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Induced polarization (IP) is a geophysical imaging technique used to identify the electrical chargeability of subsurface materials, such as ore. The polarization effect was originally discovered by Conrad Schlumberger when measuring the resistivity of rock. The survey method is similar to electrical resistivity tomography (ERT), in that an electric current is transmitted into the subsurface through two electrodes, and voltage is monitored through two other electrodes. The IP survey can be made in time-domain and frequency-domain mode:

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  • Polarisasi terimbas (in)
  • Induced polarization (en)
  • Метод вызванной поляризации (ru)
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  • Мé‎тод вы́званной поляриза́ции (ВП) — метод электроразведки, основанный на изучении возникающих вторичных токов и поляризации в телах под действием первичного электрического и магнитного полей. Используется в основном для поиска вкрапленных руд и подземных вод. (ru)
  • Induced polarization (IP) is a geophysical imaging technique used to identify the electrical chargeability of subsurface materials, such as ore. The polarization effect was originally discovered by Conrad Schlumberger when measuring the resistivity of rock. The survey method is similar to electrical resistivity tomography (ERT), in that an electric current is transmitted into the subsurface through two electrodes, and voltage is monitored through two other electrodes. The IP survey can be made in time-domain and frequency-domain mode: (en)
  • Metode polarisasi terimbas atau polarisasi terinduksi merupakan metode geofisika aktif. Metode ini merupakan pengembangan dari metode geolistrik pemetaan (resistivitas). Pada metode polarisasi terimbas, arus listrik dinjeksikan melalui elektrode arus pada selang waktu tertentu kemudian dihentikan. Ketika sumber arus dihentikan voltmeter yang berada pada elektrode potensial tidak langsung menunjuk nol namun turun secara perlahan-lahan. Gejala ini disebut sebagai efek polarisasi terimbas. Efek polarisasi terimbas inilah yang menjadi elemen dasar pada metode IP. Efek polarisasi terimbas bisa terjadi karena tanah atau batuan memiliki unsur kapasitif yaitu kemampuan suatu medium untuk menyimpan muatan listrik ketika diberi arus listrik. (in)
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  • January 2022 (en)
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  • Induced polarization (IP) is a geophysical imaging technique used to identify the electrical chargeability of subsurface materials, such as ore. The polarization effect was originally discovered by Conrad Schlumberger when measuring the resistivity of rock. The survey method is similar to electrical resistivity tomography (ERT), in that an electric current is transmitted into the subsurface through two electrodes, and voltage is monitored through two other electrodes. Induced polarization is a geophysical method used extensively in mineral exploration and mine operations. 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. The IP survey can be made in time-domain and frequency-domain mode: In the method, the voltage response is observed as a function of time after the injected current is switched off or on. In the mode, an alternating current is injected into the ground with variable frequencies. Voltage phase-shifts are measured to evaluate the impedance spectrum at different injection frequencies, which is commonly referred to as spectral IP. The 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. (en)
  • Metode polarisasi terimbas atau polarisasi terinduksi merupakan metode geofisika aktif. Metode ini merupakan pengembangan dari metode geolistrik pemetaan (resistivitas). Pada metode polarisasi terimbas, arus listrik dinjeksikan melalui elektrode arus pada selang waktu tertentu kemudian dihentikan. Ketika sumber arus dihentikan voltmeter yang berada pada elektrode potensial tidak langsung menunjuk nol namun turun secara perlahan-lahan. Gejala ini disebut sebagai efek polarisasi terimbas. Efek polarisasi terimbas inilah yang menjadi elemen dasar pada metode IP. Efek polarisasi terimbas bisa terjadi karena tanah atau batuan memiliki unsur kapasitif yaitu kemampuan suatu medium untuk menyimpan muatan listrik ketika diberi arus listrik. Efek polarisasi ini menyebabkan timbulnya potensial ekstra yang disebut over voltage. Nilai over voltage akan semakin besar apabila frekuensi arus yang diinjeksikan rendah atau mendekati arus searah. Ketika arus yang diinjeksikan berhenti maka potensial polarisasi akan terdeteksi dan akan turun secara perlahan disebut decay potential. Decay potential merupakan indikator besarnya polarisasi. Apabila potensial ini direkam dan dihitung harga integralnya maka besaran yang dihitung dinamakan chargeability (M). Semakin besar nilai polarisasi maka nilai chargeabilitynya juga semakin besar. Metode ini sering digunakan dalam pertambangan terutama eksplorasi logam mulia seperti emas dan perak. (in)
  • Мé‎тод вы́званной поляриза́ции (ВП) — метод электроразведки, основанный на изучении возникающих вторичных токов и поляризации в телах под действием первичного электрического и магнитного полей. Используется в основном для поиска вкрапленных руд и подземных вод. (ru)
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