Onshore CSEM > In time domain
  • Step 1: Back to signal processing
    Figure shows transmitter pulse shape, repeated periodically, as a modified squared signal. Secondary fields occur when transmitter current varies.

  • Step 2: Field equipment
    Transient EM is acquired with a magnetic dipole as a transmitter and magnetic field is usually acquired vertically (sometimes horizontally depending on technologies and objectives at stake). With electric current about 300 A in the 26-meter transmitter loop, depth of investigation could reach 800 meters.
    www.geotech.ca

  • Step 3: Transmitter current shapes library (from Allard, 2007)

  • Step 4: Acquisition mode example
    Primary and secondary magnetic fields with a transmitter current shape from HELIGEOTEM system (from Allard, 2007).
    Key information from the figure is that decay of the secondary field is faster for poor conductors during off-times. However, that is not surprising since current loops vanish rapidly in poor conductors.
    That could be easily demonstrated by taking the analogy of an electric circuit crossed by a magnetic field and containing a resistance and a self-inductance.