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Multi-Transient ElectroMagnetics Multi-Transient EM Aug 2007
The need for an EM solution ,[object Object],[object Object],[object Object],[object Object]
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 ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],MTEM Challenges to date
Gas storage monitoring
Shallow Heavy Oil resistivity scale
Thrust Belt
Thrust belt
 
 
 
 
 
 
 
MTEM Global Operations Onshore Offshore
Land acquisition ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
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 ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Well Logs
1D Modeling ,[object Object]
[object Object],[object Object],[object Object],[object Object],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

Editor's Notes

  1. 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