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The induced polarisation probe measures the charge separation or ‘chargeability’ in porous, water-saturated, mineralised rocks caused by the passage of a low-frequency alternating current. The main cause of induced polarisation is a current-induced electron-transfer reaction between ions of an electrolyte in contact with grains of semi-conducting metallic minerals.

Principle of Measurement:

The probe passes a controlled, alternating current through the formation between two outer electrodes and detects the variation with time of the resulting voltage measured between two inner electrodes after the device is removed. The integrated area under the voltage-time curve is a measure of chargeability.


  • Microprocessor-controlled drive voltage
  • Down-hole integration and ratio computation


  • Chargeability
  • Formation resistance
  • Natural gamma



  • Indication of mineralisation, particularly of disseminated sulphides


  • Qualititive permeability studies


Diameter: 45mm
Length: 1.33 + 1.45m (splits for transport)
Weight: 11kg
Temperature: 0-70⁰C (extended ranges available)
Max. pressure: 20MPa

Operating Conditions

  • Borehole type: open-hole, water-filled

Sales Information

I002102 Induced polarisation probe with natural gamma

Download Induced-polarisation sheet


...Practical Innovation with Global Service & Support...

Robertson Geologging Ltd., 2017

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