|
Title: |
Rough Fracture Characterization in Enhanced Geothermal Systems (EGS): Numerical Simulation Updates |
|
Authors: |
Sarah SAUSAN, Roland HORNE |
|
Key Words: |
rough fracture, EGS, numerical simulation, roughness, CFD, Navier-Stokes |
|
Conference: |
Stanford Geothermal Workshop |
|
Year: |
2025 |
|
Session: |
Enhanced Geothermal Systems |
|
Language: |
English |
|
Paper Number: |
Sausan1 |
|
File Size: |
2851 KB |
|
View File: |
|
The artificial fractures in EGS are created within the context of natural factors such as geology, geomechanics, and geochemistry, as well as engineering techniques used during stimulation, such as the use of proppant and acids. Fracture characterization, i.e., gathering information regarding fractures’ physical properties, such as aperture, hydraulic conductivity, and network distribution patterns, provides the source of information for modeling and engineering the subsurface reservoir appropriately. At the near-wellbore scale, the fracture planes around the well are examined to provide an understanding of the feed zone behavior. At the EGS Collab site, it was observed that during a downhole camera survey of a flowing wellbore the inflow pattern from the producing fractures was not sheet-like but rather composed of sporadic point sources. This observation can be explained by considering that fracture surfaces are rough; preferential fluid flow pathways emerged across a fracture plane due to its roughness. To simulate the fluid flow behavior between the crevices of rough fracture, a displacement discontinuity model (DDM) was used to represent rough fracture faces under varying stress regimes. Then, the geometry of the fracture space was built into a three-dimensional model to simulate the fluid flow and heat transfer across the fracture planes using a Computational Fluid Dynamics (CFD) simulator. The rough fracture modeling in this study could successfully model the fluid flow for a roughness distribution corresponding to a shear stress and normal stress combination of -6MPa and 6MPa, respectively. As the stress regimes heavily influence the aperture distribution, subsequent scenarios were modeled across parametric simulation involving a range of shear and normal stress and compared with the reference. Radial flow behavior for each stress regime was simulated to investigate the roughness relationship with varying stress regimes.
Press the Back button in your browser, or search again.
Copyright 2025, Stanford Geothermal Program: Readers who download papers from this site should honor the copyright of the original authors and may not copy or distribute the work further without the permission of the original publisher.
Attend the nwxt Stanford Geothermal Workshop,
click here for details.