Marine Vibrator Source Deconvolution for Ghost Attenuation
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Solution Overview
Problem
Marine seismic surveys face challenges in obtaining accurate, high-resolution images of subterranean formations due to contamination from coherent noise, particularly receiver ghosts and source wavefield effects, which reduce image resolution and obscure geological structures.
Innovation Solution
The use of marine vibrators generating random sweeps allows for continuous recording of seismic data, enabling the attenuation of receiver ghost and source wavefield effects through specific processing techniques, such as deconvolution, to improve image resolution and clarity.
Engineering Contradictions & Design Principles
Engineering Contradiction Analysis
1Productivity
If marine vibrators generate random sweeps for continuous recording, then productivity is improved, but coherent noise contamination increases
Solution Approach 1:
The patent converts the harmful coherent noise (receiver ghosts and source wavefield effects) into a solvable problem through deconvolution processing. By treating the random sweep signature as a known filter, the system can mathematically remove its convolved effect from the recorded data, transforming the harmful contamination into recoverable signal information.
Solution Approach 2:
The patent applies deconvolution processing as a preliminary step in the seismic data workflow. By removing the source signature and receiver ghost effects early in the processing sequence, subsequent imaging operations work with cleaner data, improving overall efficiency and reducing the need for later corrective processing.
2Measurement precision
If deconvolution processing is applied to remove source wavefield effects, then measurement precision is improved, but device complexity increases
Solution Approach 1:
The patent replaces complex physical measurement systems with mathematical processing. Instead of using multiple sensors or complex hardware configurations to directly measure subsurface properties, the system uses deconvolution algorithms to computationally extract the desired information from the recorded wavefield, substituting mechanical/physical complexity with mathematical processing.
3Manufacturing precision
If receiver ghost attenuation is performed through deconvolution, then manufacturing precision is improved, but loss of time increases
Solution Approach 1:
The patent employs continuous random sweeps instead of traditional impulsive sources, enabling continuous data acquisition. The deconvolution process then continuously removes receiver ghost effects throughout the recording, maintaining image quality improvement without requiring间断 processing steps that would increase total processing time.
Applied Scientific Principles
This section explains which scientific principles are used to turn an abstract innovation direction into a practical engineering solution.
Function Achieved in This Case
This approach enhances the quality of seismic images by reducing coherent noise contamination, resulting in higher resolution and more accurate representations of subterranean formations, facilitating better identification of hydrocarbon reservoirs.
Implementation Method 1
A seismic source may be a marine vibrator that emits acoustic energy over a longer time period. The acoustic energy generated by a seismic source spreads out in all directions. A portion of the acoustic energy travels down through the water and into a subterranean formation to propagate as sound waves within the subterranean formation.
Implementation Method 2
At each interface between different types of liquid, rock and sediment, a portion of the sound wave is refracted, a portion is transmitted, and another portion is reflected into the body of water to propagate as a reflected wavefield toward the water surface.
Implementation Method 3
deconvolve the downgoing vertical acceleration wavefield from the upgoing pressure wavefield to generate a subsurface reflectivity wavefield
Data Source
AI summary
Processes and systems described herein are directed to imaging a subterranean formation from seismic data recorded in a marine survey with moving marine vibrators. The marine vibrators generate random sweeps with random sweep signatures. Processes and systems generate an up-going pressure wavefield from measured pressure and vertical velocity wavefield data recorded in the marine survey and obtain a downgoing vertical acceleration wavefield that records source wavefields, directivity, source ghosts, and random signatures of the random sweeps. The downgoing vertical acceleration wavefield data is deconvolved from the up-going pressure wavefield to obtain a subsurface reflectivity wavefield that is used to generate an image of the subterranean formation with reduced contamination from source wavefields, directivity, source ghosts, and random signatures of the random sweeps.


