3D modeling of deep borehole electromagnetic measurements with energized casing source for fracture mapping at the Utah Frontier Observatory for Research in Geothermal Energy

We present a 3D numerical modelling analysis evaluating the deployment of a borehole electromagnetic measurement tool to detect and image a stimulated zone at the Utah Frontier Observatory for Research in Geothermal Energy geothermal site. As the depth to the geothermal reservoir is several kilometr...

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Veröffentlicht in:Geophysical Prospecting 2024-10, Vol.72 (8), p.3104-3128
Hauptverfasser: Um, Evan Schankee, Alumbaugh, David, Capriotti, Joseph, Wilt, Michael, Nichols, Edward, Li, Yaoguo, Kang, Seogi, Osato, Kazumi
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container_end_page 3128
container_issue 8
container_start_page 3104
container_title Geophysical Prospecting
container_volume 72
creator Um, Evan Schankee
Alumbaugh, David
Capriotti, Joseph
Wilt, Michael
Nichols, Edward
Li, Yaoguo
Kang, Seogi
Osato, Kazumi
description We present a 3D numerical modelling analysis evaluating the deployment of a borehole electromagnetic measurement tool to detect and image a stimulated zone at the Utah Frontier Observatory for Research in Geothermal Energy geothermal site. As the depth to the geothermal reservoir is several kilometres and the size of the stimulated zone is limited to several 100 m, surface‐based controlled‐source electromagnetic measurements lack the sensitivity for detecting changes in electrical resistivity caused by the stimulation. To overcome the limitation, the study evaluates the feasibility of using a three‐component borehole magnetic receiver system at the Frontier Observatory for Research in Geothermal Energy site. To provide sufficient currents inside and around the enhanced geothermal reservoir, we use an injection well as an energized casing source. To efficiently simulate energizing the injection well in a realistic 3D resistivity model, we introduce a novel modelling workflow that leverages the strengths of both 3D cylindrical‐mesh‐based electromagnetic modelling code and 3D tetrahedral‐mesh‐based electromagnetic modelling code. The former is particularly well‐suited for modelling hollow cylindrical objects like casings, whereas the latter excels at representing more complex 3D geological structures. In this workflow, our initial step involves computing current densities along a vertical steel‐cased well using a 3D cylindrical electromagnetic modelling code. Subsequently, we distribute a series of equivalent current sources along the well's trajectory within a complex 3D resistivity model. We then discretize this model using a tetrahedral mesh and simulate the borehole electromagnetic responses excited by the casing source using a 3D finite‐element electromagnetic code. This multi‐step approach enables us to simulate 3D casing source electromagnetic responses within a complex 3D resistivity model, without the need for explicit discretization of the well using an excessive number of fine cells. We discuss the applicability and limitations of this proposed workflow within an electromagnetic modelling scenario where an energized well is deviated, such as at the Frontier Observatory for Research in Geothermal Energy site. Using the workflow, we demonstrate that the combined use of the energized casing source and the borehole electromagnetic receiver system offer measurable magnetic field amplitudes and sensitivity to the deep localized stimulated zone. The measu
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As the depth to the geothermal reservoir is several kilometres and the size of the stimulated zone is limited to several 100 m, surface‐based controlled‐source electromagnetic measurements lack the sensitivity for detecting changes in electrical resistivity caused by the stimulation. To overcome the limitation, the study evaluates the feasibility of using a three‐component borehole magnetic receiver system at the Frontier Observatory for Research in Geothermal Energy site. To provide sufficient currents inside and around the enhanced geothermal reservoir, we use an injection well as an energized casing source. To efficiently simulate energizing the injection well in a realistic 3D resistivity model, we introduce a novel modelling workflow that leverages the strengths of both 3D cylindrical‐mesh‐based electromagnetic modelling code and 3D tetrahedral‐mesh‐based electromagnetic modelling code. The former is particularly well‐suited for modelling hollow cylindrical objects like casings, whereas the latter excels at representing more complex 3D geological structures. In this workflow, our initial step involves computing current densities along a vertical steel‐cased well using a 3D cylindrical electromagnetic modelling code. Subsequently, we distribute a series of equivalent current sources along the well's trajectory within a complex 3D resistivity model. We then discretize this model using a tetrahedral