Geophysics GPh3202: Electromagnetic Methods
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Questions and Answers

What is a key advantage of EM methods over contacting electrical resistivity surveys?

  • Greater penetrating depth
  • Improved data quality
  • Faster survey times (correct)
  • No requirement for inductive coupling
  • What is the main difference between Active and Passive Electromagnetic methods?

  • The type of measurement used
  • The frequency of the signal
  • The source of the electromagnetic field (correct)
  • The depth range of investigation
  • What is one of the main applications of electromagnetic methods in terms of resource assessment and exploration?

  • Mineral resource assessment and exploration (correct)
  • Geothermal resource investigations
  • Contaminant plume mapping
  • Hydrocarbon reserve monitoring
  • In which type of land model do EM surveys counter survey difficulties?

    <p>Models with very conductive uppermost layers</p> Signup and view all the answers

    What is the primary factor that affects the level of inquiry in TEM?

    <p>Loop size</p> Signup and view all the answers

    What is the relationship between the distance between the transmitter and receiver coils and the depth range under investigation in FEM?

    <p>Directly proportional</p> Signup and view all the answers

    What is the main parameter measured by Electromagnetic and Electric methods?

    <p>Electrical conductivity</p> Signup and view all the answers

    What is the purpose of Electromagnetic methods?

    <p>To measure the electrical conductivity of the Earth's materials</p> Signup and view all the answers

    Which of the following is NOT a typical use of electromagnetic methods?

    <p>Seismic data acquisition</p> Signup and view all the answers

    What are the three types of measurements that can be conducted using Electromagnetic methods?

    <p>Mapping, profiling, and sounding</p> Signup and view all the answers

    Study Notes

    Basic Concepts

    • Electromagnetic methods are categorized into two types: Active (controlled source) methods and Passive (natural field) methods.
    • Controlled source methods include GBR and MagnetoMetric resistivity, while natural field methods include Magnetotelluric and Telluric Methods.
    • Electromagnetic methods can be classified as frequency-domain (FEM) or time-domain (TEM) systems.
    • These methods measure the electrical conductivity (resistivity) of the Earth's materials, which is the same measured parameter as Electric methods, but with different measurement methods.
    • Electromagnetic methods can be used for land-based and airborne surveys, marine surveys, and borehole logging.
    • Surveys can be conducted through three types of measurements: mapping, profiling, and sounding.
    • Electromagnetic methods provide information about the variation in conductivity within a certain depth range.

    TEM Method

    • The level of inquiry is closely correlated with the loop size, recording time interval, and shut-off time in TEM.
    • TEM methods have a greater penetrating depth than electric methods.

    Advantages

    • One of the main advantages of EM methods is that they do not require direct contact with the ground.
    • EM surveys can be made faster than equivalent surveys using contacting electrical resistivity.
    • EM methods counter some survey difficulties with land models having very conductive uppermost layers.

    Uses

    • Electromagnetic methods are applicable for:
      • Mineral resource assessment and exploration
      • Investigating and monitoring hydrocarbon reserves
      • Surveys of groundwater
      • Mapping contaminant plumes
      • Geothermal resource investigations
      • Contaminated land mapping
      • Landfill surveys
      • Finding man-made and natural cavities
      • Location of geological faults
      • Geological mapping and Permafrost mapping
      • UneXploded Ordnance (UXO)

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    Description

    This quiz covers the basics of electromagnetic methods in geophysics, including active and passive methods, and their applications in geology.

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