DC Resistivity Studies of Shallow Geology in the Vicinity of Vistula River Flood Bank in Czernichów Village (Near Kraków in Poland)
, , and | Jun 13, 2014
Published Online: Jun 13, 2014
Page range: 63 - 70
DOI: https://doi.org/10.2478/sgem-2014-0008
Keywords
© 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 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.