introduction to pole-dipole array disadvantages advantages
TRANSCRIPT
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Alexey Bobachev, Moscow University
The uThe ussee HalfHalf--Schlumberger array for multiSchlumberger array for multi--electrode resistivity surveyelectrode resistivity survey
! Introduction to Pole-Dipole array! Disadvantages! Advantages! Difference between AMN and MNB sounding curves
as indication of 2D object! Distortion of VES curves by 2D inhomogeneities ! Field example
WEB: http://geophys.geol.msu.ru E-mail: [email protected]
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Introduction to Introduction to PPoleole--DDipole arrayipole array
AV
Ι
M NA
∆UMN
ABElectrodeconfiguration
M
M
BN
NForward pole-dipole array
Reverse pole-dipole array
A
MNB
AMN
AM MN
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PolePole--DDipole and Schlumberger arrayipole and Schlumberger arrayss
Apparent resistivity for pole-dipole and Schlumberger arrays is the same in 1D case
ρAa a a
MN= ρMNB= ρAMNB(Schlumberger)
General case
ρAa
MN +2
a ρMNB=a ρAMNB
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Reference pointReference point for Polefor Pole--Dipole arrayDipole array
Pole-Dipole is asymmetrical array
M NA X
Pseu
do d
epth
Res2dInv, Res2dMod
Electre
x2ipi
O
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Length of infinity line for PoleLength of infinity line for Pole--Dipole arrayDipole array
B∞
AOm
ax
B∞
AOm
ax
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DisadvantagesDisadvantages of Poleof Pole--Dipole arrayDipole array
! Unconventional array for modelling, measurements and presentation of results
! Infinity line! Small value of measured signal! Great number of possible
measurements! All measurements are doing twice
for forward and reverse array! High sensitivity to
inhomogeneities! Segmented VES curve
! Common used software does not support Pole-Dipole array
! A lot of problems! High current! Special software to make
optimal SEQ files! Long time of
measurements! Complicated app. resistivity
pseudo section! Special data preprocessing
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Problems using infinity lineProblems using infinity line
• Additional good wire (300-700m)• Extra work and space to set up infinity• Infinity electrode should be with minimal grounding
resistance• Danger of electrical current leakage from wire,
especially in wet weather• Probability of accident break of wire by somebody• Danger of electrical shock from infinity wire
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Small Small value of measured value of measured signalsignal
Wenner
4 .. 20=MN ∆UMN ∆UAMN
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Great number of possible measurementsGreat number of possible measurementsSEQ files are generated by
“Electre II”
for array with 64 electrodes
Wenner - N quadripoles = 651
AMN – Nq = 1488(for 32 lines)
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High sensitivityHigh sensitivity to to inhomogeneitiesinhomogeneities
Wen
ner
AM
N
Data by Henri Robain, pseudo section from �IPI2win�
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Merger of segmented curveMerger of segmented curve
On level of right segment Mean
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Pseudo section after different segments’ mergerPseudo section after different segments’ merger
Mea
nR
ight
seg
men
t
Data by Henri Robain, pseudo section from �IPI2win�
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Advantages Advantages
! Maximal depth of research! Optimal using of rolling array along profile! Two VES curves for each location! Regularity of geological distortion
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Depth of research for PoleDepth of research for Pole--Dipole andDipole and WennerWennerarraysarrays
AO, AB/3 m a = 1 m
Wenner
AMN
X,m
1a
3a
9a
21a
MN
SEQ file for AMN array is generated by “x2ipi” (Nq=441)
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Depth of research for PoleDepth of research for Pole--Dipole andDipole and WennerWennerarrays for field example (a=4m, arrays for field example (a=4m, NNelel=64)=64)
Wen
ner
AM
N
Data by Henri Robain, pseudo section from �IPI2win�
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Rolling array along profileRolling array along profile1 64
AO, AB/3 m a = 1 m X,m
AMNMNB
Wenner
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Comparing pseudo sections for Comparing pseudo sections for AMN and MNB arraysAMN and MNB arrays
ρAa
MN +2
a ρMNB=a ρAMNB
ρAa
MNa ρMNB
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Comparing pseudo sections for AMN and Comparing pseudo sections for AMN and MNB arrays (field example)MNB arrays (field example)
AM
NM
NB
D –
trans
f.
