Induced Polarization
Get Induced Polarization essential facts below. View Videos or join the Induced Polarization discussion. Add Induced Polarization to your topic list for future reference or share this resource on social media.
Induced Polarization

Induced polarization (IP) is a geophysical imaging technique used to identify the electrical chargeability of subsurface materials, such as ore.[1] The method is similar to electrical resistivity tomography, in that an electric current is transmitted into the subsurface through two electrodes, and voltage is monitored through two other electrodes. Induced polarization (IP) is a geophysical method used extensively in mineral exploration and mine operations. The IP survey is very similar to electrical resistivity tomography (ERT). Resistivity and IP methods are often applied on the ground surface using multiple four-electrode sites. In an IP survey, in addition to resistivity measurement, capacitive properties of the subsurface materials are determined as well. As a result, IP surveys provide additional information about the spatial variation in lithology and grain-surface chemistry.

IP survey can be made in time-domain and frequency-domain mode. In time domain Induced polarization method, voltage decay is observed as a function of time after the injected current is switched off. In frequency-domain Induced polarization mode, an alternating current is injected into the ground with variable frequencies. Voltage phase-shifts are measured to evaluate impedance spectrum at different injection frequencies, which is commonly referred to as spectral IP.

IP method is one of the most widely used techniques in mineral exploration and mining industry and it has other applications in hydrogeophysical surveys, environmental investigations and geotechnical engineering projects.[2]


Time domain

Typical transmitted current waveform and potential response for time domain resistivity and induced polarization measurements.

Time domain IP methods measure considers the resulting voltage following a change in the injected current. The time domain IP potential response can be evaluated by considering the mean value on the resulting voltage, known as integral chargeability[1] or by evaluating the spectral information and considering the shape of the potential response, for example describing the response with a Cole-Cole model.[3]

Frequency domain

Frequency domain IP methods (see Spectral Induced Polarisation) use alternating currents (AC) to induce electric charges in the subsurface, and the apparent resistivity is measured at different AC frequencies.


  1. ^ a b K. Zonge; J. Wynn; S. Urquhart (2005). 9. Resistivity, Induced Polarization, and Complex Resistivity. Society of Exploration Geophysicists. pp. 265-300. 
  2. ^ [1]
  3. ^ Pelton, W. H.; Ward, S. H.; Hallof, P. G.; Sill, W. R.; Nelson, P. H. "MINERAL DISCRIMINATION AND REMOVAL OF INDUCTIVE COUPLING WITH MULTIFREQUENCY IP". Geophysics. 43 (3): 588-609. doi:10.1190/1.1440839. 

Further reading

  • Kearey, Philip; Michael Brooks (1991). An Introduction to Geophysical Exploration (Second ed.). Blackwell Science. ISBN 0-632-02923-4. 

External links

  • [2] Example IP equipment and image results

  This article uses material from the Wikipedia page available here. It is released under the Creative Commons Attribution-Share-Alike License 3.0.



Top US Cities