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7/28/2019 Ch6 Electrical Natural Field Based
http://slidepdf.com/reader/full/ch6-electrical-natural-field-based 1/19
ELECTRICAL METHODS
NATURAL SOURCE
BASED METHODS
ARTIFICIAL SOURCE
BASED METHODS
SELF
POTENTIALMETHOD
MAGNETO
TELLURICMETHOD
TELLURIC
METHOD
RESISTIVITY
METHOD
INDUCED
POLARISATION
METHOD
ELECTRO-
MAGNETICMETHOD
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CAUSES BEHIND NATURAL OR SPONTANEOUS
POTENTIALS OCCURING IN THE SUBSURFACE
Weathering of sulphide mineral bodies
Variation in rock properties (mineral content) at
geologic contacts
Bioelectric activity of organic material
Corrosion
Thermal and pressure gradients in
underground fluids etc.
The controlling factor in allcases is underground water
SP Method
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Mechanism
Chemical Mechanical
Electro kineticPotential
Or,StreamingPotential
DiffusionOr,
LiquidJunctionPotential
ShaleOr,
NernstPotential
Mineralisation
Potential
Electrochemical or,
Static Self Potential
Background Potentials Main interestduringprospecting
SP Method
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A Few Things
About theMineralizationPotential
Most common mineralisation
potential anomalies occur overPyrite, Chalcopyrite, Pyrrhotite,Sphalerite, Galena & Graphite Amplitudes range from a few
millivolts to one volt e.g. 200mVcan be considered a good SPanomaly
Potentials are almost always
‘-‘ve near the upper end of the body and are quite stable intime
SP Method
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A FewThings
About theBackgroundPotential
Amplitudes vary greatly but
generally are <100 mill volts
Characteristic regionalbackground potentials
Created by fluid streaming,bioelectric activity in
vegetation, varying electrolyticconcentrations in ground waterand other geochemical action Say, gradient of the order of 10mV/1000ft over severalmiles and may be ‘+’ve or’-‘ve.Also, regional gradientassociated with topography.‘-‘ve while going uphill.
SP Method
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SP Method
Negative Center
Oxidizing Zone
(Lower pH
value- pH=2-4,Highly acidic)/
Cathode Half
Cell
Reducing Zone
( Higher pH value-
pH=7-9, Highly
basic/ Anode Half
Cell
Figure: Shows Self-potential mechanism in pyrite (Sato and Mooney, 1960)
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SP Method
Key points about the SP Phenomenon
Two electrochemical half-cell reactions of opposite sign, one
cathodic above the water table, the other anodic at depth.
In the cathodic half- cell there is chemical reduction of the
substance in solution-that is, they gain electrons
In the anodic half-cell an oxidation reaction takes place and
electrons are lost.
The mineral zone itself functions only to transport electrons from
anode to cathode.The magnitude of the overall SP effect is determined by the
difference in oxidation potential (Eh) between the solutions at the two
half-cells.
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SP MethodField Equipments
Figure: A walking –stick SP electrode
What is a walking –stick electrode ?
A walking stick electrode is a type of
non-polarizing electrode that consists
of a metal immersed in a saturated
solution of its own salt, such as Cu
in CuSO4, Zn in ZnSO4 etc., and
contained in a porous pot which
allows the solution to leak slowly and
make contact with the ground.
Why a non polarizing electrode used?
A simple metal rod used as an electrode results
into electrochemical reactions at the ground
contact creating thereby spurious potentials
magnitude of which is comparable to that of the
SP anticipated from the causative body.
Moreover, the magnitude of this spurious potential
varies from place to place. So, a constant
correction factor can not be introduced. Non-
polarizing electrodes diffuse the effect due to the
spurious potentials.
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SP MethodField Equipments
A Potentiometer
The main requirement of the
milli-voltmeter is that its inputimpedance should be large
enough that negligible current will
be drawn from the ground during
the measurement
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SP Method
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SP Method
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SP Method
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SP Method
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SP Method
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SP Method
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SP Method
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Telluric Method
What is telluric current?
Telluric current is an alternating
electric current with a variable
frequency of I Hz or smaller flowing
horizontally in the upper part of the
earth’s crust, the cause of their
generation being induction effect dueto the electric currents in the
ionosphere produced due to the
motion of particles ionized by solar
radiation.
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Telluric Method
RLμvT
f R
2
1h
ΔZZZOS
00
Z
ΔZ
μ
Δμ
With the linear assumption,
0
00S
μ
ΔμZZZ
Some Working
Formula
Here
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