The EGS collab hydrofracture experiment at the Sanford underground research facility - Campaign cross-borehole seismic characterization

EGS Collab Team

Research output: Chapter in Book/Report/Conference proceedingConference contribution

Abstract

The enhanced geothermal system (EGS) multi-laboratory and multi-university collaborative (Collab) project brings together skilled and experienced scientists and engineers in the areas of subsurface process modeling, monitoring, and a series of experiments to focus on intermediate‐scale EGS reservoir generation processes and related model validation at crystalline rock sites. Cooperative research under the EGS Collab project will provide a foundation of knowledge and modeling capability that form a bridge to meeting the challenges of EGS development and proliferation. The EGS Collab project is being performed within the re-purposed mine workings (drifts) of Sanford Underground Research Facility (SURF), located in Lead, South Dakota, USA. For the first experiment, a suite of sub-horizontal boreholes was drilled from within one of the SURF mine drifts directly into the surrounding crystalline rock formation. The suite is comprised of one stimulation well, one production well, and six monitoring wells. The goal of this experiment is to generate fractures radiating from the stimulation well that intersect the production well, and then perform flow testing of this inter-well/hydrofracture system. Stimulation and flow is monitored with micro-earthquake (MEQ) and acoustic emission (AE) instrumentation that is grouted into the monitoring wells. A fundamental component of MEQ/AE monitoring requires campaign-style cross-borehole seismic characterization. Cross-borehole techniques include compressional (P-) and Shear (S-) wave tomography. The results provide baseline P- and S-wave velocity models that are critical in calibrating hypocenter locations from MEQ/AE monitoring, and also yield elastic moduli data/constraints that will be utilized for stimulation modeling. A supplemental goal is to perform velocity change detection analysis by collecting cross-borehole P- and S-wave data between the stimulation and production wells prior and subsequent to fracture stimulation.

Original languageEnglish (US)
Title of host publicationGeothermal's Role in Today's Energy Market - Geothermal Resources Council 2018 Annual Meeting, GRC 2018
PublisherGeothermal Resources Council
Pages766-775
Number of pages10
ISBN (Electronic)0934412235
StatePublished - Jan 1 2018
EventGeothermal Resources Council 2018 Annual Meeting: Geothermal's Role in Today's Energy Market, GRC 2018 - Reno, United States
Duration: Oct 14 2018Oct 17 2018

Publication series

NameTransactions - Geothermal Resources Council
Volume42
ISSN (Print)0193-5933

Conference

ConferenceGeothermal Resources Council 2018 Annual Meeting: Geothermal's Role in Today's Energy Market, GRC 2018
CountryUnited States
CityReno
Period10/14/1810/17/18

Fingerprint

research facilities
boreholes
Boreholes
stimulation
borehole
microearthquake
S-wave
acoustic emission
well
Acoustic emissions
Crystalline rocks
Monitoring
monitoring
Earthquakes
S waves
crystalline rock
earthquakes
experiment
Experiments
P-wave

All Science Journal Classification (ASJC) codes

  • Renewable Energy, Sustainability and the Environment
  • Energy Engineering and Power Technology
  • Geophysics

