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For project, contracts and operations, contact Joseph Moore:
utahforge@utah.edu

For Modeling and Simulation Forum information:
utahforge-modeling@utah.edu

For general information, outreach activities and communications:
utahforge-info@utah.edu

For information regarding Solicitations and funding opportunities:
utahforgesolicitations@utah.edu

University of Utah
Energy & Geoscience Institute
423 Wakara Way, Suite 300
Salt Lake City, UT 84108
Phone: (801) 581-5126

Department of Energy Logo
Professor Ahmad Ghassemi represents the University of Oklahoma as a Utah FORGE partner. He leads the Reservoir Geomechanics and Seismicity Research (RGSR) Group, which investigates reservoir geomechanics in geothermal and petroleum systems. He is part of the Mewbourne School of Petroleum and Geological Engineering at the University of Oklahoma (OU), which is rated among the top petroleum engineering programs in the nation, and it has had a large impact in research and development since the late 1980’s. Today, the program is recognized for its world-class experimental and numerical modeling infrastructures, which has important applications for geothermal research and development of EGS-type reservoirs.

Professor Ghassemi’s group focuses on understanding the dynamics of reservoir rocks and fracture networks in response to hydraulic, poroelastic, thermal, and chemical stimulations. The aim of this work is to facilitate economic production of the nation's vast geothermal resources through development of effective completions and stimulation techniques. Active topics of research include:

  • Stimulation Optimization using Geologic and Geomechanics Principles
  • Modeling Fracture Clusters in Geothermal Reservoirs
  • Geomechanics-Based Stochastic Analysis of Injection-Induced Seismicity
  • Variation of In-situ Stress, and Fracture Slip in Response to Injection/Production
  • Optimum Wellbore Trajectory and Wellbore Stability Analysis
  • Experimental and Numerical Investigation of Coupled Poro-thermo-chemo-mechanical Analysis of Fracture Permeability

This research is conducted in partnership with the geothermal industry, and in collaboration with the National Laboratories.

Professor Ghassemi’s research at Utah FORGE addresses reservoir characterization, hydraulic fracturing design, diagnostic fracture induced testing (DFIT) in fracture rock, and other stress in-situ stress determination methods. In addition to providing experimental expertise to assess rock and fracture characteristics, and the potential impact of shear and mixed-mode stimulation, we contribute to stimulation design optimization using the GeoFrac family of thermo-poromechanical hydraulic fracturing and fracture network models that have been developed for large-scale studies.  The 2D version of GeoFrac considers rock anisotropy and natural fractures including their slip and propagation to form a network. The 3D version called GeoFeac3D incorporates rock heterogeneity and non-linearity, allows for poroelasticity, thermoelasticity, and mixed-mode propagation, and can be used to model multiple hydraulic fractures involving proppant transport and heat extraction. These will be used to help future stimulation design at FORGE.

The RGSR group has a world-class rock mechanics facility consisting of a number of MTS Material Testing Systems, 3 Polyaxial Testing units, 1 TTK Triaxial Test System, 1 Creep Test System, 1 API Fracturing Conductivity Test System, 3D laser Scanning System, etc. In addition to conventional rock mechanics testing such as uniaxial/triaxial compressive, static/dynamic, tensile strength, AE monitoring, hardness, fracture conductivity,  advanced/novel rock mechanics tests are used to evaluate large-scale hydraulic fracturing under true triaxial conditions, tracer performance, high temperature and high pressure effects, triaxial shear, direct shear, and fracture propagation and coalescence.  Currently, there are nine graduate students and two post-docs involved in the modeling and experimental work in the group.

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Advancing innovative technologies to unlock Earth’s limitless geothermal energy.