SC Deconvolution - calculate |
Top Previous Next |
|
Calculating Surface Consistent Deconvolution
What is Surface Consistent? A Single Operator calculated for all traces that have the same surface point location in common. Why do we perform surface consistent? During the seismic acquisition survey design phase we design the survey parameters for a normal situation however when we acquire the data in different terrains the conditions will be quite different. Due to sub-surface nature, the data is recorded with many distortions due to various reasons like the survey design, acquisition instruments or the sub-surface change in properties. Surface consistent deconvolution assumes that a seismic trace consists of the convolution of a number of components which go together to produce the seismic trace. For example, each shot, each receiver position, each CDP and each trace offset (or channel number) contributes its own spectral modification to the seismic trace. Surface consistent deconvolution attempts to reverse this process by extracting the original log spectra (for each shot, each receiver) from all of the original input data. This is done by averaging the log spectra for each shot, each receiver, each CDP and each offset (Channel) and then using a Gauss-Seidel iterative technique to isolate the individual components. Using the Gauss-Seidel method, it computes the deconvolution filters for each frequency band to improve the resolution of the seismic wavelet.
Input DataItemInput SEG-Y data handle - connect/reference to the input data that went through all the denoise procedures and statics.Input trace headers - connect/reference to the output trace headers of the input seismic gather.4D mute picking - Mute is useful if there is any data above the first arrivals. It is necessary to remove any noise the first breaks. Provide the input mute picks file if necessary.Use trace vector on disk - This option is used when the input data size is big. By default, FALSE. If checked, the user should provide the Input traces data handle.Input traces data handle - connect/reference to the Output traces data handle of the Open seismic traces module. This option isn't available for "Read seismic traces" or "Read SEG-Y traces" modules.
Read Traces per chunk - Number of traces to read in for the calculationDesired amplitude level - Set the desired amplitude level. By default, 1.Domain for calculation { CS CR, CS CR Offset, CS CR Offset Bin } - Surface Consistent Deconvolution (SCDCN) will be performed in 3 different domains. There are many reasons to perform/calculate the SCDCN in different domains.Common Source domain takes care of the distortions created by the source wavelet or seismic source like dynamite/vibroseis/air gun.Common Receiver domain will look into the distortions recorded at the receives due to receiver sensitivity and noise levels recorded.Common Offset domain handles all the amplitude variations caused by the offsets.Common Bin takes care of any distortions spatially.
Mute taper - It is used to avoid any sharp boundaries. This option is required when the user used the input mute file.Advance for Solver - This section deals with the solver parameters. For solving, we use Gauss-Seidel method to resolve all the distortions of the seismic wavelet and improves the spatial and temporal resolution of the seismic wavelet in an iterative method. We do the iteration until the parameters are stabilized (convergence). This is controlled by the threshold value where the difference between the successive iteration processes should be smaller and smaller as we proceed further.Threshold Factor - specify the threshold value that should be considered for stopping the iteration process where the successive iteration values reaches the user defined threshold factor/value.Solver iterations - specify total number of iterations to be performed for calculation.Maximum offset - specify the maximum offset to be considered.Minimum offset - specify the minimum offset to be considered.Offset step - specify the offset step sizeUse azimuth domain - In case the seismic distortions are caused due to azimuths (distortions due to the directional variations). By default, FALSE. If checked, the user has to be provide the number of azimuths to be considered in the calculation.Number of azimuths - specify the number of azimuths considered for the calculation.Restore - This sections deals with the restoration of the seismic reflection energy by performing the deconvolution in time or frequency domain.Deconvolution Domain { Time (Predictive), Frequency } - choose the preferred domain from the drop down menu to perform the deconvolution. By default, Time (Predictive).DeconvolDomain - Frequency - In case the deconvolution domain is frequency, the deconvolution calculation happens in the frequency domain where the data is transformed from time domain to frequency domain by using Fourier transform. In that case, the user needs to provide the phase domain parameters.Phase Domain { Minimum Phase, Zero Phase } - Naturally, Deconvolution expects the data in minimum phase where it is easier to distinguish between the signal and noise (seismic energy is concentrated at the very beginning) unlike the zero phase wavelet where the energy is distributed symmetrically with a slight delay of time.DeconvolDomain - Time (Predictive) - Deconvolution will be performed in time domain.Predictive interval - specify the predictive interval valueNoise - specify the percentage white noise added to the deconvolution process to stabilizes the result. |