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How to Measure Bedrock Resistivity

Bedrock is the solid rock underneath the ground, usually beneath soil, sand, clay or gravel. Electrical resistivity is a unit of measurement that determines the resistance that a substance has to electric current. Electrical conductivity is the inverse of resistivity and is a measurement of the ease of current flow. Most rocks, sediments and soils allow at least some electrical flow. Knowing the electrical resistivity can help you to know the type of bedrock underneath the ground, as well as the qualities of that bedrock, such as porosity, permeability, particle size and water content. Rocks tend to have higher conductivity, hence, less resistivity, than sediments and soils. This information has application in the building trades, in helping to determine water flow and in archaeology.

Things You'll Need

  • Electric resistivity meter
  • (or) Conductivity meter
  • Paper and pencil
  • Field markers (or cones)
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Instructions

    • 1

      Design a simple topographic survey of the area that you will be testing for electrical resistivity. Since you cannot measure every point in the area you are testing, determine the number of samplings needed and from where in the field the samples will be taken. Mark these points on the topographic survey. Using that map as a guide, place easily visible field markers in the field where you will be taking the actual readings.

    • 2

      Insert the four electrodes of the electrical resistivity meter in the ground. Probes should be equally spaced 3 feet to 30 feet apart in a straight line, with each probe the same distance from the probe next to it. The farther apart the probes, the deeper in the ground the soil resistivity will be tested. This is why it is important to take multiple readings from the same location. Electrodes should be inserted at shallow depths, typically 6 inches, 1 foot, 1 1/2 feet, 2 feet, 2 1/2 feet. All four probes should be inserted at the same depth for each individual reading.

    • 3

      Move the electricity resistivity meter with electrodes to a second location, using your topographic survey as your guide. Repeat Step 2, taking and recording additional readings at the new location. Continue using your plan to take additional readings until you have completed all samples. Because no sub-surface geography is homogeneous, it is important to take multiple readings at various locations in order to get an accurate picture of the subsurface bedrock.