zeszyty Naukowe Instytutu Gospodarki Surowcami Mineralnymi i Energią Polskiej Akademii Nauk 92: 131-140.
• Poprawa D., Rączkowski W. (2003) Osuwiska Karpat. Przegląd Geologiczny 51, 8: 685-692.
• Rączkowski W., Wójcik A., Nescieruk P. (2016) Karta dokumentacyjna osuwiska wraz z opinią 24-17-092-002621. Państwowy Instytut Geologiczny, Państwowy Instytut Badawczy, Oddział Karpacki, Kraków.
• Sass O., Bell R., Glade T. (2008) Comparison of GPR, 2D-resistivity and traditional techniques for the subsurface exploration of the Öschingen landslide, Swabian Alb (Germany). Geomorphology 93: 89–103, DOI: 10.1016/j.geomorph.2006.12.019.
• Sikora R., Piotrowski A., Wilanowski S. (2011) Karta rejestracyjna osuwiska 2/Ra. Państwowy Instytut Geologiczny, Oddział Górnośląski, Sosnowiec.
• Telford W.M., Geldart L.P., Sheriff R.E. (1990) Electrical Properties of Rocks and Minerals. [In:] Applied Geophysics. Cambridge University Press, New York, 283-292.

Uwagi

Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).