Broadband Single-Sensor Seismic Data Processing Workflow
Find Innovative SolutionsGenerate Solutions
Solution Overview
Problem
Existing seismic data processing workflows for broadband single-sensor single-source land seismic data fail to restore received signals to desired broadband zero-phase wavelets, particularly struggling with signal smearing and noise impact, which hampers the recovery of low and high-frequency signals and structural interpretation.
Innovation Solution
The approach involves deterministic differential filtering to convert seismic traces from receiver-measured particle motion to source-represented motion, followed by deterministic inverse-Q filtering to correct for earth absorption, and iterative derivation of surface-consistent filters and attributes for noise removal and deconvolution, enhancing temporal resolution and signal recovery.
Engineering Contradictions & Design Principles
Engineering Contradiction Analysis
1Manufacturing precision
If traditional seismic processing workflows are used, then processing simplicity is maintained, but signal recovery quality deteriorates due to inability to restore broadband zero-phase wavelets
Solution Approach 1:
The processing workflow is segmented into distinct functional modules: deterministic differential filtering module, deterministic inverse-Q filtering module, and iterative surface-consistent filtering module. Each module addresses specific signal degradation aspects, allowing complex processing to be broken down into manageable, targeted operations that collectively restore broadband zero-phase wavelets
Solution Approach 2:
Deterministic differential filtering is applied as a preliminary step to convert particle motion measurements before subsequent processing. This preliminary action prepares the signal in the correct form for inverse-Q filtering, enabling more effective signal recovery in later stages without requiring complete reprocessing
2Manufacturing precision
If deterministic differential filtering and inverse-Q filtering are applied, then low and high-frequency signal recovery is improved, but processing computational load increases
Solution Approach 1:
The iterative surface-consistent filtering module dynamically adjusts filter parameters based on statistical analysis of the seismic data. Rather than using fixed computational parameters, the system adapts filtering strength and characteristics to the actual signal properties, optimizing computational efficiency while maintaining frequency recovery quality
Solution Approach 2:
Deterministic inverse-Q filtering applies parameter changes to compensate for frequency-dependent attenuation. By modeling and reversing the effects of earth absorption with specific Q-values, the process restores both low and high-frequency components that would otherwise be lost, achieving comprehensive frequency spectrum recovery
3Manufacturing precision
If iterative surface-consistent filtering is used, then noise removal and deconvolution effectiveness is enhanced, but processing time increases
Solution Approach 1:
The iterative surface-consistent filtering module uses feedback from statistical analysis of filtered traces to continuously refine filter parameters. Each iteration uses the results of previous filtering to adjust subsequent filtering operations, progressively improving noise removal effectiveness while converging to an optimal solution that balances quality and processing time
4Measurement precision
If broadband zero-phase wavelet restoration is achieved, then structural interpretation accuracy is improved, but processing complexity increases
Solution Approach 1:
The deterministic filtering modules serve multiple functions: they correct particle motion representations, compensate for frequency attenuation, and prepare signals for subsequent imaging. This multi-functionality reduces the need for separate dedicated processing steps, achieving wavelet restoration without proportionally increasing overall system complexity
Data Source
AI summary
A method for processing broadband single-sensor single-source land seismic data includes receiving seismic traces, the seismic traces generated using at least one source and at least one receiver; converting the seismic traces from particle motion measured by the at least one receiver to particle motion represented by the at least one source by applying a deterministic differential filtering operation; applying a deterministic inverse-Q filtering operation on the converted seismic traces; processing the inverse-Q filtered seismic traces using a set of surface-consistent filter and attribute corrections; and generating a seismic image based on the processed seismic traces.