Data by Henri Robain, pseudo section from �IPI2win� and �IPI_2d�
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Regularity of geological distortionRegularity of geological distortion VES VES curvescurves
AM
NW
enne
r
App. resistivity )ln()ln(
AOa
∂ρ∂
Data by Henri Robain, pseudo section from �IPI2win�
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Difference between AMN and MNB Difference between AMN and MNB sounding curves as indication of 2D sounding curves as indication of 2D
objectobject
by �Res2dMod�
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One vertical boundaryOne vertical boundary
D=Ro_a(AMN)-Ro_a(MNB)R=d D / d X
Modelling by �Ie2dl�, Modin & Bobatchev, transformation by �Ipi_2d�
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Two vertical boundariesTwo vertical boundaries
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Wide 2D objectWide 2D object
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Fault zoneFault zone
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Two 2D objectsTwo 2D objects
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Distortion of VES curves by 2DDistortion of VES curves by 2D shallow depthshallow depthinhomogeneitiesinhomogeneities
! P&C – effects for pole dipole array VES curves! Distortion of Wenner-Alpha and Wenner-Beta array! Median polish of data
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Distortion of VES dataDistortion of VES dataPole-dipole
Wenner-alpha
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Distortion of VES dataDistortion of VES dataPole-dipole
Wenner-alpha
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PP--effect effect –– distortion of VES curve by distortion of VES curve by anomalous anomalous object near DIPOLEobject near DIPOLE--element of arrayelement of array
1
30
0
jj
IUK
jMNEMNU
MNΜΝ
AB
MN
MNΜΝMNMN
ρ≈
∆=ρ
ρ=⋅≈∆
α
→
1050-5-10
0
2
4
10
100
X, m
Dep
th, m
App. res istivity
Current lines distribution by �DC_Flow�
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CC--effect effect –– distortion of VES curve by distortion of VES curve by anomalous anomalous object near POLEobject near POLE--element of arrayelement of array
2
410
0
20-40 -20 0 20 40
A A*
10
20
-40 -20 0 20 40X, м
H, м
H, м
10
20 Anomalous potential
Current lines and potential distribution by �DC_Flow�
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Comparing P and C effectsComparing P and C effects
P P -- effecteffect! Great amplitude
! Does not depend on spacing! Depends on MN length
! Usually the same for both AMN and MNB array
! Does not change VES curve form (reference point – MN center)
C C -- effecteffect! Small amplitude
! Decreases slowly with spacing
! Different sign and usually different amplitude for AMN and MNB array
! Changes VES curve form (reference point – MN center)
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Distortion of WennerDistortion of Wenner--Alpha and Alpha and WennerWenner--Beta arrayBeta array
10 10010
100
2005
10
15
30
100
a, m
App
. res
istiv
ity, O
hm.m
a) Model
b) Variants ofarrays
c) VES curves for Wenner and α β
Wenner α
Wenner α
Wenner β
Wenner β
Modeling by �Res2Dmod�
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Field example forField example for WennerWenner--Alpha (Alpha (NNelel=160)=160)
V-transformation (d Ln(Ro)/d Ln (a))
Data by Henri Robain, pseudo section from �IPI2win�2D inversion by �Res2Dinv�
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P and C effects for different arraysP and C effects for different arrays
Mainly C-effectWenner
P-effectP-effectDipole-Dipole
C-effectC-effectPole-Pole
P-effectC-effectSchlumberger,
Pole-Dipole
Potential electrodesCurrent electrodesArray
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Median polish to decrease P and C effectMedian polish to decrease P and C effect
XX
XX
X
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Median polish on field data (Median polish on field data (NNelel=64, 2 x shift)=64, 2 x shift)
AM
NM
NB
Data by Henri Robain, pseudo section from �IPI2win�, data processing by �Median�
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DD--transformation before and after Median polishtransformation before and after Median polish
Fielddata
After polishby “Median”
Inversionfield data
for MNB arrayby “Res2dInv”
Data by Henri Robain, pseudo section from �IPI_2d�, 2D inversion by �Res2dInv�
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Field exampleField example
! Date: Mai, 1999! Place: South of Madagascar, semi-arid area! Goals: Hydrogeological research.
Problems of water resource: rarity and high mineralization! Geological section:
! Basement –vertical-layered, weathered, metamorphic precambrian rocks (saprolite), depth (0-12 m)
! Upper part – laterite and sand! Equipment: Syscal R2, 64-electrodes array! Array: Pole-Dipole, distance between electrodes – 3 m,
MN – 3 and 9 m, AOmax=94.5 m
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Median polish on field data (Median polish on field data (NNelel=64, 2 x shift)=64, 2 x shift)
AM
NM
NB
Data by Vero Rabemanana, pseudo section from �IPI2win�, data processing �Median�
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2D inversion AMN+MNB array2D inversion AMN+MNB array
Afte
r pol
ish
With
out p
olis
h
Data by Vero Rabemanana, pseudo section from �IPI2win�, 2D inversion by �Res2dInv�
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ConclusionConclusion
The practical use of Half-Schlumberger array for multi-electrode resistivity measurement is more complicate in comparing with Wenner (α,β) array for field measurement, data processing and inversion.
On the other hand, Half-Schlumberger array allows to receive maximum geophysical information by multi-electrode resistivity survey and to improve quality of interpretation, especially for deepest part of geological section.