<abstract xmlns="http://www.w3.org/1999/xhtml"><p> DC resistivity methods, soundings and Electrical Resistivity Tomography, were applied to study shallow geology in the place of planned construction of an experimental flood bank. The geoelectrical surveys provided quantitative information about the spatial presence of the various geoelectrical/geological layers: alluvial soils, sands, gravels and clays. ERT allowed maps to be constructed showing subsurface structure. A combination of geoelectrical and geological information resulted in a much better identification of the geological structure.</p></abstract>

DC resistivity methods, soundings and Electrical Resistivity Tomography, were applied to study shallow geology in the place of planned construction of an experimental flood bank. The geoelectrical surveys provided quantitative information about the spatial presence of the various geoelectrical/geological layers: alluvial soils, sands, gravels and clays. ERT allowed maps to be constructed showing subsurface structure. A combination of geoelectrical and geological information resulted in a much better identification of the geological structure.

DC Resistivity Studies of Shallow Geology in the Vicinity of Vistula River Flood Bank in Czernichów Village (Near Kraków in Poland)

AGH University of Science and Technology in Kraków, Faculty of Geology, Geophysics and Environmental Protection

Studia Geotechnica et Mechanica

This article is distributed under the terms of the Creative Commons Attribution Non-Commercial License, which permits unrestricted non-commercial use, distribution, and reproduction in any medium, provided the original work is properly cited.

DC resistivity methods, soundings and Electrical Resistivity Tomography, were applied to study shallow geology in the place of planned construction of an...

DC Resistivity Studies of Shallow Geology in the Vicinity of Vistula River Flood Bank in Czernichów Village (Near Kraków in Poland)

Publicado en línea: 13 jun 2014

Páginas: 63 - 70

DOI: https://doi.org/10.2478/sgem-2014-0008

Palabras clave
DC resistivity methods, vertical electrical soundings, Electrical Resistivity Tomography, shallow geology, flood bank, Quaternary, geophysics in civil engineering

© by Włodzimierz Jerzy Mościcki

This article is distributed under the terms of the Creative Commons Attribution Non-Commercial License, which permits unrestricted non-commercial use, distribution, and reproduction in any medium, provided the original work is properly cited.

DC Resistivity Studies of Shallow Geology in the Vicinity of Vistula River Flood Bank in Czernichów Village (Near Kraków in Poland)

Publicado en línea: 13 jun 2014

Páginas: 63 - 70

DOI: https://doi.org/10.2478/sgem-2014-0008

Palabras claveDC resistivity methods, vertical electrical soundings, Electrical Resistivity Tomography, shallow geology, flood bank, Quaternary, geophysics in civil engineering

© by Włodzimierz Jerzy Mościcki

This article is distributed under the terms of the Creative Commons Attribution Non-Commercial License, which permits unrestricted non-commercial use, distribution, and reproduction in any medium, provided the original work is properly cited.

Palabras clave
DC resistivity methods, vertical electrical soundings, Electrical Resistivity Tomography, shallow geology, flood bank, Quaternary, geophysics in civil engineering