Simulations of carbon dioxide push-pull into a conjugate fault system modeled after Dixie Valley—Sensitivity analysis of significant parameters and uncertainty prediction by data-worth analysis
- Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
- University of Louisiana at Lafayette, Lafayette, LA (United States)
- Schlumberger-Doll Research, Cambridge, MA (United States)
Characterizing the faults and fractures that provide flow pathways for efficient geothermal energy production is critical for design of sustainable geothermal energy production. Both natural faults and stimulated fractures in enhanced geothermal systems (EGS) are difficult to image and map by seismic methods because hot brine filling the fractures and faults does not create a strong seismic property contrast relative to surrounding rock. We investigate here the technical feasibility of using supercritical CO2 (scCO2) injection into faults in a single-well push-pull scenario to characterize the hydraulic properties of the fault zone by emplacing scCO2 that can serve as a contrast fluid for seismic monitoring. We develop a conceptual and numerical reservoir model of two intersecting faults based on the Dixie Valley geothermal system in Nevada, USA.
- Research Organization:
- Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
- Sponsoring Organization:
- USDOE Office of Energy Efficiency and Renewable Energy (EERE), Renewable Power Office. Geothermal Technologies Office; USDOE Office of Fossil Energy (FE); Environmental Design Research Association (EDRA); USDOE Office of Science (SC)
- Grant/Contract Number:
- AC02-05CH11231
- OSTI ID:
- 1477326
- Alternate ID(s):
- OSTI ID: 1496280
- Journal Information:
- Geothermics, Vol. 74, Issue C; ISSN 0375-6505
- Publisher:
- ElsevierCopyright Statement
- Country of Publication:
- United States
- Language:
- English
Similar Records
CO2 Push-Pull Dual (Conjugate) Faults Injection Simulations
Simulations of CO2 injection into fractures and faults for improving their geophysical characterization at EGS sites