Cite this

EGS Collab Team (2018). The EGS collab hydrofracture experiment at the Sanford underground research facility - Campaign cross-borehole seismic characterization. In Geothermal's Role in Today's Energy Market - Geothermal Resources Council 2018 Annual Meeting, GRC 2018 (pp. 766-775). (Transactions - Geothermal Resources Council; Vol. 42). Geothermal Resources Council.
EGS Collab Team. / The EGS collab hydrofracture experiment at the Sanford underground research facility - Campaign cross-borehole seismic characterization. Geothermal's Role in Today's Energy Market - Geothermal Resources Council 2018 Annual Meeting, GRC 2018. Geothermal Resources Council, 2018. pp. 766-775 (Transactions - Geothermal Resources Council).
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title = "The EGS collab hydrofracture experiment at the Sanford underground research facility - Campaign cross-borehole seismic characterization",
abstract = "The enhanced geothermal system (EGS) multi-laboratory and multi-university collaborative (Collab) project brings together skilled and experienced scientists and engineers in the areas of subsurface process modeling, monitoring, and a series of experiments to focus on intermediate‐scale EGS reservoir generation processes and related model validation at crystalline rock sites. Cooperative research under the EGS Collab project will provide a foundation of knowledge and modeling capability that form a bridge to meeting the challenges of EGS development and proliferation. The EGS Collab project is being performed within the re-purposed mine workings (drifts) of Sanford Underground Research Facility (SURF), located in Lead, South Dakota, USA. For the first experiment, a suite of sub-horizontal boreholes was drilled from within one of the SURF mine drifts directly into the surrounding crystalline rock formation. The suite is comprised of one stimulation well, one production well, and six monitoring wells. The goal of this experiment is to generate fractures radiating from the stimulation well that intersect the production well, and then perform flow testing of this inter-well/hydrofracture system. Stimulation and flow is monitored with micro-earthquake (MEQ) and acoustic emission (AE) instrumentation that is grouted into the monitoring wells. A fundamental component of MEQ/AE monitoring requires campaign-style cross-borehole seismic characterization. Cross-borehole techniques include compressional (P-) and Shear (S-) wave tomography. The results provide baseline P- and S-wave velocity models that are critical in calibrating hypocenter locations from MEQ/AE monitoring, and also yield elastic moduli data/constraints that will be utilized for stimulation modeling. A supplemental goal is to perform velocity change detection analysis by collecting cross-borehole P- and S-wave data between the stimulation and production wells prior and subsequent to fracture stimulation.",
author = "{EGS Collab Team} and Schwering, {Paul C.} and Knox, {Hunter A.} and Hoots, {Charles R.} and Dorothy Linneman and Jonathan Ajo-Franklin and Bauer, {S. J.} and T. Baumgartner and K. Beckers and Blankenship, {D. A.} and A. Bonneville and L. Boyd and Brown, {S. T.} and Burghardt, {J. A.} and T. Chen and Y. Chen and K. Condon and Cook, {P. J.} and Dobson, {P. F.} and Doe, {T. W.} and Doughty, {C. A.} and D. Elsworth and J. Feldman and A. Foris and Frash, {L. P.} and Derek Elsworth and P. Fu and K. Gao and A. Ghassemi and H. Gudmundsdottir and Y. Guglielmi and G. Guthrie and B. Haimson and A. Hawkins and J. Heise and M. Horn and Horne, {R. N.} and J. Horner and M. Hu and H. Huang and L. Huang and K. Im and M. Ingraham and Johnson, {T. C.} and B. Johnston and S. Karra and K. Kim and King, {D. K.} and Kneafsey, {T. J.} and Knox, {J. M.} and Marone, {Chris J.}",
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EGS Collab Team 2018, The EGS collab hydrofracture experiment at the Sanford underground research facility - Campaign cross-borehole seismic characterization. in Geothermal's Role in Today's Energy Market - Geothermal Resources Council 2018 Annual Meeting, GRC 2018. Transactions - Geothermal Resources Council, vol. 42, Geothermal Resources Council, pp. 766-775, Geothermal Resources Council 2018 Annual Meeting: Geothermal's Role in Today's Energy Market, GRC 2018, Reno, United States, 10/14/18.

The EGS collab hydrofracture experiment at the Sanford underground research facility - Campaign cross-borehole seismic characterization. / EGS Collab Team.

Geothermal's Role in Today's Energy Market - Geothermal Resources Council 2018 Annual Meeting, GRC 2018. Geothermal Resources Council, 2018. p. 766-775 (Transactions - Geothermal Resources Council; Vol. 42).

Research output: Chapter in Book/Report/Conference proceedingConference contribution

TY - GEN

T1 - The EGS collab hydrofracture experiment at the Sanford underground research facility - Campaign cross-borehole seismic characterization

AU - EGS Collab Team

AU - Schwering, Paul C.

AU - Knox, Hunter A.

AU - Hoots, Charles R.

AU - Linneman, Dorothy

AU - Ajo-Franklin, Jonathan

AU - Bauer, S. J.

AU - Baumgartner, T.

AU - Beckers, K.

AU - Blankenship, D. A.

AU - Bonneville, A.

AU - Boyd, L.

AU - Brown, S. T.

AU - Burghardt, J. A.

AU - Chen, T.

AU - Chen, Y.

AU - Condon, K.

AU - Cook, P. J.

AU - Dobson, P. F.

AU - Doe, T. W.

AU - Doughty, C. A.

AU - Elsworth, D.

AU - Feldman, J.

AU - Foris, A.

AU - Frash, L. P.

AU - Elsworth, Derek

AU - Fu, P.

