SC Amplitude correction advanced - Calculate |
Top Previous Next |
|
Calculating Surface consistent amplitude correction operators with user defined domains and trace headers
SC Amplitude correction advanced - Calculate is used to calculate operators for variations in amplitude that are caused by the seismic acquisition geometry, surface irregularities, and/or differences in source-receiver positions. This correction helps ensure that amplitude variations in seismic data are more consistent across the surface, making the data more uniform thus improving the reliability of subsequent interpretation steps. The correction also helps in improving the signal to noise ratio. Different factors such as irregular surface, acquisition geometry parameters, distance between source and receiver (offset) contribute to the variation in amplitudes of the seismic data. To compensate the amplitudes, seismic data is decomposed into to time and frequency domains. Amplitudes are computed for each source-receiver pairs. Unlike SC Amplitude Correction - Calculate, SC Amplitude correction advanced - calculate module calculates the operators as per the user defined domains and the trace headers iteratively. We calculate the scale factors/coefficients/operators for each trace and distribute equally to the each of the domains and their respective selected headers. The scale factors continue calculating for the particular trace 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. After the operators are calculated, the operators are applied to the seismic data using the SC Amplitude correction advanced – Apply module. Prior to that, QC the data by using SC Amplitude correction advanced - QC module. It generates the Source and Receiver amplitude correction map. For more details look at the SC Amplitude correction advanced - QC module.
Input DataItemInput SEG-Y data handle - connect/reference to the Output SEG-Y data handle that will be considered for calculating the amplitude operators. The input data ideally should be noise attenuated, refraction statics applied gathers.Input trace headers - connect/reference to the Output trace headers of the input data.4D mute picking - this is useful in case any noise present before the first breaks/arrivals of the input data. Providing the mute picking file if required.
Read Traces per chunk - Number of traces to read in for the calculation.Desired amplitude level - Set the desired amplitude level. By default, 1.Domains for calculation - Surface Consistent Amplitude correction (SCAMP) can be performed in different domains. Unlike the SC Amplitude correction - Calculate module, here the user has the flexibility to calculate the operators/coefficients for different domains along with different trace headers. In case there are additional trace headers created by the user which are not standard trace headers, these trace headers can be accessed from the headers field and used for calculating the amplitude operators. It is a dynamic approach that allows the user to decompose the data and calculate the optimum amplitude operators/coefficients.
There are many reasons to perform/calculate the SCAMP in different domains.Common Source (CS) domain takes care of the distortions created by the source wavelet or seismic source like dynamite/vibroseis/air gun.Common Receiver(CR) domain will look into the distortions recorded at the receives due to receiver sensitivity and noise levels recorded.Common Offset (CO) domain handles all the amplitude variations caused by the offsets.Common Bin (CDP/CMP) 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. SC Amplitude correction - calculate module calculates the operators for each source, receiver, cmp and offset iteratively. We calculate the scale factors/coefficients/operators for each trace and distribute equally to the each source, receiver, cmp and offsets respectively. The scale factors continue calculating for the particular trace 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. By default, 5%Solver iterations - specify total number of iterations to be performed for calculation. By default, 30. |