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Geophysics for  Geothermal Exploration Dr. Hendra Grandis Geofisika - ITB
Agenda ,[object Object],[object Object],[object Object],[object Object],[object Object]
Basic concepts of Geophysics ,[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],Basic concepts of Geophysics subsurface  model interpreta t i on
Basic concepts of Geophysics
Basic concepts of Geophysics
Elements of a geothermal system ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],( Cumming  Geoscience)
Role of Geophysics ,[object Object],[object Object],[object Object],[object Object],[object Object],( Cumming  Geoscience)
Role of Geophysics ,[object Object],[object Object],[object Object],[object Object]
Geophysical signatures ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Geophysical signatures ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Geophysical Techniques Geothermal Exploration Standard: MT, T-MT, TDEM, Gravity Legacy: Dipole-Dipole, Tensor Dipole-Bipole Special: VES, AMT, CSAMT, SP, HEM Aeromagnetics, Precision Ground Magnetics Research: Reflection / Refraction Seismic   Special Applications Development: Microgravity, Microearthquake, Subsidence Proprietary: E-Scan, E-Map  Unreviewed: Aquatrack Suspect: Seismic Noise, Low Res Ground Magnetics    Plausible methods with weak technical support ( Cumming  Geoscience)
[object Object],[object Object],[object Object],[object Object],[object Object],Geophysic al Survey Design
[object Object],[object Object],Geophysic al Survey Design
Typical  Geophysical  Survey s ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
 
 
Alteration – Resistivity
 
transmitter generates time varying   EM field     ↓ induces  Eddy currents   in the conductor (Earth)   ↓ generate secondary   magnetic field   ↓ electric and magnetic fields   are sensed at the receiver   Electromagnetic Induction
[object Object],[object Object]
Magnetotellurics  (MT)
MT time series
1-D MT smooth modeling
 
2-D and 3-D interpretation of MT data  in the Bajawa geothermal field Flores, Indonesia  (Uchida et al., 2002)
2-D and 3-D interpretation of MT data  in the Bajawa geothermal field Flores, Indonesia (Uchida et al., 2002)
Karaha-Telaga Bodas
The Karaha-Telaga Bodas  Geothermal System, Indonesia  (Raharjo et al., 2002) ,[object Object],[object Object],[object Object]
The Karaha-Telaga Bodas  Geothermal System, Indonesia  (Raharjo et al., 2002) ,[object Object],[object Object],[object Object]
The Karaha-Telaga Bodas  Geothermal System, Indonesia  (Raharjo et al., 2002)
The Karaha-Telaga Bodas  Geothermal System, Indonesia  (Raharjo et al., 2002)
Repeat SP measurements at the Sumikawa geothermal field, Japan  (Matsushima et al., WGC 2000)
Using surface SP to monitor underground fluid flow - an example from a HDR stimulation (Darnet et al., EAGE 64th Conference, 2002)
SP monitoring during the hydraulic fracturing using the TG-2 well  (Kawakami & Takasugi, EAGE 56th Conference, 1994)
Field set-up of Fluid Flow Tomography, i.e. SP monitoring integrated with mise- à-la-masse (MAM) measurement Reservoir monitoring by a 4-D electrical technique  (Ushijima et al., The Leading Edge, vol. 18 no. 12, 1999)
Hot dry rock (HDR) hydraulic fracturing experiment, Ogachi Electric Power Industry, Akita Perfecture, Japan
 

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Geofisika Geotermal

  • 1. Geophysics for Geothermal Exploration Dr. Hendra Grandis Geofisika - ITB
  • 2.
  • 3.
  • 4.
  • 5. Basic concepts of Geophysics
  • 6. Basic concepts of Geophysics
  • 7.
  • 8.
  • 9.
  • 10.
  • 11.
  • 12. Geophysical Techniques Geothermal Exploration Standard: MT, T-MT, TDEM, Gravity Legacy: Dipole-Dipole, Tensor Dipole-Bipole Special: VES, AMT, CSAMT, SP, HEM Aeromagnetics, Precision Ground Magnetics Research: Reflection / Refraction Seismic Special Applications Development: Microgravity, Microearthquake, Subsidence Proprietary: E-Scan, E-Map Unreviewed: Aquatrack Suspect: Seismic Noise, Low Res Ground Magnetics Plausible methods with weak technical support ( Cumming Geoscience)
  • 13.
  • 14.
  • 15.
  • 16.  
  • 17.  
  • 19.  
  • 20. transmitter generates time varying EM field ↓ induces Eddy currents in the conductor (Earth) ↓ generate secondary magnetic field ↓ electric and magnetic fields are sensed at the receiver Electromagnetic Induction
  • 21.
  • 24. 1-D MT smooth modeling
  • 25.  
  • 26. 2-D and 3-D interpretation of MT data in the Bajawa geothermal field Flores, Indonesia (Uchida et al., 2002)
  • 27. 2-D and 3-D interpretation of MT data in the Bajawa geothermal field Flores, Indonesia (Uchida et al., 2002)
  • 29.
  • 30.
  • 31. The Karaha-Telaga Bodas Geothermal System, Indonesia (Raharjo et al., 2002)
  • 32. The Karaha-Telaga Bodas Geothermal System, Indonesia (Raharjo et al., 2002)
  • 33. Repeat SP measurements at the Sumikawa geothermal field, Japan (Matsushima et al., WGC 2000)
  • 34. Using surface SP to monitor underground fluid flow - an example from a HDR stimulation (Darnet et al., EAGE 64th Conference, 2002)
  • 35. SP monitoring during the hydraulic fracturing using the TG-2 well (Kawakami & Takasugi, EAGE 56th Conference, 1994)
  • 36. Field set-up of Fluid Flow Tomography, i.e. SP monitoring integrated with mise- à-la-masse (MAM) measurement Reservoir monitoring by a 4-D electrical technique (Ushijima et al., The Leading Edge, vol. 18 no. 12, 1999)
  • 37. Hot dry rock (HDR) hydraulic fracturing experiment, Ogachi Electric Power Industry, Akita Perfecture, Japan
  • 38.