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Fracture Characterization at Reykjanes
Using Time-Lapse Electric Potential
Data
Lilja Magnúsdóttir and Magnús Þór Jónsson
GEORG Geothermal Workshop 2016
Lilja Magnúsdóttir and Magnús Þór Jónsson
Outline
Introduction
Electrical Resistivity
iTOUGH2 Simulations
Electric Field Solved Using
iTOUGH2
Inverse Analysis
Summary
2
Lilja Magnúsdóttir and Magnús Þór Jónsson
Introduction
Fracture characterization is crucial
to ensure adequate supply of
geothermal fluids and efficient
thermal operation of wells
Interconnected conductive fractures
control mass and heat transport in
the system
IDDP-2 is expected to be drilled
down to 5 km depth at Reykjanes
Proposed project and workplan
discussed for characterizing
fracture networks at Reykjanes
3
Source: iddp.is
Lilja Magnúsdóttir and Magnús Þór Jónsson
Objective
Water with less electrical conductivity than the brine will be
injected into the reservoir
Electrical potential will increase as the injected water fills
fracture paths
Time-lapse electric potential data is related to the
connectivity of the fracture network
Estimate fracture connectivity at Reykjanes using direct
current electric potential measurements during water
injection
4
Lilja Magnúsdóttir and Magnús Þór Jónsson
Electrical Resistivity
Fractures initially filled with
brine (sea water)
Water injected to enhance
contrast in resistivity between
rock and fractures
5
Source: Ucok et al., 1980
Lilja Magnúsdóttir and Magnús Þór Jónsson 6
Electrical Resistivity
Direct current
injected and
electric potential
measured
Electric potential
difference/Resistivity
changes between
wells as fluid is
injected
Lilja Magnúsdóttir and Magnús Þór Jónsson
Electrical Resistivity
7
Source: Northwest Geophysical Associates
Lilja Magnúsdóttir and Magnús Þór Jónsson
Simulations using iTOUGH2
Develop a model of Reykjanes to a depth of >5 km
Use EOS1SC in iTOUGH2 to model heat source
Develop a discrete fracture model of Reykjanes using an
approach by Karimi-Fard et al.
iTOUGH2 used to simulate the flow of injected water
iTOUGH2 used to simulate electric
field
Inverse analysis used with resistivity
measurements to estimate fracture
network
8
Lilja Magnúsdóttir and Magnús Þór Jónsson
Electric Field Solved Using iTOUGH2
Ohm’s law:
Darcy’s law:
Analogy between Darcy’s law and Ohm’s law
9
VJ  
IQm  
Darcy’s law: Ohm’s law:
Flux of: Water q Charge J
Potential: Pressure p Voltage V
Medium
property:
Hydraulic
conductivity
k/μ
Electrical
conductivity
σ
Source: Hyperphysics, Georgia State University
p
k
q 

k
Lilja Magnúsdóttir and Magnús Þór Jónsson
Inverse Analysis
10
Lilja Magnúsdóttir and Magnús Þór Jónsson
Summary
Proposed project and workplan discussed for estimating
fracture networks at Reykjanes
Resistivity will be measured as water is injected into the
reservoir
iTOUGH2 will be used to model the flow of water in the
reservoir as well as the electric field as the resistivity
changes
Inverse analysis used with resistivity measurements to
estimate fracture network
We thank the Icelandic Research Fund for the
support
11
Lilja Magnúsdóttir and Magnús Þór Jónsson
Acknowledgements
Icelandic Research Fund
IDDP
DEEPEGS
HS orka
ÍSOR
Vatnaskil
12
Lilja Magnúsdóttir and Magnús Þór Jónsson
Questions?
Cust
omiz

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A1 ​ Magnús Þór Jónsson Fracture Characterization at Reykjanes Using Time-Lapse Electric Potential Data

  • 1. Fracture Characterization at Reykjanes Using Time-Lapse Electric Potential Data Lilja Magnúsdóttir and Magnús Þór Jónsson GEORG Geothermal Workshop 2016
  • 2. Lilja Magnúsdóttir and Magnús Þór Jónsson Outline Introduction Electrical Resistivity iTOUGH2 Simulations Electric Field Solved Using iTOUGH2 Inverse Analysis Summary 2
  • 3. Lilja Magnúsdóttir and Magnús Þór Jónsson Introduction Fracture characterization is crucial to ensure adequate supply of geothermal fluids and efficient thermal operation of wells Interconnected conductive fractures control mass and heat transport in the system IDDP-2 is expected to be drilled down to 5 km depth at Reykjanes Proposed project and workplan discussed for characterizing fracture networks at Reykjanes 3 Source: iddp.is
  • 4. Lilja Magnúsdóttir and Magnús Þór Jónsson Objective Water with less electrical conductivity than the brine will be injected into the reservoir Electrical potential will increase as the injected water fills fracture paths Time-lapse electric potential data is related to the connectivity of the fracture network Estimate fracture connectivity at Reykjanes using direct current electric potential measurements during water injection 4
  • 5. Lilja Magnúsdóttir and Magnús Þór Jónsson Electrical Resistivity Fractures initially filled with brine (sea water) Water injected to enhance contrast in resistivity between rock and fractures 5 Source: Ucok et al., 1980
  • 6. Lilja Magnúsdóttir and Magnús Þór Jónsson 6 Electrical Resistivity Direct current injected and electric potential measured Electric potential difference/Resistivity changes between wells as fluid is injected
  • 7. Lilja Magnúsdóttir and Magnús Þór Jónsson Electrical Resistivity 7 Source: Northwest Geophysical Associates
  • 8. Lilja Magnúsdóttir and Magnús Þór Jónsson Simulations using iTOUGH2 Develop a model of Reykjanes to a depth of >5 km Use EOS1SC in iTOUGH2 to model heat source Develop a discrete fracture model of Reykjanes using an approach by Karimi-Fard et al. iTOUGH2 used to simulate the flow of injected water iTOUGH2 used to simulate electric field Inverse analysis used with resistivity measurements to estimate fracture network 8
  • 9. Lilja Magnúsdóttir and Magnús Þór Jónsson Electric Field Solved Using iTOUGH2 Ohm’s law: Darcy’s law: Analogy between Darcy’s law and Ohm’s law 9 VJ   IQm   Darcy’s law: Ohm’s law: Flux of: Water q Charge J Potential: Pressure p Voltage V Medium property: Hydraulic conductivity k/μ Electrical conductivity σ Source: Hyperphysics, Georgia State University p k q   k
  • 10. Lilja Magnúsdóttir and Magnús Þór Jónsson Inverse Analysis 10
  • 11. Lilja Magnúsdóttir and Magnús Þór Jónsson Summary Proposed project and workplan discussed for estimating fracture networks at Reykjanes Resistivity will be measured as water is injected into the reservoir iTOUGH2 will be used to model the flow of water in the reservoir as well as the electric field as the resistivity changes Inverse analysis used with resistivity measurements to estimate fracture network We thank the Icelandic Research Fund for the support 11
  • 12. Lilja Magnúsdóttir and Magnús Þór Jónsson Acknowledgements Icelandic Research Fund IDDP DEEPEGS HS orka ÍSOR Vatnaskil 12
  • 13. Lilja Magnúsdóttir and Magnús Þór Jónsson Questions? Cust omiz