mesh and simulate the borehole electromagnetic responses excited by the casing source using a 3D finite‐element electromagnetic code. This multi‐step approach enables us to simulate 3D casing source electromagnetic responses within a complex 3D resistivity model, without the need for explicit discretization of the well using an excessive number of fine cells. We discuss the applicability and limitations of this proposed workflow within an electromagnetic modelling scenario where an energized well is deviated, such as at the Frontier Observatory for Research in Geothermal Energy site. Using the workflow, we demonstrate that the combined use of the energized casing source and the borehole electromagnetic receiver system offer measurable magnetic field amplitudes and sensitivity to the deep localized stimulated zone. The measurements can also distinguish between parallel‐fracture anisotropic reservoirs and isotropic cases, providing valuable insights into the fracture system of the stimulated zone. Besides the magnetic field measurements, vertical electric field measurements in the open well sections are also highly sensitive to the stimulated zone and can be used as additional data for detecting and imaging the target. We can also acquire additional multiple‐source data by grounding the surface electrode at various locations and repeating borehole electromagnetic measurements. This approach can increase the number of monitoring data by several factors, providing a more comprehensive dataset for analysing the deep‐localized stimulated zone. The numerical analysis indicates that it is feasible to use the combination of the energized casing and downhole electromagnetic measurements in monitoring localized stimulated zone at large depths.</description><identifier>ISSN: 0016-8025</identifier><identifier>EISSN: 1365-2478</identifier><identifier>DOI: 10.1111/1365-2478.13579</identifier><language>eng</language><publisher>Houten: Wiley Subscription Services, Inc</publisher><subject>borehole geophysics ; Boreholes ; Casing ; Casings ; Current sources ; Data analysis ; Electric fields ; Electrical resistivity ; Electromagnetic measurement ; electromagnetics ; Feasibility studies ; Geological structures ; GEOSCIENCES ; Geothermal energy ; Geothermal power ; Image enhancement ; Injection ; Injection wells ; Magnetic field ; Magnetic fields ; Modelling ; Monitoring ; Numerical analysis ; Numerical models ; Observatories ; Reservoirs ; Sensitivity analysis ; Target detection ; Workflow</subject><ispartof>Geophysical Prospecting, 2024-10, Vol.72 (8), p.3104-3128</ispartof><rights>Published 2024. This article is a U.S. Government work and is in the public domain in the USA.</rights><rights>2024 European Association of Geoscientists &amp; Engineers.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c2269-5fda2600fb9ea080590bc237ac0708c099a2fc4576b47791d8e76bcd3137d593</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1111%2F1365-2478.13579$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1111%2F1365-2478.13579$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>230,314,776,780,881,1411,27901,27902,45550,45551</link.rule.ids><backlink>$$Uhttps://www.osti.gov/biblio/2440669$$D View this record in Osti.gov$$Hfree_for_read</backlink></links><search><creatorcontrib>Um, Evan Schankee</creatorcontrib><creatorcontrib>Alumbaugh, David</creatorcontrib><creatorcontrib>Capriotti, Joseph</creatorcontrib><creatorcontrib>Wilt, Michael</creatorcontrib><creatorcontrib>Nichols, Edward</creatorcontrib><creatorcontrib>Li, Yaoguo</creatorcontrib><creatorcontrib>Kang, Seogi</creatorcontrib><creatorcontrib>Osato, Kazumi</creatorcontrib><creatorcontrib>Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)</creatorcontrib><title>3D modeling of deep borehole electromagnetic measurements with energized casing source for fracture mapping at the Utah Frontier Observatory for Research in Geothermal Energy</title><title>Geophysical Prospecting</title><description>We present a 3D numerical modelling analysis evaluating the deployment of a borehole electromagnetic measurement tool to detect and image a stimulated zone at the Utah Frontier Observatory for Research in Geothermal Energy geothermal site. As the depth to the geothermal reservoir is several kilometres and the size of the stimulated zone is limited to several 100 m, surface‐based controlled‐source electromagnetic measurements lack the sensitivity for detecting changes in electrical resistivity caused by the stimulation. To overcome the limitation, the study evaluates the feasibility of using a three‐component borehole magnetic receiver system at the Frontier Observatory for Research in Geothermal Energy site. To provide sufficient currents inside and around the enhanced geothermal reservoir, we use an injection well as an energized casing source. To efficiently simulate energizing the injection well in a realistic 3D resistivity model, we introduce a novel modelling workflow that leverages the strengths of both 3D cylindrical‐mesh‐based