2003
DOI: 10.1016/s0926-9851(03)00002-8
|View full text |Cite
|
Sign up to set email alerts
|

Electric imaging and laboratory resistivity testing for geotechnical investigation of Pusan clay deposits

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

5
58
1

Year Published

2012
2012
2024
2024

Publication Types

Select...
5
4

Relationship

0
9

Authors

Journals

citations
Cited by 137 publications
(69 citation statements)
references
References 10 publications
5
58
1
Order By: Relevance
“…1a). Electrical resistivity decreases with increasing moisture content in soils as reported in various previous studies [1,2,6,9,10,16]. Higher moisture content facilitates conduction of electrical current through movement of ions in pore water.…”
Section: Correlations Of Geotechnical and Resistivity Datasupporting
confidence: 62%
“…1a). Electrical resistivity decreases with increasing moisture content in soils as reported in various previous studies [1,2,6,9,10,16]. Higher moisture content facilitates conduction of electrical current through movement of ions in pore water.…”
Section: Correlations Of Geotechnical and Resistivity Datasupporting
confidence: 62%
“…ER values abruptly drop to values of around 10 Ohm m atthewater content higher than around 20%, because of continuity of pore water (Fukue et al, 1999). Resistivity measured on clay samples collected worldwide varies in a very narrow range (from 1 to 12 Ohm m), and this conductive behaviour makes clayey horizons clearly discernible from overlaying silty and sandy soil layers (Giao et al, 2003). In our case, values of 12 Ohm m and lower were found below 30 cm, with some horizontal variation, and can be attributed to the presence of clay.…”
Section: Resultsmentioning
confidence: 99%
“…Using such techniques, we are able to visualize soil features related to their electrical behavior; as current flux in soil is mostly electrolytic, resistivity is very sensitive to the two components that are mainly involved in charge transfer: the degree of pore water saturation and salinity (Lesch 2005) and the specific surfaces associated to the presence of clay particles (Tabbagh et al 2000). Resistivity is even sensitive to the microstructure of clays, based on lab measurements of worldwide collected clay samples; a first database of clays resistivity was compiled by Giao and coauthors (Giao et al 2003). A soil conductivity survey conducted across different soils showed strong and consistent correlations with clay ).…”
Section: Principles Of Geophysical Techniques For Agriculturementioning
confidence: 99%