A conditional diffusion-based wavefield propagator that advances seismic wavefields recursively from one time step to the next, conditioned by a short history of recent wavefield time steps, the velocity model, and the wavefield time step index is introduced.
Abstract
Seismic wavefield simulation is fundamental to seismology, but conventional finite-difference (FD) methods remain limited by numerical dispersion and stability constraints, which often require dense spatial grids and small time steps and thereby severely limit the effectiveness of iterative inversion workflows. We introduce a conditional diffusion-based wavefield propagator that advances seismic wavefields recursively from one time step to the next. Instead of learning an unconditional data distribution of wavefield evolution, the model is conditioned by a short history of recent wavefield time steps (snapshots), the velocity model, and the wavefield time step index, allowing it to represent the conditional transition between adjacent physical states. By training the network to directly predict the clean next wavefield snapshot, this strong physical conditioning makes it possible to replace the iterative reverse diffusion process with a single network evaluation for each predicted snapshot. To improve stability over long recursive rollouts, we further introduce a causal time-weighted loss, in which adaptive weights, accumulated as exponential moving averages of per-snapshot training errors, emphasize training directions that are consistent with the forward propagation sequence and reduce the amplification of one-step prediction errors. Because the learned propagator is tied to the temporal spacing of the training snapshots rather than to the FD stability limit, it can advance the wavefield using a physical time step ten times larger than that required by the underlying solver. Experiments on the Overthrust, SEG/EAGE, and Marmousi models show that the proposed method accurately reproduces wavefield snapshots and shot gathers and achieves an end-to-end speedup of 2.17 x over a GPU-accelerated tenth-order staggered-grid FD implementation under matched hardware conditions.
Full waveform inversion (FWI) estimates subsurface velocity from seismic recordings, but its ill-posedness and nonlinearity make accurate reconstruction strongly dependent on initialization and prior information. Diffusion posterior sampling provides a learned geological prior, yet directly coupling its denoiser to the...
Chen Min, Hao-Wen Jiang, Zheng Ma et al.· 0 citations
Scalar travel-time relations can identify propagation geometry without velocity inputs, ray labels or equation supervision during learning. Physical interpretation is applied after learning through the high-frequency isotropic eikonal relation (Aki and Richards, 2002). Here we show that local value differences constrai...
Wave Function Backpropagation is introduced, a wave-parameterized learning formulation in which neural responses are represented by learnable amplitude, wavenumber, angular frequency, and phase and the present evidence supports the effectiveness of the wave representation.
Accurate shear wave velocity (VS) estimates are essential for seismic inversion and reservoir characterisation. The cost and operational requirements of dipole sonic logging can limit the availability of measured VS. Predicting VS from conventional well logs is a practical alternative. Empirical relationships can be...
Jiang-Bei Huang, Mok-Ha Jin, Yue-Ming Ye et al.· Journal of Geophysics and En...· 0 citations
Seismic diffraction events contain high‐wavenumber information that is critical for imaging small‐scale discontinuities, yet their weak amplitudes are often obscured by strong reflection energy. Diffusion models offer a powerful framework for diffraction separation, but their iterative reverse‐diffusion sampling is com...
We present a distributed framework for large-scale Bayesian inverse problems governed by the eikonal equation, with a specific focus on seismic traveltime tomography. Traditional deterministic approaches often fail to provide the uncertainty quantification (UQ) necessary for ill-posed problems, while conventional Bayes...
Akshay Vishwakarma, K. Aghazade, Ali Siahkoohi et al.· 0 citations
We use cookies to run the site and, with your consent, for analytics and to show ads.
See our Cookie Policy.