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Multi-Transient ElectroMagnetics Multi-Transient EM Aug 2007
The need for an EM solution Seismic methods determine structure The structure may reveal a potential reservoir (in general a porous rock bounded by a cap) The porous rock contains a fluid (water or hydrocarbons, or a mixture) but seismics cannot usually determine the nature of that fluid – drill! Resistivity – a physical rock property determined through EM – can make that distinction – drill in the right place!
Resistivities of Rocks Diagram courtesy Henri Brasse http://userpage.fu-berlin.de~hbrasse
Fluid saturation and rock properties  P-wave velocity is affected only slightly by hydrocarbon saturation in a porous rock. Resistivity can vary by more than an order of magnitude. Picture redrawn from Wilt M. and Alumbaugh D. 1998, The Leading Edge 17, 487-492.
Direct Resistivity Indicator Seismic traces Seismic amplitudes and attributes Logging measurements Logging before drilling MTEM Resistivity
MTEM for resistivity MTEM is sensitive to transverse resistance.  Red is more resistive.  Stronger resistivity comes from: Thicker interval Higher saturation Higher porosity Less clay and shale
Cases Gas storage monitoring Imaging Heavy Oil  Imaging in structurally complex subsurface Imaging thrust belt.  Imaging where seismic and drilling is very expensive Locating steam flood front in SAGD production monitoring  Identifying channel sands with low acoustic impedance contrast Proving up reserves to increase reserves-production ratio De-risking drilling location decisions.  MTEM Challenges to date
Gas storage monitoring
Shallow Heavy Oil resistivity scale
Thrust Belt
Thrust belt
 
 
 
 
 
 
 
MTEM Global Operations Onshore Offshore
Land acquisition Surface conditions successfully operated in Farmland Desert Jungle Plantation Urban Rice paddies Muskeg Open prairie Beach / Littoral
MTEM Hardware
Receiver station and battery Receiver box and battery in the line.  Box with acquisition and telemetry electronics. Grounded with earth electrode.
Source Buggy and Unit Source buggy with generator and source unit.  Source engineer with Zonge and control electronics.
Source Electrodes An array of 1 to 40 electrodes hammered into 80-100cm into the ground.  Fenced off (3m) and manned when source cables are connected.
Source Safety system Source activation and emergency shut off at the source electrode array.  Emergency shutoff cuts power to the entire system.
Source electrode transport Source electrode transport buggy.  Low ground pressure buggy to transport the 40 electrodes per source pole location.
Land Operations
A Step Change in the use of EM Input   Recording (combination of Earth and System Responses) Airwave Earth response
Impulse response - land Offset = 1 km Air Wave Earth Impulse  Response
1D model Source 1A.m Source Receiver (V) x = 1000m 500m 20 Ohm.m 500 Ohm.m Dx 25m
Impulse response Effect of fluid saturation Offset = 1 km
Impulse response – land Convolution with a system response Air Wave
Impulse response measurements Full Waveform Amplitudes Travel Time
Multi-Transient Theoretical PRBS In red Measured Signal In black
Deconvolution Input amps at source Output volts at receiver Deconvolved impulse response (ohms/m 2 /s)
Deconvolved Data – common offset  Air Wave High peak amplitude and early arrival time indicate a resistor.
Data Processing Apparent resistivity Step Response Integration Peak picking Impulse Response
Inversion model and response Offset 1000m
Inversion model and response Offset 2000m
Inversion model and response Offset 2500m
Inversion model and response Offset 3000m
Inversion model and response Multi-offsets 2000m, 2500m and 3000m
Results summary 4 ways to detect hydrocarbons 2-D DC resistivity inversion Traveltime to resistivity mapping 1-D Occam Inversion 1800m Common offset section
What does MTEM provide Feasibility study – desktop Feasibility study – field assessment Survey design Acquisition Processing Inversion Technical/interpretation support 3D modeling, advanced inversions
Well Logs
1D Modeling % difference in impulse response .
We take a collaborative approach with the client Problem solving, asset-based  Oilfield services contractor Support asset team with their interpretation and decisions How do we work? Top Reservoir from seismic
Multi-Transient EM
Inversion model and response Offset 1500m
Inversion model and response Offset 3500m

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Multi-Transient ElectroMagnetics

