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Vol 229
Pages:
3-12
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RUS ENG
Article
Geology

Collaborative interpretation of the data obtained by resistivity and ground penetrating radar methods for assessing the permeability of sandy clay soils

Authors:
D. A. Lalomov1
V. V. Glazunov2
About authors
  • 1 — Ph.D. Senior Geophysicist Fertoing, Ltd.
  • 2 — Ph.D., Dr.Sci. professor Saint-Petersburg Mining University
Date submitted:
2017-09-17
Date accepted:
2017-11-06
Date published:
2018-02-22

Abstract

A method for estimating the filtration factor of sandy clay soils is considered on the basis of a joint interpretation of the data of a set of methods of engineering electrical exploration, including electrical resistivity tomography and ground penetrating radar studies. The solution of this problem is based on the use of known empirical connections between the imaginary and real parts of the complex dielectric permittivity, specific electrical resistance, and Q factor. An example of the effective joint use of the ground penetrating radar and non-contact electrical resistivity tomography shows how to obtain qualitative and quantitative estimates of a changing filtration factor in a draining road layer. It is necessary to use precise engineering geological information in order to provide the required estimates. The proposed approach makes it possible to describe continuous profiles of a pavement and underlying layers by ground penetrating radar and electrical resistivity tomography, as well as to assess soil properties when conducting an electrical survey from the surface of asphalt concrete pavement. Recommendations for the implementation of the developed methods of complex engineering and geophysical research are given for solving issues of repair work design, supervision, and quality control of road construction.

Область исследования:
Geology
Keywords:
groundpenetratingradar non-contact electrical resistivity tomography complex dielectric permittivity specific electrical resistance Q factor clay content filtration factor pavement monitoring
10.25515/pmi.2018.1.3
Go to volume 229

Funding

The authors are grateful to the staff of the InzhGeofizika company (St.Petersburg) and to its Director General A.I.Kulikov for the rendered assistance in field works and geophysical equipment provided

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