SALIM JABEED ROLL NO-4 APGD IN PETROLEUM EXPLORATION GEOPHYSICS DEPARTMENT OF APPLIED GEOLOGY DIBRUGARH UNIVERSITY PRESENTED BY VIBROSEIS DECONVOLUTION
SALIM JABEEDROLL NO-4APGD IN PETROLEUM EXPLORATION GEOPHYSICS DEPARTMENT OF APPLIED GEOLOGYDIBRUGARH UNIVERSITY
PRESENTED BY
VIBROSEIS DECONVOLUTION
MECHANISM
WHY USE V IBROSEIS METHOD? L I N K S \ U S E O F V B . p p t x
PROBLEMS
• EMBEDDED WAVELET
• MIXED PHASE WAVELET
CROSS CORRELATION OF SWEEP
TRACE
EMBEDDED SWEEP
KLAUDER WAVELET WAVELETLINKS\klauder.pptx
BASICS OF DECONVOLUTIONLINKS\conv.ppt
LEAVES AREFLECTION COEFFICIENT WHEREEVER A CHANGE IN ACOUSTIC IMPEDANCE
TEMPORAL RESOLUTION
TWO ASSUMPTIONS ARE NECESSARY FOR DECONVOLUTION
1. WAVEFORM DOESNOT CHANGES ITS SHAPE
2. MINIMUM PHASELINKS\ZERO PHASE.pptx
METHODS OF MINIMUM PHASE DECONVOLUTION METHODS
FREQUENCY DOMAIN DECONVOLUTION
• FREQUENCY-DOMAIN SWEEP DECONVOLUTION (FDSD) UTILIZES THE CONCEPT THAT CONVOLUTION IN THE TIME-DOMAIN IS EQUIVALENT TO
MULTIPLICATION IN THE FREQUENCY DOMAIN.
•DECONVOLUTION OF THE SWEEP IN THE TIME DOMAIN CAN BE COMPLETED IN THE FREQUENCY DOMAIN THROUGH DIVISION.
THE BASIC CONVOLUTION EQUATION FOR A VIBROSEIS SOURCE ISx(t) = s(t) * r(t)
WHERE X(T) IS THE TRACE RECORDED BY THE GEOPHONE, S(T) IS THE SOURCE SWEEP AND R(T) IS THE REFLECTIVITY.
FOR FDSD IT IS EASIER TO EXPRESS THE BASIC CONVOLUTION EQUATION FOR A VIBROSEIS SOURCE IN THE FREQUENCY-DOMAIN AS
x (ω ) = s(ω )r(ω ). THE SWEEP CAN THEN BE REMOVED IN THE FREQUENCY-DOMAIN BY DIVIDING THE TRACE BY THE SWEEP,
S(ω), giving a solution of:
If the sweep input into the ground is equal to the sweep generated then the result is the exact reflectivity.
MIXED PHASE WAVELET
ZONE NEAR THE SHOT
REFLECTIVITY SEQUENCE OF WAVES
NEAR SURFACE WAVES
EARTH ATTENUATION
The earth filtering e(t), is included in the basic convolution equation for avibroseis source as,
x(t) = r(t) * e(t) * s(t).
In the frequency-domain the convolutional equation is defined as,
X (ω ) = R(ω )E(ω )S(ω ).
THE RESULT IS THE REFLECTIVITY CONVOLVED WITH THE MINIMUM-PHASE WAVELET THAT IS CREATED BY THE EARTH-ATTENUATION
MINIMUM-PHASE DECONVOLUTION SHOULD BE ABLE TO COMPLETELY REMOVE THE MINIMUM-PHASE WAVELET FROM THE DATA
METHODS HAVE BEEN DESIGNED TO REMOVE THE MIXED-PHASE WAVELET THAT IS CREATED THROUGH THE INITIAL VIBROSEIS PROCESSING
A KLAUDER WAVELET FROM THE PROCESSING OFVIBROSEIS SOURCE DATA
CONVERTING THE MIXED-PHASE WAVELET TO ZERO-PHASE BY CONSTRUCTING A MINIMUM-PHASE EQUIVALENT OF THE KLAUDER WAVELET AND FILTERING THE VIBROSEIS RECORD TO MATCH THE PHASE
A MINIMUM-PHASE WAVELET
ONCE THIS IS COMPLETED, IT IS POSSIBLE TO USE MINIMUM-PHASE SPIKING DECONVOLUTION TO REMOVE THE MINIMUM-PHASE WAVELET, CREATING A ZERO-PHASE RECORD
generated wavelet recorded in vibroseis acquisition.
CONCLUSIONS
FREQUENCY-DOMAIN SWEEP DECONVOLUTION USES THE FREQUENCY-DOMAIN TO REPLACE DECONVOLUTION WITH DIVISION.
THIS ELIMINATES THE EMBEDDED KLAUDER WAVELET THAT REMAINS IN THE DATA WHEN CROSSCORRELATION IS UTILIZED.
THIS ASSISTS IN REMOVING THE PROBLEM OF THE MIXED-PHASE WAVELET ASSOCIATED WITH THE KLAUDER WAVELET AND THE MINIMUM-PHASE EARTH FILTER.
THANK YOU