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 contributionpeer-review

3 Scopus citations

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
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 - 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
Country/TerritoryUnited States
CityReno
Period10/14/1810/17/18

Funding

Sandia National Laboratories is a multi-mission laboratory managed and operated by National Technology & Engineering Solutions of Sandia, LLC, a wholly owned subsidiary of Honeywell International Inc., for the U.S. Department of Energy’s National Nuclear Security Administration under contract DE-NA0003525. This material was based upon work supported by the U.S. Department of Energy (DOE), Office of Energy Efficiency and Renewable Energy (EERE), Office of Technology Development, Geothermal Technologies Office (GTO), under Award Number DE-AC52-07NA27344 with LLNL, Award Number DE-AC05-76RL01830 with PNNL, and Award Number DE-AC02-05CH11231 with LBNL. The United States Government retains, and the publisher, by accepting the article for publication, acknowledges that the United States Government retains a nonexclusive, paid-up, irrevocable, world-wide license to publish or reproduce the published form of this manuscript, or allow others to do so, for United States Government purposes. The research supporting this work took place in whole or in part at the Sanford Underground Research Facility in Lead, South Dakota. The assistance of the Sanford Underground Research Facility and its personnel in providing physical access and general logistical and technical support is acknowledged. Rendered images of the well paths were generated from a 3D model developed using Leapfrog Software. Copyright © Aranz Geo Limited. Leapfrog and all other Aranz Geo Limited product or service names are registered trademarks or trademarks of Aranz Geo Limited. This material was based upon work supported by the U.S. Department of Energy (DOE), Office of Energy Efficiency and Renewable Energy (EERE), Office of Technology Development, Geothermal Technologies Office (GTO), under Award Number DE-AC52-07NA27344 with LLNL, Award Number DE-AC05-76RL01830 with PNNL, and Award Number DE-AC02-05CH11231 with LBNL. The United States Government retains, and the publisher, by accepting the article for publication, acknowledges that the United States Government retains a nonexclusive, paid-up, irrevocable, world-wide license to publish or reproduce the published form of this manuscript, or allow others to do so, for United States Government purposes. The research supporting this work took place in whole or in part at the Sanford Underground Research Facility in Lead, South Dakota. The assistance of the Sanford Underground Research Facility and its personnel in providing physical access and general logistical and technical support is acknowledged. Rendered images of the well paths were generated from a 3D model developed using Leapfrog Software. Copyright © Aranz Geo Limited. Leapfrog and all other Aranz Geo Limited product or service names are registered trademarks or trademarks of Aranz Geo Limited. Sandia National Laboratories is a multi-mission laboratory managed and operated by National Technology & Engineering Solutions of Sandia, LLC, a wholly owned subsidiary of Honeywell International Inc., for the U.S. Department of Energy's National Nuclear Security Administration under contract DE-NA0003525. This paper describes objective technical results and analysis. Any subjective views or opinions that might be expressed in the paper do not necessarily represent the views of the U.S. Department of Energy or the United States Government.

FundersFunder number
U.S. Department of Energy
Office of Energy Efficiency and Renewable Energy
Office of Technology Development
National Nuclear Security AdministrationDE-NA0003525
Lawrence Livermore National LaboratoryDE-AC05-76RL01830
Sandia National Laboratories
U.S. Navy
Pacific Northwest National LaboratoryDE-AC02-05CH11231
Geothermal Technologies OfficeDE-AC52-07NA27344

    Keywords

    • Acoustic emission
    • Cross-borehole seismic
    • EGS Collab
    • Hydrofracture
    • Micro-earthquake

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