Marine Seismic Source Deghosting Using Complex Laplace Transform

Resolve Bottlenecks,
Find Innovative Solutions
Generate Solutions

Solution Overview

Problem

Current methods for deghosting marine seismic data are unstable at spectral notches, leading to irreparable artifacts and reduced resolving power, especially when operating without prior knowledge of the subsurface.

Innovation Solution

The method employs a complex Laplace frequency parameter with a nonzero real part to transform seismic data from the space-time domain to the spectral domain, using an iterative conjugate gradient scheme with a physically-based preconditioner to solve source deghosting equations, ensuring stability across the full seismic bandwidth.

Engineering Contradictions & Design Principles

VSEngineering Contradiction Analysis

1Adaptability or versatility

If conventional deghosting methods are used, then processing can be performed without prior subsurface knowledge, but the results become unstable at spectral notches causing artifacts

Engineering Contradiction:
ImproveAbility to process without prior subsurface knowledgeVSAvoidStability at spectral notches
Core Design Contradiction:
Adaptability or versatilityVSReliability

Solution Approach 1:

The patent changes the fundamental parameter of the frequency domain transformation by using a complex Laplace frequency parameter with a nonzero real part instead of the conventional purely imaginary frequency parameter. This parameter change stabilizes the deghosting process at spectral notches while maintaining the ability to process data without prior subsurface knowledge

Inventive Principle:
Principle #35Parameter changes

Solution Approach 2:

The patent introduces an iterative conjugate gradient scheme with a physically-based preconditioner as an intermediary computational mechanism. This intermediary process solves the system of equations in a stable manner, bridging the gap between the transformed seismic data and the final deghosted result, particularly at problematic spectral notches

Inventive Principle:
Principle #24Intermediary (Mediator)

2Measurement precision

If full-bandwidth deghosting is attempted, then resolving power improves, but instability at spectral notches creates artifacts

Engineering Contradiction:
ImproveResolving powerVSAvoidStability at spectral notches
Core Design Contradiction:
Measurement precisionVSReliability

Solution Approach 1:

By modifying the frequency parameter to include a nonzero real part in the complex Laplace domain, the patent enables stable full-bandwidth processing. This parameter modification allows the system to maintain stability across the entire frequency spectrum including spectral notches, thereby achieving full resolving power without artifacts

Inventive Principle:
Principle #35Parameter changes

Solution Approach 2:

The iterative conjugate gradient scheme incorporates a physically-based preconditioner that provides feedback during the solution process. This feedback mechanism continuously adjusts the solution to maintain stability at spectral notches while preserving the full bandwidth information needed for high resolving power

Inventive Principle:
Principle #23Feedback

Data Source

PatentEP2330443B1Method for full-bandwidth source deghosting of marine seismic streamer data
Publication Date: 2019.02.20 PGS GEOPHYSICAL AS
  • EP2330443B1 patent drawingFigure 1
  • EP2330443B1 patent drawingFigure 2
  • EP2330443B1 patent drawingFigure 3

AI summary

Seismic data recorded in a marine streamer are obtained, sorted as a common receiver gather. A complex Laplace frequency parameter is used to transform the seismic data from a space-time domain to a spectral domain. An iterative conjugate gradient scheme, using a physically-based preconditioner, is applied to the transformed seismic data, to provide a least squares solution to a normal set of equations for a source deghosting system of equations. The solution is inverse-transformed back to a space-time domain to provide source deghosted seismic data, which is useful for imaging the earth's subsurface.