Wave-field Separation for Non-Flat Seismic Recorders

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Solution Overview

Problem

Current seismic data processing techniques struggle to accurately separate up-going and down-going wave fields due to the assumption of a planar recording surface, which is not valid for non-flat acquisition surfaces such as the ocean bottom or varying depths in land seismic data, leading to spurious effects in the final image.

Innovation Solution

A method and system that receive seismic data recorded on a non-flat datum, establish a mathematical relation between transformed seismic data and up-going and down-going wave fields on a planar datum, and solve this relation using an inversion procedure to obtain the wave fields, accounting for the non-planar surface by using wave-field extrapolation terms and specialized computer software.

Engineering Contradictions & Design Principles

VSEngineering Contradiction Analysis

1Measurement precision

If traditional wave-field separation techniques are used assuming a planar recording surface, then the processing is simple and computationally efficient, but the separation accuracy deteriorates when the actual recording surface is non-flat

Engineering Contradiction:
Improvewave-field separation accuracyVSAvoidprocessing complexity
Core Design Contradiction:
Measurement precisionVSDevice complexity

Solution Approach 1:

The patent transforms the seismic data from the time-space domain to the frequency-wavenumber domain, changing the parameter representation to enable accurate wave-field separation on non-flat datums. This domain transformation allows the application of plane datum separation techniques to corrected data, resolving the contradiction between accuracy and complexity.

Inventive Principle:
Principle #35Parameter changes

Solution Approach 2:

The patent introduces an intermediate step of datum correction that transforms non-flat datum seismic data into an equivalent plane datum representation. This intermediary transformation enables the use of simpler plane datum separation algorithms while maintaining accuracy for the original non-flat surface.

Inventive Principle:
Principle #24Intermediary (Mediator)

2Adaptability or versatility

If seismic recorders are deployed on non-flat surfaces to adapt to complex terrain or ocean bottom, then the adaptability improves, but the wave-field separation accuracy deteriorates due to violation of planar surface assumption

Engineering Contradiction:
Improvedeployment flexibilityVSAvoidwave-field separation accuracy
Core Design Contradiction:
Adaptability or versatilityVSMeasurement precision

Solution Approach 1:

The patent applies parameter changes by transforming the spatial domain representation of seismic data to account for the non-flat datum geometry. Through coordinate transformations and wave-field extrapolation, the method adapts the separation algorithm to handle arbitrary datum surfaces while maintaining separation accuracy.

Inventive Principle:
Principle #35Parameter changes

Solution Approach 2:

The patent moves the problem from the spatial domain to the frequency-wavenumber domain, adding a dimensional transformation that enables the handling of non-flat surfaces. This domain change allows the application of plane datum techniques to corrected data through proper wave-field extrapolation.

Inventive Principle:
Principle #17Another dimension (Dimensionality change)

Data Source

PatentUS10310111B2Wave-fields separation for seismic recorders distributed at non-flat recording surfaces
Publication Date: 2019.06.04 CGG SERVICES SAS
  • US10310111B2 patent drawing
  • US10310111B2 patent drawing
  • US10310111B2 patent drawing

AI summary

Apparatus, computer instructions and method for separating up-going and down-going wave fields (U, D) from seismic data recorded within or beneath a body of water, or in general below the surface of the earth. The method includes a step of receiving seismic data (Po, Zo) recorded in the time-space domain with seismic recorders distributed on a first datum, wherein the first datum is non-flat; a step of establishing a mathematical relation between transformed seismic data (P, Z) and the up-going and down-going wave fields (U, D) on a second planar datum; and a step of solving with an inversion procedure, run on a processor, the mathematical relation to obtain the up-going and down-going wave fields (U, D) for the second datum. The second datum is different from the first datum.