electromagnetic modelling code and 3D tetrahedral‐mesh‐based electromagnetic modelling code. The former is particularly well‐suited for modelling hollow cylindrical objects like casings, whereas the latter excels at representing more complex 3D geological structures. In this workflow, our initial step involves computing current densities along a vertical steel‐cased well using a 3D cylindrical electromagnetic modelling code. Subsequently, we distribute a series of equivalent current sources along the well's trajectory within a complex 3D resistivity model. We then discretize this model using a tetrahedral mesh and simulate the borehole electromagnetic responses excited by the casing source using a 3D finite‐element electromagnetic code. This multi‐step approach enables us to simulate 3D casing source electromagnetic responses within a complex 3D resistivity model, without the need for explicit discretization of the well using an excessive number of fine cells. We discuss the applicability and limitations of this proposed workflow within an electromagnetic modelling scenario where an energized well is deviated, such as at the Frontier Observatory for Research in Geothermal Energy site. Using the workflow, we demonstrate that the combined use of the energized casing source and the borehole electromagnetic receiver system offer measurable magnetic field amplitudes and sensitivity to the deep localized stimulated zone. The measurements can also distinguish between parallel‐fracture anisotropic reservoirs and isotropic cases, providing valuable insights into the fracture system of the stimulated zone. Besides the magnetic field measurements, vertical electric field measurements in the open well sections are also highly sensitive to the stimulated zone and can be used as additional data for detecting and imaging the target. We can also acquire additional multiple‐source data by grounding the surface electrode at various locations and repeating borehole electromagnetic measurements. This approach can increase the number of monitoring data by several factors, providing a more comprehensive dataset for analysing the deep‐localized stimulated zone. The numerical analysis indicates that it is feasible to use the combination of the energized casing and downhole electromagnetic measurements in monitoring localized stimulated zone at large depths.</description><subject>borehole geophysics</subject><subject>Boreholes</subject><subject>Casing</subject><subject>Casings</subject><subject>Current sources</subject><subject>Data analysis</subject><subject>Electric fields</subject><subject>Electrical resistivity</subject><subject>Electromagnetic measurement</subject><subject>electromagnetics</subject><subject>Feasibility studies</subject><subject>Geological structures</subject><subject>GEOSCIENCES</subject><subject>Geothermal energy</subject><subject>Geothermal power</subject><subject>Image enhancement</subject><subject>Injection</subject><subject>Injection wells</subject><subject>Magnetic field</subject><subject>Magnetic fields</subject><subject>Modelling</subject><subject>Monitoring</subject><subject>Numerical analysis</subject><subject>Numerical models</subject><subject>Observatories</subject><subject>Reservoirs</subject><subject>Sensitivity analysis</subject><subject>Target detection</subject><subject>Workflow</subject><issn>0016-8025</issn><issn>1365-2478</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><recordid>eNqFkc1u1DAURiMEEkNhzfYK1mn9EyfxEpV2qFSpqCpry3FuJq4SO9gequGheEacpmKLN7bsc-61_RXFR0rOaR4XlNeiZFXTnlMuGvmq2P3beV3sCKF12RIm3hbvYnwkhBMhql3xh3-F2fc4WXcAP0CPuEDnA45-QsAJTQp-1geHyRqYUcdjwBldivBk0wjoMBzsb-zB6LjWiP4YDMLgAwxBm5RxmPWyrGc6QRoRfiQ9wnXwLlkMcNdFDL908uH0bN1jRB3MCNbBHn0WwqwnuFobnd4XbwY9RfzwMp8VD9dXD5ffytu7_c3ll9vSMFbLUgy9ZjUhQydRk5YISTrDeKMNaUhriJSaDaYSTd1VTSNp32Jemp5T3vRC8rPi01bWx2RVNDahGY13Ln-HYlVF6nqFPm_QEvzPI8akHvPbXb6W4pRJSTlr60xdbJQJPsaAg1qCnXU4KUrUGpxaY1JrTOo5uGyIzXiyE57-h6v99_vN-wsIDJ0x</recordid><startdate>202410</startdate><enddate>202410</enddate><creator>Um, Evan Schankee</creator><creator>Alumbaugh, David</creator><creator>Capriotti, Joseph</creator><creator>Wilt, Michael</creator><creator>Nichols, Edward</creator><creator>Li, Yaoguo</creator><creator>Kang, Seogi</creator><creator>Osato, Kazumi</creator><general>Wiley Subscription Services, Inc</general><general>Wiley</general><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>F1W</scope><scope>FR3</scope><scope>H96</scope><scope>KR7</scope><scope>L.G</scope><scope>OTOTI</scope></search><sort><creationdate>202410</creationdate><title>3D modeling of deep borehole electromagnetic measurements with energized casing source for fracture mapping at the Utah Frontier Observatory for Research in Geothermal Energy</title><author>Um, Evan Schankee ; 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Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>OSTI.GOV</collection><jtitle>Geophysical Prospecting</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Um, Evan