AU - Gao, K.

AU - Ghassemi, A.

AU - Gudmundsdottir, H.

AU - Guglielmi, Y.

AU - Guthrie, G.

AU - Haimson, B.

AU - Hawkins, A.

AU - Heise, J.

AU - Horn, M.

AU - Horne, R. N.

AU - Horner, J.

AU - Hu, M.

AU - Huang, H.

AU - Huang, L.

AU - Im, K.

AU - Ingraham, M.

AU - Johnson, T. C.

AU - Johnston, B.

AU - Karra, S.

AU - Kim, K.

AU - King, D. K.

AU - Kneafsey, T. J.

AU - Knox, J. M.

AU - Marone, Chris J.

PY - 2018/1/1

Y1 - 2018/1/1

N2 - The enhanced geothermal system (EGS) multi-laboratory and multi-university collaborative (Collab) project brings together skilled and experienced scientists and engineers in the areas of subsurface process modeling, monitoring, and a series of experiments to focus on intermediate‐scale EGS reservoir generation processes and related model validation at crystalline rock sites. Cooperative research under the EGS Collab project will provide a foundation of knowledge and modeling capability that form a bridge to meeting the challenges of EGS development and proliferation. The EGS Collab project is being performed within the re-purposed mine workings (drifts) of Sanford Underground Research Facility (SURF), located in Lead, South Dakota, USA. For the first experiment, a suite of sub-horizontal boreholes was drilled from within one of the SURF mine drifts directly into the surrounding crystalline rock formation. The suite is comprised of one stimulation well, one production well, and six monitoring wells. The goal of this experiment is to generate fractures radiating from the stimulation well that intersect the production well, and then perform flow testing of this inter-well/hydrofracture system. Stimulation and flow is monitored with micro-earthquake (MEQ) and acoustic emission (AE) instrumentation that is grouted into the monitoring wells. A fundamental component of MEQ/AE monitoring requires campaign-style cross-borehole seismic characterization. Cross-borehole techniques include compressional (P-) and Shear (S-) wave tomography. The results provide baseline P- and S-wave velocity models that are critical in calibrating hypocenter locations from MEQ/AE monitoring, and also yield elastic moduli data/constraints that will be utilized for stimulation modeling. A supplemental goal is to perform velocity change detection analysis by collecting cross-borehole P- and S-wave data between the stimulation and production wells prior and subsequent to fracture stimulation.

AB - The enhanced geothermal system (EGS) multi-laboratory and multi-university collaborative (Collab) project brings together skilled and experienced scientists and engineers in the areas of subsurface process modeling, monitoring, and a series of experiments to focus on intermediate‐scale EGS reservoir generation processes and related model validation at crystalline rock sites. Cooperative research under the EGS Collab project will provide a foundation of knowledge and modeling capability that form a bridge to meeting the challenges of EGS development and proliferation. The EGS Collab project is being performed within the re-purposed mine workings (drifts) of Sanford Underground Research Facility (SURF), located in Lead, South Dakota, USA. For the first experiment, a suite of sub-horizontal boreholes was drilled from within one of the SURF mine drifts directly into the surrounding crystalline rock formation. The suite is comprised of one stimulation well, one production well, and six monitoring wells. The goal of this experiment is to generate fractures radiating from the stimulation well that intersect the production well, and then perform flow testing of this inter-well/hydrofracture system. Stimulation and flow is monitored with micro-earthquake (MEQ) and acoustic emission (AE) instrumentation that is grouted into the monitoring wells. A fundamental component of MEQ/AE monitoring requires campaign-style cross-borehole seismic characterization. Cross-borehole techniques include compressional (P-) and Shear (S-) wave tomography. The results provide baseline P- and S-wave velocity models that are critical in calibrating hypocenter locations from MEQ/AE monitoring, and also yield elastic moduli data/constraints that will be utilized for stimulation modeling. A supplemental goal is to perform velocity change detection analysis by collecting cross-borehole P- and S-wave data between the stimulation and production wells prior and subsequent to fracture stimulation.

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EGS Collab Team. The EGS collab hydrofracture experiment at the Sanford underground research facility - Campaign cross-borehole seismic characterization. In Geothermal's Role in Today's Energy Market - Geothermal Resources Council 2018 Annual Meeting, GRC 2018. Geothermal Resources Council. 2018. p. 766-775. (Transactions - Geothermal Resources Council).