  • 2. The need for an EM solution Seismic methods determine structure The structure may reveal a potential reservoir (in general a porous rock bounded by a cap) The porous rock contains a fluid (water or hydrocarbons, or a mixture) but seismics cannot usually determine the nature of that fluid – drill! Resistivity – a physical rock property determined through EM – can make that distinction – drill in the right place!
  • 3. Resistivities of Rocks Diagram courtesy Henri Brasse http://userpage.fu-berlin.de~hbrasse
  • 4. Fluid saturation and rock properties P-wave velocity is affected only slightly by hydrocarbon saturation in a porous rock. Resistivity can vary by more than an order of magnitude. Picture redrawn from Wilt M. and Alumbaugh D. 1998, The Leading Edge 17, 487-492.
  • 5. Direct Resistivity Indicator Seismic traces Seismic amplitudes and attributes Logging measurements Logging before drilling MTEM Resistivity
  • 6. MTEM for resistivity MTEM is sensitive to transverse resistance. Red is more resistive. Stronger resistivity comes from: Thicker interval Higher saturation Higher porosity Less clay and shale
  • 7. Cases Gas storage monitoring Imaging Heavy Oil Imaging in structurally complex subsurface Imaging thrust belt. Imaging where seismic and drilling is very expensive Locating steam flood front in SAGD production monitoring Identifying channel sands with low acoustic impedance contrast Proving up reserves to increase reserves-production ratio De-risking drilling location decisions. MTEM Challenges to date
  • 9. Shallow Heavy Oil resistivity scale
  • 12.  
  • 13.  
  • 14.  
  • 15.  
  • 16.  
  • 17.  
  • 18.  
  • 19. MTEM Global Operations Onshore Offshore
  • 20. Land acquisition Surface conditions successfully operated in Farmland Desert Jungle Plantation Urban Rice paddies Muskeg Open prairie Beach / Littoral
  • 22. Receiver station and battery Receiver box and battery in the line. Box with acquisition and telemetry electronics. Grounded with earth electrode.
  • 23. Source Buggy and Unit Source buggy with generator and source unit. Source engineer with Zonge and control electronics.
  • 24. Source Electrodes An array of 1 to 40 electrodes hammered into 80-100cm into the ground. Fenced off (3m) and manned when source cables are connected.
  • 25. Source Safety system Source activation and emergency shut off at the source electrode array. Emergency shutoff cuts power to the entire system.
  • 26. Source electrode transport Source electrode transport buggy. Low ground pressure buggy to transport the 40 electrodes per source pole location.
  • 28. A Step Change in the use of EM Input Recording (combination of Earth and System Responses) Airwave Earth response
  • 29. Impulse response - land Offset = 1 km Air Wave Earth Impulse Response
  • 30. 1D model Source 1A.m Source Receiver (V) x = 1000m 500m 20 Ohm.m 500 Ohm.m Dx 25m
  • 31. Impulse response Effect of fluid saturation Offset = 1 km
  • 32. Impulse response – land Convolution with a system response Air Wave
  • 33. Impulse response measurements Full Waveform Amplitudes Travel Time
  • 34. Multi-Transient Theoretical PRBS In red Measured Signal In black
  • 35. Deconvolution Input amps at source Output volts at receiver Deconvolved impulse response (ohms/m 2 /s)
  • 36. Deconvolved Data – common offset Air Wave High peak amplitude and early arrival time indicate a resistor.
  • 37. Data Processing Apparent resistivity Step Response Integration Peak picking Impulse Response
  • 38. Inversion model and response Offset 1000m
  • 39. Inversion model and response Offset 2000m
  • 40. Inversion model and response Offset 2500m
  • 41. Inversion model and response Offset 3000m
  • 42. Inversion model and response Multi-offsets 2000m, 2500m and 3000m
  • 43. Results summary 4 ways to detect hydrocarbons 2-D DC resistivity inversion Traveltime to resistivity mapping 1-D Occam Inversion 1800m Common offset section
  • 44. What does MTEM provide Feasibility study – desktop Feasibility study – field assessment Survey design Acquisition Processing Inversion Technical/interpretation support 3D modeling, advanced inversions
  • 46. 1D Modeling % difference in impulse response .
  • 47. We take a collaborative approach with the client Problem solving, asset-based Oilfield services contractor Support asset team with their interpretation and decisions How do we work? Top Reservoir from seismic
  • 49. Inversion model and response Offset 1500m
  • 50. Inversion model and response Offset 3500m

Editor's Notes

  • #2: Multi Transient ElectroMagnetics. Table of content: (sorry Add 3 to numbers above 9!) 2-5 What MTEM is. Logging Before Drilling 6-9 MTEM applications 10-11 EM techniques 12-21 MTEM method 22-26 – France test and Reciprocity 27-40 RTA 41-46 Processing and Inversion 47-49 Data Examples 49-50 Recording System 51 Conclusion