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Depth of Current Penetration Current flow tends to occur close to the surface. Current penetration can be increased by increasing separation of current electrodes. Electrode Arrays An electrode array consists of two electrodes at which DC current flows into and out of the ground plus two electrodes between which the potential difference at the surface is measured . The apparent resistivity measured by different arrays is not the same, because the geometric factor K is different. Wenner: Alternating +ve and –ve near-surface regions cancel, and main response is from depth, which is fairly uniform laterally. Good for determining depth variations in 1-D Earth. B. Schlumberger: Equivalent vertical resolution to Wenner (distance between contours), but deep response is concave upwards. More sensitive to lateral variation in Earth. C.Dipole-Dipole: Poor vertical resolution as contours spaced widely. Lobes from each dipole penetrate deeply indicating good sensitivity to lateral variation at depth. Resistivity profiling or imaging is a method for investigating the subsurface by measuring the capacity of earth materials to pass electrical current. resistivity imaging can resolve small

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Depth of Current PenetrationCurrent flow tends to occur close to the surface. Current penetration can be increased by increasing separation of current electrodes.Electrode Arrays An electrode array consists of two electrodes at which DC current flows into and out of the ground plus two electrodes between which the potential difference at the surface is measured .

The apparent resistivity measured by different arrays is not the same, because the geometric factor K is different.

Wenner: Alternating +ve and ve near-surface regions cancel, and main response is from depth, which is fairly uniform laterally. Good for determining depth variations in 1-D Earth. B. Schlumberger: Equivalent vertical resolution to Wenner (distance between contours), but deep response is concave upwards. More sensitive to lateral variation in Earth. C.Dipole-Dipole: Poor vertical resolution as contours spaced widely. Lobes from each dipole penetrate deeply indicating good sensitivity to lateral variation at depth.Resistivity profiling or imaging is a method for investigating the subsurface by measuring the capacity of earth materials to pass electrical current. resistivity imaging can resolve small and irregular anomalies even in areas of complex subsurface geometry.

pseudosection

Increasing the electrode separation, increases depth of penetration.Repeating the same profile with different electrode spacing, allows construction of a pseudosection of apparent resistivity.Pseudosection is constructed by plotting measured value at intersection of lines drawn at 45o from current and potential dipoles, and contouring resulteLktrode arraysAn electrode array is a configuration of electrodes used for measuring either an electric current or voltage. Some electrode arrays can operate in a bidirectional fashion, in that they can also be used to provide a stimulating pattern of electric current or voltage.

Common arrays include:

Schlumberger (Wenner)

Wenner alpha

Wenner beta

Wenner gamma

Pole-pole

Dipole-dipole

Pole-dipole

Equatorial dipole-dipoleSignal-contribution sectionsNear-surface inhomogeneities strongly influence the choice of array. Their

effects are graphically illustrated by contours of the signal contributions that

are made by each unit volume of ground to the measured voltage, and hence

to the apparent resistivity

Depth of Current Penetration Current flow tends to occur close to the surface. Current penetration can be increased by increasing separation of current electrodes.