Searcharxiv⌕ Search

arXiv · 2609.31251

Structure-dependent failure modes of neural priors in acoustic full-waveform inversion

Abstract

Frequency continuation does not improve every neural representation, and better velocity recovery need not imply better prediction of unseen waveforms. We compare a velocity grid with total-variation regularization, an adapted sinusoidal coordinate network (SIREN), and a frozen image generator with a full-grid residual in two-dimensional acoustic full-waveform inversion. All methods use the same frozen SWEEP discretization, acquisition, observations, background, and budget of 1,500 shot--model gradient evaluations. Three exposed synthetic targets represent inclined layering, curved layering, and a high-contrast curved interface drawn from a fault-labelled family. With 2-to-10 Hz continuation, the generative-residual model attains velocity RMSEs of 218.7, 108.0, and 341.9 m/s, compared with 232.5, 100.3, and 412.9 m/s for Grid+TV. Thus the latter wins on curved layering, while the former improves model RMSE by 5.9% and 17.2% on the other targets. Grid+TV nevertheless predicts held-out 10 Hz shots better on all three. SIREN is worse than the common background in every cell; continuation worsens two targets but improves one. A five-weight TV sensitivity study preserves the CurveFault model-error ranking. An equal-budget variational extension fails both recovery and interval coverage. These results establish conditional rankings, not universal superiority or an isolated spectral-bias mechanism. Full-grid residuals also prevent attributing gains uniquely to the generator. We advocate joint reporting of model recovery, unseen-shot prediction, optimization cost, and negative outcomes when auditing neural FWI.

Explore related subjects

Keep this discovery

Explore connections, maps & timelines

BibTeXRIS

Ziye Yu, Xin Liu, Yuqi Cai. 2026-09-25. Structure-dependent failure modes of neural priors in acoustic full-waveform inversion. https://arxiv.org/abs/2609.31251

Cite the original work for its findings. Save a collection to share your selection of sources.

KEEP EXPLORING

Related papers

The Glacier Model Intercomparison Project (GlacierMIP): Towards standardisation of global glacier projections

The Glacier Model Intercomparison Project (GlacierMIP) provides an international framework for the coordinated evaluation and comparison of global glacier evolution models and their projections of glacier change. Its fourth phase, GlacierMIP4, updates previous global glacier projections through a standardised experimental design. For the first time, the protocol includes simulations extending to 2300 and an overshoot scenario for a subset of climate projections and requires monthly output of individual mass-balance components such as melt, accumulation and refreezing, in addition to annual results for glacier mass and area. While permitting model-specific approaches to calibration and other aspects of model implementation, the protocol prescribes common atmospheric forcing data, inventory boundary conditions, and reporting conventions to enable consistent analyses of inter-model differences. Here, we describe the GlacierMIP4 experimental protocol, including the simulation domain, initialisation, atmospheric forcing, and standardised output requirements. More broadly, we emphasize the need for standardised terminology, units, sign convention and file formats in global glacier modelling to improve the traceability, interoperability, and comparability of results, and recommend this protocol as a blueprint for future global glacier modelling studies.

physics.geo-ph↗

Learning relaxation time distributions from spectral induced polarization data with a complex-valued variational autoencoder

Spectral induced polarization (SIP) is a geophysical method used to characterize subsurface materials. It measures the frequency-dependent complex electrical resistivity of rocks and soils through the application of an alternating current. Debye and Warburg decompositions are standard methods for analyzing and interpreting SIP data, as they allow estimation of the relaxation time distribution (RTD) of geomaterials. However, conventional decomposition approaches treat measurements independently, work in real-valued spaces despite the complex-valued nature of SIP data, and provide limited uncertainty quantification. These limitations reduce the effectiveness of conventional decomposition on heterogeneous datasets. We reformulate the decomposition approach as an unsupervised machine learning problem and introduce a conditional variational autoencoder (CVAE) that learns a shared mapping from SIP datasets to continuous RTDs. The model is validated on a dataset comprising 140 laboratory and field SIP measurements of granular mixtures, sedimentary and igneous rock, and cementitious materials. The CVAE operates in complex-valued data space and achieves reconstruction errors of 0.53 % and 0.27 % for the imaginary and phase components of resistivity, respectively, with evidence of improvement over conventional methods at corresponding p-values of 0.007 and 0.06. The inferred RTDs are stable and physically consistent, and their total chargeability and mean relaxation time correlate with polarizable grain content and grain size, respectively, with coefficients of determination up to 0.98. An additional contribution of the proposed method is the learned latent representation, which organizes SIP spectra into a structured space. Unsupervised clustering in a two-dimensional projection of this space improves the silhouette score by nearly a factor of two relative to conventional RTD parameters.

physics.geo-ph↗

DiffSpecMatch: Differentiable Waveform Inverse Design with Configurable Optimization Modules for Response-Spectrum Matching of Ground Motions

Response-spectrum matching is an underdetermined waveform inverse problem in which spectral compatibility must be achieved without uncontrolled changes in other engineering-relevant ground-motion characteristics. This study formulates the problem as differentiable waveform inverse design using a fixed SDOF dynamics engine and configurable optimization modules. An envelope-guided parameterization defines the correction waveform, while a hard projection enforces zero correction-induced terminal velocity and displacement. Differentiable SDOF responses then provide gradients for waveform optimization. Spectral fidelity and Arias-intensity accumulation are treated as adaptive objectives. Spectral feasibility, PGA, total Arias intensity, and displacement-path requirements are incorporated as constraints. The differentiable spectrum operator agrees with an exact solution of the equation of motion to within 0.002%. The complete five-damping configuration achieves a maximum spectral error of 5.00% over 375 ordinates. On a common benchmark, maximum errors of 2.61% and 8.47% are obtained for single- and multi-damping matching, respectively, while retaining the additional waveform constraints. Three-component applications further show that different engineering acceptance requirements can be accommodated through module reconfiguration without changing the forward dynamics.

physics.geo-ph↗