Wavefield Decomposition for High-Resolution Seismic Diffraction Imaging

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Solution Overview

Problem

Current seismic data processing methods for generating diffraction images are limited by high computational costs, making wave-equation-based techniques impractical for 3D seismic imaging, which is essential for efficient oil and gas exploration.

Innovation Solution

The approach decomposes source and receiver wavefields into opposite propagating directions, generating two seismic images that are then multiplied to produce a diffraction image, effectively suppressing reflectors and enhancing diffractors, thereby reducing computational costs and enabling high-resolution diffraction imaging.

Engineering Contradictions & Design Principles

VSEngineering Contradiction Analysis

1Measurement precision

If wave-equation-based techniques are used for generating diffraction images, then image resolution is improved, but computational cost increases

Engineering Contradiction:
Improveimage resolutionVSAvoidcomputational cost
Core Design Contradiction:
Measurement precisionVSPower

Solution Approach 1:

The wavefield is decomposed into upgoing and downgoing components through directional filtering, separating the imaging process into distinct directional passes. This segmentation allows each component to be processed independently and combined to form the final diffraction image, reducing overall computational burden while maintaining high resolution

Inventive Principle:
Principle #1Segmentation

Solution Approach 2:

The method extracts only the diffractor-related information by multiplying the upgoing and downgoing wavefield images. This extraction process removes reflector components and other unwanted signals, isolating the diffraction events that contain the target subsurface information at lower computational cost

Inventive Principle:
Principle #2Taking out (Extraction)

2Power

If conventional seismic imaging methods are used, then computational cost is reduced, but diffraction image quality deteriorates

Engineering Contradiction:
Improvecomputational costVSAvoiddiffraction image quality
Core Design Contradiction:
PowerVSMeasurement precision

Solution Approach 1:

The method changes the imaging parameter from conventional reflection imaging to diffraction-specific imaging by using the product of upgoing and downgoing wavefields. This parameter change enables the imaging process to selectively enhance diffractors while suppressing reflectors, improving diffraction image quality without proportionally increasing computational cost

Inventive Principle:
Principle #35Parameter changes

3Measurement precision

If full 3D seismic imaging is performed, then exploration accuracy is improved, but processing time increases

Engineering Contradiction:
Improveexploration accuracyVSAvoidprocessing time
Core Design Contradiction:
Measurement precisionVSLoss of time

Solution Approach 1:

The 3D seismic imaging process is segmented into separate directional passes (upgoing and downgoing wavefields). Each pass processes specific directional information independently, allowing for optimized computation and reducing overall processing time while maintaining accurate 3D diffraction imaging capability

Inventive Principle:
Principle #1Segmentation

Solution Approach 2:

The method extracts only the essential diffraction information needed for exploration accuracy by multiplying the directional wavefield components. This extraction eliminates redundant computational steps associated with full conventional imaging while preserving the critical diffraction signals required for accurate hydrocarbon exploration

Inventive Principle:
Principle #2Taking out (Extraction)

Data Source

PatentUS11275190B2Generating diffraction images based on wave equations
Publication Date: 2022.03.15 SAUDI ARABIAN OIL CO
  • US11275190B2 patent drawing
  • US11275190B2 patent drawing
  • US11275190B2 patent drawing

AI summary

A method of generating diffraction images based on wave equations includes generating a source wavefield and a receiver wavefield. Based on the source wavefield, a first source wavefield propagating in a first direction and a second source wavefield propagating in a second direction are generated. Based on the receiver wavefield, a first receiver wavefield propagating in the first direction and a second receiver wavefield propagating in the second direction are generated. A first seismic image is generated based on the first source wavefield and the first receiver wavefield. A second seismic image is generated based on the second source wavefield and the second receiver wavefield. A final seismic image is generated based on the first seismic image and the second seismic image.