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| | -Seismic Reflection
| | -DC Resistivity
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| | -Gravity
| | -Cross-Hole
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| | -Surface Wave Analysis
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DC Resistivity (M-3)

  1. Q: How does it work?
    A: An electrical current is impressed into the ground through two electrodes. Voltages on the surface are
    measured revealing the direction and amount of current flow in the subsurface. These data are interpreted
    in terms of the resistivity (bulk resistance to current flow) of the earth materials.

  2. Q: What are the requirements?
    A:
    A powerful source:
    Special purpose transmitters put up to 3 kilowatts of power into the ground

    A low-noise receiver:
    Multichannel voltmeters capable of resolving a few microvolts

    Low interference from:
    Grounded fences
    Operating power plants or power lines
    Shockable people or animals

    Surface Access:
    electrodes driven or drilled into ground

    Ground truth:
    Well logs
    Drill holes

  3. Q: What are the pitfalls?
    A: Interpretation is one-dimensional (electric drilling) or two-dimensional (electric trenching).

    Ambiguity:
    Conductivity-thickness equivalence.
    Current channeling in conductive environments


  4. Q: What logistics are needed?
    A: Crew size usually 2 or 3 people. Portable if source can be carried.

  5. Q: What are the deliverables?
    A: Plan maps, data presentations, inverse models, forward calculations of the same
    model or cross-section, and a narrative description of the work done.


  6. More detailed information.