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Deep Stimulation at Newberry Volcano EGS Demonstration Kyla Grasso, Trenton Cladouhos, Susan Petty, Geoffrey Garrison, Matt Uddenberg, Michael Swyer, Yini Nordin AltaRock Energy, Inc., Seattle, WA. Contact: [email protected] Paper H43A-0940 Abstract: The Newberry Volcano EGS Demonstration is a 5 year field project designed to demonstrate recent technological advances for engineered geothermal systems (EGS) development. Advances in reservoir stimulation, diverter, and monitoring are being tested in a hot (>300 C), dry well (NWG 55-29) drilled in 2008. These technologies could reduce the cost of electrical power generation. The project began in 2010 with two years of permitting, technical planning, and development of a project-specific Induced Seismicity Mitigation Plan (ISMP), and is funded in part by the Department of Energy. Well stimulation carried out in 2012 indicated wellbore casing repairs were needed, and further wellbore analysis in 2013 confirmed 2012 results. Repairs were completed and the well was re-stimulated in 2014. Injectivity changes, thermal profiles and seismicity indicate that fracture permeability in well NWG 55-29 was enhanced by hydraulic stimulation at water pressures below the principle stress resulting in hydroshearing. Maximum wellhead pressure reached 200 bar (2850 psi) and 15,000 m3 of groundwater was injected at depth. The fifteen-station microseismic array (MSA) detected and located 392 events during 2014 stimulation, ranging in magnitude up to M 2.2. Injection of thermally- degradable zonal isolation material (TZIM) successfully shifted the stimulation target at depth, resulting in multiple zone reservoir development. This work successfully demonstrates the viability of large-volume low-pressure stimulation coupled with non-mechanical diverter technology and microseismic monitoring for reservoir mapping. Location: Western flank of Newberry Volcano in central Oregon, ~35 km south of Bend Deschutes National Forest, managed by US Forest Service and Bureau of Land Management Outside of Newberry National Volcanic Monument Geothermal injection well NWG 55- 29, drilled in 2008 High desert area with little rainfall and significant snow accumulation Engineered Geothermal Systems Multi-zone stimulation utilizing hydroshearing technology Pump at moderate pressure over long time period to open fractures, increase permeability Thermally-degradable zonal isolation material (TZIM) for multi-zone system Low-risk, low-cost alternative to hydraulic fracturing for improving both injection and production wells This material is based upon work supported by the Department of Energy under Award Number DE-EE0002777. Disclaimer: This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. TZIM Diverter Injection and Temperature Logging Granular TZIM injected on 11/18 and fibrous TZIM on 11/19. Temperature logs run after TZIM injection (figure at right) indicate that second TZIM treatment o blocked primary zone at 9550ft, o enhanced a new zone at 9700ft, and o completely blocked flow below 9750ft, o allowing rapid heat-up of the bottom of the hole. Initial DTS cable did not reach bottom hole. Therefore, the DTS was not used to track TZIM treatment. The DTS did provide a valuable tool for tracking the relationship between injection flow rate and cooling and reheating of the wellbore, which will provide input to thermal models. Further, the DTS confirmed that no fluid was lost from the cased portion of the well. Pressure and Flow Maximum sustained WHP 200 bar (2850 psi) Maximum sustained flow of 10.5 L/s (165 gal/min) Two rounds of stimulation Injected Volume and Seismicity Risk Cumulative injected volume versus seismic moment to track induced seismicity risk. B-value tracking Increase in B-value over time indicates increased activity on smaller faults, an advantage for both greater heat exchange and lower seismic risk. Project Goals Demonstrate current technology and advances in EGS technology Stimulate 3 zones in existing hot, dry well Drill production well, test wells, and produce economic quantities of fluid Phase I (2010-2012) Data review, characterize baseline seismicity and hydrological Stimulation and data analysis Technical review Permitting and public outreach Phase II (2012-2014) Microseismic monitoring array installation Stimulate NWG 55-29 and flow test Seismic and hydrologic monitoring Ongoing public outreach Technical review Phase III (2015) Plan and drill production well Circulation test injection and production well pair Continue environmental monitoring Technical review 2014 Field Campaign Run tie-back and repair well casing Background groundwater sampling Install stimulation pumps and piping Initial stimulation and flow test 9/23-10/15 Initial flow-back test 10/23-24 Perforation shots through casing 11/12 Second stimulation 11/11-11/20 Final flow-back test 11/24-26 Distributed Temperature Sensing (DTS) Microseismic Monitoring Results The fifteen station seismic array located 397 microseismic events during stimulation. The largest event detected was M 2.2. Data analysis is ongoing. Next Steps Finish 2014 data analysis Determine production well target — into seismic cloud ~400 m from injector Permit and drill production well Stimulate production well 30 day circulation test Technical review 1828 m 3048 m 2438 m 37 C 204 C looking north looking west map view color scale shows timing of events (see legend on map view) Round 1 Round 2 200 bar 100 bar 0 bar 15 L/s 5 L/s 0 L/s

Deep Stimulation at Newberry Volcano EGS Demonstration · •Geothermal injection well NWG 55-29, drilled in 2008 •High desert area with little rainfall and significant snow accumulation

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Page 1: Deep Stimulation at Newberry Volcano EGS Demonstration · •Geothermal injection well NWG 55-29, drilled in 2008 •High desert area with little rainfall and significant snow accumulation

