2007 | OriginalPaper | Chapter
Direct Current Resistivity Methods
Authors : Knut Seidel, Gerhard Lange
Published in: Environmental Geology
Publisher: Springer Berlin Heidelberg
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Direct current (dc) resistivity methods use artificial sources of current to produce an electrical potential field in the ground. In almost all resistivity methods, a current is introduced into the ground through point electrodes (C
1
, C
2
) and the potential field is measured using two other electrodes (the potential electrodes P
1
and P
2
), as shown in
Fig. 4.3-1
. The source current can be direct current or low-frequency (0.1 – 30 Hz) alternating current. The aim of generating and measuring the electrical potential field is to determine the spatial resistivity distribution (or its reciprocal - conductivity) in the ground. As the potential between P
1
and P
2
, the current introduced through C
1
and C
2
, and the electrode configuration are known, the resistivity of the ground can be determined; this is referred to as the “apparent resistivity”.