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  2. Spontaneous potential - Wikipedia

    en.wikipedia.org/wiki/Spontaneous_potential

    It is generally accepted that the streaming potential across the mud-cake is compensated by that across the shale. As such, in most cases, the spontaneous potential measured is only related to the electrochemical potential. Electrochemical potential (E C) is the sum of liquid junction or diffusion potential (E J), and membrane potential (E M)

  3. Spontaneous potential logging - Wikipedia

    en.wikipedia.org/wiki/Spontaneous_potential_logging

    Spontaneous potential log, commonly called the self potential log or SP log, is a passive measurement taken by oil industry well loggers to characterise rock formation properties. The log works by measuring small electric potentials (measured in millivolts) between depths with in the borehole and a grounded electrode at the surface.

  4. Well logging - Wikipedia

    en.wikipedia.org/wiki/Well_logging

    Well logging, also known as borehole logging is the practice of making a detailed record (a well log) of the geologic formations penetrated by a borehole.The log may be based either on visual inspection of samples brought to the surface (geological logs) or on physical measurements made by instruments lowered into the hole (geophysical logs).

  5. Electrical resistivity tomography - Wikipedia

    en.wikipedia.org/wiki/Electrical_resistivity...

    2D resistivity inversion of ERT data Deployment of a permanent electrical resistivity tomography profile on a longitudinal section of an active landslide.. Electrical resistivity tomography (ERT) or electrical resistivity imaging (ERI) is a geophysical technique for imaging sub-surface structures from electrical resistivity measurements made at the surface, or by electrodes in one or more ...

  6. Physical geodesy - Wikipedia

    en.wikipedia.org/wiki/Physical_geodesy

    Potential is expressed as gravity times distance, m 2 ·s −2. Travelling one metre in the direction of a gravity vector of strength 1 m·s −2 will increase your potential by 1 m 2 ·s −2 . Again employing G as a multiplier, the units can be changed to joules per kilogram of attracted mass.

  7. Induced polarization - Wikipedia

    en.wikipedia.org/wiki/Induced_polarization

    Induced polarization is a geophysical method used extensively in mineral exploration and mining operations. Resistivity and IP methods are often applied on the ground surface using multiple four-electrode sites. In an IP survey (and when making resistivity measurements), capacitive properties of the subsurface materials are determined as well.

  8. Geopotential - Wikipedia

    en.wikipedia.org/wiki/Geopotential

    Geopotential is the potential of the Earth's gravity field.For convenience it is often defined as the negative of the potential energy per unit mass, so that the gravity vector is obtained as the gradient of the geopotential, without the negation.

  9. Telluric current - Wikipedia

    en.wikipedia.org/wiki/Telluric_current

    The electric potential on the Earth's surface ... Magnetotellurics – Electromagnetic geophysical ... Telluric traverse and self potential data release in ...