Deep Stimulation at Newberry Volcano EGS DemonstrationKyla Grasso, Trenton Cladouhos, Susan Petty, Geoffrey Garrison, Matt Uddenberg, Michael Swyer, Yini Nordin

AltaRock Energy, Inc., Seattle, WA. Contact: [email protected] H43A-0940

Abstract:The Newberry Volcano EGS Demonstration is a 5 year field project designed to demonstraterecent technological advances for engineered geothermal systems (EGS) development.Advances in reservoir stimulation, diverter, and monitoring are being tested in a hot (>300 C),dry well (NWG 55-29) drilled in 2008. These technologies could reduce the cost of electricalpower generation. The project began in 2010 with two years of permitting, technical planning,and development of a project-specific Induced Seismicity Mitigation Plan (ISMP), and is fundedin part by the Department of Energy. Well stimulation carried out in 2012 indicated wellborecasing repairs were needed, and further wellbore analysis in 2013 confirmed 2012 results.Repairs were completed and the well was re-stimulated in 2014. Injectivity changes, thermalprofiles and seismicity indicate that fracture permeability in well NWG 55-29 was enhanced byhydraulic stimulation at water pressures below the principle stress resulting in hydroshearing.Maximum wellhead pressure reached 200 bar (2850 psi) and 15,000 m3 of groundwater wasinjected at depth. The fifteen-station microseismic array (MSA) detected and located 392events during 2014 stimulation, ranging in magnitude up to M 2.2. Injection of thermally-degradable zonal isolation material (TZIM) successfully shifted the stimulation target at depth,resulting in multiple zone reservoir development. This work successfully demonstrates theviability of large-volume low-pressure stimulation coupled with non-mechanical divertertechnology and microseismic monitoring for reservoir mapping.

Location:

• Western flank of Newberry Volcano in central Oregon, ~35 km south of Bend

• Deschutes National Forest, managed by US Forest Service and Bureau of Land Management

• Outside of Newberry National Volcanic Monument

• Geothermal injection well NWG 55-29, drilled in 2008

• High desert area with little rainfall and significant snow accumulation

Engineered Geothermal Systems

• Multi-zone stimulation utilizing hydroshearing technology

• Pump at moderate pressure over long time period to open fractures, increase permeability

• Thermally-degradable zonal isolation material (TZIM) for multi-zone system

• Low-risk, low-cost alternative to hydraulic fracturing for improving both injection and production wells

This material is based upon work supported by the Department of Energy under Award Number DE-EE0002777. Disclaimer: This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof.

TZIM Diverter Injection and Temperature Logging• Granular TZIM injected on 11/18 and fibrous TZIM on 11/19.• Temperature logs run after TZIM injection (figure at right)

indicate that second TZIM treatmento blocked primary zone at 9550ft, o enhanced a new zone at 9700ft, ando completely blocked flow below 9750ft, o allowing rapid heat-up of the bottom of the hole.

Initial DTS cable did not reach bottomhole. Therefore, the DTS was notused to track TZIM treatment. TheDTS did provide a valuable tool fortracking the relationship betweeninjection flow rate and cooling andreheating of the wellbore, which willprovide input to thermal models.Further, the DTS confirmed that nofluid was lost from the cased portionof the well.

Pressure and Flow• Maximum sustained WHP 200 bar (2850 psi)• Maximum sustained flow of 10.5 L/s (165 gal/min)• Two rounds of stimulation

Injected Volume and Seismicity RiskCumulative injected volume versus seismicmoment to track induced seismicity risk.

B-value trackingIncrease in B-value over time indicates increasedactivity on smaller faults, an advantage for bothgreater heat exchange and lower seismic risk.

Project Goals• Demonstrate current technology and advances in EGS

technology• Stimulate 3 zones in existing hot, dry well• Drill production well, test wells, and produce economic

quantities of fluidPhase I (2010-2012)• Data review, characterize baseline seismicity and

hydrological Stimulation and data analysis• Technical review • Permitting and public outreachPhase II (2012-2014)• Microseismic monitoring array installation• Stimulate NWG 55-29 and flow test• Seismic and hydrologic monitoring• Ongoing public outreach• Technical review

Phase III (2015)• Plan and drill production well• Circulation test injection and production well pair• Continue environmental monitoring • Technical review

2014 Field Campaign• Run tie-back and repair well casing• Background groundwater sampling• Install stimulation pumps and piping• Initial stimulation and flow test 9/23-10/15• Initial flow-back test 10/23-24• Perforation shots through casing 11/12• Second stimulation 11/11-11/20• Final flow-back test 11/24-26

Distributed Temperature Sensing (DTS)

Microseismic Monitoring ResultsThe fifteen station seismic array located 397 microseismicevents during stimulation. The largest event detected wasM 2.2. Data analysis is ongoing.

Next Steps• Finish 2014 data analysis• Determine production well

target — into seismic cloud ~400 m from injector

• Permit and drill production well

• Stimulate production well• 30 day circulation test• Technical review

1828 m

3048 m

2438 m

37 C 204 C

looking northlooking west

map view

color scale shows timing of events (see legend on map view)

Round 1

Round 2

200 bar

100 bar

0 bar

15 L/s5 L/s0 L/s