LGJun 18, 2025

Acoustic Waveform Inversion with Image-to-Image Schrödinger Bridges

arXiv:2506.15346v1h-index: 1Has CodeComput Math Math Phys
Originality Incremental advance
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This work addresses limitations in deep learning-based seismic inversion for geophysics, offering a more efficient method for high-resolution velocity model reconstruction, though it appears incremental as it builds on existing diffusion model approaches.

The paper tackles the problem of acoustic Full Waveform Inversion (FWI) by proposing a conditional Image-to-Image Schrödinger Bridge (cI²SB) framework to reconstruct velocity models from smoothed approximations and seismic signals, outperforming prior diffusion models with fewer neural function evaluations and achieving superior sample fidelity.

Recent developments in application of deep learning models to acoustic Full Waveform Inversion (FWI) are marked by the use of diffusion models as prior distributions for Bayesian-like inference procedures. The advantage of these methods is the ability to generate high-resolution samples, which are otherwise unattainable with classical inversion methods or other deep learning-based solutions. However, the iterative and stochastic nature of sampling from diffusion models along with heuristic nature of output control remain limiting factors for their applicability. For instance, an optimal way to include the approximate velocity model into diffusion-based inversion scheme remains unclear, even though it is considered an essential part of FWI pipeline. We address the issue by employing a Schrödinger Bridge that interpolates between the distributions of ground truth and smoothed velocity models. To facilitate the learning of nonlinear drifts that transfer samples between distributions we extend the concept of Image-to-Image Schrödinger Bridge ($\text{I}^2\text{SB}$) to conditional sampling, resulting in a conditional Image-to-Image Schrödinger Bridge (c$\text{I}^2\text{SB}$) framework. To validate our method, we assess its effectiveness in reconstructing the reference velocity model from its smoothed approximation, coupled with the observed seismic signal of fixed shape. Our experiments demonstrate that the proposed solution outperforms our reimplementation of conditional diffusion model suggested in earlier works, while requiring only a few neural function evaluations (NFEs) to achieve sample fidelity superior to that attained with supervised learning-based approach. The supplementary code implementing the algorithms described in this paper can be found in the repository https://github.com/stankevich-mipt/seismic_inversion_via_I2SB.

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