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Title: Numerical modeling of injection, stress and permeability enhancement during shear stimulation at the Desert Peak Enhanced Geothermal System

Journal Article · · International Journal of Rock Mechanics and Mining Sciences
ORCiD logo [1];  [2];  [3];  [4];  [5]
  1. Los Alamos National Lab. (LANL), Los Alamos, NM (United States); Stanford Univ., CA (United States). Dept. of Geophysics
  2. Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
  3. Temple Univ., Philadelphia, PA (United States)
  4. U.S. Geological Survey, Menlo Park, CA (United States)
  5. Baker Hughes Inc., Palo Alto, CA (United States)

Creation of an Enhanced Geothermal System relies on stimulation of fracture permeability through self-propping shear failure that creates a complex fracture network with high surface area for efficient heat transfer. In 2010, shear stimulation was carried out in well 27-15 at Desert Peak geothermal field, Nevada, by injecting cold water at pressure less than the minimum principal stress. An order-of-magnitude improvement in well injectivity was recorded. In this work, we describe a numerical model that accounts for injection-induced stress changes and permeability enhancement during this stimulation. We use the coupled thermo-hydrological–mechanical simulator FEHM to (i) construct a wellbore model for non-steady bottom-hole temperature and pressure conditions during the injection, and (ii) apply these pressures and temperatures as a source term in a numerical model of the stimulation. A Mohr–Coulomb failure criterion and empirical fracture permeability is developed to describe permeability evolution of the fractured rock. The numerical model is calibrated using laboratory measurements of material properties on representative core samples and wellhead records of injection pressure and mass flow during the shear stimulation. The model captures both the absence of stimulation at low wellhead pressure (WHP ≤1.7 and ≤2.4 MPa) as well as the timing and magnitude of injectivity rise at medium WHP (3.1 MPa). Results indicate that thermoelastic effects near the wellbore and the associated non-local stresses further from the well combine to propagate a failure front away from the injection well. Elevated WHP promotes failure, increases the injection rate, and cools the wellbore; however, as the overpressure drops off with distance, thermal and non-local stresses play an ongoing role in promoting shear failure at increasing distance from the well.

Research Organization:
Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)
Sponsoring Organization:
USDOE Office of Energy Efficiency and Renewable Energy (EERE), Renewable Power Office. Geothermal Technologies Office
Grant/Contract Number:
AC52-06NA25396; GT-1000036-12_Revision 1
OSTI ID:
1468563
Alternate ID(s):
OSTI ID: 1556193
Report Number(s):
LA-UR-14-27904
Journal Information:
International Journal of Rock Mechanics and Mining Sciences, Vol. 78, Issue C; ISSN 1365-1609
Publisher:
ElsevierCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 40 works
Citation information provided by
Web of Science

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Cited By (5)

An analytical model for heat extraction through multi-link fractures of the enhanced geothermal system journal October 2019
A Numerical Model for the Effect of Permeability Change on Faulting During Fluid Injection journal February 2019
A coupled thermomechanical nonordinary state‐based peridynamics for thermally induced cracking of rocks journal July 2019
Thermal Cracking in Westerly Granite Monitored Using Direct Wave Velocity, Coda Wave Interferometry, and Acoustic Emissions journal March 2018
The spatial footprint of injection wells in a global compilation of induced earthquake sequences journal August 2018