Uncertainty quantification in time-lapse full-waveform inversion of vertical seismic profiling data: contrasting the Hamiltonian Monte Carlo and Stein Variational Gradient Descent methods

Abstract Time-lapse full-waveform inversion (TL-FWI) is increasingly important in energy-transition applications, particularly for monitoring CO2 geological storage. Because TL-FWI is highly nonlinear and baseline and monitor surveys commonly differ in acquisition, illumination, and noise conditions, uncertainty quantification is essential for reliable interpretation. Two promising Bayesian approaches are Hamiltonian Monte Carlo (HMC) and Stein variational gradient descent (SVGD), which represent the posterior in fundamentally different ways. HMC constructs the posterior through stochastic sampling with gradient-based proposals, whereas SVGD approximates it using a deterministically evolving particle ensemble. Here, we investigate the feasibility of 2D VSP-based TL-FWI using these two approaches under a matched computational budget. Both methods recover the main injection-related velocity anomaly, but they express posterior uncertainty differently. Under this resource-limited comparison, HMC yields uncertainty fields that remain comparatively diffuse and become increasingly difficult to interpret in deeper and off-well regions where illumination is weak. SVGD, in contrast, produces uncertainty patterns that are more strongly organized by acquisition geometry, placing larger uncertainty more explicitly in poorly constrained regions, although this also causes the posterior means and profiles to inherit stronger illumination-shaped artifacts. These results suggest that the practical distinction between HMC and SVGD is not simply one of better or worse uncertainty quantification, but rather how limited computational effort is converted into posterior information. The preferred method is therefore budget- and objective-dependent. Specifically, HMC remains attractive when more exhaustive posterior exploration is computationally feasible, whereas SVGD provides a more scalable and practically interpretable route for rapid uncertainty assessment in TLFWI monitoring applications.

Authors

Institutions

Publication Details

Journal
Geophysics
Published
2026-10-14
DOI
https://doi.org/10.1190/geo-2025-1009
Primary Topic
Seismic Imaging and Inversion Techniques
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Uncertainty quantification in time-lapse full-waveform inversion of vertical seismic profiling data: contrasting the Hamiltonian Monte Carlo and Stein Variational Gradient Descent methods

Alison Malcolm, Jinji Li, Kris Innanen
Geophysics
Seismic Imaging and Inversion Techniques
article

Uncertainty quantification in time-lapse full-waveform inversion of vertical seismic profiling data: contrasting the Hamiltonian Monte Carlo and Stein Variational Gradient Descent methods

Alison Malcolm, Jinji Li, Kris Innanen
article en

Abstract

Abstract Time-lapse full-waveform inversion (TL-FWI) is increasingly important in energy-transition applications, particularly for monitoring CO2 geological storage. Because TL-FWI is highly nonlinear and baseline and monitor surveys commonly differ in acquisition, illumination, and noise conditions, uncertainty quantification is essential for reliable interpretation. Two promising Bayesian approaches are Hamiltonian Monte Carlo (HMC) and Stein variational gradient descent (SVGD), which represent the posterior in fundamentally different ways. HMC constructs the posterior through stochastic sampling with gradient-based proposals, whereas SVGD approximates it using a deterministically evolving particle ensemble. Here, we investigate the feasibility of 2D VSP-based TL-FWI using these two approaches under a matched computational budget. Both methods recover the main injection-related velocity anomaly, but they express posterior uncertainty differently. Under this resource-limited comparison, HMC yields uncertainty fields that remain comparatively diffuse and become increasingly difficult to interpret in deeper and off-well regions where illumination is weak. SVGD, in contrast, produces uncertainty patterns that are more strongly organized by acquisition geometry, placing larger uncertainty more explicitly in poorly constrained regions, although this also causes the posterior means and profiles to inherit stronger illumination-shaped artifacts. These results suggest that the practical distinction between HMC and SVGD is not simply one of better or worse uncertainty quantification, but rather how limited computational effort is converted into posterior information. The preferred method is therefore budget- and objective-dependent. Specifically, HMC remains attractive when more exhaustive posterior exploration is computationally feasible, whereas SVGD provides a more scalable and practically interpretable route for rapid uncertainty assessment in TLFWI monitoring applications.

Geophysics
Memorial University of Newfoundland (CA), University of Calgary (CA), Alberta Energy (CA)
Openalex Percentile: Top 17%
Seismic Imaging and Inversion Techniques
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.