GEOLOGICAL
STRUCTURE:
In
areas where the depth to bedrock is considerably variable, electrical
images can be provide more useful information than is obtained by conventional
resistivity sounding. Providing there is a significant resistivity contrast
at the interface between the bedrock and the overlying strata, reasonably
accurate results may be expected.
CONTAMINATED
GROUNDWATER:
The presence of contaminated groundwater can often be recognized by
a decrease in formation resistivity, since the latter is primarily dependent
on the resistivity of the pore water.