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Real-world application of deep learning in large-scale seismic interference attenuation: A case study in the Camie field of Angola

Jing Sun, Song Hou

arXiv:2610.09663v1physics.geo-phcs.AI

TL;DR

Published evidence for SI attenuation across very large real-world survey areas was limited. This paper applies a DNN-based workflow to a large real-world project and compares it with a conventional geophysical algorithm. The DNN workflow required less than half the conventional algorithm’s computational time and generally improved processing quality.

  • Problem

    Published evidence for SI attenuation across very large real-world survey areas was limited.

    Source: INTRODUCTION · p. 9
  • Method

    The paper applies a DNN-based SI-attenuation workflow to a large real-world project and compares it with a conventional geophysical algorithm.

    Source: INTRODUCTION · p. 8, DISCUSSION · p. 26
  • Results

    Less than half the computational time of the conventional geophysical algorithm was required by the DNN workflow, which also showed general improvement in processing quality.

    Source: DISCUSSION · p. 26
  • Takeaways & Limitations

    The case study supports the DNN-based workflow as a promising SI-attenuation option for the Camie survey.

    Source: DISCUSSION · p. 26

    Overfitting is identified as a critical concern.

    Source: DISCUSSION · p. 28

Abstract

from arXiv · show

In marine seismic acquisition, seismic interference (SI) occurs when energy from nearby external seismic source(s) is captured. It typically appears as coherent noise with linear or non-linear movement and varying amplitudes across different sail lines. SI is commonly observed and poses a challenge for seismic data processing. We present a case history of a previously proposed deep neural network (DNN)-based workflow applied for SI attenuation across a marine seismic block in the Camie Field of Angola. This field survey covers over 345 km2 and is marked by the challenge of multiple SI types. The employed DNN-based workflow performs SI attenuation in the common shot domain based on a supervised learning framework: a small subset of the SI-contaminated data was first processed by a conventional geophysical algorithm to obtain an estimate of the SI noise, which was then manually blended with the SI-free common shot gathers from the same survey to generate the training pairs. To ensure signal fidelity, several techniques were applied to improve the DNN's performance. A key highlight of this case history is its scale: this represents a real-world, large-scale processing project and we present a comprehensive comparison of the DNN-based workflow with the conventional geophysical algorithm across the entire survey block, focusing on both processing quality and processing time. The results demonstrate the outstanding performance of the employed DNN-based workflow, which achieved higher SI removal accuracy, with less signal leakage and more complete SI removal. The promising results of this application also open up possibilities for integrating deep learning into other seismic denoising tasks. In addition, we discuss the limitations of this case history, aiming to provide insights for future research and applications in the field.

INTRODUCTION

The introduction reviews conventional seismic-interference attenuation approaches and their limitations when interference varies or resembles desired reflections. It then frames a full-block, large-scale DNN application to diverse SI in Angola’s Camie Field in light of the limited scale and industrial validation of earlier work.

INTRODUCTION

  • SI varies in incidence and amplitude across sail lines and can arrive from ahead, broadside, or astern of the recording vessel.Its amplitude depends in part on the external source’s distance, while incidence varies with its orientation relative to receivers.Source: INTRODUCTION · pp. 2–3
  • High-amplitude SI can overlap much weaker subsurface reflections, making it difficult to separate interference from desired seismic signals.SI can remain consistent over large distances, increasing concern when it overlaps the reflections.Source: INTRODUCTION · p. 3
  • Geophysical SI attenuation methods broadly either break coherence through data resorting and denoising or model the noise for subtraction.The second group depends strongly on building an accurate SI model (Jansen 2013).Source: INTRODUCTION · pp. 5–6
  • A shipping-lane grid method requires prior lane knowledge, can be time-consuming, and has accuracy limited by grid size.A method based on detected apices fails when apices are absent from the seismic record.Source: INTRODUCTION · p. 7
  • Conventional methods may require labor-intensive manual parameter selection for varying SI moveout and struggle when SI comes from multiple directions or has a dip like the underlying signal.These conditions make separating SI from desired reflections especially challenging.Source: INTRODUCTION · p. 7
  • Earlier DNN studies showed potential on field data, but had not validated SI attenuation at industrial standards or compared full-block processing with a field-tested geophysical algorithm.A prior workflow was tested on two sail lines, while no full-block large-scale comparison had been presented.Source: INTRODUCTION · p. 8
  • The study applies Sun et al. (2023)’s DNN workflow to the entire 345 km2 Camie marine block, presenting a large-scale real-world case study.The introduction describes it as the first published case study covering an area of this scale.Source: INTRODUCTION · pp. 8–9
  • The comparison covers common-shot and stacked CMP examples, high-frequency RMS measures across sail lines and the survey, and total processing times.The timing comparison is not fully controlled across a shared computational environment, but reflects production scenarios with diverse resources and project-specific optimization.Source: INTRODUCTION · p. 9
  • SI from other seismic vessels and local fishing vessels had diverse characteristics, including simultaneous sources from two directions, flat profiles, and dips resembling desired signals.Moveout- or dip-based filters can leave residual noise or leak useful signals when SI resembles primary reflections.Source: INTRODUCTION · p. 11

THE EMPLOYED DNN-BASED WORKFLOW AND GEOPHYSICAL ALGORITHM

The Camie workflow trained a U-Net using synthetic SI-contaminated shots built from SI models and naturally SI-free data, then applied it to most of the survey. It also used signal-fidelity procedures and compared performance with conventional geophysical processing.

