Apparent Resistivity in Geophysics



Apparent resistivity is the measure of the earth resistivity  between two point  which correspond to the sensitivity the ground would have if it were homogenous.
Resistivity is one of the properties used to detect any matter, as no two substances have equal resistivity. In electrical resistivity method there are two device used in determining the apparent resistivity, a schlumberger array and wenger array. They are four electrode device, two as current electrode used for introducing current into the earth the other two electrode called the potential electrode used for detecteing the earth voltages.
Electrical resistivity method is one of the geophysical tools used in finding earth surfaces structures (profile and matters). Vertical displacement method or electrical drilling and horizontal profiling method both used in probing the earth’s sub-surface from the surface in electrical resistivity method.
The electrical drilling method is generally to determining the presence and depth of resource like water level, oil level, mineral deposit etc while the horizontal profiling id for determining the  size and spread of a mineral deposit , crude or water spread.
 from the diagram above





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