Source Model for Non-steady Flow Within Fractures
Description:
Understanding fluid flow in subsurface reservoirs is critical for advancing geothermal energy, subsurface waste and energy storage, and in-situ mineral extraction. In these reservoirs, fractures often serve as the primary conduits for fluid movement. Under certain conditions where high flow rates and steep pressure gradients exist, non-steady flow can occur. This state, which generates seismic energy, has been hypothesized to explain numerous field observations and is considered a key mechanism behind fracture resonance commonly detected in stimulated reservoirs. In this work, we develop a physics-based theoretical source model for turbulent fluid flow within fractures. Our approach extends existing fluid-source frameworks by incorporating fracture-specific characteristics such as geometry, roughness, aperture variability, and the potential for channelized flow pathways. Using this model, we characterize the expected source spectra and identify conditions under which this phenomenon is most likely to occur. By refining fluid-source models for fractured systems, we move closer to achieving precision monitoring and improved control of subsurface reservoirs. LA-UR-26-20136
Session: Data-Driven and Computational Characterization of Non-Earthquake Seismoacoustic Sources - I
Type: Oral
Date: 4/16/2026
Presentation Time: 08:45 AM (local time)
Presenting Author: Nathan Maier
Student Presenter: No
Invited Presentation:
Poster Number:
Authors
Nathan Maier Presenting Author Corresponding Author nmaier@lanl.gov Los Alamos National Laboratory |
Carly Donahue cmd@lanl.gov Los Alamos National Laboratory |
Jeong-Ung Woo woo@lanl.gov Los Alamos National Laboratory |
Luke Frash lfrash@lanl.gov Los Alamos National Laboratory |
|
|
|
|
|
Source Model for Non-steady Flow Within Fractures
Category
Data-Driven and Computational Characterization of Non-Earthquake Seismoacoustic Sources