Schankee</au><au>Alumbaugh, David</au><au>Capriotti, Joseph</au><au>Wilt, Michael</au><au>Nichols, Edward</au><au>Li, Yaoguo</au><au>Kang, Seogi</au><au>Osato, Kazumi</au><aucorp>Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)</aucorp><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>3D modeling of deep borehole electromagnetic measurements with energized casing source for fracture mapping at the Utah Frontier Observatory for Research in Geothermal Energy</atitle><jtitle>Geophysical Prospecting</jtitle><date>2024-10</date><risdate>2024</risdate><volume>72</volume><issue>8</issue><spage>3104</spage><epage>3128</epage><pages>3104-3128</pages><issn>0016-8025</issn><eissn>1365-2478</eissn><abstract>We present a 3D numerical modelling analysis evaluating the deployment of a borehole electromagnetic measurement tool to detect and image a stimulated zone at the Utah Frontier Observatory for Research in Geothermal Energy geothermal site. As the depth to the geothermal reservoir is several kilometres and the size of the stimulated zone is limited to several 100 m, surface‐based controlled‐source electromagnetic measurements lack the sensitivity for detecting changes in electrical resistivity caused by the stimulation. To overcome the limitation, the study evaluates the feasibility of using a three‐component borehole magnetic receiver system at the Frontier Observatory for Research in Geothermal Energy site. To provide sufficient currents inside and around the enhanced geothermal reservoir, we use an injection well as an energized casing source. To efficiently simulate energizing the injection well in a realistic 3D resistivity model, we introduce a novel modelling workflow that leverages the strengths of both 3D cylindrical‐mesh‐based electromagnetic modelling code and 3D tetrahedral‐mesh‐based electromagnetic modelling code. The former is particularly well‐suited for modelling hollow cylindrical objects like casings, whereas the latter excels at representing more complex 3D geological structures. In this workflow, our initial step involves computing current densities along a vertical steel‐cased well using a 3D cylindrical electromagnetic modelling code. Subsequently, we distribute a series of equivalent current sources along the well's trajectory within a complex 3D resistivity model. We then discretize this model using a tetrahedral mesh and simulate the borehole electromagnetic responses excited by the casing source using a 3D finite‐element electromagnetic code. This multi‐step approach enables us to simulate 3D casing source electromagnetic responses within a complex 3D resistivity model, without the need for explicit discretization of the well using an excessive number of fine cells. We discuss the applicability and limitations of this proposed workflow within an electromagnetic modelling scenario where an energized well is deviated, such as at the Frontier Observatory for Research in Geothermal Energy site. Using the workflow, we demonstrate that the combined use of the energized casing source and the borehole electromagnetic receiver system offer measurable magnetic field amplitudes and sensitivity to the deep localized stimulated zone. The measurements can also distinguish between parallel‐fracture anisotropic reservoirs and isotropic cases, providing valuable insights into the fracture system of the stimulated zone. Besides the magnetic field measurements, vertical electric field measurements in the open well sections are also highly sensitive to the stimulated zone and can be used as additional data for detecting and imaging the target. We can also acquire additional multiple‐source data by grounding the surface electrode at various locations and repeating borehole electromagnetic measurements. This approach can increase the number of monitoring data by several factors, providing a more comprehensive dataset for analysing the deep‐localized stimulated zone. The numerical analysis indicates that it is feasible to use the combination of the energized casing and downhole electromagnetic measurements in monitoring localized stimulated zone at large depths.</abstract><cop>Houten</cop><pub>Wiley Subscription Services, Inc</pub><doi>10.1111/1365-2478.13579</doi><tpages>25</tpages></addata></record>
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source Wiley Online Library Journals Frontfile Complete
subjects borehole geophysics
Boreholes
Casing
Casings
Current sources
Data analysis
Electric fields
Electrical resistivity
Electromagnetic measurement
electromagnetics
Feasibility studies
Geological structures
GEOSCIENCES
Geothermal energy
Geothermal power
Image enhancement
Injection
Injection wells
Magnetic field
Magnetic fields
Modelling
Monitoring
Numerical analysis
Numerical models
Observatories
Reservoirs
Sensitivity analysis
Target detection
Workflow
title 3D modeling of deep borehole electromagnetic measurements with energized casing source for fracture mapping at the Utah Frontier Observatory for Research in Geothermal Energy
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