Resistivity in Archaeology: A Tool for Identifying Underground Objects?

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In summary, resistivity and resistance are two different properties that are used in identifying objects under the ground. Resistivity is a local property that measures the intrinsic resistance of a material to electric current, while resistance is a global property that depends on various factors. By measuring resistivity, one can gather clues about the composition of underground objects, as different materials have different resistivity values. This can be helpful in determining the presence of certain objects such as metal.
  • #1
Johntoby
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Hi all, I am writing an assignment at the moment, asking me to report on the use of resistivity in identifying objects under the ground.
I've gotten confused as to whether resistivity is used at all - surely resistance is all that is needed? For example, in any multi probe resistive survey, the resistance is measured between points to give a map of resistances and then show areas of abnormality. Where does resistivity come into it?

Thanks very much
 
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Welcome to PF!

Hi Johntoby! Welcome to PF! :smile:
Johntoby said:
Where does resistivity come into it?

Different materials have different resistivity … can you write something about that? :wink:
 
  • #3
Resistivity is a local property: specifically it is the magnitude of electric field required to produce 1 amp per unit cross section of current in the material. It doesn't depend on the length or thickness of the material, so it is a good measure of the intrinsic resistance of a certain material to electric current.

Resistance is a global property: it's the voltage needed to make 1 amp of current to flow between two pre-defined points. Clearly, this depends on where the points are, how thick the conductor is, how long it is, etc. It's typically what you measure.

Why is this useful ? Resistivity gives you clues about what is underground. If you know the resistivity is low in certain areas, then it's likely you might find some metal in there because metal has a lower resistivity. So if you put two probes either side of this metal, you'll measure a lower resistance than if you put two probes between a lump of coal!
 

Related to Resistivity in Archaeology: A Tool for Identifying Underground Objects?

What is resistivity in archaeology?

Resistivity in archaeology refers to the measurement of the resistance of a material to the flow of electricity. It is commonly used in archaeological surveys to detect buried features and structures by measuring the differences in electrical conductivity between the ground and any buried objects.

How is resistivity used in archaeology?

Resistivity is used in archaeology as a non-intrusive method to detect and map buried features, such as walls, ditches, and pits. By passing an electrical current through the ground and measuring the resistance, archaeologists can create a detailed map of the subsurface, which can help identify potential areas for excavation.

What are the benefits of using resistivity in archaeology?

One of the main benefits of using resistivity in archaeology is that it is a non-destructive method, meaning that it does not require any digging or excavation. It is also relatively quick and cost-effective compared to other geophysical methods. Additionally, resistivity can provide detailed information about the size, shape, and depth of buried features, which can help inform excavation strategies.

What are the limitations of resistivity in archaeology?

While resistivity can be a useful tool in archaeological surveys, it does have some limitations. The method is most effective in areas with high soil moisture, which can limit its use in dry or rocky environments. Additionally, resistivity can only detect features that have a significant contrast in electrical conductivity, so it may not be effective in identifying smaller or shallow features.

How does resistivity compare to other geophysical methods in archaeology?

Resistivity is often used in conjunction with other geophysical methods, such as ground-penetrating radar and magnetometry, to provide a more comprehensive understanding of the subsurface. Each method has its strengths and limitations, and the combination of multiple methods can provide a more accurate and detailed picture of buried features and structures.

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