Resistivity Method Flashcards

1
Q

Resistivity Survey

A
  • Uses Man-made (active) electric field which is applied to
    the ground via a battery
  • Measures current passing through soil
  • Resistivity of metals = very low because electrons move
    easily through metal
  • Resistivity can distinguish between metals
  • Not effected by nearby cars
  • Cheap and Easy to use
  • Can be used to detect a body buried in a moorland
  • Sample interval of 1m is unlikely to be enough to be
    capable of defining a grave effectively
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2
Q

What is Resistivity and the Resistivity Survey?

A
  • A property of the surface layers of the soil
  • This is an active method, it requires a man-made electric
    field to be created.
  • Used to look for archaeological structure
  • Anomalies can indicate recent burial
  • Accuracy in position = 50cm
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3
Q

Resistance (R)

A
  • Can be measured by applying a current (I) - in amps and
    measuring voltage (V) - in volts
    R = V / I
  • Units = Ω (ohms)
  • Depends on size of area being investigated
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4
Q

Resistivity (ρ)

A
- Calculated from values of resistance (R)
           ρ = (R * area) / L
- Units = Ω.m   (ohm meters)
- Conductors = 0
- Insulators = unlimited
- Human tissue = 2Ωm
- Clay/soil = 1-10Ωm
- Sea water = 0.3Ωm
- Porous rocks =  100-1000 Ωm
- Non-porous rocks = up to 106 Ωm
- Copper = 1.7 x10^-8 Ωm
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5
Q

Changes in resistivity can be due to …

A
  • Soil type (Infill due to burial)
  • Soil density (excavation due to burials)
  • Moisture content (decaying bodies)
  • Chemical content of water
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6
Q

Effects on resistivity in changes in soil

A
  • Decreased density variable ( air and water)
  • Increased air pockets increases
  • Increased water content decreases
  • Decreased salt content increases
  • Presence of large rocks increases
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7
Q

Measurements in Resistivity Surveys

A
  • Two electrodes distance (L) apart and power supply
    generates current (I)
  • V is measured with a voltmeter
  • I is measured with an ammeter
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8
Q

Four terminal method

Wenner Array

A
  • Common in Archaeology
  • V from inner terminals and I from outer terminals
  • Better at averaging out variations due to soil
  • Simplest of arrays
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9
Q

Two terminal method

A
  • Both V and I from same terminals
  • Faster
  • Can measure on smaller grids
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10
Q

The Maths

A
  • A current of 20mA is applied over a distance of 1m and
    gives a voltage of 10V.
    Cross sectional area of 2cm^2
RESISTANCE:
F = 20mA
V = 10 V
R = 10V / 20 x10^-3 A
The resistance (R)  R = V / I = 500Ω

RESISTIVITY:
ρ = (500Ω x 2m^2 ) / 1 m
The Resistivity (ρ) = 1000Ωm

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11
Q

Factors that effect the resistivity survey

A
  • Walk electrode arrangement to successive positions
    along grid lines
    = Easy, Cheap, Non-invasive
  • Distance L determines the smallest features in survey
    map.
    = 0.5 m grid spacing is necessary in order to detect
    grave-sized anomalies
    = for small value of L, the resistivity is of soil close the
    surface
  • Effects due to burial and soil
    = Results different if L is aligned parallel or
    perpendicular to a grave
    = vertical features like pits are less noticeable than
    horizontal features like ditches
    = Sources of noise - variable soil, wires, rough terrain
    = Difficult to detect burials
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12
Q

Interpreting the images produced

A
  • White = Low resistance

- Black = High resistance

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13
Q

Tomography

A
  • Recent advances in this direction
  • Readings are acquired from a large number of electrode
    positions simultaneously
  • Computer programs can be used to unscramble the
    contribution of each element
  • Greater information results in a 2-dimensional image
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