TY - GEN
T1 - Feasibility of a deep direct-use geothermal system at the University of Illinois Urbana-Champaign
AU - Stumpf, Andrew
AU - Damico, James
AU - Okwen, Roland
AU - Stark, Timothy
AU - Elrick, Scott
AU - John Nelson, W.
AU - Lu, Yongqi
AU - Holcomb, Franklin
AU - Tinjum, James
AU - Yang, Fang
AU - Frailey, Scott
AU - Lin, Yu Feng
N1 - This material is based on work supported by the U.S. Department of Energy's Office of Energy Efficiency and Renewable Energy (EERE) under Geothermal Technologies Office Award Number DE-EE0008106.0000. We acknowledge Hannes Leetaru for through editing and review of this paper as well as scientific input. Steve Whittaker also provided a constructive review. We acknowledge Charles Monson for his scientific input and for providing regional structure and isopach maps of the St. Peter Sandstone. Yaghoob Lasemi, Zohreh Askari Khorasgani, and Samuel Panno are acknowledged for their feedback and consultation. We also thank Damon Garner and Michelle Johnson for their assistance on the project. Edits to this submission by Arlene Anderson and Susan Krusemark are gratefully acknowledged. We acknowledge Landmark Graphics for use of their software via the University Donation Program, Schlumberger, Ltd. for donation of the PetrelTM E&P software platform, and IHS for use of their Petra geological interpretation software via the University Grant Program.
This material is based on work supported by the U.S. Department of Energy’s Office of Energy Efficiency and Renewable Energy (EERE) under Geothermal Technologies Office Award Number DE-EE0008106.0000.
PY - 2018
Y1 - 2018
N2 - This study assesses the feasibility of using deep direct-use (DDU) geothermal energy in agricultural research facilities on the University of Illinois at Urbana-Champaign campus to exploit low-temperature sedimentary basins, such as the Illinois Basin. Subsurface components of the system include extraction and injection wells and downhole pumps. Surface equipment includes heat pumps/exchangers, and fluid transport and monitoring systems. Two geologic formations in the region exhibit a potential as sources for geothermal energy, based on pre initial temperatures and flow rates of fluids. The St. Peter and Mt. Simon Sandstones lie at depths of 634 and 1,280 m, respectively. Geocellular modeling is used to characterize the reservoirs. A St. Peter Sandstone model was made for an area south of the campus. Petrophysical and geothermal properties used are based on data from the closest wells penetrating the formations. Characterization of the Mt. Simon Sandstone is in progress and is not discussed here. Extraction and injection flows simulated with different wellbore configurations provide estimates of fluid flow out of and into the reservoir. The models are used to optimize flow rates, bottomhole pressure, and temperature of the produced fluid. Individual wellbore models simulate subsurface heat loss and gain, providing guidance on the optimal type and amount of insulation in the wellbore. Design of the surface facilities will address aspects of fluid delivery, heat exchange, capital operating costs, heat loss, and corrosion. Heat capacity and flow rates are assessed to estimate life-cycle costs and benefits, including the environmental benefits of reducing greenhouse gases and water use and increased energy efficiency. A preliminary analysis of surface configurations for the DDU system (including cascading applications) based on building heat loads is being conducted to identify multiple system designs that will maximize performance, energy efficiency, and cost recovery.
AB - This study assesses the feasibility of using deep direct-use (DDU) geothermal energy in agricultural research facilities on the University of Illinois at Urbana-Champaign campus to exploit low-temperature sedimentary basins, such as the Illinois Basin. Subsurface components of the system include extraction and injection wells and downhole pumps. Surface equipment includes heat pumps/exchangers, and fluid transport and monitoring systems. Two geologic formations in the region exhibit a potential as sources for geothermal energy, based on pre initial temperatures and flow rates of fluids. The St. Peter and Mt. Simon Sandstones lie at depths of 634 and 1,280 m, respectively. Geocellular modeling is used to characterize the reservoirs. A St. Peter Sandstone model was made for an area south of the campus. Petrophysical and geothermal properties used are based on data from the closest wells penetrating the formations. Characterization of the Mt. Simon Sandstone is in progress and is not discussed here. Extraction and injection flows simulated with different wellbore configurations provide estimates of fluid flow out of and into the reservoir. The models are used to optimize flow rates, bottomhole pressure, and temperature of the produced fluid. Individual wellbore models simulate subsurface heat loss and gain, providing guidance on the optimal type and amount of insulation in the wellbore. Design of the surface facilities will address aspects of fluid delivery, heat exchange, capital operating costs, heat loss, and corrosion. Heat capacity and flow rates are assessed to estimate life-cycle costs and benefits, including the environmental benefits of reducing greenhouse gases and water use and increased energy efficiency. A preliminary analysis of surface configurations for the DDU system (including cascading applications) based on building heat loads is being conducted to identify multiple system designs that will maximize performance, energy efficiency, and cost recovery.
KW - Deep direct-use
KW - Geologic models
KW - Geothermal modeling
KW - Illinois basin
KW - Mt. simon sandstone
KW - St. peter sandstone
KW - Techno-economic simulation
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M3 - Conference contribution
AN - SCOPUS:85059912272
SN - 9781510875852
T3 - Transactions - Geothermal Resources Council
SP - 227
EP - 248
BT - Geothermal's Role in Today's Energy Market - Geothermal Resources Council 2018 Annual Meeting, GRC 2018
PB - Geothermal Resources Council
T2 - Geothermal Resources Council 2018 Annual Meeting: Geothermal's Role in Today's Energy Market, GRC 2018
Y2 - 14 October 2018 through 17 October 2018
ER -