THE EMPLOYED DNN-BASED WORKFLOW AND GEOPHYSICAL ALGORITHM

  • Training data came from 5 sail lines × 6 cables, representing 6% of the survey’s SI-contaminated data and covering the previously observed SI types.A conventional geophysical algorithm processed these selected gathers to estimate SI models.Source: THE EMPLOYED DNN-BASED WORKFLOW AND… · p. 12
  • The conventional algorithm preconditioned common-shot gathers, used rank-reduction denoising, and modelled SI with sparse tau-p inversion.Complex wavelet adaptation combined a complex Morlet wavelet frame with unary complex Wiener filters.Source: THE EMPLOYED DNN-BASED WORKFLOW AND… · p. 12
  • The study shuffled the conventional-algorithm SI model and blended it with naturally SI-free shots from a survey with 5 sail lines × 3 cables, augmenting both via vertical translation and amplitude modulation.Source: THE EMPLOYED DNN-BASED WORKFLOW AND… · p. 12
  • The DNN used adjacent shots on both sides of the to-be-processed shot as additional input channels and was trained to predict both the SI and a blend of the SI-free shot with the intact shot.It followed a standard U-Net encoder-decoder structure with skip connections.Source: THE EMPLOYED DNN-BASED WORKFLOW AND… · pp. 13, 15
  • Once trained, the DNN can attenuate SI noise in the remaining SI-contaminated survey data (91% of this case-study dataset); reprocessing the 6% used to generate training pairs could be commercially justified, but raises research concerns.Source: THE EMPLOYED DNN-BASED WORKFLOW AND… · pp. 13–14
  • Evaluation compared the trained U-Net with the conventional algorithm on unseen survey data in shot and stacked CMP domains, including processing time.The authors state that examples were not from the exact same cables as the training data, to avoid repeatedly using the same dataset for DNN training and testing.Source: THE EMPLOYED DNN-BASED WORKFLOW AND… · pp. 15–16

Comparison in Processing Quality

Across shot-gather, CMP-stack, and survey-wide comparisons, the DNN workflow generally achieved more complete SI removal with less signal damage and leakage than conventional processing. Both methods remained limited in the most heavily contaminated areas.

Comparison in Processing Time

For the 345 km2 survey, the DNN-based workflow took approximately 54 hours versus 143.5 hours for the conventional algorithm, and its trained application processed each sail line in 15 minutes.

Comparison in Processing Time

  • Conventional processing took 3.5 hours per sail line, excluding parameter optimization; scaling this to 41 sail lines gives approximately 143.5 hours.Source: Comparison in Processing Time · p. 25
  • After training, the DNN processed each sail line in 15 minutes, or 10.25 hours across the survey; SI-model preparation took 8.75 hours and data preparation plus training took 35 hours.The reported total DNN time accounts for potential reprocessing of the SI-contaminated sail line used to provide an SI model for training pairs.Source: Comparison in Processing Time · p. 25
  • Approximately 54 hours for the DNN-based workflow versus 143.5 hours for the conventional algorithm—roughly one-third the time using the same computational resources.The survey covered 345 km2.Source: Comparison in Processing Time · p. 25
  • For larger surveys, DNN training time is not expected to increase significantly, while application-phase efficiency benefits are expected to scale up.Source: Comparison in Processing Time · p. 25

DISCUSSION

The discussion presents the DNN workflow as promising for SI attenuation while emphasizing limits tied to training coverage, evaluation dependency, and transfer to new surveys.

DISCUSSION

  • Less than half the conventional algorithm’s computational time was required, and the DNN generally improved processing quality, especially in poor-SnR regions or where SI dips resembled signal dips.The time includes data preparation and DNN training.Source: DISCUSSION · p. 26
  • The DNN attenuated SI despite training on incomplete, discontinuous SI models because those models covered expected SI types; SI too weak for conventional detection was absent from training and could also evade detection.Source: DISCUSSION · pp. 26–27
  • When the entire survey is SI-contaminated, conventional processing must produce both SI models and pseudo-SI-free training shots, introducing uncertainty into DNN performance.Source: DISCUSSION · p. 27
  • The evaluation excluded the 6% of raw data used to construct training pairs because its SI models were derived from those shots, creating partial dependency and fairness concerns despite possible production use.Source: DISCUSSION · p. 27
  • Overfitting remains a concern despite augmentation and pairing strategies, while training SI models may not capture field complexity; sampling multiple sail lines broadens coverage of SI types.Source: DISCUSSION · p. 28
  • Survey-specific training limits generalization: models may require retraining, fine-tuning, or domain adaptation for new data distributions, and future work should test robustness and other coherent noise types.Source: DISCUSSION · p. 28

CONCLUSIONS

In the 345 km2 Camie Field survey in Angola, the U-Net workflow outperformed conventional processing in quality and time, while remaining dependent on geophysical labels and expert input.

  • The study applied a U-Net workflow to attenuate SI across the entire 345 km2 Camie Field survey, presenting the largest-ever real-world comparison of this kind.The survey was in Angola.Source: CONCLUSIONS · p. 29
  • The DNN workflow outperformed the conventional algorithm in processing quality and time across shot gathers, CMP stacks, and deep high-frequency RMS analysis.The comparison covered the full marine seismic survey block.Source: CONCLUSIONS · p. 29
  • Future work includes investigating robustness and capability, applying the workflow to other surveys, evaluating alternative architectures, and exploring physics-based constraints to enhance generalization.Source: CONCLUSIONS · p. 29
  • The supervised workflow depends on geophysical algorithms for labels covering inference-time SI types; training-pair quality is crucial, and selecting good samples requires human effort and experience.The paper notes that developing better geophysical algorithms remains important.Source: CONCLUSIONS · p. 29
  • For large-scale real-world processing, a solid conventional algorithm remains essential, and experienced practitioners must balance effort across geophysical and deep-learning components.The conventional algorithm provides the foundation for the DNN to further improve SI attenuation.Source: CONCLUSIONS · p. 29
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