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
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
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
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
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
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
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
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
9
Q
Two terminal method
A
- Both V and I from same terminals
- Faster
- Can measure on smaller grids
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
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
12
Q
Interpreting the images produced
A
- White = Low resistance
- Black = High resistance
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